Field evidence of pore pressure diffusion in clayey soils prone to landsliding

The hydrologic behavior of shallow weathered soils commonly determines the propensity for slope failure. Here we use laboratory data and field data collected by an automated monitoring system to assess the character of pore water pressure responses in a natural clay slope subject to intermittent rai...

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Vydáno v:	Journal of Geophysical Research: Earth Surface Ročník 115; číslo F3
Hlavní autoři:	Berti, Matteo, Simoni, Alessandro
Médium:	Journal Article
Jazyk:	angličtina
Vydáno:	Washington, DC Blackwell Publishing Ltd 01.09.2010 American Geophysical Union
Témata:	Assessments clayey soil Earth sciences Earth, ocean, space Exact sciences and technology Failure hydrologic modeling Hydrology Meters monitoring pore pressure Porosity Pressure sensors shallow slope stability Soils Water pressure water pressure slopes clay rupture amplitude pore pressure Ground surface pore water Diffusion soils calibration clastic rocks Gravity models Transient response rainfall atmospheric precipitation documentation Pressure distribution monitoring sedimentary rocks depth diffusivity prediction transient phenomena saturated zone
ISSN:	0148-0227, 2169-9003, 2156-2202, 2169-9011
On-line přístup:	Získat plný text
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