Results 71 to 80 of about 110 (90)
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Journal of Heat Recovery Systems, 1986
Abstract The effective utilization of geothermal energy is dependent on a knowledge of the total amount and character of the heat available in a particular geothermal field. The development of a conceptual model of a hydrothermal resource is essential for estimating its value and the proper mode of exploitation.
D. Nieva +5 more
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Abstract The effective utilization of geothermal energy is dependent on a knowledge of the total amount and character of the heat available in a particular geothermal field. The development of a conceptual model of a hydrothermal resource is essential for estimating its value and the proper mode of exploitation.
D. Nieva +5 more
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2021
Oxygen isotope investigations were carried out on hydrothermally altered rocks, authigenic quartz and calcite of the active geothermal field Los Azufres, Mexico. The δ18O values of the analysed whole rock samples vary from +2.2%0 to +16.7%0. The δ18O range of the analysed authigenic minerals is +3.93%0 to +20.23%0 for the quartz and +3.38%0 to + 12.23 ...
Ignacio S. Torres-Alvarado +2 more
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Oxygen isotope investigations were carried out on hydrothermally altered rocks, authigenic quartz and calcite of the active geothermal field Los Azufres, Mexico. The δ18O values of the analysed whole rock samples vary from +2.2%0 to +16.7%0. The δ18O range of the analysed authigenic minerals is +3.93%0 to +20.23%0 for the quartz and +3.38%0 to + 12.23 ...
Ignacio S. Torres-Alvarado +2 more
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Journal of Volcanology and Geothermal Research, 2020
Abstract Monitoring the impact of brine reinjection is crucial to the sustainable exploitation of geothermal resources. Reinjection monitoring at the Los Azufres Geothermal Field (Mexico) has historically been carried out by investigating the temporal and spatial evolution of chloride and the stable isotopic composition of water.
Sandra Nuñez-Hernández +8 more
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Abstract Monitoring the impact of brine reinjection is crucial to the sustainable exploitation of geothermal resources. Reinjection monitoring at the Los Azufres Geothermal Field (Mexico) has historically been carried out by investigating the temporal and spatial evolution of chloride and the stable isotopic composition of water.
Sandra Nuñez-Hernández +8 more
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International Geology Review, 2010
Subsurface reservoir temperatures of two important Mexican geothermal systems (Los Azufres and Las Tres Virgenes) were estimated by applying all available solute geothermometers for 88 and 56 chemical data measurements of the spring waters and fluids of the deep geothermal wells, respectively.
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Subsurface reservoir temperatures of two important Mexican geothermal systems (Los Azufres and Las Tres Virgenes) were estimated by applying all available solute geothermometers for 88 and 56 chemical data measurements of the spring waters and fluids of the deep geothermal wells, respectively.
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Heat Recovery Systems and CHP, 1988
The thermal conductivity of rocks is a basic parameter needed for a number of underground heat transfer studies. However, data are not readily available and its determination is not straightforward. Available predictive correlations have been developed for sedimentary rocks, while estimative methods are based on chemical or mineral analyses. It is thus
A. García +3 more
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The thermal conductivity of rocks is a basic parameter needed for a number of underground heat transfer studies. However, data are not readily available and its determination is not straightforward. Available predictive correlations have been developed for sedimentary rocks, while estimative methods are based on chemical or mineral analyses. It is thus
A. García +3 more
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Natural Hazards, 1989
A radon anomaly in a nuclear track detector placed on a fault was detected prior to the destructive (Ms = 8.1) Mexican earthquake of 19 September 1985. The fault is a structural feature of the geothermal field ‘Los Azufres’, 260 km NE of the epicentral area.
N. Segovia +5 more
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A radon anomaly in a nuclear track detector placed on a fault was detected prior to the destructive (Ms = 8.1) Mexican earthquake of 19 September 1985. The fault is a structural feature of the geothermal field ‘Los Azufres’, 260 km NE of the epicentral area.
N. Segovia +5 more
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00/00344 Residual steam to energy: a project for Los Azufres geothermal field, Mexico
Fuel and Energy Abstracts, 2000openaire +1 more source