CHEMISTRY OF LOW-TEMPERATURE GEOTHERMAL WATERS AT KLAMATH FALLS, OREGON.
By: C. J. Janik, A.H. Truesdell, E.A. Sammel, and A. F. White
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Abstract
Chemical and isotopic analyses of well discharges indicate that in the aquifer mixing occurs between shallow cold groundwater containing 2. 0 TU tritium and a deeper tritium-free thermal groundwaer at 100 to 120 degree C. This deeper water apparently results from the mixing of old, tritium-free cold groundwater and deep thermal groundwater at about 190 degree C and 120 mg/kg Cl. The temperature and chlorinity of the deep thermal water are based on SO//4-isotope and silica geothermometers and chloride and silica mixing models.
| Publication type | Conference Paper |
|---|---|
| Publication Subtype | Conference Paper |
| Title | CHEMISTRY OF LOW-TEMPERATURE GEOTHERMAL WATERS AT KLAMATH FALLS, OREGON. |
| ISBN | 0934412596 |
| Volume | 9 |
| Issue | pt 1 |
| Year Published | 1985 |
| Language | English |
| Publisher | Geothermal Resources Council |
| Publisher location | Davis, CA, USA |
| Larger Work Title | Transactions - Geothermal Resources Council |
| First page | 325 |
| Last page | 331 |
| Conference Title | 1985 International Symposium on Geothermal Energy. Geothermal Resources Council 1985 Annual Meeting. |
| Conference Location | Kailua-Kona, HI, USA |
| Google Analytic Metrics | Metrics page |