Cooperative geochemical investigation of geothermal resources in the Imperial Valley and Yuma areas. Final report
Preliminary studies indicate that the Imperial Valley has a large geothermal potential. In order to delineate additional geothermal systems a chemical and isotopic investigation of samples from water wells, springs, and geothermal wells in the Imperial Valley and Yuma areas was conducted. Na, K, and Ca concentrations of nearly 200 well water, spring water, hot spring, and geothermal fluid samples from the Imperial Valley area were measured by atomic absorption spectrophotometry. Fournier and Truesdell's function was determined for each water sample. Suspected geothermal areas are identified. Hydrogen and oxygen isotope abundances were determined in order to determine and to identify the source of the water in the Mesa geothermal system. (JGB)
- Research Organization:
- Bureau of Reclamation, Denver, Colo. (USA)
- OSTI ID:
- 5244171
- Report Number(s):
- IGPP-UCR-73-48
- Country of Publication:
- United States
- Language:
- English
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Related Subjects
ARIZONA
GEOCHEMICAL SURVEYS
GEOTHERMAL EXPLORATION
CALCIUM
ABUNDANCE
DEUTERIUM
ISOTOPE RATIO
HYDROGEN
IMPERIAL VALLEY
OXYGEN 16
OXYGEN 18
POTASSIUM
SODIUM
THERMAL WATERS
CHEMICAL COMPOSITION
COLORADO RIVER
GEOTHERMAL WELLS
GROUND WATER
THERMAL SPRINGS
WELLS
ALKALI METALS
ALKALINE EARTH METALS
CALIFORNIA
CRYOGENIC FLUIDS
ELEMENTS
EVEN-EVEN NUCLEI
EXPLORATION
FLUIDS
HYDROGEN COMPOUNDS
HYDROGEN ISOTOPES
ISOTOPES
LIGHT NUCLEI
METALS
NONMETALS
NORTH AMERICA
NUCLEI
ODD-ODD NUCLEI
OXYGEN COMPOUNDS
OXYGEN ISOTOPES
RIVERS
STABLE ISOTOPES
STREAMS
SURFACE WATERS
USA
WATER
Geothermal Legacy
150302* - Geothermal Exploration & Exploration Technology- Geochemical Techniques & Surveys