An efficient workflow to accurately compute groundwater recharge for the study of rainfall-triggered deep-seated landslides, application to the Séchilienne unstable slope (western Alps)
Pore water pressure build-up by recharge of underground hydrosystems is one of the main triggering factors of deep-seated landslides. In most deep-seated landslides, pore water pressure data are not available since piezometers, if any, have a very short lifespan because of slope movements. As a cons...
| Autors principals: | , , , |
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| Format: | Article |
| Idioma: | English |
| Publicat: |
Copernicus Publications
2015-01-01
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| Col·lecció: | Hydrology and Earth System Sciences |
| Accés en línia: | http://www.hydrol-earth-syst-sci.net/19/427/2015/hess-19-427-2015.pdf |