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U.S. Department of Energy
Office of Scientific and Technical Information

Geothermal development and the Salton Sea. Memorandum report

Technical Report ·
OSTI ID:7091244

The purpose of this study is to examine the relationship of the Salton Sea, a key element of the Imperial Valley water system, to potential geothermal development. The most damaging effect would be the direct flow of geothermal brines into the Sea in large quantity (e.g., flow from several typical production wells). Not only would the rate of salinity increase be noticeably accelerated, but the added water would aggravate an already disturbingly high surface level situation. Both water quantity and quality considerations suggest that the Salton Sea cannot be used as a repository for large amounts of geothermal brine. Diversion of some of the inflow to the Salton Sea will have the beneficial effect of lowering the surface level, but will also tend to increase the salinity level. The use of Salton Sea water for injection fluid to maintain geothermal reservoir pressure will lower the elevation of the Sea and reduce its salinity. However, these beneficial effects will only be felt after the passage of many years, thus geothermal development does not offer an instant solution to the immediate problems of water quality in the Salton Sea.

Research Organization:
California Inst. of Tech., Pasadena (USA). Environmental Quality Lab.
OSTI ID:
7091244
Report Number(s):
PB-263796; EQL-MR-17
Country of Publication:
United States
Language:
English