Comparison of δBr and δCl composition of volatiles, salt precipitates, and associated water in terrestrial evaporative saline lake systems.

This study provides the first characterization of the variability of bromine and chlorine stable isotopic composition in evaporites, associated residual brines, and shoreline gases in terrestrial evaporative saline lakes. The lakes investigated here are groundwater discharge locations, and include both potash-rich alkaline lakes and sodic-dominated neutral pH lakes at a variety of salinities and evaporative stages. The chlorine and bromine isotope systems behave consistently different during evaporative salt precipitation, with Cl more enriched in the salt than in the fluid, but Br more enriched in the fluid compared with the precipitated salt.