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Terrestrial water load and groundwater fluctuation in the Bengal Basin
Groundwater-level fluctuations represent hydraulic responses to changes in groundwater storage due to aquifer recharge and drainage as well as to changes in stress that include water mass loading and unloading above the aquifer surface. The latter ‘poroelastic’ response of confined aquifers is a wel...
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| Publicado no: | Sci Rep |
|---|---|
| Main Authors: | , , , , , , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Nature Publishing Group UK
2017
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5478667/ https://ncbi.nlm.nih.gov/pubmed/28634399 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41598-017-04159-w |
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