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Computer modelling of geothermal brines from the Salton Sea Geothermal Field, California

Conference · · EOS, Trans., Am. Geophys. Union; (United States)
OSTI ID:5384339
To produce electric power from energy stored in the hypersaline brines of the Salton Sea Geothermal Field, methods must be developed for controlling the sulfides and silicates which precipitate as scale deposits on process equipment. To circumvent costly, time-consuming, and potentially difficult laboratory experiments, equilibria were predicted in these brines by two different computational techniques, the Helgeson-Herrick code and individual reaction calculations using effective activity coefficients which take into account chloride complexing. The results of both methods are consistent with one another in predicting precipitation behavior in the temperature interval 100 to 300/sup 0/C. For example, results for the Magmamax No. 1 brines indicate that quartz, pyrrhotite, galena, chalcopyrite, sphalerite, and Fe-silicates can precipitate. This predicted sulfide-silicate assemblage agrees generally with observations on scale from the field test site, although the silica-silicate scale matrix is amorphous. Carbonate equilibria are especially interesting; large Ca/sup +2/ and CO/sub 2/ concentrations in the Magmamax No. 1 brine suggest that the reservoir fluid is saturated with respect to calcite. At a downhole temperature of 260/sup 0/C using the calcite curve as a guide, saturation would occur at pH of 3.5 to 4.0.
Research Organization:
Univ. of California, Livermore
OSTI ID:
5384339
Conference Information:
Journal Name: EOS, Trans., Am. Geophys. Union; (United States) Journal Volume: 57:12
Country of Publication:
United States
Language:
English