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Influence of swelling behavior on the stability of an infinite unsaturated expansive soil slope

机译:膨胀特性对无限饱和非饱和膨胀土边坡稳定性的影响

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The influence of the stress regime change and associated softening can be significant on unsaturated expansive soil slope stability due to soil swelling upon wetting, which cannot be considered in conventional hydrological models. In this paper, the shallow expansive soil slope failure mechanism is addressed in the framework of an infinite slope formulation. The unsaturated soil elasto-plastic constitutive relationship is utilized for interpretation of stress regime evolution induced by expansive soil swelling during infiltration. The extended Mohr-Coulomb failure criterion for unsaturated soils is used as the yield surface, under which the nonlinear elastic behavior is considered by quantifying the effect of two stress state variables (net stress and suction) on elasticity parameters. The strain softening behavior in unsaturated soils is accounted for via reducing the material parameters of the yield surface with respect to plastic deviatoric strain. A numerical exercise is performed on a relatively gentle slope in Regina, Canada with highly expansive soil properties, using the developed computer program that implements the constitutive model into infinite slope formulation. The results suggest that neglecting the swelling-induced stress change and associated softening behavior can significantly overestimate the stability of expansive soil shallow layer under infiltration, in terms of both failure occurrence and failure time. Additional parametric study shows that all the considered parameters (including initial stress condition, softening rate and slope angle) have a considerable effect on the failure time and failure depth of the shallow deposit, which have important implications for the engineering design of expansive soil slopes. (C) 2016 Elsevier Ltd. All rights reserved.
机译:应力状态变化和相关软化的影响可能对不饱和膨胀土边坡的稳定性造成显着影响,这是由于湿润时土壤溶胀引起的,这在常规水文模型中是无法考虑的。本文在无限边坡公式化的框架内解决了浅层膨胀土边坡的破坏机理。利用非饱和土的弹塑性本构关系来解释渗透过程中膨胀土膨胀引起的应力状态演化。将扩展的针对非饱和土壤的Mohr-Coulomb破坏准则用作屈服面,在该屈服面下,通过量化两个应力状态变量(净应力和吸力)对弹性参数的影响来考虑非线性弹性行为。通过降低屈服面相对于塑性偏应变的材料参数,可以解释非饱和土壤中的应变软化行为。使用发达的计算机程序将本构模型实现为无限的斜坡公式,在加拿大里贾纳的一个相对缓和的斜坡上进行了数值模拟,该斜坡具有高度膨胀的土壤特性。结果表明,在破坏发生和破坏时间方面,忽略膨胀引起的应力变化和相关的软化行为可以显着高估渗透下膨胀土浅层的稳定性。额外的参数研究表明,所有考虑的参数(包括初始应力条件,软化速率和倾斜角度)对浅层沉积物的破坏时间和破坏深度都有相当大的影响,这对于膨胀土边坡的工程设计具有重要意义。 (C)2016 Elsevier Ltd.保留所有权利。

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