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2D Infiltration in Unsaturated Porous Media
Coupling between water infiltration and mechanical deformation in partially saturated porous media is central to many natural and man-made systems in civil and environmental engineering. During water infiltration, the pore-water pressure is redistributed, on one hand, by the hydraulic properties of the partially saturated soil including retention characteristics and permeability, and, on the other hand, by the external loading due to climate conditions (rainfall intensity, duration, and evapo-transpiration rate).
2D Infiltration in Unsaturated Porous Media
Coupling between water infiltration and mechanical deformation in partially saturated porous media is central to many natural and man-made systems in civil and environmental engineering. During water infiltration, the pore-water pressure is redistributed, on one hand, by the hydraulic properties of the partially saturated soil including retention characteristics and permeability, and, on the other hand, by the external loading due to climate conditions (rainfall intensity, duration, and evapo-transpiration rate).
2D Infiltration in Unsaturated Porous Media
Wu, Lizhou (author) / Huang, Runqiu (author) / Li, Xu (author)
Hydro-mechanical Analysis of Rainfall-Induced Landslides ; Chapter: 4 ; 99-138
2020-01-15
40 pages
Article/Chapter (Book)
Electronic Resource
English
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