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Numerical modelling of rainfall effects on the stability of soil slopes

机译:降雨对土质边坡稳定性影响的数值模拟

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High intensity rainfall leads to slope failures that are initially unsaturated. Rainfall is the main triggering factor for the slope failure; however, the denseness of the soil with associated soil properties has not received adequate attention on the stability of the slopes. In this study, the finite difference analysis of transient water flow through unsaturated-saturated soil is carried out to study the effects of rainfall intensity and duration on pore pressure generation, degree of saturation, slope stability and shear strain increment during rainfall event. A parametric sensitivity analysis is performed considering three rainfall intensities applied over the soil slopes consisting of three different soil states namely loose, medium and dense. Results indicate that the rainfall affects the stability of loose and medium soil slopes much as compared to the dense soil slope.The rain-induced instability is much more in loose soil slope as compared to the medium soil slope.
机译:高强度降雨导致坡度破坏,最初是不饱和的。降雨是导致边坡破坏的主要因素。然而,土壤的密实性和相关的土壤特性并未对斜坡的稳定性引起足够的重视。本文通过对非饱和饱和土壤中瞬态水流的有限差分分析,研究降雨强度和持续时间对降雨过程中孔隙压力产生,饱和度,边坡稳定性和剪切应变增量的影响。考虑在三种坡度上施加的降雨强度进行了参数敏感性分析,坡度包括三种不同的土壤状态,即松散,中度和稠密。结果表明,降雨对松散和中等土质边坡的稳定性影响远大于密实土质边坡;与中土质边坡相比,降雨对松散土质边坡的失稳影响更大。

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