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- W2006419687 abstract "Wellhead and downhole water samples were collected and analyzed from a 114.3‐m well at Coso Hot Springs (Coso No. 1) and a 1477‐m well (CGEH No. 1) 3.2 km to the west. The same chloride concentration is present in hot waters entering both wells (about 2350 mg/kg), indicating that a hot‐water‐dominated geothermal system is present. The maximum measured temperatures are 142°C in the Coso No. 1 well and 195°C in the CGEH No. 1 well. Cation and sulfate isotope geothermometers indicate that the reservoir feeding water to the Coso Hot Spring well has a temperature of about 240°–250°C, and the reservoir feeding the CGEH well has a temperature of about 205°C. The variation in the chemical composition of water from the two wells suggests a model in which water‐rock chemical equilibrium is maintained as a convecting solution cools from about 245°C to 205°C by conductive heat loss." @default.
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- W2006419687 date "1980-05-10" @default.
- W2006419687 modified "2023-09-27" @default.
- W2006419687 title "Interpretation of chemical analyses of waters collected from two geothermal wells at Coso, California" @default.
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- W2006419687 doi "https://doi.org/10.1029/jb085ib05p02405" @default.
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