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The effect of soil type on matric suction and stability of unsaturated slope under uniform rainfall

机译:均匀降雨条件下土壤类型对基质吸力和非饱和边坡稳定性的影响

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It is well understood that rainfall infiltration decreases the unsaturated shear strength of soil slope due to reduction in matric suction as the wetting front moves through it. However, how much the matric suction is reduced that may affect slope stability results is still unknown. The paper presents the numerical results of wetting front depth, matric suction and stability results in term of reliability index for a single rainfall intensity. The analyses are for five soils using the modified Mohr-Coulomb failure criterion in conjunction with a finite element saturated-unsaturated seepage model. The numerical results show that the matric suction results are differently affected for soils with rainfall infiltration. The change in reliability index result is insignificant as long the soil remains unsaturated as the wetting front moves. The reliability index results are however become noticeable if the infiltrated rainfall produces saturation and positive pore-water pressure. The difference in results may be attributed to the wetting front depth and its saturation that depends on saturated-unsaturated hydraulic conductivity and matric suction head.
机译:众所周知,由于浸润前沿移动,降雨入渗会降低基质吸力的不饱和抗剪强度,这是由于基质吸力的降低。但是,基质吸力降低多少会影响边坡稳定性结果仍是未知的。本文根据单个降雨强度的可靠性指标,给出了润湿锋面深度,基体吸力和稳定性结果的数值结果。使用修正的Mohr-Coulomb破坏准则结合有限元饱和-不饱和渗流模型对五种土壤进行分析。数值结果表明,降雨入渗土壤对基质吸力的影响不同。只要土壤随着润湿锋线的移动而保持不饱和状态,可靠性指标结果的变化就可以忽略不计。但是,如果渗入的降雨产生饱和度和正的孔隙水压力,则可靠性指标的结果将变得明显。结果的差异可能归因于润湿前深度及其饱和度,其取决于饱和-不饱和水力传导率和基质吸头。

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