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Minerals 2020, 10, 284 Table 1. Major features of the dry lakes in the Barstow-Bristol Trough. Other geothermal waters from the region are included for comparison. 9 of 34 Characteristic Watershed size (km2) Brine type Average Maximum Total dissolved solids (g/L) in basin brines Maximum calcium concentration (g/L) in basin brines K:Mg ratio (meq/L) Maximum lithium Maximum boron Maximum fluoride concentration (mg/L) In basin brines Percentage of halite by volume in cores from basin centers Greatest depth of drilling in sediments in the basin * (m) Range of brine temperatures based on Mg:Li and Na:K geothermometry (◦C) Bouse Formation present Bristol Dry Lake Brine Historic: 3130 Current: 2146 Na–Ca–Cl 259 357 56 0.2–1.4 110 8.8 1.8 40% 537 Mg–Li: 161–152 Na–K: 192– <150 Cadiz Dry Lake Brine 4244 Na–Ca–Cl 255 375 40 0.3–1.3 80 14 1.6 <1%; one 1 m thick bed near the surface 152 Mg–Li: 153–132 Danby Dry Lake Brine 2265 Na–Cl 128 187 0.4 1.0–3.8 4.1 3.9 6.4 <1%; three <1 m thick beds near the surface 268 Mg–Li: 5–107 References Salton Sea Geothermal Well - Na–Ca–Cl - 387 40 2.3– >500 400 380 18 - 1000 200–340 ** - * None of the basins have been drilled to basement; ** measured temperature [42,43]. Long Valley Geothermal Springs and Wells - Na–HCO3 –Cl - 0.74 0.04 138 3.2 11.1 11.4 - >200 Mg–Li: 220 Na–K: 222 - One shoreline outcrop 200 m above playa Na–K: <150 In core Na–K: <150 In core This paper [6–8,26,28,42–44] This paper [6–8,26,28,42], this paper This paper [6–8,26,28,42,44] This paper [6–8,34,43,44] This paper, data from [44] for Long Valley [32–34]PDF Image | Bristol Dry Lake Brine Compared to Brines from Cadiz
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Product and Development Focus for Infinity Turbine
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