Geochemical evolution of brines in the Salar of Uyuni, Bolivia.

Chemical Geology
By: , and 



Recent analyses of brines from the Salars of Uyuni and Coipasa have been compared with published data for Lakes Titicaca and Poopo to evaluate solute compositional trends in these remnants of two large Pleistocene lakes once connected by overflow from the N to the S of the Bolivian Altiplano. From Titicaca to Poopo the water shows an increase in Cl and N somewhat greater than the total solutes. Ca and SO4 increase to a lesser extent than total dissolved solids, and carbonate species are relatively constant. Between Poopo and Coipasa proportions of Ca, SO4 and CO3 continue to decrease. At Coipasa and Uyuni, the great salars frequently evaporate to halite saturation. Halite crystallization is accompanied by an increased K, Mg and SO4 in residual brines. - from Authors
Publication type Article
Publication Subtype Journal Article
Title Geochemical evolution of brines in the Salar of Uyuni, Bolivia.
Series title Chemical Geology
DOI 10.1016/0009-2541(80)90116-3
Volume 30
Issue 1-2
Year Published 1980
Language English
Publisher Elsevier
Larger Work Type Article
Larger Work Subtype Journal Article
Larger Work Title Chemical Geology
First page 57
Last page 79
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