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Analysis of soil water movement inside a footslope and a depression in a karst catchment, Southwest China
Soil water movement is difficult to explain with event-scale approaches, especially in karst regions. This paper focuses on investigating seasonal recharge and mean residence time (MRT) of soil water based on temporal variation of stable isotopes (δD and δ(18)O) and a dispersion model (DM), and disc...
Autores principales: | , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2017
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5451417/ https://www.ncbi.nlm.nih.gov/pubmed/28566763 http://dx.doi.org/10.1038/s41598-017-02619-x |