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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Detalles Bibliográficos
Autores principales: Burgess, W. G., Shamsudduha, M., Taylor, R. G., Zahid, A., Ahmed, K. M., Mukherjee, A., Lapworth, D. J., Bense, V. F.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2017
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5478667/
https://www.ncbi.nlm.nih.gov/pubmed/28634399
http://dx.doi.org/10.1038/s41598-017-04159-w

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5478667/
https://www.ncbi.nlm.nih.gov/pubmed/28634399
http://dx.doi.org/10.1038/s41598-017-04159-w

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