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U.S. Department of Energy
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Use of geochemical-equilibrium computer calculations to estimate precipitation from geothermal brines

Technical Report ·
DOI:https://doi.org/10.2172/7213963· OSTI ID:7213963
The Helgeson-Herrick geochemical code was used to calculate the solubility of NaCl, KCl, and KCl-NaCl in water and to predict which minerals will precipitate from Salton Sea Geothermal Field brines. The code's predictions of sulfide-silicate precipitation from the Magmamax No. 1 brine are in good agreement with field tests of scaling, although the observed sulfide-silicate scale matrix is in amorphous form, rather than the crystalline form predicted by the code. The code's predictions of scale precipitation from wells with different brine compositions are also in good agreement with field tests. The code appears to be a useful screening tool, despite reservations about the use of purely thermodynamic predictions in systems with important kinetic constraints. Several ways to improve and apply the code in the future are suggested.
Research Organization:
California Univ., Livermore (USA). Lawrence Livermore Lab.
DOE Contract Number:
W-7405-ENG-48
OSTI ID:
7213963
Report Number(s):
UCRL-52197
Country of Publication:
United States
Language:
English