| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4675219 | Procedia Earth and Planetary Science | 2013 | 4 Pages |
Abstract
Water-rock interactions within the main thermal aquifer in the Long Valley Caldera are evaluated using water chemistry data from a new suite of samples. The results reflect the impact of increased geothermal production and major CO2 loss, which appears to drive calcite precipitation in the aquifer. The study provides qualitative information on the rates of mineral reactions and the response times of chemical geothermometers to declining temperatures.
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Physical Sciences and Engineering
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Atmospheric Science
