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Determination of the rate of formation of solids from hypersaline geothermal brine as a function of pH

Technical Report ·
DOI:https://doi.org/10.2172/7080659· OSTI ID:7080659

Preliminary results obtained in the analysis of the effluent brine from the LLL four-stage flash system are reported. Of principal interest was the rate of formation of suspended solids and the rate of decrease of dissolved silicon (or silica) in the solution as a function of the pH of the effluent brine. The experiments were conducted using Magmamax No. 1 brine at the LLL Test Facility near Calipatria, California. The wellhead brine (having a pH of approximately 5.7) was acidified in the flash system to pH values of 5.0, 4.0, and 3.0, +- 0.2 pH unit, and the solids and silica in the effluent at approximately 90/sup 0/C were measured, respectively, by filtration and atomic absorption spectrophotometry. Changes in solids and silica concentration were determined after holding the brine at 90 +- 5/sup 0/C for periods of time up to one week. Data from studies of the size distribution of suspended particles in three solutions are summarized.

Research Organization:
California Univ., Livermore (USA). Lawrence Livermore Lab.
DOE Contract Number:
W-7405-ENG-48
OSTI ID:
7080659
Report Number(s):
UCID-17596
Country of Publication:
United States
Language:
English