Please use this identifier to cite or link to this item: https://hdl.handle.net/10356/101447
Title: Effect of rising water table in an unsaturated slope
Authors: Schnellmann, Reto
Busslinger, Matthias
Rahardjo, Harianto
Schneider, Hans R.
Keywords: DRNTU::Engineering::Civil engineering::Geotechnical
Issue Date: 2010
Source: Schnellmann, R., Busslinger, M., Schneider, H. R., & Rahardjo, H. (2010). Effect of Rising Water Table in an Unsaturated Slope. Engineering Geology, 114(1-2), 71-83.
Series/Report no.: Engineering geology
Abstract: Recently, climatic changes have caused more extreme weather conditions such as heavy rain falls and droughts. Therefore, climatic changes are expected to produce increased variations in infiltration characteristics and positions of water table in slopes. A physical slope model has been developed to study the effects of climatic changes in an unsaturated slope. The effect of rising water table in an unsaturated slope was investigated experimentally in the physical slope model. In addition, finite element analyses were carried out to simulate infiltration in slopes under steady-state and transient conditions. A comparison between the results of laboratory model measurements and numerical analyses shows good agreement despite the complex unsaturated soil conditions. Both, experimental data and numerical analyses demonstrate a delayed response in pore-water pressure in the unsaturated zone due to the rising of water table. A conceptual framework is presented to describe the physically possible lower and upper limits of pore-water pressures in a slope resulting from the rise in water table.
URI: https://hdl.handle.net/10356/101447
http://hdl.handle.net/10220/7374
DOI: 10.1016/j.enggeo.2010.04.005
Rights: © 2010 Elsevier Ltd.
Fulltext Permission: none
Fulltext Availability: No Fulltext
Appears in Collections:CEE Journal Articles

Google ScholarTM

Check

Altmetric


Plumx

Items in DR-NTU are protected by copyright, with all rights reserved, unless otherwise indicated.