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Three-dimensional seismic stability of unsaturated soil slopes using a semi-analytical method

机译:使用半分析方法的不饱和土斜坡的三维地震稳定性

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Seismic stability analyses of soil slopes are routinely performed with dry and/or saturated assumptions under two-dimensional (2D) conditions. However, in practice, soils are often unsaturated and slopes usually fail in 3D fashion. Three-dimensional (3D) effect and suction-induced effect are essential to be considered to produce more realistic solutions in the slope stability analyses. In this regard, an analytical framework is developed in this paper for assessing the 3D seismic stability of unsaturated soil slopes. A semi-analytical method including the simplified method (SM) and the layer-wise summation method (LSM) is developed to deal with the highly variable nature of suction. The validity of the analytical framework in assessing the soil slope stability is checked with published solutions. Examples are given to illustrate the 3D effect and the effect of suction on the slope seismic stability. The described framework allows the user to quantify the effect of changes in moisture content on effective stress distribution and effective unit weight distribution in the slope and thus, changes in the slope stability.
机译:在二维(2D)条件下用干燥和/或饱和的假设常规进行土壤斜率的地震稳定性分析。然而,在实践中,土壤通常是不饱和的,斜坡通常以3D方式失败。三维(3D)效应和吸附诱导的效果是必不可及的,以便在坡稳定性分析中产生更现实的解决方案。在这方面,本文开发了一种分析框架,用于评估不饱和土坡的3D地震稳定性。开发了一种半分析方法,包括简化方法(SM)和层 - 方向求和方法(LSM),以处理吸力的高度可变性质。通过发布的解决方案检查了评估土壤边坡稳定性的分析框架的有效性。给出了示例以说明抽吸对倾斜地震稳定性的3D效应和效果。所描述的框架允许用户量化水分含量变化对斜率中有效应力分布和有效单位重量分布的影响,因此斜率稳定性的变化。

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