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INFLUENCES OF A RAINFALL ON THE STABILITY OF GRANITE RESIDUAL SOIL SLOPES

机译:降雨对花岗岩残质土壤边坡稳定性的影响

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Observations showed that an overwhelming majority of landslides occurred during or after a rainfall.Infiltration of rainwater into slope would increase weight of the slope, change pore water pressure in the slope, and reduce shear strength of the soil. In an unsaturated soil slope, the matrix suction, which could be regarded as negative pore water pressure, was one of the major factors that influenced the stability of a slope. The influences of a rainfall on negative pore water pressures and the stability of a slope have been analyzed in this paper by simulating negative pore water pressure distribution of the slope under various rainfall intensities, with the help of a finite element software—GEO-SLOPE-SEEP/W. The importance of matrix suction to the stability of a slope was elaborated through the calculation of a granite residual soil slope project. Results showed that the safety factor of a slope was obviously underestimated if no matrix suction was considered. It differs much from the actual case.
机译:观测表明,绝大多数山体滑坡发生在降雨期间或降雨之后,雨水渗入斜坡会增加斜坡的重量,改变斜坡的孔隙水压力,并降低土壤的抗剪强度。在非饱和土质边坡上,基质吸力可以看作是负孔隙水压力,是影响边坡稳定性的主要因素之一。本文借助于有限元软件GEO-SLOPE-,通过模拟各种降雨强度下斜坡的负孔隙水压力分布,分析了降雨对负孔隙水压力和边坡稳定性的影响。 SEEP / W。通过计算花岗岩残余土的边坡工程,阐述了基体吸力对边坡稳定性的重要性。结果表明,如果不考虑基质吸力,则斜坡的安全系数明显被低估。它与实际情况有很大不同。

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