Field evidence of pore pressure diffusion in clayey soils prone to landsliding
- 1 September 2010
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research: Earth Surface
- Vol. 115 (F3)
- https://doi.org/10.1029/2009jf001463
Abstract
No abstract availableKeywords
This publication has 29 references indexed in Scilit:
- Rainfall thresholds for shallow landsliding derived from pressure‐head monitoring: cases with permeable and impermeable bedrocks in Boso Peninsula, JapanEarth Surface Processes and Landforms, 2007
- A physically based model for the hydrologic control on shallow landslidingWater Resources Research, 2006
- Response of a residual soil slope to rainfallCanadian Geotechnical Journal, 2005
- Floods, channel change, and the hyporheic zoneWater Resources Research, 1999
- A physically based model for the topographic control on shallow landslidingWater Resources Research, 1994
- How permeable are clays and shales?Water Resources Research, 1994
- The capillary fringe and its effect on water-table responseJournal of Hydrology, 1984
- Water flux in soil and subsoil on a steep forested slopeJournal of Hydrology, 1977
- River flow forecasting through conceptual models part I — A discussion of principlesJournal of Hydrology, 1970
- CAPILLARY CONDUCTION OF LIQUIDS THROUGH POROUS MEDIUMSPhysics, 1931