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The evolution of (17)O-excess in surface water of the arid environment during recharge and evaporation
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...
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| Publicado no: | Sci Rep |
|---|---|
| Main Authors: | , , , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Nature Publishing Group UK
2018
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5862851/ https://ncbi.nlm.nih.gov/pubmed/29563523 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41598-018-23151-6 |
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