Mineralogy of the silica-epidote mineralized zone (SEMZ) in the Cerro Prieto geothermal reservoir, B.C., Mexico; Mineralogia de la zona mineralizada de silice-epidota (ZMSE) del yacimiento geotermico de Cerro Prieto, B.C., Mexico

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Izquierdo, Georgina; Aragon, Alfonso; Portugal, Enrique; Arellano; Victor M [Instituto de Investigaciones Electricas, Gerencia de Geotermia, Cuernavaca, Morelos (Mexico)]. E-mail: gim@iie.org.mx; Leon, Jesus de; Alvarez, Julio [Comision Federal de Electricidad, B.C. (Mexico)

2006-07-15

The distribution of hydrothermal minerals, mineral assemblages and fluid inclusion data were taken from drill cuttings from the production zone of wells all over the Cerro Prieto geothermal field. The production zone has been termed the silica-epidote mineralized zone (SEMZ), and is located in the deep part of the gray shale where thick layers of sandstone are found. Common mineral assemblages show three temperature ranges in the SEMZ: <200 degrees Celsius, 200-250 degrees Celsius and 250-300 degrees Celsius. The first range is characterized by clays, calcite and quartz; the second by quartz, epidote, chlorite and mica, and the third by epidote, amphibole, illite and chlorite. The study of fluid inclusions in authigenic grain quartz has shown two-phase fluid inclusions (liquid + vapor) of different salinities. A wide range exists of homogenization temperatures (Th) and for some wells there is a good agreement between Th and direct temperature measurements. [Spanish] Se determino la distribucion de minerales hidrotermales y las asociaciones parageneticas y se realizo el estudio microtermometrico de inclusiones fluidas a partir de recortes de perforacion de pozos de las distintas areas del campo geotermico de Cerro Prieto. Las muestras de recortes y nucleos de perforacion estudiados provienen de la zona de produccion a la que se le ha denominado Zona Mineralizada de Silice-Epidota (ZMSE), que se encuentra en la parte profunda de la lutita gris con importantes horizontes de areniscas. En esta zona las asociaciones parageneticas mas comunes han mostrado tres intervalos de temperatura para la ZMSE: <200 degrees Celsius, 200-250 degrees Celsius, 250-300 degrees Celsius. El primer intervalo esta caracterizado principalmente por arcillas, calcita y cuarzo; el segundo por cuarzo, epidota, clorita y micas, y el tercero por epidota, anfiboles, illita y clorita. El estudio de inclusiones fluidas en fragmentos de cuarzo autigenico mostro la presencia de inclusiones de dos fases

The aggressiveness of the geothermal steam controlled; La agresividad del vapor geotermico controlada

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Mercado, Sergio [Instituto de Investigaciones Electricas, Cuernavaca (Mexico)

1990-12-31

The first two units of Cerro Prieto have generated electric energy since 1973; in 1988 completed 15 years of continuous operation, without corrosion problems in the turbines in spite of the utilization of geothermal steam. The experience and the good results obtained during the first years of operation of these two units of 37.5 MW each, were of great help for the Cerro Prieto extension, having as of this date an installed capacity of 620 MW. [Espanol] Las dos primeras unidades de Cerro Prieto han generado energia electrica desde 1973; cumplieron 15 anos de operacion continua en 1988, sin problemas de corrosion en las turbinas a pesar del uso de vapor geotermico. La experiencia y los buenos resultados obtenidos durante los primeros anos de operacion de estas dos unidades de 37.5 MW cada una fueron de gran apoyo para la aplicacion de Cerro Prieto, teniendose a la fecha 620 MW de capacidad instalada.

The aggressiveness of the geothermal steam controlled; La agresividad del vapor geotermico controlada

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Mercado, Sergio [Instituto de Investigaciones Electricas, Cuernavaca (Mexico)

1989-12-31

The first two units of Cerro Prieto have generated electric energy since 1973; in 1988 completed 15 years of continuous operation, without corrosion problems in the turbines in spite of the utilization of geothermal steam. The experience and the good results obtained during the first years of operation of these two units of 37.5 MW each, were of great help for the Cerro Prieto extension, having as of this date an installed capacity of 620 MW. [Espanol] Las dos primeras unidades de Cerro Prieto han generado energia electrica desde 1973; cumplieron 15 anos de operacion continua en 1988, sin problemas de corrosion en las turbinas a pesar del uso de vapor geotermico. La experiencia y los buenos resultados obtenidos durante los primeros anos de operacion de estas dos unidades de 37.5 MW cada una fueron de gran apoyo para la aplicacion de Cerro Prieto, teniendose a la fecha 620 MW de capacidad instalada.

Hydrothermal alteration zones and present reservoir conditions: an approach to define production zones at the eastern portion of the Cerro Prieto geothermal field, BC; Zonas de alteracion hidrotermal y condiciones actuales del yacimiento: un enfoque para determinar zonas productoras al oriente del campo geotermico de Cerro Prieto, BC

Energy Technology Data Exchange (ETDEWEB)

Camacho Hernandez, Juan Manuel [Comision Federal de Electricidad, Residencia General de Cerro Prieto, Mexicali, Baja California (Mexico)]. E-mail: juan.camacho02@cfe.gob.mx

2009-07-15

Geological factors are as essential for locating new wells as they are for defining the production zones of these wells. At the Cerro Prieto geothermal field (CGCP), one of the most important geological factors is identification of the hydrothermal alteration zones (ZAH). These are divided into silica and epidote mineralogical zones (ZMSE), without CaCO{sub 3}, and silica and epidote mineralogical transition zones (ZTMSE), with CaCO{sub 3}. It has been observed that the continuous variation of reservoir thermodynamic conditions (temperature, pressure and enthalpy) is due mainly to the exploitation of geothermal resources. The presence of new thermodynamic conditions recorded at the reservoir has led to the re-location of production wells originally located during the drilling campaign of 2004 to 2006. At the geological sections on the eastern part of the CGCP, adjustments made to the well completions lie on the limits between the ZMSE and ZTMSE zones. In turn, this is related to the current, superior, thermodynamic reservoir conditions. Based on this, a new geologic approach is proposed to define possible production zones for new wells, relating the ZAH zones to current thermodynamic reservoir conditions. [Spanish] Los factores geologicos son determinantes, tanto para establecer nuevos sitios de perforacion como para determinar el intervalo productor de un pozo nuevo. En el campo geotermico de Cerro Prieto (CGCP) una de los factores mas importantes es la determinacion de las zonas de alteracion hidrotermal (ZAH) que se dividen en dos: zona mineralogica de silice y epidota (ZMSE), sin presencia de CaCO{sub 3}, y zona de transicion mineralogica de silice y epidota (ZTMSE), con presencia de CaCO{sub 3}. Por otra parte, tambien se ha constatado que la continua variacion de las condiciones termodinamicas del yacimiento (temperatura, presion y entalpia) es originada en buena medida por la explotacion del recurso geotermico. La ocurrencia de nuevas condiciones

Geothermal drilling in Cerro Prieto

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Dominguez A., Bernardo

1982-08-10

The number of characteristics of the different wells that have been drilled in the Cerro Prieto geothermal field to date enable one to summarize the basic factors in the applied technology, draw some conclusions, improve systems and procedures, and define some problems that have not yet been satisfactorily solved, although the existing solution is the best now available. For all practical purposes, the 100 wells drilled in the three areas or blocks into which the Cerro Prieto field has been divided have been completed. Both exploratory and production wells have been drilled; problems of partial or total lack of control have made it necessary to abandon some of these wells, since they were unsafe to keep in production or even to be used for observation and/or study. The wells and their type, the type of constructed wells and the accumulative meters that have been drilled for such wells are summarized.

Gaseous equilibrium in sector CP IV of the Cerro Prieto, B.C. Mexico geothermal field; Equilibrio gaseoso en el sector CP IV del campo geotermico Cerro Prieto, B.C., Mexico

Energy Technology Data Exchange (ETDEWEB)

Barragan Reyes, Rosa Maria; Arellano Gomez, Victor Manuel; Portugal Marin, Enrique [Instituto de Investigaciones Electricas, Cuernavaca, Morelos (Mexico); De Leon Vivar, Jesus [Comision Federal de Electricidad, Campo Geotermico Cerro Prieto, Cerro Prieto, B. C. (Mexico)

2007-07-01

Sector CP IV is located in the NE portion of the Cerrro Prieto geothermal field. The wells of this zone produce two-phase fluids, with different characteristics as far as their steam fraction content; in the central part and towards the NW the fluids are of dominant liquid type whereas towards the E and the S, the fluid contains a relatively higher steam fraction. The results of gaseous equilibrium FT- HSH3 showed that the fluids in the deposit are at temperatures between 275 Celsius degrees and 310 Celsius degrees and contain steam fractions between 0.01 and 0.5. The data found for the natural state are aligned in a tendency defined in the diagram FT- HSH3, that suggest the wells receive different proportions from preexisting steam in the deposit, which are mixed with the liquid phase to produce the observed discharges. The present data, besides showing the presence of deposit steam, also indicates the entrance of lower temperature fluid in the central part of sector CP IV. [Spanish] El sector CP IV se localiza en la porcion NE del campo geotermico Cerro Prieto. Los pozos de esta zona producen fluidos bifasicos, con diferentes caracteristicas en cuanto a su contenido de fraccion de vapor: en la parte central y hacia el NW los fluidos son de tipo liquido dominante mientras que hacia el E y hacia el S, el fluido contiene una fraccion relativamente alta de vapor. Los resultados de equilibrio gaseoso FT-HSH3 mostraron que los fluidos en el yacimiento se encuentran a temperaturas de entre 275 grados Celsius y 310 grados Celsius y contienen fracciones de vapor de entre -.01 y .5. Los datos hallados para el estado natural se alinean en una tendencia definida en el diagrama FT-HSH3, que sugiere que los pozos reciben diferentes proporciones de vapor pre-existente en el yacimiento, que se mezclan con fase liquida para producir las descargas que se observan. Los datos actuales, ademas de mostrar la presencia de vapor de yacimiento, tambien indican la entrada de fluidos de

Overview of Cerro Prieto studies

Energy Technology Data Exchange (ETDEWEB)

Lippmann, M.J.

1983-01-01

The studies performed on the Cerro Prieto geothermal field, Mexico, since the late 1950's are summarized. Emphasis is given to those activities leading to the identification of the sources of heat and mass, the fluid flow paths, and the phenomena occurring in the field in its natural state and under exploitation.

Analysis of productive evolution of well M-19A, Cerro Prieto geothermal field, BC; Analisis de la evolucion productiva del pozo M-19A del campo geotermico de Cerro Prieto, BC

Energy Technology Data Exchange (ETDEWEB)

Rodriguez-Rodriguez, Marco H; Romero-Rios, Francisco [Comision Federal de Electricidad, Residencia General de Cerro Prieto, B.C (Mexico)]. E-mail: marco.rodriguez01@cfe.gob.mx

2007-07-15

Well M-19A has been the most productive in the Cerro Prieto field, producing around 40 million tons of fluid. The well went on line in February 1975 and was in continuous operation until June 2006. Monthly measurements for over 30 years of operating conditions and chemical and isotopic analyses of the fluids allow identification of the most significant processes occurring in the zone where the well is located. Three dominant recharge types have been identified, each lasting about 10 years. They are a) a recharge of fluids of lower temperature than the production fluids, even though the chemical and isotopic compositions are similar; b) a recharge of lower-temperature fluids with diluted chemical and isotopic compositions; and c) a progressive recharge of reinjected water with a higher chloride concentration and heavy isotopic composition. The production and reinjection rates for over 30 years of production history in the M-19A well zone allow for speculation of a reservoir pressure recovery, which is confirmed with a calculation using production data from well M-19A. The evolution of the reservoir pressure in the zone contrasts with the rest of the reservoir, where a constant pressure drop is observed, particularly toward the central and eastern parts of the field. [Spanish] El pozo M-19A ha sido el mas productivo del campo geotermico de Cerro Prieto, BC, alcanzando una extraccion de mas de 40 millones de toneladas de fluido. Fue integrado a produccion en febrero de 1975 y hasta junio de 2006 ha permanecido en produccion en forma continua. Las mediciones mensuales de sus condiciones operativas y los analisis quimicos e isotopicos del agua producida permiten identificar los procesos mas significativos que han ocurrido a lo largo de esos mas de 30 anos en la zona donde se localiza el pozo. Se han identificado tres tipos de recarga dominantes que se presentan durante un periodo cercano a 10 anos cada uno, los cuales son: a) una recarga de fluidos de menor temperatura

Criteria for determining casing depth in Cerro Prieto

Energy Technology Data Exchange (ETDEWEB)

Olivas M., H.M.; Vaca S., J.M.E.

1982-08-10

On the basis of geological data obtained during drilling and its relation to electric logs, together with the problems that arose when drilling through formations until the production zone was reached, it is possible to establish the most suitable manner to line a well and thus formulate an optimum casings program. The main criteria to be taken into consideration in preparing such a program and its application in the drilling of wells programmed in Cerro Prieto to optimize and economize such drilling and achieve suitable techniques for well completion are presented. The criteria are based on the characteristics of the Cerro Prieto field and on casing design factors, as well as a experience gained during drilling in such a field.

Heat losses estimation associated with the physical state of the thermal insulation of pipes vaporductos network in Cerro Prieto geothermal field; Estimacion de perdidas de calor asociadas al estado fisico del aislamiento termico de las tuberias de la red de vaporductos del campo geotermico Cerro Prieto

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Ovando Castelar, Rosember; Martinez Estrella, Juan Ignacio; Garcia Gutierrez, Alfonso [Instituto de Investigaciones Electricas, Cuernavaca, Morelos (Mexico)]. E-mail: rovando@iie.org.mx; jime@iie.org.mx; aggarcia@iie.org.mx; Canchola Felix, Ismael; Miranda Herrera, Carlos; Jacobo Galvan, Paul [Campo Geotermico de Cerro Prieto, Comision Federal de Electricidad, Mexicali, B.C. (Mexico)

2010-11-15

The Cerro Prieto Geothermal Field (CPGF) steam transportation network is constituted by 140 km of pipes with diameters ranging from 8 to 48 inches, which transport the steam of 165 producing wells to 13 power plants which have a total installed capacity of 720 MWe. Originally, the pipes are thermally insulated with a mineral wool or fiber glass layer and an external aluminum or iron cover. Due to the insulation material has been exposed to weather conditions during the field operation it shows nowadays different grades of wear-out, or even it is lacking in some parts of the network, causing higher heat losses from the pipes to the environment. In this work, the magnitude of the heat losses related with the present condition of the thermal insulation throughout the pipeline network is assessed. This involved determining the longitude and diameter, as well as the insulation condition of each single pipeline section, and the calculation of the heat transfer coefficients for the different thermal insulation conditions defined for this study. [Spanish] La red de transporte de vapor del campo geotermico Cerro Prieto (CGCP) esta constituida por aproximadamente 140 km de tuberias de 8 a 48 pulgadas de diametro, las cuales conducen el vapor producido por 165 pozos hacia 13 plantas generadoras, cuya capacidad instalada es de 720 MWe. Originalmente, estas tuberias son aisladas termicamente con una capa de 2 pulgadas de material aislante a base de lana mineral o fibra de vidrio, y una proteccion exterior de aluminio o hierro. Debido principalmente al impacto de las condiciones meteorologicas durante el tiempo de operacion del campo, en algunas porciones de la red el aislante presenta actualmente distintos grados de deterioro, o incluso se encuentra ausente, lo cual se traduce en una mayor perdida de calor desde las tuberias hacia el medio ambiente. En el presente trabajo se evalua la magnitud de las perdidas de calor asociadas al estado fisico del aislamiento termico de las

Exploration and development of Cerro Prieto

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Teilman, M.A.; Cordon, U.J.

1981-01-01

A brief retrospective of the exploration and field model development at Cerro Prieto are presented. Representative field models are presented for each of the work phases. These models demonstrate how the concept of the field evolved - from a small 2 km/sup 2/ area with a relatively unknown reservoir configuration - to a geothermal resource area over 20 km/sup 2/ where the hydrothermal processes and structural environment are being studied in detail. A model integrating information from these studies was developed.

Microfaunal evidence of age and depositional environments of the Cerro Prieto section (Plio-Pleistocene), Baja California, Mexico

Energy Technology Data Exchange (ETDEWEB)

Ingle, J.C. Jr.

1982-01-01

Microfossils including benthic and planktic foraminifera, ostracodes, calcareous algae, fish skeletal material, and fragments of pelecypods were found in 14 core samples from depths of 185 to 1952 m in the Cerro Prieto geothermal field, providing evidence of both the age and depositional history of sediments comprising the 3000-m-thick Pliocene and Pleistocene section in this area. Ostracodes of brackish water and marine origin constitute the most common microfossils present in this sequence occurring in 8 samples; in situ littoral and neritic species of benthic foraminifera occur in 5 samples with planktic species present in 2 samples. Distributional patterns of ostracodes and foraminifera together with previously analyzed lithofacies (Lyons and van de Kamp, 1980) indicate that the Cerro Prieto section represents an intertonguing complex of alluvial, deltaic, estuarine, and shallow marine environments deposited along the front of the Colorado River delta as it prograded across the Salton Trough during Pliocene and Pleistocene time. Foraminiferal evidence indicates that a sand and shale unit commonly present at depths between 700 and 1100 m represents a significant mid-Pleistocene marine incursion in the Cerro Prieto area. Tentative correlation of the Cerro Prieto section with the well dated Palm Springs Formation of the Imperial Valley, California area suggests that the Pliocene/Pleistocene boundary occurs at a depth of approximately 2000 m in the area of well M-93. Reworked specimens of Cretaceous foraminifera and fragments of the Cretaceous pelecypod Inoceramus were found in five samples further substantiating the Colorado Plateau provenance of a significant portion of the Colorado River deltaic sediments in the Cerro Prieto area.

Extension of the Cerro Prieto field and zones in the Mexicali Valley with geothermal possibilities in the future

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Fonseca L, H.L.; de la Pena L, A.; Puente C, I.; Diaz C, E.

1981-01-01

This study concerns the possible extension of the Cerro Prieto field and identification of other zones in the Mexicali Valley with geothermal development potential by assessing the structural geologic conditions in relation to the regional tectonic framework and the integration of geologic and geophysical surveys carried out at Cerro Prieto. This study is based on data obtained from the wells drilled to date and the available geological and geophysical information. With this information, a geologic model of the field is developed as a general description of the geometry of what might be the geothermal reservoir of the Cerro Prieto field. In areas with geothermal potential within the Mexicali Valley, the location of irrigation wells with anomalous temperatures was taken as a point of departure for subsequent studies. Based on this initial information, gravity and magnetic surveys were made, followed by seismic reflection and refraction surveys and the drilling of 1200-m-deep multiple-use wells. Based on the results of the final integration of these studies with the geology of the region, it is suggested that the following areas should be explored further: east of Cerro Prieto, Tulecheck, Riito, Aeropuerto-Algodones, and San Luis Rio Colorado, Sonora.

Exploration and development of the Cerro Prieto geothermal field

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Lippmann, M.J.; Goldstein, N.E.; Halfman, S.E.; Witherspoon, P.A.

1983-07-01

A multidisciplinary effort to locate, delineate, and characterize the geothermal system at Cerro Prieto, Baja California, Mexico, began about 25 years ago. It led to the identification of an important high-temperature, liquid-dominated geothermal system which went into production in 1973. Initially, the effort was undertaken principally by the Mexican electric power agency, the Comision Federal de Electricidad (CFE). Starting in 1977 a group of US organizations sponsored by the US Department of Energy, joined CFE in this endeavor. An evaluation of the different studies carried out at Cerro Prieto has shown that: (1) surface electrical resistivity and seismic reflection surveys are useful in defining targets for exploratory drilling; (2) the mineralogical studies of cores and cuttings and the analysis of well logs are important in designing the completion of wells, identifying geological controls on fluid movement, determining thermal effects and inferring the thermal history of the field; (3) geochemical surveys help to define zones of recharge and paths of fluid migration; and (4) reservoir engineering studies are necessary in establishing the characteristics of the reservoir and in predicting its response to fluid production.

222Radon Concentration Measurements biased to Cerro Prieto Fault for Verify its Continuity to the Northwest of the Mexicali Valley.

Science.gov (United States)

Lazaro-Mancilla, O.; Lopez, D. L.; Reyes-Lopez, J. A.; Carreón-Diazconti, C.; Ramirez-Hernandez, J.

2009-05-01

The need to know the exact location in the field of the fault traces in Mexicali has been an important affair due that the topography in this valley is almost flat and fault traces are hidden by plow zone, for this reason, the southern and northern ends of the San Jacinto and Cerro Prieto fault zones, respectively, are not well defined beneath the thick sequence of late Holocene Lake Cahuilla deposits. The purpose of this study was to verify if Cerro Prieto fault is the continuation to the southeast of the San Jacinto Fault proposed by Hogan in 2002 who based his analysis on pre-agriculture geomorphy, relocation and analysis of regional microseismicity, and trench exposures from a paleoseismic site in Laguna Xochimilco, Mexicali. In this study, four radon (222Rn) profiles were carried out in the Mexicali Valley, first, to the SW-NE of Cerro Prieto Volcano, second, to the W-E along the highway Libramiento San Luis Río Colorado-Tecate, third, to the W-E of Laguna Xochimilco and fourth, to the W-E of the Colonia Progreso. The Radon results allow us to identify in the Cerro Prieto profile four regions where the values exceed 100 picocuries per liter (pCi/L), these regions can be associated to fault traces, one of them associated to the Cerro Prieto Fault (200 pCi/L) and other related with Michoacán de Ocampo Fault (450 pCi/L). The profile Libramiento San Luis Río Colorado-Tecate, show three regions above 100 pCi/L, two of them related to the same faults. In spite of the results of the Laguna Xochimilco, site used by Hogan (2002), the profile permit us observe three regions above the 100 pCi/L, but we can associate only one of the regions above this level to the Michoacán de Ocampo Fault, but none region to the Cerro Prieto Fault. Finally in spite of the Colonia Progreso is the shortest profile with only five stations, it shows one region with a value of 270 pCi/L that we can correlate with the Cerro Prieto Fault. The results of this study allow us to think in the

Relationship between water chemistry and sediment mineralogy in the Cerro Prieto geothermal field: a preliminary report

Energy Technology Data Exchange (ETDEWEB)

Valette-Silver, J.N. (Univ. de Perpignan, France); Thompson, J.M.; Ball, J.W.

1981-01-01

The chemical compositions of waters collected from the Cerro Prieto geothermal production wells and hydrothermal emanations are different. Compared to the Cerro Prieto well waters, the surficial waters generally contain significantly less potassium, slightly less calcium and chloride, and significantly more magnesium and sulfate. In comparison to the unaltered sediments, the changes in the mineralogy of the altered sediments appear to be controlled by the type of emanation (well, spring, mud pot, geyser, fumarole, or cold pool). However, an increase in quartz and potassium feldspar percentages seems to be characteristic of the majority of the sediments in contact with geothermal fluids. Preliminary attempts to model the chemical processes occurring in the Cerro Prieto geothermal field using chemical equilibrium calculations are reported. For this purpose the chemical compositions of thermal waters (well and surficial emanation) were used as input data to make calculations with SOLMNEQ and WATEQ2 computer programs. Then the theoretical mineral composition of altered sediments was predicted and compared to the mineralogy actually observed in the solid samples.

Evaluation of a process for the removal of gases contained in geothermal steam through condensation and re-evaporation; Evaluacion de un proceso de remocion de gases contenidos en el vapor geotermico, por medio de la condensacion y de revaporacion

Energy Technology Data Exchange (ETDEWEB)

Angulo C, Raul; Lam Rea, Luis; Garmino, Hector; Jimenez, Humberto [Instituto de Investigaciones Electricas, Cuernavaca (Mexico)

1986-12-31

The Cerro Prieto I Geothermal Field, developed and operated by the Comision Federal de Electricidad (CFE), has currently an installed electric power generation capacity of 180 MW and is at a very advanced stage in the development of Cerro Prieto II and III, which will allow to raise the generation capacity to 620 MW. During the exploitation of a geothermal field, in producing steam with the purpose of generating electricity, brines and waste gases are obtained. The hydrogen sulfide exhaust to the environment implies pollution problems, for this reason processes have been developed for the oxidation of these gases downstream the turbogenerator either in the flow of separated gases in the steam condensation or in the condensate produced. The Instituto de Investigaciones Electricas (IIE) has collaborated with CFE in the evaluation of the environmental impact of this gas and in the development of the processes for its abatement. [Espanol] El campo geotermico de Cerro Prieto I, desarrollado y operado por la Comision Federal de Electricidad (CFE), actualmente tiene una capacidad instalada de generacion de energia electrica de 180 MW, y se encuentra en etapa muy avanzada, el desarrollo de Cerro Prieto II y III, lo que permitira incrementar la capacidad de generacion a 620 MW. Durante la explotacion de un campo geotermico, al producir vapor con el proposito de generar electricidad, se obtienen salmueras y gases de desecho. La descarga de acido sulfhidrico a la atmosfera implica problemas de contaminacion, por esta razon se han desarrollado procesos para la oxidacion de este gas aguas abajo de la turbina generadora, ya sea en la corriente de gases que se separan en la condensacion del vapor o en el condensado producido. El Instituto de Investigaciones Electricas (IIE) ha colaborado con la CFE en la evaluacion del impacto ambiental de este gas y en el desarrollo de sus procesos de abatimiento.

Evaluation of a process for the removal of gases contained in geothermal steam through condensation and re-evaporation; Evaluacion de un proceso de remocion de gases contenidos en el vapor geotermico, por medio de la condensacion y de revaporacion

Energy Technology Data Exchange (ETDEWEB)

Angulo C, Raul; Lam Rea, Luis; Garmino, Hector; Jimenez, Humberto [Instituto de Investigaciones Electricas, Cuernavaca (Mexico)

1985-12-31

The Cerro Prieto I Geothermal Field, developed and operated by the Comision Federal de Electricidad (CFE), has currently an installed electric power generation capacity of 180 MW and is at a very advanced stage in the development of Cerro Prieto II and III, which will allow to raise the generation capacity to 620 MW. During the exploitation of a geothermal field, in producing steam with the purpose of generating electricity, brines and waste gases are obtained. The hydrogen sulfide exhaust to the environment implies pollution problems, for this reason processes have been developed for the oxidation of these gases downstream the turbogenerator either in the flow of separated gases in the steam condensation or in the condensate produced. The Instituto de Investigaciones Electricas (IIE) has collaborated with CFE in the evaluation of the environmental impact of this gas and in the development of the processes for its abatement. [Espanol] El campo geotermico de Cerro Prieto I, desarrollado y operado por la Comision Federal de Electricidad (CFE), actualmente tiene una capacidad instalada de generacion de energia electrica de 180 MW, y se encuentra en etapa muy avanzada, el desarrollo de Cerro Prieto II y III, lo que permitira incrementar la capacidad de generacion a 620 MW. Durante la explotacion de un campo geotermico, al producir vapor con el proposito de generar electricidad, se obtienen salmueras y gases de desecho. La descarga de acido sulfhidrico a la atmosfera implica problemas de contaminacion, por esta razon se han desarrollado procesos para la oxidacion de este gas aguas abajo de la turbina generadora, ya sea en la corriente de gases que se separan en la condensacion del vapor o en el condensado producido. El Instituto de Investigaciones Electricas (IIE) ha colaborado con la CFE en la evaluacion del impacto ambiental de este gas y en el desarrollo de sus procesos de abatimiento.

Evolution of the Cerro Prieto geothermal system as interpreted from vitrinite reflectance under isothermal conditions

Energy Technology Data Exchange (ETDEWEB)

Barker, C.E. (US Geological Survey, Denver, CO); Pawlewicz, M.J.; Bostick, N.H.; Elders, W.A.

1981-01-01

Temperature estimates from reflectance data in the Cerro Prieto system correlate with modern temperature logs and temperature estimates from fluid inclusion and oxygen isotope geothermometry indicating that the temperature in the central portion of the Cerro Prieto System is now at its historical maximum. Isoreflectance lines formed by contouring vitrinite reflectance data for a given isothermal surface define an imaginary surface that indicates an apparent duration of heating in the system. The 250/sup 0/C isothermal surface has a complex dome-like form suggesting a localized heat source that has caused shallow heating in the central portion of this system. Isoreflectance lines relative to this 250/sup 0/C isothermal surface define a zone of low reflectance roughly corresponding to the crest of the isothermal surface. Comparison of these two surfaces suggest that the shallow heating in the central portion of Cerro Prieto is young relative to the heating (to 250/sup 0/C) on the system margins. Laboratory and theoretical models of hydrothermal convection cells suggest that the form of the observed 250/sup 0/C isothermal surface and the reflectance surface derived relative to it results from the convective rise of thermal fluids under the influence of a regional hydrodynamic gradient that induces a shift of the hydrothermal heating effects to the southwest.

Two-phase characteristics of the feeding fluid of Cerro Prieto IV wells (Mexico) obtained by gas equilibrium; Caracteristicas bifasicas del fluido de alimentacion de pozos de Cerro Prieto IV (Mexico), obtenidas por equilibrio gaseoso

Energy Technology Data Exchange (ETDEWEB)

Barragan-Reyes, Rosa Maria; Arellano-Gomez, Victor Manuel; Portugal-Marin, Enrique [Instituto de Investigaciones Electricas (Mexico); De Leon-Vivar, Jesus [Comision Federal de Electricidad, Residencia General de Cerro Prieto, B.C (Mexico)

2008-10-15

The gas composition of fluids produced by CP IV geothermal wells from the Cerro Prieto field was studied in order to identify different types of fluids entering the wells by estimating their temperature and excess steam. A method based on the Fischer Tropsch reaction and H2S equilibrium with pyrite-pyrrhotite as mineral buffer (FTHSH3) was used. The results for the reservoir natural state indicated the presence of fluids with heterogeneous reservoir temperature (between 275 and 310 degrees Celsius) and excess steam values, which were found from negative (boiled liquid that has lost steam when flowing to the well) to one (steam phase with zero liquid saturation). The study for individual wells in which boiling processes were identified, showed that through time, the feeding fluids consist of a two-phase mixture with different liquid/steam proportions. Also, the results suggested that a steam phase could occur at CP IV which is added to the feeding fluid, depending on the operation conditions of the wells. The origin of this steam could be the boiling of the deeper liquid due to a pressure drop. [Spanish] Se estudio la composicion gaseosa de los fluidos producidos por pozos geotermicos del sector CP IV del campo de Cerro Prieto para tratar de distinguir aportes de fluidos diferentes mediante la estimacion de su temperatura de yacimiento y del exceso de vapor. Se utilizo un metodo de equilibrio gaseoso basado en la reaccion de Fischer Tropsch y el equilibrio combinado pirita-pirrotita (FT-HSH3). Los resultados obtenidos indican que en el estado inicial del yacimiento existen fluidos que muestran heterogeneidad en los valores de temperatura de yacimiento (entre 275 y 310 grados Celsius), asi como en el exceso de vapor con valores desde negativos (liquido que despues de ebullir ha perdido vapor en su trayecto hacia el pozo) hasta uno (vapor con cero saturacion de liquido). El estudio individual de los pozos con fenomenos de ebullicion muestra que a traves del tiempo

Reservoir Simulation on the Cerro Prieto Geothermal Field: A Continuing Study

Energy Technology Data Exchange (ETDEWEB)

Castaneda, M.; Marquez, R.; Arellano, V.; Esquer, C.A.

1983-12-15

The Cerro Prieto geothermal field is a liquid-dominated geothermal reservoir of complex geological and hydrological structure. It is located at the southern end of the Salton-Mexicali trough which includes other geothermal anomalies as Heber and East Mesa. Although in 1973, the initial power plant installed capacity was 75 MW of electrical power, this amount increased to 180 MW in 1981 as field development continued. It is expected to have a generating capacity of 620 MW by the end of 1985, when two new plants will be completely in operation. Questions about field deliverability, reservoir life and ultimate recovery related to planned installations are being presently asked. Numerical modeling studies can give very valuable answers to these questions, even at the early stages in the development of a field. An effort to simulate the Cerro Prieto geothermal reservoir has been undergoing for almost two years. A joint project among Comision Federal de Electricidad (CFE), Instituto de Investigaciones Electricas (IIE) and Intercomp of Houstin, Texas, was created to perform reservoir engineering and simulation studies on this field. The final project objective is tosimulate the behavior of the old field region when production from additional wells located in the undeveloped field zones will be used for feeding the new power plants.

Progress on the biphase turbine at Cerro Prieto

Energy Technology Data Exchange (ETDEWEB)

Cerini, D.; Hays, L.; Studhalter, W. [Douglas Energy Company, Placentia, CA (United States)

1997-12-31

The status of a Biphase turbine power plant being installed at the Cerro Prieto geothermal field is presented. The major modules for the power plant are completed except for a back pressure steam turbine. The power plant will be started in April 1997 with the Biphase turbine alone followed by the addition of the steam turbine module two months later. The current power plant performance level is 2780 kWe due to a decline in the well. An increase in power output to 4060 kWe by adding the flow from another well is planned. The addition of five Biphase power plants with a total power output of 21.2 megawatts is described.

Subsurface imaging in a sector of Cerro Prieto transform fault near to pull-apart basin, Mexicali Valley, Baja California, Mexico, based on crooked lines 2D seismic reflection.

Science.gov (United States)

Mares-Agüero, M. A.; González-Escobar, M.; Arregui, S.

2016-12-01

In the transition zone between San Andres continental transformation system and the coupled transform faults system and rifting of Gulf of California is located the Cerro Prieto pull-apart basin delimitated by Imperial fault (northeast) and Cerro Prieto fault (CPF) (southwest), this last, is the limit west of Cerro Prieto geothermic field (CPGF). Crooked lines 2D seismic reflection, covering a portion near the intersection of CPF and CPGF are processed and interpreted. The seismic data were obtained in the early 80's by Petróleos Mexicanos (PEMEX). By decades, technical and investigation works in Cerro Prieto geothermic field and its vicinity had mapped faults at several depths but do not stablish a clear limit where this faults and CPF interact due the complex hydrothermal effects imaging the subsurface. The profiles showing the presence of a zone of uplift effect due to CPF. Considering the proximity of the profiles to CPF, it is surprising almost total absence of faults. A strong reflector around 2 km of depth, it is present in all profiles. This seismic reflector is considered a layer of shale, result of the correlation with a well located in the same region.

Land subsidence in the Cerro Prieto Geothermal Field, 1 Baja California, Mexico, from 1994 to 2005. An integrated analysis of DInSAR, levelingand geological data.

Energy Technology Data Exchange (ETDEWEB)

Sarychikhina, O; Glowacka, E; Mellors, R; Vidal, F S

2011-03-03

Cerro Prieto is the oldest and largest Mexican geothermal field in operation and has been producing electricity since 1973. The large amount of geothermal fluids extracted to supply steam to the power plants has resulted in considerable deformation in and around the field. The deformation includes land subsidence and related ground fissuring and faulting. These phenomena have produced severe damages to infrastructure such as roads, irrigation canals and other facilities. In this paper, the technique of Differential Synthetic Aperture Radar Interferometry (DInSAR) is applied using C-band ENVISAR ASAR data acquired between 2003 and 2006 to determine the extent and amount of land subsidence in the Mexicali Valley near Cerro Prieto Geothermal Field. The DInSAR results were compared with published data from precise leveling surveys (1994- 1997 and 1997-2006) and detailed geological information in order to improve the understanding of temporal and spatial distributions of anthropogenic subsidence in the Mexicali Valley. The leveling and DInSAR data were modeled to characterize the observed deformation in terms of fluid extraction. The results confirm that the tectonic faults control the spatial extent of the observed subsidence. These faults likely act as groundwater flow barriers for aquifers and reservoirs. The shape of the subsiding area coincides with the Cerro Prieto pull-apart basin. In addition, the spatial pattern of the subsidence as well as changes in rate are highly correlated with the development of the Cerro Prieto Geothermal Field.

Evaluation of geologic characteristics at Cerro Prieto

Energy Technology Data Exchange (ETDEWEB)

Howard, J.H.; Halfman, S.E.; Vonder Haar, S.P.

1981-01-01

Computerized well-log analysis of Cerro Prieto has led to the identification of a relatively large and irregular low-density volume extending from near the surface in the vicinity of Laguna Volcano to greater depths toward the northeast. This low-density volume is located about a plane of symmetry of a self-potential anomaly and a group of northeast trending active faults. The presence of a volume of relatively high-density rock has been recognized at shallow depths in the initially developed part of the resource. It is believed to be due to minerals deposited by cooled, rising geothermal brine. Storativity calculated from well logs at the south end of the western part of the field shows acceptable comparison with storativity calculated from well tests. The amount of fluid produced from the field during the period 1973-1977 is greater than the amount in situ calculated from the completed interval thicknesses. Because this part of the field is still producing today, fluid must be recharging this part of the field.

Groundwater Chemistry and Overpressure Evidences in Cerro Prieto Geothermal Field

Directory of Open Access Journals (Sweden)

Ivan Morales-Arredondo

2017-01-01

Full Text Available In order to understand the geological and hydrogeological processes influencing the hydrogeochemical behavior of the Cerro Prieto Geothermal Field (CP aquifer, Mexico, a characterization of the water samples collected from geothermal wells was carried out. Different hydrochemical diagrams were used to evaluate brine evolution of the aquifer. To determine pressure conditions at depth, a calculation was performed using hydrostatic and lithostatic properties from CP, considering geological characteristics of the study area, and theoretical information about some basin environments. Groundwater shows hydrogeochemical and geological evidences of the diagenetic evolution that indicate overpressure conditions. Some physical, chemical, textural, and mineralogical properties reported in the lithological column from CP are explained understanding the evolutionary process of the sedimentary material that composes the aquifer.

Determination of heat losses in the Cerro Prieto, Baja California, geothermal field steam transportation network based on the thermal insulation condition of the steam pipelines; Determinacion de perdidas de calor en la red de transporte de vapor del campo geotermico de Cerro Prieto, Baja California, con base en el estado fisico del aislamiento termico de vaporductos

Energy Technology Data Exchange (ETDEWEB)

Ovando Castelar, Rosember; Garcia Gutierrez, Alfonso; Martinez Estrella, Juan Ignacio [Instituto de Investigaciones Electricas, Cuernavaca, Morelos (Mexico)]. E-mail: rovando@iie.org.mx; Canchola Felix, Ismael; Jacobo Galvan, Paul; Miranda Herrera, Carlos; Mora Perez, Othon [Comision Federal de Electricidad, Gerencia de Proyectos Geotermoelectricos, Residencia General de Cerro Prieto, Mexicali, B.C. (Mexico)

2011-07-15

In Cerro Prieto Geothermal Field (CPGF), the steam from producing wells is transported to power plants through a large and complex system of pipes thermally insulated with a 2 inches thick mineral wool or a fiber glass layer and an external aluminum or iron cover. The insulation material has been exposed to weather conditions during the field operation and has suffered density and thickness changes. In some cases the insulation has been lost completely, increasing heat transfer from the pipes to the environment. This paper analyzes the impact of the conditions of thermal insulation on heat losses in the CPGF steam-pipeline network. The heat losses are calculated by applying an iterative method to determine the surface temperature based on a heat balance calculated from the three basic mechanisms of heat transfer: conduction, convection, and radiation. Finally, using length and diameter data corresponding to the condition of the thermal insulation of each pipeline-and field operation data, the overall heat losses are quantified for steam lines throughout the pipeline network in the field. The results allow us to evaluate the magnitude of the heat losses in comparison with the overall energy losses occurring during steam transport from wells to the power plants. [Spanish] En el Campo Geotermico de Cerro Prieto (CGCP), BC, el transporte de vapor desde los pozos hasta las plantas generadoras de electricidad se lleva a cabo mediante un extenso y complejo sistema de tuberias que tipicamente se encuentran aisladas termicamente con una capa de 2 pulgadas de material aislante a base de lana mineral o fibra de vidrio, y una proteccion mecanica de aluminio o hierro galvanizado. Debido a la exposicion a las condiciones meteorologicas a traves del tiempo de operacion del campo, el aislamiento ha experimentado cambios en su densidad y espesor y en ocasiones se ha perdido por completo, lo cual repercute en una mayor transferencia de calor de las tuberias hacia el medio ambiente

Fault Length Vs Fault Displacement Evaluation In The Case Of Cerro Prieto Pull-Apart Basin (Baja California, Mexico) Subsidence

Science.gov (United States)

Glowacka, E.; Sarychikhina, O.; Nava Pichardo, F. A.; Farfan, F.; Garcia Arthur, M. A.; Orozco, L.; Brassea, J.

2013-05-01

The Cerro Prieto pull-apart basin is located in the southern part of San Andreas Fault system, and is characterized by high seismicity, recent volcanism, tectonic deformation and hydrothermal activity (Lomnitz et al, 1970; Elders et al., 1984; Suárez-Vidal et al., 2008). Since the Cerro Prieto geothermal field production started, in 1973, significant subsidence increase was observed (Glowacka and Nava, 1996, Glowacka et al., 1999), and a relation between fluid extraction rate and subsidence rate has been suggested (op. cit.). Analysis of existing deformation data (Glowacka et al., 1999, 2005, Sarychikhina 2011) points to the fact that, although the extraction changes influence the subsidence rate, the tectonic faults control the spatial extent of the observed subsidence. Tectonic faults act as water barriers in the direction perpendicular to the fault, and/or separate regions with different compaction, and as effect the significant part of the subsidence is released as vertical displacement on the ground surface along fault rupture. These faults ruptures cause damages to roads and irrigation canals and water leakage. Since 1996, a network of geotechnical instruments has operated in the Mexicali Valley, for continuous recording of deformation phenomena. To date, the network (REDECVAM: Mexicali Valley Crustal Strain Measurement Array) includes two crackmeters and eight tiltmeters installed on, or very close to, the main faults; all instruments have sampling intervals in the 1 to 20 minutes range. Additionally, there are benchmarks for measuring vertical fault displacements for which readings are recorded every 3 months. Since the crackmeter measures vertical displacement on the fault at one place only, the question appears: can we use the crackmeter data to evaluate how long is the lenth of the fractured fault, and how quickly it grows, so we can know where we can expect fractures in the canals or roads? We used the Wells and Coppersmith (1994) relations between

Performance of casings in Cerro Prieto production wells

Energy Technology Data Exchange (ETDEWEB)

Dominguez A, B.; Vital B, F.; Bermejo M, F.; Sanchez G, G.

1981-01-01

A careful evaluation of different production casings used at Cerro Prieto from 1964 to date has shown that the following casings have yielded particularly impressive results: 7 5/8-in. diameter, J-55, 26 lb/ft; 7 5/8-in. diameter, K-55, 45.3 lb/ft; and 5-in. diameter, K-55, 23.2 lb/ft. These casings differ from others of the same diameter but lighter weight which were also used at the field. The results are favorable in spite of severe construction problems, especially the loss of circulation during cementing operations, which we encountered in some of the wells where these casings were used. The use of gravity-fed fine sand as packing material and the arrangement of the production and intermediate casings were important in avoiding damage due to tension-compression stresses and, above all, damage due to internal or external corrosion over time. This situation is clearly evidenced if we compare the damage to the above casings with that experienced by grade N-80 production casings, especially in a corrosive environment.

A preliminary interpretation of gas composition in the CP IV sector wells, Cerro Prieto geothermal field, Mexico

Energy Technology Data Exchange (ETDEWEB)

Barragan Reyes, Rosa Maria; Arellano Gomez, Victor M; Portugal Marin, Enrique [Instituto de Investigaciones Electricas, Gerencia de Geotermia, Morelos (Mexico)]. E-mail: rmb@iie.org.mx; Perez Hernandez, Alfredo; Rodriguez Rodriguez, Marco Helio; Leon Vivar, Jesus de [Comision Federal de Electricidad, Residencia General Cerro Prieto, B.C. (Mexico)

2007-07-15

-temperature fluids descending through the H fault to the reservoir was inferred, since results for the wells affected by this process (located at the center of the CP IV area) showed small or negative excess steam values and slightly lower temperatures (265-270 degrees Celsius). [Spanish] A fin de aumentar la capacidad de generacion de 620 a 720 MW, se desarrollo el sector Cerro Prieto IV (CP IV) en la porcion NE del campo geotermico de Cerro Prieto, donde se perforaron catorce pozos nuevos a partir del ano 2000. Los pozos de la zona de CP IV producen fluidos bifasicos con caracteristicas heterogeneas en cuanto a la fraccion de vapor: en la porcion central y hacia el NW los pozos producen liquido dominante mientras que hacia el E y S producen una fraccion de vapor relativamente alta. En este trabajo se estudia la composicion gaseosa de los fluidos producidos para obtener parametros del yacimiento tales como la temperatura y la fraccion de vapor e identificar diferentes aportes de fluidos a los pozos. Se utilizo un metodo basado en la reaccion de Fischer Tropsch y el equilibrio del H{sub 2}S con pirita-pirrotita como amortiguador (FT-HSH3). Los resultados para el estado inicial indican que existen fluidos con temperaturas de yacimiento entre 275 y 310 grados Celsius asi valores de exceso de vapor entre -1 y 50%. Los resultados se alinean en un patron de mezcla FT-HSH3 que sugiere que los pozos descargan una mezcla de los dos miembros finales en diferentes proporciones. Uno de ellos parece ser un liquido con una temperatura superior a los 300 grados Celsius con exceso de vapor negativo o insignificante. El otro parece ser un fluido bifasico con temperatura de unos 275 grados Celsius y un exceso de fraccion de vapor de aproximadamente 0.5. De acuerdo con datos de cada pozo y dependiendo de las condiciones de produccion de cada uno, pueden ocurrir mezclas de fluidos con diferentes proporciones de liquido y vapor en el yacimiento. Datos de 2005 de pozos perforados despues del ano 2000

Configuration of the mudstones, gray- and coffee-colored shale lithologic units, zones of silica and epidote, and their relation to the tectonics of the Cerro Prieto geothermal field

Energy Technology Data Exchange (ETDEWEB)

Cobo R, J.M.

1981-01-01

Based on well cuttings, five lithological units have been recognized within the area of what is now the Cerro Prieto geothermal field. These five units are described. Differences in origin, mineralogy, grading, color, compaction, etc., are shown.

Research on heat pumps in Mexico operating with geothermal energy and waste heat; Investigacion sobre bombas de calor en Mexico operando con energia geotermica y calor de desecho

Energy Technology Data Exchange (ETDEWEB)

Garcia-Gutierrez, A; Barragan-Reyes, R.M; Arellano-Gomez, V [Instituto de Investigaciones Electricas, Cuernavaca, Morelos (Mexico)]. E-mail: aggarcia@iie.org.mx

2008-01-15

The Instituto de Investigaciones Electricas and the Comision Federal de Electricidad have done research and development (R&D) on heat pumps (HP) in past years. Tested systems include mechanical compression, absorption and heat-transformers. The main R&D aspects on HP are briefly described, and also a more detailed description about three of the main studies is presented: (a) a mechanical compression HP of the water-water type operated with low-pressure geothermal steam at the Los Azufres; Mich., geothermal field, and designed for purification of brine; (b) an absorption HP for cooling and refrigeration operating with ammonia-water and low-enthalpy geothermal energy, which was tested in the Los Azufres and Cerro Prieto, BC, geothermal fields; and (c) a heat-transformer by absorption-Absorption Heat Pump Type II-tested to assess the performance of several ternary solutions as work fluids. Plans exist to install and test a geothermal heat pump at Cerro Prieto or Mexicali, BC. [Spanish] El Instituto de Investigaciones Electricas y la Comision Federal de Electricidad han realizado trabajo de investigacion y desarrollo (I&D) sobre bombas de calor (BC) en el pasado. Los sistemas probados incluyen compresion mecanica, absorcion y transformadores termicos. Este trabajo describe brevemente los principales aspectos de I&D sobre bombas de calor en forma general, y se da una descripcion mas detallada de tres de los principales estudios: (a) una BC por compresion mecanica tipo agua-agua disenada para purificacion de salmueras operando con vapor geotermico de baja presion en el campo geotermico de Los Azufres, Mich.; (b) una BC por absorcion para enfriamiento y refrigeracion operando con amoniaco-agua y energia geotermica de baja entalpia, la cual fue probada en los campos geotermicos de Los Azufres y Cerro Prieto, BC; y (c) un transformador termico por absorcion -llamado Bomba de Calor por Absorcion Tipo II--, el cual fue probado para evaluar el comportamiento de diversas

Production induced boiling and cold water entry in the Cerro Prieto geothermal reservoir indicated by chemical and physical measurements

Energy Technology Data Exchange (ETDEWEB)

Grant, M.A. (DSIR, Wellington, New Zealand); Truesdell, A.H.; Manon, A.

1981-01-01

Chemical and physical data suggest that the relatively shallow western part of the Cerro Prieto reservoir is bounded below by low permeability rocks, and above and at the sides by an interface with cooler water. There is no continuous permeability barrier around or immediately above the reservoir. Permeability within the reservoir is dominantly intergranular. Mixture with cooler water rather than boiling is the dominant cooling process in the natural state, and production causes displacement of hot water by cooler water, not by vapor. Local boiling occurs near most wells in response to pressure decreases, but no general vapor zone has formed.

Hydrothermal alteration of sediments associated with surface emissions from the Cerro Prieto geothermal field

Energy Technology Data Exchange (ETDEWEB)

Valette-Silver, J.N.; Esquer P., I.; Elders, W.A.; Collier, P.C.; Hoagland, J.R.

1981-01-01

A study of the mineralogical changes associated with these hydrothermal vents was initiated with the aim of developing possible exploration tools for geothermal resources. The Cerro Prieto reservoir has already been explored by extensive deep drilling so that relationships between surface manifestations and deeper hydrothermal processes could be established directly. Approximately 120 samples of surface sediments were collected both inside and outside of the vents. The mineralogy of the altered sediments studied appears to be controlled by the type of emission. A comparison between the changes in mineralogy due to low temperature hydrothermal activity in the reservoir, seen in samples from boreholes, and mineralogical changes in the surface emission samples shows similar general trends below 180 C: increase of quartz, feldspar and illite, with subsequent disappearance of kaolinite, montmorillonite, calcite and dolomite. These mineral assemblages seem to be characteristic products of the discharge from high intensity geothermal fields.

Comments on some of the drilling and completion problems in Cerro Prieto geothermal wells

Energy Technology Data Exchange (ETDEWEB)

Dominguez A, B.; Sanchez G, G.

1981-01-01

From 1960 to the present, 85 wells with a total drilling length exceeding 160,000 m have been constructed at Cerro Prieto, a modest figure compared to an oil field. This activity took place in five stages, each characterized by changes and modifications required by various drilling and well-completion problems. Initially, the technical procedures followed were similar to those used in the oil industry. However, several problems emerged as a result of the relatively high temperatures found in the geothermal reservoir. The various problems that have been encountered can be considered to be related to drilling fluids, cements and cementing operations, lithology, geothermal fluid characteristics, and casings and their accessories. As the importance of high temperatures and the characteristics of the geothermal reservoir fluids were better understood, the criteria were modified to optimize well-completion operations, and satisfactory results have been achieved to date.

Analysis of the Nuevo Leon magnetic anomaly and its possible relation to the Cerro Prieto magmatic-hydrothermal system

Energy Technology Data Exchange (ETDEWEB)

Goldstein, N.E.; Wilt, M.J.; Corrigan, D.J.

1982-10-01

The broad dipolar magnetic anomaly whose positive peak is centered near Ejido Nuevo Leon, some 5 km east of the Cerro Prieto I Power Plant, has long been suspected to have a genetic relationship to the thermal source of the Cerro Prieto geothermal system. This suspicion was reinforced after several deep geothermal wells, drilled to depths of 3 to 3.5 km over the anomaly, intersected an apparent dike-sill complex consisting mainly of diabase but with minor rhyodacite. A detailed fit of the observed magnetic field to a computer model indicates that the source may be approximated by a tabular block 4 by 6 km in area, 3.7 km in depth, 2.3 km thick, and dipping slightly to the north. Mafic dike chips from one well, NL-1, were analyzed by means of electron microprobe analyses which showed tham to contain a titanomagnetite that is paramagnetic at in-situ temperature conditions. As the dike mineralogy does not account for the magnetic anomaly, the magnetic source is believed to be a deeper, magnetite-rich assemblage of peridotite-gabbro plutons. the suite of igneous rocks was probably passively emplaced at a shallow depth in response to crustal extension and thinning brought on by strike-slip faulting. The bottom of the magnetic source body, at an estimated depth of 6 km, is presumed to be at or near that of the Curie isotherm (575/sup 0/C) for magnetite, the principal ferromagnetic mineral in peridotitic-gabbroic rocks. The geological model derived from the magnetic study is generally supported by other geophysical data. In particular, earthquake data suggest dike injection is occurring at depths of 6 to 11 km in an area beneath the magnetic source. Thus, it is possible that heat for the geothermal field is being maintained by continuing crustal extension and magmatic activity.

Research and technological development on heat pumps in Mexico operating with geothermal energy; Investigacion y desarrollo tecnologico sobre bombas de calor en Mexico operando con energia geotermica

Energy Technology Data Exchange (ETDEWEB)

Garcia Gutierrez, Alfonso; Barragan Reyes, Rosa Maria; Arellano Gomez, Victor Manuel [Instituto de Investigaciones Electricas, Cuernavaca, Morelos (Mexico)

2008-07-01

The Instituto de Investigaciones Electricas (IIE) and the Comision Federal de Electricidad (CFE) carried out in the past an extensive work of research and development (R&D) on heat pumps (HP). The systems tried on include heat pumps by mechanical compression, thermal absorption and thermal transformers. This paper briefly describes the main aspects of R&D on heat pumps and presents a more detailed description of three of the main studies: a) a Heat Pump (HP) by mechanical compression water-water type, designed for brine purification, operating with low pressure geothermal steam at the geothermal field Los Azufres, Michoacan, Mexico; b) a HP by absorption for cooling and refrigeration, operating with ammoniac/water and low enthalpy geothermal energy, which was tested in the geothermal fields of Los Azufres, Michoacan and Cerro Prieto, Baja California, and c) a thermal transformer by absorption, named Heat Pump by Absorption Type 2, which was tested to evaluate the behavior of diverse ternary solutions as working fluids. To date, there are plans to install and test a geothermal heat pump (connected to the subsoil), in Cerro Prieto, Mexicali, Baja California, Mexico. [Spanish] El Instituto de Investigaciones Electricas (IIE) y la Comision Federal de Electricidad (CFE) realizaron un trabajo extenso de investigacion y desarrollo (I&D) sobre bombas de calor (BC) en el pasado. Los sistemas que se probaron incluyen bombas de calor por compresion mecanica, absorcion y transformadores termicos. Este trabajo describe brevemente los principales aspectos de I&D sobre bombas de calor y se da una descripcion mas detallada de tres de los principales estudios: a) una Bomba de Calor (BC) por compresion mecanica tipo agua-agua, disenada para purificacion de salmueras, operando con vapor geotermico de baja presion en el campo geotermico de Los Azufres, Michoacan; b) una BC por absorcion para enfriamiento y refrigeracion, operando con amoniaco/agua y energia geotermica de baja entalpia

Soil mercury levels in the area surrounding the Cerro Prieto geothermal complex, MEXICO.

Science.gov (United States)

Pastrana-Corral, M A; Wakida, F T; García-Flores, E; Rodriguez-Mendivil, D D; Quiñonez-Plaza, A; Piñon-Colin, T D J

2016-08-01

Even though geothermal energy is a renewable energy source that is seen as cost-effective and environmentally friendly, emissions from geothermal plants can impact air, soil, and water in the vicinity of geothermal power plants. The Cerro Prieto geothermal complex is located 30 km southeast of the city of Mexicali in the Mexican state of Baja California. Its installed electricity generation capacity is 720 MW, being the largest geothermal complex in Mexico. The objective of this study was to evaluate whether the emissions generated by the geothermal complex have increased the soil mercury concentration in the surrounding areas. Fifty-four surface soil samples were collected from the perimeter up to an approximate distance of 7660 m from the complex. Additionally, four soil depth profiles were performed in the vicinity of the complex. Mercury concentration in 69 % of the samples was higher than the mercury concentration found at the baseline sites. The mercury concentration ranged from 0.01 to 0.26 mg/kg. Our results show that the activities of the geothermal complex have led to an accumulation of mercury in the soil of the surrounding area. More studies are needed to determine the risk to human health and the ecosystems in the study area.

Update of Geothermics in Mexico

Energy Technology Data Exchange (ETDEWEB)

Gutierrez Negrin, Luis C.A.; Quijano Leon, Jose Luis [Comision Federal de Electricidad, Morelia, Michoacan (Mexico)

2004-12-01

Four geothermal fields are currently operating in Mexico (Cerro Prieto, Los Azufres, Los Humeros and Las Tres Virgenes), with a total installed geothermal-electric capacity of 953 megawatts (MW). This means the country is located in third place, worldwide, just behind the USA and Philippines. Thirty-six power plants of several types (condensing, back pressure and binary cycle), between 1.5 and 110 MW, operate in the fields, fed by 197 wells with a combined production of 7,700 metric tons of steam per hour (t/h). These production wells have depths between 600 and 4,400 meters. Steam comes with 8,750 t/h of brine that is injected through 19 injection wells or treated in a solar evaporation pond of 14 km2 in Cerro Prieto. During 2003, steam produced in those fields equaled 67.5 million metric tons, and the power plants generated 6,282 gigawatt-hours (GWh), which represented 3.1% of the electric energy produced in Mexico. All the power plants and the geothermal fields are operated bye the public utility, the Comision Federal de Electricidad (Comision Federal de Electricidad (CFE)). [Spanish] Actualmente se operan en Mexico cuatro campos geotermicos (Cerro Prieto, Los Azufres, Los Humeros y Las Tres Virgenes), con una capacidad geotermoelectrica total de 953 megawatts (MW). Esto coloca al pais en el tercer lugar mundial, detras de Estados Unidos y Filipinas. En esos campos operan treinta y seis unidades de tipos diversos (a condensacion, a contrapresion y de ciclo binario), entre 1.5 y 110 MW, alimentadas por 197 pozos con una produccion combinada de 7,700 toneladas de vapor por hora (t/h). Estos pozos productores tienen profundidades entre 600 y 4,400 metros. El vapor sale acompanado por 8,750 t/h de salmuera, que se inyecta en 19 pozos inyectores o se trata en una laguna de evaporacion solar de 14 km2 en Cerro Prieto. Durante 2003 el vapor producido en los campos sumo 67.5 millones de toneladas y las unidades generaron 6,282 gigawatts-hora (GWh), lo que represento el

Application of oil-field well log interpretation techniques to the Cerro Prieto Geothermal Field

Energy Technology Data Exchange (ETDEWEB)

Ershaghi, I.; Phillips, L.B.; Dougherty, E.L.; Handy, L.L.

1979-10-01

An example is presented of the application of oil-field techniques to the Cerro Prieto Field, Mexico. The lithology in this field (sand-shale lithology) is relatively similar to oil-field systems. The study was undertaken as a part of the first series of case studies supported by the Geothermal Log Interpretation Program (GLIP) of the US Department of Energy. The suites of logs for individual wells were far from complete. This was partly because of adverse borehole conditions but mostly because of unavailability of high-temperature tools. The most complete set of logs was a combination of Dual Induction Laterolog, Compensated Formation Density Gamma Ray, Compensated Neutron Log, and Saraband. Temperature data about the wells were sketchy, and the logs had been run under pre-cooled mud condition. A system of interpretation consisting of a combination of graphic and numerical studies was used to study the logs. From graphical studies, evidence of hydrothermal alteration may be established from the trend analysis of SP (self potential) and ILD (deep induction log). Furthermore, the cross plot techniques using data from density and neutron logs may help in establishing compaction as well as rock density profile with depth. In the numerical method, R/sub wa/ values from three different resistivity logs were computed and brought into agreement. From this approach, values of formation temperature and mud filtrate resistivity effective at the time of logging were established.

Design of a seismic energy dissipator for an interruptor type 3AS2-45; Diseno de un disipador de energia sismica para un interruptor tipo 3AS2-45

Energy Technology Data Exchange (ETDEWEB)

Castro Felix, Jaime

2004-02-15

With the aid of the theory behind seismically isolated structures and the bi-linear behavior of an isolated system of Multiple Degrees of Freedom (MDOF), the information obtained on the spectral analysis is complemented with the purpose of simulating one itself for the design of a dissipator of seismic energy. The seismicity in the world is briefly explained, (in Mexico in special for the Geothermal Field of Cerro Prieto), the types of earthquakes, etc., to give way to a documentation of the state-of-the-art in advanced seismic resistant systems and to a procedure to establish the level of seismic qualification of electrical equipment from the level of seismic performance for the Mexican Republic. [Spanish] Con la ayuda de la teoria detras de estructuras aisladas sismicamente y el comportamiento bilineal de un sistema de aislamiento de Multiples Grados de Libertad (MDOF), se complementa la informacion recabada sobre el analisis espectral con el fin de simular uno propio para el diseno de un disipador de energia sismica. Se explica brevemente la sismicidad en el mundo, en Mexico, en especial el Campo Geotermico de Cerro Prieto, los tipos de sismos, etc., para dar paso a una documentacion del estado del arte en sistemas sismorresistentes avanzados y a un procedimiento para establecer el nivel de calificacion sismica de equipos electricos a partir del Nivel de desempeno sismico para la Republica Mexicana.

Origin and evolution of geothermal fluids from Las Tres Vírgenes and Cerro Prieto fields, Mexico – Co-genetic volcanic activity and paleoclimatic constraints

International Nuclear Information System (INIS)

Birkle, Peter; Marín, Enrique Portugal; Pinti, Daniele L.; Castro, M. Clara

2016-01-01

Major and trace elements, noble gases, and stable (δD, δ 18 O) and cosmogenic ( 3 H, 14 C) isotopes were measured from geothermal fluids in two adjacent geothermal areas in NW-Mexico, Las Tres Vírgenes (LTV) and Cerro Prieto (CP). The goal is to trace the origin of reservoir fluids and to place paleoclimate and structural-volcanic constraints in the region. Measured 3 He/ 4 He (R) ratios normalized to the atmospheric value (R a  = 1.386 × 10 −6 ) vary between 2.73 and 4.77 and are compatible with mixing between a mantle component varying between 42 and 77% of mantle helium and a crustal, radiogenic He component with contributions varying between 23% and 58%. Apparent U–Th/ 4 He ages for CP fluids (0.7–7 Ma) suggest the presence of a sustained 4 He flux from a granitic basement or from mixing with connate brines, deposited during the Colorado River delta formation (1.5–3 Ma). Radiogenic in situ 4 He production age modeling at LTV, combined with the presence of radiogenic carbon (1.89 ± 0.11 pmC – 35.61 ± 0.28 pmC) and the absence of tritium strongly suggest the Quaternary infiltration of meteoric water into the LTV geothermal reservoir, ranging between 4 and 31 ka BP. The present geochemical heterogeneity of LTV fluids can be reconstructed by mixing Late Pleistocene – Early Holocene meteoric water (58–75%) with a fossil seawater component (25–42%), as evidenced by Br/Cl and stable isotope trends. CP geothermal water is composed of infiltrated Colorado River water with a minor impact by halite dissolution, whereas a vapor-dominated sample is composed of Colorado River water and vapor from deeper levels. δD values for the LTV meteoric end-member, which are 20‰–44‰ depleted with respect to present-day precipitation, as well as calculated annual paleotemperatures 6.9–13.6 °C lower than present average temperatures in Baja California point to the presence of humid and cooler climatic conditions in the Baja California peninsula

Structure of the Wagner Basin in the Northern Gulf of California From Interpretation of Seismic Reflexion Data

Science.gov (United States)

Gonzalez, M.; Aguilar, C.; Martin, A.

2007-05-01

The northern Gulf of California straddles the transition in the style of deformation along the Pacific-North America plate boundary, from distributed deformation in the Upper Delfin and Wagner basins to localized dextral shear along the Cerro Prieto transform fault. Processing and interpretation of industry seismic data adquired by Petroleos Mexicanos (PEMEX) allow us to map the main fault structures and depocenters in the Wagner basin and to unravel the way strain is transferred northward into the Cerro Prieto fault system. Seismic data records from 0.5 to 5 TWTT. Data stacking and time-migration were performed using semblance coefficient method. Subsidence in the Wagner basin is controlled by two large N-S trending sub-parallel faults that intersect the NNW-trending Cerro Prieto transform fault. The Wagner fault bounds the eastern margin of the basin for more than 75 km. This fault dips ~50° to the west (up to 2 seconds) with distinctive reflectors displaced more than 1 km across the fault zone. The strata define a fanning pattern towards the Wagner fault. Northward the Wagner fault intersects the Cerro Prieto fault at 130° on map view and one depocenter of the Wagner basin bends to the NW adjacent to the Cerro Prieto fault zone. The eastern boundary of the modern depocenter is the Consag fault, which extends over 100 km in a N-S direction with an average dip of ~50° (up to 2s) to the east. The northern segment of the Consag fault bends 25° and intersects the Cerro Prieto fault zone at an angle of 110° on map view. The acoustic basement was not imaged in the northwest, but the stratigraphic succession increases its thickness towards the depocenter of the Wagner basin. Another important structure is El Chinero fault, which runs parallel to the Consag fault along 60 km and possibly intersects the Cerro Prieto fault to the north beneath the delta of the Colorado River. El Chinero fault dips at low-angle (~30°) to the east and has a vertical offset of about 0

Calc-silicate mineralization in active geothermal systems

Energy Technology Data Exchange (ETDEWEB)

Bird, D.K.; Schiffman, P.; Elders, W.A.; Williams, A.E.; McDowell, S.D.

1983-01-01

The detailed study of calc-silicate mineral zones and coexisting phase relations in the Cerro Prieto geothermal system were used as examples for thermodynamic evaluation of phase relations among minerals of variable composition and to calculate the chemical characteristics of hydrothermal solutions compatible with the observed calc-silicate assemblages. In general there is a close correlation between calculated and observed fluid compositions. Calculated fugacities of O{sub 2} at about 320{degrees}C in the Cerro Prieto geothermal system are about five orders of magnitude less than that at the nearby Salton Sea geothermal system. This observation is consistent with the occurrence of Fe{sup 3+} rich epidotes in the latter system and the presence of prehnite at Cerro Prieto.

Operation and Performance of a Biphase Turbine Power Plant at the Cerro Prieto Geothermal Field (Final Report)

Energy Technology Data Exchange (ETDEWEB)

Hays, Lance G. [Douglas Energy Company, Placentia, CA (United States)

2000-09-01

A full scale, wellhead Biphase turbine was manufactured and installed with the balance of plant at Well 103 of the Cerro Prieto geothermal resource in Baja, California. The Biphase turbine was first synchronized with the electrical grid of Comision Federal de Electricidad on August 20, 1997. The Biphase power plant was operated from that time until May 23, 2000, a period of 2 years and 9 months. A total of 77,549 kWh were delivered to the grid. The power plant was subsequently placed in a standby condition pending replacement of the rotor with a newly designed, higher power rotor and replacement of the bearings and seals. The maximum measured power output of the Biphase turbine, 808 kWe at 640 psig wellhead pressure, agreed closely with the predicted output, 840 kWe. When combined with the backpressure steam turbine the total output power from that flow would be increased by 40% above the power derived only from the flow by the present flash steam plant. The design relations used to predict performance and design the turbine were verified by these tests. The performance and durability of the Biphase turbine support the conclusion of the Economics and Application Report previously published, (Appendix A). The newly designed rotor (the Dual Pressure Rotor) was analyzed for the above power condition. The Dual Pressure Rotor would increase the power output to 2064 kWe by incorporating two pressure letdown stages in the Biphase rotor, eliminating the requirement for a backpressure steam turbine. The power plant availability was low due to deposition of solids from the well on the Biphase rotor and balance of plant problems. A great deal of plant down time resulted from the requirement to develop methods to handle the solids and from testing the apparatus in the Biphase turbine. Finally an online, washing method using the high pressure two-phase flow was developed which completely eliminated the solids problem. The availability of the Biphase turbine itself was 100

Geothermal potential in Mexico; Potencial geotermico de la republica mexicana

Energy Technology Data Exchange (ETDEWEB)

Ordaz Mendez, Christian Arturo; Flores Armenta, Magaly; Ramirez Silva, German [Comision Federal de Electricidad, Gerencia de Proyectos Geotermoelectricos, Morelia, Michoacan (Mexico)]. E-mail: christian.ordaz@cfe.gob.mx

2011-01-15

parte de la estrategia de la CFE para incrementar la generacion de energia electrica mediante fuentes no convencionales llevo a cabo un calculo del potencial geotermico del pais. Este calculo se efectuo a traves del inventario nacional de manifestaciones termales con que cuenta la GPG, el cual ha permitido identificar 1380 manifestaciones termales distribuidas en todo el pais, con informacion de las temperaturas tomadas superficialmente y las temperaturas obtenidas por medio de geotermometros. El calculo del potencial geotermico se hizo con base en la clasificacion de estas manifestaciones por rangos de temperatura geotermometrica, obteniendose asi recursos de alta, media y baja entalpia. Posteriormente se utilizo el metodo volumetrico para obtener el potencial geotermico nacional. Los resultados indican que para las Reservas Posibles los recursos de alta entalpia ascienden a 5691 MWe, para los de moderada entalpia son de 881 MWe y los de baja entalpia de 849 MWe dando un total de 7422 MWe. Por otra parte, las Reservas Probables para el recurso de alta entalpia son de 1643 MWe, para los de moderada entalpia de 220 MWe y para los de baja entalpia de 212 MWe dando un total de 2077 MWe. Por ultimo las Reservas Probadas se tomaron como la capacidad adicional que puede instalarse en cada uno de los campos geotermicos conocidos, dando un total de 186 MWe. La informacion se proceso y se integro por medio del Sistema de Informacion Geografica (SIG) ArcGis 9.2 (c), dando como resultado la publicacion via Intranet del Mapa del Potencial Geotermico de la Republica Mexicana.

Cerro Largo South orientation

International Nuclear Information System (INIS)

Pradier, B.

1982-01-01

This work is about Cerro Largo South orientation. The site is located in the northeast of Uruguay in the south of Melo city, Department of Cerro Largo. The study was carried out in the young edge socket in the East side of a small valley. This metamorphic socket constituted by gneisses and crystalline limestone are in contact with upper carboniferous formations and basal deposits composed by sandstones and conglomerates

Imperial County geothermal development annual meeting: summary

Energy Technology Data Exchange (ETDEWEB)

1983-01-01

All phases of current geothermal development in Imperial County are discussed and future plans for development are reviewed. Topics covered include: Heber status update, Heber binary project, direct geothermal use for high-fructose corn sweetener production, update on county planning activities, Brawley and Salton Sea facility status, status of Imperial County projects, status of South Brawley Prospect 1983, Niland geothermal energy program, recent and pending changes in federal procedures/organizations, plant indicators of geothermal fluid on East Mesa, state lands activities in Imperial County, environmental interests in Imperial County, offshore exploration, strategic metals in geothermal fluids rebuilding of East Mesa Power Plant, direct use geothermal potential for Calipatria industrial Park, the Audubon Society case, status report of the Cerro Prieto geothermal field, East Brawley Prospect, and precision gravity survey at Heber and Cerro Prieto geothermal fields. (MHR)

Geophysical Investigations of Magma Plumbing Systems at Cerro Negro Volcano, Nicaragua

Science.gov (United States)

MacQueen, Patricia Grace

Cerro Negro near Leon, Nicaragua is a very young (163 years), relatively small basaltic cinder cone volcano that has been unusually active during its short lifespan (recurrence interval 6--7 years), presenting a significant hazard to nearby communities. Previous studies have raised several questions as to the proper classification of Cerro Negro and its relation to neighboring Las Pilas-El Hoyo volcano. Analysis of Bouguer gravity data collected at Cerro Negro has revealed connected positive density anomalies beneath Cerro Negro and Las Pilas-El Hoyo. These findings suggest that eruptions at Cerro Negro may be tapping a large magma reservoir beneath Las Pilas-El Hoyo, implying that Cerro Negro should be considered the newest vent on the Las Pilas-El Hoyo volcanic complex. As such, it is possible that the intensity of volcanic hazards at Cerro Negro may eventually increase in the future to resemble those pertaining to a stratovolcano. Keywords: Cerro Negro; Las Pilas-El Hoyo; Bouguer gravity; magmatic plumbing systems; potential fields; volcano.

Geochemical model of a geothermal system: an approach on the analytical uncertainty; Modelo geoquimico de sistema geotermico: un enfoque sobre la incertidumbre analitica

Energy Technology Data Exchange (ETDEWEB)

Pal Verma, Mahendra [Instituto de Investigaciones Electricas, Cuernavaca, Morelos (Mexico)

2008-07-01

A procedure was developed to consider the analytical uncertainty in each parameter of geochemical analysis of geothermal fluid. The estimation of the uncertainty is based on the results of the geochemical analyses of geothermal fluids (numbered from the 0 to the 14), obtained within the framework of the comparisons program among the geochemical laboratories in the last 30 years. Also the propagation of the analytical uncertainty was realized in the calculation of the parameters of the geothermal fluid in the reservoir, through the methods of interval of uncertainty and GUM (Guide to the expression of Uncertainty of Measurement). The application of the methods is illustrated in the pH calculation of the geothermal fluid in the reservoir, considering samples 10 and 11 as separated waters at atmospheric conditions. [Spanish] Se desarrollo un procedimiento para estimar la incertidumbre analitica en cada parametro de analisis geoquimico de fluido geotermico. La estimacion de la incertidumbre esta basada en los resultados de los analisis geoquimicos de fluidos geotermicos (numerados del 0 al 14), obtenidos en el marco del programa de comparaciones entre los laboratorios geoquimicos en los ultimos 30 anos. Tambien se realizo la propagacion de la incertidumbre analitica en el calculo de los parametros del fluido geotermico en el yacimiento, a traves de los metodos de intervalo de incertidumbre y GUM (Guide to the expression of Uncertainty of Measurement). La aplicacion de los metodos se ilustra en el calculo de pH del fluido geotermico en el yacimiento, considerando las muestras 10 y 11 como aguas separadas a las condiciones atmosfericas.

First evidence of lamprophyric magmatism within the Subbetic Zone (Southern Spain)

NARCIS (Netherlands)

Puga, E.; Beccaluva, L.; Bianchini, G.; De Federico, A.D.; Puga, M.A.D.; Alvarez-Valero, A.M.; Galindo-Zaldivar, J.; Wijbrans, J.R.

2010-01-01

Two drillings carried out at Cerro Prieto (Province of Málaga), together with additional geophysical data, revealed the existence of an igneous body formed of rock-types previously unknown in the Subbetic zone. The recovered rocks, emplaced under hypoabyssal conditions, are predominantly porphyric,

Simulator of a geotermoelectric unit for the training of operators; Simulador de una unidad geotermoelectrica para entrenamiento de operadores

Energy Technology Data Exchange (ETDEWEB)

Tavira Mondragon, Jose Antonio; Lopez Aguilera, Diana Monica; Roldan Villasana, Edgardo Javier; Rodriguez Lozano, Saul [Instituto de Investigaciones Electricas, Temixco, Morelos (Mexico)

1999-07-01

The use of simulators replica in real time for operators training has demonstrated to be one of the best forms to enable the personnel of the Comision Federal de Electricidad (CFE). This article shows the basic characteristics of a simulator replica of the Cerro Prieto geotermoelectric power station of Baja California. It is expected that with this simulator 400 people between operators, shift superintendents and operation and maintenance auxiliary personnel become qualified. [Spanish] El uso de simuladores replica en tiempo real para entrenamiento de operadores de centrales generadoras ha demostrado ser una de las mejores formas de capacitar al personal de la Comision Federal de Electricidad (CFE). Este articulo muestra las caracteristicas principales de un simulador replica de la central geotermoelectrica de Cerro Prieto Baja California. Se espera que con este simulador se capaciten 400 personas entre operadores, superintendentes de turno y auxiliares de operacion y mantenimiento.

Seismicity and arrival-time residuals from the Victoria Earthquake of June 9, 1980

Energy Technology Data Exchange (ETDEWEB)

Wong, V.; Frez, J.

1981-01-01

Hypocenter distribution in space and time of the aftershock activity from the Victoria Earthquake of June 9, 1980 was studied. It was concluded that the main event excited aftershocks in several pre-existing nests at the northwest end of the Cerro Prieto Fault, but no significant activity occurred at the immediate neighborhood of the main event. The depth of the aftershocks increases with the distance from the northwest end of the fault and this feature might be related with the higher temperatures and the spreading center located between the ends of the Imperial and Cerro Prieto Faults. The significance of the arrival-times residuals for local and regional stations is discussed both for P and S-waves and the importance of obtaining station corrections is emphasized. The non-uniqueness in determining a structure which minimizes the residuals is illustrated. Two different structures which satisfy the local data are presented.

Cerro Prieto geothermal field: exploration during exploitation

Energy Technology Data Exchange (ETDEWEB)

1982-07-01

Geological investigations at Momotombo included photogeology, field mapping, binocular microscope examination of cuttings, and drillhole correlations. Among the geophysical techniques used to investigate the field sub-structure were: Schlumberger and electromagnetic soundings, dipole mapping and audio-magnetotelluric surveys, gravity and magnetic measurements, frequency domain soundings, self-potential surveys, and subsurface temperature determinations. The geochemical program analyzed the thermal fluids of the surface and in the wells. The description and results of exploration methods used during the investigative stages of the Momotombo Geothermal Field are presented. A conceptual model of the geothermal field was drawn from the information available at each exploration phase. The exploration methods have been evaluated with respect to their contributions to the understanding of the field and their utilization in planning further development.

Summary of the 2010 assessment on medium- to low-temperature geothermal resources in Mexico; Resumen de la evaluacion 2010 de los recursos geotermicos mexicanos de temperatura intermedia a baja

Energy Technology Data Exchange (ETDEWEB)

Iglesias, Eduardo R.; Torres, Rodolfo J.; Martinez Estrella, J. Ignacio; Reyes Picasso, Neftali [Instituto de Investigaciones Electricas, Cuernavaca, Morelos (Mexico)]. E-mail: iglesias@iie.org.mx

2011-07-15

geothermal systems lies between 1,168 EJ and 1,274 EJ, with 90% confidence. The statistical distribution of the (conservatively) inferred reservoir temperatures indicates that 5% of these systems have temperatures between 151 and 208 degrees Celsius, 40% of these systems have temperatures between 102 and 151 degrees Celsius, 50% of these systems have temperatures between 60 and 102 degrees Celsius, and 5% of these systems have temperatures between 36 and 60 degrees Celsius. These resources contain massive amounts of thermal energy that could be used in a wide variety of direct applications and power generation projects. Potentially they are important for the economy of 26 of the 32 Mexican States. This work does not include any attempt to estimate the recuperation factor of the estimated resources. [Spanish] En 2003 publicamos nuestra primera estimacion de los recursos geotermicos mexicanos de temperatura intermedia a baja (T {<=} 200 grados centigrados) con base en datos de 1358 manifestaciones superficiales identificadas en ese momento. Debido a falta de informacion en uno o mas parametros relevantes, como coordenadas geograficas, temperatura de muestra o del yacimiento, etc., dicha evaluacion incluyo aproximadamente 30% de las manifestaciones identificadas. Desde entonces nuestro grupo incremento significativamente la cantidad de la informacion en la base de datos, mediante compilacion de datos de diferentes fuentes y trabajo de campo. Posteriormente desarrollamos una base de datos relacional y la implementamos en un Sistema de Informacion Geografica (SIG). En este trabajo presentamos un resumen de nuestra evaluacion 2010 de los recursos geotermicos mexicanos de temperatura intermedia a baja resultante de nuestra base de datos actualizada, que incluye 2361 manifestaciones geotermicas. Como en la version precedente, utilizamos el metodo volumetrico y simulaciones Montecarlo para estimar los recursos geotermicos y sus correspondientes incertidumbres para cada sistema

Geophysical investigations of magma plumbing systems at Cerro Negro volcano, Nicaragua

OpenAIRE

MacQueen, Patricia Grace

2013-01-01

Cerro Negro near Léon, Nicaragua is a very young (163 years), relatively small basaltic cinder cone volcano that has been unusually active during its short lifespan (recurrence interval 6-7 years), presenting a significant hazard to nearby communities. Previous studies have raised several questions as to the proper classification of Cerro Negro and its relation to neighboring Las Pilas-El Hoyo volcano. Analysis of Bouguer gravity data collected at Cerro Negro has revealed connected positive d...

Magnetotelluric studies at the Cerro Prieto geothermal field

Energy Technology Data Exchange (ETDEWEB)

Goubau, W.M. (Lawrence Berkeley Lab., CA); Goldstein, N.E.; Clarke, J.

1981-01-01

During three years of magnetotelluric surveying, data were acquired at 26 sites distributed over 190 km/sup 2/ around the production area. A relatively well-defined strike of N27W +- 1.5/sup 0/ (magnetic) was established. The simple model shown suggests a lateral discontinuity in the vicinity of Nueva Leon.

Drilling rate for the Cerro Prieto stratigraphic sequence

Energy Technology Data Exchange (ETDEWEB)

Prian C, R.

1981-01-01

Drilling practice at the field has been modified in several ways as better information is being obtained. The stratigraphic sequence of the area is made up of three sedimentary rock units of deltaic origin having different densities. These units have been named non-consolidated, semi-consolidated, and consolidated rocks; the thermal reservoirs are located in the latter. To investigate how the drilling rates are affected by the three rock units, plots of drilling advance versus time were made for a large number of wells. A typical plot is shown and drilling rates are practically constant in three different zones; that is, the drilling rate has only two breaks or changes in slope.

Uruguay mining Inventory: geochemical prospecting results of Cerro de las Cuentas mapping

International Nuclear Information System (INIS)

Spangenberg, J.; Filippini, J.

1986-01-01

This work is about the geochemical prospecting carried out into the Uruguay mining inventory framework. In this case the survey was in Cerro de las Cuentas mapping. Cerro Largo department. Scale 1 / 50000.

Cerro Baúl: un enclave wari en interacción con Tiwanaku

OpenAIRE

Williams, Patrick Ryan; Isla, Johny A.; Nash, Donna J.

2012-01-01

Cerro Baul: A Wari Enclave Interacting with TiwanakuWari expansion to the extreme south of Peru is a phenomenon whose study began 20 years ago, with the discovery of a great arquitectonic complex at Cerro Baul. The excavations undertaken in the last 3 years have revealed that Cerro Baul was more than a military fortress; it was the most important political and religious center that Wari established in the only region where there is direct evidence of interaction with Tiwanaku, the altiplano s...

Refined localization of the Prieto-syndrome locus

Energy Technology Data Exchange (ETDEWEB)

Martinez, F.; Prieto, F. [Unidad de Genetica, Valencia (Spain); Gal, A. [Universitaets-Krankenhaus Eppendorf, Hamburg (Germany)

1996-07-12

PRS designates the locus for a syndromal form of X-linked mental retardation (Prieto syndrome) characterized by minor facial anomalies, ear malformation, abnormal growth of teeth, clinodactyly, sacral dimple, patellar luxation, malformation of lower limbs, abnormalities of the fundus of the eye, and subcortical cerebral atrophy. Linkage analysis localized the disease locus between DXS84 (Xp21.1) and DXS255. Here we present additional linkage data that provide further support and refinement of this localization. Individual III-18 gave birth to a male, currently aged 2 7/12 years, who clearly shows delayed psychomotor development. He began to walk at 23 months and his speech is delayed. In addition, he shows the characteristic facial anomalies, {open_quotes}dysplastic{close_quotes} ears, sacral dimple, and clinodactyly, as do all other affected males in this family. 7 refs., 1 tab.

Connected magma plumbing system between Cerro Negro and El Hoyo Complex, Nicaragua revealed by gravity survey

Science.gov (United States)

MacQueen, Patricia; Zurek, Jeffrey; Williams-Jones, Glyn

2016-11-01

Cerro Negro, near León, Nicaragua is a young, relatively small basaltic cinder cone volcano that has been unusually active during its short lifespan. Multiple explosive eruptions have deposited significant amounts of ash on León and the surrounding rural communities. While a number of studies investigate the geochemistry and stress regime of the volcano, subsurface structures have only been studied by diffuse soil gas surveys. These studies have raised several questions as to the proper classification of Cerro Negro and its relation to neighboring volcanic features. To address these questions, we collected 119 gravity measurements around Cerro Negro volcano in an attempt to delineate deep structures at the volcano. The resulting complete Bouguer anomaly map revealed local positive gravity anomalies (wavelength 0.5 to 2 km, magnitude +4 mGal) and regional positive (10 km wavelength, magnitudes +10 and +8 mGal) and negative (12 and 6 km wavelength, magnitudes -18 and -13 mGal) Bouguer anomalies. Further analysis of these gravity data through inversion has revealed both local and regional density anomalies that we interpret as intrusive complexes at Cerro Negro and in the Nicaraguan Volcanic Arc. The local density anomalies at Cerro Negro have a density of 2700 kg m-3 (basalt) and are located between -250 and -2000 m above sea level. The distribution of recovered density anomalies suggests that eruptions at Cerro Negro may be tapping an interconnected magma plumbing system beneath El Hoyo, Cerro La Mula, and Cerro Negro, and more than seven other proximal volcanic features, implying that Cerro Negro should be considered the newest cone of a Cerro Negro-El Hoyo volcanic complex.

Simulation of the flow phenomena in geothermal wells: developments and applications; Simulacion de los fenomenos de flujo en pozos geotermicos: desarrollos y aplicaciones

Energy Technology Data Exchange (ETDEWEB)

Garcia Gutierrez, Alfonso [Instituto de Investigaciones Electricas, Cuernavaca (Mexico)

1994-07-01

In this paper the numerical simulators and the specialized computer programs that have been developed in the Departamento de Geotermia of the Instituto de Investigaciones Electricas (IIE) for the study of mass transport phenomena, momentum and heat in geothermal wells, are delineated. The developments can be assembled in 5 types: a) Fluid circulation during geothermal well construction; b) Production; c) Construction; d) Return to the thermal equilibrium; e) Thermodynamic and fluid transport properties, cements, and rocks. The applications realized include, besides the normal flow phenomena that occur in geothermal wells, the study of special problems that have been found in several wells of the geothermal fields in the country. These developments constitute a tool of great utility for the reservoir engineer`s daily work and for the understanding of the specific phenomena of infrequent occurrence. [Espanol] En este trabajo se describen los simuladores numericos y programas de computo especializados que se han desarrollado en el Departamento de Geotermia del Instituto de Investigaciones Electricas (IIE), para estudiar los fenomenos de transporte de masa, momentum y calor en pozos geotermicos. Los desarrollos pueden agruparse en 5 tipos: a) circulacion de fluidos durante la construccion de pozos, b) produccion, c) inyeccion, d) retorno a equilibrio termico, e) propiedades termodinamicas y de transporte de los fluidos, cementos y rocas. Las aplicaciones realizadas incluyen, ademas de los fenomenos normales de flujo que ocurren en pozos geotermicos, el estudio de problemas especiales que se han encontrado en diversos pozos de los campos geotermicos del pais. Estos desarrollos constituyen una herramienta de gran utilidad para el trabajo diario del ingeniero de yacimientos y para el entendimiento de fenomenos especificos de ocurrencia poco frecuente.

Geology and geochemistry of Pelagatos, Cerro del Agua, and Dos Cerros monogenetic volcanoes in the Sierra Chichinautzin Volcanic Field, south of México City

Science.gov (United States)

Agustín-Flores, Javier; Siebe, Claus; Guilbaud, Marie-Noëlle

2011-04-01

This study focuses on the geology and geochemistry of three closely-spaced monogenetic volcanoes that are located in the NE sector of the Sierra Chichinautzin Volcanic Field near México City. Pelagatos (3020 m.a.s.l.) is a small scoria cone (0.0017 km 3) with lava flows (0.036 km 3) that covered an area of 4.9 km 2. Cerro del Agua scoria cone (3480 m.a.s.l., 0.028 km 3) produced several lava flows (0.24 km 3) covering an area of 17.6 km 2. Dos Cerros is a lava shield which covers an area of 80.3 km 2 and is crowned by two scoria cones: Tezpomayo (3080 m.a.s.l., 0.022 km 3) and La Ninfa (3000 m.a.s.l., 0.032 km 3). The eruptions of Cerro del Agua and Pelagatos occurred between 2500 and 14,000 yr BP. The Dos Cerros eruption took place close to 14,000 yr BP as constrained by radiocarbon dating. Rocks from these three volcanoes are olivine-hypersthene normative basaltic andesites and andesites with porphyritic, aphanitic, and glomeroporphyritic textures. Their mineral assemblages include olivine, clinopyroxene, and orthopyroxene phenocrysts (≤ 10 vol.%) embedded in a trachytic groundmass which consists mainly of plagioclase microlites and glass. Pelagatos rocks also present quartz xenocrysts. Due to their high Cr and Ni contents, and high Mg#s, Pelagatos rocks are considered to be derived from primitive magmas, hence the importance of this volcano for understanding petrogenetic processes in this region. Major and trace element abundances and petrography of products from these volcanoes indicate a certain degree of crystal fractionation during ascent to the surface. However, the magmas that formed the volcanoes evolved independently from each other and are not cogenetically related. REE, HFSE, LILE, and isotopic (Sr, Nd, and Pb) compositions point towards a heterogeneous mantle source that has been metasomatized by aqueous/melt phases from the subducted Cocos slab. There is no clear evidence of important crustal contributions in the compositions of Pelagatos and

Optical atmospheric extinction over Cerro Paranal

NARCIS (Netherlands)

Patat, F.; Moehler, S.; O'Brien, K.; Pompei, E.; Bensby, T.; Carraro, G.; de Ugarte Postigo, A.; Fox, A.; Gavignaud, I.; James, G.; Korhonen, H.; Ledoux, C.; Randall, S.; Sana, H.A.A.; Smoker, J.; Stefl, S.; Szeifert, T.

2011-01-01

Aims. The present study was conducted to determine the optical extinction curve for Cerro Paranal under typical clear-sky observing conditions, with the purpose of providing the community with a function to be used to correct the observed spectra, with an accuracy of 0.01 mag airmass-1.

Geological map of Uruguay Esc 1,100,000. Cerro Partido Sheet F-24

International Nuclear Information System (INIS)

Diaz, R; Albanell, H.; Bossi, J.

1990-01-01

This work is about the geological map of Uruguay Esc.1.100.000 (Cerro Partido) and the explanatory memoranda which describes the geological , lithological and sedimentological characteristics soils. The area corresponding to the Cerro Partido fotoplano is located in the orogenic belt or Don Feliciano belt

Investigating the subsurface connection beneath Cerro Negro volcano and the El Hoyo Complex, Nicaragua

Science.gov (United States)

Venugopal, Swetha; Moune, Séverine; Williams-Jones, Glyn

2016-10-01

Cerro Negro, the youngest volcano along the Central American Volcanic Belt (CAVB), is a polygenetic cinder cone with relatively frequent basaltic eruptions. The neighbouring El Hoyo complex, of which Las Pilas is the dominant edifice, is a much larger and older complex with milder and less frequent eruptions. Previous studies have suggested a deep link beneath these two closely spaced volcanoes (McKnight, 1995; MacQueen, 2013). Melt inclusions were collected from various tephra samples in order to determine whether a connection exists and to delineate the features of this link. Major, volatile, and trace elemental compositions reveal a distinct geochemical continuum with Cerro Negro defining the primitive endmember and El Hoyo representing the evolved endmember. Magmatic conditions at the time of melt inclusion entrapment were estimated with major and volatile contents: 2.4 kbar and 1170 °C for Cerro Negro melts and 1.3 kbar and 1130 °C for El Hoyo melts with an overall oxygen fugacity at the NNO buffer. Trace element contents are distinct and suggest Cerro Negro magmas fractionally crystallise while El Hoyo magmas are a mix between primitive Cerro Negro melts and residual and evolved El Hoyo magma. Modelling of end member compositions with alphaMELTS confirms the unique nature of El Hoyo magmas as resulting from incremental mixing between Cerro Negro and residual evolved magma at 4 km depth. Combining all available literature data, this study presents a model of the interconnected subsurface plumbing system. This model considers the modern day analogue of the Lemptégy cinder cones in Massif Central, France and incorporates structurally controlled dykes. The main implications of this study are the classification of Cerro Negro as the newest conduit within the El Hoyo Complex as well as the potential re-activation of the El Hoyo edifice.

Lichens as biological monitors in the Los Azufres geothermal field, Michoacan, Mexico; Liquenes como indicadores biologicos en el campo geotermico Los Azufres, Michoacan, Mexico

Energy Technology Data Exchange (ETDEWEB)

Gomez Peralta, Marlene; Chavez Carmona, Arturo [Universidad Michoacana de San Nicolas de Hidalgo, Morelia (Mexico)

1995-09-01

The results obtained in the monitoring of the atmospheric emissions of the Los Azufres geothermal field in Michoacan State, Mexico utilizing lichens as monitors of the presence of sulphur and arsenic, at the areas near geothermal sites, both under evaluation and production, are presented. The results are based on symptoms which included: chlorosis, necrosis, brown and reddish spots, loss of adherence to substrate, thalli disintegration and disappearance of sensitive species; and also on the amounts of sulphur and arsenic contained in the lichens thallus. [Espanol] Se presentan los resultados obtenidos en el monitoreo de las emisiones atmosfericas del campo geotermico Los Azufres, Michoacan, Mexico en el que se utilizaron liquenes como indicadores de la presencia de azufre y arsenico, en las areas cercanas a los sitios de pozos geotermicos tanto en evaluacion como en produccion. Los resultados estan basados en sintomas que incluyen clorosis, necrosis, manchas cafes y rojizas, perdida de adherencia al sustrato, desintegracion del talo y desaparicion de especies sensibles; asi como en los contenidos de azufre y arsenico en los talos liquenicos.

Sedimentary rocks Uranium in Cerro Largo Province; Uranio en rocas sedimentarias en el departamento de Cerro Largo

Energy Technology Data Exchange (ETDEWEB)

Scaron, P; Garau Tous, M

1976-07-01

With the aim of the uranium minerals exploration has been carried out several studies by UTE technicians in Cerro Largo Province from 1968 to 1969. In uranium concentration has been found pyrite, phosphate, iron oxides and manganese in uranium. Furthermore in La Divisa Ore were studied concentration Uranium enrichment has been studied in La Divisa ore.

Daniel Prieto Castillo y la utopía pedagógica

Directory of Open Access Journals (Sweden)

Kintto Lucas

2015-01-01

Full Text Available En la entrevista realizada a Daniel Prieto Castillo, éste afirma que entre lo que produce la cultura, las prácticas, los saberes y quienes están en situación de aprender siempre hay mediaciones sociales. Al opinar sobre la educación alternativa dice que hay una explosión de lo alternativo porque hay una explosión de la sociedad civil en todos, los campos. Discrepa de los programas infantiles como el dirigido por XUXA por su terrible violencia referida a la saturación de sonido de la animadora no hay silencio, pausa o respiro solo gritos, es de un manipuleo insoportable.

Numerical study on the effect of non-condensable gases on the bi-phasic flow in geothermal wells; Estudio numerico del efecto de gases incondensables sobre el flujo bifasico en pozos geotermicos

Energy Technology Data Exchange (ETDEWEB)

Santoyo Gutierrez, Edgar; Garcia Gutierrez, Alfonso; Santoyo Gutierrez, Socrates; Morales Rosas, Jose Manuel [Instituto de Investigaciones Electricas, Cuernavaca (Mexico)

1993-09-01

The objective of this paper is to describe a numerical study to determine the flow characteristics that predominate in geothermal wells and that produces a significant amount of non-condensable gases. It is known that these gases affect the thermodynamic conditions that dominate the fluid transport in the well or inclusively within the proper producing reservoir, therefore, it is extremely important to evaluate this effect. For this purpose the numerical model Geopozo V2.0 was developed. This model considers the carbon dioxide (CO{sub 2}) as the representative gas of the non-condensable gases present in the geothermal fluid. Due to this consideration, Geopozo V2.0 includes a methodology or the estimation of the thermodynamic and transport properties of geothermal fluids, considering these as a mix of two components: H{sub 2}O (vapor and liquid) and CO{sub 2}, under conditions of monophasic and biphasic flow. The application of Geopozo V2.0 for a typical case of flow in geothermal wells with high CO{sub 2} content revealed that the presence of this gas affects significantly the location of the flashing point inside the well and consequently, the amount of steam produced. This is of importance or the design and selection of the surface and generation equipment, aspect that to this date has been ignored (Suwana, 1991). [Espanol] El objetivo de este trabajo es describir un estudio numerico para determinar las caracteristicas del flujo que predominan en pozos geotermicos y que producen una cantidad significante de gases incondensables. Se tiene conocimiento de que estos gases afectan las condiciones termodinamicas que dominan el transporte de fluidos en el pozo o incluso dentro del mismo yacimiento geotermico productor, por lo que es de suma importancia evaluar dicho efecto. Para ello fue desarrollado el modelo numerico Geopozo V2.0. Este modelo considera al dioxido de carbono (CO{sub 2}) como el gas representativo de los incondensables presentes en el fluido geotermico

Sedimentary rocks Uranium in Cerro Largo Province

International Nuclear Information System (INIS)

Scaron, P.; Garau Tous, M.

1976-01-01

With the aim of the uranium minerals exploration has been carried out several studies by UTE technicians in Cerro Largo Province from 1968 to 1969. In uranium concentration has been found pyrite, phosphate, iron oxides and manganese in uranium. Furthermore in La Divisa Ore were studied concentration Uranium enrichment has been studied in La Divisa ore

Evaluation of the Cerro Solo nuclear ore, province of Chubut. The Cerro Solo project within the frame of uranium exploration in Argentina. Pt. 1

International Nuclear Information System (INIS)

Solis, R.J.; Navarra, P.R.; Benitez, A.F.; Gallucci, A.R.

1993-01-01

The Cerro Solo ore deposit was selected by the CNEA to invest in an assessment project because of their promising grade and amount of known and potential resources, significant to Argentina's uranium requirements. The deposit, which is located in the central region of the Chubut Province, belongs to the sandstone type and is hosted by the cretaceous Chubut Group. Technical studies carried out forecast an important growth of nuclear capacity to meet Argentina's energy requirements in the first two decades of of the the next century. To be in position to confront the challenge presented by increasing uranium resources to fuel the nuclear powers plants it is very important, as a first step, to improve the geological knowledge of uranium favorability in the country. The preliminary results of the Cerro Solo project indicate that the eastern slope of the Pichinan hills is a promising area for development of uranium resources, increasing the favorability of the San Jorge Basin in order to allow contributing to meet future uranium requirements. The Cerro Solo Project was planned in a sequential manner, as a multidisciplinary effort which includes studies on: geologic setting of mineralization, resource estimates, costs of mining and milling methods, economic analysis and environmental impact research. Among the mining methods, studies include the alternative of the in-situ leaching technology, which is becoming a low producing cost interesting possibility. (Author)

Report of mortmorilloniticas clay in the Medina swamp (Cerro Largo district)

International Nuclear Information System (INIS)

Gomez Rifas, C.; Heinzen, W.; Theune, C.

1980-01-01

This report describes the prospect ion work for the montmorillonitics clay in the region of Medina swamp in Cerro Largo district. The existence of new deposits was detected by cartography and geological study.

Análisis de la estabilidad del cerro Shishio mediante el empleo de técnicas numéricas

OpenAIRE

Vintimilla Avila, Maribel Cristina

2011-01-01

La presente investigación analiza la estabilidad existente en el Cerro Shishio ubicado en el sector de La Josefina por medio de técnicas numéricas. El deslizamiento del cerro Shishio provocado por el desfogue de las aguas represadas por el deslizamiento del cerro Tamuga, se originó en el material de la Formación Tarqui, el mismo que se deslizó sobre un roca intrusiva muy alterada. En la actualidad se puede observar el material deslizado acumulado al pie del talud, que ahora sirve de soporte ...

Miguel Prieto y la escenografía en la España de los años treinta

Directory of Open Access Journals (Sweden)

Cabañas Bravo, Miguel

2011-12-01

Full Text Available The artist Miguel Prieto (1907-1956 worked in three main areas: painting-drawing, graphic design and set design. The latter was the one in which he demonstrated most interest in avant-garde and political commitment during the thirties, but due to his subsequent Mexican exile, has not been dealt with in recent research. This article, focused on his years in Spain, analyses his contributions to scenic design. Prieto’s first professional period, when he worked for the puppet theatre, coincided with the young Second Republic and then the convulsion of the Civil War. This popular genre was utilized for agitation, propaganda and the revolutionary theatre, and adopted both the classical repertoire and modern works by Alberti, Dieste, Lorca and other committed youthful intellectuals.

Las tres grandes vertientes en las que el pintor Miguel Prieto (1907-1956 plasmó su creatividad fueron la pintura-dibujo, el diseño gráfico y la escenografía. Esta última, que fue en la que más énfasis puso tanto en su acercamiento a la vanguardia y el compromiso socio-político de los años treinta, como en los años finales de su trayectoria en el exilio mexicano, no ha sido suficientemente atendida. Este artículo, centrado en esa etapa española, analiza y pone en valor la aportación a la escena de Prieto coincidente con esos momentos de construcción de la joven II República y la convulsión de la Guerra Civil, que principalmente se plasmó en la escenificación de espectáculos de guiñol (extraídos del repertorio clásico o expresamente escritos por Alberti, Dieste, Lorca y otros jóvenes inquietos, ya que su tradición y clara aceptación popular los convertían en adecuado instrumento para encauzar la agitación y propaganda que querían sembrar el teatro revolucionario y la creatividad más avanzada y comprometida.

Report of boring made in the South of Cerro Largo district (Cerro Largo) 1977-1978

International Nuclear Information System (INIS)

Massa, E.

1984-01-01

The present work are within the framework and compiles the data obtained by means of the study of the perforations executed in the District Cerro Largo Sur of the detailed prospection of uranium minerals. This study was carried out by technicians of Geologic ex--Institute of Uruguay (IGU) - at the moment National Direction of Mining and Geology. (DINAMIGE). The works began at the beginning of 1977 and continued until 1978 July; The headquarters of the program of prospection of uranium was carried out by Ing. Hector Goso. In this report the conclusions drawn at the time of the detection of the works in the District already published, as well as the litologicos cuts of all the executed perforations are included

Hidrogeologic and geophysical studies into Agro school Melo UTU Cerro Largo province

International Nuclear Information System (INIS)

Heinzen, W.; Santana, I.; Mari, C.

1986-01-01

The technical University UTU of Uruguay requested and Hidrogeologic study with the aim to analyze the factibility to discover underground stream waters which supply groundwaters into agro school Ing Agr. Alcides E Pintos Melo, Cerro Largo province.

Characterization of pottery from Cerro de Las Ventanas, Zacatecas, Mexico

International Nuclear Information System (INIS)

Lopez-del-Rio, H.; Mireles-Garcia, F.; Mendez-Cardona, R.Y.; Nicolas-Caretta, M.; Speakman, R.J.; Glascock, M.D.

2009-01-01

With the aim of classifying prehispanic pottery from Cerro de Las Ventanas site, Juchipila, Zacatecas, Mexico, instrumental neutron activation analysis (INAA) was used to analyze ceramic samples at the University of Missouri Research Reactor Center. Thirty-two chemical elements were measured: Al, As, Ba, Ca, Ce, Co, Cr, Cs, Dy, Eu, Fe, Hf, K, La, Lu, Mn, Na, Nd, Rb, Sb, Sc, Sm, Sr, Ta, Tb, Ti, Th, U, V, Yb, Zn, and Zr. Two multivariate statistical methods, cluster analysis and principal component analysis, were performed on the dataset to examine similarities between samples and to establish compositional groups. The statistical analyses of the dataset suggest that the pottery samples form a unique chemically homogeneous group, with the exception of one pottery sample. The compositional data were compared to an existing Mesoamerican ceramic database. It was found that the newly generated data fit best with data from a previous chemical analysis of pottery from the Malpaso Valley. However, despite the apparent similarity, pottery samples from the site of Cerro de Las Ventanas represent a new and unique chemical fingerprint in the region. (orig.)

Characterization of pottery from Cerro de Las Ventanas, Zacatecas, Mexico

Energy Technology Data Exchange (ETDEWEB)

Lopez-del-Rio, H.; Mireles-Garcia, F. [Unidad Academica de Estudios Nucleares, UAZ, Zacatecas (Mexico); Mendez-Cardona, R.Y. [Unidad Academica de Antropologia, UAZ, Zacatecas (Mexico); Nicolas-Caretta, M. [INAH Delegacion Zacatecas (Mexico); Coordinacion de Ciencias Sociales y Humanidades, UASLP, Fracc. Talleres, SLP (Mexico); Speakman, R.J. [Museum Conservation Inst., Smithsonian Institution, Suitland, MD (United States); Glascock, M.D. [Research Reactor Center, Univ. of Missouri, Columbia, MO (United States)

2009-09-15

With the aim of classifying prehispanic pottery from Cerro de Las Ventanas site, Juchipila, Zacatecas, Mexico, instrumental neutron activation analysis (INAA) was used to analyze ceramic samples at the University of Missouri Research Reactor Center. Thirty-two chemical elements were measured: Al, As, Ba, Ca, Ce, Co, Cr, Cs, Dy, Eu, Fe, Hf, K, La, Lu, Mn, Na, Nd, Rb, Sb, Sc, Sm, Sr, Ta, Tb, Ti, Th, U, V, Yb, Zn, and Zr. Two multivariate statistical methods, cluster analysis and principal component analysis, were performed on the dataset to examine similarities between samples and to establish compositional groups. The statistical analyses of the dataset suggest that the pottery samples form a unique chemically homogeneous group, with the exception of one pottery sample. The compositional data were compared to an existing Mesoamerican ceramic database. It was found that the newly generated data fit best with data from a previous chemical analysis of pottery from the Malpaso Valley. However, despite the apparent similarity, pottery samples from the site of Cerro de Las Ventanas represent a new and unique chemical fingerprint in the region. (orig.)

ALFONSO X EL SABIO, General Estoria, VI partes (tomos I-X, Pedro SÁNCHEZ-PRIETO (coord.,

Directory of Open Access Journals (Sweden)

Irene SALVO GARCÍA

2010-06-01

Full Text Available La General Estoria compuesta en el taller historiográfico de Alfonso X (1221-1284 se publica íntegra por primera vez gracias a esta edición dirigida por Pedro Sánchez-Prieto y patrocinada por la Biblioteca Castro. Por las características intrínsecas de la obra y por la calidad y rigurosidad editorial esta publicación supone un acontecimiento de importantísimas consecuencias para las letras castellanas medievales que hasta ahora se encontraban incompletas sin la edición íntegra de la obra alf...

Report of the Cerro Chato ultrabasic geophysical studies

International Nuclear Information System (INIS)

Cicalese, H.; Mari, C.; Lema, F.; Valverde, C.; Haut, R.

1987-01-01

This report refers to the obtained results of geophysical practiced during the year 1985 in the area of the ultrabasic of Cerro Chato, located in the area called Puntas del Malbajar in Durazno province. The aim was rehearsed an answer of an ultrabasic behaviour of the geophysical prospecting methods.They were carried out studies in magnetometry, induced polarization, electromagnetism and resistivity measurements in electric vertical sound. As well conclusions as recommendations express that applied geophysical methods allow to make ultrabasic charts or maps.

LA CERÁMICA CERRO LOS HORNOS, PRESENCIA INKA EN LA COSTA DE TACNA, SUR DEL PERÚ

OpenAIRE

Vela Velarde, Carlos

2004-01-01

Se estudia el sitio Cerro Los Hornos, ubicado en la costa de Tacna, sur del Perú. Presenta cerámica con filiación Inka Imperial o Cuzco Policromo, pero de fabricación local; esta presencia cultural es consecuencia del proceso de expansión Inka a la costa sur del Perú, la cual establece relaciones con la sociedad local The place studied is Cerro Los Hornos located in the coast of Tacna, south of Peru, presents ceramic with filiation Inka Imperial or Cuzco Policromo, but of local production;...

The last glacial cycle and palaeolake synchrony in the southern bolivian Altiplano: Cerro Azanaques case study

Directory of Open Access Journals (Sweden)

1995-01-01

Full Text Available SYNCHRONISME ENTRE LE DERNIER CYCLE GLACIAIRE ET L'EXTENSION DES PALÉOLACS DANS LE SUD DE L'ALTIPLANO BOLIVIEN : EXEMPLE DU CERRO AZANAQUES. Dans la Cordillère Orientale, au niveau du Cerro Azanaques (18°S, Bolivie, des moraines, des sédiments glaciaires, des rivages paléolacustres, des deltas et des stromatolites qui se sont préservés, révèlent des conditions climatiques fortement différentes dans le passé. La culmination de la dernière avancée du glacier Lijunimani a été datée par la méthode du radiocarbone à 13 000 ans BP à partir de sédiments glaciaires ayant remanié un horizon organique de tourbe. La cartographie de cette diacmitite argileuse particulière révèle un delta en forme de cône bordé par un glacier cela montre que les glaciers et les anciens systèmes lacustres font partie d'un processus d'expansion simultanée. L'étude stratigraphique détaillée réalisée au Cerro Azanaques fournit de fortes évidences allant dans le sens d'une réponse commune des glaciers et des lacs à un signal piloté par un changement climatique les lacs ne sont donc pas le simple résultat de la fonte des glaciers des cordillères. SINCRONISMO ENTRE EL ÚLTIMO CICLO GLACIAL Y LA EXTENSIÓN DE LOS PALEOLAGOS EN EL SUR DEL ALTIPLANO BOLIVIANO: CASO DEL CERRO AZANAQUES. En la Cordillera Oriental, a la altura del Cerro Azanaques (18º S, Bolivia aparecen preservadas morrenas y sedimentos glaciares, líneas de costa paleolacustres, deltas y estromatolitos, lo que revela condiciones climáticas pasadas significativamente diferentes. La culminación del último avance del glaciar Lijunimani ha sido fechada mediante radiocarbono a 13 000 años BP a partir de sedimentos glaciares que han desplazado un horizonte orgánico de turba. La cartografía de esta particular diamictita arcillosa revela un delta en forma de abanico con hielo en sus márgenes lo que indica que los glaciares y los sistemas paleolacustres sufrieron un proceso

Mining inventory of Uruguay. Results of geochemical prospecting of Cerro Partido fotoplano

International Nuclear Information System (INIS)

Zeegers, H.; Artignan, D.; Vairon, P.

1982-01-01

This work is about the analitical results of the geological prospection carried out in Cerro Partido zone within the framework of Mining inventory of Uruguay. In this fotoplano (Esc. 1/50.000 and 1/400.000 there are metamorphic, mesozoic and carbonated formations

U-Pb and K-Ar geochronology from the Cerro Empexa Formation, 1st and 2nd Regions, Precordillera, northern Chile

International Nuclear Information System (INIS)

Tomlinson, A.J; Martin, M.W; Blanco, N.; Perez de Arce, C

2001-01-01

The Cerro Empexa Formation (Galli, 1957) is a regionally distributed andesitic volcanic and continental sedimentary unit exposed in the Precordillera of the 1st and 2nd Regions of northern Chile. The formation has generally been considered to lie within the Lower or 'mid' Cretaceous, however, this assignment is based on scant, unreliable geochronologic data. Furthermore, there are conflicting interpretations as to whether the unit predates or postdates the first major Mesozoic shortening event affecting northern Chile. Because of the formation's presumed mid-Cretaceous age and its stratigraphic position over older back-arc sedimentary successions, the unit has been interpreted to represent products of the first eastward jump in the Andean magmatic arc from the arc's initial position in the Cordillera de la Costa (Scheuber and Reutter, 1992). In this paper we present the results of mapping and field observations that indicate exposures previously assigned to the Cerro Empexa Formation include two andesitic volcanic units separated by a major unconformity. The Cerro Empexa Formation proper lies above this unconformity. We also present U-Pb zircon and K-Ar geochronology that indicate the Cerro Empexa Formation is latest Cretaceous in its lower levels, and integrate our data with previously reported 40 Ar/ 39 Ar and fission-track data in the Cerros de Montecristo area (Maksaev, 1990; Maksaev and Zentilli, 1999) to show that 1800±600 m of rocks were deposited within ca. 2.5 m.y (au)

Proceedings: third symposium on the Cerro Prieto geothermal field, Baja California, Mexico

Energy Technology Data Exchange (ETDEWEB)

1981-01-01

These proceedings include both English and Spanish versions of each paper presented at the symposium. Illustrations and tables, which have been placed between the two versions, include captions in both languages. Forty-one papers are included. Five papers were indexed for EDB previously. Separate abstracts were prepared for thirty-three papers and three were listed by title.

Elemental analysis of pottery from Cerro de las Ventanas, Zacatecas, by INAA

Energy Technology Data Exchange (ETDEWEB)

Lopez del Rio, H.; Mireles G, F. [Universidad Autonoma de Zacatecas, Unidad Academica de Estudios Nucleares, Calle Cipres No. 10, Fracc. La Penuela, 98068 Zacatecas (Mexico); Mendez C, R. Y. [Universidad Autonoma de Zacatecas, Unidad Academica de Antropologia, Apdo. Postal 555 Suc. C, Zacatecas (Mexico); Nicolas C, M. [Universidad Autonoma de San Luis Potosi, Coordinacion de Ciencias Sociales y Humanidades, Av. Industrias 101-A, Fracc. Talleres, 78494 San Luis Potosi (Mexico); Speakman, R. J. [Museum Conservation Institute, Smithsonian Institution, Suitland, 20746 Maryland (United States); Glascock, M. D. [Reactor Center, University of Missouri, Columbia, 65211 Missouri (United States)

2009-10-15

Fifteen ceramic fragments samples from Cerro de las Ventanas site, Zacatecas, were analyzed by instrumental neutron activation analysis. Thirty-two elements were measured: Al, As, Ba, Ca, Ce, Co, Cr, Cs, Dy, Eu, Fe, Hf, K, La, Lu, Mn, Na, Nd, Rb, Sb, Sc, Sm, Sr, Ta, Tb, Ti, Th, U, V, Yb, Zn, and Zr. Cluster analysis and principal component analysis were performed on the dataset to examine similarities between samples and to establish compositional groups. The statistical analyses of the dataset suggest that the pottery samples form a unique chemically homogeneous group, with the exception of one pottery sample. The compositional data were compared to an existing Meso american ceramic database. It was found that the newly generated data fit best with data from a previous chemical analysis of pottery from the Mal paso Valley. However, despite the apparent similarity, pottery samples from the site of Cerro de las Ventanas represent a new and unique chemical fingerprint in the region. (Author)

Elemental analysis of pottery from Cerro de las Ventanas, Zacatecas, by INAA

International Nuclear Information System (INIS)

Lopez del Rio, H.; Mireles G, F.; Mendez C, R. Y.; Nicolas C, M.; Speakman, R. J.; Glascock, M. D.

2009-10-01

Fifteen ceramic fragments samples from Cerro de las Ventanas site, Zacatecas, were analyzed by instrumental neutron activation analysis. Thirty-two elements were measured: Al, As, Ba, Ca, Ce, Co, Cr, Cs, Dy, Eu, Fe, Hf, K, La, Lu, Mn, Na, Nd, Rb, Sb, Sc, Sm, Sr, Ta, Tb, Ti, Th, U, V, Yb, Zn, and Zr. Cluster analysis and principal component analysis were performed on the dataset to examine similarities between samples and to establish compositional groups. The statistical analyses of the dataset suggest that the pottery samples form a unique chemically homogeneous group, with the exception of one pottery sample. The compositional data were compared to an existing Meso american ceramic database. It was found that the newly generated data fit best with data from a previous chemical analysis of pottery from the Mal paso Valley. However, despite the apparent similarity, pottery samples from the site of Cerro de las Ventanas represent a new and unique chemical fingerprint in the region. (Author)

Magma-Tectonic Interactions along the Central America Volcanic Arc: Insights from the August 1999 Magmatic and Tectonic Event at Cerro Negro, Nicaragua

Science.gov (United States)

La Femina, P.; Connor, C.; Strauch, W.

2002-12-01

Volcanic vent alignments form parallel to the direction of maximum horizontal stress, accommodating extensional strain via dike injection. Roughly east-west extension within the Central America Volcanic Arc is accommodated along north-northwest-trending basaltic vent alignments. In Nicaragua, these alignments are located in a northwest-trending zone of dextral shear, with shear accommodated along northeast trending bookshelf faults. The recent eruption of Cerro Negro volcano, Nicaragua and Marabios Range seismic swarm revealed the interaction of these fault systems. A low energy (VEI 1), small volume (0.001 km3 DRE) eruption of highly crystalline basalt occurred at Cerro Negro volcano, Nicaragua, August 5-7, 1999. This eruption followed three tectonic earthquakes (each Mw 5.2) in the vicinity of Cerro Negro hours before the onset of eruptive activity. The temporal and spatial pattern of microseismicity and focal mechanisms of the Mw 5.2 earthquakes suggests the activation of northeast-trending faults northwest and southeast of Cerro Negro within the Marabios Range. The eruption was confined to three new vents formed on the southern flank of Cerro Negro along a preexisting north-northwest trending alignment; the El Hoyo alignment of cinder cones, maars and explosion craters. Surface ruptures formed > 1 km south and southeast of the new vents suggest dike injection. Numerical simulations of conduit flow illustrate that the observed effusion rates (up to 65 ms-1) and fountain heights (50-300 m) can be achieved by eruption of magma with little or no excess fluid pressure, in response to tectonic strain. These observations and models suggest that 1999 Cerro Negro activity is an excellent example of tectonically induced small-volume eruptions in an arc setting.

Report of boring made in the South of Cerro Largo district (Cerro Largo) 1977-1978[Study of Uranium prospection in Uruguay]; Informe de los trabajos de perforacion efectuados en el distrito Cerro Largo Sur (Dpto. Cerro Largo) 1977 - 1978

Energy Technology Data Exchange (ETDEWEB)

Massa, E

1984-07-01

The present work are within the framework and compiles the data obtained by means of the study of the perforations executed in the District Cerro Largo Sur of the detailed prospection of uranium minerals. This study was carried out by technicians of Geologic ex--Institute of Uruguay (IGU) - at the moment National Direction of Mining and Geology. (DINAMIGE). The works began at the beginning of 1977 and continued until 1978 July; The headquarters of the program of prospection of uranium was carried out by Ing. Hector Goso. In this report the conclusions drawn at the time of the detection of the works in the District already published, as well as the litologicos cuts of all the executed perforations are included.

Un proyecto de Francisco Prieto-Moreno de cuatro casas en la Huerta de los Ángeles

Directory of Open Access Journals (Sweden)

Miguel Ángel Sorroche Cuerva

2009-12-01

Full Text Available La realización de promociones de viviendas en algunos sectores de Granada, adquirió unas especiales características en el barrio del Realejo. En torno a la calle Molinos se consolidó en los años cuarenta del siglo XX, un modelo de urbanización con viviendas unifamiliares que adquirió tintes de lujo, curiosamente a partir de iniciativas sociales. La presencia de arquitectos como Francisco Prieto-Moreno, habla de las pretensiones de algunos de estos proyectos que ayudaron a conformar la imagen residencial de esta zona de Granada, y que a lo largo del siglo XIX comenzaría a configurar el aspecto que hoy la caracteriza.

Role of forest conservation in lessening land degradation in a temperate region: the Monarch Butterfly Biosphere Reserve, Mexico.

Science.gov (United States)

Manzo-Delgado, Lilia; López-García, José; Alcántara-Ayala, Irasema

2014-06-01

With international concern about the rates of deforestation worldwide, particular attention has been paid to Latin America. Forest conservation programmes in Mexico include Payment for Environmental Services (PES), a scheme that has been successfully introduced in the Monarch Butterfly Biosphere Reserve. To seek further evidence of the role of PES in lessening land degradation processes in a temperate region, the conservation state of the Cerro Prieto ejido within the Reserve was assessed by an analysis of changes in vegetation cover and land-use between 1971 and 2013. There were no changes in the total forest surface area, but the relative proportions of the different classes of cover density had changed. In 1971, closed and semi-closed forest occupied 247.81 ha and 5.38 ha, 82.33% and 1.79% of the total area of the ejido, respectively. By 2013, closed forest had decreased to 230.38 ha (76.54% of the ejido), and semi-closed cover was 17.23 ha (5.72% of the ejido), suggesting that some semi-closed forest had achieved closed status. The final balance between forest losses and recovery was: 29.63 ha were lost, whereas 13.72 ha were recovered. Losses were mainly linked to a sanitation harvest programme to control the bark beetle Scolytus mundus. Ecotourism associated with forest conservation in the Cerro Prieto ejido has been considered by inhabitants as a focal alternative for economic development. Consequently, it is essential to develop a well-planned and solidly structured approach based on social cohesion to foster a community-led sustainable development at local level. Copyright © 2013 Elsevier Ltd. All rights reserved.

The Cerro Grande Fire - From Wildfire Modeling Through the Fire Aftermath

Energy Technology Data Exchange (ETDEWEB)

Rudell, T. M. (Theresa M.); Gille, R. W. (Roland W.)

2001-01-01

The Cerro Grande Fire developed from a prescribed burn by the National Park Service at Bandelier National Monument near Los Alamos, New Mexico. When the burn went out of control and became a wildfire, it attracted worldwide attention because it threatened the birthplace of the atomic bomb, Los Alamos National Laboratory (LANL). Was LANL prepared for a fire? What lessons have been learned?

The Cerro Grande Fire - From Wildlife Modeling Through the Fire Aftermath

Energy Technology Data Exchange (ETDEWEB)

Rudell, T. M. (Theresa M.); Gille, R. W. (Roland W.)

2001-01-01

The Cerro Grande Fire developed from a prescribed burn by the National Park Service at Bandelier National Monument near Los Alamos, New Mexico. When the burn went out of control and became a wildfire, it attracted worldwide attention because it threatened the birthplace of the atomic bomb, Los Alamos National Laboratory (LANL). Was LANL prepared for a fire? What lessons have been learned?

Minería, conflicto y mediadores locales: Minera San Xavier en Cerro de San Pedro, México Mineira, conflito e mediadores locais: Minera San Xavier em Cerro de San Pedro Mining, conflict and local brokers: Minera San Xavier in Cerro de San Pedro

Directory of Open Access Journals (Sweden)

Hernán Horacio Schiaffini

2011-12-01

Full Text Available Este trabajo indaga en las instancias de mediación que intervienen en la articulación de procesos económicos de gran escala y su puesta en práctica local. Basándonos en el conflicto que se produjo en el Municipio de Cerro de San Pedro (San Luis Potosí, México entre la empresa Minera San Xavier y el Frente Amplio Opositor (FAO a la misma, aplicamos el método etnográfico con el objetivo de describir las estructuras locales de mediación política y analizar sus prácticas y racionalidad. Intentamos demostrar así la importancia de los factores políticos locales en las vinculaciones entre estado, empresa y población.Este trabalho indaga nas instâncias de mediação que intervêm em processos econômicos de grande escala e sua posta em prática local. Baseando-nos no conflito no Cerro de San Pedro (San Luis Potosí, México entre a empresa Minera San Xavier e a Frente Amplio Opositor (FAO aplicamos o método etnográfico pra descrever as estruturas de mediação política locais e analisar suas práticas e racionalidade. Tenta-se demonstrar assim a importância dos fatores políticos locais nas vinculações entre estado, empresa e população.This paper investigates in instances of mediation involved in large-scale economic processes and local implementation. Analyzing the conflict in Cerro de San Pedro (San Luis Potosí, México among San Xavier mining company and the Frente Amplio Opositor (FAO, it applies an ethnographic approach to describe the local structures of political mediation and its practices and rationality. The work shows the relevance of local factors in the relationships between State, company and people.

Geología de la región del Cerro Guanaquero, Río Diamante, Mendoza Geology of Cerro Guanaquero region, Diamante River, Mendoza

OpenAIRE

Federico Fuentes; Victor A. Ramos

2008-01-01

El estudio realizado presenta nuevos datos sobre un sector poco conocido de la Cordillera Principal de Mendoza, en la alta cuenca del río Diamante en las adyacencias del cerro Guanaquero, y los primeros datos geocronológicos de sus rocas volcánicas. Las unidades geológicas presentes en el área se dividen en cuatro grupos principales: secuencias sedimentarias mesozoicas marinas y continentales intensamente plegadas y falladas; intrusivos y volcanitas intermedias de edad neógena; rocas volcánic...

Determination of the geothermal well damage from its production tests; Determinacion del dano en pozos geotermicos a partir de sus pruebas de produccion

Energy Technology Data Exchange (ETDEWEB)

Aragon Aguilar, Alfonso; Izquierdo Montalvo, Georgina; Arellano Gomez, Victor [Instituto de Investigaciones Electricas, Cuernavaca, Morelos (Mexico)

2011-06-13

. Sin embargo, la ejecucion de este tipo de pruebas requiere de periodos relativamente largos de tiempo para lograr la estabilizacion del pozo y de costos significativos. Por lo anterior se empezaron a desarrollar tecnicas para determinar el dano a partir de pruebas de produccion. En este articulo se presenta la curva-tipo de influjo geotermico afectada por dano, a partir de la cual se puede determinar el valor de este en un pozo geotermico para el tiempo en que se realiza su prueba de produccion. Se propone la metodologia para determinar el efecto de dano en el pozo usando la curva-tipo propuesta y se demuestra su aplicabilidad con ejemplos de mediciones de pruebas de descarga en pozos de campos geotermicos mexicanos. De los analisis efectuados se encuentra que el valor numerico del dano determinado en los pozos seleccionados aumenta en funcion del tiempo de explotacion, lo cual indica un deterioro en sus caracteristicas productivas. Lo anterior ayuda a conformar un respaldo tecnico para la toma de decisiones, sobre las acciones pertinentes que pueden ejecutar en el pozo.

Forecast of environmental impact in the evaluation of Cerro Solo nuclear mine

International Nuclear Information System (INIS)

Gallucci, A.R.

1993-01-01

This work presents a project for the study of the environmental impact of the Cerro Solo uranium mine. The survey is to be carried out performing different kinds of studies: mineralization, tectonics, hydrogeology, preliminary studies on different exploitation methods, costs, reserves estimation, economical studies and preliminary studies on possible environmental impacts. (author). 24 refs., 1 fig., 1 tab

Burn Severities, Fire Intensities, and Impacts to Major Vegation Types from the Cerro Grande Fire

International Nuclear Information System (INIS)

Balice, R.G.; Bennett, K.D.; Wright, M.A.

2005-01-01

The Cerro Grande Fire resulted in major impacts and changes to the ecosystems that were burned. To partially document these effects, we estimated the acreage of major vegetation types that were burned at selected burn severity levels and fire intensity levels. To accomplish this, we adopted independently developed burn severity and fire intensity maps, in combination with a land cover map developed for habitat management purposes, as a basis for the analysis. To provide a measure of confidence in the acreage estimates, the accuracies of these maps were also assessed. In addition, two other maps of comparable quality were assessed for accuracy: one that was developed for mapping fuel risk and a second map that resulted from a preliminary application of an evolutionary computation software system, called GENIE. According to the burn severity map and the fire intensity map, the Cerro Grande Fire is estimated to have covered 42,885.4 acres and 42,854.7 acres, respectively. Of this, 57.0 percent was burned at low severity and 34.7 percent was burned at high severity. Similarly, 40.0 percent of the Cerro Grande Fire burned at high fire intensity, greater than 70 percent mortality, while 33.1 percent burned at moderately low intensity, 10 to 40 percent mortality. The most frequently burned cover types over the entire Cerro Grande Fire were ponderosa pine forest and mixed conifer forest, at approximately 43 percent each. However, portions of the fire that burned on Los Alamos National Laboratory (LANL) property were predominantly in ponderosa pine forests, whereas the Cerro Grande Fire burned primarily in mixed conifer forests on lands managed by other agencies. Some of the polygons of burn severities and fire intensities were extensive. The two largest burn severity polygons were 10,111 acres and 10,903 acres and these were burned at low severity. The next two largest polygons were 8999 acres (14 square miles) and 1551 acres (2.4 square miles) and both of these polygons

Subsurface Connections and Magma Mixing as revealed by Olivine- and Pyroxene-Hosted Melt Inclusions from Cerro Negro Volcano and the Las Pilas-El Hoyo Complex, Nicaragua.

Science.gov (United States)

Venugopal, S.; Moune, S.; Williams-Jones, G.

2015-12-01

Cerro Negro, the youngest volcano in the Central American Volcanic Belt, is a polygenetic cinder cone with relatively frequent explosive basaltic eruptions. Las Pilas, on the other hand, is a much larger and older complex with milder and less frequent eruptions. Based on historical data, these two closely spaced volcanoes have shown concurrent eruptive behavior, suggesting a subsurface connection. To further investigate this link, melt inclusions, which are blebs of melt trapped in growing crystals, were the obvious choice for optimal comparison of sources and determination of pre-eruptive volatile contents and magmatic conditions. Olivine-hosted inclusions were chosen for both volcanoes and pyroxene-hosted inclusions were also sampled from Las Pilas to represent the evolved melt. Major, volatile and trace elements reveal a distinct geochemical continuum with Cerro Negro defining the primitive end member and Las Pilas representing the evolved end member. Volatile contents are high for Cerro Negro (up to 1260 ppm CO2, 4.27 wt% H2O and 1700 ppm S) suggesting that volatile exsolution is likely the trigger for Cerro Negro's explosive eruptions. Las Pilas volatile contents are lower but consistent with degassing and evolutionary trends shown by major oxides. Trace element contents are rather unique and suggest Cerro Negro magmas fractionally crystallize while Las Pilas magmas are the products of mixing. Magmatic conditions were estimated with major and volatile contents: at least 2.4 kbar and 1170 °C for Cerro Negro melts and 1.3 kbar and 1130 °C for Las Pilas melts with an overall oxygen fugacity at the NNO buffer. In combination with available literature data, this study suggests an interconnected subsurface plumbing system and thus Cerro Negro should be considered as the newest vent within the Las Pilas-El Hoyo Complex.

Steam saving during maintenance of the 50-MW Unit 7 at Los Azufres geothermal field, Michoacan; Ahorro de vapor durante el mantenimiento de la Unidad 7 de 50 MW en el campo geotermico de Los Azufres, Michoacan

Energy Technology Data Exchange (ETDEWEB)

Medina Barajas, Elvia Nohemi; Ruiz Lemus, Alejandro [Comision Federal de Electricidad, Gerencia de Proyectos Geotermoelectricos, Residencia de Los Azufres, Morelia, Michoacan (Mexico)]. E-mail: elvia-medina@cfe.gob.mx

2011-07-15

Commercial-steam production in the southern area of Los Azufres, Mich., Mexico, Geothermal Field began in 1982 with the operation of Unit 2, the backpressure 5-MW unit, and continued in 1988 when the 50-MW condensing Unit 7 was commissioned. Today to supply steam to Unit 7, it is necessary to gather steam from 15 production wells, amounting 450 tons per hour (t/h) under operating conditions. During maintenance periods for Unit 7, production wells are removed from the steam-supply system but continue producing steam that is discharged to the atmosphere-a loss affecting the economic life of the geothermal reservoir. Therefore several actions have been proposed and tried to save the steam and preserve the geothermal resource. This paper presents the results of the actions and the technical and economic benefits obtained from them. [Spanish] La produccion de vapor con fines comerciales en la zona sur del campo geotermico de Los Azufres, Mich., Mexico, empezo en 1982 con la puesta en marcha de la Unidad 2 de 5 MW a contrapresion, para continuar en 1988 con la Unidad 7 de 50 MW a condensacion. Para cumplir con el suministro de vapor a la U-7, a la fecha es necesario integrar la produccion de 15 pozos productores, que producen un total de 450 toneladas por hora (t/h) a condiciones de operacion. Durante los periodos de mantenimiento de la U-7 los pozos son desintegrados del sistema de suministro, pero continuan produciendo vapor, el cual es descargado a la atmosfera sin ningun provecho, lo que representa una perdida que afecta la vida util del yacimiento geotermico. Por ello se han propuesto y aplicado diversas acciones operativas en cada uno de esos pozos con el objetivo de ahorrar vapor y preservar el recurso geotermico. En este trabajo se presentan los resultados de esas acciones y los beneficios tecnicos y economicos obtenidos.

Spatial analysis of noise emission at the Los Azufres geothermal field, Mich.; Analisis espacial de emision de ruido en el campo geotermico de Los Azufres, Mich.

Energy Technology Data Exchange (ETDEWEB)

Camarena Magana, Emilio; Ordaz Mendez, Christian A. [Comision Federal de Electricidad, Residencia de Los Azufres, Morelia, Michoacan (Mexico)]. E-mail: emilio.camarena@cfe.gob.mx

2010-01-15

To verify noise emissions from the usual activities in an operating geothermal field, noise measurements were carried out in a 4.2 km{sup 2} area in the southern zone of the Los Azufres, Mich., geothermal field. There are seven production wells operating here and three abandoned wells. The average noise emission in the southern zone was 36.5 decibels (dB), regarded as the natural reading of environmental-noise emission. In the Christmas (valves) tree for operating production wells, the noise ranges from 70.9 to 91.7 dB, while in open discharging valves for steam-pipes, the noise can reach 118 dB. In Mexico the maximum permissible limit of noise on the periphery of a property is 68 dB in daytime and 65 dB at night. Based on measurements made at the periphery of lots where the geothermal wells are located, four out of seven production wells measured do not exceed the maximum allowable level, while the other three seem to exceed it. However no definite limits exist for the lots. It is recommended that the measurement points as indicated by the official standard in environmental matters be re-established, which will enable noise emissions by several wells that have exceeded the permissible limit, to actually fall within it. [Spanish] Se realizaron mediciones sonicas en un area de 4.2 km{sup 2} localizada en la zona sur del campo geotermico de Los Azufres, Mich., a fin de verificar la emision de ruido asociada a las actividades usuales en un campo geotermico en operacion. En esta area se encuentran siete pozos productores en operacion y tres pozos abandonados. La emision promedio de ruido en estos ultimos fue de 36.5 decibeles (dB), considerandose como la condicion natural de emision de ruido ambiental. En el arbol de valvulas de los pozos productores en operacion el ruido va de los 70.9 a los 91.7 dB, mientras que en valvulas abiertas de descarga de vaporductos la emision puede llegar hasta los 118 dB. En Mexico el limite maximo permisible de ruido en la periferia de

Tectonoestratigraphic and Thermal Models of the Tiburon and Wagner Basins, northern Gulf of California Rift System

Science.gov (United States)

Contreras, J.; Ramirez Zerpa, N. A.; Negrete-Aranda, R.

2014-12-01

The northern Gulf of California Rift System consist sofa series faults that accommodate both normal and strike-slip motion. The faults formed a series of half-greens filled with more than 7 km of siliciclastic suc­cessions. Here, we present tectonostratigraphic and heat flow models for the Tiburón basin, in the southern part of the system, and the Wag­ner basin in the north. The models are constrained by two-dimensional seis­mic lines and by two deep boreholes drilled by PEMEX­-PEP. Analysis of the seismic lines and models' results show that: (i) subsidence of the basins is controlled by high-angle normal faults and by flow of the lower crust, (ii) basins share a common history, and (iii) there are significant differences in the way brittle strain was partitioned in the basins, a feature frequently observed in rift basins. On one hand, the bounding faults of the Tiburón basin have a nested geometry and became active following a west-to-east sequence of activation. The Tiburon half-graben was formed by two pulses of fault activity. One took place during the protogulf extensional phase in the Miocene and the other during the opening of Gulf of California in the Pleistocene. On the other hand, the Wagner basin is the result of two fault generations. During the late-to middle Miocene, the west-dipping Cerro Prieto and San Felipe faults formed a domino array. Then, during the Pleistocene the Consag and Wagner faults dissected the hanging-wall of the Cerro Prieto fault forming the modern Wagner basin. Thermal modeling of the deep borehole temperatures suggests that the heat flow in these basins in the order of 110 mW/m2 which is in agreement with superficial heat flow measurements in the northern Gulf of California Rift System.

Trilobite-based biostratigraphy (arthropoda-trilobita) and related faunas of the Cambrian from Sonora, Mexico

Science.gov (United States)

Cuen-Romero, F. J.; Valdez-Holguín, J. E.; Buitrón-Sánchez, B. E.; Monreal, R.; Enríquez-Ocaña, L. F.; Aguirre-Hinojosa, E.; Ochoa-Granillo, J. A.; Palafox-Reyes, J. J.

2018-04-01

A biostratigraphic analysis based on trilobites of the main Cambrian outcrops from Sonora, Mexico is performed. The data are based on a combination of field work and published sources, including four previously studied locations from northern and eastern Sonora (Caborca, Cananea, Mazatán, and Arivechi) as well as a new location in the central part of the state of Sonora (San José de Gracia). Chronostratigraphic positions are assigned to the Cambrian outcrops according to Peng et al., 2012 and Cohen et al., 2017. In the Caborca area, the Puerto Blanco, Proveedora, Buelna, Cerro Prieto, Arrojos and El Tren formations comprise a wide range of biozones, which starts from the Fritzaspis Zone until the Glossopleura walcotti Zone (Begadean-Lincolnian Series, global Stage 3-Stage 5, Series 2-Series 3). The Bolsa Quartzite and the Abrigo Limestone exposed in Cananea area are assigned to the Cedaria/Cedarina dakotaensis Zone until the Crepicephalus Zone (Lincolnian Series-Marjuman Stage, global Series 3-Guzhangian). In the San José de Gracia area, The Proveedora, Buelna, Cerro Prieto and El Gavilán formations range from the ?Bristolia mohavensis or ?Bristolia insolens zones until the upper part of Mexicella mexicana Zone, Albertella highlandensis Subzone (Series 2-Series 3, Stage 4-Stage 5). In the Arivechi area, the La Sata, El Mogallón, La Huerta and the Milpillas formations range from Poliella denticulata Zone to the Elvinia Zone (Lincolnian-Millardan, Delamaran-Steptoean, global Series 3-Furongian, Stage 5-Paibian). Paleozoic marine fauna distribution in northwest Mexico and the southwest United States of America, suggest that during this time an extensive faunal province existed, containing a great variety of marine invertebrates with notorious intraspecific affinity. The biotic association includes poriferans, archaeocyathids, brachiopods, mollusks, arthropods and echinoderms as predominant elements.

Analysis of exploratory wells in the Cerro Prieto Field and the Mexicali Valley

Energy Technology Data Exchange (ETDEWEB)

Cobo R., J.M.; Bermejo M., F.J.

1982-08-10

Agricultural development in the Mexicali Valley and in the high cost of electric power required to operate the irrigation wells in the Valley prompted the Mexican government to investigate the possibility of taking advantage of thermal manifestations in the area located 28 km southeast of the city of Mexicali to generate electric power and thereby partially decrease the flight of foreign exchange. In 1958, a geologic study of the southern and southeastern zone of Mexicali was conducted to identify the possibilities of tapping geothermal resources. The purpose of this study was to gain knowledge of the geologic conditions in this area and, if possible, to establish the location of exploratory and production wells and, on the basis of the results of the former, examine the geologic history in order to gain knowledge and understanding of the structural control of the steam. On the basis of this study, it was recommended that 3 exploratory wells should be drilled in order to locate weak zones that would easily allow for steam flow.

Analysis of heavy oils: Method development and application to Cerro Negro heavy petroleum

Energy Technology Data Exchange (ETDEWEB)

None

1989-12-01

On March 6, 1980, the US Department of Energy (DOE) and the Ministry of Energy and Mines of Venezuela (MEMV) entered into a joint agreement which included analysis of heavy crude oils from the Venezuelan Orinoco oil belt. The purpose of this report is to present compositional data and describe new analytical methods obtained from work on the Cerro Negro Orinoco belt crude oil since 1980. Most of the chapters focus on the methods rather than the resulting data on Cerro Negro oil, and results from other oils obtained during the verification of the method are included. In addition, published work on analysis of heavy oils, tar sand bitumens, and like materials is reviewed, and the overall state of the art in analytical methodology for heavy fossil liquids is assessed. The various phases of the work included: distillation and determination of routine'' physical/chemical properties (Chapter 1); preliminary separation of >200{degrees} C distillates and the residue into acid, base, neutral, saturated hydrocarbon and neutral-aromatic concentrates (Chapter 2); further separation of acid, base, and neutral concentrates into subtypes (Chapters 3--5); and determination of the distribution of metal-containing compounds in all fractions (Chapter 6).

Analysis of heavy oils: Method development and application to Cerro Negro heavy petroleum

Energy Technology Data Exchange (ETDEWEB)

Carbognani, L.; Hazos, M.; Sanchez, V. (INTEVEP, Filial de Petroleos de Venezuela, SA, Caracas (Venezuela)); Green, J.A.; Green, J.B.; Grigsby, R.D.; Pearson, C.D.; Reynolds, J.W.; Shay, J.Y.; Sturm, G.P. Jr.; Thomson, J.S.; Vogh, J.W.; Vrana, R.P.; Yu, S.K.T.; Diehl, B.H.; Grizzle, P.L.; Hirsch, D.E; Hornung, K.W.; Tang, S.Y.

1989-12-01

On March 6, 1980, the US Department of Energy (DOE) and the Ministry of Energy and Mines of Venezuela (MEMV) entered into a joint agreement which included analysis of heavy crude oils from the Venezuelan Orinoco oil belt.The purpose of this report is to present compositional data and describe new analytical methods obtained from work on the Cerro Negro Orinoco belt crude oil since 1980. Most of the chapters focus on the methods rather than the resulting data on Cerro Negro oil, and results from other oils obtained during the verification of the method are included. In addition, published work on analysis of heavy oils, tar sand bitumens, and like materials is reviewed, and the overall state of the art in analytical methodology for heavy fossil liquids is assessed. The various phases of the work included: distillation and determination of routine'' physical/chemical properties (Chapter 1); preliminary separation of >200{degree}C distillates and the residue into acid, base, neutral, saturated hydrocarbon and neutral-aromatic concentrates (Chapter 2); further separation of acid, base, and neutral concentrates into subtypes (Chapters 3-5); and determination of the distribution of metal-containing compounds in all fractions (Chapter 6).

Impact of Santiago de Chile urban atmospheric pollution on anthropogenic trace elements enrichment in snow precipitation at Cerro Colorado, Central Andes

Science.gov (United States)

Cereceda-Balic, F.; Palomo-Marín, M. R.; Bernalte, E.; Vidal, V.; Christie, J.; Fadic, X.; Guevara, J. L.; Miro, C.; Pinilla Gil, E.

2012-02-01

Seasonal snow precipitation in the Andes mountain range is evaluated as an environmental indicator of the composition of atmospheric emissions in Santiago de Chile metropolitan area, by measuring a set of representative trace elements in snow samples by ICP-MS. Three late winter sampling campaigns (2003, 2008 and 2009) were conducted in three sampling areas around Cerro Colorado, a Central Andes mountain range sector NE of Santiago (36 km). Nevados de Chillán, a sector in The Andes located about 500 km south from the metropolitan area, was selected as a reference area. The experimental results at Cerro Colorado and Nevados de Chillán were compared with previously published data of fresh snow from remote and urban background sites. High snow concentrations of a range of anthropogenic marker elements were found at Cerro Colorado, probably derived from Santiago urban aerosol transport and deposition combined with the effect of mining and smelting activities in the area, whereas Nevados de Chillán levels roughly correspond to urban background areas. Enhanced concentrations in surface snow respect to deeper samples are discussed. Significant differences found between the 2003, 2008 and 2009 anthropogenic source markers profiles at Cerro Colorado sampling points were correlated with changes in emission sources at the city. The preliminary results obtained in this study, the first of this kind in the southern hemisphere, show promising use of snow precipitation in the Central Andes as a suitable matrix for receptor model studies aimed at identifying and quantifying pollution sources in Santiago de Chile.

Fire Management Lessons Learned From the Cerro Grande (Los Alamos) Fire and Actions Needed to Reduce Fire Risks

National Research Council Canada - National Science Library

Hill, Barry

2000-01-01

We are here today to discuss two related issues, lessons learned from the recent Cerro Grande fire, and, on a broader note, actions needed to mitigate current hazardous forest conditions in the interior West...

Mexican geothermal development and the future

International Nuclear Information System (INIS)

Serrano, J.M.E.V.

1998-01-01

Geothermics in Mexico started in 1954, by drilling the first geothermal well in Pathe, State of Hidalgo, which reached a depth of 237 meters. In 1959 electrical generation from geothermal origin began, with an installed capacity of 3.5 MW. From 1959 to 1994 Mexico increased its installed capacity to 753 MW, by developing three geothermal fields: Cerro Prieto, Los Azufres, and Los Humeros. Currently, 177 wells produce steam at a rate of 36 tons per hour (t/h) each. Comision Federal de Electricidad (CFE, Federal Commission of Electricity) has planned to increase the geothermal-electric installed capacity through construction and installation of several projects. Repowering of operating units and development of new geothermal zones will also allow Mexican geothermal growth

Cerro Grande Fire Impact to Water Quality and Stream Flow near Los Alamos National Laboratory: Results of Four Years of Monitoring

Energy Technology Data Exchange (ETDEWEB)

B.M. Gallaher; R.J. Koch

2004-09-15

In May 2000, the Cerro Grande fire burned about 7400 acres of mixed conifer forest on the Los Alamos National Laboratory (LANL), and much of the 10,000 acres of mountainside draining onto LANL was severely burned. The resulting burned landscapes raised concerns of increased storm runoff and transport of contaminants by runoff in the canyons traversing LANL. The first storms after the fire produced runoff peaks that were more than 200 times greater than prefire levels. Total runoff volume for the year 2000 increased 50% over prefire years, despite a decline in total precipitation of 13% below normal and a general decrease in the number of monsoonal thunderstorms. The majority of runoff in 2000 occurred in the canyons at LANL south of Pueblo Canyon (70%), where the highest runoff volume occurred in Water Canyon and the peak discharge occurred in Pajarito Canyon. This report describes the observed effects of the Cerro Grande fire and related environmental impacts to watersheds at and near Los Alamos National Laboratory (LANL) for the first four runoff seasons after the fire, from 2000 through 2003. Spatial and temporal trends in radiological and chemical constituents that were identified as being associated with the Cerro Grande fire and those that were identified as being associated with historic LANL discharges are evaluated with regard to impacts to the Rio Grande and area reservoirs downstream of LANL. The results of environmental sampling performed by LANL, the New Mexico Environment Department (NMED), and U.S. Geological Survey (USGS) after the Cerro Grande fire are included in the evaluation. Effects are described for storm runoff, baseflow, stream sediments, and area regional reservoir sediment.

Photosynthesis within Mars' volcanic craters?: Insights from Cerro Negro Volcano, Nicaragua

Science.gov (United States)

Rogers, K. L.; Hynek, B. M.; McCollom, T. M.

2011-12-01

Discrete locales of sulfate-rich bedrocks exist on Mars and in many cases represent the products of acid-sulfate alteration of martian basalt. In some places, the products have been attributed to hydrothermal processes from local volcanism. In order to evaluate the habitability of such an environment, we are investigating the geochemical and biological composition of active fumaroles at Cerro Negro Volcano, Nicaragua, where fresh basaltic cinders similar in composition to martian basalts are altered by acidic, sulfur-bearing gases. Temperatures at active fumaroles can reach as high as 400°C and the pH of the steam ranges from Cyanobacteria and Ktedonobacteria, however Actinobacteria, alpha-Proteobacteria and Acidobacteria were also identified. Many of the cyanobacterial sequences were similar to those of the eukaryotic Cyanidiales, red algae that inhabit acidic, geothermal environments. Many of sequences related to Ktedonobacteria and Actinobacteria have also been found in acid mine drainage environments. The Archaeal community was far less diverse, with sequences matching those of unclassified Desulfurococcales and unclassified Thermoprotei. These sequences were more distant from isolated species than the bacterial sequences. Similar bacterial and archaeal communities have been found in hot spring environments in Yellowstone National Park, Greenland, Iceland, New Zealand and Costa Rica. Some of Mars' volcanoes were active for billions of years and by analogy to Cerro Negro, may have hosted photosynthetic organisms that could have been preserved in alteration mineral assemblages. Even on a generally cold and dry Mars, volcanic craters likely provided long-lived warm and wet conditions and should be a key target for future exploration assessing habitability.

El recorrido al Cerro Gordo y el ritual tepehuano de las ofrendas en los cerros de la comunidad de San Bernardino de Milpillas

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Chantal CRAMAUSSEL

2014-01-01

Full Text Available El ritual de las ofrendas es una ceremonia propiciatoria de la lluvia que se efectúa al terminar la estación seca en los cerros más altos de la comunidad de San Bernardino de Milpillas Chico, en la Sierra Tepehuana del estado de Durango. A esos rituales distintos de los cató- licos que forman parte del ciclo anual de costumbre concurren las autoridades civiles, los curanderos y miembros del Consejo de ancianos. Es un momento muy importante en el que se refuerza la cohesión de los tepehuanos que tienen un patrón de asentamiento muy disperso, como los demás grupos del norte, pero sus rituales presentan también similitudes con los mesoamericanos.

Petrografía, caracterización geoquímica y análisis microestructural del granito del cerro Siempre Amigos, sierras de Azul, Tandilia

OpenAIRE

Angeletti, Melisa; Frisicale, María Cristina; Dimieri, Luis V

2016-01-01

El cerro Siempre Amigos integra las sierras de Azul, Tandilia, distante 28 km al sur de la ciudad de Azul y 3 km al norte de la megacizalla de Azul, zona de cizalla subvertical donde el basamento se encuentra deformado a milonitas y ultramilonitas. La litología predominante en el cerro Siempre Amigos es un granito paleoproterozoico deformado que en el centro y hacia los bordes se encuentra interdigitado con una roca gnéisica y cuerpos de anfibolitas subverticales de rumbo similar a la foliaci...

ANALYSIS OF MUNICIPAL WASTEWATER AND ACID MINE DRAINAGE PASSIVE CO-TREATMENT AT CERRO RICO DE POTOSÍ, BOLIVIA

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William H.J. Strosnider

2015-06-01

Full Text Available Acid mine drainage (AMD is a worldwide environmental problem. The passive co-treatment of AMD with municipal waste water (MWW is a cost effective approach that uses nutrients in MWW in order to treat high concentrations of metals and sulfate found in AMD. Cerro Rico de Potosí in Bolivia is one of the biggest mining cities in the world, and it is constantly facing problems with AMD. The goal of this study was to determine the reaction rates of Al, Fe, Mn, Zn, and other metals found in an AMD discharge from Cerro Rico by a three-stage reactor system. The AMD had a pH of 3.58 and acidity of 1080 mg/L as CaCO3 equivalent containing 12, 68, 17 and 550 mg/L of dissolved Al, Fe, Mn, and Zn respectively. The reaction rates of Al, Fe, Mn, and Zn were 1.43, 2.09, 0.01, and 0.10 d-1, respectively.

Spanish exiles and the dilemma of the Cold War. Prieto, Esplá, Araquistáin and Llopis | Exiliados españoles en la encrucijada de la Guerra Fría. Prieto, Esplá, Araquistáin y Llopis

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Pedro Luis Angosto Vélez

2003-12-01

Full Text Available Personal attitudes were a determining factor in the position of Spanish Republican exiles regarding the question of restoring democracy in Spain at the beginning of the Cold War. After the Second World War had ended, many exiles came cherish a hope that such a development might be possible with the help of the victorious democracies, particularly the United States and the United Kingdom. They failed, however, to reach agreement as to which tactic to use in order to enlist this help, with some arguing in favour of giving the leading role to the government in exile, while others felt it was preferable to strike an agreement between all Spanish anti-Francoist groups in order to present a united democratic front to the new international institutions which had emerged in the post-war climate. The subtleties of both positions may be examined through a study of influential figures such as Indalecio Prieto, Carlos Esplá, Rodolfo Llopis and Luis Araquistán, of whom we now have a greater knowledge thanks to recent biographies, which form the basis of this work. | Las actitudes personales es un factor determinante de la posición del exilio republicano español ante el problema de la restauración de la democracia en España en la coyuntura del inicio de la Guerra Fría. Finalizada la Segunda Guerra Mundial, en los medios del exilio se generalizó la esperanza de que tal cosa era posible gracias a la ayuda de las democracias vencedoras, en particular de Estados Unidos y el Reino Unido. Sin embargo, no hubo unanimidad sobre la táctica a seguir para recabar esa ayuda, pues mientras unos abogaron por conceder el máximo protagonismo al gobierno en el exilio, otros consideraron más oportuno establecer un acuerdo entre las fuerzas antifranquistas españolas para presentar un frente democrático unido ante las nuevas instituciones internacionales surgidas del conflicto mundial. Ambas posturas presentan matices que pueden ser examinados a partir del talante

LA ARQUITECTURA DE TIERRA Y LAS OCUPACIONES HUMANAS EN EL SITIO ARQUEOLÓGICO CERRO PUÑAY, CANTÓN CHUNCHI, PROVINCIA DE CHIMBORAZO, ECUADOR (Earth Architecture and Human Occupations at Cerro Puñay Archaeological Site, Chunchi Canton, Chimborazo Province, Ecuador

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Mary Jadán V.

2017-06-01

Full Text Available Este artículo se refiere a la arquitectura de tierra del sitio arqueológico Cerro Puñay, ubicado al sur de la provincia de Chimborazo. Algunos perfiles estratigráficos de diferentes partes del cerro demuestran que existen cambios relacionados con la estructura del sitio: un reforzamiento de talud en la cima central, arqueosedimentos en ciertos sectores, nivelación de las cimas, construcción de terrazas, entre otras modificaciones. Aunque hay evidencias de ocupación desde el Formativo Tardío con la cultura narrío (2000-1600 a. C., las edificaciones se iniciaron con la sociedad cañari (500-1460 d. C.. Por otra parte, el sitio evidencia una reconstrucción y utilización por parte de la sociedad inca (1460-1533 d. C.. ENGLISH: This article refers to the land architecture of the Cerro Puñay archaeological site, located to the south of the province of Chimborazo. Some stratigraphic profiles, from different parts of the hill, show that there are changes related to the structure of the site: a reinforcement of slope in the central summit, archaeological sediments in certain sectors, leveling of the tops, and construction of terraces, among other modifications. Although there is evidence of occupation from the Late Formative with the Narrío culture (2000–1600 BC, the construction started with the Cañari society (500–1460 AD. On the other hand, the site shows evidence of a reconstruction and use by the Inca society (1460–1533 AD.

Application of heating in dex in Los Humeros geothermal reservoir; Comportamiento de los indices de calentamiento en el yacimiento geotermico de los Humeros

Energy Technology Data Exchange (ETDEWEB)

Aragon, Alfonso; Arellano, Victor M; Izquierdo, Georgina; Garcia, Alfonso; Barragan, Rosa Maria; Verma, Mahendra P [Instituto de Investigaciones Electricas, Temixco, Morelos (Mexico); Pizano, Arturo [Comision Federal de Electricidad, Los Humeros (Mexico)

2000-12-01

: volumen de perdidas de circulacion, litologia, velocidades de penetracion, etc. Este metodo es usado para identificar las caracteristicas de interes de los intervalos de la formacion en cada pozo tanto para la explotacion como para inyeccion. Como una calibracion previa del metodo se utilizaron datos del pozo Br-2, del campo geotermico de Boadlands en Nueva Zelandia. Posteriormente con datos de los pozos H-11, H-31, y H-33 del campo geotermico de Los Humeros, en Mexico, fue factible determinar el comportamiento de los indices de calentamiento, orientando de esta manera su utilidad a los analisis del yacimiento.

Description of a New Galapagos Giant Tortoise Species (Chelonoidis; Testudines: Testudinidae from Cerro Fatal on Santa Cruz Island.

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Nikos Poulakakis

Full Text Available The taxonomy of giant Galapagos tortoises (Chelonoidis spp. is currently based primarily on morphological characters and island of origin. Over the last decade, compelling genetic evidence has accumulated for multiple independent evolutionary lineages, spurring the need for taxonomic revision. On the island of Santa Cruz there is currently a single named species, C. porteri. Recent genetic and morphological studies have shown that, within this taxon, there are two evolutionarily and spatially distinct lineages on the western and eastern sectors of the island, known as the Reserva and Cerro Fatal populations, respectively. Analyses of DNA from natural populations and museum specimens, including the type specimen for C. porteri, confirm the genetic distinctiveness of these two lineages and support elevation of the Cerro Fatal tortoises to the rank of species. In this paper, we identify DNA characters that define this new species, and infer evolutionary relationships relative to other species of Galapagos tortoises.

Status of geothermal resources in Mexico

International Nuclear Information System (INIS)

Le-Bert, G.

1990-01-01

Except for some isolated instances with tourist or therapeutic objectives and some attempts in the Cerro Prieto geothermal field, there are no projects for direct heat utilization of geothermal resources in Mexico. Therefore, all places that are studied are studied with geothermal-electric objectives. It is convenient to keep in mind that in Mexico, by law, the Comision Federal de Electricidad (CFE) is the public utility in charge of electrical energy service. This institution is directly responsible for the exploration, development and commercial use of geothermal energy for electrical generation. Therefore, this paper includes the present and planned exploration and utilization of geothermal resources only for electricity generation for the period 1985 to the present. Likewise, starting 5 years ago, the CFE efforts have been directed toward the development of high enthalpy fields

Uranium prospecting in Cerro Partido Region-Encruzilhada do Sul Basin-RS, Brazil

International Nuclear Information System (INIS)

Fraenkel, M.O.

1974-01-01

The Cerro Partido residual basin is a shallow (85 meters) and small (25km 2 ) sedimentary basin, a remainder of the erosive cicle, enclosed in the pre-cambrian granitic rocks of the Rio Grande do Sul Shield. Grades of 0.2 + U 3 O 8 were found in its upper-paleozoic sandstones and shales drilles for uranium. The small size and thicknesses of these concentrations prevent their economic mining. However, the different levels of the shield exposed by tectonics, the intrusive granitic, riolitic and syenitic rocks, the anomalous uranium contents in sedimentary and crystalline rocks recommend further investigations on the shield area

Consideration of the ultramafic intrusive rocks in Arroyo Las Palmas (ex Cerro Chato - Las Canias) Durazno. R. O. del Uruguay

International Nuclear Information System (INIS)

Coronel, N.

1987-01-01

This work is about the ultramafic rocks which its chemistry composition fluctuate since the basic to the ultra basic field and appear in the nascent of the Las Palmas stream near Las Canias and Cerro Chato district.

Synthesis of the works of geophysical (electrical soundings) carried out in the region of the anomalies of Yerba Sola (Cerro Largo) Uruguay

International Nuclear Information System (INIS)

Perrin, J.

1983-01-01

In this report has been studied geographical localization, geology, geophysics prospection, equipment and methods used and their results in Yerba Sola anomalies Province Cerro Largo and Fraile Muerto formation

Importaciones áticas del siglo V a.C. del Cerro del Prado (Algeciras, Cádiz

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Cabrera, Paloma

1996-12-01

Full Text Available In this paper we analyze a group of Attic imports, found in the excavations of Cerro del Prado, a settlement situated in the Bahía de Algeciras (Cádiz. The great interest of this group lies in the fact that it belongs to a particular chronological period, the last third of the 5th century B.C., as we have not found later imports, and in the almost exclusive presence of black glazed vases, which gives US an idea of a very definitive demand of the punic society of the Iberian Peninsula regarding the trade of greek goods.

Presentamos en este trabajo un conjunto de importaciones áticas halladas en las excavaciones del Cerro del Prado, situado en la bahía de Algeciras (Cádiz. El interés de este conjunto reside en su pertenencia a un momento cronológico muy concreto: el último tercio del siglo V a.C., no habiéndose hallado importaciones más modernas y en la presencia absoluta de vasos de barniz negro, lo que nos habla de una demanda muy determinada de la sociedad púnica peninsular frente al comercio de productos griegos.

Evaluation of the Cerro Solo nuclear ore, province of Chubut. Geological characteristics of the deposit and of the basin. Pt. 2

International Nuclear Information System (INIS)

Benitez, A.F.; Fuente, A.; Maloberti, A.; Landi, V.A.; Bianchi, R.E.; Marveggio de Bianchi, N.; Gayone, M.R.

1993-01-01

The Cerro Solo uranium ore deposit, is located 420 km west from Trelew city, Chubut province, in the extra-andean. The geologic environment belongs to the northwest edge portion of the intracratonic San Jorge Gulf Basin. The uraniferous district is named Pichinanes Ridge district. The mineralization lies 25 to 130 m depth, and is hosted by Los Adobes formation aged Aptian-Albian, made up by conglomerates, sandstones, coarse-sandstones and less abundant siltstones and claystones. The Cerro Solo ore deposit that belongs to the sandstone type-uranium occurrences are lenticular or tabular shaped, associated with organic material and pyrite, generally roughly parallel to the bedding (Trend-Type). The uranium minerals are uraninite and coffinite associated with organic material and pyrite, and frequently hematite, goethite, calcite, siderite and barite are observed. (Author)

Drilling of bilateral wells: analysis and selection of wells in the Los Humeros, Pue., geothermal field; Perforacion de pozos bilaterales: analisis y seleccion de pozos en el campo geotermico de Los Humeros, Pue.

Energy Technology Data Exchange (ETDEWEB)

Flores Armenta, Magaly del Carmen; Ramirez Montes, Miguel [Comision Federal de Electricidad, Gerencia de Proyectos Geotermoelectricos, Morelia, Michoacan (Mexico)]. E-mail: miguel.ramirez02@cfe.gob.mx

2010-01-15

Drilling bilateral geothermal wells has been conducted successfully in fields in the U.S., the Philippines and Japan, among other places. The reason for drilling a second leg in a well is to increase production by penetrating additional production zones. In this report, criteria are presented for selecting wells in Los Humeros, Pue., geothermal field to be considered for a second leg, taking into account the mechanical condition of the wells, geological targets, distances between wells, production characteristics and thermodynamic conditions. The cases of wells H-3, H-8, H-11, H-16, H-33, H-34 and H-36, which have low production, were reviewed. Wells H-3, H-8 and H-34 were selected as the best subjects for bi-directional drilling. A design is proposed for constructing a second leg in well H-8. [Spanish] La perforacion de pozos bilaterales se ha venido realizando de manera exitosa en campos geotermicos de Estados Unidos, Filipinas y Japon, entre otros. El objetivo de perforar una segunda pierna en un mismo pozo es incrementar su produccion, ya que habran mas zonas de produccion. En este reporte se presentan los criterios para la seleccion de pozos del campo geotermico de Los Humeros, Pue., candidatos para una segunda pierna, considerando el estado mecanico de los mismos, los objetivos geologicos, la distancia entre pozos, sus caracteristicas de produccion y sus condiciones termodinamicas. Para ello se revisaron los casos de los pozos H-3, H-8, H-11, H-16, H-33, H-34 y H-36, que presentan una produccion baja. Posteriormente, aplicando los criterios de evaluacion y con la informacion obtenida de cada pozo, se seleccionaron los pozos H-3, H-8 y H-34 como los que presentan mejores condiciones para la perforacion bidireccional. Finalmente, se establecio un diseno para la construccion de una segunda pierna en el pozo H-8.

Analysis of inflow in geothermal wells to determine their maximum flow; Analisis del influjo en pozos geotermicos para la determinacion de sus flujos maximos

Energy Technology Data Exchange (ETDEWEB)

Aragon-Aguilar, Alfonso; Izquierdo-Montalvo, Georgina; Pal-Verma, Mahendra; Santoyo-Gutierrez, Socrates [Instituto de Investigaciones Electricas (Mexico); Moya-Acosta, Sara L [Centro Nacional de Investigacion y Desarrollo Tecnologico (Mexico)

2009-01-15

Inflow performance relationships developed for petroleum and geothermal reservoirs are presented. Four of them were selected to be used in this work. Such relationships were developed considering features of a typical geothermal system. The performance of the selected relationships was assessed using data from production tests in several wells of different fields. A methodology is presented to determine the value of the maximum flow (W{sub max}) from the inflow relationships; its application is demonstrated using the data of the 10 production tests. It was found that the calculated value of W{sub max} under stabilization conditions may be related to the reservoir response. In general, there is a good agreement between the calculated values of W{sub max} from the different methods. The differences in the W{sub max} values vary within 10%. It was found that the stability in the calculated values of W{sub max} as a response of the reservoir is a function of the flow magnitude. So, the wells with flow greater than 200 t/h reach the stability of W{sub max} at openings 50% less of their total capacity. [Spanish] Se presentan las relaciones del comportamiento de influjo desarrolladas para yacimientos petroleros y geotermicos. Se seleccionaron cuatro de ellas para usar en este trabajo. Tales relaciones fueron desarrolladas considerando condiciones de un sistema geotermico tipico. Se analizo el comportamiento de las relaciones escogidas utilizando datos de pruebas de produccion de varios pozos de diferentes campos. Se presenta una metodologia para determinar el valor del flujo maximo (W{sub max}) a partir de las relaciones de influjo; se demuestra su aplicabilidad usando los datos de diez pruebas de produccion. Se encontro que el valor de W{sub max} calculado bajo condiciones de estabilizacion se puede relacionar con la respuesta del yacimiento. En general se encuentra buena concordancia entre los valores calculados de W{sub max} usando los diferentes metodos. Las

A reverse method to estimate initial temperatures in geothermal reservoirs; Un metodo inverso para estimacion de la temperatura inicial de yacimientos geotermicos

Energy Technology Data Exchange (ETDEWEB)

Garcia Gutierrez, Alfonso [Instituto de Investigaciones Electricas, Gerencia de Geotermia, Cuernavaca, Morelos (Mexico)]. E-mail: aggarcia@iie.org.mx; Ramos Alcantara, Jose R. [Centro Nacional de Investigacion y Desarrollo Tecnologico, Departamento de Ingenieria Mecanica, Cuernavaca, Morelos (Mexico); Arellano Gomez, Victor M. [Instituto de Investigaciones Electricas, Gerencia de Geotermia, Cuernavaca, Morelos (Mexico)

2010-01-15

A method is presented for estimating the initial temperature in geothermal-reservoir formations. The method is based on control theory where the measured temperatures or temperature logs are compared with corresponding simulated temperatures for different times with the well closed. The comparison is made using a control algorithm that makes changes to the originally assumed reservoir temperatures and performs iterations until the best fit between the temperature logs and the simulated temperatures is obtained. The simulation of fluid transport and heat in the well includes the processes of circulation and stop in the presence of circulation losses, modeled on macroscopic balances of momentum and energy. The transport processes in the formation regard the reservoir as an isotropic porous medium and fluid flow is described by Darcy's law. This model generates the fields of temperatures, pressures and speeds as a function of time and space. The method was tested with data from well LV-3 in Las Tres Virgenes geothermal field, Baja California Sur, Mexico. The estimated temperatures of the undisturbed formation-or initial temperatures-are compared within {+-}15 degrees Celsius with the measured temperatures, which is an acceptable outcome from an engineering point of view. [Spanish] Se presenta un metodo para la estimacion de la temperatura inicial en las formaciones de yacimientos geotermicos. El metodo se basa en la teoria de control donde las temperaturas medidas o registros de temperatura se comparan con las correspondientes temperaturas simuladas a diferentes tiempos con el pozo cerrado. La comparacion se hace usando un algoritmo de control el cual hace cambios a las temperaturas de yacimiento originalmente supuestas y realiza iteraciones hasta que se obtiene el mejor ajuste entre los registros de temperatura y las temperaturas simuladas. La simulacion del transporte de fluidos y calor en el pozo incluye los procesos de circulacion y paro en presencia de

Experimental and petrological constraints on long-term magma dynamics and post-climactic eruptions at the Cerro Galán caldera system, NW Argentina

Science.gov (United States)

Grocke, Stephanie B.; Andrews, Benjamin J.; de Silva, Shanaka L.

2017-11-01

Cerro Galán in NW Argentina records > 3.5 Myr of magmatic evolution of a major resurgent caldera complex. Beginning at 5.72 Ma, nine rhyodacitic ignimbrites (68-71 wt% SiO2) with a combined minimum volume of > 1200 km3 (Dense Rock Equivalent; DRE) have been erupted. The youngest of those ignimbrites is the eponymous, geochemically homogenous, caldera-forming 2.08 ± 0.02 Ma Cerro Galán Ignimbrite (CGI; > 630 km3 DRE). Following this climactic supereruption, structural and magmatic resurgence led to the formation of a resurgent dome and post-climactic lava domes and their associated pyroclastic deposits. A clear transition from amphibole to sanidine-bearing magmas occurred during the evolution of Cerro Galán and is inferred to represent a shallowing of the magma system. We test this hypothesis here using experimental phase equilibria. We conducted a series of phase equilibria experiments on the post-climactic dome lithologies under H2O-saturated conditions using cold seal Waspaloy pressure vessels with an intrinsic log fO2 of NNO + 1 ± 0.5 across a temperature-pressure range of 750-900 °C and 50-200 MPa (PH2O = Ptotal), respectively. Petrologic and geochemical analysis of the post-climactic lithologies shows that the natural phase assemblage (plagioclase + quartz + biotite + sanidine + Fe-Ti oxides ± apatite ± zircon) is stable at history of Cerro Galán is informed through a detailed investigation of the textural differences among the post-climactic dome lithologies, and a comparison of those textures with previously published decompression experiments. These suggest that the highly vesiculated, pumiceous clasts with rare microlites represent magma stored within the core of the lava dome that decompressed relatively rapidly (0.003-0.0003 MPa s-1) and evolved via closed system degassing. Resulting over-pressure of the dome may have triggered superficial explosion. In contrast, dense clasts with abundant crystalline silica precipitates represent more typical

ESTUDIO PRELIMINAR DE LA FAUNA AMPHIBIA EN EL CERRO MURRUCUCÚ, PARQUE NATURAL NACIONAL PARAMILLO Y ZONA AMORTIGUADORA, TIERRALTA, CÓRDOBA, COLOMBIA

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ROMERO-MARTÍNEZ HERÓN JOSÉ

2008-07-01

Full Text Available Con el objetivo de estudiar la fauna anfibia en el Cerro Murrucucú (PNN Paramillo,Tierralta, Córdoba, se realizaron muestreos durante los meses de diciembre de2004, enero y febrero de 2005 en diferentes localidades; se utilizaron dos estrategiasde muestreo (búsqueda libre por inspección visual y trampas de caída. En primerainstancia se comparó la riqueza y la abundancia de las especies en tres zonasaltitudinales en uno de los sectores mejor conservados del Cerro. Se encontró queen la parte baja y media predominan las especies de la familia Hylidae, mientras queen la parte alta predominan representantes de la familia Brachycephalidae, en sumayoría especies del género Eleutherodactylus. Se registran 52 especies para el CerroMurrucucú, que representan el 8% del total de especies en Colombia y más del 80% delas documentadas para el Departamento de Córdoba; las cuales están agrupadas en dosórdenes, 10 familias y 26 géneros. Las familias más representativas, Brachycephalidaee Hylidae, concentran un poco más del 50% de las especies. También se registraronpor primera vez 18 especies para el Departamento de Córdoba y se amplia el rangode distribución geográfico de 18 especies y altitudinal de siete de estas. Se tiene elprimer registro de Eleutherodactylus cruentus para Colombia y el primero de E. viejaspara la Cordillera Occidental Colombiana

Paracas Cultural Readaptation To The Nasca Entity: An Approach From The Settlement Of Cerro Cordova

OpenAIRE

Llanos Jacinto, Oscar Daniel

2017-01-01

Except rare exceptions, the Paracas society of the Ica valley has been extensively studied from decontextualized materials, including pottery collected from clandestine tomb excavations in the Ocucaje basin. From the stylistic analysis of these pieces, which also included Nasca specimens, the hypothesis was elaborated that assumed the birth from the Paracas, expressed in the well-known axiom «transition paracas-nasca». The works carried out in Cerro Córdova and those that since 2009 are carri...

Works carried out in the south of Cerro Largo district. Uranium prospection programme. Preliminary report

International Nuclear Information System (INIS)

Goso, H.

1978-01-01

During the carried out work of radimetric preliminary Investigation in the northeast of the uraniferous country were detected radimetric anonalias which are associated to the formation San Gregorio and Tres Islas. Later the works of prospection ratified those anomalies to which they defined in the environs other anomalies. The studies of revision of these conducted anomalies they took to conclude the necessity to carry out a detailed study of the area to that district was denominated Cerro Largo Sur

The rules of urban planning and administrative responsibilities in protecting to the vulnerability and risk of Cerro Tapezco in Santa Ana

International Nuclear Information System (INIS)

Castro Leiton, Karina

2014-01-01

An analysis of regulation is made of land use and administrative management of the Cerro Tapezco to show that as the years have passed it has been verified that the Costa Rican law on town planning has been inadequate for current problems due to lack of updating of various scientific and technical sources also dispersion and proliferation of competences of administrative authorities. The physical setting and planning rules is identified for CerroTapezco and surrounding towns. Local actions are explored in the elaboration of improvement and reform of the regulatory plan of Santa Ana. The administrative entities and institutions with competence in the development and implementation of plans have been identified, assessing deficiencies, inconsistencies and administrative omissions in urban planning of the city of Santa Ana and recommending changes necessary for the proper application of the Costa Rican law [es

Grado de discapacidad en pacientes hemipléjicos del "Policlínico Docente Universitario del Cerro" Evaluation of disability in hemiplegic patients from Cerro university teaching polyclinic

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Abel Estévez Perera

2012-12-01

Full Text Available Introducción: la hemiplejía como consecuencia de un ictus constituye una importante causa de discapacidad. La continuidad y calidad en el proceso rehabilitador supone mejores perspectivas en el pronóstico de los pacientes. Objetivo: evaluar el grado de discapacidad en los pacientes hemipléjicos del área de salud del Policlínico Docente Universitario del Cerro. Métodos: estudio descriptivo, transversal en los pacientes que acudieron consecutivamente al área de rehabilitación del citado policlínico, desde septiembre de 2009 hasta julio de 2011. La muestra estuvo constituida por 124 hemipléjicos por enfermedad cerebrovascular mayores de 15 años, los cuales fueron evaluados con la Escala de Discapacidad de Rosetón. Se excluyeron los enfermos con afasia sensorial o mixta y aquellos que se negaron a participar. Resultados: en 84 (67,8 % pacientes se encontró independencia para la orientación y predominó la semidependencia para el desplazamiento y las necesidades físicas. Para la higiene personal, 48 (38,7 % pacientes resultaron ser dependientes. La falta de motivación para ocupar el tiempo libre se encontró en 92 (74,2 % pacientes, casi siempre por dificultades en la convivencia y en las relaciones familiares. Conclusiones: el grado de discapacidad de los pacientes hemipléjicos evaluados viene dado por la semidependencia en el desplazamiento y las necesidades físicas y la dependencia para el autocuidado. Las dificultades en la convivencia y las relaciones familiares interfieren en la motivación del paciente para ocupar el tiempo libre.Introduction: hemiplegia is an important cause of disability as a result of a stroke. The persistence and quality of the rehabilitative process lead to better results in the patient prognosis. Objective: to evaluate the extent of disability in hemiplegic patients from the health area under "Cerro" university teaching polyclinics. Methods: a cross-sectional and descriptive study was conducted in

Cerro Amarillo rhyolites, advanced AFC in the northern SVZ, Chile

International Nuclear Information System (INIS)

Godoy, E; Hildreth, W

2001-01-01

Cerro Amarillo is a Quaternary medium size (500m high, 2 km 2 ) rhyolite dome complex located close to the Chile-Argentina border, reaching a height of 4162 m, between the headwaters of the Rio Colina and the Nieves Negras Pass. It overlies a broad anticline of thick Middle Jurassic pelites (Alvarez et al., 1997). Thiele (1980) includes this complex in his 'Unidad Volcanica Antigua', a Pleistocene composite map unit made up of andesites and trachyandesites. Ramos et al. (1997), while recognizing its rhyolitic character, assigned a Tertiary age to the lava domes, most likely based on the late Pliocene age of silicic dikes outcropping eastward, in Argentina. Both the lack of younger overlying units and freshness of its components, together with preservation of the unconsolidated, easily eroded pyroclastic deposits at its base, suggest, however, that it is not older than Pleistocene (au)

Trace Element Geochemistry of Silica Phases: Understanding the Evolution of the Cerro Pabellón Geothermal System

Science.gov (United States)

Alvear, B.; Morata, D.; Leisen, M.; Reich, M.; Barra, F.

2017-12-01

The study of mineral textures coupled with trace element geochemistry has proven to be a useful tool to understand the evolution of geological environments. The purpose of this study is to provide new constrains on the formation of an active geothermal system, specifically the Cerro Pabellón field. The Cerro Pabellón system is located at 4500 m above sea level and is the first geothermal power plant in operation in Chile and South America. Thirteen samples were collected from a 550 m long drill core. Samples were first studied under petrographic microscopy followed by scanning electron microscopy coupled with a cathodoluminescence detector (CL-SEM). The different textures recognized using petrography and the CL-SEM technique were later analyzed by Laser Ablation Inductively Coupled Plasma Mass Spectrometry (LA-ICP-MS) in order to determine variations in the trace element concentrations as a function of silica textures. Two vein types (A and B) with different silica polymorphs were identified by CL-SEM. Vein type A has only a colloform texture, whereas vein type B, younger and crosscutting the type A, shows zonation, colloform, and jigsaw textures. LA-ICPMS results show high concentrations of Li, Al, Na, K, As, and Sb for all types of silica. A comparison between vein type A and B, show that vein type A is Al-Na-K-Li poor (2088, 36, 309, and 122 ppm average, respectively) and As-Sb rich (43 and 249 ppm average, respectively). On the other hand, vein type B has variable concentrations of Al-Na-K-Li-Sb, but usually higher than in vein type A. Overall, the Cerro Pabellón geothermal system shows high concentrations of Li and Sb, reaching up to 360 and 703 ppm, respectively. Our preliminary results show that the trace element geochemistry is strongly related to the different silica textures, which formed as a response to different thermodynamic conditions and fluid-rock ratios. This work is a contribution to the FONDAP-CONICYT 15090013 Project.

GeoSteamNet: A computer code to simulate geothermal steam flow in a pipeline network; GeoSteamNet: Programa de computo para simular el flujo de vapor geotermico de una red de vaporductos

Energy Technology Data Exchange (ETDEWEB)

Verma P., Mahendra; Aragon A., Alfonso [Instituto de Investigaciones Electricas, Cuernavaca, Morelos (Mexico)]. E-mail: mahendra@iie.org.mx; Ruiz L., Alejando; Mendoza C., Alfredo [Comision Federal de Electricidad, Campo Geotermico Los Azufres, Campamento Agua Fria, Michoacan (Mexico)

2011-07-15

transporte del flujo de vapor en una red de vaporductos de un campo geotermico. El movimiento del fluido se rige por los siguientes principios basicos: la conservacion de la masa, el principio de movimiento lineal (segunda ley de Newton o las ecuaciones de Navier Stokes) y la primera y segunda leyes de la termodinamica. La segunda ley de la termodinamica permite definir la direccion de un proceso espontaneo, que esta indirectamente validado en el algoritmo, debido a que el vapor fluye de alta a baja presion y el calor fluye de alta a baja temperatura. Las ecuaciones no lineales se resuelven con el metodo de Newton-Raphson. Utilizando el componente ActiveX OrificeMeter, se realizo el balance de masa para el flujo de vapor en las unidades de generacion U-15 y U-16 del campo geotermico de Los Azufres, Mich., en febrero de 2009. La U-15 fue alimentada por los pozos productores AZ-04, Z-28, Z-30, AZ-65D, y AZ-66, mientras que los pozos AZ-28A, AZ-45, Z-56, Z-67 y AZ- 69D estaban conectados a la U-16. La diferencia entre la cantidad de vapor recibida en las unidades y producida por los pozos respectivos esta dentro de {+-}4%, lo cual es aceptable para fines practicos para el suministro de vapor, tomando en cuenta las incertidumbres en varios parametros tales como la presion, la temperatura, la fluctuacion de la presion en el cabezal del pozo, entre otros. Los resultados de la simulacion de una red hipotetica de vaporductos de un sistema geotermico con dos pozos productores y una planta de generacion de energia electrica ilustran la funcionalidad de GeoSteamNet, mostrando varios puntos importantes a destacar. Para una geometria especifica de las redes de vaporductos solo hay una cierta cantidad de masa (vapor) que puede ser transportado a una presion dada de los pozos y de la planta generadora. La construccion y modificacion de una red de vaporductos son muy costosas y la produccion de pozos geotermicos responde a los factores de su naturaleza, por lo tanto, hay necesidad de

Diameter characterization of timber species in primary forests of Cerro Murrucucu

International Nuclear Information System (INIS)

Villa G, Ana Maria

2006-01-01

This study in Cerro Murrucucu forests establishes the minimum fell diameter (DMC) and its fell cycle (C). It classifies the forest in 1 (Iess damaged) and 2 (severely damaged). Ten species were selected by means of the importance Value Index (IVI) and the DMC was determined. C was estimated through the times of step method. Pentaclethra macroloba showed the highest IVI (21.5% and 21.09% for forests 1 and 2, respectively). In spite of the deterioration of forest 2 the species still showed highest importance. In forest 1 an equilibrium can be deduced, whereas in forest 2 most of the considered species show instability. The DMC for forests 1 and 2 were 30 and 20 cm respectively, indicating extractive activities are deteriorating the latest. C was 51.8 years

Geología de la región del Cerro Guanaquero, Río Diamante, Mendoza

OpenAIRE

Federico Fuentes; Victor A. Ramos

2008-01-01

El estudio realizado presenta nuevos datos sobre un sector poco conocido de la Cordillera Principal de Mendoza, en la alta cuenca del río Diamante en las adyacencias del cerro Guanaquero, y los primeros datos geocronológicos de sus rocas volcánicas. Las unidades geológicas presentes en el área se dividen en cuatro grupos principales: secuencias sedimentarias mesozoicas marinas y continentales intensamente plegadas y falladas; intrusivos y volcanitas intermedias de edad neógena; rocas volcánic...

Age and kinematics of ductile deformation in the Cerro Durazno area, NW Argentina: Significance for orogenic processes operating at the western margin of Gondwana during Ordovician - Silurian times

Science.gov (United States)

Wegmann, Maja I.; Riller, Ulrich; Hongn, Fernando D.; Glodny, Johannes; Oncken, Onno

2008-07-01

The Cerro Durazno Pluton belongs to a suite of Paleozoic granitoid intrusions in NW-Argentina, that are central for understanding the tectonic setting of the western margin of Gondwana in Ordovician and Silurian times. The pluton and its host rocks were tectonically overprinted by metamorphic mineral shape fabrics formed under middle greenschist-facies metamorphic conditions and associated with the nearby Agua Rosada Shear Zone. Kinematic analysis of the shear zone based on the geometric relationship between individual segments of the shear plane and principal axes of mineral fabric ellipsoids indicates reverse-sense of shear with a minor component of left-lateral displacement. This is compatible with the kinematics of other ductile deformation zones in this area, collectively forming a network, which accomplished orogen-parallel extension in addition to vertical thickening. Using the Rb-Sr isotopic system, an undeformed pegmatite dike of the Cerro Durazno Pluton was dated at 455.8 ± 3.6 Ma and mineral fabrics of the Agua Rosada Shear Zone formed at middle greenschist-facies metamorphism gave deformation ages of 437.0 ± 3.8 Ma and ⩽428.4 ± 4.5 Ma. Thus, tectonic overprint at low metamorphic grade occurred about 20-30 Ma after terminal magmatism in the Cerro Durazno area. Our data from the Cerro Durazno area and regional considerations suggest that the western margin of Gondwana was characterized by orogen-parallel extension in addition to crustal thickening as well as episodes of magmatism and ductile deformation that varied greatly in time and space.

Comentarios a las ponencias de Lourenzo Fernández Prieto y Marcela Sabaté Sort

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Ricardo ROBLEDO HERNÁNDEZ

2010-02-01

Full Text Available La ponencia de Lorenzo Fernández Prieto empieza por reivindicar los problemas del presente como punto de partida en la construcción de la historia aconsejando tener en cuenta como referente la crisis del modelo de modernización y el fin de la ideología del progreso. Resulta llamativo que al mismo tiempo, aunque sea de forma marginal, eche una lanza a favor de Fukuyama, tildado habitualmente de ideología conservadora. Pero esto, por decirlo de algún modo, es casi una anécdota puesto que el principal foco de atención es la historia rural como el ámbito más pertinente de historia transnacional. Su ponencia es un alegato más que engrosa la corriente de opinión cada vez más caudalosa en contra de la tesis del fracaso o del excepcionalismo hispánicos. Casi hace treinta años que se está hablando en esta dirección, desde que Martínez Alier y Naredo descartaron que existiera una evolución muy diferente de la agricultura española y que el comportamiento de los grandes labradores o el carácter de las instituciones fueran factores explicativos relevantes en esa supuesta diferenciación.

El sistema de yacimientos de mamíferos miocenos del Cerro de los Batallones, Cuenca de Madrid: estado actual y perspectivas

NARCIS (Netherlands)

Morales, J.; Pozo, M.; Silva, P.G.; Domingo, M.S.; López-Antoñanzas, R.; Álvarez Sierra, A.; Antón, M.; Martín Escorza, C.; Quiralte, V.; Salesa, M.J.; Sánchez, I.M.; Azanza, B.; Calvo, J.P.; Carrasco, P.; García-Paredes, I.; Knoll, F.; Hernández Fernández, M.; Hoek Ostende, van den L.W.; Merino, L.; Meulen, van der A.J.; Montoya, P.; Peigné, S.; Peláez-Campomanes, P.; Sánchez-Marco, A.; Turner, A.; Abella, J.; Alcalde, G.M.; Andrés, M.; DeMiguel, D.; Cantalapiedra, J.L.; Fraile, S.; García Yelo, B.A.; Gómez Cano, A.R.; López Guerrero, P.; Oliver Pérez, A.; Siliceo, G.

2008-01-01

The Cerro de los Batallones (Los Batallones Butte) is located in the central-northern area of the Madrid Basin, central Spain. Nine vertebrates localities containing a large variety of mammals of Upper Vallesian Age (Late Miocene) have been found associated with the sediments forming the butte. From

Downwelling Far-Infrared Emission Spectra Measured By First at Cerro Toco, Chile and Table Mountain, California

Science.gov (United States)

Mast, J. C.; Mlynczak, M. G.; Cageao, R.; Kratz, D. P.; Johnson, D. G.; Mlawer, E. J.; Turner, D. D.

2014-12-01

The Far-Infrared Spectroscopy of the Troposphere (FIRST) instrument is a Fourier transform spectrometer developed to measure the important far-infrared spectrum between 100 and 650 cm-1. Presented here are measurements made by FIRST during two successful deployments in a ground-based configuration to measure downwelling longwave radiation at Earth's surface. The initial deployment was to Cerro Toco, Chile, where FIRST operated from August to October, 2009 as part of the Radiative Heating in Underexplored Bands Campaign (RHUBC-II) campaign. After recalibration, FIRST was deployed to the Table Mountain Facility from September through October, 2012. Spectra observed at each location are substantially different, due in large part to the order of magnitude difference in integrated precipitable water vapor (0.3 cm at Table Mountain, 0.03 cm at Cerro Toco). Dry days for both campaigns are chosen for analysis - 09/24/2009 and 10/19/2012. Also available during both deployments are coincident radiosonde temperature and water vapor vertical profiles which are used as inputs a line-by-line radiative transfer program. Comparisons between measured and modeled spectra are presented over the 200 to 800 cm-1 range. An extensive error analysis of both the measured and modeled spectra is presented. In general, the differences between the measured and modeled spectra are within their combined uncertainties.

Evolución de las relaciones nutricionales suelo-planta desarrolladas en suelos de la D. O. "Tierra de León" dedicados al cultivo de Vitis vinífera L. cv. Prieto Picudo

OpenAIRE

Olego Morán, Miguel Ángel

2013-01-01

Se constata la gran influencia e importancia que tiene el pH de los suelos, sobre la biodisponibilidad de los nutrientes minerales presentes en los mismos. Se ha constatado que los nutrientes minerales Mg y Cu de los tejidos vegetales de Vitis vinífera L. cv. Prieto Picudo, aparecen con una interacción antagónica y significativa, lo cual reviste gran importancia, dada la escasez del nutriente Mg en estos suelos, y los continuos tratamientos con base cúprica que actualmente se realizan

A re-appraisal of the stratigraphy and volcanology of the Cerro Galán volcanic system, NW Argentina

Science.gov (United States)

Folkes, Christopher B.; Wright, Heather M.; Cas, Ray A.F.; de Silva, Shanaka L.; Lesti, Chiara; Viramonte, Jose G.

2011-01-01

From detailed fieldwork and biotite 40Ar/39Ar dating correlated with paleomagnetic analyses of lithic clasts, we present a revision of the stratigraphy, areal extent and volume estimates of ignimbrites in the Cerro Galán volcanic complex. We find evidence for nine distinct outflow ignimbrites, including two newly identified ignimbrites in the Toconquis Group (the Pitas and Vega Ignimbrites). Toconquis Group Ignimbrites (~5.60–4.51 Ma biotite ages) have been discovered to the southwest and north of the caldera, increasing their spatial extents from previous estimates. Previously thought to be contemporaneous, we distinguish the Real Grande Ignimbrite (4.68 ± 0.07 Ma biotite age) from the Cueva Negra Ignimbrite (3.77 ± 0.08 Ma biotite age). The form and collapse processes of the Cerro Galán caldera are also reassessed. Based on re-interpretation of the margins of the caldera, we find evidence for a fault-bounded trapdoor collapse hinged along a regional N-S fault on the eastern side of the caldera and accommodated on a N-S fault on the western caldera margin. The collapsed area defines a roughly isosceles trapezoid shape elongated E-W and with maximum dimensions 27 × 16 km. The Cerro Galán Ignimbrite (CGI; 2.08 ± 0.02 Ma sanidine age) outflow sheet extends to 40 km in all directions from the inferred structural margins, with a maximum runout distance of ~80 km to the north of the caldera. New deposit volume estimates confirm an increase in eruptive volume through time, wherein the Toconquis Group Ignimbrites increase in volume from the ~10 km3 Lower Merihuaca Ignimbrite to a maximum of ~390 km3 (Dense Rock Equivalent; DRE) with the Real Grande Ignimbrite. The climactic CGI has a revised volume of ~630 km3 (DRE), approximately two thirds of the commonly quoted value.

La «embajada oficiosa» de Indalecio Prieto en México durante la presidencia de Lázaro Cárdenas, 1939-1940

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Mateos, Abdón

2003-08-01

Full Text Available The author tries to set Indalecio Prieto’s mission in Cárdenas’ Mexico within its political context, emphasizing the background of the relationship between the Spanish republican socialists and the Mexican leftist nationalists and its development from the 1920’s onwards. The present monograph is an account of the JARE’s management and of President L. Cárdenas’ policy towards the Spanish republican refugees until the beginning of Ávila Camacho’s presidency

El autor contextualiza la misión de Indalecio Prieto en el México cardenista, destacando los antecedentes de las relaciones entre los republicanos-socialistas españoles y la izquierda nacionalista mexicana establecidas desde los años veinte. La monografía analiza la gestión de la JARE y la política de Lázaro Cárdenas hacia los refugiados republicanos españoles hasta el comienzo de la presidencia de Manuel Ávila Camacho.

Changing fluvial styles in volcaniclastic successions: A cretaceous example from the Cerro Barcino Formation, Patagonia

Science.gov (United States)

Umazano, A. Martín; Krause, J. Marcelo; Bellosi, Eduardo S.; Perez, Mariano; Visconti, Graciela; Melchor, Ricardo N.

2017-08-01

The Cretaceous Puesto La Paloma (PLPM) and Cerro Castaño (CCM) members (Cerro Barcino Formation, Chubut Group) are pyroclastic-rich, alluvial successions deposited in the Somuncurá-Cañadón Asfalto Basin during sag and endorheic conditions. The PLPM comprises sheet-like tuffaceous sandstone strata, whereas the overlying CCM includes sheet-to ribbon-channel sandstone bodies intercalated within tuffaceous and fine-grained sediments. In this context, the goals of this contribution were: i) to make a detailed documentation of the contrasting sedimentary palaeonvironments; and ii) to infer the allocyclic controls that governed the sedimentation of both units. The study area is located in the western sector of the basin, where six localities, which were studied. Six facies associations were defined including ash-falls, sheet-floods, shallow lakes, aeolian, fluvial channel-belts, and reworked debris-flows. We defined four stratigraphic intervals for the studied sections, denominated 1 to 4 in chronological order of deposition, which increase their thicknesses toward the Puesto Mesa-Cerro León site. The interval 1 (18-42 m thick) corresponds to the PLPM and includes numerous pedogenized sheet-flood deposits, carbonate-rich lacustrine, aeolian sandy facies, and ash-fall beds. The interval 1 is interpreted as an ephemeral and unconfined alluvial system that interacted with aeolian dunes and dry interdune zones. The interval 2 (20-47 m thick) represents the lower part of the CCM. It shows an alternation of fluvial channel-belt deposits and vegetated floodplain facies with sediments originated from sheet-floods, lakes, and few ash-falls and debris-flows. The mean palaeoflow was toward E-SE, except in the northernmost locality where the drainage was towards SW. Proportion of channel-belt bodies ranges from 10 to 36%, reaching higher values in the northern part of the study area, where they are also thicker. The interval 2 represents a permanent, meandering or locally low

ANALISIS DEL CO-TRATAMIENTO PASIVO DE AGUAS RESIDUALES MUNICIPALES Y DRENAJE ACIDO DE MINAS EN CERRO RICO DE POTOSÍ, BOLIVIA

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William H.J. Strosnider

2015-01-01

Full Text Available El drenaje acido de minas (DAM es un problema a nivel mundial. El co-tratamiento pasivo de DAM con aguas residuales municipales (ARM es una manera efectiva y de bajo costo que utiliza los nutrientes de ARM para tratar las concentraciones de metales y sulfato en DAM. Cerro Rico de Potosí, Bolivia es una de las grandes ciudades mineras en el mundo que tiene muchos problemas con el DAM. El objetivo de este estudio fue determinar velocidades de reacción de Al, Fe, Mn, Zn, y otros metales en DAM provenientes de un flujo de agua en Cerro Rico usando un sistema reactor de tres etapas. El DAM tenía un pH de 3.58, acidez de 1080 mg/L equivalente a CaCO3 conteniendo concentraciones de 12, 68, 17, y 550 mg/L de Al, Fe, Mn y Zn respectivamente. Las velocidades de reacción de Al, Fe, Mn y Zn fueron de 1.43, 2.09, 0.01 y 0.10 d-1, respectivamente.

Uranium and Molybdenum extraction from a Cerro Solo deposit ore

International Nuclear Information System (INIS)

Becquart, Elena T.; Arias, Maria J.; Fuente, Juan C. de la; Misischia, Yamila A.; Santa Cruz, Daniel E.; Tomellini, Guido C.

2009-01-01

Cerro Solo, located in Chubut, Argentina, is a sandstone type uranium-molybdenum deposit. Good recovery of both elements can be achieved by acid leaching of the ore but the presence of molybdenum in pregnant liquors is an inconvenient to uranium separation and purification. A two steps process is developed. A selective alkaline leaching of the ore with sodium hydroxide allows separating and recovering of molybdenum and after solid-liquid separation, the ore is acid leached to recover uranium. Several samples averaging 0,2% uranium and 0,1% molybdenum with variable U/Mo ratio have been used and in both steps, leaching and oxidant reagents concentration, temperature and residence time in a stirred tank leaching have been studied. In alkaline leaching molybdenum recoveries greater than 96% are achieved, with 1% uranium extraction. In acid leaching up to 93% of the uranium is extracted and Mo/U ratio in solvent extraction feed is between 0,013 and 0,025. (author)

Stratigraphic and tectonic revision of Cerro Olivo Complex located of Southeastern of Uruguay

International Nuclear Information System (INIS)

Masquelin, E.

2004-01-01

This paper presents a stratigraphic and tectonic revision of Cerro Olivo Complex, located in the Southeastern part of the Uruguayan Predevonian Shield. This informal lithostratigraphic unit constitutes the country rock for the emplacement of late-orogenic granitoids, during Neoproterozoic to Cambrian times. This unit groups all the lithodemes affected by deformation and metamorphism. Recent studies indicate the presence of straight gneisses of quartzo-feldspathic composition in the coast of Maldonado Department. These rocks were interpreted as the result of intense deformation in high temperature. These tectonites base a new stratigraphic insight for the complex. They allow their lithotypes to be organized by petrotectonic features, being a function of PT conditions for every last strain process [es

Volcanic hazard map for Telica, Cerro Negro and El Hoyo volcanoes, Nicaragua

Science.gov (United States)

Asahina, T.; Navarro, M.; Strauch, W.

2007-05-01

A volcano hazard study was conducted for Telica, Cerro Negro and El Hoyo volcanoes, Nicaragua, based on geological and volcanological field investigations, air photo analyses, and numerical eruption simulation. These volcanoes are among the most active volcanoes of the country. This study was realized 2004-2006 through technical cooperation of Japan International Cooperation Agency (JICA) with INETER, upon the request of the Government of Nicaragua. The resulting volcanic hazard map on 1:50,000 scale displays the hazards of lava flow, pyroclastic flows, lahars, tephra fall, volcanic bombs for an area of 1,300 square kilometers. The map and corresponding GIS coverage was handed out to Central, Departmental and Municipal authorities for their use and is included in a National GIS on Georisks developed and maintained by INETER.

High-resolution carbonate isotopic study of the Mural Formation (Cerro Pimas section), Sonora, México: Implications for early Albian oceanic anoxic events

Science.gov (United States)

Madhavaraju, J.; Lee, Yong Il; Scott, R. W.; González-León, C. M.; Jenkyns, H. C.; Saucedo-Samaniego, J. C.; Ramasamy, S.

2018-03-01

The 420-m thick stratigraphic section of the Mural Formation that is exposed in the Cerro Pimas area of northern Sonora, Mexico, is composed of limestone lithofacies ranging from bioclastic wackestone to boundstone, whose biota is characterized by low diversity. Prominent age-diagnostic fossils are benthic foraminifera and long-ranging calcareous algae that indicate the Aptian/Albian boundary is close to the base of the Los Coyotes Member. The carbonates of this formation have negative to positive δ13C values (-4.63 to +2.6‰) and highly depleted δ18O values that range from -12.74 to -8.34‰. The absence of correlation between δ13C and δ18O values supports a primary marine origin for the δ13C values of these limestones. The carbon-isotopic curve of the Cerro Pimas stratigraphic section has well-defined δ13C segments (C8 - C15) that compare with published curves of similar age. In the lower part of the early Albian Los Coyotes Member, the presence of OAE 1b is indicated by an increase followed by a decrease in δ13C values, suggesting correlation with the Kilian Event. The middle part of the Los Coyotes Member has a significant negative carbon-isotope excursion correlated with the globally recognizable early Albian Paquier event. Moreover, another significant negative carbon-isotope shift is observed in the upper part of the Los Coyotes Member, which can be correlated with the Leenhardt Event. The occurrence of the Kilian, Paquier and Leenhardt Events (OAE 1b cluster) in the Cerro Pimas stratigraphy confirms the global nature of these early Albian disturbances of the carbon cycle.

Summary of a Gas Transport Tracer Test in the Deep Cerros Del Rio Basalts, Mesita del Buey, Los Alamos NM.

Energy Technology Data Exchange (ETDEWEB)

Stauffer, Philip H. [Los Alamos National Lab. (LANL), Los Alamos, NM (United States); Rahn, Thomas A. [Los Alamos National Lab. (LANL), Los Alamos, NM (United States); Ortiz, John Philip [Los Alamos National Lab. (LANL), Los Alamos, NM (United States); Salazar, Larry Joseph [Los Alamos National Lab. (LANL), Los Alamos, NM (United States); Boukhalfa, Hakim [Los Alamos National Lab. (LANL), Los Alamos, NM (United States); Snyder, Emily Elisabeth [Los Alamos National Lab. (LANL), Los Alamos, NM (United States)

2018-01-16

Here we describe results from a tracer test in the Cerros del Rio basalt beneath Mesita del Buey, Technical Area 54 (TA-54) at Los Alamos National Laboratory (LANL or the Laboratory). This report follows from plans outlined in our previous Tracer Test Work Plan (LANL 2016). These activities were conducted by LANL to further characterize subsurface properties of the Cerros del Rio basalts at Material Disposal Area (MDA) L (Figure 1.1-1). The work presented follows from the “Interim Measures Work Plan for Soil-Vapor Extraction of Volatile Organic Compounds from Material Disposal Area L, Technical Area 54, Revision 1,” submitted to the New Mexico Environment Department (NMED) in September 2014 (LANL 2014). Remediation of the MDA L vapor plume by soil-vapor extraction (SVE) is recommended as part of the final remedy in the “Corrective Measures Evaluation Report for Material Disposal Area L, Solid Waste Management Unit 54-006, at Technical Area 54, Revision 2” to meet a remedial action objective of preventing groundwater from being impacted above a regulatory standard by the transport of volatile organic compounds (VOCs) to groundwater through soil vapor (LANL 2011).

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.

Pinus Culminicola Andresen y Beaman y sus asociaciones en la ladera sur del cerro La Viga, Coahuila

Directory of Open Access Journals (Sweden)

Rubén Sánchez Silva

1990-01-01

Full Text Available Pinus culminicola was described in 1961 with samples from the Cerro Potosí, State of Nuevo León, Mexico. The species was reported in the Sierras La Marta in 1962, and San Antonio de las Alazanas in 1975, State of Coahuila, indicating that there were not pure associations. In 1979 the species was colected in the Sierra La Viga, Coahuila, at 3 300 m, without data on environmental conditions in which it grows. The distribution of  P. culminicola is restricted to the south slope of the Cerro La Viga. The associations identified and described in this paper are: (1 Scrub of Quercus rugosa – Quercus durifolia – Cercocarpus montanus with elements of P. culminicola; (2 Pinus montezumae–Pseudotsuga macrolepisy with elements of P. culminicola, Quercus spp. and Arbutus xalapensis (3 P. culminicola– Quercus rugosa (both of them as shrubs; (4 P. montezumac–P. macrolepis–Pinus ayacahuite–P. culminicola; (5 pure scrub of P. culminicola; (6 P. culminicola– Dasylirion tezanum (sometimes with Arctostaphylos pungens and Quercus spp., shrublike; (7 Pinus hartwegii–P. culminicola; (8 P. hartwegii with elements of P. macrolepis and P. culminicola; and (9 induced prairie. There are differences in dominance of the species in accordance to the particular characteristics of each place, with presence of herbaceous from high altitudes. The altitude at which these associations occur, varies from 2 900 m to 3 700 m, although isolated elements of P. culminicola–were found at 2 700 m.

Evaluación Integral del Riesgo Volcánico del Cerro Machín, Colombia

OpenAIRE

Leonel Vega Mora; Fernando Javier Diaz

2013-01-01

El volcán Cerro Machín (VCM) se encuentra situado en la Cordillera Central de Colombia. Por la composición química, magnitud y extensión de sus erupciones pasadas se reconoce como un volcán explosivo de gran potencial de daño, cuya actividad futura podría afectar intensamente y durante mucho tiempo (meses hasta años) una región estratégica para la economía del país, que cubre áreas pertenecientes a los departamentos de Tolima, Quindío, Valle del Cauca y Cundinamarca, en las cuales habitan cer...

The Cerro Tololo Inter-American Observatory Summer Student Programs in La Serena, Chile

Science.gov (United States)

Kaleida, Catherine C.; Smith, C.; Van Der Bliek, N. S.; James, D.

2014-01-01

The Cerro Tololo Inter-American Observatory (CTIO) offers positions for U.S. and Chilean student interns during the Chilean summer months of January-March (northern winter semester) at the CTIO offices in La Serena, Chile. CTIO is part of the National Optical Astronomy Observatory (NOAO) of the United States, focused on the development of astronomy in the southern hemisphere. Six undergraduate research assistantships are offered for U.S. physics and astronomy undergraduate students through the NSF-funded Research Experiences for Undergraduates (REU) program. The CTIO-funded Prácticas de Investigación en Astronomía (PIA) program is run concurrently with the REU program, and offers two research assistantships for Chilean undergraduate or 1st or 2nd year masters students, also at the CTIO offices in La Serena, Chile. The CTIO REU and PIA programs provide exceptional opportunities for students considering a career in astronomy to engage in substantive research activities with scientists working at the forefront of contemporary astrophysics. Student participants work on specific research projects in close collaboration with members of the CTIO scientific and technical staff, such as galaxy clusters, gravitational lensing, supernovae, planetary nebulae, stellar populations, star clusters, star formation, variable stars and interstellar medium. The CTIO REU and PIA programs emphasize observational techniques and provide opportunities for direct observational experience using CTIO's state-of-the-art telescopes and instrumentation. The programs run for 10 weeks, from mid-January to the end of March. A two-night observing run on Cerro Tololo and a field trip to another observatory in Chile are included for students of both programs. These positions are full time, and those selected will receive a modest stipend and subsidized housing on the grounds of the offices of CTIO in La Serena, as well as travel costs to and from La Serena. In addition, the students have the

Proyecto de electrificación y alumbrado de la urbanización "Cerro Belmonte" en Madrid

OpenAIRE

García Galiano, Alejandro

2010-01-01

En primer lugar lo que el lector se encontrará será una Memoria Descriptiva donde se explican los elementos constructivos utilizados y diseñados para cumplir con el objetivo de dotar a la Urbanización “Cerro Belmonte” de Madrid de los servicios de Energía Eléctrica y Alumbrado Público. Los servicios de Energía Eléctrica comprenden: • Redes de Media Tensión • Centros de Transformación • Redes de Baja Tensión • Canalizaciones y arquetas Se contempla la definición de e...

Estudio de la líqueno flora encontrada en el Cerro de Quininí, Tibacuy, Cundinamarca

OpenAIRE

Alejandro Parra; Oscar Vivas; Francisco Hormaza

2000-01-01

Se realizó un muestreo de la liquen o flora del cerro de Quininí, Tibacuy, Cundinamarca para estudiar las características morfológicas externas de los géneros de líquenes encontrados en el. A su vez se hizo la revisión bibliográfica acerca de dichos géneros, datando así la riqueza de líquenes en la zona con 8 géneros en total y con respecto al papel de bioindicadores se mostró el grado de intervención para el lugar.

Relación entre la Comunicación y su Eficacia de los Programas Sociales del Ministerio de Desarrollo e Inclusión Social en el Cono Norte Distrito de Cerro Colorado, Arequipa, 2016

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Llanos Mendoza, Daniela Flora

2017-01-01

La presente tesis cuyo enunciado del problema es: Relación entre la comunicación y su eficacia de los programas sociales del Ministerio de Desarrollo e Inclusión Social en el Cono Norte, distrito de Cerro Colorado de Arequipa “2016”; tiene como objetivo: determinar la relación entre la comunicación y su eficacia de los programas sociales del Ministerio de Desarrollo de Inclusión Social en el Cono Norte, Cerro Colorado, Arequipa. Se planteó la siguiente hipótesis para el presente estudio:...

The Spanish Exile Put to the Test: Polemics in the Pres between Indalecio Prieto and the Mexican Alfonso Junco regarding the gold aboard the yacht “Vita”

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Carlos Sola Ayape

2014-04-01

Full Text Available In November, 1946, just a few days before Miguel Alemán took charge as new president of Mexico, the Mexican press –concretely, the newspaper Novedades– would become an ink-and-paper stage for an important dialectic dispute between Alfonso Junco, a Mexican Catholic hispanicist, and Indalecio Prieto, a Spanish Socialist exile and undoubtedly, one of the most important political references of the Second Spanish Republic. Among the many questions left unanswered, there appeared the edges of one of the major issues that haunted the Spanish pilgrimage during its diaspora: the treasures removed before the end of the Civil War. This was so because the legitimation of Franco's regime was also built from the constant pages of accusations towards the “reds” in exile.

The age and thermal history of Cerro Rico de Potosi, Bolivia

Science.gov (United States)

Cunningham, C.G.; Zartman, R.E.; McKee, E.H.; Rye, R.O.; Naeser, C.W.; Sanjines, V.O.; Ericksen, G.E.; Tavera, V.F.

1996-01-01

Cerro Rico de Potosi, Bolivia, is the world's largest silver deposit and has been mined since the sixteenth century for silver, and for tin and zinc during the twentieth century, together with by-product copper and lead. The deposit consists primarily of veins that cut an altered igneous body that we interpret to be a dacitic volcanic dome and its underlying tuff ring and explosion breccia. The deposit is compositionally and thermally zoned, having a core of cassiterite, wolframite, bismuthinite, and arsenopyrite surrounded by a peripheral, lower-temperature mineral assemblage consisting principally of sphalerite, galena, lead sulfosalt, and silver minerals. The low-temperature assemblage also was superim-posed on the high-temperature assemblage in response to cooling of the main hydrothermal system. Both the dacite dome and the ore fluids were derived from a larger magmatic hydrothermal source at depth. The dome was repeatedly fractured by recurrent movement on the fault system that guided its initial emplacement. The dome was extruded at 13.8 ?? 0.2 Ma (2??), based on U-Th-Pb dating of zircon. Mineralization and alteration occurred within about 0.3 my of dome emplacement, as indicated by a 40Ar/39Ar date of 13.76 ?? 0.10 Ma (1??) for sericite from the pervasive quartz-sericite-pyrite alteration associated with the main-stage, high-temperature, mineralization. The last thermal event able to reset zircon fission tracks occurred no later than 12.5 ?? 1.1 Ma (1??). as indicated by fission-tract dating. Minor sericite. and magmatic-steam alunite veins, were episodically formed around 11 Ma and between 8.3 and 5.7 Ma; the younger episodes occurring at the time of extensional fracturing at Cerro Rico and widespread volcanism in the adjacent Los Frailes volcanic field. None of these younger events appear to be signific-ant thermal/mineralizing events: the exceptionally flat thermal release pattern of 39Ar from sericite and the results of the fission-tract dating of

TECNOLOGÍA Y SUBSISTENCIA EN EL SITIO ARQUEOLÓGICO CERRO TAPERA VÁZQUEZ (PARQUE NACIONAL PRE-DELTA, REPÚBLICA ARGENTINA

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Mariano Bonomo

2014-10-01

Full Text Available In this paper the results of the studies carried out on ceramic and bone materials recorded at Cerro Tapera Vázquez site (Argentinean Northeast are presented. Taxonomic, anatomic and taphonomic studies of bone assemblages and technological-decorative analysis and refitting of pottery were undertaken. The site is located on a mound next to El Ceibo Creek, where 16 m2 were excavated in 2008. Abundant smooth, incised and modeled pottery (handles and zoomorphic appendages and numerous bones remains of Myocastor coypus (most frequent taxon, Blastocerus dichotomus, Ozotoceros bezoarticus, Cavia aperea, Leopardus geoffroyi, Lycalopex gymnocercus, Hydrochaeris hydrochaeris, birds and fish (Siluriformes and Characiformes were recorded. Except Cavia aperea rodent and Dusicyon gimnocercus fox, all taxa show evidence of anthropic modification (cut marks, fresh fractures and burning. Two radiocarbon dates were obtained: 650 and 520 yrs. BP. The results reached in this study lead to the conclusion that the pre-Hispanic populations that occupied Cerro Tapera Vázquez by the end of the Late Holocene were riverine canoe peoples, with complex ceramic technology and subsistence based on hunting of coypu, capybara and cervids, fishing and small-scale horticulture.

Tornos de alfarero protohistóricos del Cerro de las Cabezas (Valdepeñas, Ciudad Real = Protohistoric potter’s wheels in the Iberian archaeological site ‘Cerro de las Cabezas’ (Valdepeñas, Ciudad Real

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Domingo Fernández Maroto

2015-11-01

Full Text Available El yacimiento ibérico del “Cerro de las Cabezas” ha proporcionado cuatro piezas líticas que identificamos como pertenecientes a tornos de alfarero. Este oppidum ya ha sido puesto de manifiesto como un centro productor y difusor de cerámica ibérica. A través del análisis e interpretación de estas piezas y de las referencias obtenidas en otros yacimientos de la Península Ibérica y del Próximo Oriente, hemos podido confirmar que dos de estas piezas corresponden a un mismo torno, por lo que podemos considerar esta circunstancia como excepcional, dado que hasta el momento, en la Península Ibérica solo se tienen noticias de hallazgos de piezas descontextualizadas y dispersas. Nos encontramos así, con el primer torno  protohistórico completo adscrito a una cronología en torno al siglo III a.C.The Iberian archaeological site ‘Cerro de las Cabezas’ has provided four stone pieces that we identify as belonging to potter’s wheels. This oppidum has been revealed as a producer and spreading centre of Iberian pottery. Through the analysis and interpretation of these pieces, as well as the references obtained from other sites in the Iberian Peninsula and the Middle East, we are able to confirm that two of these findings correspond to the same potter’s wheel. As a result, we could take into account this fact as an exceptional circumstance, because, so far, we only know about some scattered pieces taken out of context in the Iberian Peninsula. Consequently, we have maybe found the first complete protohistoric slow potter’s wheel dating from around the third century BC.

MOVIMIENTOS DE LADERA Y PLANEAMIENTO URBANÍSTICO: EL CONFLICTO DEL CERRO DEL OPE, ARCHENA (MURCIA

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María Dolores Gómez Moreno

2009-01-01

Full Text Available Los desprendimientos son un proceso natural que afecta, de forma generalizada en el Valle de Ricote, a las laderas del tipo cantil-talud. Su peligrosidad radica en que los bloques desprendidos del escarpe ruedan con facilidad, talud abajo, cuando son descalzados por efecto de la escorrentía superfi cial o desestabilizados por movimientos sísmicos. El planeamiento urbanístico se convierte en factor inductor del riesgo al clasifi car como urbanizables y urbanos suelos que, por su ubicación en pie de ladera, deberían excluirse de cualquier proceso urbanizador. Este es el caso de Archena en el entorno inmediato del cerro del Ope.

Anchoring the landscape: human utilization of the Cerro Gavilán 2 rockshelter, Middle Orinoco, from the Early Holocene to the present

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Kay Scaramelli

Full Text Available Abstract Initial archaeological investigations at Cerro Gavilán 2, a rockshelter located in the Bolívar State of Venezuela, reveal evidence for human activity that spans the Early Holocene to the present. This report summarizes the information obtained through surface collection, limited excavation, and documentation of the surface features and rock art in the cave. Accelerator mass spectrometry (AMS 14C analysis established dates from excavated strata that range between 9250 ± 60 BP to 3440 ± 40 BP, and are associated with a unifacial flake technology and charred faunal and floral remains, whereas surface remains span the known ceramic sequence for the area. Rock art corresponds to distinctive superimposed styles that indicate continual repainting of the cave through time, serving to anchor the site to the landscape for multiple societies inhabiting the region. It is suggested that the shelter may have fulfilled different functions over time and a sequence of seasonal residential, ritual, and funerary activities is proposed. The rich cultural context found in Cerro Gavilán 2 contributes to advances in Amazonian archaeology that are redefining our knowledge of early developments and the complexity of human/environmental interactions in tropical America.

Gestión del agua subterránea en el Barrio Cerro Los Leones de Tandil (Argentina)

OpenAIRE

Rodriguez, Corina Iris; Jacinto, Guillermina; Ruiz de Galarreta, Alejandro; Banda Noriega, Roxana

2010-01-01

En este trabajo se describen y analizan los actores y modos de explotación y uso involucrados en la gestión del recurso hídrico subterráneo en un barrio periférico de Tandil -Cerro Los Leones- (Provincia de Buenos Aires, Argentina), que carece de servicios de agua potable y cloacas. Estudios previos demostraron contaminación química y bacteriológica del agua que pone en riesgo la salud de la población. Se caracterizan los modos de uso y explotación del agua, señalando importantes deficiencias...

Mid amphibolite facies metamorphism of harzburgites in the Neoproterozoic Cerro Mantiqueiras Ophiolite, southernmost Brazil

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HARTMANN LÉO A.

2003-01-01

Full Text Available Valuable information is retrieved from the integrated investigation of the field relationships, microstructure and mineral compositions of harzburgites from the Neoproterozoic Cerro Mantiqueiras Ophiolite. This important tectonic marker of the geological evolution of southernmost Brazilian Shield was thoroughly serpentinized during progressive metamorphism, because the oldest mineral assemblage is: olivine + orthopyroxene + tremolite + chlorite + chromite. This M1 was stabilized in mid amphibolite facies - 550-600ºC as calculated from mineral equilibria. No microstructural (e.g. ductile deformation of olivine or chromite or compositional (e.g. mantle spinel remnant of mantle history was identified. A metamorphic event M2 occurred in the low amphibolite facies along 100 m-wide shear zones, followed by intense serpentinization (M3 and narrow 1-3 m-wide shear zones (M4 containing asbestos.

Burning down the brewery: establishing and evacuating an ancient imperial colony at Cerro Baul, Peru.

Science.gov (United States)

Moseley, Michael E; Nash, Donna J; Williams, Patrick Ryan; DeFrance, Susan D; Miranda, Ana; Ruales, Mario

2005-11-29

Before the Inca reigned, two empires held sway over the central Andes from anno Domini 600 to 1000: the Wari empire to the north ruled much of Peru, and Tiwanaku to the south reigned in Bolivia. Face-to-face contact came when both colonized the Moquegua Valley sierra in southern Peru. The state-sponsored Wari incursion, described here, entailed large-scale agrarian reclamation to sustain the occupation of two hills and the adjacent high mesa of Cerro Baúl. Monumental buildings were erected atop the mesa to serve an embassy-like delegation of nobles and attendant personnel that endured for centuries. Final evacuation of the Baúl enclave was accompanied by elaborate ceremonies with brewing, drinking, feasting, vessel smashing, and building burning.

Paleomagnetism in the Determination of the Emplacement Temperature of Cerro Colorado Tuff Cone, El Pinacate Volcanic Field, Sonora, Mexico.

Science.gov (United States)

Rodriguez Trejo, A.; Alva-Valdivia, L. M.; Vidal Solano, J. R.; Garcia Amador, B.; Gonzalez-Rangel, J. A.

2014-12-01

Cerro Colorado Maar is located at the World Heritage Site, biosphere reserve El Pinacate and Gran Desierto del Altar, at the NNW region of Sonora, Mexico (in El Pinacate Volcanic Field). It is a tuff cone, about 1 km diameter, result of several phreatomagmatic episodes during the late Quaternary. We report paleomagnetic and rock magnetic properties from fusiform volcanic bombs obtained from the borders of Cerro Colorado. This study is based in the thermoremanent magnetization TRM normally acquired by volcanic rocks, which can be used to estimate the emplacement temperature range. We performed the experiments on 20 lithic fragments (10 cm to 20 cm approximately), taking 6-8 paleomagnetic cores from each. Rock magnetic experiments (magnetic susceptibility vs. temperature (k-T), hysteresis curves and FORC analysis, shows that the main magnetic mineral carriers of magnetization are titanomagnetite and titanohematite in different levels of intergrowth. The k-T curves suggest in many cases, only one magnetic phase, but also in other cases a second magnetic phase. Thermal demagnetization was used to demagnetize the specimens in detailed short steps and make a well-defined emplacement temperature determination ranges. We found that temperature emplacement determination range for these two magnetic phases is between 350-450 °C, and 550-580 °C, respectively. These results are consistent with those expected in an eruption of Surtsey type, showing a distinct volcanic activity compared to the other craters from El Pinacate volcanic field.

Parasitosis intestinales en niños ingresados en el Hospital Universitario Pediátrico del Cerro, La Habana, Cuba

OpenAIRE

Núñez, Fidel A.; González, Odalys M.; Bravo, . José R.; Escobedo, Ángel A.; González, Ida

2003-01-01

Se realizó un estudio sobre parasitismo intestinal en 401 niños ingresados en el Hospital Universitario Pediátrico del Cerro entre los meses de mayo y junio de 1999. Para esta finalidad se tomó una muestra representativa, aleatoria y estratificada por servicios. Por cada niño, se recogieron 3 muestras de heces preservadas en formaldehído, las que se procesaron por 3 métodos parasitológicos. La prevalencia de parasitismo intestinal fue de 15 % en el hospital, y no se encontraron diferencias en...

Notas sobre la ecología de Phyllodactylus reissi (Phyllodactylidae: Sauria) en el Parque Nacional Cerros de Amotape (Tumbes, Perú)

OpenAIRE

Jordán Arizmendi, Juan Carlos

2012-01-01

Some basics aspects on the ecology of the nocturnal gecko Phyllodactylus reissi from Parque Nacional Cerros de Amotape (Tumbes, Peru) are described. This species used rock boulders (57,4%) and trees (31,9%) as microhabitats primarily, exhibiting a nocturnal activity pattern, with a peak between 2100-2200 hours, remaining active until midnight. Body temperature (mean 24,4 ºC) was correlated with both air and substrate temperature, with the last variable affecting in higher degree (47%) the bod...

Gas geochemistry of Los Humeros geothermal field, Mexico; Geoquimica de gases del campo geotermico de Los Humeros, Puebla, Mexico

Energy Technology Data Exchange (ETDEWEB)

Barragan R, Rosa Maria; Arellano G, Victor M; Nieva G, David; Portugal M, Enrique; Garcia G, Alfonso; Aragon A, Alfonso [Instituto de Investigaciones Electricas, Temixco, Morelos (Mexico); Torres A, Ignasio S [Centro de Investigacion en Energia, Temixco, Morelos (Mexico); Tovar A, Rigoberto [Comision Federal de Electricidad, Los Humeros, Puebla (Mexico)

1999-12-01

Gas data of Los Humeros geothermal field were analyzed. A new method, which is based on the Fischer-Tropch reactions and on the combined pyrite-magnetite mineral equilibrium, was used. Reservoir temperature and reservoir excess steam were estimated for the starting stage of the field by using early data taken from producing wells at controlled conditions. The same parameters were also obtained for the present stage by using 1997 gas data. Reservoir temperatures ranged from 275 and 337 Celsius degrees and positive values for reservoir excess steam fractions were obtained for the starting stage. For well H-1 no excess steam was found since this well was fed by the shallower liquid-dominated reservoir. Results for 1997 showed lower scattering compared to early data and the possible occurrence of a heating process in the shallower stratum which could due to exploitation. [Spanish] En este articulo se presenta un analisis de datos de la fase gaseosa producida por pozos productores del campo geotermico de Los Humeros mediante un metodo que considera el equilibrio de la reaccion de Fischer-Tropsh y el equilibrio de minerales pirita-hematia y pirita-magnetita. Este metodo provee la temperatura del yacimiento y el exceso de vapor presente en la descarga total de los pozos. Los resultados se discuten tanto para el estado inicial del yacimiento utilizando los primeros datos de produccion en los que el flujo del pozo estuvo controlado y los obtenidos en 1997 que representan el estado actual del yacimiento. En el estado inicial se estimaron temperaturas de yacimiento de entre 275 y 337 grados Celsius y excesos de vapor positivos, con excepcion del pozo H-1 que se alimenta del estrato somero dominado por liquido. Los resultados obtenidos para 1997 muestran una dispersion menor y la probable ocurrencia de un proceso de calentamiento del estrato somero propiciado por la explotacion.

Burn Severities, Fire Intensities, and Impacts to Major Vegetation Types from the Cerro Grande Fire

Energy Technology Data Exchange (ETDEWEB)

Balice, Randy G. [Los Alamos National Lab. (LANL), Los Alamos, NM (United States); Bennett, Kathryn D. [Los Alamos National Lab. (LANL), Los Alamos, NM (United States); Wright, Marjorie A. [Los Alamos National Lab. (LANL), Los Alamos, NM (United States)

2004-12-15

The Cerro Grande Fire resulted in major impacts and changes to the ecosystems that were burned. To partially document these effects, we estimated the acreage of major vegetation types that were burned at selected burn severity levels and fire intensity levels. To accomplish this, we adopted independently developed burn severity and fire intensity maps, in combination with a land cover map developed for habitat management purposes, as a basis for the analysis. To provide a measure of confidence in the acreage estimates, the accuracies of these maps were also assessed. In addition, two other maps of comparable quality were assessed for accuracy: one that was developed for mapping fuel risk and a second map that resulted from a preliminary application of an evolutionary computation software system, called GENIE.

Calidad de adn de personas impactadas por la minería artesanal en el cerro el toro, huamachuco, la libertad 2010

OpenAIRE

Casanova Herrera, Hugo Enrique

2013-01-01

The present research work is to determine the toxic substances and DNA damage for people impacted by artisanal mining of Cerro El Toro, using the comet assay. Knowing that at present the impact of mining is a problem that affects the global environment and to Peru by the. gold mining in people causing health problems that could reach various cancer diseases, caused by a genotoxic effect of the chemicals used in mining affecting chromosomal DNA. Atomic absorption spectroscopy was used as a met...

Dimensión sociopolítica y religiosa de la Capacocha del Cerro Aconcagua

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1996-01-01

Full Text Available DIMENTION SOCIO-POLITIQUE ET RELIGIEUSE DE LA CAPACOCHA DE L'ACONCAGUA. Sur un contrefort de l’Aconcagua un groupe d’andinistes a trouvé une sépulture ayant les caractéristiques d’une capacocha. Dans cet essai nous étudierons et commenterons quelques éléments qui la composent, spécialement des petites figures en métal et mullu avec leurs tenues, en prenant comme référence les informations coloniales et les données de l’archéologie. Parmi les sujets traités nous trouverons : la présence de Huayna Capac au Chili, l’alliance entre Chinchaysuyu et Collasuyu sous la domination inca, les chemins rituels, l’oracle et le maintien du souvenir de l’ancien dieu Con. En un contrafuerte del cerro Aconcagua, un grupo de andinistas encontró un entierro que reúne las condiciones que lo definen como una capacocha. En este ensayo se estudian y comentan algunos de los elementos que la componen -especialmente las figuritas de metal y mullu con sus atuendos- tomando como referencia las noticias coloniales y los datos arqueológicos. Entre los temas tratados tenemos: la presencia de Huayna Capac en Chile la alianza entre Chinchaysuyu y Collasuyu bajo el dominio incaico los caminos rituales el oráculo y la supervivencia del recuerdo del antiguo dios Con. SOCIAL, POLITICAL AND RELIGIOUS DIMENSION OF THE CAPACOCHA OF THE CERRO ACONCAGUA. In a secondary mountain range of the Aconcagua Mt., a group of mountain-climbers found an interment possessing the attributes of a capacocha. In this essay some of the elements composing it namely the small metal and mullu figures with their garments, drawing on colonial documents and archaeological data, are studied and commented upon. Among the subjects considered the following: the presence of Huayna Capac in Chile, the coalition between Chinchaysuyu and Collasuyu under the Inca empire, the ritual roads, the oracle and the survival of the memories of the ancient god Con.

Intense Seismic Activity at Chiles and Cerro Negro Volcanoes on the Colombia-Ecuador Border

Science.gov (United States)

Torres, R. A.; Cadena, O.; Gomez, D.; Ruiz, M. C.; Prejean, S. G.; Lyons, J. J.; White, R. A.

2015-12-01

The region of Chiles and Cerro Negro volcanoes, located on the Colombian-Ecuadorian border, has experienced an ongoing seismic swarm beginning in Aug. 2013. Based on concern for local residents and authorities, a cooperative broadband monitoring network was installed by the Servicio Geológico Colombiano in Colombia and the Instituto Geofísico of the Escuela Politécnica Nacional in Ecuador. Since November 2013 more than 538,000 earthquakes were recorded; although since May 2015 the seismicity has decreased significantly to an average of 70 events per day. Three large earthquake swarms with increasing energy occurred in Aug.-Oct. 2013, March-May 2014, and Sept.-Dec. 2014. By the end of 2014, roughly 400 earthquakes greater than M 3 had occurred with a maximum rate of 8000 earthquakes per day. The largest earthquake was a 5.6 ML on Oct. 20, 2014. This event produced an InSAR coseismic deformation of ~23 cm (S. Ebmeier, personal communication). Most events are typical brittle failure volcano-tectonic (VT) earthquakes that are located in a cluster beneath the southern flank of Chiles volcano, with depths between 1.5 and 10 km. Although the great majority of earthquakes are VT, some low-frequency (LF, ~0.5 Hz) and very-low-frequency (VLF) events have occurred. Particle motion analysis suggests that the VLF source migrated with time. While a VLF on Oct. 15, 2014 was located south of Chiles volcano, near the InSAR source, the VLF registered on Feb. 14, 2015 was likely located very close to Chiles Volcano. We infer that magma intrusion and resulting fluid exsolution at depths greater than 5 km are driving seismicity in the Chiles-Cerro Negro region. However earthquakes are failing in a manner consistent with regional tectonics. Relative relocations reveal a structure consistent with mapped regional faults. Thus seismicity is likely controlled by an interaction of magmatic and tectonic processes. Because the regional stress field is highly compressional and the volcanoes

Burning down the brewery: Establishing and evacuating an ancient imperial colony at Cerro Baúl, Peru

Science.gov (United States)

Moseley, Michael E.; Nash, Donna J.; Williams, Patrick Ryan; deFrance, Susan D.; Miranda, Ana; Ruales, Mario

2005-01-01

Before the Inca reigned, two empires held sway over the central Andes from anno Domini 600 to 1000: the Wari empire to the north ruled much of Peru, and Tiwanaku to the south reigned in Bolivia. Face-to-face contact came when both colonized the Moquegua Valley sierra in southern Peru. The state-sponsored Wari incursion, described here, entailed large-scale agrarian reclamation to sustain the occupation of two hills and the adjacent high mesa of Cerro Baúl. Monumental buildings were erected atop the mesa to serve an embassy-like delegation of nobles and attendant personnel that endured for centuries. Final evacuation of the Baúl enclave was accompanied by elaborate ceremonies with brewing, drinking, feasting, vessel smashing, and building burning. PMID:16293691

INVENTARIO FLORÍSTICO EN EL CERRO DEL CUCHILLO, TAPÓN DEL DARIÉN COLOMBIANO

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CÁRDENAS-LÓPEZ DAIRON

2003-06-01

Full Text Available Se presentan los resultados del inventario florístico realizado entre agosto de 1987y julio de 1988, en el Cerro del Cuchillo, municipio de Riosucio (Chocó, Tapón delDarién colombiano. Se efectuaron diez salidas de campo con duración de quincedías cada una . Se registraron 127 familias, 428 géneros y 747 especies. Las divisionesmejor representadas fueron Magnoliophyta con 112 familias, 402 géneros y 705especies; Pteridophyta con trece familias, 23 géneros y 40 especies. Cycadophytaestuvo representada por la familia Zamiaceae con una especie y Gnetophyta por lafamilia Gnetaceae con una especie. Entre las plantas con flores (Magnoliophyta, elgrupo mejor representado fue la clase Magnoliopsida con 94 familias, 324 génerosy 573 especies. La clase Liliopsida estuvo representada por 18 familias, 78 génerosy 132 especies.

Reporte de un opilión cavernícola de la familia Gonyleptidae encontrado en el cerro de Quininí, Tibacuy, Cundinamarca

Directory of Open Access Journals (Sweden)

Alejandro Parra

2000-07-01

Full Text Available En la observación bioespelológica en una gruta ubicada en el cerro de Quinini, inspección de policía de Cumaca, Cundinamarca, se encontró una población de Opiliones de la Familia Gonyleptidae ,familia por primera vez reportada para Colombia. Se observó en los opiliones conductas de apareamiento y se realizó un estudio morfológico para una determinación taxonómica profunda.

Reporte de un opilión cavernícola de la familia Gonyleptidae encontrado en el cerro de Quininí, Tibacuy, Cundinamarca

OpenAIRE

Alejandro Parra; Oscar Vivas; Francisco Hormanza

2000-01-01

En la observación bioespelológica en una gruta ubicada en el cerro de Quinini, inspección de policía de Cumaca, Cundinamarca, se encontró una población de Opiliones de la Familia Gonyleptidae ,familia por primera vez reportada para Colombia. Se observó en los opiliones conductas de apareamiento y se realizó un estudio morfológico para una determinación taxonómica profunda.

A new species of Cryptonympha Lugo-Ortiz McCafferty (Ephemeroptera, Baetidae) from Cerro Duida (Venezuela).

Science.gov (United States)

Derka, TomÁŠ; Nieto, Carolina

2018-02-05

The genus Cryptonympha includes three species: C. copiosa Lugo-Ortiz McCafferty, 1998; C. dasilvai Salles Francischetti, 2004 and C. genevievae Thomas, Manchon Glémet, 2013, known only from the nymphal stage. A description of the nymph of a fourth representative, Cryptonympha tracheata sp. n. is provided here, based on material collected in a blackwater stream on the slopes of the Cerro Duida mountain in south-western Venezuela. The nymph of the new species can be easily distinguished from the other species of the genus by very long tracheal gills II-VII, 2.5 times the length of each tergum, gill I small, nearly half length of gill IV and by posterior margin of terga with rounded spines. A complete description of the new species and a key for nymphs of all known Cryptonympha species are provided.

Estimation of the resource and technological prospective of geothermal energy in Mexico (Annexe 3 in 'A vision of year 2030 on the use of the renewable energies in Mexico'); Estimacion del recurso y prospectiva tecnologica de la geotermia en Mexico (Anexo 3 en 'Una vision al 2030 de la utilizacion de las energias renovables en Mexico')

Energy Technology Data Exchange (ETDEWEB)

Iglesias R, Eduardo; Arellano G, Victor; Torres R, Rodolfo Joaquin [Instituto de Investigaciones Electricas, Cuernavaca, Morelos (Mexico)

2005-08-15

Due to its individual geologic-structural characteristics, Mexico counts on abundant geothermal resources. At the moment we count on a database that includes 2,332 geothermal manifestations distributed in 27 of the 32 Mexican states, the geothermal resources are classified as high temperature and intermediate or low temperature resources. Those of high temperature can be used for the generation of electrical energy. Those of intermediate to low temperature are more appropriate for direct applications of the geothermal heat. As of today, in Mexico exist four geothermal fields of high temperature that are being exploded for the electrical generation. [Spanish] Debido a sus particulares caracteristicas geologico-estructurales, Mexico cuenta con abundantes recursos geotermicos. Actualmente contamos con una base de datos que incluye 2,332 manifestaciones geotermicas distribuidas en 27 de los 32 estados mexicanos, los recursos geotermicos se clasifican en de alta temperatura y recursos de temperatura intermedia a baja. Los de alta temperatura pueden utilizarse para la generacion de energia electrica. Los de temperatura intermedia a baja son mas apropiados para aplicaciones directas del calor geotermico. Actualmente en Mexico existen cuatro campos geotermicos de alta temperatura que estan siendo explotados para la generacion electrica.

Development of the Cerro solo deposit and uranium favorability of the San Jorge Gulf Basin, province of Chubut

International Nuclear Information System (INIS)

Navarra, P.R.; Benitez, A.F.

1997-01-01

In the future the uranium exploration activities of CNEA would tend to improve the knowledge of geology and uranium favorability; to perform prospection tasks, and research and development in exploration technologies, to contribute to be in a position to meet the requirements of the country in the long term. On the other hand, a strong growth of nuclear capacity is expected in the first two decades of the next century. Based on its promising grade, the Cerro Solo uranium ore deposit was selected in 1990 by the CNEA to carry out an assessment project. The intensive exploration level was accomplished, as follows: definition of general characteristics of the main orebodies; detailed geologic studies; estimation of resources with adequate data; and preliminary selection of mining-milling methods to estimate the potential profitability of the project. The deposit belongs to the sandstone type. The mineralized layers are distributed into the fluvial sandstones and conglomerates of the cretaceous Chubut Group, lying 50 to 130 m deep Resources of the deposit, with an average grade of 0.3% U, in tonnes of recoverable uranium at costs of up to $80/kg U, are: Reasonable Assured Resources (RAR): 800 t U, Estimated Additional Resources, Category I (EAR-I): 2100 t U. Follow-up drilling programmes are being performed at present in some of the target sites defined in the paleochannel that hosts the Cerro Solo deposit, in order to establish the hypothetical resources of the area. The sites were determined as a result of the exploration that CNEA conducted in the Pichinan uranium district. Recently a regional research project was formulated, for the detailed exploration in the San Jorge Gulf Basin, where the Chubut Group is distributed. 17 refs, 4 figs

Notes on the ecology of Phyllodactylus reissi (Phyllodactylidae: Sauria in Parque Nacional Cerros de Amotape (Tumbes, Peru

Directory of Open Access Journals (Sweden)

Juan Carlos Jordán Arizmendi

2012-02-01

Full Text Available Some basics aspects on the ecology of the nocturnal gecko Phyllodactylus reissi from Parque Nacional Cerros de Amotape (Tumbes, Peru are described. This species used rock boulders (57,4% and trees (31,9% as microhabitats primarily, exhibiting a nocturnal activity pattern, with a peak between 2100-2200 hours, remaining active until midnight. Body temperature (mean 24,4 ºC was correlated with both air and substrate temperature, with the last variable affecting in higher degree (47% the body temperature of this species. The slightly high body temperature of Phyllodactylus reissi, compared to other Phyllodactylus geckos, could be related to nocturnal microhabitat use and diurnal retreat site selection. More studies on lizard ecology from this endangered ecosystem are needed.

Procesos históricos y ambientales en Cerro de San Pedro, San Luis Potosí, México, 1948-1997

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Paula Andrea Martínez Chaves

2010-01-01

Full Text Available Los estudios sobre el municipio Cerro de San Pedro enfatizan la continuidad ambiental aparente que estimula la minería; sin embargo, esta lectura subvalora otras dinámicas que ocurren en la zona. Con base en observaciones directas de trabajo en campo, para realizar análisis de coberturas vegetales, entrevistas con los habitantes de la zona, revisión de cartografía e investigación de archivo, el presente trabajo muestra procesos como la explotación de recursos vegetales y el pastoreo, como actividades económicas paralelas a las labores mineras, y que no habían sido tratados hasta ahora.

El Cerro de los Santos: paisaje, negociación social y ritualidad entre el mundo ibérico y el hispano

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García Cardiel, Jorge

2015-12-01

Full Text Available The Iberian shrine of Cerro de los Santos is located next to one of the main roads in the Southeast of the Meseta, in the middle of an area without any town of some entity. This paper aims to highlight its status as a shrine of passage, i.e. as a sacred, safe point where voyagers could rest overnight under the protection of the god. The creation of a statio by the Romans in such a place and its dedication to the goddess Pales provide more circumstantial evidence for this theory. Furthermore, some domestic material contexts can be defined, probably connected with this activity, and clearly different from the well-known ritual contexts of the shrine.La ubicación del santuario ibérico del Cerro de los Santos junto a una de las principales vías de comunicación del sureste meseteño y en el centro de una comarca desprovista de núcleos urbanos de cierta entidad permite subrayar en este artículo su uso continuado como santuario de paso, lugar sacro y seguro al que los caminantes podrían acogerse para pernoctar bajo la protección de la divinidad. La creación de una statio en el enclave en época romana y su dedicación a la diosa Pales no son sino argumentos ulteriores en este sentido. Se identifican además contextos materiales domésticos, distintos de los espacios de culto bien conocidos del santuario, relacionables con esta otra actividad.

Decree 343/012. Is regulated the servitude established by Decree-Law 10,383, on several lines of electricity conduction -150 KV to be built in the departments of Florida, Cerro Largo, Maldonado, Flores, San Jose and Tacuarembo

International Nuclear Information System (INIS)

2012-01-01

This decree regulates the establishment of electricity conduction in Florida, Cerro Largo, Maldonado, Flores, San Jose and Tacuarembo towns. These electrical lines are necessary to provide the public service by UTE

Report about drilling works made in 13 Anomaly de Taylor and in the N- NE of its, around Fraile Muerto (Cerro Largo district): Uranium project

International Nuclear Information System (INIS)

Massa, J; Pirelli, H.

1983-01-01

The perforations were carried out to investigate in depth denominated anomaly 13 detected during the Taylor Mission (1975) and extended the punch area of study during you are suitable DINAMIGE-BRGM (Project the present report details the activities realised in the environs Fraile Muerto (Cerro Largo district) by the command team of perforations of the uranium project. Previously and contemporarily to the executed works, prospection became geophysical ground geochemistry geology and, works. (Uranium)

Seismologic study of Los Hum eros geothermal field, Pueblo, Mexico. Part I: Seismicity, source mechanisms and stress distribution; Estudio sismologico del campo geotermico de Los Humeros, Puebla, Mexico. Parte I: Sismicidad, mecanismos de fuente y distribucion de esfuerzos

Energy Technology Data Exchange (ETDEWEB)

Lermo, Javier; Antayhua, Yanet [Instituto de Ingenieria, Universidad Nacional Autonoma de Mexico, Mexico D.F (Mexico)]. E-Mail: jles@pumas.iingen.unam.mx; Quintanar, Luis [Instituto de Geofisica, Universidad Nacional Autonoma de Mexico, Mexico D.F (Mexico); Lorenzo, Cecilia [Gerencia de Proyectos Geotermoelectricos, Comision Federal de Electricidad, Michoacan (Mexico)

2008-01-15

The distribution of earthquakes at the surface and at depth in the Los Humeros geothermal field, Puebla (Mexico), is analyzed from 1997-2004. Data for 95 earthquakes were registered at more than five permanent and temporary stations installed by the Comision Federal de Electricidad and the Instituto de Ingenieria of the Universidad Nacional Autonoma de Mexico. The duration magnitudes of the quakes are equal to or lower than 3.6 Md and the focal depths do not exceed 4.0 km. Simple focal mechanisms and moment tensor inversions were made, and the number of earthquakes registered by two stations of the permanent network (numbers S05, S06) was compared with water-injection and steam-production volumes over a certain period. The results at the surface and at depth show seismic activity occurring in the northern zone of the field around injection wells I29 (well H-29) and I38 (well H-38); whereas, the simple focal mechanisms and moment tensors demonstrate stresses of heterogeneous origin, suggesting that part of the seismic activity in Los Humeros is probably induced, mainly by injecting water. [Spanish] Se analiza la distribucion en superficie y en profundidad de los sismos ocurridos en el campo geotermico de Los Humeros, Puebla (Mexico), durante el periodo 1997-2004. Los datos corresponden a 95 sismos registrados por mas de cinco estaciones permanentes y temporales instaladas por la Comision Federal de Electricidad y el Instituto de Ingenieria de la Universidad Nacional Autonoma de Mexico, cuyas magnitudes de duracion son menores o iguales a 3.6 Md y profundidades focales que no sobrepasan los 4.0 km. Asimismo, se realizaron mecanismos focales simples y de inversion de tensor de momento, y se comparo el numero de sismos registrados por dos estaciones de la red permanente (numeros S05, S06) con la inyeccion de agua y la produccion de vapor durante cierto tiempo. Los resultados en superficie y en profundidad muestran actividad sismica en la zona norte del campo, alrededor

Measurement of radon (222Rn) in thermal water of Cerro Pacho, Coatepeque Caldera, El Salvador

International Nuclear Information System (INIS)

Rodriguez, Ramiro; Olmos, Rodolfo; Payes, Julio

2014-01-01

Radon ( 222 Rn) concentrations and radio ( 226 Ra) evaluation dissolved in thermal spring water are presented to contribute to volcanic monitoring, adapting and validating analytical methodology. Sampling was discreet and monthly type, from June 2011 to March 2013. Radon levels was vary from 0,48 ± 0,1 to 1,54 ± 0,13 Bq/L (average 1,24 Bq/L). Radio concentrations were evaluated from January to December 2012. The values found do not show radio detection confidence level of 95% with respect to the detection limit (4,2 mBq/L). A decrease in radon was observed possibly related to subduction anomalies with epicenter at 143 km from Cerro Pacho, in November 2012, volcanic seismicity was also recorded 40 days before with increments of microearthquakes and volcano-tectonic activity. The first measurements of radon in thermal water have been generated, establishing the baseline to evaluate the behavior of these radionuclides with seismic activity. (author) [es

Micas at magmatic and hydrothermal stages in the environment of the Cerro Verde Santa Rosa porphyry copper type deposit

Energy Technology Data Exchange (ETDEWEB)

Le Bel, L

1979-01-01

The chemical composition of biotites and sericites from the Cerro Verde porphyry copper type deposit have been investigated in detail, using an electron microprobe. The main results of the study are: Al/sup vi/ and Ti contents of biotites of magmatic as well as hydrothermal origin may be related to the temperature of crystallization estimed by independent methods. On the other hand the Mg/Fe and Mg/(Mg + Fe) ratios are almost constant. This fact is interpreted in terms of fO/sub 2/; sericites have a phengitic composition in which the solubilities of the two end-members celadonite and paragonite are controlled by a fluid phase under P, T conditions that could be estimated.

The Final Days of Paracas in Cerro del Gentil, Chincha Valley, Peru

Science.gov (United States)

2016-01-01

This article describes and analyzes a highly significant archaeological context discovered in a late Paracas (400–200 BCE) sunken patio in the monumental platform mound of Cerro Gentil, located in the Chincha Valley, Peru. This patio area was used for several centuries for ritual activities, including large-scale feasting and other public gatherings. At one point late in this historical sequence people deposited a great deal of objects in what is demonstrably a single historical event. This was quickly followed by a series of minor events stratigraphically immediately above this larger event. This entire ritual process included the consumption of liquids and food, and involved the offering of whole pottery, pottery fragments, botanical remains, bone, lithics, baskets, pyro-engraved gourds, mummies, and other objects. We interpret these events as an “abandonment ceremony” or “termination ritual” during the late Paracas period, one that may have lasted for weeks or even months. The subsequent Topará occupation at the site (ca. 200 BCE- AD 100) involved the architectural enhancement of the mound area, but the pattern of use of the patio itself ended. Such a termination ritual signals a reorganization in the regional political structure of Paracas society. PMID:27144824

Measurements of air contaminants during the Cerro Grande fire at Los Alamos National Laboratory

Energy Technology Data Exchange (ETDEWEB)

Eberhart, Craig

2010-08-01

Ambient air sampling for radioactive air contaminants was continued throughout the Cerro Grande fire that burned part of Los Alamos National Laboratory. During the fire, samples were collected more frequently than normal because buildup of smoke particles on the filters was decreasing the air flow. Overall, actual sampling time was 96% of the total possible sampling time for the May 2000 samples. To evaluate potential human exposure to air contaminants, the samples were analyzed as soon as possible and for additional specific radionuclides. Analyses showed that the smoke from the fire included resuspended radon decay products that had been accumulating for many years on the vegetation and the forest floor that burned. Concentrations of plutonium, americium, and depleted uranium were also measurable, but at locations and concentrations comparable to non-fire periods. A continuous particulate matter sampler measured concentrations that exceeded the National Ambient Air Quality Standard for PM-10 (particles less than 10 micrometers in diameter). These high concentrations were caused by smoke from the fire when it was close to the sampler.

Improvement in using steam for electric generation at the Los Azufres, Mich., geothermal field; Mejora en el aprovechamiento del vapor para generar energia electrica en el campo geotermico de Los Azufres, Mich.

Energy Technology Data Exchange (ETDEWEB)

Torres Rodriguez, Marco A.; Flores Armenta, Magaly; Mendoza Covarrubias, Alfredo [Comision Federal de Electricidad, Gerencia de Proyectos Geotermoelectricos, Morelia, Michoacan (Mexico)]. E-mail: magaly.flores@cfe.gob.mx

2010-01-15

Commercial exploitation in the Los Azufres geothermal field, Michoacan, Mexico, started in 1982 when the first five backpressure-power units of 5-MW each were commissioned. Nowadays the installed capacity is 188 MW from 14 units: five in the South Zone fed by steam produced from 18 production wells plus two binary-cycle power units fed by residual brines; and seven in the North Zone with steam supplied by 22 production wells. There are seven backpressure-power units with high specific consumption [between 14.5 and 13.6 tons per hour of steam (t/h) per MW]. Three operate in the South Zone and four in the North Zone. This paper shows a way to achieve more efficient use of the geothermal resource by replacing the seven backpressure units, which have completed their useful lifetime-or are close to do it-with two, new condensing power units with lower specific consumption: one unit of 50 MW to be located in the North Zone and the other of 25 MW to be placed in the South Zone. No new wells need be drilled. In this way, the average specific consumption would be reduced to 8.8-7.2 t/h per MW (saving 47% of the steam), the income for electric generation would be increased and the steam-extraction rate would remain the same. [Spanish] En 1982 empezo la explotacion comercial del campo geotermico de Los Azufres, Mich., Mexico, con la instalacion y puesta en servicio de las primeras cinco unidades turbogeneradoras a contrapresion de 5 MW cada una. Actualmente la capacidad instalada es de 188 MW, con catorce unidades: cinco en la zona sur, alimentadas por el vapor de 18 pozos productores, mas dos unidades de ciclo binario que utilizan salmuera residual, y siete unidades en la zona norte, alimentadas por 22 pozos. Hay siete unidades a contrapresion con un consumo especifico elevado [entre 14.5 y 13.6 toneladas por hora (t/h) de vapor por MW], tres de las cuales se localizan en la zona sur y cuatro en la zona norte. En este documento se presenta un proyecto para hacer mas

Construcciones y cementerios del período Intermedio Tardío en el cerro Ñañañique (departamento de Piura

Directory of Open Access Journals (Sweden)

1989-01-01

Full Text Available Après un abandon de plus d'un millénaire, le site de Cerro Ñañañique est réoccupé sans doute à partir du Xème siècle de notre ère. Les fouilles réalisées ont permis de reconnaître l'existence d'un ensemble monumental, composé de terrasses artificielles, et d'un complexe de bâtiments et structures couvrant tout le sommet du cerro. De petites constructions furent édifiées sur le bas versant Est et au moins cinq cimetières sont connus dans les environs immédiats. L'ensemble de ces vestiges prouve le maintien d'une occupation du secteur jusqu'à la fin de la période préhispanique. L'article est centré sur l'analyse de quatorze contextes funéraires provenant d'un des cimetières de cette époque. Y sont décrits les positions, orientations et associations des différents corps exhumés ainsi que le mobilier funéraire associé. Une comparaison avec les traditions voisines connues permet de confirmer certaines similitudes et en particulier les relations étroites avec les zones méridionales. Después de un abandono de más de un milenio, el sitio de Cerro Ñañañique se reocupó, posiblemente desde el siglo X d.c. Las excavaciones realizadas permitieron reconocer la existencia de un conjunto monumental compuesto de terrazas artificiales y de un complejo de edificios y estructuras que cubre toda la cumbre del cerro. Pequeñas construcciones fueron también edificadas en la parte baja de la vertiente este y hubo, por lo menos, cinco cementerios a proximidad. El conjunto de estos vestigios comprueba la permanencia de una ocupación del sector hasta el final de la época prehispánica. El artículo está centrado en el análisis de catorce contextos funerarios de aquella época. Se describen la posición, la orientación y las asociaciones de los varios cuerpos exhumados, así como el material funerario asociado. Una comparación con las tradiciones vecinas permite confirmar ciertas semejanzas y particularmente las relaciones

Tecnología para la producción artesanal del Jabón Prieto de Jatropha curcas L

Directory of Open Access Journals (Sweden)

Enrique Casanovas Cosío

2014-09-01

Full Text Available La producción de jabón artesanal es una práctica local en el Cantón de Chone de la provincia de Manabí, Ecuador, pero que no está descrito el proceso en literatura científica. Se ha tratado de describir la tecnología artesanal de producción del Jabón Prieto con las nueces del piñón (Jatropha curcas L., para lo cual se empleó un diseño observacional apoyado con encuestas a tres productores y una comparación entre tres muestras de producciones de jabones obtenidos del aceite de la Jatropha en laboratorios del INIAP y las artesanales. Los procesos de producción de jabones artesanales son similares y se describe la tecnología en la cual no se encontraron gastos de insumos externos que apunta a la sostenibilidad de su producción. El jabón artesanal es más oscuro y con un olor penetrante parecido al del fruto seco, ambos son de consistencia sólida; que en el jabón artesanal se expresa por la adición de grasa de vaca con ácidos grasos saturados. Los jabones obtenidos presentaron similares valores de pH (alcalinos. El jabón artesanal presentó mayor contenido de humedad (12.73 % y menor contenido de grasa (34.77 %. La variabilidad de los indicadores físico químicos fueron mayores en el jabón artesanal pero siempre con un CV menor de 10.0 %, que indica similitud en los procesos. Desde el punto de vista bacteriológico ambos jabones se declaran aptos para el consumo con recuentos de aerobios mesófilos totales menores que 10 UFC, y ausencia de Echerichia coli, Salmonella sp. y Shigelia sp.

Cerro Negro bitumen degradation by a consortium of marine benthic microorganisms

Energy Technology Data Exchange (ETDEWEB)

Potter, T.L.; Duval, B. [USDA-ARA, Tifton, GA (USA). Southeast Watershed Research Laboratory

2001-01-01

Cerro Negro bitumen, separated from an Orimulsion sample, was incubated for up to 120 days with sediments collected at a petroleum-impacted site in Tampa Bay, Florida. Biodegradation conditions were optimized by increasing bitumen surface area, continuous agitation on a shaker apparatus, use of a complete growth medium, and maintenance at 37{degree}C. Aerobic degradation conditions were promoted by maintaining sediment contact with the laboratory atmosphere. Bitumen recovered in solvent extracts when compared to autoclaved controls decreased by up to 40% during the first 56 days. There was no detectable change after this. Molasses addition and use of a culture enriched from the sediments did not change the extent or rate of decrease in bitumen recovery. Chemical fractionation of bitumen control and degraded bitumen showed that aromatic and aliphatic fractions were depleted by {approx} 50%. Accumulation of polars was observed; however, the apparent increase was relatively small when compared to the mass loss of the other fractions. Selected biomarker ratios were not affected by incubation indicating their utility for fingerprinting the source bitumen in environmental samples. PAH distribution in the aromatic fraction favored the higher alkyl-homologues with the relative degree of alkylation increasing as the mass of bitumen recovered decreased with degradation. The study showed that up to 40% of the bitumen was bioaccessible and that bioremediation may be a treatment option for sediments contaminated with bitumen by an Orimulsion spill. 36 refs., 8 figs., 5 tabs.

Far-IR measurements at Cerro Toco, Chile: FIRST, REFIR, and AERI

Science.gov (United States)

Cageao, Richard P.; Alford, J. Ashley; Johnson, David G.; Kratz, David P.; Mlynczak, Martin G.

2010-09-01

In mid-2009, the Radiative Heating in the Underexplored Bands Campaign II (RHUBC-II) was conducted from Cerro Toco, Chile, a high, dry, remote mountain plateau, 23°S , 67.8°W at 5.4km, in the Atacama Desert of Northern Chile. From this site, dominant IR water vapor absorption bands and continuum, saturated when viewed from the surface at lower altitudes, or in less dry locales, were investigated in detail, elucidating infrared (IR) absorption and emission in the atmosphere. Three Fourier Transform InfraRed (FTIR) instruments were at the site, the Far-Infrared Spectroscopy of the Troposphere (FIRST), the Radiation Explorer in the Far Infrared (REFIR), and the Atmospheric Emitted Radiance Interferometer (AERI). In a side-by-side comparison, these measured atmospheric downwelling radiation, with overlapping spectral coverage from 5 to 100μm (2000 to 100cm-1), and instrument spectral resolutions from 0.5 to 0.643cm-1, unapodized. In addition to the FTIR and other ground-based IR and microwave instrumentation, pressure/temperature/relative humidity measuring sondes, for atmospheric profiles to 18km, were launched from the site several times a day. The derived water vapor profiles, determined at times matching the FTIR measurement times, were used to model atmospheric radiative transfer. Comparison of instrument data, all at the same spectral resolution, and model calculations, are presented along with a technique for determining adjustments to line-by-line calculation continuum models. This was a major objective of the campaign.

Entre el sueño del proyecto y la lógica del lugar. La arquitectura imposible de los cerros de Valparaíso

Directory of Open Access Journals (Sweden)

Pablo M. Millán-Millán

2016-04-01

Full Text Available Valparaíso es el resultado de la unión de dos ciudades en una: la ciudad vertical de los cerros y la ciudad horizontal del Plan –parte plana–. Esta doble naturaleza ha ido configurando una dualidad obligada a convivir y a establecer un continuo diálogo, acabando en la mayoría de los casos en conflicto. Si por un lado está la ciudad global y ortogonal como resultado de la ocupación europea, por otro lado estará la ciudad onírica agarrada a los acantilados ajena a cualquier orden preestablecido. Cada una de estas dos ciudades irá materializando su propia arquitectura: una real y estandarizada, propia de cualquier periferia de ciudad, y otra imposible. Será esta segunda la que vaya evolucionando en un intento continuo de adaptación y será el propio lugar el encargado de rechazar cualquier construcción que no le sea propia. Esta dicotomía quedará plasmada en numerosos proyectos que nunca verán la luz. El objetivo del artículo será mostrar, a partir de numerosos proyectos inéditos descubiertos en Valparaíso, cómo la arquitectura pensada para los cerros nunca llegó a construirse y fue dando paso a unas construcciones a medio camino entre lo real y lo imaginario, entre la lógica y el sueño.

La intrusión de Cerro Redondo (Pérmico Inferior, Cordillera Ibérica, Zaragoza): reconstrucción 3D y modelo de emplazamiento

OpenAIRE

Majarena Serrano, Urbez; Gil Imaz, Andrés; Lago San José, Marceliano; Galé, Carlos

2017-01-01

La intrusión subvolcánica de Cerro Redondo (Cordillera Ibérica, Zaragoza), de edad Pérmico Inferior, muestra una composición dactíca, una naturaleza calcoalcalina y se caracteriza por presentar una marcada estructuración interna determinada por un bandeado subvertical y d e espaciado variable (1-25 cm), que se encuentra afectado por numerosos pliegues d e flujo magmático de distinta escala (desde centimétrica hasta hectométrica). El estudio cartográfico y de la anisotropia de la susceptib...

Unrest of Chiles - Cerro Negro volcanic complex: A binational Ecuador - Colombia effort

Science.gov (United States)

Ruiz, M. C.; Gomez, D.; Torres, R.; Cadena, O.; Mothes, P. A.; Anzieta, J. C.; Pacheco, D. A.; Bernard, B.; Acero, W.; Hidalgo, S.; Enriquez, W.; Cordova, A.

2014-12-01

The increasing seismic activity at the area of Chiles - Cerro Negro volcanic complex, located at the Ecuador-Colombian border, has been jointly monitored by the Instituto Geofisico - Ecuador and the Observatorio Vulcanologico y Sismologico de Pasto OVSP, a division of the Servicio Geologico Colombiano. Since April 2013, three seismic swarms have been detected in this area and more than 100.000 events are recorded since November 2013. The largest and more recent swarm has a daily average of 676 events between March and June 2014. Currently a seismic network of 8 seismic stations (5 in the Colombian and 3 in Ecuadorean side) are deployed in this area. Epicenters of more than 315 seismic events with magnitudes Ml>2.0 and 10 or more phases are located in an area 1-4 km south of Chiles volcano with shallow depths (up to 14 km). Most of events have magnitudes between 1.0 to 4.0. Nine events have magnitudes larger than 4.0 and the largest event occurred on April 30. 2014 with a local magnitude of 4.7 and inverse-transcurrent component focal mechanism. Waveforms and spectral patterns define these events as volcano-tectonic. Events with large magnitudes (above 3.0) show a very long-period component. Hot spring and deformation measurements also show signals of volcanic unrest.

PATRONES DE CONSUMO FINAL DE CÉRVIDOS EN EL PARANÁ MEDIO: EL CASO DEL SITIO CERRO AGUARÁ / Cervids final consumption patterns in middle Paraná River: the case of Cerro Aguará archaeological site

Directory of Open Access Journals (Sweden)

Leonardo Mucciolo

2015-06-01

Full Text Available Los cérvidos fueron amplia y regularmente explotados por los cazadores-recolectores que habitaron la macroregión del Paraná-Plata durante el Holoceno tardío. En la cuenca media del Paraná, sin embargo, muy pocos estudios han enfocado sobre las estrategias empleadas para su obtención, procesamiento y consumo. Teniendo en cuenta esto, el objetivo de este trabajo es explorar dichos aspectos a partir del análisis de los conjuntos de cérvidos provenientes del sitio arqueológico Cerro Aguará, localizado en el departamento General Obligado (provincia de Santa Fe. La perspectiva seleccionada propone al consumo como factor preponderante en la configuración del registro zooarqueológico dentro del continuum de actividades que componen la explotación faunística. Desde esta perspectiva, y tomando en consideración que las carcasas de los cérvidos proveen distintos tipos de recursos alimenticios con diferentes costos de extracción (carne, médula y grasa ósea, se evalúan diferentes indicadores para establecer si existió diferente intensidad en su procesamiento. Los resultados indican que las dos especies de cérvidos identificadas en el sitio, Blastocerus dichotomus y Ozotoceros bezoarticus, ocuparon un rol preponderante en la dieta, aunque las carcasas del primero fueron empleadas más intensivamente probablemente en correlación con su mayor disponibilidad de nutrientes internos, tales como la médula y posiblemente la grasa ósea.  Abstract  Cervids were wide and regularly exploited by several Late Holocene hunter-gatherers inhabiting Paraná Plata macroregion. In the middle Paraná river, however, few research has been made on strategies involving their procurement, processing and consumption. The purpose of this article is to explore those aspects from the analysis of cervid assemblages of Cerro Aguará archaeological site (General Obligado, Santa Fe province. The selected perspective proposes final consumption as one of the most

Optical and infrared observations of SN 1987A from Cerro Tololo Inter-American Observatory

International Nuclear Information System (INIS)

Phillips, M.M.

1988-01-01

Results from optical and infrared observations of SN 1987A obtained at Cerro Tololo Inter-American Observatory over the first seven months since core collapse are reviewed. Around 130 days after outburst, the bolometric light curve began to smoothly decline at a rate of ∼ 0.01 mag day-1, providing dramatic confirmation of the prediction that radioactivity had powered the optical display after the first month./ the peculiar color changes are kinks observed beginning on the 25th day probably signaled the initial release of trapped energy from mass 56 material. The bolometric luminosity of SN 1987A was unusually low at first, but reached a value more typical of other type II supernovae by the time that the final exponential decline had begun. Over much of the period covered by these observations, the optical and infrared spectra were characterized by strong absorption lines of Ba II and Sr II. Comparison with the spectra of other type II supernovae at similar stages of evolution supports the suggestion that s-processed elements were enriched in the hydrogen envelope of the progenitor, Sanduleak - 69 degrees 202

3-cerro y 4-mundo: los números del banquete en las ofrendas quechuas

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David Lorente Fernández

2010-12-01

Full Text Available Las ofrendas quechuas del sur del Perú son platos alimenticios, banquetes destinados principalmente a la pachamama y los apus, pero también elaborados sistemas matemáticos regidos por operaciones sofisticadas. Sirviéndose de dos números fundamentales, el 3 y el 4, los especialistas rituales son capaces de transmitir mensajes polisémicos. Mediante el número 3 aglutinan clientes, parajes y cerros, en suma, «personas» capaces de interactuar entre sí. El 3 aparece en los k’intus de hojas de coca y en las oraciones que se recitan durante el proceso de realizar la ofrenda. Por el contrario, el número 4 no indica relaciones sino formas espaciales: es un operador geométrico que unifica la servilleta ceremonial (unk’uña, el papel envoltorio y el paquete acabado para representar las cuatro direcciones del mundo y hacer de la ofrenda un mundo en miniatura. Gracias a los dos números el ritualista puede recrear el cosmos, establecer convenios con los dioses y definir nuevas situaciones favorables para la vida de sus clientes.

Comportamiento del asma bronquial en un área de salud del policlínico Cerro Behavior of bronchial asthma in a health area of the "Cerro" polyclinic

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Marlene Álvarez Carmenate

2011-03-01

Full Text Available Introducción: el asma bronquial es la enfermedad crónica más frecuente en pediatría y una de las principales causas de consulta. Objetivo: describir el comportamiento del asma bronquial como problema de salud. Métodos: trabajo descriptivo, prospectivo, de corte longitudinal, en 309 niños con edades comprendidas entre 0 y 19 años con el diagnóstico de asma bronquial, atendidos en los 15 consultorios médicos del grupo básico de trabajo A del policlínico universitario "Cerro", en el período comprendido entre el 1º de enero de 2007 y el 31 de diciembre de 2007. Método empírico para la obtención de los datos clínicos epidemiológicos, y como técnica, la encuesta a través de un cuestionario. Resultados: 148 pacientes (48 % se encontraban entre 10 y 14 años, 175 (56,6 % del sexo masculino, 136 (44 % fueron clasificados como persistentes ligeros, 140 (58 % presentaron rinitis y 57 (24 % dermatitis. Había fumadores en las viviendas de 303 pacientes (98 %, hacinamiento en 290 casos (94 % y el polvo en el hogar 284 (92 %. Conclusiones: predominio en el grupo de edades de 10 a 14 años, sexo masculino. En cuanto a la severidad de la enfermedad predominó la forma persistente ligera, las manifestaciones atópicas más frecuentes fueron la rinitis y la dermatitis, los principales factores de riesgo fueron el humo del tabaco, el polvo en el hogar y el hacinamiento, y el tratamiento de elección fue el de la crisis. Se observó la falta de organización y unidad de criterios para el enfoque integral de la política intercrisis o de sostén en la atención de los pacientes.Introduction: bronchial asthma is the more frequent chronic disease in Pediatrics and one of the major causes of consultation. Objective: to describe the behavior of bronchial asthma as a health problem. Methods: a longitudinal, prospective and descriptive study was conducted in 309 children aged between 0 and 19 diagnosed with bronchial asthmas seen in the 15 medical

Report about drilling works made in 13 Anomaly de Taylor and in the N- NE of its, around Fraile Muerto (Cerro Largo district): Uranium project[Study of Uranium prospection in Uruguay]; Informe sobre los trabajos de perforacion efectuados en la Anomalia 13 de Taylor y al N-NE de la misma , en los alrededores de Fraile Muerto (Departamento de Cerro Largo). Proyecto Uranio

Energy Technology Data Exchange (ETDEWEB)

Massa, J; Pirelli, H

1983-07-01

The perforations were carried out to investigate in depth denominated anomaly 13 detected during the Taylor Mission (1975) and extended the punch area of study during you are suitable DINAMIGE-BRGM (Project the present report details the activities realised in the environs Fraile Muerto (Cerro Largo district) by the command team of perforations of the uranium project. Previously and contemporarily to the executed works, prospection became geophysical ground geochemistry geology and, works. (Uranium)

Mineralized breccia clasts: a window into hidden porphyry-type mineralization underlying the epithermal polymetallic deposit of Cerro de Pasco (Peru)

Science.gov (United States)

Rottier, Bertrand; Kouzmanov, Kalin; Casanova, Vincent; Bouvier, Anne-Sophie; Baumgartner, Lukas P.; Wälle, Markus; Fontboté, Lluís

2018-01-01

Cerro de Pasco (Peru) is known for its large epithermal polymetallic (Zn-Pb-Ag-Cu-Bi) mineralization emplaced at shallow level, a few hundred meters below the paleo-surface, at the border of a large diatreme-dome complex. Porphyry-style veins crosscutting hornfels and magmatic rock clasts are found in the diatreme breccia and in quartz-monzonite porphyry dikes. Such mineralized veins in clasts allow investigation of high-temperature porphyry-style mineralization developed in the deep portions of magmatic-hydrothermal systems. Quartz in porphyry-style veins contains silicate melt inclusions as well as fluid and solid mineral inclusions. Two types of high-temperature (> 600 °C) quartz-molybdenite-(chalcopyrite)-(pyrite) veins are found in the clasts. Early, thin (1-2 mm), and sinuous HT1 veins are crosscut by slightly thicker (up to 2 cm) and more regular HT2 veins. The HT1 vein quartz hosts CO2- and sulfur-rich high-density vapor inclusions. Two subtypes of the HT1 veins have been defined, based on the nature of mineral inclusions hosted in quartz: (i) HT1bt veins with inclusions of K-feldspar, biotite, rutile, and minor titanite and (ii) HT1px veins with inclusions of actinolite, augite, titanite, apatite, and minor rutile. Using an emplacement depth of the veins of between 2 and 3 km (500 to 800 bar), derived from the diatreme breccia architecture and the supposed erosion preceding the diatreme formation, multiple mineral thermobarometers are applied. The data indicate that HT1 veins were formed at temperatures > 700 °C. HT2 veins host assemblages of polyphase brine inclusions, generally coexisting with low-density vapor-rich inclusions, trapped at temperatures around 600 °C. Rhyolitic silicate melt inclusions found in both HT1 and HT2 veins represent melt droplets transported by the ascending hydrothermal fluids. LA-ICP-MS analyses reveal a chemical evolution coherent with the crystallization of an evolved rhyolitic melt. Quartz from both HT1 and HT2 veins

Charnockitic ortho gneisses and mafic granulites of Cerro Olivo complex, proterozoic basement of SE Uruguay, Part 1: Geology

International Nuclear Information System (INIS)

Masquelin, H.

2008-01-01

Charnockitic ortho gneisses and mafic granulite s exposed in the Cerro Bori Block, in the center of Punta del Este terrain, were the first document occurrence of granulitic rocks from SE sector of the Uruguayan Shield. We present here their main geological features, with the purpose to suggest some petrologic and structural interesting problems for a future lithogeochemical, mineral chemistry, stable isotopes and fluid inclusion studies about these rocks. We propose some speculation form field-based studies considering a cognate magmatic origin of both kinds of rocks, previous to a homogeneous granulitic metamorphism. Some structural evidences indicate that after their uplift, these rocks were located on over thickened crust, at great to medium deepness. A cataclasis during anatexis and amphibolite-facies mineral association stabilization are common phenomena. Other evidences suggest a polycyclic character for the regional geologic evolution

Evaluation of the Cerro Solo nuclear ore, province of Chubut. On the economic parameters of the deposit. Pt. 3

International Nuclear Information System (INIS)

Navarra, P.R.; Sardin, P.G.; Urquiza, L.; Bernal, G.J.; Guzman Lobos, D.

1993-01-01

Preliminary results of the resources estimation carried out in the Cerro Solo uranium ore deposit, located in the Chubut Province, 1900 km SW from Buenos Aires and 380 Km W from Trelew, presented in tonnes of uranium recoverable at costs up to U$S 80/kgU, are as follows: a) Reasonable assured resources (indicated): 800 tU; b) Estimates Additional Resources (inferred): 2200 tU. Economic evaluation at the order-of-magnitude level, performed using the grade-tonnage model of the deposit, resulted a useful tool in the different stages of the project to identify the influence of technical parameters on the potential profitability. Research about feasibility of in-situ leaching method of exploitation for this deposit introduces an interesting alternative for future uranium production in the country. (Author)

Age and kinematics of ductile deformation in the Cerro Durazno area, NW Argentina: Significance for orogenic processes operating at the western margin of Gondwana during Ordovician-Silurian times

OpenAIRE

M. I. Wegmann; U. Riller; F. D. Hongn; Johannes Glodny; Onno Oncken

2008-01-01

The Cerro Durazno Pluton belongs to a suite of Paleozoic granitoid intrusions in NWArgentina, that are central for understanding the tectonic setting of the western margin of Gondwana in Ordovician and Silurian times. The pluton and its host rocks were tectonically overprinted by metamorphic mineral shape fabrics formed under middle greenschist-facies metamorphic conditions and associated with the nearby Agua Rosada Shear Zone. Kinematic analysis of the shear zone based on the geometric relat...

IMPACT OF ADDITIONALS CONTAMINANTS DUE TO ACID MINE DRAINAGE IN TRIBUTARIES OF THE PILCOMAYO RIVER FROM CERRO RICO, POTOSÍ, BOLIVIA

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William H.J. Strosnider

2014-09-01

Full Text Available Intensive mining and processing of the polymetallic sulfide ore body of Cerro Rico de Potosí (Bolivia has occurred since 1545. To further investigate acid mine drainage (AMD discharges and their link to downstream contamination, data were gathered during two sampling events during the most extreme periods of the dry and wet seasons of one year. Concentrations of Ag, B, Ba, Mo, Sb, Se, Sn and V in AMD and receiving streams were greater than Bolivian discharge limits and receiving water body guidelines as well as international agricultural use standards. High concentrations of rare earth metals have been documented in this area. Results indicate that contamination from mining has a larger scope than previously thought and underscore the importance of remediation.

EMPLEO DEL PROGRAMA VOLCFLOW PARA SIMULAR FLUJOS PIROCLÁSTICOS DEL VOLCÁN CERRO MACHÍN, TOLIMA, COLOMBIA

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Elsa Adriana Cárdenas Quiroga

2013-01-01

Full Text Available Se presentan los resultados de simular futuros flujos piroclásticos que podría producir el Volcán Cerro Machín, ubicado en la Cordillera Central de Colombia. Esta simulación se realizó con el programa VolcFlow desarrollado por el Laboratorio de Magmas y Volcanes de la Universidad Blaise Pascal, Francia, diseñado especialmente para modelar el comportamiento de este tipo de productos volcánicos, ya que está basado en las características reológicas de esos flujos. Se comparan las áreas que serían potencialmente afectadas por una erupción de ese tipo y los espesores del material que se depositaría con resultados obtenidos de simulaciones realizadas con un Model Builder desarrollado en ARC GIS por el Grupo de Investigación Geomática Aplicada de la Universidad Militar Nueva Granada en Colombia, obteniéndose resultados similares.

Geographic Information System (GIS) Emergency Support for the May 2000 Cerro Grande Wildfire, Los Alamos, New Mexico, USA

Energy Technology Data Exchange (ETDEWEB)

C.R.Mynard; G.N.Keating; P.M.Rich; D.R. Bleakly

2003-05-01

In May 2000 the Cerro Grande wildfire swept through Los Alamos, New Mexico, burning approximately 17,400 ha (43,000 acres) and causing evacuation of Los Alamos National Laboratory (LANL) and the communities of Los Alamos and White Rock. An integral part of emergency response during the fire was the use of geographic information system (GIS) technology, which continues to be used in support of post-fire restoration and environmental monitoring. During the fire Laboratory GIS staff and volunteers from other organizations worked to produce maps and provide support for emergency managers, including at an emergency GIS facility in Santa Fe. Subsequent to the fire, Laboratory GIS teams supported the multiagency Burned Area Emergency Rehabilitation (BAER) team to provide GIS data and maps for planning mitigation efforts. The GIS teams continue to help researchers, operations personnel, and managers deal with the tremendous changes caused by the fire. Much of the work is under the auspices of the Cerro Grande Rehabilitation Project (CGRP) to promote recovery from fire damage, improve information exchange, enhance emergency management, and conduct mitigation activities. GIS efforts during the fire provided important lessons about institutional matters, working relationships, and emergency preparedness. These lessons include the importance of (1) an integrated framework for assessing natural and human hazards in a landscape context; (2) a strong GIS capability for emergency response; (3) coordinated emergency plans for GIS operations; (4) a method for employees to report their whereabouts and receive authoritative information during an evacuation; (5) GIS data that are complete, backed-up, and available during an emergency; (6) adaptation of GIS to the circumstances of the emergency; (7) better coordination in the GIS community; (8) better integration of GIS into LANL operations; and (9) a central data warehouse for data and metadata. These lessons are important for planning

Estudio de la Orientación Cristalográfica Preferente del Cuarzo en el Contacto entre Gneises y Metatexitas - Diatexitas del Macizo Cerro Pelado (Sierra de Comechingones, Argentina)

OpenAIRE

Castellarlni, P.; Fernández Rodríguez, Carlos; Otamendi, Juan E.

2003-01-01

The quartz c-axis fabrics measured in the rocks of the high-grade unit of the Cerro Pelado massif (northern Sierra de Comechingones, Sierras Pampeanas, Argentina) allow to deduce a normal-sinistral sense of movement for the south-dipping shear zone separating the diatexite-metatexite domain to the north, from the gneissic terrane to the south. The crystallographic fabrics also indicate that the activity of this shear zone took place under high-T conditions. The deduced kinematics can account ...

Mineralogical and micro-thermometric features of the Los Humeros geothermal reservoir, Pue., Mexico; Caracteristicas mineralogicas y microtermometricas del yacimiento geotermico de Los Humeros, Pue., Mexico

Energy Technology Data Exchange (ETDEWEB)

Izquierdo, Georgina; Arellano, Victor M; Aragon, Alfonso [Instituto de Investigaciones Electricas, Cuernavaca, Morelos (Mexico)]. E-mail: gim@iie.org.mx

2008-07-15

Studies on many topics have been undertaken during the exploratory and exploitation stages of the development of Los Humeros geothermal field. From a geochemical and mineralogical view-including hydrothermal mineralogy and fluid-inclusion micro-thermometry, features have been reported differing from those observed in other geothermal fields. Sometimes this has led to ambiguous conclusions. Studies of fluid-inclusion micro-thermometry have shown low-salinity and high-temperature fluids, suggesting a slight temperature decrease in the deepest portion associated with a boiling process rather than a cooling process. In 1998, Arellano et al. performed a multi-disciplinary study and proposed the existence of at least two, distinct reservoirs at depth. Mineralogical data from wells drilled at the Colapso Central zone tend to support this idea. However wells drilled in the zone known as Corredor Mastaloya seemingly show evidence of a single reservoir. [Spanish] Durante las etapas de exploracion y explotacion del campo geotermico de Los Humeros se han realizado diversos estudios cubriendo distintos topicos. Desde el punto de vista geoquimico y mineralogico (mineralogia hidrotermal y microtermometria de inclusiones fluidas) se han reportado comportamientos diferentes a los observados en otros campos del mundo, los que en ocasiones han llevado a conclusiones imprecisas. La microtermometria de inclusiones fluidas ha mostrado fluidos poco salinos de alta temperatura, asi como una ligera disminucion de temperatura en la parte profunda la cual se asocia a un proceso de ebullicion mas que a un enfriamiento del sistema. En 1998 Arellano et al realizaron un estudio multidisciplinario proponiendo la existencia de al menos dos reservorios. La informacion mineralogica de pozos perforados en la zona del Colapso Central fortalece esta propuesta. Sin embargo, para pozos localizados en la zona conocida como Corredor Mastaloya se tiene evidencia de lo que parece ser un solo yacimiento.

New mammalian records in the Parque Nacional Cerros de Amotape, northwestern Peru

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Cindy M. Hurtado

2015-04-01

Full Text Available The Pacific Tropical Rainforest and Equatorial Dry Forest are found only in southern Ecuador and northern Peru, and are among the most poorly known ecosystems of South America. Even though these forests are protected in Parque Nacional Cerros de Amotape (PNCA, they are threatened by fragmentation because of farming and agriculture. The aim of this study was to determine the medium and large mammalian species richness, using transect census, camera trapping, and specimen bone collection. Nine transects were established and 21 camera trap stations were placed along 16 km2 in three localities of PNCA, from August 2012 to April 2013. Total sampling effort was 215 km of transects and 4077 camera-days. We documented 22 species; including 17 with camera trapping, 11 with transect census, and 10 with specimen collection.  Camera traps were the most effective method, and four species (Dasyprocta punctata, Cuniculus paca, Leopardus wiedii and Puma concolor were documented only with this method. This comprised the first Peruvian record for Dasyprocta punctata, and the first record for the western slope of the Peruvian Andes for Cuniculus paca. Also, both specimen collections and sightings confirm the presence of Potos flavus, first record in the western slope of the Peruvian Andes. Panthera onca, Tremarctos ornatus and Saimiri sciureus are considered locally extinct, while several species are in need of further research. We highlight the importance of the high diversity of this rainforests and encourage local authorities to give the area the highest priority in conservation.

Gestión del agua subterránea en el Barrio Cerro Los Leones de Tandil (Argentina

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Corina Iris Rodriguez

2010-01-01

Full Text Available En este trabajo se describen y analizan los actores y modos de explotación y uso involucrados en la gestión del recurso hídrico subterráneo en un barrio periférico de Tandil -Cerro Los Leones- (Provincia de Buenos Aires, Argentina, que carece de servicios de agua potable y cloacas. Estudios previos demostraron contaminación química y bacteriológica del agua que pone en riesgo la salud de la población. Se caracterizan los modos de uso y explotación del agua, señalando importantes defi ciencias en el diseño, construcción y mantenimiento de perforaciones y sistemas de disposición de efl uentes. Ante la necesidad y el desafío de la gestión integrada del recurso, se plantean linea mientos tendientes a su sustentabilidad, referidos a la planifi cación del uso, el abastecimiento de agua potable, el diseño de perforaciones y la educación ambiental.

El patrimonio industrial petrolero en la Patagonia: Comodoro Rivadavia (Argentina y Cerro Sombrero (Chile. Una perspectiva comparada

Directory of Open Access Journals (Sweden)

Pía Acevedo Méndez

2016-01-01

Full Text Available El hallazgo de petróleo en Comodoro Rivadavia (Chubut, Argentina y en Manantiales (Tierra del Fuego, lado chileno, motivó la construcción de espacios socioproductivos bajo el modelo de Company Towns. En el caso argentino la empresa estatal Yacimientos Petrolíferos Fiscales (Y.P.F creó el Campamento Central y la Empresa Nacional del Petróleo (ENAP creó Cerro Sombrero en Chile, los que en la década de 1970 formaron dos tejidos urbanos (barrio en el caso argentino y pueblo en el caso chileno. En esta dinámica se transformó el modo de habitar de ambos espacios, que se convirtieron en potenciales elementos turísticos, teniendo en cuenta que desde el año 2014 poseen reconocimiento patrimonial relacionado con su pasado petrolero y su arquitectura moderna. El objetivo es comparar cómo ambas empresas petroleras estatales construyeron dichos espacios “urbanos” y sus comunidades sociolaborales e indagar en la relación identidad/ patrimonio de ypefeanos y enapinos.

Cambio del uso de la tierra y pérdida de la cobertura boscosa, comunidades agrarias Sechina, La Ensenada y Cerro San Gil, Izabal Guatemala

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Eddi Alejandro Vanegas Chacón

2016-07-01

Full Text Available En Guatemala, pocas temáticas son abordadas con tanta pasión como el acceso a la tierra y sus relaciones de productividad. Ante el juicio histórico y la evidencia de las estadísticas se deslumbra que las políticas agrarias de los últimos cincuenta años, si bien mitigaron la pobreza en el agro rural conllevaron con ellas daños ambientales irreversibles y deudas agrarias millonarias. Se estudió la dinámica del cambio de uso de la tierra y la pérdida de la cobertura boscosa en las comunidades agrarias beneficiadas por la Ley de Transformación Agraria, Sechina, La Ensenada y Cerro San Gil ubicadas en el departamento de Izabal. Se utilizó fotointerpretación y se realizaron estudios semidetallados de la intensidad de la tierra para el periodo 1958 a 2010. Se concluyó que bajo las premisas de “mejora a la tierra” de la Ley de Transformación Agraria ocurrió cambio de uso y cobertura de la tierra, de forestal a agropecuaria, en las comunidades agrarias Sechina 42%, La Ensenada 46,2% y Cerro San Gil 48,6%, donde se promovieron sistemas de aprovechamiento agrícola que conllevaron al sobre-uso de las tierras en 42%, 78% y 30%, respectivamente. Esto sugiere, que la adquisición de la tierra no es el fin, más bien es el medio, para promover desarrollo rural sostenible, a través de acompañamiento técnico agropecuario, monitoreo y evaluación tanto económica como ambiental.

Experiences in the use of an electronic tool to measure pressure, temperature and spinner logs in the Mexican geothermal fields; Experiencias en el uso de sondas electronicas de presion, temperatura y flujo en campos geotermicos de Mexico

Energy Technology Data Exchange (ETDEWEB)

Flores Armenta, Magaly; Jaimes Maldonado, Guillermo [Gerencia de Proyectos Geotermoelectricos, Comision Federal de Electricidad, Morelia, Michoacan (Mexico)

1999-08-01

In this article are exposed the results of an electronic tool to measure pressure-temperature and spinner profiles in the geothermal wells of Mexico, utilized in order to identify unobservable phenomena with traditional Kuster type pressure and temperature logs. Some examples of the applications are the identifications of production zones, interaction from between two or more zones of contribution under several conditions of operation, casing damages and apparition of sink flow intervals into the formation in producer wells. It is also presented the quantitative method utilized to calculate the masic contribution of the intervals of interest. [Spanish] En este articulo se exponen los resultados obtenidos mediante el uso de una sonda electronica para la medicion de presion-temperatura y flujo en los pozos geotermicos de Mexico, utilizada para identificar fenomenos que no son observables con las mediciones tradicionales tipo Kuster de presion y temperatura. Se ejemplifican algunas de las aplicaciones hechas, tales como la identificacion de zonas de produccion, forma de interaccion entre dos o mas zonas de aporte bajo diferentes condiciones de operacion, roturas en tuberias y aparicion de zonas ladronas en pozos. Se presenta brevemente el metodo cuantitativo utilizado para calcular el aporte masico de las intervalos de interes.

Infection levels and seasonality of monogeneans in the largemouth bass Micropterus salmoides (Perciformes: Centrarchidae) from Nuevo León, Mexico.

Science.gov (United States)

Galaviz-Silva, L; Iruegas-Buentello, F J; Escobar-González, B; Molina-Garza, Z J

2016-11-01

Largemouth bass, Micropterus salmoides, is a native fish species with special importance for sport fishing competitions in Nuevo León, Mexico. However, no study has investigated the parasitic fauna of M. salmoides, and no reports are available on monogenean parasites in this fish species. Therefore, we described the monogenean parasites of M. salmoides and the effects of season and fish condition factor in five reservoirs: La Boca (LB), El Cuchillo-Solidaridad (CS), Sombreretillo (S), Laguna Salinillas (LS) and Cerro Prieto (CP). The monogeneans infecting M. salmoides were Clavunculus unguis and Acolpenteron ureteroecetes (collected in all localities), as well as Syncleithrium fusiformis, Haplocleidus furcatus, Clavunculus bifurcatus and Urocleidus principalis (CS). Clavunculus unguis had the highest prevalence in fish from all reservoirs. The abundance of monogeneans was generally greater in late spring to autumn than in winter. Although season was not correlated with abundance (r s = 0.0934, P <  0.0154), the months of highest temperature (from May to September) were positively correlated with parasite abundance. A significant association was observed between fish condition factor and the presence of monogeneans (P <  0.05), except for A. ureteroecetes. Our findings include five new geographic records for C. unguis, S. fusiformis, H. furcatus and C. bifurcatus.

State-of-the-art of liquid waste disposal for geothermal energy systems: 1979. Report PNL-2404

Energy Technology Data Exchange (ETDEWEB)

Defferding, L.J.

1980-06-01

The state-of-the-art of geothermal liquid waste disposal is reviewed and surface and subsurface disposal methods are evaluated with respect to technical, economic, legal, and environmental factors. Three disposal techniques are currently in use at numerous geothermal sites around the world: direct discharge into surface waters; deep-well injection; and ponding for evaporation. The review shows that effluents are directly discharged into surface waters at Wairakei, New Zealand; Larderello, Italy; and Ahuachapan, El Salvador. Ponding for evaporation is employed at Cerro Prieto, Mexico. Deep-well injection is being practiced at Larderello; Ahuachapan; Otake and Hatchobaru, Japan; and at The Geysers in California. All sites except Ahuachapan (which is injecting only 30% of total plant flow) have reported difficulties with their systems. Disposal techniques used in related industries are also reviewed. The oil industry's efforts at disposal of large quantities of liquid effluents have been quite successful as long as the effluents have been treated prior to injection. This study has determined that seven liquid disposal methods - four surface and three subsurface - are viable options for use in the geothermal energy industry. However, additional research and development is needed to reduce the uncertainties and to minimize the adverse environmental impacts of disposal. (MHR)

Chemical changes in well fluids from the Los Humeros geothermal field: Evidences for deep recharge; Cambios quimicos en fluidos de pozos del campo geotermico de Los Humeros: Evidencia de recarga profunda

Energy Technology Data Exchange (ETDEWEB)

Barragan Reyes, Rosa Maria; Arellano Gomez, Victor Manuel [Instituto de Investigaciones Electricas, Gerencia de Geotermia, Cuernavaca, Morelos (Mexico)]. E-mail: rmb@iie.org.mx; Flores Armenta, Magaly [Comision Federal de Electricidad, Gerencia de Proyectos Geotermoelectricos, Morelia, Michoacan (Mexico); Tovar Aguado, Rigoberto [Comision Federal de Electricidad (Mexico)

2008-07-15

Fluid (water and steam) chemical changes over time were studied in 20 wells in the Los Humeros, Mexico, geothermal field for the purpose of correlating such changes with physical processes occurring in the reservoir due to exploitation. Most wells (except well H-1) produce high-enthalpy fluids with almost no liquid, making gas geochemistry important in this field. Liquid-phase studies include fluid classification, determination of water-rock equilibrium state, and reservoir-temperature estimates. Changes in gas composition through time were studied using the Fischer-Tropsch (FT) reaction and the combined balance pyrite-hematite-magnetite (HSH2) as the buffer controlling H{sub 2}S fluid concentration. Data for most wells from 1987-1995 and 2000-2005 indicate the presence of deeper-fluid recharge, with maximum temperatures occurring in 1994-95 and 2005. The estimated temperature in well H-1 in 1994 was 305 degrees Celsius and the estimated temperature in well H-7 was 338 degrees Celsius in 1995. Temperature estimations from 2005 data were 222 degrees Celsius in well H-1D and 350 degrees Celsius in well H-7. These results are considered caused by the entrance of deeper fluids due to the increase of secondary permeability, which in turn is related to the seismicity increase in the zone. At the same time, re-injection returns in the steam phase were identified in well discharges during 1995-2000 by means of the FT-HSH2 diagram. [Spanish] Se realizo un estudio de los cambios quimicos ocurridos en fluidos (liquido y vapor) de veinte pozos del campo geotermico de Los Humeros, Pue., Mexico, con objeto de investigar la ocurrencia de procesos del yacimiento relacionados con la explotacion. La mayoria de los pozos (excepto el pozo H-1) se caracterizan por producir descargas de alta entalpia con escasa produccion de liquido, por lo que en este campo la geoquimica de gases juega un papel importante. El estudio de la fase liquida incluyo la clasificacion de los fluidos, la

Downwelling Far-Infrared Radiance Spectra Measured by FIRST at Cerro Toco, Chile

Science.gov (United States)

Mast, J. C.; Mlynczak, M. G.; Cageao, R.; Kratz, D. P.; Latvakoski, H.; Johnson, D. G.; Mlawer, E. J.; Turner, D. D.

2015-12-01

The Far-Infrared Spectroscopy of the Troposphere (FIRST) instrument is a Fourier transform spectrometer developed by NASA Langley Research Center in collaboration with the Space Dynamics Laboratory and the Harvard-Smithsonian Center for Astrophysics. FIRST was initially developed for measuring the far-infrared portion of Earth's longwave spectrum as a balloon borne instrument and later was reconfigured to operate as a ground-based instrument. In its current ground-based configuration FIRST was deployed at 17500 ft on Cerro Toco, a mountain in the Atacama Desert of Chile, from August to October, 2009. There the integrated precipitable water (IPW) was as low as 0.02 cm. FIRST measurements from days with IPW between 0.024 and 0.035 cm during the campaign are presented here between 200 cm-1 and 800 cm-1. Significant spectral development in the far-IR is observed over the entire 200 cm-1 to 800 cm-1 band. Water vapor and temperature profiles from radiosonde and GVRP measurements are used as inputs to the AER Line-by-Line Radiative Transfer Model (LBLRTM) utilizing the AER v3.2 line parameter database. Uncertainties in both the measured and modeled radiances are accounted for in this study. The residual LBLRTM - FIRST is calculated to assess agreement between the measured and modeled spectra. Measured and model radiances generally agree to within the combined uncertainties for wavenumbers greater than 360 cm-1. At wavenumbers less than 360 cm-1 persistent troughs in the residual are present outside of the combined uncertainties. These features are present on different days and at different water vapor amounts. Possible solutions for these features are discussed.

The CCAT-prime Extreme Field-of-View Submillimeter Telescope on Cerro Chajnantor

Science.gov (United States)

Koopman, Brian; Bertoldi, Frank; Chapman, Scott; Fich, Michel; Giovanelli, Riccardo; Haynes, Martha P.; Herter, Terry L.; Murray, Norman W.; Niemack, Michael D.; Riechers, Dominik; Schilke, Peter; Stacey, Gordon J.; Stutzki, Juergen; CCAT-prime Collaboration

2017-01-01

CCAT-prime is a six meter aperture off-axis submillimeter telescope that we plan to build at 5600m elevation on Cerro Chajnantor in Chile. The CCAT-prime optics are based on a cross-Dragone design with high throughput and a wide field-of-view optimized to increase the mapping speed of next generation cosmic microwave background (CMB) observations. These characteristics make CCAT-prime an excellent platform for a wide range of next generation millimeter and submillimeter science goals, and a potential platform for CMB stage-IV measurements. Here we present the telescope design for CCAT-prime and review the science goals.Taking advantage of the high elevation site, the first generation instrument for CCAT-prime will measure seven different frequency bands from 350um to 3mm. These seven bands will enable precise measurements of the Sunyaev-Zel’dovich effects (SZE) by separating contributions from CMB, thermal SZE, kinetic SZE, bright submm galaxies, and radio sources with a goal of extracting the peculiar velocities from a large number of galaxy clusters. Additional science priorities for CCAT-prime include: Galactic Ecology studies of the dynamic intersteller medium by mapping the fine structure lines [CI], [CII] and [NII] as well as high-excitation CO lines at the shortest wavelength bands; high redshift intensity mapping of [CII] emission from star-forming galaxies that likely dominates cosmic reionization at z~5-9 to probe the Epoch of Reionization; and next generation CMB polarization measurements to constrain inflation and cosmological models. The CCAT-prime facility will further our understanding of astrophysical processes from moments after the Big Bang to the present-day evolution of the Milky Way.

Sedimentología y estratigrafía de la Formación Vaca Muerta (Tithoniano-Berriasiano en el área del cerro Domuyo, norte de Neuquén, Argentina Sedimentology and stratigraphy of the Vaca Muerta Formation in the Cerro Domuyo area, Northern Neuquén, Argentina

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Diego A Kietzmann

2013-01-01

Full Text Available Los depósitos de la Formación Vaca Muerta en el área del cerro Domuyo muestran una interesante interca-laclón de depósitos con paleocorrientes opuestas. La unidad está representada por facies de cuenca y rampa externa con dirección de progradación hacia el oeste. Sin embargo, en su parte media se intercalan depósitos de talud, con desarrollo de deslizamientos sinsedimentarios hacia el NE, que pueden asignarse al Miembro Huncal. Este intervalo se compone de facies carbonáticas que probablemente se asocien con el desarrollo de un talud relacionado con una plataforma carbonática o una rampa distalmente profundizada. A partir de la fauna de amonites reconocida, la Formación Vaca Muerta se extiende desde el Tithoniano temprano hasta el Berriasiano tardío, aunque podría alcanzar el Valanginiano temprano. El Miembro Huncal contiene representantes de la Biozona de Substeueroceras koeneni (Tithoniano tardío, por lo que su edad sería más antigua que la propuesta en la localidad tipo y permitiría su correlación con las unidades aflorantes en el territorio chileno.The Vaca Muerta Formation in the Cerro Domuyo area shows an interesting intercalation of facies with opposite paleocurrents. The unit is represented by outer ramp to basinal facies with a westward direction of progradation. However, in its middle section, slope deposits correlatable with the Huncal Member, are intercalated with slumped strata verging NE. This interval is composed of carbonate facies and it is probably associated with the development of a slope related to a carbonate platform or a distally steepened carbonate ramp. Based on the ammonoid fauna, the age of the Vaca Muerta Formation ranges from the early Tithonian to the late Berriasian, but it could also reach the early Valanginian. The Huncal Member yields representatives of the Substeueroceras koeneni Biozone (late Tithonian, hence its age is older than that proposed in its type locality allowing its correlation

Chemical variations in the Cerro de Mercado (Durango, Mexico) fluorapatite: Assessing the effect of heterogeneity on a geochronologic standard.

Science.gov (United States)

Boyce, J. W.; Hodges, K. V.

2001-12-01

Despite the lack of an official pronouncement, the fluorapatite of Cerro de Mercado, Durango, Mexico has become the de facto standard for (U-Th)/He geochronology. In addition to being relatively inclusion-free and easily obtained, these crystals are commonly in excess of 5mm in diameter, permitting the removal of the outer skin of the crystal, theoretically eliminating the alpha-ejection correction. However, bulk analyses of the Durango fluorapatite indicate a substantial variation in U and Th concentrations from aliquot to aliquot (167-238 ppm Th; 9.7-12.3 ppm U, [1]). If similar variations were to occur on the sub-grain scale, small fragments of single crystals could contain helium excesses or deficiencies due to alpha-ejection exchange between zones with varying parent element content. We have performed a series of experiments to quantify the intra-grain variation in U and Th, in order to model the effect of this variation on ages determined on Durango fluorapatite. X-ray maps show concentric zonation in U and Th, with similar, but more apparently pronounced zonation in Si and Cl. Preliminary laser-ablation ICPMS data indicate, not surprisingly, that intra-grain variations in U and Th concentrations obtained by analysis of ~35 μ m spots are larger than that which had been previously obtained by bulk analytical techniques (with overall concentrations greater than for bulk analyses). Thus far, analyses yield U concentrations varying from 11 to 16 ppm, and Th concentrations ranging from 220 to 340 ppm. Modeling underway suggests that parent element variations on the order of 50%, such as those observed, and the resulting differential alpha-exchange could lead to several percent error in age, for ~100 μ m fragments. The effect scales inversely with fragment size, with 300 μ m fragments (roughly the size of a large, single grain analysis) having only ~1% error. This may offer an explanation for the previously observed inability to reproduce ages for the Durango

NUEVOS APORTES AL CONOCIMIENTO DE LA HERPETOFAUNA DE LA FORMACIÓN CERRO AZUL (MIOCENO SUPERIOR, PROVINCIA DE LA PAMPA, ARGENTINA

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AGUSTÍN SCANFERLA

2015-01-01

Full Text Available RESUMENSe describen nuevos materiales fósiles de anfibios y reptiles hallados en sedimentos referidos a la Formación Cerro Azul (Mioceno Superior, procedentes de numerosas localidades de la provincia de La Pampa, Argentina. Los nuevos registros se basan en un resto craneano de anuro asignado al géneroCeratophrys, restos de caparazón de tortugas terrestres del géneroChelonoidis, vértebras asignables al lagarto de la familia TeiidaeTupinambis, y una vértebra troncal de serpiente comparable al género de colubroideos actualesPhilodryas. Tanto los registros terciarios previos de géneros actuales de anfibios y reptiles en América del Sur, como así también la asociación recuperada en el Mioceno Superior de La Pampa sugieren que la mayoría de los géneros que componen la herpetofauna Neotropical estaban presentes en el Mioceno, patrón similar al observado en otras regiones del mundo.

Dieta de murciélagos nectarívoros del Parque Nacional Cerros de Amotape, Tumbes

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Edith Arias

2011-07-01

Full Text Available En el Perú se reporta la presencia de 18 especies de murciélagos nectarívoros, sin embargo se cuenta con poca información sobre la dieta de estas especies. En este estudio se reporta por primera vez la dieta de los nectarívoros Glossophaga soricina, Lonchophylla hesperia y Anoura geoffroyi en el bosque seco ecuatorial y del bosque tropical del Pacífico del Parque Nacional Cerros de Amotape, Tumbes. Analizamos 21 contenidos gastrointestinales e identificamos ocho morfotipos de polen pertenecientes a las familias Bombacaceae, Cactaceae, Fabaceae, Solanaceae, Rubiaceae, Myrtaceae, Malvaceae y Rosaceae. Encontramos evidencia del síndrome de quiropterofilia en Bombacaceae, Cactaceae, Fabaceae, Solanaceae y Rubiaceae. Observamos que A. geoffroyi consume polen de Ceiba trichistandra, Solanaceae y Rubiacea; G. soricina consume de Abutilon reflexum, Armathocereus cartwrightianus, C. trichistandra y Rubiaceae; y L. hesperia de A. cartwrightianus, Eriobotrya japonica, Fabaceae y Psidium sp.; sugiriendo una dieta generalista en estas especies. Los murciélagos G. soricina y A. geoffroyi comparten el consumo del ceibo C. trichistandra y de la Rubiaceae, mientras que G. soricina comparte con L. hesperia el consumo del cactus A. cartwrightianus. Los otros morfotipos de polen no fueron compartidos entre murciélagos. Se encuentra además que el ceibo C. trichistandra fue la especie más consumida, especialmente por G. soricina.

Petrological evolution of subducted rodingite from seafloor metamorphism to dehydration of enclosing antigorite-serpentinite (Cerro del Almirez massif, southern Spain)

Science.gov (United States)

Laborda-López, Casto; López Sánchez-Vizcaíno, Vicente; Marchesi, Claudio; Gómez-Pugnaire, María Teresa; Garrido, Carlos J.; Jabaloy-Sánchez, Antonio; Padrón-Navarta, José Alberto

2016-04-01

Rodingites are common rocks associated with serpentinites in exhumed terrains that experienced subduction and high pressure metamorphism. However, the response of these rocks to devolatilization and redox reactions in subduction settings is not well constrained. In the Cerro del Almirez ultramafic massif (southern Spain) rodingites constitute about 1-2% of the total volume of exposed rocks. Metarodingites are enclosed in antigorite-serpentinite and chlorite-harzburgite separated by a transitional zone that represents the front of prograde serpentinite-dehydration in a paleo-subduction setting (Padrón-Navarta et al., 2011). Metarodingites occur as boudin lenses, 1 to 20 m in length and 30 cm to 2 m in thickness. During serpentinization of peridotite host rocks, dolerites and basalts precursor of rodingites underwent intense seafloor metasomatism, causing the enrichment in Ca and remobilization of Na and K. Subsequent metamorphism during subduction transformed the original igneous and seafloor metamorphic mineralogy into an assemblage of garnet (Ti-rich hydrogrossular), diopside, chlorite, and epidote. During prograde metamorphism, garnet composition changed towards higher andradite contents. High-pressure transformation of enclosing antigorite-serpentinite to chlorite-harzburgite released fluids which induced breakdown of garnet to epidote in metarodingites. Ti liberation by this latter reaction produced abundant titanite. Released fluids also triggered the formation of amphibole by alkalis addition. Highly recrystallized metarodingites in chlorite-harzburgite present a new generation of idiomorphic garnet with composition equal to 10-30% pyrope, 30-40% grossular and 35-55% almandine + spessartine. This garnet has titanite inclusions in the core and rutile inclusions in the rim. The contact between metarodingites and ultramafic rocks consists of a metasomatic zone (blackwall) with variable thickness (7 to 40 cm) constituted by chlorite, diopside, and titanite

Distribución de las principales causas de morbilidad por ingresos domiciliarios en el municipio Cerro durante el año 2000

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Migdalia Rafaela Reyes Sigarreta

2003-04-01

Full Text Available Se hace un estudio, aplicando el método descriptivo cualitativo con una muestra representativa de las áreas de salud del municipio Cerro, de los ingresos en el domicilio de los pacientes adultos y niños en el año 2000 para determinar las causas de morbilidad y su distribución por cada área de salud. Para la recogida de información se utilizó como técnica fundamental la recolección de datos en formularios, utilizando como fuentes de información la hoja de trabajo de los médicos de los policlínicos y el registro de ingreso domiciliario. Los datos se analizan utilizando el tanto por ciento como medida de frecuencia y se presentan en tablas estadísticas. Se encontró que el mayor número de ingresos por área de salud correspondió al Policlínico "Antonio Maceo", tanto en adultos como en niños, y los meses de mayor ingreso en las áreas se corresponden con los meses de cambios climáticos, lo que se relaciona con las principales causas de morbilidad (las enfermedades respiratorias, las diarreicas y la hipertensión arterial.A descriptive qualitative study was carried out with a representative sample from the home care services given in the health areas of Cerro municipality to children and adults in the year 2000 to determine the morbidity causes and their distribution by health areas. For gathering information, the fundamental technique used was data collection in questionnaires and the worksheet of physicians working in various polyclinics and the home care service register as sources of information. The data analysis used percentage as a measure of frequency and such information was shown in statistical tables. It was found that the higher number of home care services by health area corresponded to "Antonio Maceo" polyclinics both in children and adults, and the time when more home care services were provided in the health areas was the months of climatic changes, which was related to the main causes of morbidity (respiratory

Estudio de los fundentes utilizados en la metalurgia del cobre en Cerro Muriano (Córdoba durante el período Romano Altoimperial

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Criado, A. J.

1996-10-01

Full Text Available There are no doubts that Hispania was, under the Roman Empire, the most profitable and abundant in resources of all the mining districts exploded by Rome -Hispania, Galia, Danubian Provinces, Dacia, Greece, Asia Minor, Syria, Egypt and North Africa-. Plinius gives the same data and hands many more in the passages dedicated to the mining and the working of the metals in his Natural History. Of all the many mining places that this author refers, the exploiting in copper at Cerro Muriano presents the main interest; of this he says that it was of an unbeatable quality, used, among other applications, to manufacture the very famous "Copper of Campania". The utilization of fusing agents, adapted to the process of copper obtainment, is fundamental for obtaining this high quality. The addition of these fusing agents was very important for the control of the work parameters and to reach the required temperatures. The high purity of the obtained copper shows a very close knowledge of the phenomena involved in the process.

Durante el Imperio Romano, de todos los distritos mineros explotados por Roma -Hispania, Galia, las provincias danubianas, Dacia, Grecia, Asia Menor, Siria, Egipto y el Norte de África-, sin duda el más rentable y más abundante en recursos era Hispania. Plinio facilita muchos datos en los pasajes dedicados a la minería y el trabajo de los metales en su Historia Natural. Entre los muchos lugares mineros que este autor cita, nos interesa ahora la explotación de cobre en Cerro Muriano, del cual dice que era de una calidad inmejorable, utilizado, entre otras aplicaciones, para fabricar el famosísimo cobre de Campania. Para poder obtener esta elevada calidad, es fundamental la utilización de fundentes adecuados en el proceso de obtención de cobre. La adición de estos fundentes era vital para controlar los parámetros de trabajo y alcanzar las temperaturas requeridas. La elevada pureza del cobre obtenido demuestra un

Evaluación ambiental de las condiciones de explotación y uso del recurso hidríco subterráneo en el Barrio Cerro Los Leones, Tandil

OpenAIRE

Rodríguez, Corina Iris

2009-01-01

Se basa esta investigación en la evaluación ambiental de las condiciones de explotación y uso del recurso hídrico subterráneo en el Barrio Cerro Los Leones, ubicado al Oeste de la ciudad de Tandil, en el centro-SE de la provincia de Buenos Aires. El interés por dicho sector surgió a partir de las falencias en la provisión de agua potable y servicios sanitarios. El objetivo principal consistió en la generación de pautas de gestión sustentable basadas en el análisis y evaluación del sistema sub...

Woodland diagnosis of ecological reserve "Cerro de Amalucan" in the City of Puebla, México

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Francisco Domínguez Hernández

2016-12-01

Full Text Available Trees in urban parks play a key role in the sustainability of cities. The tree is urban landscape of a city, provides environmental, aesthetic, scenic, recreational, cultural and economic benefits. The obwas to study the current state of woodland in the Cerro de Amalucan Ecological Reserve in the city of Puebla, Mexico, a forest dasometric diagnosis was applied by sampling in the area. Settling 17 sampling sites area of 1000 m2, completely randomized design with dasometric data. The results were averaged 183.5 trees per hectare, the most dominant Eucalyptus sp with 61.5% of actual stocks species. Following the species Cupressus lindleyi with 22.2%. Subsequently, the species Juniperus deppeana, with 6.8%, and the species Ipomoea murocoides, which had 2.9% of the total population, like the species polystachya Eysenhardtia, continuing the species flaccid Juniperus, with 1.6%, followed Cupressus sempervirens with 0.96%, Casuarina equisetifolia, with 0.64%, finally Pinus patula with 0.64%. Are cataloged as exotic tree species the next in line: Eucalyptus sp, and Casuarina equisetifolia, Cupressus lindleyi, Cupressus semprevirens and Pinus patula and were characterized as native species: Juniperus deppeana Eysenhardtia polystachya, Juniperus flacida. The areas are to manage 20 hectares with reforestation for restoration, on 75 hectares’ protection is carried out in areas prone to invasion and species conservation and recreation area with 40 hectares for hiking, ecological tours, bike paths and recreation.

Origin and evolution of mineralizing fluids and exploration of the Cerro Quema Au-Cu deposit (Azuero Peninsula, Panama) from a fluid inclusion and stable isotope perspective

Science.gov (United States)

Corral, Isaac; Cardellach, Esteve; Corbella, Merce; Canals, Angels; Griera, Albert; Gomez-Gras, David; Johnson, Craig A.

2017-01-01

Cerro Quema is a high sulfidation epithermal Au-Cu deposit with a measured, indicated and inferred resource of 35.98 Mt. @ 0.77 g/t Au containing 893,600 oz. Au (including 183,930 oz. Au equiv. of Cu ore). It is characterized by a large hydrothermal alteration zone which is interpreted to represent the lithocap of a porphyry system. The innermost zone of the lithocap is constituted by vuggy quartz with advanced argillic alteration locally developed on its margin, enclosed by a well-developed zone of argillic alteration, grading to an external halo of propylitic alteration. The mineralization occurs in the form of disseminations and microveinlets of pyrite, chalcopyrite, enargite, tennantite, and trace sphalerite, crosscut by quartz, barite, pyrite, chalcopyrite, sphalerite and galena veins.Microthermometric analyses of two phase (L + V) secondary fluid inclusions in igneous quartz phenocrysts in vuggy quartz and advanced argillically altered samples indicate low temperature (140–216 °C) and low salinity (0.5–4.8 wt% NaCl eq.) fluids, with hotter and more saline fluids identified in the east half of the deposit (Cerro Quema area).Stable isotope analyses (S, O, H) were performed on mineralization and alteration minerals, including pyrite, chalcopyrite, enargite, alunite, barite, kaolinite, dickite and vuggy quartz. The range of δ34S of sulfides is from − 4.8 to − 12.7‰, whereas δ34S of sulfates range from 14.1 to 17.4‰. The estimated δ34SΣS of the hydrothermal fluid is − 0.5‰. Within the advanced argillic altered zone the δ34S values of sulfides and sulfates are interpreted to reflect isotopic equilibrium at temperatures of ~ 240 °C. The δ18O values of vuggy quartz range from 9.0 to 17.5‰, and the δ18O values estimated for the vuggy quartz-forming fluid range from − 2.3 to 3.0‰, indicating that it precipitated from mixing of magmatic fluids with surficial fluids. The δ18O of kaolinite ranges from 12.7 to 18.1‰ and �

Addition of schelita residue from the mine in Cerro Cora Bodo / RN in the composition of ceramic materials; Adicao de residuo de scheelita da mina Bodo em Cerro Cora/RN na composicao de materiais ceramicos

Energy Technology Data Exchange (ETDEWEB)

Almeida, A.B.D. de; Souza, M. M. de; Farias, D.S.U. de; Lima, T.C. de; Nobrega, L.F.P. de M. [Instituto Federal de Ciencia e Tecnologia do Rio Grande do Norte (IFRN), RN (Brazil); Mendes, L.B., E-mail: anabeatriz.d.a@outlook.com [Fundacao de Apoio a Pesquisa do Rio Grande do Norte (FAPERN), Natal RN (Brazil)

2016-07-01

Mining activities produce mineral waste that can degrade the environment. The waste generated by companies is not reused due to the fact they fail to present an application for it that proves to be economically viable. Seeking the reuse of mineral waste and reduce the environmental impacts, this work addresses the chemical characterization by x-ray fluorescence (FRX), of the processing of scheelite reject at Bodo mine in Cerro Cora-RN. For the procedure, the sample was collected, grounded and sieved to #200, and then characterized to evaluate its chemical composition and its potential to be incorporated into materials. Besides the characterization, a water absorption test and also a bending test were performed to analyze the power and tension of the material. The result of the analysis indicated that the sample researched presents a greater concentration of SiO{sub 2} to be used as a structuring element in ceramic mass, but in the traditional formulation, it will only be added 10% of the reject in its formulation, because besides the SiO{sub 2} in the sample analyzed other elements that act with fluxes were found. It was also observed the material has low water absorption, but the reject reached low strength and breakdown voltage. We concluded that the reject of scheelite presents great potential, and therefore, further tests can be conducted to analyze the possibility of being added as raw material for the formulation of other materials like cement. (author)

Symposium in the field of geothermal energy

Energy Technology Data Exchange (ETDEWEB)

Ramirez, Miguel; Mock, John E.

1989-04-01

Mexico and the US are nations with abundant sources of geothermal energy, and both countries have progressed rapidly in developing their more accessible resources. For example, Mexico has developed over 600 MWe at Cerro Prieto, while US developers have brought in over 2000 MWe at the Geysers. These successes, however, are only a prologue to an exciting future. All forms of energy face technical and economic barriers that must be overcome if the resources are to play a significant role in satisfying national energy needs. Geothermal energy--except for the very highest grade resources--face a number of barriers, which must be surmounted through research and development. Sharing a common interest in solving the problems that impede the rapid utilization of geothermal energy, Mexico and the US agreed to exchange information and participate in joint research. An excellent example of this close and continuing collaboration is the geothermal research program conducted under the auspices of the 3-year agreement signed on April 7, 1986 by the US DOE and the Mexican Comision Federal de Electricidad (CFE). The major objectives of this bilateral agreement are: (1) to achieve a thorough understanding of the nature of geothermal reservoirs in sedimentary and fractured igneous rocks; (2) to investigate how the geothermal resources of both nations can best be explored and utilized; and (3) to exchange information on geothermal topics of mutual interest.

Seismologic study of Los Humeros geothermal field, Puebla, Mexico. Part II: Seismic tomography by attenuation of coda waves (Qc-1) of local earthquakes; Estudio sismologico del campo geotermico de Los Humeros, Puebla, Mexico. Parte II: Tomografia sismica por atenuacion a partir de ondas de coda (Qc-1) de sismos locales

Energy Technology Data Exchange (ETDEWEB)

Antayhua, Yanet; Lermo, Javier [Instituto de Ingenieria, Universidad Nacional Autonoma de Mexico, D.F (Mexico); Carlos, Vargas [Departamento de Geociencias, Universidad Nacional de Colombia (Colombia)]. E-mail: jles@pumas.iingen.unam.mx

2008-07-15

In the Los Humeros geothermal field, Puebla, seismic tomography has been studied using the attenuation of coda waves (Qc{sup -1}). Ninety-five local earthquakes (Md{<=}3.6) have been used with depths up to 4.0 km registered in the seismic network stations from December 1997 to December 2004. A simple backscattering model was used, filtered in four ranks of frequencies (2, 4, 6, and 8 Hz) and one window of 5 seconds. For the 3D-representation, we used an approximation based on first-order scattering of ellipsoids. The results show that values of Qc for the used frequencies have a frequency dependency shown in the equation: Qc=24{+-}12f{sup 0.86}{+-}{sup 0.06}, where the low values of Qc were observed in the zone of higher seismic and tectonic activity and in the location of injection and production wells. The high values are located in the periphery of the geothermal field. The distribution of the Qc{sup -1} attenuation in 3D and 2D shows the anomalies of high-seismic attenuation are located in the north, south, and southwestern ends of the zone presently under operation, at depths greater than 2.5 km. [Spanish] Para realizar la tomografia sismica por atenuacion de ondas de coda (Qc{sup -1}) en el campo geotermico de Los Humeros, Puebla, se han utilizado 95 sismos locales (Md{<=}3.6) con profundidades hasta 4.0 km, registrados en las estaciones de su red sismica, durante el periodo de diciembre 1997 a diciembre 2004. Se utilizo el modelo de retrodispersion simple, filtrados en cuatro rangos de frecuencias (2, 4, 6, y 8 Hz) y una ventana de 5 segundos. Para la representacion en 3D, se utilizo una aproximacion basada en elipsoides que representan dispersion de primer orden. Los resultados muestran que los valores de Qc para las frecuencias utilizadas tienen una dependencia con la frecuencia de la forma: Qc=24{+-}12f{sup 0.86}{+-}{sup 0.06}, donde los valores bajos de Qc fueron observados en la zona de mayor actividad sismica y en la ubicacion de pozos inyectores y

Evaluación de la contaminación por metales en pasivos ambientales de actividades metalúrgicas históricas en el distrito minero Cerro de San Pedro, S.L.P. (México)

OpenAIRE

Rodríguez y Rodríguez, Yolanda

2011-01-01

Pasivos ambientales minero-metalúrgicos son frecuentemente encontrados en regiones donde estas actividades se han desarrollado históricamente, como es el caso del Estado de San Luis Potosí, en donde desde el siglo XVI han existido importantes centros mineros, destacando entre ellos el Distrito Minero de Cerro de San Pedro que se localiza en la porción centro-sur del Estado, 19.5 kilómetros al NW de la ciudad de San Luis Potosí. La situación geográfica del sitio donde se descubriero...

Proceedings of the Annual National Conference on ADA Technology (9th) Held in Washington, DC on 4-7 March 1991

Science.gov (United States)

1991-03-07

have three daughters: Gia, Sheri 1980, he returned to Air Force and Alicia . headquarters as Chief of the Joint Matters Group, Directorate of Command...process in the GSFC environment-- it is by developer choice rather than Prieto- Diaz (1990) discusses the management directive, thus the developers...Prieto- Diaz , R. 1990. Implementing Faceted Cavaliere, M.J. 1989. Reusable Code at Classification for Software Reuse. In the Hartford Insurance Group

Economic, environmental and social impacts of geothermal development, and energy savings and efficient use of power in Baja California, Mexico; Impactos economicos, ambientales y sociales del desarrollo geotermico y del ahorro y uso eficiente de la electricidad en Baja California, Mexico

Energy Technology Data Exchange (ETDEWEB)

Campbell R, Hector E.; Montero A, Gisela [Universidad Autonoma de Baja California, Instituto de Ingenieria, Mexicali, Baja California (Mexico)]. E-mail: hecr@iing.mxl.uabc.mx; Lambert A., Alejandro A. [Universidad Autonoma de Baja California, Facultad de Ingenieria, Mexicali, Baja California (Mexico)

2011-01-15

geotermico a combustoleo hacia 1 a 1 de geotermia a gas natural. El costo unitario de energia del gas natural con una eficiencia de 50% es 24 veces el costo de la misma unidad de vapor geotermico con 16% de eficiencia. Generar con combustoleo o gas natural en turbinas simples cuesta el doble que con gas natural en ciclo combinado, mientras que con vapor geotermico cuesta tres veces menos. Al disminuir la participacion geotermica los costos de produccion de electricidad se incrementaron para llegar en 2005 a 122.80 USD/MWh. La salida del combustoleo disminuyo las emisiones de SO{sub x} de 4.16 kg/MWh a 0.19 kg/MWh. Los ciclos combinados con gas natural abatieron las emisiones relativas de NO{sub x} y CO{sub 2} en 30%, pero las 2.6 millones de toneladas anuales de CO{sub x} no variaron significativamente. La geotermia evita que se quemen anualmente 20 millones de barriles equivalentes de petroleo. La Prospectiva 2005-2025 implica para Baja California instalar 4500 MW adicionales para alcanzar 7200 MW. La matriz energetica se transformara dependiendo mas del gas natural que incrementara su participacion del 60% al 86%. La geotermia disminuira su participacion en la capacidad instalada al 10%, eliminando su efecto amortiguador en el costo de produccion. Las emisiones de SO{sub x} se mantendran en 2,200 toneladas por ano (t/a) emitiendose principalmente por la geotermoelectricidad, las de NO{sub x} aumentaran de 6,000 t/a en 2005 a 24,000 t/a en 2025, y las de CO{sub x} se incrementaran de 3.4 millones de t/a en 2005 a 12.7 millones de t/a en 2025. El costo de generacion sera afectado por los cambios en la matriz energetica al predominar el uso del gas natural. En terminos absolutos aumentara de 648 millones de dolares en 2005 a 2273 millones de dolares en 2025. El costo de generacion dependera en 70% del uso de gas natural. En la Planeacion Sistemica las metas planteadas se orientaron a: a) reducir los usos propios en los procesos de generacion, b) reducir los usos propios y las

“La parte alta del cerro es para los pequeños mineros”. Sobre la vigencia del régimen minero especial para Marmato y su influencia en la construcción de territorialidad

Directory of Open Access Journals (Sweden)

Gloria Patricia Lopera Mesa

2015-12-01

Full Text Available Este artículo examina las circunstancias que motivaron la expedición de un régimen especial para las minas de Marmato a mediados del siglo XX, el cual reserva la parte alta del cerro para el ejercicio de la pequeña minería. Asimismo, explora la vigencia de dichas normas y la manera en que ellas han influido la construcción de territorialidad y el desarrollo de una forma de vida en torno al ejercicio de la pequeña minería tradicional.

Antioxidant synergistic effects of Osmanthus fragrans flowers with green tea and their major contributed antioxidant compounds

OpenAIRE

Mao, Shuqin; Wang, Kaidi; Lei, Yukun; Yao, Shuting; Lu, Baiyi; Huang, Weisu

2017-01-01

The antioxidant synergistic effects of Osmanthus fragrans flowers with green tea were evaluated, and their major antioxidant compounds contributed to the total amount of synergy were determined. The antioxidant compounds in O. fragrans flowers with green tea were identified by LC-MS and quantified by UPLC-PDA. The synergistic antioxidant interactions between O. fragrans flowers with green tea and their antioxidant compounds were tested using the Prieto?s model after the simulated digestion. T...

Initial thermal state of the Los Humeros, Puebla, Mexico, geothermal field; Estado termico inicial del campo geotermico de Los Humeros, Puebla, Mexico

Energy Technology Data Exchange (ETDEWEB)

Garcia Gutierrez, Alfonso [Instituto de Investigaciones Electricas, Cuernavaca, Morelos (Mexico)]. E-mail: aggarcia@iie.org.mx

2009-01-15

The initial temperatures field is presented for 40 wells in the Los Humeros geothermal reservoir, along with an elevation curve based on the formation temperature or the most probable reservoir temperature. Stabilized temperatures were estimated using the Radial Spherical Heat Flow method, chosen over the Horner method based on the numerical simulation of the circulation and stop processes of well H-26. In this well, the last temperature log series was reproduced, considering circulation losses. The temperatures were used to produce isothermal curves over three geological sections of the field, which represent the initial distribution of temperatures in the reservoir and show the thermal characteristics and the relationships among thermal anomalies and faults in the reservoir. The elevation curve plotted against the initial temperature of the formation was generated based on detection of the main feed zones at each well, which in turn was developed using detailed analyses of diverse information, such as temperature logs, circulation losses, lithology, well completion, and heat velocities. Based on the results, two groups of wells may be distinguished: one between 1000 and 1600 masl with temperatures from 290 to 330 degrees Celsius, and one between 900 and 0 masl with temperatures from 300 to 400 degrees Celsius. [Spanish] En este trabajo se presenta el campo de temperatura inicial del yacimiento geotermico de Los Humeros y una curva de elevacion contra la temperatura de formacion o temperatura mas probable del yacimiento, obtenida para 40 pozos del campo. Las temperaturas estabilizadas se estimaron mediante el metodo de Flujo de Calor Esferico Radial, y su eleccion sobre las temperaturas del metodo de Horner se soporta con simulacion numerica de los procesos de circulacion y paro del pozo H-26, en la cual la ultima serie de registros se reprodujo considerando perdidas de circulacion. Con estas temperaturas se generaron curvas isotermicas para tres secciones

Mecanismo de inserción del Laboratorio Tecnológico del Uruguay en el Parque Tecnológico Industrial del Cerro

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Laura Márquez

2011-05-01

Full Text Available El Laboratorio Tecnológico del Uruguay, LATU, teniendo en cuenta su misión: "Impulsar el desarrollo sustentable del país y su inserción internacional a través de la innovación y transferencia de soluciones de valor, en servicios analíticos, metrológicos, tecnológicos, de gestión y evaluación de la conformidad de a cuerdo a la normativa aplicable", está trabajando en el apoyo a las micro, pequeñas y medianas empresas del país. Como estrategia para contribuir al logro de la misión, se ha iniciado una política de descentralización, eligiendo zonas de actividad con requerimientos similares, en cuanto a las necesidades de mejora de la competitividad de las empresas. En la zona de Montevideo llamada el Cerro, el gobierno municipal gestiona un Parque Tecnológico Industrial, PTIC, apoyando y alojando en su predio, 58 empresas. Este Parque se puede ver como un conglomerado de empresas, en una misma zona, con necesidades similares. El mecanismo de inserción del LATU en el PTIC, ha contado con una herramienta fundamental que es la instalación de una oficina en el propio Parque, cuyo objetivo principal es facilitar y asegurar la contribución del LATU al desarrollo y competitividad de las mipymes allí agrupadas.AbstractAttending to the Technological Laboratory of Uruguay (LATU's mission, to promote the sustainable development of the country and its international insertion through innovation and transfer of valuable solutions, it is working on support for micro, small and medium companies. As a management strategy to achieve the mission, a policy of decentralization, approaching to the enterprises, it's being implemented. In this context, it has been developed a methodology for insertion in the Industrial Technological Park of Cerro, PTIC. This park, which is managed by the municipal government, agglomerates a group of companies, in the same area with similar needs. The LATU's mechanism of insertion in the PTIC, has counted on with a

Patrones de distribución espacial de árboles en un bosque estacionalmente seco del Parque Nacional Cerros de Amotape en el noroeste peruano

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Reynaldo Linares-Palomino

2013-05-01

Full Text Available Se realizó un estudio de los patrones de distribución espacial de cuatro especies de árboles características de los bosques secos del Parque Nacional Cerros de Amotape en el noroeste peruano, inventariando seis parcelas de una hectárea cada una. Para ello se utilizó la versión modificada de la estadística K de Ripley. Eriotheca ruizii (K. Schum. A. Robyns (Bombacaceae, Bursera graveolens (Kunth Triana & Planch. (Burseraceae, Caesalpinia glabrata Kunth (Leguminosae y Cochlospermum vitifolium (Willd. Spreng. (Cochlospermaceae presentan patrones que no son significantemente diferentes de un patrón completamente al azar en 11 de los 17 casos analizados. Al nivel de la escala espacial analizada, esto está en desacuerdo con el postulado general para bosques tropicales de que las especies vegetales tienden a encontrarse agrupadas. Estos resultados se analizan y discuten a la luz de los diversos factores que influyen en producirlos.

Initial temperature distribution in Los Humeros, Mexico, geothermal field; Distribucion de temperatura inicial en el campo geotermico de Los Humeros, Puebla

Energy Technology Data Exchange (ETDEWEB)

Garcia, A; Arellano, V; Aragon, A; Barragan, R.M; Izquierdo, G [Instituto de Investigaciones Electricas, Temixco, Morelos (Mexico); Pizano, A [Comision federal de Electricidad, Los Humeros, Puebla (Mexico)

2000-12-01

The initial formation temperatures surrounding 40 wells from the Los Humeros geothermal field are presented. These temperatures were estimated using the Horner and the sphere methods. A brief discussion on the applicability of each method is presented and previous applications are detailed. Then the more likely reservoir temperature of each well versus elevation is plotted based on the estimations about the main feed zone and the temperature of each well. The boiling with depth curve for pure water is also included. Two longitudinal and one traverse geological sections are presented to illustrate the field initial temperature distribution, the lithology and layers thickness, the basement topography and the wells traversed along each sections. Also, the main feed zones of the wells are indicated. Finally, the last series of measured temperature logs in well H-26 are produced by numerical simulation. This considers the well circulation losses and an assumed initial temperature profile. This profile iteratively modified until the computed profiles match the measured temperature profiles. The last assumed temperature profile is then considered as the best approximation to the undisturbed formation temperature around well H-26 and it is then compared with the stabilized temperatures obtained via the Horner and Sphere methods. [Spanish] Se presentan las temperaturas iniciales o estabilizadas de la formacion circundante a 40 pozos del campo geotermico Los Humeros, las cuales se estimaron mediante los metodos de Horner y el metodo de la esfera. Se presenta una discusion sobre la aplicacion de cada metodo y se detallan las aplicaciones previas del metodo de la esfera. Posteriormente y con base en las estimaciones de las principales zonas de aporte de cada pozo y sus correspondientes temperaturas se grafican las temperaturas mas probables de yacimiento para cada pozo contra la elevacion y se incluye en la misma grafica la curva de ebullicion del agua contra la elevacion. Se

La Desnutrición, Malnutrición y el Rendimiento Académico de los Estudiantes del sexto grado de Educación Primaria de I.E.2028 Cerro Candela, SM.P. Lima, 2007

OpenAIRE

Zagastizabal Gamarra, Zaira Ruth

2015-01-01

Sabemos que la Fuente de la Vida de todo ser humano es la alimentación y el hombre sin alimento no puede sobrevivir por lo que; viendo los problemas de salud de los estudiantes desarrollé esta investigación titulada “La Desnutrición, mal nutrición y el rendimiento académico de los estudiantes del sexto grado de Educación Primaria de la I.E.2028 Cerro Candela, SMP. Lima, 2007”, siendo la muestra de 49 estudiantes. En el contenido de esta tesis se encuentra un conjunto de ante...

An empirical calibration for 4He quantification in minerals and rocks by laser fusion and noble gas mass spectrometry using Cerro de Mercado (Durango, Mexico) fluorapatite as a standard

International Nuclear Information System (INIS)

Sole, Jesus; Pi, Teresa

2005-01-01

An empirical calibration with a natural mineral standard (fluorapatite from Cerro de Mercado, Mexico) is proposed as a method to determine the 4 He concentration of mineral and rock samples. The procedure is based on the fusion of several aliquots of the fluorapatite standard with a well-spaced weight distribution in order to obtain a good correlation in coordinates of 4 He peak height versus fluorapatite weight. The weight is then converted to moles using the accepted mineral age (31.4 Ma) and appropriate formula. Experimental peak height of 4 He for the unknown samples are converted to moles with the regression determined for fluorapatite. The procedure is fast and inexpensive, and both precision and accuracy are always below 10% and usually about 3-5%

Geothermal infrastructure for an historic village in Tuscany: a sustainable retrofit solution

Directory of Open Access Journals (Sweden)

Valentina Marino

2016-06-01

Full Text Available Il comune di Montieri ha recentemente costruito una rete di teleriscaldamento alimentata a vapore geotermico. L’aspetto innovativo risiede nell’uso del vapore geotermico di scarto dalla produzione di elettricità, per fornire riscaldamento e acqua calda sanitaria per 425 utenze del centro storico. Con il progetto Geothermal Community (Concerto, FP7 sono stati intrapresi ulteriori obiettivi per l’ambiente costruito: la riduzione del consumo energetico degli edifici e l’aumento della quota delle risorse energetiche rinnovabili utilizzate dalla comunità. L’articolo propone una analisi dei benefici ambientali ed economici delle misure di efficienza energetica pianificate dal progetto Europeo alla luce dell’installazione della rete di teleriscaldamento. I risultati presentano uno spunto di riflessione interessante per la formulazione dei piani di riduzione delle emissioni delle aree urbane storiche Italiane ed Europee dove sono presenti simili infrastrutture. 

SIMULACIÓN DE FLUJOS PIROCLÁSTICOS DEL VOLCÁN CERRO MACHÍN, COLOMBIA, MEDIANTE LA APLICACIÓN DE HERRAMIENTAS DE ARCGIS©

Directory of Open Access Journals (Sweden)

Elsa Adriana Cárdenas Quiroga

2012-01-01

Full Text Available Cerro Machín es un volcán activo, caracterizado en el pasado por erupciones explosivas de tipo pliniano y ubicado en un sector de gran importancia económica. Desde la década de los noventa se han desarrollado varios modelos de simulación para determinar el área que podría resultar afectada en una nueva erupción, pero estos modelos se basan en programas con variables predeterminadas que no son fácilmente modificables. Por tanto, se diseñó una aplicación del modelo de simulación Model Builder de las herramientas del software ArcGIS© para facilitar el proceso de análisis de los flujos piroclásticos expulsados por ese volcán en tres eventos eruptivos identificados y modelados previamente, con el objetivo de crear una aplicación fácilmente adaptable a cambios en las variables de simulación y que pudiera ser empleada también para modelar otros volcanes. Los resultados obtenidos resultan compatibles y similares a los obtenidos en simulaciones previas, lo que indica que la aplicación desarrollada es funcional.

Initial Pressure Distribution in the Geothermal Field of Los Humeros, Puebla, Mexico; Distribucion de presion inicial en el campo geotermico de Los Humeros, Puebla, Mexico

Energy Technology Data Exchange (ETDEWEB)

Arellano, Victor M.; Izquierdo, Georgina; Aragon, Alfonso; Barragan, Rosa Maria; Garcia, Alfonso [Instituto de Investigaciones Electricas (Mexico); Pizano, Arturo [Comision Federal de Electricidad (Mexico)

2001-09-01

To obtain the undisturbed distribution of pressures of a field flow, a significant amount of data concerning geological, geochemical, geophysical, and field drilling and engineering aspects, from 42 wells located at the geothermal field of Los Humeros, was analysed. Based on the studied data, models of the field pressure distribution in its initial state were developed. The models reveal the existence of at least two deposits. One of them, the most superficial, is located between 1025 and 1600 meters over the sea level, and from its excellent congruence with the pressure profile of a boiling water column, it may be considered as a predominantly liquid field. The pressure profile of this field is that of a boiling water column, at a temperature of about 300-330 Celsius degrees. The second field is below 850 meters over the sea level and from the known data it reaches at least 100 meters over the sea level. It is considered a low-liquid saturated field. The temperatures of the wells supplied by this field were estimated to be about 300-40 Celsius degrees. [Spanish] Para inferir las distribuciones de presion no perturbadas del fluido del yacimiento, se analizo una considerable cantidad de informacion relacionada con los aspectos geologicos, geoquimicos, geofisicos, de perforacion e ingenieria de yacimientos, correspondiente a 42 pozos del camo geotermico de Los Humeros, Puebla. Sobre la base de los datos analizados se desarrollaron modelos de distribucion de la presion del yacimiento en su estado inicial. Dichos modelos revelan la existencia de, cuando menos, dos yacimientos. El primero y mas superficial se encuentra localizado entre 1,600 y 1,025 metros sobre el nivel del mar (msnm), y dada su excelente concordancia con el perfil de presion correspondiente a una columna de agua en ebullicion, puede afirmarse que se trata de un yacimiento de liquido dominante. El perfil de presion de este yacimiento corresponde a una columna de agua en ebullicion de 300 a 330

Estudios bioarqueológicos en el sitio Los Tres Cerros 1 (Delta Superior del río Paraná, Entre Ríos, Argentina

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Clara Scabuzzo

Full Text Available Resumen: En este trabajo se presentan los resultados de los estudios bioarqueológicos efectuados en la serie de esqueletos humanos del sitio Los Tres Cerros 1 (departamento de Victoria, Entre Ríos, Argentina, una estructura antropogénica monticular ocupada entre ca. 1227 y 560 años AP por cazadores, recolectores, pescadores y horticultores, asignados a la entidad arqueológica Goya-Malabrigo. Las investigaciones bioarqueológicas se enfocaron en determinar la estructura sexo-etaria de la muestra, estudiar las lesiones óseas y analizar las prácticas mortuorias. De acuerdo a estos estudios, en el sitio se enterraron al menos 16 individuos de distintos grupos etarios y ambos sexos. La variabilidad de modos de disponer a los muertos incluye entierros primarios, secundarios y elementos óseos dispersos. Algunos huesos presentaban termoalteración y ocre sobre la superficie. Se discuten estas evidencias a nivel regional con otros sitios del Delta del Paraná con presencia de esqueletos humanos asignados a la entidad Goya-Malabrigo.

Geophysical characterization of subaerial hydrothermal manifestations in Punta Banda, Baja California, Mexico.

Science.gov (United States)

Flores-Marquez, L.; Prol-Ledesma, R. M.; Arango, C.; Canet, C.

2009-04-01

Important growth of population in Baja California Peninsula has triggered the need for energy and fresh water. The most sustainable possibility for increasing the availability of fresh water is the use of renewable energy sources in desalination plants. The abundance of geothermal manifestations in the peninsula provides a reliable energy source for desalination purposes. Geothermal development of the Baja California Peninsula dates from the 70's, when the Cerro Prieto geothermal field started producing electricity. Two important cities, Tijuana and Ensenada, are located in the north-western area of Baja California. The city of Ensenada has a desalination plant that is due to be replaced and the geothermal resources of the area could be an option for the new desalination plant. Punta Banda, a region near Ensenada, was specially investigated to determine its geothermal potential. Subaerial springs and the submarine vents were sampled and studied in this work, also geological and geochemical studies were performed, moreover geoelectrical surveys were accomplished to characterize the hydrothermal system at depth. Even though saline intrusion is a severe problem in Ensenada (TDS higher than 3000), thermal springs away from the coast and coastal springs have salinities lower than sea water. According to the geoelectrical models obtained from profiles, the inferred conductive features can be related to thermal anomalies. The existence of hot springs located along a trend suggests that the dynamic of the thermal fluid is restricted by secondary faults.

Validating numerical simulations of snow avalanches using dendrochronology: the Cerro Ventana event in Northern Patagonia, Argentina

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A. Casteller

2008-05-01

Full Text Available The damage caused by snow avalanches to property and human lives is underestimated in many regions around the world, especially where this natural hazard remains poorly documented. One such region is the Argentinean Andes, where numerous settlements are threatened almost every winter by large snow avalanches. On 1 September 2002, the largest tragedy in the history of Argentinean mountaineering took place at Cerro Ventana, Northern Patagonia: nine persons were killed and seven others injured by a snow avalanche. In this paper, we combine both numerical modeling and dendrochronological investigations to reconstruct this event. Using information released by local governmental authorities and compiled in the field, the avalanche event was numerically simulated using the avalanche dynamics programs AVAL-1D and RAMMS. Avalanche characteristics, such as extent and date were determined using dendrochronological techniques. Model simulation results were compared with documentary and tree-ring evidences for the 2002 event. Our results show a good agreement between the simulated projection of the avalanche and its reconstructed extent using tree-ring records. Differences between the observed and the simulated avalanche, principally related to the snow height deposition in the run-out zone, are mostly attributed to the low resolution of the digital elevation model used to represent the valley topography. The main contributions of this study are (1 to provide the first calibration of numerical avalanche models for the Patagonian Andes and (2 to highlight the potential of Nothofagus pumilio tree-ring records to reconstruct past snow-avalanche events in time and space. Future research should focus on testing this combined approach in other forested regions of the Andes.

Glacier mass balance reconstruction by sublimation induced enrichment of chemical species on Cerro Tapado (Chilean Andes

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P. Ginot

2006-01-01

Full Text Available A 36 m long ice core down to bedrock from the Cerro Tapado glacier (5536 m a.s.l, 30°08' S, 69°55' W was analyzed to reconstruct past climatic conditions for Northern Chile. Because of the marked seasonality in the precipitation (short wet winter and extended dry summer periods in this region, major snow ablation and related post-depositional processes occur on the glacier surface during summer periods. They include predominantly sublimation and dry deposition. Assuming that, like measured during the field campaign, the enrichment of chloride was always related to sublimation, the chemical record along the ice core may be applied to reconstruct the history of such secondary processes linked to the past climatic conditions over northern Chile. For the time period 1962–1999, a mean annual net accumulation of 316 mm water equivalent (weq and 327 mm weq loss by sublimation was deduced by this method. This corresponds to an initial total annual accumulation of 539 mm weq. The annual variability of the accumulation and sublimation is related with the Southern Oscillation Index (SOI: higher net-accumulation during El-Niño years and more sublimation during La Niña years. The deepest part of the ice record shows a time discontinuity; with an ice body deposited under different climatic conditions: 290 mm higher precipitation but with reduced seasonal distribution (+470 mm in winter and –180 mm in summer and –3°C lower mean annual temperature. Unfortunately, its age is unknown. The comparison with regional proxy data however let us conclude that the glacier buildup did most likely occur after the dry mid-Holocene.

Ocorrência de lepidópteros de importância médica (Lepidoptera: Aididae, Lasiocampidae, Limacodidae e Megalopygidae no Cerro da Buena, município de Morro Redondo, Rio Grande do Sul, Brasil

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Ricardo Russo Siewert

2012-08-01

Full Text Available http://dx.doi.org/10.5007/2175-7925.2012v25n4p279   O propósito deste estudo foi registrar a fauna de lepidópteros de importância médica ocorrente no Cerro da Buena, município de Morro Redondo, Rio Grande do Sul, Brasil, entre fevereiro de 2009 a janeiro de 2011. Foram registradas 32 espécies de mariposas, pertencentes à Aididae (1, Lasiocampidae (17, Limacodidae (7 e Megalopygidae (7. Três novas ocorrências de Lasiocampidae para o Rio Grande do Sul foram realizadas: Artace argentina Schaus, 1924, Euglyphis kotzschi Draudt, 1927 e Tolype trilinea (Dognin, 1901.

Addition of schelita residue from the mine in Cerro Cora Bodo / RN in the composition of ceramic materials

International Nuclear Information System (INIS)

Almeida, A.B.D. de; Souza, M. M. de; Farias, D.S.U. de; Lima, T.C. de; Nobrega, L.F.P. de M.; Mendes, L.B.

2016-01-01

Mining activities produce mineral waste that can degrade the environment. The waste generated by companies is not reused due to the fact they fail to present an application for it that proves to be economically viable. Seeking the reuse of mineral waste and reduce the environmental impacts, this work addresses the chemical characterization by x-ray fluorescence (FRX), of the processing of scheelite reject at Bodo mine in Cerro Cora-RN. For the procedure, the sample was collected, grounded and sieved to #200, and then characterized to evaluate its chemical composition and its potential to be incorporated into materials. Besides the characterization, a water absorption test and also a bending test were performed to analyze the power and tension of the material. The result of the analysis indicated that the sample researched presents a greater concentration of SiO_2 to be used as a structuring element in ceramic mass, but in the traditional formulation, it will only be added 10% of the reject in its formulation, because besides the SiO_2 in the sample analyzed other elements that act with fluxes were found. It was also observed the material has low water absorption, but the reject reached low strength and breakdown voltage. We concluded that the reject of scheelite presents great potential, and therefore, further tests can be conducted to analyze the possibility of being added as raw material for the formulation of other materials like cement. (author)

Scaling control in superficial installations at the Las Tres Virgenes, geothermal field, BCS; Control de incrustacion en instalaciones superficiales del campo geotermico de Las Tres Virgenes, BCS

Energy Technology Data Exchange (ETDEWEB)

Tapia Salazar, Ruth [Comision Federal de Electricidad (Mexico)]. E-mail: ruth.tapia@cfe.gob.mx

2007-01-15

Silica scaling is one of the most important problems in the Las Tres Virgenes geothermal field. It affects not only the superficial installations, like brine injection pipelines, but also the injection wells where it reduces injection capacity. Separated brine passes from production wells to injection wells by means of steel pipelines 10 and 14 inches in diameter. The pipelines are affected by silica scaling that occurs when the two-phase fluid is discharged at atmospheric pressure and the separated brine is cooled and concentrated and then over saturated with amorphous silica. Even when the pipelines were cleaned periodically, it was necessary to implement a technique for prevent scaling. Two methods considered appropriate to the specific field conditions were studied, and finally the technique of modifying the brine pH was adopted. After over a year of using this technique in the general injection system, no mechanical cleaning of the pipelines has been necessary-and once cleaning was needed at least every third day. This represents an important improvement in the steam supply system. [Spanish] Uno de los problemas mas importantes en el campo geotermico de Las Tres Virgenes es la incrustacion por silice, la cual afecta no solo a instalaciones superficiales como lineas de inyeccion de salmuera, sino tambien a los pozos inyectores al reducir su capacidad de aceptacion. El agua producida por los pozos productores se conduce hasta los pozos inyectores por medio de tuberias de acero al carbon de 10 y 14 pulgadas de diametro, que se ven afectadas por la incrustacion de silice. La incrustacion ocurre debido a que cuando el fluido en dos fases es descargado a presion atmosferica, la salmuera separada, enfriada y concentrada, esta usualmente sobresaturada con respecto a la solubilidad de la silice amorfa. Aunque las tuberias se limpiaban mecanicamente, fue necesario seleccionar una tecnica para prevenir la incrustacion, para lo cual se estudiaron dos de los metodos que

Seismic monitoring during acid stimulation of wells LV-4 and LV-13 at the Las Tres Virgenes geothermal field, BCS, Mexico; Monitoreo sismico durante la estimulacion acida de los pozos LV-4 y LV-13 del campo geotermico de Las Tres Virgenes, BCS, Mexico

Energy Technology Data Exchange (ETDEWEB)

Venegas Salgado, Saul; Arredondo Fragoso, Jesus; Ramirez Silva, German; Flores Armenta, Magaly; Ramirez Montes, Miguel [Comision Federal de Electricidad, Gerencia de Proyectos Geotermoelectricos, Morelia, Michoacan (Mexico)]. E-mail: magaly.flores@cfe.gob.mx

2006-07-15

From September through December 2004 a seismic monitoring in the Las Tres Virgenes, BCS, geothermal field was carried out simultaneously with the acid stimulation of wells LV-4 and LV-13. The seismic network had four digital seismographs and recorded 174 local seismic events, 131 regional ones and many more volcanic signals at seismic station TV20 during the acid stimulation. Additionally, 37 seismic events were located, 22 of them inside the most important geothermal zone at depths between 0.4 and 4 km with typically low magnitudes (0.7 to 2.2 Md). Two relevant zones were determined: Zone A related to the El Volcan fault system and Zone B related to injection well LV-8. In Zone A the well-induction stage and the operation start of the wells LV-4 and LV-13 after acidification on October 30 and November 17, 2004, increased seismic activity to a maximum of 12 daily events in early December. When the two wells in Zone B were cooled before the acidification, the seismic events recorded there increased to a maximum of 6 daily events on October 2, and then decreased. Also in Zone B the seismic activity increased after well-induction and the start of well production once they were acidified, recording up to 11 daily events in late November. According to the seismic distribution, we may conclude that the most active fault systems are El Volcan and El Viejo. New proposals for well locations in the field are supported by these results. [Spanish] De septiembre a diciembre de 2004 se realizo un estudio de monitoreo sismico en el campo geotermico de Las Tres Virgenes, BCS, simultaneamente con las estimulaciones acidas de los pozos LV-4 y LV-13. Se utilizo una red sismica conformada por cuatro sismografos digitales, logrando registrar en la estacion sismica TV20 un total de 174 sismos locales, 131 sismos regionales y muchas mas senales de tipo volcanico, durante el periodo del monitoreo de la estimulacion acida. Ademas, se localizaron un total de 37 sismos, de los cuales 22 se

Ecological Impacts of the Cerro Grande Fire: Predicting Elk Movement and Distribution Patterns in Response to Vegetative Recovery through Simulation Modeling October 2005

Energy Technology Data Exchange (ETDEWEB)

Rupp, Susan P. [Texas Tech Univ., Lubbock, TX (United States)

2005-10-01

In May 2000, the Cerro Grande Fire burned approximately 17,200 ha in north-central New Mexico as the result of an escaped prescribed burn initiated by Bandelier National Monument. The interaction of large-scale fires, vegetation, and elk is an important management issue, but few studies have addressed the ecological implications of vegetative succession and landscape heterogeneity on ungulate populations following large-scale disturbance events. Primary objectives of this research were to identify elk movement pathways on local and landscape scales, to determine environmental factors that influence elk movement, and to evaluate movement and distribution patterns in relation to spatial and temporal aspects of the Cerro Grande Fire. Data collection and assimilation reflect the collaborative efforts of National Park Service, U.S. Forest Service, and Department of Energy (Los Alamos National Laboratory) personnel. Geographic positioning system (GPS) collars were used to track 54 elk over a period of 3+ years and locational data were incorporated into a multi-layered geographic information system (GIS) for analysis. Preliminary tests of GPS collar accuracy indicated a strong effect of 2D fixes on position acquisition rates (PARs) depending on time of day and season of year. Slope, aspect, elevation, and land cover type affected dilution of precision (DOP) values for both 2D and 3D fixes, although significant relationships varied from positive to negative making it difficult to delineate the mechanism behind significant responses. Two-dimensional fixes accounted for 34% of all successfully acquired locations and may affect results in which those data were used. Overall position acquisition rate was 93.3% and mean DOP values were consistently in the range of 4.0 to 6.0 leading to the conclusion collar accuracy was acceptable for modeling purposes. SAVANNA, a spatially explicit, process-oriented ecosystem model, was used to simulate successional dynamics. Inputs to the

Microbialitas lacustres de secuencias triásicas de Argentina

OpenAIRE

Benavente, Cecilia Andrea

2014-01-01

Las sucesiones triásicas Cerro de las Cabras y Cerro Puntudo corresponden al relleno sedimentario de la Cuenca Cuyana de rift. La cuenca presenta dos hemigrábenes asimétricos, uno ubicado al norte y otro al sur de polaridad opuesta y desvinculados por un alto topográfico. Los depocentros estudiados son Cerro Puntudo que forma parte del hemigraben norte en donde aflora la Formación Cerro Puntudo; y el depocentro Potrerillos que forma parte del hemigraben sur en el que aflora la Formación Cerro...

Evolution evidence of a basic fluid to an acid based in the analysis of hydrothermal alteration of the geothermic field of the Azufres, Michoacan; Evidencias de evolucion de un fluido basico a acido a partir del analisis de la alteracion hidrotermal del campo geotermico de los Azufres, Michoacan

Energy Technology Data Exchange (ETDEWEB)

Gonzalez Partida, Eduardo [Universidad Nacional Autonoma de Mexico, Mexico, D.F. (Mexico)

2000-07-01

Hydrothermal alteration at the Los Azufres geothermal field is mostly composed of calc-silicate minerals that define a propylitic alteration zone, which shows progressive dehydration with depth and temperature increase. A generalized zoning of the calc-silicate zone can be observed, with zeolites in the upper part and epidote-clinozoisite at the deepest levels. An argillic alteration zone overlies the calc-silicate zone and is the dominant surface manifestation of the hydrothermal alteration. In some parts, there is a mineral assemblage composed of kaolinite-alunite-native sulfur-quartz (advanced argillic zone) formed by the interaction of vapor and shallow groundwater. The proto-fluid at the Los Azufres geothermal system is related to a neutral sodium chlorine brine, which favors deep propyllitic alteration (productive zone). This zone is characterized by secondary permeability due to fracturing. At depth the geothermal field is dominated by a pressurized liquid, yielding to vapor at more shallow zone. The gradual change from a liquid to a vapor phase occurs through boiling at depths between 1,200 and 1,500 m, and is accompanied by changes in the hydrothermal alteration mineralogy. The type of alteration passes from proylitic to argillic by means of an oxidation-acidification process, which includes the participation of a gas, particularly CO{sub 2}. Considering the physicochemical characteristic of the brine and the evolution of the paragenetic sequence, the Los Azufres geothermal field could de considered a model for hydrothermal behavior at ore deposits which develop by boiling and oxidation of low sulfidation fossil hydrothermal fluids. [Spanish] En el campo geotermico de Los Azufres la zona de alteracion hidrotermal esta formada en su mayor parte por calcosilicatos (que definen una zona paragenetica del tipo propilitico), los cuales muestran una deshidratacion progresiva conforme se va profundizando e incrementandose la temperatura. Se puede generalizar un

Systematic heat flow measurements across the Wagner Basin, northern Gulf of California

Science.gov (United States)

Neumann, Florian; Negrete-Aranda, Raquel; Harris, Robert N.; Contreras, Juan; Sclater, John G.; González-Fernández, Antonio

2017-12-01

A primary control on the geodynamics of rifting is the thermal regime. To better understand the geodynamics of rifting in the northern Gulf of California we systematically measured heat-flow across the Wagner Basin, a tectonically active basin that lies near the southern terminus of the Cerro Prieto fault. The heat flow profile is 40 km long, has a nominal measurement spacing of ∼1 km, and is collocated with a seismic reflection profile. Heat flow measurements were made with a 6.5-m violin-bow probe. Although heat flow data were collected in shallow water, where there are significant temporal variations in bottom water temperature, we use CTD data collected over many years to correct our measurements to yield accurate values of heat flow. After correction for bottom water temperature, the mean and standard deviation of heat flow across the western, central, and eastern parts of the basin are 220 ± 60, 99 ± 14, 889 ± 419 mW m-2, respectively. Corrections for sedimentation would increase measured heat flow across the central part of basin by 40 to 60%. We interpret the relatively high heat flow and large variability on the western and eastern flanks in terms of upward fluid flow at depth below the seafloor, whereas the lower and more consistent values across the central part of the basin are suggestive of conductive heat transfer. Moreover, heat flow across the central basin is consistent with gabbroic underplating at a depth of 15 km and suggests that continental rupture here has not gone to completion.

Evaluation of recurrent radiation with Cobalt 60 gamma rays on agronomic traits of barley (Hordeum Vulgare L.) in the R2M1 generation

International Nuclear Information System (INIS)

Vega G, M.G.

1994-01-01

The objective of this work was to evaluate the effect of recurrent radiation on agronomic traits in two barley varieties. The research was carried out at experimental fields pertaining to the Instituto de Investigacion Agropecuaria, Acuicola y Forestal of the Estado de Mexico (ICAMEX). The biological material was irradiated in the Gamma Cell 220 at the Instituto Nacional de Investigaciones Nucleares (ININ). The experimental design was divided plots in the randomized blocks, with four replications. The factor varieties (Cerro Prieto and Puebla) was assigned to the big plots mean while in the factor doses was assignated to the small plots (0, 10, 20, 30, 40 and 50 krad of gamma rays). The variables under study were: germination, number of shoots, plant height, incidence of Puccinia striiformis, days to flowering, days to physiological maturity, spike length and yield. The analysis of variance exhibited no significant differences between varieties for all the studied variables. Regarding to dose, most of the studied variables exhibited significant differences, except for incidence of Puccinia striiformis and days to flowering. The interaction variety x doses showed significance only for the variable days to flowering and days to physiological maturity. The mean separation by Tukey test at 0.05 and the regression analysis showed that the variables: germination, number of shoots, plant height, spike length and yield decreased as the dose increased. On the other hand in the variables incidence of Puccinia striiformis, days to flowering and days to physiological maturity exhibited a direct relationship with the dose. (Author)

Observations of the Breakdown of Mountain Waves Over the Andes Lidar Observatory at Cerro Pachon on 8/9 July 2012

Science.gov (United States)

Hecht, J. H.; Fritts, D. C.; Wang, L.; Gelinas, L. J.; Rudy, R. J.; Walterscheid, R. L.; Taylor, M. J.; Pautet, P. D.; Smith, S.; Franke, S. J.

2018-01-01

Although mountain waves (MWs) are thought to be a ubiquitous feature of the wintertime southern Andes stratosphere, it was not known whether these waves propagated up to the mesopause region until Smith et al. (2009) confirmed their presence via airglow observations. The new Andes Lidar Observatory at Cerro Pachon in Chile provided the opportunity for a further study of these waves. Since MWs have near-zero phase speed, and zero wind lines often occur in the winter upper mesosphere (80 to 100 km altitude) region due to the reversal of the zonal mean and tidal wind, MW breakdown may routinely occur at these altitudes. Here we report on very high spatial/temporal resolution observations of the initiation of MW breakdown in the mesopause region. Because the waves are nearly stationary, the breakdown process was observed over several hours; a much longer interval than has previously been observed for any gravity wave breakdown. During the breakdown process observations were made of initial horseshoe-shaped vortices, leading to successive vortex rings, as is also commonly seen in Direct Numerical Simulations (DNS) of idealized and multiscale gravity wave breaking. Kelvin-Helmholtz instability (KHI) structures were also observed to form. Comparing the structure of observed KHI with the results of existing DNS allowed an estimate of the turbulent kinematic viscosity. This viscosity was found to be around 25 m2/s, a value larger than the nominal viscosity that is used in models.

Palynological analysis of camelid coprolites: seasonality in the use of the site Cerro Casa de Piedra 7 (Santa Cruz, Argentina)

Science.gov (United States)

Velázquez, Nadia Jimena; Burry, Lidia Susana; Fugassa, Martín Horacio; Civalero, María Teresa; Aschero, Carlos Alberto

2014-01-01

Palynological, palaeoparasitological and paleobotanical studies of coprolites found in archaeological sites from Perito Moreno National Park (47°57‧S72°05‧W) yielded information on diet, palaeoenvironment and health. These studies allowed adding evidence to the reconstruction of life history of the hunter-gatherers that inhabited Patagonia during the Holocene. We examined the season of the year when camelid Lama guanicoe coprolites (5400 ± 64 yr 14C BP to 9640 ± 190 yr 14C BP) were deposited at Cerro Casa de Piedra 7 (site CCP7). The study used palynological evidence and comparison with pollen spectra of modern feces collected during summer, fall, winter and spring of 2010. The dominant types were: pollen of Nothofagus, Empetrum rubrum, Asteraceae subfam. Asteroideae, Nassauvia, Caryophyllaceae and Poaceae; fern spores; remains of Eimeria macusaniensis; and plant remains of Poaceae, Festuca pallescens, Stipa speciosa, Armeria maritima, Gaultheria mucronata and E. rubrum. Pollen spectra of modern and fossil feces were used for multivariate analysis. Coprolites associated to fall and winter modern feces. These results and those obtained from pollen concentration values and the presence of pollen types indicators of seasonality, allowed the determination of summer, fall and winter coprolites. However, caution must be taken with the seasonality results of coprolites dated earlier than 9000 years BP since the environmental conditions differed from now. The site was probably a camelid shelter during the unfavorable seasons.

Intermittent Catheterization: The Devil Is in the Details.

Science.gov (United States)

Christison, Kathleen; Walter, Matthias; Wyndaele, Jean-Jacques J M; Kennelly, Michael; Kessler, Thomas M; Noonan, Vanessa K; Fallah, Nader; Krassioukov, Andrei V

2018-02-01

During the last few years, the international community debated urinary tract infection and re-use of catheters when managing neurogenic lower urinary tract dysfunction (NLUTD) among individuals with spinal cord injury (SCI). In this respect, the 2014 Cochrane review by Prieto and colleagues, "Intermittent catheterisation for long-term bladder management," became one of the leading documents that captured the minds and attention of clinicians around the world. Although numerous countries had switched to single-use catheters for management of NLUTD following SCI, the opinion that was expressed in the 2014 Cochrane review had a strong influence on healthcare providers and agencies to recommend re-use of catheters. However, many clinicians have expressed concern regarding the conclusions in the 2014 Cochrane review by Prieto and colleagues. We therefore conducted an independent appraisal of the data and analyses presented in the review. Our appraisal identified crucial discrepancies of data extraction and analyses within the review. In appraisal to that of Prieto and colleagues' review, our analysis revealed a trend to favor single over multiple use of catheters. After addressing our concerns to Cochrane's acting Editor-in-Chief, the most recent version of the 2014 Cochrane review was withdrawn from publication.

Isotopic Evolution of Wells in the Geothermal Field of Los Azufres, Michoacan, Mexico; Evolucion isotopica de fluidos de pozos del campo geotermico de Los Azufres, Michoacan, Mexico

Energy Technology Data Exchange (ETDEWEB)

Barragan Reyes, Rosa Maria; Portugal Marin, Enrique; Arellano Gomez, Victor Manel; Aragon Aguilar, Alfonso [Instituto de Investigaciones Electricas (Mexico); Sandoval Medina, Fernando [Comision Federal de Electricidad (Mexico)

2002-12-01

Isotopic ({delta}{sup 1}8 O and {delta}D) data from production and reinjection web fluids from the Los Azufres geothermal field were interpreted in order to define reservoir evolution and the occurrence of physical processes as a result of exploitation. The study included data of 30 wells, which were sampled in September, 2000. General results indicate that different phenomena seem to occur in both zones of the field. In the southern zone there are two different trends of behavior: a mixture of fluids evidenced by the {delta}D versus {delta}{sup 1}8 O trend with a positive slope, was interpreted as the result of reservoir vapor separation at a temperature above 220 Celsius degrees, since for temperatures above 220 Celsius degrees deuterium behaves as a volatile component. No well-defined {delta}{sup D} vs {delta}{sup 1}8 O trend was found for the northern zone, but some points seem to fit the same negative slope trend found in the souther zone. The study of reservoir temperatures estimated by different approaches for particular wells through time, as well as temperature results obtained with a heat and flow well simulator, suggest that reservoir boiling occurs in localized areas in both zone of the field. This process is probably due to exploitation. [Spanish] Se interpretaron datos isotopicos ({delta}{sup 1}8 O y {delta}D) de fluidos de pozos productores y de reinyeccion del campo geotermico de Los Azufres, Michoacan, Mexico, para definir la evolucion del yacimiento y la ocurrencia de procesos fisicos como resultado de la explotacion. En el estudio se consideran datos de treinta pozos segun el muestreo realizado en septiembre de 2000. El estudio de la evolucion en el tiempo de las estimaciones de temperatura de yacimiento mediante diferentes tecnicas, asi como la temperatura obtenida de simulacion de pozos, sugiere que ocurre ebullicion en areas localizadas en ambas zonas del campo debido a la explotacion. Los resultados generales indican la existencia de

A new method of damage determination in geothermal wells from geothermal inflow with application to Los Humeros, Mexico

Energy Technology Data Exchange (ETDEWEB)

Aragon, A [Instituto de Investigaciones Electricas, Cuernavaca, Morelos (Mexico); Moya, S. L [Centro Nacional de Investigacion y Desarrollo Tecnologico, Cuernavaca, Morelos (Mexico); Garcia-Gutierrez, A; Arellano, V [Instituto de Investigaciones Electricas, Cuernavaca, Morelos (Mexico)

2008-10-15

Geothermal inflow type curves were obtained for different values of well damage (i.e., inflow performance relationships). The method was evaluated by diagnosing the damage of thirteen producing wells in the Los Humeros, Puebla, Mexico geothermal field. Permeability determinations were carried out for these wells and their productivity indices were estimated. Comparison of the diagnoses made via damage effects against the results of field pressure tests showed that the maximum difference between both approaches is on the order of 0.7 damage units. The methodology allows reservoir characterization along its productive life, since several production tests are carried out while the reservoir is producing. The data obtained from production tests are used to determine the damage effect and permeability of the rock formation. Previously the damage (skin factor) could only be determined from the analyses of transient pressure tests. [Spanish] Se presenta la obtencion de curvas-tipo de influjo geotermico para diferentes valores de dano, y se demuestra su aplicacion en los analisis de produccion de pozos geotermicos determinando el dano en trece pozos del campo geotermico de Los Humeros, Puebla, Mexico. Tambien se hicieron determinaciones de la permeabilidad en las zonas de produccion de estos pozos y de sus respectivos indices de productividad. Se compararon los resultados del valor de dano obtenido con la metodologia propuesta, con los valores de dano obtenidos a partir de pruebas de presion, encontrando que las diferencias maximas entre ambas tecnicas es del orden de 0.7 unidades de dano. La presente metodologia permite la caracterizacion del yacimiento a lo largo de su vida productiva a partir de las mediciones de las pruebas de produccion efectuadas en los pozos. La metodologia propuesta es innovadora porque anteriormente el dano solamente se podia determinar a partir de los analisis de las mediciones de la pruebas de presion.

Geochemistry and isotopic characterization of rain in the zones of Los Azufres, Michoacan and Los Humeros, Puebla and its relation with geothermal fluids; Caracterizacion geoquimica e isotopica de lluvia en las zonas de Los Azufres, Michoacan y Los Humeros, Puebla y su relacion con fluidos geotermicos

Energy Technology Data Exchange (ETDEWEB)

Verma, Mahendra P; Santoyo, Socrates; Aragon, Alfonso [Instituto de Investigaciones Electricas, Temixco, Morelos (Mexico); Fernandez, Ma. Elena [Comision Federal de Electricidad Morelia, Michoacan (Mexico); Tovar, Rigoberto [Comision Federal de Electricidad, Los Azufres (Mexico); Casimiro, Emigdio; Sandoval, Fernando [Comision Federal de Electricidad, Los Humeros, Puebla (Mexico); Johnson, Craig [USGS, Denver, Colorado, (United States); Gerardo-Abaya, Jane [IAEA, Viena (Austria)

1999-12-01

, whereas there is less then 10% sea spray sulfate at Los Azufres. The {delta}{sup 3}4S values of H{sub 2}S of geothermal fluid are very similar to those of rainwater. A compilation of {delta}{sup 3}4S values for different sources of sulfur emissions indicates that it is practically impossible to define the origin of sulfur in rainwater, but the combined results of chemical and isotopic monitoring suggest that the geothermal emissions have no contribution to rainwater acidity. [Spanish] Se presentan los resultados preliminares obtenidos del estudio de monitoreo quimico e isotopico de las precipitaciones pluviales en los campos geotermicos de Los Humeros, Los Azufres y sus zonas de referencia durante el periodo de lluvia 1995-1998. Se recolectaron las muestras de lluvia en siete de los sitios de Los Humeros y ocho de Los Azufres. Los valores de la alcalinidad resultaron positivos para casi todas las muestras de lluvia en Los Humeros, lo que indica que en esta zona no existe acidez. Algunos valores de alcalinidad en los sitios Vivero y Guadalajara de Los Azufres fueron negativos, aunque muy pequenos, por lo que se concluye que existe poca acidez en la lluvia en Los Azufres. En el caso de Los Humeros se encontro buena correlacion entre la alcalinidad y la concentracion de calcio, lo que sugiere que las muestras puedan estar afectadas probablemente por el polvo de la zona. La concentracion de aniones, Cl{sup -}, SO{sub 4} y NO{sub 3} es baja en ambos campos y con una tendencia bien definida. La concentracion de NO{sub 3} y SO{sub 4} en las lluvias de Los Azufres disminuye con el avance de la temporada. En el caso de Los Humeros casi no existe NO{sub 3} y SO{sub 4} en las lluvias de Los Azufres disminuye con el avance de la temporada. En el caso de Los Humeros casi no existe NO{sub 3}. Como referencia cabe senalar que los valores de NO{sub 3} en las lluvias de la ciudad de Mexico son superiores a 10 ppm e indican una relacion con la contaminacion industrial. Esto sugiere que el

An application of neural network in geophysical prospecting. Electrical resistivity at Las Virgenes geothermal field, Baja California Sur, Mexico; Una aplicacion de las redes neuronales a la prospeccion geofisica. Resistividad electrica en las Tres Virgenes, Baja California Sur, Mexico

Energy Technology Data Exchange (ETDEWEB)

Palma Guzman, Sergio Hugo [Comision Federal de Electricidad, Morelia, Michoacan (Mexico)

2000-12-01

The technology of the neural network is presented with geophysical focus in the Las Virgenes geothermal field, Baja California Sur, Mexico. The results obtained when extrapolating the associative data of the prospecting magnetoteluria and Vertical Electric Sounding, on the area of the geothermal wells to the rest of the area, allows to classify zones of interest for the geothermal exploitation. Also, the use of these associative parameters with the information of the stabilized temperature of the wells, they allow to predict temperatures for the rest of the area. [Spanish] Se presenta una aplicacion de la tecnologia de las redes neuronales con enfoque geofisico en el campo geotermico de Las Virgenes, Baja California Sur, Mexico. Los resultados obtenidos al extrapolar los datos asociativos de las prospecciones geoelectricas de magnetoteluria y sondeos electricos verticales, en la zona de los pozos geotermicos al resto del area, permiten clasificar zonas de interes para la explotacion geotermica. Tambien, la utilizacion de estos parametros asociativos con la informacion de la temperatura estabilizada de los pozos, permiten predecir temperaturas para la misma area.

Síndrome de Burnout en estudiantes internos durante su estancia por el Hospital Pediátrico del Cerro

Directory of Open Access Journals (Sweden)

José Ramón Acosta-Torres

2016-05-01

Full Text Available Objetivos: Determinar la presencia del síndrome de Burnout en su orientación unidimensional entre los estudiantes internos del sexto año de la carrera de Medicina durante su rotación por Pediatría. Materiales y Métodos: Se realizó un estudio transversal y descriptivo mediante la aplicación de la Escala Unidimensional del Burnout Estudiantil de Barraza Macías a una muestra de 230 alumnos del sexto año de la carrera de Medicina, durante su rotación por el Hospital Docente Pediátrico del Cerro, previo consentimiento informado; se indagó la presencia del mismo, sus características y se relacionó la entidad con las variables de la edad y el sexo de los estudiantes. Una vez obtenidos los datos, éstos se almacenaron en una página Excel y se procesaron por el programa XLSTAT 9, mediante la aplicación del método porcentual y el estadígrafo X2, con una significación de p < 0,05. Resultados: Se observó una incidencia del síndrome de Burnout con un nivel leve (83,91% y moderado (13,42% en la población estudiada. Su predominio se identificó en el sexo femenino, con significación estadística e independiente de la edad. Conclusiones: Los alumnos internos en su rotación por la asignatura de Pediatría se encuentran afectados en su mayoría por el síndrome de Burnout en un nivel leve, observándose dependencia del mismo en relación con el sexo femenino.

Condensers for measuring steam quality at the inlet of back-pressure units of the Los Azufres, Mich., geothermal field; Condensadores para medir la calidad del vapor a la entrada de las turbinas a contrapresion del campo geotermico de Los Azufres, Mich.

Energy Technology Data Exchange (ETDEWEB)

Sandoval Medina, Fernando; Gonzalez Gonzalez, Rubi; Reyes Delgado, Lisette; Medina Martinez, Moises [Comision Federal de Electricidad, Gerencia de Proyectos Geotermoelectricos, Residencia de Los Azufres (Mexico)]. E-mail: fernando.sandoval@cfe.gob.mx

2007-01-15

Electrical conductivity is an indirect measurement of the quality of the steam supplied to power units. In the Los Azufres, Mich., geothermal field, the electrical conductivity once was measured in a discrete and periodic way by condensing steam samples through a water-cooled condenser. In an attempt to continuously measure conductivity, conductivity meters were installed where the units discharged, but the values proved unstable and unrepresentative. Thereafter, taking into account that steam quality should be measured at the steam delivery-reception point, equipment was designed and tested for continuously condensing steam. Finally it was possible to get an air-cooled condenser able to condense 500 milliliters per minute, enough to collect a representative flow of the steam and to measure its electrical conductivity. The equipment was installed in all seven back-pressure units operating in the field and to date has been operating in an optimal manner. [Spanish] La conductividad electrica es una medida indirecta de la calidad del vapor que se suministra a las unidades turbogeneradoras. En el campo geotermico de Los Azufres, Mich., la conductividad electrica se media en forma puntual y periodica, condensando muestras de vapor por medio de un serpentin enfriado con agua. Despues, ante la necesidad de medirla en forma continua, se instalaron conductivimetros en las descargas de las unidades, pero los valores resultaron muy inestables y poco representativos. Considerando, ademas, que la calidad del vapor debe medirse en el punto de entrega-recepcion, se disenaron y probaron equipos para condensar vapor de manera continua, lograndose construir un condensador enfriado por aire que logra condensar un flujo de 500 mililitros por minuto, cantidad suficiente para tener un flujo representativo del vapor que alimenta a las turbinas y medirle su conductividad electrica. Se instalaron estos equipos en las siete unidades turbogeneradoras a contrapresion que funcionan en el campo

Gazetteer of El Salvador,

Science.gov (United States)

1982-06-01

Pitahaya PPL 13󈧬’N 88 08’W ES08 CL71 ND16-10 La Pitahaya . Cerro HLL 1339’N 88...8217 Pishishapa PPL 13 58’N 89 1O’W ESIO BL64 ND16-09 Pita Floja PPL 1423’N 89 35W ESl BL29 ND16.05 I’itahaya. see La Pitahaya PPL 13 40’N 88 08W ES08 CL71...ND16-10 I’ilahaya. Cerro. see La Pitahaya . Cerro HLL 13 39’N 88 08’W ES08 CL70 ND16.1C I’ilahaya. Cerro I(v see La Pitahaya , Cerro HLL 13 39’N 88

The Marianas-San Marcos vein system: characteristics of a shallow low sulfidation epithermal Au-Ag deposit in the Cerro Negro district, Deseado Massif, Patagonia, Argentina

Science.gov (United States)

Vidal, Conrado Permuy; Guido, Diego M.; Jovic, Sebastián M.; Bodnar, Robert J.; Moncada, Daniel; Melgarejo, Joan Carles; Hames, Willis

2016-08-01

The Cerro Negro district, within the Argentinian Deseado Massif province, has become one of the most significant recent epithermal discoveries, with estimated reserves plus resources of ˜6.7 Moz Au equivalent. The Marianas-San Marcos vein system contains about 70 % of the Au-Ag resources in the district. Mineralization consists of Upper Jurassic (155 Ma) epithermal Au- and Ag-rich veins of low to intermediate sulfidation style, hosted in and genetically related to Jurassic intermediate composition volcanic rocks (159-156 Ma). Veins have a complex infill history, represented by ten stages with clear crosscutting relationships that can be summarized in four main episodes: a low volume, metal-rich initial episode (E1), an extended banded quartz episode with minor mineralization (E2), a barren waning stage episode (E3), and a silver-rich late tectonic-hydrothermal episode (E4). The first three episodes are interpreted to have formed at the same time and probably from fluids of similar composition: a 290-230 °C fluid dominated by meteoric and volcanic waters (-3‰ to -0‰ δ18Owater), with geothermal features. The last tectonic-hydrothermal mineralization episode (E4), interpreted to have formed at lower temperatures, could be related to this late tectonic and hydrothermal activity.

The use of residual geothermal energy in an edible mushroom production plant, Los Humeros geothermal fields (Mexico): Achievements and alternatives; El uso de la energia geotermica residual en la planta productora de hongos comestibles del campo geotermico Los Humeros (Mexico): Logros y alternativas

Energy Technology Data Exchange (ETDEWEB)

Rangel Rangel, Maria Elena [Proteccion ambiental, Puebla (Mexico)

2000-12-01

A plant for raising edible mushrooms with residual geothermal energy is a project of the Comision Federal de Electricidad (CFE). The results reflect important achievements in the development of technology for the productions of wholesome and available food with geothermal heat instead of conventional energy sources. The installations have an enormous technological and commercial potential- demonstrated by the cultivation of oyster mushrooms (Pleurotus ostreatus), which success has awakened the interest of research institutions. The Instituto of Ecologia, A.C., has begun a joint project with CFE cultivating shiitake mushrooms (Lentinula edodes) with geothermal energy. These achievements mark a clear trend toward the integral use of facilities, the establishment of a crop with greater economic advantages, and the diffusion of this project. [Spanish] La planta productora de hongos comestibles es un proyecto de la Comision Federal de Electricidad (CFE) para dar un uso alterno a la energia geotermica residual. Los resultados obtenidos hasta el momento reflejan logros importantes en la generacion de tecnologia propia para la produccion de un alimento sano y accesible, sustituyendo la energia proveniente de combustibles convencionales por calor geotermico. Las instalaciones creadas cuentan con un enorme potencial tecnologico y comercial demostrando con el cultivo de las setas (Pleurotus ostreatus) con un exito tal que ha despertado el interes de instituciones dedicadas a la investigacion. Tal es el caso de Instituto de Ecologia, A.C que acualmente se encuentra involucrado en un proyecto conjunto sobre el cultivo del hongo Lentinula edodes (shiitake) utilizando energia geotermica en su proceso productivo. Con lo anterior, se esta marcando una clara tendencia hacia el aprovechamiento integral de las instalaciones, el establecimiento de un cultivo con mayores ventajas economicas y la difusion de este proyecto.

Mineralogy, structural control and age of the Incachule Sb epithermal veins, the Cerro Aguas Calientes collapse caldera, Central Puna

Science.gov (United States)

Salado Paz, Natalia; Petrinovic, Iván; Do Campo, Margarita; Brod, José Affonso; Nieto, Fernando; da Silva Souza, Valmir; Wemmer, Klauss; Payrola, Patricio; Ventura, Roberto

2018-03-01

The Incachule Sb epithermal veins is located near to the N-E rim of the Cerro Aguas Calientes collapse caldera (17.5-10.8 Ma), in the geologic province of Puna, Salta- Argentina. It is hosted in Miocene felsic volcanic rocks with continental arc signature. The district includes twelve vein systems with mineralization of Sb occurring in hydrothermal breccias and stockwork. The veins are composed of quartz-sulfide with pyrite, stibnite and arsenopyrite. All around the veins, wall rocks are variably altered to clay minerals and sulfates in an area of around 2.5 km wide by more than 7 km long. The hydrothermal alterations recognized are: silicic, phyllic and argillic. The veins are characterized by high contents of Sb, As, and Tl and intermediate contents of Pb-Zn-Cu, and traces of Ag and Au. Homogenization and ice-melting temperatures of fluid inclusions vary from 125 °C to 189 °C and -2.4 °C to -0.8 °C. The isotopic data indicated a range of δ34S -3.04‰ to +0.72‰ consistent with a magmatic source for sulfur. We present the firsts K-Ar ages for hydrothermal illite/smectite mixed layers (I/SR1, 60% illite layers) and illite that constrain the age of the ore deposit (8.5-6.7 ± 0.2 Ma). The data shown here, let characterized the Incachule district as a shallow low sulfidation epithermal system hosted in a collapse caldera. Our data also indicate that mineralization is structurally controlled by a fault system related to the 10.3 Ma collapse of Aguas Calientes caldera. The interpreted local stress field is consistent with the regional one.

Rock-magnetism and ore microscopy of the magnetite-apatite ore deposit from Cerro de Mercado, Mexico

Science.gov (United States)

Alva-Valdivia, L. M.; Goguitchaichvili, A.; Urrutia-Fucugauchi, J.; Caballero-Miranda, C.; Vivallo, W.

2001-03-01

Rock-magnetic and microscopic studies of the iron ores and associated igneous rocks in the Cerro de Mercado, Mexico, were carried out to determine the magnetic mineralogy and origin of natural remanent magnetization (NRM), related to the thermo-chemical processes due to hydrothermalism. Chemical remanent magnetization (CRM) seems to be present in most of investigated ore and wall rock samples, replacing completely or partially an original thermoremanent magnetization (TRM). Magnetite (or Ti-poor titanomagnetite) and hematite are commonly found in the ores. Although hematite may carry a stable CRM, no secondary components are detected above 580°, which probably attests that oxidation occurred soon enough after the extrusion and cooling of the ore-bearing magma. NRM polarities for most of the studied units are reverse. There is some scatter in the cleaned remanence directions of the ores, which may result from physical movement of the ores during faulting or mining, or from perturbation of the ambient field during remanence acquisition by inhomogeneous internal fields within these strongly magnetic ore deposits. The microscopy study under reflected light shows that the magnetic carriers are mainly titanomagnetite, with significant amounts of ilmenite-hematite minerals, and goethite-limonite resulting from alteration processes. Magmatic titanomagnetites, which are found in igneous rocks, show trellis, sandwich, and composite textures, which are compatible with high temperature (deuteric) oxy-exsolution processes. Hydrothermal alteration in ore deposits is mainly indicated by martitization in oxide minerals. Grain sizes range from a few microns to >100 mm, and possible magnetic state from single to multidomain, in agreement with hysteresis measurements. Thermal spectra, continuous susceptibility measurements, and IRM (isothermal remanent magnetization) acquisition suggest a predominance of spinels as magnetic carriers, most probably titanomagnetites with low

A bottom-driven mechanism for distributed faulting in the Gulf of California rift

Science.gov (United States)

Persaud, Patricia; Tan, Eh; Contreras, Juan; Lavier, Luc

2017-11-01

Observations of active faulting in the continent-ocean transition of the Northern Gulf of California show multiple oblique-slip faults distributed in a 200 × 70 km2 area developed some time after a westward relocation of the plate boundary at 2 Ma. In contrast, north and south of this broad pull-apart structure, major transform faults accommodate Pacific-North America plate motion. Here we propose that the mechanism for distributed brittle deformation results from the boundary conditions present in the Northern Gulf, where basal shear is distributed between the Cerro Prieto strike-slip fault (southernmost fault of the San Andreas fault system) and the Ballenas Transform Fault. We hypothesize that in oblique-extensional settings whether deformation is partitioned in a few dip-slip and strike-slip faults, or in numerous oblique-slip faults may depend on (1) bottom-driven, distributed extension and shear deformation of the lower crust or upper mantle, and (2) the rift obliquity. To test this idea, we explore the effects of bottom-driven shear on the deformation of a brittle elastic-plastic layer with the help of pseudo-three dimensional numerical models that include side forces. Strain localization results when the basal shear abruptly increases in a step-function manner while oblique-slip on numerous faults dominates when basal shear is distributed. We further explore how the style of faulting varies with obliquity and demonstrate that the style of delocalized faulting observed in the Northern Gulf of California is reproduced in models with an obliquity of 0.7 and distributed basal shear boundary conditions, consistent with the interpreted obliquity and boundary conditions of the study area.

Vsjo natshalos s oshibki / Boris Tuch

Index Scriptorium Estoniae

Tuch, Boris, 1946-

2007-01-01

Mängufilm "Paabel" ("Babel") : stsenarist Guillermo Arriaga : režissöör Alejandro Gonzalez Inarritu : operaator Rodrigo Prieto : osades Brad Pitt, Kate Blanchett : Ameerika Ühendriigid - Mehhiko, 2006

Initial distribution of pressure and temperature in the geothermal field of Los Humeros, Puebla; Distribucion inicial de presion y temperatura del campo geotermico de Los Humeros, Puebla

Energy Technology Data Exchange (ETDEWEB)

Arellano Gomez, Victor M.; Garcia Gutierrez, Alfonso; Barragan Reyes, Rosa Maria; Aragon Aguilar, Alfonso; Pizano, Arturo [Instituto de Investigaciones Electricas, Temixco, Morelos (Mexico)

2000-07-01

In order to infer the distributions of non disturbed pressure and temperature of the reservoir fluid, a considerable amount of information originating from several disciplines was analyzed, corresponding to 42 wells of the geothermal field of Los Humeros. On the base of the analyzed data models were developed, in one and two dimensions, of the reservoir in an initial state. The models reveal the existence of at least two reservoirs. The first one and most superficial is located between 1600 and 1025 m.a.s.l. and it is a reservoir of dominant liquid. The pressure profile of this reservoir corresponds to a boiling water column approximately between 300 and 339 Celsius degrees. The second reservoir is located underneath the 850 m.a.s.l. and as far as the collected data, it can be said that it extends at least until the 100 m.a.s.l and it is estimated that it is a reservoir of low liquid saturation. For the wells that are fed from this zone of the field temperatures between 300 and 400 Celsius degrees were estimated. A table of the geology of the subsoil of the region of the Los Humeros is shown and a table where the chemical composition of the separated water is indicated and the enthalpy of some of the wells of Los Humeros, Puebla, Mexico. [Spanish] Para inferir las distribuciones de presion y temperatura no perturbadas del fluido del yacimiento, se analizo una considerable cantidad de informacion proveniente de varias disciplinas, correspondiente a 42 pozos del campo geotermico de Los Humeros. Sobre la base de los datos analizados se desarrollaron modelos, en una y dos dimensiones, del yacimiento en un estado inicial. Los modelos revelan la existencia de cuando menos dos yacimientos. El primero y mas superficial se encuentra localizado entre 1600 y 1025 m.s.n.m. y es un yacimiento de liquido dominante. El perfil de presion de este yacimiento corresponde a una columna de agua en ebullicion aproximadamente entre 300 y 339 grados centigrados. El segundo yacimiento se

Paleoparasitological finding of eggs of nematodes in rodent coprolites dated at the early Holocene from the archaeological site Cerro Casa de Piedra 7, Santa Cruz, Argentina.

Science.gov (United States)

Sardella, N H; Fugassa, M H

2011-12-01

The aim of the present study was to examine the parasite remains present in rodent coprolites collected from the archaeological site Cerro Casa de Piedra 7 (CCP7), located in the Perito Moreno National Park (47°57'S, 72°05'W), Santa Cruz Province, Argentina. Eight coprolites obtained from the layer 17, dated at 10,620 ± 40 to 9,390 ± 40 yr B.P., were examined for parasites. Feces were processed whole, rehydrated, homogenized, subjected to spontaneous sedimentation, and examined via light microscopy. Eggs of parasites were measured and photographed. Seven of 8 coprolites possessed 199 eggs of 2, probably new, species of nematodes, including 43 eggs of Heteroxynema sp. Hall, 1916 (Cavioxyura sp. Quentin, 1975) (Oxyurida, Heteroxynematidae), and 156 eggs of Trichuris sp. Roederer, 1761 (Trichinellida, Trichuridae). Heteroxynema sp. is cited for the first time from ancient material worldwide. The finding of Trichuris spp. in both rodents and other host samples from the area under study is indicative of the stability of the biological and environmental conditions for this nematode genus to establish in the Patagonian Early Holocene. The rodent host was assigned to an unknown species of Caviomorpha (Hystricognathi) that lived during the Pleistocenic transition in Patagonia.

Effect of artificial feeders on pollen loads of the hummingbirds of Cerro de La Muerte, Costa Rica

Directory of Open Access Journals (Sweden)

Gerardo Avalos

2012-03-01

Full Text Available Although sugar-water feeders are commonly used by enthusiasts to attract hummingbirds, little is known about how they affect hummingbird behavior and flower use. We studied the highland hummingbird assemblage of Cerro de La Muerte, Costa Rica, both at a site with permanent feeders (La Georgina Restaurant and further from it. We examined how feeder use and monopolization affected seasonal changes in pollen loads during four sampling periods, including dry and wet seasons, from 2003-2005. We expected that species monopolizing the feeders would carry little or no pollen whatsoever, and would have pollen loads characterized by low floral diversity, in contrast with species less dependent on feeders. We obtained pollen samples from 183 individuals of four hummingbird species captured around the feeders using mist nets, which were compared with a pollen reference collection of plants with a pollination syndrome by hummingbirds. The same methods were implemented at a site 3km away from the feeders. Feeder usage was quantified by counting the number of times hummingbirds drank from the feeders in periods of 4min separated by 1min. The effects of hummingbird species and season on pollen load categories were assessed using a nominal logistic regression. The alpha species at the site, the Fiery-throated Hummingbird (Panterpe insignis, dominated the feeders during the dry season. Meanwhile, in the wet season, feeder usage was more evenly distributed across species, with the exception of the Volcano Hummingbird, Selasphorus flammula, which occupies the last place in the dominance hierarchy. Pollen loads of hummingbirds captured near feeders were low in abundance (more than 50% of captured individuals had zero or low pollen loads, and low in species richness (96% of the hummingbirds with pollen from only one plant genus, Centropogon. Overall pollen loads increased during the dry season coinciding with peaks in flower availability, although the majority of

Pretensioonikas embus / Kadri Kõusaar

Index Scriptorium Estoniae

Kõusaar, Kadri

2007-01-01

Mängufilm "Paabel" ("Babel") : stsenarist Guillermo Arriaga : režissöör Alejandro Gonzalez Inarritu : operaator Rodrigo Prieto : peaosades Cate Blanchett, Brad Pitt, Gael Garcia Bernal : Ameerika Ühendriigid - Mehhiko, 2006

Geochemical characteristics of water from the reservoir of the hydrothermal system of Las Tres Virgenes, Baja California Sur, Mexico; Caracteristicas geoquimicas de las aguas del reservorio del sistema hidrotermal actual de Las Tres Virgenes, Baja California Sur, Mexico

Energy Technology Data Exchange (ETDEWEB)

Gonalez Partida, Eduardo [Universidad Nacional Autonoma de Mexico (Mexico); Tello Hinojosa, Enrique [Comision Federal de Electricidad (Mexico); Pal Verma, Mahendra [Instituto de Investigaciones Electricas (Mexico)

2001-03-01

The Las Tres Virgenes geothermal field is a liquid dominated system. The separated produced by the wells are sodium-chloride type, which is a characteristic of totally equilibrated geothermal brine. The temperature of water-rock interaction in the reservoir is 280 Celsius degrees. the chemical composition of gases corresponds to the one expected in a geothermal environment. The CO{sub 2} is the predominating gas and it is superior in 90% in weight to the total of existing gases. The gas contents is less than 1% in weight, in the case of the wells LV-1 and LV-3. It is also possible to conclude that the gases are in equilibrium with the liquid phase at a temperature of 280 Celsius degrees. With respect to water quality, it is saline, from high to very high and the contents of exchangeable sodium is also very high, resulting in waters not fit for agricultural usage. [Spanish] El yacimiento geotermico de Las Tres Virgenes, en Baja California Sur, Mexico, es un sistema de liquido dominante, en donde el agua separada producida por los pozos presenta un caracter clorurado-sodico caracteristico de una salmuera de origen geotermico totalmente equilibrada. El sistema agua-roca se encuentra en equilibrio a una temperatura de 280 grados centigrados , dicha temperatura son congruentes con las estimadas para las fases gaseosas y liquidas. La composicion quimica de los gases corresponde a la esperada en un ambiente geotermico. El CO{sub 2} es el predominante y es superior a 90% en peso del total de los gases presentes. El contenido de gas es menor de 1% en peso en el caso de los pozos LV-1 y LV-3. Tambien se puede concluir que los gases estan en equilibrio en las fases liquidas a una temperatura de 280 grados centigrados. Con respecto a la calidad del agua, presenta una salinidad de alta a muy alta y el contenido de sodio intercambiable tambien es muy alto, por lo que dichas aguas no son muy aptas para el cultivo.

La aldea del Hierro Inicial del Cerro de San Vicente (Salamanca, España: Resultados de las excavaciones entre 1990 y 2006 a la luz de algunos debates actuales

Directory of Open Access Journals (Sweden)

Antonio BLANCO-GONZÁLEZ

2017-01-01

Full Text Available Este artículo recoge algunos de los principales resultados de las excavaciones arqueológicas efectuadas entre 1990 y 2006 en el yacimiento de la Primera Edad del Hierro (800-400 cal AC del Cerro de San Vicente (Salamanca. El trabajo aborda dos cuestiones mal conocidas, centrándose en las últimas ocupaciones del asentamiento, por ser las mejor investigadas: a los procesos de formación y acumulación de restos en una aldea con arquitectura de barro; y b una caracterización social de sus habitantes. La anatomía interna de este asentamiento muestra la persistencia de usos y la superposición de desechos y estructuras. Las viviendas carecen de enseres domésticos, aparecen colmatadas con adobes y en ocasiones incendiadas. Respecto a la organización social, se detectan síntomas de división interna: las casas con atrio y sus dependencias auxiliares se cercan. Las estrategias agrarias complejas constatadas pudieron haber facilitado la acumulación de riqueza por algunas familias, dentro de una organización social heterárquica.

Maailm kui globaalne piirsituatsioon / Jan Kaus

Index Scriptorium Estoniae

Kaus, Jan, 1971-

2007-01-01

Mängufilm "Paabel" ("Babel") : stsenarist Guillermo Arriaga : režissöör Alejandro Gonzalez Inarritu : operaator Rodrigo Prieto : peaosades Cate Blanchett, Brad Pitt, Gael Garcia Bernal, Koji Yokusho : Ameerika Ühendriigid - Mehhiko, 2006

"Paabel" kuulutab meile ette hävingut / Marianne Kõrver

Index Scriptorium Estoniae

Kõrver, Marianne, 1980-

2007-01-01

Mängufilm "Paabel" ("Babel") : stsenarist Guillermo Arriaga : režissöör Alejandro Gonzalez Inarritu : operaator Rodrigo Prieto : peaosades Cate Blanchett, Brad Pitt, Gael Garcia Bernal, Koji Yokusho : Ameerika Ühendriigid - Mehhiko, 2006

Geothermics and neural networks: A first approach; Geotermia y redes neuronales: Una primera aproximacion

Energy Technology Data Exchange (ETDEWEB)

Flores Armenta, Magaly del Carmen [Gerencia de Proyectos Geotermoelectricos de la Comision Federal de Electricidad, Morelia (Mexico); Barragan Orbe, Carlos [Comision Federal de Electricidad, Mexico, D. F. (Mexico)

1995-09-01

Neural networks have been hailed as the greatest technological advance since the transistor. They are predicted to be a common household item by the year 2000. This new form of machine intelligence is able to solve problems, without using rules of math, they only need examples to learn from. The first geothermal problem, to solve with this powerful tool, is the prediction of liquid and steam production, as well as the well`s termination in Los Humeros, Puebla, Mexico. The first attempt shows the learning`s capacity of the developed model, and its precision on the predictions that were done. [Espanol] Las redes neuronales se consideran como uno de los mas grandes avances tecnologicos desde la invencion del transistor, de tal forma que se perfilan como una de las herramientas mas comunes del ano 2000. Esta nueva forma de inteligencia artificial es capaz de resolver problemas sin utilizar reglas matematicas, solamente requiere de ejemplos para aprender de ellos. El primer problema geotermico, atacado con esta poderosa herramienta, es la prediccion de las producciones de vapor y liquido, asi como la terminacion de pozos en el campo geotermico de Los Humeros, Puebla, Mexico. Los primeros intentos demuestran la capacidad de aprender del modelo desarrollado, y su certeza en las predicciones realizadas.

Prácticas de sacrificio en el Cerro de la Mesa (Alcolea de Tajo, Toledo: el depósito ritual de la Casa 1

Directory of Open Access Journals (Sweden)

Ana CABRERA DÍEZ

2014-06-01

Full Text Available Los depósitos con restos óseos animales enterrados bajo el pavimento en ámbitos domésticos forman parte de prácticas rituales bien conocidas en la Protohistoria peninsular, tradicionalmente asociadas a la fundación o remodelación de nuevos edificios o a ritos vinculados a la propiciación y la fertilidad. Aunque los ejemplos mejor estudiados se encuentran en la zona levantina, el fenómeno también se conoce en yacimientos del interior. Este artículo tiene por objeto presentar un depósito ritual excavado en el poblado vetón del Cerro de la Mesa, en el valle medio del Tajo, cuyas características formales lo emparentan con las ofrendas domésticas de la zona ibérica. Se trata de un hoyo situado en el umbral de la Casa 1, que contiene los restos seleccionados de varios ovinos y un pequeño cuenco cerámico colocado en posición invertida. El análisis de los restos óseos, el contenido del cuenco y el estudio del contexto arqueológico en que se situaba el depósito han permitido relacionarlo con prácticas de sacrificio y libación dentro del marco de la religiosidad vetona. Este trabajo pretende igualmente contribuir a la formación de un corpus peninsular de inhumaciones rituales de animales en contextos domésticos, que impulse el adecuado estudio de la ritualidad protohistórica.

Effect of artificial feeders on pollen loads of the hummingbirds of Cerro de La Muerte, Costa Rica

Directory of Open Access Journals (Sweden)

Gerardo Avalos

2012-03-01

Full Text Available Although sugar-water feeders are commonly used by enthusiasts to attract hummingbirds, little is known about how they affect hummingbird behavior and flower use. We studied the highland hummingbird assemblage of Cerro de La Muerte, Costa Rica, both at a site with permanent feeders (La Georgina Restaurant and further from it. We examined how feeder use and monopolization affected seasonal changes in pollen loads during four sampling periods, including dry and wet seasons, from 2003-2005. We expected that species monopolizing the feeders would carry little or no pollen whatsoever, and would have pollen loads characterized by low floral diversity, in contrast with species less dependent on feeders. We obtained pollen samples from 183 individuals of four hummingbird species captured around the feeders using mist nets, which were compared with a pollen reference collection of plants with a pollination syndrome by hummingbirds. The same methods were implemented at a site 3km away from the feeders. Feeder usage was quantified by counting the number of times hummingbirds drank from the feeders in periods of 4min separated by 1min. The effects of hummingbird species and season on pollen load categories were assessed using a nominal logistic regression. The alpha species at the site, the Fiery-throated Hummingbird (Panterpe insignis, dominated the feeders during the dry season. Meanwhile, in the wet season, feeder usage was more evenly distributed across species, with the exception of the Volcano Hummingbird, Selasphorus flammula, which occupies the last place in the dominance hierarchy. Pollen loads of hummingbirds captured near feeders were low in abundance (more than 50% of captured individuals had zero or low pollen loads, and low in species richness (96% of the hummingbirds with pollen from only one plant genus, Centropogon. Overall pollen loads increased during the dry season coinciding with peaks in flower availability, although the majority of

Effect of artificial feeders on pollen loads of the hummingbirds of Cerro de la Muerte, Costa Rica.

Science.gov (United States)

Avalos, Gerardo; Soto, Alejandra; Alfaro, Willy

2012-03-01

Although sugar-water feeders are commonly used by enthusiasts to attract hummingbirds, little is known about how they affect hummingbird behavior and flower use. We studied the highland hummingbird assemblage of Cerro de La Muerte, Costa Rica, both at a site with permanent feeders (La Georgina Restaurant) and further from it. We examined how feeder use and monopolization affected seasonal changes in pollen loads during four sampling periods, including dry and wet seasons, from 2003-2005. We expected that species monopolizing the feeders would carry little or no pollen whatsoever, and would have pollen loads characterized by low floral diversity, in contrast with species less dependent on feeders. We obtained pollen samples from 183 individuals of four hummingbird species captured around the feeders using mist nets, which were compared with a pollen reference collection of plants with a pollination syndrome by hummingbirds. The same methods were implemented at a site 3km away from the feeders. Feeder usage was quantified by counting the number of times hummingbirds drank from the feeders in periods of 4min separated by 1min. The effects of hummingbird species and season on pollen load categories were assessed using a nominal logistic regression. The alpha species at the site, the Fiery-throated Hummingbird (Panterpe insignis), dominated the feeders during the dry season. Meanwhile, in the wet season, feeder usage was more evenly distributed across species, with the exception of the Volcano Hummingbird, Selasphorus flammula, which occupies the last place in the dominance hierarchy. Pollen loads of hummingbirds captured near feeders were low in abundance (more than 50% of captured individuals had zero or low pollen loads), and low in species richness (96% of the hummingbirds with pollen from only one plant genus, Centropogon). Overall pollen loads increased during the dry season coinciding with peaks in flower availability, although the majority of captured

Oral pathology in the Iberian Neanderthals

African Journals Online (AJOL)

enoh

2012-03-20

Mar 20, 2012 ... The specimen studied herein, a mandible catalogued as. SDR 7-8 (SIDRON ... corresponds to the dorsal third of the sigmoid notch and condyle. (Prieto et al. ... angle, there is a rounded protrusion, with fracture of the internal.

Duplicación, redundancia y ética en las publicaciones médicas

Directory of Open Access Journals (Sweden)

Germán Enrique Pérez Romero

2006-10-01

Full Text Available A raíz de la reciente publicación del trabajo de Rodríguez J, Prieto S, Ortiz L, Bautista A, Bernal P, Vargas N. Diagnóstico Matemático de la Monitoría Fetal. Aplicando la Ley de Zipf-Mandelbrott; en el número 2 del volumen 54 de nuestra revista (1 y la simultánea aparición en la Revista Colombiana de Obstetricia y Ginecología de: Rodríguez J, Prieto S, Ortiz L, Bautista A, Álvarez L, Correa C, Avilán N. Diagnóstico matemático de la monitoría fetal con la Ley de Zipf-Mandelbrot y la teoría de los sistemas dinámicos aplicados a la fisiología cardiaca (2; el editor desea precisar como es costumbre en las revistas médicas que (3:

Measurements of downwelling far-infrared radiance during the RHUBC-II campaign at Cerro Toco, Chile and comparisons with line-by-line radiative transfer calculations

Science.gov (United States)

Mast, Jeffrey C.; Mlynczak, Martin G.; Cageao, Richard P.; Kratz, David P.; Latvakoski, Harri; Johnson, David G.; Turner, David D.; Mlawer, Eli J.

2017-09-01

Downwelling radiances at the Earth's surface measured by the Far-Infrared Spectroscopy of the Troposphere (FIRST) instrument in an environment with integrated precipitable water (IPW) as low as 0.03 cm are compared with calculated spectra in the far-infrared and mid-infrared. FIRST (a Fourier transform spectrometer) was deployed from August through October 2009 at 5.38 km MSL on Cerro Toco, a mountain in the Atacama Desert of Chile. There FIRST took part in the Radiative Heating in Unexplored Bands Campaign Part 2 (RHUBC-II), the goal of which is the assessment of water vapor spectroscopy. Radiosonde water vapor and temperature vertical profiles are input into the Atmospheric and Environmental Research (AER) Line-by-Line Radiative Transfer Model (LBLRTM) to compute modeled radiances. The LBLRTM minus FIRST residual spectrum is calculated to assess agreement. Uncertainties (1-σ) in both the measured and modeled radiances are also determined. Measured and modeled radiances nearly all agree to within combined (total) uncertainties. Features exceeding uncertainties can be corrected into the combined uncertainty by increasing water vapor and model continuum absorption, however this may not be necessary due to 1-σ uncertainties (68% confidence). Furthermore, the uncertainty in the measurement-model residual is very large and no additional information on the adequacy of current water vapor spectral line or continuum absorption parameters may be derived. Similar future experiments in similarly cold and dry environments will require absolute accuracy of 0.1% of a 273 K blackbody in radiance and water vapor accuracy of ∼3% in the profile layers contributing to downwelling radiance at the surface.

Translations on Eastern Europe Political, Sociological, and Military Affairs, Number 1363

Science.gov (United States)

1977-03-10

help of the socialist countries. Moises Prieto, director of Peruvian television, said that the positive reasonance of the GDR program broadcast in...we publish over 70 million copies of books or eight times as many as before liberation. The audiences of theatres, concerts and cinemas and the

Species Profiles: Life Histories and Environmental Requirements of Coastal Fishes and Invertebrates (South Florida): Gray, Lane, Mutton and Yellowtail Snappers.

Science.gov (United States)

1986-06-01

pargo prieto, pargo, criollo , vivaneau sorbe (Cervigon pargo dienton, pargo de piedra, 1966, Fisher 1978) pargo moreno, vivaneau sarde grise, aquadera... criollo , Lutjanus 1970-79. Florida landings, analis. Cent. Invest. Pesq. annual summary 1969-1978. U.S. uba. Nota 2:1-16. Natl. Mar. Fish. Serv. Curr

Fifteen years of seismic monitoring at the Las Tres Virgenes, BCS, geothermal field; Quince anos de monitoreo sismico en el campo geotermico de Las Tres Virgenes, BCS

Energy Technology Data Exchange (ETDEWEB)

Ortiz Prieto, Irais; Lorenzo Pulido, Cecilia [Comision Federal de Electricidad, Gerencia de Proyectos Geotermoelectricos, Morelia, Michoacan (Mexico)]. E-mail: cecilia.lorenzo@cfe.gob.mx

2009-07-15

Seismic monitoring at the Las Tres Virgenes, BCS, geothermal field started in 1992 with an analog station of vertical components detecting a large number of earthquakes of varying magnitudes. In February 1993, a seismic network was installed, composed of six digital stations DR-2000-with S-6000 and S-5000 sensors and three registration channels (N-S, E-W and vertical). This was the basis for the development of a program to correct arrival-time data for P and S waves due to instrument drift. From January to April 1994 and May to August 1995, based on the 170 seismic events recorded, a velocity model was proposed. From December 1995 to July 1996, seismic data were processed and interpreted, and zones of occurrence were determined for events according to magnitude and the predominant noise in the field. From September 2003 to December 2004, 10 seismic stations (permanent and temporary) were installed and monitored and it was concluded the most active fault system was El Volcan. From September to December 2004, production wells LV-4 and LV-13 were acid-stimulated and seismic monitoring during this period allowed for the definition of two important seismic zones, both related to the El Volcan fault system and to injection well LV-8. After reopening these production wells, it was concluded an increase in seismic activity had occurred. From May to August 2006, information was compiled from the seismic network and it was concluded El Partido had became the most active fault system. Presently the seismic network in this field is composed of one SARA station and four K2 units. The SARA station is telemetrically connected to the base station. [Spanish] En el campo geotermico de Las Tres Virgenes, BCS, el monitoreo sismico empezo a partir de 1992 con una sola estacion analogica de registro vertical, la cual detecto una gran cantidad de temblores de distintas magnitudes. En febrero de 1993 se instalo una red sismica con seis estaciones digitales DR-2000 con sensores S-6000 y S

The Springhill Formation (Jurassic-Cretaceous) as a potential low enthalpy geothermal reservoir in the Cerro Sombrero area, Magallanes Basin, Chile.

Science.gov (United States)

Lagarrigue, S. C.; Elgueta, S.; Arancibia, G.; Morata, D.; Sanchez, J.; Rojas, L.

2017-12-01

Low enthalpy geothermal energy technologies are being developed around the world as part of policies to replace the use of conventional sources of energy by renewable ones. The reuse of abandoned oil and gas wells in sedimentary basins, whose reservoirs are saturated with water at temperatures above 120°C, is of increasing interest due to the low initial cost.In Chile, interest in applying this technology is focused on the Magallanes Basin (Austral Basin in Argentina) in the extreme south of the country, where important hydrocarbon deposits have been exploited for more than six decades with more than 3,500 wells drilled to depths of over 4,000m. Hydrocarbons have been extracted mainly from the Upper Jurassic to lowermost Cretaceous Springhill Formation, which includes sandstone lithofacies with porosities of 12% to 19% and permeability of 10mD and 1100mD. This formation has been drilled mainly at depths of 1500m to 3000m, the estimated geothermal gradient in the zone is 4.9 °C/100m with well bottom temperature measurements oscillating between 60° and 170°C, sufficient for district heating, and even, electricity generation by means of ORC technologies.To understand in detail the behavior and distribution of the different lithofacies of the Springhill Formation in the Sombrero Oil and Gas Field, sedimentological and geological 3D models have been generated from existing well logs and seismic data. To comprehend the quality of the reservoirs on the other hand, many petrophysical studies of drill core samples representative of the different lithofacies, complemented by electric well log interpretations, were carried out. Results confirm the existence of at least two quartz-rich sandstone lithofacies as potential geothermal reservoirs. In the principal settlement in this area, Cerro Sombrero township (1,800 population), the annual average temperature is 6.4°C, requiring constant domestic heating which, at present comes exclusively from natural gas. The study shows

Emplacement and deformation of the Cerro Durazno Pluton delineates stages of the lower Paleozoic tectono-magmatic evolution in NW-Argentina

Science.gov (United States)

Hongn, F.; Riller, U.

2003-04-01

Regional-scale transpression and transtension are considered to be important in the lower Paleozoic tectono-magmatic evolution of metamorphic and granitoid basement rocks of the southern central Andes. In order to test whether such kinematic changes affected Paleozoic basement rocks on the local scale, i.e. in the Eastern Cordillera of NW-Argentina, we performed a detailed field-based structural analysis of the 456 Ma granitoid Cerro Durazno pluton (CDP). The results of our analysis point to the following stages in the geodynamic evolution of this area: (1) Metamorphism and deformation of Neoproterozoic-Paleozoic basement rocks occurred at high T and low to medium P prior to emplacement of the CDP. This lead to the formation of schists and migmatites characterized by pervasive planar and linear mineral shape fabrics and the growth of andalusite, cordierite and fibrolite. (2) Magmatic foliation in the CDP is defined by the shape-preferred orientation of euhedral feldspar phenocrysts and microgranitoid enclaves. These fabrics are concordant to the NE-SW striking intrusive contact with migmatitic host rocks. The lack of submagmatic or high-T solid-state fabrics in the CDP may indicate that cooling and solidification of granitoid magma was not accompanied by regional deformation. Alternatively, emplacement of granitoid magma may have been facilitated by the creation of open space at mid-crustal level induced by regional deformation. (3) Ductile deformation under greenschist metamorphic conditions overprinted magmatic fabrics of the CDP. This is evident by NW-SE striking metamorphic foliation surfaces transecting magmatic shape fabrics at high angles. During this deformation, the pluton was thrust on a SW-dipping shear zone toward the NE over low-grade metamorphic host rocks which lead to a condensation of metamorphic isograds in the host rocks. Ages of strained pegmatitic dikes indicate that this deformation occurred at about 430 Ma. In summary, the difference in age

Recycling of water, carbon, and sulfur during subduction of serpentinites: A stable isotope study of Cerro del Almirez, Spain

Science.gov (United States)

Alt, Jeffrey C.; Garrido, Carlos J.; Shanks, Wayne C.; Turchyn, Alexandra; Padrón-Navarta, José Alberto; López Sánchez-Vizcaíno, Vicente; Gómez Pugnaire, María Teresa; Marchesi, Claudio

2012-01-01

We use the concentrations and isotope compositions of water, carbon, and sulfur in serpentinites and their dehydration products to trace the cycling of volatiles during subduction. Antigorite serpentinites from the Cerro del Almirez complex, Spain, contain 9–12 wt.% H2O and 910 ± 730 ppm sulfur, and have bulk δ18O values of 8.6 ± 0.4‰, δD = − 54 ± 5‰, and δ34S = 5.0‰, consistent with serpentinization at temperatures of ~ 200 °C by seawater hydrothermal fluids in a seafloor setting. The serpentinites were dehydrated to chlorite–harzburgite (olivine + orthopyroxene + chlorite) at 700 °C and 1.6–1.9 GPa during subduction metamorphism, resulting in loss of water, and sulfur. The chlorite–harzburgites contain 5.7 ± 1.9 wt.% H2O, and have bulk δ18O = 8.0 ± 0.9‰, and δD = − 77 ± 11‰. The rocks contain 650 ± 620 ppm sulfur having δ34S = 1.2‰. Dehydration of serpentinite resulted in loss of 5 wt.% H2O having δ18O = 8–10‰ and δD = − 27 to − 65‰, and loss of 260 ppm sulfur as sulfate, having δ34S = 14.5‰. The contents and δ13C of total carbon in the two rock types overlap, with a broad trend of decreasing carbon contents and δ13C from ~ 1300 to 200 ppm and − 9.6 to − 20.2‰. This reflects mixing between reduced carbon in the rocks (210 ppm, δ13C ≈ − 26‰) and seawater-derived carbonate (δ13C ≈ − 1‰). Our results indicate: 1) Serpentinized oceanic peridotites carry significant amounts of isotopically fractionated water, carbon and sulfur into subduction zones; 2) Subduction of serpentinites to high P and T results in loss of water, and sulfur, which can induce melting and contribute to 18O, D, and 34S enrichments and oxidation of the sub-arc mantle wedge; and 3) Isotopically fractionated water, carbon, and sulfur in serpentinite dehydration products are recycled deeper into the mantle where they can contribute to isotope heterogeneities and may be significant for volatile budgets of the deep Earth.

Proposal to neutralize acid fluids from wells in the Los Humeros, Pue., geothermal field; Propuesta para la neutralizacion de fluidos acidos provenientes de pozos del campo geotermico de Los Humeros, Pue.

Energy Technology Data Exchange (ETDEWEB)

Flores Armenta, Magaly del Carmen; Ramirez Montes, Miguel; Garcia Cuevas, Juan Manuel [Comision Federal de Electricidad, Gerencia de Proyectos Geotermoelectricos, Morelia, Michoacan (Mexico)]. E-mail: magaly.flores@cfe.gob.mx

2009-07-15

Neutralizing an acidic fluid consists of adding a sodium hydroxide solution to neutralize the H group of acids, therefore increasing the pH. The injection of sodium hydroxide has to be continuous and at a proper depth inside the well to protect against the corrosion of casing and surface equipment. Neutralization is a common practice used in geothermal fields, such as at The Geysers in the US and Miravalles in Costa Rica-places where aggressive fluids cause problems for extracting and using geothermal fluids commercially. A zone surrounding wells H-4, H-16 and H-29 in the northern section of the Los Humeros, Pue., geothermal field, known as the Colapso Central, has shown evidence of aggressively acidic fluids. Several wells drilled in the area had to be repaired, thus plugging and isolating the deepest production zones. Well H-43 was drilled two years ago in the northern zone of the field, and even though it is not located in the aggressive-fluid zone, the well presents mineralogical features possibly indicating the presence of acidic fluids. Therefore, before producing this well it has been proposed we install a neutralization system with general characteristics presented in this paper. The system will prevent corrosion that up to now has prevented exploitation of the deep portion of Colapso Central, helping to develop the field in a more profitable way. [Spanish] Neutralizar un fluido acido consiste en agregarle una solucion de hidroxido de sodio. Esto neutraliza el grupo de acidos H y en consecuencia aumenta el pH. La inyeccion de hidroxido de sodio se realiza de manera continua y a una profundidad adecuada dentro del pozo para proteger a la tuberia y a todo el equipo superficial contra la corrosion. La neutralizacion es una practica comun que se viene realizando en campos como Los Geysers en Estados Unidos y en Miravalles, Costa Rica, donde la presencia de fluidos agresivos causa problemas en la extraccion y aprovechamiento del fluido geotermico con fines

Study of the mining possibilities in the surroundings of Mahoma - Guaycuru phase I Feasibility of the mafic body of Mahoma-Guaycuru and of the complex mafic - Stratified ultramafic of the Cerros Negros and San Jose and Colonia provinces

International Nuclear Information System (INIS)

Coronel, N.; Techera, J.; Ramos, E.; Pineyro, G.

1990-01-01

In Mahoma - Guaycuru area has been carried out regional cartography to place the geologic context, mainly the Mahoma bodies magmatic intrusive s, Guaycuru and Cerros Negros. The area has good mining possibilities due to their geologic environment. They exist also geochemical anomalies in the area that they should be taken as base for future works in the same one. In this environment studies were begun with the bodies magmatic mafic and ultramafic, due to its feasibility in Platino ides, Chromium, Nickel, Cobalt . It intent to adjust in a following stage (it Leaves II) a work methodology in an occurrence of minerals metallic. for future works,la occurrence of metallic minerals it lacks elements of economic interest in concentrations high, just as it demonstrates it the geochemical of rocks carried out, and the lack of anomalies in the geochemical of active silts and of floors. As element of interest single Gold appears in samples alluvial deposits but their source would not be the mafic rocks. Other occurrence of metallic minerals appears

Sadhana | Indian Academy of Sciences

Indian Academy of Sciences (India)

Home; Journals; Sadhana. A M CAMACHO. Articles written in Sadhana. Volume 42 Issue 12 December 2017 pp 2147-2155. Quantitative analysis of prediction models for hot cracking in industrial stainless steels using standardized requirements · A RODRÍGUEZ-PRIETO A M CAMACHO M A SEBASTIÁN · More Details ...

Estimation of production characteristic curves of geothermal wells and of the permeability of rocky formations through one single mass flow-pressure-enthalpy (W-P-h) measurement at the wellhead; Estimacion de curvas caracteristicas de produccion de pozos geotermicos y de permeabilidades de formaciones rocosas a partir de una sola medicion flujo masico-presion- entalpia (W-P-h) a boca de pozo

Energy Technology Data Exchange (ETDEWEB)

L Moya, Sara; Aragon, Alfonso [Instituto de Investigaciones Electricas, Cuernavaca (Mexico)

1997-12-31

The proposed methodology described ahead (Moya et al.,1996; Moya et al.,1997a, 1997b and 1997c) simplifies the construction of production characteristic curves of geothermal wells and of its associated thermal productivity, in requiring one single measurement of mass flow-pressure-enthalpy (W-P-h) at the wellhead. Therefore it is an ecological option, technically and economically more feasible. On the other hand, the methodology also allows to diagnose the rocky formation absolute permeability in the well feeding zone. This permeability is usually determined through well bottom pressure tests, than in some cases are difficult to interpret. The permeability inferred by means of the proposed technology represents a complementary tool for these field tests and for the laboratory measurements on drilling cores. [Espanol] La metodologia propuesta que se describe a continuacion [Moya et al., 1995d; Moya et al., 1996; Moya et al., 1997a, 1997b y 1997c] simplifica la construccion de curvas caracteristicas de produccion de pozos geotermicos y de su productividad termica asociada al requerir solo una medicion de flujo masico-presion-entalpia (W-P-h) a boca de pozo. Es por tanto una alternativa ecologica, tecnica y economicamente mas factible. Por otra parte, la metodologia tambien permite diagnosticar el valor de la permeabilidad absoluta de la formacion rocosa en la zona de alimentacion al pozo. Esta permeabilidad se determina usualmente a partir de pruebas de presion a fondo de pozo que en algunos casos son dificiles de interpretar. La permeabilidad inferida mediante la metodologia propuesta representa una herramienta complementaria a estas pruebas de campo y a las mediciones de laboratorio sobre nucleos de perforacion.

Estimation of production characteristic curves of geothermal wells and of the permeability of rocky formations through one single mass flow-pressure-enthalpy (W-P-h) measurement at the wellhead; Estimacion de curvas caracteristicas de produccion de pozos geotermicos y de permeabilidades de formaciones rocosas a partir de una sola medicion flujo masico-presion- entalpia (W-P-h) a boca de pozo

Energy Technology Data Exchange (ETDEWEB)

L Moya, Sara; Aragon, Alfonso [Instituto de Investigaciones Electricas, Cuernavaca (Mexico)

1998-12-31

The proposed methodology described ahead (Moya et al.,1996; Moya et al.,1997a, 1997b and 1997c) simplifies the construction of production characteristic curves of geothermal wells and of its associated thermal productivity, in requiring one single measurement of mass flow-pressure-enthalpy (W-P-h) at the wellhead. Therefore it is an ecological option, technically and economically more feasible. On the other hand, the methodology also allows to diagnose the rocky formation absolute permeability in the well feeding zone. This permeability is usually determined through well bottom pressure tests, than in some cases are difficult to interpret. The permeability inferred by means of the proposed technology represents a complementary tool for these field tests and for the laboratory measurements on drilling cores. [Espanol] La metodologia propuesta que se describe a continuacion [Moya et al., 1995d; Moya et al., 1996; Moya et al., 1997a, 1997b y 1997c] simplifica la construccion de curvas caracteristicas de produccion de pozos geotermicos y de su productividad termica asociada al requerir solo una medicion de flujo masico-presion-entalpia (W-P-h) a boca de pozo. Es por tanto una alternativa ecologica, tecnica y economicamente mas factible. Por otra parte, la metodologia tambien permite diagnosticar el valor de la permeabilidad absoluta de la formacion rocosa en la zona de alimentacion al pozo. Esta permeabilidad se determina usualmente a partir de pruebas de presion a fondo de pozo que en algunos casos son dificiles de interpretar. La permeabilidad inferida mediante la metodologia propuesta representa una herramienta complementaria a estas pruebas de campo y a las mediciones de laboratorio sobre nucleos de perforacion.

How Pore-Fluid Pressure due to Heavy Rainfall Influences Volcanic Eruptions, Example of 1998 and 2008 Eruptions of Cerro Azul (Galapagos)

Science.gov (United States)

Albino, F.; Amelung, F.; Gregg, P. M.

2016-12-01

About 30 worldwide seismic studies have shown a strong correlation between rainfall and earthquakes in the past 22 years (e.g. Costain and Bollinger, 2010). Such correlation has been explained by the phenomenon of hydro-seismicity via pore pressure diffusion: an increase of pore-fluid in the upper crust reduces the normal stress on faults, which can trigger shear failure. Although this pore pressure effect is widely known for earthquakes, this phenomenon and more broadly poro-elasticity process are not widely studied on volcanoes. However, we know from our previous works that tensile failures that open to propagate magma through the surface are also pore pressure dependent. We have demonstrated that an increase of pore pressure largely reduces the overpressure required to rupture the magma reservoir. We have shown that the pore pressure has more influence on reservoir stability than other parameters such as the reservoir depth or the edifice loading. Here, we investigate how small pore-fluid changes due to hydrothermal or aquifer refill during heavy rainfall may perturb the conditions of failure around magma reservoirs and, what is more, if these perturbations are enough to trigger magma intrusions. We quantify the pore pressure effect on magmatic system by combining 1) 1D pore pressure diffusion model to quantify how pore pressure changes from surface to depth after heavy rainfall events and 2) 2D poro-elastic numerical model to provide the evolution of failure conditions of the reservoir as a consequence of these pore pressure changes. Sensitivity analysis is also performed to characterize the influence on our results of the poro-elastic parameters (hydraulic diffusivity, permeability and porosity) and the geometry of the magma reservoir and the aquifer (depth, size, shape). Finally, we apply our methodology to Cerro Azul volcano (Galapagos) where both last eruptions (1998 and 2008) occurred just after heavy rainfall events, without any pre-eruptive inflation. In

PRIMEROS RESULTADOS SOBRE EL USO PREHISPÁNICO DE LOS VEGETALES EN EL SITIO ARQUEOLÓGICO LOS TRES CERROS 1 (VICTORIA, ENTRE RÍOS, ARGENTINA: ANÁLISIS DEL REGISTRO BIOSILÍCEO.

Directory of Open Access Journals (Sweden)

Jorge O. Sánchez

2013-01-01

Full Text Available El registro de microfósiles biosilíceos posee un alto grado de preservación en distintos contextos naturales y culturales. Por esta razón, el estudio de los fitolitos y otros microrrestos biosilíceos puede contribuir a determinar las condiciones ambientales de las comunidades vegetales que rodearon un sitio arqueológico, así como también identificar especies vegetales domesticadas. En esta contribución se rea- lizó el análisis de fitolitos en el marco de otros bioindicadores de los depósitos superiores de la secuencia sedimentaria antrópica del sitio Los Tres Cerros 1 (LTC1, isla Las Moras, Departamento Victoria, Entre Ríos, Argentina. Los análisis desarrollados permitieron identificar morfotipos silíceos relacionados con la presencia de vegetales silvestres que caracterizan a la unidad fitogeográfica actual del área de em- plazamiento, y morfotipos silíceos asignables a recursos vegetales de interés cultural, pertenecientes a las familias Arecaceae, Cucurbitaceae, y Poaceae (subfamilias Maideae y Oryzoideae. El registro de microfósiles biosilíceos del perfil del sitio LTC1 tiene un cambio neto que puede ser correlacionado con diferentes actividades culturales desempeñadas durante el proceso de construcción del montículo, que tuvo lugar durante ca.1000 - 500 años 14C AP.

Paracas geoglyphs of the peruvian south coast: Cerro Lechuza and Cerro Pico

OpenAIRE

García Soto, Rubén

2015-01-01

Traditionally, the manufacture of large found drawings on desert plains and hill slopes of the Peruvian south coast was at-tributed to the Nasca society. However, since the 1980s, it is known that this cultural manifestation is a tradition that wouldhave begun towards the 750 BC during the early part of the development of the Paracas culture. Paracas geoglyphs have beenreported from Pisco to the Rio Grande Basin of Nasca, particularly in the area of Palpa where the where they have identifiedm...

Ítems de referencia para publicar Revisiones Sistemáticas y Metaanálisis: La Declaración PRISMA

Directory of Open Access Journals (Sweden)

David Moher

2014-09-01

Full Text Available Artículo original: Moher D, Liberati A, Tetzlaff J, Altman DG, The PRISMA Group. Preferred Reporting Items for Systematic Reviews and Meta-Analyses: The PRISMA Statement. PLoS Med. 2009;6:e1000097.The original authors have not revised and verified the Spanish translation, and not necessary endorse it. Los autores originales no han revisado ni verificado la traducción del manuscrito al español, y no necesariamente están de acuerdo con su contenido.Publicación del artículo original: 21 Julio 2009 Derechos: © 2009 Moher et al. Este es un artículo de acceso abierto distribuido bajo las condiciones de The Creative Commons Attribution License, que permite el uso ilimitado, su distribución y reproducción en cualquier medio, siempre y cuando se acredite el autor y su fuente original.Procedencia: No comisionado; revisión científica externa. Para promover la publicación de la Declaración PRISMA, el artículo se ha publicado como acceso abierto y se puede encontrar en la página web de PLoS Medicine (http://medicine.plosjournals.org/ y también se ha publicado en Annals of Internal Medicine, BMJ, Journal of Clinical Epidemiology, y Open Medicine. Los autores tienen unánimemente los derechos de este artículo. Para más detalles de su uso ver la página web de PRISMA (http://www.prisma-statement.org/.Traducción y adaptación al español: Mercedes Sotos-Prieto, Johana Prieto, Maria Manera, Eduard Baladia, Rodrigo Martínez-Rodríguez y Julio Basulto.Autor de correspondencia de la traducción: Mercedes Sotos-Prieto (merchesotosprieto@gmail.com

Subsidence monitoring with geotechnical instruments in the Mexicali Valley, Baja California, Mexico

Science.gov (United States)

Glowacka, E.; Sarychikhina, O.; Márquez Ramírez, V. H.; Robles, B.; Nava, F. A.; Farfán, F.; García Arthur, M. A.

2015-11-01

The Mexicali Valley (northwestern Mexico), situated in the southern part of the San Andreas fault system, is an area with high tectonic deformation, recent volcanism, and active seismicity. Since 1973, fluid extraction, from the 1500-3000 m depth range, at the Cerro Prieto Geothermal Field (CPGF), has influenced deformation in the Mexicali Valley area, accelerating the subsidence and causing slip along the traces of tectonic faults that limit the subsidence area. Detailed field mapping done since 1989 (González et al., 1998; Glowacka et al., 2005; Suárez-Vidal et al., 2008) in the vicinity of the CPGF shows that many subsidence induced fractures, fissures, collapse features, small grabens, and fresh scarps are related to the known tectonic faults. Subsidence and fault rupture are causing damage to infrastructure, such as roads, railroad tracks, irrigation channels, and agricultural fields. Since 1996, geotechnical instruments installed by CICESE (Centro de Investigación Ciéntifica y de Educación Superior de Ensenada, B.C.) have operated in the Mexicali Valley, for continuous recording of deformation phenomena. Instruments are installed over or very close to the affected faults. To date, the network includes four crackmeters and eight tiltmeters; all instruments have sampling intervals in the 1 to 20 min range. Instrumental records typically show continuous creep, episodic slip events related mainly to the subsidence process, and coseismic slip discontinuities (Glowacka et al., 1999, 2005, 2010; Sarychikhina et al., 2015). The area has also been monitored by levelling surveys every few years and, since the 1990's by studies based on DInSAR data (Carnec and Fabriol, 1999; Hansen, 2001; Sarychikhina et al., 2011). In this work we use data from levelling, DInSAR, and geotechnical instruments records to compare the subsidence caused by anthropogenic activity and/or seismicity with slip recorded by geotechnical instruments, in an attempt to obtain more information

Subsidence monitoring with geotechnical instruments in the Mexicali Valley, Baja California, Mexico

Directory of Open Access Journals (Sweden)

E. Glowacka

2015-11-01

Full Text Available The Mexicali Valley (northwestern Mexico, situated in the southern part of the San Andreas fault system, is an area with high tectonic deformation, recent volcanism, and active seismicity. Since 1973, fluid extraction, from the 1500–3000 m depth range, at the Cerro Prieto Geothermal Field (CPGF, has influenced deformation in the Mexicali Valley area, accelerating the subsidence and causing slip along the traces of tectonic faults that limit the subsidence area. Detailed field mapping done since 1989 (González et al., 1998; Glowacka et al., 2005; Suárez-Vidal et al., 2008 in the vicinity of the CPGF shows that many subsidence induced fractures, fissures, collapse features, small grabens, and fresh scarps are related to the known tectonic faults. Subsidence and fault rupture are causing damage to infrastructure, such as roads, railroad tracks, irrigation channels, and agricultural fields. Since 1996, geotechnical instruments installed by CICESE (Centro de Investigación Ciéntifica y de Educación Superior de Ensenada, B.C. have operated in the Mexicali Valley, for continuous recording of deformation phenomena. Instruments are installed over or very close to the affected faults. To date, the network includes four crackmeters and eight tiltmeters; all instruments have sampling intervals in the 1 to 20 min range. Instrumental records typically show continuous creep, episodic slip events related mainly to the subsidence process, and coseismic slip discontinuities (Glowacka et al., 1999, 2005, 2010; Sarychikhina et al., 2015. The area has also been monitored by levelling surveys every few years and, since the 1990's by studies based on DInSAR data (Carnec and Fabriol, 1999; Hansen, 2001; Sarychikhina et al., 2011. In this work we use data from levelling, DInSAR, and geotechnical instruments records to compare the subsidence caused by anthropogenic activity and/or seismicity with slip recorded by geotechnical instruments, in an attempt to obtain

New constraints on slip rates and locking depths of the San Andreas Fault System from Sentinel-1A InSAR and GAGE GPS observations

Science.gov (United States)

Ward, L. A.; Smith-Konter, B. R.; Higa, J. T.; Xu, X.; Tong, X.; Sandwell, D. T.

2017-12-01

After over a decade of operation, the EarthScope (GAGE) Facility has now accumulated a wealth of GPS and InSAR data, that when successfully integrated, make it possible to image the entire San Andreas Fault System (SAFS) with unprecedented spatial coverage and resolution. Resulting surface velocity and deformation time series products provide critical boundary conditions needed for improving our understanding of how faults are loaded across a broad range of temporal and spatial scales. Moreover, our understanding of how earthquake cycle deformation is influenced by fault zone strength and crust/mantle rheology is still developing. To further study these processes, we construct a new 4D earthquake cycle model of the SAFS representing the time-dependent 3D velocity field associated with interseismic strain accumulation, co-seismic slip, and postseismic viscoelastic relaxation. This high-resolution California statewide model, spanning the Cerro Prieto fault to the south to the Maacama fault to the north, is constructed on a 500 m spaced grid and comprises variable slip and locking depths along 42 major fault segments. Secular deep slip is prescribed from the base of the locked zone to the base of the elastic plate while episodic shallow slip is prescribed from the historical earthquake record and geologic recurrence intervals. Locking depths and slip rates for all 42 fault segments are constrained by the newest GAGE Facility geodetic observations; 3169 horizontal GPS velocity measurements, combined with over 53,000 line-of-sight (LOS) InSAR velocity observations from Sentinel-1A, are used in a weighted least-squares inversion. To assess slip rate and locking depth sensitivity of a heterogeneous rheology model, we also implement variations in crustal rigidity throughout the plate boundary, assuming a coarse representation of shear modulus variability ranging from 20-40 GPa throughout the (low rigidity) Salton Trough and Basin and Range and the (high rigidity) Central

¿Quién está contra quién en los cerros orientales de Bogotá? La perspectiva local desde el barrio la Cecilia = Who is against who in the eastern hills of Bogotá? The local perspective from the neighborhood of la Cecilia

Directory of Open Access Journals (Sweden)

Ana María López Ortego

2016-09-01

Full Text Available Este trabajo aborda las controversias medioambientales, jurídicas y habitacionales que confluyen en el área de reserva medioambiental de los Cerros Orientales de Bogotá. La lógica socio-urbanística de la ciudad -ligada a las urbanizaciones piratas y la invasión-; los movimientos migratorios -acentuados por el conflicto armado- y la falta de definición de una política pública clara en los últimos 30 años, ha desembocado en un conflicto entre pobladores, organizaciones civiles de defensa del medioambiente, empresas privadas e instituciones públicas, mediados casi exclusivamente por resoluciones judiciales puntuales. Este trabajo recoge -a través de fuentes secundarias- las que se consideran principales iniciativas y acciones de gobierno impartidas de arriba a abajo (Top Down e investiga -a través de fuentes primarias recogidas en el barrio La Cecilia-, las percepciones territoriales e iniciativas de acción comunitaria de abajo a arriba (Bottom up, indagando en los estériles procesos de diálogo entre estas dos formas de hacer ciudad.This paper addresses the environmental, legal and housing disputes that converge in the environmental reserve located at the Cerros Orientales (eastern hills of Bogota. The socio-urban logic of the city -linked to pirate developments and invasion-, the migration flows -emphasized by the armed conflict- and the lack of definition of a clear public policy for the last 30 years, has led to a conflict between residents, civil environmental protection organizations, private companies and public institutions in which almost only specific judgments have interceded. This paper duly reflects -through secondary sources- those considered main government initiatives and actions implemented with a top-down approach and it investigates -through primary sources collected in the neighborhood La Cecilia- the bottom-up community action initiatives and territorial perceptions, looking into

Eesti graafika edu Hispaanias / Benjamin Vasserman

Index Scriptorium Estoniae

Vasserman, Benjamin

1999-01-01

Hispaanias Orenses dets. 1998/jaan. 1999 peetud V rahvusvahelisel graafikabiennaalil "Julio Prieto Nespereira auhind" pälvisid žürii kiituse eesti graafikud R. Saks, V. Tolli, B. Vasserman. I preemia ئ T. Uchida. Näitusel osales S. Liiva. 1998. a. sügisel Jaapanis toimunud II Tokio rahvusvahelisest väikegraafika triennaalist võttis osa N. Neidre.

Tecnologías prehispánicas de la obsidiana

OpenAIRE

Darras, Véronique

2014-01-01

En esta obra se presentan los trabajos dedicados a las minas taller de obsidiana de la región de Zináparo-Prieto, situada en el Centro-Norte del estado de Michoacán, pertenecientes al proyecto del mismo nombre. Parte de sus resultados ya han sido publicados en la colección Cuadernos de Estudios Michoacanos.

Journal of Biosciences | Indian Academy of Sciences

Indian Academy of Sciences (India)

... V Morales1 Laura E Bortoni2 Paula C Turk-Noceto1 Elio A Prieto1. Centro de Altos Estudios en Ciencias Humanas y de la Salud, Universidad Abierta Interamericana (UAI); Instituto de Oncología Ángel H Roffo, Buenos Aires, Argentina; Consejo Nacional de Investigaciones Científicas y Técnicas, Buenos Aires, Argentina ...

Objectivity and Ideology

CERN Document Server

Prieto,L

1976-01-01

Conférence donné par le Prof.Luis J.Prieto, Argentin, qui était Prof.à Cordoba, Buenos Aires, Alger et Paris et appelé à l'Université de Genève (analyse du langage, structure social....) Il parle des problèmes epistomologiques (science de l'homme)et reflexion sur l'expérience scientifique.

Site Protection Efforts at the AURA Observatory in Chile

Science.gov (United States)

Smith, R. Chris; Smith, Malcolm G.; Sanhueza, Pedro

2015-08-01

The AURA Observatory (AURA-O) was the first of the major international observatories to be established in northern Chile to exploit the optimal astronomical conditions available there. The site was originally established in 1962 to host the Cerro Tololo Inter-American Observatory (CTIO). It now hosts more than 20 operational telescopes, including some of the leading U.S. and international astronomical facilities in the southern hemisphere, such as the Blanco 4m telescope on Cerro Tololo and the Gemini-South and SOAR telescopes on Cerro Pachón. Construction of the next generation facility, the Large Synoptic Survey Telescope (LSST), has recently begun on Cerro Pachón, while additional smaller telescopes continue to be added to the complement on Cerro Tololo.While the site has become a major platform for international astronomical facilities over the last 50 years, development in the region has led to an ever-increasing threat of light pollution around the site. AURA-O has worked closely with local, regional, and national authorities and institutions (in particular with the Chilean Ministries of Environment and Foreign Relations) in an effort to protect the site so that future generations of telescopes, as well as future generations of Chileans, can benefit from the dark skies in the region. We will summarize our efforts over the past 15 years to highlight the importance of dark sky protection through education and public outreach as well as through more recent promotion of IDA certifications in the region and support for the World Heritage initiatives described by others in this conference.

Las habas en el ajuar funerario de El Rincón de Almendricos (Lorca, Murcia

Directory of Open Access Journals (Sweden)

María Manuela AYALA JUAN

2009-10-01

Full Text Available El yacimiento de El Rincón, situado al N. O. de la población de Almendricos, Lorca, al Sur de la Región Murciana colindando con la Andaluza —desde lo cerros meridionales— de la Sierra de Enmedio próximos al yacimiento, se puede observar perfectamente el cerro de El Oficio-poblado argárico Alménense.

Cerro Negro, Nicaragua Images

Data.gov (United States)

National Oceanic and Atmospheric Administration, Department of Commerce — This cinder cone in western Nicaragua has a name that means "black hill." It has erupted more than 20 times since its birth in 1850. Explosive eruptions from the...

Aproximación a La Caracterización Ecológica de La Quebrada Fucha en La Reserva Forestal de los Cerros Orientales en La Localidad de San Cristóbal. (Bogotá, Colombia

Directory of Open Access Journals (Sweden)

Mónica Restrepo Villamil (Página 96-113

2009-07-01

Full Text Available En este trabajo se presentan los resultados obtenidos en la práctica de campo realizada el día 10 de octubre de 2008, en la quebrada Fucha en una reserva forestal protegida por la Empresa de Acueducto y Alcantarillado de Bogotá en los cerros orientales de la localidad de San Cristóbal. El objetivo principal de este estudio fue realizar una aproximación a la caracterización de este sistema acuático, para lo cual, se colectaron insectos acuáticos (entomofauna y perifiton, se caracterizaron los suelos de la ribera y se realizaron análisis de las variables fisicoquímicas de la zona. Los insectos acuáticos que se encontraron sumaron un total de 188 individuos, en donde las familias más abundantes fueron Simuliidae y Ceratopogonidae con 60 individuos cada una (32% c/u y las de menor abundancia fueron Odontoceridae, Lepharoceridae y Pyralidae con 1 individuo c/u (0.53% c/u; por otra parte, se encontraron 14 géneros de perifiton. El sistema presenta una diversidad media de acuerdo al índice de Shannon (1.55. La principal fuente de energía del sistema es la materia orgánica disuelta, por lo que la vía que predomina es la detrítica.

Comportamiento del índice de bajo peso al nacer en el Policlínico Docente Cerro durante los años 2009-2010

Directory of Open Access Journals (Sweden)

Ramona Moraima Torres Zulueta

Full Text Available Introducción: el bajo peso al nacerconstituye el índice predictivo más importante de la mortalidad infantil y se plantea que es 20 veces mayor que en el recién nacido con peso adecuado. Objetivo: comparar el comportamiento del índice de bajo peso al nacer en recién nacidos de un Policlínico durante los años 2009 y 2010. Método: se realizó un estudio comparativo de tipo descriptivo en el Policlínico Universitario Cerro, en la provincia La Habana, durante los años 2009 y 2010. El Universo estuvo constituido por los 350 recién nacidos vivos en el 2009 y los 318 en el 2010, y la muestra estuvo conformada por 23 niños con bajo peso al nacer en el 2009 y por 21 en el 2010. Se revisaron las historias obstétricas de las madres y se identificaron algunas variables socio-demográficas. Resultados: en ambos años estudiados la edad materna de mayor bajo peso al nacer fue de 20 a 34 años, con 73,9 y 80,9 %. Los factores de riesgo que se asociaron al bajo peso fueron: el hábito de fumar, que predominó en ambos años de estudio, representado por un 60,8 % en 2009 y por un 61,9 % en el 2010; el trastorno hipertensivo, con un 35 % en el año 2010 y un 27,7 % en el año 2009, y en ambos años fue superior en el grupo de gestantes con hipertensión arterial crónica. La anemia aumentó considerablemente en el 2010 en un 80,9 %, comparado con un 69,5 % en el año 2009. Conclusiones: el bajo peso al nacer resultó más frecuente en las gestantes de 20 a 34 años. Los factores de riesgo asociados al bajo peso al nacer con mayor frecuencia fueron: la anemia, el hábito de fumar y los trastornos hipertensivos.

Model to predict the flow of tracers in naturally fractured geothermal reservoirs; Modelo para predecir el flujo de trazadores en yacimientos geotermicos naturalmente fracturados

Energy Technology Data Exchange (ETDEWEB)

Ramirez Sabag, Jetzabeth

1988-02-01

{sub e1} fixes the characteristic of the family of curves. Also it was found that the irruption time for a given concentration depends strongly on {alpha}. [Spanish] El modelo propuesto ha sido desarrollado para estudiar el flujo de trazadores a traves de yacimientos geotermicos naturalmente fracturados. El sistema idealizado del yacimiento esta compuesto por dos regiones: Una region movil donde mecanismos de difusion y conveccion estan presentes y una region estancada o inmovil donde se consideran los mecanismos de difusion y adsorcion: en ambas regiones se considera la perdida de masa por decaimiento radioactivo. Las soluciones de las ecuaciones basicas de flujo estan en el espacio de Laplace y se utilizo el algoritmo de Stehfest para su inversion numerica. A pesar de la dispersion numerica que presentan estas soluciones, se encontro una tendencia bien definida para inferir el comportamiento del sistema bajo diferentes condiciones de flujo. Se encontro que, para propositos practicos el tamano de los bloques de matriz no tiene influencia sobre la respuesta de la concentracion, y la solucion se reduce a la presentada por Tang y asociados. Bajo estas condiciones, el comportamiento del sistema puede ser descrito por dos parametros adimensionales: El numero de Peclet en las fracturas y un parametro. Se derivo tambien la respuesta del trazador para la solucion pico. Se encontro una solucion analitica limite para el caso en que {alpha} tienda a cero, el cual corresponde al caso de un sistema homogeneo. Se comprobo que esta solucion limite es valida, para {alpha}<0.01. Para el caso de inyeccion continua esta solucion se reduce a la presentada por Coasts y Smith. Para la solucion pico, se encontro que el tiempo de irrupcion correspondiente a la maxima concentracion esta relacionada directamente con el grupo adimensional. Por lo tanto, es posible obtener el valor de P{sub e1} para una X{sub D} dada, o viceversa. Un grupo de graficas de concentracion adimensional en la fractura

Geochemical and isotopic behavior of fluids from wells in Los Humeros geothermal field, Puebla, Mexico; Comportamiento geoquimico e isotopico del fluido de los pozos del campo geotermico Los Humeros, Puebla, Mexico

Energy Technology Data Exchange (ETDEWEB)

Tovar Aguado, Rigoberto; Lopez Romero, Oscar [Comision Federal de Electricidad, Los Humeros, Puebla (Mexico)

1999-12-01

In general the wells in Los Humeros geothermal fields produce sodium bicarbonate water with a low salinity because the fluids are produced from the shallow part of the reservoir. The fluids in wells H-33 and H-6 are sodium chloride: the first influenced by fluids from deep levels in the reservoir and the second by fluids coming only from the deeps part of the reservoir. Fluid mixture for other wells depends on operating conditions. To date, it has been difficult with the geothermetric temperatures to establish the underground flow directions and whether or not an infiltration of shallow low-temperature fluids occurs. Well H-16 has the lowest-temperature fluid in the liquid phase, which suggests infiltration of shallow local fluids-a result corroborated by an isotopic study. Using the methodology of Giggenbach and Goguel, we found that the gases are in equilibrium with the liquid phase at temperatures between 275 and 325 Celsius degrees. The maximum temperature is measured in wells H-12 and H-9, where good agreement exists between this temperature and those calculated with a geothermometer of CO{sub 2}/H{sub 2} . Isotopic results show, in general, that the wells with the highest levels of oxygen-18 are those with the highest geothermetric temperatures (CO{sub 2}/H{sub 2})- both in the north (H-35 and H-9) and in the south (H-6 and H-12)-results that agree with the temperatures measured in the field. The initial thermodynamic conditions of the wells show that they produce fluids from the liquid region. This fact, together with the low salinity, permit the application of the D' Amore methodology, with which the estimations of vapor fractions in the reservoir are relatively low. [Spanish] En general, los pozos del campo geotermico de Los Humeros producen agua del tipo bicarbonato sodico con baja salinidad. Esto se debe a que extraen fluidos de la parte somera del yacimiento. Los pozos H-33 y H-6 son clorurados sodicos; el primero por cierta influencia de la zona

Evaluation of particle dispersal from mining and milling operations using lead isotopic fingerprinting techniques, Rio Pilcomayo Basin, Bolivia

International Nuclear Information System (INIS)

Miller, Jerry R.; Lechler, Paul J.; Mackin, Gail; Germanoski, Dru; Villarroel, Lionel F.

2007-01-01

Mining and milling of ores from the Cerro Rico de Potosi precious metal-polymetallic tin deposits of Bolivia have led to severe contamination of water and sediments of the Rio Pilcomayo drainage system. Lead (Pb) isotopic data were used in this study to first document downstream dispersal patterns of Pb contaminated sediment within the channel of the Rio Pilcomayo, and then to determine the relative contribution of Pb from Cerro Rico within alluvial terrace soils that are used for agriculture. The concentration and isotopic composition of Pb within channel bed sediments differed significantly between 2000, 2002, and 2004. These differences presumably reflect changes in the type of ore mined and milled at Cerro Rico, and alterations in dispersal and grain-size dilution mechanisms associated with interannual variations in rainfall and runoff. Within agricultural terrace soils, both Pb concentrations and the percentage of Pb from Cerro Rico: (1) semi-systematically decrease downstream, (2) were found to decrease with terrace height above the channel, and (3) reflect the use of contaminated irrigation water. In upstream reaches (within 30 km of the mills), Pb from mining represents the most significant Pb source, accounting for more than 80% of Pb in the examined agricultural fields. At Sotomayor, located approximately 170 km from the mills, the relative contribution of Pb from Cerro Rico is highly variable between fields, but can be significant, ranging from approximately 15% to 35%. The analysis demonstrates that Pb isotopic ratios can be used to effectively trace contaminated particles through river systems and into adjacent alluvial soils, even where multiple Pb sources exist and Pb concentrations are similar to background values

Crystallization conditions and petrogenesis of the lava dome from the ˜900 years BP eruption of Cerro Machín Volcano, Colombia

Science.gov (United States)

Laeger, Kathrin; Halama, Ralf; Hansteen, Thor; Savov, Ivan P.; Murcia, Hugo F.; Cortés, Gloria P.; Garbe-Schönberg, Dieter

2013-12-01

The last known eruption at Cerro Machín Volcano (CMV) in the Central Cordillera of Colombia occurred ˜900 years BP and ended with the formation of a dacitic lava dome. The dome rocks contain both normally and reversely zoned plagioclase (An24-54), unzoned and reversely zoned amphiboles of dominantly tschermakite and pargasite/magnesio-hastingsite composition and olivine xenocrysts (Fo = 85-88) with amphibole/clinopyroxene overgrowth, all suggesting interaction with mafic magma at depth. Plagioclase additionally exhibits complex oscillatory zoning patterns reflecting repeated replenishment, fractionation and changes in intrinsic conditions in the magma reservoir. Unzoned amphiboles and cores of the reversely zoned amphiboles give identical crystallization conditions of 910 ± 30 °C and 360 ± 70 MPa, corresponding to a depth of about 13 ± 2 km, at moderately oxidized conditions (f = +0.5 ± 0.2 ΔNNO). The water content in the melt, calculated based on amphibole chemistry, is 7.1 ± 0.4 wt.%. Rims of the reversely zoned amphiboles are relatively enriched in MgO and yield higher crystallization temperatures (T = 970 ± 25 °C), slightly lower melt H2O contents (6.1 ± 0.7 wt.%) and overlapping pressures (410 ± 100 MPa). We suggest that these rims crystallized following an influx of mafic melt into a resident magma reservoir at mid-crustal depths, further supported by the occurrence of xenocrystic olivine. Crystallization of biotite, albite-rich plagioclase and quartz occurred at comparatively low temperatures (probably during early stages of ascent or storage at shallower levels. Based on amphibole mineral chemistry, the felsic resident melt had a rhyolitic composition (71 ± 2 wt.% SiO2), whereas the hybrid magma, from which the amphibole rims crystallized, was dacitic (64 ± 3 wt.% SiO2). The bulk rock chemistry of the CMV lava dome dacites is homogenous. They have elevated (La/Nb)N ratios of 3.8-4.5, typical for convergent margin magmas, and display several

Validation of Hiriart equation to compute steam production by the lip pressure method; Validacion de la ecuacion de Hiriart para calculo de gasto de vapor por el metodo de presion de labio

Energy Technology Data Exchange (ETDEWEB)

Flores Armenta, Magaly [Gerencia de Proyectos Geotermoelectricos de la Comision Federal de Electricidad, Morelia (Mexico)

1996-09-01

Mainly in new geothermal wells, it is necessary to evaluate the production in a very fast, simple and not expensive way, to know the convenience to install surface equipment, such as silencers and separators, to drive the steam to the commercial gathering system. In practice, one of the most known methods is the lip pressure one, which requires a simple set of installations. The objective of this paper is to validate the steam flow rate calculated by the lip pressure method, with respect to the ASME method. The ASME method is known for its accuracy, and is done by measuring the steam and liquid after a high pressure separator, by an orifice plate of known diameter and a triangular weir. Results of the validation show up the feasibility of application of the lip pressure method by using a simple adjustment equation. Percentage of mistake results less than 1%, without any notable influence of the production enthalpy. That equation to be applied in a general case, is as follows: Q{nu} =(20642)(F*P*D{sup 2}/{radical}h-2000). For the particular case of the Los Azufres geothermal field, the equation is: Q{nu}= 810*P*D{sup 2} [Espanol] En los pozos geotermicos, principalmente en los nuevos, es necesario evaluar su produccion de manera rapida, sencilla y economica, para determinar la conveniencia de instalar equipo superficial, como separadores, silenciadores, etc., que permita la integracion del vapor al sistema comercial de generacion electrica. Para fines practicos uno de los metodos mas conocidos es el de presion de labio, que solo requiere un arreglo sencillo de instalaciones superficiales. En este documento se validan y ajustan los calculos de produccion de vapor por ese metodo de presion de labio, con respecto a las mediciones exactas efectuadas con el metodo ASME. Este ultimo es reconocido internacionalmente por su precision, y se lleva a cabo separando la mezcla obtenida en superficie en un recipiente a presion para medir el vapor a traves de una placa de orificio

Modification of the water-level control system at the Unit 12 of Los Azufres, Mich., geothermal field; Modificacion del sistema de control de nivel de agua en la Unidad 12 del campo geotermico de Los Azufres, Mich.

Energy Technology Data Exchange (ETDEWEB)

Tello Hinojosa, Raul; Aburto Huerta, S. Ramon; Mendoza Covarrubias, Hector M [Comision Federal de Electricidad, Gerencia de Proyectos Geotermoelectricos, Morelia, Michoacan (Mexico)]. E-mail: raul.tello@cfe.gob.mx

2007-01-15

Unit 12 of the Los Azufres, Mich., geothermal field is a binary cycle unit of 1.45 MW, installed at the pad of production well Az-22. There are two separators on this pad. One separates the mix extracted from well Az-22 and the other from adjacent wells. The separated brine from both separators is gathered in a horizontal tank and sent to Unit 12. The steam is sent to Unit 7, which generates 50 MW. Once some interference occurred affecting the power generation of Unit 7 when Unit 12 was off line. This was caused by the original flow arrangement and water-level control system. To avoid interference, a water-level control system was designed and installed in the separators. The system operates independently of Unit 12, with tanks in each separator connected by a pipe. Regulation of the water level is accomplished by three motor valves and a level sensor. To ensure permanent feeding of electrical power to the valves, an automatic system was installed from transmission lines of 23 and 115 kV. In case both lines fail, there is an uninterrupted power supply (UPS) unit. At the beginning of 2005, Unit 12 was again online with a modified water-level control system that has operated satisfactorily since then. Its short periods offline have not affected Unit 7. [Spanish] La Unidad 12 del campo geotermico de Los Azufres, Mich., es una unidad de ciclo binario de 1.45 MW, instalada en la plataforma del pozo productor Az-22. En esta plataforma hay dos separadores, uno de los cuales separa la mezcla extraida del pozo Az-22 y el otro la de varios pozos aledanos. El agua separada de ambos se concentra en un tanque horizontal y de este pasa a la Unidad 12, mientras que el vapor se envia a la Unidad 7, de 50 MW. Por el tipo de arreglo original de flujo y control de nivel de agua en los equipos, ocurrian interferencias que provocaban que cuando la Unidad 12 se disparaba se afectara la generacion en la Unidad 7. Para evitar esta interferencia se diseno e instalo un sistema de control de

Exploration report in mining reserve XIV

International Nuclear Information System (INIS)

Spoturno Pioppo, J.; Lara Vigil, P.

1991-01-01

This report has been referred to the antecedents and works developed in the mining Reservation XIV. This Reservation, covered a 1900 km2 surface, involving the aerial photography Valentines Cerro Chato, Chileno, Rossel y Rius, Sarandi del Yi and Cuchilla del Pescado. It has been reduced this area to western part of the aerial phothograpy Pavas, releasing other areas such as Chileno, Rossel y Rius, Cuchilla del Pescado y Cerro Chato. Finally, gold, sulphures, pirite and carbonates iron oxides findings have been found.

New K-Ar ages of volcanic rocks and associated mineralization in Canada Honda district, San Luis, Argentina

International Nuclear Information System (INIS)

Urbina, N.E.; Oggier, F.P

2001-01-01

New K-Ar ages in the Late Tertiary gold-bearing volcanic belt of the Sierras Pampeanas of San Luis, Argentina are presented. At Canada Honda district, an age of 8.49±0.2 Ma yielded by Cerro del Valle andesite indicates that the dome emplacement postdates the Diente Verde eruptive event. An even younger age of 7.3±0.2 Ma was obtained for illite from hydrothermal alteration at La Reynela mineralization which is hosted by Cerro del Valle andesite (au)

Evaluation of the energy potential, biogenesis and essential characteristics of the geothermal submarine systems in Mexico; Evaluacion del potencial, biogenesis y caracteristicas esenciales de los sistemas geotermicos submarinos en Mexico

Energy Technology Data Exchange (ETDEWEB)

Suarez Arriaga, Mario Cesar [Universidad Michoacana de San Nicolas Hidalgo, Morelia, Michoacan (Mexico)

2004-12-01

profundidad, hasta los recursos geotermicos profundos, a mas de 3000 metros de profundidad. Las fuentes geotermicas no tradicionales incluyen las partes profundas y los limites de los reservorios hidrotermales tradicionales, los sistemas en roca seca o humeda caliente, los yacimientos geopresurizados del Golfo de Mexico y los sistemas submarinos hidrotermales observados principalmente en la costa norte mexicana del Oceano Pacifico. La energia geotermica submarina surge por la existencia de rupturas profundas en el fondo marino, a lo largo de los centros de dispersion oceanicos entre las placas tectonicas. Estos sistemas tienen una longitud total aproximada de 65,000 Km. en la corteza oceanica. Hay dos tipos basicos de sistemas marinos existentes en el Golfo de California: los recursos profundos, localizados a lo largo de las cordilleras entre las placas de la corteza oceanica a mas de 2000 m bajo el nivel del mar, y los recursos poco profundos cerca de las plataformas continentales, entre 20 y 50 metros de profundidad. El calor submarino poco profundo tambien se relaciona con fallas y fracturas en el fondo del mar cerca de algunas costas. Este subsistema se encuentra tambien en la costa de Punta Banda en Ensenada, Baja California. El potencial preliminar de la energia contenida en tales reservorios se estima, en promedio, en 1120 MWt por cada km3 de roca submarina. Las caracteristicas quimicas especificas de las aguas hidrotermales encontradas en esos sistemas oceanicos indican que las interacciones agua-roca, ocurren bajo condiciones de presion y temperatura altas. La energia geotermica submarina soporta ricas variedades de comunidades biologicas a profundidades donde las plantas no tienen acceso a la luz solar para realizar la fotosintesis. Hay indicios de que las posibles condiciones para la sintesis de sustancias y elementos quimicos necesaria para el origen de la vida primitiva, pudieron ser los sistemas hidrotermales submarinos.

Does training with beat gestures favour children's narrative discourse abilities?

OpenAIRE

Vilà Giménez, Ingrid

2016-01-01

There is consensus evidence that gestures and prosody are important precursors of children’s early language abilities and development. Previous literature has investigated the beneficial role of beat gestures in the recall of information by preschoolers (Igualada, Esteve-Gibert, & Prieto, under review; Austin & Sweller, 2014). However, to our knowledge, little is known about whether the use of beat gestures can promote children’s later linguistic abilities and specifically whether training wi...

[Reseñas Bibliográficas] Atlas de la flora vascular silvestre de Burgos

Directory of Open Access Journals (Sweden)

Iñaki Aizpuru

2005-01-01

Full Text Available Es una reseña bibliográfica de la obra, Atlas de la flora vascular silvestre de Burgos / Alejandre Sáenz, J.M. García-López, L. Marín Padellano, G. Mateo Sanz, E. Miguélez del coso, C. Molina Martín, G. Montamarta Prieto, S. Patino Sánchez, M.A. Pinto Cebrián 6 J. Valencia Janices.

CURRENT STATE OF CONSERVATION, FIRST PHOTOGRAPHIC RECORD AND POPULATION ESTIMATION OF THE COASTAL JAGUAR (Panthera onca centralis AND RECORDS OF COMPANION FAUNA OF MEDIUM-SIZED AND HIGHER MAMMALS IN THE PROTECTED FOREST CERRO BLANCO OF THE CHONGÓN COLONCHE MOUNTAIN RANGE, GUAYAQUIL – ECUADOR

Directory of Open Access Journals (Sweden)

Miguel Saavedra

2013-12-01

Full Text Available The Chongón-Colonche Mountain Range is important for their goods and environmental services, its high biodiversity, and being one of the few coastal regions of Ecuador, which still houses the coastal Jaguar Panthera onca centralis. In the Forest Protector Cerro Blanco (BPCB, last Southeast extension of the mountain chain, it was developed the field research through the data collection with direct and indirect medium-sized and higher mammals’ records. Besides a Cuddeback Digital camera trap was used, by selecting a sampling point within a probable route of the jaguar. Inspections in a nearby quarry were made to observe traces of major feline registries. The same consolidated past sightings or evidence of witnesses which complemented the study for the determination of the status of the species in the BPCB. The study showed indirect and direct records of white-tailed deer, peccaries, raccoons, agoutis, wild rabbits, howler monkeys, Capuchin white or monkeys, agouti, bears Anteaters and Jaguars from the coast for which it is considered that the BPCB is probably a meeting place between two individuals; however, it is important to note that the results presented are preliminary.

FLOODPLAIN, CERRO GORDO COUNTY, USA

Data.gov (United States)

Federal Emergency Management Agency, Department of Homeland Security — The Floodplain Mapping/Redelineation study deliverables depict and quantify the flood risks for the study area. The primary risk classifications used are the...

HYDRAULICS, Cerro Gordo County, Iowa

Data.gov (United States)

Federal Emergency Management Agency, Department of Homeland Security — Survey data includes spatial datasets and data tables necessary to digitally represent data collected in the survey phase of the study. (Source: FEMA Guidelines and...

Vigilancia de la salud pública después de una erupción volcánica: lecciones aprendidas en Cerro Negro, Nicaragua, 1992

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Malilay Josephine

1997-01-01

Full Text Available La erupción del volcán Cerro Negro cerca de León, Nicaragua, el 9 de abril de 1992 lanzó alrededor de 1,7 millones de toneladas de ceniza en una zona de 200 km². Se efectuó una evaluación inicial de los efectos en la salud de cerca de 300 000 residentes, con los datos normalmente obtenidos mediante el sistema nacional de vigilancia epidemiológica. Se determinó que el número de consultas a los establecimientos de atención de salud por diarrea e infecciones respiratorias agudas (IRA aumentó en las dos comunidades estudiadas, una dentro de la zona del desastre y otra en sus cercanías. En particular, las consultas por diarrea aguda fueron casi 6,0 veces más numerosas que antes de la erupción en ambas comunidades y las consultas por IRA, 3,6 veces más frecuentes en Malpaisillo (la comunidad cercana a la zona del desastre y 6,0 veces más frecuentes en Telica (la comunidad situada dentro de esa zona. Casi todas fueron consultas por enfermedad en lactantes y niños menores de 5 años. El aumento de la tasa de morbilidad por diarrea, que frecuentemente se produce después de las erupciones volcánicas, exige que se investiguen detalladamente el tipo y la calidad del abastecimiento de agua después de una acumulación cuantiosa de ceniza. Es preciso examinar con mayor detenimiento los problemas respiratorios asociados con la ceniza para determinar el espectro de esas enfermedades y el momento en que se presentan en lactantes y otros subgrupos especiales de la población. Los datos acopiados por medio de la vigilancia pasiva sobre las condiciones de salud antes y después de una erupción pueden emplearse para detectar la morbilidad relacionada con la erupción. Los sistemas que ya están establecidos, como el sistema nacional de vigilancia epidemiológica de Nicaragua, se pueden modificar o ampliar para mejorar su sensibilidad a nuevos casos y, por ende, su capacidad de ofrecer servicios de notificación apropiados a los organismos de

Caracterización petrográfica y geoquímica del batolito Cerro Aspero-Alpa Corral (32°34'-32°42' LS y 64°43'-64°52' LO, provincia de Córdoba, Argentina

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Porta, G.

1992-12-01

Full Text Available The Cerro Aspero-Alpa Corral (CA-AC batholith is a 440 km2 granite body present in the Southern edge of the Eastern Pampean Ranges, Córdoba province, central Argentina. The intrusive body of probably paleozoic age shows both post-tectonic and epizonal character. Country rocks include Upper Precambrian-Lower Paleozoic metasedimentary rocks mainly represented by mica-schists, gneisses and migmatites, locally interrupted by minor amphibolite and marble outcrops.This paper deals with representative petrographic and geochemical data that characterize a 150 km2 central stripe between 32°34'-32°42'S and 64°43'-64°52'W.Three granitic facies have been distinguished based on their distinctive modal mineralogy and texture, and upon well known chemical parameters.A K-feldspar megacryst porphydic-type is the areally prevalent facies, but dykes of micro- leucogranites and biotite-phenocryst bearing granite are also well represented. They are all monzogranites of subalkaline and peraluminous chemistry. Their mineralogy shows variable proportions of QAP constituents and micas, with minor phases represented by Fe-Ti oxides, apatite (Ap, titanite (Tt, allanite (Aln.Microgranular enclaves, abundantly distributed in the porphydic facies, provide valuable information for a better understanding of parental magma evolution.The high-Ca content of the melt makes this body quite distinctive compared to its larger northern neighbour, the Achala batholith.Pegmatite and aplite bodies, as well as fluorite bearing breccias and quartz veins, barren or mineralized, are also present within the CA-AC batholith.El batolito Cerro Aspero-Alpa Corral (CA-AC es un cuerpo granítico que aflora en el extremo sur de las Sierras Pampeanas Orientales, en la provincia de Córdoba, República Argentina, cubriendo una superficie cercana a los 440 km2.Es un cuerpo intrusivo postcinemático de probable edad paleozoica. Las rocas encajantes son metamorfitas correspondientes al Prec

La fuente Inca de Aypate

OpenAIRE

Astuhuamán Gonzáles, César W.; Ministerio de Cultura

2013-01-01

La mayor parte del cerro Aypate está cubierto por la tupida vegetación del húmedo bosque de neblina, la cual concentra y produce el elemento más valioso para los pueblos andinos: el agua. El asentamiento Inca de Aypate se construyó sobre el cerro que forma parte de una cadena montañosa de la que nacen pequeñas quebradas que alimentan las subcuencas de los ríos Quiroz y Macará, que a su vez integran la cuenca del Chira.

A bottom-driven mechanism for distributed faulting: Insights from the Gulf of California Rift

Science.gov (United States)

Persaud, P.; Tan, E.; Choi, E.; Contreras, J.; Lavier, L. L.

2017-12-01

The Gulf of California is a young oblique rift that displays a variation in rifting style along strike. Despite the rapid localization of strain in the Gulf at 6 Ma, the northern rift segment has the characteristics of a wide rift, with broadly distributed extensional strain and small gradients in topography and crustal thinning. Observations of active faulting in the continent-ocean transition of the Northern Gulf show multiple oblique-slip faults distributed in a 200 x 70 km2area developed some time after a westward relocation of the plate boundary at 2 Ma. In contrast, north and south of this broad pull-apart structure, major transform faults accommodate Pacific-North America plate motion. Here we propose that the mechanism for distributed brittle deformation results from the boundary conditions present in the Northern Gulf, where basal shear is distributed between the Cerro Prieto strike-slip fault (southernmost fault of the San Andreas fault system) and the Ballenas Transform fault. We hypothesize that in oblique-extensional settings whether deformation is partitioned in a few dip-slip and strike-slip faults, or in numerous oblique-slip faults may depend on (1) bottom-driven, distributed extension and shear deformation of the lower crust or upper mantle, and (2) the rift obliquity. To test this idea, we explore the effects of bottom-driven shear on the deformation of a brittle elastic-plastic layer with pseudo-three dimensional numerical models that include side forces. Strain localization results when the basal shear is a step-function while oblique-slip on numerous faults dominates when basal shear is distributed. We further investigate how the style of faulting varies with obliquity and demonstrate that the style of faulting observed in the Northern Gulf of California is reproduced in models with an obliquity of 0.7 and distributed basal shear boundary conditions, consistent with the interpreted obliquity and boundary conditions of the study area. Our

Seismic reflection-based evidence of a transfer zone between the Wagner and Consag basins: implications for defining the structural geometry of the northern Gulf of California

Science.gov (United States)

González-Escobar, Mario; Suárez-Vidal, Francisco; Hernández-Pérez, José Antonio; Martín-Barajas, Arturo

2010-12-01

This study examines the structural characteristics of the northern Gulf of California by processing and interpreting ca. 415 km of two-dimensional multi-channel seismic reflection lines (data property of Petróleos Mexicanos PEMEX) collected in the vicinity of the border between the Wagner and Consag basins. The two basins appear to be a link between the Delfín Superior Basin to the south, and the Cerro Prieto Basin to the north in the Mexicali-Imperial Valley along the Pacific-North America plate boundary. The seismic data are consistent with existing knowledge of four main structures (master faults) in the region, i.e., the Percebo, Santa María, Consag Sur, and Wagner Sur faults. The Wagner and Consag basins are delimited to the east by the Wagner Sur Fault, and to the west by the Consag Sur Fault. The Percebo Fault borders the western margin of the modern Wagner Basin depocenter, and is oriented N10°W, dipping (on average) ˜40° to the northeast. The trace of the Santa María Fault located in the Wagner Basin strikes N19°W, dipping ˜40° to the west. The Consag Sur Fault is oriented N14°W, and dips ˜42° to the east over a distance of 21 km. To the east of the study area, the Wagner Sur Fault almost parallels the Consag Sur Fault over a distance of ˜86 km, and is oriented N10°W with an average dip of 59° to the east. Moreover, the data provide new evidence that the Wagner Fault is discontinuous between the two basins, and that its structure is more complex than previously reported. A structural high separates the northern Consag Basin from the southern Wagner Basin, comprising several secondary faults oriented NE oblique to the main faults of N-S direction. These could represent a zone of accommodation, or transfer zone, where extension could be transferred from the Wagner to the Consag Basin, or vice versa. This area shows no acoustic basement and/or intrusive body, which is consistent with existing gravimetric and magnetic data for the region.

Lithospheric Structure and Active Deformation in the Salton Trough from Coseismic and Postseismic Models of the 2010 Mw 7.2 El Mayor-Cucapah Earthquake

Science.gov (United States)

Fielding, E. J.; Huang, M. H.; Dickinson, H.; Freed, A. M.; Burgmann, R.; Gonzalez-Ortega, J. A.; Andronicos, C.

2016-12-01

The 4 April 2010 Mw 7.2 El Mayor-Cucapah (EMC) Earthquake ruptured about 120 km along several NW-striking faults to the west of the Cerro Prieto Fault in the Salton Trough of Baja California, Mexico. We analyzed interferometric synthetic aperture radar (SAR), SAR and optical pixel offsets, and continuous and campaign GPS data to optimize an EMC coseismic rupture model with 9 fault segments, which fits the complex structure of the faults. Coseismic slip inversion with a layered elastic model shows that largely right-lateral slip is confined to upper 10 km with strong variations along strike. Near-field GPS measures slip on a north-striking normal fault that ruptured at the beginning of the earthquake, previously inferred from seismic waveforms. EMC Earthquake postseismic deformation shows the Earth's response to the large coseismic stress changes. InSAR shows rapid shallow afterslip at the north and south ends of the main ruptures. Continuous GPS from the Plate Boundary Observatory operated by UNAVCO measures the first six years of postseismic deformation, extremely rapid near the rupture. Afterslip on faults beneath the coseismic rupture cannot explain far-field displacements that are best explained by viscoelastic relaxation of the lower crust and upper mantle. We built a viscoelastic 3D finite element model of the lithosphere and asthenosphere based on available data for the region with the EMC coseismic faults embedded inside. Coseismic slip was imposed on the model, allowed to relax for 5 years, and then compared to the observed surface deformation. Systematic exploration of the viscoelastic parameters shows that horizontal and vertical heterogeneity is required to fit the postseismic deformation. Our preferred viscoelastic model has weaker viscosity layers beneath the Salton Trough than adjacent blocks that are consistent with the inferred differences in the geotherms. Defining mechanical lithosphere as rocks that have viscosities greater than 10^19 Pa s (able

Heat pump for purification of geothermal brines; Bomba de calor para purificacion de salmuera geotermica

Energy Technology Data Exchange (ETDEWEB)

Santoyo-Gutierrez, S; Barragan-Reyes, R.M; Holland, F.A [Instituto de Investigaciones Electricas, Cuernavaca, Morelos (Mexico)]. E-mail: rmb@iie.org.mx

2007-01-15

Integrated use of geothermal resources is one of the most important goals for the future. Presently geothermal heat pumps offer two benefits: using heat from residual brines and converting these brines into very pure water. Designs and descriptions are presented of an experimental system to purify geothermal brines integrated to an adsorption heat-pump. The system was constructed and tested in the IIE (Institute for Electrical Research) facilities. During the experimental stage, pure water was obtained. Maximum capacity for pure water was 4.3 kg per hour, presenting an Actual Coefficient of Performance (COP)A of 1.4. The results are encouraging to project units at an industrial level for operating with geothermal and/or solar heat. [Spanish] El aprovechamiento integral de los recursos geotermicos en todas sus formas es una de las metas importantes a lograr en los proximos anos. Hoy en dia, el uso de las bombas de calor en la geotermia ofrece un doble beneficio: aprovechan el calor de los fluidos de desecho y tienen la capacidad de transformar la salmuera geotermica en agua de alta pureza. Se presenta el diseno y descripcion de un sistema experimental para purificacion de salmuera geotermica integrado a una bomba de calor por absorcion, el cual fue construido y probado en el Instituto de Investigaciones Electricas. En toda la etapa de experimentacion se obtuvo agua pura. La capacidad maxima alcanzada de produccion de agua pura de este sistema fue de 4.3 kg por hora, mostrando un rendimiento en terminos del Coeficiente Real de Rendimiento (COP)A de 1.4. Estos resultados se consideran alentadores para la proyeccion de unidades a escala industrial que puedan ser operadas con calor geotermico y/o solar.

Melhoramento do trigo: XX. Herdabilidades e correlações entre os componentes de produção em populações híbridas envolvendo fontes de nanismo Wheat breeding: XX. Heritabilities and correlations among yield components in hybrid populations involving different sources of dwarfism

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Carlos Eduardo de Oliveira Camargo

1989-01-01

Full Text Available Foram estimados os valores da herdabilidade em sentido restrito para a produção de grãos, altura das plantas, número de espigas por planta e de grãos por espiga e peso de cem grãos, bem como as correlações entre esses parâmetros através de cruzamentos em forma dialética entre os cultivares BH-1146, Atlas-66, Tordo e Siete Cerros. Plantas representando os pais, as gerações F1 e F2 e os retrocruzamentos para ambos os pais foram estudadas em um ensaio em blocos ao acaso, com cinco repetições, na Estação Experimental de Hyslop, da Universidade Estadual de Oregon, EUA, em 1978. Os valores da herdabilidade em sentido restrito para altura das plantas foram moderadamente altos para os cruzamentos BH-1146 x Atlas-66 (0,55, BH-1146 x Siete Cerros (0,60 e Atlas-66 x Siete Cerros (0,74; moderados para os cruzamentos Atlas-66 x Tordo (0,43 e Tordo x Siete Cerros (0,41, e baixo para o BH-1146 x Tordo (0,24. Foram estimados valores médios da herdabilidade em sentido restrito para número de espigas por planta variando de 0,43 a 0,58 para todos os cruzamentos, com exceção do BH-1146 x Atlas-66 e Atlas-66 x Tordo, que apresentaram valores baixos. Para o caráter peso de cem grãos, os indices da herdabilidade foram baixos para todos os cruzamentos, à exceção do BH-1146 x Atlas-66 e BH-1146 x Siete Cerros, que foram médios (0,40 e 0,45 respectivamente. Os valores da herdabilidade para produção de grãos foram baixos, à exceção dos verificados para os cruzamentos BH-1146 x Tordo (0,73 e BH-1146 x Siete Cerros (0,62. As correlações fenotípicas entre a produção de grãos e o número de espigas por planta, a altura das plantas, o número de grãos por espiga e o peso de cem grãos foram positivas e altamente significativas (com exceção da correlação produção de grãos e peso de cem grãos para a população BH-1146 x Atlas-66, que foi não-significativa. Os resultados sugerem ser possível selecionar somente plantas de porte

Ionosphere Scintillation at Low and High Latitudes (Modelling vs Measurement)

Science.gov (United States)

Béniguel, Yannick

2016-04-01

This paper will address the problem of scintillations characteristics, focusing on the parameters of interest for a navigation system. Those parameters are the probabilities of occurrence of simultaneous fading, the bubbles surface at IPP level, the cycle slips and the fades duration statistics. The scintillation characteristics obtained at low and high latitudes will be compared. These results correspond to the data analysis performed after the ESA Monitor ionosphere measurement campaign [1], [2]. A second aspect of the presentation will be the modelling aspect. It has been observed that the phase scintillation dominates at high latitudes while the intensity scintillation dominates at low latitudes. The way it can be reproduced and implemented in a propagation model (e.g. GISM model [3]) will be presented. Comparisons of measurements with results obtained by modelling will be presented on some typical scenarios. References [1] R. Prieto Cerdeira, Y. Beniguel, "The MONITOR project: architecture, data and products", Ionospheric Effects Symposium, Alexandria (Va), May 2011 [2] Y. Béniguel, R Orus-Perez , R. Prieto-Cerdeira , S. Schlueter , S. Scortan, A. Grosu "MONITOR 2: ionospheric monitoring network in support to SBAS and other GNSS and scientific purposes", IES Conference, Alexandria (Va), May 2015-05-22 [3] Y. Béniguel, P. Hamel, "A Global Ionosphere Scintillation Propagation Model for Equatorial Regions", Journal of Space Weather Space Climate, 1, (2011), doi: 10.1051/swsc/2011004

Propagation of the endangered Azorean cherry Prunus azorica using stem cuttings and air layering

OpenAIRE

Moreira, Orlanda; Martins, José; Silva, Luís; Moura, Mónica

2009-01-01

Prunus azorica (Hort. ex Mouillef.) Rivas Mart., Lousã, Fern. Prieto, E. Dias, J.C. Costa & C. Aguiar is an endangered tree endemic to the Azores, with an ecological and ornamental interest. The objective of this study was to determine the conditions necessary for the successful propagation of P. azorica by stem cuttings and air-layering. Stem cuttings collected in March with two apical leaf pairs pruned to 1/3 of their leaf area were submitted to different treatments, including a basal split...

Environmental impact in geothermal fields; Impacto ambiental en campos geotermicos

Energy Technology Data Exchange (ETDEWEB)

Birkle, P; Torres R, V; Gonzalez P, E; Guevara G, M [Instituto de Investigaciones Electricas. Departamento de Geotermia. Cuernavaca (Mexico)

1997-12-31

Generally, water exploitation and deep steam of geothermal fields may be cause of a pollution potential on the surface, specially by the chemical composition of geothermal water which has a high concentration of minerals, salts and heavy metals. The utilization of stable isotopes as deuterium and oxygen 18 as radioactive tracers and water origin indicators allow to know the trajectories and sources of background waters as well as possible moistures between geothermal waters and meteoric waters. Some ions such as chlorides and fluorides present solubilities that allow their register as yet long distances of their source. (Author).

Groundwater arsenic in Chimaltenango, Guatemala.

Science.gov (United States)

Lotter, Jason T; Lacey, Steven E; Lopez, Ramon; Socoy Set, Genaro; Khodadoust, Amid P; Erdal, Serap

2014-09-01

In the Municipality of Chimaltenango, Guatemala, we sampled groundwater for total inorganic arsenic. In total, 42 samples were collected from 27 (43.5%) of the 62 wells in the municipality, with sites chosen to achieve spatial representation throughout the municipality. Samples were collected from household faucets used for drinking water, and sent to the USA for analysis. The only site found to have a concentration above the 10 μg/L World Health Organization provisional guideline for arsenic in drinking water was Cerro Alto, where the average concentration was 47.5 μg/L. A health risk assessment based on the arsenic levels found in Cerro Alto showed an increase in noncarcinogenic and carcinogenic risks for residents as a result of consuming groundwater as their primary drinking water source. Using data from the US Geological Survey and our global positioning system data of the sample locations, we found Cerro Alto to be the only site sampled within the tertiary volcanic rock layer, a known source of naturally occurring arsenic. Recommendations were made to reduce the levels of arsenic found in the community's drinking water so that the health risks can be managed.

VizieR Online Data Catalog: Solar neighborhood. XXXII. L and M dwarfs (Dieterich+, 2014)

Science.gov (United States)

Dieterich, S. B.; Henry, T. J.; Jao, W.-C.; Winters, J. G.; Hosey, A. D.; Riedel, A. R.; Subasavage, J. P.

2015-01-01

We obtained VRI photometry for all targets in our sample using the Cerro Tololo Inter-American Observatory (CTIO) 0.9m telescope for the brighter targets and the SOuthern Astrophysical Research (SOAR) Optical Imager camera on the SOAR 4.1m telescope for fainter targets. SOAR observations were conducted between 2009 September and 2010 December during six observing runs comprising NOAO programs 2009B-0425, 2010A-0185, and 2010B-0176. A total of 17 nights on SOAR were used for optical photometry. Table 1 shows the photometry in the photometric system used by the telescope with which the measurements were taken (Johnson-Kron-Cousins for the CTIO 0.9m telescope and Bessell for SOAR). Astrometric observations are based in part on observations obtained via the Cerro Tololo Inter-American Observatory Parallax Investigation (CTIOPI), at the Cerro Tololo 0.9m telescope. CTIOPI is a large and versatile astrometric monitoring program targeting diverse types of stellar and substellar objects in the solar neighborhood. Observations are taken using the CTIO 0.9m telescope and its sole instrument, a 2048*2048 Tektronix imaging CCD detector with a plate scale of 0.401''/pixel. (4 data files).

Notes on the “Lima orchid” Chloraea undulata and its record in the hills of Asia, Cañete, Peru

Directory of Open Access Journals (Sweden)

Miguel Lleellish Juscamayta

2015-12-01

Full Text Available Chloraea undulata is an orchid endemic to Peru. Originally collected by Antonio Raimondi in XIX century, until first half of the last century it has been regarded as a species characteristic of the hills around Lima. The “Lima orchid” Chloraea undulata is considered to be in decline in the hills of Lima province, especially in the type localities of Cerro Amancaes and Cerro El Agustino where urban growth and expansion has been significant. In this paper its presence in the hills of Asia District, 100 km south of Lima, is documented, and we also analyzed the implications of this finding for the species conservation and their habitat.

TERRAIN, CERRO GORDO COUNTY, IOWA, USA

Data.gov (United States)

Federal Emergency Management Agency, Department of Homeland Security — Terrain data, as defined in FEMA Guidelines and Specifications, Appendix N: Data Capture Standards, describes the digital topographic data that was used to create...

Tolerância de cultivares de trigo a diferentes níveis de alumínio em solução nutritiva e no solo Tolerance op wheat cultivars to different levels of aluminum toxicity

Directory of Open Access Journals (Sweden)

Carlos Eduardo de Oliveira Camargo

1981-01-01

Full Text Available Foram estudados dez cultivares de trigo em soluções nutritivas contendo cinco diferentes níveis de alumínio tóxico. A tolerância foi medida pela capacidade de as raízes primárias continuarem a crescer em solução sem alumínio, após um período prévio de 48 horas em solução contendo uma concentração conhecida de alumínio. Os cultivares Siete Cerros e Tobari-66 foram sensíveis, respectivamente, a 1 e 3 ppm de alumínio. 'Alondra-S-46', 'Alondra-S-45' e 'IAC-17' foram sensíveis a 6 ppm; 'BH-1146', 'IAC-5', 'IAC-18', 'IAC-13' e 'Londrina' foram tolerantes a 10 ppm, porém 'BH-1146', 'IAC-18' e 'IAC-13' foram mais tolerantes que 'IAC-5' e 'Londrina'. Os cultivares BH-1146, IAC-17, Alondra-S-46, Tobari-66 e Siete Cerros foram cultivados em vasos contendo solo ácido mostrando a presença de alumínio. Metade do número de vasos recebeu uma aplicação de calcário. Os resultados desse experimento mostraram que o cultivar BH-1146 diferiu significativamente em produção de grãos por planta de 'Tobari-66', 'Alondra-S-46', 'IAC-17' e 'Siete Cerros'. Esse resultado confirmou a tolerância ao alumínio do cultivar BH-1146, observada quando se empregou solução nutritiva com a presença desse elemento.Ten wheat cultivars were studied to aluminum toxicity using five different levels of this element. The tolerance was measured taking into account the root growth in a aluminum-free complete nutrient solution after a previous Al treatment. With toxic amounts of Al, the primary roots did not grow at all and remained thickned at the tip as a typical Al injury. The wheat cultivars Siete Cerros and Tobari-66 were sensitive to 1 and 3 ppm of aluminum, respectively. The cultivars Alondra-S-46, Alondra-S-45 and IAC-17 were sensitive to 6 ppm. The cultivars BH-1146, IAC-5, IAC-18, IAC-13 and Londrina showed tolerance to 10 ppm but BH-1146, IAC-18 and IAC-13 were more tolerant than IAC-5 and Londrina. The cultivars BH-1146, IAC-17, Alondra-S-46

Programa piloto municipal "mejorar la calidad de la vida del diabético".: Resultados sobre mortalidad, complicaciones y costos en la diabetes mellitus

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Alberto Quirantes Hernández

2000-06-01

Full Text Available Se presentan los primeros resultados del programa Mejorar la Calidad de la Vida del Diabético, que está basado en una estrecha interrelación entre los niveles de salud primario y secundario, así como en un método asistencial que propicia el cumplimiento por parte de los pacientes con diabetes mellitus de lo que hemos llamado Las 7 Leyes del Éxito del Paciente Diabético. Este programa ha sido desarrollado en el municipio Cerro de Ciudad de La Habana durante el segundo semestre de 1997 y todo el año 1998. Se compra el tiempo de aplicación del programa con una etapa de tiempo similar inmediatamente anterior al mismo. En la etapa previa, los diabéticos residentes en el municipio Cerro constituían el 31,8 % de los fallecidos por esta enfermedad en el Hospital Docente "Dr. Salvador Allende"; después de la aplicación del programa, este grupo sólo constituyó el 9,1 % del total de diabéticos fallecidos. En todo el municipio, los diabéticos fallecidos disminuyeron en un 41 % después de la aplicación del programa. Se dejaron de ingresar 91 diabéticos, perteneciendo 89 (97,8 % al municipio Cerro lo que representó un ahorro de $ 25 705.87. Se concluye que dada la efectividad demostrada por este programa se recomienda su aplicación en todos los municipios del paísThe first results of the program "To improve the quality of the diabetic´s life", which is based on a close interrelation between the primary and secondary health care levels, as well as on an assistance method that propitiates the fulfillment on the part of the patients of what we have called The 7 Laws of Success of the Diabetic Patient are shown in this paper. This program has been implemented in the Cerro municipality of Havana City during the second semester of l997 and throughout 1998.The time of application of the program is compared with a similar period of time immediately before it. In the previous stage, the diabetics living in Cerro municipality were 31,8 % of the

Segue: A Spectroscopic Survey of 240,000 Stars With g = 14-20

Science.gov (United States)

2009-05-01

Departamento de Fisica y Astronomia , Facultad de Ciencias, Universidad de Valparaiso, Valparaiso, Chile 30 Department of Physics and Astronomy, Austin Peay...types. The sample spectra are plotted with flux in units of 10−17 erg cm−2 s−1 Å on the y -axis versus wavelength in Å on the x-axis. If more than one...the University of Washington. C. Allende Prieto acknowledges support from NASA grants NAG 5-13057 and NAG 5-13147. T. C. Beers, Y . S. Lee, and S

Trigo duro: tolerância à toxicidade de alumínio, manganês e ferro em soluções nutritivas Durum wheat: tolerance to aluminum, manganese and iron toxicities in nutrient solutions

Directory of Open Access Journals (Sweden)

Carlos Eduardo de Oliveira Camargo

1995-01-01

Full Text Available Avaliou-se o comportamento diferencial de 23 linhagens de trigo duro (Triticum durum L. em compraração com os seguintes cultivares de trigo (T. aestivum L.: IAC-24, BH-1146, Siete Cerros e IAC-60, quanto aos níveis de Al3+ (0;0,2;0,4; 0,6; 0,8 e 1,0 mg/L, de Mn2+ (0,11; 300; 600 c 1.200 mg/L e de Fe2+ (0,56; 5; 10 e 20 mg/L em solução nutritiva. Os cultivares de trigo Siete Cerros (sensível à toxicidade de Al3+, BH-1146, IAC-60 e IAC-24 (tolerantes à toxicidade de Al3+, exibiram crescimento das raízes na presença de 1 mg/L de Al3+, e todas as linhagens de trigo duro avaliadas foram totalmente sensíveis a 0,4 mg/L de Al3+, com paralisação irreversível do crescimento das raízes. O aumento das concentrações de Mn2+(0,11 a 1.200 mg/L e de Fe2+ (0,56 a 20 mg/L nas soluções causou uma redução significativa no comprimento das raízes dos genótipos em estudo. As linhagens de trigo duro I (Avetoro "S" x Anhinga "S" - Purcell "S"/D.67.2, 2 (Cando - Yavaros "S", 6 (Chen "S" e 8 (Carcomum "S" apresentaram-se muito tolerantes à toxicidade de Mn2+ em relação ao controle 'Siete Cerros'. O 'Siete Cerros' e as linhagens de trigo duro 1, 6, 12 (CI 14955 x Yavaros "S"- Gediz "S"/Tropic Bird, 16 e 21 (Swan "S" c 20 (Boyeros "S"/Cocorit-71/5/Crane/Ganso//Marte "S"/3/Tildillo "S"/4/ Memo "S" exibiram tolerância à presença de elevadas quantidades de Fe2+ nas soluções nutritivas.Twenty three durum wheat inbred lines were evaluated with four bread wheat cultivars (IAC-24, BH-1146, Siete Cerros and IAC-60 in three experiments, using nutrient solutions. In the first experiment, the following levels of Al3+ were used: 0; 0.2; 0.4; 0.6; 0.8 and 1.0 mg/L; in the second experiment, the following levels of Mn2+ were used: 0.11; 300; 600 and 1.200 mg/L; and in the third experiment, Fe2+ was used at: 0.56; 5; 10 and 1.200 mg/L. The wheat cultivars Siete Cerros (sensitive to Al3+ toxicity and BH-1146, IAC-24 and IAC-60 (tolerant to Al3+ toxicity

Morphometrics parallel genetics in a newly discovered and endangered taxon of Galápagos tortoise.

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Ylenia Chiari

2009-07-01

Full Text Available Galápagos tortoises represent the only surviving lineage of giant tortoises that exhibit two different types of shell morphology. The taxonomy of Galápagos tortoises was initially based mainly on diagnostic morphological characters of the shell, but has been clarified by molecular studies indicating that most islands harbor monophyletic lineages, with the exception of Isabela and Santa Cruz. On Santa Cruz there is strong genetic differentiation between the two tortoise populations (Cerro Fatal and La Reserva exhibiting domed shell morphology. Here we integrate nuclear microsatellite and mitochondrial data with statistical analyses of shell shape morphology to evaluate whether the genetic distinction and variability of the two domed tortoise populations is paralleled by differences in shell shape. Based on our results, morphometric analyses support the genetic distinction of the two populations and also reveal that the level of genetic variation is associated with morphological shell shape variation in both populations. The Cerro Fatal population possesses lower levels of morphological and genetic variation compared to the La Reserva population. Because the turtle shell is a complex heritable trait, our results suggest that, for the Cerro Fatal population, non-neutral loci have probably experienced a parallel decrease in variability as that observed for the genetic data.

El ii coloquio de matemáticas

OpenAIRE

Boletín de, Matemáticas

2012-01-01

Del 3 al 29 de Julio se celebre en la ciudad de Bogotá el II Coloquio de "Matemáticas organizado por la Sociedad Colombiana de Matemáticas y el Departamento de Matemáticas y Estadística de la Universidad Nacional per intermedio de un comité constituido por los profesores Carlos Ruiz Salguero (Presidente de la Sociedad Colombiana de Matemáticas), Víctor Hugo Prieto (entonces Director del Departamento de Matemáticas y Estadística, Universidad Nacional),Carlos Lemoine, Antonio Donado y Yu Takeuc...

Boletín bibliográfico

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Revista, Facultad de Medicina

2011-01-01

Parasitosis intestinales, por el doctor Fidel Fernández. Un volumen en cuarto menor de 134 páginas. Salvat Editores, S. A. Barcelona- Buenos Aires. 1940. Doctor Alvarez Herrera. - Tanatología forense. - "Manuales de Medicina Práctica" Salvat Editores, S. A. 1940. Dr. F. Gallart Monés: Ocho lesiones clínicas.- Quinta serie. Un tomo de 212 páginas y 110 fgs. Editorial Salvat. 1939. Enfermedades piogenas y parasitarias de la piel. Por el doctor José Gay Prieto catedrático numerario de Dermatolog...

Los artesanos de la luz. Boceto picassiano de Pablo Picasso

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Hector Rojas Herazo

1966-11-01

Full Text Available En una playa de Antíbes -enérgico vaho de limoneros, de crustáceos, de fúlgidos peces entre el cobre solar- aparece Pablo Picasso. Sólido él, prieto de sí mismo, grave y concentrado, con su sólida arquitectura de toro bravo, de toro de lidia español, de toro altamirense que trae enredados en sus cuernos los primarios racimos atesorados en la caverna. Corajuda la vida de este hombre. Un primitivo peligroso. Ojos saltones, desafiantes, inquisitivos...

78 FR 44602 - Amendment of Statement of Organization and Functions; Restructuring of National Labor Relations...

Science.gov (United States)

2013-07-24

..., Buchanan, Buena Vista, Butler, Calhoun, Carroll, Cass, Cedar, Cerro Gordo, Cherokee, Chickasaw, Clarke..., Florence, Fond du Lac, Forest, Grant, Green, Green Lake, Iowa, Jefferson, Juneau, Kenosha, Kewaunee, La...

Observations of Runoff Generation During the Dry/Wet Seasonal Transition in Panama

National Research Council Canada - National Science Library

Ogden, Fred L

2005-01-01

.... Instrumentation installed include an eddy-correlation flux system on a 36 m tall tower near Cerro Pelado, and throughfall troughs, soil moisture sensors, rain gages, interflow collector, piezometers...

Chemical and isotopic characteristics of rainwater at Los Humeros geothermal field, Puebla, Mexico and surrounding areas; Caracteristicas quimicas e isotopicas del agua de lluvia en el campo geotermico de Los Humeros, Puebla, Mexico y zonas aledanas

Energy Technology Data Exchange (ETDEWEB)

Tovar Aguado, Rigoberto; Cruz Grajales, Irma [Comision Federal de Electricidad, Los Humeros, Puebla (Mexico)

2000-12-01

A study of chemical and isotopic characteristics of rainwater at Los Humeros geothermal field was undertaken for the second consecutive year. Samples were collected in seven stations-two inside the field and five on the periphery. In 1996, a total of 99 samples were collected and 104 were collected in 1997. Of these, 19-18.26% of the total-had a negative alkalinity. The Atempan (No.5) and Campamento (No.1) stations showed the highest number of anomalous samples (31.25 and 27.8%, respectively). Anomalous samples in Perote station were not observed a result that we attribute to the predominant wind direction. The results for the Campamento station are attributed to the thermal inversion phenomena occurring when the samples with negative alkalinity were obtained. Concentrations of cations in some samples were relatively high, with the maximum concentration of calcium in the Los Humeros station (79.7 ppm) . Other significantly high values were found in the Texcal station (34.8 ppm) and Perote (33.8 ppm) due to the presence of dust particles scattered in the air and because of the lack of pavement where the sampling stations are located. Another factor affecting these figures could be the presence of block and lime factories in the neighborhood. Although measured concentrations may seem high, reports exist with similar concentrations in nongeothermal areas. Oxygen-18 and deuterium contents were determined for each stations, mixing anomalous samples. The results show that the most enriched samples correspond to the San Juan Xiutetelco, Puebla (No. 6) station and the minimum to the Perote Veracruz (No. 7) station. The concentration of SO{sub 4} has marine and industrial origins, with a contribution of the first source ranging between 10 and 25 percent. [Spanish] En el campo geotermico de Los Humeros, Puebla se realizo, por segundo ano consecutivo, la caracterizacion quimica e isotopica de agua de lluvia en muestras colectadas en siete estaciones, dos localizadas dentro

Application of ethanol as a geothermal tracer: a field-test in the Los Azufres geothermal field, Michoacan, Mexico

Energy Technology Data Exchange (ETDEWEB)

Tello Hinojosa, Enrique [Comision Federal de Electricidad, Morelia, Michoacan (Mexico); Pal Verma, Mahendra [Comision Federal de Electricidad, Morelia, Michoacan (Mexico); Suarez Arriaga, Mario C. [Universidad Michoacana de San Nicolas de Hidalgo, Morelia, Michoacan (Mexico); Barrera Conzalez, Victor; Sandoval Medina, Fernando [Comision Federal de Electricidad, Morelia, Michoacan (Mexico)

2005-12-01

The thermal decomposition rate of ethanol, rhodamine WT and fluoroscein was determined from laboratory data obtained under conditions of temperature and pressure that simulated a geothermal reservoir. It was found that ethylic alcohol had better thermal stability rhodamine and fluoroscein. Using data obtained from de-ionized water experiments after 168 hours and 200 degree centigrade of temperature, the rhodamine WT and fluoroscein presented a degradation of 99.4% and 99.7%, respectively, while for the ethanol the degradation percentage under the same conditions was only of 44.6%. According to this, ethylic alcohol can be used as a conservative tracer up to about 250 degree centigrade, while rhodamine WT and fluoroscein can be used only at less than 200 degree centigrade, and only where the transit return time is expected to be less than 7 days. Ethanol was used as a conservative tracer in a field test in the southern zone of the Los Azufres geothermal field. The highest concentration was detected in a monitoring well in the steam phase 15 days after the injection, and in the liquid phase, or brine, 34 days after the injection. This suggests that alcohol fractionates preferentially in the steam phase and moves or migrates twice as fast than it does in the liquid phase. The tracer speed can be calculated in 176 m/day in the steam phase and 77.5 m/day in the brine. The ethanol presents good enough characteristics to be used as a tracer in both phases in geothermal environments. [Spanish] Se determino la velocidad de descomposicion termica del etanol, la rodamina y la fluoresceina a partir de datos de laboratorio obtenidos bajo condiciones de presion y de temperatura que simulan las de un yacimiento geotermico. Se encontro que el alcohol etilico presenta una mayor estabilidad termica que la rodamina y la fluoresceina. Empleando los datos obtenidos de experimentos con agua de-ionizada despues de 168 horas y a 200 grados centigrados de temperatura, la rodamina y la

La construcción de un cielo: Casa Goycoolea

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Rodrigo Lagos Vergara

1995-12-01

Full Text Available La casa se ubicará en una de las cuencas que deja el cerro Caracol a lo largo del río Bío-Bío en Concepción. El terreno es de dimensiones modestas y es un sitio entre medianeros que se encuentra dominado por vistas de las casas vecinas. La calle Los Copihues, hacia la que da el predio, es de tráfico limitado salvo los días de fiesta debido a que da acceso al Country Club de la ciudad. Esto determina que las únicas vistas apetecibles desde el sitio sean el horizonte de cerros, el cielo, y el acceso al Country Club, ya que por ese punto se abre el espacio y se accede.

Aspectos de los sobrenatural en Pampas-La Florida (Chancay

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Isabelle Lausent

1984-12-01

Full Text Available La Pacarina del pueblo de "San Salvador del Mundo" de Pampas (valle de Chancay es el cerro Mango. Las repetidas Extirpaciones de Idolatría que sufrieron "sus hijos", el mestizaje y el transcurso del tiempo han, poco a poco, hecho desaparecer los mitos que frataban del Mango. La tradición oral de Pampas que da mucha importercia al mundo de lo sobrenatural sigue, sin embargo, ofreciendo numerosos cuentos y leyendas mencionando este cerro ya no como pacarina sino como una mina fuente de riqueza y lugar de encanto.El análisis que sigue ha sido realizado a partir de Ics cuentos recopilados por Jorgc Osterling durante la Semana Santa del año de 1980 en el rnismo Pampas La Florida.

El neopaleozoico de la Sierra de Castaño (Cordillera Frontal andina, San Juan, Argentina: Reconstrucción tectónica y paleoambiental The neopaleozoic of the Sierra de Castaño (Andean Cordillera Frontal, San Juan, Argentina: Tectonic and paleoenviromental reconstruction

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Pedro Busquets

2013-01-01

Full Text Available Se efectúa el análisis estratigráfico de la secuencia neopaleozoica aflorante en la Sierra de Castaño (Cordillera Frontal de la provincia de San Juan, donde han sido reconocidas tres unidades estratigráficas. La basal corresponde a la Formación Cerro Agua Negra (Carbonífero tardío-Pérmico temprano?, formada por areniscas y pelitas depositadas en ambiente marino de plataforma somera y litoral. Sobre ella se dispone la Formación San Ignacio, compuesta por sedimentitas silicoclásticas (desde conglomerados hasta pelitas, calizas estromatolíticas-microbiales, rocas volcánicas, en su mayoría de composición mesosilícica y ácida, y depósitos volcanoclásticos. Estas últimas rocas, probablemente depositadas hacia fines del Carbonífero tardío o en el Pérmico más temprano, cubren en discordancia angular a las de la Formación Cerro Agua Negra en la Sierra de Castaño. Dentro de la Formación San Ignacio fueron identificadas 3 asociaciones de facies sedimentarias. La inferior (AFa está formada por brechas, conglomerados brechosos y areniscas líticas, sedimentadas en sistemas aluviales y fluviales entrelazados que rellenaron una irregular topografía labrada sobre la Formación Cerro Agua Negra. La asociación de facies media (AFb, compuesta por conglomerados, areniscas y pelitas, desarrolla ciclos granodecrecientes de escala métrica muy probablemente originados en sistemas fluviales de alta sinuosidad. La asociación de facies superior (AFc comprende calizas estromatolíticas microbiales, pelitas, niveles de volcanitas y piroclastitas, originadas en cuerpos de aguas someros sujetos a recurrente actividad volcánica. La Formación San Ignacio permite caracterizar el pasaje entre las sucesiones no volcánicas de la Formación Cerro Agua Negra y el intenso magmatismo representado en el Grupo Choiyoi (Pérmico medio-Triásico Inferior. Además demuestra la existencia de dos eventos mayores de deformación tectónica en la regi

Detailed chronology of a giant Pleistocene rock-avalanche sequence in the hyperarid southern Peru revealed by jointly applied 10Be and 3He cosmic ray exposure dating : The Study case of the Cerro Caquilluco landslide complex.

Science.gov (United States)

Swann, Zerathe; Laurence, Audin; Carlos, Benavente; Régis, Braucher; Pierre-Henri, Blard; Didier, Bourlès; Julien, Carcaillet; Fabrizio, Delgado; Pascal, Lacroix; Valderrama Patricio, Murillo; Aster Team

2015-04-01

Giant landslides are recognized to be remarkably abundant on the Western Andean front of southern Peru and northern Chile, especially in the Arica Bend region (e.g. Crosta et al., 2014a). This area is characterized by strong topographic gradients and subsequent incision of deep canyons, due to the evolution of the Andean range that provide suitable conditions for the development of such instabilities. The climate is hyper-arid (Atacama Desert), although rare but highly impulsive wet events have been evidenced since the Pleistocene. In parallel, this region is submitted to strong (Mw 8-9) and recurrent (~100 yrs) subduction earthquakes. Previous studies suggest that large landslides represent the main agent of erosion of the Western Cordillera, providing soft material for subsequent fluvial remobilization. However the lack of time constrains on the numerous fossil landslides identified away from major canyons still hamper to assess a real mass balance of sliding material versus the known fluvial erosion and tectonic uplift rates. Finally the role of landslides in the long-term erosion rates of the Andean range on its arid flank remains quantitatively unknown. Recently, two studies gave divergent opinions about the main factor supposed to control the slope failures in that region. Based on cosmogenic nuclides derived erosion rates, McPhillips et al. (2014) argue that the last Holocene climate variation did not have had any effect on the rate of landsliding, suggesting that here landslides are mainly triggered by earthquake. On the other hand, Margirier et al. (2014) have showed a temporal correlation between a failure episode of the giant Chuquibamba landslide and the Ouki wet climatic event identified on the Altiplano ~100 ka ago. In this study we focus on dating the Cerro Caquilluco rock avalanche complex described by Crosta et al. (2014). With a total volume of about 15 km3, a length of 43 km and an internal structure characterized by various depositional lobes

Intermittency of gravity wave momentum flux in the mesopause region observed with an all-sky airglow imager

Science.gov (United States)

Cao, Bing; Liu, Alan Z.

2016-01-01

The intermittency of gravity wave momentum flux (MF) near the OH airglow layer (˜87 km) in the mesopause region is investigated for the first time using observation of all-sky airglow imager over Maui, Hawaii (20.7°N, 156.3°W), and Cerro Pachón, Chile (30.3°S, 70.7°W). At both sites, the probability density function (pdf) of gravity wave MF shows two distinct distributions depending on the magnitude of the MF. For MF smaller (larger) than ˜16 m2 s-2 (0.091 mPa), the pdf follows a lognormal (power law) distribution. The intermittency represented by the Bernoulli proxy and the percentile ratio shows that gravity waves have higher intermittency at Maui than at Cerro Pachón, suggesting more intermittent background variation above Maui. It is found that most of the MF is contributed by waves that occur very infrequently. But waves that individually contribute little MF are also important because of their higher occurrence frequencies. The peak contribution is from waves with MF around ˜2.2 m2 s-2 at Cerro Pachón and ˜5.5 m2 s-2 at Maui. Seasonal variations of the pdf and intermittency imply that the background atmosphere has larger influence on the observed intermittency in the mesopause region.

Ciberperiodismo en el estado Zulia: Hacia las nuevas competencias profesionales

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Carmen Mara Prieto

2009-05-01

Full Text Available El objetivo de la investigación se centró en describir el perfil profesional de los periodistas que laboran en los cibermedios del estado Zulia. Para abordar el problema se tomó como punto de partida las experiencias periodsticas vivenciadas en cibermedios zulianos (Faras y Prieto, 2006, 2007; Mogollón y Prieto, 2006 y el perfil del ciberperiodista definido por Albarrán (2008, Aguirre (2006, Saba (2006, Camus (2002 y Gil (1999. Esto implicó describir y caracterizar los equipos de profesionales que integran los cibermedios de la región zuliana en función de aportar a la configuración del perfil del nuevo periodista que pretenda desempeñarse con acierto en el ciberespacio. Desde el punto de vista metodológico, se trató de una investigación descriptiva de carácter cuantitativo con diseño transeccional donde se aplicó como instrumento la encuesta. Entre las conclusiones de la investigación destacan que las competencias ciberperiodsticas en su mayora están instrumentalizadas y asociadas al manejo de editores de texto y datos, as como Internet, siendo estas herramientas suficientes para cubrir las expectativas de sus labores, revelando en este sentido estar muy lejos de los constructos teórico-éticos que deben fundamentar el ciberperiodismo. Predomina en las ciberredacciones del estado Zulia profesionales jóvenes del género masculino egresados en el último lustro, y existe una falta de consenso en las denominaciones de cargos y funciones.

Evolution of the geothermal system in Acoculco, Pue., Mexico: Study based on petrography of well EAC-2 and other information; Evolucion del sistema geotermico de Acoculco, Pue., Mexico: un estudio con base en estudios petrograficos del pozo EAC-2 y en otras consideraciones

Energy Technology Data Exchange (ETDEWEB)

Viggiano Guerra, Julio Cesar [Universidad Michoacana de San Nicolas de Hidalgo, Michoacan (Mexico)]. E-mail: cesar.viggiano@live.com; Flores Armenta, Magaly; Ramirez Silva, German R. [Comision Federal de Electricidad, Gerencia de Proyectos Geotermoelectricos, Morelia, Michoacan (Mexico)

2011-01-15

yacimientos tipo kaipohan. Dos pozos exploratorios se han perforado en la zona: en 1995 el EAC-1 a 1810 m de profundidad y en 2008 el EAC-2 a 1900 m de profundidad. En este reporte se discuten los resultados e interpretacion de los estudios petrograficos del segundo pero se emplea parte de la informacion del primero para la interpretacion de la evolucion del sistema hidrotermal. De manera sintetica se puede establecer que la zona geotermica de Acoculco se encuentra en su etapa hidrotermal senil dado que se ha verificado, de acuerdo con los estudios de mineralogia hidrotermal y con otras consideraciones, un cambio en el regimen de convectivo hacia convectivo forzado o conductivo. Sobresale el hecho de que el sistema no se ha reciclado, quiza porque las rocas no lo han permitido y, por lo tanto, esta feneciendo. Esto, naturalmente, no ha sido obice para la presencia de un importante volumen de masa caliente (300 grados centigrados) hornfelsica y granitica en el subsuelo que abre un espectro de posibilidades para la explotacion de un sistema geotermico mejorado (EGS, por sus siglas en ingles). Quedaria por investigar la factibilidad del proyecto en el tema de la vulnerabilidad de las rocas de yacimiento (hornfels y granito) para su mejora de permeabilidad por los medios convencionales experimentados en estos proyectos, ya que parece ser que la naturaleza fracaso en ese intento.

Cerámica común tardorromana, imitación de sigillata, en la provincia de Segovia. Aproximación al estudio de las producciones cerámicas del siglo V en la Meseta Norte y su transición al mundo hispano-visigodo

Directory of Open Access Journals (Sweden)

Juan Tovar, Luis Carlos

1997-12-01

Full Text Available The Vth century A.D. is possibly the least known period of Roman Hispania, especially as far as its material culture is concerned: town planning, architecture, pottery, metalwork, glass, and so on. In this paper we tackle a particular area of that material culture within a specific region: the common pottery (table and kitchen ware, imitation of the terra sigillata, in the Segovia province. Our essential aim has been to define its technical, typological and decorative characteristics, as well as the features it bears in common with the terra sigillata, and its significance in the origin of Hispanic-Visigothic pottery. In order to do so, we have taken into account ceramics from towns such as Cauca, Cerro del Castillo (in Bernardos or Cerro de la Virgen de Tormejón (in Armuña, as well as rural settlements (villae rusticae?, burying grounds (El Cantosal, Aguilafuente, Duratón, etc., and single findings.De la Hispania romana tal vez el periodo más desconocido sea el siglo V, sobre todo en los aspectos referidos a sus restos materiales: urbanismo, arquitectura, cerámica, metalistería, vidrio, etc. En este trabajo hemos abordado una parte concreta de esta cultura material en una zona determinada: la cerámica común (tanto de mesa, como de cocina, imitación de sigillata, en la provincia de Segovia. Definir sus características técnicas, tipológicas, decorativas, así como su similitud con la terra sigillata y su significado en la formación de la cerámica hispano-visigoda, ha sido nuestro objetivo básico. Para ello, hemos tenido en cuenta tanto cerámica proveniente de núcleos urbanos como Cauca, el Cerro del Castillo (en Bernardos o el Cerro de la Virgen de Tormejón (en Armuña, como de asentamientos rurales (¿villae rusticae?, necrópolis (El Cantosal, Aguilafuente, Duratón, etc. y hallazgos aislados.

Initial isotopic geochemistry ({delta} 18 O, {delta} D) of fluids from wells of the Los Humeros, Pue., geothermal field; Geoquimica isotopica ({delta} 18 O, {delta} D) inicial de fluidos de pozos del campo geotermico de Los Humeros, Pue.

Energy Technology Data Exchange (ETDEWEB)

Barragan Reyes, Rosa Maria; Arellano Gomez, Victor Manuel [Instituto de Investigaciones Electricas, Gerencia de Geotermia, Cuernavaca, Morelos (Mexico)]. E-mail: rmb@iie.org.mx; Ramirez Montes, Miguel; Tovar Aguado, Rigoberto [Comision Federal de Electricidad, Gerencia de Proyectos Geotermoelectricos, Morelia, Michoacan (Mexico)

2010-01-15

Isotopic data ({delta} 18 O, {delta} D) from fluids from production wells at the Los Humeros, Pue., geothermal field were analyzed to investigate the possible origin of these fluids and the dominant processes of the reservoir at its initial state. According to pre-exploitation data, it is suggested the Los Humeros reservoir fluids are made of a mixture of meteoric water of very light isotopic composition (paleo-fluids) and andesitic water. The relationship {delta} D vs {delta} 18 O from pre-exploitation data indicates the produced fluids are composed of a mixture of (at least) two fluids with distinct isotopic compositions. At the more enriched end of the mixing relationship are the isotopic compositions of the wells H-23 and H-18 (located in the southern area of the field), while the lighter fluids were found in well H-16 (originally) and then in well H-16 (repaired). It was found that the liquid phases of deep wells are more enriched in {delta} 18 O while the shallow wells present lower values, suggesting a convection process at the initial state. Based on this isotopic profile, it is considered that even the production depths of the wells H-1, H-12 and H-16 (repaired) are just about the same, but their respective isotopic compositions are quite different. The {delta} 18 O value for well H-16 (repaired) seems to be that of condensate steam, while the corresponding values for wells H-1 and H-12 fall within the value interval of the deep wells (H-23). This suggests wells H-1 and H-12 are collecting very deep fluids enriched in {delta} 18 O. These results could be useful in creating a conceptual model of the reservoir. [Spanish] Se analizaron datos isotopicos ({delta}18 O, {delta}D) de los fluidos de pozos productores del campo geotermico de Los Humeros, Pue., para investigar el posible origen de los fluidos asi como los procesos dominantes del yacimiento en su estado inicial. De acuerdo con datos previos a la explotacion, se plantea que los fluidos del yacimiento

De miasmas a mosquitos: el pensamiento médico sobre la fiebre amarilla en Yucatán, 1890-1920

OpenAIRE

Alcalá Ferráez,Carlos

2012-01-01

La fiebre amarilla fue un problema de salud pública desde la época colonial debido a la frecuencia con que se presentaba en forma epidémica y a su alta letalidad. El objetivo de este trabajo es analizar el pensamiento médico y su evolución con respecto al vómito prieto entre 1890 y 1921 en Yucatán. Dos aspectos serán abordados: algunos antecedentes con respecto a la enfermedad y las ideas predominantes hasta 1881; y la propuesta de Carlos Finlay para vencer el escepticismo ante su teoría por ...

De miasmas a mosquitos: el pensamiento médico sobre la fiebre amarilla en Yucatán, 1890-1920 From miasmas to mosquitoes: medical thought on yellow fever in Yucatan, 1890-1920

OpenAIRE

Carlos Alcalá Ferráez

2012-01-01

La fiebre amarilla fue un problema de salud pública desde la época colonial debido a la frecuencia con que se presentaba en forma epidémica y a su alta letalidad. El objetivo de este trabajo es analizar el pensamiento médico y su evolución con respecto al vómito prieto entre 1890 y 1921 en Yucatán. Dos aspectos serán abordados: algunos antecedentes con respecto a la enfermedad y las ideas predominantes hasta 1881; y la propuesta de Carlos Finlay para vencer el escepticismo ante su teoría por ...

Department of Energy: Opportunities Exist to Improve Los Alamos' Equipment Purchasing Practices

National Research Council Canada - National Science Library

2001-01-01

In fiscal year 2000, the Department of Energy (DOE) received $13.2 million in supplemental funding to replace equipment lost in the May 2000 Cerro Grande fire that damaged the Los Alamos National Laboratory...

Mining reservation X IV. Present state of geological researchs; Reserva Minera XIV estado actual de las investigaciones geologicas

Energy Technology Data Exchange (ETDEWEB)

Gomez Rifas, C; Tabo, F

1991-07-01

The mining reservation includes the aerial photo of Cerro Chato, Valentines, Chileno and Rossell y Rius. The main objective of this work is the regional metals characterization in special basic metals such as gold.

Mining reservation X IV. Present state of geological research s

International Nuclear Information System (INIS)

Gomez Rifas, C.; Tabo, F.

1991-01-01

The mining reservation includes the aerial photo of Cerro Chato, Valentines, Chileno and Rossell y Rius. The main objective of this work is the regional metals characterization in special basic metals such as gold.

Uranium project in Cerro Largo south orientation

International Nuclear Information System (INIS)

Pradier, B.

1982-01-01

This study of orientation was realized with the purpose of recognizing the extension of the anomalies from a known source , and of being able to determine the choice of the places and the quality of the material to sampling to obtain an ideal response. We have chosen the introduction of this study in a place that offers a source in power of Uranium located accurately and that presents a sequence pedology that group the main types of soils

La explotación tartésica de la casiterita entre los ríos Tajo y Guadiana: San Cristóbal de Logrosán (Cáceres

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Rodríguez Díaz, Alonso

2013-06-01

Full Text Available The objective of this work is to offer a synthesis of the archaeological and archaeo-mining investigation carried out in recent years (1998 and 2000-2002 in the Cerro de San Cristobal site, Logrosán (Cáceres. The results allow us to propose a chaîne opératoire for the cassiterite treatment and use in Cerro de San Cristóbal during the transition from the Late Bronze Age to the Orientalizing period. The management and role of this mineral in the Tajo-Guadiana relations and in the Atlantic- Mediterranean circuits meeting in the Southwest of the Iberian Peninsula, together with other factors, seems to justify the early integration of the territory of Extremadura in Tartessos. The investigation in Logrosán and the archaeology of tin were suddenly interrupted by the unexpected death of its main promoter, Dr. Craig Merideth. The continuation of this project is now to be channelled through the recent declaration of the Cerro de San Cristobal as a ‘geosite’ in the ‘Ibores-Villuercas- Jara Geopark’ and through the National Research, Development and Innovation Scheme’s project El tiempo del tesoro de Aliseda, among whose actions is the archaeomining survey from the West of the peneplain of Cáceres made in 2011.El objetivo de este trabajo es ofrecer una síntesis de la investigación arqueológica y arqueominera realizada entre 1998 y 2000-2002 en el Cerro de San Cristóbal de Logrosán (Cáceres. Esta permite proponer una probable ‘cadena operativa’ del beneficio de la casiterita en este lugar durante el tránsito Bronce Final-Periodo Orientalizante. La gestión e imbricación del mineral en las relaciones Tajo-Guadiana y en los circuitos atlántico-mediterráneos confluyentes en el Suroeste de la Península Ibérica parecen justificar, entre otras razones, la temprana integración del actual territorio extremeño en Tartessos. La investigación en Logrosán y la arqueología del estaño se vieron bruscamente interrumpidas por el

Efectos negativos de las plantas exóticas maderables sobre el bosque nativo andino

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Fidel Antonio Gutiérrez

2011-07-01

Full Text Available Los abusos que el hombre ha cometido con la naturaleza han provocado que muchas áreas, que debían ser santuarios vegetales, padezcan el deterioro del bosque nativo, con el consiguiente daño ambiental, hídrico, de flora y fauna. No escapa a ello la Escuela Nacional de Carabineros, pues su cerro tutelar fue sometido a una plantación de árboles exóticos maderables, con la consabida tala del bosque nativo. Los daños en dicho cerro han provocado la implementación de una reforestación técnica, que permita devolver la dinámica propia a la vegetación nativa, lo cual debe dar como resultado un Plan Estratégico de Manejo Ambiental, para futuras aplicaciones.

Función pulmonar en niños sanos de 7 y 8 años de las comunas de Cerro Navia y Los Andes expuestos a diferentes niveles de contaminación por MP10

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Daniel Cebulj Navarrete

2011-01-01

Full Text Available Objetivo: Determinar si difieren los valores espirométricos evaluados en niños sanos de 7- 8 años provenientes de comunas con niveles históricos de alta versus baja contaminación atmosférica en Chile. Materiales y métodos: Estudio descriptivo, no experimental, exploratorio y transversal y ex post facto causa y efecto. Se realizaron en total 261 encuestas de salud respiratoria y calificaron, según criterios de inclusión, 110 niños sanos de 7 y 8 años (55 niños en cada comuna. Se realizaron exámenes espirométricos: Con espirómetro de turbina SPIROBANK G, considerando variables VEF1, FEF25-75, PEF y CVF. La obesidad, actividad física, contaminación intramuros por calefacción y exposición a humo de tabaco también fueron descritas. Resultados: Las variables espirométricas analizadas VEF1 y FEF25-75 mostraron diferencias significativas (p<0.05 y PEF mostró diferencias altamente significativas (p <0.005 según localidad, es decir, que la media de estas variables en Los Andes, comuna agroindustrial con baja contaminación atmosférica, es mayor que la de Cerro Navia, comuna con altos niveles de contaminación del aire. En la variable PEF se encontró, además, significancia entre género. La CVF no presentó diferencia entre comunas. Conclusiones: Los niños sanos de 7 y 8 años que habitan en comunas donde la exposición a contaminación atmosférica es alta presentan una menor función pulmonar comparada con los niños sanos, de similares características, que habitan en comunas con bajos niveles de contaminación atmosférica. Existen otros factores que podrían influir en el detrimento de la función pulmonar y que en este estudio fueron descritos como factores confundentes.

Uranium project in Cerro Largo south orientation[Geochemical prospection of Uranium in Uruguay]; Proyecto uranio: orientacion Cerro Largo Sur

Energy Technology Data Exchange (ETDEWEB)

Pradier, B

1982-07-01

This study of orientation was realized with the purpose of recognizing the extension of the anomalies from a known source , and of being able to determine the choice of the places and the quality of the material to sampling to obtain an ideal response. We have chosen the introduction of this study in a place that offers a source in power of Uranium located accurately and that presents a sequence pedology that group the main types of soils.

Anomalously high values of cesium-137 in soils on the Peninsula de Paraguana (Venezuela)

International Nuclear Information System (INIS)

LaBrecque, J.J.; Rosales, P.A.; Cordoves, P.R.

2001-01-01

The activity of 137 Cs in surface soils (2-5 cm) was determined at twenty-one sampling sites along the northwestern and eastern coast of the Paraguana peninsula (Venezuela), as well as, at nine locations, between 95 and 535 m.a.s.l. on Cerro Santa Ana. The measurements were performed by high-resolution gamma-ray spectroscopy employing a compatible IBM computer. Most of the values were much higher than those found along the coastline of the mainland; four sites were found to be anomalously high, with 137 Cs values greater than 10 Bq/kg. It is difficult to explain these anomalous 137 Cs values by geographical or climatological factors since there is little rainfall here and the clouds and fog are rarely if never present along the coast of the peninsula. Possibly, some mechanism of the mist that is blown ashore could explain these anomalies. The values of the 137 Cs versus altitude on the Cerro Santa Ana show an increase of two or three times at 500 m.a.s.l. level, thus we have concluded that the base of the clouds was at this height when the fallout was directly deposited by condensation in this cloud forest. These results in the Cerro Santa Ana cloud forest are similar to those of other cloud forests along the Venezuelan coast, but the altitude (m.a.s.l.) of the base of the clouds here are much lower. (author)

Presencia del tinamú canelo (Crypturellus cinnamomeus en dos áreas naturales protegidas del centro de Nuevo León, México

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David Alberto Borré González

2011-07-01

Full Text Available Reportamos la presencia de dos individuos de Crypturellus cinnamomeus y proporcionamos evidencia fotográfica de dichos registros en el Monumento Natural Cerro de la Silla y Sierra “Cerro de la Silla”; áreas naturales protegidas de competencia federal y estatal respectivamente que forman parte del corredor biológico de la Sierra Madre Oriental para especies neotropicales. La importancia de la información que proporcionamos aquí sobre los registros realizados el 27 de mayo y 5 de julio de 2011 radica en que constituyen una ampliación en la distribución de esta especie sujeta a protección especial (Pr según la NOM-059-SEMARNAT-2010, y a que se registra por primera vez en ambas vertientes del macizo montañoso Sierra de la Silla.

Light in Rural Schools, polyclinics and police detachment : inventory of 210 rural units, energetic and socio economics review

International Nuclear Information System (INIS)

Santiago Silva, T.

1994-01-01

With the aim to the future solar installations system in the rural area it has been done a report about 210 rural units placed in: Rivera, Tacuarembo, Salto, Paysandu, Florida, Flores, Lavalleja, Durazno, Cerro largo y Rio Negro departments

Light in Rural Schools, polyclinics and police detachment : inventory of 210 rural units, energetic and socio economics review; Luz para Escuelas, policlinicas y destacamentos policiales rurales: relevamiento de 210 unidades rurales, evaluacion energetica y socioeconomica

Energy Technology Data Exchange (ETDEWEB)

Santiago Silva, T [Red fotovoltaica Latino-Europea patrocinada por CC.EE. (Uruguay)

1994-07-01

With the aim to the future solar installations system in the rural area it has been done a report about 210 rural units placed in: Rivera, Tacuarembo, Salto, Paysandu, Florida, Flores, Lavalleja, Durazno, Cerro largo y Rio Negro departments.

Melhoramento do trigo: VIII. Associações entre produção de grãos e outros caracteres agronômicos em populações híbridas envolvendo diferentes fontes de nanismo Wheat breeding: VIII. Associations of grain yield with other agronomic characteristics in crosses involving different sources of dwarfism in wheat

Directory of Open Access Journals (Sweden)

Carlos Eduardo de Oliveira Camargo

1984-01-01

Full Text Available Foram estimados os valores da herdabilidade para várias características da planta do trigo (comprimento da espiga, número de espiguetas por espiga, número de grãos por espiga e de grãos por espigueta, peso de cem grãos, número de espigas por planta, altura das plantas e produção de grãos, bem como as correlações entre produção de grãos e os demais caracteres agronômicos. Os estudos foram realizados em cruzamentos entre o cultivar C-3, de porte alto, e os cultivares Tordo, Vican-71 e Olesen, de porte anão, e 'Siete Cerros', de porte semi-anão. Sementes representando os pais e as gerações F1 e F2 e os retrocruzamentos para ambos os pais foram utilizados em um ensaio, em blocos ao acaso, com quatro repetições, conduzido na Estação Experimental de Itararé, do Instituto Agronômico. Os dados foram coletados na base de plantas individuais. A herdabilidade no sentido amplo, para número de espiguetas por espiga e altura das plantas foi, respectivamente, 0,533 e 0,525, enquanto para comprimento da espiga, número de grãos por espiga e de grãos por espigueta, peso de cem grãos e número de espigas por planta, os valores observados variaram de 0,339 a 0,473. Para produção de grãos a estimativa obtida da herdabilidade no sentido amplo foi 0,255. Os valores da herdabilidade no sentido restrito, para os caracteres estudados, com exceção do número de espigas por planta, mostraram que grande parte da variabilidade de origem genética encontrada nas populações está também associada a uma ação aditiva dos genes. As correlações fenotípicas entre a produção de grãos e todos os demais caracteres agronômicos foram positivas e significativas ao nível de 1% para quase todas as populações estudadas. Constituíram exceções as correlações fenotípicas entre produção de grãos e número de espiguetas por espiga para as populações C-3 x Siete Cerros e C-3 x Vican-71; entre produção de grãos e peso de cem gr

Melhoramento do trigo: XXX. Avaliação de linhagens com tolerância a toxicidade de alumínio, manganês e ferro em condições de campo Wheat breeding: XXX. Evaluation of inbred lines tolerant to aluminum, manganese and iron toxicities under field conditions

Directory of Open Access Journals (Sweden)

Carlos Eduardo de Oliveira Camargo

1995-01-01

Full Text Available Compararam-se 23 linhagens tolerantes, ao mesmo tempo, à toxicidade de Al3+ Mn2+ e Fe2+, provindas do cruzamento entre 'BH-1146' (tolerante à toxicidade de A1(3+ e sensível à de Mn2+ e Fe2+ e 'Siete Cerros' (sensível à toxicidade de A1(3+ e tolerante à de Mn2+ e Fe2+ e os dois cultivares utilizados como pais em quatro ensaios instalados nas Estações Experimentais de Itararé (1990-92 e de Capão Bonito (1992, em solos ácidos, e em cinco ensaios realizados no Centro Experimental de Campinas (1990-92 e na Fazenda Santa Lúcia (1990-91, município de Cruzália, em solos corrigidos, analisando os seguintes parâmetros: rendimento de grãos, características agronômicas e resistência às doenças. Em solos ácidos, vinte linhagens e o 'BH-1146' mostraram maior rendimento de grãos em relação ao 'Siete Cerros' indicando que a toxicidade de alumínio foi um dos principais fatores limitantes à produção. Em solos corrigidos, não se verificaram diferenças significativas entre os genótipos estudados quanto ao rendimento de grãos, mostrando não haver urna associação entre baixa produtividade e tolerância ao A1(3+ nessas condições. A linhagem 21 foi moderadamente resistente ao agente causal de oídio em condições naturais de infecção. Todos os genótipos avaliados revelaram suscetibilidade aos agentes causais das manchas foliares. O 'Siete Cerros' e as linhagens 3 a 12 apresentaram porte baixo associado à menor porcentagem de acamamento; as 13, 14 e 23 mostraram espigas compridas; a 12, maior número de espiguetas e grãos por espiga, e a 17, grãos mais pesados, representando fontes genéticas de valor para essas características.Twenty three inbred lines showing at the same time tolerance to A1(3+, Mn2+ and Fe2+ toxicities, originated from the cross between 'BH-1146' (tolerant to Al3+ toxicity and sensitive to Mn2+ and Fe2+ toxicities and 'Siete Cerros' (sensitive to Al3+ and tolerant to Mn2+ and Fe2+ toxicities, and the two

Equivalent and Alternative Forms for BF Gravity with Immirzi Parameter

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Merced Montesinos

2011-11-01

Full Text Available A detailed analysis of the BF formulation for general relativity given by Capovilla, Montesinos, Prieto, and Rojas is performed. The action principle of this formulation is written in an equivalent form by doing a transformation of the fields of which the action depends functionally on. The transformed action principle involves two BF terms and the two Lorentz invariants that appear in the original action principle generically. As an application of this formalism, the action principle used by Engle, Pereira, and Rovelli in their spin foam model for gravity is recovered and the coupling of the cosmological constant in such a formulation is obtained.

Nanofósiles calcáreos paleógenos y biostratigrafía para dos pozos en el este de la Cuenca Austral, Patagonia, Argentina Paleogene calcareous nannofossil biostratigraphy for two boreholes in the eastern Austral Basin, Patagonia, Argentina

Directory of Open Access Journals (Sweden)

Juan Pablo Pérez Panera

2013-01-01

Full Text Available Calcareous nannofossils from two boreholes (Campo Bola and Sur Río Chico in the subsurface of eastern Austral Basin, Santa Cruz Province, Argentina, allowed the identification of Early to Middle Paleocene, Early to Middle Eocene and Late Eocene to Early Oligocene assemblages. These assemblages match the formations logged in the boreholes Campo Bola, Man Aike and Río Leona respectively, and represent three paleogene sedimentary cycles within the basin. These results permitted the reinterpretation of previous data from an adjacent borehole (Cerro Redondo. The southern boreholes (Cerro Redondo and Sur Río Chico yield an Early to Middle Paleocene calcareous nannofossil assemblage and an almost continuous record of nannofossils from Early Eocene to Early Oligocene. A discontinuity is interpreted by the absence of Late Paleocene assemblages. The northern borehole (Campo Bola yield only late Early Eocene to Early Oligocene assemblages. The data also indicates that the Paleogene beds unconformably overlie Upper Cretaceous strata.El estudio de los nanofósiles calcáreos recuperados en muestras de subsuelo de dos pozos de exploración (Campo Bola y Sur Río Chico en el este de la Cuenca Austral, provincia de Santa Cruz, Argentina, permitió reconocer asociaciones del Paleoceno Temprano a Medio, Eoceno Temprano a Medio y Eoceno Tardío a Oligoceno Temprano. Estas asociaciones son coincidentes con las formaciones atravesadas en los sondeos hechos en Campo Bola, Man Aike y Río Leona, respectivamente, y representan tres ciclos sedimentarios paleógenos dentro de la cuenca. Estos resultados permitieron la reinterpretación de datos previos de un pozo adyacente (Cerro Redondo. Los pozos ubicados al sur (Cerro Redondo y Sur Río Chico contienen asociaciones de nanofósiles calcáreos del Paleoceno Temprano a Medio y un registro prácticamente continuo de nanofósiles del Eoceno Temprano al Oligoceno Temprano. Se interpreta una discontinuidad por ausencia de

An InSAR-based survey of volcanic deformation in the central Andes

Science.gov (United States)

Pritchard, M. E.; Simons, M.

2004-02-01

We extend an earlier interferometric synthetic aperture radar (InSAR) survey covering about 900 remote volcanos of the central Andes (14°-27°S) between the years 1992 and 2002. Our survey reveals broad (10s of km), roughly axisymmetric deformation at 4 volcanic centers: two stratovolcanoes are inflating (Uturuncu, Bolivia, and Hualca Hualca, Peru); another source of inflation on the border between Chile and Argentina is not obviously associated with a volcanic edifice (here called Lazufre); and a caldera (Cerro Blanco, also called Robledo) in northwest Argentina is subsiding. We explore the range of source depths and volumes allowed by our observations, using spherical, ellipsoidal and crack-like source geometries. We further examine the effects of local topography upon the deformation field and invert for a spherical point-source in both elastic half-space and layered-space crustal models. We use a global search algorithm, with gradient search methods used to further constrain best-fitting models. Inferred source depths are model-dependent, with differences in the assumed source geometry generating a larger range of accepted depths than variations in elastic structure. Source depths relative to sea level are: 8-18 km at Hualca Hualca; 12-25 km for Uturuncu; 5-13 km for Lazufre, and 5-10 km at Cerro Blanco. Deformation at all four volcanoes seems to be time-dependent, and only Uturuncu and Cerro Blanco were deforming during the entire time period of observation. Inflation at Hualca Hualca stopped in 1997, perhaps related to a large eruption of nearby Sabancaya volcano in May 1997, although there is no obvious relation between the rate of deformation and the eruptions of Sabancaya. We do not observe any deformation associated with eruptions of Lascar, Chile, at 16 other volcanoes that had recent small eruptions or fumarolic activity, or associated with a short-lived thermal anomaly at Chiliques volcano. We posit a hydrothermal system at Cerro Blanco to explain the

Water quality of springs and water wells which are used in human consumption, in the Jocotitlan volcano region at State of Mexico

International Nuclear Information System (INIS)

Baca G, A.; Segovia, N.; Iturbe, J.L.; Martinez, V.; Armienta, M.A.; Seidel, J.L.

1998-01-01

In this work are presented the results of water quality of seven springs (San Antonio Enchisi, Las Fuentes, El Cerro, Pasteje, Los Reyes, Santa Cruz and Tiacaque) and two water wells (Jocotitlan No. 2 and La Providencia No. 35) which are used for human consumption and that are located surrounding area to Jocotitlan volcano, state of Mexico. It was determined the 222 Rn concentration through liquid scintillation, the 226 Ra by Gamma spectroscopy, the physical-chemical parameters (major elements) and bacteriological, using standardized methods. The minor elements and trace in solution were determined by Icp-Ms mass spectroscopy. The water quality was established in function of the standing standards. Therefore Las Fuentes, El Cerro, Santa Cruz, Tiacaque springs and the Jocotitlan No. 2 well, are drinkable water. So, Pasteje, Los Reyes, San Antonio Enchisi springs and the La Providencia No. 35 well are chemically drinkable but presenting bacteriological pollution. (Author)

New species of Scolytodes (Coleoptera: Scolytidae from Costa Rica and Panamá

Directory of Open Access Journals (Sweden)

Bjarte H. Jordal

1998-06-01

Full Text Available Seven species of Scolytodes (tribe Ctenophorini are described as new to science: S. concavus and S. circumsetosus (from Ficus branches, La Selva, S. montanus (Monteverde, S. nudifrons (Las Cruces near San Vito, and S. triangulus (fogging sample, La Selva, all from Costa Rica, and S. ungulatus (Cerro Punta and S. punctifrons (from Astronium graveolens, Canal Zone, both from Panama. New distributional and host plant data are given for the following species: S. amoenus (Ficus branch, La Selva, and the first record south of Mexico, S. immanis (Cerro de La Muerte, S. impressus (Xylopia branch, Peninsula de Osa, S. ochromae (Ochroma branch, La Selva, S. piceus (fogging sample, La Selva, the first low altitude record, and S. swieteniae (fogging sample, La Selva and Braulio Carrillo, the first exact locality data, all from Costa Rica, and S. nanellus (Barro Colorado Island from Panama.

Os isotopes and cooper sources for stratiform (mantos) cooper deposits of Chile

International Nuclear Information System (INIS)

Munizaga, Francisco; Ruiz, Joaquin; Freydier, Claire

1998-01-01

The sources of copper have been determined by studying trace elements osmium and rhenium as well as osmium isotope ratio in copper-bearing porphyry of Chuquicamata, el Teniente and Andacollo and in the stratiform copper deposits of Mantos Blancos, El Soldado, Cerro Negro and Talcuna

KEGS Discovery of 28 Supernova Candidates in the K2 Campaign 17 Field with DECam

Science.gov (United States)

Narayan, G.; Rest, A.; Strampelli, G. M.; Zenteno, A.; James, D. J.; Smith, R. C.; Tucker, B. E.; Garnavich, P.; Margheim, S.; Kasen, D.; Olling, R.; Shaya, E.; Buron, F. Forster; Villar, V. A.

2018-05-01

The Kepler Extra-Galactic Survey (KEGS, see http://www.mso.anu.edu.au/kegs/ ) reports the discovery of 28 supernova candidates with the Dark Energy Camera (DECam, NOAO 2017B-0285) on the 4m Blanco Telescope at Cerro Tololo Inter-American Observatory (CTIO).

Project overview of OPTIMOS-EVE: the fibre-fed multi-object spectrograph for the E-ELT

NARCIS (Netherlands)

Navarro, R.; Chemla, F.; Bonifacio, P.; Flores, H.; Guinouard, I.; Huet, J.-M.; Puech, M.; Royer, F.; Pragt, J.H.; Wulterkens, G.; Sawyer, E.C.; Caldwell, M.E.; Tosh, I.A.J.; Whalley, M.S.; Woodhouse, G.F.W.; Spanò, P.; Di Marcantonio, P.; Andersen, M.I.; Dalton, G.B.; Kaper, L.; Hammer, F.

2010-01-01

OPTIMOS-EVE (OPTical Infrared Multi Object Spectrograph - Extreme Visual Explorer) is the fibre fed multi object spectrograph proposed for the European Extremely Large Telescope (E-ELT), planned to be operational in 2018 at Cerro Armazones (Chile). It is designed to provide a spectral resolution of

Chemostratigraphy of Neoproterozoic Banded Iron Formation (BIF)

DEFF Research Database (Denmark)

Gaucher, Claudio; Sial, Alcides N.; Frei, Robert

2015-01-01

Sawawin BIF (Saudi Arabia), and the Jucurutu Formation of the Seridó Belt (NE Brazil). Lake Superior type BIFs are represented by the Tonian Shilu Group (South China) and the late Ediacaran Arroyo del Soldado Group (Yerbal and Cerro Espuelitas formations, Uruguay). Useful chemostratigraphic tools...

Parque Cultural Valparaíso: Cerro Cárcel

OpenAIRE

Holmes,Jonathan; Labbé,Martín; Portugueis,Carolina; Spichiger,Osvaldo

2009-01-01

Los edificios y terreno de la ex cárcel de Valparaíso son propuestos, a través de un concurso público, para ser remodelados y convertidos en un parque cultural, con programas tales como auditorios, centro de documentación, locales comerciales, y espacios públicos; dejando como testimonio del pasado la antigua Casa de la Pólvora.

Taxonomic and geographic novelties in the genus Plantago (Plantaginaceae) in Chile, including the description of a new species

DEFF Research Database (Denmark)

Hassemer, Gustavo; Shipunov, Alexey; Rønsted, Nina

2018-01-01

We present taxonomic and geographic novelties in the genus Plantago from Chile. More specifically, we describe P. nebularis, a new species endemic to Cerro Moreno, Antofagasta region, and propose P. zoellneriana, a new name for P. sericea subsp. araucana. We also lectotypify the name P. sericea, ...

VizieR Online Data Catalog: UBVI photometry of NGC4337 (Carraro+, 2014)

Science.gov (United States)

Carraro, G.; Giorgi, E. E.; Costa, E.; Vazquez, R. A.

2015-11-01

We took UBVI images of NGC 4337 in a 20x20 squared arcmin area during two observing runs, on 2010 Feb 14 and 2010 Mar 11, at Cerro Tololo Inter-American Observatory, using the 0.9m and the 1.0m telescopes. (1 data file).

Multiple territories in dispute : water policies, participation and Mapuce indigenous rights in Patagonia, Argentina

NARCIS (Netherlands)

Moreyra, A.

2009-01-01

This thesis is about the multiple territories which dispute the shape and control of
the development of the Trahunco-Quitrahue watershed, at Cerro Chapelko,
Neuquén province in Argentinean Patagonian. Built into these disputes are the
struggles of Mapuce peoples -indigenous peoples

Results of the first simultaneous X-ray, optical, and radio campaign on the blazar PKS 1622-297

NARCIS (Netherlands)

Meyer, Angela Osterman; Miller, H. Richard; Marshall, Kevin; Ryle, Wesley T.; Aller, Hugh; Aller, Margo; McFarland, John P.; Pollock, Joseph T.; Reichart, Daniel E.; Crain, J. Adam; Ivarsen, Kevin M.; LaCluyze, Aaron P.; Nysewander, Melissa C.

Coordinated X-ray, optical, and radio observations of the blazar PKS 1622-297 were obtained during a three-week campaign in 2006 using the Rossi X-Ray Timing Explorer (RXTE), the University of Michigan Radio Astronomy Observatory, and optical telescopes at Cerro Tololo Inter-American Observatory.

44 CFR 295.50 - Definitions.

Science.gov (United States)

2010-10-01

... Administrative Appeal. It excludes the opinions, memoranda and work papers of our attorneys and drafts of... liability company, estate, trust, county, city, State, school district, special district or other non..., conclusive and irrevocable election to have all Losses resulting from the Cerro Grande Fire reviewed by FEMA...

Study of liquid and steam tracers at the Maritaro - La Cumbre area of the Los Azufres geothermal field, Mich.; Estudio con trazadores de liquido y vapor en la zona Maritaro - La Cumbre del campo geotermico de Los Azufres, Mich.

Energy Technology Data Exchange (ETDEWEB)

Iglesias, Eduardo R [Instituto de Investigaciones Electricas, Cuernavaca, Morelos, (Mexico)]. E-mail: iglesias@iie.org.mx; Flores Armenta, Magaly; Quijano Leon, Jose Luis; Torres Rodriguez, Marco A [Comision Federal de Electricidad, Morelia, Michoacan (Mexico); Torres, Rodolfo J; Reyes Picasso, Neftali [Instituto de Investigaciones Electricas, Cuernavaca, Morelos, (Mexico)

2008-01-15

We ran two simultaneous tracer tests in the Maritaro-La Cumbre area of the Los Azufres geothermal field in Mexico. We wished to determine whether or not fluids injected in well Az-15 recharged the productive areas of six production wells and to estimate the fractions of injected fluid recovered in them, if any. Because only three of the wells produce water and all of them produce steam, two tracers were used, sulfur hexafluoride (SF{sub 6}) for the gas phase and 1,3,6 naphthalene trisulfonate (1,3,6-nts) for the liquid phase. All of the observation wells recorded SF{sub 6}, and the three water-producing wells recorded 1,3,6-nts, proving that fluids injected in well Az-15 do recharge the area of interest. When sampling was suspended, the three water-producing wells were still producing 1,3,6-nts at significant rates. The total recovery of 1,3,6-nts at wells Az-65D, Az-04 and Az-28, 279 days after injection when sampling was halted, were, respectively, 6.1%, 0.90% y 0.16%, for a total of 7.61%. We concluded that these quantities constitute the lower boundaries for the respective recovery factors. When sampling was halted, wells Az-65D, Az-66D and Az-30 were still producing some SF{sub 6} at lower rates, and the rest of the wells were no longer recording the gas phase tracer. The total recovery of SF{sub 6} at wells Az-65D, Az-04, Az-41, Az-30, Az-28 and Az-66D were, respectively, 4.82 e-02%, 1.37 e-03%, 1.48 e-03%, 6.38 e-04%, 1.38 e-03% y 4.31 e-04%, for a total of 5.35 e-02%. The liquid recharge occurred in orders of magnitude greater than the steam. [Spanish] Se efectuaron dos pruebas simultaneas en la zona Maritaro-La Cumbre del campo geotermico de Los Azufres, Mich., Mexico. Los objetivos de estas pruebas fueron determinar si la salmuera de desecho inyectada en el pozo Az-15 recarga las zonas de alimentacion de seis pozos productores designados por CFE, y estimar que fraccion de lo inyectado recarga dichos pozos productores. Debido a que solo tres de los pozos

Atmospheric scintillation at Dome C, Antarctica: implications for photometry and astrometry

Science.gov (United States)

Kenyon, S.; Lawrence, J.; Ashley, M. C. B.; Storey, J. W. V.; Tokovinin, A.; Fossat, E.

2006-08-01

Night-time turbulence profiles of the atmosphere above Dome C, Antarctica, were measured during 2004, using a MASS instrument. We compare this data with turbulence profiles above Cerro Tololo and Cerro Pachon, also measured with a MASS, and find, with the exception of the owest layer, that Dome C has significantly less turbulence. In addition, the integrated at turbulence 16 km above Dome C is always less than the median values at the two Chilean sites. Using average wind speed profiles, we assess the photometric noise produced by scintillation, and the atmospheric contribution to the error budget in narrow angle differential astrometry. In comparison with the two mid-latitude sites in Chile, Dome C offers a potential gain of about 3.6 in both photometric precision (for long integrations) and narrow-angle astrometry precision. Although the data from Dome C cover a fairly limited time frame, they lend strong support to expectations that Dome C will offer significant advantages for photometric and astrometric studies.

A new Miocene baleen whale from Peru deciphers the dawn of cetotheriids

Science.gov (United States)

Marx, Felix G.; Lambert, Olivier; de Muizon, Christian

2017-09-01

Cetotheriidae are an iconic, nearly extinct family of baleen whales (Mysticeti) with a highly distinct cranial morphology. Their origins remain a mystery, with even the most archaic species showing a variety of characteristic features. Here, we describe a new species of archaic cetotheriid, Tiucetus rosae, from the Miocene of Peru. The new material represents the first mysticete from the poorly explored lowest portion of the highly fossiliferous Pisco Formation (allomember P0), and appears to form part of a more archaic assemblage than observed at the well-known localities of Cerro Colorado, Cerro los Quesos, Sud-Sacaco and Aguada de Lomas. Tiucetus resembles basal plicogulans (crown Mysticeti excluding right whales), such as Diorocetus and Parietobalaena, but shares with cetotheriids a distinct morphology of the auditory region, including the presence of an enlarged paroccipital concavity. The distinctive morphology of Tiucetus firmly places Cetotheriidae in the context of the poorly understood `cetotheres' sensu lato, and helps to resolve basal relationships within crown Mysticeti.

Water quality of springs and water wells which are used in human consumption, in the Jocotitlan volcano region at State of Mexico; Calidad del agua de manantiales y pozos que se utilizan para consumo humano, en la region del volcan Jocotitlan, Estado de Mexico

Energy Technology Data Exchange (ETDEWEB)

Baca G, A.; Segovia, N.; Iturbe, J.L. [Instituto Nacional de Investigaciones Nucleares, A.P. 18-1027, 11801 Mexico D.F. (Mexico); Martinez, V. [CIRA, UAEM, Unidad San Cayetabo, Toluca-Ixtlahuaca (Mexico); Armienta, M.A. [IGFUNAM, C. Universitaria, Mexico D.F. (Mexico); Seidel, J.L. [CNRS, Univ. Montpellier (France)

1998-07-01

In this work are presented the results of water quality of seven springs (San Antonio Enchisi, Las Fuentes, El Cerro, Pasteje, Los Reyes, Santa Cruz and Tiacaque) and two water wells (Jocotitlan No. 2 and La Providencia No. 35) which are used for human consumption and that are located surrounding area to Jocotitlan volcano, state of Mexico. It was determined the {sup 222} Rn concentration through liquid scintillation, the {sup 226} Ra by Gamma spectroscopy, the physical-chemical parameters (major elements) and bacteriological, using standardized methods. The minor elements and trace in solution were determined by Icp-Ms mass spectroscopy. The water quality was established in function of the standing standards. Therefore Las Fuentes, El Cerro, Santa Cruz, Tiacaque springs and the Jocotitlan No. 2 well, are drinkable water. So, Pasteje, Los Reyes, San Antonio Enchisi springs and the La Providencia No. 35 well are chemically drinkable but presenting bacteriological pollution. (Author)

Diosas de la montaña, espíritus tutelares, seres con máscaras vegetales y chamanes sobre árboles en el arte rupestre levantino español (Sureste de la Península Ibérica

Directory of Open Access Journals (Sweden)

Juan Francisco JORDÁN MONTÉS

2009-12-01

Full Text Available RESUMEN: Propuestas de interpretación, desde perspectivas antropológicas, para algunas escenas del arte rupestre levantino español, en la estaciones rupestres de Solana de las Covachas (Nerpio, Cerro Barbatón (Letur, El Milano (Mula, Peña Rubia (Cehegín, Minateda (Hellín, cueva de la Vieja (Alpera y Alcaine (Teruel. Se destaca la probable narración de mitos en los que participaban diosas de las montañas y chamanes.RÉSUMÉ: Propositions d'interprétation, du point de vue des perspectives anthropologiques, pour quelques scènes de Tart rupestre du Levant Espagnol, dans les station rupestres de Solana de las Covachas (Nerpio, Cerro Barbatón (Letur, el Milano (Mula, Peña Rubia (Cehegín, Minateda (Hellín, CUeva de la Vieja (Alpera et Alcaine (Teruel. Il se détache la narration probable de mythes ou participaient des déesses de la montagne et des chamans.

Machines and Metaphors

Directory of Open Access Journals (Sweden)

Ángel Martínez García-Posada

2016-10-01

Full Text Available The edition La ley del reloj. Arquitectura, máquinas y cultura moderna (Cátedra, Madrid, 2016 registers the useful paradox of the analogy between architecture and technique. Its author, the architect Eduardo Prieto, also a philosopher, professor and writer, acknowledges the obvious distance from machines to buildings, so great that it can only be solved using strange comparisons, since architecture does not move nor are the machines habitable, however throughout the book, from the origin of the metaphor of the machine, with clarity in his essay and enlightening erudition, he points out with certainty some concomitances of high interest, drawing throughout history a beautiful cartography of the fruitful encounter between organics and mechanics.

Estimation of the electric potential at Los Humeros, Puebla, Mexico; Estimacion del potencial electrico del yacimiento de los Humeros, Puebla, Mexico

Energy Technology Data Exchange (ETDEWEB)

Morales Solano, Nora Blanca [Comision Federal de Electricidad, Perote, Veracruz (Mexico)

2000-12-01

The evaluation of the electric potential of geothermal reservoir allows us to estimate the stored energy and the maximum power that could be installed at determined time. The method that was employed for the evaluation is that gradual pressure depletion of the reservoir. It consists of decompressing the system until an abandonment pressure or predetermined time of exploitation is reached. Results indicate that it is possible to generate more than 250 MW during 20 years. [Spanish] La evaluacion del potencial electrico del yacimiento geotermico permite estimar la energia recuperable y la potencia maxima que se puede instalar en un tiempo determinado. El metodo que se empleo para la evaluacion es el de descompresion gradual del yacimiento, que consiste en despresurizar el sistema hasta llegar a una presion de abandono de explotacion predeterminado, y calcular cual es la maxima potencia electrica del yacimiento bajo tales condiciones. El resultado indica que en Los Humeros es posible generar mas de 250 MW durante 20 anos.

Geochemical evidences of the boiling phenomena in Los Humeros geothermal field; Evidencias geoquimicas del fenomeno de ebullicion en el campo de Los Humeros

Energy Technology Data Exchange (ETDEWEB)

Munguia Bracamontes, Fernando; Lopez Mendiola, Juan Manuel [Instituto de Investigaciones Electricas, Cuernavaca (Mexico)

1990-12-31

The geochemical behavior of the fluids in the geothermal field Los Humeros suggests the existence of a reservoir of relatively low permeability, with hydrostatic pressure gradients and thermodynamic conditions of pressure-temperature close to the boiling point in stationary conditions, that is, non-disturbed. Nevertheless, the fluid geochemistry also indicates the presence of steam under stationary conditions, mainly in the fault, fracture, fissure, etc. zones. The steam diminishes progressively as the extraction time increases, being replaced by boiling fluid. [Espanol] El comportamiento geoquimico de los fluidos en el campo geotermico de Los Humeros sugiere la existencia de un yacimiento de relativa baja permeabilidad, con gradientes de presion hidrostatica y condiciones termodinamicas de presion-temperatura cercanas al punto de ebullicion a condiciones estables; es decir, no perturbadas. Sin embargo, la geoquimica de los fluidos tambien indica la existencia de vapor bajo condiciones estables, principalmente en las zonas de fallas, fracturas, fisuras, etc. El vapor disminuye progresivamente conforme aumenta el tiempo de extraccion, siendo reemplazado por fluido en ebullicion.

Geochemical evidences of the boiling phenomena in Los Humeros geothermal field; Evidencias geoquimicas del fenomeno de ebullicion en el campo de Los Humeros

Energy Technology Data Exchange (ETDEWEB)

Munguia Bracamontes, Fernando; Lopez Mendiola, Juan Manuel [Instituto de Investigaciones Electricas, Cuernavaca (Mexico)

1989-12-31

The geochemical behavior of the fluids in the geothermal field Los Humeros suggests the existence of a reservoir of relatively low permeability, with hydrostatic pressure gradients and thermodynamic conditions of pressure-temperature close to the boiling point in stationary conditions, that is, non-disturbed. Nevertheless, the fluid geochemistry also indicates the presence of steam under stationary conditions, mainly in the fault, fracture, fissure, etc. zones. The steam diminishes progressively as the extraction time increases, being replaced by boiling fluid. [Espanol] El comportamiento geoquimico de los fluidos en el campo geotermico de Los Humeros sugiere la existencia de un yacimiento de relativa baja permeabilidad, con gradientes de presion hidrostatica y condiciones termodinamicas de presion-temperatura cercanas al punto de ebullicion a condiciones estables; es decir, no perturbadas. Sin embargo, la geoquimica de los fluidos tambien indica la existencia de vapor bajo condiciones estables, principalmente en las zonas de fallas, fracturas, fisuras, etc. El vapor disminuye progresivamente conforme aumenta el tiempo de extraccion, siendo reemplazado por fluido en ebullicion.

77 FR 21485 - Final Flood Elevation Determinations

Science.gov (United States)

2012-04-10

..., Milwaukee, St. Paul and Pacific Railroad. Clear Creek At the confluence with + 1180 City of Clear Lake... City of Mason City, upstream of Chicago, Unincorporated Areas of Milwaukee, St. Paul and Cerro Gordo... at the Chariton County Courthouse, 306 South Cherry Street, Keytesville, MO 65261. Village of Dalton...

Residential metal contamination and potential health risks of exposure in adobe brick houses in Potosí, Bolivia

Science.gov (United States)

Potosí, Bolivia, is the site of centuries of historic and present-day mining of the Cerro Rico Mountain, known for its rich polymetallic deposits, and was the site of large-scale Colonial era silver refining operations, both of which have left a legacy of pollution. In this study...

Inventario y estado de conservación de puya raimondii (bromeliaceae) en el departamento de moquegua, Perú

NARCIS (Netherlands)

Montesinos, D.B.

2014-01-01

El presente estudio recopilatorio informa de la existencia de Puya raimondii Harms (Bromeliaceae) en cinco localidades de la provincia General Sánchez Cerro, departamento de Moquegua, Perú, donde se han reportado 6040 ejemplares de la especie. Se establece el estado actual de conservación de cada

Geology and stratigraphy of the sheet 3246-II Miramar, Costa Rica; Geologia y estratigrafia de la hoja 3246-II Miramar, Costa Rica

Energy Technology Data Exchange (ETDEWEB)

Zacek, Vladimir; Vorel, Tomas; Kycl, Petr; Mixa, Petr; Havlicek, Pavel; Cech, Stanislav; Hrazdira, Petr; Metelka, Vaclav; Sevcik, Josef [Czech Geological Survey (Servicio Geologico Checo, CGS), Klarov 3 CZ-118 21 Praha 1 (Czech Republic); Huapaya, Sofia [MINAET, Direccion de Geologia y Minas, Apdo. 10104, San Jose (Costa Rica); Grygar, Radek [VSB - Technical University of Ostrova, 17, listopadu 15 CZ-708 33 Ostrava-Poruba, (Czech Republic); Pecskay, Zoltan [Inst. on Nuclear Research of the Hungarian Academy of Science, H-4001 Debrecen, P.O. Box 51 (Hungary)

2012-07-15

The oldest rocks of the Miramar sheet are represented by sediments of the Formacion Punta Carballo (Miocene), which are exposed at the SW of the sheet. However, volcanic rocks of the older Grupo Aguacate (Miocene-Pliocene) and overlying Formacion Monterverde (Lower Pleistocene) have dominated in the map area. The Pliocene of Pleistocene silicic ignimbrites and Quaternary sediments are subordinated in minor surface. New K-Ar ages yielded 4,41{+-}0,15 and 4,99{+-}0,36 Ma for the Grupo Aguacate and 1,77{+-}0,11 and 1,71{+-}0,22 Ma for the Formacion Monteverde. Gabrodioritic stock was newly mapped in the Grupo Aguacate accompanying numerous other intrusive bodies of variable composition and is described for the first time in this work. New K-Ar ages were obtained for the rhyodacitic domes; 1,71{+-}0,14 Ma for the cerro La Cruz Dome and 1,59{+-}0,12 Ma for the cerro San Miguel Dome. Definition of volcanic units is based on detailed petrography, XRD, microprobe and 33 new bulk-rock chemical analyses. (author) [Spanish] Las rocas mas antiguas de la hoja Miramar estan conformadas por los sedimentos de la Formacion Punta Carballo del Mioceno que afloran al SO de la hoja. Sin embargo, las vulcanitas del Grupo Aguacate (Mioceno-Plioceno) sobreyacidas por vulcanitas de la Formacion Monteverde (Pleistoceno Inferior), han representado la mayor extension del mapa. Las ignimbritas silicicas del Plioceno hasta Pleistoceno y sedimientos del Cuaternario se han encontrado en menor superficie. Nuevas dataciones con el metodo K-Ar han establecido edades de 4,41{+-}0,15 y 4,99{+-}0,36 Ma para el Grupo Aguacate y de 1,77{+-}0,11 y 1,71{+-}0,22 Ma para la Formacion Monteverde. El Grupo de Aguacate tambien esta conformado por una serie de cuerpos intrusivos de composicion variable, entre ellos un stock gabrodioritico que fue recien mapeado y es descrito por primera vez con este trabajo. Nuevas dataciones K-Ar se han hecho del domo riodacitico cerro La Cruz, cuya edad fue datada en 1

Confirmation of 5 SN in the Kepler/K2 C16 Field with Gemini

Science.gov (United States)

Margheim, S.; Tucker, B. E.; Garnavich, P. M.; Rest, A.; Narayan, G.; Smith, K. W.; Smartt, S.; Kasen, D.; Shaya, E.; Mushotzky, R.; Olling, R.; Villar, A.; Forster, F.; Zenteno, A.; James, D.; Smith, R. Chris

2018-01-01

We report new spectroscopic classifications by KEGS of supernova discovered by Pan-STARRS1 during a targeted search of the Kepler/K2 Campaign 16 field using the Gemini Multi-Object Spectrograph (GMOS) on both the Gemini North Observatory on Mauna Kea, and the Gemini South Observatory on Cerro Pachon.

Study with liquid and steam tracers at the Tejamaniles area, Los Azufres, Mich., geothermal field; Estudio con trazadores de liquido y vapor en el area Tejamaniles del campo geotermico de Los Azufres, Mich.

Energy Technology Data Exchange (ETDEWEB)

Iglesias, Eduardo R. [Instituto de Investigaciones Electricas, Gerencia de Geotermia, Cuernavaca, Morelos (Mexico)]. E-mail: iglesias@iie.org.mx; Flores Armenta, Magaly [Comision Federal de Electricidad, Gerencia de Proyectos Geotermoelectricos, Morelia, Michoacan (Mexico); Torres, Rodolfo J. [Instituto de Investigaciones Electricas, Gerencia de Geotermia, Cuernavaca, Morelos (Mexico); Ramirez Montes, Miguel [Comision Federal de Electricidad, Gerencia de Proyectos Geotermoelectricos, Morelia, Michoacan (Mexico); Reyes Picasso, Neftali [Instituto de Investigaciones Electricas, Gerencia de Geotermia, Cuernavaca, Morelos (Mexico); Reyes Delgado, Lisette [Comision Federal de Electricidad, Gerencia de Proyectos Geotermoelectricos, Morelia, Michoacan (Mexico)

2011-01-15

monitored producing wells, and (ii) there is vertical permeability in the reservoir area between the distances mentioned. The vertical flow implies the injected fluid, relatively cold (about 40 degrees Celsius), is heated sufficiently to flow upward by convection, thus preventing, or at least slowing down, thermal interference. Results suggest the recovery of steam generated by injection into Az-08 generally tends to decrease exponentially with the horizontal distance of the studied wells to the injector, and with the vertical distance between the injection area and the corresponding production areas. [Spanish] La Comision Federal de Electricidad (CFE) inyecta salmueras producidas por pozos de la zona en el pozo Az-08, localizado en el area Tejamaniles, al suroeste del campo geotermico de Los Azufres, Mich. Los objetivos principales de este estudio son: determinar si el fluido inyectado recarga nueve pozos productores del area y, si esto ocurre, estimar que fraccion del fluido inyectado recarga a cada pozo productor. Cinco de los pozos seleccionados producen mezcla; el resto produce solo vapor. Por esta razon se diseno este estudio con inyeccion simultanea de trazadores de liquido y de vapor. Los nueve pozos productores seleccionados detectaron el trazador de vapor, y los cinco pozos que producen mezcla detectaron el trazador de fase liquida. Las curvas de residencia de ambos trazadores presentan series de picos que reflejan la conocida naturaleza fracturada de este yacimiento. Los resultados demuestran que las areas de alimentacion de los nueve pozos seleccionados son recargadas por el fluido inyectado en el pozo Az-08. Conviene aclarar que al momento de preparar este trabajo se habia completado el arribo del trazador de vapor en todos los pozos, pero los pozos que producen mezcla continuaban registrando arribo del trazador de liquido. Hasta 407 dias despues de la inyeccion de los trazadores, el porcentaje total de recuperacion del trazador de fase liquida en los cinco

E-ELT Site Chosen - World's Biggest Eye on the Sky to be Located on Armazones, Chile

Science.gov (United States)

2010-04-01

On 26 April 2010, the ESO Council selected Cerro Armazones as the baseline site for the planned 42-metre European Extremely Large Telescope (E-ELT). Cerro Armazones is a mountain at an altitude of 3060 metres in the central part of Chile's Atacama Desert, some 130 kilometres south of the town of Antofagasta and about 20 kilometres from Cerro Paranal, home of ESO's Very Large Telescope. "This is an important milestone that allows us to finalise the baseline design of this very ambitious project, which will vastly advance astronomical knowledge," says Tim de Zeeuw, ESO's Director General. "I thank the site selection team for the tremendous work they have done over the past few years." ESO's next step is to build a European extremely large optical/infrared telescope (E-ELT) with a primary mirror 42 metres in diameter. The E-ELT will be "the world's biggest eye on the sky" - the only such telescope in the world. ESO is drawing up detailed construction plans together with the community. The E-ELT will address many of the most pressing unsolved questions in astronomy, and may, eventually, revolutionise our perception of the Universe, much as Galileo's telescope did 400 years ago. The final go-ahead for construction is expected at the end of 2010, with the start of operations planned for 2018. The decision on the E-ELT site was taken by the ESO Council, which is the governing body of the Organisation composed of representatives of ESO's fourteen Member States, and is based on an extensive comparative meteorological investigation, which lasted several years. The majority of the data collected during the site selection campaigns will be made public in the course of the year 2010. Various factors needed to be considered in the site selection process. Obviously the "astronomical quality" of the atmosphere, for instance, the number of clear nights, the amount of water vapour, and the "stability" of the atmosphere (also known as seeing) played a crucial role. But other

JPRS Report: Environmental Issues

Science.gov (United States)

1993-06-16

tiful River Is Now Languishing"] emergency measures and drastic action comparable to the shutting down of the sawmills." [Text] Rancho Arriba , Cerros...Murmansk POLYARNA YA ZVEZDA such a large fine insufficient in order to make it neces- in Russian 5 Mar 93 p 2 sary to think before doing? [Lobov] Alas

Application of SPCALC for chemical and thermodynamic speciation of fluids -example for wells LV-4A, LV-11 and LV-13, Las Tres Virgenes geothermal field, BCS; Aplicacion del SPCALC en la especiacion quimica y termodinamica de fluidos: ejemplo del caso de los pozos LV-4A, LV-11 y LV-13, del campo geotermico de Las Tres Virgenes, BCS

Energy Technology Data Exchange (ETDEWEB)

Viggiano Guerra, J.C.; Sandoval Medina, F.; Flores Armenta, M.C. [Comision Federal de Electricidad, Gerencia de Proyectos Geotermoelectricos, Morelia, Michoacan (Mexico)]. E-mail: fernando.sandoval@cfe.gob.mx, E-mail: magaly.flores@cfe.gob.mx; Perez, R.J. [Universidad de Calgary (Canada); Gonzalez Partida, E. [Universidad Nacional Autonoma de Mexico, Centro de Geociencias, Mexico, D.F. (Mexico)

2009-01-15

+ CO{sub 2}) if boiling occurs or is induced, for instance, by flashing. Reactions occurring during the process produce the rest of the observed minerals in rocks (illite+quartz{+-}epidote), although the balance diagrams do not truly represent the process due to the just-mentioned explanation. On the other hand the oversaturated phases, according to SPCALC, are mainly silica varieties (from quartz to chalcedony), a prediction that is confirmed by the silica scaling occurring at superficial installations. Calcite, on the contrary, is reported as unsaturated, an apparent contradiction with reality, which shows problematic calcite scaling produced during the well exploitation according to the same just-mentioned mechanism. It is therefore recommended to adjust the SPCALC calculations at the reservoir level to be able to prevent imminent calcite scaling. Chemical and multi-phase speciation by using SPCALC results are useful and practical, if results are interpreted carefully. [Spanish] El SPCALC es un excelente software recientemente adquirido por la Comision Federal de Electricidad (CFE) a traves de un contrato con la Universidad Nacional Autonoma de Mexico (UNAM) y la universidad de Calgary, Canada, mediante el cual se obtiene la especiacion quimica y multifasica de fluidos geotermicos. La metodologia consiste en el calculo de variables termodinamicas, tales como las actividades (a) y las fugacidades (f) de las especies quimicas, asi como los indices de saturacion (log Q/K) de las fases minerales del yacimiento, lo que implica que modela condiciones termodinamicas de yacimiento (pH entre otras cosas) contribuyendo asi a pronosticar incrustaciones y corrosion dado que tambien simula la tasa de corrosion de los fluidos. En este articulo se modelan fluidos que han percolado a traves de rocas granodioriticas cretacicas de los pozos LV-4A, LV-11 y LV-13 del campo geotermico de Las Tres Virgenes, BCS, haciendo uso del software mencionado a partir de sus analisis quimicos. Asi

Thickness of the oligo-neogene sedimentary cover in the Central Depression, northern Chile (Pampa del Tamarugal, 20°45'-21°30'S), based on seismic reflection

Science.gov (United States)

Garcia, M.; Simicic, Y.; Contreras Reyes, E.; Charrier, R.

2013-12-01

The estimation of the Pampa de Tamarugal oligo-neogene sedimentary cover thickness from seismic interpretation is crucial for scientific and applied subjects, such as placing aquifers traps and Mesozoic-Paleogene basement top location for mining exploration drilling. The Chilean National Petroleum Company (ENAP) has explored hydrocarbon resources in the area, raising several reflection seismic lines and drilling some wells. Previous studies used the paper seismic data by determining the cover geometry and defining the basement-cover boundary. We have obtained directly SGY digital files, which allow a better definition and modeling of stratigraphy and cover thickness. This thickness was estimated by the travel time in the seismic reflection lines and the value of the p-wave propagation velocity (0.91 to 1.97 km/s for cover). The last value was obtained by density measurements of field samples, which resulted from 1,895 to 2,065 g/cm3. In the central-south part of the Pampa del Tamarugal, immediately south of Cerro Challacollo, the west-east-oriented 99_7 seismic line shows a 'basement high' whose top is at 100 m from the surface. The basement was uplift by a north-trend west-verging reverse fault and separates two sub-basins of 9.5 km and 13.8 km wide, and maximum cover thicknesses of 600 and 850 m, west and east respectively. To the north of Cerro Challacollo, the subparallel 99_6 line shows a similar geometry, and increasing the depth of the basement high top up to 350 m in the central part of the section. For seismic lines south of Cerro Challacollo, the basement high disappears and the cover thickness increases. To improve the accuracy of the cover thickness estimations, we will test directly measurements of p-wave propagation velocity in field samples of basement and cover (instead of approximations from the density measurements).

A paleolimnological perspective on industrial-era metal pollution in the central Andes, Peru.

Science.gov (United States)

Cooke, Colin A; Abbott, Mark B

2008-04-15

To date, few studies have investigated the environmental legacy associated with industrialization in the South American Andes. Here, we present an environmental archive of industrial pollution from (210)Pb-dated lake cores recovered from Laguna Chipian, located near the Cerro de Pasco metallurgical region and Laguna Pirhuacocha, located near the Morococha mining region and the La Oroya smelting complex. At Laguna Chipian, trace metal concentrations increase beginning ~1900 AD, coincident with the construction of the central Peruvian railway, and the rapid industrial development of the Cerro de Pasco region. Trace metal concentrations and fluxes peak during the 1950s before subsequently declining up-core (though remaining well above background levels). While Colonial mining and smelting operations are known to have occurred at Cerro de Pasco since at least 1630 AD, our sediment record preserves no associated metal deposition. Based on our (14)C and (210)Pb data, we suggest that this is due to a depositional hiatus, rather than a lack of regional Colonial pollution. At Laguna Pirhuacocha, industrial trace metal deposition first begins ~1925 AD, rapidly increasing after ~1950 AD and peaking during either the 1970s or 1990s. Trace metal concentrations from these lakes are comparable to some of the most polluted lakes in North America and Europe. There appears to be little diagenetic alteration of the trace metal record at either lake, the exception being arsenic (As) accumulation at Laguna Pirhuacocha. There, a correlation between As and the redox-sensitive element manganese (Mn) suggests that the sedimentary As burden is undergoing diagenetic migration towards the sediment-water interface. This mobility has contributed to surface sediment As concentrations in excess of 1100 microg g(-1). The results presented here chronicle a rapidly changing Andean environment, and highlight a need for future research in the rate and magnitude of atmospheric metal pollution.

A paleolimnological perspective on industrial-era metal pollution in the central Andes, Peru

International Nuclear Information System (INIS)

Cooke, Colin A.; Abbott, Mark B.

2008-01-01

To date, few studies have investigated the environmental legacy associated with industrialization in the South American Andes. Here, we present an environmental archive of industrial pollution from 210 Pb-dated lake cores recovered from Laguna Chipian, located near the Cerro de Pasco metallurgical region and Laguna Pirhuacocha, located near the Morococha mining region and the La Oroya smelting complex. At Laguna Chipian, trace metal concentrations increase beginning ∼ 1900 AD, coincident with the construction of the central Peruvian railway, and the rapid industrial development of the Cerro de Pasco region. Trace metal concentrations and fluxes peak during the 1950s before subsequently declining up-core (though remaining well above background levels). While Colonial mining and smelting operations are known to have occurred at Cerro de Pasco since at least 1630 AD, our sediment record preserves no associated metal deposition. Based on our 14 C and 210 Pb data, we suggest that this is due to a depositional hiatus, rather than a lack of regional Colonial pollution. At Laguna Pirhuacocha, industrial trace metal deposition first begins ∼ 1925 AD, rapidly increasing after ∼ 1950 AD and peaking during either the 1970s or 1990s. Trace metal concentrations from these lakes are comparable to some of the most polluted lakes in North America and Europe. There appears to be little diagenetic alteration of the trace metal record at either lake, the exception being arsenic (As) accumulation at Laguna Pirhuacocha. There, a correlation between As and the redox-sensitive element manganese (Mn) suggests that the sedimentary As burden is undergoing diagenetic migration towards the sediment-water interface. This mobility has contributed to surface sediment As concentrations in excess of 1100 μg g -1 . The results presented here chronicle a rapidly changing Andean environment, and highlight a need for future research in the rate and magnitude of atmospheric metal pollution

Goldmining, dispossessing the commons and multi-scalar responses

NARCIS (Netherlands)

Stoltenborg, Didi; Boelens, Rutgerd

2017-01-01

In 1996, Minera San Xavier (MSX), a Mexican tributary of the Canadian mining company Newgold Inc., announced it wanted to start a large open-pit gold and silver mine in the municipality of Cerro de San Pedro, in the state of San Luis Potosí. The mining site occupies 373 hectares of ejido 2

Tololo and Tourism | CTIO

Science.gov (United States)

Program PIA Program GO-FAAR Program Other Opportunities Tourism Visits to Tololo Astro tourism in Chile Tourism in Chile Information for travelers Visit Tololo Media Relations News Press Release Publications ‹› You are here CTIO Home » Outreach » Tololo and Tourism Tololo and Tourism Visits to Cerro

Conversaciones sobre el litoral cordillerano

OpenAIRE

Browne,Enrique; Browne,Tomás

2009-01-01

Dos arquitectos dialogan sobre los Andes desde su propia vivencia. El territorio de Chile se entiende como límite natural entre mar y cordillera, donde suceden apretadamente una serie de eventos particulares: fallas geológicas, cerros que penetran en las ciudades y torrentes que bajan al mar caracterizan y diferencian sus paisajes.

Determination of Barium and selected rare-earth elements in geological materials employing a HpGe detector by radioisotope excited x-ray fluorescence

International Nuclear Information System (INIS)

LaBrecque, J.J.; Preiss, I.L.

1984-01-01

The laterite material (geological) from Cerro Impacto was first studied by air radiometric techniques in the 1970's and was found to have an abnormally high radioactive background. Further studies showed this deposit to be rich in thorium, columbium, barium and rare-earth elements (mostly La, Ce, Pr and Nd). A similar work has been reported for the analysis of Brazil's lateritic material from Morro do Ferro to determine elemental compositions (including barium and rare-earth elements) and its relationship to the mobilization of thorium from the deposit using a Co-57 radioisotope source. The objective of this work was to develop an analytical method to determine barium and rare-earth element present in Venezuelan lateritic material from Cerro Impacto. We have employed a method before, employing a Si(Li) detector, but due to the low detection efficiencies in the rare-earth K-lines region (about 30 KeV - 40 KeV), we have decided to study the improvement in sensitivities and detection limits using an hyperpure germanium detector

Dos casas en el cerro Pochoco: Lo Barnechea, Chile

OpenAIRE

Carreño, Mario; Sartori, Piera

2009-01-01

A partir de la remodelación de una vivienda, se generan dos casas superpuestas que comparten el mismo volumen y una torre-terraza asomada a un cajón cordillerano en la periferia de la ciudad de Santiago. La dimensión vertical de la montaña aparece en los interiores, orientados hacia el suelo inmediato y las vistas lejanas. Starting with the renovation of a dwelling, two superimposed houses are generated that share the same volume, a tower-terrace leaning out of a mountain valley in the out...

Mining inventory of Uruguay: Uranium report of synthesis annexes GQE

International Nuclear Information System (INIS)

1984-01-01

This report is about place, analysis and radiometric results in Amarillo, Acegua, Alborada,Arbolito,Caraguata,Centurion,Cerro de las Cuentas, Cuchilla de Ombu, Fraile Muerto, Las Flores, Lechiguana, Melo, Moirones, La Paloma de Durazno,Paso Mazangano, Paso del Minuano, Paso Pereira, Paso del Puerto, Paso San Diego, Polanco, Porrua, Sierra de los Rios, Tacuari, Vichadero, MoironesZanja Honda

VizieR Online Data Catalog: Hα and [NII] survey in local 11 Mpc (Kennicutt+, 2008)

Science.gov (United States)

Kennicutt, R. C. Jr; Lee, J. C.; Funes, J. G.; Sakai, S.; Akiyama, S.

2009-11-01

Most of the Hα and R imaging reported in this paper was obtained in 2001-2004 using CCD direct imagers on the Steward Observatory Bok 2.3m telescope on Kitt Peak (Bok), the Lennon 1.8m Vatican Advanced Technology Telescope (VATT), and the 0.9m telescope at Cerro Tololo Interamerican Observatory (CTIO). (3 data files).

Considerations ages of rocks analyzed at the Institute of Geosciences - University of Sao Paulo - Brazil

International Nuclear Information System (INIS)

Medina, E.

1990-01-01

This work is about the radimetric studies with the proposal to determine the age of the rocks. The rocks selected were from different places of Uruguay such as Mahoma-Guaycuru, Cerros Negros y Paso Lugo - Arroyo el Minero. The data obtained allow determine their structure as well as the location of new area with this kind of rock

Additions to the reptile fauna of Paraguay with notes on a small herpetological collection from Amambay

Science.gov (United States)

McDiarmid, Roy W.; Foster, Mercedes S.

1987-01-01

Specimens in a small collections of reptiles and amphibians from Parque Nacional Cerro Cora, Departamento Amambay, Paraguay are reported. Included are the first records of Bachia bresslaui, Phrynops gibbus, and Ololygon fuscomarginata for that country. Brief notes on morphology, distribution, and natural history of species collected are included. The systematic status of Phrynops tuberculatus vanderhaegei is evaluated.

Discovery of Ten ASAS-SN Supernovae

Science.gov (United States)

Nicholls, B.; Brimacombe, J.; Kiyota, S.; Stone, G.; Cruz, I.; Trappett, D.; Vallely, P.; Stanek, K. Z.; Kochanek, C. S.; Brown, J. S.; Shields, J.; Thompson, T. A.; Shappee, B. J.; Holoien, T. W.-S.; Prieto, J. L.; Bersier, D.; Dong, Subo; Bose, S.; Chen, Ping; Stritzinger, M.; Holmbo, S.

2018-03-01

During the ongoing All Sky Automated Survey for SuperNovae (ASAS-SN, Shappee et al. 2014), using data from the quadruple 14-cm "Brutus" telescope in Haleakala, Hawaii, the "Leavitt" telescope in Fort Davis, Texas, the "Payne-Gaposchkin" telescope in Sutherland, South Africa, and the "Cassius" and "Paczynski" telescopes in Cerro Tololo, Chile, we discovered several new transient sources.

Discovery of 11 ASAS-SN Supernovae

Science.gov (United States)

Brimacombe, J.; Fernandez, J. M.; Stone, G.; Vallely, P.; Stanek, K. Z.; Kochanek, C. S.; Brown, J. S.; Shields, J.; Thompson, T. A.; Shappee, B. J.; Holoien, T. W.-S.; Prieto, J. L.; Bersier, D.; Dong, Subo; Bose, S.; Chen, Ping; Stritzinger, M.; Holmbo, S.; Nicholls, B.

2018-04-01

During the ongoing All Sky Automated Survey for SuperNovae (ASAS-SN, Shappee et al. 2014), using data from the quadruple 14-cm "Brutus" telescope in Haleakala, Hawaii, the "Leavitt" telescope in Fort Davis, Texas, the "Payne-Gaposchkin" telescope in Sutherland, South Africa, and the "Cassius" and "Paczynski" telescopes in Cerro Tololo, Chile, we discovered several new transient sources.

Espacios cohabitados: Proposiciones sobre la ambigüedad espacial de Valparaíso

Directory of Open Access Journals (Sweden)

Claudio Astudillo

2011-12-01

El siguiente artículo intenta explicar la incidencia que tiene la autoconstrucción de la vivienda en las diversas relaciones cotidianas de la ciudad que llegan a constituir nuevas formas de cohabitación ambiguas pero complejas, basándose en los resultados de una investigación experiencial en el Cerro Cordillera titulada "la casa inacabada".

Violencia intrafamiliar en un área de salud Intrafamily violence in a health area

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Annia Duany Navarro

2005-04-01

Full Text Available Se realizó un estudio exploratorio y descriptivo, en el cual a través de una selección por conglomerado bietápico, se escogieron 3 consultorios del Médico de Familia, y en cada uno, 50 familias con residencia permanente en el Consejo Popular Cerro. Nos propusimos explorar la frecuencia y características de la violencia intrafamiliar (VIF en un área de salud del municipio Cerro, así como su posible influencia en el funcionamiento familiar. Mediante entrevista domiciliaria se conversó con un miembro adulto de cada familia y con el Médico de Familia, con el propósito de identificar la presencia de VIF, la(s víctima(s, los victimarios, y la relación de la VIF con el funcionamiento familiar y con la presencia de afecciones psiquiátricas en la familia. Como resultados se percibió VIF en el 24 % de las familias, siendo el tipo psicológico la más frecuente (58,6 %, y como víctimas, las mujeres. No se detectó abuso sexual ni se encontró relación entre el funcionamiento familiar y la VIF, aunque en las pocas familias disfuncionales encontradas hubo violencia. Se concluye que en el área de salud existe VIF, a pesar de que la comunidad no la reconoce como uno de sus problemas de salud.An exploratory and descriptive study was undertaken. Three family physician's oficces were selected by bistage cluster and, in each of them, 50 families with permanent residence in the Cerro People's Council. Our purpose was to explore the frequency and characteristics of intrafamily violence (IFV in a health area of Cerro municipality and their possible influence on family functioning. An adult member of every family and the family physician were interviewed at home aimed at identifying the presence of IFV, the victims, the victimaries and the connection of IFV with family functioning and with the existance of psychiatric affections in the family. IFV was observed in 24 % of the families. The psychological type was the most frequent (58,6 %, and women

Volcanoes of México: An Interactive CD-ROM From the Smithsonian's Global Volcanism Program

Science.gov (United States)

Siebert, L.; Kimberly, P.; Calvin, C.; Luhr, J. F.; Kysar, G.

2002-12-01

The Smithsonian Institution's Global Volcanism Program is nearing completion of an interactive CD-ROM, the Volcanoes of México. This CD is the second in a series sponsored by the U.S. Department of Energy Office of Geothermal Technologies to collate Smithsonian data on Quaternary volcanism as a resource for the geothermal community. It also has utility for those concerned with volcanic hazard and risk mitgation as well as an educational tool for those interested in Mexican volcanism. We acknowledge the significant contributions of many Mexican volcanologists to the eruption reports, data, and images contained in this CD, in particular those contributions of the Centro Nacional de Prevencion de Desastres (CENAPRED), the Colima Volcano Observatory of the University of Colima, and the Universidad Nacional Autónoma de México (UNAM). The Volcanoes of México CD has a format similar to that of an earlier Smithsonian CD, the Volcanoes of Indonesia, but also shows Pleistocene volcanic centers and additional data on geothermal sites. A clickable map of México shows both Holocene and Pleistocene volcanic centers and provides access to individual pages on 67 volcanoes ranging from Cerro Prieto in Baja California to Tacaná on the Guatemalan border. These include geographic and geologic data on individual volcanoes (as well as a brief paragraph summarizing the geologic history) along with tabular eruption chronologies, eruptive characteristics, and eruptive volumes, when known. Volcano data are accessible from both geographical and alphabetical searches. A major component of the CD is more than 400 digitized images illustrating the morphology of volcanic centers and eruption processes and deposits, providing a dramatic visual primer to the country's volcanoes. Images of specific eruptions can be directly linked to from the eruption chronology tables. The Volcanoes of México CD includes monthly reports and associated figures and tables cataloging volcanic activity in M�

The evolution of shallow crustal structures in early rift-transform interaction: a case study in the northern Gulf of California.

Science.gov (United States)

Farangitakis, Georgios-Pavlos; van Hunen, Jeroen; Kalnins, Lara M.; Persaud, Patricia; McCaffrey, Kenneth J. W.

2017-04-01

The Gulf of California represents a young oblique rift/transtensional plate boundary in which all of the transform faults are actively shearing the crust, separated by active rift segments. Previous workers have shown that in the northern Gulf of California, the relative plate motion between the Pacific and North American plates is distributed between: a) the Cerro Prieto Fault (CPF) in the NE b) the Ballenas Transform Fault (BTF) in the SW and c) a pull-apart structure located between these two faults consisting of a number of extensional basins (the Wagner, Consag, and Upper and Lower Delfin basins). A plate boundary relocation at approximately 2 Ma, continued to separate Isla Angel de la Guarda from the Baja California peninsula and created the 200x70 km2 NE-SW pull-apart structure located northeast of the BTF. Here we use seismic stratigraphy analysis of the UL9905 high resolution reflection seismic dataset acquired by the Lamont-Doherty Earth Observatory, Caltech, and the Centro de Investigación Científica y de Educación Superior de Ensenada to build on previous structural interpretations and seek to further understand the processes that formed the structural and sedimentary architecture of the pull-apart basin in the northern Gulf of California. We examine the formation of depositional and deformation structures in relation to the regional tectonics to provide insight into the development of structural patterns and related seismic-stratigraphic features in young rift-transform interactions. Using bathymetric data, characteristic seismic-stratigraphic packages, and seismic evidence of faulting, we confirm the existence of three major structural domains in the northern Gulf of California and examine the interaction of the seismic stratigraphy and tectonic processes in each zone. The first and most distinctive is an abrupt NE-SW 28x5 km2 depression on the seabed of the Lower Delfin Basin. This is aligned orthogonally to the BTF, is situated at its northern

222 Rn determination and physicochemical characteristic and biological in aquifers in the Toluca Valley

International Nuclear Information System (INIS)

Hernandez A, A.

1998-01-01

Concentration levels of 222 Rn and 226 Rn have been analyzed in water samples from boreholes belonging to the drinking water supply system around Toluca, Mexico. The 222 Rn source is the decay of 226 Rn within the solid matrix of the aquifer. The study was performed during the dry and rainy seasons. 222 Rn concentration was determined by the liquid scintillation technique, 226 Rn was determined by gamma spectrometry, the physicochemical parameters and bacteriological analysis were performed by conventional chemical techniques. Solubilized trace elements were determined by Inductively Coupled Plasma - Mass Spectrometry (Icp-Ms). The radon level fluctuations at the boreholes in Toluca city and Almoloya spring indicated differences in the radon content. At borehole Lodos Prietos 2, the temperature and radon level were systematically the highest in comparison with the other boreholes and the spring indicating a contribution of a regional flow to the water of this particular borehole. The result for 226 Rn, the average 222 Rn observed during the sampling period, no correspondence occurs between the radium and the radon content indicating that, radon is not supported by radium, but is incorporated into the water through fissures in the rocks in contact with the water. The radon levels obtained in house faucets which water is supplied by boreholes decrease as a function of the distance from the source borehole to the house. With the chemical composition of each one of the studied boreholes and spring a Piper diagram was draw indicating the kind of water. The boreholes and spring can be classified as bicarbonate calcium/magnesium. Almost no fluctuation on time was observed in the chemical species and trace elements only a slight increase was observed at the end of the rain season. At Almoloya, spring pollution with coliform bacteria and nitrates showed an anthropogenic contribution to the water deterioration probable and fertilizers and detritus. Most of the studied water

{sup 222} Rn determination and physicochemical characteristic and biological in aquifers in the Toluca Valley; Determinacion de {sup 222} Rn y caracteristicas fisicoquimicas y biologicas en acuiferos del Valle de Toluca

Energy Technology Data Exchange (ETDEWEB)

Hernandez A, A

1998-10-01

Concentration levels of {sup 222} Rn and {sup 226} Rn have been analyzed in water samples from boreholes belonging to the drinking water supply system around Toluca, Mexico. The {sup 222} Rn source is the decay of {sup 226} Rn within the solid matrix of the aquifer. The study was performed during the dry and rainy seasons. {sup 222} Rn concentration was determined by the liquid scintillation technique, {sup 226} Rn was determined by gamma spectrometry, the physicochemical parameters and bacteriological analysis were performed by conventional chemical techniques. Solubilized trace elements were determined by Inductively Coupled Plasma - Mass Spectrometry (Icp-Ms). The radon level fluctuations at the boreholes in Toluca city and Almoloya spring indicated differences in the radon content. At borehole Lodos Prietos 2, the temperature and radon level were systematically the highest in comparison with the other boreholes and the spring indicating a contribution of a regional flow to the water of this particular borehole. The result for {sup 226} Rn, the average {sup 222} Rn observed during the sampling period, no correspondence occurs between the radium and the radon content indicating that, radon is not supported by radium, but is incorporated into the water through fissures in the rocks in contact with the water. The radon levels obtained in house faucets which water is supplied by boreholes decrease as a function of the distance from the source borehole to the house. With the chemical composition of each one of the studied boreholes and spring a Piper diagram was draw indicating the kind of water. The boreholes and spring can be classified as bicarbonate calcium/magnesium. Almost no fluctuation on time was observed in the chemical species and trace elements only a slight increase was observed at the end of the rain season. At Almoloya, spring pollution with coliform bacteria and nitrates showed an anthropogenic contribution to the water deterioration probable and

Nem Florida, nem Boedo: assegura o 'escritor fracassado' de Roberto Arlt

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Adriana de Borges Gomes

2017-06-01

Full Text Available Florida e Boedo são nomes de ruas da cidade de Buenos Aires, com características distintas bem expressivas: Florida era a rua do “ócio distraído”, da boemia da arte gratuita, sem motivações que não fossem estéticas. Boedo era a rua do “tráfego fabril”, situada num bairro onde muitas fábricas estavam instaladas, o que fomentava a agitação das consciências para o levante de uma bandeira subversiva. Das designações topográficas do bairrismo portenho nasceu uma contenda cultural de classes, em que a literatura foi o veio central. A polêmica literária deve ser vista no seu interior, recorrendo-se ao momento histórico em que ocorreu, pois somente com a distância temporal o historiador da literatura pode avaliar o que representou na época e o que significa na contemporaneidade tal controvérsia para a história da literatura argentina. E, ainda assim, manter certa desconfiança, pois o historiador é um pesquisador que muitas vezes recorta acontecimentos e os dota de significado de acordo com suas ideologias; como chama a atenção o historiador da literatura latino-americana Antonio Cornejo Polar (2000. Na conformação dos dois grupos e na localização dos escritores em cada um deles, houve muitas discrepâncias. Castelnuovo, nos diz Adolfo Prieto (2009, declarou que o grupo Boedo não existiu, o que existia era uma literatura de arrabalde. Assim, Prieto mapeia em seu ensaio “Boedo e Florida” algumas esclarecimentos e tentativas de encaixar os escritores em um grupo ou outro. Em uma dessas demonstrações está claro que Roberto Arlt não se localizava em nenhum dos dois grupos.

Renuncia a los gananciales y opción a porción conyugal

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Mabel Rasines del Campo

2015-10-01

Full Text Available Ponencia presentada en el marco de la XXXIII Jornada Notarial Uruguaya "Prof. Esc. María Emilia Gleiss". celebrada del 30 de octubre al 10 de noviembre de 1992 en la ciudad de Melo, Opto. de Cerro LargoContenido: Porción conyugal. Renuncia de gananciales. Abandono de bienes y porciónconyugal. Conclusiones

Diversidad Florística de la cuenca alta del rio Tambo-Ichuña, Moquegua, Perú

NARCIS (Netherlands)

Montesinos, D.B.

2011-01-01

La diversidad florística de plantas vasculares es estudiada en la cuenca del río Tambo-Ichuña, la puna y bofedales altoandinos en los distritos de Ichuña, Ubinas y Yunga (3400 – 4700 m de altitud), provincia General Sánchez Cerro, departamento de Moquegua, Perú. La flora vascular de esta región está

Lista anotada de nuevas adiciones para la flora andina de Moquegua, Perú

NARCIS (Netherlands)

Montesinos, D.B.

2012-01-01

Se presentan nuevos registros de 103 especies reunidas en 79 géneros y 33 familias para la flora del norte de la cuenca alta del Río Tambo-Ichuña, en la Provincia General Sánchez Cerro en el Departamento de Moque-gua. Con esto la flora de la región andina del norte de Moquegua se eleva a 507

ASASSN-18gq: Discovery of A Low-Luminosity Transient Towards Very Nearby ( 3.4 Mpc) Galaxy ESO 325- G?011

Science.gov (United States)

Nicholls, B.; Brimacombe, J.; Vallely, P.; Dong, Subo; Stanek, K. Z.; Kochanek, C. S.; Brown, J. S.; Shields, J.; Thompson, T. A.; Shappee, B. J.; Holoien, T. W.-S.; Prieto, J. L.; Bersier, D.; Bose, S.; Chen, Ping; Stritzinger, M.; Holmbo, S.

2018-04-01

During the ongoing All Sky Automated Survey for SuperNovae (ASAS-SN, Shappee et al. 2014), using data from the quadruple 14-cm "Payne-Gaposchkin" telescope in Sutherland, South Africa, and the quadruple 14-cm "Cassius" and "Paczynski" telescopes in Cerro Tololo, Chile, we discovered a new transient source, most likely a supernova, in the low surface brightness galaxy ESO 325- G?011.

Preselección de especies para la piscicultura marina en el Pacífico Sur de México

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Sergio Escárcega Rodríguez

2018-01-01

Full Text Available Dada la diversidad de peces en el Pacífico Sur de México y el deterioro que enfrenta más de 50% de las pesquerías que en él existen, se requiere identificar a las especies con los mayores atributos acuícolas para promover su conservación y el desarrollo regional. Se analizaron 36 especies sobre tres precondiciones básicas: valor comercial, eurihalinidad y talla. Resultaron como especies de primera elección: el robalo prieto (Centropomus nigrescens, el mero (Epinephelus itajara y el guachinango del Pacífico (Lutjanus peru. La pesca constituye la mayor fuente de impacto ecológico en los océanos. La piscicultura marina tropical representa una vertiente productiva a impulsarse en México.

Variational principles for locally variational forms

International Nuclear Information System (INIS)

Brajercik, J.; Krupka, D.

2005-01-01

We present the theory of higher order local variational principles in fibered manifolds, in which the fundamental global concept is a locally variational dynamical form. Any two Lepage forms, defining a local variational principle for this form, differ on intersection of their domains, by a variationally trivial form. In this sense, but in a different geometric setting, the local variational principles satisfy analogous properties as the variational functionals of the Chern-Simons type. The resulting theory of extremals and symmetries extends the first order theories of the Lagrange-Souriau form, presented by Grigore and Popp, and closed equivalents of the first order Euler-Lagrange forms of Hakova and Krupkova. Conceptually, our approach differs from Prieto, who uses the Poincare-Cartan forms, which do not have higher order global analogues

Room temperature isotherms for Mo and Ni

International Nuclear Information System (INIS)

Masse, J.L.

1986-11-01

Isotherms at room temperature for Mo and Ni are proposed. They are of three types: BIRCH, KEANE and BORN-MIE. The adjustable constants appearing in these isotherms have been determined from experimental quantities at zero pressure. An evaluation of the limit of (δB T /δP) T as P #-> # ∞, where B T is the isothermal bulk modulus, has been also used. These three isotherms obtained for Mo and Ni are compared with isotherms derived from shock-wave data according to the PRIETO's model. There is a good agreement between these and these derived from shock-wave data. The three isotherms proposed for Mo and Ni can be considered as valid until pressures of several B To , where B To is the bulk modulus B T at P = o [fr

The writing and the voice in three Grail novels

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Demétrio Alves Paz

2014-07-01

Full Text Available The objetive of this paper is to analyse the narrator and the characters in the romances of chivalry about the Grail: Perceval, by Chrétien de Troyes; Parsifal, by Wolfram von Eschenbach and A Demanda do Santo Graal, an anonymous portuguese text. After analysing the prodution context of these works, it is used the ideas of Paul Zumthor and Walter Benjamim about the relation of orality and writing to discuss the narrator of the novels. Then, the characters are investigated according to the typology proposed by Antonio Prieto. The first two romances of chivalry about the Grail are closer not only to the orality as well as the myth, whereas in the portuguese text there is a greater control of the narrative due to its religious characteristic.

Boletín bibliográfico

Directory of Open Access Journals (Sweden)

Facultad de Medicina Revista

1941-07-01

Full Text Available Parasitosis intestinales, por el doctor Fidel Fernández. Un volumen en cuarto menor de 134 páginas. Salvat Editores, S. A. Barcelona- Buenos Aires. 1940. Doctor Alvarez Herrera. - Tanatología forense. - "Manuales de Medicina Práctica" Salvat Editores, S. A. 1940. Dr. F. Gallart Monés: Ocho lesiones clínicas.- Quinta serie. Un tomo de 212 páginas y 110 fgs. Editorial Salvat. 1939. Enfermedades piogenas y parasitarias de la piel. Por el doctor José Gay Prieto catedrático numerario de Dermatología y Sifilografia de la Universidad de Granada, médico de la Lucha Oficial Antivenérea. - Un volumen de 187 pags. Salvat Editores, S. A", Barcelona, Buenos Aires, 1940. "Manuales de Medicina práctica".

La Formación Los Llantenes en la Precordillera de Jagüé (La Rioja y la identificación de un episodio de extensión en la evolución temprana de las cuencas del Paleozoico superior en el oeste argentino The Los Llantenes Formation in the Precordillera of Jagüé (La Rioja Province and the recognition of a rifting stage in the early evolution of the late Paleozoic basins in western Argentina

Directory of Open Access Journals (Sweden)

Ricardo A Astini

2011-07-01

Full Text Available En la región septentrional de la Precordillera, al NW de La Rioja, en el centro occidental de Argentina, afloran más de 4.000 m de rocas sedimentarias del Paleozoico superior entre las que se destaca una unidad basal psefítica, no descrita con anterioridad y cuyo análisis permite identificar un importante episodio de extensión cortical. El potente conglomerado (>1.000 m de color morado, que proponemos denominar Formación Los Llantenes, se dispone en no concordancia sobre el basamento de la Precordillera Septentrional y por debajo del primer nivel con clara impronta glacigénica, asociado a la glaciación gondwánica. Mientras que su gran espesor y escasa distribución areal indican subsidencia localizada, la estratofábrica cruda, la mala selección granulométrica y la presencia de bloques superiores al metro indicarían que se trata de depósitos de abanicos aluviales de alto gradiente, dominados por flujos de gravedad. Su composición y granulometría gruesa revelan procedencia local, resaltos topográficos pronunciados y fuerte compartimen-tación paleogeográfica. Una compleja historia glacial sucede a la Formación Los Llantenes sobre la que se han labrado profundos paleovalles en forma de 'U' que alojan tilitas y diamictitas glacigénicas, pertenecientes a la Formación Cerro Tres Cóndores de edad viseana (Misisipiano Medio. La edad de los conglomerados de la Formación Los Llantenes, de naturaleza preglacial, quedaría acotada entre el sustrato del Devónico Medio, aflorante inmediatamente al sur de la región estudiada en sierra de Las Minitas, y el Misisipiano Medio (Formación Cerro Tres Cóndores, pudiendo parcialmente constituir un equivalente de la Formación Agua de Lucho (Tournaisiano-Viseano que, en la región del Río del Peñón, también subyace a los niveles glacigénicos de la Formación Cerro Tres Cóndores. La expresión cartográfica con limitada extensión areal y el gran espesor que presentan las psefitas de la

Protección civil, población, vulnerabilidad y riesgo en Santiago Miltepec, Toluca

Directory of Open Access Journals (Sweden)

Alejandra Toscana Aparicio

2012-02-01

Full Text Available El objetivo fue analizar la forma en que el nivel de gobierno municipal actúa frente a los “pequeños desastres” asociados a fenómenos naturales, entendiendo por “pequeños desastres” aquéllos que impactan en la escala local pero sus consecuencias no trascienden del ámbito municipal. Se toma como punto de partida el evento ocurrido el 30 de junio de 2006 en la delegación Santiago Miltepec de la ciudad de Toluca, Estado de México, en el que durante una intensa precipitación pluvial, grandes bloques de roca se desprendieron de las laderas del cerro El Barrigón y rodaron hasta el piedemonte del cerro afectando algunas de las viviendas ahí construidas. Este caso, como otros similares, permite observar el distanciamiento que existe entre la población y el Sistema Nacional de Protección Civil en sus diferentes niveles organizativos, así como el distanciamiento entre las diferentes instancias gubernamentales que inciden en la organización del territorio y en la prevención de desastres.

The X-ray globular cluster NGC 1851

CERN Document Server

Alcaino, G

1976-01-01

A BV photometric investigation of the Southern Globular Cluster NGC 1851, was carried out using the 1 m telescope of Cerro La Silla (ESO) for the photoelectric work and the 1 m telescope of Cerro Las Campanas (CARSO) for the photographic work. Nineteen stars were observed photoelectrically, the limiting magnitude being V=16.18. Using this sequence, 156 stars were measured photographically. The derived apparent distance modulus is (m-M)/sub app/=15/sup m/.50. The reddening is E(B-V)=0/sup m/.10. The true distance modulus is (m-M) /sub 0/=15/sup m/.20. The distance is 11 kpc from the sun, 6 kpc from the galactic plane and 17 kpc from the galactic centre. The main features of the colour-magnitude diagram are: a well defined horizontal branch abundant in red stars and deficient in blue stars, a rich subgiant and asymptotic branch and a moderately populated red giant branch of medium steepness rising to Delta V=2/sup m/.5 at (B-V) /sub 0/=1.4. At the distance of 11 kpc the maximum observed luminosity of the X-ray ...

Serum immunoreactive erythropoietin in high altitude natives with and without excessive erythrocytosis.

Science.gov (United States)

León-Velarde, F; Monge, C C; Vidal, A; Carcagno, M; Criscuolo, M; Bozzini, C E

1991-05-01

We report the estimation of blood hemoglobin (Hb), arterial blood oxygen saturation (SaO2), and serum immunoreactive erythropoietin (siEPO) in a group of Peruvian workers residing in Cerro de Pasco at 4300 m showing "excessive erythrocytosis" (EE, Monge's disease, chronic mountain sickness). These estimates were compared with those of humans residing either in Cerro de Pasco and showing "normal erythrocytosis" (NE) or in Lima (sea level, SL) to determine whether Hb and SaO2 are related to siEPO in high altitude (HA) natives with NE or EE. The three parameters showed statistically significant differences between HA and SL groups--the values in SL being lower. Significant differences were also found between NE and EE groups in Hb and SaO2. There was no statistical difference in siEPo between the two groups. The results indicate, therefore, that HA residents who develop EE are not distinguishable from residents who develop NE on the basis of estimates of siEPO. As a result, siEPO and Hb do not show a dose-response relationship in HA residents, and variation in EPO does not explain the striking variation in Hb at high altitudes.

Neoproterozoic diamictite-cap carbonate succession and δ13C chemostratigraphy from eastern Sonora, Mexico

Science.gov (United States)

Corsetti, Frank A.; Stewart, John H.; Hagadorn, James W.

2007-01-01

Despite the occurrence of Neoproterozoic strata throughout the southwestern U.S. and Sonora, Mexico, glacial units overlain by enigmatic cap carbonates have not been well-documented south of Death Valley, California. Here, we describe in detail the first glaciogenic diamictite and cap carbonate succession from Mexico, found in the Cerro Las Bolas Group. The diamictite is exposed near Sahuaripa, Sonora, and is overlain by a 5 m thick very finely-laminated dolostone with soft sediment folds. Carbon isotopic chemostratigraphy of the finely-laminated dolostone reveals a negative δ13C anomaly (down to − 3.2‰ PDB) characteristic of cap carbonates worldwide. Carbon isotopic values rise to + 10‰ across ∼ 400 m of section in overlying carbonates of the Mina el Mezquite and Monteso Formations. The pattern recorded here is mostly characteristic of post-Sturtian (ca. ≤ 700 Ma), but pre-Marinoan (ca. ≥ 635 Ma) time. However, the Cerro Las Bolas Group shares ambiguity common to most Neoproterozoic successions: it lacks useful radiometric age constraints and biostratigraphically useful fossils, and its δ13C signature is oscillatory and therefore somewhat equivocal.

Astrometry of the Orcus/Vanth occultation on UT 7 March 2017

Science.gov (United States)

Bosh, Amanda S.; Zuluaga, Carlos; Levine, Stephen; Sickafoose, Amanda A.; Genade, Anja; Schindler, Karsten; Lister, Tim; Person, Michael J.

2017-10-01

On UT 7 March 2017, Orcus was predicted to occult a star with m=14.3. Observations were made at five observatories: the 0.6-m Astronomical Telescope of the University of Stuttgart (ATUS) at Sierra Remote Observatories (SRO), California; Las Cumbres Observatory’s 1-m telescope (ELP) at McDonald Observatory, Fort Davis, Texas; NASA’s 3-m InfraRed Telescope Facility (IRTF) on Mauna Kea, Hawaii; the 4.1-m Southern Astrophysical Research telescope (SOAR) on Cerro Pachón, Chile; and the 0.6-m Southeastern Association for Research in Astronomy telescope (SARA-CT) at Cerro Tololo, Chile. While observations at all sites were successful, only two—ELP and IRTF—observed solid-body occultation signatures. We will discuss the various predictions for this event and the reasons for the differences among them, including an offset of 130 mas for the star position from the position in the Gaia catalog. The sum of the positive and negative detections place constraints on the geometry of the Orcus/Vanth system, and we present our astrometric results for the geometric solution for this occultation. The implications of the light curve analyses are presented by Sickafoose et al., this conference.

Guaviare: Reencontrando Espacios e Identidades (pág. 216-223

Directory of Open Access Journals (Sweden)

Cristian Alexis Gil Ruiz

2010-07-01

Full Text Available La riqueza colombiana está en las selvas, claro, la faunística y florística que enluce a nuestro querido país, a continuación les mostraré rasgos de esa riqueza encontrada en el departamento del Guaviare, más exactamente en la vereda cerro azul, en un sitio llamado Cerro pinturas y que es un patrimonio cultural y arqueológico del departamento, espacios como hay en muchos escenarios de Colombia , que es un país hermoso, con varios sitios que no se han visitado, y que son dignos de ver, es triste que como estudiantes, como docentes en formación y más que todo, como colombianos, nos estemos perdiendo estas oportunidades. Además de ello debe entenderse al docente como un sujeto no sólo educativo, también es un sujeto con vocación social, política y cultural y que sea como sea, es un ciudadano y nunca dejara de serlo, así que como docentes es nuestro deber apropiarnos de sitios como éste y educar para que sean admirados, protegidos y sobre todo respetados.

Waste-to-Energy Plant Environmental Assessment, Dyess Air Force Base, Texas

Science.gov (United States)

2011-09-01

Integrated Material Management Plan IWMP Integrated Waste Management Plan MACT Maximum Achievable Control Technology MRL Minimum Risk Level MRR...Education, Cerro Coso College, CA, 1994 Years of Experience: 15 Kevin J. Peter, Program Manager B.A., Anthropology, Pomona College, CA, 1975 M.A...hazardous wastes would occur with selection of any proposed action alternative. Under the no-action alternative, existing procedures for the management

Good Seeing: Best Practices for Sustainable Operations at the Air Force Maui Optical and Supercomputing Site

Science.gov (United States)

2016-01-01

wavelengths. Gemini North is the northern hemisphere component of a dual-telescope observatory. Gemini South is an identical telescope in Chile , which means...funds and support are being applied disproportionately towards the Cerro-Tololo Interamerican Observatory (CTIO) in Chile , which is seen by some at...constructing and operating observatories on ecologically and culturally sensitive lands. Interviews conducted via phone with NOAO personnel, July 18

ASAS-SN Discovery of ASASSN-18dw, a 4+ Magnitudes Stellar Outburst Towards Orion

Science.gov (United States)

Stanek, K. Z.; Kochanek, C. S.; Shields, J. V.; Thompson, T. A.; Shappee, B. J.; Holoien, T. W.-S.; Prieto, J. L.; Dong, Subo; Stritzinger, M.

2018-02-01

During the ongoing All Sky Automated Survey for SuperNovae (ASAS-SN, Shappee et al. 2014), using data from the quadruple 14-cm "Leavitt" telescope in Fort Davis, Texas, the quadruple 14-cm "Payne-Gaposchkin" telescope in Sutherland, South Africa, and the quadruple 14-cm "Paczynski" telescope in Cerro Tololo, Chile, we detect a bright, rapidly raising transient source Object RA (J2000) DEC (J2000) Disc.

Selection of new drill sites using a Geographic Information System (GIS) at Los Azufres, Mexico; Seleccion de nuevos sitios de perforacion empleando un Sistema de Informacion Geografica (SIG) en Los Azufres, Mexico

Energy Technology Data Exchange (ETDEWEB)

Garcia-Estrada, G.H [Comision Federal de Electricidad, Morelia, Michoacan (Mexico)]. E-mail: gerardo.garcia04@cfe.gob.mx; Lopez-Hernandez, A [Facultad de Ingenieria Civil, Universidad Michoacana de San Nicolas de Hidalgo, Morelia (Mexico); Quijano Leon, J.L Cuauhtemoc [Comision Federal de Electricidad, Morelia, Michoacan (Mexico)

2008-07-15

con niveles de produccion de energia. Se usaron pesos relativos asignados por inspeccion visual para extender este conocimiento al total del area de exploracion. Se compararon diferentes criterios para calcular un indice geotermico que representa la produccion geotermica potencial de cada celda en las que se dividio el area estudiada. Tomando en cuenta la geometria de los planos de fallas a profundidades de 700 a 2000 m, asi como un zona de exclusion de 250 m alrededor de los pozos productores, se determinaron areas de indices geotermicos normalizados para proponer nuevos sitios de perforacion con diferentes niveles de riesgo, que van de pozos productores (riesgo bajo) a exploratorios (riesgo alto).

DECOMMISSIONING THE HIGH PRESSURE TRITIUM LABORATORY AT LOS ALAMOS NATIONAL LABORATORY

International Nuclear Information System (INIS)

Peifer, M.J.; Rendell, K.; Hearnsberger, D.W.

2003-01-01

In May 0f 2000, the Cerro Grande wild land fire burned approximately 48,000 acres in and around Los Alamos. In addition to the many buildings that were destroyed in the town site, many structures were also damaged and destroyed within the 43 square miles that comprise the Los Alamos National Laboratory (LANL). A special Act of Congress provided funding to remove Laboratory structures that were damaged by the fire, or that could be threatened by subsequent catastrophic wild land fires. The High Pressure Tritium Laboratory (HPTL) is located at Technical Area (TA) 33, building 86 in the far southeast corner of the Laboratory property. It is immediately adjacent to Bandelier National Park. Because it was threatened by both the Cerro Grande fire in 2000, and the 16,000- acre Dome fire in 1996, the former tritium processing facility was placed on the list of facilities scheduled for Decontamination and Decommissioning under the Cerro Grande Rehabilitation Project. The work was performed through the Facilities and Waste Operations (FWO) Division and is integrated with other Laboratory D and D efforts. The primary demolition contractor was Clauss Construction of San Diego, California. Earth Tech Global Environmental Services of San Antonio, Texas was sub-contracted to Clauss Construction, and provided radiological decontamination support to the project. Although the forty-seven year old facility had been in a state of safe-shutdown since operations ceased in 1990, a significant amount of tritium remained in the rooms where process systems were located. Tritium was the only radiological contaminant associated with this facility. Since no specific regulatory standards have been set for the release of volumetrically contaminated materials, concentration guidelines were derived in order to meet other established regulatory criteria. A tritium removal system was developed for this project with the goal of reducing the volume of tritium concentrated in the concrete of the

A paleolimnological perspective on industrial-era metal pollution in the central Andes, Peru

Energy Technology Data Exchange (ETDEWEB)

Cooke, Colin A. [Department of Geology, University of Pittsburgh, Pittsburgh, PA 15260 (United States); Earth and Atmospheric Sciences, University of Alberta, Edmonton, AB, T6G 2E3 (Canada)], E-mail: cacooke@ualberta.ca; Abbott, Mark B. [Earth and Atmospheric Sciences, University of Alberta, Edmonton, AB, T6G 2E3 (Canada); Section of Anthropology, Carnegie Museum of Natural History, Pittsburgh, PA 15206 (United States)

2008-04-15

To date, few studies have investigated the environmental legacy associated with industrialization in the South American Andes. Here, we present an environmental archive of industrial pollution from {sup 210}Pb-dated lake cores recovered from Laguna Chipian, located near the Cerro de Pasco metallurgical region and Laguna Pirhuacocha, located near the Morococha mining region and the La Oroya smelting complex. At Laguna Chipian, trace metal concentrations increase beginning {approx} 1900 AD, coincident with the construction of the central Peruvian railway, and the rapid industrial development of the Cerro de Pasco region. Trace metal concentrations and fluxes peak during the 1950s before subsequently declining up-core (though remaining well above background levels). While Colonial mining and smelting operations are known to have occurred at Cerro de Pasco since at least 1630 AD, our sediment record preserves no associated metal deposition. Based on our {sup 14}C and {sup 210}Pb data, we suggest that this is due to a depositional hiatus, rather than a lack of regional Colonial pollution. At Laguna Pirhuacocha, industrial trace metal deposition first begins {approx} 1925 AD, rapidly increasing after {approx} 1950 AD and peaking during either the 1970s or 1990s. Trace metal concentrations from these lakes are comparable to some of the most polluted lakes in North America and Europe. There appears to be little diagenetic alteration of the trace metal record at either lake, the exception being arsenic (As) accumulation at Laguna Pirhuacocha. There, a correlation between As and the redox-sensitive element manganese (Mn) suggests that the sedimentary As burden is undergoing diagenetic migration towards the sediment-water interface. This mobility has contributed to surface sediment As concentrations in excess of 1100 {mu}g g{sup -1}. The results presented here chronicle a rapidly changing Andean environment, and highlight a need for future research in the rate and magnitude

Discovery of 7 ASAS-SN Supernovae

Science.gov (United States)

Brimacombe, J.; Castro, N.; Clocchiatti, A.; Stone, G.; Nicholls, B.; Fernandez, J. M.; Cacella, P.; Vallely, P.; Stanek, K. Z.; Kochanek, C. S.; Brown, J. S.; Shields, J.; Thompson, T. A.; Shappee, B. J.; Holoien, T. W.-S.; Prieto, J. L.; Bersier, D.; Dong, Subo; Bose, S.; Chen, Ping; Stritzinger, M.; Holmbo, S.; Bock, G.

2018-06-01

During the ongoing All Sky Automated Survey for SuperNovae (ASAS-SN, Shappee et al. 2014), using data from the quadruple 14-cm "Brutus" telescope in Haleakala, Hawaii, the quadruple 14-cm "Leavitt" telescope in Fort Davis, Texas, the quadruple 14-cm "Payne-Gaposchkin" telescope in Sutherland, South Africa, and the quadruple 14-cm "Cassius" and "Paczynski" telescopes in Cerro Tololo, Chile, we discovered several new transient sources.

Discovery of 9 ASAS-SN Supernovae

Science.gov (United States)

Brimacombe, J.; Castro, N.; Clocchiatti, A.; Cacella, P.; Wiethoff, W.; Krannich, G.; Stone, G.; Kiyota, S.; Vallely, P.; Stanek, K. Z.; Kochanek, C. S.; Brown, J. S.; Shields, J.; Thompson, T. A.; Shappee, B. J.; Holoien, T. W.-S.; Prieto, J. L.; Bersier, D.; Dong, Subo; Bose, S.; Chen, Ping; Stritzinger, M.; Holmbo, S.; Bock, G.

2018-05-01

During the ongoing All Sky Automated Survey for SuperNovae (ASAS-SN, Shappee et al. 2014), using data from the quadruple 14-cm "Brutus" telescope in Haleakala, Hawaii, the quadruple 14-cm "Leavitt" telescope in Fort Davis, Texas, the quadruple 14-cm "Payne-Gaposchkin" telescope in Sutherland, South Africa, and the quadruple 14-cm "Cassius" and "Paczynski" telescopes in Cerro Tololo, Chile, we discovered several new transient sources.

Discovery of 8 ASAS-SN Supernovae

Science.gov (United States)

Brimacombe, J.; Kiyota, S.; Wiethoff, W.; Stone, G.; Vallely, P.; Stanek, K. Z.; Kochanek, C. S.; Brown, J. S.; Shields, J.; Thompson, T. A.; Shappee, B. J.; Holoien, T. W.-S.; Prieto, J. L.; Bersier, D.; Dong, Subo; Bose, S.; Chen, Ping; Stritzinger, M.; Holmbo, S.; Bock, G.

2018-06-01

During the ongoing All Sky Automated Survey for SuperNovae (ASAS-SN, Shappee et al. 2014), using data from the quadruple 14-cm "Brutus" telescope in Haleakala, Hawaii, the quadruple 14-cm "Leavitt" telescope in Fort Davis, Texas, the quadruple 14-cm "Payne-Gaposchkin" telescope in Sutherland, South Africa, and the quadruple 14-cm "Cassius" and "Paczynski" telescopes in Cerro Tololo, Chile, we discovered several new transient sources.

A sedimentological analysis of sediments corresponding to the San Gregorio Formation )Lower Permian), located in the eastern border of the North Uruguayan Basin, Sierra Guazunambi

International Nuclear Information System (INIS)

Goso Aguilar, C.; Gama, E.

1998-01-01

A sedimentological analysis of sediments corresponding to the San Gregorio Formation (Lower Permian), located in the eastern border of the Norte Uruguayan Basin, Sierra Guazunambi, Cerro Largo Departament was made. Facies analysis of about 100 otucrops fand more than 1.300 meters, in an area of 45 square kilometers showed diamictites rhytmites and massive sandstones, formed by gravitational sedimentary flows. Also present are prodelta mudrocks and deltaic front sandstones.(author)

Domestic Ritual and Identity in the Teotihuacan State: Exploring Regional Processes of Social Integration Through Ceramic Figurines

OpenAIRE

Hagerman, Kiri Louise

2018-01-01

Teotihuacan was a sprawling urban center that came to rule an eponymous expansive polity in the central Mexican highlands from approximately 200 to 600 CE. The conditions that facilitated its initial expansion, however, are not fully understood. This dissertation examines ceramic figurines from Teotihuacan and the three rural sites of Axotlan, Cerro Portezuelo, and Huixtoco in the Basin of Mexico to investigate ancient social relationships, cultural changes, and political transformations duri...

Discovery of Six ASAS-SN Supernovae

Science.gov (United States)

Brimacombe, J.; Stone, G.; Kiyota, S.; Vallely, P.; Stanek, K. Z.; Kochanek, C. S.; Brown, J. S.; Shields, J.; Thompson, T. A.; Shappee, B. J.; Holoien, T. W.-S.; Prieto, J. L.; Bersier, D.; Dong, Subo; Bose, S.; Chen, Ping; Stritzinger, M.; Holmbo, S.; Bock, G.; Cornect, R.

2018-02-01

During the ongoing All Sky Automated Survey for SuperNovae (ASAS-SN, Shappee et al. 2014), using data from the quadruple 14-cm "Brutus" telescope in Haleakala, Hawaii, the quadruple 14-cm "Leavitt" telescope in Fort Davis, Texas, the quadruple 14-cm "Payne-Gaposchkin" telescope in Sutherland, South Africa, and the quadruple 14-cm "Cassius" and "Paczynski" telescopes in Cerro Tololo, Chile, we discovered several new transient sources.

Discovery of 8 ASAS-SN Supernovae

Science.gov (United States)

Brimacombe, J.; Tomasella, Lina; Krannich, G.; Stone, G.; Vallely, P.; Stanek, K. Z.; Kochanek, C. S.; Brown, J. S.; Shields, J.; Thompson, T. A.; Shappee, B. J.; Holoien, T. W.-S.; Prieto, J. L.; Bersier, D.; Dong, Subo; Bose, S.; Chen, Ping; Stritzinger, M.; Holmbo, S.; Nicholls, B.; Cacella, P.; Kiyota, S.

2018-05-01

During the ongoing All Sky Automated Survey for SuperNovae (ASAS-SN, Shappee et al. 2014), using data from the quadruple 14-cm "Brutus" telescope in Haleakala, Hawaii, the quadruple 14-cm "Leavitt" telescope in Fort Davis, Texas, the quadruple 14-cm "Payne-Gaposchkin" telescope in Sutherland, South Africa, and the quadruple 14-cm "Cassius" and "Paczynski" telescopes in Cerro Tololo, Chile, we discovered several new transient sources.

Discovery of Eight ASAS-SN Supernovae

Science.gov (United States)

Stone, G.; Brimacombe, J.; Cacella, P.; Farfan, R. G.; Vallely, P.; Stanek, K. Z.; Kochanek, C. S.; Brown, J. S.; Shields, J.; Thompson, T. A.; Shappee, B. J.; Holoien, T. W.-S.; Prieto, J. L.; Bersier, D.; Dong, Subo; Bose, S.; Chen, Ping; Stritzinger, M.; Holmbo, S.; Trappett, D.

2018-02-01

During the ongoing All Sky Automated Survey for SuperNovae (ASAS-SN, Shappee et al. 2014), using data from the quadruple 14-cm "Brutus" telescope in Haleakala, Hawaii, the quadruple 14-cm "Leavitt" telescope in Fort Davis, Texas, the quadruple 14-cm "Payne-Gaposchkin" telescope in Sutherland, South Africa, and the quadruple 14-cm "Cassius" and "Paczynski" telescopes in Cerro Tololo, Chile, we discovered several new transient sources.

Discovery of Four ASAS-SN Supernovae

Science.gov (United States)

Brimacombe, J.; Kiyota, S.; Cruz, I.; Stone, G.; Vallely, P.; Stanek, K. Z.; Kochanek, C. S.; Brown, J. S.; Shields, J.; Thompson, T. A.; Shappee, B. J.; Holoien, T. W.-S.; Prieto, J. L.; Bersier, D.; Dong, Subo; Bose, S.; Chen, Ping; Stritzinger, M.; Holmbo, S.

2018-02-01

During the ongoing All Sky Automated Survey for SuperNovae (ASAS-SN, Shappee et al. 2014), using data from the quadruple 14-cm "Brutus" telescope in Haleakala, Hawaii, the quadruple 14-cm "Leavitt" telescope in Fort Davis, Texas, the quadruple 14-cm "Payne-Gaposchkin" telescope in Sutherland, South Africa, and the quadruple 14-cm "Cassius" and "Paczynski" telescopes in Cerro Tololo, Chile, we discovered several new transient sources.

Discovery of Six ASAS-SN Supernova Candidates

Science.gov (United States)

Brimacombe, J.; Stone, G.; Vallely, P.; Stanek, K. Z.; Brown, J. S.; Kochanek, C. S.; Shields, J.; Thompson, T. A.; Shappee, B. J.; Holoien, T. W.-S.; Prieto, J. L.; Bersier, D.; Dong, Subo; Bose, S.; Chen, Ping; Conseil, E.

2018-01-01

During the ongoing All Sky Automated Survey for SuperNovae (ASAS-SN, Shappee et al. 2014), using data from the quadruple 14-cm "Brutus" telescope in Haleakala, Hawaii, the quadruple 14-cm "Leavitt" telescope in Fort Davis, Texas, the quadruple 14-cm "Payne-Gaposchkin" telescope in Sutherland, South Africa, and the quadruple 14-cm "Cassius" and "Paczynski" telescopes in Cerro Tololo, Chile, we discovered several new transient sources.

Discovery of Nine ASAS-SN Supernovae

Science.gov (United States)

Cacella, P.; Brimacombe, J.; Fernandez, J. M.; Kiyota, S.; Krannich, G.; Koff, R. A.; Vallely, P.; Stanek, K. Z.; Kochanek, C. S.; Brown, J. S.; Shields, J.; Thompson, T. A.; Shappee, B. J.; Holoien, T. W.-S.; Prieto, J. L.; Bersier, D.; Dong, Subo; Bose, S.; Chen, Ping; Stritzinger, M.; Holmbo, S.; Aslan, L.; Bock, G.; Stone, G.

2018-01-01

During the ongoing All Sky Automated Survey for SuperNovae (ASAS-SN, Shappee et al. 2014), using data from the quadruple 14-cm "Brutus" telescope in Haleakala, Hawaii, the quadruple 14-cm "Leavitt" telescope in Fort Davis, Texas, the quadruple 14-cm "Payne-Gaposchkin" telescope in Sutherland, South Africa, and the quadruple 14-cm "Cassius" and "Paczynski" telescopes in Cerro Tololo, Chile, we discovered several new transient sources.

Discovery of Five ASAS-SN Supernovae

Science.gov (United States)

Brimacombe, J.; Stone, G.; Kiyota, S.; Vallely, P.; Stanek, K. Z.; Kochanek, C. S.; Brown, J. S.; Shields, J.; Thompson, T. A.; Shappee, B. J.; Holoien, T. W.-S.; Prieto, J. L.; Bersier, D.; Dong, Subo; Bose, S.; Chen, Ping; Stritzinger, M.; Holmbo, S.

2018-02-01

During the ongoing All Sky Automated Survey for SuperNovae (ASAS-SN, Shappee et al. 2014), using data from the quadruple 14-cm "Brutus" telescope in Haleakala, Hawaii, the quadruple 14-cm "Leavitt" telescope in Fort Davis, Texas, the quadruple 14-cm "Payne-Gaposchkin" telescope in Sutherland, South Africa, and the quadruple 14-cm "Cassius" and "Paczynski" telescopes in Cerro Tololo, Chile, we discovered several new transient sources.