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Sample records for calderas utilizando intercambio

  1. Desarrollo de un nuevo tratamiento para la conservación de piedras con alto contenido en carbonatos utilizando la Tecnología de Resinas de Intercambio Iónico

    Directory of Open Access Journals (Sweden)

    Pérez-Alonso, M.

    2003-12-01

    de forma artificial del carbonato de calcio presente en piedras calcáreas en oxalato cálcico utilizando para ello la tecnología de intercambio iónico. La resina puesta en su forma oxalato debe ser puesta en contacto con la piedra mediante una solución conductora de iones, produciendo la formación de una microcapa cristalina de oxalato cálcico sobre la superficie de la piedra. Los resultados se han evaluado mediante espectroscopia FT-Raman. Los cristales formados inicialmente son CaC2O4 · 2H2O (weddellita que evoluciona parcialmente hacia la especie CaC2O4 · H2O (whewellita en función de las condiciones atmosféricas (humedad y temperatura.

  2. Reacciones de intercambio de carga

    Science.gov (United States)

    Errea, L. F.

    Se discute la validez de diversas metodologías y su aplicación al estudio de procesos de intercambio de carga electrónico entre iones y blancos atómicos y moleculares. Para energías de impacto entre 0.05 y 5 eV / amu se emplea el método cuántico de la Coordenada de Reacción Común (CRC). A mayores energías, se utiliza el método semiclásico iconal con un desarrollo de la función de onda dinámica en estados moleculares adiabáticos, modificados con un factor de traslación común (FTC). Estos estados pueden obtenerse con cálculos ab initio o empleando potenciales modelo. Cuando la ionización compite con la transferencia de carga, la inclusión de pseudoestados en estos desarrollos permite calcular simultáneamente las secciones eficaces de ambos procesos. Otra técnica utilizada es el método estadístico CTMC. En el tratamiento de colisiones ión-molécula (diatómica) contrastamos la aplicabilidad de distintos métodos, desde la llamada aproximación Franck-Condon hasta un desarrollo en estados vibrónicos, pasando por la aproximación súbita vibro-rotacional, obteniéndose secciones eficaces de captura electrónica total y a estados individuales, así como secciones de excitación vibracional a estados ligados y del continuo (disociación). En todos los casos es necesario calcular superficies de energía y los correspondientes acoplamientos dinámicos entre los estados. La aplicación de estos métodos permite determinar el grado de contaminación de los haces por estados metaestables en un experimento dado, el cambio en los resultados con diferentes isótopos, la importancia de procesos de doble captura, seguida de explosión culombiana, todo ello con precisión comparable a la de medidas experimentales, para sistemas de interés en distintos tipos de plasmas.

  3. PREFACE: Collapse Calderas Workshop

    Science.gov (United States)

    Gottsmann, Jo; Aguirre-Diaz, Gerardo

    2008-10-01

    Caldera-formation is one of the most awe-inspiring and powerful displays of nature's force. Resultant deposits may cover vast areas and significantly alter the immediate topography. Post-collapse activity may include resurgence, unrest, intra-caldera volcanism and potentially the start of a new magmatic cycle, perhaps eventually leading to renewed collapse. Since volcanoes and their eruptions are the surface manifestation of magmatic processes, calderas provide key insights into the generation and evolution of large-volume silicic magma bodies in the Earth's crust. Despite their potentially ferocious nature, calderas play a crucial role in modern society's life. Collapse calderas host essential economic deposits and supply power for many via the exploitation of geothermal reservoirs, and thus receive considerable scientific, economic and industrial attention. Calderas also attract millions of visitors world-wide with their spectacular scenic displays. To build on the outcomes of the 2005 calderas workshop in Tenerife (Spain) and to assess the most recent advances on caldera research, a follow-up meeting was proposed to be held in Mexico in 2008. This abstract volume presents contributions to the 2nd Calderas Workshop held at Hotel Misión La Muralla, Querétaro, Mexico, 19-25 October 2008. The title of the workshop `Reconstructing the evolution of collapse calderas: Magma storage, mobilisation and eruption' set the theme for five days of presentations and discussions, both at the venue as well as during visits to the surrounding calderas of Amealco, Amazcala and Huichapan. The multi-disciplinary workshop was attended by more than 40 scientist from North, Central and South America, Europe, Australia and Asia. Contributions covered five thematic topics: geology, geochemistry/petrology, structural analysis/modelling, geophysics, and hazards. The workshop was generously supported by the International Association of Volcanology and the Chemistry of The Earth's Interior

  4. Intercambio direccional en roseta – Suiza

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    Guisan, François

    1964-11-01

    Full Text Available This crossing, at Ecublens, Switzerland, involves five viaducts. The number of roads that the Lausanne-Berne motorway had to cross presented a difficult problem, since technical, aesthetic and economic questions had to be considered, all on a complex scale. As the soil was not suitable to support heavy structures, it was decided to build five viaducts, each providing a traffic route. Some of these viaducts cross each other at three levels. The viaducts consist of box girder sections, joined together to form continuous beams. The two central piles of each section are rigid, to withstand wind forces, and the others are hinged at the top and bottom. The sections are separated by dilatation joints, fitted with a metal attachment, which provides continuity for the pavement, and allows for a relative displacement of 16 cm. Some of the supports were placed on pile foundations, to overcome the weak bearing strength of the subsoil. One of the road sections did not have any rigid central supports, and this arrangement was chosen for aesthetic reasons.El intercambio direccional en roseta, de Ecublens (Suiza, está constituido por un conjunto de cinco viaductos. La multiplicidad de vías que debía salvar la autopista Lausana-Berna planteó un problema importante, ya que era preciso tener en cuenta factores de tipo técnico, en lo que respecta a las obras de fábrica; estéticos, en cuanto a armonía con el paisaje local, y económicos. Técnicamente, y teniendo en cuenta que las condiciones del terreno eran poco apropiadas para levantar obras pesadas, la solución adoptada consiste, en esencia, en cinco viaductos que constituyen otros tantos pasos, algunos de ellos intermedios, es decir, situados entre dos vías: una superior y otra inferior. Cada uno de los pasos se ha subdividido en varios tramos de viga cajón continua. Las dos pilas centrales de cada tramo son rígidas, para poder absorber los efectos del viento; las demás están articuladas en la

  5. Calderas and magma reservoirs

    Science.gov (United States)

    Cashman, Katharine; Giordano, Guido

    2015-04-01

    Large caldera-forming eruptions have long been a focus of both petrological and volcanological studies; traditionally, both have assumed that eruptible magma is stored within a single long-lived melt body. Over the past decade, however, advances in analytical techniques have provided new views of magma storage regions, many of which provide evidence of multiple melt lenses feeding a single eruption, and/or rapid pre-eruptive assembly of large volumes of melt. These new petrological views of magmatic systems have not yet been fully integrated into volcanological perspectives of caldera-forming eruptions. We discuss the implications of syn-eruptive melt extraction from complex, rather than simple, reservoirs and its potential control over eruption size and style, and caldera collapse timing and style. Implications extend to monitoring of volcanic unrest and eruption progress under conditions where successive melt lenses may be tapped. We conclude that emerging views of complex magma reservoir configurations provide exciting opportunities for re-examining volcanological concepts of caldera-forming systems

  6. Burnout en profesores: Una perspectiva social del intercambio

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    WILMAR B. SCHAUFELI

    2005-01-01

    Full Text Available Se propone una perspectiva teórica sobre burnout en profesores, basada en principios de intercambio social. Se argumenta que el burnout se produce por una falta de reciprocidad; por un desajuste entre inversiones y resultados. Los profesores quemados se caracterizan por haber dado demasiado durante demasiado tiempo y por recibir demasiado poco a cambio. Según la teoría del intercambio social, la falta de reciprocidad podría desarrollarse a tres niveles: interpersonal (relación con estudiantes, a nivel de equipo (relaciones con compañeros, y a nivel organizacional (relación con la escuela. Estudios empíricos en profesores mostraron que el ajuste entre 'dar y recibir' se rompe, sobretodo en los niveles interpersonal y organizacional. Además, la falta de reciprocidad se asocia con distrés y conductas de abandono. Se observa un efecto genérico: cuando el equilibrio 'dar y recibir' se rompe se produce agotamiento emocional (síntoma corazón del burnout. Además, se observan efectos de las conductas de abandono específico para cada nivel de intercambio social: la falta de reciprocidad con los estudiantes provoca despersonalización (segunda dimensión del burnout; la falta de reciprocidad con los colegas acaba en conductas de abandono de los colegas; y la falta de reciprocidad con la escuela en abandono psicológico (reducido compromiso organizacional y conductual (absentismo por enfermedad de la escuela.

  7. Cuba. Intercambios socioculturales en el periodo aborigen con el Caribe

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    Alfredo Pérez Carratalá

    2010-07-01

    Full Text Available Se expresa la importancia que ha tenido el Caribe, no solo como componente físico-geográfico, sino también como área de intercambio de la biota, incluyendo los seres humanos. La ubicación geográfica del archipiélago cubano propició que fuera lugar de obligado paso o estancia de las comunidades aborígenes que habitaron el circumcaribe, en todos los períodos de desarrollo de los procesos migratorios en el área. En cuanto al intercambio sociocultural se entiende en sentido amplio del tema, es decir, lo tradicionalmente cultural, incluyendo las formas vivenciales de la cultura de los pueblos, donde lo cultural se convierte en vía y clave de realización de la intervención, donde los aspectos socioeconómicos en última instancia tienen un papel preponderante, por lo que comporta mucho más que la simple transferencia de materia prima y objetos.

  8. Viajes comerciales de intercambio en el departamento de Antofagasta de la Sierra, Puna meridional argentina: pasado y presente.

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    García, Silvia P.

    2002-05-01

    Full Text Available Los viajes hacia valles interserranos a lomo de mula fueron una experiencia compartida por todos en esta región de la puna argentina, hasta hace veinte años. En este trabajo se relacionan los datos obtenidos a través de entrevistas a informantes en el departamento de Antofagasta de la Sierra, con los surgidos tras la consulta de las Actas del Registro Civil y se arriba a conclusiones respecto de los vínculos de parentesco que unieron a quienes comerciaban e intercambiaban mercaderías producidas en alturas diferentes. También se compara la situación de entonces con la actualidad. En la capital del departamento los viajes de intercambio han desaparecido casi en su totalidad, en cambio en otras poblaciones del mismo departamento se han modificado incluyendo en ellos a las mercaderías obtenidas por compra y utilizando la sal como principal elemento de canje.

  9. Content Analysis Schedule for Bilingual Education Programs: BICEP Intercambio de la Cultura.

    Science.gov (United States)

    Shore, Marietta Saravia; Nafus, Charles

    This content analysis schedule for BICEP Intercambio de la Cultura (San Bernardino, California), presents information on the history, funding, and scope of the project. Included are sociolinguistic process variables such as the native and dominant languages of students and their interaction. Information is provided on staff selection and the…

  10. Experiencia de intercambio docente en dos asignaturas de Inteligencia Artificial en universidades argentinas

    OpenAIRE

    Mariño, Sonia Itatí; Rambo, Alice

    2014-01-01

    En ámbitos de Educación Superior se propicia la generación de redes de intercambio y difusión de conocimientos y experiencias. Se describe una iniciativa docente desarrollada en dos asignaturas que abordan temas de Inteligencia Artificial.

  11. Calderas and mineralization: volcanic geology and mineralization in the Chianti caldera complex, Trans-Pecos Texas

    Energy Technology Data Exchange (ETDEWEB)

    Duex, T.W.; Henry, C.D.

    1981-01-01

    This report describes preliminary results of an ongoing study of the volcanic stratigraphy, caldera activity, and known and potential mineralization of the Chinati Mountains area of Trans-Pecos Texas. Many ore deposits are spatially associated with calderas and other volcanic centers. A genetic relationship between calderas and base and precious metal mineralization has been proposed by some and denied by others. Steven and others have demonstrated that calderas provide an important setting for mineralization in the San Juan volcanic field of Colorado. Mineralization is not found in all calderas but is apparently restricted to calderas that had complex, postsubsidence igneous activity. A comparison of volcanic setting, volcanic history, caldera evolution, and evidence of mineralization in Trans-Pecos to those of the San Juan volcanic field, a major mineral producer, indicates that Trans-Pecos Texas also could be an important mineralized region. The Chianti caldera complex in Trans-Pecos Texas contains at least two calderas that have had considerable postsubsidence activity and that display large areas of hydrothermal alteration and mineralization. Abundant prospects in Trans-Pecos and numerous producing mines immediately south of the Trans-Pecos volcanic field in Mexico are additional evidence that ore-grade deposits could occur in Texas.

  12. Caldera Formation on the Vance Seamounts

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    Clague, D.; Paduan, J.; Cousens, B.; Cornejo, L.; Perfit, M.; Wendt, R.; Stix, J.; Helo, C.

    2006-12-01

    The Vance Seamounts are a chain of near-ridge volcanoes located just west of the southern Juan de Fuca Ridge. The six volcanoes are built on ocean crust ranging from 0.78 Ma at the southeastern end to 2.55 Ma in the northwest. Morphologic analysis indicates that the volcanoes were constructed sequentially and get younger to the southeast towards the ridge axis. Like many near-ridge volcanoes, some of the Vance Seamounts have large offset calderas that presumably formed above evacuated shallow magma chambers within the upper ocean crust. In summer 2006, we completed 6 dives using MBARI's ROV Tiburon to study the formation of these calderas. The floor of each caldera consists of flat-lying volcaniclastite, under about 25 cm of pelagic sediment. Some caldera floors have mounds of post-caldera pillow flows. The caldera walls have a lower section covered by talus and an upper section of interbedded massive flows with columnar joints (to 11 m thick) and pillow basalts. The top of each caldera wall has a unit of volcanic mudstone to sandstone ranging from 20 cm to 2 m thick. The fine matrix of many of these samples is green hydrothermal clay. The finest siltstone to mudstone samples appear to be layers of massive tan hydrothermal clays. Talus fragments, lava and volcaniclastite outcrops are universally coated and cemented by 1 to 4 cm-thick deposits of hydrothermal Mn-oxide crusts, even on the youngest of the volcanoes. Volcanic particles in the sandstones are mostly dense angular glass, but bubble-wall fragments (limu o Pele) are present and indicate formation during low-energy pyroclastic eruptions. Without the few percent limu o Pele fragments, the glass fragments would resemble those inferred to form by quench granulation. We suggest that quench granulation is actually pyroclastic fragmentation that occurs as coalesced magmatic gas bubbles disrupt the molten lava surface at the vents. Our observations confirm that the more southeasterly offset calderas truncated thick

  13. Krakatau caldera deposits: revisited and verification by geophysical means

    OpenAIRE

    Izumi Yokoyama

    2014-01-01

     One of the differences between volcanic craters and calderas is that the latter bottoms are flatways filled with caldera deposit with lower density in comparison to country rocks. The 1883 Krakatau eruption affords us important knowledge on caldera formation even if it was not observed with modern sophisticated instruments. First, volcanic activities of the Krakatau Islands before and after the 1883 eruption are reexamined: previous suppositions involving a caldera-forming eruption of the pr...

  14. Automatización de una columna de intercambio iónico

    OpenAIRE

    Martínez González, Ismael

    2012-01-01

    El trabajo ha sido realizado en el Departamento de Ingeniería de Sistemas y Automática de la Universidad Politécnica de Cartagena, y el objetivo principal es el estudio e implementación del sistema de control necesario para hacer funcionar correctamente una columna de intercambio iónico. El sistema de control que se va a utilizar se compone de un controlador lógico programable (PLC) que contendrá el programa principal, y un Scada que será el interface entre l hombre y la máquina. ...

  15. Desarrollo de un prototipo de biorreactor con sistema de intercambio de medios de cultivo

    OpenAIRE

    LEÓN ORTUÑO, ANA LEONOR

    2016-01-01

    [ES] En el presente Trabajo Final de Grado se ha desarrollado un prototipo de biorreactor basado en un sistema automático de intercambio del medio de cultivo presente en una siembra de células, que permite mantener unas condiciones de cultivo óptimas, y por consiguiente, garantizar la supervivencia celular. Éste está integrado por dos bombas que trabajan de forma coordinada para retirar y suministrar el medio y un sensor óptico que se encarga de medir el pH, medida que se toma ...

  16. Electrocatalizadores para pilas de combustible de membrana de intercambio protónico

    OpenAIRE

    Lázaro Elorri, María Jesús; Moliner Álvarez, Rafael; Calvillo Lamana, Laura; Pastor Ferrer, Elsa

    2008-01-01

    Electrocatalizadores para pilas de combustible de membrana de intercambio protónico. Procedimiento de obtención de un material de carbono mesoporoso (SMC) que comprende: la adición de sílice coloidal a un precursor polimérico de carbono; el curado térmico; el carbonizado del compuesto obtenido; lavado del compuesto carbonizado con ácido fluorhídrico (HF) o NaOH; y la oxidación del material lavado. Además la invención se refiere a un catalizador para pilas de combustibl...

  17. Taller de capacitación e intercambio en procesos de innovación rural

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    Veterinaria.org

    2008-01-01

    Full Text Available ResumenCon un rotundo éxito se celebró en Bayamo, el Taller de capacitación e intercambio en procesos de innovación rural, el día 7 de diciembre del 2007, organizado por el Órgano de Base “Jorge Dimitrov” de Bayamo, auspiciado por la Filial Granma del Consejo Científico de Veterinaria de Cuba. Se impartieron cuatro conferencias desarrolladas por prestigiosos investigadores que abordaron diversos temas de gran impacto e importancia en la ganadería de la provincia y el país.

  18. El Estado Moderno y la sociedad de intercambio en la obra de Thomas Hobbes

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    Fernando Salazar Silva

    2007-01-01

    Full Text Available El soberano, como manifestación de la organización social, mas allá de expresar de un modo inevitable la seguridad de los hombres ante el desorden del "Estado natural", establece el origen de la sociedad de intercambio y la propiedad. El desarrollo de este proceso histórico, lejos de ser un acto espontáneo de los hombres como efecto de su propensión natural al cambio, es posible a partir de las condiciones generadas por el Leviatán.

  19. Microearthquakes at Valles Caldera, New Mexico: Improved Detection and Location with Two Additional Caldera Stations

    Science.gov (United States)

    Roberts, P. M.; House, L. S.; Ten Cate, J. A.

    2015-12-01

    The Los Alamos Seismic Network (LASN) has operated for 43 years, providing data to locate more than 2,500 earthquakes in north-central New Mexico. Roughly 1-2 earthquakes are detected and located per month within about 150 km of Los Alamos, a total of over 900 from 1973 to present. LASN's primary purpose is to monitor seismicity close to the Los Alamos National Laboratory (LANL) for seismic hazards; monitoring seismicity associated with the nearby Valles Caldera is secondary. Until 2010 the network was focused on monitoring seismic hazards and comprised only 7 stations, all near LANL or in the nearby Jemez Mountains. Just one station—PER, installed in 1998—was close enough to Valles Caldera to be able to detect microearthquakes located in or near the caldera. An initial study of the data from station PER between 1998 and 2002 identified and located 13 events with magnitudes less than 0.5 using the single-station hodogram technique. Those events were all located south of the caldera within a few kilometers of PER. Recently, two new digital broadband stations were installed inside the caldera, one on a northeastern ring-fracture dome, station CDAB, and the other on a northwestern dome, station SAMT. Also, station PER was upgraded with digital broadband instrumentation. Thus, LASN now can detect and record microearthquakes as small as magnitude -1.5 near the caldera, and they can be located using multiple arrival times. Several recent events located near station SAMT on the caldera's ring fracture are the first that have been seen in that area. Additional events were recorded (by all three stations) and located in the area south of the caldera where the earlier hodogram-only events were located. These new multi-station event recordings allow a more quantitative assessment of the uncertainties in the initial single-station hodogram locations. Each event is located using multiple arrival times as well as the hodogram method at as many as three stations. Thus

  20. Damping of power oscillations of exchange lines using a DC link; Amortecimento de oscilacoes de potencia de linhas de intercambio utilizando um elo de CC

    Energy Technology Data Exchange (ETDEWEB)

    Paccini, Rodrigo de O.; Custodio, Diogo T.; Kopcak, Igor; Costa, Vivaldo F. da [Universidade Estadual de Campinas (UNICAMP), SP (Brazil). Dept. de Sistemas de Energia Eletrica], Emails: rodrigo@dsee.fee.unicamp.br, totti@dsee.fee.unicamp.br, kopcak@dsee.fee.unicamp.br, vivaldo@dsee.fee.unicamp.br.

    2009-07-01

    This article presents a study that evaluates the effectiveness of a DC link in order to damp power oscillations, of inter area exchange, under small disturbance conditions, operating with Automatic Control Generation. The DC link was represented by a power injection model included the Sensitivity Power Model. Through this representation, the DC link was inserted in the block diagram, modeled as an injection power in the bars terminals in the net active and reactive, closing a new power balance at every instant. It was also designed a controller for damping power oscillations (POD-Power Oscillation Damping Controller) for modulation the power of the DC link and, therefore, insertion of additional damping in a frequency oscillations of exchange lines. The results confirm that the DC link has a great potential for maintaining the damping of oscillations frequency so inter area when equipped with POD controllers.

  1. Buried caldera of mauna kea volcano, hawaii.

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    Porter, S C

    1972-03-31

    An elliptical caldera (2.1 by 2.8 kilometers) at the summit of Mauna Kea volcano is inferred to lie buried beneath hawaiite lava flows and pyroclastic cones at an altitude of approximately 3850 meters. Stratigraphic relationships indicate that hawaiite eruptions began before a pre-Wisconsin period of ice-cap glaciation and that the crest of the mountain attained its present altitude and gross form during a glaciation of probable Early Wisconsin age.

  2. Magnetic study of the Furnas caldera (Azores

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    J. M. Torta

    1997-06-01

    Full Text Available A local ground magnetic study of the Furnas caldera (S. Miguel Island, Azores has provided new insight into the magnetic structure of this volcano. Analysis of the data comprised removal of the IGRF, reduction to the pole, pseudogravity integration and upward continuation. Also, a spectral method was applied to estimate the depth to the magnetic sources, as well as a 2.5D forward modelling technique. Magnetic properties obtained at the laboratory for some representative sample rocks were considered in the modelling process. The most relevant features are the existence of an important negative anomaly inside the caldera and of an intense positive anomaly to the south of the coast. The former points out a decrease in the magnetization of the caldera filling materials with respect to the surrounding rocks, which could be explained as the result of post-eruption processes such as hydrothermal alteration. This is expected as Furnas has an active hydrothermal system probably related with a magmatic reservoir at high temperature. The positive anomaly suggests the existence of a strongly-magnetized body beneath the south coast.

  3. Caldera processes and magma-hydrothermal systems continental scientific drilling program: thermal regimes, Valles caldera research, scientific and management plan

    Energy Technology Data Exchange (ETDEWEB)

    Goff, F.; Nielson, D.L. (eds.)

    1986-05-01

    Long-range core-drilling operations and initial scientific investigations are described for four sites in the Valles caldera, New Mexico. The plan concentrates on the period 1986 to 1993 and has six primary objectives: (1) study the origin, evolution, physical/chemical dynamics of the vapor-dominated portion of the Valles geothermal system; (2) investigate the characteristics of caldera fill and mechanisms of caldera collapse and resurgence; (3) determine the physical/chemical conditions in the heat transfer zone between crystallizing plutons and the hydrothermal system; (4) study the mechanism of ore deposition in the caldera environment; (5) develop and test high-temperature drilling techniques and logging tools; and (6) evaluate the geothermal resource within a large silicic caldera. Core holes VC-2a (500 m) and VC-2b (2000 m) are planned in the Sulphur Springs area; these core holes will probe the vapor-dominated zone, the underlying hot-water-dominated zone, the boiling interface and probable ore deposition between the two zones, and the deep structure and stratigraphy along the western part of the Valles caldera fracture zone and resurgent dome. Core hole VC-3 will involve reopening existing well Baca number12 and deepening it from 3.2 km (present total depth) to 5.5 km, this core hole will penetrate the deep-crystallized silicic pluton, investigate conductive heat transfer in that zone, and study the evolution of the central resurgent dome. Core hole VC-4 is designed to penetrate deep into the presumably thick caldera fill in eastern Valles caldera and examine the relationship between caldera formation, sedimentation, tectonics, and volcanism. Core hole VC-5 is to test structure, stratigraphy, and magmatic evolution of pre-Valles caldera rocks, their relations to Valles caldera, and the influences of regional structure on volcanism and caldera formation.

  4. Yellowstone and Long Valley - A Comparison of Two Restless Calderas

    Science.gov (United States)

    Hill, D. P.; Smith, R. B.

    2007-12-01

    Three large, silicic calderas in the conterminous United States have explosively erupted volumes > 300 km3 within in the last 2 million years -- Yellowstone caldera (Wyoming) Long Valley caldera (California) and the Vallez caldera (New Mexico) all located in extensional tectonic environments. All have shown varying levels of historic unrest. Pronounced unrest episodes at Yellowstone and Long Valley calderas over the past three decades stimulated extensive research on these two closely monitored calderas, and we explore some emerging similarities and differences. Yellowstone caldera is underlain by a long-lived (> 17 my) upper-mantle hot-spot that has fed a series of caldera-forming, extending to the southwest across southern Idaho to central Oregon including three caldera-forming eruptions from the Yellowstone caldera system in the last 2 my, the most recent at 600,000 ybp. It is marked by relatively low density and low seismic velocities extending to depths of at least 400 km and a regional topographic swell with elevations exceeding 2000 m. The extensive Yellowstone hydrothermal system has a thermal output of 5 GW. The most recent magmatic eruption dated at 70,000 ybp. By comparison, Long Valley caldera is underlain by a relatively modest "hot-spot", the locus of which appears to be influenced by a dilatational jog between the dextral Eastern California Shear Zone and the Walker Lane and westward delamination of the dense lithospheric root of the adjacent Sierra Nevada. The Long Valley system has fed multiple eruptions of over the past 4 my and a single caldera-forming eruption at 760,000 ybp. It is marked by a limited topographic swell but with the elevation of the caldera floor and adjacent basins comparable to the 2000-plus m elevation of the Yellowstone swell. Long Valley caldera hydrothermal system has a thermal output of 0.3 GW (including a 40 MW geothermal power plant). The most recent eruptions from the Long Valley Caldera- Mono Domes volcanic field

  5. Cooperación e intercambio de conocimiento en redes inter-organizativas informales

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    Carlos Martin-Rios

    2013-06-01

    Full Text Available El presente artículo explora el papel que juegan las redes informales de colaboración entre empresas para el intercambio de conocimiento. Para ello, se reportan los resultados de un estudio empírico llevado a cabo con una muestra de empresas localizadas en un campus tecnológico gestionado por una universidad que constituyen una red completa inter-organizacional. El estudio presenta evidencia sobre el papel que desempeñan las relaciones informales en el desarrollo de redes de conocimiento como vehículo para la transferencia de conocimiento tecnológico, de mercado y de gestión empresarial.

  6. Hacia una critica interna de la teoría del intercambio desigual de Emmanuel

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    Garay S. Luis Jorge

    1980-12-01

    Full Text Available El presente ensayo constituye apenas una versión parcial y preliminar de un trabajo más extenso que el autor está desarrollando sobre la teoría del intercambio desigual de Emmanuel. Entendido así el carácter de éste, su objetivo se limita únicamente a estudiar los principales supuestos, inconsistencias y vicios teóricos y metodológicos implícitos en
    el "traslado" particular que Emmanuel realiza del esquema de precios de Marx al plano del comercio internacional. En otras palabras, el análisis aquí incluido corresponde más a lo que en la literatura se denomina una crítica interna que a una crítica externa de la teoría de intercamhio desigual de Emmanuel.

  7. Determinantes del intercambio directo de drogas ilegales a pequeña escala en Cali

    Directory of Open Access Journals (Sweden)

    Bustamante Amaya Christian David

    2012-09-01

    Full Text Available Este documento centra su análisis en el estudio de los determinantes que explican el intercambio directo de drogas ilegales a pequeña escala en la ciudad de Cali, a partir de la estimación de modelos de datos de conteo. Se verifica el cumplimiento de los supuestos teóricos de la elección racional de los individuos que son esbozados en la economía del crimen. Los resultados del modelo sugieren que si un expendedor considera su actividad como riesgosa, reduce en una significativa cantidad el número de horas dedicadas al expendio. Por otra parte, el precio de un cigarrillo de marihuana afecta negativamente el número de veces que un individuo consume al día; no obstante, la magnitud del efecto para esta variable denota el alto grado de inelasticidad al precio que tiene el consumo de esta droga.

  8. La traducción globalizada: herramientas de intercambio y comunicación

    Directory of Open Access Journals (Sweden)

    Andrés López Ciruelos

    2009-06-01

    Full Text Available El trabajo del traductor está dejando de ser una actividad más o menos artesana centrada en el idioma para alinearse en una cadena de producción en la que el acto de la traducción ocupa un espacio cada vez más reducido. Los recursos tecnológicos se desarrollan deprisa y es imprescindible que el traductor los conozca y sepa hacer uso de ellos. Uno de los temas que más investigan las grandes empresas de «software» es el intercambio de la información. En este artículo se comentan dos niveles de intercambio y comunicación de datos con los que el traductor debería estar familiarizado, y se presentan las herramientas más representativas de cada uno: las plataformas de gestión y los archivos TMX. -------------------------------- Globalized translation — exchange and communication tools. The translator's work is no longer a craft focused exclusively on language, as it becomes a link in a production chain where the act of translation tends to take an increasingly smaller place. Technological resources are quickly developed and it is essential for the translator to know their existence and the way to use them. One of the issues that major software companies are investigating most intensively is the management and exchange of information. This articles discusses two levels of data communication and exchange that the translator should familiarize with, and also describes the tools that better handle these two issues: management platforms and TMX files.

  9. Setting A Stopwatch for Post-Caldera Effusive Rhyolite Eruptions at Yellowstone caldera, Wyoming

    Science.gov (United States)

    Till, C. B.; Vazquez, J. A.; Boyce, J. W.

    2015-12-01

    Rejuvenation of previously intruded silicic magma is an important process leading to effusive rhyolite, which is the most common product of volcanism at calderas with protracted histories of eruption and unrest such as Yellowstone caldera (Wyoming), Long Valley caldera (California), and Valles caldera (New Mexico) in the United States. Although orders of magnitude smaller in volume than rare caldera-forming supereruptions, these relatively frequent effusions of rhyolite are comparable to the largest eruptions of the 20th century and pose a considerable volcanic hazard. However, the physical pathway from rejuvenation to eruption of silicic magma is unclear, particularly because the time between reheating of a subvolcanic intrusion and eruption is poorly quantified. This study uses trace element diffusion in sanidine crystals measured at nanometer-scale with NanoSIMS to reveal that rejuvenation of a near-solidus or subsolidus silicic intrusion occurred within ~10 months following a protracted period (220 k.y.) of volcanic repose, and resulted in effusion of ~3 km3 of high-silica rhyolite lava at the onset of Yellowstone's last volcanic interval. In addition we find that the frequently made assumption in geospeedometry of a step-function initial condition can be inaccurate despite petrographic evidence for resorption, and can be addressed by interrogating diffusion time scale concordance between multiple trace elements that are geochemically similar. The results of this study reveal that a sufficiently energetic rejuvenation of Yellowstone's shallow crystal-melt mush and/or hydrothermally altered wall rock could lead to an effusive eruption within months. Fortunately, any significant rejuvenation of the reservoir is likely to be associated with deformation or seismicity and identifiable by geophysical monitoring.

  10. Elongate summit calderas as Neogene paleostress indicators in Antarctica

    Science.gov (United States)

    Paulsen, T.S.; Wilson, T.J.

    2007-01-01

    The orientations and ages of elongate summit calderas on major polygenetic volcanoes were compiled to document Miocene to Pleistocene Sh (minimum horizontal stress) directions on the western and northern flanks of the West Antarctic rift system. Miocene to Pleistocene summit calderas along the western Ross Sea show relatively consistent ENE long axis trends, which are at a high angle to the Transantarctic Mountain Front and parallel to the N77ºE Sh direction at Cape Roberts. The elongation directions of many Miocene to Pleistocene summit calderas in Marie Byrd Land parallel the alignment of polygenetic volcanoes in which they occur, except several Pleistocene calderas with consistent NNE to NE trends. The overall pattern of elongate calderas in Marie Byrd Land is probably due to a combination of structurally controlled orientations and regional stress fields in which Sh is oriented NNE to NE at a moderate to high angle to the trace of the West Antarctic rift system.

  11. The graben caldera of Guanajuato, Mexico

    Science.gov (United States)

    Aguirre-Diaz, G. J.; Tristán-González, M.; Labarthe-Hernández, G.; Marti, J.

    2013-05-01

    Guanajuato has been an important gold and silver mineral district of Mexico since the 16th century until Present. Famous mines such as Rayas, La Valenciana and El Cubo, are part of this important mining development. Stratigraphy and structures are well known, and major faults and vein systems are precisely mapped. The series include a Mesozoic metamorphosed volcano-sedimentary sequence interpreted as a tectonically accreted terrane during Early Cretaceous subduction; a >1000 m thick red beds sequence, apparently Eocene and interpreted originally as molasses posterior to K/T Laramide orogeny, but more probably fanglomerates filling a graben formed during mid-Tertiary extension; an Eocene-Miocene volcanic sequence that accumulated in this tectonic basin and the surrounding area, including andesitic lavas, silicic ignimbrites and surge deposits, and rhyolitic domes. Pyroclastic rocks have not been studied with a volcanological approach, with the purpose of understanding the physical volcanic processes that formed them. Randall (1994) suggested a caldera source for some of them. Our purpose is to describe the volcanic processes involved in the mid-Tertiary units of Guanajuato. There are dacitic and andesitic lavas that were apparently contemporaneous with deposition of the Red Conglomerate of Guanajuato. The ignimbrites correspond to the Sierra Madre Occidental volcanic province. These units were originated as two main pyroclastic densety currents sequences that formed the Loseros-Bufa and the Calderones formations. The former is rhyolitic and the later andesitic-dacitic. Loseros is composed of a series of thin-bedded to laminated pyroclastic surge deposits in continuous and concordant contact with overlying Bufa massive ignimbrite. Bufa ignimbrite is partly welded, with columnar jointing, completely devitrified, and highly silicified by post-deposition hydrothermalism and/or vapor phase alteration. Co-ignimbrite lithic lag breccias are observed at several sites in

  12. Caldera collapse at near-ridge seamounts: an experimental investigation

    Science.gov (United States)

    Coumans, Jason P.; Stix, John

    2016-10-01

    Collapse calderas are sub-circular volcanic depressions caused by subsidence of the magma reservoir roof during an eruption. Scaled physical models of caldera collapse using flat topography have been instrumental in investigating the spatial and temporal development of calderas, in particular, two distinctive sets of concentric ring faults, one reverse and one normal. More recent analog studies have investigated the effect of non-flat topography which alters the principle stress trajectories and resulting collapse structure. This work provides the basis for investigating how naturally scaled topographic loads may affect caldera collapse in relation to shallow magma reservoirs. The objective of this study is to understand how a near-ridge seamount affects caldera collapse from both a central and offset position as the seamount migrates above the magma reservoir as a result of plate motion. We utilize scaled analog models of caldera collapse in conjunction with three-dimensional (3D) laser scanning and digital particle image velocimetry (DPIV) to investigate caldera collapse dynamics at near-ridge seamounts. Experiments using a seamount cone positioned centrally above the magma reservoir result in (1) increased subsidence along the interior outward-dipping faults and (2) a preference to more symmetric collapse patterns as indicated by the subsidence profile and structure of the caldera relative to experiments with an offset cone. When the cone is offset, the collapse is asymmetric and trapdoor in nature, with the center of greatest subsidence displaced away from the region of largest topographic load. For these latter experiments, subsidence is focused where the roof is thinnest along an initial reverse fault, followed by a transition to an antithetic graben structure. The asymmetric collapse in the experiments results in a caldera with a tilted profile. Offset calderas at near-ridge seamounts are tilted towards the ridge axis, suggesting that they may have collapsed

  13. Geologic Map of the Valles Caldera, Jemez Mountains, New Mexico

    Science.gov (United States)

    Goff, F.; Gardner, J. N.; Reneau, S. L.; Kelley, S. A.; Kempter, K. A.; Lawrence, J. R.

    2011-12-01

    Valles caldera is famous as the type locality of large resurgent calderas (Smith and Bailey, 1968), the location of a classic 260-300 °C liquid-dominated geothermal system (Goff and Gardner, 1994), and the site of a long-lived late Pleistocene lake (Fawcett et al., 2011). We have published a detailed color geologic map of the Valles caldera and surrounding areas at 1:50,000 scale obtainable from New Mexico Bureau of Geology and Mineral Resources (geoinfo.nmt.edu/publications/maps/geologic/gm/79/). The new Valles map has been compiled from all or parts of nine 1:24,000 geologic maps completed between 2004 and 2008 (Bland, Cerro del Grant, Jarosa, Jemez Springs, Polvadera Peak, Redondo Peak, Seven Springs, Valle San Antonio, and Valle Toledo). Our map provides more detailed geology on the resurgent dome, caldera collapse breccias, post-caldera lava and tuff eruptions, intracaldera sedimentary and lacustrine deposits, and precaldera volcanic and sedimentary rocks than previous maps and incorporates recent stratigraphic revisions to the geology of the Jemez Mountains volcanic field. Three cross sections supported by surface geology, geophysical data and deep borehole logs (≤4500 m) show an updated view of the caldera interior, depict a modern interpretation of caldera collapse and resurgence, and provide caldera-wide subsurface isotherms (≤500 °C). A 30 page booklet included with the map contains extensive rock descriptions for 162 stratigraphic units and figures showing physiographic features, structural relations between Valles (1.25 Ma) and the earlier, comparably sized Toledo caldera (1.62 Ma), correlation charts of map units, and the distribution of pre- and post-caldera hydrothermal alteration styles, including recently documented zeolite-type alteration. Finally, the booklet includes a generalized model showing our interpretation of intracaldera structure and subjacent magma chambers, and relations of Valles to earlier Quaternary-Precambrian units.

  14. Optimum geometry for boiler soot blowers nozzles; Geometria optima de toberas para deshollinadores de caldera

    Energy Technology Data Exchange (ETDEWEB)

    Espinoza Garza, Jesus; Garcia Tinoco, Guillermo J.; Martinez Flores, Jose Oscar [Instituto de Investigaciones Electricas, Cuernavaca (Mexico)

    1989-12-31

    For boiler soot blowing converging-diverging nozzles are employed, whose function is to convert thermal energy of a gas into kinetic energy to remove the deposits that adhere to the heat exchanger surfaces. In this paper are described the experimental equipment and the methods for flow, dynamic pressure, discharge velocity and air expansion factor calculation in each nozzle, as a function of its design geometry, utilizing air from a five stage centrifugal compressor. The graphic analysis of the results, concludes that the most efficient nozzles are not the ones than develop the greatest velocity, but the ones of highest dynamic pressure at the outlet. The nozzle geometry that allows obtaining the maximum dynamic air pressure at the discharge is A{sub 2}/A{sub g}=1.3676 [Espanol] Para el deshollinado de calderas se utilizan las toberas convergentes-divergentes, cuya funcion es convertir la energia termica de un gas en energia cinetica para remover los depositos que se adhieren a las superficies de intercambio de calor. En este trabajo se describen el equipo experimental y los metodos de calculo para flujo, presion dinamica, velocidad a la descarga y factor de expansion del aire en cada tobera, como funcion de su geometria de diseno. Durante la experimentacion se evaluaron siete disenos diferentes de toberas, empleando aire de un compresor centrifugo de cinco etapas. Del analisis grafico de los resultados, se concluye que las toberas mas eficientes no son las que desarrollan mayor velocidad sino las de mayor presion dinamica de la salida. La geometria de tobera que permite obtener la maxima presion dinamica del aire a la descarga es A{sub 2}/A{sub g} = 1.3676.

  15. Stratigraphy of Reforma Caldera, Baja California Sur, Mexico

    Science.gov (United States)

    García Sánchez, L.; Macias, J. L.; Osorio, L. S.; Pola, A.; Avellán, D. R.; Arce, J. L.; Saucedo, R.; Sánchez, J. M.; García-Tenorio, F.; Cisneros, G.; Reyes-Agustín, G.; Cardona, S.; Jimenez, A.

    2015-12-01

    The Reforma caldera is located at ~35 km to the northwest of Santa Rosalía in the central part of the Baja California peninsula. It has 10 km in diameter and a maximum height of 1200 masl in the center and between 100 and 500 masl in its slopes. Reforma is within a tectonic zone affected by two fault systems: A NW-SE normal fault system linked to the opening of the Gulf of California, and a NNW-SSE and NW-SE strike-slip fault system associated with an active Riedel system. Reforma was built upon Cretaceous granites that outcrop at the caldera center, Miocene to Pliocene volcano-sedimentary rocks of the Comondú group, and Miocene marine sediments of the Santa Rosalía basin. On top of these rocks outcrop at least four submarine to subaerial ignimbrites interbedded with marine fossiliferous beds and the lower Pleistocene deposits associated to the Reforma caldera. These deposits are formed by a ignimbrite that shifts to different lithofacies that change gradually their welding, here dubbed basal, transitional, intermediate, and upper (all of then enriched in black fiammes), followed by a pumice-rich, white fiammes, and vitrophyre lithofacies, which are distributed around the 9 km wide caldera and have been associated to the caldera formation episode. Deposits related to post-caldera volcanism are andesite-basaltic lava flows erupted along the caldera rim through localized feeding dikes and andesitic and rhyolitic domes, and scoria cinder cones exposed inside and outside the caldera. On top of these deposits rest the middle Pleistocene Aguajito caldera deposits.

  16. Intercambio cationico calcio-magnesio-sodio en algunos suelos del Valle del Cauca

    Directory of Open Access Journals (Sweden)

    Torres M. Jorge Ilian

    1989-12-01

    Full Text Available Para estudiar la influencia de diferentes cantidades de Ca, Mg y Na en las aguas de riego sobre las propiedades químicas y físicas de los suelos, se caracterizó el intercambio Ca-Mg en presencia de diferentes saturaciones de Na en la solución de equilibrio en términos de las isotemas de intercambio de 4 suelos pertenecientes a los tres principales ordenes predominantes en el Valle del Cauca. En general hubo ligera preferencia por Ca sobre Mg en los suelos; pero a bajas concentraciones de Mg en la solución el suelo Doronzoro mostró preferencia por Mg y el suelo Crucero una tendencia hacia mayor afinidad por el Mg+2a altos valores de Mg y de la RAS en la solución. Las preferencias de los suelos por Mg parecen estar asociadas en parte con la presencia de carbonatos y materia orgánica. Con excepción del suelo Crucero, las isotermas no mostraron influencia de la RAS o del PSI resultante sobre la selectividad por Ca+2 o Mg+2. Las altas saturaciones de Mg+2 encontradas en muchos suelos del Valle del Cauca se deben a la presencia de altas cantidades de este ión en las aguas de riego en las aguas freáticas y no a preferencia de los suelos por el mismo.To study the influence of different amounts of Ca, Mg and Na in the irrigation water on chemical and physical properties of soils, four soils from the Cauca Valle y were used to characterize their cation distribution and the Ca-Mg exchange in presence of different concentrations of Na in the equilibrium solution. A general preference for Ca over Mg was found; however, the Doronzoro soil isotherms showed that at low ion concentrations of Mg in the solutions there is a preference for Mg2+relative to Ca2+ and Crucero soil showed an increasing affinity to Mg2+as its concentration and SAR increase in the solution. Soil preferences for magnesium seem to be related to the presence of organic matter or to the presence of carbonates. Excluding the Crucero soil the isotherms did not show influence of SAR

  17. Consecuencias de la caída de la fecundidad sobre los intercambios entre generaciones

    Directory of Open Access Journals (Sweden)

    Meil Landwerlin, Gerardo

    2007-12-01

    Full Text Available This article analyzes the effects of the number of siblings and their sex composition as well as other indicators of individualization which are intertwined with the development of a beanpole type kin structure on interchanges among generations in Spain. The effects of this development varies according to the point of view adopted, the parents one or that of the adult children. Though this development increases the probability not to have daughters, there are no clear signs of a weakening of intergenerational ties derived from the development of a beanpole type kin structure. The biggest threat for the density of intergenerational relationships derives not as much from this development, but from the geographical dispersion of the generations caused by the lack of professional and employment opportunities for the younger generations.

    El objeto de este trabajo es analizar los efectos de la caída de la fecundidad sobre los intercambios materiales e inmateriales entre las generaciones (adultas y residentes en hogares independientes en España. El análisis atiende, entre otras variables, al número y a la composición por sexos de la generación más joven, analizando los intercambios entre las díadas hijo varón emancipado / padres e hija emancipada / padres. Los efectos de la caída de la fecundidad y otros cambios familiares asociados a la misma dependen del punto de vista que se adopte, esto es, si se analizan desde el punto de vista de los padres o de los hijos. A pesar de que la caída de la fecundidad aumenta la probabilidad de no tener hijas, no hay signos claros de un debilitamiento de las relaciones intergeneracionales derivadas de la caída de la fecundidad. Las mayores amenazas para la densidad de las relaciones intergeneracionales no derivan tanto de la caída de la fecundidad, como de la dispersión de las generaciones como consecuencia de la ausencia de expectativas laborales y profesionales para la generación más joven en

  18. Imaging radar observations of Askja Caldera, Iceland

    Science.gov (United States)

    Malin, M. C.; Evans, D.; Elachi, C.

    1978-01-01

    A 'blind' test involving interpretation of computer-enhanced like- and cross-polarized radar images is used to evaluate the surface roughness of Askja Caldera, a large volcanic complex in central Iceland. The 'blind' test differs from earlier analyses of radar observations in that computer-processes images and both qualitative and quantitative analyses are used. Attention is given to photogeologic examination and subsequent survey-type field observations, along with aerial photography during the field trip. The results indicate that the 'blind' test of radar interpretation of the Askja volcanic area can be considered suitable within the framework of limitations of radar data considered explicitly from the onset. The limitations of the radar techniques can be eliminated by using oblique-viewing conditions to remove geometric distortions and slope effects.

  19. Magma storage in a strike-slip caldera.

    Science.gov (United States)

    Saxby, J; Gottsmann, J; Cashman, K; Gutiérrez, E

    2016-01-01

    Silicic calderas form during explosive volcanic eruptions when magma withdrawal triggers collapse along bounding faults. The nature of specific interactions between magmatism and tectonism in caldera-forming systems is, however, unclear. Regional stress patterns may control the location and geometry of magma reservoirs, which in turn may control the spatial and temporal development of faults. Here we provide new insight into strike-slip volcano-tectonic relations by analysing Bouguer gravity data from Ilopango caldera, El Salvador, which has a long history of catastrophic explosive eruptions. The observed low gravity beneath the caldera is aligned along the principal horizontal stress orientations of the El Salvador Fault Zone. Data inversion shows that the causative low-density structure extends to ca. 6 km depth, which we interpret as a shallow plumbing system comprising a fractured hydrothermal reservoir overlying a magmatic reservoir with vol% exsolved vapour. Fault-controlled localization of magma constrains potential vent locations for future eruptions. PMID:27447932

  20. Magma storage in a strike-slip caldera

    Science.gov (United States)

    Saxby, J.; Gottsmann, J.; Cashman, K.; Gutiérrez, E.

    2016-07-01

    Silicic calderas form during explosive volcanic eruptions when magma withdrawal triggers collapse along bounding faults. The nature of specific interactions between magmatism and tectonism in caldera-forming systems is, however, unclear. Regional stress patterns may control the location and geometry of magma reservoirs, which in turn may control the spatial and temporal development of faults. Here we provide new insight into strike-slip volcano-tectonic relations by analysing Bouguer gravity data from Ilopango caldera, El Salvador, which has a long history of catastrophic explosive eruptions. The observed low gravity beneath the caldera is aligned along the principal horizontal stress orientations of the El Salvador Fault Zone. Data inversion shows that the causative low-density structure extends to ca. 6 km depth, which we interpret as a shallow plumbing system comprising a fractured hydrothermal reservoir overlying a magmatic reservoir with vol% exsolved vapour. Fault-controlled localization of magma constrains potential vent locations for future eruptions.

  1. The Campi Flegrei caldera: unrest mechanisms and hazards

    OpenAIRE

    De Natale, G.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia; Troise, C.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia; Pingue, F.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia; Mastrolorenzo, G.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia; Pappalardo, L.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia; Battaglia, M.; Department of Structural Geology & Geodynamics, University of Göttingen, 37077 Göttingen, Germany; Boschi, E.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione AC, Roma, Italia

    2006-01-01

    In the last four decades, Campi Flegrei caldera has been the world’s most active caldera characterized by intense unrest episodes involving huge ground deformation and seismicity, but, at the time of writing, has not culminated in an eruption. We present a careful review, with new analyses and interpretation, of all the data and recent research results. We deal with three main problems: the tentative reconstruction of the substructure; the modelling of unrest episodes to shed l...

  2. Geology and structure of the Malpaso caldera and El Ocote ignimbrite, Aguascalientes, Mexico

    Energy Technology Data Exchange (ETDEWEB)

    Nieto-Obregon, Jorge [Facultad de IngenierIa, UNAM, Coyoacan, 04510, Mexico D.F. (Mexico); Aguirre-DIaz, Gerardo [Centro de Geociencias, UNAM, Campus Juriquilla, 76220, Queretaro, Qro. (Mexico)], E-mail: nieto@servidor.unam.mx, E-mail: ger@geociencias.unam.mx

    2008-10-01

    A new caldera, named Malpaso, is reported west of the city of Aguascalientes, Mexico. The Malpaso caldera is a volcano-tectonic depression, highly fractured and faulted, and was filled by voluminous pyroclastic products related to the caldera collapse. Due to these characteristics it as a graben caldera. It is truncated by younger normal faults of the Calvillo and Aguascalientes grabens. In this work we present a summary of the geologic and structural observations on this caldera, as well as a description of the main caldera product, the high-grade El Ocote ignimbrite.

  3. Intercambio de experiencias de capacitación y de práctica profesional

    Directory of Open Access Journals (Sweden)

    Marielos Vargas Morales

    2010-06-01

    Full Text Available

    Recibido 11 de agosto de 2009 • Aceptado 02 de diciembre de 2009 • Corregido 02 de marzo de 2010

     

    Resumen. Este artículo surge como producto de la implementación del proyecto Intercambio Académico entre la División de Educación Rural (DER, de la Universidad Nacional (UNA y escuelas colaboradoras. Desde su quehacer se abordan dos acciones fundamentales; la primera, la concepción teórico-metodológica de la práctica profesional de la DER y la segunda, el proceso de capacitación dirigido a maestros rurales en servicio. A partir de estas actividades académicas se exponen productos gestados a lo interno del proyecto y algunas reflexiones sobre la experiencia académica como resultado de lecciones aprendidas durante el proceso.

     

    Abstract. The present article arises from the implementation of the Academic Exchange project between the Division de Educación Rural (Rural Education School from Universidad Nacional and other collaborating schools. There are two fundamental actions that are approached; first, the theoretical methodological conception of the professional field practicum of the DER and second, the teaching training to rural teachers in service. From these academic activities, products developed are exposed in the project and some reflections about the academic experience were also exposed as a result of lessons learned during the whole process.

  4. La Identificación Social y las Instituciones Informales: su Efecto en el Intercambio de Conocimiento

    Directory of Open Access Journals (Sweden)

    Eréndira Fierro Moreno

    2014-01-01

    Full Text Available El efecto de los recursos organizaciones en la gestión del conocimiento ha sido ampliamente estudiado. Sin embargo, esta investigación analiza las instituciones informales y la identificación social como determinantes del intercambio de conocimiento. Se constata una brecha en el conocimiento respecto del análisis de la incidencia de las instituciones informales en las estrategias de gestión y de organización en las organizaciones en países de economías emergente. Con base en la teoría de recursos y capacidades, se formula la hipótesis de que las instituciones informales y la identificación social afectan al intercambio de conocimiento. Con un estudio transeccional y con una muestra de organizaciones del sector público del Estado de México, se encontró confirmación de las hipótesis. Se utilizó la técnica de modelación de ecuaciones estructurales. Los resultados de esta investigación confirman que los recursos al ser únicos y valiosos tales como las instituciones informales (siempre y cuando no sean factores restrictivos que afectan a las estrategias de las organizaciones y no sean ineficientes de modo que afecten a la organización y la identificación social ayudan a generar nuevas capacidades. Esta investigación permitió considerar la importancia de recursos organizacionales como generadores de intercambio de co nocimiento.

  5. Efficiency and exchange. neoclassical, institutionalist and neoinstitutionalist schools Eficiencia e intercambio. Corriente neoclásica, institucionalismo y neoinstitucionalismo

    Directory of Open Access Journals (Sweden)

    Morales F Fabio

    1997-06-01

    Full Text Available This article presents a brief review of the role played by institutions in economic exchange and decision-making within the neoclassical, institutionalist, and neoinstitutionalist schools of economic thought. For the neoclassical school, institutions are exogenous, don't affect exchange or economic decisions and, paradoxically, exclude from their analysis the main economic institution: the market. The author contrasts this point of view with the institutionalist and neoinstitutionalist visions in which institutions are essential in shaping the system of exchange and ensuring the functioning of markets, and presents a synthesis of the analytical concerns and contributions of these two approaches to economic thought.En este artículo se presenta una breve revisión del papel que juegan las instituciones en el intercambio y la toma de decisiones económicas dentro de las corrientes del pensamiento económico neoclásica, institucionalista y neoinstitucionalista. Para la corrientr neoclásica, las instituciones son exógenas, no afectan el intercambio ni las decisiones económicas y paradójicamente, se excluye del análisis la principal institución económica: el mercado. El autor contrasta este punto de vista con las visiones institucionalista y neoinstitucionalista en las que las instituciones son esenciales para configurar el sistema de intercambio y asegurar el funcionamiento del mercado, y presenta una síntesis de las preocupaciones analíticas y las contribuciones de estas dos vertientes del pensamiento económico.

  6. Science guide for the Long Valley Caldera deep hole

    Energy Technology Data Exchange (ETDEWEB)

    Rundle, J.B.; Eichelberger, J.C. (eds.)

    1989-05-01

    The Magma Energy Program of the US Department of Energy, Geothermal Technology Division, is planning to begin drilling a deep (6 km) exploration well in Long Valley Caldera, California, in September 1988. The location of the well is in the central part of the caldera, coincident with a large number of shallow (5-7 km) geophysical anomalies identified through many independent investigations. Results from the hole will permit the following: direct investigation of the geophysical anomalies interpreted to be magma; investigation of the patterns and conditions of deep fluid circulation and heat transport below the caldera floor; determination of the amount of collapse and subsequent resurgence of the central portion of Long Valley caldera; and determination of the intrusion history of the central plutonic complex beneath the caldera, and establishment of the relationship of intrusive to eruptive events. The hole will thus provide a stringent test of the hypothesis that magma is still present within the central plutonic complex. If the interpretation of geophysical anomalies is confirmed, the hole will provide the first observations of the environment near a large silicic magma chamber. 80 refs., 7 figs., 2 tabs.

  7. Juego de manos: un intercambio entre niños y adultos. El pasado y el presente

    OpenAIRE

    Sopeña Hurtado, Ana

    2015-01-01

    Los juegos de manos se han practicado durante generaciones. Se trata de un tipo de juego sencillo que consiste básicamente en realizar distintos movimientos con las manos, ya sea de forma independiente o con el acompañamiento de una canción o retahíla. Hoy en día estos juegos se están perdiendo, por ello nos interesamos por contribuir a su recuperación a través de un intercambio intergeneracional que se realizó fuera de la escuela, pero que bien podría ser una propuesta para trabajar en el au...

  8. Análisis crítico de los modelos interpretativos dominantes sobre el intercambio desigual en la historia

    OpenAIRE

    Carlos Alberto Tomás Astarita

    1989-01-01

    En este trabajo se considerará la situación historiográfica sobre el intercambio desigual o asimétrico, noción que aparece vinculada con el de desarrollo diferenciado entre países. La posición más conocida en el estudio de la historia europea es la de Immanuel Wallerstein, quien ha tratado el problema entre 1450 y 1750, en trabajos de muy amplia difusión internacional. La base del razonamiento de Wallerstein es que la transferencia de materias primas por manufacturas de un área o país haci...

  9. EFECTOS DEL CONTROL DE CAMBIO EN EL INTERCAMBIO COMERCIAL CON COLOMBIA. CONSECUENCIAS DEL RETIRO DE VENEZUELA DE LA COMUNIDAD ANDINA

    Directory of Open Access Journals (Sweden)

    Humberto José Mayora Guaita

    2013-02-01

    Full Text Available Trade between Colombia and Venezuela has been totally affected in the past four years. One of the salient features is evidenced by the records of imports and exports of billions of dollars that experienced their peak in 2008 with 7.289 million dollars of trade. However, since 2009 this trade declined due to political confrontations that made to rethink the challenges and strategies in Caracas and Bogota to recover, rather than economic, the political, institutional and even social. This research aims to analyze the causes that led to a stage where it is ob-served a booming in bilateral trade, momentum, maximum and steep drops, but one way or another are needed for its complement. The methodology used in this study was the documentary research. Finally these events are related to the rigors of exchange control in Venezuela, CADIVI, that affect the price of the products that are recorded daily in various transactions made by entrepreneurs and marketers on the Colombian side and by the end 2011 recorded an exchange of 2,193 million.El intercambio comercial entre Colombia y Venezuela ha estado totalmente afectado en los últimos cuatro años. Uno de los rasgos más destacados se evidencia con registros de importaciones y exportaciones de miles de millones de dólares que experimentaron sus máximas en 2008 con 7.289 millones de dólares de intercambio comercial. Sin embargo, des-de el año 2009 este intercambio disminuyó a causa de las confrontaciones políticas que hizo replantear los retos y estrategias en Caracas y Bogotá para recuperar más que las relaciones económicas, las políticas, institucionales y hasta sociales. Esta investigación tiene como objetivos analizar las causas que propiciaron un escenario donde se observa el comercio binacional con auge, impulso, máximas y caídas abruptas, pero que de una manera u otra manera se necesitan para su complemento. La metodología empleada consiste en la investigación documental. Finalmente

  10. Control adaptable utilizando Redes Neuronales Artificiales Polinomiales

    OpenAIRE

    Gómez, E.; A. S. Poznyak; Lozano, R, R.

    2000-01-01

    Existen en la literatura de Control Adaptable, diferentes procedimientos en los que es posible identificar un sistema lineal. El problema fundamental es que una cantidad importante de fenómenos de la vida real son de tipo no lineal y no es tan sencillo el modelar este tipo de dinámicas. En este trabajo se presenta una forma de identificar sistemas no lineales utilizando las propiedades de las Redes Neuronales Artificiales y las técnicas de Algoritmo Genético en la optimización de ...

  11. Geophysical expression of the batholith beneath Questa Caldera, New Mexico

    Science.gov (United States)

    Cordell, Lindrith; Long, Carl L.; Jones, David W.

    1985-11-01

    Gravity gradients delineate uncharacteristically straight, north-south trending graben faults in the Rio Grande rift west of Questa caldera, and gravity and audiomagnetotelluric (AMT) data show north-south trending low-density and high-resistivity zones from the caldera southward. A gravity inversion technique was used to isolate the gravity anomaly of the caldera and related intrusive rocks from the complicated Bouguer gravity field. The residual gravity anomaly together with AMT data reported in a companion paper by C. L. Long seem to delineate the subcaldera batholith. Geophysical models indicate this to be a north-south trending dikelike or beamlike body about 25 km long, 5 km wide, and >4 km thick, thickness estimate being limited by the penetration depth of the AMT soundings. The north-south trend is not consistent with the regional pattern of early Miocene southwest directed extension and instead may reflect passive control by preexisting north-south strike-slip faults.

  12. Carbonatite ring-complexes explained by caldera-style volcanism.

    Science.gov (United States)

    Andersson, Magnus; Malehmir, Alireza; Troll, Valentin R; Dehghannejad, Mahdieh; Juhlin, Christopher; Ask, Maria

    2013-01-01

    Carbonatites are rare, carbonate-rich magmatic rocks that make up a minute portion of the crust only, yet they are of great relevance for our understanding of crustal and mantle processes. Although they occur in all continents and from Archaean to present, the deeper plumbing system of carbonatite ring-complexes is usually poorly constrained. Here, we show that carbonatite ring-complexes can be explained by caldera-style volcanism. Our geophysical investigation of the Alnö carbonatite ring-complex in central Sweden identifies a solidified saucer-shaped magma chamber at ~3 km depth that links to surface exposures through a ring fault system. Caldera subsidence during final stages of activity caused carbonatite eruptions north of the main complex, providing the crucial element to connect plutonic and eruptive features of carbonatite magmatism. The way carbonatite magmas are stored, transported and erupt at the surface is thus comparable to known emplacement styles from silicic calderas. PMID:23591904

  13. Modes and times of caldera resurgence: The Ischia Caldera, Italy, from high-precision archaeomagnetic dating

    Science.gov (United States)

    Vezzoli, Luigina; Principe, Claudia; Malfatti, Jonas; Arrighi, Simone; Tanguy, Jean-Claude; Le Goff, Maxime

    2009-10-01

    Ischia is a well exposed and densely populated late Quaternary caldera in the Campanian magmatic province of Italy. Ischia Caldera experienced an average uplift rate of 3.3 cm/year in the last ca. 30 ka and is still actively resurging. During the last 10 ka, coeval with the resurgence, a volcanic field of alkali-trachytic to trachyandesitic lava domes, lava flows, tuff and scoria rings, and pumice cones developed, mainly on the eastern sector of the caldera, along both resurgence-related faults and regional NNW- and NE-striking faults. In order to improve both our understanding of the recent volcanic history and the evaluation of future risks on Ischia Island, a high-precision archaeomagnetic dating method was applied to the products of 12 volcanic centres with probable age Ischia volcanism occurred in five periods separated by phases of quiescence and coeval with earthquake and landslide events. This fact suggests a pulsating mode of uplifting and deformations of the Ischia resurgence. During the two oldest periods of activity (7200-6800 BC and 4100-2300 BC), resurgence probably produced a dome-shaped structure. Location and geometry of vents suggest the occurrence of magma uprise along the fractures produced by bending of the overburden crustal block. Most of magma was emplaced as intrusions at the interior of the resurgent block, whereas volcanism was represented by very viscous, differentiated, and crystallized lavas that emplaced as domes and high aspect-ratio flows. The resurgent dome caused recurrent lateral collapses that removed about 2.5 km 3 of rocks. During the three youngest periods of activity (1800-1000 BC; 650 BC -355 AD; and 1302 AD), resurgence affected a fault-bounded, asymmetric block. This resulted from both (a) hydrostatic rebound of the crustal block after removal of material involved into huge slope instability triggering an increase in uplift rate, and (b) new influxes of less evolved magma batches into the shallow reservoir that, in turn

  14. Workshop on recent research in the Valles caldera

    Energy Technology Data Exchange (ETDEWEB)

    Heiken, G. (comp.)

    1985-02-01

    Over the last 5 years, there has been increased interest in the geology of the Jemez Mountains volcanic field, New Mexico. Of special interest is the Toledo-Valles caldera complex, which is targeted for research coring as part of the Continental Scientific Drilling Program. The general topics covered in this workshop were (1) hydrothermal systems and rock-water interactions, (2) volcanology and structural framework of the Jemez volcanic field, (3) determining the presence or absence of melt below the Valles caldera, and (4) deep coring and drilling technology. Separate abstracts were prepared for each presentation.

  15. GPS time series at Campi Flegrei caldera (2000-2013

    Directory of Open Access Journals (Sweden)

    Prospero De Martino

    2014-05-01

    Full Text Available The Campi Flegrei caldera is an active volcanic system associated to a high volcanic risk, and represents a well known and peculiar example of ground deformations (bradyseism, characterized by intense uplift periods, followed by subsidence phases with some episodic superimposed mini-uplifts. Ground deformation is an important volcanic precursor, and, its continuous monitoring, is one of the main tool for short time forecast of eruptive activity. This paper provides an overview of the continuous GPS monitoring of the Campi Flegrei caldera from January 2000 to July 2013, including network operations, data recording and processing, and data products. In this period the GPS time series allowed continuous and accurate tracking of ground deformation of the area. Seven main uplift episodes were detected, and during each uplift period, the recurrent horizontal displacement pattern, radial from the “caldera center”, suggests no significant change in deformation source geometry and location occurs. The complete archive of GPS time series at Campi Flegrei area is reported in the Supplementary materials. These data can be usefull for the scientific community in improving the research on Campi Flegrei caldera dynamic and hazard assessment.

  16. Potential Hazards of Eruptions around the Tianchi Caldera Lake, China

    Institute of Scientific and Technical Information of China (English)

    WEI Haiquan; HONG Hanjing; R.S.J. SPARKS; J.S. WALDER; HAN Bin

    2004-01-01

    Since the eruption of the Tianchi volcano about 1000 years ago, there have been at least 3 to 5 eruptions of small to moderate size. In addition, hazardous avalanches, rock falls and debris flows have occurred during periods between eruptions. A future eruption of the Tianchi volcano is likely to involve explosive interaction between magma and the caldera lake. The volume of erupted magma is almost in a range of 0.1-0.5 km3. Tephra fallout may damage agriculture in a large area near the volcano. If only 1% of the lake water were ejected during an eruption and then precipitated over an area of 200 km2, the average rainfall would be 100 mm. Moreover, lahars are likely to occur as both tephra and water ejected from the caldera lake fall onto flanks of the volcano. Rocks avalanching into the caldera lake also would bring about grave hazards because seiches would be triggered and lake water with the volume equal to that of the landslide would spill out of the existing breach in the caldera and cause flooding downstream.

  17. REMOCIÓN DE COBRE Y NÍQUEL POR INTERCAMBIO CATIÓNICO CON UNA ZEOLITA NATURAL

    Directory of Open Access Journals (Sweden)

    Arnoldy Estupiñan

    2010-10-01

    Full Text Available Se empleó la zeolita natural clinoptilolita, para remover cobre y níquel de aguas residuales de una industria de galvanotecnia. La capacidad de intercambio determinada para la zeolita transformada al estado homoiónico sódico, fue de 0,794 meq/g para cobre y 0,447 meq/g para níquel. Se realizaron ensayos en cochada y en columna, alcanzando éste último un mayor acercamiento al equilibrio. En los ensayos de regeneración, la zeolita sódica concentró el cobre hasta 23,5 veces con respecto al valor que presenta en los enjuagues de los baños de recubrimiento en medio ácido, mostrando su potencialidad para usarla en el tratamiento de estos residuos, por su efectividad y bajo costo.

  18. Intercambio gaseoso en el síndrome de dificultad respiratoria aguda Gas exchange in acute respiratory distress syndrome

    OpenAIRE

    G. A. Raimondi

    2003-01-01

    El síndrome de dificultad respiratoria aguda (ARDS) se caracteriza por presentar alteraciones severas del intercambio gaseoso (IG) causadas por «shunt» e importante irregularidad de la ventilación perfusión (V A/Q). Esto es consecuencia del edema intersticial y el colapso y ocupación alveolar. Además de la fracción inspirada de oxígeno y la evolución de la patología pulmonar, hay distintas variables que son capaces de alterar la presión parcial de oxígeno arterial (PaO2). Es así que los cambi...

  19. Riobamba y el ferrocarril. Nuevas dinámicas de intercambio regional en el primer cuarto del siglo XX

    Directory of Open Access Journals (Sweden)

    Franklin Cepeda Astudillo

    2006-11-01

    Full Text Available Este artículo analiza los conflictos que produjo el paso del ferrocarril por Riobamba. Describe la lucha por la rectificación de la vía férrea, que enlazaba las ciudades de Guayaquil y Quito, y subraya las pugnas y aspiraciones locales relacionadas con el nuevo medio de transporte. Señala las reacciones de la opinión pública riobambeña, expuestas en su prensa local, y las posturas tanto de los gobiernos como de la empresa que construyó la obra. Además, estudia las consecuencias que se derivaron del paso del ferrocarril: la ampliación del mercado interno como consecuencia del incremento del comercio interregional, el desarrollo de los poblados situados a lo largo del trazado ferroviario y la aceleración del intercambio de personas y bienes.

  20. Temperature data from wells in Long Valley Caldera, California

    Science.gov (United States)

    Farrar, Christopher; DeAngelo, Jacob; Williams, Colin; Grubb, Frederick; Hurwitz, Shaul

    2010-01-01

    The 30-by-20-km Long Valley Caldera (LVC) in eastern California (fig.1) formed at 0.76 Ma in a cataclysmic eruption that resulted in the deposition of 600 km? of Bishop Tuff outside the caldera rim (Bailey, 1989). By approximately 0.6 Ma, uplift of the central part of the caldera floor and eruption of rhyolitic lava formed the resurgent dome. The most recent eruptive activity in the area occurred approximately 600 yr ago along the Mono-Inyo craters volcanic chain (Bailey, 2004; Hildreth, 2004). LVC hosts an active hydrothermal system that includes hot springs, fumaroles, mineral deposits, and an active geothermal well field and power plant at Casa Diablo along the southwestern boundary of the resurgent dome (Sorey and Lewis, 1976; Sorey and others, 1978; Sorey and others, 1991). Electric power generation began in 1985 with about 10 Mwe net capacity and was expanded to about 40 Mwe (net) in 1991 (Campbell, 2000; Suemnicht and others, 2007). Plans for further expansion are focused mainly on targets in the caldera?s western moat (Sass and Priest, 2002) where the most recent volcanic activity has occurred (Hildreth, 2004). LVC has been the site of extensive research on geothermal resources and volcanic hazards (Bailey and others, 1976; Muffler and Williams, 1976; Miller and others, 1982; Hill and others 2002). The first geothermal exploratory drilling was done in the shallow (geothermal exploration and by the U.S. Geological Survey (USGS) and Sandia National Laboratory for volcanic and geothermal research and exploration. Temperature logs were obtained in some of these wells during or immediately following drilling, before thermal equilibration was complete. Most of the temperature logs, however, were obtained weeks, months, or years after well completion and are representative of dynamic thermal equilibrium. The maximum reservoir temperature for LVC is estimated to be about 220?C on the basis of chemical geothermometers (Fournier and Truesdell, 1973) using analytical

  1. How summit calderas collapse on basaltic volcanoes: new insights from the April 2007 caldera collapse of Piton de la Fournaise volcano

    Energy Technology Data Exchange (ETDEWEB)

    Michon, Laurent; Catry, Thibault; Merle, Olivier [Laboratoire GeoSciences Reunion, Universite de la Reunion, Institut de Physique du Globe de Paris, CNRS, UMR 7154 - Geologie des Systemes Volcaniques, 15 avenue Rene Cassin, 97715 Saint Denis (France); Villeneuve, Nicolas [Institut de Recherche pour le Developpement, US 140, BP172, 97492 Sainte-Clotilde cedex (France)], E-mail: laurent.michon@univ-reunion.fr

    2008-10-01

    In April 2007, Piton de la Fournaise volcano experienced a caldera collapse during its largest historical eruption. We present here the resulting deformation and a synthesis of the seismicity recorded during recent caldera collapses. It allows us to propose a unifying mechanism that explains the pulsating collapse dynamics.

  2. How summit calderas collapse on basaltic volcanoes: new insights from the April 2007 caldera collapse of Piton de la Fournaise volcano

    International Nuclear Information System (INIS)

    In April 2007, Piton de la Fournaise volcano experienced a caldera collapse during its largest historical eruption. We present here the resulting deformation and a synthesis of the seismicity recorded during recent caldera collapses. It allows us to propose a unifying mechanism that explains the pulsating collapse dynamics.

  3. Hollow volcanic tumulus caves of Kilauea Caldera, Hawaii County, Hawaii

    Directory of Open Access Journals (Sweden)

    William R. Halliday

    1998-01-01

    Full Text Available In addition to lava tube caves with commonly noted features, sizable subcrustal spaces of several types exist on the floor of Kilauea Caldera. Most of these are formed by drainage of partially stabilized volcanic structures enlarged or formed by injection of very fluid lava beneath a plastic crust. Most conspicuous are hollow tumuli, possibly first described by Walker in 1991. Walker mapped and described the outer chamber of Tumulus E-I Cave. Further exploration has revealed that it has a hyperthermic inner room beneath an adjoining tumulus with no connection evident on the surface. Two lengthy, sinuous hollow tumuli also are present in this part of the caldera. These findings support Walkers conclusions that hollow tumuli provide valuable insights into tumulus-forming mechanisms, and provide information about the processes of emplacement of pahoehoe sheet flows.

  4. Hollow volcanic tumulus caves of Kilauea Caldera, Hawaii County, Hawaii

    OpenAIRE

    William R. Halliday

    1998-01-01

    In addition to lava tube caves with commonly noted features, sizable subcrustal spaces of several types exist on the floor of Kilauea Caldera. Most of these are formed by drainage of partially stabilized volcanic structures enlarged or formed by injection of very fluid lava beneath a plastic crust. Most conspicuous are hollow tumuli, possibly first described by Walker in 1991. Walker mapped and described the outer chamber of Tumulus E-I Cave. Further exploration has revealed that it has a hyp...

  5. Maars to calderas: end-members on a spectrum of explosive volcanic depressions

    OpenAIRE

    Danilo M. Palladino; Valentine, Greg A.; Sottili, Gianluca; Taddeucci, Jacopo

    2015-01-01

    We discuss maar-diatremes and calderas as end-members on a spectrum of negative volcanic landforms (depressions) produced by explosive eruptions (note—we focus on calderas formed during explosive eruptions, recognizing that some caldera types are not related to such activity). The former are dominated by ejection of material during numerous discrete phreatomagmatic explosions, brecciation, and subsidence of diatreme fill, while the latter are dominated by subsidence over a partly evacuated ma...

  6. Maars to calderas: end-members on a spectrum of explosive volcanic depressions

    OpenAIRE

    Danilo M. Palladino; Valentine, Greg A.; Gianluca eSottili; Jacopo eTaddeucci

    2015-01-01

    We discuss maar-diatremes and calderas as end-members on a spectrum of negative volcanic landforms (depressions) produced by explosive eruptions (note – we focus on calderas formed during explosive eruptions, recognizing that some caldera types are not related to such activity). The former are dominated by ejection of material during numerous discrete phreatomagmatic explosions, brecciation, and subsidence of diatreme fill, while the latter are dominated by subsidence over a partly evacuated...

  7. El español en los intercambios de ciencia y tecnología durante el siglo XX

    Directory of Open Access Journals (Sweden)

    Nicolás Cuvi

    2005-06-01

    Full Text Available En un amplio estudio sobre los intercambios de ciencia y tecnología entre España e Hispanoamérica durante el siglo XX, nos hemos cuestionado sobre el peso relativo del lenguaje común en la intensidad de esta comunicación. Encontramos que durante el siglo XX, diversas voces de científicos y lingüistas han realizado esfuerzos —retóricos en ocasiones, prácticos en otras— por fortalecer el conocimiento y el uso de las voces en español de la ciencia y la tecnología. Testimonio de ello son los intentos de compilar diccionarios y vocabularios que se suceden a lo largo de la centuria. Pero aun considerando tal interés por «normalizar» las voces de la ciencia y la tecnología en español —un campo que, lejos de agotarse, demanda atención cada día—, resulta difícil concluir si durante el siglo XX, además de facilitar las comunicaciones (lo que ya es importante, el idioma común fue o no determinante para los intercambios de ciencia y tecnología entre Hispanoamérica y España. -------------------------------------------- The Spanish language in scientific and technological exchanges during the twentieth century. In an extensive study on the scientific and technological exchanges that took place between Spain and Spanish America during the twentieth century, we looked at the relative influence of everyday language on the intensity of that communication. In doing so we discovered that in the twentieth century efforts were made by scientists and linguists alike, both on a rhetorical and practical level, to promote the knowledge and use of Spanish scientific and technical terms, as witnessed by numerous attempts at compiling dictionaries and glossaries throughout the century. But even in the face of such efforts to standardize scientific and technological vocabulary in Spanish —an enterprise that, far from being obsolete, demands increasing attention— it is difficult to ascertain whether everyday language, aside from having made

  8. Una aplicación móvil para mejorar la integración de los estudiantes de intercambio en la ETSINF

    OpenAIRE

    SÁEZ REQUENA, ALBERTO

    2013-01-01

    En este proyecto final de carrera se desarrolla una aplicación para la plataforma iOS con el fin de contribuir a la integración de los estudiantes de intercambio que van a estudiar a la ETS. de Ingeniería Informática de la Universitat Politècnica de València. Para ello se estudiaron los requisitos que una aplicación de ese tipo podía tener y se desarrolló mediante Xcode una aplicación para iOS que se basa principalmente en la Guía de Intercambio proporcionada por la UPV a di...

  9. Satellites images, digitized topography, and the recognition of the Xela Caldera, Quezaltenango Valley, Guatemala

    Energy Technology Data Exchange (ETDEWEB)

    Foley, D. (Pacific Lutheran Univ., Tacoma, WA (United States). Dept. of Earth Sciences); McEwen, A.; Duffield, W. (Geological Survey, Flagstaff, AZ (United States)); Heiken, G. (Los Alamos National Lab., NM (United States))

    1992-01-01

    The authors propose, based on reconnaissance geology studies and interpretation of landforms as depicted by Landsat Thematic Mapper (TM) images combined with digitized topography, that the Quezaltenango basin of Guatemala is part of a caldera. The Quezaltenango basin is an elliptical depression, about 12 by 25 km and about 500 m deep. The proposed Xela Caldera extends beyond the basin more than 10 km to the north. The geomorphological features of the area that are typical of a geologically young large-scale caldera include bounding walls that have steep interior and gentle exterior slopes; broad flat areas at the base of the walls; at least one large block, about 3 by 12 km, that only partly floundered as the caldera collapsed; resurgence of a younger volcanic dome, flow and small-scale caldera complex (last active in 1818); younger volcanoes located along the structural margin of the major caldera (one of which is currently active) lobate features on the caldera margins that may indicate a multiple sequence of eruptions; and an active, high-temperature geothermal system. The valley is coincident with a gravity low. Extensive ash-flow tuff sheets that have no identified source are located north of the caldera, and may be the outflow deposits. The Xela caldera is similar in size to the Atitlan caldera, which lies about 50 km southeast of Quezaltenango. The Xela Caldera, if confirmed by future studies, may contain undiscovered geothermal resources, may present a significant geologic hazard to the more than 400,000 people who occupy the Quezaltenango valley, and may be a new member of the list of magmatic systems that have the capability to change global climate for several years.

  10. Estudio de las características del intercambio gaseoso de variedades de geranio en cultivo protegido en zonas de clima mediterráneo

    OpenAIRE

    Sant i Vilella, M. Dolors

    1987-01-01

    [spa] En plantas de geranio dedicadas a la producción de esquejes (Pelargonium x hortorum cv. Orange Ricard, P. grandiflorum cv. FJamingo y P. peltatum cv. Old Lady, cultivadas en contenedor, en substrato artificial, en un invernadero comercial) se realizaron series estacionales de medidas del intercambio gaseoso en laboratorio en respuesta a cambios de irradiancia, temperatura y humedad del aire, y se determinaron en el invernadero la respuesta en el ciclo diario de la fotosíntesis neta, tra...

  11. Un modelo matemático para fenómenos de intercambio y difusión en pañales superabsorbentes

    OpenAIRE

    Estrada, Hernán; Mantilla, Ignacio; Roncancio, Weimar

    2013-01-01

    Se presenta un modelo matemático que permite estudiar dosde los fenómenos físicos que ocurren internamente en un pañal, como lo son el transporte de líquido en la celulosa y el intercambio de éste entre la celulosa y los gránulos. El desarrollo conduce a un sistema de ecuaciones diferenciales parciales, complementado con condiciones iniciales y de frontera.

  12. Geochemistry of low-temperature springs northwest of Yellowstone caldera: Seeking the link between seismicity, deformation, and fluid flow

    Science.gov (United States)

    Evans, William C.; Bergfeld, D.; van Soest, M.C.; Huebner, M.A.; Fitzpatrick, J.; Revesz, K.M.

    2006-01-01

    A comprehensive geochemical survey of springs outside the northwest margin of the Yellowstone caldera was undertaken in 2003 and 2004. This survey was designed to detect: (1) active leakage from a huge reservoir of CO2 gas recently postulated to extend from beneath the caldera into this area; and (2) lingering evidence for subsurface flow of magmatic fluids into this area during the 1985 seismic swarm and concomitant caldera subsidence. Spring temperatures are low (fluids through the caldera rim in this area.

  13. Long Valley Caldera 2003 through 2014: overview of low level unrest in the past decade

    Science.gov (United States)

    Wilkinson, Stuart K.; Hill, David P.; Langbein, John O.; Lisowski, Michael; Mangan, Margaret T.

    2014-01-01

    Long Valley Caldera is located in California along the eastern escarpment of the Sierra Nevada Range. The caldera formed about 760,000 years ago as the eruption of 600 km3 of rhyolite magma (Bishop Tuff) resulted in collapse of the partially evacuated magma chamber. Resurgent doming in the central part of the caldera occurred shortly afterwards, and the most recent eruptions inside the caldera occurred about 50,000 years ago. The caldera remains thermally active, with many hot springs and fumaroles, and has had significant deformation and seismicity since at least 1978. Periods of intense unrest in the 1980s to early 2000s are well documented in the literature (Hill and others, 2002; Ewert and others, 2010). In this poster, we extend the timeline forward, documenting seismicity and deformation over the past decade.

  14. Carbonatite ring-complexes explained by caldera-style volcanism

    OpenAIRE

    Andersson, Magnus; Malehmir, Alireza; Troll, Valentin R.; Dehghannejad, Mahdieh; Juhlin, Christopher; Ask, Maria

    2013-01-01

    Carbonatites are rare, carbonate-rich magmatic rocks that make up a minute portion of the crust only, yet they are of great relevance for our understanding of crustal and mantle processes. Although they occur in all continents and from Archaean to present, the deeper plumbing system of carbonatite ring-complexes is usually poorly constrained. Here, we show that carbonatite ring-complexes can be explained by caldera-style volcanism. Our geophysical investigation of the Alnö carbonatite ring-co...

  15. Sand Dunes Moving in the Nili Patera Caldera on Mars

    OpenAIRE

    Sparavigna, Amelia Carolina

    2013-01-01

    Recently, it was discovered that the sand dunes on Mars are moving. This important result was obtained by means of some high resolution HiRISE images, recorded three years apart, of the dunes in the Nili Patera caldera. Here we compare an image HiRISE of 2007 with an image of 1999 recorded by the Mars Global Surveyor. Using Gimp, a GNU image processing software, to enhance the images, we can see and measure the motion of the dunes during a longer period of time

  16. A multidisciplinary study of the 2014-2015 Bárðarbunga caldera collapse, Iceland

    Science.gov (United States)

    Tumi Gudmundsson, Magnus; Jonsdóttir, Kristin; Hooper, Andy; Holohan, Eoghan; Halldorsson, Saemundur

    2016-04-01

    The collapse of the ice-filled Bárðarbunga caldera in central Iceland occurred in autumn and winter, when weather was highly unsettled and conditions for monitoring in many ways difficult. Nevertheless several detailed time series could be obtained on the collapse and to a degree the associated flood-basalt eruption in Holuhraun. This was achieved through applying an array of sensors, that were ground, air and satellite based, partly made possible through the EU-funded FUTUREVOLC supersite project. This slow caldera collapse lasted six months, ending in February 2015. The array of sensors used, coupled with the long duration of the event, allowed unprecedented detail in observing a caldera collapse. The deciphering of the course of events required the use of aircraft altimeter surveys of the ice surface, seismic and GPS monitoring, the installation of a GPS station on the glacier surface in the centre of the caldera that continuously recorded the subsidence. Full Stokes 3-D modelling of the 700-800 m thick ice in the caldera, constrained by observations, was applied to remove the component of ice deformation that had a minor effect on the measured subsidence. The maximum subsidence of the subglacial caldera floor was about 65 meters. The combined interpretation of geochemical geobarometers, subsidence geometry with GPS and InSAR deformation signals, seismicity and distinct element deformation modelling of the subsidence provided unprecedented detail of the process and mechanism of caldera collapse. The collapse involved the re-activation of pre-existing ring faults, and was initiated a few days after magma started to drain from underneath the caldera towards the eventual eruption site in Holuhraun, 45 km to the northeast. The caldera collapse was slow and gradual, and the flow rate from underneath the caldera correlates well with the lava flow rate in Holuhraun, both in terms of total volume and variations in time.

  17. A tectonic model of the Askja caldera system based on FEM analysis

    Science.gov (United States)

    Browning, John; Gudmundsson, Agust; Thordarson, Thorvaldur

    2015-04-01

    The Askja volcanic system lies on the boundary between the Eurasian and North American tectonic plates and is an example of a multiple caldera formed in an extensional regime. Askja is composed of at least three calderas, the last of which formed during an explosive eruption in A.D. 1875. The caldera floor has been subsiding almost continuously since 1983; total subsidence in this period is around 1.1 metres. Perhaps surprisingly, there has been no slip or movement on the caldera bounding ring-faults during this subsidence period. Various models have been proposed to explain this unusual signal. Previous models suggest two magma sources, one shallow at around 3 km depth and one much larger at around 16 km depth. In this model, subsidence is caused by depressurisation in both sources as a result of cooling contraction and crystallisation. In other models subsidence results from magma being squeezed out of the shallow chamber laterally; or somehow draining back into a deep seated reservoir. In this study we examine the contribution of regional extension and structural discontinuities to the current subsidence of Askja caldera. Using a finite element numerical analysis, we ascertain the state of stresses at Askja caldera over time based on several different magma body geometries. We calculate surface displacements expected from extension around a shallow magma body, and place these findings in the context of Icelandic calderas. In addition we investigate the likely stress effects of the Askja caldera on the associated part of the Northern Volcanic Zone. The proposed model seeks to understand the volcano-tectonic conditions at Askja during caldera formation, as well as during rifting episodes. The models presented will be useful in assessing likely future rifting events and fissure swarm activity in Askja caldera, and neighbouring volcanoes.

  18. Fuel oil-water emulsions to reduce unburned particle emissions from boilers; Emulsiones agua en combustoleo para reducir las emisiones de particulas inquemadas en calderas

    Energy Technology Data Exchange (ETDEWEB)

    Diego Marin, Antonio; Ocampo Barrera, Rene; Martinez Flores, Marco Antonio; Tamayo Flores, Gustavo Adolfo; Alarcon Quiroz, Ernesto [Instituto de Investigaciones Electricas, Cuernavaca (Mexico)

    1997-12-31

    To diminish the problems caused by fuels in boilers such as abnormal soiling of heat interchange surfaces, decrease of thermal and combustion efficiencies and increment of pollutants it is proposed the utilization of fuel oil water emulsions. This technology process is described, its development and application in other countries is shown and mention is made of the experiences in this regard at the Instituto de Investigaciones Electricas (IIE), as well as the perspectives this technology has in Mexico. In conclusion, the fuel oil water emulsion is an alternative that can help burning efficiently the fuel oil and so to contribute to fulfill with the limits established by the environmental regulations on pollutant emissions. The development of this technology is economical and of simple application, compared with others, such as the installation of new burners, the utilization of a commercial technology for flue gas conditioning, etcetera [Espanol] Para disminuir los problemas ocacionados por el combustoleo en las calderas como: ensuciamientos anormales de las superficies de intercambio de calor, disminucion de eficiencias termicas y de combustion e incremento de las emisiones, se propone la utilizacion de la emulsion de agua en combustoleo. Se describe el proceso de esta tecnologia, se muestra su desarrollo y aplicacion en otros paises y se mencionan las experiencias a este respecto en el Instituto de Investigaciones Electricas (IIE), asi como las perspectivas que tiene esta tecnologia en Mexico. En conclusion, la emulsion de agua en combustoleo es una alternativa que puede ayudar a quemar eficientemente al combustoleo y asi contribuir a cumplir con los limites de emisiones que establecen normas ambientales. El desarrollo de esta tecnologia es economica y de aplicacion sencilla, comparada con otras como: la instalacion de nuevos quemadores, la utilizacion de una tecnologia comercial para acondicionar los gases de combustion, etcetera

  19. Desarrollo de un nuevo tratamiento para la conservación de piedras con alto contenido en carbonatos utilizando la Tecnología de Resinas de Intercambio Iónico

    OpenAIRE

    Pérez-Alonso, M; K. Castro; Rodriguez-Laso, María D.; Madariaga, J.M.

    2003-01-01

    Atmospheric contamination is the main cause of erosion of stone in urban monuments. Gas emissions produce a gradual acidification in the environment, reducing the resistance of all types of stone. Stones with high CaCO3 content (limestone, carbonated marble and sandstone) are those most affected by acid rain. Numerous studies into the influence of calcium oxalate on calcareous stones conclude that this compound, produced naturally from certain lichens, can act as protection against acid. Calc...

  20. Physical volcanology of the mafic segment of the subaqueous New Senator caldera, Abitibi greenstone belt, Quebec, Canada

    Energy Technology Data Exchange (ETDEWEB)

    Moore, Lyndsay N; Mueller, Wulf U [Universite du Quebec a Chicoutimi, 555 boul. du l' Universite, Chicoutimi, Quebec, G7H2B1 (Canada)], E-mail: lyndsay.moore@uqac.ca

    2008-10-01

    Archean calderas provide valuable insight into internal geometries of subaqueous calderas. The New Senator caldera, Abitibi greenstone belt, Canada, is an Archean example of a subaqueous nested caldera with a basal stratigraphy dominated by gabbro-diorite dykes and sills, ponded magmas and basalt and andesite lava flows. The aim of our study is to focus on the use of physical volcanology to differentiate between the various mafic units found at the base of the New Senator caldera. Differentiation between these various mafic units is important from an exploration point of view because in modern subaqueous summit calders (e.g. Axial Seamount) margins of ponded magmas are often sites of VMS formation.

  1. Radon in groundwater of the Long Valley Caldera, California

    International Nuclear Information System (INIS)

    In the Long Valley caldera, an area of recently (∼550 y) active volcanism and current seismic activity, 222Rn concentrations in hot, warm, and cold spring waters have been measured since 1982. Rn contents of the waters correlate inversely with temperature and specific conductance, with high concentrations (1500 to 2500 pCi/l) occurring in dilute cold springs on the margins of the caldera, and low concentrations (12 to 25 pCi/l) in hot to boiling springs. Rn correlates only slightly with the uranium contents of the wide range of rocks which host the hydrological system feeding the springs. These environmental effects on the radon record may mask responses to small or distant seismic, volcanic, or crustal deformation events. To date, anomalous changes in water-borne Rn have been observed in connection with at least one earthquake, which occurred close to the monitoring site. This continuing study points out that an understanding of the geological setting, its associated hydrological system, and environmental influences is necessary to properly evaluate concentrations and changes in groundwater radioactivity

  2. Sheet flow caves of Kilauea Caldera, Hawaii County, Hawaii

    Directory of Open Access Journals (Sweden)

    William R. Halliday

    1998-01-01

    Full Text Available Terminal lobes of sheet flows of pahoehoe lava sometimes form three-dimensional nests, initially separated by partitions consisting of accreted ‘skins” of each lobe. Melting breaks down these partitions, forming a uniform flow unit. In Kilauea Caldera we have found and mapped sizable drained cavities in low-slope sheet flows. Their general pattern includes three-dimensional nests, with partially melted septa evident in some examples. Christmas Cave is the most extensive found to date, with 632 meters surveyed on two levels. It is located at the lower end of an inflated sheet flow tongue which underwent local deflation as a result of drainage through the cave after its parameters were partially fixed. Small conduit remnants persist in its boundary ridges. The major part of the cave consists of wide, low nestled chambers. Meltdown of such partitions is one of the few emplacement mechanisms of thermal erosion which may not involve any mechanical element. Additional caves in this caldera are being identified and studied.

  3. Renewed inflation of Long Valley Caldera, California (2011 to 2014)

    Science.gov (United States)

    Montgomery-Brown, Emily; Wicks, Chuck; Cervelli, Peter F.; Langbein, John O.; Svarc, Jerry L.; Shelly, David R.; Hill, David P.; Lisowski, Michael

    2015-01-01

    Slow inflation began at Long Valley Caldera in late 2011, coinciding with renewed swarm seismicity. Ongoing deformation is concentrated within the caldera. We analyze this deformation using a combination of GPS and InSAR (TerraSAR-X) data processed with a persistent scatterer technique. The extension rate of the dome-crossing baseline during this episode (CA99 to KRAC) is 1 cm/yr, similar to past inflation episodes (1990–1995 and 2002–2003), and about a tenth of the peak rate observed during the 1997 unrest. The current deformation is well modeled by the inflation of a prolate spheroidal magma reservoir ∼7 km beneath the resurgent dome, with a volume change of ∼6 × 106 m3/yr from 2011.7 through the end of 2014. The current data cannot resolve a second source, which was required to model the 1997 episode. This source appears to be in the same region as previous inflation episodes, suggesting a persistent reservoir.

  4. Months between rejuvenation and volcanic eruption at Yellowstone caldera, Wyoming

    Science.gov (United States)

    Till, Christy B.; Vazquez, Jorge A.; Boyce, Jeremy W

    2015-01-01

    Rejuvenation of previously intruded silicic magma is an important process leading to effusive rhyolite, which is the most common product of volcanism at calderas with protracted histories of eruption and unrest such as Yellowstone, Long Valley, and Valles, USA. Although orders of magnitude smaller in volume than rare caldera-forming super-eruptions, these relatively frequent effusions of rhyolite are comparable to the largest eruptions of the 20th century and pose a considerable volcanic hazard. However, the physical pathway from rejuvenation to eruption of silicic magma is unclear particularly because the time between reheating of a subvolcanic intrusion and eruption is poorly quantified. This study uses geospeedometry of trace element profiles with nanometer resolution in sanidine crystals to reveal that Yellowstone’s most recent volcanic cycle began when remobilization of a near- or sub-solidus silicic magma occurred less than 10 months prior to eruption, following a 220,000 year period of volcanic repose. Our results reveal a geologically rapid timescale for rejuvenation and effusion of ~3 km3 of high-silica rhyolite lava even after protracted cooling of the subvolcanic system, which is consistent with recent physical modeling that predict a timescale of several years or less. Future renewal of rhyolitic volcanism at Yellowstone is likely to require an energetic intrusion of mafic or silicic magma into the shallow subvolcanic reservoir and could rapidly generate an eruptible rhyolite on timescales similar to those documented here.

  5. Intercambio, novedad y estrategias: las misiones jesuíticas del sur desde la perspectiva indígena

    Directory of Open Access Journals (Sweden)

    María Paula Irurtia

    2007-07-01

    Full Text Available En este trabajo propongo abordar la cuestión de la visión de los indios acerca de la presencia de misiones jesuíticas en territorios al sur de la frontera representada por el río Salado en el actual territorio de la provincia de Buenos Aires. Ante el establecimiento de las misiones los indígenas de la región mostraron diversos tipos de reacciones entre la aceptación y el rechazo según distintos intereses. Entre los grupos que aceptaban y los que rechazaron las misiones no puede establecerse una clara delimitación dados los profusos vínculos entre ambos y el valor estratégico de las diferentes actitudes. Los contactos de los indios con las misiones parecen enmarcarse dentro de los sistemas de intercambio, territoriales y de relaciones interétnicas, mientras que a medida que tenían lugar las interacciones se fueron conformando un particular modo de relación y una determinada visión respecto del otro.This paper is about the Indian perspective concerning the presence of Jesuit missions in the south of the Salado river in the present territory of the State of Buenos Aires. With the settlement of the missions the Indigenous showed different kind of reactions from acceptance to repelling according to different interests. It is not possible to differentiate between the groups that accepted and those which repelled the missions because of the profuse ties among them and the strategic value of the different positions. The Indian contacts with the missions seem to be part of the systems of barter, territory and interethnic relations whereas as the interactions took place a particular form of relationship and a certain vision about the other were shaping.

  6. Recuperación de oro desde un medio amoniaco-tiosulfato con resina de intercambio iónico Amberlite IRA-410

    Directory of Open Access Journals (Sweden)

    Navarro, P.

    2006-10-01

    Full Text Available The adsorption and elution of gold in thiosulfate-ammonia media were studied at laboratory level using the Amberlite IRA-410 ionic exchange resin. Tests were carried out in a stirred reactor, maintaining constant temperature (25 ºC, with a volume of solution/mass of resin ratio of 833,3 ml/g and during 3 h. The variables tested were the following: pH (9-11, thiosulfate concentration (0-0,5 M, ammonia concentration (0-0,5 M and selectivity in the presence of cupric ion. The obtained results indicate that gold adsorption was quick; the presence of thiosulfate decreased strongly the adsorption; and the presence of ammonia did not affect the adsorption mostly. The copper was in a certain measure a competitor of the gold, but its biggest negative effect was that acted as catalyst of the oxidizing reaction of thiosulfate (S2O3 2– to tetrathionate (S4O6 2– and trithionate (S3O6 2–, which can cause a partial elution of gold during the load stage. Also, the behavior of ClO– 4, SO3 2– and ClO– as eluents was studied in both gold and copper elution. These tests were also carried out in a stirred reactor, to constant temperature (25 ºC, with a volume of aqueous solution/mass of resin ratio of 200 ml/g and for 3 h. Results demonstrated that the copper was eluted more quickly that the gold in all the cases.

    Se estudió, a nivel de laboratorio, la adsorción y desorción de oro utilizando la resina de intercambio iónico Amberlite IRA-410 en medio tiosulfato-amoniaco. Los ensayos se realizaron en un reactor agitado, manteniendo constante la temperatura en 25 ºC y con una razón volumen de disolución/masa de resina de 833,3 ml/g durante 3 h. Las variables evaluadas fueron las siguientes: pH de 9 a 11, concentración de tiosulfato de 0 a 0,5 M, concentración de amoniaco de 0 a 0,5 M y selectividad frente al i

  7. Radiometric Dating of tephras from Pre-caldera and Caldera-forming stages, Towada volcano, Northeast Japan

    International Nuclear Information System (INIS)

    Towada volcano is an active volcano located in the northern part of the Northeast Japan arc. We carried out fission-track (FT) and AMS radiocarbon (14C) dating of tephras from Towada and Hakkoda volcanoes to establish a detailed eruptive history during the Pre-caldera and Caldera-forming stages of Towada volcano. The obtained FT ages were 0.23 ± 0.05 Ma for Shirobeta tephra (WP), 0.19 ± 0.05 Ma for T-6 tephra, 0.08 ± 0.03 Ma for Zarame 1 tephra (ZP1), and 0.09 ± 0.03 Ma for Okuse Pyroclastic Flow Deposits. Although these FT ages are consistent with stratigraphy, they have large error ranges of several tens of thousands of years. Therefore, further examinations including application of other chronological dating methods are necessary to obtain more precise estimates of the eruptive age of these tephras. The obtained 14C age was 17,730 ± 70 BP for Biscuit 2 tephra (BP2). Based on stratigraphical consistency, this 14C age is appropriate for the eruptive age of BP2. (author)

  8. Subsurface architecture of a strike-slip collapse structure: insights from Ilopango caldera, El Salvador

    Science.gov (United States)

    Saxby, Jennifer; Gottsmann, Joachim; Cashman, Katherine; Gutierrez, Eduardo

    2016-04-01

    While most calderas are created by roof collapse along ring-like faults into an emptying magma reservoir during a large and violent explosive eruption, an additional condition for caldera formation may be tectonically induced extensional stresses. Here we provide geophysical insights into the shallow sub-volcanic plumbing system of a collapse caldera in a major strike-slip tectonic setting by inverting Bouguer gravity data from the Ilopango caldera in El Salvador. Despite a long history of catastrophic eruptions with the most recent in 500 A.D., the internal architecture of the caldera has not been investigated, although studies of the most recent eruption have not identified the ring faults commonly associated with caldera collapse. The gravity data show that low-density material aligned along the principal stress orientations of the El Salvador Fault Zone (ESFZ) forms a pronounced gravity low beneath the caldera. Extending to around 6 km depth, the low density structure likely maps a complex stacked shallow plumbing system composed of magmatic and fractured hydrothermal reservoirs. A substantial volume of the plumbing system must be composed of a vapour phase to explain the modeled negative density contrasts. We use these constraints to map the possible multi-phase parameter space contributing to the subsurface architecture of the caldera and propose that the local extension along the complex ESFZ controls accumulation, ascent and eruption of magma at Ilopango. The data further suggest that future eruptions at Ilopango could be facilitated by rapid rise of magma along conjugate fault damage zones through a mechanically weak crust under tension. This may explain the absence of clear ring fault structures at the caldera.

  9. An overview of the Valles Caldera National Preserve: the natural and cultural resources

    Science.gov (United States)

    Parmenter, Robert R.; Steffen, Anastasia; Allen, Craig D.

    2007-01-01

    The Valles Caldera National Preserve is one of New Mexico’s natural wonders and a popular area for public recreation, sustainable natural resource production, and scientific research and education. Here, we provide a concise overview of the natural and cultural history of the Preserve, including descriptions of the ecosystems, flora and fauna. We note that, at the landscape scale, the Valles caldera appears to be spectacularly pristine; however, humans have extracted resources from the Preserve area for many centuries, resulting in localized impacts to forests, grasslands and watersheds. The Valles Caldera Trust is now charged with managing the Preserve and providing public access, while preserving and restoring these valuable public resources.

  10. Demanda externa, términos de intercambio y el papel de la política monetaria durante la crisis de 2008

    OpenAIRE

    Johana Maritsa Hernández Henao

    2013-01-01

    Esta investigación tiene como propósito investigar la respuesta de la economía colombiana frente a un choque a los términos de intercambio y una caída en la demanda de exportaciones. Asimismo, se está interesado en dilucidar el papel que desempeña la autoridad monetaria en presencia de dichos choques. Para tal fin, se calibra un modelo de equilibrio general dinámico y estocástico para una economía pequeña y abierta. El comportamiento del banco central se modela mediante dos reglas de interés ...

  11. Transporte cuántico en grafeno: interacción dinámica de intercambio y estados cuasi-unidimensionales estacionarios

    OpenAIRE

    Yaro Medina, Simeón Moisés

    2014-01-01

    Esta tesis doctoral versa sobre el transporte electrónico en sistemas de baja dimensión. En particular, se utlizan diferentes formalismos para abordar fenómenos cuánticos en el transporte electrónico en grafeno. Por una parte, se estudia la interacción de intercambio en los procesos de transporte electrónico dependientes del tiempo, mediante la teoría de trayectorias Bohmianas para paquetes de ondas. Se demuestra que la densidad de estados en el espacio de fases puede entenders...

  12. Modelando el cortejo humano: negociación e intercambio en las relaciones de pareja desde la perspectiva de la sociología económica

    OpenAIRE

    Antonio Villalpando Acuña

    2012-01-01

    Las interacciones de los grupos primarios y la dinámica del emparejamiento son temas recurrentes en la sociología económica. No obstante, los trabajos dedicados a analizar las interacciones involucradas en el cortejo humano siguen siendo territorio de la antropología y de la biología evolutiva. En el presente trabajo se explora el contexto en el que se desempeña la sociología económica, haciendo hincapié en la Teoría del Intercambio Social. También se discute sobre la necesidad de una teoría ...

  13. Recordatorio para mejorar el intercambio en las listas profesionales de Veterinaria.org y hacer mejor uso de los boletines informativos

    Directory of Open Access Journals (Sweden)

    Veterinaria.org

    2008-02-01

    Full Text Available ResumenRecordar que los mensajes se deberían enviar a la lista más adecuada, así por ejemplo los casos clínicos específicos a L_Cons, los de temas profesionales generales a L_VET, los de asuntos informales a L_SOCIAL, etc, y no utilizar para ello los boletines, que están destinados para otro uso. Las especificaciones de cada lista de intercambio y boletines informativos están en http://www.veterinaria.org/listasyboletines

  14. Perspectivas de integración energética México- norteamericana: Intercambios de electricidad y gas natural en el noroeste mexicano

    Directory of Open Access Journals (Sweden)

    Agustín Sández Pérez

    1992-09-01

    Full Text Available Históricamente, la relación comercial México-norteamericana en el plano energético ha sido hegemonizada por el intercambio de hidrocarburos. En épocas de conflagración mundial, y más recientemente de conflictos bélicos en el Medio Oriente, el acceso preferencial a este recurso ha representado un factor importante de tensión para México. Fuera de las etapas de tensión, tal intercambio continúa siendo eje de la negociación comercial y aún más lejos, ha llegado a ocupar en algunos periodos un rol clave en la planeación económica global de la nación. Esta relación abrumadora, que parece privilegiar a toda costa el examen del intercambio petrolero en la relación comercial bilateral es, en cambio, ajena y distante al panorama social y productivo de la frontera norte y muy especialmente del noroeste mexicano. En éste, el intercambio energético se circunscribe hoya la venta de electricidad hacia el norte y la venta de gas natural hacia el sur de la frontera entre ambos países. El seguimiento de los circuitos eléctricos interconectados entre Baja California y California es un proceso relativamente reciente. Hacia mediados de los ochenta se realizaron las negociaciones entre autoridades y representantes de ambos países. Esta negociación reflejó, a su vez, la disparidad organizacional de la producción eléctrica. Más recientemente se han establecido programas y políticas destinadas al uso eficiente de la energía. A la vez se presencian procesos paralelos de gran trascendencia. Una de las alternativas que se discuten hoy para el abatimiento de costos de producción es la utilización del gas natural como alimento de la termoelectricidad a fin de sostener la capacidad instalada y asegurar la exportación.

  15. Modelamiento y análisis del transporte de iones a través de membranas de intercambio aniónico usadas en celdas de combustible

    OpenAIRE

    Castañeda Ramírez, Sergio

    2012-01-01

    Se derivó un modelo para membranas de intercambio aniónico usadas en celdas de combustible alcalinas basado en la teoría de termodinámica de procesos irreversibles. Las pruebas llevadas a cabo en un modelo simplificado de celda de combustible incluyeron combinaciones de condiciones de operación tales como humedad relativa de los gases de alimento, presión en los electrodos y densidad de corriente. En general, el modelo de la membrana representó bien los diferentes modos de transporte que pued...

  16. Un final abierto: circulación, colaboración e intercambio en las prácticas sonoras independientes a través de Internet

    Directory of Open Access Journals (Sweden)

    Ana María Romano G.

    2015-09-01

    Internet se ha constituido en un entorno en el que pueden confluir almacenamiento, difusión y distribución, por ello es fácil entender que goce de gran aceptación, pues día a día se fortalece como una tecnología que favorece  el intercambio y la colaboración musical. Internet, el gran aliado de las iniciativas independientes, ha ayudado a que lleguen a diversos públicos, muchas veces insospechados, y ha dado lugar a un empoderamiento sorprendente de los movimientos que reivindican la autogestión.

  17. Closing crack earthquakes within the Krafla caldera, North Iceland

    Science.gov (United States)

    Mildon, Zoë K.; Pugh, David J.; Tarasewicz, Jon; White, Robert S.; Brandsdóttir, Bryndís

    2016-11-01

    Moment tensor analysis with a Bayesian approach was used to analyse a non-double-couple (non-DC) earthquake (Mw ˜ 1) with a high isotropic (implosive) component within the Krafla caldera, Iceland. We deduce that the earthquake was generated by a closing crack at depth. The event is well located, with high signal-to-noise ratio and shows dilatational P-wave first arrivals at all stations where the first arrival can be picked with confidence. Coverage of the focal sphere is comprehensive and the source mechanism stable across the full range of uncertainties. The non-DC event lies within a cluster of microseismic activity including many DC events. Hence, we conclude that it is a true non-DC closing crack earthquake as a result of geothermal utilization and observed magma chamber deflation in the region at present.

  18. Oblique synoptic images, produced from digital data, display strong evidence of a "new" caldera in southwestern Guatemala

    Science.gov (United States)

    Duffield, W.; Heiken, G.; Foley, D.; McEwen, A.

    1993-01-01

    The synoptic view of broad regions of the Earth's surface as displayed in Landsat and other satellite images has greatly aided in the recognition of calderas, ignimbrite plateaus and other geologic landforms. Remote-sensing images that include visual representation of depth are an even more powerful tool for geologic interpretation of landscapes, but their use has been largely restricted to the exploration of planets other than Earth. By combining Landsat images with digitized topography, we have generated regional oblique views that display compelling evidence for a previously undocumented late-Cenozoic caldera within the active volcanic zone of southwestern Guatemala. This "new" caldera, herein called Xela, is a depression about 30 km wide and 400-600 m deep, which includes the Quezaltenango basin. The caldera depression is breached only by a single river canyon. The caldera outline is broadly circular, but a locally scalloped form suggests the occurrence of multiple caldera-collapse events, or local slumping of steep caldera walls, or both. Within its northern part, Xela caldera contains a toreva block, about 500 m high and 2 km long, that may be incompletely foundered pre-caldera bedrock. Xela contains several post-caldera volcanoes, some of which are active. A Bouguer gravity low, tens of milligals in amplitude, is approximately co-located with the proposed caldera. The oblique images also display an extensive plateau that dips about 2?? away from the north margin of Xela caldera. We interpret this landform to be underlain by pyroclastic outflow from Xela and nearby Atitla??n calderas. Field mapping by others has documented a voluminous rhyolitic pumiceous fallout deposit immediately east of Xela caldera. We speculate that Xela caldera was the source of this deposit. If so, the age of at least part of the caldera is between about 84 ka and 126 ka, the ages of deposits that stratigraphically bracket this fallout. Most of the floor of Xela caldera is covered

  19. Maars to calderas: end-members on a spectrum of explosive volcanic depressions

    Directory of Open Access Journals (Sweden)

    Danilo M. Palladino

    2015-07-01

    Full Text Available We discuss maar-diatremes and calderas as end-members on a spectrum of negative volcanic landforms (depressions produced by explosive eruptions (note – we focus on calderas formed during explosive eruptions, recognizing that some caldera types are not related to such activity. The former are dominated by ejection of material during numerous discrete phreatomagmatic explosions, brecciation, and subsidence of diatreme fill, while the latter are dominated by subsidence over a partly evacuated magma chamber during sustained, magmatic volatile-driven discharge. Many examples share characteristics of both, including landforms that are identified as maars but preserve deposits from non-phreatomagmatic explosive activity, and ambiguous structures that appear to be coalesced maars but that also produced sustained explosive eruptions with likely magma reservoir subsidence. A convergence of research directions on issues related to magma-water interaction and shallow reservoir mechanics is an important avenue toward developing a unified picture of the maar-diatreme-caldera spectrum.

  20. Field trip guide to the Valles Caldera and its geothermal systems

    Energy Technology Data Exchange (ETDEWEB)

    Goff, F.E.; Bolivar, S.L.

    1983-12-01

    This field trip guide has been compiled from extensive field trips led at Los Alamos National Laboratory during the past six years. The original version of this guide was designed to augment a workshop on the Valles Caldera for the Continental Scientific Drilling Program (CSDP). This workshop was held at Los Alamos, New Mexico, 5-7 October 1982. More stops were added to this guide to display the volcanic and geothermal features at the Valles Caldera. The trip covers about 90 miles (one way) and takes two days to complete; however, those who wish to compress the trip into one day are advised to use the designated stops listed in the Introduction. Valles Caldera and vicinity comprise both one of the most exciting geothermal areas in the United States and one of the best preserved Quaternary caldera complexes in the world.

  1. Proceedings of the second workshop on hydrologic and geochemical monitoring in the Long Valley Caldera

    Energy Technology Data Exchange (ETDEWEB)

    Sorey, M.L.; Farrar, C.D.; Wollenberg, H.A. (eds.)

    1986-12-01

    A workshop was held to review the results of hydrologic and geochemical monitoring and scientific drilling in the Long Valley caldera. Such monitoring is being done to detect changes in the hydrothermal system induced by ongoing magmatic and techonic processes. Data from a 2400-ft deep core hole completed in June 1986 were presented at the 1986 workshop and participants discussed the need and rationale for siting locations for future scientific drilling in the caldera.

  2. Dynamics and structural evolution of collapse calderas: A comparison between field evidence, analogue and mathematical models

    OpenAIRE

    Geyer Traver, Adelina

    2007-01-01

    Collapse calderas are defined as the volcanic depression that result from the disruption of the geometry of the magma chamber roof due to down faulting during the course of an eruption. These structures have received considerable attention due to their link to Earth's ore deposits and geothermal energy resources, but also because large pyroclastic eruptions and associated caldera collapse structures represent one of the most catastrophic geologic events that have occurred on the Earth's surfa...

  3. How caldera collapse shapes the shallow emplacement and transfer of magma in active volcanoes

    Science.gov (United States)

    Corbi, Fabio; Rivalta, Eleonora; Pinel, Virginie; Maccaferri, Francesco; Bagnardi, Marco; Acocella, Valerio

    2016-04-01

    Calderas are topographic depressions formed by the collapse of a partly drained magma reservoir. At volcanic edifices with calderas, eruptive fissures can circumscribe the outer caldera rim, be oriented radially and/or align with the regional tectonic stress field. Constraining the mechanisms that govern this spatial arrangement is fundamental to understand the dynamics of shallow magma storage and transport and evaluate volcanic hazard. Here we use numerical models to show that the previously unappreciated unloading effect of caldera formation may contribute significantly to the stress budget of a volcano. We first test this hypothesis against the ideal case of Fernandina, Galápagos, where previous models only partly explained the peculiar pattern of circumferential and radial eruptive fissures and the geometry of the intrusions determined by inverting the deformation data. We show that by taking into account the decompression due to the caldera formation, the modeled edifice stress field is consistent with all the observation. We then develop a general model for the stress state at volcanic edifices with calderas based on the competition of caldera decompression, magma buoyancy forces and tectonic stresses. These factors control the shallow accumulation of magma in stacked sills, consistently with observations as well as the conditions for the development of circumferential and/or radial eruptive fissures, as observed on active volcanoes. This top-down control exerted by changes in the distribution of mass at the surface allows better understanding of how shallow magma is transferred at active calderas, contributing to forecasting the location and type of opening fissures.

  4. Conduit enlargement during the precursory Plinian eruption of Aira Caldera, Japan

    Science.gov (United States)

    Geshi, Nobuo; Miyabuchi, Yasuo

    2016-09-01

    Increase in magma flux as the result of conduit enlargement is one of the key processes that triggered caldera collapse and eruption of the Ito ignimbrite from Aira Caldera at ~29 ka. We examine the total volume of the pumice fall deposit, vertical variations in grain size of pumice, and the lithic content in the Osumi pumice deposit to investigate the trigger for caldera collapse. Wider distribution of the later-stage unit and the upward coarsening of grain size throughout the Osumi pumice fall deposit indicate an increase in magma discharge toward the onset of collapse. The total volume of lithic fragments in the Osumi pumice fall deposit is estimated as ~1.6 km3, based on the lithic content in several representative outcrops and the total volume of the Osumi pumice fall deposit. The lithic fragments in the Osumi pumice fall deposit indicate intense mechanical erosion of the conduit during the Plinian eruption prior to caldera collapse. Caldera collapse requires decompression of the magma chamber by withdrawal of magma; effective enlargement of the conduit diameter during precursory eruptive phases is one of the important processes that subsequently allow the rapid discharge of a large volume of magma, which in turn facilitates decompression of the reservoir and induces caldera collapse.

  5. Catastrophic isotopic modification of rhyolitic magma at times of caldera subsidence, Yellowstone plateau volcanic field.

    Science.gov (United States)

    Hildreth, W.; Christiansen, R.L.; O'Neil, J.R.

    1984-01-01

    This Wyoming volcanic field has undergone repeated eruption of rhyolitic magma strongly depleted in 18O. Large calderas subsided 2.0, 1.3 and 0.6 m.y. ago on eruption of ash-flow sheets. More than 60 other rhyolite lavas and tuffs permit reconstruction of the long-term chemical and isotopic evolution of the silicic system. Narrow delta 18O ranges in the ash-flow sheets contrast with wide delta 18O variation in post-caldera lavas. The earliest post-collapse lavas are 3-6per mille lighter than the preceding ash-flow sheets. The 18O depletions were short-lived events that immediately followed caldera subsidence and sequences of post-caldera lavas record partial recovery toward pre-caldera delta 18O values. Contemporaneous extra-caldera rhyolites show no effects of the repeated depletions. Although some contamination by foundering roof rocks seems to be required, water was probably the predominant contaminant.-W.H.B.

  6. Taupo in time and space: dynamics of a rhyolitic caldera volcano and its magmatic system

    Science.gov (United States)

    Wilson, C. J.; Allan, A. S.; Barker, S. J.; Morgan, D. J.; Charlier, B. L.; Baker, J. A.; Wooden, J. L.

    2012-12-01

    Traditional views see the caldera-forming event as the eruptive career pinnacle of any aspiring large silicic magma system, around which perspectives focus in 'pre-', syn-' and 'post-caldera' groupings of eruptions. Important question arising from such notions are: (1) Is the caldera-forming eruption a freak event, reflecting unusual circumstances, or does it represent a stochastic extreme on a continuously evolving record? (2) How rapidly does the melt-dominant large magma body accumulate? (3) What are the recovery/renewal processes and timings after a caldera-forming eruption? (4) What hangover from the main event is seen in behaviour of the 'post-caldera' system? The central Taupo Volcanic Zone (New Zealand) is a valuable area in which to test models for large silicic systems because of its rapid frequency of moderate to large sizes of its eruptions over the past ~1.6 Ma. Here we review the eruptive record for Taupo volcano itself over the last 50,000 years, highlighting old and new results that detail its evolution over that period, during which the 25.4 ka, ~530 cubic km Oruanui event formed the main caldera-related eruption. In the Taupo area, erupting at vents hangover reflected in the modern system, despite the geographic superposition of vent sites.

  7. Eficiencia en la prescripción de medicamentos: impacto de un programa de intercambio terapéutico The efficiency of drug prescription: impact of a therapeutic exchange program

    OpenAIRE

    Isabel Rosich; Alejandro Allepuz; Glòria Alba; Núria Benages; Teresa Arranz

    2012-01-01

    Objetivo: Evaluar el impacto de un programa de intercambio terapéutico a omeprazol de los inhibidores de la bomba de protones (IBP). Método: Ensayo comunitario que compara el impacto de un programa de intercambio terapéutico en los equipos de atención primaria de una comarca respecto a la no aplicación en una comarca control. Se incluyó a los pacientes con prescripción de un IBP entre mayo de 2008 y junio de 2009. La intervención consistió en sesiones educativas y facilitar a cada médico (n=6...

  8. The confirmation of a work hypothesis: a new caldera in the center of the Mexican Volcanic Belt; La confirmacion de una hipotesis de trabajo: una nueva caldera en el centro del Cinturon Volcanico Mexicano

    Energy Technology Data Exchange (ETDEWEB)

    Anguita Virella, Francisco; Pal Verma, Surendra; Milan, Marcos; Garcia Cacho, Luis; Samaniego M, Daniel [Instituto de Investigaciones Electricas, Cuernavaca (Mexico)

    1991-12-31

    After synthesizing the most relevant aspects of the current volcanology and the genesis process of the collapse calderas, a process is described on the location and confirmation of a new caldera (the Mazahua) in the central part of the Mexican Volcanic Belt (MVB). [Espanol] Tras sintetizar los aspectos mas destacados de la vulcanologia actual y el proceso de genesis de las calderas de colapso, se describe el proceso de localizacion y confirmacion de una nueva caldera (la Mazahua) en la parte central del Cinturon Volcanico Mexicano (CVM).

  9. Explosive eruptions during the first 100-150 years of Kilauea's caldera

    Science.gov (United States)

    Swanson, D. A.

    2007-12-01

    The collapse of Kilauea's summit to form its modern caldera took place in 1480-1500 C.E. and was apparently almost nonexplosive. Only a layer of medium-coarse ash 1-4 cm thick at the base of the Keanakako`i Ash can reasonably be ascribed to the collapse itself. Soon thereafter, however, lava fountains probably much higher than 300 m played from multiple vents in the caldera, depositing a layer of nearly pure reticulite as thick as 65 cm on the rim. Multiple fountains, possibly from fractures bounding the collapsed blocks, best explain lateral changes in texture and componentry of the reticulite and its presence completely around the caldera. High fountains, related to high ascent rate, are required for reticulite production (Rust and Cashman, 2006). A paucity of denser material (pumice, Pele's tears) in the reticulite deposit indicates that only the top of the fountains cleared the caldera rim, with denser fallout trapped within the caldera. Thus the caldera was already several hundred meters deep when the reticulite erupted (about 1500 C.E., according to C-14 ages.) A lithic block fall and associated ash fall or surge, with subordinate vitric components, occurred soon (a few weeks to years?) after the reticulite eruption. This deposit occurs beyond the northern and northeastern rim of the caldera and is thickest and coarsest in the national park's housing area, where it contains clasts several tens of centimeters across. The block fall and ash are both pale pink, indicative of a dry, high temperature eruption. For the next 100-150 years, numerous small eruptions produced vitric ash containing several percent of lithic clasts in all grain sizes greater than 0.5 mm. The mixed deposits are dominated by poorly vesicular ash, have only small amounts of pumice, contain chunks of black glass with planar to gently concave surfaces, and commonly are somewhat palagonitized. Together, these features indicate that the explosions were phreatomagmatic, a conclusion also reached

  10. The Tala Tuff, La Primavera caldera Mexico. Pre-eruptive conditions and magma processes before eruption

    Science.gov (United States)

    Sosa-Ceballos, G.

    2015-12-01

    La Primavera caldera, Jalisco Mexico, is a Pleistocenic volcanic structure formed by dome complexes and multiple pyroclastic flows and fall deposits. It is located at the intersection of the Chapala, Colima, and Tepic grabens in western Mexico. The first volcanic activity associated to La Primavera started ~0.1 Ma with the emission of pre-caldera lavas. The caldera collapse occurred 95 ka and is associated to the eruption of ~20 km3of pumice flows known as the Tala tuff (Mahood 1980). The border of the caldera was replaced by a series of domes dated in 75-30 ky, which partially filled the inner depression of the caldera with pyroclastic flows and falls. For more than a decade the Federal Commission of Electricity in Mexico (CFE) has prospected and evaluated the geothermal potential of the Cerritos Colorados project at La Primavera caldera. In order to better understand the plumbing system that tapped the Tala tuff and to investigate its relation with the potential geothermal field at La Primavera we performed a series of hydrothermal experiments and studied melt inclusions hosted in quartz phenocrysts by Fourier Infra red stectroscopy (FTIR). Although some post caldera products at La Primavera contain fayalite and quartz (suggesting QFM conditions) the Tala tuff does not contain fayalite and we ran experiments under NNO conditions. The absence of titanomagnetite does not allowed us to calculate pre-eruptive temperature. However, the stability of quartz and plagioclase, which are natural phases, suggest that temperature should be less than 750 °C at a pressure of 200 MPa. The analyses of H2O and CO2 dissolved in melt inclusions yielded concentrations of 2-5 wt.% and 50-100 ppm respectively. This data confirm that the pre-eruptive pressure of the Tala tuff is ~200 MPa and in addition to major elements compositions suggest that the Tala tuff is either, compositionally zoned or mixed with other magma just prior to eruption.

  11. Under Construction: Rebuilding Kīlauea's Shallow Magma Storage System After Caldera Collapse

    Science.gov (United States)

    Swanson, D. A.; Wright, T. L.

    2015-12-01

    Draining of Kīlauea's upper level magma reservoir system in ~1500 CE led to a N-S elongate, roughly circular structural caldera ~6.5 km in diameter surrounding a prominent topographic caldera (TC) 4 x 3 km in diameter. The TC was probably at least 600 m deep with a volume of ~4-6 km3. The reservoir system has been rebuilding since then, mostly during the past 200 y of relatively high magma supply. Current reservoir locations are well defined geodetically (Poland et al., 2014) but do not match the presumed configuration of magma storage before the caldera collapse, if the common assumption holds that collapse width equals reservoir width. For example, magma does not underlie the northern 1-2 km of the TC, as judged by relatively high P-wave velocities (Dawson et al., 1999) and lack of deformation related to magma storage. The northernmost reservoir, near Halemaumau, is within the TC, but an order of magnitude more magma fills the south caldera reservoir south of the TC (Poland et al., 2014). Currently, the Halemaumau reservoir is shallower than the south caldera reservoir (1-2 km vs. 3-4 km), but in the 1960s magma was likely stored 3-3.5 km deep near Halemaumau (Wright and Klein, 2014). Many deformation centers are south of the TC and have an E-W spread of ~4 km. These observations suggest an evolving storage system that, if drained today, would not form a caldera of the size or location of the TC. Yet the TC is at the summit of the volcano, the site of an older caldera (Holcomb, 1987) and a positive Bouguer gravity anomaly (Kauahikaua et al., 2000), and is apparently the preferred location of reservoir draining and caldera collapse. We think the reservoir system will continue to evolve, expanding and centering itself below the topographic caldera, which will likely be where the next collapse takes place. Dawson et al., 1999, GRL. Holcomb, 1987, USGS PP 1350. Kauahikaua et al., 2000, Geology. Poland et al., 2014, USGS PP 1801. Wright and Klein, 2014, USGS PP 1806.

  12. REFRIGERAÇÃO UTILIZANDO PASTILHAS DE EFEITO PELTIER

    OpenAIRE

    Antonio Luiz P. S. Campos; Aécio Vinícius Amorim Farias; Jainne Daniele F. S. Fernandes; Alailson de Freitas Braz; Ludmila Sayonara S. X. Machado; Edfranklin de Souza Pimentel

    2010-01-01

    Pastilhas de Peltier são dispositivos baseados no efeito Peltier e são aplicadas para produzir efeito refrigerador ou aquecedor. Este trabalho aborda conceitos envolvidos na fabricação e funcionamento desses dispositivos tais como: histórico do efeito Peltier e desenvolvimento de placas de efeito Peltier. É feito um estudo de eficiência da refrigeração de água utilizando uma placa de efeito Peltier existente no Campus Natal – Zona Norte. Para isso, é implementada uma estrutura de refrigeração...

  13. Gravity field at unrest caldera: an application to Campi Flegrei area

    Science.gov (United States)

    Russo, Guido; Capuano, Paolo

    2010-05-01

    Campi Flegrei is a well known volcanic caldera which is characterized by a slow sequence of uplifts and downlifts (bradyseism) superimposed to a sporadic but remarkable explosive activity. Last eruption occurred in 1538, while the most recent uplift episodes (1970-72 and 1982-84) produced about 3 m of cumulative displacement at the town of Pozzuoli. This behavior and the proximity of the densely urbanized town of Naples increases the volcanic hazard of the area. The knowledge of the structural characteristics of the caldera is important to better understand and interpret measured data as well as the past volcanic history. In this frame, gravity data inversion can provide useful information. We collected and inverted about 1500 gravity data covering Campi Flegrei caldera and Ischia island, which is the other main volcanic center of the area, and was characterized in the past by several explosive eruptions (the last one in 1301), and presently by hydrothermal activity. The 3D inversion method was developed by us to deal with scattered data and the presence of topography, and is based on Thichonov regularization theory. As to Campi Flegrei caldera, its shape and bordering structure is clearly singled out in agreement with seismic tomography results. Less marked borders are also present at shallow depth on the NE part of the area. As to Ischia island, our results show the presence of a central high density block and the border of a caldera roughly coinciding with the coastline of the island.

  14. Geologic Map of the Central San Juan Caldera Cluster, Southwestern Colorado

    Science.gov (United States)

    Lipman, Peter W.

    2006-01-01

    The San Juan Mountains are the largest erosional remnant of a composite volcanic field that covered much of the southern Rocky Mountains in middle Tertiary time. The San Juan field consists mainly of intermediate-composition lavas and breccias, erupted about 35-30 Ma from scattered central volcanoes (Conejos Formation) and overlain by voluminous ash-flow sheets erupted from caldera sources. In the central San Juan Mountains, eruption of at least 8,800 km3 of dacitic-rhyolitic magma as nine major ash flow sheets (individually 150-5,000 km3) was accompanied by recurrent caldera subsidence between 28.3 Ma and about 26.5 Ma. Voluminous andesitic-dacitic lavas and breccias erupted from central volcanoes prior to the ash-flow eruptions, and similar lava eruptions continued within and adjacent to the calderas during the period of more silicic explosive volcanism. Exposed calderas vary in size from 10 to 75 km in maximum dimension; the largest calderas are associated with the most voluminous eruptions.

  15. Quiescent deformation of the Aniakchak Caldera, Alaska mapped by InSAR

    Science.gov (United States)

    Kwoun, Oh-Ig; Lu, Zhiming; Neal, C.; Wicks, C.

    2006-01-01

    The 10-km-wide caldera of the historically active Aniakchak volcano, Alaska, subsides ???13 mm/yr, based on data from 19 European Remote Sensing Satellite (ERS-1 and ERS-2) interferometric synthetic aperture radar (InSAR) images from 1992 through 2002. The pattern of subsidence does not reflect the distribution of pyroclastic deposits from the last eruption in 1931 and therefore is not related to compaction of fragmental debris. Weighted least-squares inversion of the deformation maps indicates a relatively constant subsidence rate. Modeling the deformation with a Mogi point source locates the source of subsidence at ???4 km below the central caldera floor, which is consistent with the inferred depth of magma storage before the 1931 eruption. Magmatic CO2 and He have been measured at a warm soda spring within the caldera, and several sub-boiling fumaroles persist elsewhere in the caldera. These observations suggest that recent subsidence can be explained by the cooling or degassing of a shallow magma body (???4 km deep), and/or the reduction of the pore-fluid pressure of a cooling hydrothermal system. Ongoing deformation of the volcano detected by InSAR, in combination with magmatic gas output from at least one warm spring, and infrequent low-level bursts of seismicity below the caldera, indicate that the volcanic system is still active and requires close attention for the timely detection of possible hazards. ?? 2006 Geological Society of America.

  16. Confianza, influencia política e intercambio de recursos en arenas decisorias regionales Trust, Political Influence, and Exchange of Resources in Regional Decision-Making Arenas

    Directory of Open Access Journals (Sweden)

    RAMIRO BERARDO

    2012-01-01

    Full Text Available La literatura politológica destaca la importancia de la confianza en la emergencia de procesos sociopolíticos cooperativos, pero en la politología latinoamericana no existen aún exploraciones empíricas de la relación entre confianza y otras variables que también afectan la cooperación en arenas decisorias regionales. Este artículo contribuye a solucionar esta limitación examinando la relación entre confianza, intercambio de recursos y reconocimiento de influencia política, entre actores de tres regiones subnacionales de la Argentina. Los resultados sugieren que tanto el reconocimiento de influencia como el intercambio de recursos se correlacionan de manera muy significativa con las relaciones de confianza que existe entre los actores. Esta relación tiene implicancias sobre procesos de gobernanza a nivel regional, que discutimos en detalle.Research in political science has identified trust as an important variable for the emergence of cooperative social-political processes, but there are no empirical explorations in Latin American political science yet of the relationship between trust and other variables that are thought to affect cooperation in regional decision-making arenas. This article contributes to addressing this limitation by examining the relationship between trust, exchange of resources, and perception of political influence among actors in 3 sub-national regions in Argentina. Results suggest that these variables are significantly related to each other, which has implications for our understanding of how regional governance processes work. We discuss these implications in detail.

  17. Intercambio gaseoso en el síndrome de dificultad respiratoria aguda Gas exchange in acute respiratory distress syndrome

    Directory of Open Access Journals (Sweden)

    G. A. Raimondi

    2003-04-01

    Full Text Available El síndrome de dificultad respiratoria aguda (ARDS se caracteriza por presentar alteraciones severas del intercambio gaseoso (IG causadas por «shunt» e importante irregularidad de la ventilación perfusión (V A/Q. Esto es consecuencia del edema intersticial y el colapso y ocupación alveolar. Además de la fracción inspirada de oxígeno y la evolución de la patología pulmonar, hay distintas variables que son capaces de alterar la presión parcial de oxígeno arterial (PaO2. Es así que los cambios del volumen minuto circulatorio, la concentración de hemoglobina, el consumo de oxígeno o la alcalosis pueden modificar la PaO2 a través de su influencia en la PO2 de sangre venosa mixta. A pesar de la influencia de estas diferentes variables, la anormalidad del IG se ha podido analizar adecuadamente por medio de la técnica de eliminación de múltiples gases inertes (MIGET. Asimismo, se han descripto diversas estrategias ventilatorias (presión positiva de fin de espiración, relaciones inspiratorias-espiratorias invertidas, volúmenes corrientes elevados, etc. que producen mejoría del IG principalmente a través del aumento de la presión media en la vía aérea al reclutar áreas pulmonares previamente colapsadas. También el cambio de decúbito a posición ventral, por modificaciones en la distribución de presión pleural regional, disminuye el colapso alveolar con mejoría de la PaO2. Asimismo hay distintas intervenciones farmacológicas capaces de mejorar el IG tales como la administración de óxido nítrico (ON o de prostaglandinas (PGI2 o PGE1 por vía inhalatoria. Estas producen vasodilatación de las áreas bien ventiladas aumentando el flujo cardíaco a ese nivel y disminuyendo relativamente el flujo por las áreas de «shunt». La almitrina endovenosa, droga vasoconstrictora pulmonar, mejora el IG al aumentar la vasoconstricción hipóxica. Se ha demostrado efecto aditivo de la almitrina con la inhalación de ON. A pesar del

  18. Travel Time Distribution Modeling in the Valles Caldera, New Mexico

    Science.gov (United States)

    Broxton, P. D.; Troch, P. A.; Brooks, P. D.; Lyon, S. W.; Gustafson, J. R.; Veatch, W. C.

    2007-12-01

    Modeling the transit times of catchment waters is of paramount importance in hydrology. The distribution of the time it takes for individual water molecules to move through a hydrologic system (a.k.a., the travel time distribution) is a fundamental characterization of a catchment. Travel time distributions are affected by a variety of physical characteristics of catchments (e.g., vegetation type, degree of soil development) that depend on the amount of solar energy the catchment receives. These characteristics, therefore, can be considered a function of aspect. The goal of this research is to constrain travel time distributions on a series of eight radial mountain streams having different slope aspects on Redondo Peak, a resurgent dome in the center of the Valles Caldera, near Los Alamos, New Mexico. Redondo Peak is an excellent natural laboratory for this type of experiment because all aspects are represented on different sides of the mountain while the internal geology and climate are relatively consistent. To model the transit time distributions of each catchment, variations of chemical load of the snowpack, isotopic compositions of meltwater samples, and snowcover distribution data from closely related studies are coupled with periodic stream and precipitation samples that are analyzed for stable water isotopes content. Additional information comes from a network of temperature sensors to monitor the distribution of snowmelt and headwater stream discharge as well as a series of flumes to capture the flows from the streams. The travel time distributions determined in this project provide a bottom up approach to verify catchment-scale models.

  19. Servicio de M-comercio: Sistema de interacción entre un centro comercial y sus visitantes utilizando las tecnologías WAP y Bluetooth M-commerce service: Interaction system between a mall and visitors using WAP and Bluetooth technologies

    Directory of Open Access Journals (Sweden)

    Jorge Gómez Rojas

    2013-04-01

    Full Text Available El servicio de interacción es un medio de comunicación que mejora las relaciones comerciales entre los centros comerciales y sus visitantes, utilizando las tecnologías de comunicaciones móviles WAP y Bluetooth como una nueva alternativa de negocios, y sin usar la red del operador de telefonía móvil celular. El sistema de interacción mencionado permite el intercambio de información de un grupo potencial de compradores entre los visitantes de un centro comercial y la administración de los diferentes comercios utilizando el teléfono celular. El sistema se compone de una aplicación móvil en J2ME, puntos de acceso Bluetooth y Wi-Fi, un servidor Bluetooth y un servidor Web con aplicaciones para ser accedidas por dispositivos móviles.The interaction service is a means of communication that improves trade relations between the mall and visitors using mobile communications technology WAP and Bluetooth, as a new business alternative, and without operator's network using the mobile phone. The proposed system of interaction, allows the exchange of information from a potential pool of buyers among visitors to a shopping center and the administration of the various shops, through the cell phone. The system consists of a mobile application in J2ME, the access points, Bluetooth server, and Web server with applications to mobile devices.

  20. The 2014-2015 slow collapse of the Bárðarbunga caldera, Iceland

    Science.gov (United States)

    Tumi Gudmundsson, Magnus; Jónsdóttir, Kristín; Roberts, Matthew; Ófeigsson, Benedikt G.; Högnadóttir, Thórdís; Magnússon, Eyjólfur; Jarosch, Alexander H.; Pálsson, Finnur; Einarsson, Páll; Sigmundsson, Freysteinn; Drouin, Vincent; Hjörleifsdóttir, Vala; Reynolds, Hannah I.; Dürig, Tobias; Vogfjörd, Kristín; Hensch, Martin; Munoz-Cobo Belart, Joaquin; Oddsson, Björn

    2015-04-01

    The Bárðarbunga caldera is located in central Iceland, under in NW corner of Vatnajökull ice cap. The caldera is about 65 km2 in area, with 500-600 m high topographic rims and is fully covered with up to 800 m thick ice. On 16 August 2014 an intense earthquake swarm started in Bárðarbunga, the beginning of a major volcano-tectonic rifting event forming a 45 km long dyke extending from the caldera to Holuhraun lava field outside the northern margin of Vatnajökull (Sigmundsson et al., 2014). A large basaltic, effusive fissure eruption began in Holuhraun on 31 August that by January had formed a lava field of volume in excess of one cubic kilometre. The collapse of the caldera is expected to have begun a few days after the onset of the earthquake swarm, probably coinciding with the first M5 earthquake. This slow caldera collapse has been monitored through repeated mapping of the gradually increasing subsidence bowl (~80 km2 in December) with airborne profiling of the ice surface, satellite mapping, an online GPS station set up in September on the glacier surface in the centre of the caldera with a strong motion sensor added in November, and indirectly through recording of seismic activity. Satellite interferograms constrain both ice movements and the rate of collapse. The rate of collapse was greatest in the first two weeks or 0.5-1 m/day in the centre, but has since gradually declined with time. The daily rate was 0.1-0.2 m/day in January, when the maximum lowering had reached about 60 m. A gradual widening of the subsidence bowl has been observed since early September. It is asymmetric, deepest in the NE part of the caldera. Downwards displacement extends outside the pre-existing topographic caldera rims, particularly on the south side where the rims have subsided by over 10 meters. Ice-flow modelling indicates that the ice is mostly passively subsiding with the caldera floor. Thus, horizontal ice flow has had little effect on the shape of the subsidence bowl

  1. Doubly stochastic models for volcanic hazard assessment at Campi Flegrei caldera

    CERN Document Server

    Bevilacqua, Andrea

    2016-01-01

    This study provides innovative mathematical models for assessing the eruption probability and associated volcanic hazards, and applies them to the Campi Flegrei caldera in Italy. Throughout the book, significant attention is devoted to quantifying the sources of uncertainty affecting the forecast estimates. The Campi Flegrei caldera is certainly one of the world’s highest-risk volcanoes, with more than 70 eruptions over the last 15,000 years, prevalently explosive ones of varying magnitude, intensity and vent location. In the second half of the twentieth century the volcano apparently once again entered a phase of unrest that continues to the present. Hundreds of thousands of people live inside the caldera and over a million more in the nearby city of Naples, making a future eruption of Campi Flegrei an event with potentially catastrophic consequences at the national and European levels.

  2. Electrical structure of Plaine des Sables caldera, Piton de la Fournaise volcano (Reunion Island

    Directory of Open Access Journals (Sweden)

    P. A. Schnegg

    1997-06-01

    Full Text Available An Audio Magnetotelluric (AMT profile has been carried out across the Plaine des Sables, a former caldera of the active Piton de la Fournaise volcano, Reunion Island. Located in the Western Indian Ocean, between the Mascarene and Madagascar basins, this basaltic shield volcano originates from the activity of a hot spot. Our aim was to determine the internal structure of the volcano, in particular the shallow electrical properties of an area extending between the old and the new caldera rims. Although several teams had already conducted AMT work in this region a few years ago, there was a need for more a detailed, in depth survey. Our final model displays a noticeable slope of the Plaine des Sables basement oriented toward the present Fournaise summit. This slope is interpreted as resulting from successive landslides toward the ocean. We conclude that this dipping, electrically good conducting layer, probably belongs to the flat layering of an older caldera.

  3. Recrystallization and anatexis along the plutonic-volcanic contact of the Turkey Creek caldera, Arizona

    Science.gov (United States)

    du Bray, E.A.; Pallister, J.S.

    1999-01-01

    Unusual geologic and geochemical relations are preserved along the contact between intracaldera tuff and a resurgent intrusion within the 26.9 Ma Turkey Creek caldera of southeast Arizona. Thick intracaldera tuff is weakly argillically altered throughout, except in zones within several hundred meters of its contact with the resurgent intrusion, where the groundmass of the tuff has been variably converted to granophyre and unaltered sanidine phenocrysts are present. Dikes of similarly granophyric material originate at the tuff-resurgent intrusion contact and intrude overlying intracaldera megabreccia and tuff. Field relations indicate that the resurgent intrusion is a laccolith and that it caused local partial melting of adjacent intracaldera tuff. Geochemical and petrographic relations indicate that small volumes of partially melted intracaldera tuff assimilated and mixed with dacite of the resurgent intrusion along their contact, resulting in rocks that have petrographic and compositional characteristics transitional between those of tuff and dacite. Some of this variably contaminated, second-generation magma coalesced, was mobilized, and was intruded into overlying intracaldera rocks. Interpretation of the resurgent intrusion in the Turkey Creek and other calderas as intracaldera laccoliths suggests that intrusions of this type may be a common, but often unrecognized, feature of calderas. Development of granophyric and anatectic features such as those described here may be equally common in other calderas. The observations and previously undocumented processes described here can be applied to identification and interpretation of similarly enigmatic relations and rocks in other caldera systems. Integration of large-scale field mapping with detailed petrographic and chemical data has resulted in an understanding of otherwise intractable but petrologically important caldera-related features.

  4. Identification of Calderas Associated With The Acidic Jurassic Volcanism of Southern Patagonia, Argentina

    Science.gov (United States)

    Chernicoff, C. J.; Salani, F. M.

    During the Jurassic, the Patagonian region was subject to a predominantly acidic volcanism locally known as the Chon Aike Volcanic Province, related to the breakup of Gondwana. It comprises ignimbrites, breccias and agglomerates, and a minor component of rhyolitic and dacitic lava domes. In the study area (Río Seco region, Santa Cruz Province), the Jurassic volcanics are largely overlain by Neogene and Quaternary sediments. However, the aeromagnetic survey of this region has unravelled the magnetic pattern of the volcanics, notably two conspicuous calderas, since the young cover sediments are non-magnetic. The magnetic susceptibility of the volcanic rocks ranges 50 to 80 x 10-5 S.I., as oppossed to the nearly null values of the overlying sediments. The geological interpretation of the aeromagnetic survey is mostly based on the analytic signal of the total magnetic intensity, where two distinct sub-circular magnetic lineaments have been recognized and regarded as calderic structures. The eastern caldera, 30 km wide, is centered at 48º 52' S.L./ 68º 02' W.L., and the western caldera, 23 km wide, is centered at 48º 53' S.L. / 68º 29' W.L.. In addition, a number of smaller, high gradient magnetic anomalies have been identified and interpreted as intra- and extracaldera domes. In the eastern caldera, a number of domes follow an anular pattern of fractures regarded as the boundary of an older, outer caldera. A magnetic circular lineament located within the latter structure has been interpreted as a younger, inner caldera which presents a number of small domes in its central depression; additional domes are also located in between the two calderic structures. The western caldera is less complex since it comprises a single structure with intra-caldera domes. The total magnetic gradient (analytic signal) associated with the domes is one order of magnitude higher (0.1 to 0.2) than the mean value of the region (0.03). In addition to the anular fractures and domes, a

  5. REFRIGERAÇÃO UTILIZANDO PASTILHAS DE EFEITO PELTIER

    Directory of Open Access Journals (Sweden)

    Antonio Luiz P. S. Campos

    2010-06-01

    Full Text Available Pastilhas de Peltier são dispositivos baseados no efeito Peltier e são aplicadas para produzir efeito refrigerador ou aquecedor. Este trabalho aborda conceitos envolvidos na fabricação e funcionamento desses dispositivos tais como: histórico do efeito Peltier e desenvolvimento de placas de efeito Peltier. É feito um estudo de eficiência da refrigeração de água utilizando uma placa de efeito Peltier existente no Campus Natal – Zona Norte. Para isso, é implementada uma estrutura de refrigeração de água e são feitas medições para determinar a eficiência de sistema. Por fim, são apresentadas conclusões sobre o estudo desenvolvido.

  6. Planeamento de uma estrada utilizando CCS Candy - Caso de estudo

    OpenAIRE

    Oliveira, Sara Maria de

    2013-01-01

    O tema desta dissertação foi escolhido tendo em consideração a crescente necessidade de planeamento de empreitadas de construção de estradas, sendo um dos objetivos desta dissertação o de oferecer uma visão global do processo de planeamento da construção de uma estrada, focado apenas no fator tempo, recorrendo a ferramentas informáticas e utilizando um caso de estudo de uma estrada real e já construída. Inicialmente, faz-se uma breve descrição dos métodos de planeamento mais aplicados em p...

  7. Steady subsidence of a repeatedly erupting caldera through InSAR observations: Aso, Japan

    Science.gov (United States)

    Nobile, Adriano; Acocella, Valerio; Ruch, Joel; Aoki, Yosuke; Borgstrom, Sven; Siniscalchi, Valeria; Geshi, Nobuo

    2016-04-01

    The relation between unrest and eruption at calderas is still poorly understood. Aso caldera, Japan, shows minor episodic eruptions, mainly phreatic, associated with steady subsidence. We analyse the recent deformation of Aso using SAR images from 1993 to 2011 and compare this with the eruptive activity. Although the dataset suffers from limitations (e.g., atmospheric effects, coherence loss, low signal to noise ratio), we observe a steady subsidence signal from 1996 to 1998, that suggests an overall contraction of a magmatic source below the caldera centre, from 4.5 to 7 km depth. Because of the similar volumes of the contracting source and erupted material, we propose that the contraction may have been induced by the release of the magmatic fluids feeding the eruptions. If confirmed by further data, this hypothesis suggests that degassing processes play a crucial role in triggering minor eruptions within open conduit calderas, as at Aso. These features underline the importance of defining any eruptive potential also from deflating magmatic systems with open conduit.

  8. Hydrothermal fluid flow and deformation in large calderas: Inferences from numerical simulations

    Science.gov (United States)

    Hurwitz, S.; Christiansen, L.B.; Hsieh, P.A.

    2007-01-01

    Inflation and deflation of large calderas is traditionally interpreted as being induced by volume change of a discrete source embedded in an elastic or viscoelastic half-space, though it has also been suggested that hydrothermal fluids may play a role. To test the latter hypothesis, we carry out numerical simulations of hydrothermal fluid flow and poroelastic deformation in calderas by coupling two numerical codes: (1) TOUGH2 [Pruess et al., 1999], which simulates flow in porous or fractured media, and (2) BIOT2 [Hsieh, 1996], which simulates fluid flow and deformation in a linearly elastic porous medium. In the simulations, high-temperature water (350??C) is injected at variable rates into a cylinder (radius 50 km, height 3-5 km). A sensitivity analysis indicates that small differences in the values of permeability and its anisotropy, the depth and rate of hydrothermal injection, and the values of the shear modulus may lead to significant variations in the magnitude, rate, and geometry of ground surface displacement, or uplift. Some of the simulated uplift rates are similar to observed uplift rates in large calderas, suggesting that the injection of aqueous fluids into the shallow crust may explain some of the deformation observed in calderas.

  9. Galileo's Last Fly-Bys of Io: NIMS Observations of Loki, Tupan, and Emakong Calderas

    Science.gov (United States)

    Lopes, Rosaly M. C.; Kamp, L. W.; Davies, A. G.; Smythe, W. D.; Carlson, R. W.; Doute, S.; McEwen, A.; Turtle, E. P.; Leader, F.; Mehlman, R.

    2002-01-01

    NIMS results from the 2001 Galileo fly-bys of Io will be presented, focusing on three calderas that may contain lava lakes. Preliminary results from the January 2002 Io fly-by will be presented. Additional information is contained in the original extended abstract.

  10. Topographic modelling of caldera analogues using Structure from Motion - Multiview stereo-photogrammetry

    Science.gov (United States)

    Ulusoy, İnan; Aydın, Eda; Evren Çubukçu, H.

    2016-04-01

    Analogue caldera models have long been used in volcanology to investigate structural evolution of volcanoes during tumescence and collapse periods. Influence of tectonic forces on volcanic features are also in the scope of those experiments. As well as interior modelling of the caldera experiments, topographic modelling is essential for digital monitoring and quantification purposes. Topographic modelling of those sandbox models is possible using laser scanning techniques. Particle tracking using still images is another way to demonstrate and quantify the structure and movement during the experiment. The quantum leap in the digital photography and computation tools and ease of access to both, provides the use of a new modelling technique in various scales and applications in Geology. Although the roots are older, Structure from Motion - Multiview stereo-photogrammetry (SfM-MVS) is a relatively new technique for surface modelling via several high resolution photographs. We have used SfM-MVS to digitally model the elevation of the tumescence and collapse cycles in analogue caldera experiments. Several sandbox experiments have been modelled using SfM-MVS technique stage by stage during tumescence and collapse periods. It has been possible to evaluate the structural evolution of the collapse models. Additionally, using particle tracking via still images acquired during the experiments, we have modelled the superficial evolution of the caldera structure. SfM-MVS is an effective low budget method for modelling in decimetric scale down to millimetre/micrometre precision.

  11. Identification of a Kulshan caldera correlative tephra in the Palouse loess of Washington State, northwest USA

    Science.gov (United States)

    King, Georgina E.; Pearce, Nicholas J. G.; Roberts, Helen M.; Smith, Victoria C.; Westgate, John A.; Gaylord, David R.; Sweeney, Mark R.

    2016-09-01

    The Kulshan caldera formed at ∼1.15 Ma on the present-day site of Mt. Baker, Washington State, northwest USA and erupted a compositionally zoned (dacite-rhyolite) magma and a correlative eruptive, the Lake Tapps tephra. This tephra has previously been described, but only from the Puget Lowland of NW Washington. Here an occurrence of a Kulshan caldera correlative tephra is described from the Quaternary Palouse loess at the Washtucna site (WA-3). Site WA-3 is located in east-central Washington, ∼340 km southeast of the Kulshan caldera and ∼300 km east-southeast of the Lake Tapps occurrence in the Puget Lowland. Major- and trace element chemistry and location of the deposit at Washtucna within reversed polarity sediments indicates that it is not correlative with the Mesa Falls, Rockland, Bishop Ash, Lava Creek B or Huckleberry Ridge tephras. Instead the Washtucna deposit is related to the Lake Tapps tephra by fractional crystallisation, but is chemically distinct, a consequence of its eruption from a compositionally zoned magma chamber. The correlation of the Washtucna occurrence to the Kulshan caldera-forming eruption indicates that it had an eruptive volume exceeding 100 km3, and that its tephra could provide a valuable early-Pleistocene chronostratigraphic marker in the Pacific Northwest.

  12. Monitoring super-volcanoes: geophysical and geochemical signals at Yellowstone and other large caldera systems.

    Science.gov (United States)

    Lowenstern, Jacob B; Smith, Robert B; Hill, David P

    2006-08-15

    Earth's largest calderas form as the ground collapses during immense volcanic eruptions, when hundreds to thousands of cubic kilometres of magma are explosively withdrawn from the Earth's crust over a period of days to weeks. Continuing long after such great eruptions, the resulting calderas often exhibit pronounced unrest, with frequent earthquakes, alternating uplift and subsidence of the ground, and considerable heat and mass flux. Because many active and extinct calderas show evidence for repetition of large eruptions, such systems demand detailed scientific study and monitoring. Two calderas in North America, Yellowstone (Wyoming) and Long Valley (California), are in areas of youthful tectonic complexity. Scientists strive to understand the signals generated when tectonic, volcanic and hydrothermal (hot ground water) processes intersect. One obstacle to accurate forecasting of large volcanic events is humanity's lack of familiarity with the signals leading up to the largest class of volcanic eruptions. Accordingly, it may be difficult to recognize the difference between smaller and larger eruptions. To prepare ourselves and society, scientists must scrutinize a spectrum of volcanic signals and assess the many factors contributing to unrest and toward diverse modes of eruption.

  13. Evidence from cosmic-ray exposure dating based on 36Cl for the pre-Minoan caldera on Santorini, Greece

    Science.gov (United States)

    Athanassas, Constantin; Bourlès, Didier; Braucher, Regis; Druitt, Tim; Nomikou, Paraskevi; Léanni, Laetitia

    2016-04-01

    The physiography of Santorini prior to the Minoan (Late Bronze Age) eruption (17th century BCE) is of great archaeological interest, given the importance of Santorini as a commercial centre and port in the Minoan empire. However, the paleogeography of the pre-Minoan caldera has been a point of controversy: Heiken and McCoy (1984) advocated the existence, in the southern part of the present-day caldera, of a pre-existing caldera formed during the 172 ka Lower Pumice eruption, whereas Druitt and Francaviglia (1992), based on the presence of in situ plinian pumice from the Minoan eruption adhering to the modern cliff, conceived the pre-Minoan (22 ka) caldera as having occupied much of the northern basin of the present-day caldera. With the goal of settling the debate we performed cosmic ray exposure dating employing in situ-produced cosmogenic 36Cl to date different generations of caldera cliffs at Santorini, and hence to identify those cliffs predating the Minoan eruption. Our methodology involved the determination of the in situ-produced cosmogenic 36Cl in basaltic and andesitic rocks cropping out in the cliffs. The samples returned 36Cl CRE ages consistent with previously published field mapping of cliff populations based on geomorphological and stratigraphic arguments (Druitt and Francaviglia 1992), suggesting that much of the present cliff line of northern Santorini predated the Minoan eruption, or was superficially modified by landslips and rockfalls during that eruption. The 36Cl CRE ages enable us to better define the paleogeography of the pre-Minoan caldera. References [1] Druitt, T. H. and Francaviglia, V.1992. Caldera formation on Santorini and the physiography of the islands in the Late Bronze Age. Bulletin of Volcanology 54, 484-493. [2] Heiken G and McCoy F (1984) Caldera development during the Minoan eruption, Thira, Cyclades, Greece. Journal of Geophysical Research: 89 (B10), 8841-8862.

  14. Cuantificación y procedencia de los intercambios de CO2 en un ecosistema carbonatado mediante la técnica de eddy covariance y el análisis de los isótopos estables de carbono

    Directory of Open Access Journals (Sweden)

    P. Serrano-Ortiz

    2010-01-01

    Full Text Available Los intercambios de CO2 entre atmósfera y ecosistemas, así como los procesos que intervienen en dichos intercambios, son de vital interés para la caracterización del ciclo global del carbono y la repercusión del calentamiento global sobre estos ecosistemas naturales. En ecosistemas de origen carbonatado, los procesos biológicos de fotosíntesis y respiración interactúan con procesos de ventilación de cavidades y de disolución y precipitación de carbonatos que pueden incluso dominar el intercambio de CO2 en determinadas épocas del año. En este trabajo, se usó la técnica de eddy covariance junto con análisis de los isótopos estables de carbono y medidas de flujo de CO2 de suelo y otras variables meteorológicas, para determinar la procedencia del CO2 intercambiado. Los resultados obtenidos demuestran que el ecosistema actúa como sumidero o fuente de CO2 en función de las condiciones meteorológicas y la época del año. Bajo condiciones óptimas de temperatura y recursos hídricos, la huella isotópica del carbono (d13C del aire alcanza valores muy negativos indicando un origen biológico del intercambio. En épocas de sequía y senescencia biológica estos procesos se reducen considerablemente. La atmósfera externa y la cavidad toman valores de d13C muy similares indicando un alto grado de ventilación de la cavidad.

  15. FESTIVALES DE INNOVACIÓN LOCAL: UN ESPACIO PARA EL INTERCAMBIO, EL APRENDIZAJE, LA COMUNICACIÓN Y LA COMERCIALIZACIÓN

    Directory of Open Access Journals (Sweden)

    Ania Yong

    2011-01-01

    Full Text Available El fomento de huertos familiares en la comunidadde San Andrés con el objetivo de promover la producción artesanal de conservas domésticas, es resultado de la realizaciónde visitas de intercambio y talleres de aprendizaje entreproductores urbanos y rurales. Estas acciones desarrolladas durante los años 2005 y 2006 propiciaron la adopción y adaptaciónde especies hortícolas en la localidad. A finales del año 2006,productoras y productores de La Palma, Pinar del Río comenzarona demandar espacios para mostrar el resultado de sus producciones,por lo que fue necesario crear espacios para que intercambiaran,aprendieran y comercializaran sus productos en la comunidad.Estos espacios fueron denominados Festivales de InnovaciónLocal y permitieron el reconocimiento de las potencialidadeslocales para producir alimentos sanos mediante tecnologíasamigables con el medio ambiente donde el productor ofrecía directamente a los consumidores sus productos e intercambiaba directamente con los consumidores.

  16. Redes de participación e intercambios en la radio pública: los podcasting Networks of Participation and Communicative Interchanges in Public Radio: Podcasting

    Directory of Open Access Journals (Sweden)

    Carmen Salgado Santamaría

    2009-10-01

    Full Text Available El desarrollo de los podcasting, como sistema añadido de la ciberradio, impulsa a las redes de participación e intercambios comunicativos de interés social, que exhiben numerosas ventajas frente a las prácticas radiofónicas conocidas. La difusión que la radio pública realiza de los podcasts, la colocan en el actual proceso de convergencia tecnológica, y la sitúan en una sociedad de la información y del conocimiento, capaz de ofrecer diferentes servicios al alcance de todos los ciudadanos. Sólo la introducción de nuevos contenidos y servicios que aporten valor añadido a los existentes y satisfagan las necesidades de sus usuarios, procurarán la rentabilidad de este sistema. The development of podcasting as an additional system of cyberradio stimulates the appearance of networks of participation and communicative interchanges of social interest, and has numerous advantages over conventional radio practices. The spreading of podcasts through public radio situates it within the process of technological convergence and in an Information and Knowledge society which is able to offer different services within reach of all citizens. Only the introduction of new contents and services that contribute added value to the existing ones and satisfy the needs of users will make this system profitable.

  17. EVALUACIÓN DE LA ACTIVIDAD FOTOSINTÉTICA ASOCIADA CON EL INTERCAMBIO GASEOSO DE DOS VARIEDADES DE Coffea arabica OBTENIDAS POR CULTIVO In Vitro

    Directory of Open Access Journals (Sweden)

    Elizabeth Isaac

    2010-01-01

    Full Text Available El trabajo se desarrolló en el Laboratorio de Células y Cultivo de Tejidos del Centro de Bioplantas en julio de 2007, con el objetivo de evaluar la actividad fotosintética de las plántulas de Coffea arabica var. Catuai y Caturra rojo, obtenidas in vitro en fase de multiplicación. Se determinaron la tasa de fotosíntesis neta, transpiración, conductancia estomática y concentración de pigmentos clorofílicos para cada una de las variedades a las ocho semanas de cultivadas; las vitroplantas crecieron en condiciones controladas en un medio MS suplementado con 0,5 ¿mol de AIA y 5 ¿mol de 6-BAP. Los resultados mostraron que ambas variedades desarrolladas in vitro presentaron tasas de fotosíntesis neta similares a las plantas de cafeto adultas cultivadas en condiciones de campo, lo que demostró la capacidad de fotosíntesis de las plántulas, conservando un adecuado equilibrio para el intercambio gaseoso en el proceso fotosintético durante la etapa de multiplicación in vitro.

  18. Baldomero Sanín Cano y la Revista Nosotros de Buenos Aires (1907-1943. Intercambio y redes culturales e intelectuales

    Directory of Open Access Journals (Sweden)

    Rafael Rubiano Muñoz

    2014-06-01

    Full Text Available El artículo se propone evidenciar las relaciones intelectuales y culturales constituidas por Baldomero Sanín Cano durante su estancia en Argentina. A partir de un análisis interpretativo de algunas fuentes como la prensa y su obra periodística, las revistas, el epistolario y los ensayos vinculados con la obra y el pensamiento de Sanín Cano, se busca indagar como se establecieron y cuáles fueron las redes e intercambios que el colombiano instituyo en su paso por la ciudad de Buenos Aires. El estudio muestra que la estancia como periodista y diplomático de Sanín Cano en esta capital no fue insustancial y que, por el contrario, como otros intelectuales latinoamericanos de la época, se integró a una variedad de proyectos editoriales y políticos que le llevaron a gozar de un trato constante con personalidades latinoamericanas destacadas en el panorama mundial y del subsecuente reconocimiento.

  19. La dialecta Pilagá de la reciprocidad. Una concepción dialógica del intercambio étnico de bienes

    Directory of Open Access Journals (Sweden)

    Fernando Lynch

    2003-01-01

    Full Text Available Se expone aquí una primer parte de los resultados de una investigación sobre la reciprocidad entre los pilagá. Partiendo de una perspectiva comunicacional, el trabajo etnográfico es visto como un acto de intercambio realizado entre los otros étnicos, dadores de información, y nosotros, interpretantes de su significación. Se concibe así ala propia actividad antropológica de acuerdo a los dictados del principio dial6g·ico, como un tipo de contacto intercultural que toma la forma de una conversación. En este primer texto se procede a una simple descripción del discurso indígena que nos pone frente a su semántica de superficie (dejando para una segunda parte su análisis semiótico que da cuenta de la explicación de su lógica intrínseca. En última instancia, gracias a la intermediación interpretativa que brinda su consideración hermenéutica, se aspira acceder a la semántica de profundidad del discurso ajeno dado, y, a su través, a una comprensión dialógica critica tanto del sentido teórico como del valor práctico del principio de reciprocidad.

  20. Geothermal hydrology of Valles Caldera and the southwestern Jemez Mountains, New Mexico

    Science.gov (United States)

    Trainer, Frank W.; Rogers, Robert J.; Sorey, M.L.

    2000-01-01

    The Jemez Mountains in north-central New Mexico are volcanic in origin and have a large central caldera known as Valles Caldera. The mountains contain the Valles geothermal system, which was investigated during 1970-82 as a source of geothermal energy. This report describes the geothermal hydrology of the Jemez Mountains and presents results of an earlier 1972-75 U.S. Geological Survey study of the area in light of more recent information. Several distinct types of thermal and nonthermal ground water are recognized in the Jemez Mountains. Two types of near-surface thermal water are in the caldera: thermal meteoric water and acid sulfate water. The principal reservoir of geothermal fluids is at depth under the central and western parts of the caldera. Nonthermal ground water in Valles Caldera occurs in diverse perched aquifers and deeper valley-fill aquifers. The geothermal reservoir is recharged by meteorically derived water that moves downward from the aquifers in the caldera fill to depths of 6,500 feet or more and at temperatures reaching about 330 degrees Celsius. The heated geothermal water rises convectively to depths of 2,000 feet or less and mixes with other ground water as it flows away from the geothermal reservoir. A vapor zone containing steam, carbon dioxide, and other gases exists above parts of the liquid-dominated geothermal zone. Two subsystems are generally recognized within the larger geothermal system: the Redondo Creek subsystem and the Sulphur Creek subsystem. The permeability in the Redondo Creek subsystem is controlled by stratigraphy and fault-related structures. Most of the permeability is in the high-angle, normal faults and associated fractures that form the Redondo Creek Graben. Faults and related fractures control the flow of thermal fluids in the subsystem, which is bounded by high-angle faults. The Redondo Creek subsystem has been more extensively studied than other parts of the system. The Sulphur Springs subsystem is not as well

  1. How medium-size resurgent calderas work: the case of Pantelleria, Ischia and the unrest Campi Flegrei structures

    Science.gov (United States)

    Orsi, Giovanni; Civetta, Lucia; Arienzo, Ilenia; Carandente, Antonio; D'Antonio, Massimo; de Vita, Sandro; di Renzo, Valeria; di Vito, Mauro; Marotta, Enrica; Belviso, Pasquale

    2010-05-01

    Assessment of time and space relationships among magmatism, volcanism, and resurgence of medium-size calderas is a necessary tool to formulate a general model for their dynamics which also permits to forecast their evolution. To define a general hypothesis for the Campi Flegrei caldera, in a persistent state of unrest, the Ischia and Pantelleria medium-size resurgent structures, in variable stages of evolution, have been investigated. In particular some parameters such as the structural and volcanological evolution, with emphasis on resurgence dynamics and coeval volcanism, and the evolution, present state and role of the magmatic system in resurgence, have been defined. For the Campi Flegrei caldera, the data collected during unrest episodes have also been taken into account. This innovative approach adds a time-perspective on how resurgent calderas behave. The proposed general hypothesis will help in long- and short-term volcanic hazards assessment and will support Civil Defence Authorities in elaborating actions devoted to volcanic risk reduction.

  2. Understanding the link between circumferential dikes and eruptive fissures around calderas based on numerical and analog models

    Science.gov (United States)

    Corbi, Fabio; Rivalta, Eleonora; Pinel, Virginie; Maccaferri, Francesco; Acocella, Valerio

    2016-06-01

    Active calderas are seldom associated with circumferential eruptive fissures, but eroded magmatic complexes reveal widespread circumferential dikes. This suggests that, while the conditions to emplace circumferential dikes are easily met, mechanisms must prevent them from reaching the surface. We explain this discrepancy with experiments of air injection into gelatin shaped as a volcano with caldera. Analog dikes show variable deflection, depending on the competition between overpressure, Pe, and topographic unloading, Pl; when Pl/Pe = 4.8-5.3, the dikes propagate orthogonal to the least compressive stress. Due to the unloading, they become circumferential and stall below the caldera rim; buoyancy is fundamental for the further rise and circumferential fissure development. Numerical models quantitatively constrain the stress orientation within the gelatin, explaining the observed circumferential dikes. Our results explain how dikes propagate below the rim of felsic and mafic calderas, but only in the latter they are prone to feed circumferential fissures.

  3. A geological and geophysical appraisal of the Baca geothermal field, Valles Caldera, New Mexico

    Science.gov (United States)

    Wilt, Michael; Vonder Haar, Stephen

    1986-03-01

    The Baca location #1 geothermal field is located in north-central New Mexico within the western half of the Plio-Pleistocene Valles Caldera. Steam and hot water are produced primarily from the northeast-trending Redondo Creek graben, where downhole temperatures exceed 260°C at depths of less than 2 km. Stratigraphically the reservoir region can be described as a five-layer sequence that includes Tertiary and Quaternary volcanic rocks, and Mesozoic and Tertiary sediments overlying Precambrian granitic basement. Production is mainly controlled by fractures and faults that are ultimately related to activity in the Rio Grande Rift system. Geophysically, the caldera is characterized by a gravity minimum and a resistivity low in its western half. A 40-mgal gravity minimum over the caldera is due mostly to the relatively low-density volcanics and sediments that fill the caldera and probably bears no relation to deep-seated magmatic sources. Two-dimensional gravity modeling indicates that the depth to Precambrian basement in Redondo Canyon is probably at least 3 km and may exceed 5 km in eastern parts of the caldera. Telluric and magnetotelluric surveys have shown that the reservoir region is associated with low resistivity and that a deep low-resistivity zone correlates well with the depth of the primary reservoir inferred from well data. Telluric and magnetotelluric data have also identified possible fault zones in the eastern and western sections of the production region that may form boundaries to the Redondo Creek reservoir. These data also suggest that the reservoir region is located at the intersection of lineaments that trend north-south and northeast-southwest. Magnetotelluric results indicate deep low resistivity at the western edge of the caldera which may be associated with deep hot fluids. On the basis of geophysical and well data, we make three estimates of reservoir dimensions. The estimates of the areal extent of the reservoir range from 10 to 30 km 2

  4. Dynamics of the Askja caldera landslide, July 2014, from seismic signal analysis

    Science.gov (United States)

    Schöpa, Anne; Burtin, Arnaud; Hovius, Niels; Green, Robert G.

    2016-04-01

    A voluminous landslide occurred at the Askja caldera in the Icelandic highlands on July 21st, 2014. The next day, flood marks of at least ten tsunami waves, that had reached the northern shore of the caldera lake, could be mapped out. The highest flood marks were found up to 60 m above the lake level close to famous tourist spots underlining the high hazard potential of the area. Since the landslide happened at night, no direct observations of the mass movement nor of the subsequent tsunami waves in the caldera lake were made. We present the analysis of seismic data from a network of 58 seismic stations that recorded data during the event. The seismic data give valuable information on the triggering, initiation, timing, and propagation of the landslide, with additional details on precursory signals before and oscillation waves in the caldera lake after the main landslide. From the set of seismic wave forms, characteristic features were extracted that could be used for early warning proposes. The seismic data reveals that the main slope failure along the southeastern caldera wall was a large, single event starting at 23.24 UTC. The main part of the energy was released in the first two minutes followed by smaller events, before the background noise level was re-established some 40 minutes after the main failure. Subsequent mass movements, much lower in amplitude, occurred during the following hours. About 20 minutes before the main failure, the background noise level started to rise. Ground velocities were up to three times higher that the background level with dominant frequencies between 2-4 Hz. The increase in background noise level is visible in stations up to 30 km away from the landslide area. This velocity increase is followed by a prominent velocity drop five minutes before the main failure. The spatial distribution of the velocity decrease with its centre at the detachment area of the landslide has an elliptical outline with a long axis oriented NE-SW. This

  5. Evolution of the Creede Caldera and its relation to mineralization in the Creede mining district, Colorado

    Science.gov (United States)

    Barton, Paul B.; Rye, Robert O.; Bethke, Philip M.

    2000-01-01

    At 25 Ma a major epithermal silver and base metal deposit formed in rhyolitic welded tuff near Creede, Colorado. Nearly 24000 metric tons of silver, appreciable lead, and small amounts of zinc, copper, and gold, have been produced from large, crustified veins under Bachelor and Bulldog Mountains north and northwest of Creede. Prior geologic, hydrologic, and stable-isotope studies showed that ore deposition was associated with the mixing and boiling of waters from diverse sources and suggester that a critical part of the ore-forming fluid may have originated within the ancient lake and sediments of the lacustrine Creede Formation that filled the Creede caldera. Two drill holes that sampled the heretofore hidden lower half of the Creede Formation are the focus of this book. The Creede caldera formed at 26.9 Ma within a high constructional plateau of silicic ashflows that covered and were sporadically interlayed with, intermediate lavas and lahars from large stratovolcanoes. The Creede caldera lake had an inflow evaporation balance that did not permit rapid filling to create a brim-full deep lake. Thus salts were evaporatively concentrated; but, with the exception of possible gypsum, no evaporite minerals preserved. Cool springs deposited travertine as mounds and contributed to limestone interlaminations within the sediment. The lake bottom was anoxic, and bacterial reduction of sulfate led to extreme sulfur isotopic fractionation in diagenetic pyrite. The caldera gradually resurged, converting the initial equant lake into an arcuate moat. Resurgent doming, alluvial fans, lacustrine sediments, ashfalls, and lava domes displaced water, lifted the lake so that it overlapped what later became the southern edge of the mineralized are, and eventually filled the basin. At 25.1 Ma an unseen pluton intruded beneath the northen part of the Creede district and created a convecting olume that drew in brine from the Creede caldera fill, meteotic water from highlands to the north

  6. Postcaldera volcanism and hydrothermal activity revealed by autonomous underwater vehicle surveys in Myojin Knoll caldera, Izu-Ogasawara arc

    Science.gov (United States)

    Honsho, Chie; Ura, Tamaki; Kim, Kangsoo; Asada, Akira

    2016-06-01

    Myojin Knoll caldera, one of the submarine silicic calderas lying on the volcanic front of the northern Izu-Ogasawara arc, has attracted increasing attention since the discovery of a large hydrothermal field called the Sunrise deposit. Although numerous submersible surveys have been conducted in Myojin Knoll caldera, they have not sufficiently explored areas to produce a complete picture of the caldera and understand the origin of the Sunrise deposit. We conducted comprehensive deep-sea surveys using an autonomous underwater vehicle and obtained high-resolution bathymetric and magnetic data and sonar images from ~70% of the caldera. The detailed bathymetric map revealed that faulting and magma eruptions, possibly associated with an inflation-deflation cycle of the magma reservoir during postcaldera volcanism, had generally occurred in the caldera wall. The main dome of the central cone was covered with lava flows and exhibits exogenous growth, which is unusual for rhyolitic domes. The magnetization distribution in the central cone indicates preferential magma intrusion along a NW-SE direction. It is presumed that magma migrated along this direction and formed a rhyolite dome at the foot of the southeastern caldera wall, where the Sunrise deposit occurs. The Sunrise deposit is composed mainly of three ridges extending in slope directions and covers ~400 × ~400 m. Magnetization reduction in the deposit area is small, indicating that the alteration zone beneath the Sunrise deposit is slanting rather than vertical. It is presumed that several slanting and near-vertical volcanic vents serve as pathways of hydrothermal fluid in Myojin Knoll caldera.

  7. A catastrophic flood caused by drainage of a caldera lake at Aniakchak Volcano, Alaska, and implications for volcanic hazards assessment

    Science.gov (United States)

    Waythomas, C.F.; Walder, J.S.; McGimsey, R.G.; Neal, C.A.

    1996-01-01

    Aniakchak caldera, located on the Alaska Peninsula of southwest Alaska, formerly contained a large lake (estimated volume 3.7 ?? 109 m3) that rapidly drained as a result of failure of the caldera rim sometime after ca. 3400 yr B.P. The peak discharge of the resulting flood was estimated using three methods: (1) flow-competence equations, (2) step-backwater modeling, and (3) a dam-break model. The results of the dam-break model indicate that the peak discharge at the breach in the caldera rim was at least 7.7 ?? 104 m3 s-1, and the maximum possible discharge was ???1.1 ?? 106 m3 s-1. Flow-competence estimates of discharge, based on the largest boulders transported by the flood, indicate that the peak discharge values, which were a few kilometers downstream of the breach, ranged from 6.4 ?? 105 to 4.8 ?? 106 m3 s-1. Similar but less variable results were obtained by step-backwater modeling. Finally, discharge estimates based on regression equations relating peak discharge to the volume and depth of the impounded water, although limited by constraining assumptions, provide results within the range of values determined by the other methods. The discovery and documentation of a flood, caused by the failure of the caldera rim at Aniakchak caldera, underscore the significance and associated hydrologic hazards of potential large floods at other lake-filled calderas.

  8. Using InSAR to investigate long term caldera unrest: case studies from Yellowstone and Long Valley

    Science.gov (United States)

    battaglia, maurizio

    2016-04-01

    Interpreting geodetic measurements can be particularly difficult in the case of slow, years-to-decades deformation, such as that commonly observed at large Quaternary silicic calderas. For example, Yellowstone caldera has shown a complex behavior over recent decades: uplift of resurgent domes within the caldera started sometime after 1923, reaching a total of 90 cm, but in 1984 the deformation reversed to subsidence at a rate of 1-2 cm/yr until 1992. Starting in 1992, the deformation began migrating from one resurgent dome to the other, and deformation was also detected along the caldera boundary - the so-called Northern Caldera Rim - starting in the mid-1990s. Evidence from geodetic surveys suggests that magma intrusion and/or pressurization of hydrothermal fluids may both drive uplift at Yellowstone. Geodetic measurements at Long Valley caldera have also revealed multiple episodes of caldera uplift, but in contrast to Yellowstone, deformation is largely restricted to the caldera's single resurgent dome. The fact that the energy released during the resurgent dome uplift is much larger than that which can be explained by seismic activity within and around the caldera, together with the observation that the onset of accelerated deformation precedes increases in earthquake activity by several weeks, suggests that the major source of caldera unrest is probably magma intrusion beneath the resurgent dome. Here we present time series of surface deformation for Yellowstone and Long Valley retrieved by applying the SBAS InSAR technique. We estimate the average regional deformation signal by using the mean velocity values derived from coherent SAR pixels belonging to areas outside the caldera. This tectonic signal is removed from the InSAR displacement and we modeled the InSAR, leveling, and gravity measurements to retrieve the best fitting source parameters. For Yellowstone caldera, different distinct sources, either hydrothermal or magmatic, have been intermittently

  9. The structural setting of the Ischia Island Caldera (Italy): first evidence from seismic and gravity data

    Science.gov (United States)

    Capuano, Paolo; De Matteis, Raffaella; Russo, Guido

    2015-09-01

    Ischia Island is one of the active volcanoes of the Neapolitan area (Italy). Hazard assessment of active, densely populated volcano is primarily based on knowledge of the volcano's past behaviour and of its present state. As a contribution to the definition of the present structural setting of Ischia Island, we constructed a new model of the shallow crust using geophysical data: seismic wave travel times and Bouguer anomaly data. We analysed these data sets through seismic tomography and gravity data inversion. The main results inferable from the 3D seismic and gravity images are the definition of the caldera rim along the perimeter of the island, as hypothesized by many authors, and the presence of a high velocity and density area inside the caldera consistent with extension of the resurgent block that characterizes the recent deformation of the island.

  10. Gradual caldera collapse at Bárdarbunga volcano, Iceland, regulated by lateral magma outflow.

    Science.gov (United States)

    Gudmundsson, Magnús T; Jónsdóttir, Kristín; Hooper, Andrew; Holohan, Eoghan P; Halldórsson, Sæmundur A; Ófeigsson, Benedikt G; Cesca, Simone; Vogfjörd, Kristín S; Sigmundsson, Freysteinn; Högnadóttir, Thórdís; Einarsson, Páll; Sigmarsson, Olgeir; Jarosch, Alexander H; Jónasson, Kristján; Magnússon, Eyjólfur; Hreinsdóttir, Sigrún; Bagnardi, Marco; Parks, Michelle M; Hjörleifsdóttir, Vala; Pálsson, Finnur; Walter, Thomas R; Schöpfer, Martin P J; Heimann, Sebastian; Reynolds, Hannah I; Dumont, Stéphanie; Bali, Eniko; Gudfinnsson, Gudmundur H; Dahm, Torsten; Roberts, Matthew J; Hensch, Martin; Belart, Joaquín M C; Spaans, Karsten; Jakobsson, Sigurdur; Gudmundsson, Gunnar B; Fridriksdóttir, Hildur M; Drouin, Vincent; Dürig, Tobias; Aðalgeirsdóttir, Guðfinna; Riishuus, Morten S; Pedersen, Gro B M; van Boeckel, Tayo; Oddsson, Björn; Pfeffer, Melissa A; Barsotti, Sara; Bergsson, Baldur; Donovan, Amy; Burton, Mike R; Aiuppa, Alessandro

    2016-07-15

    Large volcanic eruptions on Earth commonly occur with a collapse of the roof of a crustal magma reservoir, forming a caldera. Only a few such collapses occur per century, and the lack of detailed observations has obscured insight into the mechanical interplay between collapse and eruption. We use multiparameter geophysical and geochemical data to show that the 110-square-kilometer and 65-meter-deep collapse of Bárdarbunga caldera in 2014-2015 was initiated through withdrawal of magma, and lateral migration through a 48-kilometers-long dike, from a 12-kilometers deep reservoir. Interaction between the pressure exerted by the subsiding reservoir roof and the physical properties of the subsurface flow path explain the gradual, near-exponential decline of both collapse rate and the intensity of the 180-day-long eruption. PMID:27418515

  11. Ecology of Coyotes on the Valles Caldera National Preserve, New Mexico: Implications for Elk Calf Recruitment

    OpenAIRE

    Gifford, Suzanne J.

    2013-01-01

    Valles Caldera National Preserve (VCNP) managers were concerned about low elk recruitment observed at the same time as an apparent increase in sightings of coyotes and observations of coyote predation on elk calves. The goal of this study was to describe coyotes’ ecological interactions with elk, particularly coyote diet and movements on the Valle Grande, a large grassland meadow in the southeastern portion of the VCNP. We examined coyote diet by quantifying undigested remains of food item...

  12. Water budget in the Hakone caldera using hydrogen and oxygen isotope ratios

    International Nuclear Information System (INIS)

    The water budget of the Hakone caldera is estimated by using equations describing the balance of water, of stable isotope content and of dissolved chloride. Six equations with six unknowns are obtained, three for the lake and three for the catchment area. For the lake, computation gives that 58% of water inflow derives from groundwater and 42% from precipitation. Of the outflow, 88% consists of surface drainage and 12% of evaporation. (author)

  13. Dynamic magmatic processes at a continental rift caldera, observed using satellite geodesy

    Science.gov (United States)

    Lloyd, Ryan; Biggs, Juliet; Birhanu, Yelebe; Wilks, Matt; Gottsmann, Jo; Kendall, Mike; Lewi, Elias

    2016-04-01

    Large silicic calderas are a key feature of developing continental rifts, such as the Main Ethiopian Rift (MER), and are often observed to be deforming. Corbetti is one such example of a Holocene caldera in the MER that is undergoing deformation. However, the cause of the unrest, and the relationship to rift processes such as magma storage, transport and extension remain poorly understood. To investigate, we use InSAR (ascending and descending Cosmo-SkyMed data) and continuous GPS to observe the temporal and spatial evolution of sustained uplift at the Corbetti Caldera. Within the caldera, which was thought to have formed ~200 ka, there is evidence for numerous periods of resurgent volcanism in the form of plinian eruptions as well as effusive obsidian flows. How the sources of these varying styles of volcanism are reconciled at depth and in time is currently poorly constrained. Previous research has shown that pre-rift structures have a significant influence on the strain field, and hence on the magmatic and hydrothermal processes which drive it. The Cosmo-SkyMed data used in this study was specifically chosen such that each ascending image has a corresponding descending image acquired as contemporaneously as possible. This is necessary, given the rate of uplift, so as to reduce the number of assumptions when constructing time-series from multiple look directions, and when incorporating GPS data. We decompose the ascending and descending line-of-site deformation signals into vertical and east-west components and use finite source modeling to constrain the depth and geometry of the source of deformation. These results are then compared to available seismic, dynamic microgravity and magnetotelluric data to better understand this system, and how it is related to the volcanic hazard and local geothermal resources.

  14. Caldera formation and varied eruption styles on North Pacific seamounts: the clastic lithofacies record

    Science.gov (United States)

    Portner, Ryan A.; Clague, Dave A.; Paduan, Jennifer B.

    2014-08-01

    Detailed examination of volcaniclastic and sedimentary rocks collected from the Taney (30 Ma), President Jackson (4 Ma), Vance (3 Ma) and Alarcon (2 Ma) near-ridge seamount chains of the North Pacific reveals seven clastic lithofacies that record various modes of eruption, magma fragmentation, and particle dispersal. Lithofacies are distinguished by differences in lithology, bedding habit, compositional heterogeneity, and relationship to volcanic landforms. Breccia lithofacies were produced through mechanical fragmentation during caldera collapse (polymict) or effusive eruptions onto steep slopes (monomict). Rare globular lapilli mudstone lithofacies contain clasts with morphologies formed by magma-sediment mingling processes (peperite). Seamount summit pyroclastic deposits include proximal lapilli tuff with vesicular pyroclasts, and more distal limu o Pele tuff lithofacies. Much finer-grained hydrothermal mudstone/tuff lithofacies occurs around caldera rims and contains greenschist minerals, hydrothermal clays and basaltic ash that record subsurface phreatomagmatic fragmentation processes. Very fine-grained ash is transported to distal regions by oceanic currents and hydrothermal plumes, and is a component of the regional pelagic sediment budget. Pyroclastic lithofacies only occur on seamount summits suggesting formation during the latter stages of seamount evolution. As a seamount drifts away from an adjacent ridge axis and associated heat source, its magma supply is reduced allowing for magmatic gas buildup and mild explosive eruptions. During this stage, the diminished melt supply under the seamount is unable to fully compensate for extension along the ridge axis and vertical seamount growth. Lateral intrusion into spreading-related structures in this stage causes magma withdrawal and caldera formation. Formation of caldera ring faults also promotes seawater ingress into subseafloor hydrothermal cells, which interact with magma conduits causing phreatomagmatic

  15. Facies analysis of an ancient, dismembered, large caldera complex and implications for intra-arc subsidence: Middle Jurassic strata of Cobre Ridge, southern Arizona, USA

    Science.gov (United States)

    Riggs, Nancy R.; Busby-Spera, Cathy J.

    1991-11-01

    The Middle Jurassic (˜ 170 Ma) Cobre Ridge caldera is an elongate caldera complex that formed during the eruption of the tuff of Pajarito, a crystal-rich rhyodacite ignimbrite with an estimated volume > 1000 km 3. The caldera subsided in two subequal blocks: to the southeast, caldera-forming ignimbrite is as much as 3000 m thick, whereas the northwest half of the caldera subsided to lesser depths during the initial eruption, but was the locus of subsidence during subsequent eruptions, providing a depocenter for a > 1.5 km-thick section of secondary- and post-collapse volcanic and sedimentary strata. These strata record moat formation and filling and waning volcanism, including: (1) areally restricted ignimbrites up to several tens of meters thick that may have been ponded between caldera margins and/or fault scarps; (2) a ⩾ 600 m-thick ignimbrite whose eruption probably caused further collapse of the caldera or enlargement of the caldera margins; (3) a localized debris apron deposit up to 500 m thick that represents material reworked from intra-caldera pyroclastic deposits and possibly caldera walls; and (4) eolian and fluvial sandstones and water-lain tuffs. Megabreccia blocks as large as 0.5 km along strike probably demarcate approximate caldera margins, suggesting that the composite caldera was approximately 50 km long by 25 km wide. The preserved thickness of the strata of Cobre Ridge ( > 4500 m) is greater than many ancient continental volcanic sequences, suggesting external (i.e. tectonic) controls on subsidence, but preservation of this great thickness of strata is apparently due entirely to volcanic subsidence.

  16. Reconstructing the evoluortunity to study processes related to composite volction of an eroded Miocene caldera volcano (Yamanlar volcano, İzmir, Turkey)

    Science.gov (United States)

    Karaoğlu, Özgür; Brown, Richard J.

    2016-05-01

    The Miocene Yamanlar composite volcano is located in the central part of a shear zone in western Turkey. The volcano's deeply-eroded interior provides excellent three-dimensional exposure of a faulted caldera-floor and caldera-fill rocks as well as surrounding extracaldera ignimbrites. We present a much-revised stratigraphy and geological map of Yamanlar in order to quantify the evolutionary stages of the volcano. The Yamanlar volcanic cone was composed of > 800 m of basaltic-andesite to andesite lavas and lava domes. The volcano underwent at least one phase of caldera formation associated with an explosive eruption that deposited an ignimbrite sheet within and outside the caldera. Lithofacies architecture analysis is applied to the proximal and medial exposures of the Early-Middle Yamanlar Formation, which occurs outside of the caldera. Field evidence of the succession indicates a caldera-forming eruption. Our results indicate that the formation of the Yamanlar caldera resulted from one major catastrophic eruption that generated several sustained pyroclastic density currents (PDCs) subdivided by fall deposits with sharp contacts. The ignimbrite sheet is composed of four flow units. The presence of numerous coarse-grained lithic-rich horizons within the ignimbrite sheet is consistent with caldera subsidence. Post-caldera volcanism is indicated by intrusions and lava domes erupted along the inferred caldera-bounding faults, some of which record ~ 90 m of displacement. Widespread, coarse-grained breccias that overlie the ignimbrite sheet are interpreted as debris avalanche deposits resulting from gravitational failure of the flanks of the volcano or the caldera wall during or after caldera subsidence.

  17. Numerical models of caldera deformation: Effects of multiphase and multicomponent hydrothermal fluid flow

    Science.gov (United States)

    Hutnak, M.; Hurwitz, S.; Ingebritsen, S.E.; Hsieh, P.A.

    2009-01-01

    Ground surface displacement (GSD) in large calderas is often interpreted as resulting from magma intrusion at depth. Recent advances in geodetic measurements of GSD, notably interferometric synthetic aperture radar, reveal complex and multifaceted deformation patterns that often require complex source models to explain the observed GSD. Although hydrothermal fluids have been discussed as a possible deformation agent, very few quantitative studies addressing the effects of multiphase flow on crustal mechanics have been attempted. Recent increases in the power and availability of computing resources allow robust quantitative assessment of the complex time-variant thermal interplay between aqueous fluid flow and crustal deformation. We carry out numerical simulations of multiphase (liquid-gas), multicomponent (H 2O-CO2) hydrothermal fluid flow and poroelastic deformation using a range of realistic physical parameters and processes. Hydrothermal fluid injection, circulation, and gas formation can generate complex, temporally and spatially varying patterns of GSD, with deformation rates, magnitudes, and geometries (including subsidence) similar to those observed in several large calderas. The potential for both rapid and gradual deformation resulting from magma-derived fluids suggests that hydrothermal fluid circulation may help explain deformation episodes at calderas that have not culminated in magmatic eruption.

  18. Uplift and magma intrusion at Long Valley caldera from InSAR and gravity measurements

    Science.gov (United States)

    Tizzani, Pietro; Battaglia, Maurizio; Zeni, Giovanni; Atzori, Simone; Berardino, Paolo; Lanari, Riccardo

    2009-01-01

    The Long Valley caldera (California) formed ~760,000 yr ago following the massive eruption of the Bishop Tuff. Postcaldera volcanism in the Long Valley volcanic field includes lava domes as young as 650 yr. The recent geological unrest is characterized by uplift of the resurgent dome in the central section of the caldera (75 cm in the past 33 yr) and earthquake activity followed by periods of relative quiescence. Since the spring of 1998, the caldera has been in a state of low activity. The cause of unrest is still debated, and hypotheses range from hybrid sources (e.g., magma with a high percentage of volatiles) to hydrothermal fluid intrusion. Here, we present observations of surface deformation in the Long Valley region based on differential synthetic aperture radar interferometry (InSAR), leveling, global positioning system (GPS), two-color electronic distance meter (EDM), and microgravity data. Thanks to the joint application of InSAR and microgravity data, we are able to unambiguously determine that magma is the cause of unrest.

  19. Surface Deformation of Los Humeros Caldera, Mexico, Estimated by Interferometric Synthetic Aperture Radar (InSAR).

    Science.gov (United States)

    Santos Basurto, R.; Lopez Quiroz, P.; Carrasco Nuñez, G.; Doin, M. P.

    2014-12-01

    Los Humeros caldera is located in the eastern part of the Trans-Mexican Volcanic Belt, to the north of the state of Puebla and bordering the west side of the state of Veracruz. The study of the caldera, is of great interest because there is a geothermal field currently working inside of it. In fact, Los Humeros, is the third more important geothermal field in Mexico. In this work, we used InSAR to estimate the surface deformation on the caldera, aiming to contribute to its modeling and to help preventing subsidence related hazards on the geothermal field and surroundings. On this study, we calculated 34 interferograms from 21 SAR images of the ENVISAT European Space Agency Mission. The analysis of the interferograms, allow us to detect, decorrelation of the interferometric signal increased, when time spans were greater than 70 days. Also, for those with good signal correlation, the atmospheric signal dominated the interferogram, masking completely the deformation. Moreover, residual orbital ramps were detected, in some of the calculated interferograms. An algorithm capable to remove all the interferogram signal contributions but the deformation related, has been implemented. Resulting deformation and its correlation with several variables like the geology, the hydrogeology and the seismic records, were analysed through its integration in a Geographic Information System.

  20. Imaging hydrothermal systems at Furnas caldera (Azores, Portugal): Insights from Audio-Magnetotelluric data

    Science.gov (United States)

    Hogg, Colin; Kiyan, Duygu; Rath, Volker; Byrdina, Svetlana; Vandemeulebrouck, Jean; Silva, Catarina; Viveiros, Maria FB; Ferreira, Teresa

    2016-04-01

    The Furnas volcano is the eastern-most of the three active central volcanoes of Sao Miguel Island. The main caldera formed about 30 ka BP, followed by a younger eruption at 10-12 ka BP, which forms the steep topography of more than 200 m in the measuring area. It contains several very young eruptive centers, and a shallow caldera lake. Tectonic features of varying directions have been identified in the Caldera and its vicinity. In the northern part of the caldera, containing the fumarole field of Caldeiras das Furnas, a detailed map of surface CO2 emissions was recently made available. In 2015, a pilot survey of 13 AudioMagnetoTelluric soundings (AMT) and Electrical Resistivity Tomography (ERT) data were collected along two profiles in the eastern part of Furnas caldera in order to image the electrical conductivity of the subsurface. The data quality achieved by both techniques is extraordinary and first results indicate a general correlation between regions of elevated conductivity and the mapped surface CO2 emissions, suggesting that they may both be caused by the presence hydrothermal fluids. Tensor decomposition analysis using the Groom-Bailey approach produce a generalised geo-electric strike direction, 72deg East of North, for the AMT data compared to the surface geological strike derived from the major mapped fault crossing the profiles of 105deg. An analysis of the real induction arrows at certain frequencies (at depths greater than 350 m) infer that an extended conductor at depth does not exactly correspond to the degassing structures at the surface and extends outside the area of investigation. The geometry of the most conductive regions with electrical conductivities less then1 Ώm found at various depths differ from what was expected from earlier geologic and tectonic studies and possibly may not be directly related to the mapped fault systems at the surface. On the eastern profile, which seemed to be more appropriate for 2-D modelling with 72deg strike

  1. Volcano hazards implications of rhyolitic melt or magma at shallow depth under Krafla Caldera

    Science.gov (United States)

    Eichelberger, John; Papale, Paolo; Sigmundsson, Freysteinn

    2014-05-01

    Krafla Caldera in northern Iceland is a well-monitored and extensively drilled caldera system that underwent a major rifting and eruption episode in 1975 to 1984. The recent surprise discovery of ~900oC "magma" (crystal+melt felsite and possibly crystal-poor rhyolite magma as well) in the Iceland Deep Drilling Project borehole #1 (IDDP-1) in 2009, as well as previous less publicized drilling encounters with rhyolite melt, challenges our understanding of caldera unrest. Further drilling may lead to improved understanding of volcanic hazards in calderas and better interpretation of precursory deformation and seismic signals that may herald eruption. Salient features of the IDDP-1 discovery relative to volcanic hazards are: 1. The rhyolite magma is at only 2.1 km depth. If such magma were known to have intruded to such shallow depth in a populated caldera, there would likely be serious discussion of evacuating the population. 2. The drill site was chosen because magma was not expected at shallow depth, based on the occurrence of seismicity to twice that depth beneath the site during the last eruption, and on 3-D resistivity structure. 3. The eruption was entirely basaltic; no rhyolite reached the surface. Thus, rhyolite magma intruded to shallow depth and was stored there without erupting and without being detected either geophysically or petrologically. An alternative, which seems unlikely, is that the rhyolite evolved from basalt or by basalt-induced partial melting after 1984. If it is possible to return to this magmatic body through further drilling, as recently proposed to the International Continental Scientific Drilling Program (ICDP) by the Krafla Magma Drilling Project, complementary field, laboratory experiments, and computational experiments can be conducted to understand the "source" and how it produces deformation, seismic, and geochemical signals at the surface. Experiments could include injection of fluid with tracers directly into the melt-bearing zone

  2. History of surface displacements at the Yellowstone Caldera, Wyoming, from leveling surveys and InSAR observations, 1923-2008

    Science.gov (United States)

    Dzurisin, Daniel; Wicks, Charles W.; Poland, Michael P.

    2012-01-01

    Modern geodetic studies of the Yellowstone caldera, Wyoming, and its extraordinary tectonic, magmatic, and hydrothermal systems date from an initial leveling survey done throughout Yellowstone National Park in 1923 by the U.S. Coast and Geodetic Survey. A repeat park-wide survey by the U.S. Geological Survey (USGS) and the University of Utah during 1975-77 revealed that the central part of the caldera floor had risen more than 700 mm since 1923, at an average rate of 14±1 mm/yr. From 1983 to 2007, the USGS conducted 15 smaller surveys of a single level line that crosses the northeast part of the caldera, including the area where the greatest uplift had occurred from 1923 to 1975-77. The 1983 and 1984 surveys showed that uplift had continued at an average rate of 22±1 mm/yr since 1975-77, but no additional uplift occurred during 1984-85 (-2±5 mm/yr), and during 1985-95 the area subsided at an average rate of 19±1 mm/yr. The change from uplift to subsidence was accompanied by an earthquake swarm, the largest ever recorded in the Yellowstone area (as of March 2012), starting in October 1985 and located near the northwest rim of the caldera. Interferometric synthetic aperture radar (InSAR) images showed that the area of greatest subsidence migrated from the northeast part of the caldera (including the Sour Creek resurgent dome) during 1992-93 to the southwest part (including the Mallard Lake resurgent dome) during 1993-95. Thereafter, uplift resumed in the northeast part of the caldera during 1995-96, while subsidence continued in the southwest part. The onset of uplift migrated southwestward, and by mid-1997, uplift was occurring throughout the entire caldera (essentially rim to rim, including both domes). Consistent with these InSAR observations, leveling surveys indicated 24±3 mm of uplift in the northeast part of the caldera during 1995-98. The beginning of uplift was coincident with or followed shortly after an earthquake swarm near the north caldera rim

  3. Is there a geochemical link between volcanic and plutonic rocks in the Organ Mountains caldera?

    Science.gov (United States)

    Memeti, V.; Davidson, J.

    2013-12-01

    Results from separate volcanic and plutonic studies have led to inconsistent conclusions regarding the origins and thus links between volcanic and plutonic systems in continental arcs and the magmatic processes and time scales responsible for their compositional variations. Some have suggested that there is a geochemical and geochronological disconnect between volcanic and plutonic rocks and hence have questioned the existence of magma mush columns beneath active volcanoes. Investigating contemporary volcanic and plutonic rocks that are spatially connected is thus critical in exploring these issues. The ca. 36 Ma Organ Mountains caldera in New Mexico, USA, represents such a system exposing contemporaneous volcanic and plutonic rocks juxtaposed at the surface due to tilting during extensional tectonics along the Rio Grande Rift. Detailed geologic and structural mapping [1] and 40Ar/39Ar ages of both volcanics and plutons [2] demonstrate the spatial and temporal connection of both rock types with active magmatism over >2.5 myr. Three caldera-forming ignimbrites erupted within 600 kyr [2] from this system with a total erupted volume of 500-1,000 km3 as well as less voluminous pre- and post-caldera trachyte and andesite lavas. The ignimbrite sequence ranges from a crystal-poor, high-SiO2 rhyolite at the base to a more crystal-rich, low-SiO2 rhyolite at the top. Compositional zoning with quartz-monzonite at the base grading to syenite and alaskite at the top is also found in the Organ Needle pluton, the main intrusion, which is interpreted to be the source for the ignimbrites [1]. Other contemporaneous and slightly younger plutons have dioritic to leucogranitic compositions. We examined both volcanic and plutonic rocks with petrography and their textural variations with color cathodoluminescence, and used whole rock element and Sr, Nd and Pb isotope geochemistry to constrain magma compositions and origins. Electron microprobe analyses on feldspars have been completed to

  4. Geology and complex collapse mechanisms of the 3.72 Ma Hannegan caldera, North Cascades, Washington, USA

    Science.gov (United States)

    Tucker, D.; Hildreth, W.; Ullrich, T.; Friedman, R.

    2007-01-01

    Contiguous ring faults of the 8 ?? 3.5 km Hannegan caldera enclose the Hannegan volcanics in the Cascade arc of northern Washington. The caldera collapsed in two phases, which each erupted rhyolitic ignimbrite (72.3%-75.2% SiO2). The first collapse phase, probably trap-door style, erupted the ???900-m-thick ignimbrite of Hannegan Peak at 3.722 ?? 0.020 Ma. This single cooling unit, generally welded, has an uppermost facies of nonwelded ignimbrite and fine ash. A short period of localized sedimentation followed. Eruption of the ignimbrite of Ruth Mountain then led to a second trap-door collapse as the first-phase partial ring fault propagated to the south to completely enclose the caldera. Wallrock breccias are intercalated as lenses and megabreccia blocks in both ignimbrites. The minimum intracaldera volume is 55-60 km3. No base is exposed, nor are outflow sheets preserved. Caldera collapse and glacial erosion have removed precaldera volcanic rocks, which survive only as intracaldera breccias. Rhyolite dikes and pods, one of which yielded a 40Ar/39Ar age of 3.72 ?? 0.34 Ma, intrude the ring fault and caldera fill. Dacite-andesite domes, dikes, and lava flows were emplaced subsequently; one lava flow gives a 40Ar/39Ar age of 2.96 ?? 0.20 Ma. The quartz diorite of Icy Peak and the granite of Nooksack Cirque (plutons with 206Pb/238U zircon ages of 3.42 ?? 0.10 Ma and 3.36 ?? 0.20 Ma, respectively) intrude caldera fill and basement rocks on the southwest margin of the caldera. Both plutons are now exceptionally well expose on high, glacially sculpted peaks within the caldera, indicating erosion of at least 1 km of intracaldera fill. Hannegan caldera anchors the northeast end of a linear NE-SW age-progressive migration of magmatic focus from the Chilliwack batholith to the active Mount Baker volcano. ?? 2006 Geological Society of America.

  5. Conductive heat flux in VC-1 and the thermal regime of Valles caldera, Jemez Mountains, New Mexico ( USA).

    Science.gov (United States)

    Sass, J.H.; Morgan, P.

    1988-01-01

    Over 5% of heat in the western USA is lost through Quaternary silicic volcanic centers, including the Valles caldera in N central New Mexico. These centers are the sites of major hydrothermal activity and upper crustal metamorphism, metasomatism, and mineralization, producing associated geothermal resources. Presents new heat flow data from Valles caldera core hole 1 (VC-1), drilled in the SW margin of the Valles caldera. Thermal conductivities were measured on 55 segments of core from VC-1, waxed and wrapped to preserve fluids. These values were combined with temperature gradient data to calculate heat flow. Above 335 m, which is probably unsaturated, heat flow is 247 + or - 16 mW m-2. Inteprets the shallow thermal gradient data and the thermal regime at VC-1 to indicate a long-lived hydrothermal (and magmatic) system in the southwestern Valles caldera that has been maintained through the generation of shallow magma bodies during the long postcollapse history of the caldera. High heat flow at the VC-1 site is interpreted to result from hot water circulating below the base of the core hole, and we attribute the lower heat flow in the unsaturated zone is attributed to hydrologic recharge. -from Authors

  6. The Laramide Mesa formation and the Ojo de Agua caldera, southeast of the Cananea copper mining district, Sonora, Mexico

    Science.gov (United States)

    Cox, Dennis P.; Miller, Robert J.; Woodbourne, Keith L.

    2006-01-01

    The Mesa Formation extends from Cananea, Mexico, southeast to the Sonora River and is the main host rock of Laramide porphyry copper deposits in the Cananea District and at the Alacran porphyry prospect to the east. The Mesa consists of two members-a lower andesite and an upper dacite. The lowest part of the dacite member is a crystal tuff about 100 m thick. This tuff is the outfall of a caldera centered near the village of Ojo de Agua, dated by 40Ar/39Ar at 65.8 Ma ?0.4. The Ojo de Agua Caldera is about 9 km in diameter and is filled by a light gray biotite dacite tuff with abundant flattened pumice fragments. The volume of the caldera is estimated to be 24 km3.

  7. Can we see the distal dyke communicate with the caldera? Examples of temporal correlation analysis using seismicity from the Bárðarbunga volcano

    Science.gov (United States)

    Jónsdóttir, Kristín; Jónasson, Kristján; Tumi Guðmundsson, Magnús; Hensch, Martin; Hooper, Andrew; Holohan, Eoghan; Sigmundsson, Freysteinn; Halldórsson, Sæmundur Ari; Vogfjörð, Kristín; Roberts, Matthew; Barsotti, Sara; Ófeigsson, Benedikt; Hjörleifsdóttir, Vala; Magnússon, Eyjólfur; Pálsson, Finnur; Parks, Michelle; Dumont, Stephanie; Einarsson, Páll; Guðmundsson, Gunnar

    2016-04-01

    The Bárðarbunga volcano is composed of a large oval caldera (7x11 km) and fissures extending tens of kilometers away from the caldera along the rift zone, which marks the divergent plate boundary across Iceland. On August 16th, 2014 an intense seismic swarm started below the Bárðarbunga caldera and in the two weeks that followed a dyke migrated some 47 km laterally in the uppermost 6-10 km of the crust along the rift. The dyke propagation terminated in lava fields just north of Vatnajökull glacier, where a major (1.5 km3) six months long eruption took place. Intense earthquake activity in the caldera started in the period August 21-24 with over 70 M5 earthquakes accompanying slow caldera collapse, as verified by various geodetic measurements. The subsidence is likely due to magma withdrawal from a reservoir at depth beneath the caldera. During a five months period, October-February, the seismic activity was separated by over 30 km in two clusters; one along the caldera rims (due to piecewise caldera subsidence) and the other at the far end of the dyke (as a result of small shear movements). Here we present statistical analysis comparing the temporal behaviour of seismicity recorded in the two clusters. By comparing the earthquake rate in the dyke in temporal bins before and after caldera subsidence earthquakes to the rate away from these bins (background rate), we show posing a statistical p-value test, that the number of dyke earthquakes was significantly higher (p earthquake (>M4.6) in the caldera. Increased dyke seismicity was also observed 0-3 hours following a large caldera earthquake. Elevated seismicity in the dyke before a large caldera earthquake may occur when a constriction in the dyke was reduced, followed by pressure drop in the chamber. Assuming that the large caldera earthquakes occurred when chamber pressure was lowest, the subsiding caldera piston may have caused temporary higher pressure in the dyke and thereby increased the likelihood of an

  8. Can we see the distal dyke communicate with the caldera? Examples of temporal correlation analysis using seismicity from the Bárðarbunga volcano

    Science.gov (United States)

    Jónsdóttir, Kristín; Jónasson, Kristján; Tumi Guðmundsson, Magnús; Hensch, Martin; Hooper, Andrew; Holohan, Eoghan; Sigmundsson, Freysteinn; Halldórsson, Sæmundur Ari; Vogfjörð, Kristín; Roberts, Matthew; Barsotti, Sara; Ófeigsson, Benedikt; Hjörleifsdóttir, Vala; Magnússon, Eyjólfur; Pálsson, Finnur; Parks, Michelle; Dumont, Stephanie; Einarsson, Páll; Guðmundsson, Gunnar

    2016-04-01

    The Bárðarbunga volcano is composed of a large oval caldera (7x11 km) and fissures extending tens of kilometers away from the caldera along the rift zone, which marks the divergent plate boundary across Iceland. On August 16th, 2014 an intense seismic swarm started below the Bárðarbunga caldera and in the two weeks that followed a dyke migrated some 47 km laterally in the uppermost 6-10 km of the crust along the rift. The dyke propagation terminated in lava fields just north of Vatnajökull glacier, where a major (1.5 km3) six months long eruption took place. Intense earthquake activity in the caldera started in the period August 21-24 with over 70 M5 earthquakes accompanying slow caldera collapse, as verified by various geodetic measurements. The subsidence is likely due to magma withdrawal from a reservoir at depth beneath the caldera. During a five months period, October-February, the seismic activity was separated by over 30 km in two clusters; one along the caldera rims (due to piecewise caldera subsidence) and the other at the far end of the dyke (as a result of small shear movements). Here we present statistical analysis comparing the temporal behaviour of seismicity recorded in the two clusters. By comparing the earthquake rate in the dyke in temporal bins before and after caldera subsidence earthquakes to the rate away from these bins (background rate), we show posing a statistical p-value test, that the number of dyke earthquakes was significantly higher (p M4.6) in the caldera. Increased dyke seismicity was also observed 0-3 hours following a large caldera earthquake. Elevated seismicity in the dyke before a large caldera earthquake may occur when a constriction in the dyke was reduced, followed by pressure drop in the chamber. Assuming that the large caldera earthquakes occurred when chamber pressure was lowest, the subsiding caldera piston may have caused temporary higher pressure in the dyke and thereby increased the likelihood of an earthquake

  9. Ignimbrite Analyses of Batur Caldera, Bali, based on 14C Dating

    Directory of Open Access Journals (Sweden)

    Igan S. Sutawidjaja

    2014-06-01

    Full Text Available http://dx.doi.org/10.17014/ijog.vol4no3.20094The Batur Caldera, in the northeastern part of Bali Island, is an elliptical collapse structure 13.8 by 10 km in size and another circular composite collapse structure with a diameter of 7.5 km in its centre. Two stages of the collapse were interrupted by silicic andesite lavas and domes. The first collapse was initiated by the eruption of about 84 km3 of the dacitic "Ubud Ignimbrite", about 29,300 years B.P., which caused a steep-walled depression about 1 km deep. The second ignimbrite was erupted from a large crater about the present lake, and it  produced about 19 km3 of a similar voluminous dacitic ignimbrite, called the "Gunungkawi Ignimbrite" about 20,150 years B.P. This second eruption trig- gered a second collapse, which created the central circular caldera, and formed a basin structure. Both the Ubud and Gunungkawi Ignimbrites consist of a similar dacitic composition, white to red (the most abundant nearly 90 % and dark grey to black dacitic pumice clasts. The large clasts, up to 20 cm in diameter, are in the non-welded ignimbrite, particularly in the upper part of the Gunungkawi Ignimbrite. The intracaldera ignimbrite, called the "Batur Ignimbrite" about 5 km3  in volume is a densely welded ignimbrite and generally shows typical welded features. The ignimbrite comprises at least five different flow units, separated by thin (15 - 40 cm welded pumiceous airfall deposits, with flattened pumice clasts. Another large eruption occurred about 5,500 years B.P., producing around 0.09 km3  andesitic ignimbrite. This was initiated by phreatomagmatic eruptions, indicated by thick phreatomagmatic and surge deposits, underlying the ignimbrite. The caldera and its vicinity are partly filled, and variably mantled by later eruptive products of dacitic and andesitic phreatomagmatic and airfall deposits.  

  10. Insight into Vent Opening Probability in Volcanic Calderas in the Light of a Sill Intrusion Model

    Science.gov (United States)

    Giudicepietro, Flora; Macedonio, G.; D'Auria, L.; Martini, M.

    2016-05-01

    The aim of this paper is to discuss a novel approach to provide insights on the probability of vent opening in calderas, using a dynamic model of sill intrusion. The evolution of the stress field is the main factor that controls the vent opening processes in volcanic calderas. On the basis of previous studies, we think that the intrusion of sills is one of the most common mechanism governing caldera unrest. Therefore, we have investigated the spatial and temporal evolution of the stress field due to the emplacement of a sill at shallow depth to provide insight on vent opening probability. We carried out several numerical experiments by using a physical model, to assess the role of the magma properties (viscosity), host rock characteristics (Young's modulus and thickness), and dynamics of the intrusion process (mass flow rate) in controlling the stress field. Our experiments highlight that high magma viscosity produces larger stress values, while low magma viscosity leads to lower stresses and favors the radial spreading of the sill. Also high-rock Young's modulus gives high stress intensity, whereas low values of Young's modulus produce a dramatic reduction of the stress associated with the intrusive process. The maximum intensity of tensile stress is concentrated at the front of the sill and propagates radially with it, over time. In our simulations, we find that maximum values of tensile stress occur in ring-shaped areas with radius ranging between 350 m and 2500 m from the injection point, depending on the model parameters. The probability of vent opening is higher in these areas.

  11. Survey and assessment of post volcanic activities of a young caldera lake, Lake Cuicocha, Ecuador

    Directory of Open Access Journals (Sweden)

    G. Gunkel

    2009-05-01

    Full Text Available Cuicocha is a young volcano adjacent to the inactive Pleistocene Cotacachi volcano complex, located in the western cordilleras of the Ecuadorian Andes. A series of eruptions with intensive ash emission and collapse of the caldera occurred around 4500–3000 y BP. A crater 3.2 km in diameter and a maximum depth of 450 m was formed. Further eruptions of the volcano occurred 1300 y BP and formed four smaller domes within the caldera. Over the last few hundred years, a caldera lake has developed, with a maximum depth of 148 m. The lake water is characterized by sodium carbonate with elevated concentrations of manganese, calcium and chloride. Nowadays, an emission of gases, mainly CO2, and an input of warm spring water occur in Lake Cuicocha. The zone of high activity is in the western basin of the lake at a depth of 78 m, and continuous gas emissions with sediment resuspension were observed using sonar. In the hypolimnion of the lake, CO2 accumulation occurs up to 0.2% saturation, but the risk of a limnic eruption can be excluded at present. The lake possesses monomictic stratification behaviour, and during overturn an intensive gas exchange with the atmosphere occurs. Investigations concerning the sedimentation processes of the lake suggest only a thin sediment layer of up to 10–20 cm in the deeper lake basin; in the western bay, in the area of gas emissions, the lake bottom is partly depleted of sediment in the form of holes, and no lake colmation exists. Decreases in the lake water level of about 30 cm y−1 indicate a percolation of water into fractures and fissures of the volcano, triggered by a nearby earthquake in 1987.

  12. A fluid-driven earthquake swarm on the margin of the Yellowstone caldera

    Science.gov (United States)

    Shelly, David R.; Hill, David P.; Massin, Frederick; Farrell, Jamie; Smith, Robert B.; Taira, Taka'aki

    2013-01-01

    Over the past several decades, the Yellowstone caldera has experienced frequent earthquake swarms and repeated cycles of uplift and subsidence, reflecting dynamic volcanic and tectonic processes. Here, we examine the detailed spatial-temporal evolution of the 2010 Madison Plateau swarm, which occurred near the northwest boundary of the Yellowstone caldera. To fully explore the evolution of the swarm, we integrated procedures for seismic waveform-based earthquake detection with precise double-difference relative relocation. Using cross-correlation of continuous seismic data and waveform templates constructed from cataloged events, we detected and precisely located 8710 earthquakes during the three-week swarm, nearly four times the number of events included in the standard catalog. This high-resolution analysis reveals distinct migration of earthquake activity over the course of the swarm. The swarm initiated abruptly on January 17, 2010 at about 10 km depth and expanded dramatically outward (both shallower and deeper) over time, primarily along a NNW-striking, ~55º ENE-dipping structure. To explain these characteristics, we hypothesize that the swarm was triggered by the rupture of a zone of confined high-pressure aqueous fluids into a pre-existing crustal fault system, prompting release of accumulated stress. The high-pressure fluid injection may have been accommodated by hybrid shear and dilatational failure, as is commonly observed in exhumed hydrothermally affected fault zones. This process has likely occurred repeatedly in Yellowstone as aqueous fluids exsolved from magma migrate into the brittle crust, and it may be a key element in the observed cycles of caldera uplift and subsidence.

  13. Remoción de níquel, cadmio y zinc del agua, utilizando clinoptilolita heulandita

    Directory of Open Access Journals (Sweden)

    Thelma B. Pavón Silva

    2000-01-01

    Full Text Available Se aplica el proceso de intercambio iónico con una zeolita natural obtenida en Taxco, Guerrero, México, para la remoción de Zn, Cd y Ni de soluciones acuosas. Para este proceso, el mineral se homoionizó con cloruro de sodio y posteriormente se puso en contacto con soluciones 0.01 N de sales de nitratos de Zn, Cd y Ni, durante 8 días.

  14. Mecanismo de falla de los tubos del sobrecalentador de una caldera acuotubular

    OpenAIRE

    Coronado Marín, John Jairo

    2010-01-01

    En este artículo se investigaron las causas de las fallas presentadas por fisuración longitudinal a partir de la superficie externa en los tubos del sobrecalentador de una caldera acuotubular. La superficie externa de los tubos presentó una capa de color blanco-rojizo que presentó cadenas parafínicas: C-H, grupos funcionales: C-O, N-H y compuestos de azufre, esta capa frágil impide la transferencia de calor, causando un aumento de temperatura del tubo. La falla se presentó por termofluencia d...

  15. A seismological perspective of the shallow magma and hydrothermal systems under Kilauea Caldera

    Science.gov (United States)

    Chouet, B. A.; Dawson, P. B.

    2011-12-01

    The past 20 years have seen great strides in our understanding of Kilauea Volcano, in large part due to technological developments and improvements in seismological instrumentation, which now allow the surface effects of subterranean volcanic processes to be imaged in unprecedented detail. High-resolution tomography provided an image of 3D velocity anomalies down to a scale of a few hundred meters, providing indirect evidence for the presence of reservoirs under the summit region of Kilauea. A sharper image of a shallow hydrothermal reservoir under Kilauea Caldera was obtained from frequency-slowness analyses of long-period (LP) seismicity recorded on three small-aperture seismic antennas deployed in the summit caldera. Located within the top 500 m below the caldera floor and extending ~0.6 km and ~1 km in the east-west and north-south directions, this hydrothermal reservoir broadly overlaps the east wall of the Halemaumau pit crater. Further evidence of hydrothermal processes within this zone was obtained from a study of a well-recorded LP event, indicating a source mechanism consistent with the resonance of a horizontal steam-filled crack at a depth of ~150 m near the eastern rim of Halemaumau. Recurring very-long-period (VLP) signals originating in the repeated activation of a compact source region near sea level immediately beneath this hydrothermal reservoir have allowed a gradually emerging view of the shallowest segment of the magma transport pathway under the caldera. Further elaboration of our image of the magma pathway structure, made possible through detailed modeling of VLP signals accompanying degassing activity at a new vent formed in Halemaumau in March 2008, points to a dominant dike segment in the form of a nearly vertical east-trending dike. The inferred dike features a ~20° clockwise rotation in strike under the east edge of Halemaumau, where it intersects a sub-vertical north-striking dike. The triple junction made by the intersection of the

  16. High-resolution aeromagnetic survey of the Mono Basin-Long Valley Caldera region, California

    Science.gov (United States)

    Ponce, D. A.; Mangan, M.; McPhee, D.

    2013-12-01

    A new high-resolution aeromagnetic survey of the Mono Basin-Long Valley Caldera region greatly enhances previous magnetic interpretations that were based on older, low-resolution, and regional aeromagnetic data sets and provides new insights into volcano-tectonic processes. The surveyed area covers a 8,750 km2 NNW-trending swath situated between the Sierra Nevada to the west and the Basin and Range Province to the east. The surveyed area includes the volcanic centers of Mono Lake, Mono-Inyo Craters, Mammoth Mountain, Devils Postpile, and Long Valley Caldera. The NW-trending eastern Sierra frontal fault zone crosses through the study area, including the active Mono Lake, Silver Lake, Hartley Springs, Laurel Creek, and Hilton Creek faults. Over 6,000 line-kilometers of aeromagnetic data were collected at a constant terrain clearance of 150 m, a flight-line spacing of 400 m, and a tie-line spacing of 4 km. Data were collected via helicopter with an attached stinger housing a magnetic sensor using a Scintrex CS-3 cesium magnetometer. In the northern part of the survey area, data improve the magnetic resolution of the individual domes and coulees along Mono Craters and a circular shaped magnetic anomaly that coincides with a poorly defined ring fracture mapped by Kistler (1966). Here, aeromagnetic data combined with other geophysical data suggests that Mono Craters may have preferentially followed a pre-existing plutonic basement feature that may have controlled the sickle shape of the volcanic chain. In the northeastern part of the survey, aeromagnetic data reveal a linear magnetic anomaly that correlates with and extends a mapped fault. In the southern part of the survey, in the Sierra Nevada block just south of Long Valley Caldera, aeromagnetic anomalies correlate with NNW-trending Sierran frontal faults rather than to linear NNE-trends observed in recent seismicity over the last 30 years. These data provide an important framework for the further analysis of the

  17. Hydrothermal precious-metal deposits related to graben-calderas of the Sierra Madre Occidental

    Science.gov (United States)

    Aguirre-Diaz, G. J.; Labarthe-Hernandez, G.; Nieto-Obregon, J.; Tristan-Gonzalez, M.; Gonzalez-Partida, E.

    2007-05-01

    The Sierra Madre Occidental (SMO) covers the NW portion of Mexico and it is the host for several important precious metal mine operations, such as Tayoltita, Cienega, Topia, Fresnillo, Zacatecas, Guanajuato and Bolaños, just to mention a few. The southern part of the Basin and Range extension affected also NW Mexico and formed NW- to NE-trending normal faults that bound many large grabens, which are particularly long and deep in the southern SMO. Both graben formation and mid-Tertiary silicic volcanic activity coincided in space and time, particularly for the 38-23 Ma period, the Ignimbrite Flare-up event, but this activity dates back to Eocene and was as young as Miocene. This volcanism included large rhyolitic domes, too. At the southern SMO, the vents of this silicic volcanism are related to graben's master faults and we have named them graben-calderas. Evidences include large pyroclastic dikes and post-ignimbrite aligned rhyolitic domes and lava dikes. All these features were found along the graben-caldera walls or on the graben's shoulders. Some of these vents are related to gold and silver hydrothermal mineralization. In most cases a paleo-lake filled the graben-caldera for a period of time, either during the ignimbrite emplacement or after it. Some of the graben-caldera ignimbrites were deposited in subaqueous environments and post-ignimbrite rhyolitic domes and dikes were intruded in non-consolidated water-saturated tuffs or sedimentary deposits. This lacustrine environment provided the necessary water for the hydrothermal system. The combination of all these factors in space and time, grabens+volcanism+water, resulted in the development of precious-metal hydrothermal ore deposits. Bolaños mine in the Bolaños graben represent our case-study, but we have confirmed the same tectono-volcanic-lake relationship at other mine-districts along the SMO. We conclude that locating the fissural vents of the silicic ignimbrites by means of just geologic mapping is be

  18. Geochemical Clues on the Processes Controlling the 2005-2014 Unrest at Campi Flegrei Caldera, Italy

    Science.gov (United States)

    Chiodini, G.; Vandemeulebrouck, J.; Caliro, S.; D'auria, L.; De Martino, P.; Mangiacapra, A.; Petrillo, Z.

    2014-12-01

    The understanding of the mechanism which triggers unrests at active calderas is one of the most problematic issues of modern volcanology. In particular, magmatic intrusion vs. hydrothermal dynamics is one of the central questions to understand the signals of several restless calderas of the Earth, including, for example, Yellowstone, Long Valley, and Campi Flegrei. Here we focus on Campi Flegrei caldera, sited in the densely inhabited metropolitan area of Napoli, where an inflation stage showing an accelerating trend started in 2005 and reached a maximum vertical displacement of about 24 cm in July 2014. Fumarolic compositions compared with ground deformation data suggests that this ten year's accelerating uplift is mainly caused by the overlapping of two processes: (i) short time pulses caused by injection of magmatic fluids into the hydrothermal system, and (ii) a long time process of heating of the rocks. The short pulses are highlighted by comparing the residuals of ground deformation, fitted with an accelerating curve, with the fumarolic CO2/CH4 and He/CH4 ratios which are good indicators of the arrival of magmatic gases into the hydrothermal system. These two independent datasets show an impressive temporal correlation, with the same sequence of five peaks with a delay of ~ 200 days of the geochemical signal with respect to the geodetic one. The heating of the hydrothermal system is inferred by an evident increase in the fumarolic activity and by temperature-pressure gas-geoindicators. The accelerating ground deformation is paralleled in fact by an increase in the fumarolic CO/CO2 ratio and by a general decrease of the CH4/CO2ratio, both being sign of increased equilibration temperatures. Comparing the observed fumarolic compositions with the thermodynamically derived equilibrium values we infer that the heating is caused by the condensation of increasing amounts of steam. According to a recent interpretation of fumarolic inert gas species, which relates

  19. LAS COCINAS DEL INFIERNO. LA VISUALIDAD DE LAS MUJERES EN LAS CALDERAS DE PEDRO BOTERO

    OpenAIRE

    Zuriaga Senent, Vicent Francesc

    2013-01-01

    Casi todas las religiones nos hablan del infierno como lugar en el que las almas son torturadas eternamente. El judaísmo lo llama Gehena, la mitología clásica Tártaro y Hades, las religiones paganas Inframundo, y la tradición cristiana castellana Las calderas de Pedro Botero. Los profetas del Antiguo Testamento narran con claridad los tormentos del infierno y Dante en La Divina Comedia nos lo relata con una visión particular. La literatura y el arte nos ofrecen abundancia de imáge...

  20. Reservoir processes and fluid origins in the Baca geothermal system, Valles Caldera, New Mexico ( USA).

    Science.gov (United States)

    Truesdell, A.H.; Janik, C.J.

    1986-01-01

    At the Baca geothermal field in the Valles caldera, New Mexico, 19 deep wells were drilled in an attempt to develop a 50-MW (megawatts electric) power plant. The chemical and isotopic compositions of steam and water samples have been used to indicate uniquely the origin of reservoir fluids and natural reservoir processes. Two distinct reservoir fluids exist at Baca. These fluids originate from the same deep, high-temperature (335oC), saline (2500 mg/kg Cl) parent water but have had different histories during upflow which are described.-after Authors

  1. Cálculo de estructuras utilizando elemento finito con cómputo en paralelo

    OpenAIRE

    Vargas Félix, José Miguel

    2010-01-01

    Nuestro trabajo trata sobre la solución numérica de problemas de deformación lineal de sólidos por medio del método de elementos finitos, estos problemas se resuelven utilizando estratégias de cómputo en paralelo. Hablamos sobre algunas formas de paralelizar los algoritmos, tanto utilizando modelos de memoria compartida como de memoria distribuída. En particular nos centraremos en la descomposición de dominios usando el método alternante de Schwarz para resolver problemas de elemento finito c...

  2. The late quaternary tephra layers from the caldera volcanoes in and around kagoshima bay, southern kyushu, japan

    OpenAIRE

    Nagaoka, Shinji

    1988-01-01

    The Aira, Ata and Kikai calderas of Kagoshima Bay have erupted more than twenty silicic tehra formations including more than fifty tephra falls and flows (about 1,000 km^3 in total volume) in the last 150 ka. On the basis of the sequence of eruptive phases which have many kinds of eruption types, the eruptive cycles of these caldera volcanoes are grouped into three types: 1) a plinian cycle (composed of a single plinian phase, or a plinian phase and a moderate-scale pyroclastic flow phase); 2...

  3. Eficiencia en la prescripción de medicamentos: impacto de un programa de intercambio terapéutico The efficiency of drug prescription: impact of a therapeutic exchange program

    Directory of Open Access Journals (Sweden)

    Isabel Rosich

    2012-02-01

    Full Text Available Objetivo: Evaluar el impacto de un programa de intercambio terapéutico a omeprazol de los inhibidores de la bomba de protones (IBP. Método: Ensayo comunitario que compara el impacto de un programa de intercambio terapéutico en los equipos de atención primaria de una comarca respecto a la no aplicación en una comarca control. Se incluyó a los pacientes con prescripción de un IBP entre mayo de 2008 y junio de 2009. La intervención consistió en sesiones educativas y facilitar a cada médico (n=68 los pacientes con un IBP que pudiera cambiarse a omeprazol. Se obtuvo información de la historia clínica (IBP prescrito, equipo de atención primaria y de la aplicación de farmacia (coste de la dosis diaria definida de los IBP. A partir del riesgo relativo (RR se comparó el porcentaje de intercambio terapéutico en cada comarca antes y después de la intervención. También se calculó el porcentaje de omeprazol al final de cada periodo de estudio y los cambios en los costes en IBP. Resultados: Hubo más intercambios terapéuticos en el grupo de intervención (RR: 4,2; intervalo de confianza del 95% [IC95%]:3,1-5,8 respecto al control (RR: 1,8; IC95%:1,2-2,6. En el grupo de intervención, el porcentaje de pacientes con omeprazol pasó del 86,2% al 89,3%, y en el control del 84,3% al 84,7%. El coste del grupo IBP disminuyó un 7,6% en el grupo de intervención y aumentó un 2,0% en el control. Conclusiones: El programa de intercambio terapéutico se ha mostrado efectivo. Se trata de una intervención sencilla, capaz de modificar las prescripciones y reducir sus costes.Objective: To assess the impact of substituting proton pump inhibitors (PPI for omeprazole. Method: We performed a community trial of the impact of a therapeutic exchange program in the primary care teams of a region compared with non-implementation in a control region. The study included patients prescribed a PPI between May 2008 and June 2009. The intervention consisted of

  4. Geobotanical characterization of a geothermal system using hyperspectral imagery: Long Valley Caldera, CA; TOPICAL

    International Nuclear Information System (INIS)

    We have analyzed hyperspectral Airborne Visible-Infrared Imaging System (AVIRIS) imagery taken in September of 1992 in Long Valley Caldera, CA, a geothermally active region expressed surficially by hot springs and fumaroles. Geological and vegetation mapping are attempted through spectral classification of imagery. Particular hot spring areas in the caldera are targeted for analysis. The data is analyzed for unique geobotanical patterns in the vicinity of hot springs as well as gross identification of dominant plant and mineral species. Spectra used for the classifications come from a vegetation spectral library created for plant species found to be associated with geothermal processes. This library takes into account the seasonality of vegetation by including spectra for species on a monthly basis. Geological spectra are taken from JPL and USGS mineral libraries. Preliminary classifications of hot spring areas indicate some success in mineral identification and less successful vegetation species identification. The small spatial extent of individual plants demands either sub-pixel analysis or increased spatial resolution of imagery. Future work will also include preliminary analysis of a hyperspectral thermal imagery dataset and a multitemporal air photo dataset. The combination of these remotely sensed datasets for Long Valley will yield a valuable product for geothermal exploration efforts in other regions

  5. Thermomechanical controls on magma supply and volcanic deformation: application to Aira caldera, Japan

    Science.gov (United States)

    Hickey, James; Gottsmann, Joachim; Nakamichi, Haruhisa; Iguchi, Masato

    2016-09-01

    Ground deformation often precedes volcanic eruptions, and results from complex interactions between source processes and the thermomechanical behaviour of surrounding rocks. Previous models aiming to constrain source processes were unable to include realistic mechanical and thermal rock properties, and the role of thermomechanical heterogeneity in magma accumulation was unclear. Here we show how spatio-temporal deformation and magma reservoir evolution are fundamentally controlled by three-dimensional thermomechanical heterogeneity. Using the example of continued inflation at Aira caldera, Japan, we demonstrate that magma is accumulating faster than it can be erupted, and the current uplift is approaching the level inferred prior to the violent 1914 Plinian eruption. Magma storage conditions coincide with estimates for the caldera-forming reservoir ~29,000 years ago, and the inferred magma supply rate indicates a ~130-year timeframe to amass enough magma to feed a future 1914-sized eruption. These new inferences are important for eruption forecasting and risk mitigation, and have significant implications for the interpretations of volcanic deformation worldwide.

  6. Magma storage and evolution of the most recent effusive and explosive eruptions from Yellowstone Caldera

    Science.gov (United States)

    Befus, Kenneth S.; Gardner, James E.

    2016-04-01

    Between 70 and 175 ka, over 350 km3 of high-silica rhyolite magma erupted both effusively and explosively from within the Yellowstone Caldera. Phenocrysts in all studied lavas and tuffs are remarkably homogenous at the crystal, eruption, and caldera-scale, and yield QUILF temperatures of 750 ± 25 °C. Phase equilibrium experiments replicate the observed phenocryst assemblage at those temperatures and suggest that the magmas were all stored in the upper crust. Quartz-hosted glass inclusions contain 1.0-2.5 % H2O and 50-600 ppm CO2, but some units are relatively rich in CO2 (300-600 ppm) and some are CO2-poor (50-200 ppm). The CO2-rich magmas were stored at 90-150 MPa and contained a fluid that was 60-75 mol% CO2. CO2-poor magmas were stored at 50-70 MPa, with a more H2O-rich fluid (X_{{{text{CO}}2 }} = 40-60 %). Storage pressures and volatiles do not correlate with eruption age, volume, or style. Trace-element contents in glass inclusions and host matrix glass preserve a systematic evolution produced by crystal fractionation, estimated to range from 36 ± 12 to 52 ± 12 wt%. Because the erupted products contain Yellowstone magmatic system may undergo rapid changes. The variations in depth suggest the magmas were sourced from multiple chambers that follow similar evolutionary paths in the upper crust.

  7. Late Pleistocene granodiorite beneath Crater Lake caldera, Oregon, dated by ion microprobe

    Science.gov (United States)

    Bacon, C.R.; Persing, H.M.; Wooden, J.L.; Ireland, T.R.

    2000-01-01

    Variably melted granodiorite blocks ejected during the Holocene caldera-forming eruption of Mount Mazama were plucked from the walls of the climactic magma chamber ~15 km depth. Ion-microprobe U-Pb dating of zircons from two unmelted granodiorite blocks with SHRIMP RG (sensitive high-resolution ion microprobe-reverse geometry) gives a nominal 238U/206Pb age of 101+78-80 ka, or 174+89-115 ka when adjusted for an initial 230Th deficit. SHRIMP RG U-Th measurements on a subset of the zircons yield a 230Th/238U isochron age of 112 ?? 24 ka, considered to be the best estimate of the time of solidification of the pluton. These results suggest that the granodiorite is related to andesite and dacite of Mount Mazama and not to magmas of the climactic eruption. The unexposed granodiorite has an area of at least 28 km2. This young, shallow pluton was emplaced in virtually the same location where a similarly large magma body accumulated and powered violent explosive eruptions ~7700 yr ago, resulting in collapse of Crater Lake caldera.

  8. Thermomechanical controls on magma supply and volcanic deformation: application to Aira caldera, Japan

    Science.gov (United States)

    Hickey, James; Gottsmann, Joachim; Nakamichi, Haruhisa; Iguchi, Masato

    2016-01-01

    Ground deformation often precedes volcanic eruptions, and results from complex interactions between source processes and the thermomechanical behaviour of surrounding rocks. Previous models aiming to constrain source processes were unable to include realistic mechanical and thermal rock properties, and the role of thermomechanical heterogeneity in magma accumulation was unclear. Here we show how spatio-temporal deformation and magma reservoir evolution are fundamentally controlled by three-dimensional thermomechanical heterogeneity. Using the example of continued inflation at Aira caldera, Japan, we demonstrate that magma is accumulating faster than it can be erupted, and the current uplift is approaching the level inferred prior to the violent 1914 Plinian eruption. Magma storage conditions coincide with estimates for the caldera-forming reservoir ~29,000 years ago, and the inferred magma supply rate indicates a ~130-year timeframe to amass enough magma to feed a future 1914-sized eruption. These new inferences are important for eruption forecasting and risk mitigation, and have significant implications for the interpretations of volcanic deformation worldwide. PMID:27619897

  9. High flux rates of ignimbrite and stratocone growth at Atitlan Caldera, Guatemala

    Science.gov (United States)

    Cunningham, H. S.; Jicha, B.; Singer, B. S.

    2010-12-01

    To understand the factors that govern the development of different volcanic edifices, recent studies have quantified eruptive volume, repose interval and crustal thickness among other parameters. Atitlan Caldera, Guatemala provides a compelling locality to contrast the age, volume and repose of several ignimbrite eruptions over the past 160 kyr including the 300 km3 Los Chocoyos ignimbrite, as well as, prolific mafic volcanism from three intracaldera stratocones. Since the caldera-forming eruption 84 kyr, 117 km3 of basaltic andesitic to dacitic lavas have been erupted from stratocones San Pedro, Toliman and Atitlan, resulting in a combined eruption rate of 1.46km3/kyr. These eruption rates are considered minimum values as preliminary 40Ar/39Ar age data suggest the cones are much younger than 84 kyr. Inclusion of the Los Chocoyos eruption increases eruption rates to 4.77 km3/kyr. Average eruption rates of the Atitlan system are an order of magnitude greater than most frontal arc complexes that are commonly characterized by cone growth due to large punctuated silicic eruptions. Although a minor proportion (marked by large punctuated ignimbrite eruptions, but rather by continual profuse outpouring of both rhyolitic and basaltic products.

  10. Bibliography of literature pertaining to Long Valley Caldera and associated volcanic fields

    Science.gov (United States)

    Ewert, John W.; Harpel, Christopher J.; Brooks, Suzanna K.; Marcaida, Mae

    2011-01-01

    On May 25-27, 1980, Long Valley caldera was rocked by four M=6 earthquakes that heralded the onset of a wave of seismic activity within the caldera which has continued through the present. Unrest has taken the form of seismic swarms, uplift of the resurgent dome, and areas of vegetation killed by increased CO2 emissions, all interpreted as resulting from magma injection into different levels beneath the caldera, as well as beneath Mammoth Mountain along the southwest rim of the caldera. Continuing economic development in the Mammoth Lakes area has swelled the local population, increasing the risk to people and property if an eruption were to occur. The U.S. Geological Survey (USGS) has been monitoring geophysical activity in the Long Valley area since the mid-1970s and continues to track the unrest in real time with a sophisticated network of geophysical sensors. Hazards information obtained by this monitoring is provided to local, State, and Federal officials and to the public through the Long Valley Observatory. The Long Valley area also was scientifically important before the onset of current unrest. Lying at the eastern foot of the Sierra Nevada, the deposits from this active volcanic system have provided fertile ground for research into Neogene tectonics, Quaternary geology and geomorphology, regional stratigraphy, and volcanology. In the early 1970s, intensive studies of the area began through the USGS Geothermal Investigations Program, owing to the presence of a large young silicic volcanic system. The paroxysmal eruption of Long Valley caldera about 760,000 years ago produced the Bishop Tuff and associated Bishop ash. The Bishop Tuff is a well-preserved ignimbrite deposit that has continued to provide new and developing insights into the dynamics of ignimbrite-forming eruptions. Another extremely important aspect of the Bishop Tuff is that it is the oldest known normally magnetized unit of the Brunhes Chron. Thus, the age of the Bishop Tuff is used to

  11. Volcanic flood simulation of magma effusion using FLO-2D for drainage of a caldera lake at the Mt. Baekdusan

    Science.gov (United States)

    Lee, Khil-Ha; Kim, Sung-Wook; Kim, Sang-Hyun

    2014-05-01

    Many volcanic craters and calderas are filled with large amounts of water that can pose significant flood hazards to downstream communities due to their high elevation and the potential for catastrophic releases of water. Recent reports pointed out the Baekdusan volcano that is located between the border of China and North Korea as a potential active volcano. Since Millennium Eruption around 1000 AD, smaller eruptions have occurred at roughly 100-year intervals, with the last one in 1903. Sudden release of huge volume of water stored in temporarily elevated caldera lakes are a recurrent feature of volcanic environments, due to the case with which outlet channels are blocked by and re-cut through, unwelded pyroclastic deposits. The volcano is showing signs of waking from a century-long slumber recently. Volcanic floods, including breakouts from volcanic lakes, can affect communities beyond the areas immediately affected by a volcanic eruption and cause significant hydrological hazards because floods from lake-filled calderas may be particularly large and high. Although a number of case studies have been presented in the literature, investigation of the underlying physical processes is required as well as a method for interpreting the process of the rapid release of water stored in a caldera lake. The development of various forecasting techniques to prevent and minimize economic and social damage is in urgent need. This study focuses on constructing a flood hazard map triggered by the magma effusion in the Baekdusan volcano. A physically-based uplift model was developed to compute the amount of water and time to peak flow. The ordinary differential equation was numerically solved using the finite difference method and Newton-Raphson iteration method was used to solve nonlinear equation. The magma effusion rate into the caldera lake is followed by examples at other volcanic activities. As a result, the hydrograph serves as an upper boundary condition when hydrodynamic

  12. A preliminary study of older hot spring alteration in Sevenmile Hole, Grand Canyon of the Yellowstone River, Yellowstone Caldera, Wyoming

    Science.gov (United States)

    Larson, P.B.; Phillips, A.; John, D.; Cosca, M.; Pritchard, C.; Andersen, A.; Manion, J.

    2009-01-01

    Erosion in the Grand Canyon of the Yellowstone River, Yellowstone Caldera (640??ka), Wyoming, has exposed a cross section of older hydrothermal alteration in the canyon walls. The altered outcrops of the post-collapse tuff of Sulphur Creek (480??ka) extend from the canyon rim to more than 300??m beneath it. The hydrothermal minerals are zoned, with an advanced argillic alteration consisting of an association of quartz (opal) + kaolinite ?? alunite ?? dickite, and an argillic or potassic alteration association with quartz + illite ?? adularia. Disseminated fine-grained pyrite or marcasite is ubiquitous in both alteration types. These alteration associations are characteristic products of shallow volcanic epithermal environments. The contact between the two alteration types is about 100??m beneath the rim. By analogy to other active geothermal systems including active hydrothermal springs in the Yellowstone Caldera, the transition from kaolinite to illite occurred at temperatures in the range 150 to 170????C. An 40Ar/39Ar age on alunite of 154,000 ?? 16,000??years suggests that hydrothermal activity has been ongoing since at least that time. A northwest-trending linear array of extinct and active hot spring centers in the Sevenmile Hole area implies a deeper structural control for the upflowing hydrothermal fluids. We interpret this deeper structure to be the Yellowstone Caldera ring fault that is covered by the younger tuff of Sulphur Creek. The Sevenmile Hole altered area lies at the eastern end of a band of hydrothermal centers that may mark the buried extension of the Yellowstone Caldera ring fault across the northern part of the Caldera. ?? 2009 Elsevier B.V.

  13. Post 19 ka B.P. eruptive history of Ulleung Island, Korea, inferred from an intra-caldera pyroclastic sequence

    Science.gov (United States)

    Kim, G. B.; Cronin, S. J.; Yoon, W. S.; Sohn, Y. K.

    2014-04-01

    Ulleung Island is a Quaternary volcanic island located in the mid-western part of the East Sea (Sea of Japan) back-arc basin, which has erupted from the Pliocene until the late Holocene. This study focuses on reconstructing the latest eruptive history of the island by describing the sedimentological and stratigraphic characteristics of the most recent, trachytic/phonolitic pyroclastic sequence, named the Nari Tephra Formation. This formation is preserved as a succession of unwelded pyroclastic and epiclastic deposits within an embayed margin of the Nari Caldera. The embayment acted as a topographic trap for proximal pyroclastic deposits, and contains a complete record of the past 19,000 years of eruption history. The formation includes evidence for five separate eruptive episodes (Member N-1 to N-5), with intervening weathered and/or soil horizons indicating hundreds to thousands of years of repose between each eruption. Eruption styles and depositional mechanisms varied between and during individual episodes, reflecting changing dynamics of the magma plumbing system, magmatic gas coupling, and a variable role of external water. Extra-caldera sequences show that only a few of these eruptions generated sustained eruption columns or pyroclastic density currents (PDCs) large enough to overtop the caldera wall. Thus tephra sequences outside the caldera provide an underestimate of eruption frequency, and care needs to be taken in the interpretation and correlation to distal tephra sequences recognized in marine and terrestrial records. In addition, topographic effects of caldera structures should be considered for the assessment of PDC-related hazards in such moderately sized pyroclastic eruptions.

  14. Geophysical monitoring of the submerged area of the Campi Flegrei caldera (Southern Italy): experiences and perspectives

    Science.gov (United States)

    Iannaccone, Giovanni; Guardato, Sergio; De Martino, Prospero; Donnarumma, Gian Paolo; Bobbio, Antonella; Chierici, Francesco; Pignagnoli, Luca; Beranzoli, Laura

    2016-04-01

    The monitoring system of the Campi Flegrei caldera is made up of a dense geophysical network of seismological and geodetic instruments with data acquired and processed at the Monitoring Center of INGV in Naples. As one third of the caldera is covered by the sea, a marine monitoring system has been operating since 2008 in the center of the gulf of Pozzuoli, where the sea depth is about 100 m at ~2.5 km from the coast. The main component of the monitoring system is CUMAS (Cabled Underwater Multidisciplinary Acquisition System), which consists of a sea floor module equipped with geophysical and oceanographic sensors (broad band seismometer, accelerometer, hydrophone, bottom pressure recorder and single point three component water-current meter) and status and control sensors. CUMAS is connected by cable to the top of an elastic beacon buoy equipped with the power supply and data transmission devices. The buoy consists of a float placed below sea level, surrounding and holding a steel pole that supports a turret structure above sea level. The pole, turret and float system are rigidly connected to the ballast on the sea bottom. Thus a GPS installed on the turret can record the vertical sea floor displacement related to the volcanic activity of the area. The GPS has operated since January 2012 with continuous acquisition lasting more than three years and has recorded a cumulative seafloor uplift of about 7-8 cm. The comparison of the pattern of the GPS buoy data with those of the land stations confirms a quasi-symmetrical vertical displacement field of the caldera area. Measurement of vertical sea floor displacement has also been obtained by the analysis of bottom pressure recorder data. These results, in conjunction with the analysis of seismic and hydrophone data, have encouraged us to extend the marine monitoring system with the deployment in the Gulf of Pozzuoli of three new similar systems. We also present preliminary results of the first few months of activity of

  15. Carbon Dioxide Emissions From Kill Zones Around the Resurgent Dome, Long Valley Caldera, CA

    Science.gov (United States)

    Bergfeld, D.; Evans, W. C.; Farrar, C. D.; Howle, J. F.

    2004-12-01

    An episode of seismic unrest beneath the resurgent dome at Long Valley caldera (LVC) in eastern California began in 1980 and is associated with approximately 80 cm of cumulative uplift on parts of the dome since that time. Studies of hydrologic and geochemical parameters can be useful in determining the source of uplift; and of particular relevance here, studies of diffuse soil degassing and temperature have been used to examine relations between gas emissions, uplift, and energy release. We present results from an eighteen-month investigation of soil temperature, soil-gas chemistry and CO2 efflux from fourteen discrete areas of vegetation kill that have appeared inside the caldera over the past two decades. Compared with the tree-kill around Mammoth Mountain on the southwest rim of the caldera, dead zones we studied around the resurgent dome are small. Individually the areas cover between 800 and 36,000 m2. All of the areas have some sites with elevated CO2 flux and elevated soil temperature. \\delta 13C values of CO2 from sites in eight of the studied areas are between -5.7 and -3.9\\permil, and are within the range of magmatic CO2. Results from the flux measurements indicate that on average total CO2 emissions from four of the areas sum about 10 tonnes per day. The other vegetation kill areas currently have only a few sites that exhibit anomalous soil temperatures and CO2 flux, and CO2 emissions from these areas are typically less than 0.3 of a tonne per day. The chemical composition of gas emissions from thermal ground in kill zones located 1.5 to 2 km northwest of the Casa Diablo geothermal power plant demonstrate a connection between some of the dead areas and perturbations related to geothermal fluid production. These results and estimates of thermal output from two of the high flux grids are used to evaluate the premise that the gaseous and thermal anomalies are related to magmatic intrusion beneath the resurgent dome.

  16. Intercambio gaseoso y contenido de azúcares en raíces de los genotipos de yuca TMS60444 y CAGBS1A8-3A crecidos bajo condiciones de campo

    OpenAIRE

    Maldonado Valero, Bibiana Andrea

    2012-01-01

    En la presente investigación se estudiaron los genotipos de yuca TMS60444 “silvestre” y CAGBS1A8-3A “transgénico” por su potencial promisorio para producción de bioetanol. En plantas de 3, 8 y 13 meses de edad, se evaluó en hojas mediante el análisis de gases en infrarrojo IRGA el intercambio gaseoso en relación con factores climáticos, y se determinaron en raíces los niveles de glucosa Glc, fructosa Frc y sacarosa Suc con cromatografía líquida de alta eficiencia HPLC. La respuesta fotosintét...

  17. Intercambio de ideas científicas y técnicas en la formación de los ingenieros de Minas mexicanos antes, durante y después de la Independencia

    OpenAIRE

    Ramos Lara, María De La Paz

    2012-01-01

    El plan de estudios de la primera carrera especializada en la minería creada en Nueva España se equiparó a los mejores del mundo gracias al intercambio de ideas científicas y técnicas que existía con varios países europeos. Esta profesión inició en 1792 en el Real Seminario de Minería, la escuela de minas más importante en América y en Iberoamérica, la cual se fundó a iniciativa de los novohispanos ilustrados, quienes contaban con diversos recursos para mantenerse informados de los sucesos qu...

  18. Aplicación del método de transbordo en la enseñanza de la estructuración de Redes de Intercambio Térmico

    OpenAIRE

    Paniagua, Carmen Noemí; Iglesias, Omar A.

    2005-01-01

    El trabajo reseña una experiencia educativa en la enseñanza de la estructuración de redes de intercambio térmico (RIT) mediante el método de Transbordo. La aplicación de la técnica en la que se basa el método, Programación Lineal o Lineal Entera Mixta, obligó al desarrollo de un complemento para planilla Excel, Transbordo.xla, cuyas características se resumen. Se muestra un caso donde, a través del uso del complemento, se analiza la vigencia de la heurística básica del otro método utilizad...

  19. Investigación sobre el uso de los términos ración, porción, equivalencia, intercambio y medidas caseras en nutrición humana y dietética

    OpenAIRE

    Norte Navarro, Aurora; Carballo Marrero, Silvia; Prats Moya, Soledad; Maestre Pérez, Salvador; Davó Blanes, María del Carmen; Ortiz Moncada, Rocío

    2013-01-01

    Los docentes de diversas asignaturas de la titulación de Grado en Nutrición Humana y Dietética han detectado que existe una confusión entre los alumnos del Grado en cuanto al significado y uso de diversos términos usados en la preparación y valoración de dietas y menús. Estos términos son: ración, porción, equivalencia, intercambio y medida casera de alimentos. Se piensa que el origen de esta confusión radica en el uso poco cuidadoso de los términos en diferentes asignaturas atribuyéndole, en...

  20. Desarrollo y evaluación de una aplicación Web estandarizada para el almacenamiento e intercambio de Historiales Clínicos Electrónicos (HCEs) en oftalmología: TeleOftalWeb

    OpenAIRE

    Torre Díez, Isabel de la

    2010-01-01

    El objetivo de la presente Tesis es el desarrollo, puesta en marcha y evaluación de la aplicación Web, TeleOftalWeb, en sus cuatro versiones, destinada al almacenamiento e intercambio de Historiales Clínicos Electrónicos (HCEs) y retinografías. Cada una de las versiones está desarrollada con diferentes modelos de bases de datos (BDs): dbXML 2.0 más MySQL 5.0, eXist 1.1.1 más MySQL, Xindice 1.2. más MySQL 5.0 y Oracle 10g. A su vez, se estudiarán los estándares de HCE más relevantes entre ello...

  1. Proyecto MMM (MiniWEB, Multilingüe, Maxiaprendizaje Intercambio y comunicación entre centros educativos de diferentes países vía internet

    Directory of Open Access Journals (Sweden)

    Marta Liesa Orus

    2012-04-01

    Full Text Available El presente trabajo relata un proyecto realizado en una comunidad española, con el aporte de la Universidad de Zaragoza, en que se usan ordenadores y su multiplicidad de oportunidades como herramienta actual de trabajo, en classes de educacion infantil, con los objjetivos de compensar desigualdades, prevenir el analfabetismo y el fracasso escolar, facilitar el aprendizaje de la lectura, impulsar la utilización de la tecnologia desde el inicío de la escolarización y facilitar el trabajo autônomo del niño. Es um proyecto en que participam, además de España, Francia, USA y Andorra, lo que posibilita un intercambio tanto entre los alunnos, como entre los professore, através de la internet.

  2. A Hydrologic monitoring program to detect potential impacts of geothermal development in Long Valley caldera, California

    Energy Technology Data Exchange (ETDEWEB)

    Sorey, Michael L.

    1988-01-01

    Long Valley caldera is a tectonically active area in east-central California that contains a high-temperature geothermal system currently being explored and developed for electric power production. Concerns expressed by public agencies and private citizens over the potential impacts of geothermal development on thermal springs at the Hot Creek Fish Hatchery and Hot Creek gorge have resulted in the establishment of a Hydrologic Advisory Committee. The committee includes representatives from development projects and regulatory agencies. Its role is to formulate and oversee a hydrologic monitoring program capable of detecting such impacts before they become significant. The advisory committee and the monitoring program provide effective mechanisms with which to proceed with geothermal development in areas such as Long Valley, where the level of environmental risk cannot be determined a-priori because the relevant geo-hydrologic parameters are not adequately delineated.

  3. PRESENT STATE OF THE HYDROTHERMAL SYSTEM IN LONG VALLEY CALDERA, CALIFORNIA.

    Science.gov (United States)

    Sorey, Michael L.

    1985-01-01

    Results of test drilling to depths of 2 km and data on the chemical and isotopic content of waters from hot springs and fumaroles permit a conceptual model of the present-day hydrothermal system in Long Valley caldera to be delineated. The model consists of two principal zones in which hot water flows laterally from west to east at depths less than 1 km within and around the resurgent dome. Maximum measured temperatures within these zones are near 170 degree C, but estimates from chemical geothermometers and extrapolation of a high temperature gradient measured in a recent drill hole indicate that a source reservoir at temperatures near 240 degree C may exist at greater depths in the Bishop Tuff beneath the west moat.

  4. Acoustic stratigraphy and hydrothermal activity within Epi Submarine Caldera, Vanuatu, New Hebrides Arc

    Science.gov (United States)

    Greene, H. Gary; Exon, N.F.

    1988-01-01

    Geological and geophysical surveys of active submarine volcanoes offshore and southeast of Epi Island, Vanuatu, New Hebrides Arc, have delineated details of the structure and acoustic stratigraphy of three volcanic cones. These submarine cones, named Epia, Epib, and Epic, are aligned east-west and spaced 3.5 km apart on the rim of a submerged caldera. At least three acoustic sequences, of presumed Quaternary age, can be identified on single-channel seismic-reflection profiles. Rocks dredged from these cones include basalt, dacite, and cognate gabbroic inclusions with magmatic affinities similar to those of the Karua (an active submarine volcano off the southeastern tip of Epi) lavas. ?? 1988 Springer-Verlag New York Inc.

  5. Fiber-Reinforced Rocks Akin to Roman Concrete Help Explain Ground Deformation at Campi Flegrei Caldera

    Science.gov (United States)

    Vanorio, Tiziana; Kanitpanyacharoen, Waruntorn

    2016-04-01

    The caldera of Campi Flegrei is one of the active hydrothermal systems of the Mediterranean region experiencing notable unrest episodes in a densely populated area. During the last crisis of 1982-1984, nearly 40,000 people were evacuated for almost two years from the main town of Pozzuoli, the Roman Puteoli, due to the large uplifts (~2 m over two years) and the persistent seismic activity. The evacuation severely hampered the economy and the social make-up of the community, which included the relocation of schools and commercial shops as well as the harbor being rendered useless for docking. Despite the large uplifts, the release of strain appears delayed. Seismicity begins and reaches a magnitude of 4.0 only upon relatively large uplifts (~ 70-80 cm) contrary to what is generally observed for calderas exhibiting much lower deformation levels. Over and above the specific mechanism causing the unrest and the lack of identification of a shallow magmatic reservoir (engineering the mortar of the Roman concrete. The formation of fibrous minerals by intertwining filaments confers shear and tensile strength to the caprock, contributing to its ductility and increased resistance to fracture. The importance of the findings reported in this study lies not only on the fibrous and compositionally nature of the caprock but also on its possible physicochemical deterioration. Given the P-T-XCO2 conditions regulating the decarbonation reactions, the influx of new fluids into the Campi Flegrei system lowers the temperature of the decarbonation reaction and dilutes the existing CO2, thus triggering additional CO2, methane, and steam to form. As these gases rise toward the surface, the natural cement layer halts them, leading to pore pressure increase and subsequent ground deformations.

  6. Catastrophic caldera-forming eruptions II: The subordinate role of magma buoyancy as an eruption trigger

    Science.gov (United States)

    Gregg, Patricia M.; Grosfils, Eric B.; de Silva, Shanaka L.

    2015-10-01

    Recent analytical investigations have suggested that magma buoyancy is critical for triggering catastrophic caldera forming eruptions. Through detailed assessment of these approaches, we illustrate how analytical models have been misapplied for investigating buoyancy and are, therefore, incorrect and inconclusive. Nevertheless, the hypothesis that buoyancy is the critical trigger for larger eruptions warrants further investigation. As such, we utilize viscoelastic finite element models that incorporate buoyancy to test overpressure evolution and mechanical failure in the roof due to the coalescence of large buoyant magma bodies for two model cases. In the first case, we mimic empirical approaches and include buoyancy as an explicit boundary condition. In the second set of models, buoyancy is calculated implicitly due to the density contrast between the magma in the reservoir and the host rock. Results from these numerical experiments indicate that buoyancy promotes only minimal overpressurization of large silicic magma reservoirs (implementations and the results from the numerical experiments, we conclude that buoyancy does not provide an eruption triggering mechanism for large silicic systems. Therefore, correlations of buoyancy with magma residence times, the eruption frequency-volume relationship, and the dimensions of calderas are re-assessed. We find a causal relationship with magma reservoir volume that implicates the mechanical conditions of the host rock as a primary control on eruption frequency. As magma reservoirs grow in size (> 100 km3) they surpass a rheological threshold where their subsequent evolution is controlled by host rock mechanics. Consequently, this results in a thermomechanical division between small systems that are triggered "internally" by magmatic processes and large systems that are triggered "externally" by faulting related to roof uplift or tectonism. Finally, critical assessment of recent analytical approaches illustrates that care

  7. Abrupt transition from fractional crystallization to magma mixing at Gorely volcano (Kamchatka) after caldera collapse

    Science.gov (United States)

    Gavrilenko, Maxim; Ozerov, Alexey; Kyle, Philip R.; Carr, Michael J.; Nikulin, Alex; Vidito, Christopher; Danyushevsky, Leonid

    2016-07-01

    A series of large caldera-forming eruptions (361-38 ka) transformed Gorely volcano, southern Kamchatka Peninsula, from a shield-type system dominated by fractional crystallization processes to a composite volcanic center, exhibiting geochemical evidence of magma mixing. Old Gorely, an early shield volcano (700-361 ka), was followed by Young Gorely eruptions. Calc-alkaline high magnesium basalt to rhyolite lavas have been erupted from Gorely volcano since the Pleistocene. Fractional crystallization dominated evolution of the Old Gorely magmas, whereas magma mixing is more prominent in the Young Gorely eruptive products. The role of recharge-evacuation processes in Gorely magma evolution is negligible (a closed magmatic system); however, crustal rock assimilation plays a significant role for the evolved magmas. Most Gorely magmas differentiate in a shallow magmatic system at pressures up to 300 MPa, ˜3 wt% H2O, and oxygen fugacity of ˜QFM + 1.5 log units. Magma temperatures of 1123-1218 °C were measured using aluminum distribution between olivine and spinel in Old and Young Gorely basalts. The crystallization sequence of major minerals for Old Gorely was as follows: olivine and spinel (Ol + Sp) for mafic compositions (more than 5 wt% of MgO); clinopyroxene and plagioclase crystallized at ˜5 wt% of MgO (Ol + Cpx + Plag) and magnetite at ˜3.5 wt% of MgO (Ol + Cpx + Plag + Mt). We show that the shallow magma chamber evolution of Old Gorely occurs under conditions of decompression and degassing. We find that the caldera-forming eruption(s) modified the magma plumbing geometry. This led to a change in the dominant magma evolution process from fractional crystallization to magma mixing. We further suggest that disruption of the magma chamber and accompanying change in differentiation process have the potential to transform a shield volcanic system to that of composite cone on a global scale.

  8. Fiber-Reinforced Rocks Akin to Roman Concrete Help Explain Ground Deformation at Campi Flegrei Caldera

    Science.gov (United States)

    Vanorio, Tiziana; Kanitpanyacharoen, Waruntorn

    2016-04-01

    The caldera of Campi Flegrei is one of the active hydrothermal systems of the Mediterranean region experiencing notable unrest episodes in a densely populated area. During the last crisis of 1982-1984, nearly 40,000 people were evacuated for almost two years from the main town of Pozzuoli, the Roman Puteoli, due to the large uplifts (~2 m over two years) and the persistent seismic activity. The evacuation severely hampered the economy and the social make-up of the community, which included the relocation of schools and commercial shops as well as the harbor being rendered useless for docking. Despite the large uplifts, the release of strain appears delayed. Seismicity begins and reaches a magnitude of 4.0 only upon relatively large uplifts (~ 70-80 cm) contrary to what is generally observed for calderas exhibiting much lower deformation levels. Over and above the specific mechanism causing the unrest and the lack of identification of a shallow magmatic reservoir (concrete. The formation of fibrous minerals by intertwining filaments confers shear and tensile strength to the caprock, contributing to its ductility and increased resistance to fracture. The importance of the findings reported in this study lies not only on the fibrous and compositionally nature of the caprock but also on its possible physicochemical deterioration. Given the P-T-XCO2 conditions regulating the decarbonation reactions, the influx of new fluids into the Campi Flegrei system lowers the temperature of the decarbonation reaction and dilutes the existing CO2, thus triggering additional CO2, methane, and steam to form. As these gases rise toward the surface, the natural cement layer halts them, leading to pore pressure increase and subsequent ground deformations.

  9. Petrogenesis of Rinjani Post-1257-Caldera-Forming-Eruption Lava Flows

    Directory of Open Access Journals (Sweden)

    Heryadi Rachmat

    2016-08-01

    Full Text Available After the catastrophic 1257 caldera-forming eruption, a new chapter of Old Rinjani volcanic activity beganwith the appearance of Rombongan and Barujari Volcanoes within the caldera. However, no published petrogeneticstudy focuses mainly on these products. The Rombongan eruption in 1944 and Barujari eruptions in pre-1944, 1966,1994, 2004, and 2009 produced basaltic andesite pyroclastic materials and lava flows. A total of thirty-one sampleswere analyzed, including six samples for each period of eruption except from 2004 (only one sample. The sampleswere used for petrography, whole-rock geochemistry, and trace and rare earth element analyses. The Rombonganand Barujari lavas are composed of calc-alkaline and high K calc-alkaline porphyritic basaltic andesite. The magmashows narrow variation of SiO2 content that implies small changes during its generation. The magma that formedRombongan and Barujari lavas is island-arc alkaline basalt. Generally, data show that the rocks are enriched in LargeIon Lithophile Elements (LILE: K, Rb, Ba, Sr, and Ba and depleted in High Field Strength Elements (HFSE: Y, Ti,and Nb which are typically a suite from a subduction zone. The pattern shows a medium enrichment in Light REEand relatively depleted in Heavy REE. The processes are dominantly controlled by fractional crystallization andmagma mixing. All of the Barujari and Rombongan lavas would have been produced by the same source of magmawith little variation in composition caused by host rock filter process. New flux of magma would likely have occurredfrom pre-1944 until 2009 period that indicates slightly decrease and increase of SiO2 content. The Rombongan andBarujari lava generations show an arc magma differentiation trend.

  10. New constraints on mechanisms of remotely triggered seismicity at Long Valley Caldera

    Science.gov (United States)

    Brodsky, E.E.; Prejean, S.G.

    2005-01-01

    Regional-scale triggering of local earthquakes in the crust by seismic waves from distant main shocks has now been robustly documented for over a decade. Some of the most thoroughly recorded examples of repeated triggering of a single site from multiple, large earthquakes are measured in geothermal fields of the western United States like Long Valley Caldera. As one of the few natural cases where the causality of an earthquake sequence is apparent, triggering provides fundamental constraints on the failure processes in earthquakes. We show here that the observed triggering by seismic waves is inconsistent with any mechanism that depends on cumulative shaking as measured by integrated energy density. We also present evidence for a frequency-dependent triggering threshold. On the basis of the seismic records of 12 regional and teleseismic events recorded at Long Valley Caldera, long-period waves (>30 s) are more effective at generating local seismicity than short-period waves of comparable amplitude. If the properties of the system are stationary over time, the failure threshold for long-period waves is ~0.05 cm/s vertical shaking. Assuming a phase velocity of 3.5 km/s and an elastic modulus of 3.5 x 1010Pa, the threshold in terms of stress is 5 kPa. The frequency dependence is due in part to the attenuation of the surface waves with depth. Fluid flow through a porous medium can produce the rest of the observed frequency dependence of the threshold. If the threshold is not stationary with time, pore pressures that are >99.5% of lithostatic and vary over time by a factor of 4 could explain the observations with no frequency dependence of the triggering threshold. Copyright 2005 by the American Geophysical Union.

  11. Variabilidad del ritmo de nado utilizando un sistema de información sonoro

    OpenAIRE

    Javaloyes Torres, Alejandro

    2014-01-01

    El ritmo de nado en natación es un parámetro muy importante a utilizar en el control de entrenamiento y para tener un mejor rendimiento en competición. La propuesta de nuestro estudio es comparar el ritmo de nado comparando 3 situaciones, sin información, con información visual y sonora o utilizando un dispositivo de transmisión de información audio.

  12. Pucarilla-Cerro Tipillas volcanic complex: the oldest recognized caldera in the southeastern portion of central volcanic zone of Central Andes?

    Energy Technology Data Exchange (ETDEWEB)

    Guzman, Silvina; Petrinovic, Ivan [CONICET -IBIGEO. Museo de Cs. Naturales, Universidad de Salta, Mendoza 2 (4400), Salta (Argentina)], E-mail: guzmansilvina@gmail.com

    2008-10-01

    We recognize the most eastern and oldest collapse caldera structure in the southern portion of the Central Volcanic Zone of the Andes. A description of Middle-Upper Miocene successions related to explosive- effusive events is presented. The location of this centre close to Cerro Galn Caldera attests a recurrence in the volcanism between 12 and 2 Ma in this portion of the Altiplano - Puna Plateau.

  13. Typology of Natural Hazards and Assessment of Associated Risks in the Mount Bambouto Caldera (Cameroon Line, West Cameroon)

    Institute of Scientific and Technical Information of China (English)

    Ghislain T. ZANGMO; Armand D. KAGOU; David G. NKOUATHIO; Pierre WANDJI

    2009-01-01

    Mount Bambouto is a polygenic stratovoicano of the Cameroon Volcanic Line, built between 21 Ma and 4.5 Ma. It is situated approximately 200 km NE of Mount Cameroon, between 09°55' and 10°15' longitude east and, 05°25' and 05°50' latitude north. The volcano covers an area of (13×8 km). Mount Bambouto is characterized by several natural hazards of different origins: meteorological, such as landslides and rock falls; anthropogenic, such as bushfires, tribal wars and deforestation; and volcanological, such as volcanic eruption. The thematic map shows that 55-60% of the caldera has high probability of occurrence of mass movement. The caldera has a high population density (3000 inhabitants), which increases the level of risk, evaluated at approximately $US3.8 million for patrimony, 3000 civilian deaths and destruction of biodiversity.

  14. Caldera collapse: Perspectives from comparing Galápagos volcanoes, nuclear-test sinks, sandbox models, and volcanoes on Mars

    Science.gov (United States)

    Howard, K.A.

    2010-01-01

    The 1968 trapdoor collapse (1.5 km3) of Fernandina caldera in the Galapágos Islands developed the same kinds of structures as found in small sandbox-collapse models and in concentrically zoned sinks formed in desert alluvium by fault subsidence into underground nuclear-explosion cavities. Fernandina’s collapse developed through shear failure in which the roof above the evacuating chamber was lowered mostly intact. This coherent subsidence contrasts to chaotic piecemeal collapse at small, rocky pit craters, underscoring the role of rock strength relative to subsidence size. The zoning at Fernandina implies that the deflated magma chamber underlay a central basin and a bordering inward-dipping monocline, which separates a blind inner reverse fault from an outer zone of normal faulting. Similar concentric zoning patterns can be recognized in coherent subsidence structures ranging over 16 orders of magnitude in size, from sandbox experiments to the giant Olympus Mons caldera on Mars.

  15. Measuring Variable Scales of Surface Deformation in and around the Yellowstone Caldera with TerraSAR-X Interferometry

    Science.gov (United States)

    Wicks, C. W., Jr.; Dzurisin, D.

    2014-12-01

    Utilizing three years of TerraSAR-X (TSX) Stripmap data covering the Yellowstone Caldera, Wyoming, we identify several examples showing the benefits of the high spatial and temporal resolution TSX data. Although the Stripmap footprints are small, compared to those of past SAR satellites, we are nonetheless able to track subsidence/uplift cycles of the ~50 x 80 km Yellowstone caldera using multiple strips. The Stripmap data are also useful for measuring deformation associated with the area of the North Rim anomaly, an area of repeated uplift and subsidence, ~30 km in diameter near the intersection of the north caldera rim, north-trending Mammoth-Norris Corridor, and west-northwest trending seismic belt east of Hebgen Lake. We measured ~45 mm of uplift associated with an episode that occurred mostly during the winter of 2013-2014 (as verified by GPS), and ~15 mm of subsequent subsidence in the early summer of 2014. The TSX Stripmap data have also proven effective at measuring small-scale deformation features. Because of the high-resolution of the TSX Stripmap data, we have also been able to measure many small-scale deforming features in Yellowstone National Park that are associated with apparent aquifer discharge/recharge cycles, unstable slope movement, geyser basin deformation, and deformation related to other hydrothermal features. We present an example of ~3 cm of seasonal deformation likely resulting from water movement in and out of an aquifer along the southwest caldera rim. We also document subsidence of ~1 cm/yr in a circular area nearly 0.5 km across near the vent from the Pitchstone Plateau, a thick rhyolite flow that erupted nearly 70 ka. TSX data are instrumental in identifying the seasonal variation found in some of these features, and in measuring the small spatial areas of deformation associated with other features.

  16. A 2-D FEM thermal model to simulate water flow in a porous media: Campi Flegrei caldera case study

    OpenAIRE

    V. Romano; Tammaro, U.; P. Capuano

    2012-01-01

    Volcanic and geothermal aspects both exist in many geologically young areas. In these areas the heat transfer process is of fundamental importance, so that the thermal and fluid-dynamic processes characterizing a viscous fluid in a porous medium are very important to understand the complex dynamics of the these areas. The Campi Flegrei caldera, located west of the city of Naples, within the central-southern sector of the large graben of Campanian plain, is a region where both volcani...

  17. Fluid flow in the resurgent dome of Long Valley Caldera: Implications from thermal data and deep electrical sounding

    Science.gov (United States)

    Pribnow, D.F.C.; Schutze, C.; Hurter, S.J.; Flechsig, C.; Sass, J.H.

    2003-01-01

    Temperatures of 100??C are measured at 3 km depth in a well located on the resurgent dome in the center of Long Valley Caldera, California, despite an assumed >800??C magma chamber at 6-8 km depth. Local downflow of cold meteoric water as a process for cooling the resurgent dome is ruled out by a Pecle??t-number analysis of temperature logs. These analyses reveal zones with fluid circulation at the upper and lower boundaries of the Bishop Tuff, and an upflow zone in the metasedimentary rocks. Vertical Darcy velocities range from 10 to 70 cm a-1. A 21-km-long geoelectrical profile across the caldera provides resistivity values to the order of 100 to >103 ??m down to a depth of 6 km, as well as variations of self-potential. Interpretation of the electrical data with respect to hydrothermal fluid movement confirms that there is no downflow beneath the resurgent dome. To explain the unexpectedly low temperatures in the resurgent dome, we challenge the common view that the caldera as a whole is a regime of high temperatures and the resurgent dome is a local cold anomaly. Instead, we suggest that the caldera was cooled to normal thermal conditions by vigorous hydrothermal activity in the past, and that a present-day hot water flow system is responsible for local hot anomalies, such as Hot Creek and the area of the Casa Diablo geothermal power plant. The source of hot water has been associated with recent shallow intrusions into the West Moat. The focus of planning for future power plants should be to locate this present-day flow system instead of relying on heat from the old magma chamber. ?? 2003 Elsevier B.V. All rights reserved.

  18. Aquifer Recharge Estimation through Atmospheric Chloride Mass Balance at Las Cañadas Caldera, Tenerife, Canary Islands, Spain

    OpenAIRE

    Rayco Marrero-Diaz; Alcalá, Francisco J.; Nemesio M. Pérez; Dina L. López; Gladys V. Melián; Eleazar Padrón; Germán D. Padilla

    2015-01-01

    The atmospheric chloride mass balance (CMB) method was used to estimate net aquifer recharge in Las Cañadas Caldera, an endorheic summit aquifer area about 2000 m a.s.l. with negligible surface runoff, which hosts the largest freshwater reserve in Tenerife Island, Canary Islands, Spain. The wet hydrological year 2005–2006 was selected to compare yearly atmospheric chloride bulk deposition and average chloride content in recharge water just above the water table, both deduced from periodical...

  19. Evidence from cosmic ray exposure (CRE) dating for the existence of a pre-Minoan caldera on Santorini, Greece

    Science.gov (United States)

    Athanassas, C. D.; Bourlès, D. L.; Braucher, R.; Druitt, T. H.; Nomikou, P.; Léanni, L.

    2016-05-01

    Cosmic ray exposure (CRE) dating was performed on the caldera cliffs of Santorini with the aim of detecting cliff segments predating the Minoan eruption (17th century BCE). The methodology involved the determination of in situ-produced cosmogenic 36Cl concentration in basaltic-to-rhyodacitic whole rocks cropping out in the cliffs. After the samples were processed following the chemical protocol of 36Cl preparation for silicate rocks, 36Cl concentrations were measured by accelerator mass spectrometry (AMS). Important challenges during the implementation procedure were related to large amounts of radiogenic 36Cl, complex modeling of inherited 36Cl, and dominance of the thermal and epithermal (low-energy) neutron capture production pathway. Nevertheless, quantitative assessments on the basis of the contribution of the low-energy neutron capture pathway percent to the total production rate validated the calculated CRE dates. Current CRE ages demonstrate that an ancient caldera existed on pre-Minoan Santorini, occupying at least the northern half of the modern-day caldera.

  20. 3D modelling of the Tejeda Caldera cone-sheet swarm, Gran Canaria, Canary Islands, Spain

    Science.gov (United States)

    Samrock, Lisa K.; Jensen, Max J.; Burchardt, Steffi; Troll, Valentin R.; Mattsson, Tobias; Geiger, Harri

    2015-04-01

    Cone-sheet swarms provide vital information on the interior of volcanic systems and their plumbing systems (e.g. Burchardt et al. 2013). This information is important for the interpretation of processes and dynamics of modern and ancient volcanic systems, and is therefore vital for assessing volcanic hazards and to reduce risks to modern society. To more realistically model cone-sheet emplacement an approximation of their 3D shape needs to be known. Most cone-sheet swarms are not sufficiently exposed laterally and/or vertically, however, which makes it difficult to determine the geometry of a cone-sheet swarm at depth, especially since different shapes (e.g. convex, straight or concave continuations) would produce a similar trace at the surface (cf. Burchardt et al. 2011, and references therein). The Miocene Tejeda Caldera on Gran Canaria, Canary Islands, Spain, hosts a cone-sheet swarm that was emplaced into volcaniclastic caldera infill at about 12.3-7.3 Ma (Schirnick et al. 1999). The dyke swarm displays over 1000 m of vertical exposure and more than 15 km of horizontal exposure, making it a superb locality to study the evolution of cone-sheet swarms in detail and to determine its actual geometry in 3D space. We have used structural data of Schirnick (1996) to model the geometry of the Tejeda cone-sheet in 3D, using the software Move® by Midland Valley Ltd. Based on previous 2D projections, Schirnick et al. (1999) suggested that the cone-sheet swarm is formed by a stack of parallel intrusive sheets which have a truncated dome geometry and form a concentric structure around a central axis, assuming straight sheet-intrusions. Our 3D model gives insight into the symmetries of the sheets and the overall geometry of the cone-sheet swarm below the surface. This visualization now allows to grasp the complexity of the Tejeda cone-sheet swarm at depth, particularly in relation to different possible cone-sheet geometries suggested in the literature (cf. Burchardt et al

  1. Scenario earthquake hazards for the Long Valley Caldera-Mono Lake area, east-central California

    Science.gov (United States)

    Chen, Rui; Branum, David M.; Wills, Chris J.; Hill, David P.

    2014-01-01

    As part of the U.S. Geological Survey’s (USGS) multi-hazards project in the Long Valley Caldera-Mono Lake area, the California Geological Survey (CGS) developed several earthquake scenarios and evaluated potential seismic hazards, including ground shaking, surface fault rupture, liquefaction, and landslide hazards associated with these earthquake scenarios. The results of these analyses can be useful in estimating the extent of potential damage and economic losses because of potential earthquakes and in preparing emergency response plans. The Long Valley Caldera-Mono Lake area has numerous active faults. Five of these faults or fault zones are considered capable of producing magnitude ≥6.7 earthquakes according to the Uniform California Earthquake Rupture Forecast, Version 2 (UCERF 2) developed by the 2007 Working Group of California Earthquake Probabilities (WGCEP) and the USGS National Seismic Hazard Mapping (NSHM) Program. These five faults are the Fish Slough, Hartley Springs, Hilton Creek, Mono Lake, and Round Valley Faults. CGS developed earthquake scenarios for these five faults in the study area and for the White Mountains Fault to the east of the study area. Earthquake scenarios are intended to depict the potential consequences of significant earthquakes. They are not necessarily the largest or most damaging earthquakes possible. Earthquake scenarios are both large enough and likely enough that emergency planners should consider them in regional emergency response plans. Earthquake scenarios presented here are based on fault geometry and activity data developed by the WGCEP, and are consistent with the 2008 Update of the United States National Seismic Hazard Maps (NSHM).For the Hilton Creek Fault, two alternative scenarios were developed in addition to the NSHM scenario to account for different opinions in how far north the fault extends into the Long Valley Caldera. For each scenario, ground motions were calculated using the current standard practice

  2. Sulfur Isotope Chemistry of the Uzon Caldera Active Hydrothermal System, Kamchatka, Far-East Russia

    Science.gov (United States)

    Hollingsworth, E. R.; Crowe, D. E.

    2006-05-01

    The Uzon Caldera is an actively precipitating As-Sb-Au epithermal system located on the Kamchatka Peninsula of Far-East Russia. Present at the surface of the caldera is a remarkable diversity of thermal fluid types discharging within the geothermal fields. These fluids have subsequently produced a broad array of S- bearing alteration minerals both within and around pools, hotsprings, mudpots, and fumaroles. Using the δD/δ18O/δ34S and dissolved ion chemistry of the thermal fluids, three types were distinguished as follows: 1) an acid sulfate type with δD/δ18O/δ34S values ranging between -74.66‰ to -100.33‰, - 2.30‰ to -9.57‰, and -0.3‰ to 0.3‰ respectively with sulfate being the dominant anion ranging between 504ppm and 3439ppm 2) an alkali chloride type with δD/δ18O/δ34S values ranging between -97.22‰ to -104.37‰, - 8.8‰ to -11.43‰ respectively with chloride being the dominant anion ranging between 1090ppm to 2405ppm, and 3) a dilute type resulting from the mixture of the alkali-chloride endmember with the cold meteoric waters present at the surface subsequently generating δD/δ18O/δ34S values ranging between -82.00‰ to -119.34‰, -6.02‰ to -15.76‰, and +1.9‰ to +13.5‰ with dissolved ion concentrations falling along a mixing line between the two endmember components. The interpretations made from the presence of these three fluid types were used in conjunction with the δ34S of the S-bearing alteration minerals from within and around the various water and gas sources (values ranging between -1.94‰ to +5.7‰ and -5.19‰ to +1.6‰ respectively) to construct a sulfur evolution model for the Uzon's hydrothermal system. Results of the model show the chemical and isotopic processes responsible for the speciation and isotopic signature of the S-bearing phases collected at the surface (both aqueous and mineral) are not only dictated by the geologic processes at depth, but are also influenced by microbiological processes at the

  3. Deformation of the Long Valley Caldera, California: Inferences from measurements from 1988 to 2001

    Science.gov (United States)

    Langbein, J.O.

    2003-01-01

    Two periods of volcanic unrest occurred between 1989 and 1998 in the Long Valley Caldera, eastern California. Numerous earthquakes were recorded, and these periods of unrest were documented with high-precision geodetic measurements. The first round of unrest started rapidly in late 1989 and slowly decreased in rate through the early 1990s. For this interval there are both leveling and two-color electronic distance meter (EDM) measurements. The second round of unrest started slowly in mid-1997, climaxed in late 1997, and rapidly returned to quiescence by mid-1998. Deformation was recorded by both the two-color EDM and continuous GPS. Both episodes require inflation at 6-7 km beneath the resurgent dome, and both episodes had roughly 0.1 m extension across the resurgent dome. In addition, the data presented here suggest that there is a deeper, 10-20 km, inflation source beneath the south moat of the caldera. For both episodes, the better-resolved inflation beneath the resurgent dome is a near-vertical, prolate spheroid rather than an isotropic source, which suggests that magma came up through vertical cracks. However, the modeling suggests that the location changed with the depth from 6.0 to 6.7 km for the later episode. In contrast to the earlier episode, the 1997-1998 episode has additional deformation in the south moat, where the simplest model is that of a right-lateral slip on a steeply dipping plane that is defined by the location of earthquakes in the south moat. Models of the time-dependent behavior suggest that slip on this fault occurred from late November through December 1997, corresponding to the time of greatest moment release by the earthquake swarm in the south moat. Confounding the interpretation of these data is an active geothermal field near the center of the EDM network and adjacent to the south moat and resurgent dome. Additional modeling of leveling and EDM data within the geothermal field during a period of low rate of inflation of the dome

  4. Building a flood hazard map due to magma effusion into the caldera lake of the Baekdusan Volcano

    Science.gov (United States)

    Lee, K.; Kim, S.; Yun, S.; Yu, S.; Kim, I.

    2013-12-01

    Many volcanic craters and calderas are filled with large amounts of water that can pose significant flood hazards to downstream communities due to their high elevation and the potential for catastrophic releases of water. Recent reports pointed out the Baekdusan volcano that is located between the border of China and North Korea as a potential active volcano. Since Millennium Eruption around 1000 AD, smaller eruptions have occurred at roughly 100-year intervals, with the last one in 1903. The volcano is showing signs of waking from a century-long slumber recently and the volcanic ash may spread up to the northeastern of Japan. The development of various forecasting techniques to prevent and minimize economic and social damage is in urgent need. Floods from lake-filled calderas may be particularly large and high. Volcanic flood may cause significant hydrologic hazards for this reason. This study focuses on constructing a flood hazard map triggered by the uplift of lake bottom due to magma effusion in the Baekdusan volcano. A physically-based uplift model was developed to compute the amount of water and time to peak flow. The ordinary differential equation was numerically solved using the finite difference method and Newton-Raphson iteration method was used to solve nonlinear equation. The magma effusion rate into the caldera lake is followed by the past record from other volcanic activities. As a result, the hydrograph serves as an upper boundary condition when hydrodynamic model (Flo-2D) runs to simulate channel routing downstream. The final goal of the study stresses the potential flood hazard represented by the huge volume of water in the caldera lake, the unique geography, and the limited control capability. he study will contribute to build a geohazard map for the decision-makers and practitioners. Keywords: Effusion rate, Volcanic flood, Caldera lake, Uplift, Flood hazard map Acknowledgement This research was supported by a grant [NEMA-BAEKDUSAN-2012-1-2] from

  5. LA OPULENCIA EN LA ESCASEZ. INTERCAMBIOS DE OBJETOS, RELACIONES SOCIALES Y AMBIGÜEDADES EN INSTITUTOS CORRECCIONALES DE CÓRDOBA / Opulence on scarcity. Exchange of objects, social relations and ambiguities in correctional institutes of Córdoba

    Directory of Open Access Journals (Sweden)

    Graciela María Tedesco

    2009-12-01

    Full Text Available Este artículo se propone reflexionar sobre las relaciones sociales que se entrelazan durante el proceso de dar, recibir, intercambiar distintos objetos en institutos correccionales de la ciudad de Córdoba. A través del análisis de situaciones como “la visita”, “el arreglo de las habitaciones”, “el fumar y compartir en el sector”; se analizan formas de tejer vínculos con el afuera, actualizar recuerdos sobre la calle, y de producir intercambios y reforzar ciertos valores dentro del grupo que convive en el instituto. La descripción de estas situaciones implica asimismo, indagar los mecanismos y circuitos a través de los cuales se incorporan distintos sentidos a los objetos, así como también, el modo en que éstos configuran la subjetividad de las personas. De esta manera, el artículo busca mostrar la dinámica que lleva a que, en contextos institucionales marcados por privación y escasez, los jóvenes generen diversos intercambios y utilicen la ambigüedad como un medio para un construir abundancia y poder.Palabras clave: jóvenes, institutos correccionales, relaciones sociales, objetosAbstractThis article proposes to reflect on the social relations that are intertwined in the process of giving, receiving, exchanging various objects in correctional institutes in the city of Córdoba. Across the analysis of situations as “the visit”, “the arrangement of the bedroom”, “to smoke and share in the sector”; discusses ways to weave ties to the outside, upgrade memory on the street and produce exchanges and strengthen certain values within the group that lives in institute. The description of these situations also means, investigate the mechanisms and circuits through which incorporate different meanings to objects, and also, they shape the subjectivity of people. Thus, the article shows the dynamics means that, in institutional contexts marked by deprivation and scarcity, young men exchanges and use the ambiguity, as a

  6. Duration of the Banco Bonito Rhyolite Eruption, Vales Caldera, New Mexico based on magma transport modeling

    Energy Technology Data Exchange (ETDEWEB)

    Phillips, Benjamin R. [Los Alamos National Lab. (LANL), Los Alamos, NM (United States); Baldridge, W. Scott [Los Alamos National Lab. (LANL), Los Alamos, NM (United States); Gable, Carl W. [Los Alamos National Lab. (LANL), Los Alamos, NM (United States); Sicilian, James M. [Los Alamos National Lab. (LANL), Los Alamos, NM (United States)

    2007-03-05

    Finite volume calculations of the flow of rhyolite are presented to investigate the fate of viscous magmas flowing in planar fractures with realistic length to width ratios of up to 2500:1. Heat and mass transfer for a melt with a temperature dependent viscosity and the potential to undergo phase change are considered. Magma driving pressures and dike widths are chosen to satisfy simple elastic considerations. These models are applied within a parameter space relevant to the Banco Bonito rhyolite flow, Valles caldera, New Mexico. We estimate a maximum eruption duration for the event of ~200 days, realized at a minimum possible dike width of 5-6 m and driving pressure of 7-8 MPa. Simplifications in the current model may warrant scaling of these results. However, we demonstrate the applicability of our model to magma dynamics issues and suggest that such models may be used to infer information about both the timing of an eruption and the evolution of the associated magma source.

  7. Dynamic triggering of microearthquakes in the Long Valley Caldera and Coso Geothermal Field

    Science.gov (United States)

    Aiken, C.; Peng, Z.; Wu, C.

    2010-12-01

    Recent studies have shown that microearthquakes can be dynamically triggered by the passing of surface waves from regional and teleseismic events. However, the underlying physical mechanisms and the necessary conditions that favor dynamic triggering are still in debate. Here we conduct a systematic search of dynamically triggered microearthquakes around the Long Valley Caldera (LVC) and Coso Geothermal Field (CGF) in California. In each region, we select distant mainshocks in 1999-2010 with M>=7.5 over 1000 km away, or M>=5.5 between 100-2500 km. Next, we apply 2-8 or 2-16 Hz band-pass-filtered data to the three-component seismograms recorded at each region, and identify triggered events as high-frequency seismic energy during large-amplitude surface waves of regional and teleseismic events. We calculate the beta statistic values based on events listed in the local earthquake catalogs and hand-picked events from the envelope functions, and verify that the triggering is statistically significant. Based on this simple procedure, we have identified many distant events that have triggered activity in both regions, including the recent 08/03/2009 and 04/04/2010 Baja California earthquakes at regional distances, and the 02/27/2010 Chile earthquake at teleseismic distances. Our next steps are to examine the dynamic triggering thresholds in each region, and to understand the triggering potential in terms of frequency, amplitude, incident angle, and type of surface waves.

  8. Pre-caldera collapse of the Tastau volcanoplutonic ring complex (Eastern Kazakhstan)

    Science.gov (United States)

    Dokukina, K.

    2009-04-01

    positive chondrite-normalized REE patterns and negative europium anomaly (mafic enclaves (Ce/Yb)N=4.99 - 5.54, Eu/Eu*=0.68 - 0.78; granite (Ce/Yb)N=5.48 - 8.59, Eu/Eu*=0.24 - 0.64; felsite (Ce/Yb)N=2.50, Eu/Eu*=0.006), except the unhybrid gabbro (Ce/Yb)N=5.3380, Eu/Eu*=1.02). Compositions of the Tastau magmatic rocks hit the intraplate magmatism area and the active continental margins. Relative of succession of a main intrusive events in Tastau volcanoplutonic compex. First event: the calcium basite intrusion during high-speed shear deformation. Second event: the forming of a felsic radial dike swarm, which represents the caldera forming eruption of felsic melt. Third event: the forming of a first granosyenite intrusive ring and a first granosyenite stock, which represents first stage of the collapse caldera. Fourth event: the forming of a second granite intrusive ring and a second granite stock, which represents second stage of the collapse caldera. First of all the catastrophic deformation event in an enclosed space along with the calcium basite intrusion happened. The numerous small (1-70 cm) intrusive mafic bodies are situated mainly in the linear zone of a metasedimentary rock tectonic brecciation crossing the central part of Tastaut volcanoplutonic complex. Within this zone the lithified rock underwent a brittle-ductile deformation and cataclasis. The calcium basites form a dyke swarm and are a source of other bodies: globular, bag-like and irregular morphologies. The composition of the calcium basite is unusual and characterized by wide variations of all main chemical elements (SiO2 = 46.2 - 61.2 %, Al2O3 = 12.6 - 17.7 %, TiO2 = 0.55 - 0.85 %, FeOtot = 3.77 - 6.87 %, MnO = 0.35 - 0.68 %, MgO = 2.0 - 5.64), low alkali contents (Na2O + K2O = 0.78 - 2.9 %) and high contents of CaO (10.8 - 20.7 %). The mafic magma emplacement controlled by regional compressive shear deformation. The magma fragmentation was due to the significant decreasing of viscosity of disintegrated

  9. The shallow-water chitons (Mollusca, Polyplacophora of Caldera, Region of Atacama, northern Chile

    Directory of Open Access Journals (Sweden)

    Juan Francisco Araya

    2015-03-01

    Full Text Available The Molluscan species of the northern littoral of Chile have been sparsely studied. This work reviews for the first time the diversity of polyplacophoran molluscs around the port of Caldera, in the Region of Atacama (26°45’49”S; 70°45’17”W to 27°20’23”S; 70°56’46”W, northern Chile. Eleven species were found in this study: Acanthopleura echinata (Barnes, 1824; Callistochiton pulchellus (Gray, 1828; Calloplax vivipara (Plate, 1899, Chaetopleura peruviana (Lamarck, 1819; Chiton cumingsii Frembly, 1827; Chiton granosus Frembly, 1827; Chiton magnificus Deshayes, 1827; Enoplochiton niger (Barnes, 1824, Radsia barnesii (Gray, 1828, Tonicia atrata (G. B. Sowerby II, 1840 and Tonicia chilensis (Frembly, 1827. All of the species occurring in the area have distributions in the southeastern Pacific Ocean, from Ecuador to central Chile, and three of them are species endemic to the Chilean coasts (Calloplax vivipara, Radsia barnesii, and Tonicia atrata. This diversity of species is comparable to that of better surveyed faunas of central and southern Chile or Patagonia. Of the eleven species recorded, the geographic distribution records for Callistochiton pulchellus, Radsia barnesii and Tonicia atrata are extended, and Calloplax vivipara is found alive again after 40 years, filling a gap in its known distribution. Illustrations of living specimens in their habitat, distribution records and a taxonomic key for all the studied taxa are also provided.

  10. Desarrollo e implementación de integradores de plataforma utilizando Fi-Ware

    OpenAIRE

    Diez Villamañán, Ricardo

    2015-01-01

    El objetivo del proyecto es crear un prototipo para un sistema de control de temperatura en un lugar determinada utilizando Internet de las Cosas para interconectar objetos. El prototipo será dotado de Inteligencia Artificial a través del uso de lógica difusa para su automatización. Por un lado se van a consumir datos de algunas de las plataformas Internet de las Cosas que se encuentran abiertas a usuarios ofreciendo información de multitud de sensores localizados en distintos lugares. ...

  11. Monitoramento dos extratos brutos de espécies de Polygala (Polygalaceae utilizando Artemia salina

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    A.B.P. Montanher

    2003-01-01

    Full Text Available Extratos de duas espécies de Polygala foram submetidos a um biomonitoramento utilizando o teste de toxicidade frente a Artemia salina, com a finalidade de detectar atividade citotóxica. Os resultados obtidos para o extrato bruto, frações hexânica e diclorometano de Polygala sabulosa Aw. Benn. mostraram-se promissores. No entanto, bioensaios mais específicos devem ser encorajados nos extratos vegetais que apresentam atividade diante deste bioensaio, a fim de confirmar estas conclusões.

  12. Análisis de paneles solares térmicos utilizando software gratuito

    OpenAIRE

    Castellanos Cordeiro-Crespo, Antonio

    2009-01-01

    El objetivo de este proyecto es la evaluación de dos programas que trabajan en la simulación de paneles termosolares: KOLEKTOR Y CODEPRO. Para la valoración de dichos software tomaremos datos en el panel solar con el que cuenta la Universidad Politécnica de Cracovia. Después simularemos, utilizando las aplicaciones a estudio, introduciendo las mismas condiciones de la toma de datos, y compararemos los resultados obtenidos en ambos procedimientos. Lo más positivo es que ambos software son bast...

  13. Reconstrucción 3D de malas hierbas utilizando cámaras de profundidad

    OpenAIRE

    Andújar, D.; Ribeiro, A.; Bengoechea, J. M.; San Martín, C.; Fernández Quintanilla, C.; Dorado, J.

    2015-01-01

    El objetivo de este estudio fue optimizar el ángulo de posicionamiento del sensor Kinect para la reconstrucción de la estructura tridimensional de Xanthium strumarium L., Datura stramonium L. y Chenopodium album L., utilizando para ello algoritmos que permiten la captura y combinación de imágenes de profundidad y RGB. Se han comparado diferentes ángulos, fijando en cada uno de ellos el sensor Kinect de forma estática respecto de la planta objetivo. Los resultados han confirmado la correlación...

  14. A complex magma reservoir system for a large volume intra- to extra-caldera ignimbrite: Mineralogical and chemical architecture of the VEI8, Permian Ora ignimbrite (Italy)

    Science.gov (United States)

    Willcock, M. A. W.; Bargossi, G. M.; Weinberg, R. F.; Gasparotto, G.; Cas, R. A. F.; Giordano, G.; Marocchi, M.

    2015-11-01

    Intra-caldera settings record a wealth of information on caldera-forming processes, yet field study is rarely possible due to lack of access and exposure. The Permian Ora Formation, Italy, preserves > 1000 m of vertical section through its intra-caldera succession. This provides an excellent opportunity to detail its mineralogical and geochemical architecture and gain understanding of the eruption evolution and insight into the pre-eruptive magma system. Detailed juvenile clast phenocryst and matrix crystal fragment point count and image analysis data, coupled with bulk-rock chemistry and single mineral compositional data, show that the Ora ignimbrite succession is rhyolitic (72.5-77.7% SiO2), crystal-rich (~ 25-57%; average 43%) and has a constant main mineral population (volcanic quartz + sanidine + plagioclase + biotite). Although a seemingly homogeneous ignimbrite succession, important subtle but detectable lateral and vertical variations in modal mineralogy and bulk-rock major and trace elements are identified here. The Ora Formation is comprised of multiple lithofacies, dominated by four densely welded ignimbrite lithofacies. They are crystal-rich, typically lithic-poor (cake' stratigraphy. The intra-caldera succession is divided into two depo-centres: Southern and Northern, with proximal extra-caldera deposits preserved to the south and north of the system. The Southern and Northern intra-caldera ignimbrite successions are discriminated by variations in total biotite crystal abundance. Detailed mineralogical and chemical data records decreases across the caldera system from south to north in biotite phenocrysts in the groundmass of juvenile clasts (average 12-2%), matrix biotite (average 7.5-2%) and plagioclase crystal fragments (average 18-6%), and total crystal fragment abundance in the matrix (average 47-37%); a biotite compositional change to iron-rich (0.57-0.78 Fe); and bulk-rock element decreases in Fe2O3, MgO, P2O5, Ce, Hf, V, La and Zr, and

  15. The Evolution of the Campi Flegrei caldera (Italy): High- and low-frequency multichannel 2.5D seismic surveying for an amphibian IODP/ICDP drilling approach

    Science.gov (United States)

    Steinmann, Lena; Spiess, Volkhard; Sacchi, Marco

    2016-04-01

    Caldera-forming eruptions are considered as one of the most catastrophic natural events to affect the Earth's surface and human society. The half-submerged Campi Flegrei caldera, located in southern Italy, belongs to the world's most active calderas and, thus, has received particular attention in scientific communities and governmental institutions. Therefore, it has also become subject to a joint approach in the IODP and ICDP programmes. Despite ample research, no scientific consensus regarding the formation history of the Campi Flegrei caldera has been reached yet. So far, it is still under debate whether the Campi Flegrei caldera was formed by only one ignimbritic eruption, namely the Neapolitan Yellow Tuff (NYT) eruption at 15 ka or, if it is a nested-caldera system related to the NYT and the Campanian Ignimbrite (CI) eruption at 39 ka. In the last decades, the Campi Flegrei caldera has been characterized by short-term episodes of unrest involving considerable ground deformation (uplift and subsidence of several meters), seismicity and increased temperature at fumaroles. Furthermore, long-term deformation can be observed in the central part of the caldera with uplift rates of several tens of meters within a few thousand years. Recently, it has been proposed that the long-term deformation may be related to caldera resurgence, while short-term uplift episodes are probably triggered by the injection of magmatic fluids into a shallow hydrothermal system at ~2 km depth. However, both long-term and short term uplift could be interpreted as eruption precursor, thereby posing high-concern for a future eruption, which would expose more than 1.5 million people living in the surroundings of the volcanic district to extreme volcanic risks. During a joint Italian-German research expedition in 2008, a semi-3D grid (100-150 m profile spacing) of high-frequency (up to 1000 Hz) multichannel seismic data were acquired to support both the ongoing onshore ICDP and a proposed

  16. Exportaciones, términos de intercambio y crecimiento económico de Brasil y México, de 1960 a 2002: un análisis comparativo

    Directory of Open Access Journals (Sweden)

    Carlos Alberto Fraga Castillo

    2006-01-01

    Full Text Available México y Brasil son las economías más grandes de la región, caracterizadas por una fuerte presencia de la industria. Ambas han tenido, en diferente grado, un cambio importante en su estrategia de desarrollo, pasando de un modelo centrado en la sustitución de importaciones y la intervención del Estado en la economía a otro modelo abierto a la competencia externa y concentrado en las exportaciones como motor de impulso. El propósito de este trabajo es precisamente comparar en qué medida dicha reorientación "hacia el sector externo"se revela en la capacidad de arrastre del sector exportador al resto de la economía. Para ello se evalúan las elasticidades de comercio y -con base en el modelo desarrollado por A.P. Thirlwall- se estima su impacto en la tasa de crecimiento económico de largo plazo. crecimiento, restricción, intercambio, exportaciones, balanza.

  17. Mecanismos de intercambio en períodos de transición: el caso de los arrendamientos de dos estancias de la Puna jujeña (1813-1819

    Directory of Open Access Journals (Sweden)

    Conti, Viviana E.

    1994-06-01

    Full Text Available Not available.

    Las condiciones de desarrollo y consolidación del sistema colonial mercantilista en los Andes Meridionales se modifican rápidamente en la segunda mitad del XVIII. Pero se trata de una modificación ambigua: renacer de la minería potosina y reverdecer del comercio por un lado, pero reiteradas crisis estructurales -guerras y sequias-« por el otro. En la primera década del XIX es evidente el deterioro de todo el sistema pero también las estrategias asumidas para detenerlo. En este artículo se examinan los arrendamientos de tierras en plena Guerra de Independencia como fuente rentística colonial, acceso alternativo a bienes y moneda y conjunto de estrategias comerciales del campesinado de la Puna jujeña. Se concluye que estos campesinos mantuvieron su producción e intercambios captando moneda en el circuito mercantil. Los arrendamientos, como antes el tributo, marcan el éxito de las estrategias indígenas en el manejo de plata y bienes frente al mercado y al pago mismo de sus obligaciones.

  18. Modelos de elección discreta aplicados a la estimación de la distribución geográfica de los intercambios comerciales en Andalucia

    Directory of Open Access Journals (Sweden)

    José Manuel Rueda Cantuche

    2002-01-01

    Full Text Available El trabajo que se realiza quinquenalmente para la elaboración del Marco Input-Output requiere una cantidad de recursos que difícilmente pueden ser asignados anualmente a este cometido. Por ello, pueden resultar de enorme utilidad todos aquellos trabajos de investigación sobre la aplicación de nuevos instrumentos de carácter cuantitativo y estocástico que permitan establecer estimaciones sobre determinadas variables económicas necesarias para la construcción de dicho Marco pero con carácter anual. En esta comunicación se presentan los primeros avances de un proyecto de investigación que aplica modelos de elección discreta con datos ordenados para la elaboración de una metodología que permita conocer los intercambios comerciales de productos entre Andalucía y el resto de España, a través de comerciantes mayoristas e intermediarios de comercio.

  19. Oceanographic signatures and pressure monitoring of seafloor vertical deformation in near-coastal, shallow-water areas: a case study from Santorini Caldera.

    Science.gov (United States)

    Vilaseca, Géraud; Deplus, Christine; Escartin, Javier; Ballu, Valérie; Nomikou, Paraskevi; Mével, Catherine; Andreani, Muriel

    2016-04-01

    Bottom pressure, tilt and seawater physical-properties were monitored for a year using two instruments within the immerged Santorini caldera (Greece). Piggy-backed on the CALDERA2012 cruise, this geodetic experiment was designed to monitor evolution of the 2011-2012 Santorini unrest. Conducted during a quiescent period, it allowed us to study oceanographic and atmospheric signal in our data series. We observe periodic oceanographic signals associated with tides, and seiches that are likely linked to both the caldera and Cretan basin geometries. In winter, the caldera witnesses sudden cooling events that tilt an instrument towards the Southeast, indicating cold-water influx likely originating from the north-western passage between Thirasia and Oia. We do not obtain evidence of long-term vertical seafloor deformation from the pressure signal, although it may be masked by instrumental drift. However, tilt data suggests a local seafloor tilt event ~1 year after the end of the unrest period which could be consistent with inflation under or near Nea Kameni. In addition, we illustrate that tilt sensor can roughly record seismic induced ground motion which in our case led to a shift in sensors attitude for one seismic event. Seafloor geodetic data recorded at the bottom of the Santorini caldera illustrates that the oceanographic signature is an important part of the signal, which needs to be considered for monitoring volcanic or geological seafloor deformation in shallow-water and/or nearshore areas.

  20. The earliest low and high δ18O caldera-forming eruptions of the Yellowstone plume: implications for the 30–40 Ma Oregon calderas and speculations on plume-triggered delaminations

    OpenAIRE

    Seligman, Angela N.; Bindeman, Ilya N.; McClaughry, Jason; Stern, Richard A.; Fisher, Chris

    2014-01-01

    We present new isotopic and trace element data for four eruptive centers in Oregon: Wildcat Mountain (40 Ma), Crooked River (32–28 Ma), Tower Mountain (32 Ma), and Mohawk River (32 Ma). The first three calderas are located too far east to be sourced through renewed subduction of the Farallon slab following accretion of the Yellowstone-produced Siletzia terrane at ~50 Ma. Basalts of the three eastern eruptive centers yield high Nb/Yb and Th/Yb ratios, indicating an enriched sublithospheric man...

  1. The earliest low and high δ18O caldera-forming eruptions of the Yellowstone plume: Implications for the 30–40 Ma Oregon calderas and speculations on plume-triggered delaminations

    OpenAIRE

    Angela Nicole Seligman; Bindeman, Ilya N.; Jason eMcClaughry; Richard eStern; Chris eFisher

    2014-01-01

    We present new isotopic and trace element data for four eruptive centers in Oregon: Wildcat Mountain (40 Ma), Crooked River (32–28 Ma), Tower Mountain (32 Ma), and Mohawk River (32 Ma). The first three calderas are located too far east to be sourced through renewed subduction of the Farallon slab following accretion of the Yellowstone-produced Siletzia terrane at ~50 Ma. Basalts of the three eastern eruptive centers yield high Nb/Yb and Th/Yb ratios, indicating an enriched sublithospheric man...

  2. Estudio vulcanológico y qeoquímico del maar de la Caldera del Rey. Tenerife (Canarias

    Directory of Open Access Journals (Sweden)

    Paradas Herrero, A.

    1984-12-01

    Full Text Available In this study a cartographic, morphological, geochemical and petrographic study is made of the ''Caldera del Rey". The "Caldera del Rey" is a volcanic structure formed by two overlapping maars, The second one (maar that was formed is of greaten dimensions and destroyed part of the first one, Both maars erupted throught a possible fracture N 35 E, which is one of the directions with regional importance in the Archipelago. The eruption, which was very explosive, has been thought to be due in part to the great importance of the gaseous phase of the salic magma and also to the steam produced during the interaction of the magma with underground water. This explosivity can be clearly seen in the cleaf resalte cul out in the "Serie Basáltica Antigua" to some extent penetrated and fragmented by the eruption, The phreatomagmatic character of the eruption is evident because of the existence of accretionary lapilli. The materials emitted are exc1usively of aerial projection: agglomerates, tuffs cinerites. There was no flow of lava. ' Some of the fragments of tuffs as cinerites and pumice are comagmatic. These correspond to salic trachytic phonolitic rocks, which represent one of the last stages of differentiation of the alkaline oceanic magmas. The geochemical character of the materials of the "Caldera del Rey" is characteristic and can be easily distinguished from other nearly salic deposits formed in different cycles.

    En este trabajo se hace el estudio cartográfico, morfológico, petrográfico y geoquímico de la Caldera del Rey. La Caldera del Reyes un edificio volcánico formado por dos maars imbricados. El que se formó en segundo lugar es de mayores dimensiones y destruyó en parte el primero. Ambos aprovecharon para hacer erupción una posible fractura de dirección N 35'"E, de importancia regional en el Archipiélago. La erupción fue de una gran explosividad, que se supone debida, en parte, a la gran importancia de la fase gaseosa del

  3. Caldera resurgence as a possible cause of slope failure in volcanic areas: the Ischia island case history

    Science.gov (United States)

    de Vita, Sandro; Seta Marta, Della; Paola, Fredi; Enrica, Marotta; Giovanni, Orsi; Fabio, Sansivero

    2010-05-01

    Slope instability in active volcanic areas is a factor of major hazard to be considered. Due to their rapid growth and deformation, active volcanoes experience gravitational disequilibrium and periodical structural failures. Depending on the geodynamic framework of a volcano, nature, style of activity and climatic conditions, slope instability occurs at different scales, from relatively small-volume mass movements to huge lahars and debris avalanches. Moreover, volcanoes located in coastal areas or islands, may experience lateral collapses with the potential to generate large tsunamis. Although there is very little literature on the relationships among caldera resurgence, volcanism and slope instability, recently also the caldera resurgence has been suggested as a possible cause of slope failure, as for the southern flank of the island of Ischia in the Southern Tyrrhenian sea (Italy). Ischia island gives a good opportunity to investigate such phenomena and related effects, as it is the only documented example of resurgent caldera in which, during uplift, volcanism and generation of mass movements have been very active and linked to each other in a sort of cyclical behaviour. The island of Ischia is one of the most impressive examples of resurgent calderas in the world. This caldera formed in response to a complex explosive eruption that, about 55 ka B.P., produced the Mt. Epomeo Green Tuff ignimbritic deposit. Starting from at least 30 ka B.P. the caldera floor has been uplifted of about 900 m, due to a resurgent phenomenon, which occurred through intermittent uplifting, likely triggered by the intrusion of new magma into the system, and tectonic quietness phases. During uplift, volcanism and generation of mass movements were very active. The resurgent area is composed of differentially displaced blocks and has a poligonal shape, resulting from reactivation of regional faults and activation of faults directly related to volcano-tectonism. The western sector is

  4. Real-time monitoring of seismicity and deformation during the Bárdarbunga rifting event and associated caldera subsidence

    Science.gov (United States)

    Jónsdóttir, Kristín; Ófeigsson, Benedikt; Vogfjörd, Kristín; Roberts, Matthew; Barsotti, Sara; Gudmundsson, Gunnar; Hensch, Martin; Bergsson, Bergur; Kjartansson, vilhjálmur; Erlendsson, Pálmi; Friðriksdóttir, Hildur; Hreinsdóttir, Sigrún; Guðmundsson, Magnús; Sigmundsson, Freysteinn; Árnadóttir, Thóra; Heimisson, Elías; Hjorleifsdóttir, Vala; Soring, Jón; Björnsson, Bogi; Oddsson, Björn

    2015-04-01

    We present a monitoring overview of a rifting event and associated caldera subsidence in a glaciated environment during the Bárðarbunga volcanic crisis. Following a slight increase in seismicity and a weak deformation signal, noticed a few months before the unrest by the SIL monitoring team, an intense seismic swarm began in the subglacial Bárðarbunga caldera on August 16 2014. During the following two weeks, a dyke intruded into the crust beneath the Vatnajökull ice cap, propagating 48 km from the caldera to the east-north-east and north of the glacier where an effusive eruption started in Holuhraun. The eruption is still ongoing at the time of writing and has become the largest eruption in over 200 years in Iceland. The dyke propagation was episodic with a variable rate and on several occasions low frequency seismic tremor was observed. Four ice cauldrons, manifestations of small subglacial eruptions, were detected. Soon after the swarm began the 7x11 km wide caldera started to subside and is still subsiding (although at slower rates) and has in total subsided over 60 meters. Unrest in subglacial volcanoes always calls for interdisciplinary efforts and teamwork plays a key role for efficient monitoring. Iceland has experienced six subglacial volcanic crises since modern digital monitoring started in the early 90s. With every crisis the monitoring capabilities, data interpretations, communication and information dissemination procedures have improved. The Civil Protection calls for a board of experts and scientists (Civil Protection Science Board, CPSB) to share their knowledge and provide up-to-date information on the current status of the volcano, the relevant hazards and most likely scenarios. The evolution of the rifting was monitored in real-time by the joint interpretation of seismic and cGPS data. The dyke propagation could be tracked and new, updated models of the dyke volume were presented at the CPSB meetings, often daily. In addition, deformation

  5. Strengths and strain energies of volcanic edifices: implications for eruptions, collapse calderas, and landslides

    Directory of Open Access Journals (Sweden)

    A. Gudmundsson

    2012-07-01

    Full Text Available Natural hazards associated with volcanic edifices depend partly on how fracture resistant the edifices are, i.e. on their strengths. Observations worldwide indicate that large fluid-driven extension fractures (dikes, inclined sheets, shear fractures (landslides, and mixed-mode fractures (ring dikes and ring faults normally propagate more easily in a basaltic edifice (shield volcano than in a stratovolcano. For example, dike-fed eruptions occur once every few years in many basaltic edifices but once every 102-3 yr in many stratovolcanoes. Large landslides and caldera collapses also appear to be more common in a typical basaltic edifice/shield volcano than in a typical stratovolcano. In contrast to a basaltic edifice, a stratovolcano is composed of mechanically dissimilar rock layers, i.e. layers with mismatching elastic properties (primarily Young's modulus. Elastic mismatch encourages fracture deflection and arrest at contacts and increases the amount of energy needed for a large-scale edifice failure. Fracture-related hazards depend on the potential energy available to propagate the fractures which, in turn, depends on the boundary conditions during fracture propagation. Here there are two possible scenarios: one in which the outer boundary of the volcanic edifice or rift zone does not move during the fracture propagation (constant displacement; the other in which the boundary moves (constant load. In the former, the total potential energy is the strain energy stored in the volcano before fracture formation; in the latter, the total potential energy is the strain energy plus the work done by the forces moving the boundary. Constant-displacement boundary conditions favor small eruptions, landslides, and caldera collapses, whereas constant-load conditions favor comparatively large eruptions, landslides, and collapses. For a typical magma chamber (sill-like with a diameter of 8 km, the strain energy change due to magma-chamber inflation

  6. Water-level changes induced by local and distant earthquakes at Long Valley caldera, California

    Science.gov (United States)

    Roeloffs, E.; Sneed, M.; Galloway, D.L.; Sorey, M.L.; Farrar, C.D.; Howle, J.F.; Hughes, J.

    2003-01-01

    Distant as well as local earthquakes have induced groundwater-level changes persisting for days to weeks at Long Valley caldera, California. Four wells open to formations as deep as 300 m have responded to 16 earthquakes, and responses to two earthquakes in the 3-km-deep Long Valley Exploratory Well (LVEW) show that these changes are not limited to weathered or unconsolidated near-surface rocks. All five wells exhibit water-level variations in response to earth tides, indicating they can be used as low-resolution strainmeters. Earthquakes induce gradual water-level changes that increase in amplitude for as long as 30 days, then return more slowly to pre-earthquake levels. The gradual water-level changes are always drops at wells LKT, LVEW, and CH-10B, and always rises at well CW-3. At a dilatometer just outside the caldera, earthquake-induced strain responses consist of either a step followed by a contractional strain-rate increase, or a transient contractional signal that reaches a maximum in about seven days and then returns toward the pre-earthquake value. The sizes of the gradual water-level changes generally increase with earthquake magnitude and decrease with hypocentral distance. Local earthquakes in Long Valley produce coseismic water-level steps; otherwise the responses to local earthquakes and distant earthquakes are indistinguishable. In particular, water-level and strain changes in Long Valley following the 1992 M7.3 Landers earthquake, 450 km distant, closely resemble those initiated by a M4.9 local earthquake on November 22, 1997, during a seismic swarm with features indicative of fluid involvement. At the LKT well, many of the response time histories are identical for 20 days after each earthquake, and can be matched by a theoretical solution giving the pore pressure as a function of time due to diffusion of a nearby, instantaneous, pressure drop. Such pressure drops could be produced by accelerated inflation of the resurgent dome by amounts too

  7. Hydrothermal activity and subsurface soil complexity: implication for outgassing processes at Solfatara crater, Campi Flegrei caldera

    Science.gov (United States)

    Montanaro, Cristian; Mayer, Klaus; Scheu, Bettina; Isaia, Roberto; Mangiacapra, Annarita; Gresse, Marceau; Vandemeulebrouck, Jean; Moretti, Roberto; Dingwell, Donald B.

    2016-04-01

    The Solfatara area and its fumaroles are the main surface phenomena of the vigorous hydrothermal activity within the active Campi Flegrei caldera system. The existing fault system appears to have a major control on outgassing which in turn leads to a strong alteration of the volcanic products. Moreover the maar-nature of the crater, and its filling by more recent volcanic deposits, resulted in a complex fractured and multilayered cap to the rising gases. As a consequence the hydrothermal alteration differently affects the rocks within the crater, including pyroclastic fallout ash beds, pyroclastic density current deposits, breccias and lavas. The induced changes in both original microstructure and physical and mechanical properties of the rocks control the outgassing behavior. Here, we report results from a measurement survey conducted in July 2015, and aimed to characterize the in-situ physical (temperature, humidity) and mechanical (permeability, strength, stiffness) properties. The survey also included a mapping of the surficial hydrothermal features and their distributions. Chemical analyses and laboratory measurements (porosity, granulometry) of selected samples were additionally performed. Results show that the crater floor area comprises very different kinds of soils, from fine grained, thin laminated deposits around the two bubbling Fangaia mud pools, to crusted hummock formations along the SE and NE border of the crater. Dry and solid alunite-rich deposits are present in the western and southern part. Furthermore we observed evidences of a beginning of crust formation within the central part of the crater. A large range of surface temperatures, from boiling point to ambient temperature, were measured throughout the surveyed area. Outgassing occurs mainly along the crack system, which has also generated the crusted hummocks. Elsewhere the fluid circulation in the subsoil is favored by the presence of coarse and highly porous sulfur-hardened levels, whereas

  8. Joint body and surface wave tomography applied to the Toba caldera complex (Indonesia)

    Science.gov (United States)

    Jaxybulatov, Kairly; Koulakov, Ivan; Shapiro, Nikolai

    2016-04-01

    We developed a new algorithm for a joint body and surface wave tomography. The algorithm is a modification of the existing LOTOS code (Koulakov, 2009) developed for local earthquake tomography. The input data for the new method are travel times of P and S waves and dispersion curves of Rayleigh and Love waves. The main idea is that the two data types have complementary sensitivities. The body-wave data have good resolution at depth, where we have enough crossing rays between sources and receivers, whereas the surface waves have very good near-surface resolution. The surface wave dispersion curves can be retrieved from the correlations of the ambient seismic noise and in this case the sampled path distribution does not depend on the earthquake sources. The contributions of the two data types to the inversion are controlled by the weighting of the respective equations. One of the clearest cases where such approach may be useful are volcanic systems in subduction zones with their complex magmatic feeding systems that have deep roots in the mantle and intermediate magma chambers in the crust. In these areas, the joint inversion of different types of data helps us to build a comprehensive understanding of the entire system. We apply our algorithm to data collected in the region surrounding the Toba caldera complex (north Sumatra, Indonesia) during two temporary seismic experiments (IRIS, PASSCAL, 1995, GFZ, LAKE TOBA, 2008). We invert 6644 P and 5240 S wave arrivals and ~500 group velocity dispersion curves of Rayleigh and Love waves. We present a series of synthetic tests and real data inversions which show that joint inversion approach gives more reliable results than the separate inversion of two data types. Koulakov, I., LOTOS code for local earthquake tomographic inversion. Benchmarks for testing tomographic algorithms, Bull. seism. Soc. Am., 99(1), 194-214, 2009, doi:10.1785/0120080013

  9. The Life and Times of Supervolcanoes: Inferences from Long Valley Caldera

    Science.gov (United States)

    Simon, Justin

    2014-01-01

    Cataclysmic eruptions of silicic magma from "supervolcanoes" are among the most awe-inspiring natural phenomena found in the geologic record, in terms of size, power, and potential hazard. Based on the repose intervals between eruptions of this magnitude, the magmas responsible for them could accumulate gradually in the shallow crust over time scales that may be in excess of a million years (Smith, 1979; Spera and Crisp, 1981; Shaw, 1985). Pre-eruption magma residence time scales can also be inferred from the age difference between eruption (i.e., using 40Ar/39Ar dating to determine the time when hot erupted material cools to below its Ar closure temperature, 200 to 600 degC) and early pre-eruption crystallization (i.e., zircon saturation temperatures; Reid et al., 1997). I will discuss observations from Long Valley a Quaternary volcanic center in California. Long Valley is a voluminous, dominantly silicic caldera system. Based on extensive dating of accessory minerals (e.g., U-Th-Pb dating of zircon and allanite) along with geochemical and isotopic data we find that silicic magmas begin to crystallize 10's to 100's of thousands of years prior to their eruption and that rhyolites record episodes of punctuated and independent evolution rather than the periodic tapping of a long-lived magma. The more punctuated versus more gradual magma accumulation rates required by the absolute and model ages, respectively, imply important differences in the mass and heat fluxes associated with the generation, differentiation, and storage of voluminous rhyolites and emphasize the need to reconcile the magmatic age differences.

  10. Renewed Volcano-Stratigraphc Studies of Calderas with Geothermal Potential in Mexico

    Science.gov (United States)

    Macias, J. L.; Arce, J. L.; García-Tenorio, F.; Layer, P. W.; Saucedo, R.; Castro, R.; Garduño, V. H.; Jimenez, A.; Pérez, H.; Valdez, G.; Meriggi, L.

    2014-12-01

    During the past six years we have carried out volcanologic fieldwork either in active geothermal fields in Mexico (Los Azufres, Tres Vírgenes, and Cerro Prieto) or in potential sites in which some geothermal exploration studied had been done by the National Power Company (CFE). These studies have been very successful in reassessing the location of the geothermal reservoirs within the volcanic successions through detailed mapping of the volcanic units using high resolution topography and satellite imagery to produce 3-D imagery in conjunction with field work to produce preliminary geologic maps. Detailed stratigraphy of volcanic units, assisted with 40Ar/39Ar and radiocarbon geochronology have redefined the evolution of some of these complexes. For example, our studies at Los Azufres geothermal field located in the State of Michoacán indicate that the volcanic complex of the same name sits upon a structural high transected by E-W faults related to the youngest structures of the Trans-Mexican Volcanic Belt. The volcanic complex has been emplaced during the past ~1.5 Ma. During this time, magmas evolved from basaltic to rhyolitic in composition with the emplacement of circa 100 vents. Several landforms have undergone intense hydrothermal alteration and, in some cases, generated debris avalanches. The revised stratigraphy based on drill holes and new dates of cores suggested that the geothermal reservoir is hosted in Miocene rocks bracketed between the Miocene Sierra de Mil Cumbres volcanics (17-22 Ma) and the products of the volcanic field itself. Similar studies will be carried out at four other Pleistocene calderas (Acoculco, La Primavera, Aguajito and Reforma) attempting to refine their volcanic stratigraphy, evolution, and the location of the geothermal system, and those results will help in the design of exploration strategies for geothermal sources.

  11. Mass transfer constraints on the chemical evolution of an active hydrothermal system, Valles caldera, New Mexico

    Science.gov (United States)

    White, A.F.; Chuma, N.J.; Goff, F.

    1992-01-01

    Partial equilibrium conditions occur between fluids and secondary minerals in the Valles hydrothermal system, contained principally in the Tertiary rhyolitic Bandelier Tuff. The mass transfer processes are governed by reactive phase compositions, surface areas, water-rock ratios, reaction rates, and fluid residence times. Experimental dissolution of the vitric phase of the tuff was congruent with respect to Cl in the solid and produced reaction rates which obeyed a general Arrhenius release rate between 250 and 300??C. The 18O differences between reacted and unreacted rock and fluids, and mass balances calculations involving Cl in the glass phase, produced comparable water-rock ratios of unity, confirming the importance of irreversible reaction of the vitric tuff. A fluid residence time of approximately 2 ?? 103 years, determined from fluid reservoir volume and discharge rates, is less than 0.2% of the total age of the hydrothermal system and denotes a geochemically and isotopically open system. Mass transfer calculations generally replicated observed reservoir pH, Pco2, and PO2 conditions, cation concentrations, and the secondary mineral assemblage between 250 and 300??C. The only extraneous component required to maintain observed calcite saturation and high Pco2 pressures was carbon presumably derived from underlying Paleozoic limestones. Phase rule constraints indicate that Cl was the only incompatible aqueous component not controlled by mineral equilibrium. Concentrations of Cl in the reservoir directly reflect mass transport rates as evidenced by correlations between anomalously high Cl concentrations in the fluids and tuff in the Valles caldera relative to other hydrothermal systems in rhyolitic rocks. ?? 1992.

  12. 2.8-Ma ash-flow caldera at Chegem River in the northern Caucasus Mountains (Russia), contemporaneous granites, and associated ore deposits

    Science.gov (United States)

    Lipman, P.W.; Bogatikov, O.A.; Tsvetkov, A.A.; Gazis, C.; Gurbanov, A.G.; Hon, K.; Koronovsky, N.V.; Kovalenko, V.I.; Marchev, P.

    1993-01-01

    Diverse latest Pliocene volcanic and plutonic rocks in the north-central Caucasus Mountains of southern Russia are newly interpreted as components of a large caldera system that erupted a compositionally zoned rhyolite-dacite ash-flow sheet at 2.83 ?? 0.02 Ma (sanidine and biotite 40Ar/39Ar). Despite its location within a cratonic collision zone, the Chegem system is structurally and petrologically similar to typical calderas of continental-margin volcanic arcs. Erosional remnants of the outflow Chegem Tuff sheet extend at least 50 km north from the source caldera in the upper Chegem River. These outflow remnants were previously interpreted by others as erupted from several local vents, but petrologic similarities indicate a common origin and correlation with thick intracaldera Chegem Tuff. The 11 ?? 15 km caldera and associated intrusions are superbly exposed over a vertical range of 2,300 m in deep canyons above treeline (elev. to 3,800 m). Densely welded intracaldera Chegem Tuff, previously described by others as a rhyolite lava plateau, forms a single cooling unit, is > 2 km thick, and contains large slide blocks from the caldera walls. Caldera subsidence was accommodated along several concentric ring fractures. No prevolcanic floor is exposed within the central core of the caldera. The caldera-filling tuff is overlain by andesitic lavas and cut by a 2.84 ?? 0.03-Ma porphyritic granodiorite intrusion that has a cooling age analytically indistinguishable from that of the tuffs. The Eldjurta Granite, a pluton exposed low in the next large canyon (Baksan River) 10 km to the northwest of the caldera, yields variable K-feldspar and biotite ages (2.8 to 1.0 Ma) through a 5-km vertical range in surface and drill-hole samples. These variable dates appear to record a prolonged complex cooling history within upper parts of another caldera-related pluton. Major W-Mo ore deposits at the Tirniauz mine are hosted in skarns and hornfels along the roof of the Eldjurta Granite

  13. Analytical modeling of gravity changes and crustal deformation at volcanoes: The Long Valley caldera, California, case study

    Science.gov (United States)

    Battaglia, Maurizio; Hill, D.P.

    2009-01-01

    Joint measurements of ground deformation and micro-gravity changes are an indispensable component for any volcano monitoring strategy. A number of analytical mathematical models are available in the literature that can be used to fit geodetic data and infer source location, depth and density. Bootstrap statistical methods allow estimations of the range of the inferred parameters. Although analytical models often assume that the crust is elastic, homogenous and isotropic, they can take into account different source geometries, the influence of topography, and gravity background noise. The careful use of analytical models, together with high quality data sets, can produce valuable insights into the nature of the deformation/gravity source. Here we present a review of various modeling methods, and use the historical unrest at Long Valley caldera (California) from 1982 to 1999 to illustrate the practical application of analytical modeling and bootstrap to constrain the source of unrest. A key question is whether the unrest at Long Valley since the late 1970s can be explained without calling upon an intrusion of magma. The answer, apparently, is no. Our modeling indicates that the inflation source is a slightly tilted prolate ellipsoid (dip angle between 91?? and 105??) at a depth of 6.5 to 7.9??km beneath the caldera resurgent dome with an aspect ratio between 0.44 and 0.60, a volume change from 0.161 to 0.173??km3 and a density of 1241 to 2093??kg/m3. The larger uncertainty of the density estimate reflects the higher noise of gravity measurements. These results are consistent with the intrusion of silicic magma with a significant amount of volatiles beneath the caldera resurgent dome. ?? 2008 Elsevier B.V.

  14. Selected data fron continental scientific drilling core holes VC-1 and VC-2a, Valles Caldera, New Mexico

    Energy Technology Data Exchange (ETDEWEB)

    Musgrave, J.A.; Goff, F.; Shevenell, L.; Trujillo, P.E. Jr.; Counce, D.; Luedemann, G.; Garcia, S.; Dennis, B.; Hulen, J.B.; Janik, C.; Tomei, F.A.

    1989-02-01

    This report presents geochemical and isotopic data on rocks and water and wellbore geophysical data from the Continental Scientific Drilling Program core holes VC-1 and VC-2a, Valles Caldera, New Mexico. These core holes were drilled as a portion of a broader program that seeks to answer fundamental questions about magma, water/rock interactions, ore deposits, and volcanology. The data in this report will assist the interpretation of the hydrothermal system in the Jemez Mountains and will stimulate further research in magmatic processes, hydrothermal alteration, ore deposits, hydrology, structural geology, and hydrothermal solution chemistry. 37 refs., 36 figs., 28 tabs.

  15. Persistent inflation at Aira caldera accompanying explosive activity at Sakurajima volcano: Constraining deformation source parameters from Finite Element inversions

    Science.gov (United States)

    Hickey, James; Gottsmann, Jo; Iguchi, Masato; Nakamichi, Haruhisa

    2015-04-01

    Aira caldera is located within Kagoshima Bay at the southern end of Kyushu, Japan. Sakurajima is an active post-caldera andesitic stratovolcano that sits on the caldera's southern rim. Despite frequent Vulcanian-type explosive activity, the area is experiencing continued uplift at a maximum rate of approximately 1.5 cm/yr with a footprint of 40 km, indicating that magma is being supplied faster than it is erupted. This is of particular concern as the amplitude of deformation is approaching the level inferred prior to the 1914 VEI 4 eruption. Using GPS data from 1996 - 2007 we explore causes for the uplift. To solve for the optimum deformation source parameters we use an inverse Finite Element method accounting for three-dimensional material heterogeneity (inferred from seismic tomography) and the surrounding topography of the region. The same inversions are also carried out using Finite Element models that incorporate simplified homogeneous or one-dimensional subsurface material properties, with and without topography. Results from the comparison of the six different models show statistically significant differences in the inferred deformation sources. This indicates that both subsurface heterogeneity and surface topography are essential in geodetic modelling to extract the most realistic deformation source parameters. The current best-fit source sits within a seismic low-velocity zone in the north-east of the caldera at a depth of approximately 14 km with a volume increase of 1.2 x 108 m3. The source location underlies a region of active underwater fumaroles within the Wakamiko crater and differs significantly from previous analytical modelling results. Seismic data further highlights areas of high seismic attenuation as well as large aseismic zones, both of which could allude to inelastic behaviour and a significant heat source at depth. To integrate these observations, subsequent forward Finite Element models will quantify the importance of rheology and

  16. Modelo para estudios de estabilidad de calderas de recuperación de calor (HRSG) y turbina de vapor

    OpenAIRE

    Corasaniti, Víctor Fabián; Agüero, Jorge Luis; Bianchi Lastra, Raúl E.

    2013-01-01

    En este trabajo se presenta la determinación y validación de los parámetros de un modelo digital para estudios de estabilidad que representa dos Calderas de Recuperación de Calor (HRSG, del inglés Heat Recovery Steam Generator), conjuntamente con la Turbina de Vapor a la cual suministran vapor. Los 2 HRSG producen vapor a partir de los gases de escape de 2 turbinas de gas. El modelo de simulación se implementa en el programa PSS/E (Power System Simulator), programa usado para estudios de est...

  17. Crystallization and eruption ages of Breccia Museo (Campi Flegrei caldera, Italy) plutonic clasts and their relation to the Campanian ignimbrite

    Science.gov (United States)

    Gebauer, Samantha K.; Schmitt, Axel K.; Pappalardo, Lucia; Stockli, Daniel F.; Lovera, Oscar M.

    2014-01-01

    The Campi Flegrei volcanic district (Naples region, Italy) is a 12-km-wide, restless caldera system that has erupted at least six voluminous ignimbrites during the late Pleistocene, including the >300 km3 Campanian ignimbrite (CI) which originated from the largest known volcanic event of the Mediterranean region. The Breccia Museo (BM), a petrologically heterogeneous and stratigraphically complex volcanic deposit extending over 200 km2 in close proximity to Campi Flegrei, has long remained contentious regarding its age and stratigraphic relation to the CI. Here, we present crystallization and eruption ages for BM plutonic ejecta clasts that were determined via uranium decay series and (U-Th)/He dating of zircon, respectively. Despite mineralogical and textural heterogeneity of these syenitic clasts, their U-Th zircon rim crystallization ages are indistinguishable with an average age of 49.7 ± 2.5 ka (2σ errors; mean square of weighted deviates MSWD = 1.2; n = 34). A subset of these crystals was used to obtain disequilibrium-corrected (U-Th)/He zircon ages which average 41.7 ± 1.8 ka (probability of fit P = 0.54; n = 15). This age closely overlaps with published CI 40Ar/39Ar eruption ages (40.6 ± 0.1 ka) after recalibration to recently revised flux monitor ages. Concordant eruption ages for BM and CI agree with previous chemostratigraphic and paleomagnetic correlations, suggesting their origin from the same eruption. However, they are at variance with recalibrated 40Ar/39Ar ages which have BM postdate CI by 3 ± 1 ka. BM syenites show similar geochemical and Sr-Nd isotopical features of pre-caldera rocks erupted between 58 and 46 ka, but are distinctive from subsequent caldera-forming magmas. Energy-constrained assimilation and fractional crystallization modeling of Nd-Sr isotopic data suggests that pre-caldera magmas formed a carapace of BM-type intrusions in a mid-crust magma chamber (≥8 km depth) shielding the younger CI magma from contamination by

  18. A 2-D FEM thermal model to simulate water flow in a porous media: Campi Flegrei caldera case study

    Directory of Open Access Journals (Sweden)

    V. Romano

    2012-05-01

    Full Text Available Volcanic and geothermal aspects both exist in many geologically young areas. In these areas the heat transfer process is of fundamental importance, so that the thermal and fluid-dynamic processes characterizing a viscous fluid in a porous medium are very important to understand the complex dynamics of the these areas. The Campi Flegrei caldera, located west of the city of Naples, within the central-southern sector of the large graben of Campanian plain, is a region where both volcanic and geothermal phenomena are present. The upper part of the geothermal system can be considered roughly as a succession of volcanic porous material (tuff saturated by a mixture formed mainly by water and carbon dioxide. We have implemented a finite elements approach in transient conditions to simulate water flow in a 2-D porous medium to model the changes of temperature in the geothermal system due to magmatic fluid inflow, accounting for a transient phase, not considered in the analytical solutions and fluid compressibility. The thermal model is described by means of conductive/convective equations, in which we propose a thermal source represented by a parabolic shape function to better simulate an increase of temperature in the central part (magma chamber of a box, simulating the Campi Flegrei caldera and using more recent evaluations, from literature, for the medium's parameters (specific heat capacity, density, thermal conductivity, permeability. A best-fit velocity for the permeant is evaluated by comparing the simulated temperatures with those measured in wells drilled by Agip (Italian Oil Agency in the 1980s in the framework of geothermal exploration. A few tens of days are enough to reach the thermal steady state, showing the quick response of the system to heat injection. The increase in the pressure due to the heat transport is then used to compute ground deformation, in particular the vertical displacements characteristics of the Campi Flegrei caldera

  19. Geodetic constraints to the source mechanism of the 2011-2013 unrest at Campi Flegrei (Italy) caldera

    Science.gov (United States)

    Trasatti, Elisa; Polcari, Marco; Bonafede, Maurizio; Stramondo, Salvatore

    2016-04-01

    Campi Flegrei (Italy) is a nested caldera and together with Vesuvius is one of the Italian GEO Geohazard Supersites (GSNL). The area is characterized by one of the highest volcanic hazard of the world, due to the very high density of inhabitants (1800/km²), the persistent activity of the system and the explosive character of volcanism. A major unrest episode took place in 1982-84, when the town of Pozzuoli, located at the caldera center, was uplifted by 1.80 m. Minor uplifts of few centimeters, seismic swarms and degassing episodes took place in 1989, 2000 and 2004-06. Since 2005 Campi Flegrei is uplifting, reaching a ground velocity of 9 cm/yr in 2012, showing that the caldera is in a critical state on the verge of instability. In this work, we present results from SAR Interferometry and geodetic data modelling at Campi Flegrei in the framework of the EU's FP7 MED-SUV Project. We exploit two COSMO-SkyMed data sets to map the deformation field during 2011-2013. The spatial distributions of the cumulative displacement from COSMO-SkyMed ascending/descending orbits show similar behaviors, confirming the bell-shaped pattern of the deformation at least within the inner rim of the caldera. The resulting data, together with GPS data from the Neapolitan Volcanoes Continuous GPS network (NeVoCGPS) is fitted through a geophysical inversion process using finite element forward models to account for the 3D heterogeneous medium. The best fit model is a north dipping mixed-mode dislocation source lying at ~5 km depth. The driving mechanism is ascribable to magma input into the source of the large 1982-1984 unrest (since similar source characteristics were inferred) that generates initial inflation followed by additional shear slip accompanying the extension of crack tips. The history and the current state of the system indicate that Campi Flegrei is able to erupt again. Constraining the defomation source may have important implications in terms of civil protection and the

  20. Trazado de rutas migratorias utilizando alelos HLA clase II de indígenas Wayuu venezolanos

    Directory of Open Access Journals (Sweden)

    Miriam Echeverria

    2012-01-01

    Full Text Available Se realizó un estudio comparativo utilizando las frecuencias alélicas HLA-DRB1* de la poblaciónWayuú venezolana, con datos reportados de las poblaciones Caucásicas, Negroides Americanas y Amerindias siguientes: Barí, Warao y Yucpa (venezolanas, Wayúu colombiana, Australianos, Atahabaskans, Indios americanos, Seri, Maya, Taraumara, Kogi, Cayapa, indígenas brasileros, Mataco-Wichi, Toba Pilaga y Eastern Toba, con el fin de evaluar su posible contribución al origen de esta población indígena. Los alelos DRB1*03:01, 04:01, 04:03, 04:04, 04:07, 08:02, 13:01, 14:02 y 16:02 de los Wayuú venezolanos son los únicos comunes a todas las poblaciones amerindias desde Norte América hasta la Patagonia; igualmente analizamos otras contribuciones.

  1. Aproximaciones al valor de la integral definida utilizando una calculadora graficadora

    OpenAIRE

    Ansola, Esther; Rodríguez, Eugenio Carlos; Hernández, Nelson; Gómez, Pablo Ignacio; Alfonso, Débora Oliva; Sánchez, Danelia

    2008-01-01

    Este trabajo muestra una experiencia llevada a cabo con un grupo de estudiantes de primer año de ingeniería a través de un curso facultativo en el que se retomó el cálculo de integrales definidas, utilizando la tecnología, con el propósito de:• Consolidar el concepto de integral definida a través de su definición y de su interpretación geométrica. • Mostrar otras formas de calcular una integral definida mediante aproximaciones numéricas y su interpretación geométrica. El recurso tecnológic...

  2. Una experiencia en formación inicial del profesorado utilizando la red social ELGG

    Directory of Open Access Journals (Sweden)

    Francisco Javier Álvarez Lires

    2015-01-01

    Full Text Available Una experiencia de investigación-innovación educativa en forma- ción inicial del profesorado de Grados universitarios en Educación In- fantil, Primaria y Máster de Educación Secundaria y Formación Profe- sional, sobre las posibilidades que ofrece la red social de comunidad de aprendizaje ELGG, utilizando una metodología docente focalizada en el alumnado, hacia un aprendizaje colaborativo y cooperativo. Los resulta - dos muestran amplia participación, percepción de beneficios de aprendi - zaje, por parte del alumnado, coordinación entre docentes de áreas dife - rentes y cumplimiento de objetivos en cuanto a promoción de espacios y formas de aprendizaje que rompen con modelos tradicionales aprove - chando las posibilidades educativas de las TIC.

  3. Detecção de estro em jaguatirica (Leopardus pardalis) utilizando citologia vaginal

    OpenAIRE

    R.C.R. Paz; C.H Adania; V.H. Barnabe; R.C. Barnabe

    2010-01-01

    Utilizou-se a citologia vaginal por meio de diferentes métodos de coloração para detecção de cio em jaguatirica, Leopardus pardalis, pela estimulação hormonal exógena e pela avaliação das estruturas ovarianas por videolaparoscopia. Cinco fêmeas foram tratadas com eCG/hCG e FSH/LH a cada quatro meses pelo período de dois anos. Videolaparoscopia foi realizada após cada tratamento utilizando-se cetamina-xilazina e isoflurano. Esfregaços vaginais foram obtidos 15 dias antes e após a videolaparosc...

  4. Presiones Antropogénicas Relacionadas con el Comportamiento, Hidrodinámica, Flujos e Intercambios de Compuestos Biógeno en el Estuario del Río las Casas. Isla de la Juventud, Cuba.

    Directory of Open Access Journals (Sweden)

    Eusebio Perigó Arnaud

    2005-01-01

    Full Text Available Se presentan los resultados de estudios realizados en el estuario del río Las Casas con el objetivo de evaluar el estado de la calidad del ecosistema, sometido a las presiones antropogénicas originadas por las descargas contaminantes en sus últimos 5 Km. de su desembocadura de residuales crudos industriales, agropecuarios y domésticos cuyos impactos se reflejan en una notable alteración del balance del oxígeno disuelto y altas concentraciones de materia orgánica y nutrientes en agua y sedimentos, lo cual afecta la estructura y el funcionamiento del estuario y es exportador de compuestos de C, N y P al Golfo de Batabanó de acuerdo a resultados obtenidos a partir de muestreos diurnos en la frontera estuario - golfo. Se aplicó un modelo hidronumérico de simulación acoplado de OD-DBO para conocer los porcentajes de tratamiento a que deben ser sometidos los residuales para que el cuerpo de agua alcance los valores de las normas de calidad para uso pesquero y así garantizar un manejo y uso sustentable de los recursos pesqueros, actividades portuarias y otras actividades como las recreativas y la acuicultura. La construcción de una planta comunitaria con tratamiento biológico y el uso de las aguas tratadas como fertirriegos serían las mejores alternativas para mitigar el impacto ambiental dado la cercanía de los focos y la naturaleza común de los residuos. Para la estimación de los intercambios de compuestos biógenos y el metabolismo del ecosistema estuarino se aplicó un modelo trófico de caja donde reportó que el estuario es un sumidero de estos compuestos

  5. “...Argentinos , bolivianos, todos somos lo mismo...” la comunidad cultural feriante y el problema de la frontera argentino-boliviana en las ferias de intercambios indígenas

    Directory of Open Access Journals (Sweden)

    Andrea Paola Campisi

    2001-01-01

    Full Text Available Este trabajo, un aporte más a la discusión sobre las fronteras nacionales, pretende examinar cómo perciben los agentes campesinos andinos, que llegan a las ferias indígenas a intercambiar sus productos y sus formas culturales, la línea que divide La Quiaca de Villazón, Argentina de Bolivia. El punto de partida es la idea de que la percepción de los espacios en los agentes feriantes varía de acuerdo a las acciones que realizan y a los agentes con los que interactúan. Por tal razón, si bien la frontera puede ser vista como la materialización del estado, no todos los agentes sociales, necesariamente, deben percibirla de esta manera. El límite territorial es percibido por los agentes feriantes como un obstáculo para la consecución de sus fines prácticos y no como una variable de argentinidad o bolivianidad. A partir de la descripción de una feria de intercambio y el trueque intergrupal veremos cómo se construye en la subjetividad de los agentes la imagen de frontera y a partir de quéconcreta, el trueque intergrupal, la delimitación nacional pierde relevancia en la interacción que llevan a cabo los grupos campesinos que están presentes en estos encuentros; para concluir con la idea de que el espacio relevante es el que se define en la comunidad cultural feriante

  6. A probability tomography approach to the analysis of potential field data in the Campi Flegrei caldera (Italy

    Directory of Open Access Journals (Sweden)

    D. Patella

    2001-06-01

    Full Text Available The results of the application of the 3D probability tomography imaging approach to the study of the Campi Flegrei (CF caldera are presented and discussed. The tomography approach has been applied to gravity, magnetic and ground deformation data already available in literature. The analysis of the 3D tomographic images is preceded by a brief qualitative interpretation of the original survey maps and by an outline of the probability tomography approach for each geophysical prospecting method. The results derived from the 3D tomographic images are the high occurrence probabilities of both gravity and ground deformation source centres in the CF caldera under the town of Pozzuoli. A Bouguer negative anomaly source centre is highlighted in the depth range 1.6-2 km b.s.l., whereas a positive ground deformation point source, responsible for the bradyseismic crisis of 1982-1984, is estimated at a mean depth of 3-4 km b.s.l. These inferences, combined with the results of a previous analysis of magnetotelluric, dipolar geoelectrical and self-potential data, corroborate the hypothesis that the bradyseismic events in the CF area may be explained by hot fluids vertical advection and subsequent lateral diffusion within a trapped reservoir overlying a magma chamber.

  7. Origins of felsic magmas in Japanese subduction zone: Geochemical characterizations of tephra from caldera-forming eruptions <5 Ma

    Science.gov (United States)

    Kimura, Jun-Ichi; Nagahashi, Yoshitaka; Satoguchi, Yasufumi; Chang, Qing

    2015-07-01

    Dacitic to rhyolitic glass shards from 80 widespread tephras erupted during the past 5 Mys from calderas in Kyushu, and SW, central, and NE Japan were analyzed. Laser ablation inductively coupled plasma mass spectrometry was used to determine 10 major and 33 trace elements and 207Pb/206Pb-208Pb/206Pb isotope ratios. The tephras were classified into three major geochemical types and their source rocks were identified as plutonic, sedimentary, and intermediate amphibolite rocks in the upper crust. A few tephras from SW Japan were identified as adakite and alkali rhyolite and were regarded to have originated from slab melt and mantle melt, respectively. The Pb isotope ratios of the tephras are comparable to those of the intermediate lavas in the source areas but are different from the basalts in these areas. The crustal assimilants for the intermediate lavas were largely from crustal melts and are represented by the rhyolitic tephras. A large heat source is required for forming large volumes of felsic crustal melts and is usually supplied by the mantle via basalt. Hydrous arc basalt formed by cold slab subduction is voluminous, and its heat transfer with high water content may have melted crustal rocks leading to effective felsic magma production. Coincidence of basalt and felsic magma activities shown by this study suggests caldera-forming eruptions are ultimately the effect of a mantle-driven cause.

  8. Environmental Magnetism of mid-Pleistocene Lacustrine Sediments of the Valles Caldera, New Mexico

    Science.gov (United States)

    Hurley, L. L.; Geissman, J. W.; Fawcett, P.; Tim, W.; Goff, F.

    2007-12-01

    Rock magnetic measurements are applied to almost 80 m of lacustrine sediment (VC-3) to augment independent means of interpreting the environmental conditions of a mid-Pleistocene lake in the Valle Grande of the Valles Caldera, northern New Mexico. An age model for the core is pinned to an Ar/Ar age determination of 552 ± 3 ka for a sanidine bearing ash layer at 78 m depth and major transitions in the organic carbon record at 53 m, 40 m, 27 m, and 17 m; these data suggest that deposition of VC-3 spans MIS 14 to MIS 10, including glacial terminations VI (531 ka) and V (426 ka). AF demagnetization resolves positive inclination magnetizations from most of the core, consistent with Brunhes normal polarity. Three thin (magnetizations may indicate poorly-recorded geomagnetic polarity events at ~406 ka (11α), ~536 ka (14α) and the Big Lost excursion (~580 ± 8 ka). Data from an array of rock magnetic investigations indicate magnetite, titanomagnetite, and pyrhotite characterize VC-3 sediments. Susceptibility and frequency dependent susceptibility experiments at low temperature reveal an abundance of paramagnetic and super-paramagnetic material. Scanning electron microscopy of magnetic separates show an array of Fe-oxide and Fe-sulfide grains, including titanomagnetites with trellis ilmenite intergrowths. NRM intensities of sediment deposited during glacial periods typically range from 0.04 mA/m to values as high as 1.6 mA/m; interglacial sediment NRM intensities range from 0.05 mA/m to 0.2 mA/m. NRM values increase to 3.3 mA/m, between 48 m to 43 m, where the sediment exhibits shallow mud crack, bioturbation, and oxidation. Overall, trends in susceptibility, ARM, and SIRM are similar to those in NRM intensity. Bivariate plot of susceptibility/ARM shows little variation in concentration of low coercivity minerals (i.e. magnetite) in VC-3 sediments. Also, the concentration of high coercivity minerals (i.e. hematite) indicated by the IRM/susceptibility curve show similar

  9. The Askja rockslide and the associated tsunami in the caldera lake

    Science.gov (United States)

    Vogfjörd, Kristin; Kristinn Helgason, Jon; Jonsdottir, Kristin; Brynjolfsson, Sveinn; Grimsdottir, Harpa; Johannesson, Tomas; Hensch, Martin; Ripepe, Maurizio

    2015-04-01

    A large rockslide was released in Askja, central Iceland, on the evening of 21 July 2014 and descended into the caldera lake. It is one of the largest known rockslides since the settlement of Iceland. The release area of the slide is approximately 900 m wide and 350 m above the lake. The front of the landslide travelled at least 2000 m along the lake bottom where it reached the depth of 150 m. The total run-out is approximatly 3100 m and the fall height 500 m. The estimated volume of the slide is estimated as 15-50 million m3. The rockslide appeared as shallow tremor on IMO seismographs near Askja and the data show that the slide was released at 23:24. The slide created seismic waves that travelled over most of Iceland in roughly one minute. In addition, it triggered atmospheric pressure waves that were detected on an infrasound array some 210 km southwest of the event. The infrasound waves travelled this distance in 11 minutes and were reflected in the stratosphere. Photographs from the rockslide area indicate that considerable movement had started a few years before the slide was released. Slow movement in the bedrock seems to have accelerated in the summer of 2014. There was deep snow in the mountains and fairly warm weather before the slide occurred. Percolating water from the melting snow might, thus, have increased the rate of movement. Seismic data indicate that a creeping movement started around 40 minutes before the slide, but at 23:24 the failure point was reached and the rockslide was released. The slide triggered a tsunami in the lake that washed up on the lakeshores all around the lake, reaching up to 20-30 m elevation above the water level and even higher in some places. The wave travelled farthest around 400 m (horizontally) into the flatland SE of the crater Víti. It was fortunate that the rockslide occurred late at night when nobody was close to the water, otherwise it would have been extremely hazardous. A few hours earlier, dozens of people were

  10. Lithologic Control on Secondary Clay Mineral Formation in the Valles Caldera, New Mexico

    Science.gov (United States)

    Caylor, E.; Rasmussen, C.; Dhakal, P.

    2015-12-01

    Understanding the transformation of rock to soil is central to landscape evolution and ecosystem function. The objective of this study was to examine controls on secondary mineral formation in a forested catchment in the Catalina-Jemez CZO. We hypothesized landscape position controls the type of secondary minerals formed in that well-drained hillslopes favor Si-poor secondary phases such as kaolinite, whereas poorly drained portions of the landscape that collect solutes from surrounding areas favor formation of Si-rich secondary phases such as smectite. The study focused on a catchment in Valles Caldera in northern New Mexico where soils are derived from a mix of rhyolitic volcanic material, vegetation includes a mixed conifer forest, and climate is characterized by a mean annual precipitation of ~800 mm yr-1 and mean annual temperature of 4.5°C. Soils were collected at the soil-saprolite boundary from three landscape positions, classified as well drained hillslope, poorly drained convergent area, and poorly drained hill slope. Clay fractions were isolated and analyzed using a combination of quantitative and qualitative x-ray diffraction (XRD) analyses and thermal analysis. Quantitative XRD of random powder mounts indicated the presence of both primary phases such as quartz, and alkali and plagioclase feldspars, and secondary phases that include illite, Fe-oxyhydroxides including both goethite and hematite, kaolinite, and smectite. The clay fractions were dominated by smectite ranging from 36-42%, illite ranging from 21-35%, and kaolinite ranging from 1-8%. Qualitative XRD of oriented mounts confirmed the presence of smectite in all samples, with varying degrees of interlayering and interstratification. In contrast to our hypothesis, results indicated that secondary mineral assemblage was not strongly controlled by landscape position, but rather varied with underlying variation in lithology. The catchment is underlain by a combination of porphorytic rhyolite and

  11. Estimating Catchment-Scale Snowpack Variability in Complex Forested Terrain, Valles Caldera National Preserve, NM

    Science.gov (United States)

    Harpold, A. A.; Brooks, P. D.; Biederman, J. A.; Swetnam, T.

    2011-12-01

    Difficulty estimating snowpack variability across complex forested terrain currently hinders the prediction of water resources in the semi-arid Southwestern U.S. Catchment-scale estimates of snowpack variability are necessary for addressing ecological, hydrological, and water resources issues, but are often interpolated from a small number of point-scale observations. In this study, we used LiDAR-derived distributed datasets to investigate how elevation, aspect, topography, and vegetation interact to control catchment-scale snowpack variability. The study area is the Redondo massif in the Valles Caldera National Preserve, NM, a resurgent dome that varies from 2500 to 3430 m and drains from all aspects. Mean LiDAR-derived snow depths from four catchments (2.2 to 3.4 km^2) draining different aspects of the Redondo massif varied by 30%, despite similar mean elevations and mixed conifer forest cover. To better quantify this variability in snow depths we performed a multiple linear regression (MLR) at a 7.3 by 7.3 km study area (5 x 106 snow depth measurements) comprising the four catchments. The MLR showed that elevation explained 45% of the variability in snow depths across the study area, aspect explained 18% (dominated by N-S aspect), and vegetation 2% (canopy density and height). This linear relationship was not transferable to the catchment-scale however, where additional MLR analyses showed the influence of aspect and elevation differed between the catchments. The strong influence of North-South aspect in most catchments indicated that the solar radiation is an important control on snow depth variability. To explore the role of solar radiation, a model was used to generate winter solar forcing index (SFI) values based on the local and remote topography. The SFI was able to explain a large amount of snow depth variability in areas with similar elevation and aspect. Finally, the SFI was modified to include the effects of shading from vegetation (in and out of

  12. Near real-time monitoring of surface deformation at Long Valley Caldera, California (Invited)

    Science.gov (United States)

    Ji, K.; Llenos, A. L.; Herring, T.

    2013-12-01

    Continuous monitoring of volcanic activity enables us to detect changes from usual activity, issue alerts of impending eruptions and thereby reduce volcanic risk. We have developed a near real-time monitoring tool for surface deformation: the Targeted Projection Operator (TPO). TPO is simple, fast, and easily applied whenever new data are available. With Global Positioning System (GPS) data, we have used TPO for continuous monitoring of surface deformation in the Long Valley Caldera (LVC) region in eastern California. TPO projects GPS position time series onto a target spatial pattern and obtains the amplitude of the projection at each epoch. For this, we assume that a deformation event (i.e., an inflationary or deflationary event) has the same spatial pattern as past events but with possibly different amplitude. This assumption is reasonable for the recent quiet phase in LVC because the 2007-2009 inflation is similar to the 2009-2010 deflation with respect to the deformation pattern. We selected horizontal pattern of the 2009-2010 event along which the GPS data are projected to recover the time-varying amplitudes. Large changes in amplitude imply changes in strength of the event. An anomalous change can be detected by comparing with amplitudes during relatively quiet time periods. Growing misfits between the TPO spatial pattern and the spatial variations of the GPS pattern, indicate changes in the deformation mechanism which can then be explored to assess whether potentially new mechanisms are developing. So far this has not been the case for LVC; the current spatial patterns of deformation match the shape deduced for the 2007-2009 inflation event. TPO shows that LVC has experienced inflation since late 2011 although the rate briefly slowed down in May and October 2012 and has started to slow again since June 2013. The rate of this event is about four times faster than the 2007-2009 inflation event and is consistent with a Mogi source located beneath the resurgent

  13. Geochemical exploration of a promissory Enhanced Geothermal System (EGS): the Acoculco caldera, Mexico.

    Science.gov (United States)

    Peiffer, Loic; Romero, Ruben Bernard; Pérez-Zarate, Daniel; Guevara, Mirna; Santoyo Gutiérrez, Edgar

    2014-05-01

    The Acoculco caldera (Puebla, Mexico) has been identified by the Mexican Federal Electricity Company (in Spanish 'Comisión Federal de Electricidad', CFE) as a potential Enhanced Geothermal System (EGS) candidate. Two exploration wells were drilled and promising temperatures of ~300° C have been measured at a depth of 2000 m with a geothermal gradient of 11oC/100m, which is three times higher than the baseline gradient measured within the Trans-Mexican Volcanic Belt. As usually observed in Hot Dry Rock systems, thermal manifestations in surface are scarce and consist in low-temperature bubbling springs and soil degassing. The goals of this study were to identify the origin of these fluids, to estimate the soil degassing rate and to explore new areas for a future detailed exploration and drilling activities. Water and gas samples were collected for chemical and isotopic analysis (δ18O, δD, 3He/4He, 13C, 15N) and a multi-gas (CO2, CH4, H2S) soil survey was carried out using the accumulation chamber method. Springs' compositions indicate a meteoric origin and the dissolution of CO2 and H2S-rich gases, while gas compositions reveal a MORB-type origin mixed with some arc-type contribution. Gas geothermometry results are similar to temperatures measured during well drilling (260° C-300° C). Amongst all measured CO2 fluxes, only 5% (mean: 5543 g m-2 day-1) show typical geothermal values, while the remaining fluxes are low and correspond to biogenic degassing (mean: 18 g m-2 day-1). The low degassing rate of the geothermal system is a consequence of the intense hydrothermal alteration observed in the upper 800 m of the system which acts as an impermeable caprock. Highest measured CO2 fluxes (above > 600 g m-2 day-1) have corresponding CH4/CO2 flux ratios similar to mass ratios of sampled gases, which suggest an advective fluid transport. To represent field conditions, a numerical model was also applied to simulate the migration of CO2 towards the surface through a

  14. Tephra dispersal during the Campanian Ignimbrite (Italy) eruption: implications for ultra-distal ash transport during the large caldera-forming eruption

    Science.gov (United States)

    Smith, Victoria C.; Isaia, Roberto; Engwell, Sam L.; Albert, Paul. G.

    2016-06-01

    The Campanian Ignimbrite eruption dispersed ash over much of the central eastern Mediterranean Sea and eastern Europe. The eruption started with a Plinian phase that was followed by a series of pyroclastic density currents (PDCs) associated with the collapse of the Plinian column and the caldera. The glass compositions of the deposits span a wide geochemical range, but the Plinian fallout and PDCs associated with column collapse, the Lower Pumice Flow, only erupted the most evolved compositions. The later PDCs, the Breccia Museo and Upper Pumice Flow, erupted during and after caldera collapse, tap a less evolved component, and intermediate compositions that represent mixing between the end-members. The range of glass compositions in the Campanian Ignimbrite deposits from sites across the central and eastern Mediterranean Sea allow us to trace the dispersal of the different phases of this caldera-forming eruption. We map the fallout from the Plinian column and the plumes of fine material associated with the PDCs (co-PDCs) across the entire dispersal area. This cannot be done using the usual grain-size methods as deposits in these distal regions do not retain characteristics that allow attribution to either the Plinian or co-PDC phases. The glass compositions of the tephra at ultra-distal sites (>1500 km from the vent) match those of the uppermost PDC units, suggesting that most of the ultra-distal dispersal was associated with the late co-PDC plume that was generated during caldera collapse.

  15. Ambient seismic noise tomography reveals a hidden caldera and its relation to the Tarutung pull-apart basin at the Sumatran Fault Zone, Indonesia

    Science.gov (United States)

    Ryberg, Trond; Muksin, Umar; Bauer, Klaus

    2016-07-01

    We analyzed the noise recordings of a short-period seismic network to derive a shallow crustal S-wave velocity model at the Sumatra Fault in Northern Sumatra, Indonesia. By correlating the noise of 40 seismic stations' recording for 9 months, we could recover Rayleigh waves from vertical component recordings with sufficient signal-to-noise ratio. Group velocities of the Rayleigh waves could be determined in the period range from 0.71 to 4.4 s. These group velocities were used to invert for 2D group velocity maps at specific periods. Finally, the derived group velocity maps were inverted for a 3D S-wave velocity model. This model shows a region of a strong velocity decrease off the Great Sumatran Fault Zone, at the northeastern margin of the young Tarutung pull-apart basin. This observed low velocity block coincides with a caldera-like morphological feature which is interpreted as the surface expression of a hidden volcanic caldera. Considering the surface manifestations of geothermal activity around this anomaly, we conclude that the caldera is still acting as a heat source. On the other hand, the weak morphological expression at the surface indicates a certain age of the caldera which might be older than the Tarutung pull-apart basin. The findings provide important constraints on general concepts for the formation of pull-apart basins along the Sumatran fault and their relation to volcanism.

  16. A tale of ambiguities and interpretation pitfalls: seismology based source models for the Bárðarbunga caldera collapse earthquakes, Iceland

    Science.gov (United States)

    Heimann, Sebastian; Cesca, Simone; Hensch, Martin; Dahm, Torsten; Hjörleifsdóttir, Vala

    2016-04-01

    The 2014-2015 collapse of the Bárðarbunga caldera was accompanied by a notable seismic sequence of more than 80 events with Mw >= 4.5. We analyse these earthquakes using broadband recordings from the Icelandic regional seismic network using standard and probabilistic centroid moment tensor inversion. Our results reveal that the centroids of the events cluster beneath the northern and southern caldera rims and are characterized by the superposition of a near-vertical negative compensated linear vector dipole (CLVD) and shear faulting of different orientations. It is well known that moment tensor decompositions are non-unique. We demonstrate that in this particular case, applying the standard moment tensor decomposition scheme would lead to wrong conclusions, incompatible with independent observations like the fault orientations at the caldera rims. We propose an alternative decomposition scheme which is well compatible with the observations. Furthermore, we propose a simple mechanical model for asymmetric, drainage-driven caldera collapses, capable of explaining the seismological observations at regional distances: an initial failure along a steep fault is followed by a deformation response of a deeper magmatic source. The shear faulting contribution occurs either as thrust faulting along an outward dipping fault (northern rim) or as normal faulting along an inward dipping fault (southern rim). As a side note, we discuss the parameter trade-offs in our full and deviatoric centroid moment tensor inversion problems and show how to rigorously quantify uncertainties on the results.

  17. The earliest low and high δ18O caldera-forming eruptions of the Yellowstone plume: Implications for the 30–40 Ma Oregon calderas and speculations on plume-triggered delaminations

    Directory of Open Access Journals (Sweden)

    Angela Nicole Seligman

    2014-11-01

    Full Text Available We present new isotopic and trace element data for four eruptive centers in Oregon: Wildcat Mountain (40 Ma, Crooked River (32–28 Ma, Tower Mountain (32 Ma, and Mohawk River (32 Ma. The first three calderas are located too far east to be sourced through renewed subduction of the Farallon slab following accretion of the Yellowstone-produced Siletzia terrane at ~50 Ma. Basalts of the three eastern eruptive centers yield high Nb/Yb and Th/Yb ratios, indicating an enriched sublithospheric mantle source, while Mohawk River yields trace element and isotopic (δ18O and εHf values that correlate with its location above a subduction zone. The voluminous rhyolitic tuffs and lavas of Crooked River (41 x 27 km have δ18Ozircon values that include seven low δ18Ozircon units (1.8–4.5 ‰, one high δ18Ozircon unit (7.4–8.8 ‰, and two units with heterogeneous zircons (2.0–9.0 ‰, similar to younger Yellowstone-Snake River Plain rhyolites. In order to produce these low δ18O values, a large heat source, widespread hydrothermal circulation, and repeated remelting are all required. In contrast, Wildcat Mountain and Tower Mountain rocks yield high δ18Ozircon values (6.4–7.9 ‰ and normal to low εHfi values (5.2–12.6, indicating crustal melting of high-δ18O supracrustal rocks. We propose that these calderas were produced by the first appearance of the Yellowstone plume east of the Cascadia subduction zone, which is supported by plate reconstructions that put the Yellowstone plume under Crooked River at 32–28 Ma. Given the eastern location of these calderas along the suture of the accreted Siletzia terrane and North America, we suggest that the Yellowstone hotspot is directly responsible for magmatism at Crooked River, and for plume-assisted delamination of portions of the edge of the Blue Mountains that produced the Tower Mountain magmas, while the older Wildcat Mountain magmas are related to suture zone instabilities that were created

  18. The earliest low and high δ18O caldera-forming eruptions of the Yellowstone plume: Implications for the 30-40 Ma Oregon calderas and speculations on plume-triggered delaminations

    Science.gov (United States)

    Seligman, Angela; Bindeman, Ilya; McClaughry, Jason; Stern, Richard; Fisher, Chris

    2014-11-01

    We present new isotopic and trace element data for four eruptive centers in Oregon: Wildcat Mountain (40 Ma), Crooked River (32-28 Ma), Tower Mountain (32 Ma), and Mohawk River (32 Ma). The first three calderas are located too far east to be sourced through renewed subduction of the Farallon slab following accretion of the Yellowstone-produced Siletzia terrane at ~50 Ma. Basalts of the three eastern eruptive centers yield high Nb/Yb and Th/Yb ratios, indicating an enriched sublithospheric mantle source, while Mohawk River yields trace element and isotopic (δ18O and ɛHf) values that correlate with its location above a subduction zone. The voluminous rhyolitic tuffs and lavas of Crooked River (41 x 27 km) have δ18Ozircon values that include seven low δ18Ozircon units (1.8-4.5 ‰), one high δ18Ozircon unit (7.4-8.8 ‰), and two units with heterogeneous zircons (2.0-9.0 ‰), similar to younger Yellowstone-Snake River Plain rhyolites. In order to produce these low δ18O values, a large heat source, widespread hydrothermal circulation, and repeated remelting are all required. In contrast, Wildcat Mountain and Tower Mountain rocks yield high δ18Ozircon values (6.4-7.9 ‰) and normal to low ɛHfi values (5.2-12.6), indicating crustal melting of high-δ18O supracrustal rocks. We propose that these calderas were produced by the first appearance of the Yellowstone plume east of the Cascadia subduction zone, which is supported by plate reconstructions that put the Yellowstone plume under Crooked River at 32-28 Ma. Given the eastern location of these calderas along the suture of the accreted Siletzia terrane and North America, we suggest that the Yellowstone hotspot is directly responsible for magmatism at Crooked River, and for plume-assisted delamination of portions of the edge of the Blue Mountains that produced the Tower Mountain magmas, while the older Wildcat Mountain magmas are related to suture zone instabilities that were created following accretion of the

  19. Dynamics of the 2007 Eruptions of Piton de la Fournaise and the Related Caldera Collapse from a Single Very Broad-band Seismic Station

    Science.gov (United States)

    Fontaine, Fabrice R.; Roult, Geneviève; Michon, Laurent; Barruol, Guilhem; Ferrazzini, Valérie; Di Muro, Andrea; Reymond, Dominique; Peltier, Aline; Staudacher, Thomas

    2014-05-01

    Seismic records from the RER very broad-band seismic station (La Réunion Island) belonging to the GEOSCOPE network are investigated to understand the eruptive succession (February to May) of Piton de la Fournaise and the caldera collapse episode of April 2007. Data first indicate that the short-lived, small volume, summit eruption of February 18 occurred during a phase of continuous inflation initiated in January 2007. Inflation decelerated around 2 weeks before a second short-lived small volume eruption on March 30-31 on the SE flank, almost simultaneous with a sudden, large deflation of the edifice. Deflation rate, which had stabilized at a relatively low level, increased anew on April 1 while no magma was emitted, followed on April 2 by a more distant and one of the most voluminous eruptions of the last two centuries at La Réunion Island. The RER station shows that very long period (VLP) and ultra long period (ULP) events developed during this period. Seven ULP events preceded the caldera collapse and 48 ones occurred during the caldera collapse over 9 days, most of which during the first 30 hours. A thorough examination of the seismic signals corrected for tide effects shows that each collapse event was coeval with VLP and ULP signals. Each individual collapse showed similar ULP and VLP signals characterized by periods of ~ 500 s and ~ 7 s, respectively. The back-azimuth of most ULP signals related to the caldera collapse points clearly toward the Dolomieu caldera. The strikingly constant duration of the VLP signals (around 20 s) related to the collapse events and their occurrence before the collapse initiation suggest a physical control of the volcanic edifice. Waveforms and spectrograms of the various caldera collapse events show very homogeneous patterns, suggesting a similar and repeating volcano-tectonic process for the formation of the VLP signals events. Although tilt may be responsible of part of the ULP signals observed during the collapse events, we

  20. Three-Dimensional P-wave Velocity Structure Beneath Long Valley Caldera, California, Using Local-Regional Double-Difference Tomography

    Science.gov (United States)

    Menendez, H. M.; Thurber, C. H.

    2011-12-01

    Eastern California's Long Valley Caldera (LVC) and the Mono-Inyo Crater volcanic systems have been active for the past ~3.6 million years. Long Valley is known to produce very large silicic eruptions, the last of which resulted in the formation of a 17 km by 32 km wide, east-west trending caldera. Relatively recent unrest began between 1978-1980 with five ML ≥ 5.7 non-double-couple (NDC) earthquakes and associated aftershock swarms. Similar shallow seismic swarms have continued south of the resurgent dome and beneath Mammoth Mountain, surrounding sites of increased CO2 gas emissions. Nearly two decades of increased volcanic activity led to the 1997 installation of a temporary three-component array of 69 seismometers. This network, deployed by the Durham University, the USGS, and Duke University, recorded over 4,000 high-frequency events from May to September. A local tomographic inversion of 283 events surrounding Mammoth Mountain yielded a velocity structure with low Vp and Vp/Vs anomalies at 2-3 km bsl beneath the resurgent dome and Casa Diablo hot springs. These anomalies were interpreted to be CO2 reservoirs (Foulger et al., 2003). Several teleseismic and regional tomography studies have also imaged low Vp anomalies beneath the caldera at ~5-15 km depth, interpreted to be the underlying magma reservoir (Dawson et al., 1990; Weiland et al., 1995; Thurber et al., 2009). This study aims to improve the resolution of the LVC regional velocity model by performing tomographic inversions using the local events from 1997 in conjunction with regional events recorded by the Northern California Seismic Network (NCSN) between 1980 and 2010 and available refraction data. Initial tomographic inversions reveal a low velocity zone at ~2 to 6 km depth beneath the caldera. This structure may simply represent the caldera fill. Further iterations and the incorporation of teleseismic data may better resolve the overall shape and size of the underlying magma reservoir.

  1. Permeability and continuous gradient temperature monitoring of volcanic rocks: new insights from borehole and laboratory analysis at the Campi Flegrei caldera (Southern Italy).

    Science.gov (United States)

    Carlino, Stefano; Piochi, Monica; Tramelli, Anna; Troise, Claudia; Mormone, Angela; Montanaro, Cristian; Scheu, Bettina; Klaus, Mayer; Somma, Renato; De Natale, Giuseppe

    2016-04-01

    The pilot borehole recently drilled in the eastern caldera of Campi Flegrei (Southern Italy), during the Campi Flegrei Deep Drill Project (CFDDP) (in the framework of the International Continental Scientific Drilling Program) allowed (i) estimating on-field permeability and coring the crustal rocks for laboratory experiments, and (ii) determining thermal gradient measurements down to ca. 500 m of depth. We report here a first comparative in situ and laboratory tests to evaluate the rock permeability in the very high volcanic risk caldera of Campi Flegrei, in which ground deformations likely occur as the persistent disturbance effect of fluid circulation in the shallower geothermal system. A large amount of petro-physical information derives from outcropping welded tuffs, cores and geophysical logs from previous AGIP's drillings, which are located in the central and western part of the caldera. We discuss the expected scale dependency of rock permeability results in relation with well-stratigraphy and core lithology, texture and mineralogy. The new acquired data improve the database related to physical property of Campi Flegrei rocks, allowing a better constrain for the various fluid-dynamical models performed in the tentative to understand (and forecast) the caldera behavior. We also present the first data on thermal gradient continuously measured through 0 - to 475 m of depth by a fiber optic sensor installed in the CFDDP pilot hole. As regards, we show that the obtained values of permeability, compared with those inferred from eastern sector of the caldera, can explain the different distribution of temperature at depth, as well as the variable amount of vapor phase in the shallow geothermal system. The measured temperatures are consistent with the distribution of volcanism in the last 15 ka.

  2. The Oldest Known Caldera Associated with the Yellowstone Hotspot: New Geologic Mapping, Geochemistry, and 40Ar/39Ar Geochronology for the Northern McDermitt Volcanic Field, Northern Nevada and Southeastern Oregon

    Science.gov (United States)

    Benson, T. R.; Mahood, G. A.

    2015-12-01

    McDermitt Volcanic Field (MVF) of Nevada and Oregon is one of three major caldera centers associated with Mid-Miocene Steens/Columbia River flood basalts. Pioneering geologic mapping of MVF by Rytuba and McKee (1984) and subsequent work established four main ignimbrites within the field. Our new 40Ar/39Ar ages (FCT=28.02 Ma) are 16.41±0.02 (±2σ) Ma for Tuff of Oregon Canyon, 16.35±0.04 Ma for Tuff of Trout Creek Mountains, 16.30±0.04 Ma for Tuff of Long Ridge, and 15.56±0.08 Ma for Tuff of Whitehorse Creek. We have mapped two previously unrecognized overlapping calderas that we interpret as sources for Tuff of Oregon Canyon and Tuff of Trout Creek. These ~20-km diameter calderas lie north of the well-known McDermitt Caldera; a smaller 7-km caldera that formed on eruption of the Tuff of Whitehorse Creek is nested within them. Argon ages and geochemistry of alkali rhyolite lava domes in the northern MVF define two populations: ~16.6-16.3 Ma associated with the newly recognized calderas, and ~15.5-15.3 Ma outlining the margins of the younger Whitehorse Caldera. Consistent with both ignimbrites erupting from the same evolving magma system, the high-silica alkali rhyolite Tuff of Oregon Canyon lies on compositional trends defined by the Tuff of Trout Creek, which is zoned from a moderately crystal-rich high-silica alkali rhyolite to a strongly porphyritic low-silica alkali rhyolite. They both are distinguished from the Tuff of Long Ridge from McDermitt Caldera by their higher Zr/Rb, and relatively high FeO* concentrations distinguish all MVF ignimbrites from ignimbrites from the nearby High Rock Caldera Complex, where the oldest caldera formed on eruption of the Idaho Canyon Tuff at 16.38±0.02 Ma (Coble and Mahood, in review). The Tuff of Trout Creek rests conformably on the Tuff of Oregon Canyon west and southwest of the calderas, where they overlie a thick stack of Steens Basalt lavas. To the east and southeast the two ignimbrites are separated by as much as

  3. Numerical models for ground deformation and gravity changes during volcanic unrest: simulating the hydrothermal system dynamics of an active caldera

    Directory of Open Access Journals (Sweden)

    A. Coco

    2015-08-01

    Full Text Available Ground deformation and gravity changes in active calderas during periods of unrest can signal an impending eruption and thus must be correctly interpreted for hazard evaluation. It is critical to differentiate variation of geophysical observables related to volume and pressure changes induced by magma migration from shallow hydrothermal activity associated with hot fluids of magmatic origin rising from depth. In this paper we present a numerical model to evaluate the thermo-poroelastic response of the hydrothermal system in a caldera setting by simulating pore pressure and thermal expansion associated with deep injection of hot fluids (water and carbon dioxide. Hydrothermal fluid circulation is simulated using TOUGH2, a multicomponent multiphase simulator of fluid flows in porous media. Changes in pore pressure and temperature are then evaluated and fed into a thermo-poroelastic model (one-way coupling, which is based on a finite-difference numerical method designed for axi-symmetric problems in unbounded domains. Based on data for the Campi Flegrei caldera (Italy, a series of simulations assess the influence of fluid injection rates and mechanical properties on the hydrothermal system, uplift and gravity. Heterogeneities in hydrological and mechanical properties associated with the presence of ring faults are a key determinant of the fluid flow pattern and consequently the geophysical observables. Peaks (in absolute value of uplift and gravity change profiles computed at the ground surface are located close to injection points (namely at the centre of the model and fault areas. Temporal evolution of the ground deformation indicates that the contribution of thermal effects to the total uplift is almost negligible with respect to the pore pressure contribution during the first years of the unrest, but increases in time and becomes dominant after a long period of the simulation. After a transient increase over the first years of unrest, gravity

  4. Numerical models for ground deformation and gravity changes during volcanic unrest: simulating the hydrothermal system dynamics of a restless caldera

    Science.gov (United States)

    Coco, A.; Gottsmann, J.; Whitaker, F.; Rust, A.; Currenti, G.; Jasim, A.; Bunney, S.

    2016-04-01

    Ground deformation and gravity changes in restless calderas during periods of unrest can signal an impending eruption and thus must be correctly interpreted for hazard evaluation. It is critical to differentiate variation of geophysical observables related to volume and pressure changes induced by magma migration from shallow hydrothermal activity associated with hot fluids of magmatic origin rising from depth. In this paper we present a numerical model to evaluate the thermo-poroelastic response of the hydrothermal system in a caldera setting by simulating pore pressure and thermal expansion associated with deep injection of hot fluids (water and carbon dioxide). Hydrothermal fluid circulation is simulated using TOUGH2, a multicomponent multiphase simulator of fluid flows in porous media. Changes in pore pressure and temperature are then evaluated and fed into a thermo-poroelastic model (one-way coupling), which is based on a finite-difference numerical method designed for axi-symmetric problems in unbounded domains.Informed by constraints available for the Campi Flegrei caldera (Italy), a series of simulations assess the influence of fluid injection rates and mechanical properties on the hydrothermal system, uplift and gravity. Heterogeneities in hydrological and mechanical properties associated with the presence of ring faults are a key determinant of the fluid flow pattern and consequently the geophysical observables. Peaks (in absolute value) of uplift and gravity change profiles computed at the ground surface are located close to injection points (namely at the centre of the model and fault areas). Temporal evolution of the ground deformation indicates that the contribution of thermal effects to the total uplift is almost negligible with respect to the pore pressure contribution during the first years of the unrest, but increases in time and becomes dominant after a long period of the simulation. After a transient increase over the first years of unrest

  5. The 1996-2009 borehole dilatometer installations, operation, and maintenance at sites in Long Valley Caldera, CA

    Science.gov (United States)

    Myren, Glenn; Johnston, Malcolm; Mueller, Robert

    2011-01-01

    High seismicity levels with accelerating uplift (under the resurgent dome) in Long Valley caldera in the eastern Sierra Nevada from 1989 to 1997, triggered upgrades to dilational strainmeters and other instrumentation installed in the early 1980's following a series of magnitude 6 earthquakes. This included two additional high-resolution borehole strainmeters and replacement of the failed strainmeter at Devil's Postpile. The purpose of the borehole-monitoring network is to monitor crustal deformation and other geophysical parameters associated with volcanic intrusions and earthquakes in the Long Valley Caldera. Additional instrumentation was added at these sites to improve the capability of providing continuous monitoring of the magma source under the resurgent dome. Sites were selected in regions of hard crystalline rock, where the expected signals from magmatic activity were calculated to be a maximum and the probability of an earthquake of magnitude 4 or greater is large. For the most part, the dilatometers were installed near existing arrays of surface tiltmeters, seismometers, level line, and GPS arrays. At each site, attempts are made to separate tectonic and volcanic signals from known noise sources in each instrument type. Each of these sites was planned to be a multi-parameter monitoring site, which included measurements of 3-component seismic velocity and acceleration, borehole strain, tilt, pore pressure and magnetic field. Using seismicity, geophysical knowledge, geologic and topographic maps, and geologists recommendations, lists of preliminary sites were chosen. Additional requirements were access, and telemetry constraints. When the final site choice was made, a permit was obtained from the U.S. Forest Service. Following this selection process, two new borehole sites were installed on the north and south side of the Long Valley Caldera in June of 1999. One site was located near Big Spring Campground to the east of Crestview. The second site was

  6. Modelling of Subglacial Volcanic and Geothermal Activity, during the 2014-15 Bárdarbunga-Holuhraun Eruption and Caldera Collapse

    Science.gov (United States)

    Reynolds, H. I.; Gudmundsson, M. T.; Hognadottir, T.

    2015-12-01

    Seismic unrest was observed within the subglacial caldera of Bárdarbunga on 16 August 2014, followed by seismicity tracing the path of a lateral dyke extending underneath the Vatnajökull glacier out to 45 km to the north east of the volcano. A short subaerial fissure eruption occurred at the site of the Holuhraun lavas, just north of the glacier edge on 29 August, before recommencing in earnest on 31 August with a large effusive eruption and accompanying slow caldera collapse, which lasted for approximately 6 months. The glacier surface around Bárdarbunga was monitored using aerial altimeter profiling. Several shallow depressions, known as ice cauldrons, formed around the caldera rim and on Dyngjujökull glacier above the dyke propagation path. The cauldrons range in volume from approximately 0.0003 km3 to 0.02 km3. Two types of melting were observed: high initial heat flux over a period of days which gradually disappears; and slower but more sustained melting rates. We present time series data of the development and evolution of these cauldrons, with estimates of the heat flux magnitudes involved.The nature of the heat source required to generate these cauldrons is not obvious. Two scenarios are explored: 1) small subglacial eruptions; or 2) increased geothermal activity induced by the dyke intrusion. We investigate these scenarios using numerical modelling, considering the surface heat flux produced, and timescales and spatial extent of associated surface anomalies. It is found that a magmatic intrusion into rocks where the groundwater is near the boiling point curve can cause rapid increase in geothermal activity, but even a shallow intrusion into a cold groundwater reservoir will have a muted thermal response. Thus, our results indicate that minor subglacial eruptions are the most plausible explanation for the observed rapid melting far from known geothermal areas. These results have implications for the interpretation of thermal signals observed at ice

  7. P, S velocity and VP/VS ratio beneath the Toba caldera complex (Northern Sumatra) from local earthquake tomography

    Science.gov (United States)

    Koulakov, Ivan; Yudistira, Tedi; Luehr, Birger-G.; Wandono

    2009-06-01

    In this paper, we investigate the crustal and uppermost mantle structure beneath Toba caldera, which is known as the location of one of the largest Cenozoic eruptions on Earth. The most recent event occurred 74000 yr BP, and had a significant global impact on climate and the biosphere. In this study, we revise data on local seismicity in the Toba area recorded by a temporary PASSCAL network in 1995. We applied the newest version of the LOTOS-07 algorithm, which includes absolute source location, optimization of the starting 1-D velocity model, and iterative tomographic inversion for 3-D seismic P, S (or the VP/VS ratio) and source parameters. Special attention is paid to verification of the obtained results. Beneath the Toba caldera and other volcanoes of the arc, we observe relatively moderate (for volcanic areas) negative P- and S-velocity anomalies that reach 18 per cent in the uppermost layer, 10-12 per cent in the lower crust and about 7 per cent in the uppermost mantle. Much stronger contrasts are observed for the VP/VS ratio that is a possible indicator of dominant effect of melting in origin of seismic anomalies. At a depth of 5 km beneath active volcanoes, we observe small patterns (7-15 km size) with a high VP/VS ratio that might be an image of actual magmatic chambers filled with partially molten material feeding the volcanoes. In the mantle wedge, we observe a vertical anomaly with low P and S velocities and a high VP/VS ratio that link the cluster of events at 120-140 km depth with Toba caldera. This may be an image of ascending fluids and melts released from the subducted slab due to phase transitions. However, taking into account poor vertical resolution, these results should be interpreted with prudence. Although the results show clear signatures that are quite typical for volcanic areas (low velocity and high VP/VS ratio beneath volcanoes), we do not observe any specific features in seismic structure that could characterize Toba as a super volcano.

  8. The eruptive history and chemical stratigraphy of a post-caldera, steady-state volcano: Yasur, Vanuatu

    Science.gov (United States)

    Firth, Chris W.; Handley, Heather K.; Cronin, Shane J.; Turner, Simon P.

    2014-07-01

    The persistent activity of Yasur volcano, a post-caldera scoria cone in the southern Vanuatu Arc, along with the uniformity exhibited by its eruptive products, indicates that it is a "steady-state" volcano. This implies that rates of magma replenishment and tapping are in equilibrium. Examination of recently exposed tephra sequences suggests that Strombolian-style activity at Yasur has persisted in its current form for the last 630-850 years. Eruption of tephra with uniform grain size and texture throughout this period indicates invariant eruption magnitude and style. Based on tephra accumulation rates, a uniform, time-averaged eruption flux of ˜410-480 m3 days-1 is estimated. Major and trace element analyses of glass shards and mineral grains from these tephra deposits show limited variation in magma composition throughout that time, consistent with a chemically buffered magma reservoir and models for steady-state volcanism. Similarly, mineral crystallisation temperature estimates are within error, suggesting the magma reservoir has retained a constant temperature through this time, while pressure estimates suggest shallow crystallisation. Eruptions appear to be driven by gas release, with small fluctuations in magma chemistry and eruptive behaviour governed by perturbations in volatile flux. This period of steady-state activity was preceded by ˜600 years of higher-magnitude, lower-frequency eruptions during which less evolved compositions were erupted. Variation between these two styles of eruptive behaviour may be explained by a shift from a periodically closed to fully opened conduit, allowing more regular magma release and changes to degassing regimes. New radiocarbon ages suggest a period of irregular eruptive behaviour extending >1,400 year B.P. Overall, a transition from an irregular to a very steady magmatic system has occurred over the past ˜2 kyr. Previously determined tectonic indicators for caldera resurgence in the area suggest revived magma

  9. Avaliacao da Relacao entre a Doenca Hepatica Nao Gordurosa e CAD utilizando TCMF

    Directory of Open Access Journals (Sweden)

    Duran Efe

    2014-01-01

    Full Text Available Fundamento: Alguns fatores de risco para a aterosclerose são acompanhados pela doença hepática gordurosa não alcoólica (DHGNA. Desejamos usar a tomografia computadorizada multi-fatias (TCMF como a técnica para encontrar relação entre a DHGNA e a doença arterial coronariana (DAC. Objetivo: A relação entre a DHGNA e a DAC foi investigada através de TCMF. Métodos: Um total de 372 indivíduos com ou sem sintomas cardíacos, que foram submetidos à angiografia por TCMF, foram incluídos no estudo. Os pacientes foram divididos em dois grupos, de acordo com a presença da DHGNA. Os segmentos arteriais coronarianos foram avaliados visualmente via angiografia por TCMF. Com base no grau de estenose arterial coronariana, aqueles com placas ausentes ou mínimas foram considerados como normais, enquanto aqueles que apresentavam estenose de menos do que 50% e no mínimo uma placa foram considerados como portadores da doença arterial coronariana não obstrutiva (não-obsDAC. Os pacientes que apresentaram no mínimo uma placa e estenose arterial coronariana de 50% ou mais foram considerados como portadores de doença arterial coronariana obstrutiva (obsDAC. A DHGNA foi determinada de acordo com o protocolo de TCMF, utilizando a densidade hepática. Resultados: De acordo com a densidade hepática, o número de pacientes com doença hepática gordurosa não alcoólica (grupo 1 foi de 204 (149 homens, 54,8% e com fígado normal (grupos 2 foi de 168 (95 homens, 45.2%. Houve 50 (24,5% não-obsDAC e 57 (27,9% casos de obsDAC no Grupo 1, e 39 (23,2% não-obsDAC e 23 (13,7% casos de obsDAC no Grupo 2. Conclusões: O presente estudo utilizando TCMF demonstrou que a frequência da doença arterial coronariana em pacientes com NAFDL foi significativamente superior do que nos pacientes em NAFDL.

  10. Casos curiosos, peculiaridades y formas alternativas de anotar la música en el área hispánica en el siglo XVII. Procesos de intercambio entre lo culto y lo popular

    Directory of Open Access Journals (Sweden)

    Ezquerro Esteban, Antonio

    2001-12-01

    Full Text Available The present paper deals with an approach to some cases on Spanish 17th century Music notated in a wide variety of forms. The graphic image of these cases, will help us to better understand the adopted shapes of music, in order to reach a better "circulation" among the chapel masters and composers of the period. And that concerns not only to music, but also to the accompanying poems, or other "working models" in further elaborations, such as musical incipits, etc. Then, this contribution goes to think about on the strong influence of the Catholic church -as main patron of music in Spain- on the conformed traditions and customs of Hispanic composition, as well as on the repertories, and how these "manners" conditioned peculiar ways of notating music, creating a big variety of manuscript copies. And last but not least, the paper studies possible interchanges between the "cultivated" and "popular" surroundings of music, trough an blurred round trip, that it is needed, again, to clarify today.

    El presente artículo pretende realizar una aproximación a algunos casos de música hispana del siglo XVII anotada de las formas más variadas, no por poco frecuentes, menos importantes. Se presenta la imagen "gráfica" de algunas de las múltiples vías que la música de la época llegó a adoptar para "circular" libremente entre los maestros de capilla y compositores (y no sólo la música, sino los textos que la debían acompañar, u otros patrones de trabajo y elaboración posterior, como sus incipits musicales, etc.. Se reflexiona brevemente sobre el enorme influjo del mecenazgo eclesiástico sobre las tradiciones y "costumbres" de composición hispanas, así como sobre los repertorios, y cómo estos "modos de hacer", condicionaron peculiares formas de anotar la música hispánica en una gran variedad de copias manuscritas. Por último, se abordan en este contexto posibles intercambios entre el entorno musical "culto" y el "popular", en

  11. Evaluation of minderal resource potential, Caldera geology, and volcano-tectonic framework at and near Yucca Mountain, Task 3

    Energy Technology Data Exchange (ETDEWEB)

    Weiss, S.I.; Noble, D.C.; Larson, L.T. [Univ. of Nevada, Reno, NV (United States)

    1993-09-30

    This report summarizes the results of Task 3 work that was initially discussed in our monthly reports for the period October 1, 1992 through September 30, 1993, and contained in our various papers and abstracts, both published and currently in press or in review. Our work during this period was involved (a) the continuation of studies begun prior to October, 1992, focussed mainly on aspects of the caldera geology, volcanic stratigraphy, magmatic activity, hydrothermal mineralization and extensional tectonics of the western and northwestern parts of the southwestern and Nevada volcanic field (SWNVF), studies of the subsurface rocks of Yucca Mountain utilizing drill hole samples obtained in 1991 and 1992, and (b) new studies of veins and siliceous rocks cropping out in northwestern Yucca Mountain that provide evidence for previously unrecognized hydrothermal activity during the Crater Flat Tuff period of volcanism.

  12. Evaluation of mineral resource potential, caldera geology, and volcano-tectonic framework at and near Yucca Mountain

    Energy Technology Data Exchange (ETDEWEB)

    Weiss, S.I.; Noble, D.C.; Larson, L.T. [Univ. of Nevada, Reno, NV (United States)

    1992-09-30

    This report summarizes the result of Task 3 work initially discussed in our monthly reports for the period October 1, 1991 through September 30, 1992, and contained in our various papers and abstracts, both published and currently in press or review. Our work during this period has involved (a) the continuation of studies begun prior to October, 1991, focussed mainly on aspects of the caldera geology, volcanic stratigraphy, magmatic activity, hydrothermal mineralization and extensional tectonics of the western and northwestern parts of the southwestern Nevada volcanic field (SWNVF), and (b) new studies of the alteration and trace-metal geochemistry of subsurface rocks at Yucca Mountain utilizing drill hole samples obtained in late 1991 and early 1992.

  13. Advisory expert system for energy analysis in industrial boilers; Sistema experto asesor en el analisis energetico de calderas industriales

    Energy Technology Data Exchange (ETDEWEB)

    Kemper Valverde, Nicolas; Lara Rosano, Felipe; Vazquez Nava, Rodolfo [Laboratorio de Inteligencia Artificial, Instituto de Ingenieria UNAM, Mexico, D. F. (Mexico)

    1994-12-31

    This paper presents an expert system for the operational analysis of industrial boilers, estimating the potential of heat recovery, in the small and medium size industry. The package is friendly, practical, flexible easy to maintain and expandable to take into consideration the user`s specific requirements and allows the analysis of the energy losses in the combustion, feed water, drains, and insulation, identifying the enhancements and estimating the saving potential, in energy as well as economical. [Espanol] En este trabajo se presenta un sistema experto para analizar la operacion de calderas industriales estimando el potencial de recuperacion de calor, en la pequena y mediana industria. El paquete es amigable, practico, flexible, facil en su mantenimiento y expandible para tomar en consideracion los requerimientos especificos de los usuarios y permite el analisis de las perdidas de energia en la combustion, agua de alimentacion, purgas y aislamientos, identificando las mejoras y estimando ahorros potenciales, tanto energeticos como economicos.

  14. UTILIZANDO O MÉTODO TODIM PARA AVALIAR AS MELHORES EMPRESAS PARA TRABALHAR

    Directory of Open Access Journals (Sweden)

    Renato Teixeira da Silva

    2011-06-01

    Full Text Available Este artigo expõe uma nova proposta de ordenação das 5 melhores empresas para trabalhar em termos de qualidade do ambiente de trabalho e qualidade na gestão de pessoas utilizando-se do método TODIM como suporte científico para tal. A ordenação inicial, proposta pela revista Você/SA Exame, utiliza como método classificador o índice de felicidade no trabalho, uma soma ponderada de índices resultantes da percepção dos funcionários, das práticas da empresa e da constatação feita por jornalistas em visitas às empresas. Este trabalho, que utiliza o método TODIM, considera esses itens como critérios de avaliação e realiza uma análise comparativa das alternativas. Ao final, é executada uma comparação entre as ordenações e uma análise de sensibilidade, analisando as especificidades de cada método de ordenação e a consistência de seus resultados.

  15. Modelaje geológico y de recursos del yacimiento Pastelillo utilizando el krigeaje de indicadores

    Directory of Open Access Journals (Sweden)

    José Q. Cuador-Gil

    2005-03-01

    Full Text Available En ocasiones la complejidad y variabilidad de un yacimiento mineral hace dificil establecer dominios geológicos homogéneos que puedan ser utilizados para aplicar control geológico a la estimación de los parámetros más relevantes. La imposibilidad de crear un modelo geológico con unidades bien definidas conduce a trabajar con poblaciones heterogéneas, lo cual degrada considerablemente la calidad de las estimaciones. Tal es el caso de Pastelillo, yacimiento de materia prima para cemento, en el que es difícil reproducir la geometría de los distintos tipos tecnológicos utilizando el método tradicional de correlación geológica. Las distintas litologías que conforman el yacimientos están completamente mezcladas tanto en el plano como en la vertical y estos frecuentes cambios faciales provocan una gran variabilidad litológica y tecnológica en el yacimiento. Teniendo en cuenta lo anterior se propone emplear un método de interpolación espacial que permita hacer estimaciones en presencia de poblaciones complejas. En el artículo se establece un modelo tecnológico y de recursos para el yacimiento Pastelillo a partir del empleo de una técnica de estimación de la geoestadística no lineal: el krigeaje de indicadores.

  16. Cálculo del factor de efectividad utilizando colocación ortogonal sobre elementos finitos

    Directory of Open Access Journals (Sweden)

    Javier Fontalvo Alzate

    2011-02-01

    Full Text Available En el presente documento se resuelve el problema del cálculo del factor de efectividad para la transferencia de masa y calor con reacción química en un pellet catalítico utilizando una técnica adecuada especialmente para números de Thiele elevados en donde la solución se restringe a una pequeña zona muy cercana a la superficie. La técnica aprovecha la rapidez de convergencia de la colocación ortogonal y la facilidad de ubicación de elementos en zonas en donde se presentan grandes gradientes del método para las diferencias finitas. La eficiencia del método está basada en la utilización del método LV para la descomposición de matrices. Se muestran comparaciones con otros métodos numéricos de solución del problema.

  17. DESARROLLO DE APIO MINIMAMENTE PROCESADO FORTIFICADO CON VITAMINA E, UTILIZANDO LA INGENIERIA DE MATRICES

    Directory of Open Access Journals (Sweden)

    YISELL JOHAN MARTELO CASTAÑO

    2011-01-01

    Full Text Available El objetivo de este trabajo fue desarrollar un producto minimamente procesado fortificado con vitamina E, a partir de apio (Apium graveolens L. var.dulce, utilizando la ingenieria de matrices como metodologia de obtencion de alimentos funcionales. Trozos de apio impregnados al vacio con dl¿¿tocoferol acetato emulsificado en una solucion isotonica al vegetal de NaCl, 1,2%, fueron evaluados en funcion del tiempo de almacenamiento y el envasado (con y sin vacio, en terminos de la cuantificacion de sus propiedades fisicoquimicas, color, textura, estabilidad de la vitamina E y caracteristicas sensoriales. Se formulo la emulsion con el objetivo de adicionar teoricamente un 73% del Valor Diario Recomendado (VDR vitamina E/100 g de apio fresco y su cuantificacion se realizo por HPLC. La respuesta a la impregnacion en la matriz fue de 12,10+-1,15%, lo cual permitio alcanzar un 112% VDR vitamina E/100g apio fresco, manteniendose este contenido durante el almacenamiento de 9 dias en ambos tipos de envasado. Los parametros fisicoquimicos del producto fueron afectados por la IV, el tiempo y el envasado, manteniendo su coloracion verdosa y presentando disminucion en la firmeza. La ingenieria de matrices constituye una metodologia efectiva para el desarrollo de apio minimamente procesado adicionado con vitamina E.

  18. Detecção de estro em jaguatirica (Leopardus pardalis utilizando citologia vaginal

    Directory of Open Access Journals (Sweden)

    R.C.R Paz

    2010-12-01

    Full Text Available Utilizou-se a citologia vaginal por meio de diferentes métodos de coloração para detecção de cio em jaguatirica, Leopardus pardalis, pela estimulação hormonal exógena e pela avaliação das estruturas ovarianas por videolaparoscopia. Cinco fêmeas foram tratadas com eCG/hCG e FSH/LH a cada quatro meses pelo período de dois anos. Videolaparoscopia foi realizada após cada tratamento utilizando-se cetamina-xilazina e isoflurano. Esfregaços vaginais foram obtidos 15 dias antes e após a videolaparoscopia. As lâminas foram analisadas ao microscópio de luz quanto aos tipos celulares predominantes. Todos os animais apresentaram folículos maduros (>2mm e corpos lúteos recentes em todas as intervenções. Não houve diferença significativa entre os resultados obtidos na mesma coloração de acordo com os tratamentos utilizados. Todas as técnicas mostraram-se eficientes na detecção de células superficiais queratinizadas anucleadas e nucleadas, intermediárias, parabasais e basais. Foi possível determinar a fase de estro em Leopardus pardalis por meio da citologia vaginal

  19. Monitoramento do processo de compressão de ibuprofeno utilizando controle estatístico

    Directory of Open Access Journals (Sweden)

    Sara Elis Bianchi

    2012-04-01

    Full Text Available O Controle Estatístico de Processo (CEP é uma ferramenta bastante utilizada para auxiliar no controle da qualidade de parâmetros físicos como peso médio, dureza e friabilidade. Através das cartas de controle é possível detectar desvios dos parâmetros do processo, reduzindo a quantidade de produtos fora da especificação e, consequentemente, os custos da produção. A avaliação de trinta lotes de ibuprofeno em uma indústria farmacêutica, utilizando controle estatístico de processo, permitiu o fornecimento de informações imprescindíveis para a investigação detalhada dos pontos críticos do processo, diagnosticando as possíveis não conformidades na etapa de compressão deste fármaco. Desta maneira, podem-se propor atividades de melhoria, através da identificação e eliminação das causas especiais de variação no processo, com a finalidade de produzir comprimidos com qualidade.

  20. Steam flow generation in semi-arid, forested and seasonally snow-covered catchments, Valles Caldera, New Mexico

    Science.gov (United States)

    Liu, F.; Bales, R. C.; Conklin, M. H.; Kostrzewski, J. M.

    2005-12-01

    Stream flow generation is poorly understood for semi-arid, forested and seasonally snow-covered catchments in southwest US. Here we report on initial results of a pioneer study on source waters and flowpaths using isotopic and geochemical tracers in two streams originated from Redondo Peak in Valles Caldera, New Mexico. The Valles Caldera is the latest collapse feature in the volcanic field and hosts high-temperature hydrothermal systems with several geothermal springs. It is currently covered by ponderosa pine in lower elevations and mixed conifer in higher elevations. Samples were collected from snow, hillslope groundwater, and stream water at Redondo Creek and La Jara Creek from December 2004 to July 2005. Using diagnostic tools of mixing models and end-member mixing analysis, it is suggested that stream water quantity and quality at Redondo Creek were primarily controlled by mixing of two end-members: hillslope subsurface water and geothermal springs. Hillslope subsurface water was sourced from snowmelt and then gradually released to stream flow through spring and summer. Infiltration-excess overland flow of snowmelt did not appear to occur. Contribution of hillslope subsurface water to stream flow was 90% on average from December 2004 to July 2005 and its percentage gradually increased from spring to summer with increase in discharge. Contribution of geothermal springs decreased on percentage over season with a peak (20%) in late march and lowest but relatively constant value (5%) through June and July. Stream flow generation at La Jara Creek was relatively simple, all from hillslope subsurface water. This information may improve our understanding of changes of hydrological and biogeochemical cycles in response to climate warming in these and similar catchments in southwest US.

  1. DYNAMIC MIXING MODEL OF THE CHIGNAHUAPAN THERMAL SPRING IN THE GEOTHERMAL ZONE OF THE ACOCULCO CALDERA, PUEBLA, MEXICO

    Science.gov (United States)

    Gutierrez-Cirlos, A.; Torres-Rodriguez, V.

    2009-12-01

    The Acoculco Caldera, of Pliocenic age, is located within the limits of the Transmexican Volcanic Belt (CVT) and the Sierra Madre Oriental (SMOr). The Acoculco geothermal zone consists of a 790m thick igneous sequence, related to a volcanic complex formed by andesites and rhyolitic domes emplaced in an 18 Km diameter annular fracture. It unconformably overlies a 5000 m thick section of folded and faulted Jurassic-Cretaceous carbonate rocks. The Chignahuapan Spring, located in the extreme eastern part of the Geothermal Zone of the Acoculco Caldera, yields temperatures of 49°C and discharges an estimated of 98 lps from the karstified Lower Cretaceous limestone. Both major and trace element geochemical analysis were carried out, and results were interpreted using Piper and Stiff diagrams, as well as geothermometry. The results indicate that water belongs to the calcium-bicarbonate type and yield temperatures in a range of 70-80°C at depth, which suggest an extensive lateral flow from the main reservoir and mixing with shallow groundwaters. The spring suffers significant variations in its temperature throughout the year, especially during the rainy season, when water temperature decreases up to 10°C. Analyzing the hot spring water temperature data from of the last 10 years and comparing it with the precipitation and air temperature curves of the region, we expect to develop a dynamic mixing model which depicts the relation between these factors and the importance of each one in the water temperature variation. We also look forward to be able to forecast water temperature trends for the next several years and correlate it with climate change in the area.

  2. Regulatory, Land Ownership, and Water Availability Factors for a Magma Well: Long Valley Caldera and Coso Hot Springs, California

    Energy Technology Data Exchange (ETDEWEB)

    Blackett, Robert

    1985-09-01

    The U.S. Department of Energy is currently engaged in a program to demonstrate the engineering feasibility of extracting thermal energy from high-level molten magma bodies. The program is being carried out under the direction of Sandia National Laboratories where a number of individual projects support the overall program. The existing program elements include (1) high-temperature materials compatibility testing; (2) studies of properties of melts of various compositions; and (3) the investigation of the economics of a magma energy extraction system. Another element of the program is being conducted with the cooperation of the U.S. Geological Survey, and involves locating and outlining magma bodies at selected sites using various geophysical techniques. The ultimate goal here will be to define the limits of a magma body as a drilling target. During an earlier phase of the program, more than twenty candidate study sites considered were evaluated based upon: (1) the likelihood of the presence of a shallow magma chamber, (2) the accessibility of the site, and (3) physical and institutional constraints associated with each site with respect to performing long-term experiments. From these early phase activities, the number of candidate sites were eventually narrowed to just 2. The sites currently under consideration are Coso Hot Springs and the Long Valley caldera (Figure 1). This report describes certain attributes of these sites in order to help identify potential problems related to: (1) state and federal regulations pertaining to geothermal development; (2) land ownership; and (3) water resource availability. The information sources used in this study were mainly maps, publications, and informative documents gathered from the California Division of Oil and Gas and the U.S. Department of the Interior. Environmental studies completed for the entire Long Valley caldera study area, and for portions of the Coso Hot Springs study area were also used for reference.

  3. Crónica de los intercambios entre los grupos humanos paleolíticos. La contribución del arte para el periodo 20000-12000 años BP

    Directory of Open Access Journals (Sweden)

    Georges SAUVET

    2009-08-01

    Full Text Available RESUMEN: En el transcurso de sus ciclos estacionales, los cazadores-recolectores del Paleolítico superior frecuentemente entraban en contacto con otros grupos. Testimonio de ello son la difusión de ciertas materias primas y los intercambios de bienes materiales y de las habilidades tecnológicas, pero los intercambios socioculturales no pueden evaluarse más que a través del compartimiento de valores simbólicos, revelado, principalmente, por la creación de obras de carácter artístico (arte mueble, arte rupestre y objetos de adorno personal. En un cuadro cronológicamente restringido (entre 20000 y 12000 BP y un espacio limitado (desde el norte de España al sudoeste de Francia, hemos investigado los argumentos temáticos, estilísticos y técnicos que permiten evaluar el grado de ósmosis sociocultural entre los grupos que vivían en este vasto territorio. Nuestra encuesta concluye con una visión contrastada de la historia de estas sociedades. Ciertos caracteres dejan entrever particularismos regionales de naturaleza idiosincrásica, pero, por el contrario y al menos para ciertos periodos, otros muestran una unificación de los sistemas de representación, que debe reflejar una homogeneización en las formas de organización social. Así, después de un periodo bastante largo, durante el que la Región Cantábrica desarrolló un sistema propio, independiente del de las regiones de Aquitania y Nortepirenaica, se asiste en el conjunto del territorio y durante el Magdaleniense medio, a una aproximación entre las concepciones artísticas, que probablemente sea la consecuencia de una intensificación de los contactos y del establecimiento de redes sociales operativas. Hacia el final del Magdaleniense, esta unidad de conjunto se disuelve progresivamente, a causa de una expansión territorial que hizo que los contactos se produjeran entre poblaciones cada vez más alejadas. En el plano metodológico, las obras de arte plástico son

  4. Geomorfología de la región de los lagos Moquehue y Aluminé: consideraciones acerca de las propuestas Calderas Meseta del Arco y Nacimientos del Aluminé (Neuquén Geomorphology of the Moquehue and Aluminé Lakes: Considerations about the Meseta del Arco and Nacimientos del Aluminé calderas

    Directory of Open Access Journals (Sweden)

    Emilio F. González Díaz

    2010-05-01

    Full Text Available Se exponen elementos de juicio geomórficos y estructurales, que avalan la morfogénesis glaciaria de la depresión en artesa que aloja la cuenca lacustre Moquehue-Aluminé, ubicada en la cordillera neuquina (38°30´S, adyacente al límite internacional. Trabajos anteriores distinguen en la región dos calderas de un gran complejo volcánico plio-cuaternario, situado al este del frente volcánico actual e integrado por nueve depresiones caldéricas y cuerpos dómicos asociados. En el área de estudio sólo la caldera de Pino Hachado tiene la validez necesaria, cuestionándose el reconocimiento de las calderas denominadas Nacimientos del Aluminé y Meseta del Arco, al tiempo que se avala el origen erosivo de las abruptas escarpas orientales que marginan el plateau de Lonco Luan-Meseta del Arco, las que fueran interpretadas como márgenes de las sugeridas calderas. Se analizan las fases o tipología del englazamiento pleistoceno local, su extensión, las direcciones de los principales movimientos de su flujo y su más que probable aporte de hielo por difluencia, a un contemporáneo englazamiento en Chile (laguna Icalma. Se describen aspectos de la morfogenia volcánica cenozoica y otros más locales de la remoción en masa y el proceso eólico. Se incorporan breves comentarios acerca de un propuesto drenaje atlántico de un río Bío Bío preglaciario y se cuestiona aquellos antecedentes que avalan la extensión en la región de la fosa Bío Bío-Aluminé y la presencia de las citadas calderas. Una serie de perfiles esquemáticos topográfico-geológicos contribuyen a dicho cuestionamiento.The region is situated in the Neuquén Cordillera at 38° 30´S latitud close to the international border. Geomorphic and structural features are presented which indicated a glacial morphogenesis for the depression that contains the Moquehue- Aluminé lakes. Previous works have identified a large volcanic complex related to Plio-Quaternary volcanic activity

  5. Primary welding and crystallisation textures preserved in the intra-caldera ignimbrites of the Permian Ora Formation, northern Italy: implications for deposit thermal state and cooling history

    Science.gov (United States)

    Willcock, M. A. W.; Cas, R. A. F.

    2014-06-01

    Exceptional exposure through a Permian intra-caldera ignimbrite fill within the 42 × 40 km Ora caldera (>1,290 km3 erupted volume) provides an opportunity to study welding textures in a thick intra-caldera ignimbrite succession. The ignimbrite succession records primary dense welding, a simple cooling unit structure, common crystallisation zones, and remarkably preserves fresh to slightly hydrated glass in local vitrophyre zones. Evidence for primary syn- and post-emplacement welding consists of (a) viscously deformed and sintered juvenile glass and relict shard textures; (b) complete deposit welding; (c) subtle internal welding intensity variations; (d) vitrophyre preserved locally at the base of the ignimbrite succession; (e) persistent fiamme juvenile clast shapes throughout the succession at the macroscopic and microscopic scales, defining a moderate to well-developed eutaxitic texture; (f) common undulating juvenile clast (pumice) margins and feathery terminations; (g) a general loss of deposit porosity; and (h) perlitic fracturing. A low collapsing or fountaining explosive eruption column model is proposed to have facilitated the ubiquitous welding of the deposit, which in turn helped preserve original textures. The ignimbrite succession preserves no evidence of a time break through the sequence and columnar joints cross-gradational ignimbrite lithofacies boundaries, so the ignimbrite is interpreted to represent a simple cooling unit. Aspect ratio and anisotropy of magnetic susceptibility (AMS) analyses through stratigraphic sections within the thick intra-caldera succession and at the caldera margin reveal variable welding compaction and strain profiles. Significantly, these data show that welding degree/intensity may vary in an apparently simple cooling unit because of variations in eruption process recorded in differing lithofacies. These data imply complex eruption, emplacement, and cooling processes. Three main crystallisation textural zones are

  6. EVALUACIÓN DE LA BIOESTIMULACION (NUTRIENTES EN SUELOS CONTAMINADOS CON HIDROCARBUROS UTILIZANDO RESPIROMETRIA

    Directory of Open Access Journals (Sweden)

    Roldán Fabio

    2011-04-01

    Full Text Available Se evaluó el proceso de bioestimulación por nutrientes: fertilizantes inorgánicos compuestos (FIC N:P:K 28:12:7 y sales inorgánicas simples (SIS NH4NO3 y K2HPO4 en suelos contaminados con hidrocarburos utilizando respirometría. El suelo fue contaminado con lodos aceitosos a una concentración ~40,000 mgTPH/kgps. Para cuantificar el consumo de oxigeno se utilizaron dos respirómetros de medición manométrica HACH® 2173b y OXITOP® PF600 durante ensayos de trece días. Se evaluaron dos tratamientos (FIC y SIS y tres controles (abiótico, sustrato de referencia y sin nutrientes. Se analizaron parámetros físico-químicos (pH, nutrientes y TPH y microbiológicos (heterótrofos y degradadores al inicio y al final de cada ensayo. SIS y el control sin nutrientes presentaron las mayores tasas de respiración, en el equipo HACH se obtuvieron valores de: 802.28 y 850.72 mgO2kgps-1d-1 respectivamente mientras que en el OXITOP fueron de 936.65 y 502.05 mgO2kgps-1d-1, respectivamente. En ninguno de los equipos se observo un aumento significativo de los degradadores, indicando que la bioestimulación no tuvo un efecto sobre la densidad microbiana. Por otro lado FIC, presentó los recuentos y tasas de respiración más bajas (188.18 y 139.87 mgO2kgps-1d-1 en HACH y OXITOP, respectivamente, esto pudo estar correlacionado a un efecto toxico generado por la acumulación de amoniaco.

  7. Acceso remoto seguro a cuentas de usuario utilizando plataformas de virtualización

    Directory of Open Access Journals (Sweden)

    Walter Fuertes, Maritza Enríquez y Diego Veloz

    2011-05-01

    Full Text Available En  las  universidades  persiste  el  problema  de  la subutilización de recursos tecnológicos; sin embargo, sesigue  incurriendo en gastos por adquisición de servidores,hardware  y  software. Frente  a  este  escenario,  en  laindustria se han venido desarrollando las tecnologías devirtualización, que ahorran energía y costos de inversiónde hardware. En  consecuencia,  el  artículo propone  elacceso remoto seguro a cuentas de usuario en un servidoruniversitario  virtualizado;  para  llevarlo  a  cabo  sediseñaron  e  implementaron  varias  topologías  deexperimentación, utilizando Virtual Box 3.1.3 y VMwareServer 2.0.2,  y  se  evaluaron diversas  tecnologías  deconexiones remotas seguras, bajo  idénticas condicionesy parámetros de  comprobación. En  cada  topología  seevaluó el rendimiento del servidor, el performance y  laseguridad  de  la  red  en  producción. Los  resultadosmuestran  la  funcionalidad  de  este  proyecto  deinvestigación  que  facilita  el  acceso  remoto  seguro deusuarios a los recursos informáticos universitarios.

  8. Evaluación de ataques UDP Flood utilizando escenarios virtuales como plataforma experimental

    Directory of Open Access Journals (Sweden)

    Walter Fuertes

    2012-05-01

    Full Text Available Los ataques por denegación de servicio (DoS tienen como propósito imposibilitar el acceso a los servicios de una organización durante un periodo indefinido; por lo general, están dirigidos a los servidores de una empresa, para que no puedan ser accedidos por usuarios autorizados. El presente trabajo se enfoca en la evaluación de ataques DoS tipo UDP Flood, utilizando como plataforma de experimentación un entorno virtual de red que permite identificar cómo actúan dichos ataques en la saturación del ancho de banda; para llevarlo a cabo se diseñó e implementó una red híbrida con segmentación WAN, LAN y DMZ que inhabilita el acceso interno y externo a un servicio Web expuesto. Las herramientas evaluadas fueron UPD Unicorn, Longcat Flooder y UDPl.pl Script de Perl; las dos primeras instaladas sobre Windows, y la última, sobre Linux. Para validar está investigación se desarrolló un mecanismo de detección y mitigación de los ataques a nivel del firewall e IDS/IPS, evitando de este modo la saturación de la red. Finalmente, se evaluó el consumo dememoria, CPUy ancho de banda durante el ataque, la detección y la evasión, con el fin de determinar cuál genera mayor impacto. Los resultados demuestran que el mecanismo detecta, controla y mitiga los ataques. 

  9. Evaluación de ataques UDP Flood utilizando escenarios virtuales como plataforma experimental

    Directory of Open Access Journals (Sweden)

    Deyci Toscano

    2011-07-01

    Full Text Available Los ataques por denegación de servicio (DoS tienen como propósito imposibilitar el acceso a los servicios de una organización durante un periodo indefinido; por lo general, están dirigidos a los servidores de una empresa, para que no puedan ser accedidos por usuarios autorizados. El presente trabajo se enfoca en la evaluación de ataques DoS tipo UDP Flood, utilizando como plataforma de experimentación un entorno virtual de red que permite identificar cómo actúan dichos ataques en la saturación del ancho de banda; para llevarlo a cabo se diseñó e implementó una red híbrida con segmentación WAN, LAN y DMZ que inhabilita el acceso interno y externo a un servicio Web expuesto. Las herramientas evaluadas fueron UPD Unicorn, Longcat Flooder y UDPl.pl Script de Perl; las dos primeras instaladas sobre Windows, y la última, sobre Linux. Para validar está investigación se desarrolló un mecanismo de detección y mitigación de los ataques a nivel del firewall e IDS/IPS, evitando de este modo la saturación de la red. Finalmente, se evaluó el consumo dememoria, CPUy ancho de banda durante el ataque, la detección y la evasión, con el fin de determinar cuál genera mayor impacto. Los resultados demuestran que el mecanismo detecta, controla y mitiga los ataques.

  10. Active tectonics on Deception Island (West-Antarctica): A new approach by using the fractal anisotropy of lineaments, fault slip measurements and the caldera collapse shape

    Science.gov (United States)

    Pérez-López, R.; Giner-Robles, J.L.; Martínez-Díaz, J.J.; Rodríguez-Pascua, M.A.; Bejar, M.; Paredes, C.; González-Casado, J.M.

    2007-01-01

    The tectonic field on Deception Island (South Shetlands, West Antarctica) is determined from structural and fractal analyses. Three different analyses are applied to the study of the strain and stress fields in the area: (1) field measurements of faults (strain analysis), (2) fractal geometry of the spatial distribution of lineaments and (3) the caldera shape (stress analyses). In this work, the identified strain field is extensional with the maximum horizontal shortening trending NE-SW and NW-SE. The fractal technique applied to the spatial distribution of lineaments indicates a stress field with SHMAX oriented NE-SW. The elliptical caldera of Deception Island, determined from field mapping, satellite imagery, vents and fissure eruptions, has an elongate shape and a stress field with SHMAX trending NE-SW.

  11. The 2007 eruptions and caldera collapse of the Piton de la Fournaise volcano (La Réunion Island) from tilt analysis at a single very broadband seismic station

    Science.gov (United States)

    Fontaine, Fabrice R.; Roult, Geneviève; Michon, Laurent; Barruol, Guilhem; Muro, Andrea Di

    2014-04-01

    Seismic records from La Réunion Island very broadband Geoscope station are investigated to constrain the link between the 2007 eruptive sequence and the related caldera collapse of the Piton de la Fournaise volcano. Tilt estimated from seismic records reveals that the three 2007 eruptions belong to a single inflation-deflation cycle. Tilt trend indicates that the small-volume summit eruption of 18 February occurred during a phase of continuous inflation that started in January 2007. Inflation decelerated 24 days before a second short-lived, small-volume eruption on 30 March, almost simultaneous with a sudden, large-scale deflation of the volcano. Deflation rate, which had stabilized at relatively low level, increased anew on 1 April while no magma was erupted, followed on 2 April by a major distal eruption and on 5 April by a summit caldera collapse. Long-term tilt variation suggests that the 2007 eruptive succession was triggered by a deep magma input.

  12. Tomography from 26 years of seismicity revealing that the spatial extent of the Yellowstone crustal magma reservoir extends well beyond the Yellowstone caldera

    Science.gov (United States)

    Farrell, Jamie; Smith, Robert B.; Husen, Stephan; Diehl, Tobias

    2014-05-01

    The Yellowstone volcanic field has experienced three of Earth's most explosive volcanic eruptions in the last 2.1 Ma. The most recent eruption occurred 0.64 Ma forming the 60 km long Yellowstone caldera. We have compiled earthquake data from the Yellowstone Seismic Network from 1984 to 2011 and tomographically imaged the three-dimensional P wave velocity (Vp) structure of the Yellowstone volcanic system. The resulting model reveals a large, low Vp body, interpreted to be the crustal magma reservoir that has fueled Yellowstone's youthful volcanism. Our imaged magma body is 90 km long, 5-17 km deep, and 2.5 times larger than previously imaged. The magma body extends ~15 km NE of the caldera and correlates with the location of the largest negative gravity anomaly, a -80 mGal gravity low. This new seismic image provides important constraints on the dynamics of the Yellowstone magma system and its potential for future volcanic eruptions and earthquakes.

  13. Validation of a smooth configuration surface for compact heat exchangers using a numerical method//Validación de la superficie de un intercambiador de calor compacto en configuración lisa utilizando un método numérico

    Directory of Open Access Journals (Sweden)

    José‐L. Leiro‐Garrido

    2014-08-01

    Full Text Available This work determines the thermo hydraulics behavior of smooth configuration surface for a compact heat exchanger by means of numerical simulation. The objective is to use the results as baseline for research in the enhancement of heat transfer and drag reduction, directed to reduce the energy consumption and diminish the environmental impact. The fin tube heat exchanger models described.The constraints used in the implementation of the equation solver are announced. The average heat transfer coefficient and pressure drop obtained from numerical simulation are compare to experimental results presented in literature for models with the same dimensions and configuration. A good agreement between numerical and experimental results is reached. Local mechanisms responsible for the heat transfer and pressure drop are detailed. The study is conducted inside thelaminar regime for frontal velocities ranging between 0.5 and 6 m/s.Key words: compact heat exchanger, heat transfer coefficient, numerical simulation, pressure drop.______________________________________________________________________________ResumenEste trabajo determina el comportamiento termo hidráulico de una superficie perteneciente a un intercambiador de calor compacto en configuración lisa utilizando un método de simulación numérica. El objetivo es caracterizar la superficie para poder utilizarla como una referencia en las comparaciones con superficies de intercambio de calor intensificadas. Los datos obtenidos seutilizaran en la determinación de los valores relativos de intensificación de la transferencia de calor y el arrastre intentando reducir el consumo energético y su impacto ambiental. Se describe el modelo de intercambiador de calor con tubos aletados. Los resultados numéricos obtenidos presentan unbuen ajuste con los valores experimentales. Los resultados del coeficiente de transferencia de calor global y la caída de presión son explicados a partir de las

  14. Acerca de la propuesta "Caldera de Ñireco" en el centro-oeste de los Andes Neuquinos (38º50'S - 70º50'O The "Ñireco Caldera" in the central-western Neuquén Andes (38º50'S - 70º50'O

    Directory of Open Access Journals (Sweden)

    Emilio F González Díaz

    2010-10-01

    Full Text Available En el tramo austral del alto estructural de Copahue-Pino Hachado, a la latitud de la cuenca lacustre Moquehue-Aluminé y cercanías del límite argentino-chileno, ha sido distinguido un conjunto anómalo de nueve calderas resultantes de la actividad volcánica del Plioceno-Cuaternario. La "caldera de Ñireco", parte integrante de este conjunto, es motivo del presente trabajo. Los autores objetan el reconocimiento de tal componente morfoestructural a partir de un análisis geomorfológico, estructural y estratigráfico del área. A partir de ello, se reconoce una correspondencia entre los propuestos límites de dicha caldera, y la situación de los principales valles resultantes del proceso erosivo fluvial, cuyo desarrollo estuvo controlado por fallas inversas y lineamientos regionales. No existen evidencias que faciliten el reconocimiento de un aparato volcánico que teóricamente albergue la sugerida depresión caldérica, o remanentes de sus flancos externos e internos. En el sector central de la propuesta "caldera de Ñireco" se dan las mayores alturas topográficas de la región (± 2.900 m s.n.m., valores que superan ampliamente a los de la Cordillera Principal a estas latitudes. La estratigrafía local de la propuesta área de la caldera está compuesta esencialmente por las rocas más antiguas de la zona (granitoides del Paleozoico superior y secuencias volcánicas y volcaniclásticas del Triásico y no guarda coincidencia temporal alguna con la actividad volcánica del Plioceno-Cuaternario, la que se halla bien representada inmediatamente al norte y sur del sector analizado. La zona de estudio se enmarca por el contrario dentro de una faja plegada y corrida de piel gruesa y vergencia occidental, en donde la inversión tectónica jugó un rol central.In the southern segment of the Copahue- Pino Hachado block, next to the Moquehue-Alumine lacustrine basin, an anomalous concentration of calderas, resulting from a Pliocene

  15. The 2007 eruptions and caldera collapse of the Piton de la Fournaise volcano (La Réunion Island) from tilt analysis at a single very broadband seismic station

    OpenAIRE

    Fontaine, Fabrice R.,; Roult, Geneviève; Michon, Laurent; Barruol, Guilhem; Muro, Andrea Di

    2014-01-01

    International audience Seismic records from La Réunion Island very broadband Geoscope station are investigated to constrain the link between the 2007 eruptive sequence and the related caldera collapse of the Piton de la Fournaise volcano. Tilt estimated from seismic records reveals that the three 2007 eruptions belong to a single inflation-deflation cycle. Tilt trend indicates that the small-volume summit eruption of 18 February occurred during a phase of continuous inflation that started ...

  16. Evaluating Spatial Heterogeneity and Environmental Variability Inferred from Branched Glycerol Dialkyl Glycerol Tetraethers (GDGTs) Distribution in Soils from Valles Caldera, New Mexic

    Science.gov (United States)

    Contreras Quintana, S. H.; Werne, J. P.; Brown, E. T.; Halbur, J.; Sinninghe Damsté, , J.; Schouten, S.; Correa-Metrio, A.; Fawcett, P. J.

    2014-12-01

    Branched glycerol dialkyl glycerol tetraethers (GDGTs) are recently discovered bacterial membrane lipids, ubiquitously present in peat bogs and soils, as well as in rivers, lakes and lake sediments. Their distribution appears to be controlled mainly by soil pH and annual mean air temperature (MAT) and they have been increasingly used as paleoclimate proxies in sedimentary records. In order to validate their application as paleoclimate proxies, it is essential evaluate the influence of small scale environmental variability on their distribution. Initial application of the original soil-based branched GDGT distribution proxy to lacustrine sediments from Valles Caldera, New Mexico (NM) was promising, producing a viable temperature record spanning two glacial/interglacial cycles. In this study, we assess the influence of analytical and spatial soil heterogeneity on the concentration and distribution of 9 branched GDGTs in soils from Valles Caldera, and show how this variability is propagated to MAT and pH estimates using multiple soil-based branched GDGT transfer functions. Our results show that significant differences in the abundance and distribution of branched GDGTs in soil can be observed even within a small area such as Valles Caldera. Although the original MBT-CBT calibration appears to give robust MAT estimates and the newest calibration provides pH estimates in better agreement with modern local soils in Valles Caldera, the environmental heterogeneity (e.g. vegetation type and soil moisture) appears to affect the precision of MAT and pH estimates. Furthermore, the heterogeneity of soils leads to significant variability among samples taken even from within a square meter. While such soil heterogeneity is not unknown (and is typically controlled for by combining multiple samples), this study quantifies heterogeneity relative to branched GDGT-based proxies for the first time, indicating that care must be taken with samples from heterogeneous soils in MAT and p

  17. Effect of petrophysical properties and deformation on vertical zoning of metasomatic rocks in U-bearing volcanic structures: A case of the Strel'tsovka caldera, Transbaikal region

    Science.gov (United States)

    Petrov, V. A.; Andreeva, O. V.; Poluektov, V. V.

    2014-03-01

    The development of vertical zoning of wall-rock metasomatic alteration is considered with the Mesozoic Strel'tsovka caldera as an example. This caldera hosts Russia's largest uranium ore field. Metasomatic rocks with the participation of various phyllosilicates, carbonates, albite, and zeolites are widespread in the ore field. In the eastern block of the caldera, where the main uranium reserves are accommodated, hydromica metasomatic alteration gives way to beresitization with depth. Argillic alteration, which is typical of the western block, is replaced with hydromica and beresite alteration only at a significant depth. Postore argillic alteration is superposed on beresitized rocks in the lower part of the section. Two styles of vertical metasomatic zoning are caused by different modes of deformation in the western and eastern parts of the caldera. Variations of the most important petrophysical properties of host rocks—density, apparent porosity, velocities of P- and S-waves, dynamic Young's modulus, and Poisson coefficient—have been determined by sonic testing of samples taken from different depths. It is suggested that downward migration of the brittle-ductile transition zone could have been a factor controlling facies diversity of metasomatic rocks. Such a migration was caused by a new phase of tectonothermal impact accompanied by an increase in the strain rate or by emplacement of a new portion of heated fluid. Transient subsidence of the brittle-ductile boundary increases the depth of the hydrodynamically open zone related to the Earth's surface and accelerates percolation of cold meteoric water to a greater depth. As a result, the temperature of the hydrothermal solution falls down, increasing the vertical extent of argillic alteration. High-grade uranium mineralization is also localized more deeply than elsewhere.

  18. The combined use of InSAR and GPS Time-Series to Infer the Deformation Signals at the Yellowstone Caldera

    Science.gov (United States)

    Pepe, A.; Tizzani, P.; Battaglia, M.; Castaldo, R.; Lanari, R.; Zeni, G.

    2015-12-01

    We investigate the Yellowstone caldera geological unrest between 1977 and 2010 by analyzing temporal changes in differential Interferometric Synthetic Aperture Radar (InSAR), precise spirit leveling andgravity measurements. The analysis of the 1992-2010 displacement time series has been retrieved by applying an "improved" version of the Small Baseline Subset (SBAS) InSAR technique which complements a novel multi-temporal noise filtering approach with a suitable identification of the network of small baseline pairs. As a result, we have identified three areas of deformation: (i) the Mallard Lake (ML) and Sour Creek (SC) resurgent domes, (ii) a region close to the Northern Caldera Rim (NCR), and (iii) the eastern Snake River Plain (SRP). While the eastern SRP shows a signal related to tectonic deformation, the other two regions are influenced by the caldera unrest. We removed the tectonic signal from the InSAR displacements, and we modeled the InSAR, leveling, and gravity measurements to retrieve the best fitting source parameters. Our findings confirmed the existence of different distinct sources, beneath the brittle-ductile transition zone, which have been intermittently active during the last three decades. Moreover, we interpreted our results in the light of existing seismic tomography studies. Concerning the SC dome, we highlighted the role of hydrothermal fluids as the driving force behind the 1977-1983 uplift; since 1983-1993 the deformation source transformed into a deeper one with a higher magmatic component. Furthermore, our results support the magmatic nature of the deformation source beneath ML dome for the overall investigated period. Finally, the uplift at NCR is interpreted as magma accumulation, while its subsidence could either be the result of fluids migration outside the caldera or the gravitational adjustment of the source from a spherical to a sill-like geometry.

  19. Unravelling the collapse mechanisms at a Jurassic caldera of the Chon Aike silicic LIP in Southern Patagonia (47° 15 'S, 71° 40'W), Argentina

    Science.gov (United States)

    Sruoga, P.; Japas, S.; Salani, F.; Kleiman, L.; Graffigna, M.

    2008-10-01

    La Peligrosa Caldera is located at Sierra Colorada (47° 15'S, 71° 40' W) in the Chon-Aike silicic LIP. It represents an unique window to understand the eruptive mechanisms that prevailed throughout the ignimbritic flare-up in Southern Patagonia during middle to late Jurassic times. Key pieces of lithologic and structural evidences are taken into account to reconstruct the volcanic structure.

  20. Gas geochemistry of the Valles caldera region, New Mexico and comparisons with gases at Yellowstone, Long Valley and other geothermal systems

    Science.gov (United States)

    Goff, F.; Janik, C.J.

    2002-01-01

    Noncondensible gases from hot springs, fumaroles, and deep wells within the Valles caldera geothermal system (210-300??C) consist of roughly 98.5 mo1% CO2, 0.5 mol% H2S, and 1 mol% other components. 3He/4He ratios indicate a deep magmatic source (R/Ra up to 6) whereas ??13C-CO2 values (-3 to -5???) do not discriminate between a mantle/magmatic source and a source from subjacent, hydrothermally altered Paleozoic carbonate rocks. Regional gases from sites within a 50-km radius beyond Valles caldera are relatively enriched in CO2 and He, but depleted in H2S compared to Valles gases. Regional gases have R/Ra values ???1.2 due to more interaction with the crust and/or less contribution from the mantle. Carbon sources for regional CO2 are varied. During 1982-1998, repeat analyses of gases from intracaldera sites at Sulphur Springs showed relatively constant CH4, H2, and H2S contents. The only exception was gas from Footbath Spring (1987-1993), which experienced increases in these three components during drilling and testing of scientific wells VC-2a and VC-2b. Present-day Valles gases contain substantially less N2 than fluid inclusion gases trapped in deep, early-stage, post-caldera vein minerals. This suggests that the long-lived Valles hydrothermal system (ca. 1 Myr) has depleted subsurface Paleozoic sedimentary rocks of nitrogen. When compared with gases from many other geothermal systems, Valles caldera gases are relatively enriched in He but depleted in CH4, N2 and Ar. In this respect, Valles gases resemble end-member hydrothermal and magmatic gases discharged at hot spots (Galapagos, Kilauea, and Yellowstone). Published by Elsevier Science B.V.

  1. Estudio de eliminación de arsénico con resinas de intercambio iónico en agua potable de Zimapán, Estado de Hidalgo, México

    Directory of Open Access Journals (Sweden)

    Pérez-Moreno, F.

    2006-10-01

    Full Text Available Anionic exchange resins were research with respect its capacity for removal arsenic content in water. Water of well V from Zimapán Hidalgo Mexico was used to make this research, because this water have a mean concentration of 480 ± 11 μg·L-1 of arsenic and it is
    available as drinking water. The exchange resins employed were two strong anionic, one macroreticular (IRA-900 and other gel type (IRA-400, as soon as one third anionic weak macroreticular type (IRA-96. The experiments carried with this resins showing that IRA-900 has highest efficient in the process of arsenic removal from drinking water, because, it showed a treatment capacity of 700 Vagua·Vres-1; while that capacities of IRA-400 e IRA-96 resins were 320 and 52 Vagua·Vres-1 respectively. The mean concentration of arsenic residue in the treatise water was 24 μg·l-1 and it is within the maximum level permissible by Mexican official norm for drinking water.

    Se investigaron resinas de intercambio aniónico con respecto a su capacidad para la eliminación de arsénico contenido en agua. Se utilizó agua del pozo V de Zimapán, Hidalgo, México, cuya concentración promedio es de 480 ± 11 μg·l-1 de arsénico y es utilizada para consumo humano. Se emplearon dos reinas aniónicas fuertes; una, de tipo macro reticular (IRA-900 y la otra de tipo gel (IRA-400, así como una tercera, aniónica débil, de tipo macro reticular (IRA-96. Los experimentos realizados con estas resinas muestran que la IRA-900 es la que mostró la más alta eficiencia en la eliminación de arsénico del agua potable, debido a que presentó una capacidad de tratamiento de 700 Vagua·Vres-1, mientras que las capacidades de las resinas IRA-400 e IRA-96 fueron de 320 y 52 Vagua·Vres-1, respectivamente. La concentración promedio de ars

  2. Domes, Ash and Dust - Controls on soil genesis in a montane catchment of the Valles Caldera, New Mexico

    Science.gov (United States)

    Rasmussen, C.; Meding, S. M.; Vazquez, A.; Chorover, J.

    2012-12-01

    Soil genesis in volcanic terrain may be controlled by complex assemblages of parent materials and local topography. The objective of this work was to quantify topographic and parent material controls on soil and catchment evolution in a mixed conifer, montane catchment in the Valles Caldera, New Mexico, as part of the Jemez River Basin Critical Zone Observatory. The field site is a 16 ha catchment at an elevation of 3,000 m, with a frigid soil temperature regime (0-8 *C), ustic soil moisture regime with bimodal precipitation of winter snowfall and convective summer rainfall (880 mm yr-1), and an overstory dominated by spruce and fir with dense grass cover in open areas. The catchment is located on the resurgent Redondo Dome that uplifted shortly after the last major eruption of the Valles Caldera 1.2 My ago. The dome includes a complex assemblage of pre-eruptive caldera materials and extant sedimentary rocks embedded within a welded, hydrothermally altered rhyolitic tuff. We sampled a transect of seven soil profiles spanning the dominant east-west aspect of the catchment across a catena with profiles located in summit, backslope, footslope, and toeslope positions. Soil morphology was described in the field and soil samples analyzed using a range of geochemical and mineralogical techniques including quantitative and qualitative x-ray diffraction of bulk samples and particle size fractions, elemental analysis by x-ray fluorescence, and laser particle size analysis. The data indicated strong landscape position control on soil drainage, grading from well-drained summits to poorly-drained toeslope positions based on the presence/absence of redoximorphic features. The drainage patterns were coupled with downslope thickening of dark, organic matter rich surface horizons, likely a function of both in situ organic matter production and downslope colluvial transport of carbon rich surface materials. Mineralogical and geochemical data indicated clear within profile lithologic

  3. Hydrothermal fluid flow models of Campi Flegrei caldera, Italy constrained by InSAR surface deformation time series observations

    Science.gov (United States)

    Lundgren, P.; Lanari, R.; Manzo, M.; Sansosti, E.; Tizzani, P.; Hutnak, M.; Hurwitz, S.

    2008-12-01

    Campi Flegrei caldera, Italy, located along the Bay of Naples, has a long history of significant vertical deformation, with the most recent large uplift (>1.5m) occurring in 1983-1984. Each episode of uplift has been followed by a period of subsidence that decreases in rate with time and may be punctuated by brief episodes of lesser uplift. The large amplitude of the major uplifts that occur without volcanic activity, and the subsequent subsidence has been argued as evidence for hydrothermal amplification of any magmatic source. The later subsidence and its temporal decay have been argued as due to diffusion of the pressurized caldera fill material into the less porous surrounding country rock. We present satellite synthetic aperture radar (SAR) interferometry (InSAR) time series analysis of ERS and Envisat data from the European Space Agency, based on exploiting the Small Baseline Subset (SBAS) approach [Berardino et al., 2002]; this allows us to generate maps of relative surface deformation though time, beginning in 1992 through 2007, that are relevant to both ascending and descending satellite orbits. The general temporal behavior is one of subsidence punctuated by several lesser uplift episodes. The spatial pattern of deformation can be modeled through simple inflation/deflation sources in an elastic halfspace. Given the evidence to suggest that fluids may play a significant role in the temporal deformation of Campi Flegrei, rather than a purely magmatic or magma chamber-based interpretation, we model the temporal and spatial evolution of surface deformation as a hydrothermal fluid flow process. We use the TOUGH2-BIOT2 set of numerical codes [Preuss et al., 1999; Hsieh, 1996], which couple multi-phase (liquid-gas) and multi-component (H2O-CO2) fluid flow in a porous or fractured media with plane strain deformation and fluid flow in a linearly elastic porous medium. We explore parameters related to the depth and temporal history of fluid injection, fluid

  4. Cosecha de café con aire utilizando aspiración.

    Directory of Open Access Journals (Sweden)

    Campillo O. Pablo Ignacio

    2000-12-01

    Full Text Available Las ventosas son utilizadas para sujetar y para transportar productos industriales, avícolas y agrícolas. Por su diseño, por los materiales utilizados en su fabricación y por la amplia gama de tamaños, las ventosas se adaptan a diferentes formas y rugosidades superficiales. Estos dispositivos pueden ser empleados para desprender frutos maduros en cosechadores operados por el hombre o en equipos robotizados. En este estudio se evaluaron cuatro tipos de ventosas en la sujeción y el desprendimiento de frutos maduros de café (Coffea arabica var. Colombia: de Fuelle 1, Fuelle 2, Multifuelle y Profunda. Se midieron las siguientes variables: área de contacto de la ventosa, proporción de agarre (proporción de frutos agarrados en una rama, proporción de desprendimiento (proporción de frutos maduros desprendidos en una rama, fuerza media de desprendimiento (N y presión media de vacío (kPa. Los resultados obtenidos, indicaron que la proporción de agarre fue del 100 % y la proporción de desprendimiento fue superior al 86 % para todas las ventosas estudiadas. La presión media de vacío varió entre valores de –57 kPa y –45 kPa para todas las ventosas. La fuerza media de desprendimiento varió para cada ángulo y cada ventosa, encontrándose valores entre 3,0 y 10 N. El desprendimiento del fruto de café, utilizando un sistema neumático de vacío con ventosas, depende del tipo de ventosa utilizada, siendo independiente del ángulo en el que actúa. La ventosa más adecuada, según los resultados obtenidos, para agarrar y desprender frutos maduros de café, fue la de tipo Multifuelle.

  5. Sustainability assessment of geothermal exploitation by numerical modelling: the example of high temperature Mofete geothermal field at Campi Flegrei caldera (Southern Italy)

    Science.gov (United States)

    Carlino, Stefano; Troiano, Antonio; Giulia Di Giuseppe, Maria; Tramelli, Anna; Troise, Claudia; Somma, Renato; De Natale, Giuseppe

    2015-04-01

    The active volcanic area of Campi Flegrei caldera has been the site of many geothermal investigations, since the early XX century. This caldera is characterised by high heat flow, with maximum value > 150 mWm-2, geothermal gradients larger than 200°Ckm-1 and diffuse magmatic gases discharge at the surface. These features encouraged an extensive campaign for geothermal investigation, started in 1939, with many drillings performed at Campanian volcanoes (Campi Flegrei and Ischia) and later at Vesuvius. Several wells aimed to the exploitation of high enthalpy geothermal energy, were drilled in the Campi Flegrei caldera, down to a maximum depth of ~3 km involving mainly two sites (Mofete and S.Vito geothermal fields) located in western and northern sector of caldera respectively. The most interesting site for geothermal exploitation was the Mofete zone, where a number of 4 productive wells were drilled and tested to produce electrical power. Based on data inferred from the productive tests it was established a potential electrical extractable power from Mofete field of at least 10MWe. More recently an empirical evaluation of the whole geothermal potential of the caldera provides a value of more than 1 GWe. The results of AGIP-ENEL exploration at Campi Flegrei highlighted the feasibility of geothermal exploitation. Here, we show for the first time the results of numerical simulations (TOUGH2 code ®) of fluids extraction and reinjection from the Mofete geothermal field, in order to produce at least 5MWe from zero emission power plant (Organic Rankine Cycle type). The simulation is aimed to understand the perturbation of the geothermal reservoir in terms of temperature, pressure change, and possible related seismicity, after different simulated time of exploitation. The modeling is mainly constrained by the data derived from geothermal exploration and productive tests performed since 1979 by AGIP-ENEL Companies. A general assessment of the maximum potential magnitude

  6. Fault Networks in the Northwestern Albuquerque Basin and Their Potential Role in Controlling Mantle CO2 Degassing and Fluid Migration from the Valles Caldera

    Science.gov (United States)

    Smith, J. R.; Crossey, L. J.; Karlstrom, K. E.; Fischer, T. P.; Lee, H.; McGibbon, C. J.

    2015-12-01

    The Rio Grande rift (RGR) has Quaternary and active volcanism and faulting that provide a field laboratory for examining links between mantle degassing and faults as fluid conduits. Diffuse and spring CO2 flux measurements were taken at 6 sites in the northwestern Albuquerque Basin (NWAB) and Valles caldera geothermal system. All sites progress to the southwest from the 1.25 Ma Valles caldera, down the rift-related Jemez fault network, to intersect with the Nacimiento fault system. Mantle CO2 and He degassing are well documented at 5 of 6 sites, with decreasing 3He/4He ratios away from the caldera. The instrument used to measure CO2 flux was an EGM-4 CO2 gas analyzer (PP systems) with an accumulation chamber. Carbonic springs at Penasco Springs (PS) and San Ysidro (SY), and the carbonate-cemented Sand Hill Fault (SHF) were targeted, all near the western border of the RGR. The SHF has no spring activity, had the smallest maximum flux of all the sites (8 g/m2d), but carbonate along the fault zone (network. The maximum diffuse flux recorded at SY (297 g/m2d) and PS (25 g/m2d) are high, especially along the fault and near springs. At SY and PS the instruments capacity was exceeded (2,400 g/m2d) at 6 of 9 springs. Interpretations indicate a direct CO2 flux through a fault-related artesian aquifer system that is connected to magmatic gases from the caldera. Maximum diffuse flux measurements of Alamo Canyon (20,906 g/m2d), Sulphur Springs (2,400 g/m2d) and Soda Dam (1,882 g/m2d) at Valles caldera geothermal sites are comparable to Yellowstone geothermal systems. We use geospatial analysis and local geologic mapping to examine relationships of CO2 flux to structure. Travertine mounds can create impermeable barriers that modify near-surface degassing patterns, making it difficult to decipher where CO2 and fluids preferentially migrate up the damage zones in the hanging-wall or footwall. Future work will utilize grids to more accurately assess the localized affect fault

  7. Fluid geochemistry and soil gas fluxes (CO2-CH4-H2S) at a promissory Hot Dry Rock Geothermal System: The Acoculco caldera, Mexico

    Science.gov (United States)

    Peiffer, L.; Bernard-Romero, R.; Mazot, A.; Taran, Y. A.; Guevara, M.; Santoyo, E.

    2014-09-01

    The Acoculco caldera has been recognized by the Mexican Federal Electricity Company (CFE) as a Hot Dry Rock Geothermal System (HDR) and could be a potential candidate for developing an Enhanced Geothermal System (EGS). Apart from hydrothermally altered rocks, geothermal manifestations within the Acoculco caldera are scarce. Close to ambient temperature bubbling springs and soil degassing are reported inside the caldera while a few springs discharge warm water on the periphery of the caldera. In this study, we infer the origin of fluids and we characterize for the first time the soil degassing dynamic. Chemical and isotopic (δ18O-δD) analyses of spring waters indicate a meteoric origin and the dissolution of CO2 and H2S gases, while gas chemical and isotopic compositions (N2/He, 3He/4He, 13C, 15N) reveal a magmatic contribution with both MORB- and arc-type signatures which could be explained by an extension regime created by local and regional fault systems. Gas geothermometry results are in agreement with temperature measured during well drilling (260 °C-300 °C). Absence of well-developed water reservoir at depth impedes re-equilibration of gases upon surface. A multi-gas flux survey including CO2, CH4 and H2S measurements was performed within the caldera. Using the graphical statistical analysis (GSA) approach, CO2 flux measurements were classified in two populations. Population A, representing 95% of measured fluxes is characterized by low values (mean: 18 g m- 2 day- 1) while the remaining 5% fluxes belonging to Population B are much higher (mean: 5543 g m- 2 day- 1). This low degassing rate probably reflects the low permeability of the system, a consequence of the intense hydrothermal alteration observed in the upper 800 m of volcanic rocks. An attempt to interpret the origin and transport mechanism of these fluxes is proposed by means of flux ratios as well as by numerical modeling. Measurements with CO2/CH4 and CO2/H2S flux ratios similar to mass ratios

  8. Acerca de la propuesta "Caldera de Ñireco" en el centro-oeste de los Andes Neuquinos (38º50'S - 70º50'O

    Directory of Open Access Journals (Sweden)

    Emilio F González Díaz

    2010-10-01

    Full Text Available En el tramo austral del alto estructural de Copahue-Pino Hachado, a la latitud de la cuenca lacustre Moquehue-Aluminé y cercanías del límite argentino-chileno, ha sido distinguido un conjunto anómalo de nueve calderas resultantes de la actividad volcánica del Plioceno-Cuaternario. La "caldera de Ñireco", parte integrante de este conjunto, es motivo del presente trabajo. Los autores objetan el reconocimiento de tal componente morfoestructural a partir de un análisis geomorfológico, estructural y estratigráfico del área. A partir de ello, se reconoce una correspondencia entre los propuestos límites de dicha caldera, y la situación de los principales valles resultantes del proceso erosivo fluvial, cuyo desarrollo estuvo controlado por fallas inversas y lineamientos regionales. No existen evidencias que faciliten el reconocimiento de un aparato volcánico que teóricamente albergue la sugerida depresión caldérica, o remanentes de sus flancos externos e internos. En el sector central de la propuesta "caldera de Ñireco" se dan las mayores alturas topográficas de la región (± 2.900 m s.n.m., valores que superan ampliamente a los de la Cordillera Principal a estas latitudes. La estratigrafía local de la propuesta área de la caldera está compuesta esencialmente por las rocas más antiguas de la zona (granitoides del Paleozoico superior y secuencias volcánicas y volcaniclásticas del Triásico y no guarda coincidencia temporal alguna con la actividad volcánica del Plioceno-Cuaternario, la que se halla bien representada inmediatamente al norte y sur del sector analizado. La zona de estudio se enmarca por el contrario dentro de una faja plegada y corrida de piel gruesa y vergencia occidental, en donde la inversión tectónica jugó un rol central.

  9. Contenido de ADN y nivel de ploidía en Tagetes spp. Utilizando citómetro de flujo

    OpenAIRE

    Miguel Ángel Serrato Cruz; Martha Hernández Rodríguez; Yves Savidan; Nina M. Bárcenas Ortega

    2000-01-01

    Se determinó la asociación entre el contenido de ADN nuclear y el nivel de ploidía de siete poblaciones de Tagetes spp. El contenido de ADN se estimó mediante citómetro de flujo utilizando a Zea mays L. como estándar interno. El recuento de cromosomas se hizo en preparaciones citológicas teñidas con acetocarmín. T. erecta, T. foetidissima, T. tenuifolia (dos ecotipos) y dos poblaciones silvestres no identificadas mostraron un contenido promedio de ADN de 2.61±0.23 pg correspondiendo a la ploi...

  10. UTILIZANDO NANOTUBOS DE TiO2 COMO FOTOCATALISADOR NA DEGRADAÇÃO DO CORANTE VERMELHO CONGO

    OpenAIRE

    Nilmalice Coelho Rocha; Leonardo Lopes da Costa

    2011-01-01

    Nanotubos de TiO2 foram sintetizados em um sistema hidrotérmico. Os nanomateriais foram caracterizados por microscopia eletrônica de varredura (MEV) e área superficial. O TiO2 anatase e os nanotubos de TiO2 foram utilizados no processo de fotodegradação do corante vermelho congo. A capacidade de fotodegradação de ambos catalisadores foram comparadas. O corante foi degradado por 90 minutos, utilizando ambos catalisadores, estes apresentaram alta atividade catalítica próximo ao pH 2. A capacid...

  11. Estimativa do teor de água no solo utilizando dados de radar de abertura sintética

    OpenAIRE

    O. A. Máximo; A.M. Saad; H. H. Kux

    1999-01-01

    Em virtude da crescente demanda mundial por alimentos, um monitoramento eficaz e em larga escala da umidade do solo constitui fator de grande importância para a previsão de safras. Este trabalho teve por objetivo apresentar uma técnica para o cálculo do teor de água no solo, utilizando modelos preditivos de umidade do solo, baseados em dados de radar de abertura sintética (SAR). Foram utilizados dados do SAR a bordo do JERS-1 ("Japanese Earth Resources Satellite") e dois modelos empíricos. O ...

  12. Evaluación de agua recreacional utilizando una bacteria compartida entre el hombre y los animales, Escherichia coli

    OpenAIRE

    Noseda, Ramón P.

    2007-01-01

    El Arroyo Azul posee las características típicas de un arroyo de llanura, su transcurrir urbano es utilizado por la población para su recreación. Durante el periodo 1993-2007 fue evaluada su calidad bacteriológica, utilizando la bacteria Escherichia coli fecal como indicador de contaminación, su origen entérico es compartido tanto por humanos como para animales. El objetivo fue determinar la calidad bacteriológica de dicha agua y relacionarla con distintas enfermedades de origen entérico que ...

  13. Classificação de estratos florestais utilizando redes neurais artificiais e dados de sensoriamento remoto

    OpenAIRE

    Wanderson Gonçalves e Gonçalves; Hebe Morganne Campos Ribeiro; José Alberto Silva de Sá; Gundisalvo Piratoba Morales; Hélio Raymundo Ferreira Filho; Arthur da Costa Almeida

    2016-01-01

    O presente estudo objetivou a classificação de tipologias florestais por meio de redes neurais artificiais utilizando dados provenientes de um inventário florestal, fornecido pelo Instituto de Desenvolvimento Florestal e da Biodiversidade do Estado do Pará (IDEFLOR-BIO), e das bandas 3, 4 e 5 do TM do satélite Landsat 5. As informações provenientes das imagens de satélite foram extraídas por meio do aplicativo QGIS 2.8.1 Wien e utilizadas no banco de dados para o treinamento das redes neurais...

  14. Predicción de ingresos de causas penales utilizando programación genética lineal

    OpenAIRE

    Garcete Rodríguez, Alberto David; Barán, Benjamín

    2015-01-01

    Este trabajo propone una metodología de predicción de ingresos de causas penales utilizando Programación Genética Lineal (Linear Genetic Programming - LGP). El estudio se realizó en base a datos mensuales recogidos durante siete años (2007 a 2013), en los siete Juzgados Penales de Garantías de Ciudad del Este - Paraguay. La verificación del método propuesto se hizo mediante la comparación del método LGP implementado con modelos estadísticos conocidos como la regresión lineal, promedio móvil, ...

  15. Task 3: Evaluation of mineral resource potential, caldera geology, and volcano-tectonic framework at and near Yucca Mountain

    Energy Technology Data Exchange (ETDEWEB)

    Weiss, S.I.; Noble, D.C.; Larson, L.T. [Univ. of Nevada, Reno, NV (United States)

    1994-12-31

    This report summarizes the work of Task 3 that was initially discussed in our monthly reports for the period October 1, 1993 through September 30, 1994, and is contained in our various papers and abstracts, both published and in press or currently in review. Our efforts during this period have involved the continuation of studies begun prior to October, 1993, focussed mainly on aspects of the caldera geology, magmatic activity, hydrothermal mineralization and extensional tectonics of the western and central parts of the southwestern Nevada volcanic field (SWNVF), studies of the subsurface rocks of Yucca Mountain utilizing drill-hole sampled obtained in 1991 and 1992, and studies of veins and siliceous ledges cropping out in northwestern Yucca Mountain. These veins and ledges provide evidence for near-surface hydrothermal activity in northwestern Yucca Mountain during the Crater Flat Tuff period of volcanism. During the period of this report we have concentrated our efforts on the production and publication of documents summarizing many of the data, interpretations and conclusions of Task 3 studies pertaining to hydrothermal activity and mineralization in the Yucca Mountain region and their relations to volcanism and tectonic activity. The resulting two manuscripts for journal publication and a compilation of radiometric age and trace-element geochemical data are appended to this report.

  16. Aquifer Recharge Estimation through Atmospheric Chloride Mass Balance at Las Cañadas Caldera, Tenerife, Canary Islands, Spain

    Directory of Open Access Journals (Sweden)

    Rayco Marrero-Diaz

    2015-05-01

    Full Text Available The atmospheric chloride mass balance (CMB method was used to estimate net aquifer recharge in Las Cañadas Caldera, an endorheic summit aquifer area about 2000 m a.s.l. with negligible surface runoff, which hosts the largest freshwater reserve in Tenerife Island, Canary Islands, Spain. The wet hydrological year 2005–2006 was selected to compare yearly atmospheric chloride bulk deposition and average chloride content in recharge water just above the water table, both deduced from periodical sampling. The potential contribution of chloride to groundwater from endogenous HCl gas may invalidate the CMB method. The chloride-to-bromide molar ratio was an efficient tracer used to select recharge water samples having atmospheric origin of chloride. Yearly net aquifer recharge was 631 mm year−1, i.e., 69% of yearly precipitation. This result is in agreement with potential aquifer recharge estimated through an independent lumped-parameter rainfall-runoff model operated by the Insular Water Council of Tenerife. This paper illustrates basic procedures and routines to use the CMB method for aquifer recharge in active volcanic oceanic islands having sparse-data coverage and groundwater receiving contribution of endogenous halides.

  17. Geochemical Features of the Hubin Spring Gases from the Northern Caldera Lake of the Tianchi Volcano, Changbai Mountains

    Institute of Scientific and Technical Information of China (English)

    Gao Ling; Shangguan Zhiguan; Wei Haiquan; Zhao Ciping

    2011-01-01

    This paper deals with geochemical features of gas emitted from the Hubin Springs. The Hubin Springs zone, a strong thermal emission zone, is are locatedd at the north edge of the Tianchi caldera lake. Very young deposits with uncertain eruption date are found on the top area of the Tianwenfeng, which might have been formed in one of the recent eruptions or the Millennium Eruption. It is of significance to study the geochemistry features of the emitting gas from the Hubin Springs to understand the activities of the Tianchi Volcano. This paper systematically sampled and analyzed the gases emitted from the Hubin Springs and discussed their geochemistry features. The results show that there is a high content of deep derived gases, such as CO2, He, CH4 and Ar in Hubin Springs zone. The isotopic ratio of He lies between 4. 18 and 5. 95 Ra. The averaged mantle derived gas content calculated from the ^4He/2^20Ne ratio and He content reaches 67.1%. All these show that the Hubin Springs are located on a special belt of deep gases released in high intensity and large scale. The spatial distribution of Helium isotope is characterized by concavity, showing that this special area may be related to the volcanic edifice. It is highly possible that the released gases represent the residual gas samples of the latest eruptions from the Tianchi Volcano. However more detailed studies are demanded.

  18. Near real-time monitoring of volcanic surface deformation from GPS measurements at Long Valley Caldera, California

    Science.gov (United States)

    Ji, Kang Hyeun; Herring, Thomas A.; Llenos, Andrea L.

    2013-01-01

    Long Valley Caldera in eastern California is an active volcanic area and has shown continued unrest in the last three decades. We have monitored surface deformation from Global Positioning System (GPS) data by using a projection method that we call Targeted Projection Operator (TPO). TPO projects residual time series with secular rates and periodic terms removed onto a predefined spatial pattern. We used the 2009–2010 slow deflation as a target spatial pattern. The resulting TPO time series shows a detailed deformation history including the 2007–2009 inflation, the 2009–2010 deflation, and a recent inflation that started in late-2011 and is continuing at the present time (November 2012). The recent inflation event is about four times faster than the previous 2007–2009 event. A Mogi source of the recent event is located beneath the resurgent dome at about 6.6 km depth at a rate of 0.009 km3/yr volume change. TPO is simple and fast and can provide a near real-time continuous monitoring tool without directly looking at all the data from many GPS sites in this potentially eruptive volcanic system.

  19. Radiogenic Heat Production in the Gölcük Caldera and Direkli, Isparta Angle (Southwest Anatolia)

    Science.gov (United States)

    Ayten Uyanık, Nurten; Öncü, Ziya; Akkurt, İskender

    2016-04-01

    The radiogenic heat is one of the important parameter due to the radioactivity has existed since beginning of universe as prediction of Big-Bang theory. In this study the radiogenic heat production of the Gölcük caldera and Direkli fields of the Isparta-Turkey, has been investigated. Total of 1390 data were obtained in the study area. The study area is included of the Gölcük volcanism and its around that is located in Isparta province of Turkey's Mediterranean region. The Gölcük volcanism is a young volcanism. Around this volcanism the andesite, trachy andesite, tuff, pumice and such a geological units is available. The data were collected using in-situ measurements with gamm-ray spectrometer. These measurements were covered natural radioactive elements (Uranium U, Thorium Th and Potassium K). Radiogenic heat production values were calculated using the literature relationships and in-situ measurement values of these radioactive elements. Radiogenic heat map of study area were obtained using radiogenic heat production values. In the map the red zone areas shows highest heat values while green zones areas of the map presents lowest heat values. Key words: Radioactive elements, radiogenic heat, map, Gölcük-Direkli(Isparta), Turkey

  20. Distribution, population structure, reproduction and diet of Ophiolimna antarctica (Lyman, 1879) from Kemp Caldera in the Southern Ocean

    Science.gov (United States)

    Boschen, Rachel E.; Tyler, Paul A.; Copley, Jonathan T.

    2013-08-01

    A new population of Ophiolimna antarctica (Lyman, 1879) was discovered at 1546 m in Kemp Caldera, a topographic feature with active hydrothermal venting at the southern end of the South Sandwich Islands, Southern Ocean. The distribution, population structure, reproduction, and diet of O. antarctica were investigated. O. antarctica were found predominantly on basalt with an over-dispersed distribution. The mean density was 17 individuals m-2 with a range of 9-24 individuals m-2. There was a bimodal population structure, with separate juvenile and adult peaks. Sexes were separate and the sex ratio was not significantly different from equality. The maximum oocyte diameter was 520 μm, suggesting direct or lecithotrophic development, whilst individual females reproduced asynchronously. Stomach contents included crustacean fragments, flocculate material, diatoms, forams, fish scales, and ophiuroid tissues and spines, which was indicative of omnivory. There was no apparent influence of hydrothermal vents <500 m away on the diet of Ophiolimna antarctica. The ecology of Ophiolimna antarctica is consistent with what is known for other Antarctic and deep-sea ophiuroid species.

  1. Three-dimensional electrical resistivity model of the hydrothermal system in Long Valley Caldera, California, from magnetotellurics

    Science.gov (United States)

    Peacock, Jared R.; Mangan, Margaret T.; McPhee, Darcy K.; Wannamaker, Phil E.

    2016-01-01

    Though shallow flow of hydrothermal fluids in Long Valley Caldera, California, has been well studied, neither the hydrothermal source reservoir nor heat source has been well characterized. Here a grid of magnetotelluric data were collected around the Long Valley volcanic system and modeled in 3-D. The preferred electrical resistivity model suggests that the source reservoir is a narrow east-west elongated body 4 km below the west moat. The heat source could be a zone of 2–5% partial melt 8 km below Deer Mountain. Additionally, a collection of hypersaline fluids, not connected to the shallow hydrothermal system, is found 3 km below the medial graben, which could originate from a zone of 5–10% partial melt 8 km below the south moat. Below Mammoth Mountain is a 3 km thick isolated body containing fluids and gases originating from an 8 km deep zone of 5–10% basaltic partial melt.

  2. Near real-time monitoring of volcanic surface deformation from GPS measurements at Long Valley Caldera, California

    Science.gov (United States)

    Ji, Kang Hyeun; Herring, Thomas A.; Llenos, Andrea L.

    2013-03-01

    Long Valley Caldera in eastern California is an active volcanic area and has shown continued unrest in the last three decades. We have monitored surface deformation from Global Positioning System (GPS) data by using a projection method that we call Targeted Projection Operator (TPO). TPO projects residual time series with secular rates and periodic terms removed onto a predefined spatial pattern. We used the 2009-2010 slow deflation as a target spatial pattern. The resulting TPO time series shows a detailed deformation history including the 2007-2009 inflation, the 2009-2010 deflation, and a recent inflation that started in late-2011 and is continuing at the present time (November 2012). The recent inflation event is about four times faster than the previous 2007-2009 event. A Mogi source of the recent event is located beneath the resurgent dome at about 6.6 km depth at a rate of 0.009 km3/yr volume change. TPO is simple and fast and can provide a near real-time continuous monitoring tool without directly looking at all the data from many GPS sites in this potentially eruptive volcanic system.

  3. La gestión auténtica como moderadora de la relación entre (1) la congruencia de la identidad del rol de género –características de género de la gestión– y (2) el intercambio líder-subordinado (LMX)

    OpenAIRE

    Aharon Tziner; Liron Barsheshet Picke

    2014-01-01

    Este trabajo analiza el efecto de la congruencia de la identidad del rol de género (andrógina/no andrógina) y las características de género de la gestión (comunitaria/egocéntrica) en la calidad del intercambio líder subordinado (LMX), así como que si la gestión auténtica es una variable que modere dicha relación. El estudio plantea la hipótesis de una relación positiva entre la identidad del rol de género y las características de género de la gestión con la calidad de la LMX. Otra hipótesis h...

  4. Radiopacity of restorative materials using digital images Radiopacidade de materiais restauradores utilizando imagens digitais

    Directory of Open Access Journals (Sweden)

    Leda Maria Pescinini Salzedas

    2006-04-01

    Full Text Available The radiopacity of esthetic restorative materials has been established as an important requirement, improving the radiographic diagnosis. The aim of this study was to evaluate the radiopacity of six restorative materials using a direct digital image system, comparing them to the dental tissues (enamel-dentin, expressed as equivalent thickness of aluminum (millimeters of aluminum. Five specimens of each material were made. Three 2-mm thick longitudinal sections were cut from an intact extracted permanent molar tooth (including enamel and dentin. An aluminum step wedge with 9 steps was used. The samples of different materials were placed on a phosphor plate together with a tooth section, aluminum step wedge and metal code letter, and were exposed using a dental x-ray unit. Five measurements of radiographic density were obtained from each image of each item assessed (restorative material, enamel, dentin, each step of the aluminum step wedge and the mean of these values was calculated. Radiopacity values were subsequently calculated as equivalents of aluminum thickness. Analysis of variance (ANOVA indicated significant differences in radiopacity values among the materials (PA radiopacidade dos materiais tem sido valorizada como importante requisito, incrementando o diagnóstico radiográfico. O objetivo deste estudo foi avaliar, no sistema digital Digora, as densidades radiográficas de 06 materiais restauradores comparando-os aos tecidos dentais (esmalte e dentina, expressos em milímetros de alumínio (mm Al. Foram confeccionadas 05 amostras de cada material e três cortes de um molar extraído hígido (incluindo esmalte e dentina, com 2 mm de espessura, e um penetrômetro de alumínio com 09 degraus. Sobre cada placa óptica foram colocados amostras dos diferentes materiais, um corte do dente humano, o penetrômetro e a identificação, e feita a exposição utilizando um aparelho de raios X. Foram obtidas 05 medidas de densidade radiográfica de

  5. Medial meniscus transplantation using cyanoacrylate in rabbits Transplante de menisco medial utilizando cianoacrilato em coelhos

    Directory of Open Access Journals (Sweden)

    Leandro José Reckers

    2006-04-01

    Full Text Available PURPOSE: To evaluate meniscal transplantation using as fixation method a synthetic glue derived from cyanoacrylate acid. METHODS: Twenty rabbits were used, of which 10 for autologous transplantation and 10 for homologous transplantation. For the autologous transplantation the meniscus was removed, and then transplanted in the same animal, using the synthetic glue. For the homologous transplantation, the study was divided into two stages: 1- Removal of the meniscus which was maintained at a temperature of 73ºC. 2- Use of cyanoacrylate acid-derived surgical adhesive for meniscal retransplantation in a different rabbit 30 days after the transplant. RESULTS: Due to complications, euthanasia had to be anticipated to the 15th day in the homologous group and to the 18th day in the autologous group. Macroscopically, knees submitted to transplantation presented whitish secretions from the surgical incision up to deep planes. Necrosis was observed in both groups. Statistical analysis has shown that mild (p=0.043 and moderate (p=0.001 complications emerged in a significantly earlier way in the homologous group, where euthanasia was also performed earlier (p=0,005. CONCLUSION: Synthetic surgical adhesives derived from cyanoacrylate acid promoted cortical to medullary bone necrosis bone in both groups.OBJETIVO: Avaliar macroscópica e histologicamente o transplante meniscal, utilizando-se a cola sintética derivada do ácido cianoacrilato como método de fixação. MÉTODOS: Foram utilizados 20 coelhos, tendo 10 realizado transplante autólogo e 10, homólogo. Para o transplante autólogo, o menisco foi retirado e em seguida transplantado no mesmo animal, sendo fixado com a cola sintética. Para o transplante homólogo o estudo foi dividido em duas etapas: 1- retirada do menisco e manutenção a uma temperatura de 73°C negativos. 2- Utilização do adesivo cirúrgico derivado do ácido cianoacrilato para reimplantar num coelho diferente 30 dias após o

  6. MODELACIÓN DE LA DISTRIBUCIÓN DE VIAJES EN EL VALLE DE ABURRÁ UTILIZANDO EL MODELO GRAVITATORIO

    Directory of Open Access Journals (Sweden)

    CARLOS GONZÁLEZ

    2009-01-01

    Full Text Available El presente artículo se basa en los últimos estudios de transporte que se realizaron en el ÁreaMetropolitana del Valle de Aburrá: Encuesta Origen/Destino 2005 y Estudio de rutas de buses, Modelación de la Red Vial del Valle de Aburrá, y Plan Maestro de Movilidad. Se realiza el análisis y desarrollo del modelo de distribución de viajes para el Área Metropolitana del Valle de Aburrá utilizando el software TransCAD con los datos del año 2005, utilizando el modelo gravitatorio, el cual determina los viajes que existen entre una y otra zona de acuerdo con la generación y la atracción de viajes que existen entre las zonas relacionadas y una función de impedancia que depende del tiempo de viaje entre zonas. Se analizó el modelo para diferentes períodos y motivos y se encontró que la función de impedancia que mejor se adapta al modelo estudiado es la exponencial negativa.

  7. UTILIZANDO NANOTUBOS DE TiO2 COMO FOTOCATALISADOR NA DEGRADAÇÃO DO CORANTE VERMELHO CONGO

    Directory of Open Access Journals (Sweden)

    Nilmalice Coelho Rocha

    2011-02-01

    Full Text Available Nanotubos de TiO2 foram sintetizados em um sistema hidrotérmico. Os nanomateriais foram caracterizados por microscopia eletrônica de varredura (MEV e área superficial. O TiO2 anatase e os nanotubos de TiO2 foram utilizados no processo de fotodegradação do corante vermelho congo. A capacidade de fotodegradação de ambos catalisadores foram comparadas. O corante foi degradado por 90 minutos, utilizando ambos catalisadores, estes apresentaram alta atividade catalítica próximo ao pH 2. A capacidade de fotodegradação do corante utilizando TiO2 anatase e nanotubos de TiO2 em meio iônico mostrou-se favorável com a adição de NaCl na concentração de 0,03 mol/L.

  8. Distribución y abundancia de larvas de Heterocarpus reedi Bahamonde, 1955, Cervimunida johni Porter, 1903 y Pleuroncodes monodon (H. Milne Edwards, 1837, frente a Coquimbo y Caldera, Chile Distribution and abundance of Heterocarpus reedi Bahamonde, 1955, Cervimunida johni Porter, 1903, and Pleuroncodes monodon (H. Milne Edwards, 1837, larvae off Coquimbo and Caldera, Chile

    Directory of Open Access Journals (Sweden)

    Armando Mujica

    2011-01-01

    Full Text Available Como aporte a la dinámica poblacional de especies que constituyen recursos pesqueros, se analizaron 160 muestras de zooplancton obtenidas con redes Bongo en 40 estaciones oceanógraficas entre Caldera y Coquimbo, en octubre y diciembre de 2005. De ellas se separó la totalidad de las larvas de crustáceos decápodos y se identificaron las de Heterocarpus reedi, Cervimunida johni y Pleuroncodes monodon. Las mayores abundancias de zoeas tempranas de las tres especies se encontraron en octubre en la zona de Coquimbo, mientras que en diciembre predominaron los estados más avanzados de desarrollo. En la zona de Caldera, en ambos meses de muestreo, predominaron los estados avanzados de desarrollo de H. reedi y P. monodon y zoeas tempranas de C. johni. La frecuencia de ocurrencia de las larvas de H reedi en la zona de Coquimbo fue similar en ambos meses, mientras que en la zona de Caldera fue mayor en octubre. La frecuencia de ocurrencia de las larvas de P. monodon y C. johni fue mayor en octubre en ambas zonas. Todas las megalopas capturadas en las dos zonas y meses de muestreo corresponden sólo a un morfotipo, con características morfológicas similares a los juveniles más pequeños de P. monodon. Sobre la base de la distribución y abundancia de larvas de las tres especies, se postula que el desove ocurre antes en la zona de Caldera que en la de Coquimbo, principalmente en zonas próximas a la costa, dada las diferencias de abundancia de los estados de desarrollo.To better understand the population dynamics of fishery resource species, 160 zooplankton samples were obtained with a Bongo net at 40 oceanographic stations around Caldera and Coquimbo in October and December, 2005, and analyzed. All crustacean decapod larvae were sorted, and Heterocarpus reedi, Cervimunida johni, and Pleuroncodes monodon larvae were identified. For all three species, the highest abundances of early zoea were found in October in Coquimbo, whereas advanced larval

  9. The link between volcanism and plutonism in epizonal magma systems; high-precision U–Pb zircon geochronology from the Organ Mountains caldera and batholith, New Mexico

    Science.gov (United States)

    Rioux, Matthew; Farmer, Lang; Bowring, Samuel; Wooton, Kathleen M.; Amato, Jeffrey M.; Coleman, Drew S.; Verplanck, Philip L.

    2016-01-01

    The Organ Mountains caldera and batholith expose the volcanic and epizonal plutonic record of an Eocene caldera complex. The caldera and batholith are well exposed, and extensive previous mapping and geochemical analyses have suggested a clear link between the volcanic and plutonic sections, making this an ideal location to study magmatic processes associated with caldera volcanism. Here we present high-precision thermal ionization mass spectrometry U–Pb zircon dates from throughout the caldera and batholith, and use these dates to test and improve existing petrogenetic models. The new dates indicate that Eocene volcanic and plutonic rocks in the Organ Mountains formed from ~44 to 34 Ma. The three largest caldera-related tuff units yielded weighted mean 206Pb/238U dates of 36.441 ± 0.020 Ma (Cueva Tuff), 36.259 ± 0.016 Ma (Achenback Park tuff), and 36.215 ± 0.016 Ma (Squaw Mountain tuff). An alkali feldspar granite, which is chemically similar to the erupted tuffs, yielded a synchronous weighted mean 206Pb/238U date of 36.259 ± 0.021 Ma. Weighted mean 206Pb/238U dates from the larger volume syenitic phase of the underlying Organ Needle pluton range from 36.130 ± 0.031 to 36.071 ± 0.012 Ma, and the youngest sample is 144 ± 20 to 188 ± 20 ka younger than the Squaw Mountain and Achenback Park tuffs, respectively. Younger plutonism in the batholith continued through at least 34.051 ± 0.029 Ma. We propose that the Achenback Park tuff, Squaw Mountain tuff, alkali feldspar granite and Organ Needle pluton formed from a single, long-lived magma chamber/mush zone. Early silicic magmas generated by partial melting of the lower crust rose to form an epizonal magma chamber. Underplating of the resulting mush zone led to partial melting and generation of a high-silica alkali feldspar granite cap, which erupted to form the tuffs. The deeper parts of the chamber underwent continued recharge and crystallization for 144 ± 20 ka after the

  10. Modelación de la distribución de viajes en el valle de aburrá utilizando el modelo gravitatorio

    OpenAIRE

    CARLOS GONZÁLEZ; IVÁN SARMIENTO

    2009-01-01

    El presente artículo se basa en los últimos estudios de transporte que se realizaron en el ÁreaMetropolitana del Valle de Aburrá: Encuesta Origen/Destino 2005 y Estudio de rutas de buses, Modelación de la Red Vial del Valle de Aburrá, y Plan Maestro de Movilidad. Se realiza el análisis y desarrollo del modelo de distribución de viajes para el Área Metropolitana del Valle de Aburrá utilizando el software TransCAD con los datos del año 2005, utilizando el modelo gravitatorio, el cual determina ...

  11. Cultivation and complete genome sequencing of Gloeobacter kilaueensis sp. nov., from a lava cave in Kilauea Caldera, Hawai'i.

    Directory of Open Access Journals (Sweden)

    Jimmy H W Saw

    Full Text Available The ancestor of Gloeobacter violaceus PCC 7421(T is believed to have diverged from that of all known cyanobacteria before the evolution of thylakoid membranes and plant plastids. The long and largely independent evolutionary history of G. violaceus presents an organism retaining ancestral features of early oxygenic photoautotrophs, and in whom cyanobacteria evolution can be investigated. No other Gloeobacter species has been described since the genus was established in 1974 (Rippka et al., Arch Microbiol 100:435. Gloeobacter affiliated ribosomal gene sequences have been reported in environmental DNA libraries, but only the type strain's genome has been sequenced. However, we report here the cultivation of a new Gloeobacter species, G. kilaueensis JS1(T, from an epilithic biofilm in a lava cave in Kīlauea Caldera, Hawai'i. The strain's genome was sequenced from an enriched culture resembling a low-complexity metagenomic sample, using 9 kb paired-end 454 pyrosequences and 400 bp paired-end Illumina reads. The JS1(T and G. violaceus PCC 7421(T genomes have little gene synteny despite sharing 2842 orthologous genes; comparing the genomes shows they do not belong to the same species. Our results support establishing a new species to accommodate JS1(T, for which we propose the name Gloeobacter kilaueensis sp. nov. Strain JS1(T has been deposited in the American Type Culture Collection (BAA-2537, the Scottish Marine Institute's Culture Collection of Algae and Protozoa (CCAP 1431/1, and the Belgian Coordinated Collections of Microorganisms (ULC0316. The G. kilaueensis holotype has been deposited in the Algal Collection of the US National Herbarium (US# 217948. The JS1(T genome sequence has been deposited in GenBank under accession number CP003587. The G+C content of the genome is 60.54 mol%. The complete genome sequence of G. kilaueensis JS1(T may further understanding of cyanobacteria evolution, and the shift from anoxygenic to oxygenic photosynthesis.

  12. The predominance of post-wildfire erosion in the long-term denudation of the Valles Caldera, New Mexico

    Science.gov (United States)

    Orem, Caitlin A.; Pelletier, Jon D.

    2016-05-01

    Wildfires can dramatically increase erosion rates over time scales on the order of several years, yet few data firmly constrain the relative importance of post-wildfire erosion in the long-term denudation of landscapes. We tested the hypothesis that wildfire-affected erosion is responsible for a large majority of long-term denudation in the uplands of the Valles Caldera, New Mexico, by quantifying erosion rates in wildfire-affected and non-wildfire-affected watersheds over short (~100-101 years) time scales using suspended sediment loads, multitemporal terrestrial laser scanning, and airborne laser scanning and over long (~103-106 years) time scales using 10Be inventories and incision into a dated paleosurface. We found that following the Las Conchas fire in 2011, mean watershed-averaged erosion rates were more than 1000 µm yr-1, i.e., ~103-105 times higher than nearby unburned watersheds of similar area, relief, and lithology. Long-term denudation rates are on the order of 10-100 µm yr-1. Combining data for wildfire-affected and non-wildfire-affected erosion rates into a long-term denudation rate budget, we found that wildfire-affected erosion is responsible for at least 90% of denudation over geologic time scales in our study area despite the fact that such conditions occur only at a small fraction of the time. Monte Carlo analyses demonstrate that this conclusion is robust with respect to uncertainties in the rates and time scales used in the calculations.

  13. A coupled hydrothermal and mechanical model for estimating thermo-poroelastic deformation, gravity and magnetic changes in calderas

    Science.gov (United States)

    Coco, A.; Gottsmann, J.; Whitaker, F.; Rust, A.; Currenti, G. M.; Jasim, A.

    2014-12-01

    Increasing integration of satellite and ground-based geophysical observations in volcanic areas has dramatically enhanced our ability to detect and track complex processes that can be difficult to reconcile with models of elastic mechanical behavior of upper crust. This study uses a thermo-poroelastic model to evaluate ground deformation, magnetic and gravity changes caused by hydrothermal fluid circulation and pressurization of magma chambers, in which surface topography, crustal heterogeneities and the presence of faults are taken into account. We develop a numerical framework for more realistic assessment of geophysical observations associated with volcanic processes, with particular focus on calderas. The numerical model is fully coupled with TOUGH2, a commercial software simulating multi-phase and multi-component fluid flow and heat transfer. The two-way coupling is performed through: (i) the concept of effective stress, which is controlled by pore pressure and thermal expansion, and (ii) empirical expressions for porosity, permeability, and capillary pressure, which are dependent on the effective stress. The model is applied to Campi Flegrei to simulate a generic unrest period caused by a deep injection of hot water and CO2. Vertical uplift reaches 12 cm in 3 years, with associated thermomagnetic variations of c. 14 nT and gravity changes of c. 210 μGal, comparable to those observed during the 1982-84 bradyseism. Gravity and magnetic signals continuously increase for 2 years and approach steady state after 2.5 years. The contribution of thermal effects to total ground deformation is almost negligible in the first 3 years, but reaches half of the total after 15 years, and is dominant after 35 years. We also simulated the presence of faults and the contribution of a deeper magma chamber pressurization, which affect considerably the sub-surface circulation, and consequently the geophysical changes at the surface.

  14. Simulación de una célula robotizada para la fabricación de piezas mecanizadas en un entorno industrial, utilizando RobotStudio

    OpenAIRE

    Muinelo Garrido, Gonzalo

    2015-01-01

    El trabajo consiste en la realización de la simulación de una célula robotizada, que servirá para el tratamiento de una pieza de aluminio mediante tres máquinas que estarán abastecidas por un robot central; este último será el encargado de gestionar la entrada y salida de piezas en las máquinas, y de realizar el intercambio de piezas entre máquinas, así como el gestionar la entrada y salida de piezas de la célula robotizada. La simulación se llevará a cabo con el programa RobotStudio, prop...

  15. UM ESTUDO DE IMPACTO AMBIENTAL UTILIZANDO ANÁLISES ESTATÍSTICAS ESPACIAL E MULTIVARIADA

    Directory of Open Access Journals (Sweden)

    Paulo Milton Barbosa Landim

    2001-01-01

    âncias e apenas nas entradas dos efluentes, junto aos corpos receptores, não considerando a pluma do efluente, tornando-se necessário o monitoramento desseimpacto em termos de distribuição espacial. O objetivo deste estudo foi verificar o impacto da emissão de um efluente no Rio Paraíba do Sul, nas cercanias de Pindamonhangaba (SP, utilizando a análise desuperfícies de tendência, por regressão polinomial, alem da análise estatística multivariada das componentes principais. As variáveis enfocadas foram: riqueza de gêneros do plâncton, pH, temperatura, oxigênio dissolvido, transparência da água, cor e a turbidez da água.A análise de superfície de tendências conseguiu auxiliar na interpretação do movimento da pluma do efluente no corpo receptor, podendo ser usada como base para um possível monitoramento. Os valores de resíduos da superfície polinomial de primeiro grau mostraram as diferenças locais existentes entre as margens e o meio do rio e ainda a nítida interferência do efluente na riqueza de gêneros do plâncton. A análise das componentes principais forneceu como variáveis mais importantes DBO, OD, transparência da água, cor e numero de gêneros do plâncton, separando duas componentes principais: a primeira, mais importante e denominada abiótica, controlada por fatores físico-químicos e a segundo biológica, controlada pelariqueza de gêneros planctônicos. Os scores plotados em superfícies espaciais mostraram o impacto do efluente com relação às variáveis estudadas e recuperação das águas do rio ao final da malha de amostragem.

  16. Intolerância glicêmica e o prognóstico perinatal em gestantes utilizando anti-retrovirais

    Directory of Open Access Journals (Sweden)

    El Beitune Patrícia

    2003-01-01

    Full Text Available OBJETIVOS: estudar o efeito das drogas anti-retrovirais sobre o metabolismo glicêmico em gestantes portadoras do HIV-1 e a ação dessas medicações sobre o prognóstico perinatal. MÉTODOS: estudo prospectivo realizado em 57 gestantes divididas em três grupos: grupo AZT, utilizando zidovudina (n=20; grupo TT, utilizando zidovudina+lamivudina+nelfinavir (n=25, e grupo controle, gestantes normais (n=12. Obteve-se a área sob a curva (ASC das glicemias após teste oral de tolerância à glicose com 75 g de glicose em quatro oportunidades durante a gravidez (1º=14-20 semanas, 2º=21-26 semanas, 3º=27-32 semanas e 4º=33-38 semanas. O prognóstico perinatal levou em consideração as taxas de prematuridade, restrição de crescimento intra-útero (RCIU, baixo peso ao nascer, mortalidade perinatal e transmissão vertical do HIV-1. Os dados foram analisados utilizando-se os testes não paramétricos do c², de Friedman e de Kruskal-Wallis. RESULTADOS: os valores da mediana da ASC foi de 11.685 mg/dL-2h para o grupo controle, 13.477 mg/dL-2h para o grupo AZT e 13.650 mg/dL-2h para o grupo TT (p=0,049. Não se observou efeito deletério dos anti-retrovirais sobre as taxas de prematuridade, baixo peso ao nascer, RCIU e índices de Apgar. Não houve nenhum caso de transmissão vertical do HIV-1. CONCLUSÕES: verificou-se o desenvolvimento de intolerância glicêmica em gestantes que utilizaram tratamento tríplice, não sendo observado naquelas que utilizaram apenas AZT. Não houve efeitos deletérios dos anti-retrovirais sobre o prognóstico perinatal.

  17. Warm brine lakes in craters of active mud volcanoes, Menes caldera off NW Egypt: evidence for deep-rooted thermogenic processes

    OpenAIRE

    Dupre, Stephanie; Mascle, Jean; Foucher, Jean-Paul; Harmegnies, Francois; Woodside, John; Pierre, Catherine

    2014-01-01

    The Menes caldera is a fault-controlled depression (~8 km in diameter) at ~3,000 m water depth in the western province of the Nile deep-sea fan off NW Egypt, comprising seven mud volcanoes (MVs) of which two are active. Based on multichannel and chirp seismic data, temperature profiles, and high-resolution bathymetric data collected during the 2000 Fanil, 2004 Mimes and 2007 Medeco2 expeditions, the present study investigates factors controlling MV morphology, the geometry of feeder channels,...

  18. Shallow sub-surface structure of the central volcanic complex of Tenerife, Canary Islands: implications for the evolution and the recent reactivation of the Las Canadas caldera

    Energy Technology Data Exchange (ETDEWEB)

    Gottsmann, J [Department of Earth Sciences, University of Bristol, Wills Memorial Building, Queens Road, Bristol BS8 1RJ (United Kingdom); Camacho, A G; Fernandez, J [Instituto de Astronomia y Geodesia (CSIC-UCM), Ciudad Universitaria, Pza. de Ciencias, 3, 28040 Madrid (Spain); MartI, J [Institute of Earth Sciences ' Jaume Almera' , CSIC, Lluis Sole SabarIs s/n, Barcelona 08028 (Spain); Wooller, L; Rymer, H [Department of Earth and Environmental Sciences, Open University, Walton Hall, Milton Keynes, MK7 6AA (United Kingdom); GarcIa, A [Department of Volcanology, Museo Nacional de Ciencias Naturales, CSIC, C/ Jose Gutierrez Abascal, 2, 28006 Madrid (Spain)], E-mail: j.gottsmann@bristol.ac.uk

    2008-10-01

    We present a new local Bouguer anomaly map of the Central Volcanic Complex (CVC) of Tenerife, Spain. The high-density core of the CVC and the pronounced gravity low centred in the Las Canadas caldera (LCC) in greater detail than previously available. Mathematical construction of a subsurface model from the local anomaly data, employing a 3-D inversion enables mapping of the shallow structure beneath the complex, giving unprecedented insights into the sub-surface architecture of the complex, and shedding light on its evolution.

  19. Rendimiento térmico de calderas bagaceras modernas en Tucumán, R. Argentina Thermal efficiency of modern bagasse boilers in Tucumán, Argentina

    Directory of Open Access Journals (Sweden)

    Federico J. Franck Colombres

    2011-12-01

    Full Text Available Se evaluaron tres calderas de vapor modernas instaladas en ingenios azucareros de Tucumán, R. Argentina, equipos que se encuadran dentro de las tecnologías de producción más limpia. Tomando como base la metodología de cálculo de la eficiencia térmica de generadores de vapor desarrollada en 2008 por la Sección Ingeniería y Proyectos Agroindustriales de la Estación Experimental Agroindustrial Obispo Colombres, y a partir de los datos recolectados por medio de mediciones y balances de materia y energía, se determinaron sus principales variables características de operación. Las eficiencias energéticas determinadas para cada una fueron del 73,5%; 75,2% y 77,3%. Se realizó además una comparación con las calderas de vapor convencionales y se determinó el ahorro de bagazo que puede obtenerse con las calderas modernas, el cual resultó ser de un 27,6%. Como una ventaja adicional, se hace mención a la posibilidad de mejora del rendimiento térmico del ciclo motriz de la planta, que viene acompañada con el aumento de la presión de trabajo de la caldera.Three modern steam boilers, installed in sugar mills in Tucumán, R. Argentina, to attain a cleaner production, were evaluated. Their major operating variables were determined using the methodology for calculating thermal efficiency of steam generators developed by Sección Ingeniería y Proyectos Agroindustriales of Estación Experimental Agroindustrial Obispo Colombres in 2008, and data obtained from measurements and material and energy balances. Energy efficiency values determined for each boiler were 73.5%, 75.2% and 77.3%, respectively. A comparison with conventional steam boilers was drawn and it was found that bagasse savings amounted to about 27.6% when modern boilers were used. The possibility of improving the thermal efficiency of the plant cycle by increasing boiler pressure is mentioned as an additional advantage.

  20. Investigations of volcanic and earthquake-related deformation: Observations and models from Long Valley Caldera, northwestern Peloponnese, and northwestern Costa Rica

    Science.gov (United States)

    Feng, Lujia

    2011-12-01

    The advent of Global Positioning System (GPS) has revolutionized geodesy with high accuracy, fast speed, simple use, and low cost. This dissertation investigates three topics on volcano and earthquake-related deformation using GPS measurements and models to demonstrate the power of the new generation of geodetic methods. The three topics include the 2002-2003 continued episodic inflation at Long Valley Caldera in eastern California, the coseismic and postseismic response of the energetic 2008 MW 6.4 Achaia-Elia Earthquake in northwest Peloponnese, Greece, and the interseismic megathrust coupling and forearc sliver transport near the Nicoya Peninsula in northwest Costa Rica.

  1. Caldera La Peligrosa (47º15´S, 71°40´O: un evento clave en la Provincia Silícea Chon Aike

    Directory of Open Access Journals (Sweden)

    Patricia Sruoga

    2010-05-01

    Full Text Available En el área ubicada entre el lago Ghío y la sierra Colorada, en la Cordillera Patagónica Austral, aflora una secuencia piroclástico- lávica de carácter proximal correspondiente al Complejo El Quemado, de edad jurásica tardía. A partir del análisis integrado de litofacies y estructuras se llevó a cabo la reconstrucción de la arquitectura volcánica. Se han reconocido cuatro litofacies ignimbríticas y una litofacies lávico-hipabisal de composición riolítica, cuyo emplazamiento estuvo controlado por un sistema de fallas transtensionales de orientación NNO predominante. Se propone un modelo de evolución de la caldera La Peligrosa en tres etapas:1 pre-colapso, durante la cual se define una zona dilatante propicia para la formación de la caldera, con incipiente fallamiento en bloques, 2 colapso, cuando ocurre el emplazamiento de potentes ignimbritas cristalinas y megabrechas en una cubeta de subsidencia progresiva, controlada por un régimen transtensional con dirección de extensión NE y 3 post-colapso, durante la cual se produce el derrame de lavas junto con la intrusión de cuerpos dómicos, bajo condiciones de extensión oblicua con dirección de extensión NO. El pasaje de un ambiente transtensional a condiciones de extensión oblicua acompañó las últimas etapas del desarrollo de la caldera representando un notable cambio en las condiciones de la deformación en tiempos jurásicos. La formación y desarrollo de la caldera La Peligrosa puede ser considerada como un evento clave para entender los mecanismos eruptivos del vasto volcanismo ignimbrítico de la Provincia Silícea Chon Aike.

  2. An integrated multidisciplinary re-evaluation of the geothermal system at Valles Caldera, New Mexico, using an immersive three-dimensional (3D) visualization environment

    Science.gov (United States)

    Fowler, A.; Bennett, S. E.; Wildgoose, M.; Cantwell, C.; Elliott, A. J.

    2012-12-01

    We describe an approach to explore the spatial relationships of a geothermal resource by examining diverse geological, geophysical, and geochemical data sets using the immersive 3-dimensional (3D) visualization capabilities of the UC Davis Keck Center for Active Visualization in the Earth Sciences (KeckCAVES). The KeckCAVES is a facility where stereoscopic images are projected onto four, surfaces (three walls and a floor), which the user perceives as a seamless 3D image of the data. The user can manipulate and interact with the data, allowing a more intuitive interpretation of data set relationships than is possible with traditional 2-dimensional techniques. We incorporate multiple data sets of the geothermal system at Valles Caldera, New Mexico: topography, lithology, faults, temperature, alteration mineralogy, and magnetotellurics. With the ability to rapidly and intuitively observe data relationships, we are able to efficiently and rapidly draw conclusions about the subsurface architecture of the Valles Caldera geothermal system. We identify two high-temperature anomalies, one that corresponds with normal faults along the western caldera ring fracture, and one that with the resurgent dome. A cold-temperature anomaly identified adjacent to the resurgent dome high-temperature anomaly appears to relate to a fault controlled graben valley that acts as a recharge zone, likely funneling cold meteoric water into the subsurface along normal faults observed on published maps and cross sections. These high-temperature anomalies broadly correspond to subsurface regions where previous magnetotelluric studies have identified low apparent resistivity. Existing hot springs in the Sulfur Springs area correspond to the only location where our modeled 100°C isotherm intersects the ground surface. Correlation between the first occurrence of key alteration minerals (pyrite, chlorite, epidote) in previously drilled boreholes and our temperature model vary, with chlorite showing a

  3. Application of HydroGeoSphere to model the response to anthropogenic climate change of three-dimensional hydrological processes in the geologically, geothermally, and topographically complex Valles Caldera super volcano, New Mexico: Preliminary results

    Science.gov (United States)

    Wine, M.; Cadol, D. D.

    2014-12-01

    Anthropogenic climate change is expected to reduce streamflow in the southwestern USA due to reduction in precipitation and increases in evaporative demand. Understanding the effects of climate change in this region is particularly important for mountainous areas since these are primary sources of recharge in arid and semi-arid environments. Therefore we undertook to model effects of climate change on the hydrological processes in Valles Caldera (448 km2), located in the Jemez Mountains of northern New Mexico. In Valles Caldera modeling the surficial, hydrogeological, and geothermal processes that influence hydrologic fluxes each present challenges. The surficial dynamics of evaporative demand and snowmelt both serve to control recharge dynamics, but are complicated by the complex topography and spatiotemporal vegetation dynamics. Complex factors affecting evaporative demand include leaf area index, temperature, albedo, and radiation affected by topographic shading; all of these factors vary in space and time. Snowmelt processes interact with evaporative demand and geology to serve as an important control on streamflow generation, but modeling the effects of spatiotemporal snow distributions on streamflow generation remains a challenge. The complexity of Valles Caldera's geology—and its associated hydraulic properties—rivals that of its surficial hydrologic forcings. Hydrologically important geologic features that have formed in the Valles Caldera are three-dimensionally intricate and include a dense system of faults, alluvium, landslides, lake deposits, and features associated with the eruption and collapse of this super volcano. Coupling geothermally-driven convection to the hydrologic cycle in this still-active geothermal system presents yet an additional challenge in modeling Valles Caldera. Preliminary results from applying the three-dimensional distributed hydrologic finite element model HydroGeoSphere to a sub-catchment of Valles Caldera will be

  4. The role of magma mixing and mafic recharge in the evolution of a back-arc quaternary caldera: The case of Payún Matrú, Western Argentina

    Science.gov (United States)

    Hernando, Irene Raquel; Petrinovic, Ivan Alejandro; Llambías, Eduardo Jorge; D'Elia, Leandro; González, Pablo Diego; Aragón, Eugenio

    2016-02-01

    The Quaternary Payún Matrú volcano is a long-lived edifice that developed a summit caldera 8 km wide, with abundant pre- and post-caldera volcanic activity. It is the main volcano of the Payún Matrú Volcanic Field, which is located in the back-arc Payenia Basaltic Province, at mid-western Argentina. The composition of Payún Matrú is mainly trachytic, with lesser amounts of trachyandesitic and basaltic trachyandesitic lavas. The Payún Matrú Volcanic Field includes also the Payún Liso stratovolcano and more than 200 monogenetic basaltic cones and associated lava flows that are located east and west of the caldera. The aim of this work is to show the Payún Matrú evolution based on the mineralogical and textural characterization and to make inferences on the trigger mechanism for the explosive eruption which leads to the caldera formation. Some intermediate lavas and trachytes include phenocrysts with contrasting textures and composition, such as inverse zoning in plagioclase and clinopyroxenes, sieved plagioclases with a more calcic rim and calcic plagioclases with a more sodic rim, indicating that they could not have formed together and suggesting magma mixing processes. In addition, a few lavas show mafic enclaves or texturally different groundmasses with fluidal contacts, indicating mingling between two magmas. These lavas are found in the pre-caldera stage and the early post-caldera stage of Payún Matrú. The trachytic pyroclastic deposits related to the caldera collapse do not exhibit evidence of hybridization, although they present a minor proportion of dissolved feldspars and biotite replaced by anhydrous minerals, suggesting that a restricted zone of the chamber was reheated. This may be explained by a mafic recharge event where part of the host trachytic magma was heated, but without a complete homogenization between the host and recharging magmas. These features, in addition to the abundant basaltic volcanism east and west of the caldera, suggest

  5. Una mejora a la clasificación basada en la medida calidad de la similaridad utilizando relaciones borrosas

    Directory of Open Access Journals (Sweden)

    Yumilka B. Fernández-Hernández

    2015-01-01

    Full Text Available El aprendizaje de reglas de clasificación es un problema clásic o del aprendizaje automático. El algoritmo IRBASIR para la ind ucción de reglas de clasificación basado en relaciones de similaridad per mite descubrir conocimiento a partir de sistemas de decisión qu e contienen rasgos tanto discretos como con tinuos. El mismo ha mostrado obt ener resultados superiores a otro s algoritmos conocidos en este tema. En este artículo se proponen varias modificaciones a este algoritm o basadas en la Teoría de los Conjuntos Borrosos, debido a las ventajas que estos poseen, teniendo en cuenta la medida calidad de similarid ad. Los resultados experimentales muestran que utilizando la Te oría de los Conjuntos Borrosos se obtienen resultados estadísticamente supe riores al algor itmo original.

  6. Internet de las cosas: una primera aproximación utilizando la tecnología SIGFOX

    OpenAIRE

    Terán Lozano, Israel

    2015-01-01

    El presente proyecto representa el Trabajo Final de Máster – TFM – para la obtención del título oficial de máster en ingeniería de la automoción ofertado por el ETSEIB. El proyecto denominado “Internet de las cosas: una primera aproximación utilizando la tecnología SIGFOX”, tiene como objetivo familiarizarse con el módulo TD1204 de Telecom Design desarrollado para SIGFOX y su red de Internet de las Cosas (IoT), además de conocer sus prestaciones, sus limitaciones y su uso, entre otras. Así...

  7. Arquitectura para balancear carga dinámica por demanda adaptativa, utilizando CORBA en JAVA-IDL

    Directory of Open Access Journals (Sweden)

    Jesús Chávez Esparza

    2008-01-01

    Full Text Available En este trabajo desglosaremos la elaboración de una nueva Arquitectura para balancear carga dinámica, por demanda adaptativa, utilizando CORBA en JAVA-IDL. Una arquitectura de balanceo de carga es un sistema que permite distribuir el trabajo computacional entre varias máquinas, con el objetivo de reducir el tiempo de respuesta global del sistema. A través de las pruebas se justifica el uso de la arquitectura y se definen los parámetros a considerar para obtener un óptimo desempeño, refiriéndose al número de réplicas, al tipo de requerimiento y la estrategia de balanceo.

  8. Qualificação subjetiva de imagens arquitetônicas utilizando a teoria de sistema nebuloso

    Directory of Open Access Journals (Sweden)

    Graça Valeria Azzi Collet da

    2001-01-01

    Full Text Available Esse trabalho faz parte de uma pesquisa mais abrangente, a qual pretende implementar metodologia de projeto que leve em consideração técnicas de projeto participativo, bem como a qualificação subjetiva de imagens. Nesse primeiro momento, é feita a análise de viabilidade da qualificação de imagens através da Teoria dos Sistemas Nebulosos, para a criação de banco de dados que possibilite o armazenamento de projetos arquitetônicos relacionados ao diferencial semântico. Essa avaliação foi feita com a aplicação de questionário, utilizando-se adjetivos para a qualificação de quinze fachadas. Os dados foram tabulados com base na Teoria dos Sistemas Nebulosos, o que permitiu resultados coerentes na qualificação e agrupamento de imagens.

  9. Procedimiento para la gestión de mantenimiento utilizando herramientas de la cuarta generación

    Directory of Open Access Journals (Sweden)

    Aracelis Barrios

    2013-01-01

    Full Text Available El presente artículo presenta el diseño de un procedimiento para una gestión de mantenimiento sistémico, utilizando un conjunto de herramientas, que enfocan el uso de los recursos de la empresa asociados con las Personas, los Procesos y la Tecnología, orientados a mejorar la productividad, la toma de decisiones acertadas y a maximizar el rendimiento de los equipos, considerando entre otros, los factores de Confiabilidad, Mantenibilidad, Seguridad, Calidad y Medio Ambiente. El desarrollo del procedimiento permite utilizar de manera sistémica, la información obtenida al aplicar el mantenimiento productivo total (TPM, el análisis de modo y efectos de las fallas del mantenimiento centrado en confiabilidad (RCM, para evaluar los riesgos causados por las fallas en los equipos mediante la aplicación de la Lógica Difusa.

  10. 40Ar/39Ar dating of tuff vents in the Campi Flegrei caldera (southern Italy): Toward a new chronostratigraphic reconstruction of the Holocene volcanic activity

    Science.gov (United States)

    Fedele, L.; Insinga, D.D.; Calvert, A.T.; Morra, V.; Perrotta, A.; Scarpati, C.

    2011-01-01

    The Campi Flegrei hosts numerous monogenetic vents inferred to be younger than the 15 ka Neapolitan Yellow Tuff. Sanidine crystals from the three young Campi Flegrei vents of Fondi di Baia, Bacoli and Nisida were dated using 40Ar/39Ar geochronology. These vents, together with several other young edifices, occur roughly along the inner border of the Campi Flegrei caldera, suggesting that the volcanic conduits are controlled by caldera-bounding faults. Plateau ages of ∼9.6 ka (Fondi di Baia), ∼8.6 ka (Bacoli) and ∼3.9 ka (Nisida) indicate eruptive activity during intervals previously interpreted as quiescent. A critical revision, involving calendar age correction of literature 14C data and available 40Ar/39Ar age data, is presented. A new reference chronostratigraphic framework for Holocene Phlegrean activity, which significantly differs from the previously adopted ones, is proposed. This has important implications for understanding the Campi Flegrei eruptive history and, ultimately, for the evaluation of related volcanic risk and hazard, for which the inferred history of its recent activity is generally taken into account.

  11. [Dominant phylotypes in the 16S rRNA gene clone libraries from bacterial mats of the Uzon caldera (Kamchatka, Russia) hydrothermal springs].

    Science.gov (United States)

    Akimov, V N; Podosokorskaia, O A; Shliapnikov, M G; Gal'chenko, V F

    2013-01-01

    In situ analysis of the 16S rRNA genes form bacterial mats of five hydrothermal springs (36-58 degrees C) in the Uzon caldera (Kamchatka, Russia) was carried out using clone libraries. Eight clone libraries contained 18 dominant phylotypes (over 4-5%). In most clone libraries, the phylotype of the green sulfur bacterium Chlorobaculum sp. was among the dominant ones. The phylotypes of the green nonsulfur bacteria Chloroflexus and Roseiflexus and of purple nonsulfur bacteria Rhodoblastus, Rhodopseudomonas, and Rhodoferax were also among the dominant ones. Cyanobacteria were represented by one dominant phylotype in a single spring. Among nonphototrophic bacteria, the dominant phylotypes belonged to Sulfyrihydrogenibium sp., Geothrixsp., Acidobacterium sp., Meiothermus sp., Thiomonas sp., Thiofaba sp., and Spirochaeta sp. Three phylotypes were not identified at the genus level. Most genera of phototrophic and nonphototrophic organisms corresponding to the phylotypes from Uzon hydrotherms have been previously revealed in the hydrotherms of volcanically active regions of America, Asia, and Europe. These results indicate predominance of bacterial mats carrying out anaerobic photosynthesis in the hydrotherms of the Uzon caldera.

  12. El capitán Miguel Caldera y la frontera chichimeca: entre el mestizo historiográfico y el soldado del rey

    Directory of Open Access Journals (Sweden)

    Ruiz Guadalajara, Juan Carlos

    2010-04-01

    Full Text Available This article attempts to examine critically the image that contemporary historiography has built around the figure of Captain Miguel Caldera. In contrast, it shows aspects that bring us closer to his Hispanic identity, to his role as a member of the militia in the service of Philip II of Spain and to the part he played as an instrument of domination and in the disappearance of the nomads of the Chichimecan frontier. It also contributes to the discussion of frontier cultural development in the context of the Hispanic monarchy’s expansion in the 16th century.

    Este artículo intenta un acercamiento crítico a la imagen que la historiografía contemporánea ha construido en torno a la figura del capitán Miguel Caldera. Muestra, en contraste, elementos que nos aproximan a su identidad hispánica, a su papel como miliciano al servicio de Felipe II y a su función como vehículo de la dominación y desaparición de los nómadas de la frontera chichimeca. También pretende aportar elementos de discusión sobre el proceso cultural fronterizo en el ámbito de la expansión de la monarquía hispánica en el siglo XVI.

  13. Probabilistic tsunami hazard assessment related to underwater explosions in the Campi Flegrei caldera: Gulfs of Napoli and Pozzuoli (Tyrrhenian Sea, Italy).

    Science.gov (United States)

    Ulvrova, Martina; Selva, Jacopo; Paris, Raphael; Brizuela, Beatriz; Costa, Antonio; Grezio, Anita; Lorito, Stefano; Tonini, Roberto

    2016-04-01

    Tsunami caused by underwater volcanic explosions are typically characterized by short period waves and greater dispersion compared to tsunami generated by earthquakes, and the impact in the far-field is often limited. However, the effect of dispersion is reduced for underwater explosions occurring in shallow-water environments, as the length-to-depth ratio of the waves rapidly increase, and runup inland can be locally high. This effect was particularly illustrated by the 19 m runup at Karymsky Lake, Kamchatka, in 1996 (Belousov et al., 2010; Ulvrova et al., 2014). Hazards related to underwater volcanic explosions are challenging to evaluate and might be underestimated in some cases. In this study we consider different scenarios of explosions in the offshore part of the Campi Flegrei (Phlegraean Fields) caldera in the Pozzuoli - Naples region (Tyrrhenian Sea, Italy). The onshore eruptive history of the caldera is well documented (e.g. Orsi et al., 2004), but past and future activity offshore has been rarely discussed. The probability for eruptions in the submarine part of the caldera is perhaps low (Selva et al., 2012), but scenarios of tsunamis generated by underwater explosions and their impact in the proximal field (Bay of Pozzuoli) and far field (Bay of Naples) deserve to be considered due to high population density in the adjacent coastal areas. Initial surface displacement is estimated as a function of explosion energy at a given depth. We study 17 different potential vent locations within the Pozzuoli Bay, and 3 different vent radii (200 m, 650 m and 900 m), corresponding to the three representative eruptive scenarios identified in Orsi et al. (2009) and Selva et al. (2010). We then use these sources in a Bayesian Event Tree framework, following the procedure defined in Selva et al. (2010), in order to evaluate a first order Probabilistic Hazard Analysis for this type of tsunami sources for the Gulfs of Napoli and Pozzuoli. Belousov A., Voight B., Belousova M

  14. Spatial and Temporal Analysis of Hydrometeorological Conditions in the Valles Caldera, New Mexico during the North American Monsoon

    Science.gov (United States)

    Mendez-Barroso, L. A.; Rinehart, A. J.; Aragon, C. A.; Bisht, G.; Cardenas, M. B.; Engle, E.; Forman, B.; Frisbee, M.; Gutierrez-Jurado, H. A.; Hong, S.; Tai, K.; Wyckoff, R. L.; Vivoni, E. R.

    2005-12-01

    The hydrometeorological conditions of mountain environments in semiarid regions are poorly understood, particularly during the North American Monsoon. Although it is well known that the climate and hydrology of mountain ranges are dynamically distinct of surrounding lowlands, little quantitative observational data has been collected to assess the spatial and temporal variations in hydrometeorological conditions in these settings. Factors such as topographic position, vegetation type and soil properties have a strong influence on the hydrological response to atmospheric conditions. Similarly, landscape features such as relief and aspect can play a major role on the local meteorological conditions in mountainous environments. In order to better understand the relation between mountain hydrometeorology and topographic and ecological factors, a spatially extensive field campaign was carried out in the Valles Caldera National Preserve in the Jemez Mountains of northern New Mexico, USA. This region forms a portion of the headwaters of the Rio Grande and displays distinct hydrologic responses during the summer and winter seasons. A twelve day sampling period during the summer monsoon season (July to August 2005) was selected to observe the land-atmosphere interactions resulting from convective storms in the region. The hydrometeorological field campaign included seventy-one sampling sites where daily rainfall, meteorological variables (e.g. air temperature, relative humidity, wind speed and barometric pressure), volumetric soil moisture, and soil temperature were measured. Each site consisted of a one square meter plot that was characterized in term of terrain position, vegetation and surface properties. Likewise, daily gravimetric soil samples were taken in order to compare with the volumetric measurements inferred using an impedance probe. In this study, we present a preliminary analysis of the spatial and temporal distribution of soil and atmospheric variables during

  15. Variability of the planktonic foraminifera community across the Eocene/Oligocene boundary, Fuente Caldera Section, Baetic Ranges (Spain)

    Science.gov (United States)

    Legarda-Lisarri, A.

    2013-12-01

    During the Eocene/Oligocene transition, in a massive extinction event that took place about 33.7 million years ago, the current high resolution study analyzes qualitatively and quantitatively the community structure of the planktonic foraminifera that were preserved in the hemipelagic sediments of the Tethys Sea. The sampled section of the Fuente Caldera column, located in the Baetic mountain ranges, spans a register of 396,551.7 years. Based in the identification of 27 species, that belong to 13 genera and 2 families of foraminifera, there have been found three biozones of Gonzalvo Zonation (Gonzalvo, 2002) in the studied stratigraphic interval: Turborotalia cocoaensis and Cribrohantkenina lazzarii Biozones (Rupelian), and Paragloborotalia increbescens (Priabonian). The planktonic foraminifera associations variability patterns are defined by paleoecologic indexes (diversity index, high and low latitude species index and planktonic and benthic foraminifera index), by geochemical proxies: δ18O and δ13C and by 'Q' Mode Factor Analysis. They prove that the deposition environment is outer platform and also, they suggest that the studied area in the Tethys Sea underwent many thermal pulses, during which some species extinct or appear. In the first extinction event the species Turborotalia cocoaensis and Turborotalia cunialensis became extinct. In the second one, Hantkenina alabamensis, Hantkenina brevispina, Cribrohantkenina lazzarii and Pseudohastigerina micra became extinct while a succession occured; Globigerina officinalis, Globoturborotalita anguliofficinalis and Tenuitellinata angustiumbilicata appeared. The cooling event that finished in the Lower Oligocene was the biggest of these pulses, which was extremely abrupt and corresponds to the Oi-1 event that was described by Miller (Miller, 1991). All this evidences that the planktonic foraminifera extinction in the Upper Eocene was a gradual and fast event, what is supported by the Factor Analysis application. Key

  16. Intercâmbio educacional internacional na modalidade doutorado sanduíche em enfermagem: relato de experiência Intercambio educacional internacional en la modalidad doctorado sándwich: relato de experiencia International educational exchange in nursing s andwich doctorate modality: experience report

    Directory of Open Access Journals (Sweden)

    Kleyde Ventura de Souza

    2008-06-01

    Full Text Available Relato de experiência de estágio de Doutorado Sanduíche oferecido pela Coordenação de Aperfeiçoamento de Pessoal de Nível Superior, realizado na Faculté des Sciences Infirmières/Université de Montreal, no período de agosto a dezembro de 2004. O estágio teve como enfoque o aprofundamento dos aspectos conceituais e práticos relacionados à saúde da mulher e seus direitos sexuais e reprodutivos. Este artigo tem como propósito apresentar as atividades realizadas e despertar o interesse dos estudantes de doutorado dos programas brasileiros de pós-graduação nessa modalidade de intercâmbio. Destacam-se a participação em cursos, reuniões de grupos de pesquisas e em eventos científicos; visitas técnicas e troca de experiências com pesquisadores e integrantes de organizações sociais e conferências. Com esta experiência, verificou-se a importância da cooperação entre pesquisadores e instituições do Brasil e do exterior e fortaleceu-se o compromisso com um projeto de emancipação profissional e social, por meio da pesquisa e deste tipo de cooperação.El artículo relaciona a la experiencia del entrenamiento del Doctorado Sándwich, ofrecido por Cordenación de Perfeccionamiento de Personal de Nivel Superior y realizado en la Faculté de Sciences Infirmières/Université de Montreal, de agosto al diciembre de 2004. El entrenamiento enfocó en profundizar los aspectos conceptuales y prácticos relacionados con la salud de la mujer y con sus derechos sexuales y reproductivos. Este artículo se trata de presentar las actividades realizadas e inspirar el interés de estudiantes de los programas brasileños de la post-grado en esta modalidad del intercambio. Este intercambio era distinguido por la participación en cursos, en reuniones de grupos de investigación y en conferencias científicos, y en las visitas técnicas y el intercambio de experiencias entre investigadores y miembros de organizaciones social. La experiencia

  17. La Peligrosa caldera (47° 15‧S, 71° 40‧W): A key event during the Jurassic ignimbrite flare-up in Southern Patagonia, Argentina

    Science.gov (United States)

    Sruoga, P.; Japas, M. S.; Salani, F. M.; Kleiman, L. E.

    2014-01-01

    Pyroclastic and lava vent-facies, from the Late Jurassic El Quemado Complex, are described at the southern Lake Ghío, in the Cordillera Patagónica Austral. Based on the comprehensive study of lithology and structures, the reconstruction of the volcanic architecture has been carried out. Four ignimbrites and one rhyolitic lava unit, affected by oblique-slip normal faults have been recognized. The evolution of La Peligrosa Caldera has been modeled in three different stages:1) initial collapse, consisting of a precursory downsag subsidence, related to a dilatational zone, which controlled the location of the caldera, 2) main collapse, with the emplacement of large volume crystal-rich ignimbrites and megabreccias, under a progressive subsidence controlled by a pull-apart structure related to a transtensional regime and 3) post-collapse, in which lava flows and associated domes were emplaced under an oblique-extensional regime. The caldera records a remarkable change from transtension to oblique extension, which may represent an important variation in regional deformation conditions during Jurassic times. La Peligrosa Caldera may be considered a key event to understand the eruptive mechanisms of the flare-up volcanism in the Chon Aike Silicic Province.

  18. Millennial-Scale Climate Variability During a mid-Pleistocene Glacial (MIS 12) from a Terrestrial Lacustrine Record in the Valles Caldera, New Mexico

    Science.gov (United States)

    Fawcett, P. J.; Brown, E. T.; Werne, J. P.; Contreras, S.; Anderson, R. S.; Dodd, J. P.; Sharp, Z. D.; Heikoop, J. M.; Allen, C. D.

    2011-12-01

    We present a high-resolution terrestrial climate record from the Valles Caldera, New Mexico which spans some 200,000 years from mid MIS 14 to early MIS 10. The glacial periods represented in the record exhibit millennial-scale Dansgaard-Oeschger like variability, especially in MIS 12, one of the coldest glacials in the Pleistocene. High resolution proxies from core VC-3 including scanning XRF data, sediment density, color, and magnetic susceptibility show approximately 23 millennial-scale oscillations in MIS 12 with an average duration of 2,300 years. Many of these oscillations are characterized by relatively slow coolings followed by abrupt warmings, similar to D-O events in the Greenland ice core record. MBT/CBT MAT estimates in the MIS 12 portion of the core show stadial to interstadial warmings of up to 6 °C. The VC-3 stadials correlate with high percentages of boreal taxa pollen ( Picea, Abies ) (up to 25%) while interstadials have lower boreal pollen percentages (~5%) and many correlate with local maxima in Juniperus> and Quercus> . Significant changes in the hydrologic cycle also occur at these millennial timescales. Oxygen isotope data from diatom silica record changes of up to 10 per mil from stadial to interstadial, probably reflecting a combination of changes in moisture source (Pacific vs. Gulf of Mexico), moisture transport pathway, and the seasonality of precipitation. Several interstadials correlate with increases in Cyperaceae (sedge) pollen suggesting a shallower lake with a broad marshy zone around its margin. This zone was minimized during stadials when the lake was deeper. Interstadial shallowing probably resulted from higher evaporation rates and/or a reduction in winter precipitation. This combination of proxies from the Valles Caldera suggests that glacial stage millennial-scale climate variability in the American southwest was strongly driven by changes in the strength and location of the winter polar jet, which in turn affected the local

  19. Validação Interna de Base de Conhecimentos utilizando Modelagem Matemática Bayesiana x Conexionista

    Directory of Open Access Journals (Sweden)

    Lucimar Fossatti de Carvalho

    2009-09-01

    Full Text Available Neste artigo, investigamos o aprendizado de máquina baseado na modelagem matemática envolvendo modelos bayesianos x conexionistas, aplicado no auxílio ao diagnóstico de eventos epilépticos (EEs e eventos não epilépticos (ENEs. Para esta finalidade alguns algoritmos de aprendizado de máquina foram comparados incluindo o aprendizado conexionista através das regras Delta Generalizada, Hebb, Oja, juntamente com o aprendizado em redes bayesianas. Foram considerados para este estudo 122 pacientes os quais apresentavam sintomas relacionados com EEs e ENEs. Os resultados empíricos desta pesquisa indicam que: (1 ambas as abordagens bayesianas e conexionistas são bastante similares, mostrando que os resultados são coerentes, mesmo utilizando heurísticas distintas; (2 o índice de acertos de casos positivos (EEs, por meio da modelagem bayesiana pode estar relacionado com a facilidade de implementação das probabilidades condicionais. Concluiu-se, portanto, que os modelos investigados fornecem informações importantes para o desenvolvimento de novas pesquisas tanto na área bayesiana como na área conexionista.

  20. Enfriamiento de café pergamino seco a granel utilizando aireación mecánica controlada

    Directory of Open Access Journals (Sweden)

    Julio E. Ospina M.

    2011-01-01

    Full Text Available Con el fin de garantizar que el café almacenado a granel conserve su calidad durante el tiempo necesario de almacenamiento, se estudió el enfriamiento del café pergamino seco en silos experimentales de dimensiones: 0.5m x 0.5m y 2.8 m de altura, utilizando aire enfriado mecánicamente. Los rangos estudiados fueron: temperatura de 10 a 220C humedad relativa de 66 a 98%y contenido de humedad del grano de 8 a 13.57% b.h. Durante la etapa de almacenamiento se evaluó la variación de la calidad del café según los criterios de coloración de la almendra, población de microorganismos y prueba de taza; paralelamente se dejaron muestras almacenadas en sacosa las condiciones de Chinchiná, como muestra testigo buscando determinar la bondad del almacenamiento a granel, también se dejó un silo sin aireación para determinar el efecto de la aireación controlada en la calidad del café.

  1. Preditores de prováveis transtornos mentais comuns (TMC em prostitutas utilizando o Self-Reporting Questionnaire

    Directory of Open Access Journals (Sweden)

    Carlos Eduardo Leal Vidal

    2014-09-01

    Full Text Available Objetivo Avaliar a prevalência de prováveis transtornos mentais comuns (TMC e os fatores associados em um grupo de prostitutas de Minas Gerais. Métodos Estudo transversal utilizando o Self-Reporting Questionnaire (SRQ-20 em mulheres cadastradas na Associação de Prostitutas de Minas Gerais (Aprosmig. Avaliaram-se características sociodemográficas e aspectos do trabalho na prostituição. Teste do qui-quadrado foi empregado na análise de associação entre variáveis categóricas sociodemográficas e a presença de prováveis TMC. A análise dos fatores associados à presença de prováveis TMC foi realizada por meio de modelo de regressão logística. Resultados Foram entrevistadas 216 prostitutas. A prevalência global de prováveis TMC foi de 57,9%, mais observada em mulheres com baixa escolaridade, história de violência física e ingresso precoce na prostituição. Conclusão Os resultados deste estudo mostraram que a prevalência de prováveis TMC entre prostitutas foi superior à observada na população geral, indicando a necessidade de melhorar os cuidados com a saúde dessas mulheres.

  2. Sixty thousand years of magmatic volatile history before the caldera-forming eruption of Mount Mazama, Crater Lake, Oregon

    Science.gov (United States)

    Wright, Heather M.; Bacon, Charles R.; Vazquez, Jorge A.; Sisson, Thomas W.

    2012-01-01

    The well-documented eruptive history of Mount Mazama, Oregon, provides an excellent opportunity to use pre-eruptive volatile concentrations to study the growth of an explosive silicic magmatic system. Melt inclusions (MI) hosted in pyroxene and plagioclase crystals from eight dacitic–rhyodacitic eruptive deposits (71–7.7 ka) were analyzed to determine variations in volatile-element concentrations and changes in magma storage conditions leading up to and including the climactic eruption of Crater Lake caldera. Temperatures (Fe–Ti oxides) increased through the series of dacites, then decreased, and increased again through the rhyodacites (918–968 to ~950 to 845–895 °C). Oxygen fugacity began at nickel–nickel-oxide buffer (NNO) +0.8 (71 ka), dropped slightly to NNO +0.3, and then climbed to its highest value with the climactic eruption (7.7 ka) at NNO +1.1 log units. In parallel with oxidation state, maximum MI sulfur concentrations were high early in the eruptive sequence (~500 ppm), decreased (to ~200 ppm), and then increased again with the climactic eruption (~500 ppm). Maximum MI sulfur correlates with the Sr content (as a proxy for LREE, Ba, Rb, P2O5) of recharge magmas, represented by basaltic andesitic to andesitic enclaves and similar-aged lavas. These results suggest that oxidized Sr-rich recharge magmas dominated early and late in the development of the pre-climactic dacite–rhyodacite system. Dissolved H2O concentrations in MI do not, however, correlate with these changes in dominant recharge magma, instead recording vapor solubility relations in the developing shallow magma storage and conduit region. Dissolved H2O concentrations form two populations through time: the first at 3–4.6 wt% (with a few extreme values up to 6.1 wt%) and the second at ≤2.4 wt%. CO2 concentrations measured in a subset of these inclusions reach up to 240 ppm in early-erupted deposits (71 ka) and are below detection in climactic deposits (7.7 ka). Combined H2O and

  3. Chemical abrasion-SIMS (CA-SIMS) U-Pb dating of zircon from the late Eocene Caetano caldera, Nevada

    Science.gov (United States)

    Watts, Kathryn E.; Coble, Matthew A.; Vazquez, Jorge A.; Henry, Christopher D.; Colgan, Joseph P.; John, David A.

    2016-01-01

    Zircon geochronology is a critical tool for establishing geologic ages and time scales of processes in the Earth's crust. However, for zircons compromised by open system behavior, achieving robust dates can be difficult. Chemical abrasion (CA) is a routine step prior to thermal ionization mass spectrometry (TIMS) dating of zircon to remove radiation-damaged parts of grains that may have experienced open system behavior and loss of radiogenic Pb. While this technique has been shown to improve the accuracy and precision of TIMS dating, its application to high-spatial resolution dating methods, such as secondary ion mass spectrometry (SIMS), is relatively uncommon. In our efforts to U-Pb date zircons from the late Eocene Caetano caldera by SIMS (SHRIMP-RG: sensitive high resolution ion microprobe, reverse geometry), some grains yielded anomalously young U-Pb ages that implicated Pb-loss and motivated us to investigate with a comparative CA and non-CA dating study. We present CA and non-CA 206Pb/238U ages and trace elements determined by SHRIMP-RG for zircons from three Caetano samples (Caetano Tuff, Redrock Canyon porphyry, and a silicic ring-fracture intrusion) and for R33 and TEMORA-2 reference zircons. We find that non-CA Caetano zircons have weighted mean or bimodal U-Pb ages that are 2–4% younger than CA zircons for the same samples. CA Caetano zircons have mean U-Pb ages that are 0.4–0.6 Myr older than the 40Ar/39Ar sanidine eruption age (34.00 ± 0.03 Ma; error-weighted mean, 2σ), whereas non-CA zircons have ages that are 0.7–1.3 Myr younger. U-Pb ages do not correlate with U (~ 100–800 ppm), Th (~ 50–300 ppm) or any other measured zircon trace elements (Y, Hf, REE), and CA and non-CA Caetano zircons define identical trace element ranges. No statistically significant difference in U-Pb age is observed for CA versus non-CA R33 or TEMORA-2 zircons. Optical profiler measurements of ion microprobe pits demonstrate consistent depths of ~ 1.6

  4. Deformation near the Casa Diablo geothermal well field and related processes Long Valley caldera, Eastern California, 1993-2000

    Science.gov (United States)

    Howle, J.F.; Langbein, J.O.; Farrar, C.D.; Wilkinson, S.K.

    2003-01-01

    Regional first-order leveling lines, which extend from Lee Vining, CA, to Tom's Place, CA, have been surveyed periodically since 1957 by the U.S. Geological Survey (USGS), the National Geodetic Survey (NGS), and Caltrans. Two of the regional survey lines, or leveling networks, intersect at the Casa Diablo geothermal well field. These leveling networks, referenced to a distant bench mark (C916) near Lee Vining, provide time-series vertical control data of land-surface deformation that began around 1980. These data are also useful for delineating localized subsidence at Casa Diablo related to reservoir pressure and temperature changes owing to geothermal development that began in 1985. A comparison of differences in bench-mark elevations for five time periods between 1983 and 1997 shows the development and expansion of a subsidence bowl at Casa Diablo. The subsidence coincides spatially with the geothermal well field and temporally with the increased production rates and the deepening of injection wells in 1991, which resulted in an increase in the rate of pressure decline. The subsidence, superimposed on a broad area of uplift, totaled about 310 mm by 1997. The USGS established orthogonal tilt arrays in 1983 to better monitor deformation across the caldera. One tilt array (DBR) was established near what would later become the Casa Diablo geothermal well field. This array responded to magmatic intrusions prior to geothermal development, tilting away from the well field. With the start of geothermal fluid extraction in 1985, tilt at the DBR array reversed direction and began tilting into the well field. In 1991, geothermal power production was increased by a factor of four, and reservoir pressures began a period of steep decline. These changes caused a temporary three-fold increase in the tilt rate. The tilt rate became stable in 1993 and was about 40% lower than that measured in 1991-1992, but still greater than the rates measured during 1985-1990. Data from the

  5. Geophysical imaging of the lacustrine sediments deposited in the La Calderilla Volcanic Caldera (Gran Canaria Island, Spain) for paleoclimate research

    Science.gov (United States)

    Himi, Mahjoub; Rodríguez-González, Alejandro; Criado, Constantino; Tapias, Josefina C.; Ravazzi, Cesare; Pérez-Torrado, Francisco; Casas, Albert

    2016-04-01

    The discovery of well-preserved maar structures is important not only for studying the eruptive activity and formation of volcanoes, but also for paleoclimate research, since laminated maar lake sediments may contain very detailed archives of climate and environmental history. Maars are a singular type of volcanic structure generated by explosive phreatomagmatic eruptions as a result of interaction between rising magma and groundwater. This kind of structures are characterised by circular craters, often filled with water and/or lacustrine sediments and surrounded by a ring of pyroclastic deposits.Recently a borehole was drilled at the bottom of La Calderilla volcanic complex which penetrated about 8.7 m in its sedimentary sequence and paleobotanical study has supplied the first evidence of paleoenvironmental evolution during the Holocene on the Gran Canaria Island. This survey, however, did not penetrate into the substrate because the total thickness of the sedimentary fill was unknown. Since the age of formation of La Calderilla volcanic complex based on K/Ar dating is about 85,000 years (Upper Pleistocene), the possibility of its sedimentary fill extends beyond of the Holocene is extremely attractive, since, for example, there are few paleoenvironmental data regarding how much the last glaciation that affected the Canary Islands. In these circumstances, the knowledge of the total thickness of the lacustrine sediments is crucial to design a deeper borehole in the next future. Therefore, the subsurface characterisation provided by geophysics is essential for determining thickness and geometry of the sedimentary filling. Multielectrode ERT method was used to obtain five 2-D resistivity cross-sections into La Calderilla volcanic caldera. An Iris Syscal Pro resistivity system with 48 electrodes connected to a 94 m long cable (2m electrode spacing) in Wenner-Schlumberger configuration for an investigation depth of about 20 m. Data quality (q noise ratio. All inverted

  6. Hydrothermal alteration products and stable isotope ratios of the Sulfur Creek Tuff; a window into the subsurface environment of the Yellowstone caldera in Yellowstone National Park, WY

    Science.gov (United States)

    Lonero, A.; Larson, P. B.

    2013-12-01

    The Yellowstone Caldera in northwest Wyoming is the site of active hydrothermal alteration. Hydrothermal activity relating to the Yellowstone hotspot has resulted in the alteration of rhyolites within the caldera. Specifically, the Seven Mile Hole area of the Grand Canyon of Yellowstone River provides an ideal location and opportunity to investigate the nature of the ongoing hydrothermal alteration. Here, erosion by the river has exposed a sequence of rocks which are host to hydrothermal fluids and are themselves significantly altered. Analyses of clay minerals and other alteration products, such as opal, has been undertaken in order to characterize and distinguish different zones of alteration. Hydrogen isotope ratios have been measured for the altered rock units within the Seven-Mile Hole area, and they range from -84.6 ‰ to -185.1 ‰ (VSMOW). Samples from this area commonly contain minerals such as kaolinite, illite, alunite, or buddingtonite, and the deuterium / hydrogen (D/H) ratios of these mineral phases are shown to vary considerably with respect to their location and elevation in the canyon. Additionally, oxygen isotope ratios have been measured on some samples in order to compare the samples' isotope values to the local meteoric water line. Plotting these samples in δD - δ18O space has shown that some values lie in a region trending away from the meteoric water line and along a "kaolinite line." This area is parallel to the array of Yellowstone hot spring fluids and a broad range of values are possible here depending on temperature of alteration. Furthermore, these data support a model where hydrothermal fluids flow upward through faults related to caldera collapse that are present in the sulfur creek tuff. This research may also show that the unique coloration patterns visible on the slopes of the Grand Canyon of Yellowstone can be, in part, explained as the result of both surface oxidation and hydrothermal alteration processes. Major element XRF

  7. Magma injection beneath the urban area of Naples: a new mechanism for the 2012–2013 volcanic unrest at Campi Flegrei caldera

    Science.gov (United States)

    D’Auria, Luca; Pepe, Susi; Castaldo, Raffaele; Giudicepietro, Flora; Macedonio, Giovanni; Ricciolino, Patrizia; Tizzani, Pietro; Casu, Francesco; Lanari, Riccardo; Manzo, Mariarosaria; Martini, Marcello; Sansosti, Eugenio; Zinno, Ivana

    2015-01-01

    We found the first evidence, in the last 30 years, of a renewed magmatic activity at Campi Flegrei caldera from January 2012 to June 2013. The ground deformation, observed through satellite interferometry and GPS measurements, have been interpreted as the effect of the intrusion at shallow depth (3090 ± 138 m) of 0.0042 ± 0.0002 km3 of magma within a sill. This interrupts about 28 years of dominant hydrothermal activity and occurs in the context of an unrest phase which began in 2005 and within a more general ground uplift that goes on since 1950. This discovery has implications on the evaluation of the volcanic risk and in the volcanic surveillance of this densely populated area. PMID:26279090

  8. Magma injection beneath the urban area of Naples: a new mechanism for the 2012-2013 volcanic unrest at Campi Flegrei caldera.

    Science.gov (United States)

    D'Auria, Luca; Pepe, Susi; Castaldo, Raffaele; Giudicepietro, Flora; Macedonio, Giovanni; Ricciolino, Patrizia; Tizzani, Pietro; Casu, Francesco; Lanari, Riccardo; Manzo, Mariarosaria; Martini, Marcello; Sansosti, Eugenio; Zinno, Ivana

    2015-01-01

    We found the first evidence, in the last 30 years, of a renewed magmatic activity at Campi Flegrei caldera from January 2012 to June 2013. The ground deformation, observed through satellite interferometry and GPS measurements, have been interpreted as the effect of the intrusion at shallow depth (3090 ± 138 m) of 0.0042 ± 0.0002 km(3) of magma within a sill. This interrupts about 28 years of dominant hydrothermal activity and occurs in the context of an unrest phase which began in 2005 and within a more general ground uplift that goes on since 1950. This discovery has implications on the evaluation of the volcanic risk and in the volcanic surveillance of this densely populated area. PMID:26279090

  9. The comparative evaluation of ERTS-1 imagery for resource inventory in land use planning. [Oregon - Newberry Caldera, Mt. Washington, and Big Summit Prairie in Crook County

    Science.gov (United States)

    Schrumpf, B. J. (Principal Investigator); Simonson, G. H.; Paine, D. P.; Lawrence, R. D.; Pyott, W. T.; Herzog, J. H.; Murray, R. J.; Norgren, J. A.; Cornwell, J. A.; Rogers, R. A.

    1974-01-01

    The author has identified the following significant results. Multidiscipline team interpretation and mapping of resources for Crook County is complete on 1:250,000 scale enlargements of ERTS imagery and 1:120,000 hi-flight photography. Maps of geology, soils, vegetation-land use and land resources units were interpreted to show limitations, suitabilities, and geologic hazards for land use planning. Mapping of lineaments and structures from ERTS imagery has shown a number of features not previously mapped in Oregon. A multistage timber inventory of Ochoco National Forest was made, using ERTS images as the first stage. Inventory of forest clear-cutting practices was successfully demonstrated with color composites. Soil tonal differences in fallow fields correspond with major soil boundaries in loess-mantled terrain. A digital classification system used for discriminating natural vegetation and geologic material classes was successful in separating most major classes around Newberry Caldera, Mt. Washington, and Big Summit Prairie.

  10. Gestión eficiente de modelos digitales de elevación para su visualización 3D utilizando procesamiento multinúcleo

    Directory of Open Access Journals (Sweden)

    Gilberto Arias-Naranjo

    2014-07-01

    Full Text Available En el siguiente trabajo se describe un modelo para la visualización eficiente de superficies de terrenos en tres dimensiones, que aprovecha las potencialidades de cómputo de los procesadores multinúcleos actuales. Se realiza una división lógica del terreno en cuadrantes, los cuales son representados utilizando quadtrees restringidos. La carga de los gráficos es controlada mediante una triangulación adaptativa de la superficie y aprovechando las ventajas de diferentes niveles de detalle. La escena que se está visualizando se gestiona dinámicamente, lo que permite mantener solamente en memoria los datos asociados a aquellos cuadrantes que se están visualizando. Aquellos cuadrantes que no se visualizan son almacenados en memoria externa y se gestionan utilizando una estructura de datos que permite un acceso eficiente a los datos de los mismos.

  11. Análisis del factor de intensidad de esfuerzo utilizando el método de los elementos finitos extendidos.

    Directory of Open Access Journals (Sweden)

    Agustín Sáenz López

    2013-01-01

    Full Text Available En este trabajo se presenta un método para obtener el Factor de Intensidad de Esfuerzo (FIS utilizando la Integral de Interacción acoplada al Método de Elementos Finitos Extendidos (MEFX, se desarrolló un sistema de computación propio para la implementación de este proceso utilizando el paquete MATLAB. Se usaron las condiciones de frontera de Dirichlet para simular las condiciones de frontera de la solución analítica, y todo el desarrollo se realizó en 2 dimensiones encontrándose una buena relación entre los resultados de este procedimiento y el ejemplo muestra cuya solución es bien conocida.

  12. Insights into the 3D architecture of an active caldera ring-fault at Tendürek volcano through modeling of geodetic data

    KAUST Repository

    Vasyura-Bathke, Hannes

    2015-04-28

    The three-dimensional assessment of ring-fault geometries and kinematics at active caldera volcanoes is typically limited by sparse field, geodetic or seismological data, or by only partial ring-fault rupture or slip. Here we use a novel combination of spatially dense InSAR time-series data, numerical models and sand-box experiments to determine the three-dimensional geometry and kinematics of a sub-surface ring-fault at Tendürek volcano in Turkey. The InSAR data reveal that the area within the ring-fault not only subsides, but also shows substantial westward-directed lateral movement. The models and experiments explain this as a consequence of a ‘sliding-trapdoor’ ring-fault architecture that is mostly composed of outward-inclined reverse segments, most markedly so on the volcano\\'s western flanks but includes inward-inclined normal segments on its eastern flanks. Furthermore, the model ring-fault exhibits dextral and sinistral strike-slip components that are roughly bilaterally distributed onto its northern and southern segments, respectively. Our more complex numerical model describes the deformation at Tendürek better than an analytical solution for a single rectangular dislocation in a half-space. Comparison to ring-faults defined at Glen Coe, Fernandina and Bárðarbunga calderas suggests that ‘sliding-trapdoor’ ring-fault geometries may be common in nature and should therefore be considered in geological and geophysical interpretations of ring-faults at different scales worldwide.

  13. Fluid-faulting evolution in high definition: Connecting fault structure and frequency-magnitude variations during the 2014 Long Valley Caldera, California, earthquake swarm

    Science.gov (United States)

    Shelly, David R.; Ellsworth, William L.; Hill, David P.

    2016-03-01

    An extended earthquake swarm occurred beneath southeastern Long Valley Caldera between May and November 2014, culminating in three magnitude 3.5 earthquakes and 1145 cataloged events on 26 September alone. The swarm produced the most prolific seismicity in the caldera since a major unrest episode in 1997-1998. To gain insight into the physics controlling swarm evolution, we used large-scale cross correlation between waveforms of cataloged earthquakes and continuous data, producing precise locations for 8494 events, more than 2.5 times the routine catalog. We also estimated magnitudes for 18,634 events (~5.5 times the routine catalog), using a principal component fit to measure waveform amplitudes relative to cataloged events. This expanded and relocated catalog reveals multiple episodes of pronounced hypocenter expansion and migration on a collection of neighboring faults. Given the rapid migration and alignment of hypocenters on narrow faults, we infer that activity was initiated and sustained by an evolving fluid pressure transient with a low-viscosity fluid, likely composed primarily of water and CO2 exsolved from underlying magma. Although both updip and downdip migration were observed within the swarm, downdip activity ceased shortly after activation, while updip activity persisted for weeks at moderate levels. Strongly migrating, single-fault episodes within the larger swarm exhibited a higher proportion of larger earthquakes (lower Gutenberg-Richter b value), which may have been facilitated by fluid pressure confined in two dimensions within the fault zone. In contrast, the later swarm activity occurred on an increasingly diffuse collection of smaller faults, with a much higher b value.

  14. EFECTO DEL CONTENIDO DE SODIO EN LA OBTENCIÓN DE Na+ -B-ALÚMINA UTILIZANDO EL MÉTODO DE PRECURSOR POLIMÉRICO

    Directory of Open Access Journals (Sweden)

    VANESSA RUIZ

    2011-01-01

    Full Text Available En este trabajo se muestran los resultados obtenidos al emplear el metodo de precursor polimerico (Pechini para sintetizar polvos ceramicos de Na + B Àalumina, utilizando sales inorganicas, tomando como parametro de estudio la cantidad inicial del precursor de sodio y su efecto sobre la fase cristalina obtenida al final del proceso. Los polvos fueron caracterizados utilizando espectroscopia Infrarroja (FTIR, Difraccion de Rayos X (DRX y Microscopia Electronica de Barrido (MEB. Se encontro que el efecto de la cantidad de sodio inicial en la muestra es determinante en la naturaleza del producto final obtenido. Utilizando la cantidad estequiometrica de NaOH requerida, para la obtencion del compuesto NaAl11O17, se obtuvo al final del proceso (1450oC a-alumina y B-alumina y/o Na2Al2xO3x1 en muestras tratadas termicamente entre 1000oC y 1350oC. Cuando se uso una mayor cantidad de NaOH, muestra no estequiometrica, se obtuvo un solido con el compuesto NaAl11O17 como fase mayoritaria.

  15. ESTUDO SENSORIAL DE QUEIJO SIMILAR AO MINAS PADRÃO COM LEITE DE OVELHA UTILIZANDO AGENTE COAGULANTE E COALHO

    Directory of Open Access Journals (Sweden)

    A. A. Gajo, L. R. Abreu

    2012-02-01

    Full Text Available No Brasil, o leite de ovelhas vem proporcionando certo interesse pelos institutos de pesquisa, devido a sua particular característica de rendimentos elevados na produção de queijos, além de conferir sabor e aroma peculiar aos produtos lácteos. No presente trabalho, objetivou-se averiguar a influência da utilização de três diferentes enzimas coagulantes na fabricação de queijos similar ao Minas Padrão utilizando leite de ovelhas. Foi utilizado coalho bovino (coalhopar®, composto aproximadamente de 80-85% de pepsina e 15-20% de quimosina (renina. Os agentes coagulantes empregados foram microbianos, sendo eles: genético (Chr-Hansen® e fúngico. A elaboração, análises químicas e teste sensorial dos queijos foram realizados no Departamento de Ciência dos Alimentos da Universidade Federal de Lavras. No teor de composição química dos queijos não apresentaram diferença significativa (P < 0,05 em todos os parâmetros analisados mediante aos tratamentos citados. As notas médias das amostras situaram-se na escala hedônica entre 5 e 7 (região da categoria indiferente e gostei moderadamente, respectivamente, apresentando médio índice de aceitabilidade dos queijos. O uso de agente coagulante microbiano (genético foi atribuído a melhor aceitação quanto ao parâmetro de textura. A utilização de agentes coagulantes microbianos fúngico e genético e coalho bovino não apresentaram diferenças sensoriais nos atributos de aparência, sabor e aspecto global nos queijos.

  16. Cinemática inversa de robot serial utilizando algoritmo genético basado en MCDS

    Directory of Open Access Journals (Sweden)

    Juan Jairo Vaca González

    2015-04-01

    Full Text Available Los robots manipuladores seriales son herramientas eficaces para realizar tareas repetitivas y de precisión en la industria, siempre que se comprenda la cinemática involucrada en el posicionamiento y orientación del efector final. Este artículo presenta una metodología para resolver el problema cinemático inverso de un robot serial (Melfa RV-2A utilizando un algoritmo genético (AG a partir del modelo cinemático directo Screws (MCDS. Para esto, se obtienen los parámetros Screw que modelan el robot, se calcula el espacio de trabajo asociado y se diseña el AG contemplando una función multi-objetivo de alcance de posición y orientación en que se sitúa el efector final, con respecto a una coordenada y orientación de un punto objetivo establecido. La validación del AG se realiza según la aptitud, el tiempo de convergencia y la cantidad de generaciones usadas por la función para alcanzar el objetivo. Por tanto, la implementación de un AG basado en un MCDS es una herramienta prometedora que podría utilizarse para calcular la cinemática inversa de robots seriales. Esta novedosa implementación permite establecer por primera vez la exposición matricial de un sistema cinemático directo para obtener la solución cinemática inversa de un robot serial. En consecuencia, se demuestra que esta es una metodología factible y eficiente para solucionar la cinemática inversa de cualquier tipo de robot manipulador.

  17. Estimativa do teor de água no solo utilizando dados de radar de abertura sintética

    Directory of Open Access Journals (Sweden)

    O. A. Máximo

    1999-09-01

    Full Text Available Em virtude da crescente demanda mundial por alimentos, um monitoramento eficaz e em larga escala da umidade do solo constitui fator de grande importância para a previsão de safras. Este trabalho teve por objetivo apresentar uma técnica para o cálculo do teor de água no solo, utilizando modelos preditivos de umidade do solo, baseados em dados de radar de abertura sintética (SAR. Foram utilizados dados do SAR a bordo do JERS-1 ("Japanese Earth Resources Satellite" e dois modelos empíricos. O primeiro relaciona o coeficiente de retroespalhamento com a permissividade complexa (modelo de Dubois, e o segundo relaciona a permissividade complexa com o teor de água do solo e algumas de suas características físico-hídricas, tais como percentagem de areia e argila (modelo de Hallikainen. Inicialmente, os dados do SAR/JERS-1 foram calibrados e, por meio do modelo de Dubois, foram calculados os valores de permissividade complexa. Para tanto, foi necessário inserir níveis estimados de rugosidade do solo. A partir destes resultados, utilizou-se o modelo de Hallikainen para calcular a umidade volumétrica. A análise geral dos resultados indica que a técnica de estimação de umidade do solo a partir de imagens de radar de abertura sintética, utilizada neste estudo, mostrou-se física e matematicamente exeqüível. No entanto, apresentou uma precisão moderada, não sendo ainda recomendada para o uso operacional no mapeamento de umidade do solo. A análise dos resultados revelou também que a precisão dos dados é bastante influenciada pela precisão dos valores de rugosidade introduzidos.

  18. Modelo para la evaluación del desempeño de los proveedores utilizando AHP

    Directory of Open Access Journals (Sweden)

    Juan Carlos Osorio Gómez

    2008-01-01

    Full Text Available Un elemento fundamental dentro de la gestión de proveedores de la empresa es la evaluación del desempeño del proveedor, en la cual se define si se están cumpliendo o no los acuerdos contractuales y si se está cumpliendo con los parámetros de desempeño esperados para el éxito de las operaciones de la compañía. Adicionalmente, como resultado de la evaluación, se pueden definir planes de mejoramiento y estrategias de negociación con los proveedores, lo cual se orienta a garantizar el éxito de la operación de toda la cadena de abastecimiento. Este artículo presenta un modelo para la evaluación del desempeño de los proveedores, utilizando como herramienta base, el proceso analítico jerárquico (Analytic Hierarchy Process-AHP, que consiste en la definición de los criterios para la evaluación de proveedores, la aplicación del Proceso Analítico Jerárquico (AHP en el árbol de criterios, para definir los diferentes pesos de los mismos, la definición de escalas de calificación para cada criterio y la presentación de los resultados del modelo. Se comentan también los resultados de un ejemplo de aplicación del modelo en una empresa del sector servicios de la ciudad de Cali en Colombia.

  19. FEM-based linear inverse modeling using a 3D source array to image magma chambers with free geometry. Application to InSAR data from Rabaul Caldera (PNG).

    Science.gov (United States)

    Ronchin, Erika; Masterlark, Timothy; Dawson, John; Saunders, Steve; Martí Molist, Joan

    2015-04-01

    In this study, we present a method to fully integrate a family of finite element models (FEMs) into the regularized linear inversion of InSAR data collected at Rabaul caldera (PNG) between February 2007 and December 2010. During this period the caldera experienced a long-term steady subsidence that characterized surface movement both inside the caldera and outside, on its western side. The inversion is based on an array of FEM sources in the sense that the Green's function matrix is a library of forward numerical displacement solutions generated by the sources of an array common to all FEMs. Each entry of the library is the LOS surface displacement generated by injecting a unity mass of fluid, of known density and bulk modulus, into a different source cavity of the array for each FEM. By using FEMs, we are taking advantage of their capability of including topography and heterogeneous distribution of elastic material properties. All FEMs of the family share the same mesh in which only one source is activated at the time by removing the corresponding elements and applying the unity fluid flux. The domain therefore only needs to be discretized once. This precludes remeshing for each activated source, thus reducing computational requirements, often a downside of FEM-based inversions. Without imposing an a-priori source, the method allows us to identify, from a least-squares standpoint, a complex distribution of fluid flux (or change in pressure) with a 3D free geometry within the source array, as dictated by the data. The results of applying the proposed inversion to Rabaul InSAR data show a shallow magmatic system under the caldera made of two interconnected lobes located at the two opposite sides of the caldera. These lobes could be consistent with feeding reservoirs of the ongoing Tavuvur volcano eruption of andesitic products, on the eastern side, and of the past Vulcan volcano eruptions of more evolved materials, on the western side. The interconnection and

  20. Movilidad, redes de intercambio y circulación de bienes en el sudoeste del Neuquén (Norpatagonia, Argentina: Los moluscos marinos del lago Traful Mobility, Exchange Networks And Circulation Of Goods In Southwestern Neuquén, Northern Patagonia, Argentina: The Marine Mollusks From Traful Lake

    Directory of Open Access Journals (Sweden)

    Mario Silveira

    2010-12-01

    Full Text Available Se determina la procedencia de fragmentos de moluscos marinos hallados en los aleros Los Cipreses y Lariviere, en el área del lago Traful, sur de la provincia de Neuquén. Estudios previos en áreas cercanas con mayor proximidad a la costa del océano Pacífico suponen que las piezas recuperadas evidencian contacto con grupos provenientes del lado occidental de la cordillera de Los Andes -Chile. En este trabajo se indica que parte de las valvas estudiadas corresponden a fósiles marinos o fluviales no identificados. Los fragmentos identificados corresponden al gasterópodo marino Adelomelon brasiliana procedente del Atlántico y al bivalvo Choromytilus chorus posiblemente del Pacífico. Estos datos, sumados a los recientes análisis sobre muestras de obsidiana procedentes de fuentes de aprovisionamiento del sudoeste neuquino que circularon grandes distancias hacia la costa atlántica, resaltan la complejidad y extensión de la movilidad humana y/o de las redes interregionales de intercambios.In this article the origin of fragments of marine shells found at Los Cipreses and Lariviere rock-shelters is presented. Consistent with studies by other authors in nearby areas in greater proximity to the Pacific coast, it was assumed that these fragments indicated contact with groups from the western side of the Chilean Andes. The results show that the shells correspond to marine or unknown fluvial fossils; a few pieces correspond to a marine gasteropod of great size, Adelomelon brasiliana, from the Atlantic Ocean and the bivalve Choromytilus chorus, probably from the Pacific. These data, and the recent analysis of samples of obsidian from sources located in southwestern Neuquén, which circulated far toward the Atlantic coast, highlight the complexity and extent of human mobility and interregional exchange networks.

  1. Protocolos utilizando Memoria Compartida

    OpenAIRE

    Cenci, Karina M.; Ardenghi, Jorge Raúl

    2000-01-01

    Un sistema de memoria compartida consiste de una colección de procesos en comunicación, como en un sistema de red. Pero en vez de enviar y recibir mensajes sobre un canal de comunicación, los procesos realizan operaciones instantáneas sobre datos compartidos. Los modelos para un sistema de memoria compartida pueden ser sincrónicos y asincrónicos. En el modelo sincrónico se asume que los componentes toman/ejecutan los pasos simultáneamente, esto es, la ejecución procede en completo sincr...

  2. multicast utilizando Simulated Annealing

    Directory of Open Access Journals (Sweden)

    Yezid Donoso

    2005-01-01

    Full Text Available En este artículo se presenta un método de optimización multiobjetivo para la solución del problema de balanceo de carga en redes de transmisión multicast, apoyándose en la aplicación de la meta-heurística de Simulated Annealing (Recocido Simulado. El método minimiza cuatro parámetros básicos para garantizar la calidad de servicio en transmisiones multicast: retardo origen destino, máxima utilización de enlaces, ancho de banda consumido y número de saltos. Los resultados devueltos por la heurística serán comparados con los resultados arrojados por el modelo matemático propuesto en investigaciones anteriores.

  3. Utilizando a Maquinaria Celular

    Directory of Open Access Journals (Sweden)

    Fernanda Serpa Cardoso

    2006-07-01

    Full Text Available The cell machinery, especially its molecular biology, is a subject of difficult comprehension and visualization due to its broadness and complexity. In face of this difficulty, the development of new teaching approaches that go beyond the traditional  lectures  and  textbooks  is  needed  to  deal  with  this  issue.  Educational  games  are  an  alternative  for  the teaching and learning processes, working as a tool that makes the comprehension of the subject contents easier and more enjoyable, at the same time it stimulates student's thinking, competition and cooperative work. To facilitate the teaching of Molecular Biology, a game called "Using the Molecular Biology" has been proposed. For its development, a data bank with 48 questions and answers was created based on College textbooks and web sites dealing with this issue.  The  game  uses  the  lymphocyte  B  as  a  cell  model  to  approach  the  processes  of  DNA  replication  and transcription,  and  RNA  translation,  which  are  involved in  the  synthesis  of antibodies. The  game  has  been  originally conceived as a complement for laboratory classes in the undergraduate medical courses at the Universidade Federal Fluminense.  However,  to  broaden  the  use  of  "Using  the  Molecular  Biology"  to  the  High  School,  a  survey  form  was elaborated  and  handed  out  to  nine  teachers  from  private  and  public  schools.  This  form  allowed  us  to  classify  the game  questions  into  three  difficulty  levels  for  teachers  and  students,  according  with  teacher's  opinion:  easy, intermediate, and difficult. This material has been offered to the schools registered in the "The future in the schools" Project, where  it was tested  and used  as  an educational  tool  complementary to the traditional  Biology  classes. The student's receptivity to and the efficacy of this support material have been evaluated.

  4. Atividade de extensão: estratégia para o intercâmbio de conhecimento entre os alunos de enfermagem Actividad de extensión: estrategia para el intercambio del conocimiento entre los alumnos de enfermería Extension cctivity: strategy of knowledge interchange among nursing students

    Directory of Open Access Journals (Sweden)

    Norma Valéria Dantas de Oliveira Souza

    2007-06-01

    Full Text Available Estudo qualitativo, descritivo, tipo estudo de caso, cujo objeto foi o intercâmbio de conhecimento teórico-prático estabelecido entre os bolsistas do projeto de extensão denominado "Orientando o cliente em situação cirúrgica para diferenciar o cuidado" e os internos de Enfermagem que estagiam nos cenários das enfermarias cirúrgicas do Hospital Universitário Pedro Ernesto. Objetivos: identificar e analisar as situações e modos de ensino-aprendizagem nas quais se estabelecem intercâmbios de conhecimento teórico-prático entre internos e bolsistas e discutir a importância do projeto de extensão como uma estratégia para aquisição de conhecimento teórico-prático. Aplicou-se uma entrevista semi-estruturada a quinze internos, e, após a análise de conteúdo, verificou-se que existiu intercâmbio de conhecimento quando da realização de grupos de orientação para clientes no pré-operatório, nas orientações individuais para o autocuidado no domicílio e através do material instrucional fornecido à clientela. Além disso, verificou-se que a atividade de extensão é uma importante estratégia que favorece o ensino-aprendizagem.Estudio cualitativo, descriptivo, del tipo estudio de caso, cuyo objeto fué el intercambio de conocimiento teórico-practico establecido entre los alumnos del proyecto de extensión llamado "Orientando el cliente en situación quirúrgica para distinguir el cuidado" y los internos de enfermería que practican en los escenarios de las Enfermarías Quirúrgicas del Hospital Universitario Pedro Ernesto (Rio de Janeiro - Brasil. Objetivo: identificar y analizar las situaciones y modos de enseñanza-aprendizaje, en las cuales se establecen intercambios de conocimiento teórico-práctico entre internos y practicantes y debatir la importancia del proyecto de extensión como una estrategia para adquisición de conocimiento teórico-práctico. Fue utilizada entrevista semiestructurada en quince internos y despu

  5. Oxygen isotopic and geochemical evidence for a short-lived, high-temperature hydrothermal event in the Chegem caldera, Caucasus Mountains, Russia

    Science.gov (United States)

    Gazis, Carey; Taylor, Hugh P.; Hon, Ken; Tsvetkov, Andrei

    1996-10-01

    Within the 2.8 Ma Chegem ash-flow caldera (11 × 15 km), a single cooling unit of rhyolitic to dacitic welded tuff more than 2 km thick is exposed in deep valleys incised during recent rapid uplift of the Caucasus Mountains. The intracaldera tuff is mineralogically fresh and unaltered, and is overlain by andesite lavas and cut by a resurgent granodiorite intrusion. Major- and trace-element compositions for a 1405-m stratigraphic section of intracaldera tuff display trends of upwardly increasing Na 2O, CaO, A1 2O 3, total Fe, MgO, TiO 2, Sr and Zr and decreasing SiO 2, K 2O and Rb. This mafic-upward zoning (from 76.1 to 69.9% SiO 2) reflects an inverted view of the upper part of the source magma chamber. Oxygen isotope studies of 35 samples from this 1405-m section define a striking profile with "normal" igneous δ18O values (+7.0 to +8.5) in the lower 600 m of tuff, much lower δ18O values (-4.0 to +4.3) in a 700-m zone above that and a shift to high δ18O values (+4.4 to +10.9) in the upper 100 m of caldera-fill exposure. Data from two other partial stratigraphic sections indicate that these oxygen isotope systematics are probably a caldera-wide phenomenon. Quartz and feldspar phenocrysts everywhere have "normal" igneous δ18O values of about +8.5 and +7.5, respectively, whereas groundmass and glass δ18O values range from -7.7 to +12.3. Consequently, the δ18O values of coexisting feldspar, groundmass and glass form a steep array in a plot of δfeldspar vs. δgroundmss/glass. Such pronounced disequilibrium between coexisting feldspar and groundmass or glass has never before been observed on this scale. It requires a hydrothermal event involving large amounts of low- 18O H 2O at sufficiently high temperatures and short enough time (tens of years or less) that glass exchanges thoroughly but feldspar does not. The most likely process responsible for the 18O depletions at Chegem is a very high temperature (500-600 °C), short-lived, vigorous meteoric

  6. Sintesis autopropagada a alta temperatura (SHS del masteralloy Fe(TiMoC utilizando ferroaleaciones

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    Erauskin, J. I.

    2009-06-01

    Full Text Available Titanium monocarbide TiC is very hard, stable both at high and low temperatures and relatively easy to synthesize from its constituent elements by SHS. Nevertheless, it is difficult to use, as alloying element, in the reinforcement of steels manufactured by liquid metallurgy due to its low wettability by molten steel. To achieve this purpose and due to its better wettability, it is more appropriate to use a master alloy formed by the complex carbide (TiMoC bonded in Fe. The simplest and most economic way to fabricate such a master alloy Fe(TiMoC is, again, by SHS, with the added advantage that it can be manufactured using the commercial ferroalloys FeTi and FeMo instead of the individual elements Fe, Ti and Mo. In this work, we describe such a process as well as the characteristics of the master alloy obtained.

    El carburo simple de titanio TiC es muy duro, estable, tanto a baja como a alta temperatura y, relativamente, fácil de sintetizar por SHS a partir de sus elementos. Sin embargo, debido a su baja mojabilidad por parte del acero fundido, este carburo es difícilmente aplicable, como material aleante, en el refuerzo de los aceros fabricados mediante el proceso de la metalurgia líquida. Para este propósito resulta más adecuada, por su mayor mojabilidad, la utilización de una aleación madre formada por el carburo complejo (TiMoC aglomerado en hierro. La manera más económica y sencilla de elaborar esta aleación madre Fe(TiMoC es también la del SHS y, además, utilizando como materias primas ferroaleaciones comerciales FeTi y FeMo en vez de los elementos individuales hierro, titanio y molibd eno. En el presente trabajo se describe dicho proceso, así como las características de la aleación madre obtenida.

  7. Recuperación de oro a partir de disoluciones de amoniaco y tiosulfato utilizando carbón activado

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    Vargas, C.

    2006-06-01

    Full Text Available The recovery of gold from solutions containing thiosulfate and ammonia using granular activated carbon was studied, evaluating the adsorption and elution stages. The influence of ammonia and thiosulfate concentration and the presence of impurities such as copper and zinc were also evaluated. In the presence of ammonia there was a concentration which maximized the adsorption of gold, while thiosulfate and impurities presence was harmful for the adsorption of gold. During elution, ammonia and thiosulfate concentration, pH regulator and temperature were evaluated. Ammonia favored the process as long as thiosulfate showed a maximum starting from which the elution diminishes. The effect of the pH regulator was very important; If was revealed that when the pH was regulated with caustic ammonia, a synergic effect appeared which favored the elution. Temperature favored the elution process, with activation energy of 9.13 kJ/mol.

    Se estudió la recuperación de oro de disoluciones de tiosulfato y amoniaco, utilizando carbón activado en gránulos, evaluando las etapas de adsorción y desorción. En la etapa de adsorción se evaluaron la concentración de amoniaco, de tiosulfato y de impurezas como cobre y cinc. En las condiciones experimentales ensayadas se encontró que, en presencia de amoniaco, existe una concentración óptima que maximiza la adsorción de oro, mientras que la presencia de tiosulfato e impurezas, tales como cobre y cinc, es perjudicial para la adsorción de oro. Para la desorción se evaluó la concentración de amoniaco, de tiosulfato, el regulador de pH y la temperatura. El amoniaco favoreció el proceso, en tanto que el tiosulfato presentó un máximo a partir del cual la desorción disminuyó. El efecto del regulador de pH fue muy importante, determinándose que cuando el pH era controlado con hidróxido de amonio, se presentaba un efecto sinérgico que favorecía la desorción. La temperatura favoreció el proceso de

  8. Cuantificación de AIA por HPLC utilizando el método del estándar interno

    Directory of Open Access Journals (Sweden)

    Grolamys Castillo

    2005-01-01

    Full Text Available El Ácido Indol Acético (AIA pertenece al grupo de las auxinas, sustancias endógenas bioactivas presentes en las plantas, que controlan diversos procesos del metabolismo vegetal. En general, estas sustancias tienen como efecto estimular el alargamiento celular o favorecer su depresión dependiendo de la concentración empleada. La síntesis microbiológica de estas sustancias resulta de gran importancia ya que su aplicación permite el aumento de los rendimientos y la calidad de las cosechas en la agricultura. La Cromatografía Líquida de Alta Resolución (HPLC es actualmente un método de rutina para la separación de fitohormonas, siendo la fase reversa C18 la más usada y reportada con estos fines. Se muestra el estudio realizado para la cuantificación del contenido de AIA presente en caldos de fermentación usando el Ácido Indol Propiónico (AIP como estándar interno, sobre la base de un método de HPLC ya desarrollado, utilizando la técnica de supresión iónica, sin necesidad de derivatizar. La fase móvil consistió en una relación metanol-ácido acético 0,5 (v/v (6,4 a un flujo de 0,7 mL/min. La detección se realizó por fluorescencia a una A de excitación de 280 nm y de emisión de 340 nm, a una sensibilidad baja. Las muestras de caldos analizados mostraron un valor medio de AIA en el extracto de 28 ppm. Se realizó el estudio de Repetibilidad para una muestra que se extrajo, por 10 veces consecutivas y se obtuvo un CV del 1 %.

  9. Using Computer Resources (Spreadsheet to Comprehend Rational Numbers Utilizando recursos computacionais (planilha na compreensão dos Números Racionais

    Directory of Open Access Journals (Sweden)

    Rosane Ratzlaff da Rosa

    2008-12-01

    Full Text Available This article reports on an investigation which sought to determine if the use of spreadsheets in the teaching of rational numbers in elementary education contributes to learning and improved learning retention. The study was carried out with a sample of students from two sixth-grade classes in a public school in Porto Alegre. Results indicated that the use of spreadsheets favored learning and made the classes more participatory for the students, who were able to visualize the processes they were working with. A second test applied five months after the first test showed that students who used the spreadsheets had greater learning retention of the contents. The results also show that the students felt comfortable with the technology, and almost all reported that they were more motivated by the use of computers in the classroom, despite less-than-ideal laboratory conditions. Key-words: Rational Numbers. Teaching with Spreadsheet. Teaching Rational Numbers using Spreadsheet.Este artigo relata uma investigação que procurou determinar se o uso de planilha como recurso no ensino dos números racionais na Educação Básica contribui para a aprendizagem e uma maior retenção dessa aprendizagem a médio prazo. A investigação foi realizada com uma amostra de alunos de duas turmas da sexta série de uma escola pública de Porto Alegre. Os resultados indicaram que o uso da planilha favorece a aprendizagem e torna as aulas mais participativas para os alunos, que conseguiram visualizar os processos com os quais trabalharam. Um segundo teste aplicado cinco meses após o primeiro mostrou que os alunos que utilizaram a planilha apresentaram uma maior retenção do conteúdo. Os resultados apontam ainda que os alunos se sentem à vontade com a tecnologia e quase todos disseram ficarem mais motivados com as aulas utilizando o computador apesar das condições do laboratório utilizado não ser a ideal. Palavras-chave: Números Racionais. Ensino com a

  10. Classificação de estratos florestais utilizando redes neurais artificiais e dados de sensoriamento remoto

    Directory of Open Access Journals (Sweden)

    Wanderson Gonçalves e Gonçalves

    2016-06-01

    Full Text Available O presente estudo objetivou a classificação de tipologias florestais por meio de redes neurais artificiais utilizando dados provenientes de um inventário florestal, fornecido pelo Instituto de Desenvolvimento Florestal e da Biodiversidade do Estado do Pará (IDEFLOR-BIO, e das bandas 3, 4 e 5 do TM do satélite Landsat 5. As informações provenientes das imagens de satélite foram extraídas por meio do aplicativo QGIS 2.8.1 Wien e utilizadas no banco de dados para o treinamento das redes neurais pertencentes às ferramentas do software MATLAB(r R2011b. Foram treinadas redes neurais como classificadores de dois tipos florestais: Floresta Ombrófila Densa de Terras baixas Dossel emergente (Dbe e Floresta Ombrófila Densa Terras baixas Dossel emergente mais Aberta com palmeiras (Dbe + Abp no conjunto de glebas estaduais Mamuru-Arapiuns, Pará, e avaliadas usando os indicadores matriz de confusão, cálculo de acurácia global, coeficiente Kappa e o gráfico de características do receptor operacional (ROC. O melhor resultado de classificação foi obtido por meio da rede neural probabilística de função de base radial (RBF "newpnn", com uma acurácia global de 88%, e coeficiente Kappa de 76%, sendo avaliado como um classificador muito bom, evidenciando a aplicação dessa metodologia na análise de áreas com potencial para prestar serviços ecossistêmicos e, principalmente, na prestação de serviços ambientais em áreas antrópicas que adotam sistema de produção agropecuária com baixa emissão de carbono na Amazônia.

  11. EVALUACIÓN DE TRES METODOLOGÍAS DE RECUPERACIÓN DE EMBRIONES EN CANINOS UTILIZANDO UN MODELO POSTMORTEM

    Directory of Open Access Journals (Sweden)

    Claudia Jiménez E

    2008-12-01

    Full Text Available Objetivo. Evaluar tres técnicas de recuperación de embriones, utilizando como modelos de simulación oocitos desnudos introducidos en úteros recuperados post–mortem. Materiales y métodos. Se introdujeron 10 oocitos en el extremo ovárico de cada cuerno. El tratamiento 1 (T1 consistió en realizar una punción a nivel del extremo ovárico de cada cuerno para introducir el medio de lavado. Se incidió la base de cada cuerno para ubicar un catéter TOMCAT 8-Fr, recuperando el medio en una caja de petri. En el tratamiento 2 (T2 se realizó una punción en el extremo ovárico de cada cuerno pero la recuperación de los oocitos se realizó con un catéter de 56 cm de longitud que se pasó transcervicalmente hasta la base de cada cuerno. En el tratamiento 3 (T3 se utilizó el mismo tipo de catéter por vía transcervical y el lavado y la recuperación se realizó a través del mismo catéter. Resultados. El número de estructuras recuperadas fue de 7.3 ± 2.4 (73% para el T1; 8.5 ± 1.9 (85% para el T2 y de 5.8±2.2 (58% para el T3. La tasa de recuperación fue similar para T1 y T2, pero significativamente mayores que para el T3 (p>0.01. Conclusiones. Las técnicas que se proponen son menos invasivas y tienen resultados comparables a otros estudios donde realizan histerectomía y laparotomía. Con este tipo de técnicas, se disminuye el trauma generado por incisiones quirúrgicas y la posible generación de adherencias. Adicionalmente permitirían realizar recuperaciones de embriones no quirúrgicas en caninos.

  12. Evaluación del cultivo de la dorada ( Brycon moorei sinuensis en jaulas flotantes utilizando cuatro alimentos concentrados.

    Directory of Open Access Journals (Sweden)

    Robinsón Rosado

    2003-12-01

    Full Text Available El presente estudio se inició el 30 de septiembre del2000 con el cultivo de Dorada (Brycon mooreisinuensis en jaulas flotantes en el reservorio de laGranja Piscícola Tamarindo (El Espinal, Colombia,utilizando cuatro alimentos concentrados durante 180días. Se determinó el crecimiento mediante laganancia en longitud, ganancia en peso, tasa decrecimiento específico, sobre-vivencia final, biomasatotal, factor de condición, factor de conversiónalimenticia. Se sembraron 816 juveniles con longitudpromedio de 17.8 cm y peso promedio de 78.9 g,divididos en cuatro tratamientos con densidad desiembra de 25 peces/cm3 y tres réplicas cada uno.Las dietas balanceadas (proteína bruta y la cantidadde energía (Kcal/Kg suministrada fueron: Tratamiento1: 20% y 2637; tratamiento 2: 32% y 3127;tratamiento 3: 28% y 2852; y tratamiento 4: 24% y2751, respectivamente. El diseño experimental fuecompletamente aleatorio y se aplicó la técnica deanálisis de varianza a los datos biométricos yparámetros físico-químicos. Como prueba designificancia se usó la prueba de Tukey-Kramer con95% de confiabilidad. El modelo matemático de VIONBERTALANFY y la transformación de FOR-WALFORDfueron válidos para el ajuste de las curvas decrecimiento en longitud, peso y la relación longitud– peso. Se puede afirmar que la Dorada consumiólas dietas de origen vegetal de igual manera que lasde origen animal, sin embargo la dieta del 28% deproteína bruta (tratamiento 3 muestra los mejoresresultados, sin diferencias significativas entretratamientos (p > 0.05. De acuerdo con la literaturacitada no hay investigaciones que muestren losrequerimientos nutricionales óptimos para laalimentación de esta especie. En todos los trabajosanteriores, la ganancia de peso diaria fue baja, peromejores que las obtenidas en esta investigación.Mientras que el rendimiento en biomasa fue mayorque los reportados para cultivo en tierra, para todoslos tratamientos en este estudio fue muy bajo.

  13. Interfaz Gráfica Computacional para Destilación Multicomponente utilizando Métodos Cortos

    Directory of Open Access Journals (Sweden)

    A. Osorio Mirón

    2011-12-01

    Full Text Available En este trabajo, se elaboró una interfaz gráfica que determina por medio de simulación en estado estacionario el número de platos necesarios en el proceso de destilación multicomponente, así como la composición en el flujo de destilado y fondos de una torre de destilación utilizando métodos cortos. La interfaz gráfica de usuario, se construyó en el lenguaje de programación Python 2.5, permite presentar los datos de entrada y salida para el caso de columnas de destilación operando en régimen permanente. Los resultados del uso de la interfaz gráfica muestran una forma simple de realizar diseños preliminares de torres de destilación y su potencialidad como material de apoyo para el estudio y comprensión de conceptos básicos en destilación multicomponente. En un trabajo posterior se podrá visualizar el desempeño del modelo dinámico a través de perturbaciones programadas en las condiciones de operación.   Palabras claves: destilación multicomponente; métodos cortos; interfaz gráfica de usuario; Phyton 2.5.In this work, we developed a graphical interface that determines by steady-state simulation the number of plates required for multicomponent distillation process and the composition of distillate and bottoms flow of a distillation tower using short-cut methods. The graphical user interface was built in the programming language Python 2.5, allows to present the input and output data for the case of distillation columns operating in steady state. The results of using the graphical interface shows a simple way to make preliminary designs of distillation towers and its potential as support material for the study and understanding of basic concepts in multicomponent distillation. In a later work it will can display the dynamic model performance through scheduled disturbances in operating conditions.   Keywords: multicomponent distillation; shorcut methods;graphical user interface; Phyton 2.5.

  14. Arkashin (A) to Zavarzin (Z) Geochemical and Microbiological Characterization of Core Samples Collected at Two Thermal Pools in Uzon Caldera, Kronotsky Zapovednik, Kamchatka

    Science.gov (United States)

    Burgess, E. A.; Unrine, J.; Neal, A. L.; Samarkin, V.; Joye, S. B.; Wiegel, J.

    2006-12-01

    Sulfate-reduction by thermophilic prokaryotes may contribute to sulfide mineralization in volcanically-derived hydrothermal fields such as those found in the Uzon Caldera, Kamchatka, Far East Russia. In August 2005, core samples were taken from two chemically distinct thermal pools in Uzon; Arkashin Shurf which is ~1 m2, orange and enriched in arsenic (As), and Zavarzin II Spring which is ~10 m2, yellow and enriched in sulfur (S). Cores at both pools had distinct strata delineated by changes in color and texture. Subsamples of these strata were analyzed to examine changes in sediment and pore water chemistry, mineralogy, in situ sulfate-reduction rates (SRR), and prokaryote community structure with depth. We hypothesized that there would be a shift from oxidized to reduced species in the pore water samples with increasing depth. Although the concentrations of some oxidized aqueous species, such as arsenate, increased with depth, this trend was associated with changes in total arsenic concentration and may reflect of heterogeneous plumbing among thermal fields in the caldera. Mineralized elements precipitating with sulfide produced from sulfate reduction should exhibit decreasing pore water and rising sediment concentrations associated with increased SRR, in zones of mineralization. A dramatic increase in aqueous arsenic concentration with increasing depth in the upper strata in Arkashin dropped precipitously in the next stratum and had an associated increase in both SRR and sediment arsenic concentration. The As-S mineral realgar was identified in Arkashin samples by Raman spectroscopy. Only elemental sulfur was identified in Zavarzin samples from Raman spectra. The absolute value of SRR was higher in Arkashin, 2.0 nmol-cm-3hr^{- 1}, than in Zavarzin, 0.3 nmol-cm-3hr-1. Overall, SRR were much lower than anticipated. In Zavarzin, sulfate-reduction occurred at multiple depths. Sulfate-reduction in Arkashin may be restricted to a specific depth due to the presence of

  15. Asignación de tareas a procesadores en un sistema distribuido de tiempo real duro utilizando algoritmos genéticos y lógica difusa

    OpenAIRE

    Cayssials, Ricardo; Orozco, Javier D.; Ferro, Edgardo

    1997-01-01

    Se presenta un método basado en algoritmos genéticos para atacar el problema de asignación de un conjunto de tareas apropiativas, sobre un conjunto de procesadores distribuidos que deben trabajar en un entorno de tiempo real duro. Las tareas son cooperativas y utilizan como vía de comunicación una red local. Los coeficientes que ponderan la función de costo del algoritmo genético son calculados utilizando operadores difusos. Sobre el sistema existe un conjunto de restricciones que debe ser sa...

  16. Radiografía de un margen continental utilizando campos potenciales y espesor de sedimentos: el Margen Atlántico Ibérico

    OpenAIRE

    Catalán-Morollón, Manuel; Martos, Y. M.; Martín-Davila, J.; Muñoz-Martín, A.; Carbó, A.; Druet, M

    2015-01-01

    [ES] El presente estudio realiza una revisión del estado del conocimiento en el Margen Atlántico Ibérico atendiendo a las tres provincias en las que clásicamente se sub-divide éste: margen gallego, planicie abisal suribérica, y planicie abisal del Tagus, utilizando como fuente de información datos de campos potenciales e información derivada de espesor de sedimentos. Se estudian las características de su basamento, estableciendo límites para la extensión de la corteza continental,...

  17. Radiografía de un margen continental utilizando campos potenciales y espesor de sedimentos: el Margen Atlántico Ibérico

    OpenAIRE

    Catalán, M.; Martos, J.M.; Martín-Davila, J.; Muñoz Martín, Alfonso; Carbó Gorosabel, Andrés; Druet, María

    2015-01-01

    El presente estudio realiza una revisión del estado del conocimiento en el Margen Atlántico Ibérico atendiendo a las tres provincias en las que clásicamente se sub-divide éste: margen gallego, planicie abisal suribérica, y planicie abisal del Tagus, utilizando como fuente de información datos de campos potenciales e información derivada de espesor de sedimentos. Se estudian las características de su basamento, estableciendo límites para la extensión de la corteza continental, y la amplitud de...

  18. Mejoramiento del proceso de granallado para resortes de ballesta utilizando medición de esfuerzos residuales por difracción de rayos x

    OpenAIRE

    Hernández, Héctor; Viloria, Alexander; Arango, Yulieth; Jiménez, Augusto; Mendoza, Henry; Cadena, Jhon

    2010-01-01

    Se midieron diferentes perfiles de esfuerzos residuales por difracción de rayos X en las zonas cercanas a la superficie de un acero AISI-SAE 5160H empleado en la fabricación de resortes de ballesta, utilizando diferentes condiciones de granallado y desarrollando un diseño de experimentos para encontrar condiciones de proceso que ofrezcan intensidades Almen y perfiles de esfuerzos residuales en compresión adecuados. Por último se escogieron las combinaciones de variables que tienden a presenta...

  19. Atribución inequívoca de las señales de RMN de un neolignano arilnaftalénico utilizando espectros bidimensionales

    Directory of Open Access Journals (Sweden)

    Juan C. Martínez V.

    2010-05-01

    Full Text Available La atribución sin ambigüedad de cada una de las señales de los espectros de RMN 1H y 13C del 2,3-dimetil-7-hidroxi-6-metoxi-1-(3', 4' - metilenodioxifenil naftaleno, fue realizada por medio de sus espectros bidimensionales de correlación homonuclear 1H-1H y de correlación heteronuclear 1C y 3H obtenido utilizando en la respectiva secuencia de pulsos tiempos de espera correspondientes

  20. Resistência ao cisalhamento da colagem com compósitos utilizando potencializador de adesão Shear bond strength of composites using an adhesion booster

    OpenAIRE

    Edivaldo de Morais; Fábio Lourenço Romano; Lourenço Correr Sobrinho; Américo Bortolazzo Correr; Maria Beatriz Borges de Araújo Magnani

    2011-01-01

    OBJETIVO: avaliar a resistência ao cisalhamento dos compósitos Transbond XT e Concise Ortodôntico utilizando o potencializador de adesão Ortho Primer. MÉTODOS: a amostra consistiu de 90 incisivos bovinos divididos em seis grupos (n=15). Todos os dentes receberam profilaxia com pedra-pomes e condicionamento do esmalte com ácido fosfórico. No Grupo I, utilizou-se Transbond XT de maneira convencional. O Grupo II foi semelhante ao I, porém, aplicou-se o Ortho Primer ao invés do XT Primer. No Grup...

  1. Un modelo de sistema dinámico híbrido utilizando el enfoque de la lógica difusa

    OpenAIRE

    Germán García Benítez; Carlos Vera Estrada

    2010-01-01

    Se presenta un modelo de sistema dinámico híbrido utilizando la lógica difusa. Para lograr esto se hace una breve descripción de los principales enfoques que se tienen en la actualidad de los sistemas dinámicos híbridos desarrollando las ecuaciones básicas de los bloques que conforman el modelo. Actualmente la teoría del control se ha centrado en el estudio por separado de la dinámica continua y la dinámica discreta; sin embargo, es necesario introducir el estudio de la combinación de ambos ...

  2. Diseño de una experiencia interactiva multimedia en el espacio utilizando sensores de ultrasonido Design of interactive multimedia experience in the space using ultrasound sensors

    OpenAIRE

    Galeano Roylan; Restrepo Juliana; Trujillo Gonzalo; Franco Higuita Juan Fernando

    2009-01-01

    El objetivo del trabajo fue diseñar una experiencia multimedia interactiva en el espacio, para construir un procedimiento que permita elaborar este tipo de proyectos, entendiendo los roles de las diferentes disciplinas involucradas. Se diseñó un instrumento multimedia que traducía los movimientos de las manos, en melodías acompañadas de animaciones, utilizando sensores de ultrasonido. Se hallaron cuatro etapas: Indagación, creación, materialización y evaluación, que involucraron varios diseña...

  3. Estudio cinético de una fermentación alcohólica utilizando miel de abejas como sustrato

    Directory of Open Access Journals (Sweden)

    José Ángel Gómez

    2011-06-01

    Full Text Available El artículo describe un estudio cinético de una fermentación alcohólica utilizando miel de abejas como sustrato; para este efecto se realizaron nueve fermentaciones en proceso discontinuo con un volumen, de 10 L, siguiendo el comportamiento de las concentraciones de sustrato, biomasa y producto en el tiempo. Se evaluó la conveniencia de factores como la agitación y la adición de nutrientes, además, se observa el efecto de las concentraciones iniciales de sustrato e inocula y el tipo de miel.

  4. Avaliação de Micro e Pequenas Empresas Utilizando a Metodologia Multicritério e o Método do Fluxo de Caixa Descontado

    OpenAIRE

    Marcus Vinicius Andrade de Lima; Carlos Rogério Montenegro de Lima; Ademar Dutra; Ana Lúcia Miranda Lopes

    2010-01-01

    Neste artigo é apresentada uma contribuição ao método do fluxo de caixa descontado utilizando a metodologia multicritério de apoio à decisão. Essa metodologia incorpora variáveis de natureza qualitativa e subjetiva ao método tradicional do fluxo de caixa descontado utilizado na avaliação de empresas. Para ilustrar o método proposto foi realizado um estudo descritivo de natureza exploratória aplicado a um multicaso. A intervenção foi em Micro e Pequenas Empresas (MPE) do ramo químico, farmacêu...

  5. Understanding the Dynamics of the February-April 2007 Eruptions of the Piton de la Fournaise and the Related Caldera Collapse from a Single Very Broad-band Seismic Station

    Science.gov (United States)

    Fontaine, F. R.; Roult, G. C.; Michon, L.; Barruol, G.; Ferrazzini, V.; di Muro, A.; Reymond, D.; Peltier, A.; Staudacher, T.

    2013-12-01

    Seismic records from the RER very broad-band seismic station (La Réunion Island) belonging to the GEOSCOPE network are investigated to understand the eruptive succession (February to May) of Piton de la Fournaise and the caldera collapse episode of April 2007. Data first indicate that the short-lived, small volume, summit eruption of February 18 occurred during a phase of continuous inflation initiated in end of January 2007. Inflation decelerated around 2 weeks before a second short-lived small volume eruption on March 30-31 on the SE flank, which was coeval with a sudden, large deflation of the edifice. Deflation rate, which was stabilized at a relatively low level, increased anew on April 1 while no magma was emitted, followed on April 2 by a distant and one of the most voluminous eruptions of the last two centuries at La Réunion Island. The RER station shows that very long period (VLP) and ultra long period (ULP) events developed during this period. Seven ULP events preceded the caldera collapse and 48 ones occurred during the caldera collapse over 9 days, most of which during the first 30 hours. A thorough examination of the seismic signal corrected from the tide effects shows that each collapse event was coeval with VLP and ULP signals. Each repeating individual collapse showed similar ULP and VLP signals characterized by periods of ~ 500 s and ~ 7 s, respectively. Polarization measurements (back-azimuth) of the ULP clearly point toward a source located beneath the Dolomieu crater. The strikingly constant duration of the VLP signals (around 20 s) related to the collapse events and occurring before the collapse initiation suggests a physical control of the volcanic edifice. Waveforms and spectrograms of the various caldera collapse events show very homogeneous patterns, suggesting a similar and repeating volcano-tectonic process for the formation of the VLP signals events. Although tilt may be responsible of part of the ULP signals observed during the

  6. Geomorfología de la región de los lagos Moquehue y Aluminé: consideraciones acerca de las propuestas Calderas Meseta del Arco y Nacimientos del Aluminé (Neuquén

    Directory of Open Access Journals (Sweden)

    Emilio F. González Díaz

    2010-05-01

    Full Text Available Se exponen elementos de juicio geomórficos y estructurales, que avalan la morfogénesis glaciaria de la depresión en artesa que aloja la cuenca lacustre Moquehue-Aluminé, ubicada en la cordillera neuquina (38°30´S, adyacente al límite internacional. Trabajos anteriores distinguen en la región dos calderas de un gran complejo volcánico plio-cuaternario, situado al este del frente volcánico actual e integrado por nueve depresiones caldéricas y cuerpos dómicos asociados. En el área de estudio sólo la caldera de Pino Hachado tiene la validez necesaria, cuestionándose el reconocimiento de las calderas denominadas Nacimientos del Aluminé y Meseta del Arco, al tiempo que se avala el origen erosivo de las abruptas escarpas orientales que marginan el plateau de Lonco Luan-Meseta del Arco, las que fueran interpretadas como márgenes de las sugeridas calderas. Se analizan las fases o tipología del englazamiento pleistoceno local, su extensión, las direcciones de los principales movimientos de su flujo y su más que probable aporte de hielo por difluencia, a un contemporáneo englazamiento en Chile (laguna Icalma. Se describen aspectos de la morfogenia volcánica cenozoica y otros más locales de la remoción en masa y el proceso eólico. Se incorporan breves comentarios acerca de un propuesto drenaje atlántico de un río Bío Bío preglaciario y se cuestiona aquellos antecedentes que avalan la extensión en la región de la fosa Bío Bío-Aluminé y la presencia de las citadas calderas. Una serie de perfiles esquemáticos topográfico-geológicos contribuyen a dicho cuestionamiento.

  7. Monitoreo de un sistema de secado de bagazo acoplado a una caldera en un ingenio de México Monitoring of a bagasse drying system attached to a boiler in a sugar mill in Mexico

    Directory of Open Access Journals (Sweden)

    Federico J. Franck Colombres

    Full Text Available Se evaluó el desempeño de un secador de bagazo diseñado por la Estación Experimental Agroindustrial Obispo Colombres, acoplado a una caldera bagacera convencional en un ingenio de México (caldera Nº 5. Para ello, se realizaron ensayos de mediciones y balances de materia y energía, para la caldera operando con el secador y sin él en funcionamiento. La caldera Nº 5, de una producción nominal de 60 t/h de vapor y una presión máxima de trabajo de 29 bar, cuando fue alimentada únicamente con bagazo húmedo pudo generar como máximo 33 t/h de vapor a 19 bar y 269ºC, con un rendimiento energético de 60,4% y un índice de generación de 1,6 kg de vapor/ kg de bagazo. Con la adición del secador, se logró secar 28,6 toneladas de bagazo de 50,2% a 30,4% de humedad. Aproximadamente un 72% de este bagazo presecado se mezcló con bagazo húmedo y se utilizó para alimentar la caldera, produciéndose así 58,4 t/h de vapor; es decir, 77% más de vapor que sin secador. El rendimiento energético del sistema caldera-secador fue de 73,6%, un 21,8% superior al de la caldera sin secador, mientras que el índice de generación fue de 2,0 kg de vapor/ kg de bagazo, 25% mayor que el de la caldera original. Este aumento en la producción de vapor permitió sacar de servicio a la caldera Nº 6, que producía aproximadamente 20 t/h de vapor, con un rendimiento similar al de la caldera Nº 5 sin secador. Estas mejoras dieron como resultado, un ahorro de energía de 45,4 MJ/h, aproximadamente un 18% respecto a la energía consumida por ambas calderas (Nº 5 y Nº 6 cuando no funcionaba el secador. Este ahorro equivale a 1103 l/h de "fuel oil", es decir, alrededor de 1,5 millones de dólares por zafra.A bagasse dryer designed by Estación Experimental Agroindustrial Obispo Colombres was attached to a conventional bagasse boiler (Boiler No. 5 in a sugar mill in Mexico for evaluation. Measurement tests and material and energy balances for the boiler operating

  8. Warm brine lakes in craters of active mud volcanoes, Menes caldera off NW Egypt: evidence for deep-rooted thermogenic processes

    Science.gov (United States)

    Dupré, Stéphanie; Mascle, Jean; Foucher, Jean-Paul; Harmegnies, François; Woodside, John; Pierre, Catherine

    2014-06-01

    The Menes caldera is a fault-controlled depression (~8 km in diameter) at ~3,000 m water depth in the western province of the Nile deep-sea fan off NW Egypt, comprising seven mud volcanoes (MVs) of which two are active. Based on multichannel and chirp seismic data, temperature profiles, and high-resolution bathymetric data collected during the 2000 Fanil, 2004 Mimes and 2007 Medeco2 expeditions, the present study investigates factors controlling MV morphology, the geometry of feeder channels, and the origin of emitted fluids. The active Cheops and Chephren MVs are 1,500 m wide with subcircular craters at their summits, about 250 m in diameter, generally a few tens of metres deep, and filled with methane-rich muddy brines with temperatures reaching 42 °C and 57 °C respectively. Deployments of CTDs and corers with attached temperature sensors tracked these warm temperatures down to almost 0.5 km depth below the brine lake surface at the Cheops MV, in a feeder channel probably only a few tens of metres wide. Thermogenic processes involve the dissolution of Messinian evaporites by warm fluids likely sourced even deeper, i.e. 1.7 and 2.6 km below the seabed at the Cheops and Chephren MVs respectively, and which ascend along listric faults. Seepage activity appears broadly persistent since the initiation of mud volcanism in the Early Pliocene, possibly accompanied by lateral migration of feeder channels.

  9. Exploiting the outcome of FUTUREVOLC: The 2014-2015 rifting event, effusive eruption and gradual caldera collapse at Bardarbunga volcanic system, Iceland

    Science.gov (United States)

    Sigmundsson, Freysteinn; Vogfjord, Kristin S.; Gudmundson, Magnus T.; Ofeigsson, Benedikt G.; Dumont, Stéphanie; Parks, Michelle; Jonsdottir, Kristin; Hooper, Andrew; Hreinsdottir, Sigrun; Rafn Heimisson, Elias; White, Robert; Agustsdottir, Thorbjorg; Bean, Chris; Loughlin, Susan C.; Petur Heidarsson, Einar; Barsotti, Sara; Roberts, Matthew; Ripepe, Maurizio; Ilyinskaya, Evgenia; Consortium, Futurevolc

    2016-04-01

    Activity in the Bardarbunga volcanic system in Iceland 2014-2015 included major lava eruption (~1.5 km3) and gradual caldera collapse (~66 m), connected by a 50-km-long laterally injected dyke that formed mostly over 2-4 weeks after onset of activity on 16 August 2014. This rifting event is the main magmatic activity studied by the FUTUREVOLC project, a 3.5 year, 26-partner project funded by FP7 Environment Programme of the European Commission, addressing topic "Long-term monitoring experiment in geologically active regions of Europe prone to natural hazards: the Supersite concept. The project end is 31 March 2016 and it had aims to (i) establish an innovative volcano monitoring system and strategy, (ii) develop new methods for near real-time integration of multi-parametric datasets, (iii) apply a seamless transdisciplinary approach to further scientific understanding of magmatic processes, and (iv) to improve delivery, quality and timeliness of transdisciplinary information from monitoring scientists to civil protection. A review will be presented on how FUTUREVOLC has contributed to the response and study of the Bardarbunga activity and other events in Iceland during the project period.

  10. Monitoring the hydrologic system for potential effects of geothermal and ground-water development in the Long Valley caldera, Mono County, California, U.S.A.

    Science.gov (United States)

    Farrar, C.D.; Lyster, D. L.

    1990-01-01

    In the early 1980's, renewed interest in the geothermal potential of the Long Valley caldera, California, highlighted the need to balance the benefits of energy development with the established recreational activities of the area. The Long Valley Hydrologic Advisory Committee, formed in 1987, instituted a monitoring program to collect data during the early stages of resource utilization to evaluate potential effects on the hydrologic system. Early data show declines in streamflow, spring flow, and ground-water levels caused by 6 years of below-average precipitation. Springs in the Hot Creek State Fish Hatchery area discharge water that is a mixture of nonthermal and hydrothermal components. Possible sources of nonthermal water have been identified by comparing deuterium concentrations in streams and springs. The equivalent amount of undiluted thermal water discharged from the springs was calculated on the basis of boron and chloride concentrations. Quantifying the thermal and nonthermal fractions of the total flow may allow researchers to assess changes in flow volume or temperature of the springs caused by groundwater or geothermal development.

  11. Warm Brine Lakes in Craters of Active Mud Volcanoes, Menes Caldera off NW Egypt: Evidence for Deep-Rooted Thermogenic Processes

    Science.gov (United States)

    Dupré, S.; Mascle, J.; Foucher, J. P.; Woodside, J. M.; Pierre, C.

    2015-12-01

    The Menes caldera is a fault-controlled depression (~8 km in diameter) at ~3,000 m water depth in the western province of the Nile deep-sea fan off NW Egypt, comprising seven mud volcanoes (MVs) of which two are active. Based on multichannel and chirp seismic data, temperature profiles, and high-resolution bathymetric data collected during several oceanographic expeditions, the present study investigates factors controlling mud volcano morphology, the geometry of feeder channels, and the origin of emitted fluids (Dupré et al. 2014). The active Cheops and Chephren mud volcanoes are 1,500 m wide with subcircular craters at their summits, about 250 m in diameter, generally a few tens of metres deep, and filled with methane-rich muddy brines with temperatures reaching 42 °C and 57 °C respectively. Deployments of CTDs and corers with attached temperature sensors tracked these warm temperatures down to almost 0.5 km depth below the brine lake surface at the Cheops mud volcano, in a feeder channel probably only a few tens of metres wide. Thermogenic processes involve the dissolution of Messinian evaporites by warm fluids likely sourced even deeper, i.e. 1.7 and 2.6 km below the seabed at the Cheops and Chephren MVs respectively, and which ascend along listric faults. Seepage activity appears broadly persistent since the initiation of mud volcanism in the Early Pliocene, possibly accompanied by lateral migration of feeder channels.

  12. Monitoring the hydrologic system for potential effects of geothermal and ground-water development in the Long Valley Caldera, Mono County, California, USA

    International Nuclear Information System (INIS)

    In the early 1980's, renewed interest in the geothermal potential of the Long valley caldera, California, highlighted the need to balance the benefits of energy development with the established recreational activities of the area. The Long Valley Hydrologic Advisory Committee, formed in 1987, instituted a monitoring program to collect data during the early stages of resource utilization to evaluate potential effects on the hydrologic system. This paper reports that early data show declines in streamflow, spring flow, and ground-water levels caused by 6 years of below-average precipitation. Springs in the Hot Creek State Fish Hatchery area discharge water that is a mixture of nonthermal and hydrothermal components. Possible sources of nonthermal water have been identified by comparing deuterium concentrations in streams and springs. The equivalent amount of undiluted thermal water discharged from the springs was calculated on the basis of boron and chloride concentrations. Quantifying the thermal and nonthermal fractions of the total flow may allow researchers to assess changes in flow volume or temperature of the springs caused by ground-water or geothermal development

  13. Tracking millennial-scale climate variability through the Marine Isotope Stage (MIS) 12 using terrigenous biomarkers in lacustrine sediments from Valles Caldera, New Mexico, USA

    Science.gov (United States)

    Contreras, S.; Werne, J. P.; Brown, E. T.; Anderson, R. S.; Fawcett, P. J.

    2012-12-01

    The Quaternary is characterized by cyclic intervals of warm interglacial and cold glacial stages with the MIS 12 highlighted as one of the most severe glacial stages. Recent studies reported abrupt climatic episodes at millennial scale during MIS 12 and the transition to MIS 11 similar to Dansgaard-Oeschger [D/O] and Heinrich events but weaker in amplitude than the dramatic oscillations observed in the last glacial period. The climate variability of MIS 12 is well documented in marine and ice-sheet isotopic records but terrestrial records are scarce and often fragmented. We will present a high-resolution paleoclimate reconstruction through the MIS 12, including MIS 13-12 and MIS 12-11 transitions, from paleo-lake sediments taken in Valles Caldera, New Mexico. Measurements including scanning X-ray fluorescence, pollen, terrigenous biomarkers and bulk and compound-specific stable isotopes that usually serve as paleoclimatic proxies of precipitation and vegetation will be contrasted. Terrigenous lipid biomarkers confirm that vegetation responds rapidly to millennial-scale climate variability and provide knowledge of how these millennial oscillations impacted western North America.

  14. The mechanics of unrest at Long Valley caldera, California: 1. Modeling the geometry of the source using GPS, leveling and two-color EDM data

    Science.gov (United States)

    Battaglia, Maurizio; Segall, P.; Murray, J.; Cervelli, Peter; Langbein, J.

    2003-01-01

    We surveyed 44 existing leveling monuments in Long Valley caldera in July 1999, using dual frequency global positioning system (GPS) receivers. We have been able to tie GPS and leveling to a common reference frame in the Long Valley area and computed the vertical deformation by differencing GPS-based and leveled orthometric heights. The resurgent dome uplifted 74??7 cm from 1975 to 1999. To define the inflation source, we invert two-color EDM and uplift data from the 1985-1999 unrest period using spherical or ellipsoidal sources. We find that the ellipsoidal source satisfies both the vertical and horizontal deformation data, whereas the spherical point source cannot. According to our analysis of the 1985-1999 data, the main source of deformation is a prolate ellipsoid located beneath the resurgent dome at a depth of 5.9 km (95% bounds of 4.9-7.5 km). This body is vertically elongated, has an aspect ratio of 0.475 (95% bounds are 0.25-0.65) and a volume change of 0.086 km3 (95% bounds are 0.06-0.13 km3). Failure to account for the ellipsoidal nature of the source biases the estimated source depth by 2.1 km (35%), and the source volume by 0.038 km3 (44%). ?? 2003 Elsevier B.V. All rights reserved.

  15. Detección en línea de onda-P en sismogramas 3-D utilizando redes neuronales

    Directory of Open Access Journals (Sweden)

    Alzate Carlos

    2003-08-01

    Full Text Available

    We have developed a P-wave arrival time detector of tectonic events over digital three-component records online. This process uses two different methods: the first one works with a LVR detector, and the second one uses a statistical classifier of classes (signal with P-wave and signal with seismic noise. Detection uses multi-layer perceptron neural network where is taken advantage of non-lineal input-output, relation, well-generalization, low computational demands, etc. These appropriate qualities for real time signal processing. The input data for the system becomes a normalized vector of seismic signal and its polarization arguments. Testes were done with data from IRIS and INGEOMINAS database. Although the system has a good perforance, its accuracy is not acceptable.

    Se desarrolla un detector en línea del tiempo de arribo de ondas P sobre registros electrónicos de tres componentes de eventos tectónicos. Se lleva a cabo la detección en línea de la onda-p empleando redes neuronales (RN, utilizando dos diferentes formas: en la primera se sintetiza el detector de LRV, mientras en la segunda se desarrolla un clasificador estadístico con las respectivas clases (señal con onda-p presente y señal con solo ruido presente. La detección se realiza empleando redes neuronales de tipo perceptrón multi-capa, en las cuales se aprovechan las siguientes cualidades: su capacidad de mapeo no lineal de entrada-salida, buena generalización, bajo costo computacional, entre otras. Las anteriores cualidades hacen que las RN sean apropiadas para el proceso de señales en tiempo real. Las entradas a la RN corresponden a

  16. Necesidades académicas, personales, sociales y vocacionales de estudiantes internacionales e intercambio en la Universidad de Puerto Rico, Recinto de Río Piedras / Academic, Personal, Social and Vocational Needs of International and Exchange Students at the University of Puerto Rico, Río Piedras Campus

    Directory of Open Access Journals (Sweden)

    Ángel A Villafañe Santiago

    2011-11-01

    Full Text Available Recibido 20 de setiembre de 2011 • Aceptado 24 de octubre de 2011 • Corregido 14 de noviembre de 2011 Resumen. El propósito de este estudio fue identificar las necesidades de una muestra de estudiantes internacionales y de intercambio que cursan estudios en la Universidad de Puerto Rico, Recinto de Río Piedras. Se exploraron datos socio-demográficos así como las necesidades académicas, vocacionales, y personales/sociales, con los fines de recopilar información de relevancia para universidades que sirven esta población y someter recomendaciones que atiendan las necesidades. Los hallazgos revelaron necesidades mayormente en las áreas académicas y vocacionales. Entre estas, se destacan la necesidad de aprender inglés o español, y el conocer sobre internados y ofrecimientos académicos en Puerto Rico y fuera del país, sueldo y oportunidades de empleo, ayudas económicas y servicios estudiantiles en la Universidad de Puerto Rico. Se proveen recomendaciones para trabajar con las necesidades identificadas ya que, según establece la bibliografía, las dificultades que confrontan estos/as estudiantes pueden afectar su desempeño académico e incluso su salud emocional. Abstract. The purpose of this study was to identify the needs of a sample of the international and exchange students staying at the North Tower Residence of the University of Puerto Rico, Río Piedras Campus. Social and demographic data, as well as the academic, vocational, and social/personal needs were explored with the purpose of gathering relevant information and submitting recommendations to universities serving this student population. Findings revealed particular needs in the academic, vocational areas, including English or Spanish learning, information on internships and study programs in Puerto Rico or abroad, salary and employment opportunities, financial aid and services available to the students of this University. Recommendations are provided to work with the

  17. Artrodese na coluna cervical utilizando SICAP como substituto de enxerto ósseo Artrodesis en la columna cervical utilizando SICAP como sustituto de injerto óseo Cervical spine fusion utilizing silicated calcium phosphate bone graft substitute (SICAP

    Directory of Open Access Journals (Sweden)

    Juliano Fratezi

    2011-01-01

    Full Text Available OBJETIVO: Substitutos de enxerto ósseo autólogo foram desenvolvidos para evitar as complicações da retirada de enxerto ósseo autólogo. SiCaP (Actifuse, ApaTech EUA, Reino Unido é um enxerto ósseo composto de cálcio-fosfato com um substituição de silicato na estrutura química, com uma estrutura tridimensional que parece osso natural. MÉTODOS: 19 pacientes foram submetidos à fusão óssea cervical e analisados retrospectivamente. A avaliação radiográfica e avaliação clínica foram realizadas utilizando o questionário Neck Disability Index e a escala análoga da dor (VAS pré- e pós-operação. RESULTADOS: O período médio de acompanhamento pós-operatório foi de 14 meses ± 5 meses (7-30 meses. 11 pacientes foram submetidos à fusão via anterior; 5 pacientes via posterior e 3 pacientes via anterior e posterior. A revisão radiográfica mostrou 19/19 (100% de fusão óssea, nenhum caso apresentou subsidência, quebra ou soltura de material de implante ou movimento nos níveis fusionados. Nenhum exemplo de ossificação heterotópica ou de crescimento ósseo intracanal foi observado. Clinicamente, os escores médios do Neck Disability decresceram 13,3 pontos (media pré-op. de 34,5, pós-op. de 21,2, melhora de 39%, a média da VAS para dor cervical decresceu 2 pontos (2,7 pré-op para 0,7 pós-op.; melhora de 74,1%. Não foram observadas complicações como infecção, osteólise ou edema excessivo das partes moles. CONCLUSÃO: Os resultados preliminares obtidos nesta série foram encorajadores com o uso do SICaP como enxerto ósseo, com sólida fusão óssea obtida em todos os casos e sem formação de ossificação heterotópica ou crescimento de osso intracanal. SIcaP demonstra ser um substituto confiável para o enxerto ósseo autólogo na coluna cervical.OBJETIVO: Sustitutos de injerto óseo autólogo fueron desarrollados para evitar las complicaciones de la recogida de injerto óseo autólogo. SiCaP (Actifuse, Apa

  18. Los intercambios internacionales del Ecuador : su significacion geopolitica

    OpenAIRE

    Portais, Michel

    1989-01-01

    En 1909, les relations diplomatiques de l'Equateur montrent des liens privilégiés avec l'Europe Occidentale, en particulier avec la France. C'est le reflet de la structure spatiale du commerce extérieur équatorien, caractérisé par une nette dominance européenne. Depuis 1970, le centre de gravité de ce commerce se déplace vers le continent américain, jusqu'à ce que, en 1981, il s'oriente pour la première fois vers le Pacifique. Plus du tiers des investissements étrangers dans le pays provienne...

  19. Burnout en profesores: Una perspectiva social del intercambio

    NARCIS (Netherlands)

    Schaufeli, W.B.

    2005-01-01

    This article proposes a theoretical perspective on teacher burnout that is based on the principles of social exchange. More specifically, it is argued that burnout results from a lack of reciprocity; that is, from a mismatch between investments and outcomes. Typically, burned-out teachers have given

  20. Nuestras dos bibliotecas nacionales y el intercambio de publicaciones

    OpenAIRE

    Tesler, Mario

    2005-01-01

    Besides of the present National Library of Argentina, inicially named as Public Library of Buenos Aires, the author sets the existence of another National Library created by a presidential decree on february 11 st 1870, from this he studies the contradictions, lows and highs of the official publication exchange, betwen local and forgein institutions

  1. Enhancement of soil DNA extraction by the use of a hand held mixer Otimização da extração de DNA do solo utilizando um homogeneizador manual

    Directory of Open Access Journals (Sweden)

    Jefferson Luis da Silva Costa

    2003-12-01

    Full Text Available The efficiency of soil DNA extraction using a bead beater homogenizer (Biospec Products - Germany was compared to that obtained with a hand held mixer (Moulinex - Brazil. The hand held mixer costs 100 times less and extracted seven times more crude DNA than the bead beater.A eficiência da extração de DNA do solo utilizando um homogeneizador bead beater (Biospec Products - Alemanha foi comparada àquela obtida utilizando um homogeneizador manual (Moulinex - Brasil. O homogeneizador manual tem custo 100 vezes menor e revelou-se mais eficiente que o bead beater extraindo sete vezes mais DNA.

  2. Contribution of 2009-2014 COSMO-SkyMed SAR data to the interpretation of the Campi Flegrei caldera, Italy, activity.

    Science.gov (United States)

    Amoruso, Antonella; Crescentini, Luca; Luongo, Annamaria; Zinno, Ivana; Casu, Francesco

    2015-04-01

    The Campi Flegrei (CF) caldera is located in a densely populated volcanic region in the northern suburbs of Naples (Southern Italy). The coast near CF is famous for its significant vertical motions since Roman times, which are documented by drowned and elevated harbor works that have recorded slow variations in local sea level. After the last eruption in 1538, the caldera subsided and it has been doing so more-or-less steadily since 1969 when minor uplift occurred. In the early 1970s this uplift became significant (~1.5 m max). A further large uplift episode occurred from 1982 to 1984 (~1.8 m max), and subsequently smaller uplift episodes have occurred later on. From 2006 to spring 2013, CF was mostly uplifting at an increasing rate. Uplifting started again during summer 2014. Amoruso et al. (2014a,b) have recently shown that the CF ground deformation field from 1980 to 2013 can be decomposed into two stationary parts. Large-scale deformation can be explained by a quasi-horizontal source, oriented NW to SE and mathematically represented by a pressurized finite triaxial ellipsoid (PTE) ~4 km deep, possibly related to the injection of magma and/or magmatic fluids from a deeper magma chamber into a sill. Residual deformation not accounted for by PTE is confined to the Solfatara fumarolic area and can be mathematically explained by a small (point) pressurized oblate spheroid (PS) ~2 km below the Solfatara fumarolic field, that has been equated with a poroelastic response of the substratum to pore pressure increases near the injection point of hot magmatic fluids into the hydrothermal system. A satisfying feature of this double source model is that the geometric source parameters of each are constant over the period 1980-2013 with the exception of volume changes (potencies); potency time histories for PTE and PS, to which the time evolutions of the two components of the ground displacement field are related, are somewhat similar but not identical. Amoruso et al. (2014a

  3. MED SUV TASK 6.3 Capacity building and interaction with decision makers: Improving volcanic risk communication through volcanic hazard tools evaluation, Campi Flegrei Caldera case study (Italy)

    Science.gov (United States)

    Nave, Rosella; Isaia, Roberto; Sandri, Laura; Cristiani, Chiara

    2016-04-01

    In the communication chain between scientists and decision makers (end users), scientific outputs, as maps, are a fundamental source of information on hazards zoning and the related at risk areas definition. Anyway the relationship between volcanic phenomena, their probability and potential impact can be complex and the geospatial information not easily decoded or understood by not experts even if decision makers. Focusing on volcanic hazard the goal of MED SUV WP6 Task 3 is to improve the communication efficacy of scientific outputs, to contribute in filling the gap between scientists and decision-makers. Campi Flegrei caldera, in Neapolitan area has been chosen as the pilot research area where to apply an evaluation/validation procedure to provide a robust evaluation of the volcanic maps and its validation resulting from end users response. The selected sample involved are decision makers and officials from Campanian Region Civil Protection and municipalities included in Campi Flegrei RED ZONE, the area exposed to risk from to pyroclastic currents hazard. Semi-structured interviews, with a sample of decision makers and civil protection officials have been conducted to acquire both quantitative and qualitative data. The tested maps have been: the official Campi Flegrei Caldera RED ZONE map, three maps produced by overlapping the Red Zone limit on Orthophoto, DTM and Contour map, as well as other maps included a probabilistic one, showing volcanological data used to border the Red Zone. The outcomes' analysis have assessed level of respondents' understanding of content as displayed, and their needs in representing the complex information embedded in volcanic hazard. The final output has been the development of a leaflet as "guidelines" that can support decision makers and officials in understanding volcanic hazard and risk maps, and also in using them as a communication tool in information program for the population at risk. The same evaluation /validation process

  4. Inventariando la biodiversidad en el Parque Nacional de La Caldera de Taburiente (La Palma, Islas Canarias, España: novedades científicas

    Directory of Open Access Journals (Sweden)

    Domingo-Quero, Teresa

    2003-12-01

    Full Text Available This paper is the first result of an agreement between the Organismo Autónomo Parques Nacionales and the Consejo Superior de Investigaciones Científicas, entitled “Inventory and study of the Invertebrate Fauna of the National Park of La Caldera de Taburiente”. A detailed account of the faunistic novelties found up to now among the specimens of terrestrial and freshwater invertebrates collected along the two years of sampling (July 1999 to July 2001, whose number is estimated in ca. 500,000, is given. A brief description of planning and of methodology applied to the inventory of the invertebrate fauna is made and a tabulated summary of novelties is presented. The list shows at present 284 families, 594 genera and 739 species. For the Canary Islands, the present record of new taxa is 29 families, 115 genera (1 of them confirmed as new to Science and 3 awaiting confirmation and 187 species (24 new to Science. Moreover, 242 genera and 338 species are new to the fauna of La Palma I., being known from other islands of the archipelago. Other 47 taxa, still being studied, could be new to Science as well. These results have been reached with the study of just a minimal part of the whole material, which underlines the need for systematic, continued sampling to evaluate the faunistic richness of poorly explored areas and its possible necessity for protection. Therefore, one should expect more novelties and the inventory may increase significantly when all the material is revised.

    El presente artículo es el primer resultado de un convenio entre el Organismo Autónomo Parques Nacionales y el Consejo Superior de Investigaciones Científicas, denominado “Inventario y estudio de la Fauna Invertebrada del Parque Nacional de La Caldera de Taburiente”. Se detallan las novedades faunísticas encontradas hasta el momento entre los ejemplares de invertebrados terrestres y dulceacuícolas recogidos durante los dos años de muestreo (julio de 1999 a

  5. Dynamic model of intrusion of magma and/or magmatic fluids in the large-scale deformation source of the Campi Flegrei caldera (Italy).

    Science.gov (United States)

    Crescentini, Luca; Amoruso, Antonella; Luongo, Annamaria

    2015-04-01

    The Campi Flegrei (CF) caldera is located in a densely populated area close to Naples (Southern Italy). It is renowned as a site of continual slow vertical movements. After the last eruption in 1538, the caldera generally subsided until 1969 when minor uplift occurred. In the early 1970s this uplift became significant (~1.5 m max). A further large uplift episode occurred from 1982 to 1984 (~1.8 m max), and subsequently smaller uplift episodes have occurred since then. Amoruso et al. (2014a,b) have recently shown that the CF surface deformation field from 1980 to 2013 can be decomposed into two stationary parts. Large-scale deformation can be explained by a quasi-horizontal source, oriented NW to SE and mathematically represented by a pressurized finite triaxial ellipsoid (PTE) ~4 km deep, possibly related to the injection of magma and/or magmatic fluids from a deeper magma chamber into a sill, or pressurization of interconnected (micro)cavities. Residual deformation not accounted for by PTE is confined to the Solfatara fumarolic area and can be mathematically explained by a small (point) pressurized oblate spheroid (PS) ~2 km below the Solfatara fumarolic field, that has been equated with a poroelastic response of the substratum to pore pressure increases near the injection point of hot magmatic fluids into the hydrothermal system. A satisfying feature of this double source model is that the geometric source parameters of each are constant over the period 1980-2013 with the exception of volume changes (potencies). Several papers have ascribed CF deformation to the injection of magmatic fluids at the base of the hydrothermal system. All models predict complex spatial and temporal evolution of the deformation pattern and consequently contrast with the observed deformation pattern stationarity. Also recently proposed dynamic models of sill intrusion in a shallow volcanic environment do not satisfy the observed CF deformation pattern stationarity. We have developed an

  6. Shallow geothermal investigations into the existence of the Valles Caldera outflow plume near Ponderosa and Jemez Pueblo, north-central, New Mexico

    Science.gov (United States)

    Salaz, Robert Ezekiel

    Geothermal research within the Jemez Mountains spans several decades and is documented in many papers. This study serves to extend the research boundary to the south and east outside of Valles caldera and Canon de San Diego, where the main occurrences of geothermal activity are located. The focus of this investigation is to test for a deep ~900 m, stratigraphically-bound thermal aquifer within the Madera Limestone along the western margin of the Santo Domingo basin transition zone near Ponderosa and Jemez Pueblo, in north-central New Mexico. Numerous springs were sampled for aqueous geochemistry to identify leakage of a deeper geothermal aquifer into shallow aquifers. Wells were sampled for temperature anomalies. In addition, two travertine deposits were analyzed for stable isotope composition and one deposit was dated using U-Series techniques to assess the timing and origin of deposition. This study is important because researchers in other extensional basins have identified reasonably good geothermal reservoirs in deep carbonate aquifers that are similar in geologic setting to the Madera Limestone aquifer of this study. The existence of a deep geothermal aquifer near Ponderosa and Jemez Pueblo, New Mexico could prove to be another prospect for geothermal exploration in the Jemez Mountains. Aqueous geochemistry of springs are plotted on ternary Piper diagrams to help classify similar geochemical trends and group these trends into recognizable patterns. These data indicate calcium carbonate rich waters in the north that may gradationally change to alkaline type waters as they flow south through the study area. Contrasting this data, SiO2 and TDS concentrations show two separate systems that may indicate separate confined aquifers. Two distinct TDS regions are observed, one with higher concentrations (>1000 ppm) shows a decrease from N-S and one with lower concentrations (geothermal mixing was observed in any of the samples. Temperature data taken from shallow

  7. Geochemical and isotopic insights into the assembly, evolution and disruption of a magmatic plumbing system before and after a cataclysmic caldera-collapse eruption at Ischia volcano (Italy)

    Science.gov (United States)

    Brown, R. J.; Civetta, L.; Arienzo, I.; D'Antonio, M.; Moretti, R.; Orsi, G.; Tomlinson, E. L.; Albert, P. G.; Menzies, M. A.

    2014-09-01

    New geochemical and isotopic data on volcanic rocks spanning the period ~75-50 ka BP on Ischia volcano, Italy, shed light on the evolution of the magmatic system before and after the catastrophic, caldera-forming Monte Epomeo Green Tuff (MEGT) eruption. Volcanic activity during this period was influenced by a large, composite and differentiating magmatic system, replenished several times with isotopically distinct magmas of deep provenance. Chemical and isotopic variations highlight that the pre-MEGT eruptions were fed by trachytic/phonolitic magmas from an isotopically zoned reservoir that were poorly enriched in radiogenic Sr and became progressively less radiogenic with time. Just prior to the MEGT eruption, the magmatic system was recharged by an isotopically distinct magma, relatively more enriched in radiogenic Sr with respect to the previously erupted magmas. This second magma initially fed several SubPlinian explosive eruptions and later supplied the climactic, phonolitic-to-trachytic MEGT eruption(s). Isotopic data, together with erupted volume estimations obtained for MEGT eruption(s), indicate that >5-10 km3 of this relatively enriched magma had accumulated in the Ischia plumbing system. Geochemical modelling indicates that it accumulated at shallow depths (4-6 km), over a period of ca. 20 ka. After the MEGT eruption, volcanic activity was fed by a new batch of less differentiated (trachyte-latite) magma that was slightly less enriched in radiogenic Sr. The geochemical and Sr-Nd-isotopic variations through time reflect the upward flux of isotopically distinct magma batches, variably contaminated by Hercynian crust at 8-12 km depth. The deep-sourced latitic to trachytic magmas stalled at shallow depths (4-6 km depth), differentiated to phonolite through crystal fractionation and assimilation of a feldspar-rich mush, or ascended directly to the surface and erupted.

  8. Evidences for disruption of a crystallizing front in a magma chamber during caldera collapse: an example from the Breccia Museo unit (Campanian Ignimbrite eruption, Italy)

    Science.gov (United States)

    Fulignati, P.; Marianelli, P.; Proto, M.; Sbrana, A.

    2004-05-01

    This work is focused on juvenile components and some cognate xenoliths of the Breccia Museo (BM) unit. The BM is a coarse-grained proximal unit of the caldera-forming phase of the Ignimbrite Campana (IC) eruption, southern Italy. The BM products show some peculiar characteristics that distinguish them from the other IC deposits. In particular, different types of pumice fragments constitute the juvenile fraction and their crystal contents are remarkably higher than the other IC units. Slightly porphyritic and highly porphyritic trachytic to phonolitic pumices were distinguished in each sample and investigated separately for mineralogy, matrix glass composition, melt and fluid inclusion studies. Most feldspar crystals may have formed at the margins of the magma chamber and the crystal content of both types of pumice fragments can be ascribed to variable entrainment of these crystals (from the solidification front) by the melt. Variably porphyritic (<5 to 30 vol% phenocrysts) pumice and completely crystallized nodules may represent samples of progressively crystallized magma at the chamber walls. Crystallization temperatures of magmas and xenoliths were estimated using two independent methods: a two-feldspar geothermometer and the homogenization temperatures of melt and fluid inclusions in clinopyroxene and K-feldspar. The decrease in the estimated crystallization temperatures from the melt (980-850°C) to the nodules (840-820°C) is consistent with a model of decreasing temperature at a magma chamber solidification front. The study of xenoliths revealed that exsolution of a hypersaline aqueous fluid phase occurred at the peripheral parts of the magma chamber.

  9. Transport and deposition of pyroclastic material from the ˜1000 A.D. caldera-forming eruption of Volcán Ceboruco, Nayarit, Mexico

    Science.gov (United States)

    Browne, B. L.; Gardner, J. E.

    2005-06-01

    The complex eruption sequence from the ˜1000 A.D. caldera-forming eruption of Volcán Ceboruco, known as the Jala Pumice, offers an exceptional opportunity to examine how pyroclastic material is transported and deposited from pyroclastic density currents over variable topography. Three main pyroclastic surge deposits (S1, S2, and S3) and two pyroclastic flow deposits (Marquesado and North-Flank PFDs) were emplaced during this eruption. Pyroclastic surge deposits are massive, planar, or cross-bedded, poor-to-well sorted, and display fluctuations in thickness, median diameter, sorting, and lithology as a function of distance, topography, and flow dynamics. Marquesado pyroclastic flow deposits reveal lateral variations from massive, poorly sorted deposits located within 5 km of Ceboruco to planar bedded, moderately well sorted deposits located >15 km away over the nearly horizontal topography to the south of Ceboruco. North-Flank pyroclastic flow deposits also reveal lateral variations from massive, poorly sorted deposits located within 4 km of Ceboruco to planar bedded, moderately well sorted deposits located 8 km away atop an escarpment that steeply rises 230 m from the northern valley floor. Field observations, granulometric analyses, component analyses, and crystal sedimentation calculations along flow-parallel sampling transects all suggest that both surges and flows were density stratified currents, where deposition occurred from a basal region of higher particle concentration that was supplied from an overlying dilute layer that transports particles in suspension. This supports the idea of a transition between “flow” and “surge” end members with variations in particle concentration. Topography greatly affects the transport and depositional capacity of the pyroclastic density currents as a result of “blocking”, either by topographic obstacles or by abrupt breaks at the base of volcano slopes, whereas the origin of Jala Pumice surge deposits

  10. Geomorphological and hydrogeological features of the Pocos de Caldas caldera and the Osamu Utsumi mine and Morro do Ferro analogue study sites, Brazil

    International Nuclear Information System (INIS)

    The Osamu Utsumi mine and Morro do Ferro study sites lie within the Pocos de Caldas plateau which is roughly circular in outline with a diameter of 35 km and an area of approximately 800 km2. Its general altitude lies between 1300 and 1600 m. The plateau is the eroded form of a caldera which was initially intruded some 80 million years ago. Geomorphologically, both sites occupy watershed areas adjacent to small streams in the centre of the plateau. The climate of the area has a market wet season from November to April and is dry the rest of the year. The streams are ephemeral in their upper reaches, tending to dry up in the dry season as they are fed by a declining base flow. In the wet season they exhibit flash flood fed by high-intensity rainfall causing overland flow. The wet season also provides recharge to the groundwater. Natural slopes are steep and the original vegetation was thin forest cover which is now restricted to the valley bottoms; usable slopes have poor quality grass cover used for cattle grazing. The plateau is a stable feature and its surface has been eroding at an average rate of 12 m per million years over a period of 50 million years. The mine geology is dominantly volcanic to subvolcanic phonolites that have been hydrothermally altered. Fracturing of the rock is extensive. Downward diffusion of oxygen in groundwaters during deep weathering has produced a distinct redox zone seen as a colour change from green/grey to brown/yellow. Morro do Ferro has a more weathered version (laterite/clay) of the same geology penetrated by magnetite breccia dykes. Whilst the area surrounding Morro do Ferro remains untouched, that around the mine has been seriously disturbed by mining activity which has penetrated the water-table. The existing mine has modified groundwater flow patterns and disturbed the movement of oxidising and reducing waters. (au) (47 refs.)

  11. Determinación del perfil de humedad del suelo utilizando una sola sonda TDR: el método del nomograma

    OpenAIRE

    Moret-Fernández, David; Arrúe Ugarte, José Luis; López Sánchez, María Victoria; Gracia Ballarín, Ricardo; Álvaro-Fuentes, Jorge; Salvador, María José

    2007-01-01

    [ES] El objetivo de este trabajo es presentar el método del “nomograma” para la medida por reflectometría de dominio temporal (TDR) del perfil de constante dieléctrica (K) del suelo, y, por tanto, del perfil del contenido de humedad volumétrico (θ), utilizando una única sonda TDR. El método está,basado en un nuevo análisis gráfico de la onda TDR en medios no conductivos. Este análisis consiste en representar la función ρ(t), que define la relación entre K, el coeficiente de reflexión (ρ...

  12. Otimização de secções de aço por chapas soldadas utilizando algoritmos genéticos

    OpenAIRE

    Barros, Filipa Goulão Mira

    2013-01-01

    Esta dissertação apresenta uma metodologia para otimização paramétrica de secções de vigas de aço constituídas por chapas soldadas cumprindo os requisitos de segurança propostos pelo Eurocódigo 3 no que se refere à resistência ao momento fletor, ao esforço transverso e à encurvadura lateral utilizando Algoritmos Genéticos. Os Algoritmos Genéticos são métodos de optimização inspirados na teoria de seleção natural de Charles Darwin, introduzidos por John Holland e popularizados p...

  13. Detección automática de peatones para la asistencia a la conducción utilizando fusión sensorial

    OpenAIRE

    Domínguez Fernández, Almudena

    2011-01-01

    El proyecto trata de abordar el problema de la detección automática de peatones en un contexto automovilístico utilizando diferentes sensores. El vehículo utilizado para la experimentación se encuentra en un entorno de simulación. Como sensores, cuenta con dos cámaras y un LRF (laser rangefinder o telémetro láser). El sensor láser que se utilizará es capaz de medir distancias en tiempo real. Combinando esta información de distancias con la información obtenida de las cámaras procesada usando ...

  14. OBTENCIÓN DE UNA BEBIDA FERMENTADA A PARTIR DE SUERO DE QUESO UTILIZANDO CÉLULAS INMOVILIZADAS DE KLUYVEROMYCES MARXIANUS

    OpenAIRE

    Rocío Cóndor G.; Víctor Meza C.; Fanny Ludeña U.

    2014-01-01

    El presente estudio tuvo como objetivo principal optimizar la tecnología de producción de una bebida fermentada de suero de queso, utilizando Kluyveromyces marxianus e inmovilización de células. En el biorreactor de lecho empacado, se obtuvo el mayor rendimiento (11,46±0,81 oGL) con un flujo de 140-150 mL. h-1, una biomasa inmovilizada de 10% (v/v), una relación de columna de 1:12 (diámetro: longitud), tamaño de perlas de 3 mm de diámetro, adición de metabisulfito de sodio (100 pg. mL-1) y c...

  15. REPLICAÇÃO DE FÓSSEIS DE FORAMINIFERA UTILIZANDO REAPROVEITAMENTO DE “ISOPOR” COM ALUNOS DO IFPB-CG

    OpenAIRE

    Hermes de Oliveira Machado Filho; Ana Cláudia Mousinho Ferreira; Dwight Rodrigues Soares

    2011-01-01

    Os fósseis são unidades paleontológicas preciosas e difíceis de serem coletadas para pesquisas ou principalmente para aulas práticas sobre o passado geológica da Terra. Desta forma, lançam-se mão de técnicas alternativas para se fazer réplicas dessas unidades. O presente artigo vem apresentar atividades de sistemática paleozoológica, utilizando o “isopor” como matéria prima para confecção de modelos de fósseis em aulas práticas para a comunidade escolar do Instituto Federal de Educação, Ciênc...

  16. Avaliação de Micro e Pequenas Empresas Utilizando a Metodologia Multicritério e o Método do Fluxo de Caixa Descontado

    Directory of Open Access Journals (Sweden)

    Marcus Vinicius Andrade de Lima

    2010-01-01

    Full Text Available Neste artigo é apresentada uma contribuição ao método do fluxo de caixa descontado utilizando a metodologia multicritério de apoio à decisão. Essa metodologia incorpora variáveis de natureza qualitativa e subjetiva ao método tradicional do fluxo de caixa descontado utilizado na avaliação de empresas. Para ilustrar o método proposto foi realizado um estudo descritivo de natureza exploratória aplicado a um multicaso. A intervenção foi em Micro e Pequenas Empresas (MPE do ramo químico, farmacêutico e de turismo. Como resultado, o avaliador ajustou o preço do negócio levando em conta a resultante da mixagem entre as duas metodologias.

  17. Estimativa da produtividade de trigo em função da adubação nitrogenada utilizando modelagem neuro fuzzy

    Directory of Open Access Journals (Sweden)

    Aldo A. V. da Silva

    2014-02-01

    Full Text Available Atualmente, novas técnicas de processamento de dados, tais como redes neurais, lógica nebulosa (fuzzy e sistemas híbridos, são utilizadas para elaborar modelos de predição em sistemas complexos e estimar parâmetros desejados. Neste artigo investigou-se a habilidade de se desenvolver um modelo de inferência adaptativo neuro fuzzy para estimação da produtividade de trigo utilizando-se uma base de dados da combinação dos seguintes tratamentos: cinco doses de N (0, 50, 100, 150 e 200 kg ha-1; três fontes (Entec, sulfato de amônio e ureia; duas épocas de aplicação de N (na semeadura ou em cobertura e dois cultivares de trigo (E21 e IAC 370, avaliados durante dois anos, em Selvíria, MS. Através dos dados de entrada e saída o sistema de inferência neuro fuzzy adaptativo apreende e posteriormente pode estimar um novo valor de produção de trigo com base em doses diferenciadas de N. O erro de predição da produtividade de trigo em função das cinco doses de N, obtido com o sistema neuro fuzzy, foi menor que o valor obtido utilizando-se uma aproximação quadrática. Os resultados mostraram que o sistema neuro fuzzy é viável para desenvolver um modelo de predição visando estimar a produtividade de trigo em função da dose de N.

  18. La gestión auténtica como moderadora de la relación entre (1 la congruencia de la identidad del rol de género –características de género de la gestión– y (2 el intercambio líder-subordinado (LMX

    Directory of Open Access Journals (Sweden)

    Aharon Tziner

    2014-01-01

    Full Text Available Este trabajo analiza el efecto de la congruencia de la identidad del rol de género (andrógina/no andrógina y las características de género de la gestión (comunitaria/egocéntrica en la calidad del intercambio líder subordinado (LMX, así como que si la gestión auténtica es una variable que modere dicha relación. El estudio plantea la hipótesis de una relación positiva entre la identidad del rol de género y las características de género de la gestión con la calidad de la LMX. Otra hipótesis ha sido que la gestión auténtica modera y explica esta relación. La muestra constaba de 120 mujeres dirigidas por otras mujeres. Cumplimentaron un cuestionario en el que se les pedía evaluar y describir su percepción de su jefa de acuerdo a las variables del estudio: identidad del rol de género (andrógina/no andrógina, características de género de la gestión (comunitaria/egocéntrica, la calidad de la LMX y el grado de autenticidad característico de su estilo de gestión. Además se pidió a 24 directivos que cumplimentasen un cuestionario sobre la relación líder-subordinado (LMX que les caracterizaba. Los resultados avalaban todas nuestras hipótesis, señalando una relación positiva entre las variables. Cuando la identidad del rol de género y las características de género de la gestión eran congruentes se percibía que la calidad de la LMX era superior. Además se encontró que la gestión auténtica es realmente una variable moderadora; es decir, la relación entre la congruencia de la identidad del rol de género y las características de género de la gestión y la LMX es moderada y explicada por la ges tión auténtica. Otros resultados revelan la brecha entre líderes y subordinados al evaluar la LMX e informar sobre ella. Cuando no se hallaba congruencia había una brecha entre los informes de los líderes y de los subordinados; es decir, los primeros evaluaban mejor la LMX. Por otra parte, cuando había congruencia

  19. Evaluación del Programa de Intercambio de Jeringuillas en el Centro Penitenciario de Pereiro de Aguiar (Ourense: diez años de experiencia Evaluation of needle exchange program at Pereiro de Aguiar prison (Ourense, Spain: ten years of experience

    Directory of Open Access Journals (Sweden)

    V. Ferrer-Castro

    2012-06-01

    Full Text Available Objetivos: Evaluar la eficacia de un programa de intercambio de jeringuillas (PIJ en una prisión para reducir la prevalencia de infecciones asociadas al uso de drogas intravenosas, y conocer la aceptación del programa por internos y funcionarios del centro penitenciario. Material y métodos: Estudio observacional con cortes transversales al inicio, 6 y 12 meses y 10 años de desarrollo del programa. Se realizaron entrevistas a los usuarios del programa y encuestas a muestras accidentales de funcionarios en los distintos cortes, y a una muestra aleatoria de internos a los 10 años. Se registraron diariamente los indicadores de actividad del programa, y se valoró la prevalencia de infección por VIH, hepatitis B y C al inicio y a los 10 años. Para el análisis estadístico utilizamos la prueba ji-cuadrado con la corrección de Yates en caso necesario. Resultados: Durante estos diez años se suministraron 15.962 jeringuillas a 429 usuarios (media de 20,2 usuarios/mes, recuperándose 11.327 (70,9%. La prevalencia de infección por VIH pasó del 21% en 1999 al 8,5% en 2009, la de VHC del 40% al 26,1% (pObjectives: To evaluate the effectiveness of NEPs in prison to reduce the prevalence of infections associated with intravenous drug use and to know more about acceptance of the program by inmates and staff. Material and methods: cross-sectional observational study at baseline, 6 and 12 months and 10 years of program development. Interviews were conducted with program users, as well as random sample surveys of officials at the various cuts, and a random sample of inmates from the centre after10 years. Activity indicators of the program were recorded continuously, and the prevalence of HIV, HBV and HCV at baseline and after 10 years was evaluated. For the statistical analysis, the chi-square test was used with the Yates correction when necessary. Results: In ten years we have supplied a total of 15,962 syringes to 429 users, (average 20.2 users

  20. Evolution of the 120 ka caldera-forming eruption of Kutcharo volcano, eastern Hokkaido, Japan: Geologic and petrologic evidence for multiple vent systems and rapid generation of pyroclastic flow

    Science.gov (United States)

    Hasegawa, Takeshi; Matsumoto, Akiko; Nakagawa, Mitsuhiro

    2016-07-01

    We investigated the eruptive sequence and temporal evolution of juvenile materials during the 120 ka Kutcharo pumice flow IV (Kp IV) eruption, which was the most voluminous (175 km3: bulk volume) caldera-forming eruption of Kutcharo volcano. The eruptive deposits are divided into four units in ascending order. Unit 1 is widely dispersed and consists of silt-sized, cohesive ash. Unit 2 is a thin, moderately sorted pumice fall deposit with a restricted distribution and small volume (vent systems. Although Unit 2 was derived from an eruptive column, its volume is very small compared to Plinian fall deposits of typical caldera-forming eruptions. In our interpretation, the activity of the Kp IV eruption reached its climax rapidly, depositing Unit 3, without first producing a stable Plinian column. The presence of multiple vent systems could have allowed the system to bypass an initial eruptive stage with a stable Plinian column and begin its climactic stage, represented by Unit 3, rapidly. Multiple vents could have been the result of sequential injections of mafic magma in the early stages of the Kp IV eruption.

  1. Tratamiento del condensado vegetal de los concentradores de jugos en frutos de cítricos después de la cosecha con el fin de poder utilizarlo como agua de alimentación de calderas

    Directory of Open Access Journals (Sweden)

    Alexander Roque Chávez

    2010-01-01

    Full Text Available El trabajo se desarrolla con el objetivo de determinar el valor del pH del condensado vegetal obtenido de los concentradores de jugos, su variación en dependencia con el tipo de cítrico y su madures, así como determinar la cantidad de hidróxido de sodio (NaOH necesario para su tratamiento con el fin de poder utilizarlo como agua de alimentación de calderas, para el estudio se tomaron varias muestras de pH durante la campaña 2008-2009 que abarcaron siete meses, los valores de pH se compararon con el Ratio de la fruta, obteniéndose una correlación de 0,00149, demostrándose mediante métodos estadísticos que el pH del condensado vegetal es constante durante toda la campaña y que es posible utilizarlo como agua de alimentación de calderas, adicionándole a cada metro cúbico 10, 17 g de hidróxido de sodio logrando elevar su pH de 4 hasta 8.

  2. Crustal-scale recycling in caldera complexes and rift zones along the Yellowstone hotspot track: O and Hf isotopic evidence in diverse zircons from voluminous rhyolites of the Picabo volcanic field, Idaho

    Science.gov (United States)

    Drew, Dana L.; Bindeman, Ilya N.; Watts, Kathryn E.; Schmitt, Axel K.; Fu, Bin; McCurry, Michael

    2013-01-01

    Rhyolites of the Picabo volcanic field (10.4–6.6 Ma) in eastern Idaho are preserved as thick ignimbrites and lavas along the margins of the Snake River Plain (SRP), and within a deep (>3 km) borehole near the central axis of the Yellowstone hotspot track. In this study we present new O and Hf isotope data and U–Pb geochronology for individual zircons, O isotope data for major phenocrysts (quartz, plagioclase, and pyroxene), whole rock Sr and Nd isotope ratios, and whole rock geochemistry for a suite of Picabo rhyolites. We synthesize our new datasets with published Ar–Ar geochronology to establish the eruptive framework of the Picabo volcanic field, and interpret its petrogenetic history in the context of other well-studied caldera complexes in the SRP. Caldera complex evolution at Picabo began with eruption of the 10.44±0.27 Ma (U–Pb) Tuff of Arbon Valley (TAV), a chemically zoned and normal-δ18O (δ18O magma=7.9‰) unit with high, zoned 87Sr/86Sri (0.71488–0.72520), and low-εNd(0) (−18) and εHf(0) (−28). The TAV and an associated post caldera lava flow possess the lowest εNd(0) (−23), indicating ∼40–60% derivation from the Archean upper crust. Normal-δ18O rhyolites were followed by a series of lower-δ18O eruptions with more typical (lower crustal) Sr–Nd–Hf isotope ratios and whole rock chemistry. The voluminous 8.25±0.26 Ma West Pocatello rhyolite has the lowest δ18O value (δ18Omelt=3.3‰), and we correlate it to a 1,000 m thick intracaldera tuff present in the INEL-1 borehole (with published zircon ages 8.04–8.35 Ma, and similarly low-δ18O zircon values). The significant (4–5‰) decrease in magmatic-δ18O values in Picabo rhyolites is accompanied by an increase in zircon δ18O heterogeneity from ∼1‰ variation in the TAV to >5‰ variation in the late-stage low-δ18O rhyolites, a trend similar to what is characteristic of Heise and Yellowstone, and which indicates remelting of variably hydrothermally altered tuffs

  3. Discovery of a Plains Caldera Complex and Extinct Lava Lake in Arabia Terra, Mars: Implications for the Discovery of Additional Highland Volcanic Source Regions

    Science.gov (United States)

    Bleacher, Jacob; Michalski, Joseph

    2012-01-01

    Several irregularly shaped topographic depressions occur near the dichotomy boundary in northern Arabia Terra, Mars. The geomorphology of these features suggests that they formed by collapse, opposed to meteor impact. At least one depression (approx.55 by 85 km) displays geologic features indicating a complex, multi-stage collapse history. Features within and around the collapse structure indicate volcanic processes. The complex occurs within Hesperian ridged plains of likely volcanic origin and displays no crater rim or evidence for ejecta. Instead the depression consists of a series of circumferential graben and down-dropped blocks which also display upper surfaces similar to ridged plain lavas. Large blocks within the depression are tilted towards the crater center, and display graben that appear to have originally been linked with circumferential graben outside of the complex related to earlier collapse events. A nearly 700 m high mound exists along a graben within the complex that might be a vent. The deepest depression displays two sets of nearly continuous terraces, which we interpret as high-stands of a drained lava lake. These features appear similar to the black ledge described during the Kilauea Iki eruption in 1959. A lacustrine origin for the terraces seems unlikely because of the paucity of channels found in or around the depression that could be linked to aqueous surface processes. In addition, there is no obvious evidence for lacustrine sediments within the basin. Together with the presence of significant faulting that is indicative of collapse we conclude that this crater complex represents a large caldera formed in the Late Noachian to Early Hesperian. Other linear and irregular depressions in the region also might be linked to ancient volcanism. If that hypothesis is correct, it suggests that northern Arabia Terra could contain a large, previously unrecognized highland igneous province. Evacuation of magma via explosive and effusive activity

  4. Mineralogical and sulfur isotopic characterization of the sulfur-bearing mineralization from the active degassing area of Campi Flegrei caldera (southern Italy)

    Science.gov (United States)

    Mormone, Angela; Piochi, Monica; Balassone, Giuseppina; Strauss, Harald; Troise, Claudia; De Natale, Giuseppe

    2015-04-01

    The Campi Flegrei caldera is a site of persistent hydrothermal circulation and gaseous emissions inside the Pozzuoli town and nearby the city of Napoli (Italy). The solfataric phenomena are associated with episodes of low-magnitude seismicity and vertical ground displacement since Roman times, evolving to the Monte Nuovo eruption in the 1538 AD. Pronounced geochemical anomalies, uplift rates up to 1 m/y and up to ten thousands microearthquakes per year also characterized the four most recent decades of unrest. The degassing phenomena are concentrated within the Solfatara crater, although, since 2006, the hydrothermal activity strongly increased in the Pisciarelli district, i.e. on the north-east slope of the tuff. We investigated sulfur-bearing mineral precipitates sampled from the active fumaroles both within the Solfatara and along the Pisciarelli slope. Mineral assemblage, texture and chemistry were determined for the efflorescence precipitated nearby the fumaroles and along the mud pool by x-ray diffraction, back-scattered electron microscope and electron diffuse microanalysis. δ34S compositions were also determined on separated sulfur-minerals. The new data have been compared with scattered literature data, including few existing for the previous '70 and '80 unrest episodes. Native sulfur and alunite are the main mineral phases that associate with alunogene, and, locally, pickeringite and potassium alum. Sporadically mereiterite, amarillite, and pyrite have been found as neogenesis mineralization along the outcropping rocks. The mud pool is rich in gypsum, potassium alum and pyrite. δ34S values range from -5.48 to 0.0‰, being slightly lower than previous data. The obtained results suggest that the Pisciarelli area is characterized by magmatic-hydrothermal, magmatic-steam and steam-heated environments, developed on a argillitic hydrothermal facies that thickens in correspondence of the degassing area. These environments develop and continuously evolve in

  5. Charge exchange and knockout reactions induced by Sn isotopes at relativistic energies

    OpenAIRE

    Vargas Cruz, Jossitt Williams

    2014-01-01

    El objetivo de este trabajo de tesis doctoral es estudiar excitaciones nucleares y subnucleares utilizando reacciones periféricas de núcleos pesados inducidas por proyectiles relativistas de núcleos estables e inestables. En particular se propone estudiar estas excitaciones usando reacciones de intercambio de carga isóbaras y de arranque de nucleones. Las reacciones de intercambio de carga corresponden a excitaciones espínisoesp ín que pueden proporcionar informaci´on sobre ...

  6. Estimativa da área da folha da batateira utilizando medidas lineares Evaluation of the potato plant leaf area using linear measures

    Directory of Open Access Journals (Sweden)

    Marcelo CC Silva

    2008-03-01

    Full Text Available O objetivo deste experimento foi determinar o modelo mais apropriado para estimar a área da folha da batateira, utilizando-se medidas de comprimento e largura da folha. Foram coletadas 300 folhas de 300 plantas de batata, cultivar Monalisa, de forma aleatória, aos 21 e 56 dias após a emergência (DAE. Em laboratório, foram medidos o comprimento (C, a largura (L e a área de cada folha (AF. Os dados foram submetidos à análise de regressão com o valor da AF sendo considerado a variável dependente e os valores de comprimento e largura de folha as variáveis independentes. Foram testados três modelos estatísticos: linear, exponencial e logarítmico. A AF da batateira foi mais precisamente estimada (R² = 0,88, usando as medidas, L e C (AF = 0,2798**LC + 71,267. Para maior rapidez e praticidade, a AF da batateira, foi também apropriadamente estimada medindo-se apenas L ou C da folha e utilizando-se as equações AF = 0,0479**L + 10,777 (R² = 0,83 ou AF = 0,0659**C + 12,979 (R² = 0,82. A área foliar estimada 21 DAE, utilizando o modelo linear foi de 234,41 cm², sendo que o valor real medido, foi de 185,52 cm². Aos 56 DAE, a área foliar estimada pelo mesmo modelo foi de 175,60 cm², o valor real medido, foi de 176,01 cm². Com um dos modelos propostos, a área da folha pode ser estimada em tempo real, de forma rápida e sem a necessidade de coletar a folha.The objective of this experiment was to determine the most appropriate model to estimate potato leaf area through the leaf length and width. 300 leaves of 300 potato plants, cv. Monalisa were collected in an aleatory way, 21 and 56 days after the plant emergence (DAE. In laboratory, the length (C, width (L and area of each leaf (AF were measured. The data were submitted to the regression analysis with the AF value as a dependent variable and the leaf length and width values as the independent variables. Three statistical models were tested (linear, exponential and logarithmic. Potato

  7. Evolution of the Cañadas edifice and its implications for the origin of the Cañadas Caldera (Tenerife, Canary Islands)

    Science.gov (United States)

    Ancochea, E.; Huertas, M. J.; Cantagrel, J. M.; Coello, J.; Fúster, J. M.; Arnaud, N.; Ibarrola, E.

    1999-02-01

    , the Cañadas III phase began. It is well represented in the CW sectors of Tigaiga (1.1 Ma-0.27 Ma), Las Pilas (1.03 Ma-0.78 Ma), Diego Hernández (0.54 Ma-0.17 Ma) and Guajara (1.1 Ma-0.7 Ma). The materials of this edifice are also found in the SE flank. These materials are trachybasaltic lava-flows and abundant phonolitic lava and pyroclastic flows (0.6 Ma-0.5 Ma) associated with abundant plinian falls. The CE-III was essentially built between 0.9 and 0.2 Ma, a period when the volcanic activity was also intense in the `Dorsal Edifice' situated in the easterly wing of Tenerife. The so called `valleys' of La Orotava and Güimar, transversals to the ridge axis, also formed during this period. In the central part of Tenerife, the CE-III completed its evolution with an explosive deposit resting on the top of the CE, for which ages from 0.173 to 0.13 Ma have been obtained. The CC age must be younger due to the fact that the present caldera scarp cuts these deposits. On the controversial origin of the CC (central vertical collapse vs. repeated flank failure and lateral collapse of mature volcanic edifices), the data discussed in this paper favor the second hypothesis. Clearly several debris-avalanche type events exist in the history of the volcano but most of the deposits are now under the sea. The caldera wall should represent the proximal scarps of the large slides whose intermediate scarps are covered by the more recent Teide-Pico Viejo volcanoes.

  8. PROPOSTA DE MODELO PARA IMPLANTAÇÃO DE PROCESSO DE PROJETO UTILIZANDO O CONCEITO BIM EM ESCRITÓRIOS DE ARQUITETURA

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    Marcele Ariane Lopes Garbini

    2015-02-01

    Full Text Available Este trabalho trata do modelo de processo de projeto utilizando BIM (Building Information Modeling em escritórios de arquitetura. O conceito de BIM surgiu há mais de trinta anos, no entanto vem sendo divulgado com maior abrangência no mercado da construção civil apenas nos últimos dez anos. As vantagens de sua adoção são visíveis nos projetos, considerando o aumento na rapidez do desenvolvimento e na qualidade, dentre outros benefícios. O objetivo desta pesquisa está em propor um modelo de processo de projeto, utilizando o conceito BIM voltado para escritórios de arquitetura, de tal forma que estes possam obter um grau maior de eficiência na sua utilização. Fundamenta-se metodologicamente em estudos de casos múltiplos, interpretados qualitativamente e realizados em escritórios nas cidades de Cuiabá, São Paulo e Goiânia, perfazendo quatro empresas. Na fase de preparação foi elaborado um protocolo de pesquisa com questões para a coleta de dados nos escritórios. A condução dos estudos foi de ordem exploratória, por meio de documentos, entrevistas e observação direta. Nas entrevistas foram obtidos dados de caracterização da empresa e dados sobre o desenvolvimento dos projetos: planejamento para implantação da BIM; tecnologia da informação; processo de projeto e procedimentos de trabalho. Após a validação, foi realizada uma análise comparativa destas informações, onde ficaram claras as mudanças ocorridas nos processos de projeto, nos procedimentos de trabalho e na capacitação da equipe técnica dos escritórios. Dentre os produtos desta pesquisa, destaca-se a proposta de um modelo de processo de projeto que é o objeto do presente artigo. Este modelo se compõe de diretrizes de trabalho e de instrumentos para o desenvolvimento dos projetos nos escritórios de arquitetura que vem, paulatinamente, realizando a migração para os sistemas BIM.

  9. Inyección de aire secundario caliente en calderas de vapor bagaceras y su influencia en el rendimiento térmico Injection of heated secondary air in steam bagasse boilers and its influence on thermal efficiency

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    Marcos A. Golato

    2005-12-01

    Full Text Available Como alternativa para aumentar la eficiencia térmica de calderas bagaceras productoras de vapor, se evalúa la inyección de aire secundario al hogar, previamente calentado. Además, se reúne información sobre la combustión y los factores que influyen en dicho fenómeno. Se calculó el rendimiento térmico en una caldera bagacera con inyección de aire secundario frío, mediante el empleo de balances de masa y energía con datos de ensayos experimentales. Se planteó luego un modelo teórico para el caso de calentar todo este aire secundario, y se determinó el nuevo rendimiento térmico. Finalmente se realizó un análisis técnico-económico para evaluar la rentabilidad del uso de esta tecnología, teniendo en cuenta el ahorro de bagazo y su equivalente en gas natural. Para el caso analizado, los resultados mostraron: aumento del rendimiento térmico de la caldera (1,62 puntos; mejora del índice de generación de vapor (2,27%; reducción del consumo de bagazo (2,45%; aceptable periodo de repago de la inversión (114 días de zafra.Previously heated secondary air injection is evaluated as an alternative to increase thermal efficiency of bagasse steam boilers. Aspects regarding the combustion process and the factors affecting it are also described. Tests were made in a bagasse boiler of a sugar mill. Thermal efficiency of the bagasse boiler with cold secondary air injection was determined by solving mass and energy balances. A new thermal efficiency for the case in which all secondary air is pre-heated with hot gases was determined afterwards. Finally, a technical-economic analysis was made to evaluate the yield of this technology, taking into account bagasse saving and its equivalent in natural gas. For the analyzed case, the results showed: an increase in the thermal efficiency of the boiler (1,62 points; a higher steam production index (2,27%; a reduction in bagasse consumption (2,45%; an acceptable payback period of the investment (114

  10. Complex variations during a caldera-forming Plinian eruption, including precursor deposits, thick pumice fallout, co-ignimbrite breccias and climactic lag breccias: The 184 ka Lower Pumice 1 eruption sequence, Santorini, Greece

    Science.gov (United States)

    Simmons, J. M.; Cas, R. A. F.; Druitt, T. H.; Folkes, C. B.

    2016-09-01

    The 184 ka Lower Pumice 1 eruption sequence records a complex history of eruption behaviours denoted by two significant eruptive phases: (1) a minor precursor (LP1-Pc) and (2) a major Plinian phase (LP1-A, B, C). The precursor phase produced 13 small-volume pyroclastic fallout, surge and flow deposits, which record the transition from a dominantly magmatic to a phreatomagmatic eruptive style, and exhibit a normal (dacite to andesitic-dacite) to reverse (andesitic-dacite to dacite) compositional zonation of juvenile pyroclasts in the stratigraphy. Incipient bioturbation and variability in unit thickness and lithology reflect multiple time breaks and highlight the episodic nature of volcanism prior to the main Plinian eruption phase. The Plinian magmatic eruption phase is defined by three major stratigraphic divisions, including a basal pumice fallout deposit (LP1-A), an overlying valley-confined ignimbrite (LP1-B) and a compositionally zoned (rhyodacite to basaltic andesite) lithic-rich lag breccia (LP1-C), which caps the sequence. This sequence records the initial development of a buoyant convective eruption column and the transition to eruption column and catastrophic late-stage caldera collapse events. Similarities in pyroclast properties (i.e., chemistry, density), between the Plinian fallout (LP1-A) and pyroclastic flow (LP1-B) deposits, indicate that changes in magma properties exerted no influence on the dynamics and temporal evolution of the LP1 eruption. Conversely, lithic breccias at the base of the LP1-B ignimbrite suggest that the transition from a buoyant convective column to column collapse was facilitated by mechanical erosion of the conduit system and/or the initiation of caldera collapse, leading to vent widening, an increase in magma discharge rate and the increased incorporation of lithics into the eruption column, causing mass overload. Lithic-rich lag breccia deposits (LP1-C), which cap the eruption sequence, record incremental, high

  11. Utilizando uma rede neural artificial para aproximação da função de evolução do sistema de Lorentz

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    Andrea Martiniano

    2016-04-01

    Full Text Available O objetivo principal deste artigo é realizar a aproximação da função de evolução temporal do Sistema de Lorenz utilizando uma Rede Neural Artificial do tipo MLP (Multilayer Perceptron. Além deste objetivo principal, como objetivo específico, apresentam-se os conceitos básicos das Redes Neurais Artificiais (RNAs, um breve histórico da Teoria do Caos e o Sistema de Lorentz. A metodologia adotada na estruturação deste artigo foi definida como bibliográfica e experimental. Atualmente, existe grande interesse nos modelos de redes neurais para resolver problemas não convencionais e complexos, nesse contexto, as Redes Neurais Artificiais têm surgido como alternativa para inúmeras aplicações em diversas áreas do conhecimento. Os resultados obtidos nos experimentos apontam positivamente para a utilização das RNAs. Espera-se com esse artigo incentive a utilização das RNAs em aplicações complexas em que a aprendizagem, associação, generalização e abstração são necessárias para apoio à tomada de decisão.

  12. Un modelo de sistema dinámico híbrido utilizando el enfoque de la lógica difusa

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    Germán García Benítez

    2010-01-01

    Full Text Available Se presenta un modelo de sistema dinámico híbrido utilizando la lógica difusa. Para lograr esto se hace una breve descripción de los principales enfoques que se tienen en la actualidad de los sistemas dinámicos híbridos desarrollando las ecuaciones básicas de los bloques que conforman el modelo. Actualmente la teoría del control se ha centrado en el estudio por separado de la dinámica continua y la dinámica discreta; sin embargo, es necesario introducir el estudio de la combinación de ambos en un solo tratado. En el ámbito industrial los procesos son dinámicos y toda su estructura de control está basada en la teoría de la lógica digital. Sin embargo existe el paradigma de la lógica difusa, la cual se introduce en este artículo para proponer un nuevo enfoque. Cabe mencionar que para validar el modelo se utilizan herramientas computacionales de simulación de sistemas dinámicos.

  13. OBTENCIÓN DE UNA BEBIDA FERMENTADA A PARTIR DE SUERO DE QUESO UTILIZANDO CÉLULAS INMOVILIZADAS DE KLUYVEROMYCES MARXIANUS

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    Rocío Cóndor G.

    2014-06-01

    Full Text Available El presente estudio tuvo como objetivo principal optimizar la tecnología de producción de una bebida fermentada de suero de queso, utilizando Kluyveromyces marxianus e inmovilización de células. En el biorreactor de lecho empacado, se obtuvo el mayor rendimiento (11,46±0,81 oGL con un flujo de 140-150 mL. h-1, una biomasa inmovilizada de 10% (v/v, una relación de columna de 1:12 (diámetro: longitud, tamaño de perlas de 3 mm de diámetro, adición de metabisulfito de sodio (100 pg. mL-1 y células inmovilizadas con 2% (p/v de alginato. Luego de optimizado todos los parámetros de fermentación en el biorreactor, la bebida alcohólica fue sometida a inactivación a 70 oC por 5 minutos (tratamiento térmico y clarificación con tierra de diatomeas (11 kg. M-2. Finalmente, la bebida alcohólica fue evaluada en almacenamiento por 6 meses, durante este período se le hicieron evaluaciones fisicoquímicas, microbiológicas y sensoriales. Se determinó por Escala Hedónica y Ranking que la bebida alcohólica de suero tiene aceptabilidad.

  14. Modelación computacional, utilizando el Método de los Elementos Finitos, de anclajes Tipo T Invertida para torres atirantadas de telecomunicaciones.

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    Mariela Paez Castillo

    2015-01-01

    Full Text Available Las torres de telecomunicaciones son estructuras esbeltas de poco peso propio sometidas a esfuerzos laterales producto de las cargas horizontales. Debido a la magnitud que toman estos esfuerzos, se producen desplazamientos que llegan a ser máximos en su tope y pueden poner en riesgo su estabilidad o serviciabilidad. Para reducirlos se atirantan con cables de acero, tensados de forma radial al suelo. Las cimentaciones de estos cables se denominan anclajes. En Cuba la tipología más usada para anclajes es la de tipo bloque, sin embargo resulta muy costosa por el gasto de material que conlleva su construcción. El presente artículo realiza un estudio comparativo entre las tipologías, bloque y T invertida; esta última es un anclaje prefabricado que sustituye una parte considerable del volumen de hormigón por suelo, resultando mucho más económico. La comparación se realiza a partir de simulaciones utilizando el programa ABAQUS.

  15. DISTRIBUIÇÃO ESPACIAL DO BICHO-FURÃO,Gymnandrosoma aurantiana (Lima, 1927(LEPIDOPTERA: TORTRICIDAE,EM CITROS UTILIZANDO GEOESTATÍSTICA

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    JOÃO HENRIQUE SILVA CARVALHO

    2015-09-01

    Full Text Available RESUMO O bicho-furão, Gymnandrosoma aurantiana (Lima, 1927, é uma das principais pragas da citricultura brasileira, pois os frutos atacados pelas lagartas tornam-se inviáveis para o consumo in natura e processamento industrial. Objetivou-se estudar a distribuição espacial dos danos causados por G. aurantiana utilizando geoestatística. Para tanto, foi conduzido um experimento em um pomar de laranjeira-doce da variedade ‘Valência’, enxertado sobre limoeiro ‘Cravo’, localizado em Taquaritinga-SP, Brasil. A área foi dividida em 88 parcelas, sendo cada parcela formada por 30 plantas dispostas em três linhas de 10 plantas, e em seguida foi obtido o número de frutos atacados para os anos de 2007 e 2008. A distribuição dos frutos atacados pela praga foi agregada ao longo das avaliações, com variância maior que a média para todas as amostragens. Os dados apresentaram ajuste adequado segundo o modelo esférico, e o alcance da dependência espacial (a variou entre 40,66 e 135,40 m. A estimativa de frutos atacados nas áreas não amostradas foi obtida pela krigagem, e os principais focos da praga foram observados nas parcelas próximas aos limites da área experimental.

  16. Estimation of mechanical properties of rock using artificial intelligence Estimación de propiedades mecánicas de roca utilizando inteligencia artificial

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    César Augusto Ochoa

    2011-12-01

    Full Text Available This paper discusses how two artificial intelligence techniques were combined, neural networks and genetic algorithms for the development of a computational tool used for the estimation of mechanical properties such as tensile strength, uniaxial compressive strength and triaxial compressive strength in sandstones, from petrophysical properties using data from tests of Rock Mechanics Laboratory of the Colombian Petroleum Institute - Ecopetrol SA as training data, to improve the design of non-destructive testing with some degree of confidence and resulting in cost reduction.Este artículo presenta la forma como fueron combinadas dos técnicas de inteligencia artificial, redes neuronales y algoritmos genéticos, para el desarrollo de una herramienta computacional utilizada para la estimación de propiedades mecánicas tales como la resistencia a la tensión, la resistencia a la compresión uniaxial y la resistencia a la compresión triaxial en areniscas, a partir de propiedades petrofísicas utilizando datos de pruebas del Laboratorio de Mecánica de Rocas del Instituto Colombiano del Petróleo - Ecopetrol S.A. como datos de entrenamiento facilitando el diseño de ensayos no destructivos con cierto grado de confianza y dando lugar a una reducción de costos.

  17. Avaliação do risco ambiental utilizando FMEA em um laticínio na região de Lavras – MG

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    Amanda Cássia Nogueira

    2010-11-01

    Full Text Available Uma metodologia que vem sendo paulatinamente empregada na avaliação do risco ambiental durante o processo produtivo é o FMEA (do inglês – Failure Mode and Effect Analysis, definida como uma ferramenta que busca em princípio, evitar ou minimizar as chances do produto ou processo falhar, aumentando assim a sua confiabilidade. Considerando que o impacto ambiental gerado por um laticínio apresenta diversos riscos em potencial, este método foi empregado na avaliação do risco ambiental durante o processamento de queijos em um laticínio da região de Lavras – MG. Um levantamento das entradas e saídas de cada operação do processo foi feito e as saídas que apresentaram risco ambiental foram analisadas utilizando-se um formulário para aplicação do método. Ações foram sugeridas de acordo com as mesmas, colaborando para a diminuição da probabilidade do risco ambiental gerado ocorrer à medida que estas ações foram sendo aplicadas, contribuindo para um processo mais sustentável e eficiente.

  18. ESTUDIO DE LAS FASES MINERALÓGICAS DEL CLÍNKER EN UNA CEMENTERA ESPAÑOLA, UTILIZANDO EL MÉTODO DE RIETVELD

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    ANA M. CASTAÑÓN

    2012-01-01

    Full Text Available Con el objetivo de implantar un método de control de calidad de forma continua en una fábrica de cementos española, para mejorar las características del producto final, se están desarrollando nuevas metodologías de caracterización. El método de Rietveld [1] se ha utilizado con éxito para analizar la composición de las fases principales del clínker. Utilizando esta metodología, se ha llevado a cabo un estudio para cuantificar adecuadamente la fase minoritaria de Cal Libre, de gran importancia en la calidad del clínker. El método ha permitido obtener unos resultados satisfactorios en muestras cuyos contenidos superan el 3% de CaO. Estos resultados son posibles combinando adecuadamente las técnicas de difracción y fluorescencia de rayos-X, así como los resultados del análisis por vía química.

  19. PROPOSTA EDUCATIVA UTILIZANDO O JOGO RPG MAKER: ESTRATÉGIA DE CONSCIENTIZAÇÃO E DE APRENDIZAGEM DA QUÍMICA AMBIENTAL

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    Ticiane Vieira de Paula Souza

    2016-01-01

    Full Text Available Este trabalho refere-se à utilização do RPG Maker (software educativo como objeto de aprendizagem (OA para conscientização e contextualização do ensino de Química, no âmbito do Ensino Médio. A relação entre a Educação Ambiental e o ensino de Química possibilita aos educandos observar as transformações que ocorrem no ambiente melhorando, por conseguinte, sua compreensão dos conteúdos. Visto que é o professor que tem a função de escolher a metodologia que viabilize a reflexão e uma compreensão crítica sobre a realidade em que o aluno está inserido, propõe-se que uma das formas viáveis de trabalhar a Educação Ambiental no ensino de Química é contextualizar os assuntos utilizando um OA, como o software educativo baseado no RPG Maker. Conforme foi visualizado neste trabalho, o uso do OA tornou a aula mais interessante, contextualizada e facilitou a aprendizagem do assunto relacionado à Química Ambiental.

  20. Diseño de una experiencia interactiva multimedia en el espacio utilizando sensores de ultrasonido Design of interactive multimedia experience in the space using ultrasound sensors

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    Galeano Roylan

    2009-01-01

    Full Text Available El objetivo del trabajo fue diseñar una experiencia multimedia interactiva en el espacio, para construir un procedimiento que permita elaborar este tipo de proyectos, entendiendo los roles de las diferentes disciplinas involucradas. Se diseñó un instrumento multimedia que traducía los movimientos de las manos, en melodías acompañadas de animaciones, utilizando sensores de ultrasonido. Se hallaron cuatro etapas: Indagación, creación, materialización y evaluación, que involucraron varios diseñadores gráficos, un programador y un ingeniero electrónico. Se concluyó que el diseño de una experiencia interactiva es un proceso en espiral que requiere la participación de un grupo interdisciplinario. The objective of this work was to design an interactive multimedia experience in space, to build a procedure that allows creating these experiences, understanding the roles of different disciplines involved. A multimedia instrument was designed to translate the movements of the hands, into melodies and animations, using ultrasound sensors. Four steps were found: Inquiry, creation, development and evaluation that involved several graphic designers, a musician, a programmer and an electronic engineer. Interactive experience design is a spiral and interdisciplinary process.

  1. Custo da eletricidade gerada em conjunto motor gerador utilizando biogás da suinocultura - DOI: 10.4025/actascitechnol.v26i2.1510

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    Samuel Nelson Melegari de Souza

    2004-03-01

    Full Text Available Uma das maiores fontes de energia disponíveis nas áreas rurais e agroindustriais é a biomassa. A mesma aparece na forma de resíduos vegetais e animais, tais como restos de colheita, esterco animal, plantações energéticas e efluentes agroindustriais. Estes resíduos podem ser utilizados pelo produtor rural ou agroindústria para a queima direta, visando a produção de calor ou produção de biogás em biodigestores. Nas propriedades agrícolas, onde há a atividade de suinocultura, ocorre a disponibilidade desses resíduos, caracterizando-se num grande potencial energético. No presente trabalho objetivou-se determinar o custo e viabilidade de produção de eletricidade gerada a partir do biogás EM uma propriedade rural, utilizando-se como equipamentos de conversão de biogás em eletricidade, um motor de combustão interna acoplado a um gerador elétrico

  2. REPLICAÇÃO DE FÓSSEIS DE FORAMINIFERA UTILIZANDO REAPROVEITAMENTO DE “ISOPOR” COM ALUNOS DO IFPB-CG

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    Hermes de Oliveira Machado Filho

    2011-09-01

    Full Text Available Os fósseis são unidades paleontológicas preciosas e difíceis de serem coletadas para pesquisas ou principalmente para aulas práticas sobre o passado geológica da Terra. Desta forma, lançam-se mão de técnicas alternativas para se fazer réplicas dessas unidades. O presente artigo vem apresentar atividades de sistemática paleozoológica, utilizando o “isopor” como matéria prima para confecção de modelos de fósseis em aulas práticas para a comunidade escolar do Instituto Federal de Educação, Ciência e Tecnologia da Paraíba, campus de Campina Grande. Dessa forma, o instituto está iniciando a construção de um acervo visual 3D alternativo de fósseis guia do grupo dos Foraminifera, em específico, os bioindicadores de petróleo, além de contribuir para reutilização de resíduos sólidos poluidores ao meio ambiente.

  3. PROTOTIPO PARA EL ANÁLISIS DEL RENDIMIENTO EN EL TRÁFICO DE UN SERVICIO BROADCAST UTILIZANDO LOS PROTOCOLOS HTTP Y RTP SOBRE IPV6 EN UNA RED ACADÉMICA DE TECNOLOGÍA AVANZADA

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    Roberto Ferro

    2011-08-01

    Full Text Available En el presente artículo se condensan los resultados obtenidos de la implementación y modelado de un Prototipo de Servicio Streaming sobre el Sistema Operativo Fedora 13 con el Programa VLC en la Red de Investigación y  Tecnología Avanzada de la Universidad Distrital RITA-UD sobre IPV6 utilizando como cliente la Universidad Minuto de Dios vía RUMBO mediante un Tunel 6a4.

  4. Why does the Size of the Laacher See Magma Chamber and its Caldera Size not go together? - New Findings with regard to Active Tectonics in the East Eifel Volcanic Field

    Science.gov (United States)

    Schreiber, Ulrich; Berberich, Gabriele

    2013-04-01

    The East Eifel's early Cenozoic tectonic development is characterized by a main stress field trending in NW-SE direction, causing a re-organisation of postvariscan dextral strike-slip faults in approximately 105° direction, the formation of the tectonic depression of the Neuwieder Basin and small-scale transtension zones. The 105° trending strike-slip faults are staggered in equidistant intervals of several kilometers. This system continues from the Eifel to the North into the Ruhr Carboniferous, where it has been recognized due to the extensive underground coal mining first (Loos et al. 1999). Our recent research on analyses of tectonics in quarries, quartz/ore-dykes, mapping of minerals springs and gas analyses, has revealed a prominent 105° trending strike-slip fault cutting the South of Laacher See ("Laacher See Strike-slip Fault"). Within the Laacher See caldera, the "Laacher See Strike-slip Fault" can be tracked by a wide mofette zone that was mapped with a self-propelled submarine. At present, the "Laacher See Strike-slip Fault" can be tracked from Holzmühlheim in the West, Spessart, Wehrer Kessel, Laacher See, Plaidt to Bad Ems and furthermore to the South-East. Along this direction five intersections points of the "Laacher See Strike-slip Fault" with the Lahn River are documented, creating small-scale mofette fields in the Lahn River. In the Neuwied Basin, near Plaidt, the "Laacher See Strike-slip Fault" is intersected by the NW-SE-trending Ochtendung Fault. Regional strike-slip faults in combination with block rotation and uplift could have provided the voids for the magma chambers of the Wehrer Kessel and the Laacher See Caldera. Holohan et al. (2005) showed in analogue models that regional strike-slip regimes (including Riedel shears, chamber-localised graben fault, and a partial Y-shear) play a decisive role for caldera formation. In the East Eifel tectonic movement rates of active faults are approx. 1 mm/year (Meyer & Stets 2002, Cambell et al

  5. Avaliação do tratamento da discopatia degenerativa cervical pela artrodese via anterior utilizando placas associadas a cages ou cages em peek isoladamente Evaluación del tratamiento de la enfermedad degenerativa del disco cervical por la artrodesis anterior utilizando placas asociadas con jaulas o jaulas en peec, aisladamente Evaluation of cervical degenerative disc disease treatment by anterior arthrodesis using plates associated with cages or cages in peek alone

    OpenAIRE

    André Rafael Hübner; Marcelo Ribeiro Mendes; Jean Carlo Frigotto Queruz; Jean Marcel Dambrós; Álvaro Diego Heredia Suárez; Leandro de Freitas Spinelli

    2011-01-01

    OBJETIVOS: Avaliar comparativamente o tratamento da discopatia degenerativa cervical por discectomia e artrodese cervical via anterior utilizando placas associadas a cages ou cages em PEEK isoladamente. MÉTODOS: Foi realizado um estudo retrospectivo comparativo entre dois grupos de pacientes operados pela técnica de discectomia e artrodese cervical via anterior. Foram selecionados aleatoriamente 70 pacientes, 35 operados com o método de fixação com placas associadas a cages - denominado Grupo...

  6. EVALUACIÓN DE LA BIOESTIMULACIÓN (NUTRIENTES EN SUELOS CONTAMINADOS CON HIDROCARBUROS UTILIZANDO RESPIROMETRÍA Evaluation of Biostimulation (Nutrients in Hydrocarbons Contaminated Soils by Respirometry

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    ERIKA GARCÍA

    Full Text Available Se evaluó el proceso de bioestimulación por nutrientes utilizando fertilizantes inorgánicos compuestos (FIC N:P:K 28:12:7 y sales inorgánicas simples (SIS NH4NO3 y K2HPO4 en suelos contaminados con hidrocarburos utilizando respirometría. El suelo fue contaminado con lodos aceitosos a una concentración 40.000 mgTPH/kgps. Para cuantificar el consumo de oxígeno se utilizaron dos respirómetros de medición manométrica HACH® 2173b y OXITOP® PF600 durante ensayos de 13 días (n=3. Se evaluaron dos tratamientos (FIC y SIS y tres controles (abiótico, sustrato de referencia y sin nutrientes. Se analizaron parámetros físico-químicos (pH, nutrientes y TPH y microbiológicos (heterótrofos y degradadores al inicio y al final de cada ensayo. SIS y el control sin nutrientes presentaron las mayores tasas de respiración, en el equipo HACH se obtuvieron valores de 802,28 y 850,72 mgO2kgps-1d-1 respectivamente, y en OXITOP fueron de 936,65 y 502,05 mgO2kgps-1d-1, respectivamente, indicando que los nutrientes de SIS estimularon el metabolismo microbiano. Por otro lado, FIC presentó los recuentos y tasas de respiración más bajas (188,18 y 139,87 mgO2kgps-1d-1 en HACH y OXITOP, respectivamente, esto pudo estar relacionado a un efecto inhibitorio generado por la acumulación de amoniaco, limitando el crecimiento de la población degradadora.The biostimulation process was evaluated in a hydrocarbon contaminated soil by respirometry after amendment with inorganic compound fertilizer (ICF (N:P:K 28:12:7 and simple inorganic salts (SIS (NH4NO3 and K2HPO4. The soil was contaminated with oily sludge (40,000 mgTPH/kgdw. The oxygen uptake was measured using two respirometers (HACH® 2173b and OXITOP® PF600 during thirteen days (n=3. Two treatments (ICF and SIS and three controls (abiotic, reference substance and without nutrients were evaluated during the study. Physicochemical (pH, nutrients, and TPH and microbiological analysis (heterotrophic and

  7. Modeling water movement in horizontal columns using fractal theory Modelagem de movimento horizontal de água no solo utilizando a teoria dos fractais

    Directory of Open Access Journals (Sweden)

    Tairone Paiva Leão

    2010-08-01

    horizontal de água foram realizadas no modelo numérico Hydrus 2D. Os parâmetros sortividade (S e expoente de tempo (n da equação de Philip foram estimados para cada simulação, utilizando o módulo de regressão não linear do software SAS®. A sortividade aumentou com o aumento de material de textura franca nas colunas, o que foi atribuído à dependência do parâmetro S no raio capilar. O parâmetro expoente de tempo estimado por regressão não linear mostrou valor menor que o valor empírico de 0,5 sugerido na literatura. A dimensão fractal estimada utilizando o expoente de Hurst foi 17,5 % menor do que a dimensão fractal do Conjunto de Cantor utilizado para gerar as colunas.

  8. Metodología para la toma de decisiones de inversión en portafolio de acciones utilizando la técnica multicriterio AHP

    Directory of Open Access Journals (Sweden)

    John Willmer Escobar

    2015-01-01

    Full Text Available Este artículo presenta una metodología para la toma de decisiones en el mercado accionario colombiano utilizando la técnica multicriterio Analytic Hierarchy Process (AHP. La problemática está relacionada con el proceso de inversión en un mercado bursátil considerando criterios de riesgo y rentabilidad. La metodología propuesta incluye la integración de las técnicas tradicionales de decisión de inversión en portafolio de acciones junto con la técnica multicriterio AHP que permite evaluar un número finito de alternativas de manera jerárquica bajo criterios cualitativos y cuantitativos. La metodología ha sido probada en la solución del problema de selección de portafolio de acciones de alta y media bursatilidad que cotizaron en el mercado colombiano durante el periodo de diciembre de 2007 a abril de 2010. Los resultados computacionales muestran la importancia y la eficiencia de la integración exitosa de los criterios tradicionales de inversión en portafolio de acciones junto con la metodología AHP para encontrar un balance apropiado entre rentabilidad y riesgo en el proceso de toma de decisiones de inversión en acciones en el mercado bursátil colombiano. Derechos reservados © 2015 Universidad Nacional Autónoma de México, Facultad de Contaduría y Administración. Este es un artículo de acceso abierto distribuido bajo los términos de la Licencia Creative Commons CC BY-NC-ND 4.0.

  9. Decapado del acero inoxidable AISI 316L utilizando una mezcla ecológica de H2O2-H2SO4-HF

    Directory of Open Access Journals (Sweden)

    Gómez, P. P.

    2005-12-01

    Full Text Available This study reports the pickling of austenitic AISI 316L stainless steel (SS using a mixture of hydrogen peroxide (H2O2, sulphuric acid (H2SO4 and hydrofluoric acid (HF at pH 2.0. The stability of H2O2 was also studied using different concentrations of ferric ion from 0 to 40 g/l and temperature from 25 to 60 °C. The pickling rate at 50 °C in the presence and absence of 40 g/l ferric ion was 2.6 and 0.2 mg/dm2 day (mdd, respectively. p-Toluene sulphonic acid was used as stabilizer of H2O2.En la presente investigación se estudia el decapado del acero inoxidable AISI 316L utilizando una mezcla de agua oxigenada (H2O2 y los ácidos sulfúrico (H2SO4 y fluorhídrico (HF a pH 2,0. La estabilidad de la mezcla H2O2-H2SO4-HF se ha ensayado variando el contenido de iones férrico de O a 40 g/l y la temperatura de 25 a 60 °C. La velocidad de decapado a 50 °C ha sido de 2,6 y 0,2 mg/dm2 día (mdd, en ausencia y presencia de 40 g/l de iones férrico, respectivamente. Se ha utilizado el ácido p-toluen sulfónico como estabilizante del H2O2.

  10. Evaluacion de la toxicidad de Cr+6 , Cu+2 y el efluente de cromado de una industria metalmecánica