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Precious Metals in the Salton Sea Geothermal Brines

McKibben, Michael A.; Williams, Alan E.; Hall, Gwendy E. M.

Key words
Brine Technology; USA; California; Imperial; Salton Sea; Chemistry; Brine; Analytical Methods; Sampling; Sealing; Gold; Transport; PGE; Precipitation
Location
Salton Sea, California; Imperial Valley
Conference
Geothermal Resources Council Transactions
Year
1989
Session
Direct use; Mineral extraction; Geochemical surveys; Brine c
Language
English

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Abstract

Production fluids, reservoir rock veins, well head pipe scales and downhole liner scales from the Salton Sea geothermal system have been analyzed for Au and Platinum group elements (PGE). Au and PGE levels in sampled production fluids are <0.3 ppb. Veins from reservoir rocks contain <5 ppb Au or PGE. IN scales, PGE concentrations are <13 ppb, but Au concentrations range from 0.1 to > 1000 ppm. The highest Au concentrations occur in downhole liner scales. Thermodynamic calculations indicated that the reservoir brines should be transporting 0.2 ppb Au, in excellent agreement with the measured values in production fluids Mass balance calculations suggest that, although the Au contents are relatively high in the scales, they represent scavenging of only 2% of the total Au that passes through the wellbore. A typical well produces 240 g (7.7 troy oz) of Au in one year, PGE transport appear to be legible.

Copyright 1989, Geothermal Resources Council. Readers who download papers from this site should honour the copyright of the original authors, and may not copy or distribute the work further without the permission of the original publisher.

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