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

机译:降雨对花岗岩残余土坡稳定性的影响

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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:观察结果表明,在降雨期间或之后发生了绝大多数山体滑坡。将雨水进入斜坡将增加坡度的重量,改变坡度的孔隙水压,并减少土壤的剪切强度。在不饱和的土坡中,可以被视为负孔隙水压力的基质吸力是影响斜坡稳定性的主要因素之一。通过在各种降雨强度下模拟坡度的负孔隙水压分布,在有限元软件 - 地理斜坡的帮助下,通过模拟了坡度的负孔隙水压分布,分析了降雨对负孔隙水的影响及斜坡的稳定性。渗透/ w。通过计算花岗岩残留土坡面项目,阐述了基质抽吸对斜坡稳定性的重要性。结果表明,如果没有考虑基质抽吸,显然明显低估了斜率的安全系数。它与实际情况不同。

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