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- W2009073634 abstract "Mono Lake, a major closed-basin alkaline salt lake in eastern California, derives its water from a mixture of creeks and springs, with the former providing in excess of 75% of the total. The Li isotopic composition of lake water has not varied significantly over a 4 year meromictic period (δ7Li ∼ +19.5). Springs are isotopically distinct: groundwater springs and seeps carry water enriched in isotopically heavy Li whereas thermal springs supply isotopically light (δ7Li 50% of the Li to the lake; (2) the Li budget is sensitively balanced on small thermal spring contributions, < 3% of the total spring inflow; and (3) the residence time of Li in the lake is 28 ka. Other Great Basin closed lakes have variable Li isotopic compositions (δ7Li from +16.7 to +23.7), all of which differ significantly from those of several major lakes and seawater (homogeneously ∼ +32)." @default.
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- W2009073634 date "2003-02-01" @default.
- W2009073634 modified "2023-09-27" @default.
- W2009073634 title "The lithium isotopic composition of waters of the Mono Basin, California" @default.
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- W2009073634 doi "https://doi.org/10.1016/s0016-7037(02)01132-8" @default.
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