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首页> 外文期刊>Advances in Water Resources >Poro-mechanical coupling influences on potential for rainfall-induced shallow landslides in unsaturated soils
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Poro-mechanical coupling influences on potential for rainfall-induced shallow landslides in unsaturated soils

机译:孔隙-机械耦合对非饱和土壤降雨诱发的浅层滑坡的影响

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摘要

Rainfall-induced landslides are a common occurrence in terrain with steep topography and soils that have degradable strength. Rainfall infiltration into a partially saturated slope of infinite extent can lead to either a decrease or complete elimination of soil suction, compromising the slopes' stability. In this research the rainfall infiltration coupled with deformation of a partially saturated soil slope during rainfall infiltration is analyzed. The limit equilibrium conditions and the shear strength relationship of a partially saturated soil are employed to develop an analytical solution for calculating the stability of an infinite partially saturated slope due to rainfall infiltration. The analytical solutions are able to consider the influence of the coupled effects on the stability of the slope. The factors that affect the safety of a partially saturated slope of infinite extent are discussed. The results indicate that the poro-mechanical coupling of water infiltration and deformation has an important effect on the stability of the infinite unsaturated slope. (C) 2016 Elsevier Ltd. All rights reserved.
机译:降雨诱发的滑坡在地形陡峭的地形和具有可降解强度的土壤中很常见。降雨渗透到无限程度的部分饱和斜坡会导致土壤吸力下降或完全消失,从而损害斜坡的稳定性。本研究分析了降雨入渗过程中降雨入渗与部分饱和土坡变形的关系。利用极限饱和条件和部分饱和土的抗剪强度关系来开发解析解,以计算由于降雨入渗而引起的无限部分饱和斜坡的稳定性。解析解能够考虑耦合效应对边坡稳定性的影响。讨论了影响无限范围部分饱和斜坡安全性的因素。结果表明,渗流与变形的孔隙动力耦合对无限饱和土边坡的稳定性有重要影响。 (C)2016 Elsevier Ltd.保留所有权利。

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