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• W2805495875 abstract "Abstract This study demonstrates the potential of triple O-isotopes to quantify evaporation with recharge on a salt lake from the Atacama Desert, Chile. An evaporative gradient was found in shallow ponds along a subsurface flow-path from a groundwater source. Total dissolved solids (TDS) increased by 177 g/l along with an increase in δ 18 O by 16.2‰ and in δD by 65‰. 17 O-excess decreased by 79 per meg, d-excess by 55‰. Relative humidity ( h ), evaporation over inflow ( E / I ), the isotopic composition of vapor ( * R V ) and of inflowing water ( * R WI ) determine the isotope distribution in 17 O-excess over δ 18 O along a well-defined evaporation curve as the classic Craig-Gordon model predicts. A complementary on-site simple (pan) evaporation experiment over a change in TDS, δ 18 O, and 17 O-excess by 392 g/l, 25.0‰, and −130 per meg, respectively, was used to determine the effects of sluggish brine evaporation and of wind turbulence. These effects translate to uncertainty in E / I rather than h . The local composition of * R V relative to * R WI pre-determines the general ability to resolve changes in h . The triple O-isotope system is useful for quantitative hydrological balancing of lakes and for paleo-humidity reconstruction, particularly if complemented by D/H analysis." @default.
• W2805495875 created "2018-06-13" @default.
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• W2805495875 date "2018-03-21" @default.
• W2805495875 modified "2023-10-17" @default.
• W2805495875 title "The evolution of 17O-excess in surface water of the arid environment during recharge and evaporation" @default.
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• W2805495875 doi "https://doi.org/10.1038/s41598-018-23151-6" @default.
• W2805495875 hasPubMedCentralId "https://www.ncbi.nlm.nih.gov/pmc/articles/5862851" @default.
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• W2805495875 hasPublicationYear "2018" @default.
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