Numerical modeling of small-scale unsaturated soil slope subjected to transient rainfall

Climate change is creating more extreme rain events and causing more landslides in recent years. Most of the previous studies focused on large-scale slopes such as mountainous areas. For the problem of small-scale landslides in urban areas, a hydro-mechanical analysis of soil slopes under rainfall i...

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Main Authors: Liu, Chang, Yan, Yipu, Yang, Haoqing
Other Authors: School of Civil and Environmental Engineering
Format: Article
Language:English
Published: 2024
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Online Access:https://hdl.handle.net/10356/173655
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Institution: Nanyang Technological University
Language: English
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spelling sg-ntu-dr.10356-1736552024-02-23T15:33:08Z Numerical modeling of small-scale unsaturated soil slope subjected to transient rainfall Liu, Chang Yan, Yipu Yang, Haoqing School of Civil and Environmental Engineering Engineering Slope Rainfall Climate change is creating more extreme rain events and causing more landslides in recent years. Most of the previous studies focused on large-scale slopes such as mountainous areas. For the problem of small-scale landslides in urban areas, a hydro-mechanical analysis of soil slopes under rainfall is also demanded. In this study, a numerical model of a slope under rainfall and load is established by COMSOL Multiphysics. To facilitate the analysis for practical purposes, two built-in modules are used to model a unidirectional coupling of hydro-mechanical behaviors of unsaturated soil slopes. The Richards’ module is first adopted to model an unsaturated soil slope under rainfall. Then the Extended Barcelona Basic module that considers the matric suction is adopted as the constitutive model. The effect of rainfall duration and saturated hydraulic conductivity on stress, settlement, and pore-water pressure are studied. When the rainfall proceeds, the matric suction head keeps reducing constantly. For a fixed location, the settlement decreases as ks increases. The wetting front is more apparent as the ks is reduced as the curvature of the pore pressure profile is more pronounced. The matric suction at a steady state is decreased when the ks becomes small. The simulated soil suction is comparable to these field monitoring data. Published version 2024-02-21T02:05:45Z 2024-02-21T02:05:45Z 2023 Journal Article Liu, C., Yan, Y. & Yang, H. (2023). Numerical modeling of small-scale unsaturated soil slope subjected to transient rainfall. Geosystems and Geoenvironment, 2(4), 100193-. https://dx.doi.org/10.1016/j.geogeo.2023.100193 2772-8838 https://hdl.handle.net/10356/173655 10.1016/j.geogeo.2023.100193 2-s2.0-85160632132 4 2 100193 en Geosystems and Geoenvironment © 2023 The Author(s). Published by Elsevier Ltd on behalf of Ocean University of China. This is an open access article under the CC BY license (http://creativecommons.org/licenses/by/4.0/). application/pdf
institution Nanyang Technological University
building NTU Library
continent Asia
country Singapore
Singapore
content_provider NTU Library
collection DR-NTU
language English
topic Engineering
Slope
Rainfall
spellingShingle Engineering
Slope
Rainfall
Liu, Chang
Yan, Yipu
Yang, Haoqing
Numerical modeling of small-scale unsaturated soil slope subjected to transient rainfall
description Climate change is creating more extreme rain events and causing more landslides in recent years. Most of the previous studies focused on large-scale slopes such as mountainous areas. For the problem of small-scale landslides in urban areas, a hydro-mechanical analysis of soil slopes under rainfall is also demanded. In this study, a numerical model of a slope under rainfall and load is established by COMSOL Multiphysics. To facilitate the analysis for practical purposes, two built-in modules are used to model a unidirectional coupling of hydro-mechanical behaviors of unsaturated soil slopes. The Richards’ module is first adopted to model an unsaturated soil slope under rainfall. Then the Extended Barcelona Basic module that considers the matric suction is adopted as the constitutive model. The effect of rainfall duration and saturated hydraulic conductivity on stress, settlement, and pore-water pressure are studied. When the rainfall proceeds, the matric suction head keeps reducing constantly. For a fixed location, the settlement decreases as ks increases. The wetting front is more apparent as the ks is reduced as the curvature of the pore pressure profile is more pronounced. The matric suction at a steady state is decreased when the ks becomes small. The simulated soil suction is comparable to these field monitoring data.
author2 School of Civil and Environmental Engineering
author_facet School of Civil and Environmental Engineering
Liu, Chang
Yan, Yipu
Yang, Haoqing
format Article
author Liu, Chang
Yan, Yipu
Yang, Haoqing
author_sort Liu, Chang
title Numerical modeling of small-scale unsaturated soil slope subjected to transient rainfall
title_short Numerical modeling of small-scale unsaturated soil slope subjected to transient rainfall
title_full Numerical modeling of small-scale unsaturated soil slope subjected to transient rainfall
title_fullStr Numerical modeling of small-scale unsaturated soil slope subjected to transient rainfall
title_full_unstemmed Numerical modeling of small-scale unsaturated soil slope subjected to transient rainfall
title_sort numerical modeling of small-scale unsaturated soil slope subjected to transient rainfall
publishDate 2024
url https://hdl.handle.net/10356/173655
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