Journal ArticleDOI
The geochemistry and isotope hydrology of the Southern Mexicali Valley in the area of the Cerro Prieto, Baja California (Mexico) geothermal field
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TLDR
In this paper, groundwaters from the phreatic aquifer within and surrounding of the Cerro Prieto geothermal field were analyzed geochemically and isotopically in order to establish a hydrodynamic model of the study zone.About:
This article is published in Journal of Hydrology.The article was published on 2005-11-10. It has received 40 citations till now. The article focuses on the topics: Aquifer & Phreatic zone.read more
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A groundwater isoscape (δD, δ18O) for Mexico
TL;DR: In this paper, it was shown that precipitation isocapes drive δD and δ18O patterns in surficial waters and in terrestrial food webs, while the GNIP (Global Network for Isotopes in Precipitation) da...
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Hydrogeochemical characterization of groundwater flow systems in the discharge area of a river basin
TL;DR: In this article, the authors used the major ions and pH as the input, hierarchical cluster analysis was conducted, which leads to five clusters (from C1 to C5) with distinct geochemical compositions.
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Synthesis of ground and remote sensing data for monitoring ecosystem functions in the Colorado River Delta, Mexico
TL;DR: In this paper, the authors developed ground-validated, remote sensing methods to monitor the vegetation status, habitat value, and water use of wetland and riparian ecosystems using multi-temporal, multi-resolution images.
Journal ArticleDOI
Geothermal prospects in the Baja California Peninsula
TL;DR: In this article, the Baja California Peninsula hydrothermal systems were evaluated and the minimum calculated potential is more than 400 MWe, where MWe is defined as the maximum surface heat loss from the submarine systems.
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Groundwater geochemistry of the Chihuahua City region in the Rio Conchos Basin (northern Mexico) and implications for water resources management
TL;DR: A geochemical survey was carried out to investigate the evolution from baseline to modern conditions of a 130-km flow path including the El Sauz-Chihuahua-Aldama-San Diego de Alcala regions.
References
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Journal ArticleDOI
Isotopic Variations in Meteoric Waters
TL;DR: The relationship between deuterium and oxygen-18 concentrations in natural meteoric waters from many parts of the world has been determined with a mass spectrometer and shows a linear correlation over the entire range for waters which have not undergone excessive evaporation.
Book
Study and Interpretation of the Chemical Characteristics of Natural Water
TL;DR: The chemical composition of natural water is derived from many different sources of solutes, including gases and aerosols from the atmosphere, weathering and erosion of rocks and soil, solution or precipitation reactions occurring below the land surface, and cultural effects resulting from human activities.
Book
Environmental Isotopes in Hydrogeology
Ian D. Clark,Peter Fritz +1 more
TL;DR: In this paper, the authors trace the Carbon Cycle Evolution of Carbon in Groundwater Carbonate Geochemistry Carbon-13 in the Carbonate System Dissolved Organic Carbon Methane in Groundwaters Isotopic Composition of Carbonates.
Book
The geochemistry of natural waters
TL;DR: The Hydrologic Cycle and Chemical Background of Natural Waters as mentioned in this paper, the Carbonate System and pH Control 5 Clay Minerals and Ion Exchange 6 Stability Relationships and Silicate Equilibria 7 Kinetics 8 Weathering and Water Chemistry, I: Principles 9 Water Chemistry Chemistry, II: Examples 10 Acid Deposition and Surface Water Chemistry 11 Evaporation and Saline Waters 12 The Oceans 13 Redox Eilibria 14 Redox Conditions in Natural Waters 15 Trace Elements 16 Mathematical and Numerical Models 17 Isotopes Appendices
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The kinetics of silica-water reactions
J.D. Rimstidt,H.L. Barnes +1 more
TL;DR: In this article, the authors derived a differential rate equation for silica-water reactions from 0-300°C based on stoichiometry and activities of the reactants in the reaction SiO2(s) + 2H2O(l) = H4SiO4(aq) ( ∂a H 4 SiO 4 ∂t ) P.T.