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Bristol Dry Lake Brine Compared to Brines from Cadiz

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Bristol Dry Lake Brine Compared to Brines from Cadiz ( bristol-dry-lake-brine-compared-brines-from-cadiz )

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Minerals 2020, 10, 284 25 of 34 Minerals 2020, 10, x FOR PEER REVIEW 25 of 34 Figure 11. Lithium concentrations in bulk sediment from Bristol, Cadiz and Danby Dry Lake cores. Figure 11. Lithium concentrations in bulk sediment from Bristol, Cadiz and Danby Dry Lake cores. Data from Cadiz and Danby Dry Lakes are from [6,8], respectively. Wells plotted are numbered in Data from Cadiz and Danby Dry Lakes are from [6] and [8], respectively. Wells plotted are numbered Figures 3–5 as: BDL, samples from wells 10, 13–16; CDL well CAD-1, well 104; and DDL wells; DAN-1, in Figures 3–5 as: BDL, samples from wells 10, 13–16; CDL well CAD-1, well 104; and DDL wells; well 113, DAN-2, well 114. Data from Bristol Dry Lake are from this study. DAN-1, well 113, DAN-2, well 114. Data from Bristol Dry Lake are from this study. 5. Discussion 5. Discussion 5.1. Hydrology of the Basins 5.1. Hydrology of the Basins The relatively constant correlation between alluvial fan water and basin-center brines for most The relatively constant correlation between alluvial fan water and basin-center brines for most elements suggests that evaporation is the main driver for the concentration of these elements. While elements suggests that evaporation is the main driver for the concentration of these elements. While some Ca and Sr are lost to carbonate, gypsum, and celestite precipitation in the alluvial fans and basin some Ca and Sr are lost to carbonate, gypsum, and celestite precipitation in the alluvial fans and basin margin [27], the loss of Ca and Sr does not appear to change the ratio of these elements to Li in the BDL margin [27], the loss of Ca and Sr does not appear to change the ratio of these elements to Li in the and CDL brines. The lack of ratio change, even after precipitation of gypsum may indicate input of BDL and CDL brines. The lack of ratio change, even after precipitation of gypsum may indicate input an additional source of water, possibly geothermal in origin. of an additional source of water, possibly geothermal in origin.

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