Early Evolution of Earth's Geochemical Cycle and Biosphere: Implications for Mars Exobiology

Science.gov (United States)

DesMarais, David J.; Chang, Sherwood (Technical Monitor)

1997-01-01

Carbon (C) has played multiple key roles for life and its environment. C has formed organics, greenhouse gases, aquatic pH buffers, redox buffers, and magmatic constituents affecting plutonism and volcanism. These roles interacted across a network of reservoirs and processes known as the biogeochemical C cycle. Changes in the cycle over geologic time were driven by increasing solar luminosity, declining planetary heat flow, and continental and biological evolution. The early Archean C cycle was dominated by hydrothermal alteration of crustal rocks and by thermal emanations of CO2 and reduced species (eg., H2, Fe(2+) and sulfides). Bioorganic synthesis was achieved by nonphotosynthetic CO2-fixing bacteria (chemoautotrophs) and, possibly, bacteria (organotrophs) utilizing any available nonbiological organic C. Responding both to abundant solar energy and to a longterm decline in thermal sources of chemical energy and reducing power, the blaspheme first developed anoxygenic photosynthesis, then, ultimately, oxygenic photosynthesis. O2-photosynthesis played a central role in transforming the ancient environment and blaspheme to the modem world. The geochemical C cycles of early Earth and Mars were quite similar. The principal differences between the modem C cycles of these planets arose during the later evolution of their heat flows, crusts, atmospheres and, perhaps, their blasphemes.

Perfil. María Rodilla

OpenAIRE

Rodilla, María

2017-01-01

[ES] Perfil sobre María Rodilla, ilustradora valenciana que centra su trabajo en el feminismo Rodilla, M. (2017). Perfil. María Rodilla. EME Experimental Illustration, Art & Design. (5):52-53. doi:10.4995/eme.2017.7616. 52 53 5

Geochemical modelling baseline compositions of groundwater

DEFF Research Database (Denmark)

Postma, Diederik Jan; Kjøller, Claus; Andersen, Martin Søgaard

2008-01-01

and variations in water chemistry that are caused by large scale geochemical processes taking place at the timescale of thousands of years. The most important geochemical processes are ion exchange (Valreas and Aveiro) where freshwater solutes are displacing marine ions from the sediment surface, and carbonate......Reactive transport models, were developed to explore the evolution in groundwater chemistry along the flow path in three aquifers; the Triassic East Midland aquifer (UK), the Miocene aquifer at Valreas (F) and the Cretaceous aquifer near Aveiro (P). All three aquifers contain very old groundwaters...... dissolution (East Midlands, Valreas and Aveiro). Reactive transport models, employing the code PHREEQC, which included these geochemical processes and one-dimensional solute transport were able to duplicate the observed patterns in water quality. These models may provide a quantitative understanding...

Geochemical modelling of groundwater evolution and residence time at the Haestholmen site

Energy Technology Data Exchange (ETDEWEB)

Pitkaenen, P.; Luukkonen, A. [VTT Communities and Infrastructure, Espoo (Finland); Ruotsalainen, P. [Fintact Oy, Helsinki (Finland); Leino- Forsman, H.; Vuorinen, U. [VTT Chemical Technology, Espoo (Finland)

2001-01-01

An understanding of the geochemical evolution of groundwater is an essential part of the performance assessment and safety analysis of the geological final disposal of radioactive waste. The performance of technical barriers and migration of possibly released radionuclides depend on the geochemical conditions. A prerequisite for understanding these factors is the ability to specify the water-rock interactions that control chemical conditions in groundwater. The objective of this study is to interpret the processes and factors that control the hydrogeochemistry, such as pH and redox conditions. A model of the hydrogeochemical progress in different parts of the crystalline bedrock at Haestholmen has been created and the significance of geochemical reactions and groundwater mixing along different flow paths calculated. Long term hydrodynamics have also been evaluated. The interpretation and modelling are based on water samples (64 altogether) obtained from precipitation, the Baltic Sea, the soil layer, shallow wells in the bedrock, and 14 deep boreholes in the bedrock for which a comprehensive data set on dissolved chemical species and isotopes was available. Some analyses of dissolved gases and their isotopic measurements were also utilised. The data covers the bedrock at Haestholmen to a depth of 1000 m. The results from groundwater chemistry, isotopes, petrography, hydrogeology of the site, geomicrobial studies, and PCA and speciation calculations were used to evaluate evolutionary processes at the site. The geochemical interpretation of water-rock interaction, isotope-chemical evolution ({delta}{sup 13}C and {delta}{sup 34}S) and mixing of palaeo-water types were approached by mass-balance calculations (NETPATH). Reaction-path calculations (EQ3/6) were used to verify the thermodynamic feasibility of the reaction models obtained. The interpretation and calculation of hydrochemical data from Haestholmen suggest that changes in external conditions, such as glaciation

Geochemical evolution of groundwater in carbonate aquifers of southern Latium region, central Italy

Directory of Open Access Journals (Sweden)

Giuseppe Sappa

2013-03-01

Full Text Available Spring and well water samples, from carbonate aquifers of Latium region, have been characterized to determine the hydrochemical processes governing the evolution of the groundwater. Most of the spring samples, issuing from Lepini, Ausoni and Aurunci Mts., are characterized as alkaline earth HCO3 waters, however, some samples show a composition of Cl--SO4 -- alkaline earth waters. Groundwater samples from Pontina Plain shows three different hydrochemical facies: alkaline earth HCO3 type, Cl-- SO4 -- alkaline earth type and Cl--SO4 -- alkaline type waters. Geochemical modeling and saturation index computation of the sampled waters show an interaction with calcareous and calcareous-dolomitic lithologies. Most of the springs and wells was kinetically saturated with respect to calcite and dolomite, and all the samples were below the equilibrium state with gypsum. This indicates that the groundwater has capacity to dissolve the gypsum along the flow paths. The electrical conductivity and Cl- concentrations of the sampled waters show a positive trend with the decrease in the distance from the coast, highlighting seawater intrusion in the coastal area. According to hydrochemistry results and geochemical modeling, the dominant factors in controlling the hydrochemical characteristics of groundwater are: (i water rock interaction with calcareous and calcareous-dolomitic lithologies; (ii seawater intrusion in the coastal area; (iii dissolution and/or precipitation of carbonate and (i.e. dolomite and calcite evaporate minerals (gypsum determined by saturation indexes; (iv mineral weathering process; (the high Mg/Ca ratio due to the weathering of Mg-rich dolomite.

Retention/sorption and geochemical modelling

Energy Technology Data Exchange (ETDEWEB)

Arcos, D.; Grandia, F.; Domenech, C. [Enviros Spain, S.L., Barcelona (Spain); SCK-CEN, Mol (Belgium); Sellin, P. [SKB - Swedish Nuclear Fuel and Waste Management, SE, Stockholm (Sweden); Hunter, F.M.I.; Bate, F.; Heath, T.G.; Hoch, A. [Serco Assurance, Oxfordshire (United Kingdom); Werme, L.O. [SKB - Svensk Karnbranslehantering AB, Stockholm (Sweden); Bruggeman, C.; Maes, I.A.; Breynaert, E.; Vancluysen, J. [Leuven Katholieke Univ., Lab. for Colloid Chemistry (Belgium); Montavon, G.; Guo, Z. [Ecole des Mines, 44 - Nantes (France); Riebe, B.; Bunnenberg, C.; Meleshyn, A. [Leibniz Univ. Hannover, Zentrum fur Strahlenschutz und Radiookologie, Hannover (Germany); Dultz, S. [Leibniz Univ. Hannover, Institut fur Bodenkunde, Hannover (Germany)

2007-07-01

This session gathers 4 articles dealing with: the long-term geochemical evolution of the near field of a KBS-3 HLNW repository: insights from reactive transport modelling (D. Arcos, F. Grandia, C. Domenech, P. Sellin); the investigation of iron transport into bentonite from anaerobically corroding steel: a geochemical modelling study (F.M.I. Hunter, F. Bate, T.G. Heath, A. Hoch, L.O. Werme); SeO{sub 3}{sup 2-} adsorption on conditioned Na-illite: XAS spectroscopy, kinetics, surface complexation model and influence of compaction (C. Bruggeman, A. Maes, G. Montavon, E. Breynaert, Z. Guo, J. Vancluysen); the influence of temperature and gamma-irradiation on the anion sorption capacity of modified bentonites (B. Riebe, C. Bunnenberg, A. Meleshyn, S. Dultz)

Modelling of long term geochemical evolution and study of mechanical perturbation of bentonite buffer of a KBS-3 repository

Energy Technology Data Exchange (ETDEWEB)

Marsal, Francois; Pellegrini, Delphine; Deleruyelle, Frederic; Serres, Christophe (French Institute for Radiological Protection and Nuclear Safety (IRSN) (FR)); Windt, Laurent de (Paris School of Mines (ENSMP) (FR))

2008-03-15

The Swedish Nuclear Fuel and Waste Management Co. (SKB) has recently completed a safety assessment project named SR-Can, related to the KBS-3 disposal concept. In this concept, the waste packages are surrounded by a buffer made of either MX-80 or Deponit CA-N bentonite. Interactions between the buffer and groundwater may modify the buffer composition and thus its containment properties. The Swedish Radiation Protection Authorities (SSI) requested the French Institute for Radiological Protection and Nuclear Safety (IRSN) to perform the present study in support of SSI review of the SR-Can report. The purpose is to assess the geochemical evolution of both potential buffer materials due to the intrusion of different types of groundwater, with a similar modelling layout to that reported in SR-Can. Three main categories of water inflows via a fracture intersecting a deposition hole are considered: the Forsmark reference groundwater, a high-salinity groundwater to account for up-rise of deep-seated brines and a diluted water representing ice-melting derived groundwater. In addition to this, the redox buffering capacity of Deponit CA-N bentonite and the thermal effect on MX-80 bentonite geochemistry have been assessed. This modelling work has been performed using the reactive transport modelling code HYTEC. The main outcome of the present study is that the intrusion of the considered groundwaters should not affect drastically the geochemistry of neither the Deponit CA-N nor the MX-80 bentonite on the long-term (100,000 y). Bentonite pH may reach high values (up to 10.5) in some cases but does not reach SKB criterion value related to bentonite chemical stability. Dissolution-precipitation of accessory minerals is not significant enough to induce important porosity changes (rise by maximum 2 %). Globally, the montmorillonite exchanger undergoes Na by Ca partial replacement, which may decrease the swelling pressure of the bentonite. The simulated intrusion of oxidizing waters

Modelling of long term geochemical evolution and study of mechanical perturbation of bentonite buffer of a KBS-3 repository

International Nuclear Information System (INIS)

Marsal, Francois; Pellegrini, Delphine; Deleruyelle, Frederic; Serres, Chris tophe; Windt, Laurent de

2008-03-01

The Swedish Nuclear Fuel and Waste Management Co. (SKB) has recently completed a safety assessment project named SR-Can, related to the KBS-3 disposal concept. In this concept, the waste packages are surrounded by a buffer made of either MX-80 or Deponit CA-N bentonite. Interactions between the buffer and groundwater may modify the buffer composition and thus its containment properties. The Swedish Radiation Protection Authorities (SSI) requested the French Institute for Radiological Protection and Nuclear Safety (IRSN) to perform the present study in support of SSI review of the SR-Can report. The purpose is to assess the geochemical evolution of both potential buffer materials due to the intrusion of different types of groundwater, with a similar modelling layout to that reported in SR-Can. Three main categories of water inflows via a fracture intersecting a deposition hole are considered: the Forsmark reference groundwater, a high-salinity groundwater to account for up-rise of deep-seated brines and a diluted water representing ice-melting derived groundwater. In addition to this, the redox buffering capacity of Deponit CA-N bentonite and the thermal effect on MX-80 bentonite geochemistry have been assessed. This modelling work has been performed using the reactive transport modelling code HYTEC. The main outcome of the present study is that the intrusion of the considered groundwaters should not affect drastically the geochemistry of neither the Deponit CA-N nor the MX-80 bentonite on the long-term (100,000 y). Bentonite pH may reach high values (up to 10.5) in some cases but does not reach SKB criterion value related to bentonite chemical stability. Dissolution-precipitation of accessory minerals is not significant enough to induce important porosity changes (rise by maximum 2 %). Globally, the montmorillonite exchanger undergoes Na by Ca partial replacement, which may decrease the swelling pressure of the bentonite. The simulated intrusion of oxidizing waters

Geochemical Evolution of the Louisville Seamount Chain

Science.gov (United States)

Vanderkluysen, L.; Mahoney, J. J.; Koppers, A. A.; Lonsdale, P. F.

2007-12-01

The Louisville seamount chain is a 4300 km long chain of submarine volcanoes in the southwestern Pacific that is commonly thought to represent a hotspot track. It spans an ~80 Myr age range, comparable to that of the Hawaiian-Emperor chain (Koppers et al., G-cubed, 5 (6), 2004). The few previously dredged igneous samples are dominantly basaltic and alkalic, and have been inferred to represent post-shield volcanism (Hawkins et al., AGU Monograph, 43, 235, 1987). Their isotope and trace element signatures suggest an unusually homogenous mantle source (Cheng et al., AGU Monograph, 43, 283, 1987). Dredging in 2006, during the AMAT02RR cruise of the R.V. Revelle, was carried out in the hope of recovering both shield and post-shield samples and of exploring the geochemical evolution of the chain. Igneous rocks were recovered from 33 stations on 23 seamounts covering some 47 Myr of the chain's history. Our study, focusing on the major and trace element and Sr, Nd and Pb isotopic characteristics of these samples, shows that all are alkalic basalts, basanites and tephrites containing normative nepheline. Variations in major and trace elements appear to be controlled predominantly by variable extents of melting and fractional crystallization, with little influence from mantle source heterogeneity. Indeed, age-corrected isotopic values define only a narrow range, in agreement with long-term source homogeneity relative to the scale of melting; e.g., ɛNd varies from +4.1 to +5.7, 206Pb/204Pb from 19.048 to 19.281, and 87Sr/86Sr from 0.70362 to 0.70398. These values broadly fall within the fields of the proposed "C" or "FOZO" mantle end-members. However, small variations are present, with less radiogenic Nd and Pb isotope ratios at the older, western end of the chain, defining a trend toward a broadly EM2-like composition. Although some workers have postulated that the Louisville hotspot was the source of the ~120 Myr Ontong Java Plateau, our samples are isotopically distinct

Perfiles motivacionales de deportistas adolescentes españoles

Directory of Open Access Journals (Sweden)

Bartolom\\u00E9 J. Almagro

2012-01-01

Full Text Available El objetivo del estudio fue detectar posibles perfiles motivacionales en una muestra de deportistas adolescentes. Además, el estudio analizó las diferencias en los subfactores del clima motivacional percibido y en la satisfacción de las necesidades psicológicas básicas de los diferentes perfiles encontrados. Se utilizó una muestra de 608 deportistas, con una edad media de 14.43 años. Se midió el clima motivacional percibido (PMCSQ-2, los mediadores psicológicos (BPNES y la motivación en el deporte (SMS. El análisis de cluster reveló dos perfiles: un perfil altamente motivado, con puntuaciones altas tanto en formas de motivación autodeterminada (motivación intrínseca y regulación identificada como en motivación no autodeter- minada (regulación introyectada y externa, salvando la desmotivación; y un perfil moderadamente motivado, con puntuaciones moderadas (en torno a 3 y 4 en formas de motivación autodeterminada y no autodeterminada. En el análisis multivariante de los subfactores del clima motivacional percibido y de las necesidades piscológicas básicas según el perfil, se encontraron diferencias significativas a favor del perfil altamente motivado tanto en los sub- factores del clima motivacional tarea como ego, así como en los tres mediadores psicológicos. Se discuten los resultados en función de la importancia de fomentar un clima que implique a la tarea y que trate de satisfacer las necesidades de autonomía, competencia y relación con los demás durante los entrenamientos para obtener perfiles motivacionales más autodeterminados.

Geochemical evolution of the L/ILW near-field

International Nuclear Information System (INIS)

Kosakowski, G.; Berner, U.; Wieland, E.; Glaus, M.; Degueldre, C.

2014-10-01

The deep geological repository for low- and intermediate-level radioactive waste (L/ILW) contains large amounts of cement based materials used for waste conditioning, tunnel support and the backfill of cavities. The waste inventory is composed of a wide range of organic and inorganic materials. This study describes the spatial and temporal geochemical evolution of the cementitious near-field, and the interactions with the technical barriers and the surrounding host rock. This evolution is governed by several coupled processes, an important one being the development of saturation by groundwater ingress from the host rock. Saturation of the near-field is controlled by the inflow of water from the host rock, by the transport of dissolved gases from the near-field into the host rock and in the engineered gas transport system, and by the transport of humidity in the gas phase. The production of gas by anoxic corrosion of metals and by microbial degradation of organic wastes consumes water. The mineral reactions which give rise to concrete degradation, such as carbonation or alkali-silica-aggregate reactions may also consume or produce water. The first phase of cementitious near-field degradation, which persists only for a short period of time, is related to the hydration of cement minerals. The pore water has a pH of 13 or even higher because of the high content of dissolved alkali hydroxides. A constant pH of 12.5 determines the second phase of the cement degradation. The alkali concentration is reduced by mineral reactions and/or solute transport. This phase persists for a long time. In the third phase the portlandite is completely dissolved due to the reaction with silicates/aluminates present in the near-field and carbonate in the groundwater of the host rock or associated with reactive waste materials. The pore water is in equilibrium with calcium-silicate-hydrates (C-S-H) which gives rise to a pH value near 11 or lower. The Ca/Si ratio of C-S-H changes towards

Geochemical evolution of the L/ILW near-field

Energy Technology Data Exchange (ETDEWEB)

Kosakowski, G.; Berner, U.; Wieland, E.; Glaus, M.; Degueldre, C.

2014-10-15

The deep geological repository for low- and intermediate-level radioactive waste (L/ILW) contains large amounts of cement based materials used for waste conditioning, tunnel support and the backfill of cavities. The waste inventory is composed of a wide range of organic and inorganic materials. This study describes the spatial and temporal geochemical evolution of the cementitious near-field, and the interactions with the technical barriers and the surrounding host rock. This evolution is governed by several coupled processes, an important one being the development of saturation by groundwater ingress from the host rock. Saturation of the near-field is controlled by the inflow of water from the host rock, by the transport of dissolved gases from the near-field into the host rock and in the engineered gas transport system, and by the transport of humidity in the gas phase. The production of gas by anoxic corrosion of metals and by microbial degradation of organic wastes consumes water. The mineral reactions which give rise to concrete degradation, such as carbonation or alkali-silica-aggregate reactions may also consume or produce water. The first phase of cementitious near-field degradation, which persists only for a short period of time, is related to the hydration of cement minerals. The pore water has a pH of 13 or even higher because of the high content of dissolved alkali hydroxides. A constant pH of 12.5 determines the second phase of the cement degradation. The alkali concentration is reduced by mineral reactions and/or solute transport. This phase persists for a long time. In the third phase the portlandite is completely dissolved due to the reaction with silicates/aluminates present in the near-field and carbonate in the groundwater of the host rock or associated with reactive waste materials. The pore water is in equilibrium with calcium-silicate-hydrates (C-S-H) which gives rise to a pH value near 11 or lower. The Ca/Si ratio of C-S-H changes towards

Orientation geochemical survey for uranium exploration using 230Th

International Nuclear Information System (INIS)

Xia Dingliang.

1985-01-01

The distribution of 230 Th in soils, rocks and ores and its relationship with respect to uranium ore formation are discussed for its possible use in geochemical exploration for U. 230 Th, U and Ra, being members of the same decay series, are different in their geochemical behavior upon which the study is orientated. Twenty uranium deposits and occurrences located in western and southern Hunan province are tested. Geochemical data obtained are comprehensively correlated. It is suggested that 230 Th is useful not only in U-Ra disequilibrium study but also in understanding the geochemical evolution of U ores. The data aid to interpret the genesis of uranium deposits and to assess the radioactive anomalies and uranium-bearing zones. Therefore, it can be adopted as a tool for searching in deep-buried uranium ores. The field procedure is rather simple and flexible to meet any geological environment. It is easy to read out and is less influnced by any kind of interference. In case of disequilibrium caused by oxidation and reduction during the period of ore formation it still gives good indication compared with that of radiometry, radonmetry and geochemical sampling for U

Geochemical modelling of groundwater evolution and residence time at the Olkiluoto site

International Nuclear Information System (INIS)

Pitkaenen, P.; Luukkonen, A.; Ruotsalainen, P.; Leino-Forsman, H.; Vuorinen, U.

1999-05-01

An understanding of the geochemical evolution of groundwater is an essential part of the performance assessment and safety analysis of the final disposal of radioactive waste into the bedrock. The performance of technical barriers and migration of possibly released radionuclides depend on chemical conditions. A prerequisite for understanding these factors is the ability to specify the water-rock interactions which control chemical conditions in groundwater. The objective of this study is to interpret the processes and factors which control the hydrogeochemistry, such as pH and redox conditions. A model of the hydrogeochemical progress in different parts of the crystalline bedrock at Olkiluoto has been created and the significance of chemical reactions and groundwater mixing along different flowpaths calculated. Long term hydrodynamics have also been evaluated. The interpretation and modelling are based on water samples (63 altogether) obtained from precipitation, Baltic Sea, soil layer, shallow wells in the bedrock, and eight deep boreholes in the bedrock for which a comprehensive data set on dissolved chemical species and isotopes was available. Some analyses of dissolved gases and fracture calcite and their isotopic measurements were also utilised. The data covers the bedrock at Olkiluoto to a depth of 1000 m. The results from groundwater chemistry, isotopes, petrography, hydrogeology of the site, geomicrobial studies, and PCA and speciation calculations were used in the evaluation of evolutionary processes at the site. The geochemical interpretation of water-rock interaction, isotope-chemical evolution and mixing of palaeo water types were approached by mass-balance calculations (NETPATH). Reaction-path calculations (EQ3/6) were used to verify the thermodynamic feasibility of the reaction models obtained. The interpretation and calculation of hydrochemical data from Olkiluoto reveals the complex nature of hydrogeochemical evolution at the site. Changes in

Geochemical modelling of groundwater evolution and residence time at the Olkiluoto site

Energy Technology Data Exchange (ETDEWEB)

Pitkaenen, P.; Luukkonen, A. [VTT Communities and Infrastructure, Espoo (Finland); Ruotsalainen, P. [Fintact Oy (Finland); Leino-Forsman, H.; Vuorinen, U. [VTT Chemical Technology, Espoo (Finland)

1999-05-01

An understanding of the geochemical evolution of groundwater is an essential part of the performance assessment and safety analysis of the final disposal of radioactive waste into the bedrock. The performance of technical barriers and migration of possibly released radionuclides depend on chemical conditions. A prerequisite for understanding these factors is the ability to specify the water-rock interactions which control chemical conditions in groundwater. The objective of this study is to interpret the processes and factors which control the hydrogeochemistry, such as pH and redox conditions. A model of the hydrogeochemical progress in different parts of the crystalline bedrock at Olkiluoto has been created and the significance of chemical reactions and groundwater mixing along different flowpaths calculated. Long term hydrodynamics have also been evaluated. The interpretation and modelling are based on water samples (63 altogether) obtained from precipitation, Baltic Sea, soil layer, shallow wells in the bedrock, and eight deep boreholes in the bedrock for which a comprehensive data set on dissolved chemical species and isotopes was available. Some analyses of dissolved gases and fracture calcite and their isotopic measurements were also utilised. The data covers the bedrock at Olkiluoto to a depth of 1000 m. The results from groundwater chemistry, isotopes, petrography, hydrogeology of the site, geomicrobial studies, and PCA and speciation calculations were used in the evaluation of evolutionary processes at the site. The geochemical interpretation of water-rock interaction, isotope-chemical evolution and mixing of palaeo water types were approached by mass-balance calculations (NETPATH). Reaction-path calculations (EQ3/6) were used to verify the thermodynamic feasibility of the reaction models obtained. The interpretation and calculation of hydrochemical data from Olkiluoto reveals the complex nature of hydrogeochemical evolution at the site. Changes in

A preliminary study on the geochemical environment for deep geological disposal of high level radioactive waste in Korea

International Nuclear Information System (INIS)

Kim, Chun Soo; Bae, Dae Seok; Kim, Kyung Su; Koh, Yong Kwon; Park, Byoung Yun

2000-03-01

Geochemical study on the groundwater from crystalline rocks (granite and gneiss) for the deep geological disposal of high-level radioactive waste was carried out in order to elucidate the hydrogeochemical and isotope characteristics and geochemical evolution of the groundwater. Study areas are Jungwon, Chojeong, Youngcheon and Yusung for granite region, Cheongyang for gneiss region, and Yeosu for volcanic region. Groundwaters of each study areas weree sampled and analysed systematically. Groundwaters can be grouped by their chemistry and host rock. Origin of the groundwater was proposed by isotope ( 18 O, 2 H, 13 C, 34 S, 87 Sr, 15 N) studies and the age of groundwater was inferred from their tritium contents. Based ont the geochemical and isotope characteristics, the geochemical evolutions of each types of groundwater were simulated using SOLVEQ/CHILLER and PHREEQC programs

Geochemical Constraints for Mercury's PCA-Derived Geochemical Terranes

Science.gov (United States)

Stockstill-Cahill, K. R.; Peplowski, P. N.

2018-05-01

PCA-derived geochemical terranes provide a robust, analytical means of defining these terranes using strictly geochemical inputs. Using the end members derived in this way, we are able to assess the geochemical implications for Mercury.

Geochemical evolution of groundwater in the Mud Lake area, eastern Idaho, USA

Science.gov (United States)

Rattray, Gordon W.

2015-01-01

Groundwater with elevated dissolved-solids concentrations—containing large concentrations of chloride, sodium, sulfate, and calcium—is present in the Mud Lake area of Eastern Idaho. The source of these solutes is unknown; however, an understanding of the geochemical sources and processes controlling their presence in groundwater in the Mud Lake area is needed to better understand the geochemical sources and processes controlling the water quality of groundwater at the Idaho National Laboratory. The geochemical sources and processes controlling the water quality of groundwater in the Mud Lake area were determined by investigating the geology, hydrology, land use, and groundwater geochemistry in the Mud Lake area, proposing sources for solutes, and testing the proposed sources through geochemical modeling with PHREEQC. Modeling indicated that sources of water to the eastern Snake River Plain aquifer were groundwater from the Beaverhead Mountains and the Camas Creek drainage basin; surface water from Medicine Lodge and Camas Creeks, Mud Lake, and irrigation water; and upward flow of geothermal water from beneath the aquifer. Mixing of groundwater with surface water or other groundwater occurred throughout the aquifer. Carbonate reactions, silicate weathering, and dissolution of evaporite minerals and fertilizer explain most of the changes in chemistry in the aquifer. Redox reactions, cation exchange, and evaporation were locally important. The source of large concentrations of chloride, sodium, sulfate, and calcium was evaporite deposits in the unsaturated zone associated with Pleistocene Lake Terreton. Large amounts of chloride, sodium, sulfate, and calcium are added to groundwater from irrigation water infiltrating through lake bed sediments containing evaporite deposits and the resultant dissolution of gypsum, halite, sylvite, and bischofite.

A preliminary study on the geochemical environment for deep geological disposal of high level radioactive waste in Korea

Energy Technology Data Exchange (ETDEWEB)

Kim, Chun Soo; Bae, Dae Seok; Kim, Kyung Su; Koh, Yong Kwon; Park, Byoung Yun

2000-03-01

Geochemical study on the groundwater from crystalline rocks (granite and gneiss) for the deep geological disposal of high-level radioactive waste was carried out in order to elucidate the hydrogeochemical and isotope characteristics and geochemical evolution of the groundwater. Study areas are Jungwon, Chojeong, Youngcheon and Yusung for granite region, Cheongyang for gneiss region, and Yeosu for volcanic region. Groundwaters of each study areas weree sampled and analysed systematically. Groundwaters can be grouped by their chemistry and host rock. Origin of the groundwater was proposed by isotope ({sup 18}O, {sup 2}H, {sup 13}C, {sup 34}S, {sup 87}Sr, {sup 15}N) studies and the age of groundwater was inferred from their tritium contents. Based ont the geochemical and isotope characteristics, the geochemical evolutions of each types of groundwater were simulated using SOLVEQ/CHILLER and PHREEQC programs.

Perfiles de autor en repositorios institucionales

Directory of Open Access Journals (Sweden)

Patricia Genovés

2017-10-01

Full Text Available Este trabajo describe las funciones y utilidades de la implementación de perfiles de autor en repositorios institucionales, como un servicio de valor agregado dirigido a acrecentar su uso entre los miembros de una institución y mejorar la visibilidad de la producción científica alojada en el repositorio. Incluye un relevamiento de servicios de perfiles de autor implementados en repositorios institucionales argentinos y extranjeros. Advierte que, ante el establecimiento de mandatos nacionales de depósito, la necesidad de contar con repositorios institucionales fuertes y sostenibles en el tiempo es aún mayor que antes. Integrar a los repositorios las funcionalidades de los sistemas curriculares y de gestión de información científica y tecnológica es un camino para lograr esa fortaleza, y los perfiles de autor son el resultado visible de dicha integración. Señala que el beneficio que representa para un autor contar con un perfil público en el repositorio de su institución es equivalente al beneficio que para una institución representa contar con un repositorio digital, en términos de ventaja competitiva, valor añadido, incremento de la visibilidad y facilidades de recuperación y acceso a la producción generada.

Alligator Rivers Analogue project. Geochemical Data Bases

International Nuclear Information System (INIS)

Bennett, D.G.; Read, D.

1992-01-01

The Koongarra uranium deposit in the Northern Territory of Australia is being studied to evaluate the processes involved in the geochemical alteration of the ore body and the formation of the uranium dispersion fan. A broad range of research is being undertaken into the geochemistry and hydrology of the site with the aim of understanding the transport of radionuclides through the system. During the project a range of geochemical and hydrogeochemical models have been developed to account for measured data from the site and with which to predict site evolution. The majority of these models are based on the premise of thermodynamic chemical equilibrium and employ fundamental thermodynamic data to characterise the chemistry of the system. From the differences which exist between the thermodynamic data bases (Appendices I and II) it is possible to gain a view of the level of uncertainty associated with thermodynamic data in each set of calculations. This report gives a brief introduction to the geochemical processes underlying the models, and details the equations used to quantify the more common of these processes (e.g. aqueous speciation and mineral solubility). A description is given of the computer codes (EQ3/6, PHREEQE, MINTEQ) most commonly used during the project for geochemical modelling. Their key features are highlighted and comparisons made. It is concluded that the degree of uncertainty in geochemical modelling studies arising as a result of using one code rather than another is relatively insignificant when compared to that related to differences in the underlying data bases. 73 refs., 3 figs

A case study of long-term geochemical evolution of coal waste rock drainage and its remediation

Energy Technology Data Exchange (ETDEWEB)

Jarvis, A.P.; Gandy, C.J. [Newcastle Univ. (United Kingdom). School of Civil Engineering and Geosciences, Hydrogeochemical Engineering Research and Outreach Group

2010-07-01

The geochemical evolution of drainage from an 35 hectare orphan waste rock pile over a 15-year period was described. Spoil material at the site was generated during coal mining at 2 collieries between 1922 and 1970, and was comprised of grey and black shale, ash, coal, and coal dust. The heap was founded on an impermeable clay layer. Located in northern England, drainage from the rock heap was intercepted by a small compost wetland system installed in 1997. The waste rock heap was selectively capped in 1998. Water samples were collected and analyzed. Anion concentrations were determined using an ion chromatograph. The samples were filtered periodically. Acidity concentrations and flow rates were determined. Results of the study showed measurable improvements in water quality as a result of capping the heap. The study demonstrated that a combination of selective spoil capping and wetland treatment can serve as a low-cost solution to acid mine drainage at some abandoned mine sites. 9 refs., 1 tab., 1 fig.

A case study of long-term geochemical evolution of coal waste rock drainage and its remediation

International Nuclear Information System (INIS)

Jarvis, A.P.; Gandy, C.J.

2010-01-01

The geochemical evolution of drainage from an 35 hectare orphan waste rock pile over a 15-year period was described. Spoil material at the site was generated during coal mining at 2 collieries between 1922 and 1970, and was comprised of grey and black shale, ash, coal, and coal dust. The heap was founded on an impermeable clay layer. Located in northern England, drainage from the rock heap was intercepted by a small compost wetland system installed in 1997. The waste rock heap was selectively capped in 1998. Water samples were collected and analyzed. Anion concentrations were determined using an ion chromatograph. The samples were filtered periodically. Acidity concentrations and flow rates were determined. Results of the study showed measurable improvements in water quality as a result of capping the heap. The study demonstrated that a combination of selective spoil capping and wetland treatment can serve as a low-cost solution to acid mine drainage at some abandoned mine sites. 9 refs., 1 tab., 1 fig.

Geochemical site-selection criteria for HLW repositories in Europe and North America

International Nuclear Information System (INIS)

Savage, David; Arthur, Randolph C.; Sasamoto, Hiroshi; Shibata, Masahiro; Yui, Mikazu

2000-01-01

Geochemical as well as socio-economic issues associated with the selection of potential sites to host a high-level nuclear waste repository have received considerable attention in repository programs in Europe (Belgium, Finland, France, Germany, Spain, Sweden, Switzerland and the U.K.) and North America (Canada and the United States). The objective of the present study is to summarize this international experience with particular emphasis on geochemical properties that factor into the adopted site-selection strategies. Results indicate that the geochemical properties of a site play a subordinate role, at best, to other geotechnical properties in the international site-selection approaches. In countries where geochemical properties are acknowledged in the site-selection approach, requirements are stated qualitatively and tend to focus on associated impacts on the stability of the engineered barrier system and on radionuclide transport. Site geochemical properties that are likely to control the long-term stability of geochemical conditions and radionuclide migration behavior are unspecified, however. This non-prescriptive approach may be reasonable for purposes of screening among potential sites, but a better understanding of site properties that are most important in controlling the long-term geochemical evolution of the site over a range of possible scenarios would enable the potential sites to be ranked in terms of their suitability to host a repository. (author)

The impacts of a linear wastewater reservoir on groundwater recharge and geochemical evolution in a semi-arid area of the Lake Baiyangdian watershed, North China Plain

Energy Technology Data Exchange (ETDEWEB)

Wang, Shiqin [Faculty of Horticulture, Chiba University, Matsudo-City 271-8510 (Japan); Tang, Changyuan, E-mail: cytang@faculty.chiba-u.jp [Faculty of Horticulture, Chiba University, Matsudo-City 271-8510 (Japan); Song, Xianfang [Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101 (China); Wang, Qinxue [National Institute for Environmental Studies, Tsukuba 305-8506 (Japan); Zhang, Yinghua [Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101 (China); Yuan, Ruiqiang [College of Environment and Resources, Shanxi University (China)

2014-06-01

Sewage leakage has become an important source of groundwater recharge in urban areas. Large linear wastewater ponds that lack anti-seepage measures can act as river channels that cause the deterioration of groundwater quality. This study investigated the groundwater recharge by leakage of the Tanghe Wastewater Reservoir, which is the largest industrial wastewater channel on the North China Plain. Additionally, water quality evolution was investigated using a combination of multivariate statistical methods, multi-tracers and geochemical methods. Stable isotopes of hydrogen and oxygen indicated high levels of wastewater evaporation. Based on the assumption that the wastewater was under an open system and fully mixed, an evaporation model was established to estimate the evaporation of the wastewater based on isotope enrichments of the Rayleigh distillation theory using the average isotope values for dry and rainy seasons. Using an average evaporation loss of 26.5% for the input wastewater, the estimated recharge fraction of wastewater leakage and irrigation was 73.5% of the total input of wastewater. The lateral regional groundwater inflow was considered to be another recharge source. Combing the two end-members mix model and cluster analysis revealed that the mixture percentage of the wastewater decreased from the Highly Affected Zone (76%) to the Transition Zone (5%). Ion exchange and redox reaction were the dominant geochemical processes when wastewater entered the aquifer. Carbonate precipitation was also a major process affecting evolution of groundwater quality along groundwater flow paths. - Highlights: • An unlined wastewater reservoir caused the deterioration of groundwater quality. • An evaporation fraction was estimated by Rayleigh distillation theory of isotopes. • 73.5% of wastewater recharge to groundwater by leakage and irrigation infiltration. • The region influenced by wastewater was divided into four subzones. • Mixing, ion exchange, and

Modelling of long term geochemical evolution and study of mechanical perturbation of bentonite buffer of a KBS-3 repository

Energy Technology Data Exchange (ETDEWEB)

Marsal, Francois; Pellegrini, Delphine; Deleruyelle, Frederic; Serres, Christophe (French Inst. for Radiological Protection and Nuclear Safety (IRSN), Fontenay-aux-Roses (FR)); Windt, Laurent de (Ecole des Mines de Paris, Paris (FR))

2008-03-15

PART I: The Swedish Nuclear Fuel and Waste Management Co. (SKB) has recently completed a safety assessment project named SR-Can, related to the KBS-3 disposal concept. In this concept, the waste packages are surrounded by a buffer made of either MX-80 or Deponit CA-N bentonite. Interactions between the buffer and groundwater may modify the buffer composition and thus its containment properties. The Swedish Radiation Protection Authorities (SSI) requested the French Institute for Radiological Protection and Nuclear Safety (IRSN) to perform the present study in support of SSI review of the SR-Can report. The purpose is to assess the geochemical evolution of both potential buffer materials due to the intrusion of different types of groundwater, with a similar modelling layout to that reported in SR-Can and detailed in Arcos et al. Three main categories of water inflows via a fracture intersecting a deposition hole are considered: the Forsmark reference groundwater, a high-salinity groundwater to account for up-rise of deep-seated brines and a diluted water representing ice-melting derived-groundwater. In addition to this, the redox buffering capacity of Deponit CA-N bentonite and the thermal effect on MX-80 bentonite geochemistry have been assessed. This modelling work has been performed using the reactive transport modelling code HYTEC. The main outcome of the present study is that the intrusion of the considered groundwaters should not affect drastically the geochemistry of neither the Deponit CA-N nor the MX-80 bentonite on the longterm (100,000 y). Bentonite pH may reach high values (up to 10.5) in some cases but does not reach SKB criterion value related to bentonite chemical stability. Dissolution-precipitation of accessory minerals is not significant enough to induce important porosity changes (rise by maximum 2 %). Globally, the montmorillonite exchanger undergoes Na by Ca partial replacement, which may decrease the swelling pressure of the bentonite. The

PERFILES MOTIVACIONALES EN SALVAMENTO DEPORTIVO

Directory of Open Access Journals (Sweden)

J.A. Moreno

2010-09-01

Full Text Available

RESUMEN

El objetivo de este trabajo fue establecer diferentes perfiles motivacionales en una muestra compuesta por 283 deportistas federados de salvamento deportivo (141 hombres y 142 mujeres, de edades comprendidas entre los 14 y los 38 años. Las variables analizadas fueron la percepción del clima motivacional, la motivación intrínseca, la motivación extrínseca, la desmotivación y el flow disposicional. El análisis cluster reveló tres perfiles motivacionales. El “perfil no autodeterminado” obtuvo puntuaciones altas en la percepción de un clima ego y en desmotivación, moderadas en motivación intrínseca, extrínseca y flow disposicional, y bajas en la percepción de un clima tarea. El “perfil autodeterminado” mostró puntuaciones altas en la percepción de un clima tarea y en motivación intrínseca, revelando los valores más altos de flow disposicional. También obtuvo puntuaciones moderadas en motivación extrínseca y bajas en desmotivación y en la percepción de un clima ego. El “perfil pobremente motivado” reflejó una puntuación moderada en la percepción de un clima ego y baja en el resto de variables de estudio. La puntuación más alta que obtuvo fue en desmotivación. Además, los resultados mostraron que en niveles de competición más elevados los perfiles motivacionales parecían ser más negativos.
Palabras Clave: motivación, autodeterminación, clima motivacional, flow, salvamento deportivo.

ABSTRACT

The main purpose of this article has been to analyze the motivational profiles in a group of 283 lifesavers (141 male and 142 female, of ages 14 to 38 years. There were several variables that were analyzed: perception

Geochemical evidence for waning magmatism and polycyclic volcanism at Crater Flat, Nevada

International Nuclear Information System (INIS)

Perry, F.V.; Crowe, B.M.

1992-01-01

This paper reports that petrologic and geochemical studies of basaltic rocks in the Yucca Mountain region are currently focused on understanding the evolution of volcanism in the Crater Flat volcanic field and the mechanisms of polycyclic volcanic field and the mechanisms of polycyclic volcanism at the Lathrop Wells volcanic center, the youngest center in the Crater Flat volcanic field. Geochemical and petrologic data indicate that the magma chambers which supplied the volcanic centers at Crater Flat became situated at greater crustal depths as the field evolved. Deep magma chambers may be related to a waning magma flux that was unable to sustain upper crustal magma conduits and chambers. Geochemical data from the Lathrop Wells volcanic center indicate that eruptive units identified from field and geomorphic relationships are geochemically distinct. The geochemical variations cannot be explained by fractional crystallization of a single magma batch, indicating that several magma batches were involved in the formation of the Lathrop Wells center. Considering the low magma flux in the Yucca Mountain region in the Quaternary, the probability of several magma batches erupting essentially simultaneously at Lathrop Wells is considered remote

Vertical evolution of petrographic and organic geochemical parameters in Las Duenas mire (Cantabrian Coast, North Spain)

Energy Technology Data Exchange (ETDEWEB)

Lopez-Dias, V.; Borrego, A.G.; Blanco, C.G. [Instituto Nacional del Carbon (CSIC), Oviedo (Spain)

2010-12-01

Las Duenas mire has developed on a flat siliceous substrate over the Holocene. The sedimentary cover has a thickness of around 50 cm and the mire comprises a surface area of 27 ha. A core sample obtained using a manual probe was split into sub-samples of around 3-4 cm thickness for petrographic and organic geochemical analysis. The fen originated by minerogenesis and contains a high concentration of mineral matter throughout its profile which decreases towards the top. The present day vegetation is dominated by Sphagnum. A variety of transparent textinite with intense fluorescence is evidence of the low maturity of the profile, which is also confirmed by the presence of low reflecting huminite of the A variety (Hr {proportional_to} 0.15%). The fluorescence spectra of sporinite and cutinite are similar and, compared with those of transparent textinite, they have a lower intensity and are shifted to higher wavelengths. The low maturity of the organic matter is also confirmed by the presence of unstable {beta}{beta} hopane configurations, the abundance of hopene, and the presence of functionalized hopanoids, steroids and other triterpenoids. The evolution of the geochemical parameters in the peat profile indicates the presence of more humid conditions in the top 4 cm and at a depth of 11-15 cm. These periods are characterized by a high Sphagnum/higher plant contribution as deduced from the n-alkane ratios. The low reflectance of huminite at the depth of 11-15 cm could also support less oxidizing condition. The sediment at a depth of 22 cm where peaty matter starts to accumulate has been dated as 9603 cal BC, whereas the plant fraction at the same depth dates back to a maximum of 200 years. Sediment reworking derived from radiocarbon dates indicates that this fen is not suitable for palaeoenvironmental studies. (author)

Facebook: personalidad y privacidad en los perfiles

OpenAIRE

Casado Riera, Carla; Oberst, Ursula E.; Carbonell, Xavier

2015-01-01

El objetivo del presente estudio fue investigar la relación entre la configuración de la privacidad en los perfiles de Facebook y dos dimensiones de personalidad, extraversión y neuroticismo, en relación con el sexo. Se aplicó el Cuestionario de la Privacidad en Facebook y el cuestionario de personalidad EPI a una muestra de 92 mujeres y 70 hombres, usuarios de Facebook. No se encontró una relación significativa entre extraversión o neuroticismo y la privacidad en los perfiles de Facebook, pe...

Competencias docentes digitales: propuesta de un perfil

OpenAIRE

Adriana Rangel Baca

2015-01-01

En este artículo se presenta la propuesta de un perfil de competencias docentes digitales y se describen las dimensiones, competencias e indicadores que lo componen. Se analizan distintas fuentes para determinar el conjunto de recursos a movilizar por los docentes en materia digital y se elabora una versión preliminar del perfil, la cual es puesta a consideración de un grupo de expertos en el uso de las Tecnologías de la Información y la Comunicación (TIC) para su validación. Los resultados m...

Perfil professional a les biblioteques publiques : visió dels bibliotecaris mateixos

Directory of Open Access Journals (Sweden)

Delmàs Ruiz, Maria

2015-12-01

Full Text Available El perfil professional dels bibliotecaris ha anat evolucionant al llarg dels anys, en consonància amb els canvis que han afectat la biblioteca pública. En aquest article s'analitza com és aquest perfil actualment, des de l'òptica dels professionals mateixos. S'obté així una visió de les competències més valorades avui en dia, i es detecten els vessants del perfil que requereixen més incidència formativa. Com a resultat de l'anàlisi s'ha identificat la necessitat de perfils especialitzats, que també es podria cobrir amb la incorporació de professionals complementaris. Finalment, tot i que el perfil professional de bibliotecari s'adapta a grans trets a la nova realitat de les biblioteques públiques, també s'identifiquen les mancances percebudes pels professionals.El perfil profesional de los bibliotecarios ha ido evolucionando a lo largo de los años, en consonancia con los cambios que han afectado a la biblioteca pública. En este artículo se analiza cómo es este perfil actualmente, desde la óptica de los mismos profesionales. Se obtiene así una visión de las competencias más valoradas hoy en día, y se detectan las facetas del perfil que requieren más incidencia formativa. Como resultado del análisis se ha identificado la necesidad de perfiles especializados, que también se podría suplir con la incorporación de profesionales complementarios. Finalmente, aunque el perfil profesional de bibliotecario se adapta en gran medida a la nueva realidad de las bibliotecas públicas, también se identifican las carencias percibidas por los profesionales.The professional profile of the public librarian has evolved in response to the changes that constantly affect public libraries. In this article we analyze what the public librarian’s job involves from the point of view of the professionals themselves. This allows us to examine the competences that are most highly valued and identify those areas in which professionals require more

Archean crust-mantle geochemical differentiation

Science.gov (United States)

Tilton, G. R.

Isotope measurements on carbonatite complexes and komatiites can provide information on the geochemical character and geochemical evolution of the mantle, including the sub-continental mantle. Measurements on young samples establish the validity of the method. These are based on Sr, Nd and Pb data from the Tertiary-Mesozoic Gorgona komatiite and Sr and Pb data from the Cretaceous Oka carbonatite complex. In both cases the data describe a LIL element-depleted source similar to that observed presently in MORB. Carbonatite data have been used to study the mantle beneath the Superior Province of the Canadian Shield one billion years (1 AE) ago. The framework for this investigation was established by Bell et al., who showed that large areas of the province appear to be underlain by LIL element-depleted mantle (Sr-85/Sr-86=0.7028) at 1 AE ago. Additionally Bell et al. found four complexes to have higher initial Sr ratios (Sr-87/Sr-86=0.7038), which they correlated with less depleted (bulk earth?) mantle sources, or possibly crustal contamination. Pb isotope relationships in four of the complexes have been studied by Bell et al.

Archean crust-mantle geochemical differentiation

Science.gov (United States)

Tilton, G. R.

1983-01-01

Isotope measurements on carbonatite complexes and komatiites can provide information on the geochemical character and geochemical evolution of the mantle, including the sub-continental mantle. Measurements on young samples establish the validity of the method. These are based on Sr, Nd and Pb data from the Tertiary-Mesozoic Gorgona komatiite and Sr and Pb data from the Cretaceous Oka carbonatite complex. In both cases the data describe a LIL element-depleted source similar to that observed presently in MORB. Carbonatite data have been used to study the mantle beneath the Superior Province of the Canadian Shield one billion years (1 AE) ago. The framework for this investigation was established by Bell et al., who showed that large areas of the province appear to be underlain by LIL element-depleted mantle (Sr-85/Sr-86=0.7028) at 1 AE ago. Additionally Bell et al. found four complexes to have higher initial Sr ratios (Sr-87/Sr-86=0.7038), which they correlated with less depleted (bulk earth?) mantle sources, or possibly crustal contamination. Pb isotope relationships in four of the complexes have been studied by Bell et al.

The evolution of the magmatic arc of Southern Peru (200-60 Ma), Arequipa area: insight from geochemical modeling

Science.gov (United States)

Demouy, S.; Benoit, M.; De Saint Blanquat, M.; Brunet, P.

2012-12-01

Cordilleran-type batholiths are built by prolonged arc activity along continental margins and may provide detailed magmatic records of the subduction system evolution. The magmas produced in subduction context involve both mantellic and crustal end members and are subject to various petrological processes. The MASH zones (Hildreth and Moorbath, 1988), at the basis of the continental crust, are the best places for the genesis of such hybrid magmas. The various geochemical signatures observed in the plutonic rocks, may also be attributed to source heterogeneities or generated by subsequent petrological processes. This study has focused in the Arequipa section of the Coastal Batholith of Southern Peru (200-60 Ma), in an area extending over 80x40 km. Major and trace elements as well as Sr and Nd isotopic analyses were performed in a set of 100 samples ranging from gabbro to granite. The obtained data highlight the wide heterogeneity of the geochemical signatures that is not related to the classification of the rocks. In first step, Rb/Sr systematic was used to isolate a set of samples plotting along a Paleocene isochron and defining a cogenetic suite. This suite appears to have evolved by simple fractional crystallization. By using reverse modeling, the parameters controlling the fractional crystallization process were defined, as partition coefficients, initial concentrations and amount of fractional crystallization. The other magmatic suites display a wide range of isotopic and geochemical signatures. To explain this heterogeneity, a model involving competition between fractional crystallization and magma mixing into MASH zones was proposed. A large range of hybrid magma types is potentially generated during the maturation of the system, but this range tends to disappear as fractionation and mixing occurs. Finally the model predicts the genesis of a homogeneous reservoir created at depth, from which magmas may evolve only by fractional crystallization. Therefore

Development of thermodynamic databases and geochemical/transport models for prediction of long-term radionuclide migration (Germany)

International Nuclear Information System (INIS)

Kienzler, B.

2000-01-01

The isolation capacity of a repository system for radionuclides is described by geochemical modeling. The models for interpretation of experimental findings and for long-term extrapolation of experimental results are based on thermodynamic approaches. The geochemical models include dissolution reactions of waste forms, the evolution of the geochemical milieu, interactions of radionuclides with constituents of the groundwater (brines) and the precipitation of new solid phases. Reliable thermodynamic data, understanding of radionuclide complexation in aqueous multi-electrolyte solutions at the relevant ionic strength and knowledge on the formation of pure and mixed solids and on sorption processes are urgently needed for such model calculations. (author)

Second Symposium on Chemical Evolution and the Origin of Life

International Nuclear Information System (INIS)

Devincenzi, D.L.; Dufour, P.A.

1986-05-01

Recent findings by NASA Exobiology investigators are reported. Scientific papers are presented in the following areas: cosmic evolution of biogenic compounds, prebiotic evolution (planetary and molecular), early evolution of life (biological and geochemical), evolution of advanced life, solar system exploration, and the Search for Extraterrestrial Intelligence (SETI)

Constraining Lateral Evolution of Magmatic Behavior in North Tanzania from Geophysical and Geochemical Analyses

Science.gov (United States)

Gautier, S.; Tiberi, C.; Parat, F.; Baudouin, C.

2016-12-01

In the framework of CRAFTI and CoLiBrEA experiments in 2013, we proceeded to both seismic and geochemical studies along an EW profile through the North Tanzania Divergence. The data were collected along a line starting at the Ngorongoro volcanic area, ending at Kitumbeine edifice and crossing the rift valley. Recent seismological studies show lateral and depth variations for both velocity and Vp/Vs ratio within this area, particularly a change of Moho depth between the western and central parts of the rift. These two zones also exhibit diverse geochemical signatures that involve different magma storage (depth of reservoir, magma volume) and ascent as well as higher partial melts content for the western part. We take advantage of the recent and precise 3D lithospheric velocity models and receiver functions in this area to compare the structure and nature of Ngorongoro area and rift valley. We first compute ray path and establish regional coherency maps between piercing points, Vp/Vs ratio and tomographic images. Second, those results are compared with the composition of magma at depth obtained from a petrophysical and geochemical analysis of lava samples. We will discuss those results in terms of magmatic processes, and how they interact with the rifting in a cratonic lithosphere.

Evolution of hillslope soils: The geomorphic theater and the geochemical play

International Nuclear Information System (INIS)

Yoo, Kyungsoo; Weinman, Beth; Mudd, Simon Marius; Hurst, Martin; Attal, Mikael; Maher, Kate

2011-01-01

Highlights: → We ask 'how and how fast do hillslope soils form as the landscape's morphology changes over time?'. → Over wide range of denudation rates, soil thicknesses do not vary significantly. → Colluvial soils with lower denudation rates (above the knick point) are enriched in fine size fractions, Zr, and pedogenic crystalline Fe oxides. → In the two steep hillslopes below the knickpoint, no systematic topgraphic trends were found for soil geochemistry. → Soils show increasing Zr enrichment in the downslope direction only in the hillslope above the knickpoint. - Abstract: How and how fast do hillslope soils form as the landscape's morphology changes over time? Here results are shown from an ongoing study that simultaneously examines the morphologic and geochemical evolution of soil mantled hillslopes that have been exposed to distinctively different denudation history. In Northern Sierra Nevada, California, the authors are investigating a tributary basin to the Middle Fork Feather River. A major incision signal from the river is well marked in a knickpoint within the tributary basin which stretches from its mouth to the Feather River at an elevation of ∼700 m to the plateau at an elevation of ∼1500 m. Hillslopes are significantly steeper below the knickpoint. The area's total denudation rates are currently being constrained using cosmogenic radio nuclides, but a previous study suggested an order of magnitude difference in total denudation rates below and above the knickpoint. When compared with topographic attributes calculated from LIDAR data, physical erosion rates can be modeled as a linear function of ridge top curvature. Surprisingly, over the wide range of total denudation rates, soil thicknesses do not vary significantly until a threshold point where soil mantled landscapes abruptly shift to bedrock dominated landscapes. Bioturbation by tree falls appear to buffer soil thickness over the wide range of physical soil erosion rates. From

Evolution of hillslope soils: The geomorphic theater and the geochemical play

Energy Technology Data Exchange (ETDEWEB)

Yoo, Kyungsoo, E-mail: kyoo@umn.edu [Dept. of Soil, Water, and Climate, University of Minnesota, 439 Borlaug Hall, 1991 Upper Buford Circle, St. Paul, MN, 55108-6028 (United States); Weinman, Beth [Dept. of Soil, Water, and Climate, University of Minnesota, 439 Borlaug Hall, 1991 Upper Buford Circle, St. Paul, MN, 55108-6028 (United States); Mudd, Simon Marius; Hurst, Martin; Attal, Mikael [School of GeoSciences, University of Edinburgh, Drummond Street, Edinburgh EH8 9XP, Scotland (United Kingdom); Maher, Kate [Dept. of Geological and Environmental Sciences, Braun Hall 118, 450 Serra Mall, Bldg. 320, Stanford, CA 94305-2115 (United States)

2011-06-15

Highlights: > We ask 'how and how fast do hillslope soils form as the landscape's morphology changes over time?'. > Over wide range of denudation rates, soil thicknesses do not vary significantly. > Colluvial soils with lower denudation rates (above the knick point) are enriched in fine size fractions, Zr, and pedogenic crystalline Fe oxides. > In the two steep hillslopes below the knickpoint, no systematic topgraphic trends were found for soil geochemistry. > Soils show increasing Zr enrichment in the downslope direction only in the hillslope above the knickpoint. - Abstract: How and how fast do hillslope soils form as the landscape's morphology changes over time? Here results are shown from an ongoing study that simultaneously examines the morphologic and geochemical evolution of soil mantled hillslopes that have been exposed to distinctively different denudation history. In Northern Sierra Nevada, California, the authors are investigating a tributary basin to the Middle Fork Feather River. A major incision signal from the river is well marked in a knickpoint within the tributary basin which stretches from its mouth to the Feather River at an elevation of {approx}700 m to the plateau at an elevation of {approx}1500 m. Hillslopes are significantly steeper below the knickpoint. The area's total denudation rates are currently being constrained using cosmogenic radio nuclides, but a previous study suggested an order of magnitude difference in total denudation rates below and above the knickpoint. When compared with topographic attributes calculated from LIDAR data, physical erosion rates can be modeled as a linear function of ridge top curvature. Surprisingly, over the wide range of total denudation rates, soil thicknesses do not vary significantly until a threshold point where soil mantled landscapes abruptly shift to bedrock dominated landscapes. Bioturbation by tree falls appear to buffer soil thickness over the wide range of physical soil

The Role of Geochemical Modeling in Predicting Quality Evolution of Acid Mine Drainage

Directory of Open Access Journals (Sweden)

Andrea Šlesárová

2004-12-01

Full Text Available In recent years the massive reduction of raw materials production brings a wide scale of problems. Among the most frequent exposes of mining activities belong besides old spoil heaps and sludge lagoons, also the drainage of acidic and highly mineralized mine waters known as “the Acid Mine Drainage” (thereinafter AMD from old mine workings. The acid mine drainage presents to the surrounding environment a massive problem. These waters are toxic to the plant and animal life, including fishes and aquatic insects. The primary control of the drainage pH and the metal content is the exposure of sulphide minerals to weathering, the availability of atmospheric oxygen, and the sensitivity of non-sulphide minerals to buffer acidity. A geochemical modeling software is increasingly used to solve evolution of the complex chemical systems such as the interaction of acid mine drainage with wall rocks, migration of AMD components. Beyond the better computer facilities it allows to study of thermodynamic properties substances and to enlarge thermodynamic databases. A model is a simplified version of reality based on its observation and experiments. A goal of the modeling process is the tendency to better understand processes taking place inside of the system, the attempt to assume the system’s behaviour in the future or to predict the effect of changed conditions in the system’s environment on the system itself.

Ética y perfiles administrativos de empresas diferenciadas frente al perfil deseable para el administrador de empresas de la Universidad de La Salle

Directory of Open Access Journals (Sweden)

Richard Orlando Buitrago Reyes

2005-01-01

Full Text Available El objetivo es ilustrar cómo la investigación que se realizó, encontró componentes de éticaempresarial y perfil gerencial en cuatro empresas bogotanas de acuerdo con perfiles deseablesde desarrollo universitario. Asimismo, desde el punto de vista empresarial, corroborar sicuatro empresas bogotanas exigen a sus profesionales en Administración de Empresas perfilesde desempeño y valores de desarrollo para desenvolverse en un ambiente de negocios. Esindiscutible que los cambios tecnológicos, de sistemas económicos, sociales y políticos llevaránal profesional en Administración de Empresas a prepararse de acuerdo con las exigencias delmundo moderno y a la Universidad a adecuar todos sus sistemas para crear un perfil delestudiante y del profesional coherente con las exigencias de liderazgo y capacidad de toma dedecisiones en extrema competitividad .

Controls on the geochemical evolution of Prairie Pothole Region lakes and wetlands over decadal time scales

Science.gov (United States)

Goldhaber, Martin B.; Mills, Christopher T.; Mushet, David M.; McCleskey, R. Blaine; Rover, Jennifer

2016-01-01

One hundred sixty-seven Prairie Pothole lakes, ponds and wetlands (largely lakes) previously analyzed chemically during the late 1960’s and early to mid-1970’s were resampled and reanalyzed in 2011–2012. The two sampling periods differed climatically. The earlier sampling took place during normal to slightly dry conditions, whereas the latter occurred during and immediately following exceptionally wet conditions. As reported previously in Mushet et al. (2015), the dominant effect was expansion of the area of these lakes and dilution of their major ions. However, within that context, there were significant differences in the evolutionary pathways of major ions. To establish these pathways, we employed the inverse modeling computer code NetpathXL. This code takes the initial and final lake composition and, using mass balance constrained by the composition of diluting waters, and input and output of phases, calculates plausible geochemical evolution pathways. Despite the fact that in most cases major ions decreased, a subset of the lakes had an increase in SO42−. This distinction is significant because SO42− is the dominant anion in a majority of Prairie Pothole Region wetlands and lakes. For lakes with decreasing SO42−, the proportion of original lake water required for mass balance was subordinate to rainwater and/or overland flow. In contrast, lakes with increasing SO42− between the two sampling episodes tended to be dominated by original lake water. This suite of lakes tended to be smaller and have lower initial SO42−concentrations such that inputs of sulfur from dissolution of the minerals gypsum or pyrite had a significant impact on the final sulfur concentration given the lower dilution factors. Thus, our study provides context for how Prairie Pothole Region water bodies evolve geochemically as climate changes. Because wetland geochemistry in turn controls the ecology of these water bodies, this research contributes to the prediction of the

Earth's earliest biosphere: Its origin and evolution

International Nuclear Information System (INIS)

Schopf, J.W.

1983-01-01

Some of the subjects discussed are related to the early biogeologic history, the nature of the earth prior to the oldest known rock record, the early earth and the Archean rock record, the prebiotic organic syntheses and the origin of life, Precambrian organic geochemistry, the biochemical evolution of anaerobic energy conversion, the isotopic inferences of ancient biochemistries, Archean stromatolites providing evidence of the earth's earliest benthos, Archean microfossils, the geologic evolution of the Archean-Early Proterozoic earth, and the environmental evolution of the Archean-Early Proterozoic earth. Other topics examined are concerned with geochemical evidence bearing on the origin of aerobiosis, biological and biochemical effects of the development of an aerobic environment, Early Proterozoic microfossils, the evolution of earth's earliest ecosystems, and geographic and geologic data for processed rock samples. Attention is given to a processing procedure for abiotic samples and calculation of model atmospheric compositions, and procedures of organic geochemical analysis

Geochemical exploration for uranium

International Nuclear Information System (INIS)

1988-01-01

This Technical Report is designed mainly to introduce the methods and techniques of uranium geochemical exploration to exploration geologists who may not have had experience with geochemical exploration methods in their uranium programmes. The methods presented have been widely used in the uranium exploration industry for more than two decades. The intention has not been to produce an exhaustive, detailed manual, although detailed instructions are given for a field and laboratory data recording scheme and a satisfactory analytical method for the geochemical determination of uranium. Rather, the intention has been to introduce the concepts and methods of uranium exploration geochemistry in sufficient detail to guide the user in their effective use. Readers are advised to consult general references on geochemical exploration to increase their understanding of geochemical techniques for uranium

Crustal contamination and crystal entrapment during polybaric magma evolution at Mt. Somma-Vesuvius volcano, Italy: Geochemical and Sr isotope evidence

Science.gov (United States)

Piochi, M.; Ayuso, R.A.; de Vivo, B.; Somma, R.

2006-01-01

New major and trace element analyses and Sr-isotope determinations of rocks from Mt. Somma-Vesuvius volcano produced from 25 ky BP to 1944 AD are part of an extensive database documenting the geochemical evolution of this classic region. Volcanic rocks include silica undersaturated, potassic and ultrapotassic lavas and tephras characterized by variable mineralogy and different crystal abundance, as well as by wide ranges of trace element contents and a wide span of initial Sr-isotopic compositions. Both the degree of undersaturation in silica and the crystal content increase through time, being higher in rocks produced after the eruption at 472 AD (Pollena eruption). Compositional variations have been generally thought to reflect contributions from diverse types of mantle and crust. Magma mixing is commonly invoked as a fundamental process affecting the magmas, in addition to crystal fractionation. Our assessment of geochemical and Sr-isotopic data indicates that compositional variability also reflects the influence of crustal contamination during magma evolution during upward migration to shallow crustal levels and/or by entrapment of crystal mush generated during previous magma storage in the crust. Using a variant of the assimilation fractional crystallization model (Energy Conservation-Assimilation Fractional Crystallization; [Spera and Bohrson, 2001. Energy-constrained open-system magmatic processes I: General model and energy-constrained assimilation and fractional crystallization (EC-AFC) formulation. J. Petrol. 999-1018]; [Bohrson, W.A. and Spera, F.J., 2001. Energy-constrained open-system magmatic process II: application of energy-constrained assimilation-fractional crystallization (EC-AFC) model to magmatic systems. J. Petrol. 1019-1041]) we estimated the contributions from the crust and suggest that contamination by carbonate rocks that underlie the volcano (2 km down to 9-10 km) is a fundamental process controlling magma compositions at Mt. Somma

Geochemical sensitivity analysis: Identification of important geochemical parameters for performance assessment studies

International Nuclear Information System (INIS)

Siegel, M.; Guzowski, R.; Rechard, R.; Erickson, K.

1986-01-01

The EPA Standard for geologic disposal of high level waste requires demonstration that the cumulative discharge of individual radioisotopes over a 10,000 year period at points 5 kilometers from the engineered barrier system will not exceed the limits prescribed in 40 CFR Part 191. The roles of the waste package, engineered facility, hydrogeology and geochemical processes in limiting radionuclide releases all must be considered in calculations designed to assess compliance of candidate repositories with the EPA Standard. In this talk, they will discuss the geochemical requirements of calculations used in these compliance assessments. In addition, they will describe the complementary roles of (1) simple models designed to bound the radionuclide discharge over the widest reasonable range of geochemical conditions and scenarios and (2) detailed geochemical models which can provide insights into the actual behavior of the radionuclides in the ground water. Finally, they will discuss development of sensitivity/uncertainty techniques designed to identify important site-specific geochemical parameters and processes using data from a basalt formation

Geochemical modeling of the nuclear-waste repository system. A status report

International Nuclear Information System (INIS)

Deutsch, W.J.

1980-12-01

The primary objective of the geochemical modeling task is to develop an understanding of the waste-repository geochemical system and provide a valuable tool for estimating future states of that system. There currently exists a variety of computer codes which can be used in geochemical modeling studies. Some available codes contain the framework for simulating a natural chemical system and estimating, within limits, the response of that system to environmental changes. By data-base enhancement and code development, this modeling technique can be even more usefully applied to a nuclear-waste repository. In particular, thermodynamic data on elements not presently in the data base but identified as being of particular hazard in the waste-repository system, need to be incorporated into the code to estimate the near-field as well as the far-field reactions during a hypothetical breach. A reaction-path-simulation code, which estimates the products of specific rock/water reactions, has been tested using basalt and ground water. Results show that the mass-transfer capabilities of the code will be useful in chemical-evolution studies and scenario analyses. The purpose of this report is to explain the status of geochemical modeling as it currently applies to the chemical system of a hypothetical nuclear-waste repository in basalt and to present the plan proposed for further developmet and application

Field-based tests of geochemical modeling codes: New Zealand hydrothermal systems

International Nuclear Information System (INIS)

Bruton, C.J.; Glassley, W.E.; Bourcier, W.L.

1993-12-01

Hydrothermal systems in the Taupo Volcanic Zone, North Island, New Zealand are being used as field-based modeling exercises for the EQ3/6 geochemical modeling code package. Comparisons of the observed state and evolution of the hydrothermal systems with predictions of fluid-solid equilibria made using geochemical modeling codes will determine how the codes can be used to predict the chemical and mineralogical response of the environment to nuclear waste emplacement. Field-based exercises allow us to test the models on time scales unattainable in the laboratory. Preliminary predictions of mineral assemblages in equilibrium with fluids sampled from wells in the Wairakei and Kawerau geothermal field suggest that affinity-temperature diagrams must be used in conjunction with EQ6 to minimize the effect of uncertainties in thermodynamic and kinetic data on code predictions

Agresividad, prosocialidad y estatus social: identificando perfiles admirados entre preadolescentes chilenos

Directory of Open Access Journals (Sweden)

Christian Berger

2011-01-01

Full Text Available Con base en la creciente evidencia de la asociación entre la agresividad y la prosocialidad con indicadores de estatus social, el presente estudio aborda la admiración entre pares adolescentes como una manera de operacionalizar el estatus y evalúa el potencial carácter funcional de estas conductas sociales. La hipótesis que guía este estudio es que en la medida en que la agresividad y la prosocialidad son características valoradas en el contexto de pares (con base en su asociación con el estatus, los adolescentes admirados, que pueden ejercer gran influencia sobre sus pares, serán aquellos que presenten este perfil. 274 estudiantes de 5º y 6º grado participaron del estudio. Los resultados muestran que la característica con mayor presencia entre los adolescentes admirados es la prosocialidad y luego la prominencia social. Sin embargo, se identifican dos perfiles de adolescentes admirados, que se distinguen principalmente por la agresividad, el perfil "fuerte" incluye además de la prosocialidad y la prominencia social altos puntajes en agresividad y popularidad, mientras que el perfil denominado "modelo" integra además de la prosocialidad y la prominencia social niveles muy bajos de agresividad y puntajes promedio en popularidad. Se identifican además diferencias de género en estos perfiles. Estos resultados son discutidos desde la perspectiva de las relaciones de pares y las posibles implicancias para el desarrollo tanto individual como grupal de los y las adolescentes.

New chronological and geochemical constraints on the genesis and geological evolution of Ponza and Palmarola Volcanic Islands (Tyrrhenian Sea, Italy)

Science.gov (United States)

Cadoux, Anita; Pinti, Daniele L.; Aznar, Cyril; Chiesa, Sergio; Gillot, Pierre-Yves

2005-04-01

. Palmarola volcanics represent a transitional magmatism: although a preserved collisional geochemical imprint, they show geochemical features approaching those of anorogenic lavas erupted in a within-plate context. The change of magmatism evidenced in this study can be related to the tectonic evolution of the area. Indeed, Hf, Ta and Rb contents suggest that the oldest Pliocene rhyolites of Ponza would emplace in a syn- to late-collisional setting, while the younger Pleistocene rhyolites of Palmarola would be emplaced in a post-collisional setting in which the orogenic character (Th/Ta) decreases and mantle influence (Nb/Ta) increases. Geochemical modeling strongly suggests that the Palmarola rhyolites represent the waning stages of a subduction-related magmatism. The K-Ar datings allow us to estimate precisely the transition of magmatism to last less than 1.3 Ma. The transitional magmas may be the result of the upwelling of asthenospheric mantle inducing melting of a metasomatized lithospheric mantle and the mixing between these two sources. This upwelling could occur during the extension of the Tyrrhenian basin, caused by the slab retreat and steepening, or during a process of slab break-off starting in the Pliocene.

Definición cuantitativa de perfiles profesionales en ingeniería

Directory of Open Access Journals (Sweden)

Marla Constanza Barrera Botero

2015-05-01

Full Text Available Un perfil profesional es un conjunto de conocimientos y habilidades. En el presente artículo se propone una metodología para definir perfiles profesionales basada en una evaluación cualitativa de habilidades y conocimientos asociados con un plan de estudios de ingeniería. Esta metodología puede ser usada para evaluar la flexibilidad curricular, es decir, si el plan de estudios ofrece a los estudiantes enfoques y rutas de aprendizaje que sean diversos y flexibles. Aquí se describe un modelo matemático que permite calcular el grado de satisfacción logrado por un estudiante con respecto a uno o varios perfiles. Esta propuesta ha sido aplicada en el programa de pregrado de Ingeniería Eléctrica de la Universidad Nacional de Colombia.

Synthesizing Earth's geochemical data for hydrogeochemical analysis

Science.gov (United States)

Brantley, S. L.; Kubicki, J.; Miller, D.; Richter, D.; Giles, L.; Mitra, P.

2007-12-01

For over 200 years, geochemical, microbiological, and chemical data have been collected to describe the evolution of the surface earth. Many of these measurements are data showing variations in time or in space. To forward predict hydrologic response to changing tectonic, climatic, or anthropogenic forcings requires synthesis of these data and utilization in hydrogeochemical models. Increasingly, scientists are attempting to synthesize such data in order to make predictions for new regions or for future time periods. However, to make such complex geochemical data accessible requires development of sophisticated cyberinfrastructures that both invite uploading as well as usage of data. Two such cyberinfrastructure (CI) initiatives are currently developing, one to invite and promote the use of environmental kinetics data (laboratory time course data) through ChemxSeer, and the other to invite and promote the use of spatially indexed geochemical data for the Earth's Critical Zone through CZEN.org. The vision of these CI initiatives is to provide cyber-enhanced portals that encourage domain scientists to upload their data before publication (in private cyberspace), and to make these data eventually publicly accessible (after an embargo period). If the CI can be made to provide services to the domain specialist - e.g. to provide data analysis services or data comparison services - we envision that scientists will upload data. In addition, the CI can promote the use and comparison of datasets across disciplines. For example, the CI can facilitate the use of spatially indexed geochemical data by scientists more accustomed to dealing with time-course data for hydrologic flow, and can provide user-friendly interfaces with CI established to facilitate the use of hydrologic data. Examples of the usage of synthesized data to predict soil development over the last 13ky and its effects on active hydrological flow boundaries in surficial systems will be discussed for i) a N

Perfil de salud del gamín

OpenAIRE

Ospina, Bernarda; Soto Vélez, Cecilia; Betancur Taborda, Ceneida; Jaramillo Vélez, Diva Estela; Zuloaga Posada, Luz; Berrio Castro, Vivian Adela; Escobar, Juan Darío

1992-01-01

En el presente estudio se analizó el perfil de salud del gamín de medellin en 98 niños, su situación sociofamiliar, el consumo de sustancias psicoactivas, la morbilidad general y la salud mental y oral.

Methods for geochemical analysis

Science.gov (United States)

Baedecker, Philip A.

1987-01-01

The laboratories for analytical chemistry within the Geologic Division of the U.S. Geological Survey are administered by the Office of Mineral Resources. The laboratory analysts provide analytical support to those programs of the Geologic Division that require chemical information and conduct basic research in analytical and geochemical areas vital to the furtherance of Division program goals. Laboratories for research and geochemical analysis are maintained at the three major centers in Reston, Virginia, Denver, Colorado, and Menlo Park, California. The Division has an expertise in a broad spectrum of analytical techniques, and the analytical research is designed to advance the state of the art of existing techniques and to develop new methods of analysis in response to special problems in geochemical analysis. The geochemical research and analytical results are applied to the solution of fundamental geochemical problems relating to the origin of mineral deposits and fossil fuels, as well as to studies relating to the distribution of elements in varied geologic systems, the mechanisms by which they are transported, and their impact on the environment.

Perfil docente para alumnos/as con altas capacidades

Directory of Open Access Journals (Sweden)

María Leonor Conejeros-Solar

2013-01-01

Full Text Available El presente artículo tiene por objeto determinar un perfil de competencias docentes construido desde la percepción de estudiantes con altas capacidades pertenecientes a un programa universitario para talentos académicos. Se utiliza una metodología cualitativa con una estrategia documental de carácter retrospectivo. Los resultados indican que los estudiantes realizan una evaluación profunda sobre la docencia, incluyendo elementos pedagógicos como flexibilidad, ritmo e integración teoría-práctica. Las percepciones de los estudiantes, poco incorporadas en discusiones relativas a la enseñanza, permiten repensar y delinear un perfil de las competencias docentes relevadas para un trabajo pedagógico efectivo con talentosos en el aula.

Coupling between a geochemical model and a transport model of dissolved elements

International Nuclear Information System (INIS)

Jacquier, P.

1988-10-01

In order to assess the safety analysis of an underground repository, the transport of radioelements in groundwater and their interactions with the geological medium are modelled. The objective of this work is the setting up and experimental validation of the coupling of a geochemical model with a transport model of dissolved elements. A laboratory experiment was developed at the CEA center of Cadarache. Flow-through experiments were carried out on columns filled with crushed limestone, where several inflow conditions were taken into account as the temperature, the presence of a pollutant (strontium chloride) at different concentrations. The results consist of the evolution of the chemical composition of the water at the outlet of the column. The final aim of the study is to explain these results with a coupled model where geochemical and transport phenomena are modelled in a two-step procedure. This code, called STELE, was built by introducing a geochemical code, CHIMERE, into an existing transport code, METIS. At this stage, the code CHIMERE can take into account: any chemical reaction in aqueous phase (complexation, acid-base reaction, redox equilibrium), dissolution-precipitation of minerals and solid phases, dissolution-degassing of gas. The paper intends to describe the whole process leading to the coupling which can be forecasted over the next years between geochemical and transport models

Recolectores, verificadores y reflexivos: perfiles de la competencia informacional en estudiantes universitarios de primer semestre

OpenAIRE

Harold Castañeda-Peña; Liliana González Niño; Gloria Marciales Vivas; Jorge Winston Barbosa Chacón; Juan Carlos Barbosa Herrera

2010-01-01

Artículo de investigación que explora perfiles de la competencia informacional en estudiantes universitarios de primer semestre, a partir de un concepto renovado de competencia informacional desde la perspectiva sociocultural, donde se entiende perfil como una práctica habitual que es situada y variada. Se analiza el caso de 285 estudiantes provenientes de dos universidades colombianas, por medio de un instrumento observacional (cuestionario de perfil, protocolos en voz alta y entrevistas). S...

Field-based tests of geochemical modeling codes usign New Zealand hydrothermal systems

International Nuclear Information System (INIS)

Bruton, C.J.; Glassley, W.E.; Bourcier, W.L.

1994-06-01

Hydrothermal systems in the Taupo Volcanic Zone, North Island, New Zealand are being used as field-based modeling exercises for the EQ3/6 geochemical modeling code package. Comparisons of the observed state and evolution of the hydrothermal systems with predictions of fluid-solid equilibria made using geochemical modeling codes will determine how the codes can be used to predict the chemical and mineralogical response of the environment to nuclear waste emplacement. Field-based exercises allow us to test the models on time scales unattainable in the laboratory. Preliminary predictions of mineral assemblages in equilibrium with fluids sampled from wells in the Wairakei and Kawerau geothermal field suggest that affinity-temperature diagrams must be used in conjunction with EQ6 to minimize the effect of uncertainties in thermodynamic and kinetic data on code predictions

Determinación de perfiles para rotores de compresores de tornillo con perfil simétrico. // Profiles determination for screw compressors rotors with symmetrical profile.

Directory of Open Access Journals (Sweden)

A. Rivera Torres

2005-05-01

Full Text Available Los compresores rotativos de tornillo, constituyeron el acontecimiento histórico más relevante del siglo XX en el campodel proceso de compresión. Dentro de los elementos fundamentales de los compresores rotativos de tornillo se encuentranlos rotores, los cuales tienen lóbulos o canales helicoidales con perfiles con formas simétricas o asimétricas.En este articulo se presenta un método para el diseño de los perfiles de rotores para compresores o bombas de tornillo, conperfil circular, a partir del empleo de una curva de cuarto orden y la condición de conjugación de los engranajes, sin incluirel empleo de cicloides en la generación de dichos perfiles, lográndose características similares a la de los perfiles SRM.Palabras claves: Rotores, rotor macho, rotor hembra._____________________________________________________________________________Abstract:Rotary screw compressors constitute the most relevant historic event of the twentieth century in the field of the process ofcompression. The most fundamental elements of rotary screw compressors are the rotors, which have helical lobes or canalsand symmetrical or asymmetrical profiles.This paper presents a method of circular profile design for screw compressors or pumps, based on fourth order curves andthe conjugation of gears, which does not include the application of cycloids in profile generation but have similarcharacteristics to SRM profiles.Key words: rotors, male rotor, female rotor.

Geochemical Investigations of Groundwater Stability

International Nuclear Information System (INIS)

Bath, Adrian

2006-05-01

groundwaters, and also by stable isotopes and uranium isotopes in secondary minerals. Information on timing of water and solute movements is important because it indicates any correlation with the timing of external events that might have perturbed and destabilised the groundwater system in the past, and allows a timescale to be estimated for the persistence of stable conditions. Data from a number of published site investigation projects and research programmes are reviewed to illustrate the patterns of geochemical data and the relationships between them, and how these are interpreted in terms of hydrodynamic stability. Data from Aespoe and Stripa and from exploratory boreholes at Finnsjoen and other sites in Sweden are compiled and discussed. Preliminary data from SKB's ongoing site investigations at Simpevarp/Laxemar and Forsmark are not considered in detail but their general similarities with Aespoe and Finnsjoen/SFR respectively are introduced into the discussion of geochemical evidence for groundwater stability in inland and coastal areas. Relevant data from Finnish sites including Olkiluoto, from the Whiteshell URL area in Canada, from Sellafield in the UK, and from the Tono area and URL in Japan are also summarised in appendices and discussed because they add further insights into the interpretation of geochemical indicators for a range of geological environments. The compiled data provide only limited scope for comparison of groundwater evolution and stability between inland and coastal areas in Sweden, because of the patchiness of representative data especially from early site studies. The external changes that might have perturbed stable groundwater conditions in the past are glaciation (i.e. melt water, mechanical loading/unloading and permafrost) and varying sea water infiltration at coastal sites due to changes in palaeo-Baltic and isostatic conditions. The present distributions of palaeo-Baltic sea water in groundwaters at coastal sites vary, reflecting local

Alaska Geochemical Database (AGDB)-Geochemical data for rock, sediment, soil, mineral, and concentrate sample media

Science.gov (United States)

Granitto, Matthew; Bailey, Elizabeth A.; Schmidt, Jeanine M.; Shew, Nora B.; Gamble, Bruce M.; Labay, Keith A.

2011-01-01

The Alaska Geochemical Database (AGDB) was created and designed to compile and integrate geochemical data from Alaska in order to facilitate geologic mapping, petrologic studies, mineral resource assessments, definition of geochemical baseline values and statistics, environmental impact assessments, and studies in medical geology. This Microsoft Access database serves as a data archive in support of present and future Alaskan geologic and geochemical projects, and contains data tables describing historical and new quantitative and qualitative geochemical analyses. The analytical results were determined by 85 laboratory and field analytical methods on 264,095 rock, sediment, soil, mineral and heavy-mineral concentrate samples. Most samples were collected by U.S. Geological Survey (USGS) personnel and analyzed in USGS laboratories or, under contracts, in commercial analytical laboratories. These data represent analyses of samples collected as part of various USGS programs and projects from 1962 to 2009. In addition, mineralogical data from 18,138 nonmagnetic heavy mineral concentrate samples are included in this database. The AGDB includes historical geochemical data originally archived in the USGS Rock Analysis Storage System (RASS) database, used from the mid-1960s through the late 1980s and the USGS PLUTO database used from the mid-1970s through the mid-1990s. All of these data are currently maintained in the Oracle-based National Geochemical Database (NGDB). Retrievals from the NGDB were used to generate most of the AGDB data set. These data were checked for accuracy regarding sample location, sample media type, and analytical methods used. This arduous process of reviewing, verifying and, where necessary, editing all USGS geochemical data resulted in a significantly improved Alaska geochemical dataset. USGS data that were not previously in the NGDB because the data predate the earliest USGS geochemical databases, or were once excluded for programmatic reasons

[Initial antiretroviral treatment in human immunodeficiency virus-infected patients in Spain: Decisions made in relation to particular immunovirological characteristics (PERFIL-es study)].

Science.gov (United States)

Viciana, Pompeyo; Ocampo, Antonio; Hevia, Henar; Palazuelos, Marta; Ledesma, Francisco

2014-02-01

The purpose of Perfil-es study was to identify the proportion of patients starting ARV treatment based on NNRTIs or PI/r, and to identify the variables involved in the therapeutic decision-making in standard clinical practice. An observational retrospective study performed in 65 Spanish hospitals. Was a total of 1,687 starts: 53% with NNRTI-based regimen and 42% with PI/r, and of the 642 patients analyzed, 72% had a CD4 count<350 cells/μl. The initiation of ARV treatment is still late in Spain. NNRTIs are the more frequent choice, although PI/r plays an important role. Copyright © 2012 Elsevier España, S.L. All rights reserved.

Geochemical evolution of groundwater in the Western Delta region of River Godavari, Andhra Pradesh, India

Science.gov (United States)

Nageswara Rao, P. V.; Appa Rao, S.; Subba Rao, N.

2017-05-01

The present study on geochemical evolution of groundwater is taken up to assess the controlling processes of water chemistry in the Western Delta region of the River Godavari (Andhra Pradesh), which is one of the major rice-producing centers in India. The study region is underlain by coarse sand with black clay (buried channels), black silty clay of recent origin (floodplain) and gray/white fine sand of modern beach sediment of marine source (coastal zone), including brown silty clay with fine sand (paleo-beach ridges). Groundwater is mostly brackish and very hard. It is characterized by Na+ > Mg2+ > Ca2+:HCO3 - > Cl- > SO4 2- > NO3 -, Na+ > Mg2+ > Ca2+:Cl- > HCO3 - > SO4 2-, and Mg2+ > Na+ > Ca2+ > or Cl- > or > SO4 2- facies. The ionic relations (Ca2+ + Mg2+:HCO3 -, Ca2+ + Mg2+:SO4 2- + HCO3 -, Na+ + K+:TC, Na+ + K+:Cl- + SO4 2-, HCO3 -:TC, HCO3 -:Ca2+ + Mg2+, Na+:Cl- and Na+:Ca2+) indicate that the rock weathering, mineral dissolution, evaporation and ion exchange are the processes to control the aquifer chemistry. Anthropogenic and marine sources are also the supplementary factors for brackish water quality. These observations are further supported by Gibbs mechanisms that control the water chemistry. Thus, the study suggests that the initial quality of groundwater of geogenic origin has been subsequently modified by the influences of anthropogenic and marine sources.

Petro-geochemical constraints on the source and evolution of magmas at El Misti volcano (Peru)

Science.gov (United States)

Rivera, Marco; Martin, Hervé; Le Pennec, Jean-Luc; Thouret, Jean-Claude; Gourgaud, Alain; Gerbe, Marie-Christine

2017-01-01

El Misti volcano, a large and hazardous edifice of the Andean Central Volcanic Zone (CVZ) of southern Peru, consists of four main growth stages. Misti 1 (> 112 ka) is an old stratovolcano partly concealed by two younger stratocones (Misti 2, 112-40 ka; Misti 3, 38-11 ka), capped in turn by a recent summit cone (Misti 4, Peru. Geochemical evidence indicates that magmatic evolution is mostly controlled by Assimilation-Fractional Crystallisation (AFC) mechanisms. Modelling reveals a mass-assimilated/mass-fractionated ratio (ρ) ≤ 2.2, which suggests an assimilated crust fraction below 14 wt.% on average. Our isotopic data clearly identify the Proterozoic "Charcani gneiss" basement as the main contaminant. Both contamination and assimilation processes peaked at 30 wt.%, during the Misti 3 stage when rhyolites were generated. We ascribe the general depletion in HREE and Y and elevated La/Yb and Sr/Y ratios in El Misti samples to the enrichment of the mantle wedge source of the parental magmas by a felsic melt of adakitic composition and hydrous fluids. Our work highlights that El Misti's magmatic system has remained relatively homogeneous since at least 0.12 Ma, with a marked influence of the contaminating crust in the Late Pleistocene Misti 3 stage, which resulted in highly explosive eruptions. Andesitic-dacitic compositions are dominant in the Holocene and historical Misti 4 stage, and are expected for future volcanic events at El Misti.

Solid phase evolution in the Biosphere 2 hillslope experiment as predicted by modeling of hydrologic and geochemical fluxes

Directory of Open Access Journals (Sweden)

K. Dontsova

2009-12-01

Full Text Available A reactive transport geochemical modeling study was conducted to help predict the mineral transformations occurring over a ten year time-scale that are expected to impact soil hydraulic properties in the Biosphere 2 (B2 synthetic hillslope experiment. The modeling sought to predict the rate and extent of weathering of a granular basalt (selected for hillslope construction as a function of climatic drivers, and to assess the feedback effects of such weathering processes on the hydraulic properties of the hillslope. Flow vectors were imported from HYDRUS into a reactive transport code, CrunchFlow2007, which was then used to model mineral weathering coupled to reactive solute transport. Associated particle size evolution was translated into changes in saturated hydraulic conductivity using Rosetta software. We found that flow characteristics, including velocity and saturation, strongly influenced the predicted extent of incongruent mineral weathering and neo-phase precipitation on the hillslope. Results were also highly sensitive to specific surface areas of the soil media, consistent with surface reaction controls on dissolution. Effects of fluid flow on weathering resulted in significant differences in the prediction of soil particle size distributions, which should feedback to alter hillslope hydraulic conductivities.

TAPIR--Finnish national geochemical baseline database.

Science.gov (United States)

Jarva, Jaana; Tarvainen, Timo; Reinikainen, Jussi; Eklund, Mikael

2010-09-15

In Finland, a Government Decree on the Assessment of Soil Contamination and Remediation Needs has generated a need for reliable and readily accessible data on geochemical baseline concentrations in Finnish soils. According to the Decree, baseline concentrations, referring both to the natural geological background concentrations and the diffuse anthropogenic input of substances, shall be taken into account in the soil contamination assessment process. This baseline information is provided in a national geochemical baseline database, TAPIR, that is publicly available via the Internet. Geochemical provinces with elevated baseline concentrations were delineated to provide regional geochemical baseline values. The nationwide geochemical datasets were used to divide Finland into geochemical provinces. Several metals (Co, Cr, Cu, Ni, V, and Zn) showed anomalous concentrations in seven regions that were defined as metal provinces. Arsenic did not follow a similar distribution to any other elements, and four arsenic provinces were separately determined. Nationwide geochemical datasets were not available for some other important elements such as Cd and Pb. Although these elements are included in the TAPIR system, their distribution does not necessarily follow the ones pre-defined for metal and arsenic provinces. Regional geochemical baseline values, presented as upper limit of geochemical variation within the region, can be used as trigger values to assess potential soil contamination. Baseline values have also been used to determine upper and lower guideline values that must be taken into account as a tool in basic risk assessment. If regional geochemical baseline values are available, the national guideline values prescribed in the Decree based on ecological risks can be modified accordingly. The national geochemical baseline database provides scientifically sound, easily accessible and generally accepted information on the baseline values, and it can be used in various

Geochemical of clay formations : study of Spanish clay REFERENCE

International Nuclear Information System (INIS)

Turrero, M. J.; Pena, J.

2003-01-01

Clay rocks are investigated in different international research programs in order to assess its feasibility for the disposal of high level radioactive wastes. This is because different sepcific aspects: they have low hydraulic conductivity (10''-11-10''-15 m/s), a high sorption capacity, self-sealing capacity of facults and discontinuities and mechanical resistance. Several research programs on clay formations are aimed to study the chemistry of the groundwater and the water-rock reactions that control it: e. g. Boom Clay (Mol, Belgium), Oxford Clay /Harwell, United Kingdom), Toarcian Clay (Tournemire, France), Palfris formation (Wellenberg, Switzerland), Opalinus Clay (Bure, France). Based on these studies, considerable progress in the development of techniques for hydrologic, geochemical and hydrogeochemical characterization of mudstones has been accomplished (e. g. Beaufais et al. 1994, De Windt el al. 1998. Thury and Bossart 1999, Sacchi and Michelot 2000) with important advances in the knowledge of geochemical process in these materials (e. g. Reeder et al. 1993, Baeyens and Brandbury 1994, Beaucaire et al. 2000, Pearson et al., 2003).Furtermore, geochemical modeling is commonly used to simulate the evolution of water chemistry and to understand quantitatively the processes controlling the groundwater chemistry (e. g. Pearson et al. 1998, Tempel and Harrison 2000, Arcos et al., 2001). The work presented here is part of a research program funded by Enresa in the context of its R and D program. It is focused on the characterization of a clay formation (reference Argillaceous Formation, RAF) located within the Duero Basin (north-centralSpain). The characterisation of th ephysical properties,, fluid composition, mineralogy, water-rock reaction processes, geochemical modelling and sorption properties of the clays from the mentioned wells is the main purpose of this work. (Author)

Perfiles motivacionales de estudiantes universitarios. Procesos de estudio y satisfacción con la vida

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Juan Antonio Moreno\\u2010Murcia

2015-01-01

Full Text Available El objetivo de este trabajo ha sido determinar los diferentes perfiles motivacionales en estudiantes universitarios y ver su relación con los procesos de estudio (superficial y profundo así como con la satisfacción que tiene el estudiante con su vida en general. La muestra estuvo compuesta por 431 estudiantes universitarios (202 hombres y 220 mujeres con una edad media de 22 años (DT = 2.41. Los instrumentos utilizados fueron la Escala de Motivación Académica, Cuestionario Revisado de Procesos de Estudio y la Escala de Satisfacción para la Vida. Se calcularon los estadísticos descriptivos (medias y desviaciones típicas, la consistencia interna y se realizó un análisis clúster y de varianza univariados. Los resultados muestran dos perfiles motivacionales, un perfil más autodeterminado con puntuaciones bajas en desmotivación y altas principalmente en motivación intrínseca de conocimiento, de logro y regulación identificada y un perfil menos autodeterminado con puntuaciones altas en desmotivación y moderadas en el resto de variables motivacionales. Además, los estudiantes pertenecientes al perfil más autodeterminado presentaron menor puntuación en los procesos de estudio superficial, una mayor puntuación en el proceso de estudio profundo estando más satisfechos con la vida a diferencia de los estudiantes del perfil menos autodeterminado.

EL PERFIL DEL EDITOR DE JUEGOS DE ROL

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Héctor Sevillano Pareja

2010-11-01

Full Text Available El presente trabajo estudia y analiza, a través de diversas encuestas personalizadas, el perfil tipo que presentan los profesionales que se dedican al arte de editar libros de rol en España.

Perfiles motivacionales de usuarios de servicios deportivos públicos y privados

OpenAIRE

Nuviala Nuviala, Alberto; Universidad Pablo de Olavide; Gómez-López, Manuel; Universidad de Murcia; Grao-Cruces, Alberto; Universidad Pablo de Olavide; Granero-Gallegos, Antonio; Universidad de Murcia; Nuviala Nuviala, Román; Universidad Pablo de Olavide

2012-01-01

Las altas tasas de sedentarismo y abandono deportivo y la escasez de estudios sobre motivos de práctica en el ámbito de la actividad física no competitiva han generado la necesidad de llevar a cabo investigaciones que establezcan perfiles motivacionales de usuarios de servicios deportivos. La finalidad de esta investigación fue diferenciar los perfiles motivacionales con respecto a la práctica físico-deportiva y analizar su relación con variables sociodemográficas (edad y sexo). La muestra de...

Recolectores, verificadores y reflexivos: perfiles de la competencia informacional en estudiantes universitarios de primer semestre

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Harold Castañeda-Peña

2010-01-01

Full Text Available Artículo de investigación que explora perfiles de la competencia informacional en estudiantes universitarios de primer semestre, a partir de un concepto renovado de competencia informacional desde la perspectiva sociocultural, donde se entiende perfil como una práctica habitual que es situada y variada. Se analiza el caso de 285 estudiantes provenientes de dos universidades colombianas, por medio de un instrumento observacional (cuestionario de perfil, protocolos en voz alta y entrevistas. Se encuentra que el 55% de los estudiantes de primer año de una universidad con carreras profesionales tiende a recolectar información y que el 78% de los estudiantes de primer año de una universidad con carreras tecnológicas tiende a contrastar y verificar información, en tanto que sólo entre 3% y 4% tiende a manejar la información críticamente. Se discute que, al asumir una tarea académica, estos estudiantes vinculan sus prácticas de competencia informacional a sus propias historias de vida y escolares, y que la edad y los antecedentes académicos parecen influir en tales prácticas. Los casos analizados se ubican dentro de perfiles de competencia informacional: recolectores, verificadores y reflexivos. Estos perfiles no son fijos, sino más bien fluidos, y se concretan de manera diferente según la tarea académica. Se recomienda realizar estudios de perfiles informacionales en estudiantes tanto de secundaria como universitarios, para diseñar políticas educativas sobre competencia informacional.

Geochemical Investigations of Groundwater Stability

Energy Technology Data Exchange (ETDEWEB)

Bath, Adrian [Intellisci Ltd., Loughborough (United Kingdom)

2006-05-15

groundwaters, and also by stable isotopes and uranium isotopes in secondary minerals. Information on timing of water and solute movements is important because it indicates any correlation with the timing of external events that might have perturbed and destabilised the groundwater system in the past, and allows a timescale to be estimated for the persistence of stable conditions. Data from a number of published site investigation projects and research programmes are reviewed to illustrate the patterns of geochemical data and the relationships between them, and how these are interpreted in terms of hydrodynamic stability. Data from Aespoe and Stripa and from exploratory boreholes at Finnsjoen and other sites in Sweden are compiled and discussed. Preliminary data from SKB's ongoing site investigations at Simpevarp/Laxemar and Forsmark are not considered in detail but their general similarities with Aespoe and Finnsjoen/SFR respectively are introduced into the discussion of geochemical evidence for groundwater stability in inland and coastal areas. Relevant data from Finnish sites including Olkiluoto, from the Whiteshell URL area in Canada, from Sellafield in the UK, and from the Tono area and URL in Japan are also summarised in appendices and discussed because they add further insights into the interpretation of geochemical indicators for a range of geological environments. The compiled data provide only limited scope for comparison of groundwater evolution and stability between inland and coastal areas in Sweden, because of the patchiness of representative data especially from early site studies. The external changes that might have perturbed stable groundwater conditions in the past are glaciation (i.e. melt water, mechanical loading/unloading and permafrost) and varying sea water infiltration at coastal sites due to changes in palaeo-Baltic and isostatic conditions. The present distributions of palaeo-Baltic sea water in groundwaters at coastal sites vary, reflecting

Coupled geochemical and solute transport code development

International Nuclear Information System (INIS)

Morrey, J.R.; Hostetler, C.J.

1985-01-01

A number of coupled geochemical hydrologic codes have been reported in the literature. Some of these codes have directly coupled the source-sink term to the solute transport equation. The current consensus seems to be that directly coupling hydrologic transport and chemical models through a series of interdependent differential equations is not feasible for multicomponent problems with complex geochemical processes (e.g., precipitation/dissolution reactions). A two-step process appears to be the required method of coupling codes for problems where a large suite of chemical reactions must be monitored. Two-step structure requires that the source-sink term in the transport equation is supplied by a geochemical code rather than by an analytical expression. We have developed a one-dimensional two-step coupled model designed to calculate relatively complex geochemical equilibria (CTM1D). Our geochemical module implements a Newton-Raphson algorithm to solve heterogeneous geochemical equilibria, involving up to 40 chemical components and 400 aqueous species. The geochemical module was designed to be efficient and compact. A revised version of the MINTEQ Code is used as a parent geochemical code

Perfiles de personalidad relacionados con la vulnerabilidad del deportista a lesionarse

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Joel Manuel Prieto Andreu

2014-01-01

Full Text Available En el ámbito deportivo competitivo se hace necesaria una aproximación al perfil de vulnerabilidad psicológico a la lesión del deportista. La muestra total del estudio fue de 285 hombres (23 no lesionados y 168 mujeres (24 no lesionadas, los hombres tenían una media de edad de 21.77 años y las mujeres de 20.55 años. La muestra estuvo compuesta por jugadores de deportes individuales (tenis, atletismo y natación y por jugadores de deportes colectivos (fútbol, baloncesto y balonmano pertenecientes a distintos Clubes Deportivos de la Comunidad Valenciana. Para la evaluación de la ansiedad competitiva, se utilizó el Sport Competitive Anxiety Test (SCAT; para evaluar la personalidad resistente, se utilizó la escala EPR; para evaluar la competitividad, se utilizó la escala de Competitividad-10; y, para la evaluación de las lesiones, se utilizó una hoja de registro específica. El diseño del estudio fue descriptivo, observacional y correlacional. El estudio partió de la siguiente hipótesis: el número de lesiones aumentará cuando menor sea la personalidad resistente y la motivación orientada al éxito, y cuando mayor sea la ansiedad competitiva y la motivación orientada a evitar el fracaso. Se planteó como objetivo analizar las diferencias en el número de lesiones entre los deportistas que presentaban un perfil de vulnerabilidad a la lesión frente a los que no presentaban dicho perfil. Según la fundamentación teórica, situarse en dicho perfil implicaría lesionarse más, sin embargo, los resultados del estudio indican que los hombres con perfil de vulnerabilidad a la lesión (los que se lesionarían más tuvieron menor número de lesiones moderadas, totales e índice de lesión. Se discuten los resultados y se señalan algunas conclusiones del estudio.

Application of cluster analysis to geochemical compositional data for identifying ore-related geochemical anomalies

Science.gov (United States)

Zhou, Shuguang; Zhou, Kefa; Wang, Jinlin; Yang, Genfang; Wang, Shanshan

2017-12-01

Cluster analysis is a well-known technique that is used to analyze various types of data. In this study, cluster analysis is applied to geochemical data that describe 1444 stream sediment samples collected in northwestern Xinjiang with a sample spacing of approximately 2 km. Three algorithms (the hierarchical, k-means, and fuzzy c-means algorithms) and six data transformation methods (the z-score standardization, ZST; the logarithmic transformation, LT; the additive log-ratio transformation, ALT; the centered log-ratio transformation, CLT; the isometric log-ratio transformation, ILT; and no transformation, NT) are compared in terms of their effects on the cluster analysis of the geochemical compositional data. The study shows that, on the one hand, the ZST does not affect the results of column- or variable-based (R-type) cluster analysis, whereas the other methods, including the LT, the ALT, and the CLT, have substantial effects on the results. On the other hand, the results of the row- or observation-based (Q-type) cluster analysis obtained from the geochemical data after applying NT and the ZST are relatively poor. However, we derive some improved results from the geochemical data after applying the CLT, the ILT, the LT, and the ALT. Moreover, the k-means and fuzzy c-means clustering algorithms are more reliable than the hierarchical algorithm when they are used to cluster the geochemical data. We apply cluster analysis to the geochemical data to explore for Au deposits within the study area, and we obtain a good correlation between the results retrieved by combining the CLT or the ILT with the k-means or fuzzy c-means algorithms and the potential zones of Au mineralization. Therefore, we suggest that the combination of the CLT or the ILT with the k-means or fuzzy c-means algorithms is an effective tool to identify potential zones of mineralization from geochemical data.

PERFIL DE LIDERANÇA E TOMADA DE DECISÃO

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Eduardo Botti Abbade

2009-04-01

Full Text Available O objetivo geral deste estudo foi o de identificar o estilo de liderança, perfil comportamental e decisório dos dirigentes das empresas do Distrito Industrial de Santa Maria / RS. Este estudo se configura como sendo uma pesquisa de levantamento (survey descritiva onde foram selecionadas 14 empresas, das 20 existentes, localizadas no Distrito Industrial do município de Santa Maria-RS. Com o objetivo de definir o perfil gerencial dos pesquisados, esta investigação utilizou-se de perspectivas psicológicas, de observação, de decisão e de aprendizagem. Os entrevistados correspondem a indivíduos que possuem um perfil com tendências a enfatizar detalhes e fatos, possuem foco no curto prazo e são muito realistas. Costumam elaborar regras e regulamentos para o julgamento do desempenho. Sugeremse para estudos futuros que seja realizado estudos onde se proponha um cruzamento entre os perfis observados com demais aspectos organizacionais como clima, cultura e comunicação organizacional. Propõe-se também que seja realizada a pesquisa com uma amostra mais abrangente. Aconselha-se que seja realizada a entrevista com gestores ou responsáveis de todas as áreas das empresas pesquisadas, para que se possam analisar perfis de gestores com diferentes competências e atribuições na mesma organização.

On the dynamics and the geochemical mechanism of the evolution of the continental crust. 1

International Nuclear Information System (INIS)

Wetzel, K.

1983-01-01

An investigation of the isotopic composition of oxygen in the continental crust, in the oceans, in the oceanic crust and in the upper mantle shows the dynamics of plate tectonics and continental growthto be more or less constant during the last three or four aeons independent on the geochemical mechanism of continental growth. (author)

The chemical evolution of a travertine-depositing stream: Geochemical processes and mass transfer reactions

Science.gov (United States)

Lorah, Michelle M.; Herman, Janet S.

1988-01-01

This field study focuses on quantitatively defining the chemical changes occurring in Falling Spring Creek, a travertine-depositing stream located in Alleghany County, Virginia. The processes of CO2outgassing and calcite precipitation or dissolution control the chemical evolution of the stream. The observed chemical composition of the water was used with the computerized geochemical model WATEQF to calculate aqueous speciation, saturation indices, and CO2 partial pressure values. Mass balance calculations were performed to obtain mass transfers of CO2 and calcite. Reaction times, estimated from stream discharge, were used with the mass transfer results to calculate rates of CO2, outgassing and calcite precipitation between consecutive sampling points. The stream, which is fed by a carbonate spring, is supersaturated with respect to CO2 along the entire 5.2-km flow path. Outgassing of CO2 drives the solution to high degrees of supersaturation with respect to calcite. Metabolic uptake of CO2 by photosynthetic plants is insignificant, because the high supply rate of dissolved carbon dioxide and the extreme agitation of the stream at waterfalls and rapids causes a much greater amount of inorganic CO2 outgassing to occur. Calcite precipitation is kinetically inhibited until near the crest of a 20-m vertical waterfall. Calcite precipitation rates then reach a maximum at the waterfall where greater water turbulence allows the most rapid escape of CO2. Physical evidence for calcite precipitation exists in the travertine deposits which are first observed immediately above the waterfall and extend for at least 1.0 km below the falls. Net calcite precipitation occurs at all times of the year but is greatest during low-flow conditions in the summer and early fall.

Factors controlling the geochemical evolution of fumarolic encrustations, Valley of Ten Thousand Smokes, Alaska

Science.gov (United States)

Kodosky, L.G.; Keith, T.E.C.

1993-01-01

Factor and canonical correlation analysis of geochemical data from eight fossil fumaroles suggest that six major factors controlled the formation and evolution of fumarolic encrustations on the 1912 ash-flow sheet in the Valley of Ten Thousand Smokes (VTTS). The six-factor solution model explains a large proportion (low of 74% for Ni to high of 99% for Si) of the individual element data variance. Although the primary fumarolic deposits have been degraded by secondary alteration reactions and up to 75 years of weathering, the relict encrustations still preserve a signature of vapor-phase element transport. This vapor-phase transport probably occurred as halide or oxyhalide species and was significant for As, Sb and Br. At least three, and possibly four, varied temperature leaching events affected the fumarolic deposits. High-temperature gases/liquids heavily altered the ejecta glass and mineral phases adjacent to the fumarolic conduit. As the fumaroles cooled. Fe-rich acidic condensate leached the ejecta and primary fumarolic deposits and resulted in the subsequent precipitation of Fe-hydroxides and/or Fe-oxides. Low- to ambient-temperature leaching and hydration reactions generated abundant hydrated amorphous phases. Up to 87% of the individual element data variance is apparently controlled by the chemistry of the ejecta on which the relict encrustations are found. This matrix chemistry factor illustrates that the primary fumarolic minerals surrounding the active VTTS vents observed by earlier workers have been effectively removed by the dissolution reactions. Element enrichment factors calculated for the VTTS relict encrustations support the statistical factor interpretations. On the average, the relict encrustations are enriched, relative to visibly unaltered matrix protolith, in As, Br, Cr, Sb, Cu, Ni, Pb, Fe, and LOI (an indirect measure of sample H2O content). ?? 1993.

Geochemical effects on the behavior of LLW radionuclides in soil/groundwater environments

Energy Technology Data Exchange (ETDEWEB)

Krupka, K.M.; Sterne, R.J. [Pacific Northwest Lab., Richland, WA (United States)

1995-12-31

Assessing the migration potential of radionuclides leached from low-level radioactive waste (LLW) and decommissioning sites necessitates information on the effects of sorption and precipitation on the concentrations of dissolved radionuclides. Such an assessment requires that the geochemical processes of aqueous speciation, complexation, oxidation/reduction, and ion exchange be taken into account. The Pacific Northwest National Laboratory (PNNL) is providing technical support to the U.S. Nuclear Regulatory Commission (NRC) for defining the solubility and sorption behavior of radionuclides in soil/ground-water environments associated with engineered cementitious LLW disposal systems and decommissioning sites. Geochemical modeling is being used to predict solubility limits for radionuclides under geochemical conditions associated with these environments. The solubility limits are being used as maximum concentration limits in performance assessment calculations describing the release of contaminants from waste sources. Available data were compiled regarding the sorption potential of radionuclides onto {open_quotes}fresh{close_quotes} cement/concrete where the expected pH of the cement pore waters will equal to or exceed 10. Based on information gleaned from the literature, a list of preferred minimum distribution coefficients (Kd`s) was developed for these radionuclides. The K{sub d} values are specific to the chemical environments associated with the evolution of the compositions of cement/concrete pore waters.

El nuevo perfil profesional de los profesores de secundaria

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Gemma Tribó Travería

2008-01-01

Full Text Available El objetivo del artículo es definir el nuevo perfil profesional de los profesores de secundaria. Una de las debilidades del sistema educativo español es que ha cambiado el marco legal y no se ha aplicado un nuevo modelo de formación inicial a los docentes de secundaria. El debate sobre las competencias profesionales está en la base de la propuesta de las competencias específicas del profesor del futuro. Se insiste en la importancia de las prácticas profesionales en el proceso de adquisición y de desarrollo de las competencias profesionales. Se valora positivamente que el master de formación inicial del profesorado de secundaria tenga presente en su diseño este nuevo perfil competencial profesional.

Geochemical characterisation of Taal volcano-hydrothermal system and temporal evolution during continued phases of unrest (1991-2017)

Science.gov (United States)

Maussen, Katharine; Villacorte, Edgardo; Rebadulla, Ryan R.; Maximo, Raymond Patrick; Debaille, Vinciane; Bornas, Ma. Antonia; Bernard, Alain

2018-02-01

Taal volcano (Luzon Island, Philippines) has last erupted in 1977 but has known some periods of increased activity, characterised by seismic swarms, ground deformation, increased carbon dioxide flux and in some cases temperature anomalies and the opening of fissures. We studied major, trace element and sulphur and strontium isotopic composition of Taal lake waters and hot springs over a period of 25 years to investigate the geochemical evolution of Taal volcano's hydrothermal system and its response to volcanic unrest. Long-term evolution of Main Crater Lake (MCL) composition shows a slow but consistent decrease of acidity, SO4, Mg, Fe and Al concentrations and a trend from light to heavy sulphate, consistent with a general decrease of volcanic gases dissolving in the hydrothermal system. Na, K and Cl concentrations remain constant indicating a non-volcanic origin for these elements. Sulphate and strontium isotopic data suggest this neutral chloride-rich component represents input of geothermal water into Taal hydrothermal system. A significant deviation from the long-term baseline can be seen in two samples from 1995. That year, pH dropped from 2.6 to 2.2, F, Si and Fe concentrations increased and Na, K and Cl concentrations decreased. Sulphate was depleted in 34S and temperature was 4 °C above baseline level at the time of sampling. We attribute these changes to the shallow intrusion of a degassing magma body during the unrest in 1991-1994. More recent unrest periods have not caused significant changes in the geochemistry of Taal hydrothermal waters and are therefore unlikely to have been triggered by shallow magma intrusion. A more likely cause for these events is thus pressurisation of the hydrothermal reservoir by increasing degassing from a stagnant magma reservoir. Our study indicates that new magmatic intrusions that might lead to the next eruption of Taal volcano are expected to change the geochemistry of MCL in the same way as in 1994-1995, with the most

Geochemical evolution of Ngorongoro Caldera, Northern Tanzania: Implications for crust magma interaction

Science.gov (United States)

Mollel, Godwin F.; Swisher, Carl C.; Feigenson, Mark D.; Carr, Michael J.

2008-07-01

Ngorongoro Caldera is the largest and best-preserved of nine Plio-Pleistocene volcanoes that make-up the Ngorongoro Volcanic Highlands (NVH) complex situated at the southern bifurcation of Gregory Rift, part of the East African Rift system of northern Tanzania. We report here, major and trace element abundances, Sr-Nd-Pb isotope analyses and 40Ar/ 39Ar laser incremental-heating and total fusion ages on lava and tephra sampled from stratigraphic sections exposed within the Ngorongoro Caldera. Major and trace elements measured on samples collected from the Ngorongoro Caldera wall indicate a stratified magma chamber whose silicic top and basaltic bottom was inverted by sequential eruptions. Samples from the lower part of the exposed Ngorongoro Caldera wall are high in silica, alkalis and HFSE (High Field Strength Elements). The Zr, Nb and Hf concentrations are highly correlated with each other and decrease up-section, indicative of the extent of magma evolution. Modeling of major, trace as well as Sr, Nd and Pb isotope data suggests that assimilation fractional crystallization processes were essential in producing the observed geochemical variations. The Sr and Nd isotope ratios from the Ngorongoro samples are widely dispersed ( 87Sr/ 86Sr = 0.70405 to 0.70801, 143Nd/ 144Nd = 0.512205 to 0.512623) and Pb isotope ratios are consistent with previous studies: 206Pb/ 204Pb = 18.73 to 19.37, 207Pb/ 204Pb = 15.64 to 15.69, 208Pb/ 204Pb = 39.52 to 39.55. Although Sr isotopic ratios are similar to Oceanic Island Basalt (OIB), the more radiogenic samples ( 87Sr/ 86Sr > 0.705) from the lower part of the section suggest crust-magma interaction; this is supported by Ce/Pb ratios (Ngorongoro Caldera wall section yield 40Ar/ 39Ar ages of 2.25 ± 0.02 Ma to 2.01 ± 0.02 Ma, constraining a duration of volcanism of the order of ~ 240 kyr. These ages suggest correlation of a normal to reverse geomagnetic polarity transition measured in the Ngorongoro Caldera wall section with the ~ 2

Geochemical evolution processes and water-quality observations based on results of the National Water-Quality Assessment Program in the San Antonio segment of the Edwards aquifer, 1996-2006

Science.gov (United States)

Musgrove, MaryLynn; Fahlquist, Lynne; Houston, Natalie A.; Lindgren, Richard J.; Ging, Patricia B.

2010-01-01

As part of the National Water-Quality Assessment Program, the U.S. Geological Survey collected and analyzed groundwater samples during 1996-2006 from the San Antonio segment of the Edwards aquifer of central Texas, a productive karst aquifer developed in Cretaceous-age carbonate rocks. These National Water-Quality Assessment Program studies provide an extensive dataset of groundwater geochemistry and water quality, consisting of 249 groundwater samples collected from 136 sites (wells and springs), including (1) wells completed in the shallow, unconfined, and urbanized part of the aquifer in the vicinity of San Antonio (shallow/urban unconfined category), (2) wells completed in the unconfined (outcrop area) part of the regional aquifer (unconfined category), and (3) wells completed in and springs discharging from the confined part of the regional aquifer (confined category). This report evaluates these data to assess geochemical evolution processes, including local- and regional-scale processes controlling groundwater geochemistry, and to make water-quality observations pertaining to sources and distribution of natural constituents and anthropogenic contaminants, the relation between geochemistry and hydrologic conditions, and groundwater age tracers and travel time. Implications for monitoring water-quality trends in karst are also discussed. Geochemical and isotopic data are useful tracers of recharge, groundwater flow, fluid mixing, and water-rock interaction processes that affect water quality. Sources of dissolved constituents to Edwards aquifer groundwater include dissolution of and geochemical interaction with overlying soils and calcite and dolomite minerals that compose the aquifer. Geochemical tracers such as magnesium to calcium and strontium to calcium ratios and strontium isotope compositions are used to evaluate and constrain progressive fluid-evolution processes. Molar ratios of magnesium to calcium and strontium to calcium in groundwater typically

Perfiles clínicos y hemodinámicos en pacientes con falla cardiaca aguda

Directory of Open Access Journals (Sweden)

Luis Eduardo Calderón

2017-09-01

Conclusiones: la falla cardíaca aguda descompensada es el perfil de presentación clínica más común en nuestra población con dos tercios del total de casos. El perfil hemodinámico más frecuente fue el “caliente y húmedo” (Stevenson B, resultados que concuerdan con lo observado en estudios locales y registros internacionales.

Integrative Modeling of cap-rock Integrity in the Context of CO2 Storage: Evolution of Transport and Geochemical Properties and Impact on Performance and Safety Assessment

International Nuclear Information System (INIS)

Bildstein, O.; Credoz, A.; Jullien, M.; Kervevan, C.; Audigane, P.; Jacquemet, N.; Lagneau, V.; Delaplace, P.; Perfetti, E.

2010-01-01

The objective of the 'Geocarbone-INTEGRITE' project (2005-2008) was to develop a methodology to assess the integrity of the cap-rock involved in the geological storage of CO 2 . A specific work package of the project (WP5) was dedicated to the integration of (1) the phenomenology describing the evolution of the storage system with a focus on the mechanisms occurring in the cap-rock and at the interface with the cap-rock, and (2) the data obtained from the investigation of petrographical, geomechanical, and geochemical properties, before and after reaction with CO 2 -rich solutions, performed in the other work packages (WP1 to WP4). This knowledge was introduced in numerical models and specific safety scenarios were defined in order to assess the performance of the CO 2 storage system. The results of the modeling show that the injection of CO 2 can potentially have a significant effect on the cap-rock by changing the porosity due to the dissolution and precipitation of minerals, but that the impact is limited to a zone from several decimeters to several meters of the cap-rock close to the interface with the reservoir depending on whether the supercritical carbon dioxide (SC-CO 2 ) plume enters into the cap-rock and if fractures are present at this location. The methodology used in this project can be applied to a pilot site for the injection of CO 2 in the Paris Basin. A key aspect of the safety of such a facility will be to look at the coupling of geochemical alteration and the evolution of geomechanical properties in the short and medium terms (several hundreds of years). The challenge for the future will be to structure and apply the safety assessment methodology with an operational finality, in order to support the robustness of the transition step to CGS projects at the industrial scale. (authors)

Proceedings of the workshop on geochemical modeling

International Nuclear Information System (INIS)

1986-01-01

The following collection of papers was presented at a workshop on geochemical modeling that was sponsored by the Office of Civilian Radioactive Waste Management Program at the Lawrence Livermore National Laboratory (LLNL). The LLNL Waste Management Program sponsored this conference based on their belief that geochemical modeling is particularly important to the radioactive waste disposal project because of the need to predict the consequences of long-term water-rock interactions at the proposed repository site. The papers included in this volume represent a subset of the papers presented at the Fallen Leaf Lake Conference and cover a broad spectrum of detail and breadth in a subject that reflects the diverse research interests of the conference participants. These papers provide an insightful look into the current status of geochemical modeling and illustrate how various geochemical modeling codes have been applied to problems of geochemical interest. The emphasis of these papers includes traditional geochemical modeling studies of individual geochemical systems, the mathematical and theoretical development and refinement of new modeling capabilities, and enhancements of data bases on which the computations are based. The papers in this proceedings volume have been organized into the following four areas: Geochemical Model Development, Hydrothermal and Geothermal Systems, Sedimentary and Low Temperature Environments, and Data Base Development. The participants of this symposium and a complete list of the talks presented are listed in the appendices

Proceedings of the workshop on geochemical modeling

Energy Technology Data Exchange (ETDEWEB)

1986-01-01

The following collection of papers was presented at a workshop on geochemical modeling that was sponsored by the Office of Civilian Radioactive Waste Management Program at the Lawrence Livermore National Laboratory (LLNL). The LLNL Waste Management Program sponsored this conference based on their belief that geochemical modeling is particularly important to the radioactive waste disposal project because of the need to predict the consequences of long-term water-rock interactions at the proposed repository site. The papers included in this volume represent a subset of the papers presented at the Fallen Leaf Lake Conference and cover a broad spectrum of detail and breadth in a subject that reflects the diverse research interests of the conference participants. These papers provide an insightful look into the current status of geochemical modeling and illustrate how various geochemical modeling codes have been applied to problems of geochemical interest. The emphasis of these papers includes traditional geochemical modeling studies of individual geochemical systems, the mathematical and theoretical development and refinement of new modeling capabilities, and enhancements of data bases on which the computations are based. The papers in this proceedings volume have been organized into the following four areas: Geochemical Model Development, Hydrothermal and Geothermal Systems, Sedimentary and Low Temperature Environments, and Data Base Development. The participants of this symposium and a complete list of the talks presented are listed in the appendices.

Determinación del comportamiento bajo cargas concentradas de perfiles de lámina delgada ( MM

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Maritzabel Molina Herrera

2006-09-01

Full Text Available En el campo de la lámina delgada continuamente aparecen nuevos tipos de perfiles que son desarrollados con el objeto de mejorar los ya existentes. Un ejemplo de esto es la aparición del perfil M, elaborado para melorar la eficiencia a corte del perfil C y su resistencia al arrugamiento del alma por efecto de cargas concentradas. Teóricamente, se logra el objetivo de mejorar la resistencia a corte del perfil C y de algún modo su resistencia al arrugamiento del alma, pero debido a los dobleces generados en el alma (rigidizadores intermedios para acortar la longitud de pandeo, se producen comportamientos que desde el punto de vista de esfuerzos por flexión y deflexiones no pueden ser analizados con los fundamentos teóricos de la mecánica tradicional. Este comporta- miento se ve acentuado con la presencia de cargas concentradas. Por la razón expuesta anteriormente, a parte de la determinación de la resistencia teórica del perfil M (basada en el AISI 1996, se desarrollan pruebas sobre cuatro modelos de los que se obtienen tópicos como: carga máxima resistida, identificación visual del posible tipo de falla, deflexiones (centro de la luz y deformaciones unitarias (x, y, xy, y adicionalmente se elaboran modelos matemáticos simplificados y por elementos finitos (en el programa COSMOS/M, con el fin de hacer una revisión detallada del comportamiento de los esfuerzos y deformaciones en el perfil. La calibración de estos modelos se lleva a cabo con base en los resultados obtenidos de los ensayos. De otra parte, se hacen pruebas cíclicas balo cargas pseudoestáticas, con el objeto de estudiar el comportamiento histerético del perfil MM, con y sin rigidizadores.

Propuesta de un perfil profesional para el diseño del doctorado curricular colaborativo en estomatología

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Dadonim Vila Morales

2013-03-01

Full Text Available El perfil profesional constituye un modelo, una idealización de las características, conocimientos, habilidades que debe poseer el egresado de cualquier nivel de estudios tanto terciario como del cuarto nivel. La Facultad de Estomatología de la Universidad de Ciencias Médicas de La Habana ha estado trabajando en pro de desarrollar un doctorado curricular en ciencias estomatológicas. Esta investigación pedagógica tuvo como propósito analizar teóricamente la importancia del perfil profesional y proponer un diseño de perfil profesional para un doctorado curricular colaborativo en ciencias estomatológicas. Se realizó una revisión bibliográfica de los fundamentos teóricos-metodológicos del perfil profesional, se analizó su implementación en el diseño curricular. Se señaló la importancia de un perfil de egresado correctamente instrumentado como sustento teórico-pedagógico, socio-crítico.

The Earth's heterogeneous mantle a geophysical, geodynamical, and geochemical perspective

CERN Document Server

Khan, Amir

2015-01-01

This book highlights and discusses recent developments that have contributed to an improved understanding of observed mantle heterogeneities and their relation to the thermo-chemical state of Earth's mantle, which ultimately holds the key to unlocking the secrets of the evolution of our planet. This series of topical reviews and original contributions address 4 themes. Theme 1 covers topics in geophysics, including global and regional seismic tomography, electrical conductivity and seismic imaging of mantle discontinuities and heterogeneities in the upper mantle, transition zone and lower mantle. Theme 2 addresses geochemical views of the mantle including lithospheric evolution from analysis of mantle xenoliths, composition of the deep Earth and the effect of water on subduction-zone processes. Theme 3 discusses geodynamical perspectives on the global thermo-chemical structure of the deep mantle. Theme 4 covers application of mineral physics data and phase equilibrium computations to infer the regional-scale ...

Time evolution of dissolved oxygen and redox conditions in a HLW repository

International Nuclear Information System (INIS)

Wersin, P.; Spahiu, K.; Bruno, J.

1994-02-01

The evolution of oxygen in a HLW repository has been studied using presently available geochemical background information. The important processes affecting oxygen migration in the near-field include diffusion and oxidation of pyrite and dissolved Fe(II). The evaluation of time scales of oxygen decrease is carried out with 1. an analytical approach involving the coupling of diffusion and chemical reaction, 2. a numerical geochemical approach involving the application of a newly developed diffusion-extended version of the STEADYQL code. Both approaches yield consistent rates of oxygen decrease and indicate that oxidation of pyrite impurities in the clay is the dominant process. The results obtained fRom geochemical modelling are interpreted in terms of evolution of redox conditions. Moreover, a sensitivity analysis of the major geochemical and physical parameters is performed. These results indicate that the uncertainties associated with reactive pyrite surface area impose the overall uncertainties of prediction of time scales. Thus, the obtained time of decrease to 1% of initial O 2 concentrations range between 7 and 290 years. The elapsed time at which the transition to anoxic conditions occurs is estimated to be within the same time range. Additional experimental information on redox sensitive impurities in the envisioned buffer and backfill material would further constrain the evaluated time scales. 41 refs

Geochemical studies, magmatic evolution, microstructures and replacement mechanisms in Jebale-Barez granitoid Complex (East and Southeast Jiroft

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Jamal Rasouli

2017-08-01

-related arc magmatism. The systematic variation for the major elements implies involvement of fractional crystallization in the evolution of JBPC. The trends are consistent with the fractionation of plagioclase feldspar and ferromagnesian minerals as indicated by decreasing MgO, CaO, FeOt and TiO2 with increasing SiO2 despie the content of (K2O+Na2O. It generally increases with increasing SiO2 for intermediate compositions (67 wt% SiO2 ≤ and then decreases for more felsic granitic rocks, indicating that sodic feldspar was a major fractionating phase for alkali-granite and granite suit (Rasouli, 2015. Overall REE abundances slightly decrease with increasing SiO2 consistent with plagioclase fractionation. The distribution of voluminous volcanic rocks in the studied area implies that the JBPC could be a part of the mature magmatic arc. The field petrography and geochemical studies indicated that the JPBC originated from both crustal and mantle derived magmas: The increase in temperature and excess fluid pressure caused by subduction trigged melting of mantle edge and formation of basaltic magma and its ascending and introducing into the crust was followed by partial melting (Rasouli, 2015. The juxtaposed series of mafic-felsic pulses formed a mixed magma. Finally this magma is emplaced at broad, shallow magma chamber (9-12 km, where the differentiation took place by fractional crystallization and produced a wide variety of rocks form quartz-diorite to alkali granite. In such shallow magma reservoirs, the emplacement of magma took place as sill (Fridrich et al, 1991. Combining field observations and petrofabric studies displayed a deep caldera as a feeder zone for Eocene volcanic rocks (Rasouli, 2015. The JBPC is located in a shear zone and multiple magmatic pulses were injected as sills. The magmatic fabrics show active tectonic controls on magmatism during and after magma emplacement. The transpressional tectonic regime is well compatible with our data. References Fridrich, C

Alligator Rivers Analogue project. Geochemical modelling of present-day groundwaters. Final Report - Volume 12

Energy Technology Data Exchange (ETDEWEB)

Sverjensky, D A [The John Hopkins Univ, Dept of Earth and Planetary Sciences, Baltimore (United States)

1993-12-31

The main purpose of this report is to summarize geochemical modeling studies of the present-day Koongarra groundwaters. Information on the present-day geochemistry and geochemical processes at Koongarra forms a basis for a present-day analogue for nuclear waste migration. The present-day analogue is built on studies of the mineralogy and petrology of the Koongarra deposit, and chemical analyses of present-day groundwaters from the deposit. The overall approach taken in the present study has been to carry out a series of aqueous speciation and state of saturation calculations, including chemical mass transfer calculations, to address the possible control over the chemistry of the present-day for the groundwaters at Koongarra. The most important implication of the present study for the migration of radionuclides is the strong role played by the water-rock interactions, both above and below the water table, influencing the overall chemical evolution of the groundwaters. Thus, the results show that the chemical evolution of waters is strongly controlled by the initial availability of CO{sub 2} and the mineral assemblage encountered, which together determine the major element evolution of the waters by controlling the pH. The relative rates of evolution of the pH and the oxidation state of the groundwaters are also critical to the mobility of uranium. The shallow Koongarra waters are sufficiently oxidising that they can dissolve and transport uranium even under acidic conditions. Under the more reducing condition of the deep groundwaters, is the pH level that permits uranium transport as carbonate complexes. However, if the oxidation state decreases to much lower levels, it would be expected that uranium become immobile. All the speciation and state of saturation calculations carried out in the present study are available from the author, on request 22 refs., 7 tabs., 18 figs.

Alligator Rivers Analogue project. Geochemical modelling of present-day groundwaters. Final Report - Volume 12

Energy Technology Data Exchange (ETDEWEB)

Sverjensky, D. A. [The John Hopkins Univ, Dept of Earth and Planetary Sciences, Baltimore (United States)

1992-12-31

The main purpose of this report is to summarize geochemical modeling studies of the present-day Koongarra groundwaters. Information on the present-day geochemistry and geochemical processes at Koongarra forms a basis for a present-day analogue for nuclear waste migration. The present-day analogue is built on studies of the mineralogy and petrology of the Koongarra deposit, and chemical analyses of present-day groundwaters from the deposit. The overall approach taken in the present study has been to carry out a series of aqueous speciation and state of saturation calculations, including chemical mass transfer calculations, to address the possible control over the chemistry of the present-day for the groundwaters at Koongarra. The most important implication of the present study for the migration of radionuclides is the strong role played by the water-rock interactions, both above and below the water table, influencing the overall chemical evolution of the groundwaters. Thus, the results show that the chemical evolution of waters is strongly controlled by the initial availability of CO{sub 2} and the mineral assemblage encountered, which together determine the major element evolution of the waters by controlling the pH. The relative rates of evolution of the pH and the oxidation state of the groundwaters are also critical to the mobility of uranium. The shallow Koongarra waters are sufficiently oxidising that they can dissolve and transport uranium even under acidic conditions. Under the more reducing condition of the deep groundwaters, is the pH level that permits uranium transport as carbonate complexes. However, if the oxidation state decreases to much lower levels, it would be expected that uranium become immobile. All the speciation and state of saturation calculations carried out in the present study are available from the author, on request 22 refs., 7 tabs., 18 figs.

Aspects of geochemical evolution of the SKB near field in the frame of SR-Site

International Nuclear Information System (INIS)

Sena, Clara; Salas, Joaquin; Arcos, David

2010-09-01

The concept for the final disposal of high level nuclear waste (HLNW) developed by the Swedish Nuclear Waste Management Company (SKB) entails a multi-barrier system that surrounds the HLNW, which is also known as the near-field. In the near-field, the buffer is initially subject to a high thermal gradient induced by the heat generated by the radioactive decay of the HLNW. During this period, the buffer is also subject to a hydrodynamic pressure induced by the surrounding water saturated rock massif which progressively leads to the saturation of the buffer. After saturation and cooling of the near-field, the interaction of groundwater with the bentonite buffer may result in an evolving distribution of some aqueous species in the bentonite porewater, as well as the redistribution of accessory minerals and the cation exchanger composition in the montmorillonite interlayer. The distribution of aqueous and solid species in the buffer can affect, directly or indirectly, some of the relevant safety function indicators defined by. In this context, the work developed by Arcos et al is revisited in the present work and, based on new data from SKB, additional models are developed for the SR-Site Safety Assessment. The work presented here represents an update of the model conducted within the SR-Can exercise and, therefore, similar simulation cases are developed. Three aspects must be considered regarding the geochemical evolution of the near field: (1) the effect of the thermal period; (2) the processes during the saturation of bentonite; and, (3) the interaction of the water-saturated bentonite with the local groundwater. In this numerical exercise, two types of bentonite are analysed: the MX-80 and the Deponit CA-N. The effect of the thermal period and the water saturation are analysed in a series of one-dimensional radial-symmetric simulations performed using TOUGHREACT which is a reactive transport code that accounts for variably saturated multi-phase flow under non

Aspects of geochemical evolution of the SKB near field in the frame of SR-Site

Energy Technology Data Exchange (ETDEWEB)

Sena, Clara; Salas, Joaquin; Arcos, David (Amphos 21, Barcelona (Spain))

2010-09-15

The concept for the final disposal of high level nuclear waste (HLNW) developed by the Swedish Nuclear Waste Management Company (SKB) entails a multi-barrier system that surrounds the HLNW, which is also known as the near-field. In the near-field, the buffer is initially subject to a high thermal gradient induced by the heat generated by the radioactive decay of the HLNW. During this period, the buffer is also subject to a hydrodynamic pressure induced by the surrounding water saturated rock massif which progressively leads to the saturation of the buffer. After saturation and cooling of the near-field, the interaction of groundwater with the bentonite buffer may result in an evolving distribution of some aqueous species in the bentonite porewater, as well as the redistribution of accessory minerals and the cation exchanger composition in the montmorillonite interlayer. The distribution of aqueous and solid species in the buffer can affect, directly or indirectly, some of the relevant safety function indicators defined by. In this context, the work developed by Arcos et al is revisited in the present work and, based on new data from SKB, additional models are developed for the SR-Site Safety Assessment. The work presented here represents an update of the model conducted within the SR-Can exercise and, therefore, similar simulation cases are developed. Three aspects must be considered regarding the geochemical evolution of the near field: (1) the effect of the thermal period; (2) the processes during the saturation of bentonite; and, (3) the interaction of the water-saturated bentonite with the local groundwater. In this numerical exercise, two types of bentonite are analysed: the MX-80 and the Deponit CA-N. The effect of the thermal period and the water saturation are analysed in a series of one-dimensional radial-symmetric simulations performed using TOUGHREACT which is a reactive transport code that accounts for variably saturated multi-phase flow under non

Rock–water interactions and pollution processes in the volcanic aquifer system of Guadalajara, Mexico, using inverse geochemical modeling

International Nuclear Information System (INIS)

Morán-Ramírez, J.; Ledesma-Ruiz, R.; Mahlknecht, J.; Ramos-Leal, J.A.

2016-01-01

In order to understand and mitigate the deterioration of water quality in the aquifer system underlying Guadalajara metropolitan area, an investigation was performed developing geochemical evolution models for assessment of groundwater chemical processes. The models helped not only to conceptualize the groundwater geochemistry, but also to evaluate the relative influence of anthropogenic inputs and natural sources of salinity to the groundwater. Mixing processes, ion exchange, water–rock–water interactions and nitrate pollution and denitrification were identified and confirmed using mass-balance models constraint by information on hydrogeology, groundwater chemistry, lithology and stability of geochemical phases. The water–rock interactions in the volcanic setting produced a dominant Na−HCO_3 water type, followed by Na−Mg−Ca−HCO_3 and Na−Ca−HCO_3. For geochemical evolution modeling, flow sections were selected representing recharge and non-recharge processes and a variety of mixing conditions. Recharge processes are dominated by dissolution of soil CO_2 gas, calcite, gypsum, albite and biotite, and Ca/Na exchange. Non-recharge processes show that the production of carbonic acid and Ca/Na exchange are decreasing, while other minerals such as halite and amorphous SiO_2 are precipitated. The origin of nitrate pollution in groundwater are fertilizers in rural plots and wastewater and waste disposal in the urban area. This investigation may help water authorities to adequately address and manage groundwater contamination. - Highlights: • The Inverse geochemical modeling was used to study to processes occurring in a volcanic aquifer. • Three flow sections were selected to apply inverse hydrogeochemical modeling. • Three main groundwater flows were identified: a local, intermediate and regional flow. • The models show that in the study area that groundwater is mixed with local recharge. • In the south, the aquifer has thermal influence.

Geochemical computer codes. A review

International Nuclear Information System (INIS)

Andersson, K.

1987-01-01

In this report a review of available codes is performed and some code intercomparisons are also discussed. The number of codes treating natural waters (groundwater, lake water, sea water) is large. Most geochemical computer codes treat equilibrium conditions, although some codes with kinetic capability are available. A geochemical equilibrium model consists of a computer code, solving a set of equations by some numerical method and a data base, consisting of thermodynamic data required for the calculations. There are some codes which treat coupled geochemical and transport modeling. Some of these codes solve the equilibrium and transport equations simultaneously while other solve the equations separately from each other. The coupled codes require a large computer capacity and have thus as yet limited use. Three code intercomparisons have been found in literature. It may be concluded that there are many codes available for geochemical calculations but most of them require a user that us quite familiar with the code. The user also has to know the geochemical system in order to judge the reliability of the results. A high quality data base is necessary to obtain a reliable result. The best results may be expected for the major species of natural waters. For more complicated problems, including trace elements, precipitation/dissolution, adsorption, etc., the results seem to be less reliable. (With 44 refs.) (author)

PERFIL DE LIDERANÃA E TOMADA DE DECISÃO

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Eduardo Botti Abbade

2009-04-01

Full Text Available O objetivo geral deste estudo foi o de identificar o estilo de liderança, perfil comportamental e decisório dos dirigentes das empresas do Distrito Industrial de Santa Maria / RS. Este estudo se configura como sendo uma pesquisa de levantamento (survey descritiva onde foram selecionadas 14 empresas, das 20 existentes, localizadas no Distrito Industrial do município de Santa Maria-RS. Com o objetivo de definir o perfil gerencial dos pesquisados, esta investigação utilizou-se de perspectivas psicológicas, de observação, de decisão e de aprendizagem. Os entrevistados correspondem a indivíduos que possuem um perfil com tendências a enfatizar detalhes e fatos, possuem foco no curto prazo e são muito realistas. Costumam elaborar regras e regulamentos para o julgamento do desempenho. Sugeremse para estudos futuros que seja realizado estudos onde se proponha um cruzamento entre os perfis observados com demais aspectos organizacionais como clima, cultura e comunicação organizacional. Propõe-se também que seja realizada a pesquisa com uma amostra mais abrangente. Aconselha-se que seja realizada a entrevista com gestores ou responsáveis de todas as áreas das empresas pesquisadas, para que se possam analisar perfis de gestores com diferentes competências e atribuições na mesma organização.

Intercomparison of Cement Solid-Solution Models. Issues Affecting the Geochemical Evolution of Repositories for Radioactive Waste

International Nuclear Information System (INIS)

Benbow, Steven; Savage, David; Walker, Colin

2007-05-01

Many concepts for the geological storage of radioactive waste incorporate cement based materials, which act to provide a chemical barrier, impede groundwater flow or provide structural integrity of the underground structures. Thus, it is important to understand the long-term behaviour of these materials when modelling scenarios for the potential release and migration of radionuclides. In the presence of invasive groundwater, the chemical and physical properties of cement, such as its pH buffering capacity, resistance to flow, and its mechanical properties, are expected to evolve with time. Modelling the degradation of cement is complicated by the fact that the long term pH buffer is controlled by the incongruent dissolution behaviour of calcium-silicate-hydrate (C-S-H) gel. It has been previously shown (SKI Report 2005:64) that it is possible to simulate the long term evolution of both the physical and chemical properties of cement based materials in an invasive groundwater using a fully coupled geochemical transport model. The description of the incongruent dissolution of C-S-H gel was based on a binary solid solution aqueous solution (SSAS) between end-member components portlandite (Ca(OH) 2 ) and a C-S-H gel composition expressed by its component oxides (CaH 2 SiO 4 ). The models considered a range of uncertainties including different groundwater compositions, parameterised couplings between the evolution of porosity with permeability and diffusivity and alternative secondary mineral assemblages. The results of the modelling suggested that alternative evolutions were possible under these different conditions. The focus of this report is to address the uncertainty regarding the choice of model for the C-S-H gel dissolution. We compare two alternative C-S-H SSAS models with the one that was used in the previous report, with an emphasis on a direct comparison of the model predictions. Thus we have chosen one simple simulated experimental model based on those in the

Perfil psicosocial de la persona emprendedora

OpenAIRE

Trejo López, Enrique Alberto

2015-01-01

El objeto de la tesis es estudiar el perfil psicosocial de la persona emprendedora y de la emprendedora que continúa a pesar de la crisis, constatando las diferencias respecto al resto de los grupos laborales. Se realiza un estudio multidimensional, psicosocial, de nivel descriptivo y analítico, con un carácter longitudinal, aplicando instrumentos y metodologías cualitativas y cuantitativas y aportando datos disgregado por sexo En el marco teórico recogemos los estudios e investigacion...

Perfiles Latinoamericanos: Regional sociology, connected sociologies

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Nelson Arteaga Botello

2017-07-01

Full Text Available The landscape of sociology published in the 48 numbers of the Perfiles Latinoamericanos magazineis analyzed. The diversity of topics, perspectives, and methodologies of the articles define aseries of fields of reflection around civil society, collective action, subjectivities and social identities,cities, media, violence, and theory. The essay suggests how the sociology that is producedin Latin America is not isolated but connected with international debates. It converges forms ofdoing theory and research with resonances on a global scale.

Perfil unitriádico de empresas respondables (accountability

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Migdalia Caridad

2006-01-01

Full Text Available El artículo divulga los resultados de la investigación perfil unitriádico gerencial de empresas líderes en respondabilidad (Accountability, la cual tuvo como propósito determinar dicho perfil, considerando específicamente el rol de las empresas como organización ante sus actores internos, clientes y comunidad donde actúan. El artículo establece el valor respondabilidad (Accountability como parte de la filosofía de la empresa, facilitando su interiorización bajo un enfoque unitriádico (capital intelectual racional, emocional y operacional, que se distinga por los atributos de un liderazgo relacional, que tome en cuenta el conocimiento y talento de su gente, sistemas comunicacionales con énfasis en el diálogo empático y asertivo (estilo conversacional, apoyado en sistemas de información, medición y de auditoria, así como en la publicación sistemática de resultados y con un comportamiento centrado en sus grupos de interés internos y externos

Geochemical and Geophysical Characteristics of the Balud Ophiolitic Complex (BOC, Masbate Island, Philippines: Implications for its Generation, Evolution and Emplacement

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Pearlyn C. Manalo

2015-01-01

Full Text Available This paper presents the first field, geochemical and geophysical information on the recently recognized Early Cretaceous Balud Ophiolitic Complex (BOC in the island of Masbate in the Central Philippines. Mapping of the western limb of the island revealed that only the upper crustal section of the BOC is exposed in this area. Geochemically, the pillow basalts are characterized by transitional mid-oceanic ridge basalt-island arc tholeiitic compositions. Gravity surveys yielded low Bouguer anomaly values that are consistent with the highly dismembered nature of the BOC. Short wavelength, high amplitude magnetic anomalies registered across the study area are attributed to shallow magnetic sources. This is taken to support the model that the ophiolitic complex occurs as thin crustal slivers that are not deeply-rooted in the mantle. Comparing BOC with other ophiolites in the Central Philippines, such as those in the islands of Sibuyan, Leyte and Bohol, suggests the possibility of a common or contiguous source for similarly-aged and geochemically composed crust-mantle sequences in the region.

Geochemical prospecting for uranium and thorium deposits

International Nuclear Information System (INIS)

Boyle, R.W.

1980-01-01

A brief review of analytical geochemical prospecting methods for uranium and thorium is given excluding radiometric techniques, except those utilized in the determination of radon. The indicator (pathfinder) elements useful in geochemical surveys are listed for each of the types of known uranium and thorium deposits; this is followed by sections on analytical geochemical surveys based on rocks (lithochemical surveys), unconsolidated materials (pedochemical surveys), natural waters and sediments (hydrochemical surveys), biological materials (biogeochemical surveys) and gases (atmochemical surveys). All of the analytical geochemical methods are applicable in prospecting for thorium and uranium, particularly where radiometric methods fail due to attenuation by overburden, water, deep leaching and so on. Efficiency in the discovery of uranium and/or thorium orebodies is promoted by an integrated methods approach employing geological pattern recognition in the localization of deposits, analytical geochemical surveys, and radiometric surveys. (author)

Experimental insights into geochemical changes in hydraulically fractured Marcellus Shale

International Nuclear Information System (INIS)

Marcon, Virginia; Joseph, Craig; Carter, Kimberly E.; Hedges, Sheila W.; Lopano, Christina L.; Guthrie, George D.; Hakala, J. Alexandra

2017-01-01

Hydraulic fracturing applied to organic-rich shales has significantly increased the recoverable volume of methane available for U.S. energy consumption. Fluid-shale reactions in the reservoir may affect long-term reservoir productivity and waste management needs through changes to fracture mineral composition and produced fluid chemical composition. We performed laboratory experiments with Marcellus Shale and lab-generated hydraulic fracturing fluid at elevated pressures and temperatures to evaluate mineral reactions and the release of trace elements into solution. Results from the experiment containing fracturing chemicals show evidence for clay and carbonate dissolution, secondary clay and anhydrite precipitation, and early-stage (24–48 h) fluid enrichment of certain elements followed by depletion in later stages (i.e. Al, Cd, Co, Cr, Cu, Ni, Sc, Zn). Other elements such as As, Fe, Mn, Sr, and Y increased in concentration and remained elevated throughout the duration of the experiment with fracturing fluid. Geochemical modeling of experimental fluid data indicates primary clay dissolution, and secondary formation of smectites and barite, after reaction with fracturing fluid. Changes in aqueous organic composition were observed, indicating organic additives may be chemically transformed or sequestered by the formation after hydraulic fracturing. The NaCl concentrations in our fluids are similar to measured concentrations in Marcellus Shale produced waters, showing that these experiments are representative of reservoir fluid chemistries and can provide insight on geochemical reactions that occur in the field. These results can be applied towards evaluating the evolution of hydraulically-fractured reservoirs, and towards understanding geochemical processes that control the composition of produced water from unconventional shales. - Highlights: • Metal concentrations could be at their peak in produced waters recovered 24–48 after fracturing. • Carbonate

Application of the isotopic index in isotope geochemical investigation

International Nuclear Information System (INIS)

Schuetze, H.

1982-06-01

A method is described which allows to calculate approximately isotope exchange equilibria between different crystalline silicates. The algorithm uses a newly introduced isotopic index. It is defined using isotopic increments of the variant types of silicatic bonds. This isotopic index gives a quantitative measure of the ability to enrich 18 O or 30 Si, respectively. The dependence of isotopic fractionations on temperature can be calculated approximately by means of the isotopic index, too. On this theoretical base some problems of magmatism and two varieties of an isotope geochemical model of the evolution of the Earth's crust are treated. Finally, the possibility is demonstrated to give prognostic statements about the likelihood of ore bearing of different granites. (author)

Geochemical modelling of CO2-water-rock interactions for carbon storage : data requirements and outputs

International Nuclear Information System (INIS)

Kirste, D.

2008-01-01

A geochemical model was used to predict the short-term and long-term behaviour of carbon dioxide (CO 2 ), formation water, and reservoir mineralogy at a carbon sequestration site. Data requirements for the geochemical model included detailed mineral petrography; formation water chemistry; thermodynamic and kinetic data for mineral phases; and rock and reservoir physical characteristics. The model was used to determine the types of outputs expected for potential CO 2 storage sites and natural analogues. Reaction path modelling was conducted to determine the total reactivity or CO 2 storage capability of the rock by applying static equilibrium and kinetic simulations. Potential product phases were identified using the modelling technique, which also enabled the identification of the chemical evolution of the system. Results of the modelling study demonstrated that changes in porosity and permeability over time should be considered during the site selection process.

Arsenic release and geochemical evolution of groundwater in an alluvial aquitard, West Bengal, India.

Science.gov (United States)

Desbarats, A. J.; Pal, T.; Mukherjee, P. K.; Beckie, R. D.

2017-12-01

According to the World Health Organization, contamination of groundwater by geogenic arsenic (As) represents the largest mass poisoning in history. At a field site in West Bengal, India, the source of As affecting a shallow aquifer was traced to silty sediments filling an abandoned river meander. Along with As-bearing phases, these sediments also contain 0.46 % organic carbon. The release of As within the channel fill is investigated using a geochemical mass balance model supported by detailed field observations of aqueous chemistry, sequential extraction analyses of sediment chemistry, and analyses of sediment mineralogy. The model explores the evolution of groundwater chemistry along a flow path extending from its recharge point in an abandoned channel pond, through the channel-fill sequence, to the underlying aquifer. Variations in groundwater composition within the host sediments are explained in terms of mineral weathering driven by organic carbon decay. The model yields reaction coefficients expressing amounts of minerals (and gases) reacting or precipitating along the flow path. Arsenic and phosphorus cycles appear closely linked as these species are hosted by goethite, Fe-rich chlorite, and vivianite. Arsenic is released through the rapid reductive dissolution of goethite and the slower weathering of chlorite. Concomitantly, some As is sequestered in precipitating vivianite. These competing processes reach equilibrium deeper in the channel-fill sequence as groundwater As concentrations stabilize. Using groundwater residence time in channel fill obtained from a numerical flow model and the calculated reaction coefficients, rates of organic carbon oxidation, goethite dissolution, and net As release are estimated at 1.15 mmol C L-1 a-1, 0.18 mmol L-1 a-1, and 4.57 10-4 mmol L-1 a-1, respectively. Fine-grained yet slightly permeable deposits such as channel-fill silts containing reactive organic carbon and As-bearing goethite and phyllosilicates are localized

LOS ESTUDIOS DE MERCADO Y PERFILES DE SECTOR COMO HERRAMIENTAS ÚTILES PARA LA TOMA DE DECISIONES

Directory of Open Access Journals (Sweden)

Yolanda Morejón-Bravo

2016-01-01

Full Text Available En primer lugar, se ofrece una breve explicación de los fundamentos teóricos de la inteligencia empresarial y sus productos, haciendo énfasis en los perfiles estratégicos, y dentro de ellos, en los perfiles de sector. También, se hace énfasis en los estudios de mercado y sus características. En segundo lugar, se presentan dos casos de estudio (un perfil de sector y un estudio de mercado, que demuestran la importancia de estos productos y servicios de inteligencia competitiva, para la toma de decisiones lo más acertada posible, en las organizaciones.

Simulation of the geochemical interactions in a natural CO2 deposit: the example of Springerville - Saint-Johns (USA). Final report

International Nuclear Information System (INIS)

Le Guern, C.; Gaus, I.

2004-01-01

The aim of the study is a better understanding of the geochemical operating of natural analogues by the simulation of scenario representative of the evolution of site since the arrival of CO 2 still today. This exercise concerns the Springerville site. Simulation tests with the PHREEQC code have been realized. This final report presents in the first part how the data are collected on a natural CO 2 , then a bibliographic synthesis on the observed impacts of the CO 2 on a deposit. The fourth part is the simulation of the geochemical interactions in the natural CO 2 deposit of Springerville. (A.L.B.)

Hydrogeochemical Evolution of the Laxemar Site

Energy Technology Data Exchange (ETDEWEB)

Gimeno, Maria J.; Auque, Luis F.; Gomez, Javier B. (Univ. of Zaragoza (Spain)); Salas, Joaquin; Molinero, Jorge (Amphos 21, Barcelona (Spain))

2010-11-15

The chemical composition of groundwater in the rock volume surrounding a spent nuclear fuel repository is of importance to many variables that affect repository performance. One of the questions to be addressed is whether the chemical environment will remain favourable over time under the expected environmental evolution. Different groundwater compositions will prevail around the repository as a result of the different types of climate domains and their corresponding hydraulic conditions. The successions of temperate, periglacial and glacial climate domains will affect both the groundwaters' flow and composition around the repository. For a specific location, the evolution between climate domains will be gradual. For example, during a temperate domain, temperatures may slowly decrease such that periglacial conditions slowly develop within parts of the repository region. In SR-Site, the evaluation of geochemical effects is restricted to using separate specifications for the different climatic domains. During the initial temperate period after closure, the infiltration of meteoric waters, the displacement of the Baltic shoreline, and the changes in annual precipitation are the key processes controlling the evolution of the hydrogeology of the site. On the other hand, the groundwater chemistry for periods in which the repository is under permafrost or under an ice sheet (during periglacial and glacial conditions, respectively) is expected to change by the infiltration of glacial melt waters, and by the upconing of deep saline groundwaters. Immediately after the retreat of an ice sheet, isostatic depression will set the ground surface at the repository site below the Baltic Sea surface level for a period of time. In the reference evolution, the Laxemar site is expected to be flooded under a lake of glacial melt water and, then, under marine or brackish waters during a period of time from a few thousand years up to, perhaps, ten thousand years.These phenomena will

Hydrogeochemical Evolution of the Laxemar Site

International Nuclear Information System (INIS)

Gimeno, Maria J.; Auque, Luis F.; Gomez, Javier B.; Salas, Joaquin; Molinero, Jorge

2010-11-01

The chemical composition of groundwater in the rock volume surrounding a spent nuclear fuel repository is of importance to many variables that affect repository performance. One of the questions to be addressed is whether the chemical environment will remain favourable over time under the expected environmental evolution. Different groundwater compositions will prevail around the repository as a result of the different types of climate domains and their corresponding hydraulic conditions. The successions of temperate, periglacial and glacial climate domains will affect both the groundwaters' flow and composition around the repository. For a specific location, the evolution between climate domains will be gradual. For example, during a temperate domain, temperatures may slowly decrease such that periglacial conditions slowly develop within parts of the repository region. In SR-Site, the evaluation of geochemical effects is restricted to using separate specifications for the different climatic domains. During the initial temperate period after closure, the infiltration of meteoric waters, the displacement of the Baltic shoreline, and the changes in annual precipitation are the key processes controlling the evolution of the hydrogeology of the site. On the other hand, the groundwater chemistry for periods in which the repository is under permafrost or under an ice sheet (during periglacial and glacial conditions, respectively) is expected to change by the infiltration of glacial melt waters, and by the upconing of deep saline groundwaters. Immediately after the retreat of an ice sheet, isostatic depression will set the ground surface at the repository site below the Baltic Sea surface level for a period of time. In the reference evolution, the Laxemar site is expected to be flooded under a lake of glacial melt water and, then, under marine or brackish waters during a period of time from a few thousand years up to, perhaps, ten thousand years.These phenomena will

Perfil logístico de Colombia

OpenAIRE

Cardozo Maglioni, María Victoria; Lozano Suarez, María Goretty

2012-01-01

El presente documento ofrece un estudio del perfil logístico de Colombia con la finalidad de dar a conocer el estado de arte de las ciudades, puertos e infraestructura principal para facilitar la toma de decisiones de los empresarios. Para el desarrollo de este trabajo se determinaron a partir de un análisis competitivo del país; las principales ciudades y puertos; logrando establecer un inventario de maquinaria y equipo e infraestructura logística; enmarcados en retos ya establecidos en las ...

Perfil das pacientes submetidas a gluteoplastia

OpenAIRE

José Horácio Costa Aboudib Júnior

2014-01-01

Durante nossas frequentes apresentações em cursos, congressos e jornadas e mesmo em nossas publicações, existiam constantes perguntas sobre o perfil dessas pacientes. O crescente interesse da mídia e das pacientes a este respeito e também a crescente procura pela cirurgia nos estimulou a realizar este trabalho. Segundo dados da Sociedade Brasileira de Cirurgia Plástica (SBPC) e da American Society of Plastic Surgery (ASPS), referem que 20.000 pacientes foram submetidas a esta cirurgia. Em 201...

Initial geochemical characteristics of fluid fine tailings in an oil sands end pit lake

Energy Technology Data Exchange (ETDEWEB)

Dompierre, Kathryn A. [Department of Civil and Geological Engineering, University of Saskatchewan, Saskatoon, Saskatchewan, Canada S7N 5A9 (Canada); Lindsay, Matthew B.J., E-mail: matt.lindsay@usask.ca [Department of Geological Sciences, University of Saskatchewan, Saskatoon, Saskatchewan S7N 5E2 (Canada); Cruz-Hernández, Pablo [Department of Geology, University of Huelva, Campus ‘El Carmen’, E-21071 Huelva (Spain); Halferdahl, Geoffrey M. [Environmental Research and Development, Syncrude Canada Limited, Edmonton, Alberta T6N 1H4 (Canada)

2016-06-15

Geochemical characteristics of fluid fine tailings (FFT) were examined in Base Mine Lake (BML), which is the first full-scale demonstration oil sands end pit lake (EPL) in northern Alberta, Canada. Approximately 186 Mm{sup 3} of FFT was deposited between 1994 and 2012, before BML was established on December 31, 2012. Bulk FFT samples (n = 588) were collected in July and August 2013 at various depths at 15 sampling sites. Temperature, solid content, electrical conductivity (EC), pH, Eh and alkalinity were measured for all samples. Detailed geochemical analyses were performed on a subset of samples (n = 284). Pore-water pH decreased with depth by approximately 0.5 within the upper 10 m of the FFT. Major pore-water constituents included Na (880 ± 96 mg L{sup −1}) and Cl (560 ± 95 mg L{sup −1}); Ca (19 ± 4.1 mg L{sup −1}), Mg (11 ± 2.0 mg L{sup −1}), K (16 ± 2.3 mg L{sup −1}) and NH{sub 3} (9.9 ± 4.7 mg L{sup −1}) were consistently observed. Iron and Mn concentrations were low within FFT pore water, whereas SO{sub 4} concentrations decreased sharply across the FFT–water interface. Geochemical modeling indicated that FeS{sub (s)} precipitation was favoured under SO{sub 4}-reducing conditions. Pore water was also under-saturated with respect to gypsum [CaSO{sub 4}·2H{sub 2}O], and near saturation with respect to calcite [CaCO{sub 3}], dolomite [CaMg(CO{sub 3}){sub 2}] and siderite [FeCO{sub 3}]. X-ray diffraction (XRD) suggested that carbonate-mineral dissolution largely depleted calcite and dolomite. X-ray absorption near edge structure (XANES) spectroscopy revealed the presence of FeS{sub (s)}, pyrite [FeS{sub 2}], and siderite. Carbonate-mineral dissolution and secondary mineral precipitation have likely contributed to FFT dewatering and settlement. However, the long-term importance of these processes within EPLs remains unknown. These results provide a reference for assessing the long-term geochemical evolution of oil sands EPLs, and offer

Perfil cognitivo de la dependencia emocional en estudiantes universitarios en Medellín, Colombia

OpenAIRE

Lemos Hoyos, Mariantonia; Jaller Jaramillo, Cristina; González Calle, Ana María; Díaz León, Zoraya Tatiana; De la Ossa, Daniela

2012-01-01

El objetivo de este estudio fue la identificación del perfil cognitivo de los estudiantes universitarios con dependencia emocional. Ésta se plantea como un patrón orientado al otro como fuente de satisfacción y seguridad personal, donde el perfil cognitivo les llevaría a interpretar los hechos de manera diferente, basándose en cubrir sus necesidades emocionales insatisfechas. Se tomó una muestra aleatoria estratificada de 569 estudiantes universitarios. Los resultados arrojaron un modelo que ...

Geochemical Characterization of the Upper and Middle Floridan Aquifer System, South Florida

Science.gov (United States)

Mirecki, J.; Richardson, E.; Bennett, M.; Hendel, J.

2008-05-01

Our study focus is to characterize the water quality and geochemical environment of the Floridan Aquifer System (FAS) throughout the regional flowpath. A synoptic survey of 21 wells (n=15, upper FAS; n=6 middle FAS) was supplemented by additional samples (n=11) obtained during exploratory well development at 4 aquifer storage recovery (ASR) pilot sites. Synoptic survey samples were analyzed intensively, yielding a dataset that consists of major and trace dissolved constituents (including metals), stable isotopes (δ18O, δ13C, δD, δ34S in sulfate and sulfide), carbon species (carbonate alkalinity and organic carbon), uranium-series radionuclides, nutrients, and selected microbes and pathogens. The objectives of this study are three-fold: 1) to provide baseline water-quality and geochemical information prior to initiation of ASR activities that are part of the Comprehensive Everglades Restoration Plan; 2) to quantify the major controls on geochemical evolution along upper and middle FAS flowpaths using geochemical modeling methods; and 3) to identify areas where water- quality may limit the feasibility of ASR methods in the FAS. Preliminary interpretations water quality changes along the regional FAS flowpath can be summarized as follows. Concentrations of dissolved constituents increase from north to south along the flow path; generally, the upper FAS has lower total dissolved solids than the middle FAS at locations where well pairs were analyzed. The redox environment changes from oxic to strongly anoxic, very close to the recharge area. Redox measurements, dissolved iron, sulfide, and sulfur isotope data are consistent with sulfate-reducing conditions. Uranium-series isotope concentrations and activities generally are below regulatory criteria, with few exceptions in both the upper and middle FAS. Areas with greater radionuclide activity occur primarily at distal flowpath locations or at the coast.

Geochemical differentiation processes for arc magma of the Sengan volcanic cluster, Northeastern Japan, constrained from principal component analysis

Science.gov (United States)

Ueki, Kenta; Iwamori, Hikaru

2017-10-01

In this study, with a view of understanding the structure of high-dimensional geochemical data and discussing the chemical processes at work in the evolution of arc magmas, we employed principal component analysis (PCA) to evaluate the compositional variations of volcanic rocks from the Sengan volcanic cluster of the Northeastern Japan Arc. We analyzed the trace element compositions of various arc volcanic rocks, sampled from 17 different volcanoes in a volcanic cluster. The PCA results demonstrated that the first three principal components accounted for 86% of the geochemical variation in the magma of the Sengan region. Based on the relationships between the principal components and the major elements, the mass-balance relationships with respect to the contributions of minerals, the composition of plagioclase phenocrysts, geothermal gradient, and seismic velocity structure in the crust, the first, the second, and the third principal components appear to represent magma mixing, crystallizations of olivine/pyroxene, and crystallizations of plagioclase, respectively. These represented 59%, 20%, and 6%, respectively, of the variance in the entire compositional range, indicating that magma mixing accounted for the largest variance in the geochemical variation of the arc magma. Our result indicated that crustal processes dominate the geochemical variation of magma in the Sengan volcanic cluster.

Appliance of geochemical engineering in radioactive waste disposal

International Nuclear Information System (INIS)

Li Shuang; Zhang Chengjiang; Ni Shijun; Li Kuanliang

2008-01-01

The basic foundation of applying geochemical engineering to control environment, common engineering models of disposal radioactive waste and the functions of the engineering barriers are introduced in this paper. The authors take the geochemical engineering barrier materiel research of a radioactive waste repository as an example to explain the appliance of geochemical engineering in the disposal of radioactive waste. And the results show that it can enhance the security of the nuclear waste repository if we use geochemical engineering barrier. (authors)

Geochemical modelling of Na-SO4 type groundwater at Palmottu using a mass balance approach

International Nuclear Information System (INIS)

Pitkaenen, P.

1993-01-01

The mass balance chemical modelling technique has been applied to the groundwaters at the Palmottu analogue study site (in southwestern Finland) for radioactive waste disposal. The geochemical modelling concentrates on the evolution of Na-SO 4 type groundwater, which is spatially connected to the uranium mineralization. The results calculated along an assumed flow path are consistent with available field data and thermodynamic constraints. The results show that essential production of sulphides is unrealistic in the prevailing conditions. The increasing concentrations of Na, SO 4 and Cl along the evolution trend seem to have the same source and they could originate mainly from the leakage of fluid inclusions. Some mixing of relict sea water is also possible

Neoproterozoic-Early Paleozoic Peri-Pacific Accretionary Evolution of the Mongolian Collage System: Insights From Geochemical and U-Pb Zircon Data From the Ordovician Sedimentary Wedge in the Mongolian Altai

Science.gov (United States)

Jiang, Y. D.; Schulmann, K.; Kröner, A.; Sun, M.; Lexa, O.; Janoušek, V.; Buriánek, D.; Yuan, C.; Hanžl, P.

2017-11-01

Neoproterozoic to early Paleozoic accretionary processes of the Central Asian Orogenic Belt have been evaluated so far mainly using the geology of ophiolites and/or magmatic arcs. Thus, the knowledge of the nature and evolution of associated sedimentary prisms remains fragmentary. We carried out an integrated geological, geochemical, and zircon U-Pb geochronological study on a giant Ordovician metasedimentary succession of the Mongolian Altai Mountains. This succession is characterized by dominant terrigenous components mixed with volcanogenic material. It is chemically immature, compositionally analogous to graywacke, and marked by significant input of felsic to intermediate arc components, pointing to an active continental margin depositional setting. Detrital zircon U-Pb ages suggest a source dominated by products of early Paleozoic magmatism prevailing during the Cambrian-Ordovician and culminating at circa 500 Ma. We propose that the Ordovician succession forms an "Altai sedimentary wedge," the evolution of which can be linked to the geodynamics of the margins of the Mongolian Precambrian Zavhan-Baydrag blocks. This involved subduction reversal from southward subduction of a passive continental margin (Early Cambrian) to the development of the "Ikh-Mongol Magmatic Arc System" and the giant Altai sedimentary wedge above a north dipping subduction zone (Late Cambrian-Ordovician). Such a dynamic process resembles the tectonic evolution of the peri-Pacific accretionary Terra Australis Orogen. A new model reconciling the Baikalian metamorphic belt along the southern Siberian Craton with peri-Pacific Altai accretionary systems fringing the Mongolian microcontinents is proposed to explain the Cambro-Ordovician geodynamic evolution of the Mongolian collage system.

Perfil dos Supervisores de Psicologia em Serviços-Escola Brasileiros

Directory of Open Access Journals (Sweden)

Fabiana Vieira Gauy

Full Text Available Perfil dos supervisores de psicologia em Serviços-Escola Brasileiros (treino/atendimento Este trabalho teve como objetivo descrever o perfil demográfico dos supervisores dos cursos de graduação em Psicologia, obtidos pelo projeto de pesquisa intitulado "Serviços-Escola de Psicologia no Brasil", que tinha entre seus objetivos a caracterização dos serviços-escola de psicologia brasileiros. A pesquisa foi disponibilizada on-line em umsite da internet específico para a pesquisa, divulgado através de vários meios de comunicação, no qual, o participante em potencial da pesquisa (supervisor, estagiário ou gestor de uma das clinica escolas de Psicologia do Brasil, depois de acessar a pagina e o seu campo específico, informava dados pessoais (sexo e idade, dados institucionais (vínculo de trabalho, tipo de instituição e localização e dados profissionais (abordagem teórica e tempo de experiência/área. Do total de 846 participantes potenciais apenas 147 eram supervisores de cursos de Psicologia que haviam completado totalmente o questionário e foram, por isso, considerados para presente análise. Os dados coletados, no período de 2008 a 2010, apontaram que a maioria dos respondentes era do sexo feminino (77,6%, tinha idade entre 38 a 45 anos (45,5%, possuía vínculo formal de trabalho (90% com instituições de ensino privado (56%, localizadas nas Regiões Sul e Sudeste (78%. A Psicanálise figurou como abordagem mais referida (24% e aqueles que referiam ter mais de 10 anos de experiência em Psicodiagnóstico/Psicoterapia (64,4%. Apesar do tamanho da amostra não ser representativa do perfil dos supervisores brasileiros, os dados obtidos forneceram informações importantes sobre o perfil dos supervisores, peça chave na formação do aluno de graduação.

Perfil multidimensional de personas que han realizado intento de suicidio

Directory of Open Access Journals (Sweden)

Nicolás Arturo Núñez Gómez

2008-01-01

Full Text Available Establecer el perfil multidimensional de personas con intento de suicidio. Se estudiaron 116 personas reportadas con intento de suicidio en servicios de urgencias e instituciones educativas del departamento del Huila. Diseño descriptivo; con entrevista semi-estructurada, prueba de personalidad, inventario de depresión, evaluación de alcoholismo, evaluación de ideación e intento de suicidio. El perfil multidimensional se caracterizó: adolescentes rurales, adultos citadinos; son de consideración: ama de casa, con relación de pareja estable, y personas solas, divorciadas, desempleadas. La relación neuroticismo bajo y piscoticismo alto podría ayudar a explicar que el intento de suicidio haya sido realizado de "repente" sin existir ningún síntoma previo. La estructura y dinámica familiar disfuncional están altamente asociadas a la persona con intento de suicidio.

Methodological approaches in estimating anomalous geochemical field structure

International Nuclear Information System (INIS)

Gavrilov, R; Rudmin, M

2015-01-01

Mathematical statistic methods were applied to analyze the core samples from vertical expendable wells in Chertovo Koryto gold ore field. The following methods were used to analyse gold in samples: assay tests and atomic absorption method (AAS), while emission spectrum semiquantative method was applied to identify traces. The analysis of geochemical association distribution in one central profile demonstrated that bulk metasomatic aureoles are characteristic of concentric zonal structure. The distribution of geochemical associations is correlated to the hydrothermal stages of mineral formation identified in this deposit. It was proved that the processed geochemical data by factor and cluster analyses provided additional information on the anomalous geochemical field structure in gold- bearing black-shale strata. Such methods are effective tools in interpretating specific features of geochemical field structures in analogous potential ore-bearing areas

Geochemical modeling: a review

International Nuclear Information System (INIS)

Jenne, E.A.

1981-06-01

Two general families of geochemical models presently exist. The ion speciation-solubility group of geochemical models contain submodels to first calculate a distribution of aqueous species and to secondly test the hypothesis that the water is near equilibrium with particular solid phases. These models may or may not calculate the adsorption of dissolved constituents and simulate the dissolution and precipitation (mass transfer) of solid phases. Another family of geochemical models, the reaction path models, simulates the stepwise precipitation of solid phases as a result of reacting specified amounts of water and rock. Reaction path models first perform an aqueous speciation of the dissolved constituents of the water, test solubility hypotheses, then perform the reaction path modeling. Certain improvements in the present versions of these models would enhance their value and usefulness to applications in nuclear-waste isolation, etc. Mass-transfer calculations of limited extent are certainly within the capabilities of state-of-the-art models. However, the reaction path models require an expansion of their thermodynamic data bases and systematic validation before they are generally accepted

Geochemical modeling: a review

Energy Technology Data Exchange (ETDEWEB)

Jenne, E.A.

1981-06-01

Two general families of geochemical models presently exist. The ion speciation-solubility group of geochemical models contain submodels to first calculate a distribution of aqueous species and to secondly test the hypothesis that the water is near equilibrium with particular solid phases. These models may or may not calculate the adsorption of dissolved constituents and simulate the dissolution and precipitation (mass transfer) of solid phases. Another family of geochemical models, the reaction path models, simulates the stepwise precipitation of solid phases as a result of reacting specified amounts of water and rock. Reaction path models first perform an aqueous speciation of the dissolved constituents of the water, test solubility hypotheses, then perform the reaction path modeling. Certain improvements in the present versions of these models would enhance their value and usefulness to applications in nuclear-waste isolation, etc. Mass-transfer calculations of limited extent are certainly within the capabilities of state-of-the-art models. However, the reaction path models require an expansion of their thermodynamic data bases and systematic validation before they are generally accepted.

NOAA and MMS Marine Minerals Geochemical Database

Data.gov (United States)

National Oceanic and Atmospheric Administration, Department of Commerce — The Marine Minerals Geochemical Database was created by NGDC as a part of a project to construct a comprehensive computerized bibliography and geochemical database...

Use of partial dissolution techniques in geochemical exploration

Science.gov (United States)

Chao, T.T.

1984-01-01

Application of partial dissolution techniques to geochemical exploration has advanced from an early empirical approach to an approach based on sound geochemical principles. This advance assures a prominent future position for the use of these techniques in geochemical exploration for concealed mineral deposits. Partial dissolution techniques are classified as single dissolution or sequential multiple dissolution depending on the number of steps taken in the procedure, or as "nonselective" extraction and as "selective" extraction in terms of the relative specificity of the extraction. The choice of dissolution techniques for use in geochemical exploration is dictated by the geology of the area, the type and degree of weathering, and the expected chemical forms of the ore and of the pathfinding elements. Case histories have illustrated many instances where partial dissolution techniques exhibit advantages over conventional methods of chemical analysis used in geochemical exploration. ?? 1984.

PERFILES PROFESIONALES Y VALORES RELATIVOS AL TRABAJO

OpenAIRE

Moreno, José Eduardo; Marcaccio, Antonela

2014-01-01

El objetivo del presente trabajo es evaluar la relación existente entre los valores relativos al trabajo y algunos perfiles profesionales (contabilidad y administración, marketing y ventas, y recepción). El instrumento utilizado es la Escala Argentina de Valores Relativos al Trabajo (Moreno & Marcaccio, 2012) que contiene cuatro subescalas de cinco ítems cada una, a saber: Realización Personal, Reconocimiento Social, Altruismo y Aspiraciones Económicas. La muestra incluye a 425 sujetos (40% v...

Geochemical and mineralogical characteristics of Lithomargic clay

African Journals Online (AJOL)

Administrator

Geochemical and mineralogical characteristics of Lithomargic clay. GEOCHEMICAL AND .... tries, as filling material in the pulp and paper, toothpaste and paint industries as well ..... tions very vital to human health and other ac- tivities of man.

Geochemical interpretation of gamma-ray spectrometry images from the Achala granite (Cordoba, Argentina)

International Nuclear Information System (INIS)

Lopez, Luis E.

1998-01-01

Data of an old spectrometry gamma-ray survey carried out in the Sierras Pampeanas Range by the National Atomic Energy Commission (Argentina) were reprocessed to obtain a corrected digital archive. The geochemical interpretation of the 250 x 250 meters spectrometric grids from the Achala batholith area was based on the behaviour of the radioelements in a peraluminous magma. Spectrometric maps of potassium, uranium, thorium and their ratios were used. In particular, the Th grid was very useful to define the primary magmatic evolution of the granitoids. K and U correlate roughly with Th distribution. The observed positive correlation between Th and U is thought to be the result of surficial leaching of U from uraninite. Finally, U/Th ratio allows to determine both, the magmatic evolution of the rocks and the mineral phase responsible for U content. (author)

Análisis multivariante del perfil psicológico de los deportistas universitarios. Aplicación del CPRD en México

Directory of Open Access Journals (Sweden)

Adriana Isabel Andrade Sánchez

2015-12-01

Full Text Available El presente trabajo tiene como objetivo conocer el perfil psicológico de los deportistas universitarios colimenses y analizar si existen diferencias significativas entre practicantes de modalidades individuales y colectivas. Así mismo, se pretende encontrar los perfiles de riesgo para los deportistas. Se trata de un estudio transversal, basado en una muestra no probabilística de 122 alumnos de la Licenciatura en Educación Física y Deporte de la Universidad de Colima, en México. Utilizando como instrumento de medida el cuestionario “Características Psicológicas Relacionadas con el Rendimiento Deportivo” (CPRD, en la versión adaptada para deportistas mexicanos. El cuestionario mide control de estrés, motivación, cohesión de equipo, influencia de la evaluación del rendimiento y habilidad mental. Entre los principales hallazgos, se encontraron siete perfiles de riesgo, ordenados según un gradiente de necesidad de intervención por medio de la definición de puntos de corte, para todas y cada una de las subescalas. Se encontró que, casi un 40 % de los deportistas se encuentran en algún perfil de riesgo, de los cuales 6,6 % se encontraban en el perfil menor, y un 4,1 % en el perfil de riesgo máximo.

Obtención de perfiles teóricos de elementos metálicos con velocidades macroscópicas

Science.gov (United States)

Cirigliano, D.; Costa, A.; Rovira, M.

El propósito de este trabajo es poder establecer -a partir de la modelización de perfiles de distintas especies- patrones de comparación observacional que permitan caracterizar los fenómenos físicos que están presentes en las estructuras que se observan. Para ello se resuelven las ecuaciones de equilibrio de ionización para un determinado átomo y una atmósfera de parámetros determinados. A partir de ello se definen las poblaciones para los distintos grados de ionización. Considerando distintas configuraciones e intensidades de flujos de masa se deducen la función fuente, el espesor óptico y se calculan los perfiles de las distintas líneas. Se obtuvieron perfiles teóricos de líneas del CII, CIV y del OIV para flujos entrante, saliente y pasante. La forma del perfil, las intensidades relativas entre los distintos flujos y el corrimiento Doppler da cuenta de una caracterización teórica a partir de la cual se comparará con observaciones.

O perfil do negociador nas empresas

OpenAIRE

Marques, Eduardo de Oliveira

2002-01-01

Dissertação (mestrado) - Universidade Federal de Santa Catarina, Centro Tecnológico. Programa de Pós-Graduação em Engenharia de Produção. Comparativo entre os perfis negociador e cultural da população de negociadores em relação ao perfil cultural das empresas da primeira camada de fornecedores do grupo Fiat, objetivando -se determinar os tipos de negociadores mais adequados às organizações, aferindo-se o tipo de correlação existente entre as culturas e os estilos de negociação....

The geodynamic evolution of the eastern Sierras Pampeanas based on geochemical, Sm-Nd, Pb-Pb and SHRIMP data

DEFF Research Database (Denmark)

Drobe, M; Lopez de Luchi, M; Steenken, A

2011-01-01

, have been carried out to unravel the provenance and the geodynamic history of the Eastern Sierras Pampeanas, Central Argentina. The geochemical and the Sm–Nd data point to a slightly stronger mafic and less-fractionated material in the provenance area of the Sierras de Co´rdoba when compared...

DIÁLOGO DE LAS PERSPECTIVAS DE PERFIL CONCEPTUAL Y CONGLOMERADOS DE RELEVANCIA

Directory of Open Access Journals (Sweden)

Rosa I. Pedreros-M.

2013-12-01

Full Text Available El presente artículo forma parte del desarrollo de la investigación doctoral titulada “Perfil conceptual del calor en comunidades culturalmente diferenciadas” y tiene como intención socializar las perspectivas de perfil conceptual y conglomerados de relevancia como referentes teóricos y metodológicos que permitan proponer nuevas opciones para pensar la enseñanza-aprendizaje de las ciencias o la educación en ciencias, que observen los modos de pensar y hablar de los estudiantes y las relaciones entre la cultura local y el conocimiento escolar. Se exponen el origen, los referentes, las consideraciones sobre la enseñanza-aprendizaje de las ciencias y las razones para investigar desde estas perspectivas.

Perfiles de personas con diferencia mental basados en las funciones motrices gruesas

Directory of Open Access Journals (Sweden)

Isabel Ma. Ferrándiz Vindel

2002-01-01

Full Text Available El propósito de este estudio ha sido identificar posibles subtipos de alumnos con Deficiencia Mental basados en funciones motrices gruesas. Se seleccionó un grupo de alumnos de un centro específico de Deficiencia Mental, que no presentaron deficiencias motóricas asociadas, y se les administraron los subtests de motricidad gruesa del «Test Bruininks-Ozeretsky para medir la eficacia motriz»- Los cuatro subtipos resultantes mostraron diferentes perfiles de desarrollo motor A partir de estos resultados, se recomienda diseñar programas específicos que intenten paliar los trastornos motrices gruesos, analizados para cada uno de los subtipos hallados, y realizar adaptaciones curriculares pertinentes, teniendo en cuenta los perfiles motrices estudiados

Merging metagenomics and geochemistry reveals environmental controls on biological diversity and evolution.

Science.gov (United States)

Alsop, Eric B; Boyd, Eric S; Raymond, Jason

2014-05-28

The metabolic strategies employed by microbes inhabiting natural systems are, in large part, dictated by the physical and geochemical properties of the environment. This study sheds light onto the complex relationship between biology and environmental geochemistry using forty-three metagenomes collected from geochemically diverse and globally distributed natural systems. It is widely hypothesized that many uncommonly measured geochemical parameters affect community dynamics and this study leverages the development and application of multidimensional biogeochemical metrics to study correlations between geochemistry and microbial ecology. Analysis techniques such as a Markov cluster-based measure of the evolutionary distance between whole communities and a principal component analysis (PCA) of the geochemical gradients between environments allows for the determination of correlations between microbial community dynamics and environmental geochemistry and provides insight into which geochemical parameters most strongly influence microbial biodiversity. By progressively building from samples taken along well defined geochemical gradients to samples widely dispersed in geochemical space this study reveals strong links between the extent of taxonomic and functional diversification of resident communities and environmental geochemistry and reveals temperature and pH as the primary factors that have shaped the evolution of these communities. Moreover, the inclusion of extensive geochemical data into analyses reveals new links between geochemical parameters (e.g. oxygen and trace element availability) and the distribution and taxonomic diversification of communities at the functional level. Further, an overall geochemical gradient (from multivariate analyses) between natural systems provides one of the most complete predictions of microbial taxonomic and functional composition. Clustering based on the frequency in which orthologous proteins occur among metagenomes

New evidence of effusive and explosive volcanism in the Lower Carboniferous formations of the Moroccan Central Hercynian Massif: Geochemical data and geodynamic significance

Science.gov (United States)

Ntarmouchant, A.; Smaili, H.; Bento dos Santos, T.; Dahire, M.; Sabri, K.; Ribeiro, M. L.; Driouch, Y.; Santos, R.; Calvo, R.

2016-03-01

The Azrou-Khénifra basin, located in the SE sector of the Moroccan Central Hercynian Massif of the Western Meseta of Morocco comprises volcanic and volcanoclastic rocks where two magmatic sequences can be distinguished: i) the Dhar Lahmar Sequence, composed of Upper Visean basaltic lava flows and pyroclastic deposits; and ii) the Kef Al Asri Sequence, composed of Visean - Serpukhovian intermediate to acid rocks. A continuous spatial and temporal evolution between the two volcano-sedimentary sequences was observed during the detailed geological work performed in the studied area. Petrography and geochemical studies additionally suggest a continuous compositional evolution from the more basic magmatic rocks to the intermediate/acid rocks, which implies a cogenetic magmatic differentiation controlled by crystal fractionation (with minor crustal assimilation) of a calc-alkaline trend magmatic suite. The inferred magmatic evolution is consistent with a geodynamic environment of an orogenic zone within an active continental margin setting. This partly explosive Visean - Serpukhovian volcanism, identified for the first time in the Western Meseta of Morocco, displays very similar petrographic and geochemical characteristics to its Eastern Meseta analogues, which implies that the emplacement of these magmatic rocks must have occurred in similar collisional geodynamic settings for both major geological domains, further constraining the evolution of this major crustal segment within the Carboniferous events that shaped the Hercynian Orogeny.

Perfil lipídico tecidual de ratos alimentados com diferentes fontes lipídicas

OpenAIRE

Almeida,Martha Elisa Ferreira de; Queiroz,José Humberto de; Queiroz,Maria Eliana Lopes Ribeiro de; Costa,Neuza Maria Brunoro; Matta,Sérgio Luis Pinto

2009-01-01

OBJETIVO:Determinar se fontes lipídicas com diferentes razões de ácidos graxos insaturados e saturados (PUFA+MUFA)/SFA na dieta altera o perfil lipídico tecidual, a concentração de lipídios (mg/g) dos tecidos hepáticos e mesentérico e a digestibilidade lipídica. MÉTODOS: Foi realizada cromatografia gasosa para determinar o perfil de ácidos graxos nos tecidos hepático e adiposo de ratos alimentados com diferentes fontes lipídicas. O coeficiente de digestibilidade foi determinado a partir da re...

Geochemical and petrological considerations about the basalts of upper aluminium in the Fildes Peninsula. (Rei George), Antartica

International Nuclear Information System (INIS)

Machado, A.; Fernandes de Lima, E.; Chemale, F.

1998-01-01

Petrographic, geochemical and petrological studies of lower Tertiary basaltic rocks from Fildes Peninsula in Antarctica were made to characterize their source and magmatic evolution. These basaltic rocks have porphyritic, glomeroporphyritic, intergranular and intersertal textures. The phenocrysts are of plagioclase (An), augite, pigeonite and Ti-magnetite. These basaltic rocks have AL O from 16 to 22%, Ni from 6 to 88 ppm, Co from 24 to 33 ppm and Cr from 54 to 123 ppm. Enrichment of Rb. Ba, Sr and LREE with respect to HREE is observed as relative depleted in HFSE is detected. The mass balance realized to understand the evolution of liquid that gave source the different basaltic rocks. Showed that the extracted mineral fractions were 76% of plagioclase, 2% of clinopiroxene and 21% of olivine. The intermediate volcanic rocks of Fildes Peninsula can be explained by cristalization fractionation of a basic liquid. The isotopic dates showed initial rations of Sr/Sr <0,704 and positive values of Nd epsilon. These results are strong support a mantelic source for basaltic rocks of Fildes Peninsula. On basis of geochemical, petrological and isotopic characteristics is possible concluded that these rocks were formed in an island are environment with parcial melting of mantle wedge. (author)

Proceedings of 13. International Geochemical Exploration Symposium. 2. Brazilian Geochemical Congress

International Nuclear Information System (INIS)

1989-01-01

Some works about geochemistry are presented, including themes about geochemical exploration, lithogeochemistry and isotope geochemistry, environmental geochemistry, analyical geochemistry, geochemistry of carbonatites and rare earth elements and organic geochemistry. (C.G.C.) [pt

The geochemical atlas of Alaska, 2016

Science.gov (United States)

Lee, Gregory K.; Yager, Douglas B.; Mauk, Jeffrey L.; Granitto, Matthew; Denning, Paul; Wang, Bronwen; Werdon, Melanie B.

2016-06-21

A rich legacy of geochemical data produced since the early 1960s covers the great expanse of Alaska; careful treatment of such data may provide significant and revealing geochemical maps that may be used for landscape geochemistry, mineral resource exploration, and geoenvironmental investigations over large areas. To maximize the spatial density and extent of data coverage for statewide mapping of element distributions, we compiled and integrated analyses of more than 175,000 sediment and soil samples from three major, separate sources: the U.S. Geological Survey, the National Uranium Resource Evaluation program, and the Alaska Division of Geological & Geophysical Surveys geochemical databases. Various types of heterogeneity and deficiencies in these data presented major challenges to our development of coherently integrated datasets for modeling and mapping of element distributions. Researchers from many different organizations and disparate scientific studies collected samples that were analyzed using highly variable methods throughout a time period of more than 50 years, during which many changes in analytical techniques were developed and applied. Despite these challenges, the U.S. Geological Survey has produced a new systematically integrated compilation of sediment and soil geochemical data with an average sample site density of approximately 1 locality per 10 square kilometers (km2) for the entire State of Alaska, although density varies considerably among different areas. From that compilation, we have modeled and mapped the distributions of 68 elements, thus creating an updated geochemical atlas for the State.

Las necesidades formativas del profesorado en TIC: perfiles formativos y elementos de complejidad

Directory of Open Access Journals (Sweden)

Almerich, Gonzalo

2011-09-01

Full Text Available Las necesidades formativas del profesorado en las Tecnologías de la Información y de la Comunicación (TIC se constituyen como uno de los aspectos claves para la integración de las TIC en la práctica educativa diaria, junto con las competencias en TIC y el uso de estos recursos tecnológicos por parte del profesorado. El objetivo de este artículo es establecer perfiles formativos del profesorado y relacionarlos con sus competencias en TIC y el uso de las mismas, junto con factores personales y contextuales. Para ello, se ha utilizado un diseño de encuesta, con una muestra de 868 profesores y profesoras de Educación Primaria y Secundaria de la Comunidad Valenciana, siendo el instrumento de recogida de la información un cuestionario. Los resultados indican que el profesorado demanda formación de mayor nivel en el plano personal-profesional, necesitándose más formación en los planos con el alumnado en el aula y la integración de estos recursos en el aula. Además, estas necesidades se pueden estructurar en cuatro perfiles: inicial, inicial-medio, medio y avanzado. Asimismo, se ha hallado una relación clara entre estos perfiles de necesidades formativas con las competencias en TIC, esencialmente las tecnológicas; el uso de las TIC, principalmente el plano personal-profesional. También se encuentra una influencia en estos perfiles de la edad del profesorado y la frecuencia de uso del ordenador. Esto implica que las administraciones educativas han de considerar estos resultados en el desarrollo de los planes de formación del profesorado para producir programas de mayor calidad, tal y como se demanda desde diversos ámbitos.

Perfil de los adultos mayores usuarios de atención primaria

Directory of Open Access Journals (Sweden)

Fabianne de Jesus Dias de Sousa

2017-05-01

Full Text Available Introducción: Las proyecciones indican que Brasil será el sexto país del mundo con el mayor número de adultos mayores. El objetivo de este estudio fue caracterizar las condiciones de perfil y de vida socio-demográficos y de salud de los usuarios adultos mayores de la atención primaria de un municipio en la región amazónica del Brasil. Es oportuno porque el envejecimiento de la población está creciendo rápidamente, especialmente en países en desarrollo como el Brasil. Materiales y Métodos: Estudio transversal con una muestra de 441 individuos con edad inferior a 60 años de la población de usuarios de la atención básica en el municipio de Benevides, en la Amazonia brasileña. Os datos fueron obtenidos a través del Elder notebook, un protocolo clínico del Ministerio de la Salud. La prueba del chi-cuadrado con un nivel de significancia de 5% para explorar fue utilizada las asociaciones entre las variables de las condiciones de salud y de vida, y las variables socio-demográficas. Resultados: Se presentaron un perfil predominantemente joven adultos mayores (46.0%, que no practican actividad física (p<0.02, con condiciones crónicas y uso de drogas para inducir el sueño (p<0.05. Discusión y Conclusiones: El perfil de vida desfavorable y de salud encontrados en adultos mayores exige la adopción de medidas reforzadas, sobre la salud y los presupuestos de atención integral como un desafío para efectuar la colocación de sus necesidades, principalmente por la enfermería, en la Atención Básica de Salud en áreas más necesitadas de la región amazónica. Cómo citar este artículo: Sousa FJD, Andrade FS. Perfil de los adultos mayores usuarios de atención primaria. Rev Cuid. 2017; 8(2: 1573-81. http://dx.doi.org/10.15649/cuidarte.v8i2.376

The IUGS/IAGC Task Group on Global Geochemical Baselines

Science.gov (United States)

Smith, David B.; Wang, Xueqiu; Reeder, Shaun; Demetriades, Alecos

2012-01-01

The Task Group on Global Geochemical Baselines, operating under the auspices of both the International Union of Geological Sciences (IUGS) and the International Association of Geochemistry (IAGC), has the long-term goal of establishing a global geochemical database to document the concentration and distribution of chemical elements in the Earth’s surface or near-surface environment. The database and accompanying element distribution maps represent a geochemical baseline against which future human-induced or natural changes to the chemistry of the land surface may be recognized and quantified. In order to accomplish this long-term goal, the activities of the Task Group include: (1) developing partnerships with countries conducting broad-scale geochemical mapping studies; (2) providing consultation and training in the form of workshops and short courses; (3) organizing periodic international symposia to foster communication among the geochemical mapping community; (4) developing criteria for certifying those projects whose data are acceptable in a global geochemical database; (5) acting as a repository for data collected by those projects meeting the criteria for standardization; (6) preparing complete metadata for the certified projects; and (7) preparing, ultimately, a global geochemical database. This paper summarizes the history and accomplishments of the Task Group since its first predecessor project was established in 1988.

LOS PERFILES COGNITIVOS PSICOPATOLÓGICOS EN LA FORMULACIÓN COGNITIVA DE CASO

Directory of Open Access Journals (Sweden)

Ronald Toro

2010-01-01

Full Text Available Se resaltó la relevancia de incluir los perfiles cognitivos desarrolladosde acuerdo con las categorías diagnósticas delDSM-IV TR para los trastornos de la personalidad en la formulacióncognitiva de caso. Los contenidos informacionalesdeben dar cuenta del perfil cognitivo específico del paciente,con el fin de facilitar la planeación y el curso del tratamientoajustado a sus necesidades, aunque no presente diagnósticoen el eje II. También se analizaron las implicaciones del usoinadecuado de las categorías diagnósticas en los trastornos dela personalidad; la necesidad de generar investigación en tornoal soporte empírico y psicométrico derivado de la presentepropuesta, y el entrenamiento de terapeutas cognitivos en formulacióncognitiva de caso.

A Spatially Constrained Multi-autoencoder Approach for Multivariate Geochemical Anomaly Recognition

Science.gov (United States)

Lirong, C.; Qingfeng, G.; Renguang, Z.; Yihui, X.

2017-12-01

Separating and recognizing geochemical anomalies from the geochemical background is one of the key tasks in geochemical exploration. Many methods have been developed, such as calculating the mean ±2 standard deviation, and fractal/multifractal models. In recent years, deep autoencoder, a deep learning approach, have been used for multivariate geochemical anomaly recognition. While being able to deal with the non-normal distributions of geochemical concentrations and the non-linear relationships among them, this self-supervised learning method does not take into account the spatial heterogeneity of geochemical background and the uncertainty induced by the randomly initialized weights of neurons, leading to ineffective recognition of weak anomalies. In this paper, we introduce a spatially constrained multi-autoencoder (SCMA) approach for multivariate geochemical anomaly recognition, which includes two steps: spatial partitioning and anomaly score computation. The first step divides the study area into multiple sub-regions to segregate the geochemical background, by grouping the geochemical samples through K-means clustering, spatial filtering, and spatial constraining rules. In the second step, for each sub-region, a group of autoencoder neural networks are constructed with an identical structure but different initial weights on neurons. Each autoencoder is trained using the geochemical samples within the corresponding sub-region to learn the sub-regional geochemical background. The best autoencoder of a group is chosen as the final model for the corresponding sub-region. The anomaly score at each location can then be calculated as the euclidean distance between the observed concentrations and reconstructed concentrations of geochemical elements.The experiments using the geochemical data and Fe deposits in the southwestern Fujian province of China showed that our SCMA approach greatly improved the recognition of weak anomalies, achieving the AUC of 0.89, compared

Reconnaissance Geochemical Study

African Journals Online (AJOL)

distribution patterns. The geochemical distribution maps of the elements reveal that Cu, Pb, Zn, Co, Sc, Ni, Cr, .... After filtration, the leached solutions were diluted with ultra ...... some other rare earth elements in the study area. The occurrence ...

Perfiles de regulación emocional y estrés académico en estudiantes de fisioterapia

Directory of Open Access Journals (Sweden)

Ramón González Cabanach

2017-12-01

Se obtuvieron diferencias estadísticamente significativas entre los diferentes perfiles tanto para la percepción de estresores como para las respuestas psicofisiológicas de estrés. Los estudiantes con un perfil de alta regulación emocional percibieron en menor medida el entorno académico como amenazante y experimentaron con menor frecuencia manifestaciones psicofisiológicas de estrés. Los estudiantes con perfiles de baja regulación y baja regulación con alta atención emocional mostraron resultados similares, a excepción de las alteraciones del sueño. En conclusión, los estudiantes de fisioterapia con elevadas puntuaciones en control y aceptación de sus estados emocionales perciben las circunstancias académicas de forma más adaptativa y experimentan menores respuestas de estrés.

Coupling of transport and geochemical models

International Nuclear Information System (INIS)

Noy, D.J.

1986-01-01

This report considers mass transport in the far-field of a radioactive waste repository, and detailed geochemical modelling of the ground-water in the near-field. A parallel approach to this problem of coupling transport and geochemical codes is the subject of another CEC report (ref. EUR 10226). Both studies were carried out in the framework of the CEC project MIRAGE. (Migration of radionuclides in the geosphere)

EL PERFIL COMPETITIVO LOCAL COMO FACTOR DETERMINANTE PARA EL DESARROLLO DE LA FLORICULTURA EN MADRID (CUNDINAMARCA

Directory of Open Access Journals (Sweden)

DANIEL HERNÁN SANTIAGO ROMERO

2011-01-01

Full Text Available Este artículo describe los atributos del perfil competitivo del municipio de Madrid y establece las relaciones que, con dicho perfil, ha tenido el desarrollo de cultivos de flores. Se parte de la descripción de la situación actual de la industria de la floricultura en el país. Después, tras establecer los determinantes que desde la teoría se han propuesto para medir la competitividad de un territorio, se analiza el caso particular del municipio de Madrid y define los atributos competitivos que lo caracterizan. Se presentan las relaciones entre el perfil competitivo del municipio y la floricultura, mostrando cómo aquél, se convirtió en un factor determinante para dicha actividad económica. Finalmente se presentan las conclusiones del artículo, las cuales son antecedidas por la presentación de los elementos que representan la mayor fortaleza para el desarrollo económico del municipio en el futuro.

Variabilidad de la frecuencia cardíaca y perfiles psicofisiológicos en deportes de equipo de alto rendimiento

Directory of Open Access Journals (Sweden)

Jordi Moreno S\\u00E1nchez

2013-01-01

Full Text Available En el presente trabajo se plantean dos objetivos, llevados a cabo en dos estudios diferentes. En primer lugar, se pretende analizar la utilidad del análisis de la Variabilidad de la Frecuencia Cardíaca (VFC dentro del contexto de los deportes de equipo de alto rendimiento. Por otra parte, se pretende analizar la VFC en base a los perfiles de estado de ánimo evaluados con el POMS. Para el primer estudio se seleccionaron 53 deportistas de 3 deportes de equipo de élite diferentes: baloncesto, hockey hierba y fútbol. Para el segundo estudio la muestra la formaron 18 futbolistas de élite, divididos en dos grupos: perfil iceberg y estado de ánimo alterado. Los resultados muestran que los futbolistas presentan un perfil de VFC diferente a los jugadores de baloncesto o hockey hierba, que muestran un perfil de VFC bastante parecido. En los futbolistas con perfil iceberg, el factor de Vigor correlaciona negativamente con los parámetros LF/HF y %LF, y positivamente con el parámetro HF%. En los futbolistas con estado de ánimo alterado, el factor de Fatiga correlaciona negativamente con los parámetros pNN50 y HF. Los resultados permiten profundizar en el estudio de la VFC en deportes de equipo para adaptar mejor los seguimientos, así como obtener indicadores de estado de ánimo relacionados con la VFC.

Concerning evaluation of eco-geochemical background in remediation strategy

Science.gov (United States)

Korobova, Elena; Romanov, Sergey

2015-04-01

The geochemical concept of biosphere developed by V.I. Vernadsky states the geological role of the living organisms in the course of their active chemical interaction with the inert matter (Vernadsky, 1926, 1960). Basing on this theory it is reasonable to suggest that coevolution of living organisms and their environment led to development of the dynamically stable biogeocenoses precisely adequate to their geochemical environment. Soil cover was treated by V.I. Vernadsky as a balanced bio-inert matter resulting from this interaction. Appearance of human mind and then a civilization led to global expansion of human beings, first able to survive in unfavorable geochemical conditions and then starting chemical transformation of the environment to satisfy the growing demands of mankind in food and energy. The residence in unfavorable environment and local contamination was followed by appearance of endemic diseases of plants, animals and man. Therefore zonal, regional and local chemical composition of the soil cover formed in natural conditions may be used for estimation of the optimum geochemical background, most adequate for the corresponding zonal biogeocenoses and species. Moreover, the natural geochemical background and technogenic fields have unequal spatial structure and this facilitates their identification that may be relatively easy realized in remediation strategy. On the assumption of the foregoing, the adequate methodical approach to remediation of technogenically affected areas should account of the interaction of the existing natural and the newly formed technogenic geochemical fields and include the following steps: 1) the study and mapping of geochemical structure of the natural geochemical background basing on soil maps; 2) the study of contaminants and mapping spatial distribution of technogenic releases; 3) construction of risk maps for the target risk groups with due regard to natural ecological threshold concentration in context of risk degree for

CONSUMO ALIMENTAR, PERFIL ANTROPOMÉTRICO E CONHECIMENTOS EM NUTRIÇÃO DE CORREDORES DE RUA

OpenAIRE

Ferreira, Vanessa Roriz; Bento, Ana Paula Nunes; Silva, Mara Reis

2015-01-01

Introdução A nutrição esportiva e a composição corporal são fatores importantes para o desempenho de atividades esportivas. A corrida de rua se popularizou no mundo, especialmente na última década. Os corredores de rua devem consumir uma dieta nutricionalmente adequada e ter conhecimento sobre nutrição para manter um perfil nutricional adequado. Objetivo Avaliar a adequação dietética, o perfil antropométrico e os conhecimentos em nutrição de corredores de rua. Métodos Os corredores adultos ...

Perfil formativo de los consejeros de las empresas del IBEX 35 en España

OpenAIRE

Jurado Caraballo, María Ángeles; Rodríguez Fernández, Mercedes; Gaspar González, Ana María

2017-01-01

En este estudio de carácter teórico-empírico se ha relacionado la variable Perfil formativo de los Consejeros de las empresas que componen el IBEX 35 con su evolución financiera medida en base a las ventas netas. Verificadas las hipótesis, se puede decir que el perfil más adecuado para incrementar las ventas empresariales en las empresas del IBEX en 2013 lo conforma la figura de un Consejero, que presenta un nivel formativo de Doctorado, además de haber recibido una formación adecuada al carg...

Simulación del perfil tensión-corriente para paneles solares mediante convertidor CC-CC reductor

OpenAIRE

Muñoz Palaguachi, Henry Patricio; Patiño Guiracocha, Claudio Vinicio

2017-01-01

El desarrollo de este proyecto tiene como objetivo la reconstrucción del perfil tensión-corriente para paneles solares ante diferentes condiciones de funcionamiento al variar la temperatura e irradiancia. Este perfil se logra con el control de un convertidor reductor de tipo conmutado mediante controladores de corriente y tensión. In this work the emulation of voltage-current profiles for photovoltaic panels is developed for different operating conditions, specifically for variations in ir...

The role of anthropogenic and natural factors in shaping the geochemical evolution of groundwater in the Subei Lake basin, Ordos energy base, Northwestern China.

Science.gov (United States)

Liu, Fei; Song, Xianfang; Yang, Lihu; Han, Dongmei; Zhang, Yinghua; Ma, Ying; Bu, Hongmei

2015-12-15

Groundwater resources are increasingly exploited for industrial and agricultural purposes in many arid regions globally, it is urgent to gain the impact of the enhanced anthropogenic pressure on the groundwater chemistry. The aim of this study was to acquire a comprehensive understanding of the evolution of groundwater chemistry and to identify the impact of natural and anthropogenic factors on the groundwater chemistry in the Subei Lake basin, Northwestern China. A total of 153 groundwater samples were collected and major ions were measured during the three campaigns (August and December 2013, May 2014). At present, the major hydrochemical facies in unconfined groundwater are Ca-Mg-HCO3, Ca-Na-HCO3, Na-Ca-HCO3, Na-HCO3, Ca-Mg-SO4 and Na-SO4-Cl types, while the main hydrochemical facies in confined groundwater are Ca-Mg-HCO3, Ca-Na-HCO3, Na-Ca-HCO3, Ca-HCO3 and Na-HCO3 types. Relatively greater seasonal variation can be observed in the chemical constituents of confined groundwater than that of unconfined groundwater. Rock weathering predominates the evolution of groundwater chemistry in conjunction with the cation exchange, and the dissolution/precipitation of gypsum, halite, feldspar, calcite and dolomite are responsible for the chemical constituents of groundwater. Anthropogenic activities can be classified as: (1) groundwater overexploitation; (2) excessive application of fertilizers in agricultural areas. Due to intensive groundwater pumping, the accelerated groundwater mineralization resulted in the local changes in hydrochemical facies of unconfined groundwater, while the strong mixture, especially a large influx of downward leakage from the unconfined aquifer into the confined aquifer, played a vital role in the fundamental variation of hydrochemical facies in confined aquifer. The nitrate contamination is mainly controlled by the local hydrogeological settings coupled with the traditional flood irrigation. The deeper insight into geochemical evolution of

Assessment of Muria geochemistry evolution and related to volcanic hazard to NPP site at Muria

International Nuclear Information System (INIS)

Basuki Wibowo; June Mellawati; Heni Susiati

2011-01-01

Study of geochemistry evolution aspect in Mt. Muria cycle to predict the level of volcanic hazards posed in the future on Muria nuclear power plant site was conducted. The purpose of the study was to determine the Muria geochemistry condition, tectonic patterns and to predict the level of volcanic hazard in the future on Muria nuclear power plant sites. The methodology used is the collection of secondary data on the complex geochemical conditions Muria volcanic in their life cycle, perform correlation geochemical cycle in its path towards conditions that most likely experienced tectonic, volcanic, and interpretation of the hazard posed. The study shows that geochemical conditions in Muria Volcano complex composed of potassium, low-yield product predicted high-temperature molten magma (decompression) and high potassium levels (compression). Pattern of tectonic decompression geochemical conditions associated with low potassium in Muria old, while the pattern of tectonic compression geochemical conditions associated with high potassium in young Muria. The level of volcanic hazard in the future indicated by the nature of non capable of Mt. Muria. (author)

Geochemical mapping study of Panjang island

International Nuclear Information System (INIS)

Sutisna; Sumardjo

2010-01-01

Impact of industrial and regional development are not only related to an improvement of socio-economic, but also to an environmental conservation and sustainable. This impact could be observed on a change of geochemical mapping before and after an operational of the industry. In the relation with a regional development and resources utilization, the geochemical mapping have been done in the aim to know a resources and an elemental distribution at Panjang island. In this research, ko-Instrumental Neutron Activation Analysis (k_0-INAA) have been applied in an elemental quantification on the geochemical mapping. Pencuplikan of geochemical sample have been carried out by using a grid systematic method with a sample density of about 10 sample per square kilometre involved 85 pencuplikan point. The geochemical sample of sediment and soil have been provided as a dry weight of 100 mesh. Internal quality control have done by using a number of Standard Reference Materials obtained from US. Geological Survey. Fifteen elements of Sc, Co, In, Rb, Mo, Ba, Ce, Nd, Eu, La, Yb, Th, U, lr and Hf contained in standard materials have been evaluated. The analysis result show that a relative standard deviation less than 11 %, except for Mo (13 %) and lr (26 %). Fourteen elements of Al, Br, Ca, Co, Eu, Fe, La, U, Na, Ce, Mn, As, Sc and Th have been mapped and presented in this paper. The major elements of Ca, Al and Fe, and minor elements of Mn, U and Sc are distributed at all region. The lanthanide elements of La, Ce and Eu have vary concentration and could be found at the middle to the north of the island. (author)

Hydrocarbons dating by Re-Os method: experimental study of the Re-Os couple geochemical behaviour in oils during the evolution of a petroleum system

International Nuclear Information System (INIS)

Mahdaoui, Fatima

2013-01-01

The Re-Os radiogenic system is well adapted to the dating of oils and bitumen. However the meaning of the obtained age is ambiguous. This is mainly due to gaps in our knowledge of the geochemical behavior and the speciation of Re and Os in oils. Specifically, use of the Re-Os geo-chronometer requires an understanding of how Re-Os behavior can lead to the fulfillment of the conditions necessary for the development of an isochron. These conditions are: i) the isotopic homogenization of oils at the scale of a petroleum field ii) the fractionation of Re from Os so as to obtain samples with various Re/Os ratios iii) the closure of the system during the period of radiogenic ingrowth of the daughter isotope, that is, from the time of the event of interest to the present day. Experimental investigation of the organic geochemical behavior of Re and Os in oils under various conditions, designed as analogs of the different stages of petroleum generation and evolution, were performed in order to evaluate the use of the Re-Os system as a geo-chronometer in the context of a direct use on petroleum. The possibility of Re-Os fractionation resulting from asphaltene loss during oil evolution was investigated by sequential asphaltene precipitation in the laboratory. This study determined that Re and Os are mainly located in the most polar asphaltene fractions, that is, in the first to precipitate. This study also demonstrated that Re/Os ratios are not disturbed by asphaltene loss during the evolution of oils, unless this loss is unrealistically large. Thus asphaltene precipitation during migration and emplacement is not responsible for the Re/Os fractionation required for the use of the geo-chronometer. The possibility of metal transfer from formation waters to petroleum was studied by performing contact experiments between oils and aqueous solutions of Re and Os of various concentrations over a wide range of temperatures and for varying periods of time. This study demonstrated a

The 'glass earth' - geochemical frontiers in exploration through cover

International Nuclear Information System (INIS)

Carr, G.; Denton, G.; Giblin, A.; Korsch, M.; Andrew, A.; Whitford, D.

1999-01-01

'Glass Earth' represents a number of current and planned projects within CSIRO aimed at making 'transparent' the top 1000 m of the Earth's crust It builds upon current technologies developed within a number of CSIRO divisions as well as the Australian Mineral Exploration Technologies CRC (AMET CRC), the Australian Geodynamics CRC (AG CRC) and the CRC for Landscape Evolution and Mineral Exploration (CRC LEME). New geophysical and geochemical technologies will be developed to complement these, together with new capabilities in modelling, data integration and visualisation, including hydrogeochemistry, hydrogeology, surface geochemistry and isotope geochemistry, modelling of chemical, fluid and heat flows in rock and regolith, advanced visualisation and data fusion. This paper describes some recent work in the field of isotope geochemistry, with the principal aim of 'seeing through' cover to understand basement geology and detect hidden ore systems

Late Guadalupian evolution of the Delaware Basin: insights from stable isotope and trace element geochemistry

Science.gov (United States)

Smith, B.; Kerans, C.

2017-12-01

Accurate characterization of mixed carbonate and evaporite deposits requires an understanding of basin-scale physical, chemical, and biological processes. In these settings, carbonate geochemistry often responds to changes in the prevailing conditions in the water column. It follows that the geochemical record presents a potential aid for interpretation of depositional systems provided that it is relatively free of diagenetic overprint. This is seldom the case in shallow-water settings as processes such as meteoric diagenesis and early dolomitization obscure or erase the original geochemical signal. Fine grained deep-water sediments are more likely to retain their original geochemical characteristics. If reliable shelf-to-basin correlations can be established, then basinal deposits provide critical data not only for the interpretation of deep water environments, but overall basin evolution as well. This study examines variations in trace element and stable isotope geochemistry from the Delaware Basin of West Texas and New Mexico. Interpretation of geochemical data within a pre-existing shelf-to-basin stratigraphic framework suggests a link between basin water chemistry and sea level changes during the entirety of the Guadalupian. This link is supported analogies to modern silled basins where changes in sea level and thus recharge across the sill can control nutrient input, circulation, and bottom water oxygenation. In light of these relationships, the filling of the Delaware Basin with basin-centered evaporites at the end of the Guadalupian likely represents the culmination of a more gradual, cyclic evolution towards basin restriction. Ongoing work will continue to focus on tying regional-scale changes in basin water chemistry to the combined geochemical and physical sedimentological records.

Estudo de metodologias para o dimensionamento de vigas mistas de aço e concreto com perfil celular

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A. BADKE-NETO

Full Text Available Resumo Atualmente, com o avanço da tecnologia de corte e solda, perfis de aço com aberturas sequenciais na forma circular, denominados perfis celulares, vêm sendo bastante utilizadas como vigas de edificações. A ABNT NBR 8800:2008 e as normas estrangeiras não abordam vigas de aço e vigas mistas de aço e concreto com perfil celular, o que contribui para que o seu uso seja limitado. Foi desenvolvido e aferido um programa computacional para o dimensionamento de vigas mistas de aço e concreto com perfil celular biapoiadas de acordo com duas metodologias distintas da literatura. Um estudo paramétrico abordando vigas mistas com perfis celulares obtidos de dois perfis I de aço laminados comerciais foi realizado. Nesse estudo, a influência dos parâmetros geométricos do perfil celular e do comprimento do vão da viga na resistência e na forma de colapso foi analisada. Foi possível concluir que em muitas situações o uso de vigas mistas com perfil celular é vantajoso em relação às vigas mistas de alma cheia.

Geochemical evolution of groundwater salinity at basin scale: a case study from Datong basin, Northern China.

Science.gov (United States)

Wu, Ya; Wang, Yanxin

2014-05-01

A hydrogeochemical investigation using integrated methods of stable isotopes ((18)O, (2)H), (87)Sr/(86)Sr ratios, Cl/Br ratios, chloride-mass balance, mass balance and hydrogeochemical modeling was conducted to interpret the geochemical evolution of groundwater salinity in Datong basin, northern China. The δ(2)H, δ(18)O ratios in precipitation exhibited a local meteoric water line of δ(2)H = 6.4 δ(18)O -5 (R(2) = 0.94), while those in groundwater suggested their meteoric origin in a historically colder climatic regime with a speculated recharge rate of less than 20.5 mm overall per year, in addition to recharge from a component of deep residual ancient lake water enriched with Br. According to the Sr isotope binary mixing model, the mixing of recharges from the Shentou karst springs (24%), the western margins (11%) and the eastern margins (65%) accounts for the groundwater from the deep aquifers of the down-gradient parts in the central basin is a possible mixing mechanism. In Datong, hydrolysis of silicate minerals is the most important hydrogeochemical process responsible for groundwater chemistry, in addition to dissolution of carbonate and evaporites. In the recharge areas, silicate chemical weathering is typically at the bisiallitization stage, while that in the central basin is mostly at the monosiallitization stage with limited evidence of being in equilibrium with gibbsite. Na exchange with bound Ca, Mg prevails at basin scale, and intensifies with groundwater salinity, while Ca, Mg exchange with bound Na locally occurs in the east pluvial and alluvial plains. Although groundwater salinity increases with the progress of water-rock/sediment interactions along the flow path, as a result of carbonate solubility control and continuous evapotranspiration, Na-HCO3 and Na-Cl-SO4 types of water are usually characterized respectively in the deep and the shallow aquifers of an inland basin with a silicate terrain in an arid climatic regime.

Perfil lipídico em pacientes adultos com artrite idiopática juvenil

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Thelma Larocca Skare

2013-08-01

Full Text Available O processo inflamatório articular de uma criança com artrite idiopática juvenil (AIJ pode persistir na vida adulta. A inflamação tem sido ligada a distorções do perfil lipídico e à aterogênese acelerada. Neste trabalho, estudou-se o perfil lipídico de indivíduos adultos com AIJ, comparando-o ao de pessoas saudáveis. Foram recrutados 54 adultos com AIJ (57,3% poliarticular, 37% oligoarticular, 1,9% do subtipo entesítica e 3,7% do subtipo sistêmica e 54 indivíduos saudáveis para comparação de perfil lipídico. Nos adultos AIJ, coletaram-se dados sobre sexo, idade e idade de início da doença, presença de fator reumatoide (FR e fator antinuclear (FAN, HAQ (Health Assessment Questionnaire e tempo de doença. Observou-se que hipercolesterolemia, aumento de LDL e diminuição de HDL foram mais comuns em pacientes com AIJ do que nos controles (com P = 0,016; P < 0,0001 e P = 0,0008, respectivamente. Alterações no colesterol total (CT e no LDL foram mais comuns em indivíduos com início de doença mais tardio (P = 0,0017 para CT e P = 0,023 para LDL. Em todo o grupo de pacientes com AIJ nenhuma outra variável pode ser ligada à dislipidemia tal como presença de FR, FAN, duração de doença e HAQ (P = ns. Concluiu-se que pacientes adultos com AIJ apresentam um perfil lipídico com aumento de CT e de LDL, e diminuição de HDL em relação aos controles. Nenhuma característica clínica pode ser ligada a essa alteração, exceto idade de início da doença.

The New Mars Synthesis: A New Concept Of Mars Geo-Chemical History

Science.gov (United States)

Brandenburg, J. E.

2005-02-01

A new concept of Mars climatic and geo-chemical evolution is proposed, called the NMS (New Mars Synthesis) drawing on the full spectrum of available Mars data. The proposed synthesis is that Mars and Earth, having begun with similar surface conditions, did not strongly diverge from their similar paths 4.0 Billion years ago, in the Early Noachian, instead, under the NMS, they diverged much more recently in geologic time, in the Early Amazonian. Under the NMS, biology strongly affected the geo-chemical evolution of Mars, and allowed a stable and persistent greenhouse by producing a large oxygen component in the atmosphere. The NMS assumes Mars held biology form early on, has been geologically active throughout its history, that it had a northern paleo-ocean, that it has high, approximately, 4xLunar, cratering rates and that its climate changed recently in geologic time from being basically terrestrial to its present conditions. The proposed mechanism for the stability of the Mars greenhouse was a large oxygen component in the atmosphere that created acidic and highly oxidized conditions that prevented formation of Carbonates, and the thermal and gas buffering of the paleo-ocean. The greenhouse was thus biologically and hydrologically stabilized. The greenhouse was terminated by a large atmospheric cooling event in the Early Amazonian that killed the biosphere and froze the ocean stabilizing the greenhouse. This cooling event was probably caused by the formation of the Lyot impact basin. Given the long duration of this terrestrial biosphere in this NMS, the possible appearance of fossils in some rover images is not to be unexpected and the colonization of Mars by humanity may be aided extensive fossil biomass to use as raw material.

Perfil dos trabalhadores de enfermagem no Programa de Saúde da Família

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Rafaela Azenha Teixeira

2000-09-01

Full Text Available O estudo objetiva caracterizar a configuração demográfica dos trabalhadores ligados à enfermagem de equipes do PSF de 3 municípios de São Paulo e analisar a percepção destes quanto ao perfil profissional necessário à atuação junto ao PSF. Utilizou-se como instrumento para coleta de dados a entrevista semi-estruturada. Para a sistematização inicial dos dados utilizou-se do software ETHNOGRAPH, e, posteriormente realizou-se análise temática. Os temas identificados na fala dos trabalhadores, apontam para um "perfil necessário" à atuação no PSF: há uma percepção de que os trabalhadores devem ser comunicativos, dedicados, envolvidos, solidários, carinhosos, ter bom relacionamento, disponibilidade e ajudar a população. O conjunto dos dados, embora aponte em alguns momentos para um perfil profissional que contemple uma prática de caráter assistencialista, ao mesmo tempo encaminha para uma reflexão acerca de uma nova configuração da prática assistencial alicerçada na humanização e integralidade da assistência, assim como na construção da cidadania.

2005 dossier: granite. Tome: phenomenological evolution of the geologic disposal; Dossier 2005: Granite. Tome evolution phenomenologique du stockage geologique

Energy Technology Data Exchange (ETDEWEB)

NONE

2005-07-01

This document makes a status of the researches carried out by the French national agency of radioactive wastes (ANDRA) about the phenomenological aspects of the geologic disposal of high-level and long-lived radioactive wastes (HLLL) in granite formations. Content: 1 - introduction: ANDRA's research program on disposal in granitic formation; 2 - the granitic environment: geologic history, French granites; 3 - HLLL wastes and disposal design concepts; 4 - identification, characterization and modeling of a granitic site: approach, geologic modeling, hydrologic and hydro-geochemical modeling, geomechanical and thermal modeling, long-term geologic evolution of a site; 5 - phenomenological evolution of a disposal: main aspects of the evolution of a repository with time, disposal infrastructures, B-type wastes disposal area, C-type wastes disposal area; spent fuels disposal area, radionuclides transfer and retention in the granitic environment; 6 - conclusions: available knowledge, methods and tools for the understanding and modeling of the phenomenological evolution of a granitic disposal site. (J.S.)

2005 dossier: granite. Tome: phenomenological evolution of the geologic disposal; Dossier 2005: Granite. Tome evolution phenomenologique du stockage geologique

Energy Technology Data Exchange (ETDEWEB)

NONE

2005-07-01

This document makes a status of the researches carried out by the French national agency of radioactive wastes (ANDRA) about the phenomenological aspects of the geologic disposal of high-level and long-lived radioactive wastes (HLLL) in granite formations. Content: 1 - introduction: ANDRA's research program on disposal in granitic formation; 2 - the granitic environment: geologic history, French granites; 3 - HLLL wastes and disposal design concepts; 4 - identification, characterization and modeling of a granitic site: approach, geologic modeling, hydrologic and hydro-geochemical modeling, geomechanical and thermal modeling, long-term geologic evolution of a site; 5 - phenomenological evolution of a disposal: main aspects of the evolution of a repository with time, disposal infrastructures, B-type wastes disposal area, C-type wastes disposal area; spent fuels disposal area, radionuclides transfer and retention in the granitic environment; 6 - conclusions: available knowledge, methods and tools for the understanding and modeling of the phenomenological evolution of a granitic disposal site. (J.S.)

Comportamiento termodinámico de rotores para compresores de tornillo con nuevo perfil.

Directory of Open Access Journals (Sweden)

A. Rivera Torres

2007-01-01

Full Text Available En el presente artículo se evalúa el comportamiento termodinámico de rotores para compresores de tornillo con nuevos perfiles, realizado con ayuda del software Scorpath 2000. Ello permite predecir con precisión el desempeño completo del compresor y su evaluación termodinámica, así como realizar comparaciones, en igualdad de condiciones, con el trabajo de otros compresores dotados de perfiles de otros tipos.The article displays an evaluation of the thermodynamic behaviour of screw compressor rotors with new profiles, obtained with the help of the Scorpath 2000 software. This allows predicting precisely the operation of the compressor, as well as its thermodynamic evaluation, under equal conditions, with the work of other compressors fitted with rotor profiles of other kinds.

Evaluation and prediction of oil biodegradation: a novel approach integrating geochemical and basin modeling techniques in offshore Brazil

Energy Technology Data Exchange (ETDEWEB)

Baudino, Roger [YPF S.A. (Argentina); Santos, Glauce Figueiredo dos; Losilla, Carlos; Cabrera, Ricardo; Loncarich, Ariel; Gavarrino, Alejandro [RepsolYPF do Brasil, Sao Paulo, SP (Brazil)

2008-07-01

Oil fields accounting for a large portion of the world reserves are severely affected by biological degradation. In Brazil, giant fields of the Campos Basin are producing biodegraded oils with widely variable fluid characteristics (10 to 40 deg API) and no apparent logical distribution nor predictability. Modern geochemical techniques allow defining the level of biodegradation. When original (non-degraded) oil samples and other with varying degradation level are available it might be possible to define a distribution trend and to relate it to present day geological factors such as temperature and reservoir geometry. However, other critical factors must be taken into account. But most of all, it is fundamental to have a vision in time of their evolution. This can only be achieved through 3D Basin Models coupled with modern visualization tools. The multi-disciplinary work-flow described here integrates three-dimensional numerical simulations with modern geochemical analyses. (author)

Perfiles de aprendizaje y trabajo colaborativo en entornos de simulación en 3D

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Byron Ernesto Vaca-Barahona

2016-06-01

Full Text Available Los entornos de simulación 3D con mediación pedagógica favorecen la comunicación e interacción de los estudiantes inmersos en la actividad formativa en el contexto de la secuencia pedagógica planteada, promoviendo así de manera natural el aprendizaje de los estudiantes, generándose dos tipos de comunicación: interacción entre participante y objeto 3D, e interacción del tipo participante con otro participante que en la experiencia es la que se desarrolla más espontáneamente y en mayor cantidad. Se evidencia que el comportamiento y la actuación de los perfiles Strong-Willed y Bridge son distintos. El perfil Strong-Willed se caracteriza por organizar, asumir y distribuir responsabilidades, tomar decisiones, colaborar, liderar el trabajo del grupo, ser persistente y constante. Sin embargo, el perfil Bridge se caracteriza por ser comunicativo, expresivo y motivador del grupo; se apoya en el conocimiento de los miembros del grupo para aprender y desarrollar sus actividades y carece de continuidad durante el desarrollo del trabajo grupal.

The Marbat metamorphic core-complex (Southern Arabian Peninsula) : reassessment of the evolution of a Neoproterozoic island-arc from petrological, geochemical and U-Pb zircon data

OpenAIRE

Barbey, P.; Denele, Y.; Paquette, J. L.; Berger, J.; Ganne, Jérôme; Roques, D.

2018-01-01

The Marbat basement (Sultanate of Oman) belongs to the Neoproterozoic accretion domain of the Arabian-Nubian shield. We present new geochronological, petrological and geochemical data as an extension of our previous study (Denele et al., 2017) re-interpreting this basement as a metamorphic core complex (MCC). We showed that this MCC consists of a metamorphic unit (Juffa complex) separated by an extensional detachment from a plutonic unit (Sadh complex and Tonalite plutons). Geochemical data s...

Aspectos del control de flujo con un flap Gurney rotante sobre un perfil NACA 4412

OpenAIRE

García Sainz, Mariano O.; Muñoz, Federico; Colman Lerner, Jorge León; Marañón Di Leo, Julio; Delnero, Juan Sebastián; Camocardi, Mauricio E.

2011-01-01

En el Laboratorio de Capa Límite y Fluidodinámica Ambiental, Dto. de Aeronáutica, Facultad de Ingeniería (UNLP), se realizaron ensayos con un modelo de ala con perfil NACA 4412, provisto de un miniflap Gurney móvil en el intradós, ubicado al 8%c desde el borde de fuga (c: cuerda del perfil). El modelo de ala, sin torsión, tiene 50cm de cuerda y 80cm de envergadura. El miniflap, de longitud 79.5cm y altura 2%c, posee movimiento de rotación alrededor de su eje, a través de un sistema electromec...

Proyecto Docente e Investigador. Catedrático de Universidad. Perfil Docente: Ingeniería del Software y Gobierno de Tecnologías de la Información. Perfil Investigador: Tecnologías del Aprendizaje. Área de Ciencia de la Computación e Inteligencia Artificial

OpenAIRE

García-Peñalvo, F. J.

2018-01-01

Proyecto Docente e Investigador. Catedrático de Universidad. Perfil Docente: Ingeniería del Software y Gobierno de Tecnologías de la Información. Perfil Investigador: Tecnologías del Aprendizaje. Área de Ciencia de la Computación e Inteligencia Artificial. Universidad de Salamanca 15 de mayo de 2018

Perfil dos Psicólogos Inscritos na Subsede Leste do CRP-04

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Keicy Rocha Santos

Full Text Available O objetivo deste estudo foi fazer um levantamento do perfil profissional dos psicólogos inscritos na Subsede Leste do Conselho Regional de Psicologia nº 04 (CRP-04, atuantes no município de Governador Valadares até 2010. Trata-se de um estudo quantitativo e comparativo entre os dados da presente pesquisa e aqueles que compõem o banco nacional, que se encontra na obra O trabalho do Psicólogo no Brasil, organizado por Bastos, Gondim e colaboradores (2010. Utilizou-se um questionário via e-mail marketing, respondido por 85 participantes que abarcaram as categorias do perfil profissional. Os dados levantados foram tabulados no programa Microsoft Excel e analisados no programa Sphinx Survey Edição Léxica. Verificou-se que a maioria dos participantes é branca, casada, do gênero feminino, com idade entre 26 e 30 anos e graduada em instituição privada, tendo especialização, principalmente em clínica organizacional e atuação na clínica. Ganha entre 3 e 4 salários mínimos como psicólogo, na condição de assalariado. Geralmente, a maioria não possui outra atividade profissional e a renda familiar é de, aproximadamente, 10 salários mínimos. Os dados corroboram com a média nacional do perfil profissional dessa classe de trabalhadores, trazendo algumas peculiaridades do município de Governador Valadares.

PERFIL SENSORIAL DE CULTIVARES DE FEIJÃO SOB DIFERENTES TEMPOS DE COZIMENTO

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Viviani Ruffo de OLIVEIRA

2013-04-01

Full Text Available O objetivo deste trabalho foi determinar o tempo necessário de cozimento de cultivares de feijão de grãos preto e carioca, em panela de pressão doméstica, para a identificação de cultivares de melhor perfil sensorial para o consumo. Para tanto, utilizaram-se grãos de quatro cultivares de feijão: BRS Expedito, BRS Campeiro, Pérola e Carioca e o cozimento foi realizado em panela de pressão doméstica por 15, 20, 25 e 30 minutos. A avaliação do perfil sensorial foi efetuada em três etapas: seleção, treinamento para a Análise Descritiva Quantitativa (ADQ e ADQ propriamente dita, com sete avaliadores treinados. Os avaliadores reconheceram diferenças para as cultivares de feijão quanto à uniformidade da cor do grão, cor do caldo, à viscosidade, à dureza e a granulosidade. A ruptura no tegumento dos grãos foi maior à medida que se aumentou o tempo de cozimento. A dureza e a granulosidade apresentaram maiores intensidades conforme aumentou o tempo de cozimento dos grãos de feijão. A utilização de 20 a 25 minutos de cozimento em panela de pressão doméstica possibilita a identificação de cultivares de feijão de grãos preto e carioca com melhor perfil sensorial para o consumo, mantendo a integridade dos grãos cozidos.

Kinetics of Uranium(VI) Desorption from Contaminated Sediments: Effect of Geochemical Conditions and Model Evaluation

International Nuclear Information System (INIS)

Liu, Chongxuan; Shi, Zhenqing; Zachara, John M.

2009-01-01

Stirred-flow cell experiments were performed to investigate the kinetics of uranyl (U(VI)) desorption from a contaminated sediment collected from the Hanford 300 Area at the US Department of Energy (DOE) Hanford Site, Washington. Three influent solutions of variable pH, Ca and carbonate concentrations that affected U(VI) aqueous and surface speciation were used under dynamic flow conditions to evaluate the effect of geochemical conditions on the rate of U(VI) desorption. The measured rate of U(VI) desorption varied with solution chemical composition that evolved as a result of thermodynamic and kinetic interactions between the influent solutions and sediment. The solution chemical composition that led to a lower equilibrium U(VI) sorption to the solid phase yielded a faster desorption rate. The experimental results were used to evaluate a multi-rate, surface complexation model (SCM) that has been proposed to describe U(VI) desorption kinetics in the Hanford sediment that contained complex sorbed U(VI) species in mass transfer limited domains. The model was modified and supplemented by including multi-rate, ion exchange reactions to describe the geochemical interactions between the solutions and sediment. With the same set of model parameters, the modified model reasonably well described the evolution of major ions and the rates of U(VI) desorption under variable geochemical and flow conditions, implying that the multi-rate SCM is an effective way to describe U(VI) desorption kinetics in subsurface sediments

Adjustment of geochemical background by robust multivariate statistics

Science.gov (United States)

Zhou, D.

1985-01-01

Conventional analyses of exploration geochemical data assume that the background is a constant or slowly changing value, equivalent to a plane or a smoothly curved surface. However, it is better to regard the geochemical background as a rugged surface, varying with changes in geology and environment. This rugged surface can be estimated from observed geological, geochemical and environmental properties by using multivariate statistics. A method of background adjustment was developed and applied to groundwater and stream sediment reconnaissance data collected from the Hot Springs Quadrangle, South Dakota, as part of the National Uranium Resource Evaluation (NURE) program. Source-rock lithology appears to be a dominant factor controlling the chemical composition of groundwater or stream sediments. The most efficacious adjustment procedure is to regress uranium concentration on selected geochemical and environmental variables for each lithologic unit, and then to delineate anomalies by a common threshold set as a multiple of the standard deviation of the combined residuals. Robust versions of regression and RQ-mode principal components analysis techniques were used rather than ordinary techniques to guard against distortion caused by outliers Anomalies delineated by this background adjustment procedure correspond with uranium prospects much better than do anomalies delineated by conventional procedures. The procedure should be applicable to geochemical exploration at different scales for other metals. ?? 1985.

Geochemical Astro- and Geochronological Constraints on the Early Jurassic

Science.gov (United States)

Storm, M.; Condon, D. J.; Ruhl, M.; Jenkyns, H. C.; Hesselbo, S. P.; Al-Suwaidi, A. H.; Percival, L.

2017-12-01

The Early Jurassic Hettangian and Sinemurian time scales are poorly defined due to the lack of continuous geochemical records, and the temporal constrain of the Toarcian Oceanic Anoxic Event and associated global carbon cycle perturbation is afflicted by geochemical and biostratigraphical uncertainties of the existing radiometric dates from various volcanic ash bearing sections. Here we present a continuous, orbitally paced Hettangian to Pliensbachian carbon-isotope record of the Mochras drill-core (Cardigan bay Basin, UK). The record generates new insights into the evolution and driving mechanisms of the Early Jurassic carbon cycle, and is contributing to improve the Hettangian and Sinemurian time scale. Furthermore, we introduce a new high-resolution carbon-isotope chemostratigraphy, integrated with ammonite biostratigraphy and new U/Pb single zircon geochronology of the Las Overas section (Neuquén Basin, Argentina). The studied section comprises sediments from the tenuicostatum to Dumortiera Andean Ammonite zone (tenuicostatum to levesqui European standard zones). A stratigraphically expanded negative shift in d13Corg values, from -24‰ down to -32­‰, appears in the tenuicostatum and hoelderi ammonite zone, coeval to the negative excursion in European realm which is associated with the Toarcian Oceanic Anoxic Event. The negative isotope excursion appears concomitant with an increase in sedimentary mercury levels, indicating enhanced volcanic activity. TOC values and elemental data suggest a high sedimentation dilution in the tenuicostatum to pacificum zone. The new geochronological data from several volcanic ash beds throughout the section are further improving the temporal correlation between the Early Toarcian isotope event and causal mechanisms

New results for Palaeozoic volcanic phases in the Prague Basin – magnetic and geochemical studies of Lištice, Czech Republic

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Tiiu Elbra

2015-02-01

Full Text Available Palaeo-, rock magnetic and geochemical studies were conducted on volcanic samples from the Lištice area to improve the knowledge of Palaeozoic volcanic evolution in the Prague Basin. The magnetic data display no significant differences between two studied localities, indicating one magnetizing event for both localities. Geochemical data suggest that Lištice basalt could have originated from deep melting of the garnet peridotite mantle source during the attenuation and rifting of the continental lithosphere connected with asthenospheric mantle upwelling. The dataset furthermore supports the evidence of syn- or post-intrusive fluid interactions and low-temperature stages of alteration. The Ti-magnetite within amygdales of the samples was found to be carrying the characteristic remanent magnetization and reflects probably the Permo-Carboniferous remagnetization of volcanic phases.

PERFIL SOCIOECONÔMICO E CLÍNICO DE UM GRUPO DE DIABÉTICOS EM TRATAMENTO HEMODIALÍTICO EM CURITIBA

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Cláudia Ribeiro de Vasconcelos

2013-08-01

Full Text Available A Diabetes Mellitus do tipo 2 (DM2 é uma das doenças crônicas de maior incidência na população brasileira. Sua evolução sem tratamento adequado pode ocasionar a Nefropatia Diabética (ND e a Doença Renal Crônica (DRC levando à necessidade de uma terapêutica renal substitutiva com destaque à hemodiálise (HD. O paciente renal crônico precisa adaptar-se à terapia nutricional e hídrica que se torna mais restritiva quando adicionada à DM2, precisando de orientação e apoio fornecidos por profissionais capacitados para o gerenciamento de sua nova condição. Este estudo tem como objetivo descrever o perfil social, econômico e clínico do nefropata diabético e as implicações para o cuidado de enfermagem. Foi realizada uma pesquisa quantitativa, descritiva e transversal com amostra composta por 50 pacientes de uma clínica de HD da cidade de Curitiba - PR. Os dados foram coletados de setembro a outubro de 2012. Constatou-se que o perfil socioeconômico dos pacientes é formado por uma discreta predominância de homens acima de 60 anos, casados, aposentados, cor branca, católicos, baixas escolaridade e renda familiar, conveniados ao Sistema Único de Saúde (SUS. Quanto ao perfil clínico, à maior porcentagem apresenta hipertensão, índice de massa corporal normal, normoglicemia, usam insulina e apresentam crises de hipotensão. Conclui-se que, conhecer o perfil dos clientes diabéticos em tratamento hemodialítico contribui para que as ações da equipe multiprofissional, principalmente do enfermeiro, sejam direcionadas a preservar a capacidade física dos pacientes e ainda reduzir o perfil de morbidade e mortalidade.

Monitoring active volcanoes: The geochemical approach

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Takeshi Ohba

2011-06-01

Full Text Available

The geochemical surveillance of an active volcano aims to recognize possible signals that are related to changes in volcanic activity. Indeed, as a consequence of the magma rising inside the volcanic "plumbing system" and/or the refilling with new batches of magma, the dissolved volatiles in the magma are progressively released as a function of their relative solubilities. When approaching the surface, these fluids that are discharged during magma degassing can interact with shallow aquifers and/or can be released along the main volcano-tectonic structures. Under these conditions, the following main degassing processes represent strategic sites to be monitored.

The main purpose of this special volume is to collect papers that cover a wide range of topics in volcanic fluid geochemistry, which include geochemical characterization and geochemical monitoring of active volcanoes using different techniques and at different sites. Moreover, part of this volume has been dedicated to the new geochemistry tools.

L'auptòsia psicològica en l'homicidi d'autor desconegut (el vincle víctima-victimari: la rellevància del perfil victimològic per confeccionar el perfil criminal de l'homicida desconegut)

OpenAIRE

Moré Rodríguez, Rubén

2017-01-01

Històricament, la majoria de la recerca en la investigació criminal s'ha focalitzat en el victimari i l'iter criminis en detriment de l'estudi de la víctima i l'iter victimae. No obstant, atenent a l'auge de la victimologia forense, la Psicologia Criminal en l'àmbit del perfil criminològic ha pres més atenció al perfil victimològic, el qual constitueix l'estudi exhaustiu en termes retrospectius de tota la informació disponible de la víctima, en aquest cas no supervivent i d'homicidi d'autor d...

Geochemical baseline studies of soil in Finland

Science.gov (United States)

Pihlaja, Jouni

2017-04-01

The soil element concentrations regionally vary a lot in Finland. Mostly this is caused by the different bedrock types, which are reflected in the soil qualities. Geological Survey of Finland (GTK) is carrying out geochemical baseline studies in Finland. In the previous phase, the research is focusing on urban areas and mine environments. The information can, for example, be used to determine the need for soil remediation, to assess environmental impacts or to measure the natural state of soil in industrial areas or mine districts. The field work is done by taking soil samples, typically at depth between 0-10 cm. Sampling sites are chosen to represent the most vulnerable areas when thinking of human impacts by possible toxic soil element contents: playgrounds, day-care centers, schools, parks and residential areas. In the mine districts the samples are taken from the areas locating outside the airborne dust effected areas. Element contents of the soil samples are then analyzed with ICP-AES and ICP-MS, Hg with CV-AAS. The results of the geochemical baseline studies are published in the Finnish national geochemical baseline database (TAPIR). The geochemical baseline map service is free for all users via internet browser. Through this map service it is possible to calculate regional soil baseline values using geochemical data stored in the map service database. Baseline data for 17 elements in total is provided in the map service and it can be viewed on the GTK's web pages (http://gtkdata.gtk.fi/Tapir/indexEN.html).

PERFIL ALIMENTAR E ESTADO NUTRICIONAL DE CRIANÇAS NO PRIMEIRO ANO DE VIDA

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Marisa da Silva Corrêa

2016-11-01

Full Text Available Resumo – O leite materno é a base alimentar do lactente, devendo ser oferecido de maneira exclusiva nos primeiros seis meses de vida e mantido até os dois anos de idade ou mais. O presente estudo teve como finalidade avaliar o perfil alimentar e estado nutricional de crianças no primeiro ano de vida. Para tal fim, foram captadas crianças de 0 a 12 meses atendidas na Clínica Escola de Nutrição da UFES/Alegre-ES. O perfil alimentar foi avaliado qualitativamente e o estado nutricional através das medidas de peso e comprimento, convertidos nos índices peso/idade, comprimento/idade e Índice de Massa Corporal/Idade. O estudo contemplou 34 lactentes com idade entre 10 dias e 1 ano, sendo 56% do sexo feminino. Verificou-se que 14,7% apresentavam risco de sobrepeso ou sobrepeso, 82,35% dos lactentes consumia leite materno exclusivamente ou com fórmula infantil, 66,6% das mães introduziram alimentos com 6 meses e 10% das crianças já havia consumido refrigerante, biscoito recheado e bolos artificiais no primeiro ano de vida. Faz-se necessária conscientização das mães quanto à introdução alimentar infantil. Palavras-chave: lactente, perfil alimentar, estado nutricional, aleitamento materno, introdução alimentar. Área do Conhecimento: Ciências da Saúde

Reassessment of the origin of the Dun Mountain Ophiolite, New Zealand : Nd-isotopic and geochemical evolution of magma suites

International Nuclear Information System (INIS)

Sivell, W.J.; McCulloch, M.T.

2000-01-01

Magmatic suites with contrasting isotopic and geochemical compositions, sequentially emplaced in different tectonic regimes, comprise the Dun Mountain Ophiolite Belt (DMOB), New Zealand. At D'Urville Island, the northernmost exposure of the DMOB, earliest erupted (stage 1) pillow basalts ε Nd (T) = +6.3 to +7.5, and are incompatible element enriched, like basalts from geochemically anomalous ridge segments. Overlying stage 2 basalts (sheeted flows) show a narrow range of ε Nd (T) = +8.3 + or -0.2, with chemical characteristics of depleted backarc basin basalts. These rocks are intruded by mafic to silicic stage 3 magmas, which have high uniform initial 143 Nd/ 144 Nd ratios (ε Nd (T) = +9.3 + or -0.2) over a wide range of 147 Sm/ 144 Nd values (yielding a precise Early Permian Nd-isotope age of 278 ± 4 Ma (MSWD = 0.48)). Stage 3 magmas show pronounced subduction-related geochemical signatures similar to island arc tholeiites (IAT) from immature arcs. They are closely analogous to some (boninite)-IAT magmas which characterise 'infant arc' eruptive activity in forearc basins of present-day Western Pacific island arc systems. A wide variety of stage 3 magma compositions, ranging from near-primary basaltic dikes (Mg = 74) to extremely fractionated silicic plagiogranites with uniformly very depleted isotopic ratios, is consistent with slow spreading rates which gave rise to polybaric, closed-system fractionation of magmas and periodic chamber abandonment. Some stage 3 rocks with SiO 2 levels in the andesite range have low-TiO 2 contents and high Mg, and may be fractionated equivalents of boninites. High ε Nd (T) values of stage 3 magmas indicate a lack of subducted sediment with inherited crustal residence signatures, and reflect the extent of supra-subduction zone (SSZ) mantle wedge depletion. DMOB stage 3 magmas may represent foreac magmatism that was the precursor to normal subduction-related volcanism established by c. 265 Ma in the Brook Street Arc and derived

The geochemical evolution of syncollisional magmatism and the implications for significant magmatic-hydrothermal lead-zinc mineralization (Gangdese, Tibet)

Science.gov (United States)

Zhou, Jinsheng; Yang, Zhusen; Hou, Zengqian; Liu, Yingchao; Zhao, Xiaoyan; Zhang, Xiong; Zhao, Miao; Ma, Wang

2017-09-01

In addition to well-known subduction processes, the collision of two continents also generates abundant ore deposits, as in the case of the Tibetan Plateau, which is the youngest and most spectacular collisional belt on Earth. During the building history of the Gangdese magmatic belt, several magmatic flare-up events developed, however, significant magmatic-hydrothermal lead-zinc mineralization dominantly accompanied the magmatism during the syncollisional period ( 65-41 Ma). Based on integrated geochemical and isotopic data, we provide insights into the genesis and evolution of syncollisional magmas, and their implications for significant magmatic-hydrothermal lead-zinc mineralization. The Sr-Nd isotopic compositions of most syncollisional igneous rocks (87Sr/86Sr = 0.7034-0.7123; εNd(t) = - 9.0 to + 1.8) indicate a mixing origin between mantle-derived basaltic magmas and ancient crustal melts, and fractional crystallization is a fundamental mechanism by which syncollisional magmas evolve towards intermediate to silicic compositions. Most lead-zinc mineralization-related plutons are high silica (76.14% wt.% SiO2 on average), high oxygen fugacity (average ΔFMQ + 2.5) granites with highly evolved chemical signatures [average Eun/Eun* = 0.33, high Rb/Sr (average = 3.9)], and they represent the final products from primary magmas. Due to the contribution of ancient crustal melts to the genesis of mineralization-related parent magmas, the spatial distribution of Pb-Zn deposits within the northern Gangdese magmatic belt is controlled by the lithospheric architecture. In compressional environments, magmas have low evacuation efficiency and long magma chamber lifespan, which is favorable for basaltic parents evolved to high silica granites through sufficient fractional crystallization. This scenario contributes to our understanding of the significant magmatic-hydrothermal lead-zinc mineralization that occurred in the syncollisional period.

Perfiles y estilos gerenciales, de la administracion de una empresa social del estado en el departamento de Cundinamarca

OpenAIRE

Serrano Trujillo, Adriana Carolina; Cortés Arboleda, Andrea

2015-01-01

El estudio “Identificar el perfil y el estilo del gerente, para administrar una Empresa Social del Estado en el Departamento de Cundinamarca” tiene como propósito conocer el perfil como conocimientos, habilidades o aptitudes, experticia y actitudes o comportamientos, lo mismo que el estilo gerencial en las organizaciones de hoy, como puede hacerla rentable y enfrentar los retos de un mundo globalizado, en una administración compleja, con incertidumbres y desafíos propios del Siglo XXI. Es...

PERFIL PARA REPRESENTAR UNA ARQUITECTURA DE COMPONENTES EN UML

Directory of Open Access Journals (Sweden)

Fernando Orejas Valdés

2006-04-01

Full Text Available

El lenguaje unificado de modelado (Unified Modeling Language, UML es un lenguaje de modelado estándar para problemas generales, sin embargo, es necesario extenderlo para dominios específicos como puede ser el caso de determinadas arquitecturas. Aquí se presenta una extensión mediante un perfil para una arquitectura de componentes y conectores genéricos.

Predictive geochemical mapping using environmental correlation

International Nuclear Information System (INIS)

Wilford, John; Caritat, Patrice de; Bui, Elisabeth

2016-01-01

The distribution of chemical elements at and near the Earth's surface, the so-called critical zone, is complex and reflects the geochemistry and mineralogy of the original substrate modified by environmental factors that include physical, chemical and biological processes over time. Geochemical data typically is illustrated in the form of plan view maps or vertical cross-sections, where the composition of regolith, soil, bedrock or any other material is represented. These are primarily point observations that frequently are interpolated to produce rasters of element distributions. Here we propose the application of environmental or covariate regression modelling to predict and better understand the controls on major and trace element geochemistry within the regolith. Available environmental covariate datasets (raster or vector) representing factors influencing regolith or soil composition are intersected with the geochemical point data in a spatial statistical correlation model to develop a system of multiple linear correlations. The spatial resolution of the environmental covariates, which typically is much finer (e.g. ∼90 m pixel) than that of geochemical surveys (e.g. 1 sample per 10-10,000 km 2 ), carries over to the predictions. Therefore the derived predictive models of element concentrations take the form of continuous geochemical landscape representations that are potentially much more informative than geostatistical interpolations. Environmental correlation is applied to the Sir Samuel 1:250,000 scale map sheet in Western Australia to produce distribution models of individual elements describing the geochemical composition of the regolith and exposed bedrock. As an example we model the distribution of two elements – chromium and sodium. We show that the environmental correlation approach generates high resolution predictive maps that are statistically more accurate and effective than ordinary kriging and inverse distance weighting interpolation

Estudantes de enfermagem têm perfil empreendedor?

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Paulo Fernando Roncon

Full Text Available Estudo descritivo-exploratório que teve como objetivo conhecer o perfil dos estudantes concluintes de um curso de graduação em enfermagem quanto ao empreendedorismo. O Teste de Tendência Empreendedora Geral, contendo 54 questões, foi aplicado a 41 estudantes. Os resultados demonstraram que14% apresentam cinco tendências empreendedoras e 12% quatro tendências empreendedoras; 80% apresentam fraca ou nenhuma tendência empreendedora. A grande maioria pretende encaminhar sua a profissão em atividades assistenciais, enquanto nenhum dos estudantes pretende atuar em atividades administrativas. Conclui-se que, os estudantes possuem baixo grau de presença de características empreendedoras.

Perfil de clientes colostomizados inscritos em programa de atenção aos estomizados

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Mara Rúbia Violin

2008-12-01

Full Text Available A experiência de ter uma colostomia conduz as pessoas a viverem situações diferenciadas. O objetivo deste estudo descritivo, exploratório, de natureza quantitativa, foi o de identificar o perfil do paciente colostomizado, inscrito no Programa de Atenção ao Estomizado – PAE, da 15ª Regional de Saúde do Paraná. A coleta foi realizada no mês de maio de 2007 e foi considerado o intervalo de tempo das fichas inscritas no PAE de janeiro de 2003 a maio de 2007. O perfil foi caracterizado segundo dados demográficos, doença base que levou a confecção do estoma, tipo de dispositivo, tratamento e tempo de uso do dispositivo coletor. Os resultados do estudo permitiram a obtenção de dados de importância epidemiológica para futuras intervenções como campanhas de prevenção, diagnóstico e tratamento precoce, assim como, o conhecimento da estrutura do atendimento profissional existente e as necessidades de informação das famílias dos pacientes. A definição do perfil dos pacientes além de contribuir para a melhoria do atendimento prestado permite o estabelecimento de novas proposições para a melhoria da qualidade de vida dos pacientes e da família.

Perfil do pesquisador fisioterapeuta brasileiro

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HJCG Coury

Full Text Available OBJETIVO: Traçar um perfil do pesquisador fisioterapeuta quanto a sua formação, produção científica e fomento e bolsas obtidos pela área do Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq. MÉTODOS: Foram consultados os curricula vitae de cada pesquisador fisioterapeuta com doutorado disponíveis na Plataforma Lattes do CNPq, que é uma agência do MCT dedicada à promoção da pesquisa científica e à formação de recursos humanos para a pesquisa. A escolha dessa fonte pública de informação ocorreu porque cada pesquisador interessado em auxílios de pesquisa ou envolvidos com a pós-graduação deve preencher eletronicamente um curriculum vitae com informações sobre formação e produção científica. O sistema requer uma senha pessoal e uma declaração do pesquisador atestando a veracidade das informações fornecidas, o que assegura precisão no preenchimento. Estatísticas sobre fomento e bolsas disponíveis foram também consultadas. Uma análise de regressão binária foi rodada para explicar a ocorrência de publicações ISI/JCR. RESULTADOS: Houve um crescimento extraordinário (900% no número de doutores com graduação em Fisioterapia, na última década, em áreas tradicionais ou novos campos de atuação e crescimento expressivo em número de artigos publicados, dissertações e teses orientadas. Os fatores analisados pela regressão conseguiram explicar 49,8% da ocorrência de artigos indexados. Dados de fomento e bolsas mostram um investimento pequeno do CNPq na Fisioterapia comparativamente às demais áreas da Saúde. CONCLUSÕES: O perfil do pesquisador traçado aqui poderá prover à comunidade acadêmica uma perpectiva de sua identidade e auxiliar no estabelecimento de prioridades futuras para o aprimoramento do conhecimento e prática profissional.

Perfil de los usuarios activos y finales de clubes deportivos de Bogotá D. C.

Directory of Open Access Journals (Sweden)

Billy Crissien

2010-08-01

hacia los clubes en las diferentes disciplinas deportivas y analizar el caso particular de los hinchas de equipos profesionales. Para esto, se desarrolló una investigación descriptiva con encuestas a 336 usuarios activos y finales de clubes deportivos en la ciudad de Bogotá. Los resultados muestran un perfil diferencial para jugadores y espectadores a nivel de estilo de vida, hábitos saludables y patrón de interacción con los eventos deportivos. Los hinchas de los equipos profesionales de fútbol poseen un perfil similar al de los usuarios finales de los clubes de otras disciplinas, pero evidencian un nivel de involucramiento mucho más alto.

Comportamento do Consumidor Educacional: seu Perfil e o Processo de Decisão de Compra

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Alessandra Daiana Schinaider

2016-08-01

Full Text Available O estudo do comportamento do consumidor é importante para elaboração das estratégias de marketing da empresa visando atender seu público-alvo, garantindo a satisfação dos seus clientes. Este artigo tem como objetivo analisar o comportamento do consumidor do Centro Universitário Internacional – UNINTER identificando seu perfil e como acontece seu processo de decisão de compra. Foi realizado um estudo de caso com uma pesquisa qualitativa-quantitativa e descritiva utilizando a técnica de amostragem não-probabilística por conveniência. Verificou-se que o perfil feminino jovem que possui uma vida financeira independente é o principal público-alvo desse centro universitário. Além disso, o comportamento do consumidor educacional enquadra-se em um perfil econômico e de estudante não-tradicional tendo seu processo decisório de compra influenciado por diversos fatores culturais, pessoais, sociais e psicológicos. Os resultados permitem entender o comportamento do consumidor educacional do centro universitário auxiliando os profissionais de marketing na elaboração de melhores estratégias para atingir esse público.

COMPARACIÓN DEL PERFIL LIPÍDICO POR SEXO Y EDAD EN OVINOS

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J. H. Osorio

2015-01-01

Full Text Available Se comparó el perfil lipídico y la correlación entre los componentes lipídicos del suero en cuatro grupos de ovinos. A tal fin, se tomaron muestras de sangre de 98 ovinos en ayuno, diferenciados por género y edad (23 machos y 25 hembras mayores de un año de edad; 22 machos y 28 hembras menores a un año. Se determinaron las concentraciones séricas de: triglicéridos, colesterol total (CT y colesterol de lipoproteínas de alta densidad (C-HDL mediante el método enzimático colorimétrico. El colesterol de lipoproteína de muy baja densidad (C-VLDL y de baja densidad (C-LDL se determinó usando la fórmula de Friedewald. Las medias para CT, triglicéridos, C-HDL, C-VLDL y C-LDL (mg/dL fueron de 86.19, 21.57, 39.32, 4.31 y 42.55, respectivamente. En el grupo de adultos existe diferencia significativa (P ≤0.05 en los niveles de: CT (P 0.90 para ambos, machos (P >0.405 para ambos, jóvenes (P >0.487 para ambos y adultos (P >0.179 para ambos no mostraron diferencias significativas (P -valor ≥0.05 con un nivel de confianza del 95.0%. En conclusión, debido a las diferencias estadísticamente significativas en las comparaciones del perfil lipídico entre grupos de ovinos, pueden ser considerados cuatro perfiles lipídicos: machos adultos, hembras adultas, machos jóvenes y hembras jóvenes.

The 2014-15 eruption and the short-term geochemical evolution of the Fogo volcano (Cape Verde): Evidence for small-scale mantle heterogeneity

Science.gov (United States)

Mata, J.; Martins, S.; Mattielli, N.; Madeira, J.; Faria, B.; Ramalho, R. S.; Silva, P.; Moreira, M.; Caldeira, R.; Moreira, M.; Rodrigues, J.; Martins, L.

2017-09-01

Recurrent eruptions at very active ocean island volcanoes provide the ideal means to gain insight on the scale of spatial variations at the mantle source and on temporal changes of magma genesis and evolution processes. In 2014, after 19 years of quiescence, Fogo volcano (Cape Verde Archipelago) experienced a new eruption, with the vents located 200 m from those of the 1995 eruption, and less than 2000 m from those of the 1951 event. This offered a unique opportunity to investigate the existence of small-scale mantle heterogeneities and the short-term compositional evolution of magmas erupted by a very active oceanic volcano like Fogo. Here we present petrological and geochemical data from the early stages of the Fogo's most recent eruption - started on November 23, 2014 - and compare them with the signature of previous eruptions (particularly those of 1995 and 1951). The magmas erupted in 2014 are alkaline (up to 23.4% and 0.94% of normative ne and lc, respectively) with somewhat evolved compositions (Mg # < 56), ranging from tephrites to phonotephrites. The eruption of phonotephritic lavas preceded the effusion of tephritic ones. Lavas carried to the surface clinopyroxene and kaersutite phenocrysts and cognate megacrysts, which indicate that the main stages of magma evolution occurred in magma chambers most probably located at mantle depths (25.6 ± 5.5 km below sea level). This was followed by a shallower (< 1.5 km below sea level) and shorter (≈ 50 days) magma stagnation before the eruption. 2014 magmas have more unradiogenic Sr and more radiogenic Nd compositions than those of the previous 1951 and 1995 eruptions, which generally have less radiogenic Pb ratios. These isotopic differences - coming from quasi-coeval materials erupted almost in the same place - are remarkable and reflect the small-scale heterogeneity of the underlying mantle source. Moreover, they reflect the limited isotopic averaging of the source composition during partial melting events as

A conceptual model for groundwater flow and geochemical evolution in the southern Outaouais Region, Québec, Canada

International Nuclear Information System (INIS)

Montcoudiol, N.; Molson, J.; Lemieux, J.-M.; Cloutier, V.

2015-01-01

Highlights: • Geochemical and isotope data help constrain the 2D conceptual flow model. • Stable isotopes indicate recharge occurring under conditions similar to current climate. • Mixing was found between younger ( 3 H) and older ( 14 C and 4 He) groundwater. • Mixing occurred under natural flow conditions and/or was induced during sampling. • The new conceptual model shows dominant local and intermediate flow systems. - Abstract: A conceptual model was developed for a hydrogeological flow system in the southern Outaouais Region, Quebec, Canada, where the local population relies heavily on groundwater pumped from shallow overburden aquifers and from deeper fractured crystalline bedrock. The model is based on the interpretation of aqueous inorganic geochemical data from 14 wells along a cross-section following the general flow direction, of which 9 were also analysed for isotopes (δ 18 O, δ 2 H, 3 H, δ 13 C, 14 C) and 4 for noble gases (He, Ne, Ar, Xe, Kr). Three major water types were identified: (1) Ca–HCO 3 in the unconfined aquifer as a result of silicate (Ca-feldspar) weathering, (2) Na–Cl as a remnant of the post-glacial Champlain Sea in stagnant confined zones of the aquifer, and (3) Na–HCO 3 , resulting from freshening of the confined aquifer due to Ca–Na cation exchange. Chemical data also allowed the identification of significant mixing zones. Isotope and noble gas data confirm the hypothesis of remnant water from the Champlain Sea and also support the hypothesis of mixing processes between a young tritium-rich component with an older component containing high 4 He concentrations. It is still unclear if the mixing occurs under natural flow conditions or if it is induced by pumping during the sampling, most wells being open boreholes in the bedrock. It is clear, however, that the hydrogeochemical system is dynamic and still evolving from induced changes since the last glaciation. As a next step, the conceptual model will serve as a

Sharp fronts within geochemical transport problems

International Nuclear Information System (INIS)

Grindrod, P.

1995-01-01

The authors consider some reactive geochemical transport problems in groundwater systems. When incoming fluid is in disequilibrium with the mineralogy sharp transition fronts may develop. They show that this is a generic property for a class of systems where the timescales associated with reaction and diffusion phenomena are much shorter than those associated with advective transport. Such multiple timescale problems are relevant to a variety of processes in natural systems: mathematically methods of singular perturbation theory reduce the dimension of the problems to be solved locally. Furthermore, they consider how spatial heterogeneous mineralogy can impact upon the propagation of sharp geochemical fronts. The authors developed an asymptotic approach in which they solve equations for the evolving geometry of the front and indicate how the non-smooth perturbations due to natural heterogeneity of the mineralogy on underlying ground water flow field are balanced against the smoothing effect of diffusion/dispersive processes. Fronts are curvature damped, and the results here indicate the generic nature of separate front propagation within both model (idealized) and natural (heterogeneous) geochemical systems

Análisis de Perfil de Textura en Plátanos Pelipita, Hartón y Topocho

OpenAIRE

Granados, Clemente; Acevedo, Diofanor; Cabeza, Adis; Lozano, Adriana

2014-01-01

El objetivo de este trabajo fue evaluar la textura del plátano Pelipita (Musa ABB) crudo y cocido en comparación con plátanos crudos y cocidos Hartón verde (Musa AAB) y Topocho (Musa ABB del subgrupo Silver Bluggoe) mediante un análisis de perfil de textura. El estudio de la textura como propiedad física del alimento es de suma importancia para determinar la aceptabilidad del mismo. A muestras de plátanos Pelipita de la variedad Musa ABB se les aplicó un análisis del perfil de textura a tiemp...

Role of soil geochemical and microbiological components on selenium behaviour in oxic and anoxic conditions

International Nuclear Information System (INIS)

Darcheville, O.

2008-09-01

Selenium (Se) is naturally present in the environment. Se is essential for living organisms at trace concentrations, but it becomes rapidly toxic with their increases. The 79 Se radioactive isotopes of Se, is found in nuclear wastes that may be buried in deep geological formations. In soil, Se exists in many forms and its mobility is affected by the redox potential and microbial activity. Very few studies have focused on Se behaviour at trace concentration. We have tried to distinguish the major abiotic geochemical and microbiological processes involved in the fate of trace selenite (Se(IV)) in a soil. The study was based on batch incubation in oxic or anoxic conditions of slurry suspension artificially contaminated with Se (IV) to 0.4 mg Se.kg -1 dry soil. The incubation involved sterilized and non-sterile soil samples with or without organic amendment to stimulate microbial activities. For each incubation, we followed the distribution of Se between solid, liquid and gaseous phases as well as the geochemical evolution of the solution, the composition of the atmosphere gas bottles and the soil microflora. The results showed that Se was relatively few mobile in the soil studied. Geochemical processes played a major role in controlling the Se mobility. Over time, some abiotic transformations in the solid phase contributed to increase the Se immobilisation. The microbiological processes contributed to this increase in the solid phase. Moreover, in oxic as in anoxic conditions, some microbial processes were responsible, to a lesser extent, for a dispersion of Se in the atmosphere by the production of volatile compounds. (author)

Diálogo de las perspectivas de perfil conceptual y conglomerados de relevancia

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Rosa I. Pedreros-M

2013-01-01

Full Text Available El presente artículo forma parte del desarrollo de la investiga - ción doctoral titulada “Perfil conceptual del calor en comu - nidades culturalmente diferenciadas” y tiene como intención socializar las perspectivas de perfil conceptual y conglomera - dos de relevancia como referentes teóricos y metodológicos que permitan proponer nuevas opciones para pensar la ense - ñanza-aprendizaje de las ciencias o la educación en ciencias, que observen los modos de pensar y hablar de los estudiantes y las relaciones entre la cultura local y el conocimiento escolar. Se exponen el origen, los referentes, las consideraciones so - bre la enseñanza-aprendizaje de las ciencias y las razones para investigar desde estas perspectivas.Nuestro país está conformado por comunidades culturalmen - te diferenciadas, lo cual constituye un reto y desafío para la comunidad académica. Exige, entre otras cosas, propiciar una enseñanza-aprendizaje de las ciencias que tenga en cuenta la diversidad de sistemas de conocimiento, las visiones de mun - do y los modos de pensar y hablar de las comunidades con las que se realiza la acción pedagógica. En este sentido, los perfiles conceptuales y los conglomerados de relevancia se constituyen en referentes teóricos y metodológicos que per - miten reconocer el contexto cultural, las creencias, los valores y las significaciones del entorno físico y natural que tienen los estudiantes.

Percepción del tiempo: resultados de una intervención grupal breve para el cambio del perfil temporal

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Cristián Oyanadel

2014-06-01

Full Text Available La teoría de la perspectiva del tiempo de Zimbardo (1999 plantea una clasificación de las dimensiones de la orientación temporal, medidas con el Zimbardo Time Perspective Inventory (ZTPI, la cual propone, por una parte, que si se tiene una actitud positiva y moderada hacia el pasado, el presente y el futuro, se puede desarrollar mayor bienestar y buena salud tanto mental como física, mientras que actitudes negativas o extremas reflejarían pautas de vida poco saludables. El principal objetivo de esta investigación es evaluar el efecto de una intervención grupal breve para la modificación del perfil temporal. Para este fin, se realizó un estudio cuasiexperimental con grupo control en una muestra de 28 estudiantes universitarios; 14 de ellos formaron el grupo experimental y 14 formaron el grupo control. Los resultados muestran que la intervención realizada al grupo experimental modificó la orientación temporal de los participantes hacia un perfil equilibrado. Para terminar, se concluye que, con una intervención breve y grupal que potencie un pasado positivo y un futuro y un presente más saludables, es posible lograr un perfil equilibrado. Posteriores estudios podrían evaluar el impacto de la modificación del perfil temporal en población clínica.

Significance of geochemical characterization to performance at Yucca Mountain, Nevada

International Nuclear Information System (INIS)

Simmons, A.M.

1993-01-01

The U.S. concept for permanent disposal of high-level radioactive waste resembles those of other countries in that it relies upon burial in a deep geologic medium. This concept relies upon multiple barriers to retard transport of radionuclides to the accessible environment; those barriers consist of the waste form, waste container, engineered barrier system (including possible backfill) and retardant properties of the host rock. Because mobilization of radionuclides is fundamentally a geochemical problem, an understanding of past, present, and future geochemical processes is a requisite part of site characterization studies conducted by the U.S. Department of Energy at Yucca Mountain, Nevada. Geochemical information is needed for evaluating three favorable conditions (the rates of geochemical processes, conditions that promote precipitation or sorption of radionuclides or prohibit formation of colloids, and stable mineral assemblages) and four potentially adverse conditions of the site (groundwater conditions that could increase the chemical reactivity of the engineered barried system or reduce sorption, potential for gaseous radionuclide movement, and oxidizing groundwaters) for key issues of radionuclide release, groundwater quality, and stability of the geochemical environment. Preliminary results of long-term heating experiments indicate that although zeolites can be modified by long-term, low temperature reactions, their beneficial sorptive properties will not be adversely affected. Mineral reactions will be controlled by the aqueous activity of silica in groundwater with which the minerals are in contact. Geochemical barriers alone may satisfy release requirements to the accessible environment for many radionuclides; however, additional site specific geochemical and mineralogical data are needed to test existing and future radionuclide transport models

Geochemical Processes During Managed Aquifer Recharge With Desalinated Seawater

Science.gov (United States)

Ganot, Y.; Holtzman, R.; Weisbrod, N.; Russak, A.; Katz, Y.; Kurtzman, D.

2018-02-01

We study geochemical processes along the variably-saturated zone during managed aquifer recharge (MAR) with reverse-osmosis desalinated seawater (DSW). The DSW, post-treated at the desalination plant by calcite dissolution (remineralization) to meet the Israeli water quality standards, is recharged into the Israeli Coastal Aquifer through an infiltration pond. Water quality monitoring during two MAR events using suction cups and wells inside the pond indicates that cation exchange is the dominant subsurface reaction, driven by the high Ca2+ concentration in the post-treated DSW. Stable isotope analysis shows that the shallow groundwater composition is similar to the recharged DSW, except for enrichment of Mg2+, Na+, Ca2+, and HCO3-. A calibrated variably-saturated reactive transport model is used to predict the geochemical evolution during 50 years of MAR for two water quality scenarios: (i) post-treated DSW (current practice) and (ii) soft DSW (lacking the remineralization post-treatment process). The latter scenario was aimed to test soil-aquifer-treatment (SAT) as an alternative post-treatment technique. Both scenarios provide an enrichment of ˜2.5 mg L-1 in Mg2+ due to cation exchange, compared to practically zero Mg2+ currently found in the Israeli DSW. Simulations of the alternative SAT scenario provide Ca2+ and HCO3- remineralization due to calcite dissolution at levels that meet the Israeli standard for DSW. The simulated calcite content reduction in the sediments below the infiltration pond after 50 years of MAR was low (<1%). Our findings suggest that remineralization using SAT for DSW is a potentially sustainable practice at MAR sites overlying calcareous sandy aquifers.

Geochemical processes during managed aquifer recharge with desalinated seawater

Science.gov (United States)

Ganot, Y.; Holtzman, R.; Weisbrod, N.; Russak, A.; Katz, Y.; Kurtzman, D.

2017-12-01

In this work we study the geochemical processes along the variably-saturated zone during managed aquifer recharge (MAR) with reverse-osmosis desalinated seawater (DSW) to an infiltration pond at the Menashe site, located above the Israeli coastal aquifer. The DSW is post-treated by calcite dissolution (remineralization) in order to meet the Israeli desalinated water quality criteria. Suction cups and monitoring wells inside the pond were used to monitor water quality during two MAR events on 2015 and 2016. Results show that cation exchange is dominant, driven by the high Ca2+ concentration in the post-treated DSW. Stable isotope analysis shows that the composition of the shallow groundwater is similar to the recharged DSW, but with enrichment of Mg2+, Na+, Ca2+ and HCO3-. A calibrated variably-saturated reactive transport model was used to predict the geochemical evolution during 50 years of MAR with two water quality scenarios: post-treated DSW and soft DSW (without post-treatment). The latter scenario was aimed to test soil-aquifer-treatment as an alternative post-treatment technique. In terms of water quality, the results of the two scenarios were found within the range of the desalinated water criteria. Mg2+ enrichment was stable ( 2.5 mg L-1), higher than the zero concentration found in the Israeli DSW. Calcite content reduction was low (<1%) along the variably-saturated profile, after 50 years of MAR. This suggests that using soil-aquifer-treatment as a remineralization technique for DSW is potentially a sustainable practice, which is limited only by the current hydraulic capacity of the Menashe MAR site.

Robust statistics and geochemical data analysis

International Nuclear Information System (INIS)

Di, Z.

1987-01-01

Advantages of robust procedures over ordinary least-squares procedures in geochemical data analysis is demonstrated using NURE data from the Hot Springs Quadrangle, South Dakota, USA. Robust principal components analysis with 5% multivariate trimming successfully guarded the analysis against perturbations by outliers and increased the number of interpretable factors. Regression with SINE estimates significantly increased the goodness-of-fit of the regression and improved the correspondence of delineated anomalies with known uranium prospects. Because of the ubiquitous existence of outliers in geochemical data, robust statistical procedures are suggested as routine procedures to replace ordinary least-squares procedures

Coupling of transport and geochemical models

International Nuclear Information System (INIS)

Noy, D.J.

1985-01-01

This contract stipulated separate pieces of work to consider mass transport in the far-field of a repository, and more detailed geochemical modelling of the groundwater in the near-field. It was envisaged that the far-field problem would be tackled by numerical solutions to the classical advection-diffusion equation obtained by the finite element method. For the near-field problem the feasibility of coupling existing geochemical equilibrium codes to the three dimensional groundwater flow codes was to be investigated. This report is divided into two sections with one part devoted to each aspect of this contract. (author)

Integrated geophysical-geochemical methods for archaeological prospecting

OpenAIRE

Persson, Kjell

2005-01-01

A great number of field measurements with different methods and instruments were conducted in attempts to develop a method for an optimal combination of various geochemical and geophysical methods in archaeological prospecting. The research presented in this thesis focuses on a study of how different anthropogenic changes in the ground can be detected by geochemical and geophysical mapping and how the results can be presented. A six-year pilot project, Svealand in Vendel and Viking periods (S...

Geochemical prospect ion results of Treinta y Tres aerial photo

International Nuclear Information System (INIS)

Zeegers, H.; Bonnefoy, D.; Garau, M.; Spangenberg, J.

1981-01-01

This report shows the geochemical prospect ion results carried out within the framework of the multielemental geochemical strategy. The samples were studied by e spectrometry in the laboratories of Orleans.

Investigation of the geochemical evolution of groundwater under agricultural land: A case study in northeastern Mexico

Science.gov (United States)

Ledesma-Ruiz, Rogelio; Pastén-Zapata, Ernesto; Parra, Roberto; Harter, Thomas; Mahlknecht, Jürgen

2015-02-01

Zona Citrícola is an important area for Mexico due to its citriculture activity. Situated in a sub-humid to humid climate adjacent to the Sierra Madre Oriental, this valley hosts an aquifer system that represents sequences of shales, marls, conglomerates, and alluvial deposits. Groundwater flows from mountainous recharge areas to the basin-fill deposits and provides base flows to supply drinking water to the adjacent metropolitan area of Monterrey. Recent studies examining the groundwater quality of the study area urge the mitigation of groundwater pollution. The objective of this study was to characterize the physical and chemical properties of the groundwater and to assess the processes controlling the groundwater's chemistry. Correlation was used to identify associations among various geochemical constituents. Factor analysis was applied to identify the water's chemical characteristics that were responsible for generating most of the variability within the dataset. Hierarchical cluster analysis was employed in combination with a post-hoc analysis of variance to partition the water samples into hydrochemical water groups: recharge waters (Ca-HCO3), transition zone waters (Ca-HCO3-SO4 to Ca-SO4-HCO3) and discharge waters (Ca-SO4). Inverse geochemical models of these groups were developed and constrained using PHREEQC to elucidate the chemical reactions controlling the water's chemistry between an initial (recharge) and final water. The primary reactions contributing to salinity were the following: (1) water-rock interactions, including the weathering of evaporitic rocks and dedolomitization; (2) dissolution of soil gas carbon dioxide; and (3) input from animal/human wastewater and manure in combination with by denitrification processes. Contributions from silicate weathering to salinity ranged from less important to insignificant. The findings suggest that it may not be cost-effective to regulate manure application to mitigate groundwater pollution.

Kinetic and thermodynamic modelling of geochemical effects of a nuclear waste storage in granitic environment

International Nuclear Information System (INIS)

Made, B.; Fritz, B.

1993-01-01

In the world, various experimental sites are selected to study the behavior of different types of source rocks under nuclear waste storage influence. The surrounding rock tested to receive the waste storage must be a stable geological formation. In France, four geological formations are preselected for the feasibility study of repository for spent nuclear fuel at long term: shale, salt, clay and granite. At present time, numerous studies are carried out in Europe (Germany, Belgium, Sweden, Switzerland, United-Kingdom...), in North America (U.S.A. and Canada) and in Japan. Water-rock interactions control the most of rock transformations near the surface of the earth. The rock forming minerals react with the aqueous solutions, the primary minerals dissolution releases ionic species in solution and secondary minerals precipitate if equilibrium or oversaturation is reached. The weathering processes (hydrothermal or not) are always very complicated thus, geochemical codes has been developed to simulate the water-rock interactions. The first generation of codes is based on purely thermodynamic laws without reference to the time dependence of chemical reactions and then the dissolution path calculation refer to the irreversible dissolution of reactants and reversible precipitation of products ([1] to [4]). The system evolution is followed according to the reaction progress ξ which has been introduced in chemical system by Gibbs. Since few years, the experimental studies on the kinetics of minerals dissolution have allowed to take into account of dissolution rates data for the major minerals (silicates, carbonates...). More recently, a new geochemical codes generation appears based on thermodynamic potential and kinetic laws ([5] to [8]). The system evolution is followed according to the reaction time. (authors). 8 figs., 4 tabs., 24 refs

Geochemical Exploration Techniques Applicable in the Search for Copper Deposits

Science.gov (United States)

Chaffee, Maurice A.

1975-01-01

Geochemical exploration is an important part of copper-resource evaluation. A large number of geochemical exploration techniques, both proved and untried, are available to the geochemist to use in the search for new copper deposits. Analyses of whole-rock samples have been used in both regional and local geochemical exploration surveys in the search for copper. Analyses of mineral separates, such as biotite, magnetite, and sulfides, have also been used. Analyses of soil samples are widely used in geochemical exploration, especially for localized surveys. It is important to distinguish between residual and transported soil types. Orientation studies should always be conducted prior to a geochemical investigation in a given area in order to determine the best soil horizon and the best size of soil material for sampling in that area. Silty frost boils, caliche, and desert varnish are specialized types of soil samples that might be useful sampling media. Soil gas is a new and potentially valuable geochemical sampling medium, especially in exploring for buried mineral deposits in arid regions. Gaseous products in samples of soil may be related to base-metal deposits and include mercury vapor, sulfur dioxide, hydrogen sulfide, carbon oxysulfide, carbon dioxide, hydrogen, oxygen, nitrogen, the noble gases, the halogens, and many hydrocarbon compounds. Transported materials that have been used in geochemical sampling programs include glacial float boulders, glacial till, esker gravels, stream sediments, stream-sediment concentrates, and lake sediments. Stream-sediment sampling is probably the most widely used and most successful geochemical exploration technique. Hydrogeochemical exploration programs have utilized hot- and cold-spring waters and their precipitates as well as waters from lakes, streams, and wells. Organic gel found in lakes and at stream mouths is an unproved sampling medium. Suspended material and dissolved gases in any type of water may also be useful

Aplicación y uso de herramienta open source de data mining para obtención perfiles transaccionales de clientes de tarjeta de crédito

OpenAIRE

Espol; Rivas Carrillo, Gary Glitter

2015-01-01

La presente tesis es realizada en favor al área de prevención y control de fraude electrónico del Banco ABC cuya finalidad es la de tener el adecuado conocimiento de sus tarjetahabientes, requiriendo determinar su perfil transaccional. El perfil transaccional será de apoyo para la detención de las transacciones inusuales de los clientes, ya que este identificará las inconsistencias entre las transacciones actuales y las obtenidas de su perfil. Guayaquil Magíster en Sistemas de Infor...

Perfil, competencias e fluencia digital dos enfermeiros do Programa de Aprimoramento Profissional

Directory of Open Access Journals (Sweden)

Lyvia Pini Tanabe

2013-08-01

Full Text Available Estudo descritivo, exploratório, realizado na cidade de São Paulo, que objetivou identificar o perfil, as competências e a fluência digital do enfermeiro aprimorando para uso da tecnologia no trabalho. A população composta por 60 aprimorandos do Programa de Aprimoramento Profissional respondeu um questionário com dados sobre o perfil, a fluência digital e as competências profissionais. Verificou-se que 95,0% dos participantes eram do sexo feminino, 61,7% na faixa etária entre 23 a 25 anos, 75,0% graduados em escolas públicas, 58,3% cursando enfermagem cardiovascular, 98,3% teve contato com recursos computacionais na graduação; 100,0% possuía computador em casa; 86,7% acessava a internet diariamente; 96,7% utilizava o Messenger e 58,3% apresentava grau intermediário de conhecimento e habilidade em informática. As competências profissionais requeridas frente à tecnologia referiram-se ao saber ser inovador, criativo, atualizado para conhecer e gerenciar programas e saber utilizar os recursos tecnológicos.

Geochemical behaviour of natural uranium-series nuclides in geological formation

International Nuclear Information System (INIS)

Yamakawa, Minoru

1991-01-01

Recent research and investigation show that the Tono uranium deposit and its natural uranium-series nuclides have been preserved, without any significant changes like re-migration or reconcentration, throughout geological events such as upheaval-submergence, marine transgression-regression, and faulting which can readily change geological, hydrogeological, and geochemical conditions. This situation might have come about as a result of being kept in a geometrical closure system, with reducing and milk alkalic geochemical conditions, from the hydrogeological and geochemical point of view. (author)

Perfil neuropsicológico de niños con dislalias: alteraciones mnésicas y atencionales

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Pablo Conde-Guzón

2014-10-01

Full Text Available En este estudio se pretende investigar el funcionamiento neuropsicológico de niños con dislalias. 34 niños con dislalia múltiple (distorsión o sustitución articulatoria de tres fonemas: /r/, /l/ y /s/ y exploración neurológica normal fueron comparados con 28 niños sin problemas del habla. El perfil neuropsicológico se estima mediante la Escala de Inteligencia Wechsler para Niños-Revisada (WISC-R y la Batería Neuropsicológica Luria-DNI. Los resultados indican que los niños dislálicos presentan: a un perfil mnésico globalmente deteriorado respecto al grupo de referencia aunque están preservado la memoria remota y la memoria de formas; b alteraciones en cinestesia y estereognosia; c problemas atencionales. Estos resultados indican que los niños dislálicos presentan problemas mnésicos y atencionales similares a los manifestados por niños con problemas de lenguaje secundarios a daño cerebral o afectaciones orgánicas o psicolingüísticas importantes. Debemos considerar este perfil neuropsicológico deteriorado en la orientación neurológica y psicoeducativa de estos niños.

Posiva safety case hydrogeochemical evolution of the Olkiluoto site

Energy Technology Data Exchange (ETDEWEB)

Trinchero, P.; Roman-Ross, G.; Maia, F.; Molinero, J. [Amphos 21 Consulting S.L., Barcelona (Spain)

2014-03-15

The goal of the present work is to assess the hydrochemical evolution and related changes in the buffering capacity of the Olkiluoto site using reactive transport models. The analysis covers a number of operational-related and climatic-related modelling periods that take place during a glacial cycle; namely, the present conditions with the open repository (Operational Period), the post-closure conditions (Temperate Period) and a stage of the glacial cycle representative of the ice sheet retreat phase (Melting Period). With the aim of reproducing the interplay between the hydrodynamic and geochemical processes, the reactive transport calculations summarised in this document integrate the results of a hydrogeological model with a number of geochemical reactions whose parameterisation relies on previous site investigation studies. The conceptual model on which the study is based, assumes that the hydrochemical evolution of the groundwater at repository depth is the result of infiltration processes from the surface of the domain to the repository. The infiltration occurs along flowpaths through deformation zones and fractures in the bedrock. The infiltrating water, in turn, undergo geochemical reactions with the rock and minerals, namely calcite and iron sulphide precipitation/dissolution, kinetic dissolution of aluminosilicates, cation exchange and aqueous redox reactions. Mass exchange between the transmissive fractures and the low permeability matrix is simulated using a dual porosity approach for the Temperate and Melting Periods. On the contrary, the Operational Period, which is characterised by high hydraulic gradients with advection being the dominant transport mechanism, is simulated using a single porosity model. In all the reactive transport simulations denoted as 'Base Case', pyrite is assumed to be the main iron sulphide mineral in the fracture filling. A set of sensitivity simulations, denoted as 'Variant Case', has been defined where

Geochemical prospecting for thorium and uranium deposits

International Nuclear Information System (INIS)

Boyle, R.W.

1982-01-01

The basic purpose of this book is to present an analysis of the various geochemical methods applicable in the search for all types of thorium and uranium deposits. The general chemistry and geochemistry of thorium and uranium are briefly described in the opening chapter, and this is followed by a chapter on the deposits of the two elements with emphasis on their indicator (pathfinder) elements and on the primary and secondary dispersion characteristics of thorium and uranium in the vicinity of their deposits. The next seven chapters form the main part of the book and describe geochemical prospecting for thorium and uranium, stressing selection of areas in which to prospect, radiometric surveys, analytical geochemical surveys based on rocks (lithochemical surveys), unconsolidated materials (pedochemical surveys), natural waters and sediments (hydrochemical surveys), biological materials (biogeochemical surveys), gases (atmochemical surveys), and miscellaneous methods. A final brief chapter reviews radiometric and analytical methods for the detection and estimation of thorium and uranium. (Auth.)

The mineralogic evolution of the Martian surface through time: Implications from chemical reaction path modeling studies

Science.gov (United States)

Plumlee, G. S.; Ridley, W. I.; Debraal, J. D.; Reed, M. H.

1993-01-01

Chemical reaction path calculations were used to model the minerals that might have formed at or near the Martian surface as a result of volcano or meteorite impact driven hydrothermal systems; weathering at the Martian surface during an early warm, wet climate; and near-zero or sub-zero C brine-regolith reactions in the current cold climate. Although the chemical reaction path calculations carried out do not define the exact mineralogical evolution of the Martian surface over time, they do place valuable geochemical constraints on the types of minerals that formed from an aqueous phase under various surficial and geochemically complex conditions.

Perfiles motivacionales en Educación Física: una aproximación desde la teoría de las Metas de Logro 2x2

Directory of Open Access Journals (Sweden)

Ricardo Cuevas

2013-10-01

Full Text Available Objetivo del estudio fue determinar los perfiles motivacionales del alumnado de educación física a través del análisis de las orientaciones a meta 2x2, así como las percepciones del clima motivacional en función de dichos perfiles, y las diferencias por género. Tomando la teoría de las Metas de Logro (Nicholls, 1989 como marco, 390 estudiantes de Secundaria (113 mujeres y 277 hombres entre 14 y 16 años cumplimentaron los cuestionarios de metas de logro 2x2 en educación física y de orientaciones de aprendizaje y rendimiento en las clases de educación física. El análisis por género evidenció una mayor orientación a la tarea y un mayor clima-tarea por parte de las chicas. El análisis de conglomerados obtuvo cuatro perfiles. Un primer perfil con altas metas de logro, un segundo con metas moderadas, un tercero con metas bajas y un cuarto caracterizado por altas metas de aproximación y maestría. El análisis multivariante reveló que los estudiantes del primer y cuarto perfil percibían más un clima-tarea. A partir de los resultados, se sugiere la promoción, a través del clima motivacional de clase, de metas de maestría junto con la aproximación-rendimiento para favorecer la creación de perfiles adaptativos.

Geochemical evaluation of the near-field for future HLW repository at Olkiluoto

International Nuclear Information System (INIS)

Idiart, A.; Maia, F.; Arcos, D.

2013-10-01

The concept for the final disposal of spent nuclear fuel in Finland considers an engineered and natural (crystalline rock) multi-barrier system surrounding the spent fuel. This work aims at predicting and making a quantitative assessment of the geochemical evolution of the near-field (canister, buffer, backfill and adjacent fractured bedrock) during the unsaturated thermal period and in the long-term, after saturation has been completed. The groundwater/bentonite buffer interaction during the unsaturated thermal period is tackled through a two-dimensional (2D) axisymmetric scheme using the thermo-hydro-geochemical code TOUGHREACT. In turn, the long-term interaction of the fully water-saturated buffer and backfill with groundwater is assessed through 3D numerical models using the reactive transport code PHAST under isothermal conditions. A set of base cases have been set up based on the most plausible set of input data. In addition, a limited number of sensitivity cases have been conducted to analyse the influence of key parameters controlling the system and reduce uncertainty. Predicted mineralogical changes of accessory minerals in the bentonite for the thermal period are controlled by the dependence of mineral solubilities on temperature and on the solute transport by advection during the saturation process, and diffusion during the whole period. The results of the thermal period indicate that a small amount of the primary amorphous silica is redistributed in the buffer: dissolution close to the canister and precipitation close to the buffer - rock interface. Primary calcite dissolution/precipitation is minimal, remaining stable throughout the simulation time in all cases. Anhydrite precipitates near the canister due to the elevated temperature, while it dissolves from the outside of the buffer. The results indicate that there is no significant evaporation of water near the copper canister and thus no chloride salt reaches saturation. The geochemical changes of

ELEMENTOS PARA LA CONSTRUCION DE UN PERFIL PARA EL GERENTE SOCIAL EN UN ENTORNO GLOBALIZADO

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Antonio Bastidas Unigarro

2009-07-01

Full Text Available El perfil del gerente social adecuado para enfrentar los retos del mundo globalizado se ha estructurado a partir de cuatro requerimientos fundamentales: los conocimientos, la experiencia, las habilidades y las actitudes, los cuales se analizan como competencias indispensables para administrar la problemática compleja, llena de incertidumbres y desafíos del nuevo milenio. La propuesta para la construcción de un perfil de este gerente parte de considerar tres tipos de competencias: las funcionales, las comportamentales y los requisitos de estudio y experiencia. Su construcción parte del análisis de la Gerencia Social en el estado neoliberal, escenario, que reclama la formación de gerentes sociales comprometidos en la construcción de una sociedad mas justa, incluyente, participativa, democrática y solidaria.

Percepción del tiempo: resultados de una intervención grupal breve para el cambio del perfil temporal

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Cristián Oyanadel

2014-06-01

Full Text Available La teoría de la perspectiva del tiempo de Zimbardo (1999 plantea una clasificación de las dimensiones de la orientación temporal, medidas con el Zimbardo Time Perspective Inventory (ZTPI, la cual propone, por una parte, que si se tiene una actitud positiva y moderada hacia el pasado, el presente y el futuro, se puede desarrollar mayor bienestar y buena salud tanto mental como física, mientras que actitudes negativas o extremas reflejarían pautas de vida poco saludables. El principal objetivo de esta investigación es evaluar el efecto de una intervención grupal breve para la modificación del perfil temporal. Para este fin, se realizó un estudio cuasiexperimental con grupo control en una muestra de 28 estudiantes universitarios; 14 de ellos formaron el grupo experimental y 14 formaron el grupo control. Los resultados muestran que la intervención realizada al grupo experimental modificó la orientación temporal de los participantes hacia un perfil equilibrado. Para terminar, se concluye que, con una intervención breve y grupal que potencie un pasado positivo y un futuro y un presente más saludables, es posible lograr un perfil equilibrado. Posteriores estudios podrían evaluar el impacto de la modificación del perfil temporal en población clínica.

El perfil escritor como variable moduladora de los procesos involucrados en la composición escrita en estudiantes universitarios

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Olga Arias-Gundín

2017-04-01

Full Text Available Tradicionalmente en la literatura se han identificado dos perfiles escritores, planificadores vs. revisores. En este estudio se analizan las estrategias de escritura y el perfil escritor de los estudiantes universitarios, y su influencia en la resolución de tareas híbridas; participando en el estudio 142 estudiantes de tres titulaciones diferentes. Para identificar el perfil escritor se utilizó la versión española del Cuestionario sobre Tendencias de Planificación y Revisión Escrita. Las tareas híbridas a las que tuvieron que enfrentarse los estudiantes fueron el resumen y la síntesis, valorando en ambos casos el proceso de lectura y escritura seguidos, el nivel de las estrategias de subrayado y toma de notas utilizado, el tipo de borrador elaborado y la generación de ideas. Los resultados muestran que más del 60% de los estudiantes presentan un perfil escritor mixto con puntuaciones similares en la utilización tanto de la estrategia de planificación como de revisión, aunque informan de un nivel de uso mayor en la estrategia de revisión. Asimismo se ha podido constatar que los procesos y estrategias utilizadas por los estudiantes son más complejas en función de la dificultad de la tarea; al tiempo que la estrategia de escritura que mayor influencia tiene es la de planificación.

El perfil profesional y académico de los presidentes municipales del Estado de México, 2009-2012

OpenAIRE

Rafael Cedillo Delgado

2014-01-01

Este artículo analiza el perfil profesional y académico de los ediles mexiquenses en el periodo 2009-2012. Con base en datos oficiales e información periodística, se compara su perfil profesional y académico por categoría de urbanización de los municipios, profesión, grado de estudios, género y pertenencia partidista. Los resultados muestran que la urbanización de los ayuntamientos y la filiación partidista no se relacionan con el grado académico. El nivel educativo es aceptable, pues dos ter...

El perfil de la víctima y el agresor en casos de violencia de género

OpenAIRE

Coll Mora, Miriam

2016-01-01

El present treball aprofundeix en l’estudi del perfil de la víctima i l’agressor en casos de violència de gènere, analitzant la manera en que ambdues persones es relacionen i interactuen immersos dins la relació de violència. Es pretén constatar la inexistència d’un perfil universal definit de víctima o agressor i descriure les característiques essencials de la personalitat que ambdós comparteixen i la expressió de la qual els diferencia. Com a objectiu secundari, es persegueix descriure l...

SR-Site - hydrogeochemical evolution of the Forsmark site

International Nuclear Information System (INIS)

Salas, Joaquin; Molinero, Jorge; Juarez, Iker; Gimeno, Maria Jose; Auque, Luis; Gomez, Javier

2010-12-01

The present work has involved the development of a methodology in order to simulate the evolution of the groundwater composition within the candidate repository site of the Forsmark area. A series of climate periods is expected to be probable after the repository closure (temperate, periglacial and glacial) and, eventually, the area could be submerged under seawaters or under a lake of glacial melt waters. These environmental conditions will affect groundwater flow and composition around of the candidate repository volume. The present report summarizes the results obtained by the calculations which reproduce the hydrogeochemical evolution in the Forsmark area, and within the candidate repository volume. The hydrogeochemical evolution of groundwaters is one of the key factors affecting the chemical stability of the buffer and the canister. In this way, the main objective of the hydrogeochemical simulations is to assay the evolution of a series of safety assessment factors, such as salinity, redox potential, pH, and concentrations of iron, sulphide and potassium, among others. Using ConnectFlow, previous hydrological calculations have provided the transport of (1) the fractions of selected reference waters (Deep Saline, Old Meteoric, Glacial, Littorina and Altered Meteoric groundwaters), or (2) salinities, depending on the working team (Serco or Terrasolve). The results of the regional-scale groundwater flow modelling for each specific climate period are used as input of the geochemical models. Groundwater compositions have been modelled using PHREEQC, through mixing and chemical reactions between the waters obtained from the hydrogeological models and the reactive fracture-filling minerals. Both models (hydrological and geochemical) are not fully coupled, and it allows a description of the geochemical heterogeneity, which otherwise would be hard to attain. The stage of the open repository has been non-numerically analysed. Aspects as salinity, redox conditions

SR-Site - hydrogeochemical evolution of the Forsmark site

Energy Technology Data Exchange (ETDEWEB)

Salas, Joaquin; Molinero, Jorge; Juarez, Iker (Amphos 21 (Spain)); Gimeno, Maria Jose; Auque, Luis; Gomez, Javier (Univ. of Zaragoza (Spain))

2010-12-15

The present work has involved the development of a methodology in order to simulate the evolution of the groundwater composition within the candidate repository site of the Forsmark area. A series of climate periods is expected to be probable after the repository closure (temperate, periglacial and glacial) and, eventually, the area could be submerged under seawaters or under a lake of glacial melt waters. These environmental conditions will affect groundwater flow and composition around of the candidate repository volume. The present report summarizes the results obtained by the calculations which reproduce the hydrogeochemical evolution in the Forsmark area, and within the candidate repository volume. The hydrogeochemical evolution of groundwaters is one of the key factors affecting the chemical stability of the buffer and the canister. In this way, the main objective of the hydrogeochemical simulations is to assay the evolution of a series of safety assessment factors, such as salinity, redox potential, pH, and concentrations of iron, sulphide and potassium, among others. Using ConnectFlow, previous hydrological calculations have provided the transport of (1) the fractions of selected reference waters (Deep Saline, Old Meteoric, Glacial, Littorina and Altered Meteoric groundwaters), or (2) salinities, depending on the working team (Serco or Terrasolve). The results of the regional-scale groundwater flow modelling for each specific climate period are used as input of the geochemical models. Groundwater compositions have been modelled using PHREEQC, through mixing and chemical reactions between the waters obtained from the hydrogeological models and the reactive fracture-filling minerals. Both models (hydrological and geochemical) are not fully coupled, and it allows a description of the geochemical heterogeneity, which otherwise would be hard to attain. The stage of the open repository has been non-numerically analysed. Aspects as salinity, redox conditions

Los perfiles cognitivos psicopatológicos en la formulación cognitiva de caso

Directory of Open Access Journals (Sweden)

Ronald Toro

2010-01-01

Full Text Available Se resaltó la relevancia de incluir los perfiles cognitivos desarrollados de acuerdo con las categorías diagnósticas del DSM-IV TR para los trastornos de la personalidad en la formulación cognitiva de caso. Los contenidos informacionales deben dar cuenta del perfil cognitivo específico del paciente, con el fin de facilitar la planeación y el curso del tratamiento ajustado a sus necesidades, aunque no presente diagnóstico en el eje II. También se analizaron las implicaciones del uso inadecuado de las categorías diagnósticas en los trastornos de la personalidad; la necesidad de generar investigación en torno al soporte empírico y psicométrico derivado de la presente propuesta, y el entrenamiento de terapeutas cognitivos en formulación cognitiva de caso.

Geochemical study of water-rock interaction processes on geothermal systems of alkaline water in granitic massif

International Nuclear Information System (INIS)

Buil gutierrez, B.; Garcia Sanz, S.; Lago San Jose, M.; Arranz Yague, E.; Auque Sanz, L.

2002-01-01

The study of geothermal systems developed within granitic massifs (with alkaline waters and reducing ORP values) is a topic of increasing scientific interest. These systems are a perfect natural laboratory for studying the water-rock interaction processes as they are defined by three main features: 1) long residence time of water within the system, 2) temperature in the reservoir high enough to favour reaction kinetics and finally, 3) the comparison of the chemistry of the incoming and outgoing waters of the system allows for the evaluation of the processes that have modified the water chemistry and its signature, The four geothermal systems considered in this paper are developed within granitic massifs of the Spanish Central Pyrenes; these systems were studied from a geochemical point of view, defining the major, trace and REE chemistry of both waters and host rocks and then characterizing the composition and geochemical evolution of the different waters. Bicarbonate-chloride-sodic and bicarbonate-sodic compositions are the most representative of the water chemistry in the deep geothermal system, as they are not affected by secondary processes (mixing, conductive cooling, etc). (Author)

Statistical interpretation of geochemical data

International Nuclear Information System (INIS)

Carambula, M.

1990-01-01

Statistical results have been obtained from a geochemical research from the following four aerial photographies Zapican, Carape, Las Canias, Alferez. They have been studied 3020 samples in total, to 22 chemical elements using plasma emission spectrometry methods.

Post-Eocene volcanics of the Abazar district, Qazvin, Iran: Mineralogical and geochemical evidence for a complex magmatic evolution

Science.gov (United States)

Asiabanha, A.; Bardintzeff, J. M.; Kananian, A.; Rahimi, G.

2012-02-01

The style of volcanism of post-Eocene volcanism in the Alborz zone of northern Iran is different to that of Eocene volcanism (Karaj Formation). Indeed, the volcanic succession of the Abazar district, located in a narrow volcanic strip within the Alborz magmatic assemblage, is characterized by distinct mineralogical and chemical compositions linked to a complex magmatic evolution. The succession was produced by explosive eruptions followed by effusive eruptions. Two main volcanic events are recognized: (1) a thin rhyolitic ignimbritic sheet underlain by a thicker lithic breccia, and (2) lava flows including shoshonite, latite, and andesite that overlie the first event across a reddish soil horizon. Plagioclase in shoshonite (An 48-92) shows normal zoning, whereas plagioclase in latite and andesite (An 48-75) has a similar composition but shows reverse and oscillatory zoning. QUILF temperature calculations for shoshonites and andesites yield temperatures of 1035 °C and 1029 °C, respectively. The geothermometers proposed by Ridolfi et al. (2010) and Holland and Blundy (1994) yield temperatures of 960 °C and 944 °C for latitic lava, respectively. The samples of volcanic rock show a typical geochemical signature of the continental arc regime, but the andesites clearly differ from the shoshonites, the latites and the rhyolites. The mineralogical and chemical characteristics of these rocks are explained by the following petrogenesis: (1) intrusion of a hot, mantle-depth mafic (shoshonitic) magma, which differentiated in the magma chamber to produce a latitic and then a rhyolitic liquid; (2) rhyolitic ignimbritic eruptions from the top of the magma chamber, following by shoshonitic and then latitic extrusions; (3) magma mingling between the latitic and andesitic magmas, as indicated by the occurrence of andesite clasts within the latite; and (4) andesitic effusions. The youngest volcanic events in the Alborz zone show a close chemical relationship with continental arc

Perfiles motivacionales en estudiantes de educación física de tres países y su relación con la actividad física

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Evelia Franco

2017-01-01

Full Text Available El objetivo del presente estudio fue analizar los perfiles motivacionales de estudiantes de educación física, examinar su relación con la práctica de actividad física y la intención de ser físicamente activo, así como comprobar si dichos perfiles y sus relaciones con la práctica de actividad física y la intención de realizarla resultaban estables en los adolescentes de España, Colombia y Ecuador. La muestra del estudio estaba formada por 2670 estudiantes con edades comprendidas entre los 12 y los 16 años (M = 14.30; DT = 1.66, pertenecientes a diferentes centros educativos de Madrid, Armenia y Cuenca. Los resultados señalaron la existencia de tres perfiles motivacionales: motivación baja-moderada, alta motivación-bajo ego y alta motivación. Además, el perfil de alta motivación mostró los mayores niveles de práctica de actividad física y de intención de realizarla en el futuro, seguido por el perfil de alta motivación-bajo ego y el de motivación baja-moderada. Tanto la caracterización de los perfiles como las asociaciones establecidas con las variables dependientes resultaron estables en las muestras de los tres países participantes. Como conclusión, el perfil de alta motivación mostró mayores niveles de actividad física y de intención de realizar actividad físico-deportiva en el futuro. Igualmente se observaron similitudes entre los adolescentes de los diferentes países.

Modeling background radiation using geochemical data: A case study in and around Cameron, Arizona.

Science.gov (United States)

Marsac, Kara E; Burnley, Pamela C; Adcock, Christopher T; Haber, Daniel A; Malchow, Russell L; Hausrath, Elisabeth M

2016-12-01

This study compares high resolution forward models of natural gamma-ray background with that measured by high resolution aerial gamma-ray surveys. The ability to predict variations in natural background radiation levels should prove useful for those engaged in measuring anthropogenic contributions to background radiation for the purpose of emergency response and homeland security operations. The forward models are based on geologic maps and remote sensing multi-spectral imagery combined with two different sources of data: 1) bedrock geochemical data (uranium, potassium and thorium concentrations) collected from national databases, the scientific literature and private companies, and 2) the low spatial resolution NURE (National Uranium Resource Evaluation) aerial gamma-ray survey. The study area near Cameron, Arizona, is located in an arid region with minimal vegetation and, due to the presence of abandoned uranium mines, was the subject of a previous high resolution gamma-ray survey. We found that, in general, geologic map units form a good basis for predicting the geographic distribution of the gamma-ray background. Predictions of background gamma-radiation levels based on bedrock geochemical analyses were not as successful as those based on the NURE aerial survey data sorted by geologic unit. The less successful result of the bedrock geochemical model is most likely due to a number of factors including the need to take into account the evolution of soil geochemistry during chemical weathering and the influence of aeolian addition. Refinements to the forward models were made using ASTER visualizations to create subunits of similar exposure rate within the Chinle Formation, which contains multiple lithologies and by grouping alluvial units by drainage basin rather than age. Copyright © 2016 The Authors. Published by Elsevier Ltd.. All rights reserved.

Constraints on Composition, Structure and Evolution of the Lithosphere

Science.gov (United States)

Bianchini, Gianluca; Bonadiman, Costanza; Aulbach, Sonja; Schutt, Derek

2015-05-01

The idea for this special issue was triggered at the Goldschmidt Conference held in Florence (August 25-30, 2013), where we convened a session titled "Integrated Geophysical-Geochemical Constraints on Composition and Structure of the Lithosphere". The invitation to contribute was extended not only to the session participants but also to a wider spectrum of colleagues working on related topics. Consequently, a diverse group of Earth scientists encompassing geophysicists, geodynamicists, geochemists and petrologists contributed to this Volume, providing a comprehensive overview on the nature and evolution of lithospheric mantle by combining studies that exploit different types of data and interpretative approaches. The integration of geochemical and geodynamic datasets and their interpretation represents the state of the art in our knowledge of the lithosphere and beyond, and could serve as a blueprint for future strategies in concept and methodology to advance our knowledge of this and other terrestrial reservoirs.

Regional geochemical maps of uranium in Northern Scotland. Environmental and economic considerations

International Nuclear Information System (INIS)

Plant, J.

1978-01-01

The Institute of Geological Studies geochemical mapping programme is outlined. The natural levels of uranium in rocks, soils and waters are discussed. Some practical details of geochemical mapping are given. Applications of geochemical maps of uranium in Scotland are considered: economic applications and medical geography and agriculture. A list of 38 references is appended. (U.K.)

2005 dossier: granite. Tome: phenomenological evolution of the geologic disposal

International Nuclear Information System (INIS)

2005-01-01

This document makes a status of the researches carried out by the French national agency of radioactive wastes (ANDRA) about the phenomenological aspects of the geologic disposal of high-level and long-lived radioactive wastes (HLLL) in granite formations. Content: 1 - introduction: ANDRA's research program on disposal in granitic formation; 2 - the granitic environment: geologic history, French granites; 3 - HLLL wastes and disposal design concepts; 4 - identification, characterization and modeling of a granitic site: approach, geologic modeling, hydrologic and hydro-geochemical modeling, geomechanical and thermal modeling, long-term geologic evolution of a site; 5 - phenomenological evolution of a disposal: main aspects of the evolution of a repository with time, disposal infrastructures, B-type wastes disposal area, C-type wastes disposal area; spent fuels disposal area, radionuclides transfer and retention in the granitic environment; 6 - conclusions: available knowledge, methods and tools for the understanding and modeling of the phenomenological evolution of a granitic disposal site. (J.S.)

Uranium geochemical exploration in northwestern Luzon

International Nuclear Information System (INIS)

Santos, G. Jr.; Fernandez, L.; Ogena, M.; Tauli, G.

1980-01-01

A reconnaissance geochemical stream water and sediment survey which was conducted in northwestern Luzon was able to detect ten (10) uranium anomalous areas. These anomalous areas are located along a north-south trending zone of Miocene marine clastics and sedimentary rocks with tuffaceous sediment intercalations. In general, northwest Luzon has low radioactivity except for two anomalous areas which have 3 to 6 times background radioactivity. Radon anomalies occur in sparsely scattered locations. The anomalous zones appear to be related to major north-south faults and secondary northeast-southwest trending structures. Geochemical correlations between uranium and other elements such as copper, lead, zinc, manganese, silver, cobalt and nickel are generally very poor. (author)

Identificación de perfiles ambientales en la Pyme a través de la auditoría ambiental

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Fabiola Maribel Denegri de Dios

2011-01-01

Full Text Available Las micro, pequeñas y medianas empresas (Pyme han sido consideradas como un grupo objetivo secundario de las políticas de control de contaminación en México. Aunque su impacto ambiental individual puede ser pequeño, su impacto agregado puede causar serios problemas para el ambiente y la población. Recientemente, en México se han implementando programas de autorregulación ambiental dirigidos a Pyme utilizando como herramienta principal la auditoría ambiental. El propósito de este trabajo es identificar los perfiles de contaminación y cumplimiento ambiental de las Pyme que han participado en el Programa de Autorregulación Ambiental en Mexicali, Baja California. Los datos utilizados se obtuvieron de los informes de auditoría ambiental de aproximadamente sesenta Pyme que participaron en el programa en los años 2005 y 2006. Los resultados muestran que tres de las ramas participantes obtuvieron los perfiles de contaminación más altos con perfiles de cumplimiento ambiental casi nulos.

Caracterización del perfil de los estudiantes de Negocios Internacionales de la Universidad Santo Tomás, sede Bogotá

Directory of Open Access Journals (Sweden)

Myriam Soraya Suárez R.

2013-01-01

Full Text Available Los estudios sobre el perfil de los estudiantes universitarios se han llevado a cabo permanentemente, debido a que las universidades requieren saber con qué estudiantes cuentan y cómo estos requieren ser formados, de acuerdo con las necesidades actua - les del mercado laboral y las necesidades sociales del contexto en el cual se encuentran inmersos. Esta investigación sobre la caracterización del perfil de los estudiantes de la Facultad de Negocios Internacionales de la Universidad Santo Tomás, sede Bogotá, determinó los aspectos biográficos, sociodemográficos, proyecto de vida, perfil educativo y profesional, competencias y uso del tiempo libre, con el fin de describir las motivaciones, intereses y percepciones, lo cual permitió tener un conocimiento holístico de los estudiantes y de todos los aspectos involucrados en su formación.

Personalidad y demencia: aproximación al perfil diferencial del cuidador

Directory of Open Access Journals (Sweden)

Elena de Andrés-Jiménez

2011-12-01

Full Text Available El objetivo de este estudio es determinar la existencia de un perfil de personalidad característico de los cuidadores y cuidadoras familiares de personas con demencia. El adecuado conocimiento y manejo de las variables psicológicas que afectan de alguna manera al cuidador, ayuda a promover las acciones oportunas destinadas a atenuar el impacto del cuidado y mejorar la calidad de vida del cuidador y la persona cuidada. La población objeto de estudio está formada por 69 cuidadores familiares de personas con demencia, miembros de distintas asociaciones y centros de día. Los resultados obtenidos permiten identificar un perfil de personalidad característico para estos cuidadores, revelador de un funcionamiento psicológico específico en esta muestra, que si bien no podemos relacionar directamente con las tareas propias del cuidado de una persona con esta enfermedad, si nos proporciona información muy relevante para atender de forma más precisa a las necesidades de este colectivo. Asimismo, el análisis de los estilos de personalidad en función del sexo muestra una vez más que la mujer se encuentra en este ámbito en una situación de mayor vulnerabilidad.

Genesis and evolution of the fumaroles of vulcano (Aeolian Islands, Italy): a geochemical model

Science.gov (United States)

Carapezza, M.; Nuccio, P. M.; Valenza, M.

1981-09-01

A geochemical model explaining the presence of fumaroles having different gas composition and temperature at the top of the crater and along the northeastern coast of Vulcano island is proposed. A pressurized biphase (liquid-vapor) reservoir at the depth of about 2 km is hypothesized. Energy and mass balance sheets control P-T conditions in the system. P-T must vary along a boiling curve of brine as liquid is present. The CO2 content in the steam is governed by the thermodynamic properties of the fluids in the H2-NaCl-CO2 system. On the assumption that oxygen fugacity in the system is between the HM-FMQ oxygen buffers, observed SO2/H2S, CO2/CO, CO/CH4 ratios in the fumarolic gases at the Fossa crater appear in equilibrium with a temperature higher than that observed, such as may exist at depth. The more reduced gas phases present on the sea-side may result from re-equilibrium processes in shallower aquifers. The suggested model would help in monitoring changes in volcanic activity by analyzing fumarolic gases.

Perfil de estrés y estrés crónico en migrantes mexicanos en canadá

OpenAIRE

Pozos-Radillo, Blanca Elizabeth; Pando, Manuel; Aguilera Velasco, María De los Ángeles; Acosta Fernández, Martín

2014-01-01

Objetivo Establecer la asociación existente entre el nivel alto de estrés crónico y las variables consideradas como negativas del perfil de estrés en los migrantes mexicanos radicados en Edmonton Canadá. Métodos La selección de la población fue por medio de la técnica aleatoria simple. El tamaño de la muestra fue: 58 migrantes, durante el año de 2010-20011, se aplicó el Inventario de Síntomas de Estrés y el Perfil de Nowack.Resultados Los niveles de estrés crónico fueron: 34 % alto, 45 % medi...

PERFIL AROMÁTICO DE SUCOS E FERMENTADOS DE MAÇÃ EM DIFERENTES ESTÁDIOS DE MATURAÇÃO

OpenAIRE

CÍNTIA MAIA BRAGA

2013-01-01

Fermentados de maçãs são produzidos no Brasil com frutas de baixa qualidade comercial que não passam por classificação quanto ao grau de maturação. Sabe-se que isto pode alterar a qualidade tecnológica e sensorial do produto tornando necessário um estudo para determinação do perfil aromático dos produtos processados com maçãs em diferentes estádios de maturação. O objetivo deste estudo foi identificar e determinar as diferenças de perfil aromático entre sucos e fermentados de maçã elaborados ...

Granite-repository - geochemical environment

International Nuclear Information System (INIS)

1979-04-01

Some geochemical data of importance for a radioactive waste repository in hard rock are reviewed. The ground water composition at depth is assessed. The ground water chemistry in the vicinity of uranium ores is discussed. The redox system in Swedish bedrock is described. Influences of extreme climatic changes and of repository mining and construction are also evaluated

Perfil cognitivo de niños con rendimientos bajos en comprensión lectora

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Lorena Canet-Juric

2013-10-01

Full Text Available La mayoría de los niños con dificultades en la comprensión lectora poseen rendimientos inferiores en un conjunto de procesos cognitivos. El objetivo del presente estudio es establecer un perfil cognitivo asociado al bajo rendimiento en comprensión lectora en relación a la habilidad de monitoreo, a la producción de inferencias, al vocabulario, a la amplitud de memoria de trabajo y a la capacidad inhibitoria, en niños hispanoparlantes. Para ello se administraron tareas correspondientes a dichos procesos en niños con altos y bajos rendimientos en comprensión lectora. Los resultados mostraron que si bien los niños con mala comprensión presentan bajos rendimientos en estas habilidades, no puede establecerse un perfil consistente ya que hay niños con problemas en comprensión que presentan normal o superior rendimiento en algunas de estas habilidades cognitivas.

Un acercamiento a la comprensión del perfil de la Inteligencia Emocional

Directory of Open Access Journals (Sweden)

Gloria María Isaza-Zapata*

2016-02-01

Full Text Available Este artículo es resultado de un estudio de inteligencia emocional. En la investigación nos propusimos como objetivo general, analizar el perfil de inteligencia emocional y social de una muestra de 110 docentes de educación básica primaria, vinculados a diez instituciones educativas de la ciudad de Medellín, Colombia. El alcance es descriptivo, no experimental, y correlacional; y está apoyado con método probabilístico, simple al azar y estratificado. Los resultados obtenidos desde el perfil destacan la relación con: autorregulación, automotivación, empatía, tiempo de métodos asertivos, eficaz el método y juzgarse a sí mismo; detectando una correlación con tendencia a cero entre las variables. En conclusión, la inteligencia emocional y social del maestro o maestra de básica primaria tiende a establecer un reconocimiento de sus habilidades, sus limitaciones, su sensibilidad hacia el aprendizaje personal y su influencia en el sujeto estudiante.

Un acercamiento a la comprensión del perfil de la Inteligencia Emocional

Directory of Open Access Journals (Sweden)

Gloria María Isaza-Zapata

2016-01-01

Full Text Available Este artículo es resultado de un estudio de inteligencia emocional. En la investigación nos propusimos como objetivo general, analizar el perfil de inteligencia emocional y social de una muestra de 110 docentes de educación básica primaria, vinculados a diez instituciones educativas de la ciudad de Medellín, Colombia. El alcance es descriptivo, no experimental, y correlacional; y está apoyado con método probabilístico, simple al azar y estratificado. Los resultados obtenidos desde el perfil destacan la relación con: autorregulación, automotivación, empatía, tiempo de métodos asertivos, eficaz el método y juzgarse a sí mismo; detectando una correlación con tendencia a cero entre las variables. En conclusión, la inteligencia emocional y social del maestro o maestra de básica primaria tiende a establecer un reconocimiento de sus habilidades, sus limitaciones, su sensibilidad hacia el aprendizaje personal y su influencia en el sujeto estudiante.

PERFIL DE CONSUMIDORES DO PESCADO COMERCIALIZADO EM MERCADOS DO MUNICÍPIO DE SÃO LUÍS, MARANHÃO, BRASIL

OpenAIRE

Silva, Iran Alves da; Universidade Federal do Maranhão - UFMA; Lima, Maria de Fátima Viégas; Universidade Estadual do Maranhão - UEMA; Brandão, Vivian Magalhães; Universidade Estadual do Maranhão - UEMA; Dias, Isabel Cristina Lopes; Universidade Estadual do Maranhão - UEMA; Silva, Maria Inez Santos; Universidade Estadual do Maranhão - UEMA; Lacerda, Lenka de Morais; Universidade Estadual do Maranhão - UEMA

2012-01-01

Este trabalho objetivou traçar o perfil de consumidores do pescado comercializado em São Luís, bem como avaliar os fatores que influenciam no momento da compra. Realizou-se 50 entrevistas direcionadas aos consumidores em mercados do município de São Luís-MA através de inquérito investigativo com 16 questões fechadas e abertas sobre o perfil, hábitos de consumo/preferências, prováveis fatores que afetam a decisão de compra/consumo e as características ou atributos desejáveis no produto. Verifi...

El perfil motivacional para la práctica del deporte escolar de la ciudad de Tubarao (Santa Catarina, Brasil)

OpenAIRE

Ferreira Sene, Richard

2012-01-01

Este trabajo tiene como objetivo delinear un perfil de motivación para los deportes de los escolares entre 10 y 18 años en la ciudad de Tubarão Santa Catarina en Brasil. Además, relacionar la experiencia deportiva de los padres con la motivación de los niños. Se ha utilizado una investigación descriptiva y de campo con la participación voluntaria de 418 escolares de la red municipal El instrumento utilizado para trazar este perfil fue el inventario de motivación para práctica d...

Caracterización del perfil de los estudiantes de Negocios Internacionales de la Universidad Santo Tomás, sede Bogotá

OpenAIRE

Myriam Soraya Suárez R.; Ana María Jiménez C.

2013-01-01

Los estudios sobre el perfil de los estudiantes universitarios se han llevado a cabo permanentemente, debido a que las universidades requieren saber con qué estudiantes cuentan y cómo estos requieren ser formados, de acuerdo con las necesidades actua - les del mercado laboral y las necesidades sociales del contexto en el cual se encuentran inmersos. Esta investigación sobre la caracterización del perfil de los estudiantes de la Facultad de Negocios Internacionales de la Universidad Santo...

Geochemical Distribution of Lead and Chromium in River Getsi-Kano

African Journals Online (AJOL)

Geochemical forms of lead (Pb) and Chromium (Cr) from the sediment of River Getsi Kano-Nigeria were determined using Atomic Absorption spectrometer for eighteen months. Apart from determination of the metals in water, geochemical forms of the metals were also evaluated into five fractions. Exchangeable, bound to ...

The evolution of mine waters quality at the locality of Smolník

Directory of Open Access Journals (Sweden)

Mária Kušnierová

2006-12-01

Full Text Available At the present time, acid mine drainage (AMD is considered to be one of the worst environmental problems associated with the mining activity. AMD originates as a result of natural oxidation of sulphide minerals, mainly pyrite when exposed to the combined action of water and oxygen and negative affects the whole ecology of aquatic environment. The article presents results of monitoring and trends in the evolution of acid mine drainage quality at the locality of Smolník from year 1986 till 2005 and the assumed geochemical processes occurring with the generation and evolution of acid mine drainage.

Perfil citológico pulmonar de bezerros sadios nos três primeiros meses de vida

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Raphael S. Vianna

2016-05-01

Full Text Available Resumo: A citologia é um importante exame complementar utilizado para a detecção de alterações no perfil celular do trato respiratório e auxílio no diagnóstico de doenças. No entanto, como os primeiros meses de vida compõem o período de adaptação à vida extrauterina resultando em possíveis alterações das populações celulares, é essencial a padronização das características comuns aos animais sadios, possibilitando a identificação e análise de qualquer mudança no quadro esperado. O objetivo desta pesquisa foi caracterizar o perfil celular por citologia do lavado broncoalveolar obtido semanalmente por broncoscopia de dez bezerros durante os três primeiros meses de vida. A análise estatística foi realizada utilizando-se o software Minitab® 15.0, empregando-se o teste T pareado para as amostras paramétricas e Mann-Whitney para as amostras não paramétricas, considerando nivel de significância P≤0,05. Os resultados obtidos apontaram que o perfil celular do lavado broncoalveolar de bezerros hígidos durante os primeiros 90 dias de vida apresentou predomínio de macrófagos, com média geral de 63,17%, seguido de 33,69% de neutrófilos. Porém observou-se diminuição significativa na porcentagem de macrófagos (P=0,04 e aumento de neutrófilos (P=0,05 ao longo dos momentos, comprovada pela forte correlação negativa entre as porcentagens de macrófagos e neutrófilos ao longo dos momentos. Não houve diferença entre as porcentagens de células gigantes, células epiteliais, linfócitos, eosinófilos e basófilos durante o experimento. Apesar dos resultados serem influenciados por fatores ambientais e de manejo, os resultados dessa pesquisa fornecem subsídios para a identificação de alterações críticas que descaracterizem o perfil celular de bezerros acometidos por doenças respiratórias.

The geological evolution of opalinus clay in the Zurcher Weinland Area (ne Switzerland): learning from the past to predict future evolution and stability

International Nuclear Information System (INIS)

Gautschi, A.; Mazurek, M.

2004-01-01

A number of safety-relevant issues need to be addressed when considering long-term evolution of a radioactive waste repository, out of which uplift/erosion, fault activity, and changes in the geochemical and hydrogeological environment are particularly important. Among the strongest arguments in the prediction of future evolution is the extrapolation of events and processes that occurred over a long period of time in the geological past (e.g. 10 Ma) to a shorter period in the future. The future long-term evolution of Opalinus Clay in a potential siting area for a high-level waste repository in the Zurcher Weinland (NE Switzerland) is considered over a time period of around l Ma. The geological evolution or geological stability, respectively, can be predicted plausibly within reasonable limits over such a time period based on a detailed analysis of geological history. Predictions extending beyond this time period are feasible but contain an increasing element of uncertainty. This paper summarises the project-related conclusions, which are presented in greater detail in Nagra (2002a). (author)

Geochemical prospecting in Guiana

International Nuclear Information System (INIS)

Coulomb, R.

1957-01-01

During the last few years geochemical prospecting techniques have become common usage in the field of mineral deposit prospecting. The real scope of these methods lies in their use in the prospecting of large areas. The most promising use of the geochemistry and hydro-geochemistry of uranium is in heavily forested tropical territories, with few outcrops, where radiometry is strongly handicapped. (author) [fr

Preliminary Geochemical and Rock Magnetic Study of a Stalagmite From Quintana Roo, Northeastern Yucatan Peninsula

Science.gov (United States)

Urrutia-Fucugauchi, J.; Perez-Cruz, L.; Zhao, X.; Rebolledo-Vieyra, M.; Rodriguez, A.

2012-04-01

We present the preliminary results of geochemical, stable isotopes and rock magnetic studies of a stalagmite from a cave in eastern Quintana Roo, northern Yucatan peninsula. In the past years, there has been increased interest in understanding the paleoclimatic and paleoenvironmental evolution of the Yucatan peninsula and northern Central America, investigating the relationships between climate variations and the development of the Maya civilization. In particular, the variations in regional precipitation and occurrence of several drought periods, which might have been related to the collapse of the Classic Maya period. Stable isotope data on speleothems from different sites in Yucatan and Central America have provided evidence on changes in precipitation, which have affected the Maya region. The stalagmite is ~47 cm long and about 4-5 cm wide at its base. It was collected from the Hilariós Well cave in Tulum, Quintana Roo. Magnetic susceptibility and geochemical analyses have been completed as part of the initial characterization of the stalagmite, with measurements taken every centimeter. Geochemical analyses have been carried out for x-ray fluorescence, with a Niton XRF analyzer. Magnetic susceptibility was determined with a Bartington MS2 instrument using the high resolution surface probe. Additional rock magnetic analyses include magnetic hysteresis loops and isothermal remanent magnetization (IRM) acquisition, and saturation IRM demagnetization, which have been measured with a MicroMag instrument. Hysteresis loops are diamagnetic, with small varying low-coercivity ferromagnetic components. The elemental compositions of major oxides and trace elements vary with depth. Calcium is the major element and displays a pattern of small amplitude fluctuations with a trend to lower values at the bottom, which are also shown in other elements such as barium. Silica and elements such as titanium and strontium are positively correlated and show an apparent cyclic pattern

Suscetibilidade a desinfetantes e perfil de resistência a antimicrobianos em isolados de Escherichia coli

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Carina C. Krewer

2012-11-01

Full Text Available A colibacilose, causada por Escherichia coli, é a enfermidade entérica de maior impacto na produção de suínos, podendo levar à morte do animal. Esta bactéria possui grande capacidade de desenvolver resistência a múltiplos antimicrobianos e a desinfetantes. Desta forma, estudos que abordem mecanismos de resistência e perfil de amostras de campo tornam-se necessários. E. coli é amplamente utilizada como modelo de estudos que exploram a resistência intrínseca e extrínseca a multidrogas. Neste trabalho, buscou-se verificar o perfil de sensibilidade de 62 isolados de E. coli de suínos frente a três desinfetantes e a 13 antimicrobianos. Ainda, em 31 destes isolados foi pesquisada a presença de mecanismo de efluxo. Dos três desinfetantes avaliados, o cloreto de alquil dimetil benzil amônio+poliexietilenonilfenileter foi o que se mostrou mais eficaz (100%, seguido do glutaraldeído+cloreto de alquil dimetil benzil amônio (95,2% e do cloreto de alquil dimetil benzil amônio (88,8%. Dentre os antimicrobianos testados, observou-se maior resistência para a tetraciclina (62,2% e maior sensibilidade para o florfenicol (88,6%. A alta sensibilidade dos isolados frente aos desinfetantes pode estar relacionada à ausência de mecanismo de efluxo. O índice de resistência múltipla médio aos antimicrobianos foi de 0,52, o que demonstra um perfil multirresistente dos isolados, conduzindo para a necessidade do uso racional destas drogas em suinocultura.

Summary report on geochemical barrier special study

International Nuclear Information System (INIS)

1988-12-01

Long-term management of uranium mill tailings must provide assurance that soluble contaminants will not migrate beyond the Point of Compliance. Conventional management alternatives provide containment through the use of physical barriers which are designed to prevent migration of water through the tailings pile. An alternative is to geochemically modify the tailings to immobilize the contaminants. This investigation examined three potential geochemical modifiers to determine their ability to immobilize inorganic groundwater contaminants found in uranium mill tailings. These modifiers were hydrated lime (Ca(OH) 2 ), limestone (CaCO 3 ), and a sphaegnum peat moss. This investigation focused on both the geochemical interactions between the tailings and the modifiers, and the effects the modifiers had on the physical strength of the tailings. The geochemical investigations began with characterization of the tailings by X-ray diffraction and scanning electron microscopy. This was followed by batch leaching experiments in which various concentrations of each modifier were added to tailings in shaker flasks and allowed to come to equilibrium. Finally, column experiments were conducted to simulate flow through a tailings pile. The results show that all of the modifiers were at least moderately effective at immobilizing most of the groundwater contaminants of concern at uranium mill tailings sites. Hydrated lime was able to achieve 90 percent concentration reduction of arsenic, cadmium, selenium, uranium, and sulfate when added at a two percent concentration. Limestone was somewhat less effective and peat removed greater than 90 percent of arsenic, lead, uranium, and sulfate at a one percent concentration. The column tests showed that kinetic and/or mass transfer limitations are important and that sufficient time must be allowed for the immobilization reactions to occur

Proceedings of 2. Brazilian Geochemical Congress

International Nuclear Information System (INIS)

1989-01-01

Some works about geochemistry are presented, including themes about geochemical exploration, lithogeochemistry and isotope geochemistry, environmental geochemistry, analytical geochemistry, geochemistry of carbonatites and rare earth elements and organic geochemistry. (C.G.C.) [pt

Cyanobacterial evolution during the Precambrian

Science.gov (United States)

Schirrmeister, Bettina E.; Sanchez-Baracaldo, Patricia; Wacey, David

2016-07-01

Life on Earth has existed for at least 3.5 billion years. Yet, relatively little is known of its evolution during the first two billion years, due to the scarceness and generally poor preservation of fossilized biological material. Cyanobacteria, formerly known as blue green algae were among the first crown Eubacteria to evolve and for more than 2.5 billion years they have strongly influenced Earth's biosphere. Being the only organism where oxygenic photosynthesis has originated, they have oxygenated Earth's atmosphere and hydrosphere, triggered the evolution of plants -being ancestral to chloroplasts- and enabled the evolution of complex life based on aerobic respiration. Having such a strong impact on early life, one might expect that the evolutionary success of this group may also have triggered further biosphere changes during early Earth history. However, very little is known about the early evolution of this phylum and ongoing debates about cyanobacterial fossils, biomarkers and molecular clock analyses highlight the difficulties in this field of research. Although phylogenomic analyses have provided promising glimpses into the early evolution of cyanobacteria, estimated divergence ages are often very uncertain, because of vague and insufficient tree-calibrations. Results of molecular clock analyses are intrinsically tied to these prior calibration points, hence improving calibrations will enable more precise divergence time estimations. Here we provide a review of previously described Precambrian microfossils, biomarkers and geochemical markers that inform upon the early evolution of cyanobacteria. Future research in micropalaeontology will require novel analyses and imaging techniques to improve taxonomic affiliation of many Precambrian microfossils. Consequently, a better understanding of early cyanobacterial evolution will not only allow for a more specific calibration of cyanobacterial and eubacterial phylogenies, but also provide new dates for the tree

Geochemical modelling. Pt.1, Pt.2

International Nuclear Information System (INIS)

Skytte Jensen, B.; Jensen, H.; Pearson, F.J.

1992-01-01

This work is carried out under cost-sharing contract with the European Atomic Energy Community in the framework of its fourth research programme on radioactive waste management and radioactive waste storage. This final report is subdivided into two parts. In the first part, JENSEN, a computer code for the computation of chemical equilibria in aqueous systems, describes the structure, function and use of a new geochemical computer program intended for PC's. The program, which is written in Turbo Pascal, version 4, is fundamentally similar to most other geochemical programs, but combines in one program several of the merits these programs have. The intention has been to make an advanced program, which also should be user friendly and fast, and to attain this several new algorithms have been developed and implemented. The program has a built-in database mainly based on the CHEMVAL compilation containing data for 395 soluble species and 149 minerals. The program can find equilibria in the presence of all or some of these soluble species, under conditions or fixed or floating pH and / or Redox potential. The program by itself eliminates a bad guess of a candidate for precipitation. In the present version, the program can identify which minerals and how much of them there will be formed when equilibrium is established. In the second part, LITTLE JOE, an expert system to support geochemical modelling, describes the construction of a minor expert system for use in the evaluation of analytical data for the composition of ground waters from limestone formation. Although the example given is rather limited in scope, the application of the expert system for the evaluation of the analytical data clearly demonstrates the mature expert knowledge imbedded in the system which is contrasted with the uncritical acceptance of analytical or theoretical data. With the overall neglect of ion-exchange and the formation of solid solutions in geochemical calculations, geochemistry is

Perfiles motivacionales de usuarios de servicios deportivos públicos y privados / Motivational Profiles of Users of Private and Public Sport Services

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Román Nuviala Nuviala

2013-06-01

Full Text Available Las altas tasas de sedentarismo y abandono deportivo y la escasez de estudios sobre motivos de práctica en el ámbito de la actividad física no competitiva han generado la necesidad de llevar a cabo investigaciones que establezcan perfiles motivacionales de usuarios de servicios deportivos. La finalidad de esta investigación fue diferenciar los perfiles motivacionales con respecto a la práctica físico-deportiva y analizar su relación con variables sociodemográficas (edad y sexo. La muestra del estudio estuvo compuesta por un total de 2707 usuarios de servicios deportivos, públicos y privados, de Andalucía (España, que cumplimentaron la escala de Motivos de Actividad Física-Revisada (Motives for Physical Activity Measure-Revised [MPAM-R]. Se realizó un análisis por conglomerados y, seguidamente, la prueba ji-cuadrado. Los resultados obtenidos en este análisis establecieron la existencia de tres perfiles motivacionales: uno altamente motivado, especialmente hacia la salud, con sujetos principalmente varones jóvenes de organizaciones públicas; un segundo grupo con motivación por debajo de la media en todas sus dimensiones, e inducido, especialmente por razones de salud, disfrute y apariencia, con un perfil de usuario privado, mujer, de edad media o avanzada; un tercer grupo en el que primaron los motivos sociales y de disfrute, conformado mayoritariamente por usuarios de organizaciones privadas y de sexo masculino.

Modelo matemático de la transferencia de calor para predecir el perfil de durezas en probetas Jominy

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López, E.

2013-04-01

Full Text Available The heat transfer coefficient was estimated at the bottom surface at Jominy bar end quench specimen by solution of the heat inverse conduction problem. A mathematical model based on the finite-difference method was developed to predict thermal paths and volume fraction of transformed phases. The mathematical model was codified in the commercial package Microsoft Visual Basic v. 6. The calculated thermal path and final phase distribution were used to evaluate the hardness distribution along the AISI 4140 Jominy bar.En el presente trabajo se estimó el coeficiente de transferencia de calor en la superficie que se encuentra en contacto con el chorro de agua en la probeta Jominy mediante la solución del problema inverso de conducción de calor. Con el objetivo de predecir los perfiles térmicos y las fracciones de fase transformadas se formuló un modelo matemático con el método de diferencias finitas y se codificó en el software comercial Microsoft Visual Basic v. 6. Los perfiles térmicos y las fracciones de fase calculadas se utilizaron para predecir el perfil de durezas en una probeta Jominy de acero AISI 4140 mediante el uso de correlaciones empíricas.

Review of geochemical measurement techniques for a nuclear waste repository in bedded salt

International Nuclear Information System (INIS)

Knauss, K.G.; Steinborn, T.L.

1980-01-01

A broad, general review is presented of geochemical measurement techniques that can provide data necessary for site selection and repository effectiveness assessment for a radioactive waste repository in bedded salt. The available measurement techniques are organized according to the parameter measured. The list of geochemical parameters include all those measurable geochemical properties of a sample whole values determine the geochemical characteristics or behavior of the system. For each technique, remarks are made pertaining to the operating principles of the measurement instrument and the purpose for which the technique is used. Attention is drawn to areas where further research and development are needed

Behaviour of nature and technogenic radioisotopes in buried geochemical barriers

International Nuclear Information System (INIS)

Kuznetsov, V.A.; Onoshko, M.P.; Generalova, V.A.

1998-01-01

Behaviour of potassium 40, radium 226, thorium 232, strontium 90 and cesium 137 on geochemical barriers connected with buried soils and cut-off meander sediments of the Holocene age of the Sozh river valley are examined. Some sides of the barrier geochemical structure caused by syngeneic and epigenetic processes have been taken into consideration

Long-term Geochemical Evolution of Lithogenic Versus Anthropogenic Distribution of Macro and Trace Elements in Household Attic Dust.

Science.gov (United States)

Balabanova, Biljana; Stafilov, Trajče; Šajn, Robert; Tănăselia, Claudiu

2017-01-01

Attic dusts were examined as historical archives of anthropogenic emissions, with the goal of elucidating the enrichment pathways associated with hydrothermal exploitation of Cu, Pb, and Zn minerals in the Bregalnica River basin in the eastern part of the Republic of Macedonia. Dust samples were collected from 84 settlements. Atomic emission spectrometry and mass spectrometry with inductively coupled plasma were applied as analytical techniques for the determination of 69 element contents. Multivariate analysis was applied for the extraction of dominant geochemical markers. The lithogenic distribution was simplified to six dominant geochemical markers: F1: Ga-Nb-Ta-Y-(La-Gd)-(Eu-Lu); F2: Be-Cr-Li-Mg-Ni; F3: Ag-Bi-Cd-Cu-In-Mn-Pb-Sb-Te-W-Zn; F4: Ba-Cs-Hf-Pd-Rb-Sr-Tl-Zr; F5: As-Co-Ge-V; and F6: К-Na-Sc-Ti. The anthropogenic effects on the air pollution were marked by a dominance of F3 and secondary dominance of F5. The fifth factor also was determined as a lithogenic marker for the occurrence of the very old Rifeous shales. The first factor also presents a very unique association that despite the heterogeneity relays on natural phenomena of tracking the deposition in areas of Proterosoic gneisses; related to the distribution of fine particles was associated with carbonate-silicate volcanic rocks. Intensive poly-metallic dust depositions were recorded only in the surroundings of localities where the hydrothermal extractions are implemented. Long-term deposition can be considered as pollution indexes for these hot spots. This mainly affects the Cd, Pb, and Zn deposition that is as high as 25, 3900, and 3200 mg/kg, respectively.

Perfil de extensão vocal em coristas após técnica de vibração de língua associada a escalas

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Amanda Thaís Lima

Full Text Available RESUMO: Objetivo: identificar o efeito imediato da técnica de vibração sonorizada de língua associada à variação tonal sobre o perfil de extensão vocal de coristas, analisando o tempo de prática de canto, naipe e tempo de execução do exercício. Métodos: estudo transversal quantitativo, com 13 cantores, sendo oito mulheres e cinco homens, com média de idade de 39±20,11 anos, pertencentes a diferentes naipes. O perfil de extensão vocal foi obtido a partir da análise pelo software Vocalgrama da CTS Informática. As amostras foram coletadas em três momentos: antes, após um minuto e após dois minutos de aplicação da técnica de vibração sonorizada de língua associada à variação tonal. Resultados: seis coristas (46,2% aumentaram o valor do perfil de extensão vocal, após dois minutos de execução da técnica. Os naipes sopranos e tenores apresentaram valores médios maiores do perfil de extensão vocal após dois minutos de exercício. Em relação ao tempo de prática de canto, não houve diferença entre os grupos no valor do perfil de extensão vocal em nenhum dos três momentos considerados. Conclusão: a técnica de vibração sonorizada de língua associada à variação tonal não interferiu no perfil de extensão vocal dos coristas estudados. Entretanto, o tempo de execução do exercício parece influenciar nos resultados.

Modeling coupled thermal, flow, transport and geochemical processes controlling near field long-term evolution

International Nuclear Information System (INIS)

Zhou, W.; Arthur, R.; Xu, T.; Pruess, K.

2005-01-01

precipitation/dissolution and solute transport. Preliminary results show that during the early heating phase, reactions strongly depend on the magnitude of the temperature gradient across the buffer. As the temperature gradient diminishes, reactions are increasingly dominated by groundwater solutes diffusing into the bentonite pore water from the host rock. Bentonite effective diffusion coefficient plays an important role to long-term solute transport. [1] Arthur, R., W. Zhou, and B. Stromberg, (2003), 'THC modeling of the non-isothermal phase of near-field evolution' in Proceedings of the 10. International High-Level Radioactive Waste Management Conference, March 30-April 2, 2003, Las Vegas, Nevada, USA. [2] Hoekmark, H. and B. Faelth, (2003), Thermal dimensioning of the deep repository, SKB TR-03- 09, Swedish Nuclear Fuel and Waste Management Co., Stockholm, Sweden. [3] Bruno, J. D. Arcos, and L. Duro, (1999), Processes and features affecting the near field hydro-chemistry, SKB TR-99-29, Swedish Nuclear Fuel and Waste Management Co., Stockholm, Sweden. [4] Xu, T., E. Sonnenthal, N. Spycher, and K. Pruess, (2003), TOUGHREACT User's Guide: A Simulation Program for Non-isothermal Multiphase Reactive Geochemical Transport in Variably Saturated Geologic Media, LBNL-55460, Lawrence Berkeley National Laboratory, Berkeley, California, USA. (authors)

Análisis CFD sobre la influencia de la solidez en aerogeneradores H-Darrieus con perfiles asimétricos NACA 7425

OpenAIRE

Rivero Sánchez, Alonso

2016-01-01

El presente trabajo de fin de grado es un estudio CFD de un aerogenerador de eje vertical tipo H-Darrieus de pequeñas dimensiones, compuesto por tres álabes con perfiles asimétricos NACA 7425. El objetivo principal es analizar la influencia de la solidez en un aerogenerador con estas características, para ello se estudiaran diferentes modelos posibles, rotor completo y perfiles estáticos. En la práctica se han realizado diversas simulaciones para llegar a obtener las curvas características de...

La profesión docente: escenarios, perfiles y tendencias

Directory of Open Access Journals (Sweden)

Pablo PALOMERO FERNÁNDEZ

2010-01-01

Full Text Available En este artículo se hace una presentación del número 35, volumen 13(4 de la Revista electrónica Interuniversitaria de Formación del Profesorado: La profesión docente: escenarios, perfiles y tendencias, en el que participan autores de veintiocho instituciones pertenecientes a cinco países: España, Brasil, México, Argentina y Perú. Se trata de un volumen que consta de veintiocho artículos seguidos de un conjunto de resúmenes de tesis doctorales y recensiones bibliográficas, cuyo marco general es el escenario de la profesión docente.

PERFIL DE ENGAJAMENTO PARA O AUTOCUIDADO EM PORTADORES DE HIPERTENSÃO ARTERIAL

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GISELLE ANDRADE DOS SANTOS SILVA

2008-01-01

Full Text Available Estudio descriptivo con el objetivo de identificar el perfil de compromiso con el auto cuidado en personas hipertensas acompañadas clínicamente en la Unidad Básica de Salud de la Familia. Utilizamos los instrumentos para establecer el perfil de compromiso en el autocuidado teniendo como conjetura la teoría del autocuidado de Orem. Pesquisadas 31 personas, registradas en (HIPER/DÍA el año 2004. Identificados los requisitos de autocuidado con calificación positiva en relación a las eliminaciones, a la adaptación a los cambios del ciclo vital; ajuste social; al conocimiento de la enfermedad y del tratamiento; aceptación del diagnóstico; adaptación al problema con la salud y a las conductas orientadas. Y calificación no satisfactoria a la ingestión de alimentos y líquidos; desequilibrio entre soledad e interacción social; a la prevención de riesgo de vida y al bienestar; a la promoción de la salud. Constatamos que una fracción de portadores de hipertensión acompañados clínicamente por el PSF se compromete con el auto-cuidado frente a las acciones llevadas a cabo.

PERFIL LÍPIDICO DOS PACIENTES HIV POSITIVOS EM USO DA TERAPIA ANTIRRETROVIRAL

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Maria Roseane dos Santos

2017-07-01

Full Text Available Corresponde a estudo descritivo de corte transversal, buscou-se evidenciar o impacto da TARV sobre o perfil lipídico. Realizada com 37 pacientes atendidos no ambulatório de Doenças Infecciosas e Parasitárias do centro de referência para HIV do Hospital Universitário Oswaldo Cruz em Recife-PE/Brasil. Através da realização de entrevistas, coleta de informações sobre terapia antirretroviral, curva de CD4 e carga viral obtidas nos prontuários. Tendo como aprovação no comitê de ética e pesquisa CAAE de nº 11365112.8.0000.5192. Revela o impacto no perfil lipídico associado ao uso contínuo da TARV, demostrando aumento do TG 54%, CT 49%, VLDL (41%, LDL-c 19% e diminuição do HDL-c 24%.   As associações de esquemas de ITRN e IRNN apresentaram o maior número de alterações. As drogas da TARV induzem distúrbios metabólicos graves e associados com outros fatores encontrados como HAS 19%, tabagismo 35% e sedentarismo 81% constituem uma forte predisposição de aterosclerose e consequentemente riscos cardiovasculares.

GEOBASI: The geochemical Database of Tuscany Region (Italy

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Brunella Raco

2015-03-01

Full Text Available In this study the new Regional Geochemical Database (RGDB, called GEOBASI, is presented and illustrated in the framework of a joint collaboration among the three Tuscan universities (Florence, Pisa and Siena, CNR-IGG (Institute of Geosciences and Earth Resources of Pisa, ARPAT (Regional Agency for the Environmental Protection, LAMMA (Environmental Modelling and Monitoring Laboratory for Sustainable Development Consortium and S.I.R.A. (Territorial and Environmental Informative System of Tuscany. The database has permitted the construction of a repository where the geochemical information (compositional and isotopic has been stored in a structured way so that it can be available for different groups of users (e.g. institutional, public and private companies. The information contained in the database can in fact be downloaded freely and queried to correlate geochemistry to other non compositional variables. The first phase of the project was aimed at promoting the use of the geochemical data already available from previous investigations through a powerful Web-GIS interface to implement the exploratory statistics graphical-numerical tools used to: 1 analyse the spatial variability of the investigated context, 2 highlight the geographic location of data pertaining to classes of values or single cases, 3 compare the results of different analytical methodologies applied to the determination of the same element and/or chemical species, 4 extract the geochemical data related to specific monitoring plans and/or geographical areas, and finally 5 recover information about data below the detection limit to understand their impact on the behaviour of the investigated variable. Developments of this project will be focused on the definition of rules and standardized methods in a way that external users could also interactively pursue the RGDB. Furthermore, a detailed investigation of the Scarlino-Follonica plain will permit the improvement and test of

Geochemical Anomalies in the Sediments of Lake Druksiai

International Nuclear Information System (INIS)

Kleinas, A.

1999-01-01

In order to evaluate the impact of Ignalina Nuclear Power Plant (NPP) on natural processes in Lake Druksiai and accumulation of pollutants, in 19931997, carrying on the state scientific program, the Marine Geochemistry Division of the Institute of Geography performed lithological geochemical mapping of lake bottom sediments on a scale of 1 .50 000. The results obtained enabled to distinguish zones of higher anthropogenous geochemical load, where geochemical anomalies of pollutants, including oil hydrocarbons and heavy metals, had been taken into account. Applying concentration coefficients for oil hydrocarbons and heavy metals (Cr, Cu, Ni, Pb, and Zn) and their natural background, the attempt was made to differentiate natural and technogenous components in the geochemical anomalies As expected, the finer sediments -aleurite-pelite mud - showed amounts of oil hydrocarbons and heavy metals being 12.1 times higher than in fine sand - the most coarse of the sediments studied Sediments with organic mater exceeding 20% contained 11.7 times more pollutants than those with organic matter below 1 .5%. Calculations of concentration coefficients (CC) showed no elements in no stations exceeded 10 - the sediments did not reach the category of high pollution However, in many sites, the coefficients exceeded values of 1-2, thus, showing sediments attributable to the categories of weakly polluted or just polluted. Mapping model done by GIS methods (by superimposing schemes of pollutant CCs distribution in the lake and summing them) for geochemical anomalies two derivative map-schemes were obtained for oil hydrocarbons and heavy metals. They showed that clean sediments cover just 24.75% (according to the pollutant background for soil types) and 12.35% (according to the organic matter background for its amount intervals) lake bottom area. Zones slightly polluted by an element at least cover 69.7 and 80.29% of lake area, correspondingly; whereas zones slightly polluted by all

Estudantes de enfermagem têm perfil empreendedor? ¿Estudiantes de enfermería tienen perfil emprendedor? Do nursing students have entrepreuner profile?

Directory of Open Access Journals (Sweden)

Paulo Fernando Roncon

2009-10-01

Full Text Available Estudo descritivo-exploratório que teve como objetivo conhecer o perfil dos estudantes concluintes de um curso de graduação em enfermagem quanto ao empreendedorismo. O Teste de Tendência Empreendedora Geral, contendo 54 questões, foi aplicado a 41 estudantes. Os resultados demonstraram que14% apresentam cinco tendências empreendedoras e 12% quatro tendências empreendedoras; 80% apresentam fraca ou nenhuma tendência empreendedora. A grande maioria pretende encaminhar sua a profissão em atividades assistenciais, enquanto nenhum dos estudantes pretende atuar em atividades administrativas. Conclui-se que, os estudantes possuem baixo grau de presença de características empreendedoras.Estudio descriptivo-exploratorio que tvo como objetivo conocer el perfil de los estudiantes concluintes de un curso de grado de enfermería cuanto al espíritu emprendedor. El Test General de Tendencia Emprendedora contiendo 54 cuestiones fue aplicado a 41 estudiantes. Resultados demostraran que 14% tienen cinco tendencias de emprendedor, 12% tienen cuatro tendencias de emprendedor, 80% no tienen tendencias de emprendedor. La mayoría desea trabajar con actividades asistenciales, mientras ninguno de ellos desean trabajar con actividades administrativas. Se concluye que los estudiantes tienen bajo grado de presencia de características emprendedoras.Descriptive-exploratory study that aimed at knowing the profile of nursing students regarding entrepreneurship. The General Entrepreneurship Trend Test with 54 questions was applied to 41 students. Results demonstrated that 14% present five entrepreneur tendencies, 12% present four entrepreneur tendencies, and 80% do not present entrepreneur tendencies. The majority of student intent to work as clinical nurses, while none of them intent to work in management activities. It was concluded that students have low grade of the entrepreneurship characteristics.

Effect of source integration on the geochemical fluxes from springs

International Nuclear Information System (INIS)

Frisbee, Marty D.; Phillips, Fred M.; White, Art F.; Campbell, Andrew R.; Liu, Fengjing

2013-01-01

Geochemical fluxes from watersheds are typically defined using mass-balance methods that essentially lump all weathering processes operative in a watershed into a single flux of solute mass measured in streamflow at the watershed outlet. However, it is important that we understand how weathering processes in different hydrological zones of a watershed (i.e., surface, unsaturated, and saturated zones) contribute to the total geochemical flux from the watershed. This capability will improve understanding of how geochemical fluxes from these different zones may change in response to climate change. Here, the geochemical flux from weathering processes occurring solely in the saturated zone is investigated. This task, however, remains exceedingly difficult due to the sparsity of subsurface sampling points, especially in large, remote, and/or undeveloped watersheds. In such cases, springflow is often assumed to be a proxy for groundwater (defined as water residing in fully saturated geologic formations). However, springflow generation may integrate different sources of water including, but not limited to, groundwater. The authors’ hypothesis is that long-term estimates of geochemical fluxes from groundwater using springflow proxies will be too large due to the integrative nature of springflow generation. Two conceptual models of springflow generation are tested using endmember mixing analyses (EMMA) on observations of spring chemistries and stable isotopic compositions in a large alpine watershed in the San Juan Mountains of southwestern Colorado. In the “total springflow” conceptual model, springflow is assumed to be 100% groundwater. In the “fractional springflow” conceptual model, springflow is assumed to be an integration of different sources of water (e.g., groundwater, unsaturated flow, preferential flow in the soil, etc.) and groundwater is only a fractional component. The results indicate that groundwater contributions in springflow range from 2% to 100

Drowning in Geochemical Data: The Good, the bad, and the Ugly

Science.gov (United States)

Hofmann, A. W.; Goldstein, S. L.

2008-12-01

Geochemical databases are placing unprecedented amounts of geochemical data at the fingertips of professionals and students. How these data are being used is taking an increasingly important role in shaping our thinking about the Earth. Databases have helped to expose (and eventually kill?) some long- cherished myths, such as the idea of the well-homogenized upper-mantle reservoir, and and they have made geochemical data accessible to geophysicists and enabled them to look at geochemistry with fresh eyes, leading to genuinely new insights. Yet, their very accessibility also makes them "dangerous tools" in the hands of the inexperienced. Statistical treatment of masses of geochemical data without, or with excessive, filtering can yield all sorts of "answers" we would probably be better off without. Data that are severely flawed (due to alteration or poor analytical quality, errors in published data, or errors during data entry) might not be easily identified by, say, a geodynamicist. Other dangers stem from overrepresentation of over-sampled locations and the general, but faulty, assumption of random sampling of the Earth. We will show examples where raw downloads of data from databases without extensive screening can yield data collections where the garbage swamps the useful information. We will also show impressive but meaningless correlations, e.g. upper-mantle temperature versus atmospheric temperature. The lesson is that screening is necessary. On the other hand, sound database compilations now demonstrate that average incompatible-element concentrations in global MORB are two to five times higher than published estimates. This fundamentally changes 30-year-old geochemical mass balance estimates of the mantle. OIBs are fundamentally similar to MORBs but are isotopically shifted, on average, to more "enriched" values. Mantle geochemistry is now fully consistent with dynamic models of "whole-mantle" circulation, with the likely exception of a relatively small

Biocompuestos para perfiles avanzados adaptados a la edificación = Biocomposites for Advanced Profiles Adapted to Building Envelope

Directory of Open Access Journals (Sweden)

I. Roig

2016-04-01

Full Text Available Compuestos alternativos en el sector de la envolvente se obtienen por extrusión de estirado de secciones y perfiles de panel de enclavamiento estrechas. Estos elementos estructurales, resistentes al impacto, tienen la ventaja de una instalación más rápida y segura, y su diseño modular les hace idóneos para muchos edificios y otras aplicaciones. Un desarrollo adicional en esta área puede ser la obtención de una alternativa sostenible a los perfiles compuestos actuales. Estudios anteriores han demostrado que los compuestos fabricados a partir de materiales naturales tales como fibras y polímeros bio-derivados, ofrecen una alternativa sostenible a los polímeros y materiales compuestos tradicionales. El objetivo de este desarrollo es reemplazar el típico perfil de acero ligero. Los perfiles de acabado también se pueden utilizar para terminar tabiques de mampostería existentes, revestimiento de ejes mecánicos y de extracción y revestimiento de la columna. Los perfiles se han diseñado utilizando bio-polímeros, reforzados con fibras naturales. Se han establecido los parámetros de procesamiento y las formulaciones apropiadas de bioresina y fibras naturales. También se ha evaluado la adaptación de las técnicas de procesamiento de pultrusión existentes a las características concretas de los nuevos biomateriales y fibras naturales. Como resultado, los perfiles de pultrusión adaptados a la construcción se han desarrollado con la incorporación de nuevos materiales y biomateriales basados en resina. Abstract An alternative composites answer in the envelope sector is the fabrication by pultrusion of narrow interlocking panel sections and profiles. These impact-resistant structural elements have the advantage of quicker, safer installation and their modular design equally answers many identical building and other applications¡Error! No se encuentra el origen de la referencia.. An additional development in this area can be the

Los perfiles de exigencias en la ocupación del profesional de recursos humanos

Directory of Open Access Journals (Sweden)

Santiago Pereda Marín

2003-01-01

Full Text Available En este trabajo se presentan los resultados de un estudio exploratorio que se llevó a cabo en la Universidad Complutense de Madrid para definir el perfil de exigencias ocupacionales del profesional de recursos humanos. En este estudio se considera como profesional de recursos humanos al licenciado, ingeniero o doctor que desarrolla su actividad en el área de recursos humanos sin ocupar puestos directivos dentro de la estructura de la organización. Los resultados de este estudio, que se obtuvieron a partir de una muestra de 37 profesionales de recursos humanos en activo, señalan seis competencias como claves para el desempeño de la ocupación; éstas son, por orden de importancia: trabajo en equipo, orientación al cliente, planificación/organización, comunicación, flexibilidad y colaboración. Asimismo, se comprobó que la metodología empleada es útil, aunque se considera que es preciso introducirle pequeños cambios para optimizar el trabajo en la definición de los perfiles de exigencias ocupacionales.

Geochemical nature of sub-ridge mantle and opening dynamics of the South China Sea

Science.gov (United States)

Zhang, Guo-Liang; Luo, Qing; Zhao, Jian; Jackson, Matthew G.; Guo, Li-Shuang; Zhong, Li-Feng

2018-05-01

The Indian-type mantle (i.e., above the north hemisphere reference line on the plot of 208Pb/204Pb vs. 206Pb/204Pb) has been considered as a "Southern Hemisphere" geochemical signature, whose origin remains enigmatic. The South China Sea is an extensional basin formed after rifting of the Euro-Asia continent in the Northern Hemisphere, however, the geochemical nature of the igneous crust remains unexplored. For the first time, IODP Expedition 349 has recovered seafloor basalts covered by the thick sediments in the Southwest sub-basin (Sites U1433 and U1434) and the East sub-basin (Site U1431). The Southwest sub-basin consists of enriched (E)-MORB type basalts, and the East sub-basin consists of both normal (N)-MORB-type and E-MORB-type basalts based on trace element compositions. The basalts of the two sub-basins are Indian-type MORBs based on Sr-Nd-Pb-Hf isotope compositions, and the Southwest sub-basin basalts show isotopic compositions (i.e., 206Pb/204Pb of 17.59-17.89) distinctly different from the East sub-basin (i.e., 206Pb/204Pb of 18.38-18.57), suggesting a sub-basin scale mantle compositional heterogeneity and different histories of mantle compositional evolution. Two different enriched mantle end-members (EM1 and EM2) are responsible for the genesis of the Indian-type mantle in the South China Sea. We have modeled the influences of Hainan mantle plume and lower continental crust based on Sr-Nd-Pb-Hf isotope compositions. The results indicate that the influence of Hainan plume can explain the elevated 206Pb/204Pb of the East sub-basin basalts, and the recycling of lower continental crust can explain the low 206Pb/204Pb of the Southwest sub-basin basalts. Based on the strong geochemical imprints of Hainan plume in the ridge magmatism, we propose that the Hainan plume might have promoted the opening of the South China Sea, during which the Hainan plume contributed enriched component to the sub-ridge mantle and caused thermal erosion and return of lower

The geochemical environment of nuclear fuel waste disposal

International Nuclear Information System (INIS)

Gascoyne, M.

1995-01-01

The concept for disposal of Canada's nuclear fuel waste in a geologic environment on the Canadian Shield has recently been presented by Atomic Energy of Canada Limited (AECL) to governments, scientists, and the public, for review. An important part of this concept concerns the geochemical environment of a disposal vault and includes consideration of rock and groundwater compositions, geochemical interactions between rocks, groundwaters, and emplaced vault materials, and the influences and significance of anthropogenic and microbiological effects following closure of the vault. This paper summarizes the disposal concept and examines aspects of the geochemical environment. The presence of saline groundwaters and reducing conditions at proposed vault depths (500-1000 m) in the Canadian Shield has an important bearing on the stability of the used nuclear fuel, its container, and buffer and backfill materials. The potential for introduction of anthropogenic contaminants and microbes during site investigations and vault excavation, operation, and sealing is described with examples from AECL's research areas on the Shield and in their underground research laboratory in southeastern Manitoba. (author)

Well sediments: a medium for geochemical prospecting, an example from the Nisa region, Portugal

NARCIS (Netherlands)

Vriend, S.P.; Dekkers, M.J.; Janssen, M.A.; Commandeur, J.

1991-01-01

Vriend, S.P., Dekkers, M.J.. Janssen, M.A. and Commandeur, J., 1991. Well sediments: a medium for geochemical prospecting, an example from the Nisa region. Portugal. In: A.W. Rose and P.M. Taufen I Editors). Geochemical Exploration ! 989. J. Geochem. Expior., 4 ! : ! 5 I- 167. Tile potential of

Concerning initial and secondary character of radionuclide distribution in elementary landscape geochemical systems

Science.gov (United States)

Korobova, Elena; Romanov, Sergey

2017-04-01

study confirms that Cs-137 as a label helps to trace processes and patterns of chemical elements' migration on the level of ELGS that are numerously reproduced elsewhere in natural systems. The study is aimed at and believed to provide solution for a number of important problems related to generation and evolution of soil structure, spatial redistribution of fertilizers and pesticides, other important processes of matter redistribution on the level of local LGS. References Korobova E.M., Korovaykov P.A., 1990. Landscape and geochemical approach to drawing up a soil distribution profile for Chernobyl radionuclides in distant areas //Seminar "Comparative assessment of the environmental impact of radionuclides released during three major nuclear accidents: Kyshtum, Windscale, Chernobyl". V. 1. Luxembourg, 309-327. Linnik V.G., 2008. Landscape differentiation of technogenic radionuclides: geoinformation systems and models. Thesis. Moscow: Moscow State University, 42 p. Romanov S.L., 1989. Principles of formation of radionuclide dispersion and concentration fields // Abstracts of the All-Union Conference "Principles and methods of landscape geochemical studies of radionuclide migration". Moscow: Vernadsky Institute, p. 46. Shcheglov A.I., Tsvetnova O.B., KlyashtorinA.L., 2001. Biogeochemical migration of technogenic radionuclides in forest ecosystems. Moscow: Nauka, 235 p.

Validation of the WATEQ4 geochemical model for uranium

International Nuclear Information System (INIS)

Krupka, K.M.; Jenne, E.A.; Deutsch, W.J.

1983-09-01

As part of the Geochemical Modeling and Nuclide/Rock/Groundwater Interactions Studies Program, a study was conducted to partially validate the WATEQ4 aqueous speciation-solubility geochemical model for uranium. The solubility controls determined with the WATEQ4 geochemical model were in excellent agreement with those laboratory studies in which the solids schoepite [UO 2 (OH) 2 . H 2 O], UO 2 (OH) 2 , and rutherfordine ((UO 2 CO 3 ) were identified as actual solubility controls for uranium. The results of modeling solution analyses from laboratory studies of uranyl phosphate solids, however, identified possible errors in the characterization of solids in the original solubility experiments. As part of this study, significant deficiencies in the WATEQ4 thermodynamic data base for uranium solutes and solids were corrected. Revisions included recalculation of selected uranium reactions. Additionally, thermodynamic data for the hydroxyl complexes of U(VI), including anionic (VI) species, were evaluated (to the extent permitted by the available data). Vanadium reactions were also added to the thermodynamic data base because uranium-vanadium solids can exist in natural ground-water systems. This study is only a partial validation of the WATEQ4 geochemical model because the available laboratory solubility studies do not cover the range of solid phases, alkaline pH values, and concentrations of inorganic complexing ligands needed to evaluate the potential solubility of uranium in ground waters associated with various proposed nuclear waste repositories. Further validation of this or other geochemical models for uranium will require careful determinations of uraninite solubility over the pH range of 7 to 10 under highly reducing conditions and of uranyl hydroxide and phosphate solubilities over the pH range of 7 to 10 under oxygenated conditions

Perfil cognitivo y psicopatológico asociados a la conducta antisocial

OpenAIRE

John Jairo Cifuentes González; Nora Helena Londoño Arredondo

2011-01-01

El objetivo del presente estudio fue establecer los componentes del perfil cognitivo y psicopatológico que caracterizan a los individuos judicialmente condenados, discriminando además el diagnóstico de trastorno de la personalidad antisocial (TPA). Participaron 607 personas que se dividieron en dos grupos: 398 casos (con TPA) y 209 controles (sin TPA). Instrumentos: YSQ-L (Young y Brown, 1999) validado por Castrillón et al. (2005), EEC-M (Londoño et al., 2006), el MCMI-II (Millon, 1999) y la ...

Perfil dos Servidores da UFES com Empréstimo Consignado

OpenAIRE

RIBEIRO, A. B.

2014-01-01

O crédito consignado é uma modalidade de empréstimo cujo valor da parcela incide sobre o salário do devedor. Com alto índice de adesão nos últimos anos,é o meio de acesso ao crédito mais comum entre os servidores públicos, pelas baixas taxas de juros, entre outros atrativos, o que contribui para expor a risco seus vencimentos com dívidas. Buscando atender ao objetivo principal de identificar se características do perfil demográfico dos servidores ativos da Universidade Federal do Espírito San...

Geochemical and geo-electrical study of mud pools at the Mutnovsky volcano (South Kamchatka, Russia): Behavior of elements, structures of feeding channels and a model of origin

International Nuclear Information System (INIS)

Bessonova, E.P.; Bortnikova, S.B.; Gora, M.P.; Manstein, Yu.A.; Shevko, A.Ya.; Panin, G.L.; Manstein, A.K.

2012-01-01

This study presents data on the geochemical composition of boiling mud pools at the Mutnovsky volcano. The physicochemical characteristics of the pools and the concentrations of major, minor and trace elements in pool solutions vary widely. A comparison of the geochemical compositions of host rocks and solutions indicates that leaching from rocks is not the only source of chemicals in thermal solutions. Geophysical studies reveal the inner structure of thermal fields, which reflect the shapes of the underground reservoirs and feed channels. Using geophysical methods (electrical resistivity tomography and frequency domain investigations), it was shown that the vertical structure and complex geochemical zonation of the feed channels leads to a high contrast in the compositions of the mud solutions. These findings answer questions about the origin and composition of surface manifestations. To elucidate the mechanisms of solution formation, an attempt was made to describe the magmatic fluid evolution and the resulting mixing of waters by physical and mathematical models. The model illustrates fluid migration from a magma chamber to the surface. It is shown that the formation of brines corresponding to the mud pool composition is possible during secondary boiling.

Kriging - a challenge in geochemical mapping

Czech Academy of Sciences Publication Activity Database

Štojdl, J.; Matys Grygar, Tomáš; Elznicová, J.; Popelka, J.; Váchová, T.; Hošek, Michal

2017-01-01

Roč. 19, APR (2017) ISSN 1607-7962. [EGU General Assembly 2017. 23.04.2017-28.04.2017, Vienna] Institutional support: RVO:61388980 Keywords : kriging * geochemical mapping Subject RIV: DD - Geochemistry http://meetingorganizer.copernicus.org/EGU2017/EGU2017-3615.pdf

Status report on geochemical modelling

International Nuclear Information System (INIS)

Read, D.

1991-12-01

This report describes the findings of a review undertaken on behalf of the project management group of the programme 'Endlagersicherheit in der Nachbetriebsphase' based at GSF-IfT (Forschungszentrum fuer Umwelt und Gesundheit - Institut fuer Tieflagerung) to establish the current status of research into the simulation of geochemical processes relevant to radiological assessment. The review is intended to contribute to Stage 1 of a strategy formulated to enhance the use of geochemical models in Germany. Emphasis has been placed on processes deemed to be of greatest relevance to performance assessment for a HLW-repository in a salt dome principally, speciation-solubility in high salinity solutions, complexation by natural organics and generation-transport of colloids. For each of these and other topics covered, a summary is given of fundamental concepts, theoretical representations and their limitations, highlighting, where appropriate, the advantages and disadvantages of alternative approaches. The availability of data to quantify any given representation is addressed, taking into account the need for information at elevated temperatures and pressures. Mass transfer is considered in terms of aqueous, particulate and gas-mediated transport, respectively. (orig.) [de

Role of geochemical background at evaluation of investment attractiveness of recreational territories

Directory of Open Access Journals (Sweden)

Vdovina Ol'ga Konstantinovna

2014-09-01

Full Text Available The article shows the role of natural geochemical background when estimating investment attractiveness of recreational areas. It is noted, that geochemical background influence on people's sickness rate isn't considered now. Though it's understood, that even insignificant increase of geochemical background in relation to percentage abundance of Earth crest may lead to endemic diseases of people, animals and plants. An indicator of geochemical endemicity areas was proposed for assessing the impact of storage elements and of a lack of geological environment on human health. Thanks to this measure, and taking into account landscape features of the area, the authors allocated lands, dangerous and potentially dangerous in terms of endemicity. The importance of ratings was achieved by the use of those factors that could have a great influence on the cost of land development. This includes, first of all, the factors that affect population health, and economic and geographic factors that minimize the cost of the territory development and the factors that give rise to financial risks and risks of human losses. The main risk factors include: potential ecological and geochemical risk; high absolute heights, development and activity of dangerous geological processes and phenomena. Systemacity of researches was reached by using factors, that characterize the object from different aspects; readiness of area infrastructure to its exploration and possible risks. Objectivity was achieved by the use of figures obtained from the results of geochemical and engineering surveys with their metrological support.

Relación entre la presencia de bolsas periodontales y las alteraciones del perfil lipídico en pacientes con ateroesclerosis

OpenAIRE

Ruiz Alvarez, Carmen; Pareja Vásquez, María del Carmen

2006-01-01

Objetivo: determinar la relación entre la presencia de bolsas periodontales y la alteración en los valores del perfil lipídico (niveles plasmáticos de colesterol, triglicéridos, HDL, LDL) en pacientes con ateroesclerosis. Material y método: investigación de tipo descriptiva correlacional. Se examinó a 114 pacientes de ambos sexos, con edades entre 35 y 65 años. Fueron clasificados en dos grupos: un grupo de 38 pacientes sanos y otro de 38 pacientes que tenían perfil lipídico controlado y arte...

Groundwater monitoring of an open-pit limestone quarry: groundwater characteristics, evolution and their connections to rock slopes.

Science.gov (United States)

Eang, Khy Eam; Igarashi, Toshifumi; Fujinaga, Ryota; Kondo, Megumi; Tabelin, Carlito Baltazar

2018-03-06

Groundwater flow and its geochemical evolution in mines are important not only in the study of contaminant migration but also in the effective planning of excavation. The effects of groundwater on the stability of rock slopes and other mine constructions especially in limestone quarries are crucial because calcite, the major mineral component of limestone, is moderately soluble in water. In this study, evolution of groundwater in a limestone quarry located in Chichibu city was monitored to understand the geochemical processes occurring within the rock strata of the quarry and changes in the chemistry of groundwater, which suggests zones of deformations that may affect the stability of rock slopes. There are three distinct geological formations in the quarry: limestone layer, interbedded layer of limestone and slaty greenstone, and slaty greenstone layer as basement rock. Although the hydrochemical facies of all groundwater samples were Ca-HCO 3 type water, changes in the geochemical properties of groundwater from the three geological formations were observed. In particular, significant changes in the chemical properties of several groundwater samples along the interbedded layer were observed, which could be attributed to the mixing of groundwater from the limestone and slaty greenstone layers. On the rainy day, the concentrations of Ca 2+ and HCO 3 - in the groundwater fluctuated notably, and the groundwater flowing along the interbedded layer was dominated by groundwater from the limestone layer. These suggest that groundwater along the interbedded layer may affect the stability of rock slopes.

Evaluación de la dimensión vertical de oclusión, perfil blando y maloclusión en dentición mixta

Directory of Open Access Journals (Sweden)

María Laura Hermida Bruno

2016-01-01

Full Text Available Objetivo: Verificar la relación entre dimensión vertical de oclusión, perfil blando y maloclusión en dentición mixta. Métodos: Se realizó un estudio observacional, transversal, analítico. El protocolo fue aprobado por el Comité de Ética de la Universidad Católica del Uruguay. Participaron 79 niños entre 6 y 12 años, con una media de edad de 8,66 ±1,41, alumnos del Colegio San José del Cerro, Montevideo, Uruguay. El 57,5% (n=45 correspondió al sexo masculino y 42,5% (n=34 al sexo femenino. Un observador calibrado (CCI=0,76 realizó un examen clínico y físico, medición de la dimensión vertical de oclusión (DVO y registró la clasificación de Angle. Se tomaron fotografías de perfil y se realizó el análisis de convexidad facial de Legan y Burstone (CCI=0,84. Se aplicó el test comparativo ANOVA, el de comparaciones múltiples de TUKEY y el test de Pearson (p ≤ 0,05. Resultados: La media de la DVO fue 59,16 ± 4,02. El 56,3% (n=45 fueron clasificados como Clase I de Angle; 22,5% (n=18 Clase II y 21,3% (n=17 Clase III. No hubo diferencia significativa en la media de DVO entre ambos sexos (p=0,217 ni entre los diferentes tipos de oclusión (p=0,568. La media del ángulo de la convexidad facial fue 14,57°± 3,80. Se encontró asociación estadísticamente significativa entre perfil convexo/relación molar clase II (p=0,003317, perfil recto/relación molar clase I (p=0,015887, perfil recto/relación molar clase III (p=0,003268. Conclusión: En la muestra estudiada no se encontró relación entre DVO y maloclusión, pero sí se encontró entre perfil blando y maloclusión.

Oak Ridge Geochemical Reconnaissance Program

International Nuclear Information System (INIS)

Arendt, J.W.

1977-03-01

The Oak Ridge reconnaissance program is responsible for the geochemical survey in a 12-state area covering Texas, Oklahoma, Kansas, Nebraska, South Dakota, North Dakota, Minnesota, Wisconsin, Michigan, Iowa, Indiana, and Illinois as part of the National Uranium Resource Evaluation Program. The program concept is outlined and the planning and organization of the program is discussed

PERFIL DE RENDIMIENTO TÉCNICO DEL EQUIPO TETRACAMPEÓN DE LA LIGA SUPERIOR DE BALONCESTO DE COSTA RICA

Directory of Open Access Journals (Sweden)

Braulio Sánchez Ureña

2011-12-01

Full Text Available El propósito de este estudio fue analizar y contrastar el perfil de rendimiento técnico del equipo tetracampeón de la Liga Superior de Baloncesto de Costa Rica. Se registró 142 juegos a lo largo de las temporadas 2007, 2008 y 2009. Los indicadores de rendimiento escogido fueron: lanzamientos de dos y tres puntos (convertidos, fallados, porcentaje de efectividad, lanzamientos de tiro libre (convertidos, fallados, porcentaje de efectividad, puntos, rebotes defensivos y ofensivos, faltas, pérdidas de balón, asistencias y robos de balón. La descripción de la información se basó en valores de frecuencia absoluta y relativa. El contraste de datos por temporada y periodo de juego se hizo con base en las técnicas no paramétricas U-test, test de Friedman y el Chi 2. En todos los casos se utilizó el SPSS versión 15.0 con un nivel de significancia de p ≤ 0,05. Los resultados mostraron un mejor perfil de rendimiento técnico en la temporada 2008, caracterizándose por mejores porcentajes en tiros de 2, tiros libres, menor número de pérdidas de balón y mayor cantidad de robos del balón y asistencias. En relación con el periodo de juego, el equipo mostró un mejor perfil de rendimiento técnico durante los segundos tiempos del partido. En general, el porcentaje de efectividad de tiros de 2 y tiros libres estuvo arriba del 60 % en ambos periodos de juego, mientras que el porcentaje de tiros de 3 osciló entre el 26.4 % y el 29.2 %. En conclusión, el equipo mostró un perfil de rendimiento técnico similar al reportado en la literatura y deja clara evidencia de la importancia que tiene el registro y seguimiento de los indicadores de rendimiento técnico en el baloncesto.

Fracture Sealing in Shales: Geological and Geochemical Factors

International Nuclear Information System (INIS)

Cathelineau, Michel

2001-01-01

The so-called self-sealing processes can be re-examined at the light of geological and geochemical consideration about the past history of the rocks. The concept of 'self sealing' needs to consider the formation and the sealing of fractures, especially three main stages: (i) the initiation of the fracture (development of micro-cracks initiated from previous heterogeneities up to fracturing), ii) the fracturing processes which occur generally at depth in presence of a fluid phase, iii) the healing or sealing of the fractures which corresponds basically to two main processes: a restoration of the initial permeability of the rock block by reducing the transmissivity of the discontinuity down to values equivalent to that of the homogeneous medium before fracturing, or the sealing of the open discontinuity by precipitation of newly formed minerals. In the latter case, the evolution of the open fracture is driven by re-arrangement of particles or precipitation of newly formed material, either by dissolution/crystallisation processes or by crystallisation from the percolating fluids (advective processes). Such processes are governed by chemical processes, especially the rate of precipitation of minerals which depends of the degree of saturation with respect to the mineral, and the kinetics of precipitation. (author)

El perfil del consumidor de hostel en Brasil y sus motivaciones

OpenAIRE

Mané, Alexandra; Ferreira, Lissa

2017-01-01

El creciente número de hostels en Brasil ha atraído cada vez más brasileños que buscan este tipo de establecimiento para hospedarse. No obstante, vale destacar que deben realizarse más estudios que aborden la importancia de los hostels y sus consumidores en el mercado de turismo. Podrán contribuir al conocimiento teórico y práctico posibilitando un mejor entendimiento sobre este segmento. El objetivo de este artículo es identificar y describir el perfil del consumidor de hostel, sus motivacio...

PSICAMB: perfil de afinidade ecológica: um estudo sobre os indicadores da postura perante a natureza = Ecological affinity profile: a study on indicators of positions towards nature = Perfil de la conectividad ecológica: un estudio sobre los indicadores de posicionamiento frente a la naturaleza

Directory of Open Access Journals (Sweden)

Rosa, Daniele da Costa Cunha Borges

2015-01-01

Full Text Available O presente estudo teve o objetivo de propor indicadores de um perfil de afinidade ecológica, avaliar sua relação com a importância dedicada à floresta amazônica e com a consideração do efeito das ações humanas na natureza. Participaram deste estudo 345 sujeitos, de ambos os sexos, com idade superior a 18 anos, das cidades de Manaus – AM e Ceres – GO. Os instrumentos deste estudo são compostos por escalas, que mediram dimensões cognitivas e afetivas na relação com a floresta amazônica e com a natureza no geral. Para análise dos dados foram realizadas análises fatoriais exploratórias, regressões e análises de estrutura de similaridade. Os resultados indicaram que ao avaliar as relações de afeto para com a natureza, as crenças em relação ao ambiente natural e a consideração de consequências futuras é possível identificar uma estrutura que engloba um perfil de afinidade ecológica e um perfil utilitarista

Efectos terapéuticos del ejercicio con sobrecarga en el perfil lipídico de adultos sedentarios

Directory of Open Access Journals (Sweden)

Felipe Caamaño Navarrete

2015-10-01

Conclusiones. Si bien se observa una tendencia a la baja en el perfil lipídico, una mayor duración y/o frecuencia de intervención podría ser necesaria para modificar significativamente las variables plasmáticas.

O Secretário Executivo com Perfil de Relações Públicas

Directory of Open Access Journals (Sweden)

Jéssica Aparecida Artico

2013-06-01

Full Text Available As diversas evoluções teórica e prática do perfil do Secretário Executivo (SE tornam-no staff, pois atua de maneira multifuncional, como assessor e/ou gestor, na alta administração. Além disso, o profissional exerce papel de “cartão de visita” da empresa onde trabalha, visto que é a ponte de comunicação interna (entre os níveis operacional-tático-estratégico e externa (empresa-mercado: fornecedores, clientes, parceiros – sociedade em geral, ademais de assessorar em negociações e em gestão/organização de eventos empresariais. Por isso, possui o papel de manter a identidade (o que a empresa realmente é e estabelecer, adequadamente, a imagem (como a empresa deve ser vista perante a sociedade da organização, considerando sua missão, visão, metas, nicho de atuação e demais quesitos relacionados. Nesse sentido, observa-se a necessidade de o SE obter conhecimentos relacionados à atuação do profissional de Relações Públicas (RP, para exercer seu papel com eficiência e eficácia. Assim, este estudo objetiva analisar o SE com perfil de RP e como essa área complementa a outra.DOI:10.7769/gesec.v4i1.90

Geochemical orientation for mineral exploration in the Hashemite Kingdom of Jordan

Science.gov (United States)

Overstreet, W.C.; Grimes, D.J.; Seitz, J.F.

1982-01-01

This report is a supplement to previous accounts of geochemical exploration conducted in the Hashemite Kingdom of Jordan by the Natural Resources Authority of the Royal Government of Jordan and the U.S. Geological Survey. The field work on which this report is based was sponsored by the U.S. Agency for International Development, U.S. Department of State. Procedures used in collecting various kinds of rocks, ores, slags, eluvial and alluvial sediments, heavy-mineral concentrates, and organic materials for use as geochemical sample media are summarized, as are the laboratory procedures followed for the analysis of these sample materials by semiquantitative spectrographic, atomic absorption, fluorometric, and X-ray diffraction methods. Geochemical evaluations of the possibilities for economic mineral deposits in certain areas are presented. The results of these preliminary investigations open concepts for further use in geochemical exploration in the search for metallic mineral deposits in Jordan. Perhaps the most desirable new activity would be hydrogeochemical exploration for uranium and base metals, accompanied by interpretation of such remote-sensing data as results of airborne radiometric surveys and computer-enhanced LANDSAT imagery. For more conventional approaches to geochemical exploration, however, several fundamental problems regarding proper choice of geochemical sample media for different geologic and geographic parts of the Country must be solved before effective surveys can be made. The present results also show that such common geochemical exploration techniques as the determination of the trace-element contents of soils, plant ash, and slags have direct application also toward the resolution of several archaeological problems in Jordan. These include the relation of trace-elements chemistry of local soils to the composition of botanic remains, the trace-elements composition of slags to the technological development of the extractive metallurgy of

Perfil lipídico e uso de anti-TNF-α

Directory of Open Access Journals (Sweden)

Antonio Carlos Ferraz Filho

2013-10-01

Full Text Available O uso do anti-TNF alfa tem sido associado a várias alterações no perfil lipídico, embora o estudo dessas alterações tenha gerado resultados que ainda são conflitantes. O conhecimento desse fato é de grande importância quando se observa a associação entre doenças reumáticas e aterogenêse acelerada. Esta pesquisa foi feita com o intuito de verificar alterações no perfil lipídico de usuários de anti-TNF-α na população do sul do Brasil e sua associação com tempo de uso, indicações, gênero do paciente e tipo de anti-TNF. Para tanto, analisaram-se os perfis de colesterol total (TC, HDL colesterol (HDLc, LDL colesterol (LDLc, índice aterogênico (IAT e triglicerídeos (TGs de 58 pacientes (42 com artrite reumatoide e 16 com espondiloartrites antes e depois do uso desse medicamento por um tempo mediano de 16,0 meses. Não se observaram alterações nos níveis de CT, HDLc, LDLc e IAT (P = NS. Todavia, houve um aumento significativo nos níveis de TGs (P = 0,03. A diferença mediana dos valores de TGs entre primeira e segunda medidas foi de 16 mg/dL, e esse aumento não estava associado ao gênero do paciente, tempo de uso, indicação de uso ou tipo de anti-TNF-α (P = NS. Concluiu-se que o uso de anti TNF-α está associado com aumento nos valores de TGs.

Perfil de egresso de Curso de Enfermagem nas Diretrizes Curriculares Nacionais: uma aproximação Perfil de los alumnos egresados de las Escuelas de Enfermería, según las Diretrizes Curriculares Nacionales: una aproximación Profile of Nursing Schools egresses according to the National Curriculum Guidelines: an approach

Directory of Open Access Journals (Sweden)

Silvana Sidney Costa Santos

2006-04-01

Full Text Available A reestruturação curricular no curso de graduação em enfermagem, necessária a partir das Diretrizes Curriculares Nacionais (DCN, inicia suas atividades com a leitura crítica da Resolução 03/2001 e nela encontra-se, entre outras orientações, o perfil de egressos. O objetivo desta revisão crítica de literatura foi refletir sobre as palavras ou categorias explícitas no perfil de egressos sugeridas pelas DCN, utilizando de dicionários (de língua portuguesa e de filosofia e de literaturas diversas (da enfermagem e de outras disciplinas, para compreendê-las de forma mais concreta e percebê-las relevantes na formação do profissional enfermeiro e, portanto, necessárias no Projeto Político Pedagógico (PPP. Reconhecem-se os valores da proposta do perfil de egressos das DCN na formação do enfermeiro, porém, torna-se importante perceber que não se trata só de estabelecer novos marcos, priorizar novos objetivos, mudar perfil, reestruturar conteúdos, restabelecer condições de funcionamento ou de cargas horárias, mas de realizar um trabalho coletivo de crescimento grupal.La reestructuración curricular en el curso de graduación en enfermero, necesaria a partir de las Directrices Curriculares Nacionales (DCN, se inicia sus actividades con la lectura crítica de la Resolución 03 / 2001 y en ella se encuentra, entre otras orientaciones, el perfil de egresos. E objetivo de esta revisión crítica de literatura fue reflexionar sobre las palabras o categorías explícitas en el perfil de egresos sugeridas por las DCN, utilizando de diccionarios (de lengua portuguesa y filosofía y diversas literaturas (del enfermero y de otras disciplinas, para que las comprenda de forma mas concreta y la perciba relevantes en la formación del profesional enfermero y, por lo tanto, necesarias en el Proyecto Político Pedagógico (PPP. Se reconocen los valores de la propuesta del perfil de egresos de las DCN en la formación del enfermero, pero, se

Geochemical methods for identification of formations being prospective for uranium

International Nuclear Information System (INIS)

Zhukova, A.M.; Komarova, N.I.; Spiridonov, A.A.; Shor, G.M.

1985-01-01

Geochemical methods of uranium content evaluation in metamorphic, ultrametamorphic and sedimentary formations are considered. At that, the following four factors are of the highest importance: 1) average uranium content-geochemical background; 2) character of uranium distribution; 3) forms of uranium presence; 4) the value of thorium-uranium ratio. A complex of radiogeochemical criteria, favourable for uranium presence is formulated: high average background content of total and '' mobile''uranium and high value of variation coefficient (80-100% and above); low (approximately one or lower) thorium-uranium ratio; sharp increase in uranium concentration in accessory minerals. Radiogeochemical peculiarities of metamorphic and ultrametamorphic formations prospective for uranium are enumerated. The peculiarities condition specificity of geochemical prospecting methods. Prospecting methods first of all must be directed at the evaluation of radioelement distribution parameters and specification of the forms of their presence

Semi-detailed uranium geochemical survey in Northwestern Samar (27 March 1979 - 4 July 1979)

International Nuclear Information System (INIS)

Santos, G. Jr.; Ogena, M.; Tauli, G.

1980-04-01

A uranium geochemical survey was conducted to delineate in detail the uranium prospective area(s) in northwestern Samar. A total of 805 stream sediments and 1.115 water samples were obtained from the target areas from uranium analysis. Geochemical anomalies were indicated in San Isidro and Mauo. Geochemical correlations between uranium and trace elements (Pb, Ag, Ni, Cu, Co, Zn and Mn) were generally poor. (ELC)

Geochemical Data Package for Performance Assessment Calculations Related to the Savannah River Site

Energy Technology Data Exchange (ETDEWEB)

Kaplan, Daniel I. [Savannah River Site (SRS), Aiken, SC (United States). Savannah River National Lab. (SRNL)

2016-07-22

The Savannah River Site (SRS) disposes of low-level radioactive waste (LLW) and stabilizes high-level radioactive waste (HLW) tanks in the subsurface environment. Calculations used to establish the radiological limits of these facilities are referred to as Performance Assessments (PA), Special Analyses (SA), and Composite Analyses (CA). The objective of this document is to revise existing geochemical input values used for these calculations. This work builds on earlier compilations of geochemical data (2007, 2010), referred to a geochemical data packages. This work is being conducted as part of the on-going maintenance program of the SRS PA programs that periodically updates calculations and data packages when new information becomes available. Because application of values without full understanding of their original purpose may lead to misuse, this document also provides the geochemical conceptual model, the approach used for selecting the values, the justification for selecting data, and the assumptions made to assure that the conceptual and numerical geochemical models are reasonably conservative (i.e., bias the recommended input values to reflect conditions that will tend to predict the maximum risk to the hypothetical recipient). This document provides 1088 input parameters for geochemical parameters describing transport processes for 64 elements (>740 radioisotopes) potentially occurring within eight subsurface disposal or tank closure areas: Slit Trenches (ST), Engineered Trenches (ET), Low Activity Waste Vault (LAWV), Intermediate Level (ILV) Vaults, Naval Reactor Component Disposal Areas (NRCDA), Components-in-Grout (CIG) Trenches, Saltstone Facility, and Closed Liquid Waste Tanks. The geochemical parameters described here are the distribution coefficient, Kd value, apparent solubility concentration, k_s value, and the cementitious leachate impact factor.

Geochemical and geochronological constrains on the Chiang Khong volcanic rocks (northwestern Thailand) and its tectonic implications

Science.gov (United States)

Qian, Xin; Feng, Qinglai; Chonglakmani, Chongpan; Monjai, Denchok

2013-12-01

Volcanic rocks in northwestern Thailand exposed dominantly in the Chiang Khong area, are commonly considered to be genetically linked to the tectonic evolution of the Paleo-Tethyan Ocean. The volcanic rocks consist mainly of andesitic to rhyolitic rocks and are traditionally mapped as Permian-Triassic sequences. Our zircon U-Pb geochronological results show that two andesitic samples (TL-1-B and TL-31-B), are representative of the Doi Yao volcanic zone, and give a mean weighted age of 241.2±4.6 Ma and 241.7±2.9 Ma, respectively. The rhyolitic sample (TL-32-B1) from the Doi Khun Ta Khuan volcanic zone erupted at 238.3±3.8 Ma. Such ages indicate that Chiang Khong volcanic rocks erputed during the early Middle Triassic period. Seven samples from the Doi Yao and Doi Khun Ta Khuan zones exhibit an affinity to arc volcanics. Three rhyolitic samples from the Chiang Khong area have a geochemical affinity to both arc and syn-collisional volcanic rocks. The Chiang Khong arc volcanic rocks can be geochemically compared with those in the Lampang area in northern Thailand, also consistent with those in Jinghong area of southwestern Yunnan. This indicates that the Chiang Rai arc-volcanic zone might northwardly link to the Lancangjiang volcanic zone in southwestern China.

Perfil de la Arquitectura de la Gestion del Conocimiento en Empresas Manufactureras.

OpenAIRE

Gómez Hernández, Marian; Rodríguez Monroy, Carlos; Guaita, Wilfredo

2009-01-01

La investigación tuvo como propósito determinar el perfil de la arquitectura de la GC en empresas manufactureras, tomando como referencia las variables asociadas al conocimiento organizacional en las etapas: creación; identificación y adquisición; clasificación, almacenamiento y protección; aplicación y actualización; transferencia y medición. Soportado por cuatro pilares correspondiente a la plataforma interna: cultura y liderazgo, memorias corporativas, TIC, comunidades colaborativas ...

Perfil de adolescentes gestantes de um município do interior do Paraná

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Beatriz Rosana Gonçalves de Oliveira

2011-01-01

Full Text Available Este estudio planteó como objetivo identificar el perfil de adolescentes embarazadas, en un municipio de Paraná, teniendo en cuenta la influencia de factores biológicos, psicológicos y sociales, para apoyar las acciones preventivas del embarazo precoz. Investigación cuantitativa con datos obtenidos mediante entrevista. y análisis estadístico descriptivo. Se analizaron: edad de la menarqula, ginecológica y al quedar embarazada, uso de anticonceptivos antes del embarazo, relación familiar, aceptación y planificación del embarazo, nivel educativo, repetición y abandono escolar, renta. familiar, estado civil, número de compañeros hasta el embarazo y medios de acceso a educación sexual. El perfil obtenido mostró menarquia precoz, sólo una pareja sexual, poco uso de anticonceptivos, reacción familiar positiva en relación al embarazo actual, repetición y abandono escolar, falta de empleo remunerado, baja renta familiar. Los datos aportan informaciones al equipo de salud del municipio en cuestión para que desarrolle acciones específicas que prevengan el embarazo en la adolescencia.

Geochemical fingerprints and pebbles zircon geochronology

Indian Academy of Sciences (India)

Home; Journals; Journal of Earth System Science; Volume 125; Issue 7. Geochemical fingerprints and pebbles zircon geochronology: Implications for the provenance and tectonic setting of Lower Cretaceous sediments in the Zhucheng Basin (Jiaodong peninsula, North China). Jin-Long Ni Jun-Lai Liu Xiao-Ling Tang ...

Geochemical alteration vs mechanical weathering on stability of unstable slope : Case of the deep seated landslide of Séchilienne (Isère, France)

Science.gov (United States)

Bertrand, Catherine; Nevers, Pierre; Gaillardet, Jérôme; Dubois, Laurent

2017-04-01

, GNSS and at distance by a terrestrial radar and a total station. A hydrogeochemical monitoring of the non-saturated zone in a fractured hard rock is established since 2010 on the site. This monitoring leaded by the French Landslide Observatory (OMIV) consists of continuous measurements of physical parameters (Temp. EC. Flow rate) on two groundwater outlets and weekly samplings of the waters for quality monitoring Hydrochemical studies allows a sufficient resolution to detect exchange between compartments of contrasted permeability within fractured aquifers. They enabled to determine the influence of the hydrodynamic conditions variations at the aquifer scale, on exchange modalities between the pervious zone and the less pervious zone, and to highlight that permeability variations on mechanical stress effect may induce variations of the chemical signal of a fractured aquifer. Geochemical alteration represents a significant contribution compared to mechanical weathering on the long term (multiannual evolution by mechanical and geochemical damage of the fractures and the rock matrix), to the medium and short-term (seasonal and instantaneous effect of hydro-mechanical fluctuations located in the fractures of the slope) evolution of the rock slope failures. The reconstitution of the chemical evolutions of water and minerals during the transit of water through the rock, might allow establishing local erosion balance In addition it might also allow to locate and to quantify at the scale of a rock slope, the chemical erosion able to induce "chemical tiredness" of the rock.

Geochemical, hydrological, and biological cycling of energy residual. Research plan

International Nuclear Information System (INIS)

Wobber, F.J.

1983-03-01

Proposed research goals and specific research areas designed to provide a base of fundamental scientific information so that the geochemical, hydrological, and biophysical mechanisms that contribute to the transport and long term fate of energy residuals in natural systems can be understood are described. Energy development and production have resulted in a need for advanced scientific information on the geochemical transformations, transport rates, and potential for bioaccumulation of contaminants in subsurface environments

Porosity Development in a Coastal Setting: A Reactive Transport Model to Assess the Influence of Heterogeneity of Hydrological, Geochemical and Lithological Conditions

Science.gov (United States)

Maqueda, A.; Renard, P.; Cornaton, F. J.

2014-12-01

Coastal karst networks are formed by mineral dissolution, mainly calcite, in the freshwater-saltwater mixing zone. The problem has been approached first by studying the kinetics of calcite dissolution and then coupling ion-pairing software with flow and mass transport models. Porosity development models require high computational power. A workaround to reduce computational complexity is to assume the calcite dissolution reaction is relatively fast, thus equilibrium chemistry can be used to model it (Sanford & Konikow, 1989). Later developments allowed the full coupling of kinetics and transport in a model. However kinetics effects of calcite dissolution were found negligible under the single set of assumed hydrological and geochemical boundary conditions. A model is implemented with the coupling of FeFlow software as the flow & transport module and PHREEQC4FEFLOW (Wissmeier, 2013) ion-pairing module. The model is used to assess the influence of heterogeneities in hydrological, geochemical and lithological boundary conditions on porosity evolution. The hydrologic conditions present in the karst aquifer of Quintana Roo coast in Mexico are used as a guide for generating inputs for simulations.

Análisis Exploratorio Del Perfil Demandado Para Administración Y Dirección De Empresas: Implicaciones Para El Área Contable

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José Luis Arquero-Montaño

2009-07-01

Los resultados determinan la importancia concedida por los egresados a los diferentes contenidos y habilidades que conforman el perfil profesional e indican el nivel de formación proporcionado en cada uno de ellos. A partir de estos resultados se identifican las actuaciones prioritarias. Respecto a los contenidos de contabilidad y finanzas, los principales resultados indican que los egresados consideran que son esenciales dentro del perfil, que son impartidos a un nivel adecuado y que no deberían reducir su peso en los nuevos planes de estudios.

Adakite-like volcanism of Ecuador: lower crust magmatic evolution and recycling

Science.gov (United States)

Chiaradia, Massimo; Müntener, Othmar; Beate, Bernardo; Fontignie, Denis

2009-11-01

In the Northern Andes of Ecuador, a broad Quaternary volcanic arc with significant across-arc geochemical changes sits upon continental crust consisting of accreted oceanic and continental terranes. Quaternary volcanic centers occur, from west to east, along the Western Cordillera (frontal arc), in the Inter-Andean Depression and along the Eastern Cordillera (main arc), and in the Sub-Andean Zone (back-arc). The adakite-like signatures of the frontal and main arc volcanoes have been interpreted either as the result of slab melting plus subsequent slab melt-mantle interactions or of lower crustal melting, fractional crystallization, and assimilation processes. In this paper, we present petrographic, geochemical, and isotopic (Sr, Nd, Pb) data on dominantly andesitic to dacitic volcanic rocks as well as crustal xenolith and cumulate samples from five volcanic centers (Pululagua, Pichincha, Ilalo, Chacana, Sumaco) forming a NW-SE transect at about 0° latitude and encompassing the frontal (Pululagua, Pichincha), main (Ilalo, Chacana), and back-arc (Sumaco) chains. All rocks display typical subduction-related geochemical signatures, such as Nb and Ta negative anomalies and LILE enrichment. They show a relative depletion of fluid-mobile elements and a general increase in incompatible elements from the front to the back-arc suggesting derivation from progressively lower degrees of partial melting of the mantle wedge induced by decreasing amounts of fluids released from the slab. We observe widespread petrographic evidence of interaction of primary melts with mafic xenoliths as well as with clinopyroxene- and/or amphibole-bearing cumulates and of magma mixing at all frontal and main arc volcanic centers. Within each volcanic center, rocks display correlations between evolution indices and radiogenic isotopes, although absolute variations of radiogenic isotopes are small and their values are overall rather primitive (e.g., ɛNd = +1.5 to +6, 87Sr/86Sr = 0

Ejection of iron-bearing giant-impact fragments and the dynamical and geochemical influence of the fragment re-accretion

Science.gov (United States)

Genda, Hidenori; Iizuka, Tsuyoshi; Sasaki, Takanori; Ueno, Yuichiro; Ikoma, Masahiro

2017-07-01

The Earth was born in violence. Many giant collisions of protoplanets are thought to have occurred during the terrestrial planet formation. Here we investigated the giant impact stage by using a hybrid code that consistently deals with the orbital evolution of protoplanets around the Sun and the details of processes during giant impacts between two protoplanets. A significant amount of materials (up to several tens of percent of the total mass of the protoplanets) is ejected by giant impacts. We call these ejected fragments the giant-impact fragments (GIFs). In some of the erosive hit-and-run and high-velocity collisions, metallic iron is also ejected, which comes from the colliding protoplanets' cores. From ten numerical simulations for the giant impact stage, we found that the mass fraction of metallic iron in GIFs ranges from ∼1 wt% to ∼25 wt%. We also discussed the effects of the GIFs on the dynamical and geochemical characteristics of formed terrestrial planets. We found that the GIFs have the potential to solve the following dynamical and geochemical conflicts: (1) The Earth, currently in a near circular orbit, is likely to have had a highly eccentric orbit during the giant impact stage. The GIFs are large enough in total mass to lower the eccentricity of the Earth to its current value via their dynamical friction. (2) The concentrations of highly siderophile elements (HSEs) in the Earth's mantle are greater than what was predicted experimentally. Re-accretion of the iron-bearing GIFs onto the Earth can contribute to the excess of HSEs. In addition, Iron-bearing GIFs provide significant reducing agent that could transform primitive CO2-H2O atmosphere and ocean into more reducing H2-bearing atmosphere. Thus, GIFs are important for the origin of Earth's life and its early evolution.

Ground water chemistry and geochemical modeling of water-rock interactions at the Osamu Utsumi mine and the Morro do Ferro analogue study sites, Poços de Caldas, Minas Gerais, Brazil

Science.gov (United States)

Nordstrom, D. Kirk; McNutt, R.H.; Puigdomenech, I.; Smellie, John A.T.; Wolf, M.

1992-01-01

Surface and ground waters, collected over a period of three years from the Osamu Utsumi uranium mine and the Morro do Ferro thorium/rare-earth element (Th/REE) deposits, were analyzed and interpreted to identify the major hydrogeochemical processes. These results provided information on the current geochemical evolution of ground waters for two study sites within the Poços de Caldas Natural Analogue Project.

Relevancia del aprendizaje cooperativo sobre los diferentes perfiles de la dinámica bullying: un análisis mediante pruebas de tamaño del efecto

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Benito León del Barco

2016-01-01

Full Text Available Esta investigación pretende determinar sobre qué perfil de la dinámica bullying (Agresor, Victima, Observador es más relevante una intervención en aprendizaje cooperativo. Mediante pruebas estadísticas de tamaño del efecto. Con el fin de evaluar las conductas de acoso se diseño un instrumento para evaluar el acoso escolar entre Iguales desde la perspectivas del "Agresor, Víctima y Observador". Se trabajó con dos grupos de participantes de 3er ciclo de primaria, un primer grupo de 311 alumnos que utilizamos para el análisis psicométrico del instrumento y un segundo grupo de 110 alumnos para la intervención. Los resultados manifiestan que el tamaño del efecto intergrupo ha sido elevado para el factor de exclusión social para los perfiles observador (d =0.64 y agresor (d =0.65. También, obtiene un tamaño elevado el factor agresiones verbales y físicas directas para el perfil observador (d =0.57. En síntesis, tras el análisis del tamaño del efecto podemos afirmar que el aprendizaje cooperativo es eficaz sobre el perfil agresor y, especialmente, sobre el observador.

Acceptance of the 2014 Geochemical Society Distinguished Service Award by Carla Koretsky

Science.gov (United States)

Koretsky, Carla

2015-06-01

I am deeply touched to have received the Geochemical Society Distinguished Service Award. It was a great surprise when I received the notice that I had been chosen for the award. It has been a tremendous pleasure to work on behalf of student members of the Geochemical Society, Japanese Geochemical Society and the European Association of Geochemists to organize the student travel grants over the past few years. Certainly, this is not an effort that I undertook on my own. Many, many members of the GS, the JGS and the EAG generously donated their time and expertise to serve as reviewers for the many travel grant applicants we receive each year. Seth Davis, the GS Chief Operating Officer, spent countless hours helping to organize applications, the website, distribution of funds and many other aspects of the competition. Without Seth and the many expert reviewers, we could not run the travel grant program each year and provide this important financial support to allow more students to experience the Goldschmidt Conference. I also enjoyed my time as Geochemical News co-editor, and I should point out that GN during those years was ably co-edited by Johnson Haas. It has been a pleasure to see Elements take off, and GN evolve into a timely source of important announcements and information about cutting-edge science since I stepped down as co-editor. I feel very fortunate to work with so many outstanding colleagues in the global geochemical community, and I am a little embarrassed, and also very grateful, to have been selected for the Geochemical Society Distinguished Service Award. Thank you!

Uranium exploration data and global geochemical baselines: The need for co-ordinated action

International Nuclear Information System (INIS)

Darnley, A.G.

1997-01-01

Public concern about environmental problems continues. In order to assess the magnitude of potential problems it is necessary to have comprehensive information. The absence of quantitative geochemical data to map the surface composition of the earth is one of the major information gaps in present day environmental science. An IAEA Technical Committee meeting held in November 1993 reviewed the uses of uranium exploration data for environmental purposes. Most attention was focussed on data involving radiation measurements. Uranium exploration programmes conducted since 1970 in many countries collected a considerable amount of geochemical survey data, providing information about the distribution of non-radioactive elements in the natural environment. Canada is one of several countries where such data provided the foundation for national geochemical mapping; other countries could benefit from similar actions. Increasing importance is being attached by governments to the need to enact effective environmental legislation concerning ''safe levels'' of many chemical substances. Such legislation requires geochemical variations in the natural environment. It is becoming necessary to make quantitative comparisons of element abundances across national boundaries, and from continent to continent. In 1995 the IAEA, with other organizations, supported UNESCO to publish a report concerned with the establishment of a Global Geochemical Reference Network. This is designed to provide a framework to connect all types of geochemical survey, to move towards international compatibility of data. The report contains recommendations relating to the standardization of field and laboratory methods; the use of the most sensitive analytical techniques; and standardization of data management. Ground and airborne gamma ray spectrometry, and nuclear laboratory techniques are all discussed. Following the publication of the report, the International Union of Geological Sciences has now established a

Statistical treatment of geochemical data and its application in the geologic mapping and in the definition of the geochemical anomalies in the Alvo 2-Corpo 4 -Provincia Mineral de Carajas

International Nuclear Information System (INIS)

Moura, C.A.V.

1982-01-01

It was given a statistical treatment for the geochemical data about soil in the are named Alvo2 - Corpo4- in the Provincia Mineral de Carajas, Para, Brazil, for application of the geological mapping and definition of geochemical anomalies. (A.B.) [pt

Chlorine isotopes potential as geo-chemical tracers

Digital Repository Service at National Institute of Oceanography (India)

Shirodkar, P.V.; Pradhan, U.K.; Banerjee, R.

The potential of chlorine isotopes as tracers of geo-chemical processes of earth and the oceans is highlighted based on systematic studies carried out in understanding the chlorine isotope fractionation mechanism, its constancy in seawater and its...

Geochemical typification of kimberlite and related rocks of the North Anabar region, Yakutia

Science.gov (United States)

Kargin, A. V.; Golubeva, Yu. Yu.

2017-11-01

The results of geochemical typification of kimberlites and related rocks (alneites and carbonatites) of the North Anabar region are presented with consideration of the geochemical specification of their source and estimation of their potential for diamonds. The content of representative trace elements indicates the predominant contribution of an asthenospheric component (kimberlites and carbonatites) in their source, with a subordinate contribution of vein metasomatic formations containing Cr-diopside and ilmenite. A significant contribution of water-bearing potassium metasomatic parageneses is not recognized. According to the complex of geochemical data, the studied rocks are not industrially diamondiferous.

NEW GEOCHEMICAL DATA OF BASALTS IN THE TSOROIDOG AREA, CENTRAL MONGOLIA

Directory of Open Access Journals (Sweden)

T. Oyunchimeg

2017-01-01

Full Text Available At present, geochemical data are widely used for reconstructing geodynamic settings, especially, volcanic rocks of mafic composition, i.e., basalts, because they are widespread in many orogenic belts and are indicative of different geodynamic environments. In general, we propose the reconstruction of the tectonic settings of basalts according to their relationships with associated ocean plate stratigraphy (OPS sediments, their petrogenesis and their geochemical features.

Application of radio-geochemical exploration to investigation on geo-ecological environment

International Nuclear Information System (INIS)

Ye Qingsen

2000-01-01

Taking investigation on radon hazards and natural radioactivity as examples, the author expounds the prospects of the application of radio-geochemical exploration to the investigation on geo-ecological environment. It is especially emphasized that the methods of radio-geochemical exploration can not be only widely applied in the field of traditional radio-geological prospecting but also play an important role in the investigation on geo-ecological environment

Perfil Logístico de Colombia – Sector textil y confecciones

OpenAIRE

Gomez Diaz, Stephania; Porras Rodriguez, Julian Felipe

2014-01-01

El sector textil en los últimos 10 años se ha caracterizado por pertenecer a uno de los rubros superiores frente a la economía nacional por lo cual actualmente se está enfrentando a economías emergentes como la china y a mercados como el americano con costos muchos más competentes. Este proyecto, describirá de manera específica el perfil logístico del sector textil en Colombia, el cual debido al auge que ha tenido en los últimos años es importante destacar la relevancia de la logística pa...

Perfil fitness en un grupo de estudiantes universitarios: Boyacá 2014

Directory of Open Access Journals (Sweden)

Yessica Ivonne Pérez Lemus

2016-04-01

Full Text Available Introducción: La práctica de actividad física reduce el riesgo y previene enfermedades no trasmisibles, mejora la salud ósea y funcional, mantiene el equilibrio calórico y el control del peso, mejorando no sólo la condición física o perfil fitness, el cual se ve reflejado en la habilidad para llevar a cabo las tareas diarias con vigor y sin fatiga; en relación con la salud. Objetivo: Determinar el perfil fitness de estudiantes universitarios en el departamento de Boyacá. Metodología: Estudio descriptivo con diseño transversal, el cual contó con una población de 204 universitarios, de los cuales se obtuvo una muestra de 40 con el uso del software Epidat®, con una confiabilidad del 95% y error estimado del 5%, el muestreo fue estratificado con afijación proporcional. Se evaluaron los componentes fitness relacionados con la salud: capacidad aeróbica, fuerza muscular, flexibilidad y composición corporal. Se obtuvieron medidas de tendencia central, frecuencia y se aplicaron pruebas de asociación como Chi cuadrado, Pearson, Spearman y U de Mann-Whitney. Resultados: La edad promedio de la población fue 21,13 años (DS 2,79, el 67,5% se clasifico según Índice de masa corporal en normopeso, el 35% se ubicó en el rango obeso según su porcentaje graso, la fuerza muscular promedio para prensión manual fue de 30,02 Kilogramos (DS 12,85, miembros inferiores 70,48 Kilogramos (DS 40,88 y tronco 69,6 kilogramos (DS 38,5. El 85% de las mujeres y el 81,8% de los hombres en la evaluación de la capacidad aeróbica se clasificaron en el rango muy pobre. Se reportan asociaciones estadísticamente significativas entre la capacidad aeróbica y el género (p 0.00, la fuerza de tronco, miembro superior e inferior con el género con (p 0.003, (p 0,04 y (p 0,038 respectivamente. Conclusiones: La condición física o perfil fitness no es adecuado para la edad de los participantes teniendo en cuanta los bajos niveles de la fuerza muscular y la

AVALIAÇÃO DO PERFIL LIPÍDICO SANGUÍNEO DE ATLETAS CORREDORES NO ENSAIO ERGOESPIROMÉTRICO DE BRUCE UTILIZANDO ESPECTROSCOPIA NO INFRAVERMELHO

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Francielle Pasqualotti Meinhardt

2011-08-01

Full Text Available Os constituintes do perfil lipídico são importantes marcadores bioquímicos de doenças cardiovasculares (grande causa de morbidade e mortalidade. Para um diagnóstico de alterações do perfil lipídico se apresenta o método da espectroscopia no infravermelho (FT-IR. Este estudo avalia a aplicação da FT-IR na obtenção de dados do perfil lipídico de atletas corredores. Trata-se de um estudo analítico observacional comparativo, tendo como método de referência os ensaios enzimáticos baseados na reação de Trinder, comparados à espectroscopia no infravermelho por reflectância difusa com Transformada de Fourier (DRIFTS, com auxílio das ferramentas quimiométricas de análise exploratória por agrupamento hierárquico (HCA e análise preditiva por mínimos quadrados parciais (PLS para previsão destes marcadores bioquímicos. Foram sujeitos 14 atletas da equipe de Atletismo da UNISC, de 18 a 30 anos, de ambos os sexos, avaliados em repouso e após o teste ergoespirométrico de Bruce. Os resultados apontam que, na avaliação de atletas, a técnica de infravermelho (DRIFTS juntamente com o PLS, foi adequada para a construção de modelos de calibração e na definição da correlação entre testes bioquímicos padrões no perfil lipídico e na determinação pelo infravermelho.

Geochemical Parameters Required from the SKB Site Characterisation Programme

International Nuclear Information System (INIS)

Bath, Adrian

2002-01-01

SKB has described its approach to site characterisation in a number of Technical Reports. One of the scientific topics in which specific information requirements and priorities are set out is geochemistry. This report for SKI examines critically whether the geochemical parameters identified in the SKB programme documents will be adequate for safety and regulatory requirements. It also examines some of the details of parameter requirements and interpretation tools that will be necessary to convert site investigation data into knowledge about chemical conditions and groundwater movements. The SKB strategy for geochemical data focuses on a small number of 'suitability indicators', primarily dissolved oxygen, pH and salinity. Their parameter requirements aim to assess those primary characteristics, as well as to acquire a wider range of data that will support those assessments and provide a broader understanding of candidate areas. An initial observation in this review that, though it is a primary suitability indicator, dissolved oxygen apparently will not be measured and instead will be inferred from other redox indicators. This raises a number of issues about sampling and monitoring measures, analytical data reliability and sensitivity, and the degree of confidence in geochemical understanding. A geochemical programme involves reconnaissance by desk study and acquisition of new data at levels of details that are appropriate to the stage of site investigations. As early as possible, a conceptual model of a candidate area should help to define the objectives of geochemical measurements on both rock and groundwater samples. It is recommended that parameters requirements should be defined and considered not only in terms of isolated measurements but more in terms of addressing broader objectives that relate to safety and also to geoscientific understanding. The safety priorities remain (e.g. dissolved oxygen) but will then be supported by an understanding of processes

Geochemical Parameters Required from the SKB Site Characterisation Programme

Energy Technology Data Exchange (ETDEWEB)

Bath, Adrian [Intellisci Ltd., Loughborough (United Kingdom)

2002-01-01

SKB has described its approach to site characterisation in a number of Technical Reports. One of the scientific topics in which specific information requirements and priorities are set out is geochemistry. This report for SKI examines critically whether the geochemical parameters identified in the SKB programme documents will be adequate for safety and regulatory requirements. It also examines some of the details of parameter requirements and interpretation tools that will be necessary to convert site investigation data into knowledge about chemical conditions and groundwater movements. The SKB strategy for geochemical data focuses on a small number of 'suitability indicators', primarily dissolved oxygen, pH and salinity. Their parameter requirements aim to assess those primary characteristics, as well as to acquire a wider range of data that will support those assessments and provide a broader understanding of candidate areas. An initial observation in this review that, though it is a primary suitability indicator, dissolved oxygen apparently will not be measured and instead will be inferred from other redox indicators. This raises a number of issues about sampling and monitoring measures, analytical data reliability and sensitivity, and the degree of confidence in geochemical understanding. A geochemical programme involves reconnaissance by desk study and acquisition of new data at levels of details that are appropriate to the stage of site investigations. As early as possible, a conceptual model of a candidate area should help to define the objectives of geochemical measurements on both rock and groundwater samples. It is recommended that parameters requirements should be defined and considered not only in terms of isolated measurements but more in terms of addressing broader objectives that relate to safety and also to geoscientific understanding. The safety priorities remain (e.g. dissolved oxygen) but will then be supported by an understanding of

Ionizing radiation and radionuclides in the environment: sources, origin, geochemical processes and health risks

International Nuclear Information System (INIS)

Dangic, A.

1995-01-01

Ionizing radiation related to the radioactivity and radionuclides appears to be ones of most dangerous environmental risks to the human health. The paper considers appearance and importance of radionuclides, both natural (cosmogenic and Earth's) and anthropogenic, mode of their entering into and movement through the environment. Most risk to the population are radionuclides related to the geological-geochemical systems - in Serbia, high concentrations of radionuclides related to these sources were indicated at a number of localities. Movement of radionuclides through the environment is regulated by the geochemical processes i.e. the geochemical cycles of the elements. For the discovering of radionuclides in the nature, the assessment of the health risks to the population and the related protection are necessary multilayer geochemical studies. (author)

Late Paleozoic-Early Mesozoic tectonic evolution of the Paleo-Asian Ocean: geochronological and geochemical evidence from granitoids in the northern margin of Alxa, Western China

Science.gov (United States)

Sha, Xin; Wang, Jinrong; Chen, Wanfeng; Liu, Zheng; Zhai, Xinwei; Ma, Jinlong; Wang, Shuhua

2018-03-01

The Paleo-Asian Ocean (Southern Mongolian Ocean) ophiolitic belts and massive granitoids are exposed in the Alxa block, in response to oceanic subduction processes. In this work, we report petrographic, geochemical, and zircon U-Pb age data of some granitoid intrusions from the northern Alxa. Zircon U-Pb dating for the quartz diorite, tonalite, monzogranite, and biotite granite yielded weighted mean 206Pb/238U ages of 302±9.2 Ma, 246.5±4.6 Ma, 235±4.4 Ma, and 229.5±5.6 Ma, respectively. The quartz diorites ( 302 Ma) exhibit geochemical similarities to adakites, likely derived from partial melting of the initially subducted Chaganchulu back-arc oceanic slab. The tonalites ( 246.5 Ma) display geochemical affinities of I-type granites. They were probably derived by fractional crystallization of the modified lithospheric mantle-derived basaltic magmas in a volcanic arc setting. The monzogranites ( 235 Ma) are characterized by low Al2O3, but high Y and Yb with notably negative Eu anomalies. In contrast, the biotite granites ( 229.5 Ma) show high Al2O3 but low Y and Yb with steep HREE patterns and the absence of negative Eu anomalies. Elemental data suggested that the biotite granites were likely derived from a thickened lower crust, but the monzogranites originated from a thin crust. Our data suggested that the initial subduction of the Chaganchulu oceanic slab towards the Alxa block occurred at 302 Ma. This subduction process continued to the Early Triassic ( 246 Ma) and the basin was finally closed before the Middle Triassic ( 235 Ma). Subsequently, the break-off of the subducted slab triggered asthenosphere upwelling (240-230 Ma).

Geochemical soil sampling for deeply-buried mineralized breccia pipes, northwestern Arizona

Science.gov (United States)

Wenrich, K.J.; Aumente-Modreski, R. M.

1994-01-01

Thousands of solution-collapse breccia pipes crop out in the canyons and on the plateaus of northwestern Arizona; some host high-grade uranium deposits. The mineralized pipes are enriched in Ag, As, Ba, Co, Cu, Mo, Ni, Pb, Sb, Se, V and Zn. These breccia pipes formed as sedimentary strata collapsed into solution caverns within the underlying Mississippian Redwall Limestone. A typical pipe is approximately 100 m (300 ft) in diameter and extends upward from the Redwall Limestone as much as 1000 m (3000 ft). Unmineralized gypsum and limestone collapses rooted in the Lower Permian Kaibab Limestone or Toroweap Formation also occur throughout this area. Hence, development of geochemical tools that can distinguish these unmineralized collapse structures, as well as unmineralized breccia pipes, from mineralized breccia pipes could significantly reduce drilling costs for these orebodies commonly buried 300-360 m (1000-1200 ft) below the plateau surface. Design and interpretation of soil sampling surveys over breccia pipes are plagued with several complications. (1) The plateau-capping Kaibab Limestone and Moenkopi Formation are made up of diverse lithologies. Thus, because different breccia pipes are capped by different lithologies, each pipe needs to be treated as a separate geochemical survey with its own background samples. (2) Ascertaining true background is difficult because of uncertainties in locations of poorly-exposed collapse cones and ring fracture zones that surround the pipes. Soil geochemical surveys were completed on 50 collapse structures, three of which are known mineralized breccia pipes. Each collapse structure was treated as an independent geochemical survey. Geochemical data from each collapse feature were plotted on single-element geochemical maps and processed by multivariate factor analysis. To contrast the results between geochemical surveys (collapse structures), a means of quantifying the anomalousness of elements at each site was developed. This

Perfiles de adolescentes on line y su comportamiento en el medio interactivo

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Belinda de Frutos Torres

2014-01-01

Full Text Available Normal 0 21 false false false ES X-NONE X-NONE  Internet se ha convertido en el medio de referencia entre los jóvenes y su uso está muy extendido se pueden identificar perfiles de usuarios respecto a la actitud hacia el medio interactivo y su estilo de navegación. El objetivo del estudio se centra en identificar dicho perfiles y poner a prueba su relación con su comportamiento en Internet. El estudio utiliza una metodología correlacional, con una muestra de conveniencia formada por 320 jóvenes entre 14 y 19 años procedentes de varios centros de educación secundaria. Los resultados muestran que se pueden identificar varios patrones de los adolescentes en el consumo de medios interactivos en función de su estilo de navegación y actitud hacia el medio. El estilo de navegación exploratorio está asociado a participar en actividades comerciales de la red y a dedicar más tiempo al medio interactivo particularmente durante la semana. Así mismo, los jóvenes que se enfrentan al medio con una actitud más confiada y ven el medio como un vehículo de socialización y éxito social también dedican más tiempo al medio interactivo y participan en mayor medida de las propuestas publicitarias que se ofrecen en Internet.  

Perfil del viajero internacional: el trabajo como motivo de viaje

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M.ª Belén Robles García

Full Text Available Objetivos: describir la población a estudio y comparar el motivo de viaje laboral con el motivo turístico y con la Visita de Amigos o Familiares (VFRs para estimar si existe un perfil de riesgo diferente. Metodología: estudio de las variables edad, género, duración, motivo, destino y recomendación de quimioprofilaxis en viajeros que acuden al Centro de Atención Pre-viaje Internacional de Asturias (España entre 2008 y 2016. Un total de 9. 527 (89,83% viajeros cumplieron el criterio de inclusión (edad >18 años. Resultados: en 2013 el motivo laboral constituyó el 43,85% de todas las causas de viaje internacional. La mayoría de los trabajadores (70,89% fueron hombres (p=0,00, más jóvenes que los turistas (38 vs 40 años; p=0,00 o que los VFRs (38 vs 39 años; p=0,03. Además, los trabajadores viajaban durante más tiempo que los turistas (91 vs 23 días; p=0,00 o que los VFRs (91 vs 50 días; p=0,00. África Subsahariana fue la región más visitada por el motivo profesional (35,89%. Se recomendó quimioprofilaxis en 39,19% trabajadores vs 38,72% turistas más VFRs (p=0,68. Los desplazamientos laborales internacionales por regiones no mostraron diferencia respecto a la recomendación de quimioprofilaxis vs turistas y VFRs. Conclusiones: en la población estudiada el motivo laboral de un viaje internacional tiene un perfil del viajero específico. Se deben desarrollar iniciativas de salud pública para prevenir riesgos concretos y promover el consejo sanitario individualizado.

ANÁLISIS DEL PERFIL DE COMPUESTOS VOLÁTILES DEL MANGO (Mangifera indica L. Var. Tommy Atkins) TRATADO POR MÉTODOS COMBINADOS

OpenAIRE

Angélica Moreno; David F. León; Germán A. Giraldo; Eunice Ríos

2010-01-01

Se evaluó el perfil de compuestos volátiles del mango (Mangifera indica L. Var. Tommy Atkins) al ser tratado con la combinación de los métodos de deshidratación osmótica con o sin pulso de vacío (DOPV y DO) y con secado por aire caliente o con vacío (SAC y VAC). El tiempo utilizado en la cinética del proceso de DO fue de 42 horas y la DOPV de 30 horas; en los procesos de secado, el SAC se realizó durante 24 horas y el VAC requirió 40 horas. En el perfil de compuestos volátiles del mango fresc...

Geophysical and geochemical techniques for exploration of hydrocarbons and minerals

International Nuclear Information System (INIS)

Sittig, M.

1980-01-01

The detailed descriptive information in this book is based on 389 US patents that deal with geophysical and geochemical techniques useful for the exploration of hydrocarbons and minerals. Where it was necessary to round out the complete technological picture, a few paragraphs from cited government reports have been included. These techniques are used in prospecting for oil, coal, oil shale, tar sand and minerals. The patents are grouped under the following chapters: geochemical prospecting; geobiological prospecting; geophysical exploration; magnetic geophysical prospecting; gravitational geophysical prospecting; electrical geophysical prospecting; nuclear geophysical prospecting; seismic geophysical prospecting; and exploratory well drilling. This book serves a double purpose in that it supplies detailed technical information and can be used as a guide to the US patent literature in this field. By indicating all the information that is significant, and eliminating legal jargon and juristic phraseology, this book presents an advanced, industrially oriented review of modern methods of geophysical and geochemical exploration techniques

The geochemical profile of Mn, Co, Cu and Fe in Kerteh Mangrove Forest, Terengganu

International Nuclear Information System (INIS)

Kamaruzzaman, B.Y.; Antotina, A.; Airiza, Z.; Syalindran, S.; Ong, M.C.

2007-01-01

The geochemical profile of Kerteh mangrove sediments was analyzed for the vertical and horizontal distribution. The 100 cm core sediment sample and 15 surface sediments samples were taken from the field. The geochemical elements of Mn, Co, Cu and Fe of the sediments were analyzed. Geochemical proxy of Mn, Co, Cu and Fe were analyzed by using Inductively Coupled Plasma-Mass Spectrometry (ICP-MS). The mean concentrations of Mn, Co, Cu and Fe for the vertical distribution were 210.18 μg/ g, 15.55 μg/ g, 43.65 μg/ g and 1.88 μg/ g respectively. on the other hand, the mean concentrations of the geochemical elements for horizontal distributions were 230.50 μg/ g for Mn, 17.57 μg/ g for Co, 43.381 μg/ g for Cu and 2.93 μg/ g for Fe. Enrichment factor and normalization was used to point out the level of pollution. The EF and the normalization indicated that all the geochemical elements were from the natural sources. (author)

Geochemical fingerprinting of ∼2.5 Ga forearc-arc-backarc related magmatic suites in the Bastar Craton, central India

Science.gov (United States)

Asthana, Deepanker; Kumar, Sirish; Vind, Aditya Kumar; Zehra, Fatima; Kumar, Harshavardhan; Pophare, Anil M.

2018-05-01

The Pitepani volcanic suite of the Dongargarh Supergroup, central India comprises of a calc-alkaline suite and a tholeiitic suite, respectively. The rare earth element (REE) patterns, mantle normalized plots and relict clinopyroxene chemistry of the Pitepani calc-alkaline suite are akin to high-Mg andesites (HMA) and reveal remarkable similarity to the Cenozoic Setouchi HMA from Japan. The Pitepani HMAs are geochemically correlated with similar rocks in the Kotri-Dongargarh mobile belt (KDMB) and in the mafic dykes of the Bastar Craton. The rationale behind lithogeochemical correlations are that sanukitic HMAs represent fore-arc volcanism over a very limited period of time, under abnormally high temperature conditions and are excellent regional and tectonic time markers. Furthermore, the tholeiitic suites that are temporally and spatially associated with the HMAs in the KDMB and in the mafic dykes of the Bastar Craton are classified into: (a) a continental back-arc suite that are depleted in incompatible elements, and (b) a continental arc suite that are more depleted in incompatible elements, respectively. The HMA suite, the continental back-arc and continental arc suites are lithogeochemically correlated in the KDMB and in the mafic dykes of the Bastar Craton. The three geochemically distinct Neoarchaean magmatic suites are temporally and spatially related to each other and to an active continental margin. The identification of three active continental margin magmatic suites for the first time, provides a robust conceptual framework to unravel the Neoarchaean geodynamic evolution of the Bastar Craton. We propose an active continental margin along the Neoarchaen KDMB with eastward subduction coupled with slab roll back or preferably, ridge-subduction along the Central Indian Tectonic Zone (CITZ) to account for the three distinct magmatic suites and the Neoarchean geodynamic evolution of the Bastar Craton.

El perfil profesional de los formadores de formación continua en España. [The professional profile of trainers working in continuous training in Spain].

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Mamaqi, Xhevrie

2011-04-01

Full Text Available The aim of this study is to analyze and describe the professional profile of trainers working in continuous training in Spain. For this purpose we have developed a structured questionnaire was applied in person to a sample of 606 instructors nationwide. The questionnaire has provided information on aspects such as the socio-occupational status of instructors, their degree of professionalism, and the importance of professional skills. The information gathered has been analyzed by multivariate methods to determine the dominant professional profiles. The quantitative analysis includes the Categorical of Principal Components Analysis (CATPCA to analyze the skills and capabilities of the trainer and cluster analysis in two stages to get the profiles. Four dominant profiles have been deduced by the cluster analysis. The occupational variables, professional experience profiles and competences/skills produce the major discrepancies between the four profiles. El objetivo de este trabajo es analizar y describir los perfiles profesionales del formador de formación continua en España. Con este propósito se ha elaborado un cuestionario estructurado que se ha aplicado de forma presencial a una muestra de 606 formadores a nivel nacional. El cuestionario ha proporcionado información sobre aspectos como el estatus socio-laboral del formador, el grado de profesionalización y la importancia de las competencias profesionales de los formadores. La información recabada ha sido analizada mediante métodos multivariantes para determinar los perfiles profesionales dominantes. El análisis cuantitativo incluye el Análisis de Componentes Principales Categóricos (CATPCA para analizar las competencias y capacidades del formador y el análisis Cluster en Dos Fases para obtener los perfiles. De los resultados obtenidos se han deducido cuatro perfiles profesionales dominantes siendo las variables ocupacionales, experiencia profesional y de las capacidades las que mayor

A geochemical atlas of North Carolina, USA

Science.gov (United States)

Reid, J.C.

1993-01-01

A geochemical atlas of North Carolina, U.S.A., was prepared using National Uranium Resource Evaluation (NURE) stream-sediment data. Before termination of the NURE program, sampling of nearly the entire state (48,666 square miles of land area) was completed and geochemical analyses were obtained. The NURE data are applicable to mineral exploration, agriculture, waste disposal siting issues, health, and environmental studies. Applications in state government include resource surveys to assist mineral exploration by identifying geochemical anomalies and areas of mineralization. Agriculture seeks to identify areas with favorable (or unfavorable) conditions for plant growth, disease, and crop productivity. Trace elements such as cobalt, copper, chromium, iron, manganese, zinc, and molybdenum must be present within narrow ranges in soils for optimum growth and productivity. Trace elements as a contributing factor to disease are of concern to health professionals. Industry can use pH and conductivity data for water samples to site facilities which require specific water quality. The North Carolina NURE database consists of stream-sediment samples, groundwater samples, and stream-water analyses. The statewide database consists of 6,744 stream-sediment sites, 5,778 groundwater sample sites, and 295 stream-water sites. Neutron activation analyses were provided for U, Br, Cl, F, Mn, Na, Al, V, Dy in groundwater and stream water, and for U, Th, Hf, Ce, Fe, Mn, Na, Sc, Ti, V, Al, Dy, Eu, La, Sm, Yb, and Lu in stream sediments. Supplemental analyses by other techniques were reported on U (extractable), Ag, As, Ba, Be, Ca, Co, Cr, Cu, K, Li, Mg, Mo, Nb, Ni, P, Pb, Se, Sn, Sr, W, Y, and Zn for 4,619 stream-sediment samples. A small subset of 334 stream samples was analyzed for gold. The goal of the atlas was to make available the statewide NURE data with minimal interpretation to enable prospective users to modify and manipulate the data for their end use. The atlas provides only

Central Colorado Assessment Project (CCAP)-Geochemical data for rock, sediment, soil, and concentrate sample media

Science.gov (United States)

Granitto, Matthew; DeWitt, Ed H.; Klein, Terry L.

2010-01-01

This database was initiated, designed, and populated to collect and integrate geochemical data from central Colorado in order to facilitate geologic mapping, petrologic studies, mineral resource assessment, definition of geochemical baseline values and statistics, environmental impact assessment, and medical geology. The Microsoft Access database serves as a geochemical data warehouse in support of the Central Colorado Assessment Project (CCAP) and contains data tables describing historical and new quantitative and qualitative geochemical analyses determined by 70 analytical laboratory and field methods for 47,478 rock, sediment, soil, and heavy-mineral concentrate samples. Most samples were collected by U.S. Geological Survey (USGS) personnel and analyzed either in the analytical laboratories of the USGS or by contract with commercial analytical laboratories. These data represent analyses of samples collected as part of various USGS programs and projects. In addition, geochemical data from 7,470 sediment and soil samples collected and analyzed under the Atomic Energy Commission National Uranium Resource Evaluation (NURE) Hydrogeochemical and Stream Sediment Reconnaissance (HSSR) program (henceforth called NURE) have been included in this database. In addition to data from 2,377 samples collected and analyzed under CCAP, this dataset includes archived geochemical data originally entered into the in-house Rock Analysis Storage System (RASS) database (used by the USGS from the mid-1960s through the late 1980s) and the in-house PLUTO database (used by the USGS from the mid-1970s through the mid-1990s). All of these data are maintained in the Oracle-based National Geochemical Database (NGDB). Retrievals from the NGDB and from the NURE database were used to generate most of this dataset. In addition, USGS data that have been excluded previously from the NGDB because the data predate earliest USGS geochemical databases, or were once excluded for programmatic reasons

Perfil de la mujer en la alta dirección en Colombia

OpenAIRE

Morales Castro, Clara Viviana

2011-01-01

El objetivo del presente estudio descriptivo fenomenológico es identificar los perfiles sociodemográficos que predominan en un grupo de mujeres directivas en Colombia, y observar las características de su liderazgo; para tal propósito se realizó un estudio cualitativo y un análisis de los determinantes de la participación laboral de las mujeres en Colombia. Se tomó como base de información encuestas realizadas a un grupo de mujeres de la alta dirección en Colombia, implementando un análi...

Transtorno afetivo bipolar: perfil farmacoterapêutico e adesão ao medicamento

OpenAIRE

Miasso,Adriana Inocenti; Carmo,Bruna Paiva do; Tirapelli,Carlos Renato

2012-01-01

Este estudo teve como objetivos verificar a adesão de portadores de transtorno afetivo bipolar (TAB) à terapêutica medicamentosa e identificar possíveis causas de adesão e não adesão ao medicamento de acordo com o perfil farmacoterapêutico. Trata-se de estudo transversal, descritivo, realizado em Núcleo de Saúde Mental de um município do interior paulista. Participaram do estudo 101 pacientes com TAB. Para coleta dos dados, utilizou-se a entrevista estruturada e o teste de Morisky-Green e, pa...

Implantación y perfil de los sindicatos en Euskadi

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ANDONI KAIERO URÍA

1991-01-01

Full Text Available El trabajo utiliza los resultados de las elecciones sindicales de 1980, 1982 y 1986 para describir el aspecto sindical de Euskal Herria. Análisis de la distribución de los votos a los sindicatos (elecciones de 1982 en los colegios electorales y en las empresas del territorio y de los sectores es utilizado para llegar a una primera aproximación de las características de los sindicatos. El perfil de los sindicatos mayoritarios se completa con los resultados de una encuesta, llevada a cabo en 1982, que ha permitido conocer la afiliación sindical y algunos datos personales y de opinión de los afiliados y votantes a los sindicatos.

Perfil dos discentes ingressos do Centro de Ciências da Saúde UFPE

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Ludmila Galindo França Gurgel

Full Text Available A busca pelo conhecimento das características e da opinião dos estudantes do nível superior fornece importantes subsídios para o planejamento e reorganização do desenvolvimento acadêmico. Com o objetivo de traçar o perfil do aluno do Centro de Ciências da Saúde da Universidade Federal de Pernambuco (UFPE, foram distribuídos formulários aos acadêmicos do 2º período, contendo perguntas referentes aos seus aspectos socioeconômicos e pessoais. O perfil dos estudantes (n = 210 caracterizou-se por um predomínio feminino, com idades entre 19 e 21 anos, provenientes de escolas privadas e classes sociais economicamente mais favorecidas, que receberam grande influência do núcleo familiar na escolha da profissão. A maioria dos estudantes não estava matriculada nos cursos de primeira opção, porém possuía alta expectativa com relação ao curso, considerando-o correspondente às suas expectativas. Após formados pretendem realizar algum curso de pós-graduação e trabalhar no serviço público. No entanto, persiste um problema relativo à escolha da profissão, regulada pela condição socioeconômica e influência familiar.

Landscape and bio- geochemical strategy for monitoring transformation and reclamation of the soil mining sites

Science.gov (United States)

Korobova, Elena

2010-05-01

Sites of active or abandoned mining represent areas of considerable technogenic impact and need scientifically ground organization of their monitoring and reclamation. The strategy of monitoring and reclamation depends on the scale and character of the physical, chemical and biological consequences of the disturbances. The geochemical studies for monitoring and rehabilitation of the career-dump complexes should methodically account of formation of the particular new landforms and the changes in circulation of the remobilized elements of the soil cover. However, the general strategy should account of both the initial and transformed landscape geochemical structure of the area with due regard to the natural and new content of chemical elements in the environmental components. For example the tailings and waste rocks present new geochemical fields with specifically different concentration of chemical elements that cause formation of new geochemical barriers and landscapes. The way of colonization of the newly formed landscapes depends upon the new geochemical features of the technogenic environment and the adaptive ability of local and intrusive flora. The newly formed biogeochemical anomalies need organization of permanent monitoring not only within the anomaly itself but also of its impact zones. Spatial landscape geochemical monitoring combined with bio-geochemical criteria of threshold concentrations seems to be a helpful tool for decision making on reclamation and operation of the soil mining sites to provide a long-term ecologically sustainable development of the impact zone as a whole.

Version 4. 00 of the MINTEQ geochemical code

Energy Technology Data Exchange (ETDEWEB)

Eary, L.E.; Jenne, E.A.

1992-09-01

The MINTEQ code is a thermodynamic model that can be used to calculate solution equilibria for geochemical applications. Included in the MINTEQ code are formulations for ionic speciation, ion exchange, adsorption, solubility, redox, gas-phase equilibria, and the dissolution of finite amounts of specified solids. Since the initial development of the MINTEQ geochemical code, a number of undocumented versions of the source code and data files have come into use at the Pacific Northwest Laboratory (PNL). This report documents these changes, describes source code modifications made for the Aquifer Thermal Energy Storage (ATES) program, and provides comprehensive listings of the data files. A version number of 4.00 has been assigned to the MINTEQ source code and the individual data files described in this report.

Version 4.00 of the MINTEQ geochemical code

Energy Technology Data Exchange (ETDEWEB)

Eary, L.E.; Jenne, E.A.

1992-09-01

The MINTEQ code is a thermodynamic model that can be used to calculate solution equilibria for geochemical applications. Included in the MINTEQ code are formulations for ionic speciation, ion exchange, adsorption, solubility, redox, gas-phase equilibria, and the dissolution of finite amounts of specified solids. Since the initial development of the MINTEQ geochemical code, a number of undocumented versions of the source code and data files have come into use at the Pacific Northwest Laboratory (PNL). This report documents these changes, describes source code modifications made for the Aquifer Thermal Energy Storage (ATES) program, and provides comprehensive listings of the data files. A version number of 4.00 has been assigned to the MINTEQ source code and the individual data files described in this report.

EMPREENDEDORISMO SUSTENTÁVEL: PERFIL DOS PRODUTORES DA FEIRA AGROECOLÓGICA DA ORLA DE OLINDA - PE

Directory of Open Access Journals (Sweden)

Daniel Cerqueira Lima e Penalva Santos

2013-05-01

Full Text Available Este artigo teve como objetivo definir o perfil psicossocial dos produtores rurais que comercializam seus produtos na Feira Agroecológica de Olinda, definindo-os enquanto seu grau de empreendedorismo, suas motivações e segundo os preceitos da sustentabilidade. Inicialmente discutiu-se no âmbito teórico temas como empreendedorismo, perfil do empreendedor, feiras agroecológicas e cultura de sustentabilidade, posicionando ideologicamente os conceitos adotados pelos autores deste artigo. Em seguida uma entrevista estruturada foi realizada com os produtores que participam da Feira, sendo sua abrangência bastante ampla tendo em vista que todas as barracas foram contempladas, sendo entrevistado um produtor por barraca. De uma forma geral, os resultados mostraram que os produtores são homens, em sua maioria de baixa escolaridade, que buscam além do crescimento econômico a qualidade de vida para suas famílias e seus clientes. Também ficou claro que sua atividade é um processo de inovação, e, sob o nosso conceito, os produtores se caracterizam enquanto empreendedores e suas atividades contribuem diretamente para uma cultura de sustentabilidade, podendo ser definidos enquanto empreendedores sustentáveis.

National Geochemical Survey Locations and Results for Iowa

Data.gov (United States)

Iowa State University GIS Support and Research Facility — The United States Geological Survey (USGS), in collaboration with other state and federal agencies, industry, and academia, is conducting a National Geochemical...

Hydro-geochemical and isotopic fluid evolution of the Los Azufres caldera geothermal field, Central Mexico

Energy Technology Data Exchange (ETDEWEB)

Gonzalez-Partida, E [Centro de Geociencias, Campus Juriquilla-UNAM, Queretaro (Mexico); Viggiano-Guerra, J C [Subgerencia de Estudios C.F.E., Morelia. Michocan (Mexico); Perez, R J [Universidad de Calgary (Canada)], E-mail: egp@geociencias.unam.mx, E-mail: cesar.viggiano@cfe.gob.mx, E-mail: rene@geochemicalengineering.com

2008-10-01

Hydrothermal alteration at Los Azufres geothermal held is mostly propylitic showing progressive dehydration with depth, and temperature increase. The evolution of this system is inferred to be related to deep liquid water, boiling when ascending through fractures connected to the surface.

Hydro-geochemical and isotopic fluid evolution of the Los Azufres caldera geothermal field, Central Mexico

International Nuclear Information System (INIS)

Gonzalez-Partida, E; Viggiano-Guerra, J C; Perez, R J

2008-01-01

Hydrothermal alteration at Los Azufres geothermal held is mostly propylitic showing progressive dehydration with depth, and temperature increase. The evolution of this system is inferred to be related to deep liquid water, boiling when ascending through fractures connected to the surface.

Determination of geochemical and natural radioactivity characteristics in Bilecik Marble, Turkey

Science.gov (United States)

Yerel Kandemir, Suheyla; Ozbay, Nurgul

2014-05-01

Natural stones are one of the oldest known building materials. There are more than 400 natural stone in Turkey. Recently, the demand for the natural stone types in markets has been increasing rapidly. For this reason, the geochemical and natural radioactivity characteristics of natural stone are very important. Bilecik province is located at the northwest part of Turkey and it is surrounded by Sakarya, Bursa, Eskisehir and Kutahya city. Bilecik is one of the important marble industry regions of Turkey. Thus, the geochemical and natural radioactivity characteristics of Bilecik marble are very important. In this study, Bilecik marble was collected to determine the geochemistry and natural radioactivity. Then, analyses of geochemical and natural radioactivity in the marble samples are interpreted. ACKNOWLEDGMENT This study is supported by Bilecik Seyh Edebali University scientific project (Project Number =2011-02-BIL.03-04).

The role of atomic absorption spectrometry in geochemical exploration

Science.gov (United States)

Viets, J.G.; O'Leary, R. M.

1992-01-01

In this paper we briefly describe the principles of atomic absorption spectrometry (AAS) and the basic hardware components necessary to make measurements of analyte concentrations. Then we discuss a variety of methods that have been developed for the introduction of analyte atoms into the light path of the spectrophotometer. This section deals with sample digestion, elimination of interferences, and optimum production of ground-state atoms, all critical considerations when choosing an AAS method. Other critical considerations are cost, speed, simplicity, precision, and applicability of the method to the wide range of materials sampled in geochemical exploration. We cannot attempt to review all of the AAS methods developed for geological materials but instead will restrict our discussion to some of those appropriate for geochemical exploration. Our background and familiarity are reflected in the methods we discuss, and we have no doubt overlooked many good methods. Our discussion should therefore be considered a starting point in finding the right method for the problem, rather than the end of the search. Finally, we discuss the future of AAS relative to other instrumental techniques and the promising new directions for AAS in geochemical exploration. ?? 1992.

Un estudio exploratorio del perfil de las mujeres empresarias en el Perú

OpenAIRE

Avolio Alecchi, Beatrice

2008-01-01

La investigación identifica el perfil de las mujeres empresarias en el Perú mediante la exploración cualitativa de sus características demográficas; sus antecedentes educativos, laborales y familiares; sus habilidades administrativas; la naturaleza de sus empresas; los factores que las han estimulado a convertirse en empresarias; y los obstáculos para el desarrollo de sus empresas. El estudio utiliza el paradigma cualitativo basado en estudios de caso de veinticuatro mujeres empresarias en el...

“El perfil sociocultural de los graduados universitarios: el caso de la UNGS”

OpenAIRE

Fernández, Marcos Silvestre

2015-01-01

La presente ponencia se enmarca en un proyecto de beca de investigación otorgada por Consejo Interuniversitario Nacional (CIN) en Octubre del 2014, en la carrera de grado Lic. En Educación de La Universidad Nacional de General Sarmiento (UNGS). El trabajo tiene como objetivo presentar el análisis, las metodologías empleadas y las primeras conclusiones sobre el estudio "El perfil Sociocultural de los graduados universitario: el caso de la UNGS". El proyecto se propuso elaborar un es...

Origin and evolution of the atmospheres of early Venus, Earth and Mars

Science.gov (United States)

Lammer, Helmut; Zerkle, Aubrey L.; Gebauer, Stefanie; Tosi, Nicola; Noack, Lena; Scherf, Manuel; Pilat-Lohinger, Elke; Güdel, Manuel; Grenfell, John Lee; Godolt, Mareike; Nikolaou, Athanasia

2018-05-01

We review the origin and evolution of the atmospheres of Earth, Venus and Mars from the time when their accreting bodies were released from the protoplanetary disk a few million years after the origin of the Sun. If the accreting planetary cores reached masses ≥ 0.5 M_Earth before the gas in the disk disappeared, primordial atmospheres consisting mainly of H_2 form around the young planetary body, contrary to late-stage planet formation, where terrestrial planets accrete material after the nebula phase of the disk. The differences between these two scenarios are explored by investigating non-radiogenic atmospheric noble gas isotope anomalies observed on the three terrestrial planets. The role of the young Sun's more efficient EUV radiation and of the plasma environment into the escape of early atmospheres is also addressed. We discuss the catastrophic outgassing of volatiles and the formation and cooling of steam atmospheres after the solidification of magma oceans and we describe the geochemical evidence for additional delivery of volatile-rich chondritic materials during the main stages of terrestrial planet formation. The evolution scenario of early Earth is then compared with the atmospheric evolution of planets where no active plate tectonics emerged like on Venus and Mars. We look at the diversity between early Earth, Venus and Mars, which is found to be related to their differing geochemical, geodynamical and geophysical conditions, including plate tectonics, crust and mantle oxidation processes and their involvement in degassing processes of secondary N_2 atmospheres. The buildup of atmospheric N_2, O_2, and the role of greenhouse gases such as CO_2 and CH_4 to counter the Faint Young Sun Paradox (FYSP), when the earliest life forms on Earth originated until the Great Oxidation Event ≈ 2.3 Gyr ago, are addressed. This review concludes with a discussion on the implications of understanding Earth's geophysical and related atmospheric evolution in relation

Development of geophysical and geochemical data processing software based on component GIS

International Nuclear Information System (INIS)

Ke Dan; Yu Xiang; Wu Qubo; Han Shaoyang; Li Xi

2013-01-01

Based on component GIS and mixed programming techniques, a software which combines the basic GIS functions, conventional and unconventional data process methods for the regional geophysical and geochemical data together, is designed and developed. The software has many advantages, such as friendly interface, easy to use and utility functions and provides a useful platform for regional geophysical and geochemical data processing. (authors)

Compilation of kinetic data for geochemical calculations

International Nuclear Information System (INIS)

Arthur, R.C.; Savage, D.; Sasamoto, Hiroshi; Shibata, Masahiro; Yui, Mikazu

2000-01-01

Kinetic data, including rate constants, reaction orders and activation energies, are compiled for 34 hydrolysis reactions involving feldspars, sheet silicates, zeolites, oxides, pyroxenes and amphiboles, and for similar reactions involving calcite and pyrite. The data are compatible with a rate law consistent with surface reaction control and transition-state theory, which is incorporated in the geochemical software package EQ3/6 and GWB. Kinetic data for the reactions noted above are strictly compatible with the transition-state rate law only under far-from-equilibrium conditions. It is possible that the data are conceptually consistent with this rate law under both far-from-equilibrium and near-to-equilibrium conditions, but this should be confirmed whenever possible through analysis of original experimental results. Due to limitations in the availability of kinetic data for mine-water reactions, and in order to simplify evaluations of geochemical models of groundwater evolution, it is convenient to assume local-equilibrium in such models whenever possible. To assess whether this assumption is reasonable, a modeling approach accounting for couple fluid flow and water-rock interaction is described that can be use to estimate spatial and temporal scale of local equilibrium. The approach is demonstrated for conditions involving groundwater flow in fractures at JNC's Kamaishi in-situ tests site, and is also used to estimate the travel time necessary for oxidizing surface waters to migrate to the level of a HLW repository in crystalline rock. The question of whether local equilibrium is a reasonable assumption must be addressed using an appropriate modeling approach. To be appropriate for conditions at the Kamaishi site using the modeling approach noted above, the fracture fill must closely approximate a porous mine, groundwater flow must be purely advective and diffusion of solutes across the fracture-host rock boundary must not occur. Moreover, the mineralogical and

Geochemical prospect ion results of Mariscala aerial photo

International Nuclear Information System (INIS)

Filippini, J.

1989-01-01

This report shows the geochemical prospect ion results carried out within the framework of the metalical mining prospect ion in Mariscala aerial photo. Lavalleja district belong to the Mining inventory programme of Uruguay.

Geochemical methodology for gold prospect ion in Uruguay

International Nuclear Information System (INIS)

Spangenber, J.

1987-01-01

This work is about the history of gold prospection in Uruguay. In this study there are considered the geochemical aspects, the gold performance, the applicability to mining prospection and the gold prospection aluvionar

Novel geochemical techniques integrated in exploration for uranium deposits at depth

International Nuclear Information System (INIS)

Kyser, K.

2014-01-01

Mineral deposits are in fact geochemical anomalies, and as such their detection and assessment of their impact on the environment should be facilitated using geochemical techniques. Although geochemistry has been used directly in the discovery of uranium deposits and more indirectly in shaping deposit models, the novel applications of geochemistry and integration with other data can be more effective in formulating exploration and remediation strategies. Recent research on the use of geochemistry in detecting uranium deposits at depth include: (1) more effective integration of geochemical with geophysical data to refine targets, (2) revealing element distributions in and around deposits to adequately assess the total chemical environment associated with the deposit, (3) the use of element tracing using elemental concentrations and isotopic compositions in the near surface environment to detect specific components that have migrated to the surface from uranium deposits at depth, (4) understand the effects of both macro- and micro-environments on element mobility across the geosphere-biosphere interface to enhance exploration using select media for uranium at depth. Geophysical data used in exploration can identify areas of conductors where redox contrasts may host mineralization, structures that act to focus fluids during formation of the deposits and act as conduits for element migration to the surface, and contrasts in geology that are required for the deposits. However, precision of these data is greatly diminished with depth, but geochemical data from drill core or surface media can enhance target identification when integrated with geophysical data. Geochemical orientation surveys over known unconformity-related deposits at depth clearly identify mineralization 900m deep. Drill core near the deposit, clay-size fractions separated from soil horizons and vegetation over and far from the deposit record element migration from the deposit as radiogenic He, Rn and Pb

Centros de Atenção Psicossocial Infantojuvenil no Brasil: distribuição geográfica e perfil dos usuários

Directory of Open Access Journals (Sweden)

Grey Yuliet Ceballos Garcia

2015-12-01

Full Text Available Resumo Poucos estudos brasileiros abordam a utilização de serviços de saúde mental para população infanto-juvenil. Neste trabalho, objetivou-se caracterizar a distribuição nacional dos Centros de Atenção Psicossocial Infantojuvenis (CAPSi e descrever o perfil nosológico dos atendimentos infantojuvenis entre 2008 e 2012. Realizou-se estudo ecológico, utilizando registros do sistema de Autorizações de Pagamento de Serviços de Alta Complexidade (APAC e do Cadastro Nacional de Estabelecimentos de Saúde (CNES. Aspectos sociodemográficos e perfil nosológico foram analisados. Em 2014, 208 CAPSi estavam registrados no CNES, distribuíam-se em 23 das 27 unidades da federação brasileira. Nos atendimentos, predominaram transtornos de comportamento (29,7%, transtornos de desenvolvimento (23,6% e retardo mental (12,5%. Os CAPSi são insuficientes e desigualmente distribuídos. O perfil nosológico sugere necessidade de articulação entre serviços especializados de saúde mental e atenção básica, além de inclusão do trabalho intersetorial.

Geochemical correlations between uranium and other components in U-bearing formations of Ogcheon belt

International Nuclear Information System (INIS)

Lee, M.S.; Chon, H.T.

1980-01-01

Some components in uranium-bearing formations which consist mainly of black shale, slate and low grade coal-bearing formation of Ogcheon Belt were processed statistically in order to find out the geochemical correlations with uranium. Geochemical enrichment of uranium, vanadium and molybdenum in low grade coal-bearing formations and surrounding rocks is remarkable in the studied area. Geochemical correlation coefficient of uranium and molybdenum in the rocks displays about 0.6 and that of uranium and fixed carbon about 0.4. Uranium and vanadium in uranium-bearing low grade coals denote very high correlation with fixed carbon, which is considered to be responsible for enrichment of metallic elements, especially molybdenum. Close geochemical correlation of uranium-molybdenum couple in the rocks can be applied as a competent exploration guide to low grade uranium deposits of this area. (author)

Propriedades da carne e perfil de ácidos graxos do pernil de catetos (Tayassu tajacu) alimentados com torta de babaçu (Orbignya phalerata)

OpenAIRE

Albuquerque,N.I.; Contreras,C.C.; Alencar,S.; Meirelles,C.F.; Aguiar,A.P.; Moreira,J.A.; Packer,I.U.

2009-01-01

Analisaram-se as propriedades da carne e o perfil de ácidos graxos do pernil de catetos alimentados com dietas contendo diferentes porcentagens de torta de babaçu, usada como fonte energética alternativa substituindo parte do milho na alimentação, em sistemas de produção em cativeiro. Avaliou-se o pernil de 12 animais quanto às suas propriedades - perda de peso ao cozimento, força de cisalhamento, pH e capacidade de retenção de água-, depois extraiu-se o óleo da carne e determinou-se o perfil...

Geochemical landscapes of the conterminous United States; new map presentations for 22 elements

Science.gov (United States)

Gustavsson, N.; Bolviken, B.; Smith, D.B.; Severson, R.C.

2001-01-01

Geochemical maps of the conterminous United States have been prepared for seven major elements (Al, Ca, Fe, K, Mg, Na, and Ti) and 15 trace elements (As, Ba, Cr, Cu, Hg, Li, Mn, Ni, Pb, Se, Sr, V, Y, Zn, and Zr). The maps are based on an ultra low-density geochemical survey consisting of 1,323 samples of soils and other surficial materials collected from approximately 1960-1975. The data were published by Boerngen and Shacklette (1981) and black-and-white point-symbol geochemical maps were published by Shacklette and Boerngen (1984). The data have been reprocessed using weighted-median and Bootstrap procedures for interpolation and smoothing.

Adding geochemical and isotope tracers to models of hillslope evolution: valuable constraints or monumental headache?

Science.gov (United States)

Mudd, S. M.; Yoo, K.; Hurst, M. D.; Weinman, B. A.; Maher, K.

2011-12-01

Landscapes evolve through time, both in terms of their geomorphology and their geochemistry. Past studies have highlighted that topography suffers from the problem of equifinality: the topographic configuration of landscapes can be the result of many different, yet equally plausible, erosion histories. In hillslope soils the properties and chemistry of the soils themselves could provide additional constraints on landscape evolution. Here we present results from a combination of modelling and field studies that seek to quantify the co-evolution of hillslope morphology and the solid state chemistry of hillslope soils. The models follow large numbers of individual particles as they are entrained into a physically mobile soil layer, weathered, and accumulate isotopes such as 10Be and 21Ne. We demonstrate that multiple hillslope properties mitigate (but do not eliminate) the problem of equifinality and demonstrate the importance of accounting for individual particle residence times and ages in interpretation of both isotope and weathering data.

Evaluation of disposal site geochemical performance using a containment factor

International Nuclear Information System (INIS)

Lerman, A.; Domenico, P.A.; Bartlett, J.W.

1988-01-01

The containment factor is a measure of retention by geologic setting of wastes released from a repository. The factor is alternatively defined either in terms of several measurable hydrological and geochemical parameters, or in terms of amounts of waste components that may be released to the geologic setting and, subsequently, to the environment. Containment factors for individual waste components in a given geologic setting are functions of groundwater to rock volume ratios, sorption or exchange characteristics of the rocks, and containment time to groundwater travel time ratios. For high-level radioactive wastes, containment factors based on the NRC and EPA limit values for cumulative releases from waste and to the environment provide a measure of the geochemical performance of the geologic setting in tuff, basalt, and salt. The containment factor values for individual nuclides from high-level wastes indicate that for some of the nuclides containment may be achieved by groundwater travel time along. For other nuclides, additional performance functions need to be allocated to geochemical retention by such processes as sorption, ion-exchange or precipitation

PERFIL DA DISFAGIA APÓS UM ACIDENTE VASCULAR CEREBRAL: UMA REVISÃO INTEGRATIVA

OpenAIRE

CARINA TEIXEIRA PAIXÃO; LOLITA DOPICO DA SILVA; FLAVIA GIRON CAMERINI

2010-01-01

Este artículo trata de disfagia decurrente de una enfermedad vascular cerebral (EVC). El objetivo fue determinar el perfil de las publicaciones acerca de la disfagia en pacientes víctimas de EVC. Investigación de revisión integradora que usó los mismos descriptores en las bases Medline, Scielo e Lilacs, seleccionando 17 artículos entre 1998 a 2008. Los datos fueron analizados a partir de las categorías correspondientes a los enfoques de las publicaciones encontradas. Los resultados muestran d...

Un acercamiento a la comprensión del perfil de la Inteligencia Emocional

OpenAIRE

Gloria María Isaza-Zapata; Juan Santiago Calle-Piedrahíta

2016-01-01

Este artículo es resultado de un estudio de inteligencia emocional. En la investigación nos propusimos como objetivo general, analizar el perfil de inteligencia emocional y social de una muestra de 110 docentes de educación básica primaria, vinculados a diez instituciones educativas de la ciudad de Medellín, Colombia. El alcance es descriptivo, no experimental, y correlacional; y está apoyado con método probabilístico, simple al azar y estratificado. Los resultados obtenidos desde el perf...

Perfil do estoque domiciliar de medicamentos em residências com crianças

OpenAIRE

Gabriela Colonetti Beckhauser; Cleidson Valgas; Dayani Galato

2012-01-01

Com o objetivo de identificar o perfil do estoque domiciliar de medicamentos em residências com crianças, foi realizado um estudo baseado na técnica de entrevista aplicado aos responsáveis pelos medicamentos. Para caracterização dos estoques, os medicamentos foram classificados de acordo com o primeiro nível da Anatomical Therapeutic Chemical e adotaram-se indicadores de armazenamento. Foram aplicados 83 questionários em domicílios contendo de uma a três crianças (6...

PERFIL FISIOLÓGICO DEL JUDOKA. UNA REVISIÓN

Directory of Open Access Journals (Sweden)

Raquel Hernández García

2007-01-01

Full Text Available El judo en su aspecto competitivo requiere una elevada preparación técnica, táctica, física y psicológica, ya que cada uno de estos aspectos es imprescindible para soportar las altas cargas de entrenamiento y competición llevadas a cabo por estos deportistas. A la suma, este deporte de combate está caracterizado estructuralmente por categorías de peso, lo cual alza la importancia del control fisiológico del entrenamiento en los judokas. Por lo tanto, el presente trabajo de revisión posee como principal objeto recolectar los diferentes artículos científicos sobre el perfil fisiológico del judoka, enmarcando aspectos como parámetros antropométricos (% de grasa corporal, registro de Frecuencia Cardiaca (FC, consumo máximo de oxígeno (VO2máx, indicadores hematológicos e indicadores electrolíticos.

Environmental and geochemical assessment of surface sediments on irshansk ilmenite deposit area

Directory of Open Access Journals (Sweden)

Наталия Олеговна Крюченко

2015-03-01

Full Text Available It is revealed the problem of pollution of surface sediments of Irshansk ilmenite deposit area of various chemical elements hazard class (Mn, V, Ba, Ni, Co, Cr, Mo, Cu, Pb, Zn. It is determined its average content in surface sediments of various functional areas (forest and agricultural land, flood deposits, reclaimed land, calculated geochemical criteria, so given ecological and geochemical assessment of area

Geochemical characterization of Parana Basin volcanic rocks: petrogenetic implications

International Nuclear Information System (INIS)

Marques, L.S.

1988-01-01

A detailed study of the geochemical characteristics of Parana Basin volcanic rocks is presented. The results are based on the analyses of major and trace elements of 158 samples. Ninety three of these volcanic samples belong to 8 flow sequences from Rio Grande do Sul and Santa Catarina States. The remaining sixty five samples are distributed over the entire basin. In order to study the influence of crustal contamination processes in changing chemical characteristics of the volcanic rocks, 47 samples representative of the crystalline basement of the southern and southeastern Parana Basin were also analysed. Several petrogenetic models were tested to explain the compocional variability of the volcanic rocks, in particular those of southern region. The results obtained sugest an assimilation-fractional crystallization process as viable to explain the differences of both the chemical characteristics and Sr isotope initial ratios observed in basic and intermediate rocks. A model involving melting processes of basic material, trapped at the base of the crust, with composition similar to low and high TiO 2 basalts appears to be a possibility to originate the Palmas and Chapeco acid melts, respectively. The study of ''uncontaminated'' or poorly contaminated low TiO 2 basic rocks from the southern, central and northern regions shows the existence of significant differences in the geochemical charactetistics according to their geographical occurrence. A similar geochemical diversity is also observed in high TiO 2 basalts and Chapeco volcanics. Differences in incompatible element ratios between low and high TiO 2 ''uncontaminated'' or poorly contaminated basalts suggest that they could have been produced by different degrees of melting in a garnet peridotite source. Geochemical and isotopic (Sr and Nd) data also support the view that basalts from northern and southern regions of Parana Basin originated from mantle source with different composition. (author) [pt

Polyamorphic Transformations in Fe-Ni-C Liquids: Implications for Chemical Evolution of Terrestrial Planets: Fe-Ni-C liquid structural change

Energy Technology Data Exchange (ETDEWEB)

Lai, Xiaojing [Department of Geology and Geophysics, University of Hawai‘i at Mānoa, Honolulu HI USA; Hawaii Institute of Geophysics and Planetology, University of Hawai‘i at Mānoa, Honolulu HI USA; Chen, Bin [Hawaii Institute of Geophysics and Planetology, University of Hawai‘i at Mānoa, Honolulu HI USA; Wang, Jianwei [Department of Geology and Geophysics, Center for Computation and Technology, Louisiana State University, Baton Rouge LA USA; Kono, Yoshio [HPCAT, Geophysical Laboratory, Carnegie Institution of Washington, Argonne IL USA; Zhu, Feng [Department of Earth and Environmental Sciences, University of Michigan, Ann Arbor MI USA

2017-12-01

During the formation of the Earth's core, the segregation of metallic liquids from silicate mantle should have left behind evident geochemical imprints on both the mantle and the core. Some distinctive geochemical signatures of the mantle-derived rocks likely own their origin to the metal-silicate differentiation of the primitive Earth, setting our planet apart from undifferentiated meteorites as well as terrestrial planets or moons isotopically and compositionally. Understanding the chemical evolution of terrestrial planetary bodies requires knowledge on properties of both liquid iron alloys and silicates equilibrating under physicochemical conditions pertinent to the deep magma ocean. Here we report experimental and computational results on the pressure-induced structural evolution of iron-nickel liquids alloyed with carbon. Our X-ray diffraction experiments up to 7.3 gigapascals (GPa) demonstrate that Fe-Ni (Fe90Ni10) liquids alloyed with 3 and 5 wt % carbon undergo a polyamorphic liquid structure transition at approximately 5 GPa. Corroborating the experimental observations, our first-principles molecular dynamic calculations reveal that the structural transitions result from the marked prevalence of three-atom face-sharing polyhedral connections in the liquids at >5 GPa. The structure and polyamorphic transitions of liquid iron-nickel-carbon alloys govern their physical and chemical properties and may thus cast fresh light on the chemical evolution of terrestrial planets and moons.

Energy-constrained open-system magmatic processes IV: Geochemical, thermal and mass consequences of energy-constrained recharge, assimilation and fractional crystallization (EC-RAFC)

International Nuclear Information System (INIS)

Wendy A. Bohrson Department of Geological Sciences, Central Washington University, Ellensburg, Washington, 98926, USA; Frank J. Spera Institute for Crustal Studies and Department of Geological Sciences, University of California, Santa Barbara, California, 93106, USA

2003-01-01

RAFC events may record a more complete view of the physiochemical history of an open-system magma body. The capability of EC-RAFC to track melts and solids creates a genetic link that can be compared to natural analogues such as layered mafic intrusions and flood basalts, or mafic enclaves and their intermediate-composition volcanic or plutonic hosts. The ability to quantify chemical and volume characteristics of solids and melts also underscores the need for integrated field, petrologic and geochemical studies of igneous systems. While it appears that a number of volcanic events or systems may be characterized by continuous influx or eruption of magma (''steady state systems''), reports describing compositional homogeneity for products that represent eruptions of more than one event are relatively rare. In support of this, EC-RAFC results indicate that very specific combinations of recharge conditions, bulk distribution coefficients, and element concentrations are required to achieve geochemical homogeneity during cooling of a magma body undergoing RAFC. In summary, critical points are that EC-RAFC provides a method to quantitatively investigate complex magmatic systems in a thermodynamic context; it predicts complex, nonmonotonic geochemical trends for which there are natural analogues that have been difficult to model; and finally, EC-RAFC establishes the link between the chemical and physical attributes of a magmatic system. Application of EC-RAFC promises to improve our understanding of specific tectonomagmatic systems as well as enhance our grasp of the essential physiochemical principles that govern magma body evolution

Geothermal investigations with isotope and geochemical techniques in Latin America

International Nuclear Information System (INIS)

1992-03-01

The IAEA Co-ordinated Research Programme (CRP) for Latin America on the Use of Isotope and Geochemical Techniques in Geothermal Exploration started in 1984. The first activity carried out was a Seminar on isotope and geochemical techniques in geothermal exploration, which took place in June 1984 in Morelia, Mexico. During the seminar, which was attended by representatives of the institutions which later took part in the programme, the objectives, main research lines, and geothermal fields to be studied during the CRP were discussed. The first research contracts were awarded towards the end of 1984. The field work started in 1985 and continued through 1990. During the implementation of the CRP a considerable number of geothermal fields were studied in the nine participating countries. The investigations carried out were geochemically quite comprehensive in most cases, but in some others they were still in a reconnaissance stage when the CRP ended: the latter studies are not reported in these proceedings, but the data obtained are in principle available from the relevant national institutions. While investigations with conventional geochemical techniques had already started in several fields before 1985, isotope methods were applied for the first time in all cases during this CRP. Due to the remoteness and high elevation of many of the fields studied and the adverse meteorological conditions during long periods of the year, the investigations could not proceed rapidly: this is the main reason for the unusually long duration of the CRP, which could be concluded only after more than five years after its inception

Use of natural geochemical tracers to improve reservoir simulation models

Energy Technology Data Exchange (ETDEWEB)

Huseby, O.; Chatzichristos, C.; Sagen, J.; Muller, J.; Kleven, R.; Bennett, B.; Larter, S.; Stubos, A.K.; Adler, P.M.

2005-01-01

This article introduces a methodology for integrating geochemical data in reservoir simulations to improve hydrocarbon reservoir models. The method exploits routine measurements of naturally existing inorganic ion concentration in hydrocarbon reservoir production wells, and uses the ions as non-partitioning water tracers. The methodology is demonstrated on a North Sea field case, using the field's reservoir model, together with geochemical information (SO{sub 4}{sup 2}, Mg{sup 2+} K{sup +}, Ba{sup 2+}, Sr{sup 2+}, Ca{sup 2+}, Cl{sup -} concentrations) from the field's producers. From the data-set we show that some of the ions behave almost as ideal sea-water tracers, i.e. without sorption to the matrix, ion-exchange with the matrix or scale-formation with other ions in the formation water. Moreover, the dataset shows that ion concentrations in pure formation-water vary according to formation. This information can be used to allocate produced water to specific water-producing zones in commingled production. Based on an evaluation of the applicability of the available data, one inorganic component, SO{sub 4}{sup 2}, is used as a natural seawater tracer. Introducing SO{sub 4}{sup 2} as a natural tracer in a tracer simulation has revealed a potential for improvements of the reservoir model. By tracking the injected seawater it was possible to identify underestimated fault lengths in the reservoir model. The demonstration confirms that geochemical data are valuable additional information for reservoir characterization, and shows that integration of geochemical data into reservoir simulation procedures can improve reservoir simulation models. (author)

Perfil dos microrganismos associados à colonização e infecção em Terapia Intensiva

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Adriana Cristina Oliveira

2017-06-01

Full Text Available Justificativa e Objetivos: Nas instituições hospitalares, as Unidades de Terapia Intensiva são consideradas o epicentro de resistência bacteriana devido à maior ocorrência de surtos por bactérias multirresistentes. A monitorização do perfil microbiológico dos microrganismos associados a infecções são fundamentais para apoiar o uso racional de antimicrobianos e as medidas de prevenção e controle de infecções. Assim, objetivou-se verificar o perfil de sensibilidade de microrganismos aos antimicrobianos associados à ocorrência de colonização e infecções em uma Unidade de Terapia Intensiva. Métodos: Tratou-se de uma coorte com seguimento de 2.137 pacientes (2005 – 2008 de um hospital universitário de Belo Horizonte. Resultados: Entre os 2.137 pacientes acompanhados foram realizadas 426 (19,9% culturas microbiológicas, 61,7% (263 se referiam a colonização por microrganismos resistentes destacando-se 39% Acinetobacter baumanni resistentes aos carbapenêmicos, 21% Pseudomonas aeruginosa resistentes aos carbapenêmicos e 14% Staphylococcus aureus resistentes à oxacilina seguidos de Klebsiella pneumoniae e Escherichia coli; 282 pacientes foram diagnosticados com infecções hospitalares (13,2% sendo 86 associadas a microrganismos resistentes. Conclusão: Concluiu-se que o perfil dos microrganismos associados a colonização ou infecção de pacientes na unidade de terapia intensiva entre 2005 e 2008, foi similar ao observado em outros estudos no Brasil e América Latina com predominância dos bastonetes Gram negativos. Evidenciou-se a necessidade de monitoramento das condições ambientais de limpeza e sazonais como variação de temperatura e umidade que podem favorecer a replicação de microrganismos, como parte das medidas de controle da disseminação.

Calidad Y Perfil Del Profesor Universitario

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José Vicente Sánchez Frank

2014-07-01

Full Text Available La investigación se desarrolla en un enfoque mixto, combina el paradigma cuantitativo con la finalidad de conseguir patrones de regularidad, y el cualitativo en cuanto a nivel de técnica y estrategia de captura de información, con las entrevistas a profundidad, y también a nivel del análisis de datos, e interpretación de los resultados en la reducción, disposición y transformación de los mismos, a los fines de obtener de la experiencia de los cuatro grupos etarios de educadores; la investigación se realizó con 120 docentes de la Universidad Nacional Experimental del Estado Táchira. La investigación desarrolla los aspectos teóricos de los constructos perfil del docente, en el marco de constructo calidad en la docencia. Plantea como objetivo general diseñar e implementar un sistema de medición de la calidad en la docencia universitaria. Conclusión: la implementación del sistema permitió la formulación, ejecución y seguimiento de programas, orientados a la formación del personal académico para contribuir a mejorar la calidad de la docencia.

Geochemical studies of granitic rocks of Kallur area, Manvi Taluk, Raichur district, Karnataka (India).

Science.gov (United States)

Raghavendra, N R; Reddy, R Purushottam; Nijagunappa, R

2011-01-01

The geochemical data is much widely used in establishing the overall chemical relation existing between the different rock types with their parentage. A major impetus for this shift comes not only from the need to understand and quantify better the spatial and temporal evolution, with emphasis on the younger greenstone belts (Kallur copper formations), but also from the recognition that such knowledge could form the basis for the sustainable development of our natural resources. In addition, the recurrence of natural hazards has reinforced the need to learn more about the mechanics and to develop predictive modeling with advanced technical tools. This paper is emphasizing on Granodiorites of Kallur area of Manvi Taluk, Raichur District to substantiate the classical approaches of exploration and data gathering through quantitative methods of data processing and interpretation. The trilinear diagram indicates that the granites are rich in Potash and Soda. This clearly indicates that Granites are fairly rich in K2O than Na2O.

Perfil biopsicossocial de portadores de anoftalmia no sul de Minas Gerais - Brasil

OpenAIRE

Cabral,Luiz Gustavo Megda; Martelli Júnior,Hercílio; Leite,Denise Moura; Sabatini Júnior,David; Freitas,Amanda Beatriz Dahdah Aniceto de; Miranda,Roseli Teixeira; Swerts,Mário Sérgio Oliveira; Barros,Letízia Monteiro de

2008-01-01

OBJETIVO: Avaliar o perfil biopsicossocial de portadores de anoftalmia, com ênfase no impacto psicológico e funcional da perda ocular e na reintegração social dessa população. MÉTODOS: Realizou-se estudo transversal com 84 pacientes (50 do gênero masculino e 34 do feminino), reabilitados ou em processo de reabilitação com próteses oculares, avaliados por meio de questionário que contemplava dimensões como: etiologia da perda ocular, grau de adaptação à prótese e impacto nas atividades profiss...

EL PERFIL DEL CONTADOR PÚBLICO Y DE LOS ESTUDIOS DE POSTGRADO

OpenAIRE

Polar Falcón, Ernesto Augusto

2014-01-01

La Facultad de Ciencias Contables de la UNMSM, desde su fundación hasta la fecha, siempre ha tenido muy claro el perfil del Contador Público que forma profesional mente. Su filosofía educativa está cimentada en cumplir con dos objetivos: el primero, mantener el alto nivel de formación del Contador Público que se ofrece año tras año a la sociedad peruana; y el segundo, destacar su liderazgo de educación universitaria en el consenso de dirección y ejemplo a nivel de las Facultades de la Univers...

Perfil de produção acadêmica dos programas brasileiros de pós-graduação em Ciência da Informação 2008-2012

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Marynice Medeiros Matos Autran

Full Text Available As práticas de comunicação da ciência dependem de culturas epistêmicas diferenciadas. A literatura relata inúmeras pesquisas, sob os mais diferenciados enfoques, relacionados aos programas brasileiros de pós-graduação em ciência da informação (PPGCIs. Nesta pesquisa esses programas foram caracterizados considerando o capital intelectual acumulado. Entretanto, o que se conhece sobre o perfil próprio de atuação para a produção de ciência nesses programas? Esta investigação visa: analisar a produção acadêmica - comunicações apresentadas em eventos, artigos de periódicos, capítulos de livros, livros organizados, editados, publicados e resumos expandidos - no quinquênio 2008 a 2012. A metodologia incluiu a extração automática do Currículo Lattes dos docentes, efetivos e colaboradores dos PPGCIs, em atividade até 31 de dezembro de 2012. Para a extração foi utilizada a ferramenta scriptLattes. Dentre os resultados obtidos, foi evidenciado que a produção acadêmica se concentra, majoritariamente, em comunicações apresentadas em eventos (36,8% e artigos de periódicos (34,3%. Adicionalmente, foi identificada a existência de três tipos de perfil/atuação dos PPGCIs para o quinquênio: (a perfil estável de produção, (b perfil com leve decremento de produção, e (c perfil com leve incremento de produção.

Estimation of Supraglacial Dust and Debris Geochemical Composition via Satellite Reflectance and Emissivity

Science.gov (United States)

Casey, Kimberly Ann; Kaab, Andreas

2012-01-01

We demonstrate spectral estimation of supraglacial dust, debris, ash and tephra geochemical composition from glaciers and ice fields in Iceland, Nepal, New Zealand and Switzerland. Surface glacier material was collected and analyzed via X-ray fluorescence spectroscopy (XRF) and X-ray diffraction (XRD) for geochemical composition and mineralogy. In situ data was used as ground truth for comparison with satellite derived geochemical results. Supraglacial debris spectral response patterns and emissivity-derived silica weight percent are presented. Qualitative spectral response patterns agreed well with XRF elemental abundances. Quantitative emissivity estimates of supraglacial SiO2 in continental areas were 67% (Switzerland) and 68% (Nepal), while volcanic supraglacial SiO2 averages were 58% (Iceland) and 56% (New Zealand), yielding general agreement. Ablation season supraglacial temperature variation due to differing dust and debris type and coverage was also investigated, with surface debris temperatures ranging from 5.9 to 26.6 C in the study regions. Applications of the supraglacial geochemical reflective and emissive characterization methods include glacier areal extent mapping, debris source identification, glacier kinematics and glacier energy balance considerations.

Estimation of Supraglacial Dust and Debris Geochemical Composition via Satellite Reflectance and Emissivity

Directory of Open Access Journals (Sweden)

Kimberly Casey

2012-09-01

Full Text Available We demonstrate spectral estimation of supraglacial dust, debris, ash and tephra geochemical composition from glaciers and ice fields in Iceland, Nepal, New Zealand and Switzerland. Surface glacier material was collected and analyzed via X-ray fluorescence spectroscopy (XRF and X-ray diffraction (XRD for geochemical composition and mineralogy. In situ data was used as ground truth for comparison with satellite derived geochemical results. Supraglacial debris spectral response patterns and emissivity-derived silica weight percent are presented. Qualitative spectral response patterns agreed well with XRF elemental abundances. Quantitative emissivity estimates of supraglacial SiO2 in continental areas were 67% (Switzerland and 68% (Nepal, while volcanic supraglacial SiO2 averages were 58% (Iceland and 56% (New Zealand, yielding general agreement. Ablation season supraglacial temperature variation due to differing dust and debris type and coverage was also investigated, with surface debris temperatures ranging from 5.9 to 26.6 C in the study regions. Applications of the supraglacial geochemical reflective and emissive characterization methods include glacier areal extent mapping, debris source identification, glacier kinematics and glacier energy balance considerations.

Geochemical characteristics of peat from two raised bogs of Germany

Science.gov (United States)

Mezhibor, A. M.

2016-11-01

Peat has a wide range of applications in different spheres of human activity, and this is a reason for a comprehensive study. This research represents the results of an ICP-MS study of moss and peat samples from two raised bogs of Germany. Because of the wide use of sphagnum moss and peat, determining their geochemical characteristics is an important issue. According to the results obtained, we can resume that the moss samples from Germany are rich in Cu, As, Y, Zr, Nb, and REE. The geochemical composition of the bogs reflects the regional environmental features and anthropogenic influence.

Geochemical reanalysis of historical U.S. Geological Survey sediment samples from the Tonsina area, Valdez Quadrangle, Alaska

Science.gov (United States)

Werdon, Melanie B.; Granitto, Matthew; Azain, Jaime S.

2015-01-01

The State of Alaska’s Strategic and Critical Minerals (SCM) Assessment project, a State-funded Capital Improvement Project (CIP), is designed to evaluate Alaska’s statewide potential for SCM resources. The SCM Assessment is being implemented by the Alaska Division of Geological & Geophysical Surveys (DGGS), and involves obtaining new airborne-geophysical, geological, and geochemical data. As part of the SCM Assessment, thousands of historical geochemical samples from DGGS, U.S. Geological Survey (USGS), and U.S. Bureau of Mines archives are being reanalyzed by DGGS using modern, quantitative, geochemical-analytical methods. The objective is to update the statewide geochemical database to more clearly identify areas in Alaska with SCM potential. The USGS is also undertaking SCM-related geologic studies in Alaska through the federally funded Alaska Critical Minerals cooperative project. DGGS and USGS share the goal of evaluating Alaska’s strategic and critical minerals potential and together created a Letter of Agreement (signed December 2012) and a supplementary Technical Assistance Agreement (#14CMTAA143458) to facilitate the two agencies’ cooperative work. Under these agreements, DGGS contracted the USGS in Denver to reanalyze historical USGS sediment samples from Alaska. For this report, DGGS funded reanalysis of 128 historical USGS sediment samples from the statewide Alaska Geochemical Database Version 2.0 (AGDB2; Granitto and others, 2013). Samples were chosen from the Tonsina area in the Chugach Mountains, Valdez quadrangle, Alaska (fig. 1). The USGS was responsible for sample retrieval from the National Geochemical Sample Archive (NGSA) in Denver, Colorado through the final quality assurance/quality control (QA/QC) of the geochemical analyses obtained through the USGS contract lab. The new geochemical data are published in this report as a coauthored DGGS report, and will be incorporated into the statewide geochemical databases of both agencies

Application of integrated Landsat, geochemical and geophysical data in mineral exploration

International Nuclear Information System (INIS)

Conradsen, K.; Nilsson, G.; Thyrsted, T.; Gronlands Geologiske Undersogelse, Copenhagen, Denmark)

1985-01-01

In South Greenland (20000 sq. km) a remote sensing investigation is executed in connection with uranium exploration. The investigation includes analysis of Landsat data, conversion of geological, geochemical and geophysical data to image format compatible with Landsat images, and analysis of the total set of integrated data. The available geochemical data consisted of samples from 2000 sites, analyzed for U, K, Rb, Sr, Nb, Ga, Y, and Fe. The geophysical data comprised airborne gamma-spectrometric measurements and aeromagnetic data. The interpolation routines consisted of a kriging procedure for the geochemical data and a minimum curvature routine for the geophysical data. The analysis of the integrated data set is at a preliminary stage. As example a composite image showing Landsat channel 7, magnetic values, and Fe values as respectively intensity, hue and saturation is analyzed. It reveals alkaline intrusions and basaltic layers as anomalies while other anomalies cannot be accounted for on the basis of the present geological knowledge. 12 references

Perfil dos portadores de cavidade anoftálmica: estudo na Faculdade de Medicina de Botucatu - UNESP

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Silvia Narikawa

2011-10-01

Full Text Available OBJETIVO: Avaliar o perfil dos portadores de cavidade anoftálmica e a evolução dos pacientes com os tratamentos empregados. MÉTODOS: Estudo retrospectivo, realizado na Faculdade de Medicina de Botucatu, avaliando-se o perfil e a evolução dos portadores de cavidade anoftálmica, tratados no serviço. Os dados foram estudados segundo frequência de ocorrência e análise de associação. RESULTADOS: Os portadores de cavidade anoftálmica eram mais frequentemente em homens, trabalhadores em atividades exercidas com as mãos, jovens. O trauma e a phthisis bulbi foram as causas mais encontradas, havendo diferenças de acordo com a faixa etária e sexo. O índice complicações foi alto (57,1% dos casos, a maioria ocorrendo tardiamente. CONCLUSÕES: O trauma continua sendo causa importante de perda do olho. As complicações que ocorrem durante o acompanhamento do portador de cavidade anoftálmica são frequentes e ocorrem, em geral, tardiamente, o que reforça a necessidade de acompanhamento periódico e prolongado destes pacientes.

AVALIAÇÃO E DEFINIÇÃO DO PERFIL DE TEXTURA IDEAL DE QUEIJO PETIT SUISSE

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Vanessa Rios de Souza

2011-10-01

Full Text Available A textura é um dos atributos sensoriais que afetam a aceitação do produto. Com a avaliação da textura instrumental e aceitação sensorial é possível definir o perfil de textura ideal de um determinado produto. Desta maneira, o objetivo deste trabalho foi definir o perfil de textura ideal de queijo petit suisse Para isso, foram analisadas cinco marcas comerciais de queijo tipo petit suisse Foi realizado um teste de aceitação em relação ao atributo textura, e também uma análise de TPA, sendo os parâmetros analisados dureza, coesividade, gomosidade, elasticidade, mastigabilidade, resistência e adesividade. A partir dos resultados dessas avaliações, conclui-se que a textura que apresentou a melhor aceitação sensorial possui os parâmetros de dureza variando entre 6,43 e 6,65N, coesividade variando entre 0,71 e 0,77, gomosidade variando entre 4,76 e 4,97, mastigabilidade variando entre 4,54 e 4,83, resistência variando entre 0,020 e 0,032 e adesividade variando entre 34,23 e 35,47.

Avaliação do perfil lipídico sanguíneo de atletas corredores no ensaio ergoespirométrico de bruce utilizando espectroscopia no infrevermelho

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Francielle Pasqualotti Meinhardt

2011-09-01

Full Text Available Os constituintes do perfil lipídico compõem o sangue e são importantes marcadores bioquímicos de doenças cardiovasculares, que é reconhecida como grande causa de morbidade e mortalidade. Para um diagnóstico mais amplo das possíveis alterações do perfil lipídico se apresenta o método da espectroscopia no infravermelho (FTIR que consiste de uma técnica analítica que envolve a identificação de misturas complexas. Este estudo tem como objetivo avaliar a aplicação da espectroscopia de infravermelho na obtenção de dados do perfil lipídico de atletas corredores. Trata-se de um estudo analítico observacional comparativo, tendo como método de referência os ensaios enzimáticos baseados na reação de Trinder, comparados à espectroscopia no infravermelho por reflectância difusa com Transformada de Fourier (DRIFTS, com auxílio das ferramentas quimiométricas de análise exploratória por agrupamento hierárquico (HCA e análise preditiva por mínimos quadrados parciais (PLS para previsão destes marcadores bioquímicos. Foram sujeitos 14 atletas da equipe de Atletismo da UNISC, de 18 a 30 anos, de ambos os sexos, avaliados em repouso e após o teste ergoespirométrico de Bruce. Os resultados apontam que, na avaliação de atletas, a técnica de infravermelho (DRIFTS juntamente com o PLS, foi adequada para a construção de modelos de calibração e na definição da correlação entre testes bioquímicos padrões no perfil lipídico e na determinação pelo infravermelho. Nessa perspectiva, considera-se possível a utilização da FTIR na obtenção de dados que determina o perfil lipídico em amostras de sangue total em atletas.

Perfil clínico del adulto mayor atendido ambulatoriamente en un hospital general.

OpenAIRE

Casas, Paola; Varela, Luis; Tello, Tania; Ortiz, Pedro; Chávez, Helver

2012-01-01

Objetivo: Describir el perfil clínico del adulto mayor atendido ambulatoriamente en un hospital general. Material y métodos: Estudio descriptivo, transversal, realizado a través de encuestas aplicadas a pacientes en la consulta ambulatoria de geriatría del Hospital Nacional Cayetano Heredia (HNCH), entre agosto de 2011 y enero 2012. Resultados: Se evaluaron 290 pacientes, el 69,3% fueron mujeres; el 65,5% tenía entre 60 y 79 años. La hipertensión arterial fue el diagnóstico más frecuente (55,...

Perfil dos acidentes de trabalho em refinaria de petróleo

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Carlos Augusto Vaz de Souza

2002-10-01

Full Text Available OBJETIVO: O trabalho em refinarias de petróleo envolve o risco de acidentes triviais e ampliados. Os dados nacionais apontam para a relevância dos acidentes nesse setor. Assim, realizou-se pesquisa com o objetivo de identificar o perfil e avaliar a adequação dos instrumentos de registro dos acidentes de trabalho em refinaria. MÉTODOS: Foram padronizadas e analisadas informações referentes aos acidentes de trabalho nas atividades de produção e manutenção registradas em uma refinaria de petróleo do Estado do Rio de Janeiro, no ano de 1997. A população estudada constituiu-se de 153 pessoas, sendo 83 trabalhadores próprios lesionados e 69 trabalhadores terceirizados lesionados. As variáveis analisadas foram: tipo de acidente, modo de operação e função do trabalhador lesionado. RESULTADOS: Em relação aos trabalhadores próprios, houve predominância dos chamados acidentes triviais (54,2% e quanto ao modo de operação, houve concentração dos acidentes nas atividades em operação normal (62,9%. Quanto aos trabalhadores terceirizados, os acidentes triviais (75,5% tiveram predominância mais acentuada; e quanto ao modo de operação, houve um domínio quase total dos acidentes na atividade de manutenção (96,8%. CONCLUSÕES: Os resultados mostraram um perfil de acidentes que afeta principalmente os níveis hierárquicos mais baixos, concentrando-se de modo geral nas atividades de manutenção, além da necessidade de modificações no sistema de registro e investigação de acidentes por parte da empresa.

O perfil urbano e o comportamento socioecononômico do DF

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Rômulo José da Costa Ribeiro

2007-12-01

especialmente índices simples e compostos de exclusão/inclusão social baseados na distribuição de renda, nível de escolaridade, condições ambientais e níveis de equidade. Associam-se a esses índices a análise do perfil urbano (Bertaud, 2004, que mostra a distribuição de terras por habitante e a densidade populacional, a partir do CBD, por quilômetro. Pode-se verificar, também, a relação entre exclusão-inclusão social à medida que se distancia do CBD. Para o cruzamentos dos diversos dados foram utilizadas ferramentas de geoprocessamento tais como análise por overlay, álgebra de mapas, análises zonais. Os resultados obtidos mostram que quanto mais distante do CBD piores são as condições de vida da população. Os mesmos permitiram mensurar o grau de exclusão em função da distância ao CBD e em relação ao perfil urbano. A aplicação da modelagem estruturada nos elementos anteriormente descritos permitirá o desenvolvimento de um modelo analítico que visa fornecer uma nova visão para o planejamento urbano das áreas mais críticas socio-economicamente, o que poderá vir a permitir a elaboração de propostas que visem à minimização das tensões urbanas, dando condições de vida mais dignas e socialmente mais inclusivas às populações que ali habitam.

Quem são os moradores de residências terapêuticas? Perfil de usuários portadores de transtornos mentais desinstitucionalizados

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Vanessa Vieira França

Full Text Available RESUMO Este artigo teve como objetivo caracterizar o perfil sociodemográfico e clínico de moradores de Serviços Residenciais Terapêuticos (SRT. Trata-se de um estudo transversal, censitário, com 190 moradores de SRT de Recife (PE, analisando as variáveis de perfil sociodemográfico e o histórico psiquiátrico. Observou-se que os moradores se caracterizam, em sua maioria, por homens, solteiros, idosos, analfabetos e histórico de múltiplos e longos internamentos psiquiátricos. Conclui-se que as condutas iatrogênicas praticadas no hospital deixaram sequelas importantes em diversos aspectos da vida dos usuários e tornaram-se numa dívida social que ainda precisa ser paga pela sociedade.

Manual hierarchical clustering of regional geochemical data using a Bayesian finite mixture model

International Nuclear Information System (INIS)

Ellefsen, Karl J.; Smith, David B.

2016-01-01

Interpretation of regional scale, multivariate geochemical data is aided by a statistical technique called “clustering.” We investigate a particular clustering procedure by applying it to geochemical data collected in the State of Colorado, United States of America. The clustering procedure partitions the field samples for the entire survey area into two clusters. The field samples in each cluster are partitioned again to create two subclusters, and so on. This manual procedure generates a hierarchy of clusters, and the different levels of the hierarchy show geochemical and geological processes occurring at different spatial scales. Although there are many different clustering methods, we use Bayesian finite mixture modeling with two probability distributions, which yields two clusters. The model parameters are estimated with Hamiltonian Monte Carlo sampling of the posterior probability density function, which usually has multiple modes. Each mode has its own set of model parameters; each set is checked to ensure that it is consistent both with the data and with independent geologic knowledge. The set of model parameters that is most consistent with the independent geologic knowledge is selected for detailed interpretation and partitioning of the field samples. - Highlights: • We evaluate a clustering procedure by applying it to geochemical data. • The procedure generates a hierarchy of clusters. • Different levels of the hierarchy show geochemical processes at different spatial scales. • The clustering method is Bayesian finite mixture modeling. • Model parameters are estimated with Hamiltonian Monte Carlo sampling.

Basic concepts and formulations for isotope geochemical modelling of groundwater systems

International Nuclear Information System (INIS)

Kalin, R.M.

1996-01-01

This chapter describes the basic chemical principles and methodologies for geochemical models and their use in the field of isotope hydrology. Examples of calculation procedures are given on actual field data. Summary information on available PC software for geochemical modeling is included. The specific software, NETPATH, which can be used for chemical speciation, mass balance and isotope balance along a flow path in groundwater systems, is discussed at some length with an illustrative example of its application to field data. (author). Refs, 14 figs, 15 tabs

Basic concepts and formulations for isotope geochemical modelling of groundwater systems

Energy Technology Data Exchange (ETDEWEB)

Kalin, R M [The Queen` s University, Belfast, Northern Ireland (United Kingdom). Dept. of Civil Engineering

1996-10-01

This chapter describes the basic chemical principles and methodologies for geochemical models and their use in the field of isotope hydrology. Examples of calculation procedures are given on actual field data. Summary information on available PC software for geochemical modeling is included. The specific software, NETPATH, which can be used for chemical speciation, mass balance and isotope balance along a flow path in groundwater systems, is discussed at some length with an illustrative example of its application to field data. (author). Refs, 14 figs, 15 tabs.

Some methodical questions of study of vertical geochemical zoning of ore deposits

International Nuclear Information System (INIS)

Sochevanov, N.N.; Gorelova, E.K.

1975-01-01

Taking a hydrothermal uranium deposit as an example, the advisability of dividing ore-localizing structures (for the purpose of making a calculation for a single geochemical zonality) into five zones, a supra-, an upper, a central, a lower and an infra-ore one, has been shown. It is recommended to determine the place of elements in the geochemical zonality sequence by taking into account the productivity of their aureoles and the location of the centre of gravity of their reserves in the ore, supra- and infra-ore horizons. When considering the peculiarities of a zonality, it is irrational to take account of elements determined with an insufficient sensitivity as well as of low-contrast or unstable ones. When calculating tracer ratios the most contrasting data can be obtained by using the most distant elements in the geochemical zonality sequence

Perfil cromatográfico dos componentes polifenólicos de Maytenus ilicifolia mart. (Celastraceae

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Haroudo Satiro Xavier

Full Text Available Buscando-se fornecer subsídios farmacognósticos para uma melhor caracterização da "espinheira santa" (Mavtenus ilicifolia, elaborou-se urn perfil cromatográfico a partir de folhas do vegetal disponíveis no comércio local. Heterosídeos flavonólicos a proantocianidinas foram constatados, podendo perfeitamente estas moléculas, servirem como marcadores para afeição da originalidade da droga ou de sua qualidade coma insumo farmacêutico.

Perfil de adolescentes gestantes de um município do interior do Paraná

OpenAIRE

Beatriz Rosana Gonçalves de Oliveira; Claudia Silveira Viera; Juliene Flávia Noris Almeida Fonseca

2011-01-01

Este estudio planteó como objetivo identificar el perfil de adolescentes embarazadas, en un municipio de Paraná, teniendo en cuenta la influencia de factores biológicos, psicológicos y sociales, para apoyar las acciones preventivas del embarazo precoz. Investigación cuantitativa con datos obtenidos mediante entrevista. y análisis estadístico descriptivo. Se analizaron: edad de la menarqula, ginecológica y al quedar embarazada, uso de anticonceptivos antes del embarazo, relación familiar, acep...

Propuesta de perfiles varios y competencias laborales asociadas al profesional de la información

OpenAIRE

Ramón Antonio Piña Rodríguez

2006-01-01

Se formula, desde el enfoque de la Gestión por competencias, el paradigma de las competencias cognitivas laborales y perfiles de algunos cargos definidos a desempeñar en las organizaciones por el profesional de la información. Es demostrada la versatilidad del desempeño de éste y las oportunidades que le ofrece a los empresarios que apuestan por la empresa del siglo XXI, inmersa en la era del conocimiento.

Perfiles de involucramiento del consumidor y el instrumento de medición para consumidores mexicanos "IP6"

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Jorge Vera Martínez

2003-01-01

Full Text Available Este escrito pretende esencialmente dos propósitos. En primer lugar se trata de presentar una visión general sobre el involucramiento del consumidor en el proceso de compra como una línea de investigación dentro de la mercadotecnia y el comportamiento de consumo. Además, se introduce al concepto del involucramiento en un sentido multifacético, al que se ha llamado “perfiles de involucramiento”, dependiente de diferentes factores que afectan a un consumidor cuando está en una situación de elección de compra; de igual forma se presenta una revisión de los diferentes modelos e instrumentos de medición que se han ofrecido para medir el involucramiento en este sentido multivariable. Son propuestas de operacionalización del involucramiento que se han diseñado en otros países y en idiomas distintos al español. El segundo objetivo, y más importante, radica en presentar los resultados sobre el diseño de un instrumento de medición basado en esta visión multifacética del involucramiento y en los inventarios desarrollados anteriormente en otros países; también se intenta ofrecer un instrumento que mida “los perfiles de involucramiento del consumidor en la elección de compra de un producto” en idioma español y aplicable en México. Para esto se diseñan, confiabilizan y validan (al menos de forma inicial una serie de reactivos en consumidores mexicanos que pretenden medir las distintas variables relacionadas con esta concepción del involucramiento. Este enfoque y su instrumento de medición pretende ser nombrado como el “IP6” (modelo de involucramiento de 6 perfiles. Asimismo, se obtienen 6 conjuntos de 3 reactivos cada uno con indicadores aceptables de confiabilidad y validez para medir cada perfil de involucramiento pretendido: “interés hacia el producto”, “placer percibido en su compra”, “valor simbólico que representa”, “importancia del riesgo al elegirlo”, “probabilidad percibida de ese riesgo” e �

Diferencias en el perfil de involucramiento entre productos de conveniencia y productos de comparación

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Jorge Vera Martínez

2010-01-01

Full Text Available En la literatura se ha propuesto que el perfil de involucramiento del consumidor difiere de acuerdo con el tipo de producto. Por ello, en este trabajo se retoma una tipología clásica en lacual los productos de consumo son clasificados en productos de conveniencia, de comparación y de especialidad. En este estudio se muestra empíricamente que el perfil de involucramiento hacia los productos varían significativamente entre dos tipos de productos: de conveniencia y de comparación especialidad. A través de tres tipos de análisis estadísticos se observa que cinco de los seis componentes del involucramiento, que determinan el perfil, sí muestran diferencias según el tipo de producto. En un primer procedimiento no paramétrico de asociación de variables utilizando ji-cuadrada y coeficiente de contingencia, se corrobora la interdependencia entre la mayoría de los componentes de involucramiento con el tipo de producto, quedando ciertas dudas con el componente riesgo percibido. En un segundo procedimiento no paramétrico, pero de diferenciación entre grupos, se muestra que tanto los rangos como las formas de las distribuciones varían entre estos dos grandes tipos de productos. Por último, utilizando métodos paramétricos de diferencia de medias y varianzas, nuevamente se encontraron diferencias significativas entre los valores de los componentes del involucramiento de estos tipos. Esto implica que la variabilidad de las respuestas de los sujetos es diferente en cada componente con respecto al tipo de producto, ofreciendo evidencia de que el involucramiento hacia los productos de comparación-especialidad sí varía del involucramiento hacia los productos de conveniencia, pudiéndose establecer excepciones en el aspecto de riesgo percibido hacia el desempeño de los productos. El componente del involucramiento que más claramente diferencia a estos dos tipos de productos es el grado de interés percibido en ellos.

COMPOSICIÓN CORPORAL, PERFIL LIPÍDICO Y APTITUD FÍSICA EN MUJERES ADOLESCENTES EN MÉXICO

Directory of Open Access Journals (Sweden)

José Aldo Hernández-Murúa

2016-06-01

Full Text Available El objetivo de esta investigación fue determinar la composición corporal, el perfil de lípidos sanguíneos y aptitud física en mujeres adolescentes con y sin sobrepeso, y correlacionar cada variable con las demás. Se consideró un diseño transversal. Participaron 38 mujeres adolescentes con edades entre 14 y 19 años. Clasificadas como normopeso (n = 21 o sobrepeso (n = 17 según la gráfica de la Organización Mundial de la Salud mediante el IMC (kg/m² en función del puntaje z para edades de 5 a 19 años (puntaje z: 0 a +1 DE = normopeso, +1 a +2 DE = sobrepeso. Se realizaron mediciones de composición corporal, perfil de lípidos sanguíneos (colesterol total, triglicéridos, cHDL, cLDL y aptitud física (VO2pico y 1RM. Los resultados muestran que las adolescentes con normopeso fueron significativamente (p < 0.05 más bajas (M ± DE en todas las variables de composición corporal que las mujeres adolescentes con sobrepeso. No se encontraron diferencias significativas en el VO2pico, 1RM ni en el perfil de lípidos sanguíneos. En conclusión, las mujeres adolescentes con sobrepeso presentan mayores niveles de composición y grasa corporal pero estos niveles superiores no parecen afectar los niveles de lípidos sanguíneos. Se encontró una asociación entre los niveles de aptitud física (VO2pico y la composición corporal (% grasa, pliegues cutáneos. Se sugieren otros estudios para buscar la asociación entre los niveles de VO2pico y grasa corporal.

Geochemical tracing and hydrogeochemical modelling of water-rock interactions during salinization of alluvial groundwater (Upper Rhine Valley, France)

Energy Technology Data Exchange (ETDEWEB)

Lucas, Y., E-mail: yann.lucas@eost.u-strasbg.fr [Universite de Strasbourg et CNRS, Laboratoire d' Hydrologie et de Geochimie de Strasbourg, Ecole et Observatoire des Sciences de la Terre, 1, rue Blessig, 67084 Strasbourg Cedex (France); Schmitt, A.D., E-mail: anne-desiree.schmitt@univ-fcomte.fr [Universite de Strasbourg et CNRS, Laboratoire d' Hydrologie et de Geochimie de Strasbourg, Ecole et Observatoire des Sciences de la Terre, 1, rue Blessig, 67084 Strasbourg Cedex (France)] [Universite de Franche-Comte et CNRS-UMR 6249, Chrono-Environnement, 16, Route de Gray, 25030 Besancon Cedex (France); Chabaux, F., E-mail: francois.chabaux@eost.u-strasbg.fr [Universite de Strasbourg et CNRS, Laboratoire d' Hydrologie et de Geochimie de Strasbourg, Ecole et Observatoire des Sciences de la Terre, 1, rue Blessig, 67084 Strasbourg Cedex (France); Clement, A.; Fritz, B. [Universite de Strasbourg et CNRS, Laboratoire d' Hydrologie et de Geochimie de Strasbourg, Ecole et Observatoire des Sciences de la Terre, 1, rue Blessig, 67084 Strasbourg Cedex (France); Elsass, Ph. [BRGM, GEODERIS, 1, rue Claude Chappe, 57070 Metz (France); Durand, S. [Universite de Strasbourg et CNRS, Laboratoire d' Hydrologie et de Geochimie de Strasbourg, Ecole et Observatoire des Sciences de la Terre, 1, rue Blessig, 67084 Strasbourg Cedex (France)

2010-11-15

Research highlights: {yields} Major and trace elements along with strontium and uranium isotopic ratios show that groundwater geochemical characteristics along the saline plumes cannot reflect a conservative mixing. {yields} A coupled hydrogeochemical model demonstrates that cationic exchange between alkalis from polluted waters and alkaline-earth elements from montmorillonite present in the host rock of the aquifer is the primary process. {yields} The model requires only a small amount of montmorillonite. {yields} It is necessary to consider the pollution history to explain the important chloride, sodium and calcium concentration modifications. {yields} The model shows that the rapidity of the cationic exchange reactions insures a reversibility of the cation fixation on clays in the aquifer. - Abstract: In the southern Upper Rhine Valley, groundwater has undergone intensive saline pollution caused by the infiltration of mining brines, a consequence of potash extraction carried out during the 20th century. Major and trace elements along with Sr and U isotopic ratios show that groundwater geochemical characteristics along the saline plumes cannot reflect conservative mixing between saline waters resulting from the dissolution of waste heaps and one or more unpolluted end-members. The results imply the occurrence of interactions between host rocks and polluted waters, and they suggest that cationic exchange mechanisms are the primary controlling process. A coupled hydrogeochemical model has been developed with the numerical code KIRMAT, which demonstrates that cationic exchange between alkalis from polluted waters and alkaline-earth elements from montmorillonite present in the host rock of the aquifer is the primary process controlling the geochemical evolution of the groundwater. The model requires only a small amount of montmorillonite (between 0.75% and 2.25%), which is in agreement with the observed mineralogical composition of the aquifer. The model also proves

Late Holocene evolution of the Northeast intertidal region of Sepetiba Bay, Rio de Janeiro (Brazil

Directory of Open Access Journals (Sweden)

Anita Fernandes Souza Pinto

2016-03-01

Full Text Available This work is based on the study of the core T1 collected in the Guaratiba Mangrove, located on the northeastern margin of Sepetiba Bay. Few studies dealing with the application of benthic foraminifera to study sea level changes during the Holocene have been conducted in Sepetiba Bay, State of Rio de Janeiro, Brazil. In order to fill this gap, the core T1 was studied using textural, geochemical (carbonate, total organic carbon, total sulfur and stable isotopes evaluated in Ammonia tepida and microfaunal (benthic foraminifera data, unveiling paleoecological relationships of these organisms and the evolutionary scenario of Guaratiba Mangrove. Radiocarbon results indicate an estimated age of about 2400 yrs cal BP for the core base. Textural, geochemical and benthic foraminifera data suggest that the study area changed significantly during the last 2400 yrs cal BP. It experienced coastal waves action and shoreface processes in the period between ≈2.400-1.400 yrs cal BP; then, this phase gave place to a shallow marine environment similar to that found currently in internal and protected areas of Sepetiba Bay, between ≈1.400-350 yrs cal BP. Thenceforth, the study area evolved to the present mangrove environment. Factors related to climatic oscillations and the formation, evolution and events of rupture of Marambaia sand ridge influenced the late Holocene evolution of the northeast intertidal area of Sepetiba Bay.

Perfil competitivo de empresas de tercerización de procesos de Bogotá: análisis de componentes principales

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NELSON ORLANDO ALARCÓN VILLAMIL

Full Text Available El objetivo del presente artículo de resultados de investigación es analizar el perfil competitivo de empresas de tercerización de procesos de negocio (BPO, por sus siglas en Inglés de Bogotá, evaluadas a través del Modelo de Indicadores de Gestión Sostenible y Asociatividad (MIGSA y utilizando el Análisis de Componentes Principales (ACP, para distribuir las variables estudiadas en un número reducido de grupos, con el fin de dar cuenta de los aspectos que sintetizan la variabilidad en la gestión de las empresas. El estudio permitió establecer dos ejes: el primero relaciona aspectos de sostenibilidad internos a la empresa y el segundo establece elementos de sostenibilidad externos, los dos generan cuatro perfiles diferentes de competitividad, los cuales permiten a las organizaciones, además de establecer su ubicación, la generación de planes estratégicos que favorezcan su posicionamiento en el mercado.

Low-pressure evolution of arc magmas in thickened crust: The San Pedro-Linzor volcanic chain, Central Andes, Northern Chile

Science.gov (United States)

Godoy, Benigno; Wörner, Gerhard; Kojima, Shoji; Aguilera, Felipe; Simon, Klaus; Hartmann, Gerald

2014-07-01

Magmatism at Andean Central Volcanic Zone (CVZ), or Central Andes, is strongly influenced by differentiation and assimilation at high pressures that occurred at lower levels of the thick continental crust. This is typically shown by high light to heavy rare earth element ratios (LREE/HREE) of the erupted lavas at this volcanic zone. Increase of these ratios with time is interpreted as a change to magma evolution in the presence of garnet during evolution of Central Andes. Such geochemical signals could be introduced into the magmas be high-pressure fractionation with garnet on the liquidus and/or assimilation from crustal rocks with a garnet-bearing residue. However, lavas erupted at San Pedro-Linzor volcanic chain show no evidence of garnet fractionation in their trace element patterns. This volcanic chain is located in the active volcanic arc, between 22°00‧S and 22°30‧S, over a continental crust ˜70 km thick. Sampled lavas show Sr/Y and Sm/Yb ratios Chile. We relate our geochemical observations to shallow crustal evolution of primitive magmas involving a high degree of assimilation of upper continental crust. We emphasize that low pressure AFC- (Assimilation Fractional Crystallization) type evolution of the San Pedro-Linzor volcanic chain reflects storage, fractionation, and contamination of mantle-derived magmas at the upper felsic crust (<40 km depth). The ascent of mantle-derived magmas to mid-crustal levels is related with the extensional regime that has existed in this zone of arc-front offset since Late-Miocene age, and the relatively thin portion of mafic lower crust observed below the volcanic chain.

Experiencias y consideraciones en la conformación de perfiles de competencias

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Jorge Haddad Barthelemy

2007-06-01

Full Text Available La investigación se desarrolló en el Banco Popular de Ahorro, en Santiago de Cuba, donde durante tres años se trabajó en la conformación de diversos Perfiles de Competencias Directivos y un Perfil Único o Genérico, adaptable a cualquier directivo de esta institución y otras organizaciones. Se obtuvieron y confirmaron diversas concepciones de competencias como las simples, compuestas, básicas, secundarias, genéricas y especificas, importantes y claves, y diversas experiencias como la importancia de establecer sus dimensiones, las contradicciones y similitudes entre competencias y valores, su posibilidad de enfocarse hacia diversas tareas organizacionales, como el mejoramiento del medio ambiente, la calidad del trabajo de mandos superiores, intermedios, técnicos y obreros, con el objetivo de perfeccionar la gestión del desempeño de los trabajadores y la organización.---This study was carried out in the Banco Popular de Ahorro, in Santiago de Cuba. During three years, different Profiles of Directive Competitions were made as well as a Unique or Generic Profile, adaptable to any executive of this or other organizations. Different conceptions of competitions were obtained and confirmed, such as simple, compound, basic, secondary, generic and specific competitions. Various experiences were confirmed, such as the importance of establishing their dimensions, contradictions and similarities between competitions and values, their possibility to focus on different organizational tasks, such as the improvement of the environment, the quality in the performance of top and intermediate management, technicians and workers, with the objective of improving the performance of the employees and the organization.

Geochemical characterization of the siliciclastic rocks of Chitravati ...

Indian Academy of Sciences (India)

V Somasekhar

2018-05-23

May 23, 2018 ... Chitravati Group of Cuddapah Supergroup to decipher the provenance and depositional environment. Both the units ... Based on major element geochemical classification diagram, Pulivendla Quartzite .... The youngest age limit of the Nallamalai ...... eastern Oregon and western Idaho, USA: Implications for.

Uruguay Mining inventory. Florida fotoplano geochemical prospecting results

International Nuclear Information System (INIS)

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

1982-01-01

This work is about the geochemical prospecting carried out in Florida fotoplano within the framework of Uruguay Mining inventory. In this work were covered 660 km2 obtaining 752 samples for study which were analyzed by Plasma Emission Spectrometry in Orleans BRGM laboratories

Uruguay mining Inventory: Geochemical prospecting results of Valentines mapping

International Nuclear Information System (INIS)

Spangenberg, J.; Filippini, J.

1985-01-01

This work is about geochemical prospecting carried out into the Uruguay mining inventory framework. In this case the survey was in Valentines mapping. Florida, Durazno and Treinta y Tres provinces of Uruguay .

Geochemical porosity values obtained in core samples from different clay-rocks

International Nuclear Information System (INIS)

Fernandez, A.M.

2010-01-01

Document available in extended abstract form only. Argillaceous formations of low permeability are considered in many countries as potential host rocks for the disposal of high level radioactive wastes (HLRW). In order to determine their suitability for waste disposal, evaluations of the hydro-geochemistry and transport mechanisms from such geologic formations to the biosphere must be undertaken. One of the key questions about radionuclide diffusion and retention is to know the chemistry and chemical reactions and sorption processes that will occur in the rock and their effects on radionuclide mobility. In this context, the knowledge of the pore water chemistry is essential for performance assessment purposes. This information allows to establish a reliable model for the main water-rock interactions, which control the physico-chemical parameters and the chemistry of the major elements of the system. An important issue in order to model the pore water chemistry in clayey media is to determine the respective volume accessible to cations and anions, i.e, the amount of water actually available for chemical reactions/solute transport. This amount is usually referred as accessible porosity or geochemical porosity. By using the anion inventories, i.e. the anion content obtained from aqueous leaching, and assuming that all Cl - , Br - and SO4 2- leached in the aqueous extracts originates from pore water, the concentration of a conservative ion can be converted into the real pore water concentration if the accessible porosity is known. In this work, the accessible porosity or geochemical porosity has been determined in core samples belonging to four different formations: Boom Clay from Hades URL (Belgium, BE), Opalinus Clay from Mont Terri (Switzerland, CH), and Callovo-Oxfordian argillite from Bure URL (France, FR). The geochemical or chloride porosity was defined as the ratio between the pore water volume containing Cl-bearing pore water and the total volume of a sample

Analysis on geochemical conditions of uranium mineralization in Bashibulake uranium deposit, Xinjiang

International Nuclear Information System (INIS)

Liu Zhangyue; Dong Wenming; Cai Genqing; Liu Hongxu; Deng Huabo

2011-01-01

By studying the palaeoclimate and metallogenesis related geochemical indexes, this paper proposes that the hosting rocks should form in geochemical oxidation setting under arid palaeoclimate. The study on element assemblage associated with uranium mineralization indicates that the target hosting rocks suffered from different degrees of reworking of reducing fluid at first and then being superimposed by supergene oxidative fluid at tectonic uplifting stage. The uranium mineralization is located in reworked and superimposed places of two types of fluid. (authors)

ANÁLISE COMPARATIVA ENTRE OS CONHECIMENTOS DESENVOLVIDOS NO CURSO DE GRADUAÇÃO EM CONTABILIDADE E O PERFIL DO CONTADOR EXIGIDO PELO MERCADO DE TRABALHO: UMA PESQUISA DE CAMPO SOBRE EDUCAÇÃO CONTÁBIL

Directory of Open Access Journals (Sweden)

VINICIUS SUCUPIRA DE ALENCAR MACHADO

2008-01-01

Full Text Available El objetivo de este estudio es verificar si los conocimientos adquiridos por los estu - diantes en el curso de graduación en Ciencias Contables atienden a los requisitos del mer - cado de trabajo del profesional contable en la ciudad de Sao Paulo. Con ese designio, fue desarrollado un cuestionario para investigar los perfiles del profesional contable en términos de conocimientos específicos. El cuestionario fue aplicado en una muestra de 120 gradu-ados de cuatro Instituciones de Enseñanza Superiora (IESs de la ciudad de Sao Paulo y a 31 profesionales con cargo de jefatura de grandes empresas. Los perfiles identificados en las IESs fueron comparados con el perfil logrado en las empresas y, por medio de testes estadísticos, fue posible identificar en que áreas de conocimiento esos requisitos fueron atendidos y en cuales había discrepancias. Hay clara percepción de que los perfiles profe-sionales en términos de conocimientos específicos tratados durante la graduación varían de institución para institución y de esas para el perfil exigido por las empresas, pues, incluso tratándose de un mismo tema, la Contabilidad y sus diferentes aplicaciones y los objetivos de cada uno de esos “players” se demuestran divergentes.

The geochemical chararateristics of the marble deposits east of ...

African Journals Online (AJOL)

), marbles were investigated with the view to establishing marble occurrences and their geochemical characteristics. Crystalline rocks of the Nigerian Basement Complex (migmatite – gneiss complex) underlie the area. Ten marble bodies were ...

Evolução do perfil didático-pedagógico do professor-engenheiro

Directory of Open Access Journals (Sweden)

André Luiz Molisani

2016-09-01

Full Text Available Resumo Este trabalho é uma revisão bibliográfica, cujos objetivos são analisar e compreender a evolução do perfil didático-pedagógico do professor-engenheiro no Brasil. Identificou-se que o perfil didático-pedagógico não mudou ao longo da história dos cursos de engenharia. O método de ensino-aprendizagem é caracterizado por práticas tradicionais, que envolvem aulas expositivas e práticas laboratoriais, sendo o aluno avaliado por provas. Analogamente, o parque industrial brasileiro não apresentou mudanças significativas ao longo da história, sendo caracterizado pela reprodução de bens de consumo. Entretanto, o mercado empregador brasileiro impõe uma formação técnico-científica baseada em uma visão ética e humanística, que possibilite entender e desenvolver novas tecnologias, adquirir senso crítico e criativo, além de identificar e resolver problemas e demandas da sociedade. Essas competências profissionais são observadas apenas em países desenvolvidos que possuem uma educação de nível superior globalizada, que prioriza a mobilidade internacional de estudantes, professores e profissionais. Isso significa que as referidas competências são incompatíveis com a realidade brasileira que não pratica inovação tecnológica, centrando-se na reprodução de manufaturados. O governo tem implantado tanto legislações educacionais como programas de auxílio às indústrias com o intuito de atender às demandas do mercado empregador. Entretanto, os resultados foram insatisfatórios devido ao perfil reprodutivo do setor industrial. Contudo, o docente precisa adquirir novos métodos de ensino-aprendizagem, que possibilitem a construção ao invés da reprodução do conhecimento. Objetiva-se melhorar a aprendizagem do aluno, aprimorando sua capacitação profissional, o que resulta em avanço tecnológico, mesmo que seja no âmbito da reprodução de manufaturados.

Evolução do perfil didático-pedagógico do professor-engenheiro

Directory of Open Access Journals (Sweden)

André Luiz Molisani

Full Text Available Resumo Este trabalho é uma revisão bibliográfica, cujos objetivos são analisar e compreender a evolução do perfil didático-pedagógico do professor-engenheiro no Brasil. Identificou-se que o perfil didático-pedagógico não mudou ao longo da história dos cursos de engenharia. O método de ensino-aprendizagem é caracterizado por práticas tradicionais, que envolvem aulas expositivas e práticas laboratoriais, sendo o aluno avaliado por provas. Analogamente, o parque industrial brasileiro não apresentou mudanças significativas ao longo da história, sendo caracterizado pela reprodução de bens de consumo. Entretanto, o mercado empregador brasileiro impõe uma formação técnico-científica baseada em uma visão ética e humanística, que possibilite entender e desenvolver novas tecnologias, adquirir senso crítico e criativo, além de identificar e resolver problemas e demandas da sociedade. Essas competências profissionais são observadas apenas em países desenvolvidos que possuem uma educação de nível superior globalizada, que prioriza a mobilidade internacional de estudantes, professores e profissionais. Isso significa que as referidas competências são incompatíveis com a realidade brasileira que não pratica inovação tecnológica, centrando-se na reprodução de manufaturados. O governo tem implantado tanto legislações educacionais como programas de auxílio às indústrias com o intuito de atender às demandas do mercado empregador. Entretanto, os resultados foram insatisfatórios devido ao perfil reprodutivo do setor industrial. Contudo, o docente precisa adquirir novos métodos de ensino-aprendizagem, que possibilitem a construção ao invés da reprodução do conhecimento. Objetiva-se melhorar a aprendizagem do aluno, aprimorando sua capacitação profissional, o que resulta em avanço tecnológico, mesmo que seja no âmbito da reprodução de manufaturados.

O perfil dos cuidadores de pacientes pediátricos com fibrose cística

OpenAIRE

Alves, Stella Pegoraro; Bueno, Denise

2018-01-01

Resumo O objetivo desse estudo foi identificar o perfil do cuidador principal de pacientes pediátricos com Fibrose Cística (FC). Estudo transversal, descritivo e prospectivo, no qual foi realizado, durante consulta farmacêutica, entrevista com cuidadores de pacientes fibrocísticos acompanhados em um centro de referência de um Hospital Universitário do Sul do Brasil. Foram obtidas informações gerais sobre os cuidadores, sobre o entendimento da doença, os medicamentos em uso do paciente e a din...

Concentraciones de homocisteína y perfil lipídico en preeclámpticas

OpenAIRE

Reyna-Villasmil, Eduardo; Torres-Cepeda, Duly; Peña-Paredes, Elvia; Mejia-Montilla, Jorly; Reyna-Villasmil, Nadia; González-Rodríguez, Peggy

2008-01-01

El objetivo de la investigación fue comparar las concentraciones plasmáticas de homocisteína y perfil lipídico en preeclámpticas y controles además establecer la relación entre la homocisteína y las concentraciones de colesterol, triglicéridos y lipoproteínas. Setenta pacientes fueron seleccionadas y divididas en dos grupos, preeclámpticas (grupo A) y embarazadas normotensas (grupo B), consideradas como controles, estudiadas en forma consecutiva. Se midieron las concentraciones de colesterol ...

Perfiles motivacionales como combinación de expectativas de autoeficacia y metas académicas en estudiantes universitarios

Directory of Open Access Journals (Sweden)

Antonio Valle

2015-06-01

Full Text Available Adoptando un enfoque centrado en la persona, el presente trabajo de investigación tiene como principal objetivo identificar posibles perfiles motivacionales basándose en la combinación de metas académicas (orientadas al aprendizaje y orientadas al rendimiento y expectativas de autoeficacia. Bajo la hipótesis de que la implicación del alumno no solo depende de la combinación de metas de aprendizaje sino también del nivel de expectativas de autoeficacia, se encuesta a 1858 estudiantes de cinco universidades públicas españolas (con una media de edad de 21 años y distintas titulaciones. En la línea de investigaciones previas, los resultados indican que el perfil en el que predominan las metas de aprendizaje está asociado a mejores resultados que otros. Sin embargo, los resultados de esta investigación añaden información nueva, lo que sugiere que las expectativas de autoeficacia tienen un papel central en la relación entre metas y rendimiento.

Comparison of thermodynamic databases used in geochemical modelling

International Nuclear Information System (INIS)

Chandratillake, M.R.; Newton, G.W.A.; Robinson, V.J.

1988-05-01

Four thermodynamic databases used by European groups for geochemical modelling have been compared. Thermodynamic data for both aqueous species and solid species have been listed. When the values are directly comparable any differences between them have been highlighted at two levels of significance. (author)

Uruguay Mining inventory. Minas fotoplano geochemical prospecting results

International Nuclear Information System (INIS)

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

1982-01-01

This work is about the geochemical prospecting carried out in Minas fotoplano within the framework of Uruguay Mining inventory. In this work were covered 380 km2 obtaining with 433 samples for study which were analized by Plasma Emission Spectrometry in Orleans BRGM laboratories

Aplicación web sobre los diversos perfiles de mercado en las provincias de Canadá

OpenAIRE

Caicedo Castro, Paula Andrea; Argumedo, Juliana

2014-01-01

El proyecto de creación de una Aplicación web sobre los diferentes perfiles de mercado de las provincias canadienses, consiste en la recopilación de información de diversas fuentes académicas, con el fin de crear una guía electrónica que permita a los exportadores colombianos tener información precisa y actualizada sobre cada una de las provincias canadienses.

Neutron activation analysis of geochemical samples

International Nuclear Information System (INIS)

Rosenberg, R.; Zilliacus, R.; Kaistila, M.

1983-06-01

The present paper will describe the work done at the Technical Research Centre of Finland in developing methods for the large-scale activation analysis of samples for the geochemical prospecting of metals. The geochemical prospecting for uranium started in Finland in 1974 and consequently a manually operated device for the delayed neutron activation analysis of uranium was taken into use. During 1974 9000 samples were analyzed. The small capacity of the analyzer made it necessary to develop a completely automated analyzer which was taken into use in August 1975. Since then 20000-30000 samples have been analyzed annually the annual capacity being about 60000 samples when running seven hours per day. Multielemental instrumental neutron activation analysis is used for the analysis of more than 40 elements. Using instrumental epithermal neutron activation analysis 25-27 elements can be analyzed using one irradiation and 20 min measurement. During 1982 12000 samples were analyzed for mining companies and Geological Survey of Finland. The capacity is 600 samples per week. Besides these two analytical methods the analysis of lanthanoids is an important part of the work. 11 lanthanoids have been analyzed using instrumental neutron activation analysis. Radiochemical separation methods have been developed for several elements to improve the sensitivity of the analysis

Soil Iodine Determination in Deccan Syneclise, India: Implications for Near Surface Geochemical Hydrocarbon Prospecting

International Nuclear Information System (INIS)

Mani, Devleena; Kumar, T. Satish; Rasheed, M. A.; Patil, D. J.; Dayal, A. M.; Rao, T. Gnaneshwar; Balaram, V.

2011-01-01

The association of iodine with organic matter in sedimentary basins is well documented. High iodine concentration in soils overlying oil and gas fields and areas with hydrocarbon microseepage has been observed and used as a geochemical exploratory tool for hydrocarbons in a few studies. In this study, we measure iodine concentration in soil samples collected from parts of Deccan Syneclise in the west central India to investigate its potential application as a geochemical indicator for hydrocarbons. The Deccan Syneclise consists of rifted depositional sites with Gondwana–Mesozoic sediments up to 3.5 km concealed under the Deccan Traps and is considered prospective for hydrocarbons. The concentration of iodine in soil samples is determined using ICP-MS and the values range between 1.1 and 19.3 ppm. High iodine values are characteristic of the northern part of the sampled region. The total organic carbon (TOC) content of the soil samples range between 0.1 and 1.3%. The TOC correlates poorly with the soil iodine (r 2 < 1), indicating a lack of association of iodine with the surficial organic matter and the possibility of interaction between the seeping hydrocarbons and soil iodine. Further, the distribution pattern of iodine compares well with two surface geochemical indicators: the adsorbed light gaseous hydrocarbons (methane through butane) and the propane-oxidizing bacterial populations in the soil. The integration of geochemical observations show the occurrence of elevated values in the northern part of the study area, which is also coincident with the presence of exposed dyke swarms that probably serve as conduits for hydrocarbon microseepage. The corroboration of iodine with existing geological, geophysical, and geochemical data suggests its efficacy as one of the potential tool in surface geochemical exploration of hydrocarbons. Our study supports Deccan Syneclise to be promising in terms of its hydrocarbon prospects.

Establishing geochemical background levels of selected trace elements in areas having geochemical anomalies: The case study of the Orbetello lagoon (Tuscany, Italy)

International Nuclear Information System (INIS)

Romano, Elena; Bergamin, Luisa; Croudace, Ian W.; Ausili, Antonella; Maggi, Chiara; Gabellini, Massimo

2015-01-01

The determination of background concentration values (BGVs) in areas, characterised by the presence of natural geochemical anomalies and anthropogenic impact, appears essential for a correct pollution assessment. For this purpose, it is necessary to establish a reliable method for determination of local BGVs. The case of the Orbetello lagoon, a geologically complex area characterized by Tertiary volcanism, is illustrated. The vertical concentration profiles of As, Cd, Cr, Cu, Hg, Ni, Pb and Zn were studied in four sediment cores. Local BGVs were determined considering exclusively samples not affected by anthropogenic influence, recognized by means of multivariate statistics and radiochronological dating ( 137 Cs and 210 Pb). Results showed BGVs well-comparable with mean crustal or shale values for most of the considered elements except for Hg (0.87 mg/kg d.w.) and As (16.87 mg/kg d.w.), due to mineralization present in the catchment basin draining into the lagoon. - Highlights: • Pollution assessment in areas with geochemical anomalies needs local reference values. • A new method for the determination of background values (BGV) was established. • Geochemical data from unpolluted samples of sediment cores were used. • Statistics and geochronology were applied to recognize unpolluted sediments. • Anthropogenically influenced samples were not considered for BGV determination. - A method including multivariate statistics and radiochronological dating is proposed for determining local background values for trace elements using analytical data form sediment cores

Análisis del perfil de compuestos volátiles del mango (mangifera indica l. var. tommy atkins) tratado por métodos combinados

OpenAIRE

Moreno, Angélica; León, David F.; Giraldo, Germán A.; Ríos, Eunice

2010-01-01

Se evaluó el perfil de compuestos volátiles del mango (Mangifera indica L. Var. Tommy Atkins) al ser tratado con la combinación de los métodos de deshidratación osmótica con o sin pulso de vacío (DOPV y DO) y con secado por aire caliente o con vacío (SAC y VAC). El tiempo utilizado en la cinética del proceso de DO fue de 42 horas y la DOPV de 30 horas; en los procesos de secado, el SAC se realizó durante 24 horas y el VAC requirió 40 horas. En el perfil de compuestos volátiles del mango fresc...

Alteration and geochemical zoning in Bodie Bluff, Bodie mining district, eastern California

Science.gov (United States)

Herrera, P.A.; Closs, L.G.; Silberman, M.L.

1993-01-01

Banded, epithermal quartz-adularia veins have produced about 1.5 million ounces of gold and 7 million ounces of silver from the Bodie mining district, eastern California. The veins cut dacitic lava flows, pyroclastic rocks and intrusions. Sinter boulders occur in a graben structure at the top of Bodie Bluff and fragments of sinter and mineralized quartz veins occur in hydrothermal breccias nearby. Explosive venting evidently was part of the evolution of the ore-forming geothermal systems which, at one time, must had reached the paleosurface. Previous reconnaissance studies at Bodie Bluff suggested that the geometry of alteration mineral assemblages and distribution of some of the major and trace elements throughout the system correspond to those predicted by models of hot-spring, volcanic rock hosted precious metal deposits (Silberman, 1982; Silberman and Berger, 1985). The current study was undertaken to evaluate these sugestions further. About 500 samples of quartz veins and altered rocks, including sinter, collected over a vertical extent of 200 meters within Bodie Bluff were petrographically examined and chemically analyzed for trace elements by emission spectrographic and atomic absorption methods. Sixty-five samples were analyzed for major elements by X-ray fluorescence methods. The results of these analyses showed that, in general, alteration mineral assemblage and vertical geochemical zoning patterns follow those predicted for hot-spring deposits, but that geochemical zoning patterns for sinter and quartz veins (siliceous deposits), and altered wall rocks are not always similar. The predicted depth-concentration patterns for some elements, notably Au, Ag, Hg, and Tl in quartz veins, and Hg, As and Ag in wall rocks were not as expected, or were perturbed by the main ore producing zone. For both quartz veins and altered wall rocks, the main ore zone had elevated metal contents. Increased concentration of many of these elements could indicate proximity to this

Geochemical prospecting for rare earth elements using termite mound materials

Science.gov (United States)

Horiuchi, Yu; Ohno, Tetsuji; Hoshino, Mihoko; Shin, Ki-Cheol; Murakami, Hiroyasu; Tsunematsu, Maiko; Watanabe, Yasushi

2014-12-01

The Blockspruit fluorite prospect, located in North West State of the Republic of South Africa, occurs within an actinolite rock zone that was emplaced into the Kenkelbos-type granite of Proterozoic age. There are a large number of termite mounds in the prospect. For geochemical prospecting for rare earth elements (REEs), in total, 200 samples of termite mound material were collected from actinolite rock and granite zones in the prospect. Geochemical analyses of these termite mound materials were conducted by two methods: portable X-ray fluorescence (XRF) spectrometry and inductively coupled plasma-mass spectrometry (ICP-MS). Comparison of the two methods broadly indicates positive correlations of REEs (La, Ce, Pr, Nd, and Y), in particular Y and La having a strong correlation. As the result of modal abundance analyses, the actinolite rock at surface mainly consists of ferro-actinolite (89.89 wt%) and includes xenotime (0.26 wt%) and monazite (0.21 wt%) grains as REE minerals. Termite mound materials from actinolite rock also contain xenotime (0.27 wt%) and monazite (0.41 wt%) grains. In addition, termite mound materials from the actinolite rock zone have high hematite and Fe silicate contents compared to those from granite zone. These relationships suggest that REE minerals in termite mound materials originate form actinolite rock. Geochemical anomaly maps of Y, La, and Fe concentrations drawn based on the result of the portable XRF analyses show that high concentrations of these elements trend from SW to NE which broadly correspond to occurrences of actinolite body. These results indicate that termite mounds are an effective tool for REE geochemical prospection in the study area for both light REEs and Y, but a more detailed survey is required to establish the distribution of the actinolite rock body.

Linfoma não-Hodgkin em adultos: perfil proteico do LCR e do soro de 25 doentes

Directory of Open Access Journals (Sweden)

MIELLI SYLVIA REGINA

1998-01-01

Full Text Available Vinte e cinco pacientes com linfoma não-Hodgkin estudados para detecção de sinais e sintomas de comprometimento neurológico foram investigados quanto ao perfil proteico do líquido cefalorraqueano (LCR. Amostras de LCR e de soro sanguíneo colhidas no mesmo período foram estudadas comparativamente para analisar a barreira hemato-encefálica e a produção intratecal de IgG .Em 48% dos doentes foram registradas queixas e/ou sinais ao exame neurológico. A análise demonstrou: aumento das proteínas totais no LCR em 52%; imunoliberação local em um paciente HIV soropositivo; aumento de globulinas gama no LCR de dois pacientes na ausência de células neoplásicas no LCR e melhora clínica pós-quimioterapia; e registro de banda oligoclonal apenas no LCR em um doente HTLV-I soropositivo. Esses dados mostram que o estudo do perfil proteico no LCR contribui para a caracterização das manifestações do linfoma não-Hodgkin no sistema nervoso.

ACERCAMIENTO AL PERFIL DE USO DE TIC POR DOCENTES EN EL SECTOR RURAL COLOMBIANO

Directory of Open Access Journals (Sweden)

Dolly Vargas García

2015-12-01

Full Text Available El artículo pretende hacer un acercamiento al perfil, en cuanto al uso de las TIC, por parte de docentes de instituciones educativas ubicadas en el sector rural de cuatro departamentos colombianos (Caldas, Caucas, Huila y Nariño. Se inicia con un recorrido por la influencia de las TIC en el ámbito educativo, especialmente en cuanto al rol del docente en ese nuevo ambiente escolar. Luego se presenta la metodología utilizada en el estudio, para a continuación mostrar algunos resultados que concuerdan con trabajos anteriores en otros sitios y niveles académicos, sobre los aspectos indispensables para conformar el perfil del docente de la era informáticaApproach of ICT use profile by Colombian rural sector teachersABSTRACTThe article attempts approaching profile, in the use of ICT by teachers of educational institutions located in rural areas of four Colombian departments (Caldas, Cauca, Huila and Nariño. It begins with a tour of the influence of ICT in education, especially regarding the role of the teacher in the new school environment. Then it comes to the methodology used in the study, to then show some results are consistent with previous work on other sites and academic levels on the essential aspects to form the profile of teachers in the information age.Keywords: Use profile, ICT and education, Professor, Rural Area.

Mineralogical and geochemical studies of phosphorite nodules in ...

African Journals Online (AJOL)

Mineralogical and geochemical studies of phosphorite nodules in the Dange Formation Sokoto Basin, Northwestern Niveria. OA Adekeye, SO Akande. Abstract. No Abstract Available Journal of Mining and Geology Vol.40(2) 2004: 101-106. Full Text: EMAIL FULL TEXT EMAIL FULL TEXT · DOWNLOAD FULL TEXT ...

Geochemical assessment of light gaseous hydrocarbons in near ...

Indian Academy of Sciences (India)

Light hydrocarbons in soil have been used as direct indicators in geochemical hydrocarbon exploration, which remains an unconventional path in the petroleum industry. The occurrence of adsorbed soil ... Kalpana1 D J Patil1 A M Dayal1. National Geophysical Research Institute, Uppal Road, Hyderabad 500606, India.

Geochemical consequences of the Chernobyl accident.; Geokhimicheskie posledstviya Chernobyl`skoj katastrofy.

Energy Technology Data Exchange (ETDEWEB)

Kopejkin, V A [VNIIGEOLNERUD, Kazan` (Russian Federation)

1994-12-31

Geochemical features of Cs, Sr, U, Pu behaviour in the zone of their hypergenesis are presented in the article. Necessary conditions for these elements filtration on the natural geochemical barriers are shown. Data of radionuclide composition of water for five years of observation in << Ryzhiy Les >> and dissolved forms of radionuclides are described. Geologic and hydrogeologic conditions of the Chernobyl NPP site are shortly characterized. Radionuclide composition in the ground water of contaminated water pools is analyzed. It is proposed to cover by the law all {alpha}-elements (Pu, Am, Np) and not only plutonium as it currently takes place.

PHREEQCI; a graphical user interface for the geochemical computer program PHREEQC

Science.gov (United States)

Charlton, Scott R.; Macklin, Clifford L.; Parkhurst, David L.

1997-01-01

PhreeqcI is a Windows-based graphical user interface for the geochemical computer program PHREEQC. PhreeqcI provides the capability to generate and edit input data files, run simulations, and view text files containing simulation results, all within the framework of a single interface. PHREEQC is a multipurpose geochemical program that can perform speciation, inverse, reaction-path, and 1D advective reaction-transport modeling. Interactive access to all of the capabilities of PHREEQC is available with PhreeqcI. The interface is written in Visual Basic and will run on personal computers under the Windows(3.1), Windows95, and WindowsNT operating systems.

Perfil de temperatura dos funis magnetosféricos de estrelas T Tauri com aquecimento alfvênico

Science.gov (United States)

Vasconcelos, M. J.

2003-08-01

Estrelas T Tauri Clássicas são objetos jovens circundados por discos de gás e poeira e que apresentam uma intensa atividade magnética. Seu espectro mostra linhas de emissão alargadas que são razoavelmente reproduzidas nos modelos de acresção magnetosférica. No entanto, o perfil de temperatura dos funis magnéticos é desconhecido. Aquecimento magnético compressional e difusão ambipolar foram considerados para estas estruturas, porém as temperaturas obtidas não são suficientes para explicar as observações. Neste trabalho, examinamos o aquecimento gerado pelo amortecimento de ondas Alfvén através de quatro mecanismos, os amortecimentos não-linear, turbulento, viscoso-resistivo e colisional como função da freqüência da onda. Inicialmente, a temperatura é ajustada para reproduzir as observações e o grau de turbulência requerido para que o mecanismo seja viável é calculado. Os resultados mostram que este é compatível com os dados observacionais. Apresentam-se, também, resultados preliminares do cálculo auto-consistente do perfil de temperatura dos funis, levando-se em conta fontes de aquecimento Alfvênica e fontes de resfriamento.

Hydrologic-geochemical modeling needs for nuclear waste disposal systems performance assessments from the NEA perspective

International Nuclear Information System (INIS)

Muller, A.B.

1986-01-01

Credible scenarios for releases from high level nuclear waste repositories require radionuclides to be mobilized and transported by ground water. The capability to predict ground water flow velocities and directions as well as radionuclide concentrations in the flow system as a function of time are essential for assessing the performance of disposal systems. The first of these parameters can be estimated by hydrologic modeling while the concentrations can be predicted by geochemical modeling. The complementary use of empirical and phenomenological approaches to the geochemical modeling, when effectively coupled with hydrologic models can provide the tools needed for realistic performance assessment. An overview of the activities of the NEA in this area, with emphasis on the geochemical data bases (ISIRS for Ksub(d) data and the thermochemical data base critical review), rock/water interaction modeling (code development and short-courses), and hydrologic-geochemical code coupling (workshop and in-house activities) is presented in this paper from the perspective of probabilistic risk assessment needs. (author)

In situ geochemical properties of clays subject to thermal loading

International Nuclear Information System (INIS)

Chapman, N.A.

1980-01-01

Compositional variation and geochemical environment in an argillaceous unit are a function of age, depth of burial and mode of origin. This paper considers the variation limits likely to be encountered in potential repository host rocks and examines the significance of factors such as porosity, pore-fluid pressure, total fluid content, and major and accessory mineral component behaviors in controlling the geochemical environment in the neighbourhood of a thermally active waste canister. Particular attention is paid to the use of Eh-pH diagrams in assessing corrosion environments and nuclide speciation. The paper outlines the variables which must be considered when endeavouring to interpret such plots (e.g. temperature, concentration, concurrent reactions and probabilities) and uses the behavior of various iron minerals found in clay deposits under specific conditions to illustrate the complexities. The overall thermal stability of various clay and accessory minerals is discussed and extended to attempt to predict behavior under deep repository conditions, using available data on the diagenetic characteristics of clay-rich sediments. The physical behavior of fluids in plastic clays is considered and methods evaluated for deriving induced geochemical conditions in a thermally active repository. The latter section is particularly related to canister corrosion studies, in situ experiments, and waste dissolution parameters

Perfil del incendiario forestal español: aplicación del perfilamiento criminal inductivo

OpenAIRE

Sotoca, Andrés; González, José Luis; Fernández, Santiago; Kessel, Dominique; Montesinos, Olga; Ruíz, Miguel Ángel

2013-01-01

La técnica del perfil criminológico, entendida como el proceso de inferir características identificativas de un delincuente analizando las evidencias obtenidas en la escena del delito que ha cometido, ha recibido críticas por su dudoso carácter científico y su falta de apoyo teórico y empírico. No obstante, en la actualidad ha surgido un modelo que trabaja en la profesionalización del análisis del comportamiento delictivo en los cuerpos policiales mediante la aplicación de los conocimient...

Investigación perfil en competencias y habilidades del empresario bogotano: trabajo de campo

OpenAIRE

Granada Forero, José Andrés; Lara Salinas, Karen Eliana

2013-01-01

Este documento corresponde al trabajo de campo para la investigación doctoral de Luis Alberto Estrada titulado “Perfil en competencias del empresario bogotano”. El objetivo que el equipo de investigación definió fue concretar las habilidades y competencias que acompañan a los emprendedores y fundadores de empresa en la primera década del siglo XXI. Para ello, se tomó una base de datos de la Cámara de Comercio de Bogotá, la cual contiene la información comercial de las empresas de la ciudad...

Geochemical and Isotopic Interpretations of Groundwater Flow in the Oasis Valley Flow System, Southern Nevada

International Nuclear Information System (INIS)

Thomas, J.M.; Benedict, F.C. Jr.; Rose, T.P.; Hershey, R.L.; Paces, J.B.; Peterman, Z.E.; Farnham, I.M.; Johannesson, K.H.; Singh, A.K.; Stetzenbach, K.J.; Hudson, G.B.; Kenneally, J.M.; Eaton, G.F.; Smith, D.K.

2003-01-01

This report summarizes the findings of a geochemical investigation of the Pahute Mesa-Oasis Valley groundwater flow system in southwestern Nevada. It is intended to provide geochemical data and interpretations in support of flow and contaminant transport modeling for the Western and Central Pahute Mesa Corrective Action Units

Perfil epidemiológico de los eventos atendidos en prácticas asistenciales de fisioterapia de una institución universitaria en el año 2013

OpenAIRE

Sandoval-Cuellar, Carolina; Cobo-Mejía, Elisa Andrea

2016-01-01

Introducción: La epidemiología busca reconocer los eventos de salud-enfermedad en un grupo humano, así permite a través de perfiles epidemiológicos caracterizar poblaciones objeto de atención desde tipologías sociodemográficas, de atención y condiciones de salud. Objetivo: Describir el perfil epidemiológico de los eventos que se atienden en las prácticas asistenciales de 8 y 9 semestres de Fisioterapia de una Institución de Educación Superior en el año 2013. Metodología: Estudio observacional...

Elaboração de perfil psicológico de autores de homicídios através da avaliação da cena do crime

OpenAIRE

Silveira, Leon Murelli

2013-01-01

Este trabalho busca trazer a discussão acadêmica sobre o Perfil Criminal para a realidade brasileira. Para iniciar esse debate aqui, foi abordado o que se entende hoje por Perfil Criminal. Segue-se então com um levantamento da evolução histórica da técnica e tentativas semelhantes. Isto é indispensável tanto para sua definição, diferenciando-a das outras, como para sua implementação consciente que evite a repetição de erros passados. A partir disto aprofunda-se no debate acadêmico com o que h...

Geochemical reactivity of rocks of the Czech Republic

Czech Academy of Sciences Publication Activity Database

Chuman, T.; Gürtlerová, P.; Hruška, Jakub; Adamová, M.

2014-01-01

Roč. 10, č. 2 (2014), s. 341-349 ISSN 1744-5647 R&D Projects: GA MŠk(CZ) ED1.1.00/02.0073 Institutional support: RVO:67179843 Keywords : geochemical reactivity * Czech Republic * susceptibility to weathering Subject RIV: EH - Ecology, Behaviour Impact factor: 1.193, year: 2014

Geochemical maps of stream sediments in central Colorado, from New Mexico to Wyoming

Science.gov (United States)

Eppinger, Robert G.; Giles, Stuart A.; Klein, Terry L.

2015-01-01

The U.S. Geological Survey has completed a series of geologic, mineral resource, and environmental assessment studies in the Rocky Mountains of central Colorado, from Leadville eastward to the range front and from New Mexico to the Wyoming border. Regional stream-sediment geochemical maps, useful for assessing mineral resources and environmental effects of historical mining activities, were produced as part of the study. The data portrayed in this 56-parameter portfolio of landscape geochemical maps serve as a geochemical baseline for the region, indicate element abundances characteristic of various lithologic terranes, and identify gross anthropogenic effects of historical mining. However, although reanalyzed in this study by modern, sensitive methods, the majority of the stream-sediment samples were collected in the 1970s. Thus, metal concentrations portrayed in these maps represent stream-sediment geochemistry at the time of collection.

Perfil electroforético de las proteínas de la seta comestible "Coprinus comatus"

OpenAIRE

González Rodríguez, Andrea

2017-01-01

Este trabajo consiste en un estudio experimental del perfil proteico del hongo comestible Coprinus comatus, muy relevante por su alto valor económico y gastronómico, debido a sus propiedades nutricionales y medicinales. Los hongos son considerados alimentos funcionales, pues además de sus propiedades nutricionales, se han demostrado sus efectos beneficiosos para la salud que pueden ser utilizados en la prevención o tratamiento de enfermedades. Su acción terapéutica es atribuida a los compuest...

Catahoula formation of the Texas coastal plain: origin, geochemical evolution, and characteristics of uranium deposits

International Nuclear Information System (INIS)

Galloway, W.E.; Kaiser, W.R.

1979-01-01

Uranium was released from volcanic glass deposited within the Catahoula through early pedogenic and diagenetic processes. Pedogenesis was the most efficient process for mobilizing uranium. Original uranium content in fresh Catahoula glass is estimated to have averaged at least 10 ppM; about 5 ppM was mobilized after deposition and made available for migration. Uranium was transported predominantly as uranyl dicarbonate ion. Chlorinity mapping reveals modern ground-water flow patterns. Six utranium deposits representative of the ores were studied. Uranium-bearing meteoric waters were reduced by pre-ore stage pyrite formed by extrinsically introduced fault-leaked sulfide or intrinsically by organic matter. Uranium was concentrated in part by adsorption on Ca-montmorillonite cutans, amorphous TiO 2 , and/or organic matter followed by uranyl reduction to U 4+ in amorphous uranous silicates. Clinoptilolite is not correlative with mineralization. Calcite is pervasive throughout host sands but shows no relationship to uranium mineralization. Presence of marcasite and uranium together at the alteration front strongly supports an acid pH during Catahoula mineralization. Maximum adsorption and minimum solubility of uranium occur at pH 6 in carbonate-rich waters. Log activity ratios of individual waters supersaturated with respect to montmorillonite, taken from montmorillonite-clinoptilolite activity diagrams, show positive correlation with uranium mineralization. High Ca 2+ , Mg 2+ , Al(OH) 4 - , and H + activities promote the formation of montmorillonite relative to clinoptilolite. High saturation ratios for montmorillonite show fair correlation with mineralization. The mineral-solution equilibria approach is a potential method of geochemical exploration. 56 figures, 8 tables

Perfil lipídico sérico de ratos tratados com surfactante

Directory of Open Access Journals (Sweden)

Karina Ferreira de Castro

2012-06-01

Full Text Available A aterosclerose é uma doença multifatorial, lenta e progressiva e a hiperlipidemia um dos fatores potenciais no desenvolvimento de doenças cardíacas ateroscleróticas. As vantagens da indução das dislipidemias experimentais são a produção de lesões ateromatosas em curto espaço de tempo; adequado controle dietético e fatores ambientais; a possibilidade de estudos sobre a reversibilidade de lesões ateroscleróticas e ensaios pré-clínicos de substâncias hipolipidêmicas. Este estudo visou avaliar o perfil lipídico sérico de ratos tratados com surfactante. Foram utilizados 28 ratos Wistar, machos, albinos, adultos e hígidos. Estes foram distribuídos em quatro grupos experimentais formados por sete animais cada, a saber: Grupo I – (controle; Grupo II – tratado com tyloxapol, na dose de 500 mg/kg de peso corporal, via intraperitoneal a cada 48 horas, durante duas semanas; Grupo III – tratado com tyloxapol na dose de 500 mg/kg de peso corporal, via intraperitoneal a cada 48 horas, durante três semanas; Grupo IV – tratado com tyloxapol na dose de 500 mg/kg de peso corporal, via intraperitoneal a cada 48 horas, durante quatro semanas. Na avaliação do perfil lipídico, os valores de triacilgliceróis e HDL demonstraram que o grupo III diferiu significativamente do grupo I e os valores de colesterol total e LDL indicaram que o grupo I diferiu significativamente dos grupos II, III e IV. Conclui-se que o surfactante tyloxapol foi efetivo na indução da hiperlipidemia.

Geochemical indicators of gold ore fields

International Nuclear Information System (INIS)

Shcherbakov, Yu.G.

1995-01-01

The principles of selection of indicators for genetic reconstructions and prognostic valuations of gold mineralization of diverse morphological and geochemical types have been substantiated. The neutron-activation analysis with radiochemical separation and detection limit of 1-10 -8 %, instrumental neutron-activation analysis and atomic-absorption analysis are the main methods of determination of gold low contents in the rocks, as well as diverse elements, including transition, rare earth elements and tellurium, in gold. 50 refs.; 1 fig.; 3 tabs

Lead transport in intra-oceanic subduction zones: 2D geochemical-thermo-mechanical modeling of isotopic signatures

NARCIS (Netherlands)

Baitsch-Ghirardello, B.; Stracke, A.; Connolly, J.A.D.; Nikolaeva, K.M.; Gerya, T.V.

2014-01-01

Understanding the physical-chemical mechanisms and pathways of geochemical transport in subduction zones remains a long-standing goal of subduction-related research. In this study, we perform fully coupled geochemical-thermo-mechanical (GcTM) numerical simulations to investigate Pb isotopic

Evolution of chemical and isotopic composition of inorganic carbon in a complex semi-arid zone environment: Consequences for groundwater dating using radiocarbon

Science.gov (United States)

Meredith, K. T.; Han, L. F.; Hollins, S. E.; Cendón, D. I.; Jacobsen, G. E.; Baker, A.

2016-09-01

Estimating groundwater age is important for any groundwater resource assessment and radiocarbon (14C) dating of dissolved inorganic carbon (DIC) can provide this information. In semi-arid zone (i.e. water-limited environments), there are a multitude of reasons why 14C dating of groundwater and traditional correction models may not be directly transferable. Some include; (1) the complex hydrological responses of these systems that lead to a mixture of different ages in the aquifer(s), (2) the varied sources, origins and ages of organic matter in the unsaturated zone and (3) high evaporation rates. These all influence the evolution of DIC and are not easily accounted for in traditional correction models. In this study, we determined carbon isotope data for; DIC in water, carbonate minerals in the sediments, sediment organic matter, soil gas CO2 from the unsaturated zone, and vegetation samples. The samples were collected after an extended drought, and again after a flood event, to capture the evolution of DIC after varying hydrological regimes. A graphical method (Han et al., 2012) was applied for interpretation of the carbon geochemical and isotopic data. Simple forward mass-balance modelling was carried out on key geochemical processes involving carbon and agreed well with observed data. High values of DIC and δ13CDIC, and low 14CDIC could not be explained by a simple carbonate mineral-CO2 gas dissolution process. Instead it is suggested that during extended drought, water-sediment interaction leads to ion exchange processes within the top ∼10-20 m of the aquifer which promotes greater calcite dissolution in saline groundwater. This process was found to contribute more than half of the DIC, which is from a mostly 'dead' carbon source. DIC is also influenced by carbon exchange between DIC in water and carbonate minerals found in the top 2 m of the unsaturated zone. This process occurs because of repeated dissolution/precipitation of carbonate that is dependent on

Geochemical databases. Part 1. Pmatch: a program to manage thermochemical data. Part 2. The experimental validation of geochemical computer models

International Nuclear Information System (INIS)

Pearson, F.J. Jr.; Avis, J.D.; Nilsson, K.; Skytte Jensen, B.

1993-01-01

This work is carried out under cost-sharing contract with European Atomic Energy Community in the framework of its programme on Management and Storage of Radioactive Wastes. Part 1: PMATCH, A Program to Manage Thermochemical Data, describes the development and use of a computer program, by means of which new thermodynamic data from literature may be referenced to a common frame and thereby become internally consistent with an existing database. The report presents the relevant thermodynamic expressions and their use in the program is discussed. When there is not sufficient thermodynamic data available to describe a species behaviour under all conceivable conditions, the problems arising are thoroughly discussed and the available data is handled by approximating expressions. Part II: The Experimental Validation of Geochemical Computer models are the results of experimental investigations of the equilibria established in aqueous suspensions of mixtures of carbonate minerals (Calcium, magnesium, manganese and europium carbonates) compared with theoretical calculations made by means of the geochemical JENSEN program. The study revealed that the geochemical computer program worked well, and that its database was of sufficient validity. However, it was observed that experimental difficulties could hardly be avoided, when as here a gaseous component took part in the equilibria. Whereas the magnesium and calcium carbonates did not demonstrate mutual solid solubility, this produced abnormal effects when manganese and calcium carbonates were mixed resulting in a diminished solubility of both manganese and calcium. With tracer amounts of europium added to a suspension of calcite in sodium carbonate solutions long term experiments revealed a transition after 1-2 months, whereby the tracer became more strongly adsorbed onto calcite. The transition is interpreted as the nucleation and formation of a surface phase incorporating the 'species' NaEu(Co 3 ) 2

Geochemical reanalysis of historical U.S. Geological Survey sediment samples from the Zane Hills, Hughes and Shungnak quadrangles, Alaska

Science.gov (United States)

Werdon, Melanie B.; Granitto, Matthew; Azain, Jaime S.

2015-01-01

The State of Alaska’s Strategic and Critical Minerals (SCM) Assessment project, a State-funded Capital Improvement Project (CIP), is designed to evaluate Alaska’s statewide potential for SCM resources. The SCM Assessment is being implemented by the Alaska Division of Geological & Geophysical Surveys (DGGS), and involves obtaining new airborne-geophysical, geological, and geochemical data. As part of the SCM Assessment, thousands of historical geochemical samples from DGGS, U.S. Geological Survey (USGS), and U.S. Bureau of Mines archives are being reanalyzed by DGGS using modern, quantitative, geochemical-analytical methods. The objective is to update the statewide geochemical database to more clearly identify areas in Alaska with SCM potential.The USGS is also undertaking SCM-related geologic studies in Alaska through the federally funded Alaska Critical Minerals cooperative project. DGGS and USGS share the goal of evaluating Alaska’s strategic and critical minerals potential and together created a Letter of Agreement (signed December 2012) and a supplementary Technical Assistance Agreement (#14CMTAA143458) to facilitate the two agencies’ cooperative work. Under these agreements, DGGS contracted the USGS in Denver to reanalyze historical USGS sediment samples from Alaska.For this report, DGGS funded reanalysis of 105 historical USGS sediment samples from the statewide Alaska Geochemical Database Version 2.0 (AGDB2; Granitto and others, 2013). Samples were chosen from the Zane Hills area in the Hughes and Shungnak quadrangles, Alaska (fig. 1). The USGS was responsible for sample retrieval from the National Geochemical Sample Archive (NGSA) in Denver, Colorado through the final quality assurance/quality control (QA/QC) of the geochemical analyses obtained through the USGS contract lab. The new geochemical data are published in this report as a coauthored DGGS report, and will be incorporated into the statewide geochemical databases of both agencies.

Research on geochemical exploration in geotherm development

International Nuclear Information System (INIS)

Hirowatari, Kazuo; Imaizumi, Yukio; Koga, Akito; Iwanaga, Tatsuto.

1987-01-01

The decisive factor of geotherm development is to improve the exploration techniques. By effectively carrying out the selection of promising development spots and the decision of well drilling positions, the geotherm development exceeding existing energy sources becomes feasible. There have been many problems in conventional geotherm exploration such as the high cost and long work period, therefore, it was decided to advance the research on geochemical exploration techniques which are relatively simple and can be carried out with low cost. When the techniques of geochemistry are used, for example, in the case that there are hot springs or fumaroles, the temperature, origin, properties and so on of underground hot water reservoirs can be estimated from their chemical composition. The method of examining the mercury concentration in soil and soil air has been in practical use in the geothermal districts where the ground surface symptom lacks. This time, the method of investigation using radon, thoron and gamma ray as the exploration indices was newly studied. The index compositions for geochemical exploration, new exploration index compositions, the method of measurement, the basic investigation and on-the-spot investigation are reported. (Kako, I.)

Análise de sensibilidade no processamento de dados de experimentos de perfil instantâneo

Directory of Open Access Journals (Sweden)

Q. de Jong van Lier

2002-12-01

Full Text Available Dentre as propriedades físicas do solo, a condutividade hidráulica é uma das mais importantes, quando se estudam fenômenos que estão ligados ao movimento da água no solo. O método para determinar a função condutividade hidráulica versus umidade ou função K(θ de um solo, denominada método de perfil instantâneo, tem como maior vantagem o fato de se basear em medições diretas no campo, sem necessidade de aguardar o estabelecimento de um equilíbrio dinâmico. No caso de experimentos desse tipo, não se conhecem estudos sobre sua sensibilidade em relação a erros nos dados experimentais; tampouco se conhece a influência que uma observação experimental a mais ou a menos possa ter sobre a parametrização da função K(θ O presente trabalho visou analisar a sensibilidade do método de perfil instantâneo a variações nas observações realizadas in situ Utilizaram-se dados de dois experimentos de perfil instantâneo realizados no campus "Luiz de Queiroz", da Universidade de São Paulo, em Piracicaba (SP. Por meio de um algoritmo computacional para a análise dos dados experimentais, verificou-se a sensibilidade do resultado do cálculo dos parâmetros da função K(θ para variações nos valores de entrada. Foi analisado o efeito das seguintes alterações no conjunto original de dados: retirada de uma leitura completa do conjunto de dados; retirada de leituras finais; erro no coeficiente angular de calibração do TDR; erro no intercepto da curva de calibração do TDR; erro em uma das leituras do TDR. Pelos resultados do levantamento, concluiu-se que o método do perfil instantâneo, conjuntamente com a rotina computacional utilizada para processar os valores observados no campo, apresenta alta sensibilidade a pequenas incertezas no ajuste de funções aos valores da umidade Versus tempo; é também muito sensível à leitura do tempo zero, que, portanto, deveria ser desconsiderada. Erros ou incertezas nos ajustes dos valores

Geochemical Relationships between Volcanic and Plutonic Upper to Mid Crustal Exposures of the Rosario Segment, Alisitos Arc (Baja California, Mexico): An Outstanding Field Analog to the Izu-Bonin-Mariana Arc

Science.gov (United States)

Morris, R.; DeBari, S. M.; Busby, C. J.; Medynski, S.

2015-12-01

Exposed paleo-arcs, such as the Rosario segment of the Cretaceous Alisitos Arc in Baja California, Mexico, provide an opportunity to explore the evolution of arc crust through time. Remarkable 3-D exposures of the Rosario segment record crustal generation processes in the volcanic rocks and underlying plutonic rocks. In this study, we explore the physical and geochemical connection between the plutonic and volcanic sections of the extensional Alisitos Arc, and elucidate differentiation processes responsible for generating them. These results provide an outstanding analog for extensional active arc systems, such as the Izu-Bonin-Mariana (IBM) Arc. Upper crustal volcanic rocks have a coherent stratigraphy that is 3-5 km thick and ranges in composition from basalt to dacite. The most felsic compositions (70.9% SiO2) are from a welded ignimbrite unit. The most mafic compositions (51.5% SiO2, 3.2% MgO) are found in basaltic sill-like units. Phenocrysts in the volcanic units include plagioclase +/- amphibole and clinopyroxene. The transition to deeper plutonic rocks is clearly an intrusive boundary, where plutonic units intrude the volcanic units. Plutonic rocks are dominantly a quartz diorite main phase with a more mafic, gabbroic margin. A transitional zone is observed along the contact between the plutonic and volcanic rocks, where volcanics have coarsely recrystallized textures. Mineral assemblages in the plutonic units include plagioclase +/- quartz, biotite, amphibole, clinopyroxene and orthopyroxene. Most, but not all, samples are low K. REE patterns are relatively flat with limited enrichment. Normalization diagrams show LILE enrichment and HFSE depletion, where trends are similar to average IBM values. We interpret plutonic and volcanic units to have similar geochemical relationships, where liquid lines of descent show the evolution of least to most evolved magma types. We provide a model for the formation and magmatic evolution of the Alisitos Arc.

Convergencia Europea y profesorado. Hacia un nuevo perfil para el aprendizaje flexible

Directory of Open Access Journals (Sweden)

Mª OLGA ESCANDELL BERMÚDEZ

2005-01-01

práctica, de la profesión docente, de la cultura del profesorado universitario, de sus competencias y su saber hacer. Su actuación profesional ha de ajustarse a unas exigencias de calidad que demandan un fuerte compromiso personal y laboral que pasa, sin duda, por aceptar que el EEES supondrá un cambio sustancial del proceso de enseñanza-aprendizaje convencional y electrónico (e-learning; en los perfiles profesionales que tendrán que adaptarse a las demandas crecientes de una sociedad de la información y del conocimiento y, también, en la forma de concebir la formación a lo largo de la vida (long life learning.

Using ASCEM Modeling and Visualization to Inform Stakeholders of Contaminant Plume Evolution and Remediation Efficacy at F-Basin Savannah River, SC – 15156

Energy Technology Data Exchange (ETDEWEB)

Flach, G. [Lawrence Berkeley National Lab. (LBNL), Berkeley, CA (United States); Wainwright, H. [Lawrence Berkeley National Lab. (LBNL), Berkeley, CA (United States); Molins, S. [Lawrence Berkeley National Lab. (LBNL), Berkeley, CA (United States); Davis, J. [Lawrence Berkeley National Lab. (LBNL), Berkeley, CA (United States); Arora, B. [Lawrence Berkeley National Lab. (LBNL), Berkeley, CA (United States); Faybishenko, B. [Lawrence Berkeley National Lab. (LBNL), Berkeley, CA (United States); Krishnan, H. [Lawrence Berkeley National Lab. (LBNL), Berkeley, CA (United States); Hubbard, S. [Lawrence Berkeley National Lab. (LBNL), Berkeley, CA (United States); Flach, G. [Savannah River Site (SRS), Aiken, SC (United States). Savannah River National Lab. (SRNL); Denham, M. [Savannah River Site (SRS), Aiken, SC (United States). Savannah River National Lab. (SRNL); Eddy-Dilek, C. [Savannah River Site (SRS), Aiken, SC (United States). Savannah River National Lab. (SRNL); Moulton, D. [Los Alamos National Lab. (LANL), Los Alamos, NM (United States); Lipnikov, K. [Los Alamos National Lab. (LANL), Los Alamos, NM (United States); Gable, C. [Los Alamos National Lab. (LANL), Los Alamos, NM (United States); Miller, T. [Los Alamos National Lab. (LANL), Los Alamos, NM (United States); Freshley, M. [Pacific Northwest National Lab. (PNNL), Richland, WA (United States)

2015-01-28

Communication with stakeholders, regulatory agencies, and the public is an essential part of implementing different remediation and monitoring activities, and developing site closure strategies at contaminated sites. Modeling of contaminant plume evolution plays a critical role in estimating the benefit, cost, and risk of particular options. At the same time, effective visualization of monitoring data and modeling results are particularly important for conveying the significance of the results and observations. In this paper, we present the results of the Advanced Simulation Capability for Environmental Management (ASCEM) project, including the discussion of the capabilities of newly developed ASCEM software package, along with its application to the F-Area Seepage Basins located in the U.S. Department of Energy Savannah River Site (SRS). ASCEM software includes state-of-the-art numerical methods for simulating complex flow and reactive transport, as well as various toolsets such as a graphical user interface (GUI), visualization, data management, uncertainty quantification, and parameter estimation. Using this software, we have developed an advanced visualization of tritium plume migration coupled with a data management system, and simulated a three-dimensional model of flow and plume evolution on a high-performance computing platform. We evaluated the effect of engineered flow barriers on a nonreactive tritium plume, through advanced plume visualization and modeling of tritium plume migration. In addition, we developed a geochemical reaction network to describe complex geochemical processes at the site, and evaluated the impact of coupled hydrological and geochemical heterogeneity. These results are expected to support SRS’s monitoring activities and operational decisions.

Geochemical studies of potential source minerals of radon: case studies in Hungary

Energy Technology Data Exchange (ETDEWEB)

Rajnai, G.; Nagy-Balogh, J.; Gal-Solymos, K.; Konc, Z.; Breitner, D.; Barabas, A.; Szabo, C. [Eotvos Univ., Lithosphere Fluid Research Lab, Dept. of Petrology and Geochemistry, Budapest (Hungary); Barabas, A. [Eotvos Univ., Dept. of Geophysics, Budapest (Hungary)

2006-07-01

In Hungary, during the past decade five distinct regions have been chosen to find possible explanations of the uncommonly high radon background radiation values. The main aim of the research is to study U- and Th-bearing minerals in petrographic and geochemical characters. Besides the microscopic techniques, whole rock and in situ geochemical analytical methods were applied to determine the bulk U and Th content of the studied geological samples. We assume that some of the radon measured is related to the U and Th contents of the samples. (authors)

Geochemical properties and nuclear chemical characteristics of Oklo natural fission reactors

Energy Technology Data Exchange (ETDEWEB)

Hidaka, Hiroshi [Hiroshima Univ., Higashi-Hiroshima (Japan). Faculty of Science

1997-07-01

There are six uranium deposits in the Gabonese Republic in the cnetral Africa. `Fission reactor zone`, the fission chain reactions generated about 200 billion years ago, was existed in a part of them. CEA begun geochemical researches of Oklo deposits etc. in 1991. The geochemical and nuclear chemical properties of Oklo were reviewed from the results of researches. Oklo deposits is consisted of main five sedimentary faces such as sandstone (FA), Black Shale formation (FB), mudstone (FC), tuff (FD) and volcaniclastic sandstone (FE) from the bottom on the base rock of granite in the Precambrian era. Uranium is enriched in the upper part of FA layer and the under part of FB layer. {sup 235}U/{sup 238}U, U content, fission proportion, duration time, neutron fluence, temperature, restitution factor of {sup 235}U and epithermal index ({gamma}) were investigated and compared. The geochemical properties of Oklo are as followed: large enrich of uranium, the abundance ratio of {sup 235}U as same as that of enriched uranium, interaction of natural water and small rear earth elements. These factors made casually Oklo fission reactor. (S.Y.)

Establishing nursery estuary otolith geochemical tags for Sea Bass (Dicentrarchus labrax): Is temporal stability estuary dependent?

Science.gov (United States)

Ryan, Diarmuid; Wögerbauer, Ciara; Roche, William

2016-12-01

The ability to determine connectivity between juveniles in nursery estuaries and adult populations is an important tool for fisheries management. Otoliths of juvenile fish contain geochemical tags, which reflect the variation in estuarine elemental chemistry, and allow discrimination of their natal and/or nursery estuaries. These tags can be used to investigate connectivity patterns between juveniles and adults. However, inter-annual variability of geochemical tags may limit the accuracy of nursery origin determinations. Otolith elemental composition was used to assign a single cohort of 0-group sea bass Dicentrarchus labrax to their nursery estuary thus establishing an initial baseline for stocks in waters around Ireland. Using a standard LDFA model, high classification accuracies to nursery sites (80-88%) were obtained. Temporal stability of otolith geochemical tags was also investigated to assess if annual sampling is required for connectivity studies. Geochemical tag stability was found to be strongly estuary dependent.

A preliminary report of geochemical investigations in the Blackbird District

Science.gov (United States)

Canney, F.C.; Hawkes, H.E.; Richmond, G.M.; Vhay, J. S.

1953-01-01

This paper reviews an experimental geochemical prospecting survey in the Blackbird cobalt-copper mining district. The district is in east-central Idaho, about 20 miles west-southwest of Salmon. The area is one of deeply weathered nearly flat-topped upland surfaces cut by steep-walled valleys which are tributary to the canyon of Panther Creek. Most of the area has a relatively heavy vegetative cover, and outcrops are scarce except on the sides of the steeper valleys* Because of the importance of the surficial deposits and soils and the physiographic history of the region on the interpretation of the geochemical data, a separate chapter on this subject by Gerald H. Richmond follows the following brief description of the geology of the district.

Perfil metabólico de vacas Jersey clinicamente saudáveis

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Paula B. de Alvarenga

Full Text Available RESUMO: O conhecimento do metabolismo dos animais é de suma importância para se obter sucesso em qualquer atividade que envolva rebanhos. Objetivou-se determinar o perfil bioquímico sérico de vacas Jersey clinicamente saudáveis no pré e pós-parto, mantidas em sistema de criação semi-intensivo na região de Uberlândia, Minas Gerais, Brasil. Realizou-se o exame clínico e coleta de sangue de 40 vacas da raça Jersey multíparas e lactantes em 15 momentos, entre -150 dias pré-parto até 60 dias pós-parto (DPP. No laboratório, foram analisadas as concentrações séricas de proteínas totais, albumina, globulinas, ureia, creatinina, ácidos graxos não esterificados (NEFA, β-hidroxibutirato (BHBA, triglicerídeos, colesterol, lipoproteínas de alta densidade (HDL, lipoproteínas de muita baixa densidade (VLDL, lipoproteínas de baixa densidade (LDL, aspartato aminotransferase (AST, gama-glutamil transferase (GGT, creatina quinase (CK, cálcio, fósforo e magnésio. Dos 40 animais, apenas 21 vacas atenderam aos critérios de inclusão e seus dados foram utilizados. Procedeu-se o teste de Tukey para os dados paramétricos e para os dados não paramétricos realizou-se o teste de Kruskal Wallis na comparação entre os momentos avaliados. Não houve interferência do balanço energético negativo e da hipocalcemia subclínica na ocorrência de doenças uterinas e no desempenho reprodutivo. Concluiu-se que vacas da raça Jersey apresentam perfil bioquímico caracterizado por hiperglobulinemia durante o periparto, além de níveis elevados de triglicérides, entretanto, sem comprometimento da função hepática e desempenho reprodutivo.

Overview of the geochemical code MINTEQ: applications to performance assessment for low-level wastes

International Nuclear Information System (INIS)

Graham, M.J.; Peterson, S.R.

1985-09-01

The MINTEQ geochemical computer code, developed at Pacific Northwest Laboratory, integrates many of the capabilities of its two immediate predecessors, WATEQ3 and MINEQL. MINTEQ can be used to perform the calculations necessary to simulate (model) the contact of low-level waste solutions with heterogeneous sediments or the interaction of ground water with solidified low-level wastes. The code is capable of performing calculations of ion speciation/solubility, adsorption, oxidation-reduction, gas phase equilibria, and precipitation/dissolution of solid phases. Under the Special Waste Form Lysimeters-Arid program, the composition of effluents (leachates) from column and batch experiments, using laboratory-scale waste forms, will be used to develop a geochemical model of the interaction of ground water with commercial solidified low-level wastes. The wastes being evaluated include power reactor waste streams that have been solidified in cement, vinyl ester-styrene, and bitumen. The thermodynamic database for the code is being upgraded before the geochemical modeling is performed. Thermodynamic data for cobalt, antimony, cerium, and cesium solid phases and aqueous species are being added to the database. The need to add these data was identified from the characterization of the waste streams. The geochemical model developed from the laboratory data will then be applied to predict the release from a field-lysimeter facility that contains full-scale waste samples. The contaminant concentrations migrating from the wastes predicted using MINTEQ will be compared to the long-term lysimeter data. This comparison will constitute a partical field validation of the geochemical model. 28 refs

Report on the geological-geochemical research carried out within the area of geochemical anomaly P7, Vathyrema, Drama Department

International Nuclear Information System (INIS)

Stavropoulos, Athanasios.

1982-08-01

The investigated area covering about 30 km 2 is situated in the crystalline massive of Rhodope (north of Drama deparment, E. Macedonia) where granitoids constitute its main petrological type. The geological-geochemical and radiometric investigations carried out so far in the area have localized a large number of places with high values of γ-radiation (1.000 - 15.000 c/s), as well as high concentrations of uranium (50-500 ppm). The uranium mineralization within the zone of oxidation is expressed by the uranium mineral autunite, accompanied by intensive hematitization-limonitization and chloritization-kaolinization, and additionally by small spots and veinlets of pyrite and galena. It seems that tectonic control exists on the uranium mineralization, since most of the anomalous concentrations of uranium are sitting along mylonite zones rich in chlorite and kaolin. There have been discerned seven more anomalous part areas which will have to be covered by geochemical stream sediment sampling (phase 3), as well as geological mapping (scale 1:5.000). The results from the research conducted within the concerned anomaly lead us to the conclusion that this area is very promising and possibilities of localization of uranium payable concentrations are very high. (N.Ch.)

An integrated geophysical and geochemical exploration of critical zone weathering on opposing montane hillslope

Science.gov (United States)

Singha, K.; Navarre-Sitchler, A.; Bandler, A.; Pommer, R. E.; Novitsky, C. G.; Holbrook, S.; Moore, J.

2017-12-01

Quantifying coupled geochemical and hydrological properties and processes that operate in the critical zone is key to predicting rock weathering and subsequent transmission and storage of water in the shallow subsurface. Geophysical data have the potential to elucidate geochemical and hydrologic processes across landscapes over large spatial scales that are difficult to achieve with point measurements alone. Here, we explore the connections between weathering and fracturing, as measured from integrated geochemical and geophysical borehole data and seismic velocities on north- and south-facing aspects within one watershed in the Boulder Creek Critical Zone Observatory. We drilled eight boreholes up to 13 m deep on north- and south-facing aspects within Upper Gordon Gulch, and surface seismic refraction data were collected near these wells to explore depths of regolith and bedrock, as well as anisotropic characteristics of the subsurface material due to fracturing. Optical televiewer data were collected in these wells to infer the dominant direction of fracturing and fracture density in the near surface to corroborate with the seismic data. Geochemical samples were collected from four of these wells and a series of shallow soil pits for bulk chemistry, clay fraction, and exchangeable cation concentrations to identify depths of chemically altered saprolite. Seismic data show that depth to unweathered bedrock, as defined by p-wave seismic velocity, is slightly thicker on the north-facing slopes. Geochemical data suggest that the depth to the base of saprolite ranges from 3-5 m, consistent with a p-wave velocity value of 1200 m/s. Based on magnitude and anisotropy of p-wave velocities together with optical televiewer data, regolith on north-facing slopes is thought to be more fractured than south-facing slopes, while geochemical data indicate that position on the landscape is another important characteristic in determining depths of weathering. We explore the importance

Geochemical modelling study on the age and evolution of the groundwater at the Romuvaara site

International Nuclear Information System (INIS)

Pitkaenen, P.; Vuorinen, U.; Leino-Forsman, H.; Snellman, M.

1996-09-01

The objective of the study was to interpret the processes and factors which control the hydrogeochemistry (e.g. pH and redox conditions) in the radioactive waste disposal environment. A model of the hydrogeochemical evolution and the chemical flowpaths in different parts of the bedrock at the Romuvaara (in Finland) site has been created. The significance of chemical reactions along different flowpaths is calculated. Furthermore, the consistency of the hydrogeochemical model and the hydrogeological model is examined. (107 refs.)

Geochemical modelling study on the age and evolution of the groundwater at the Romuvaara site

Energy Technology Data Exchange (ETDEWEB)

Pitkaenen, P; Vuorinen, U; Leino-Forsman, H [Technical Research Centre of Finland, Espoo (Finland); Snellman, M [Imatran Voima Oy, Helsinki (Finland)

1996-09-01

The objective of the study was to interpret the processes and factors which control the hydrogeochemistry (e.g. pH and redox conditions) in the radioactive waste disposal environment. A model of the hydrogeochemical evolution and the chemical flowpaths in different parts of the bedrock at the Romuvaara (in Finland) site has been created. The significance of chemical reactions along different flowpaths is calculated. Furthermore, the consistency of the hydrogeochemical model and the hydrogeological model is examined. (107 refs.).

PERFIL DEL TÉCNICO DE EMERGENCIAS SANITARIAS EN ESPAÑA

Directory of Open Access Journals (Sweden)

Santiago Martínez-Isasi

2017-01-01

Full Text Available Fundamentos: El Técnico Emergencias Sanitarias desempeña una labor fundamental y es la figura cuantitativamente más importante en las emergencias extrahospitalarias. El objetivo fue conocer las características socio-demográficas, laborales, de salud del técnico y formativas en emer - gencias sanitarias en España. Métodos: Estudio descriptivo transversal. Se realizó un cuestionario ad hoc mediante Google Docs® que se distribuyó entre Abril–Junio 2014 mediante correo electrónico y redes sociales. Se recogieron un total de 705 cuestionarios. El análisis estadístico se realizó con SPSS ® versión 20.0 versión Windows. Se utilizó un nivel de significación P < 0.05 en todos los análisis. Resultados: Los datos analizados muestran como el perfil del Técnico Emergencias Sanitarias (TES en España es el de un hombre de 39 años, que vive en pareja o está casado con un hijo. El IMC medio es de 27 kg/m2, realiza ejercicio de forma regular, no fuma. Su antigüedad en la empresa es de 10 años y tienen el Ciclo Medio de Técnico Emergencias Sanitarias (CMTES. El análisis por sexos muestra como los hombres tienen una media de 40 años, un IMC medio de 27,5kg/m2 y desarrollan su labor profesional en una unidad de soporte vital avanzado, mientras que las mujeres tienen una media de 36,5 años, un IMC medio de 24,7kg/m2, trabajan principal - mente en unidades de soporte vital básico y su antigüedad en la empresa es de 6,76 años. Conclusión: El perfil del TES en España es hombre con sobrepeso, que refiere realizar ejercicio físico, lleva 10 años trabajando y está en posesión del CMTES; se observan diferencias en función del sexo en IMC, recurso donde desempeña su trabajo, antigüedad y edad.