Stability Analysis of Rock Slope under Rainfall Infiltration Based on A Zero-Thickness Cohesive Element

Weng Lei, Zhijun Wu, Liangliang Ma
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Abstract

There are often a large number of joints, fissures and other water channels in rock slopes. Under the condition of short-term heavy rainfall or continuous rainfall, a large amount of rainwater enters the slope body, which can easily induce landslide disaster on rock slopes. Therefore, it is of great significance to study the stability of rock slope under the infiltration of rainfall. Based on the ABAQUS numerical simulation platform, this paper implements continuous-discontinuous simulation of the deformation and damage of rock slopes under rainfall conditions by embedding zero-thickness cohesive elements and focuses on the effects of rainfall intensity, rainfall duration and rainfall infiltration location on the slope stability using vector method safety factors as indicators. The results show that as the rainfall intensity and rainfall duration increase, the depth of fissures in the slope gradually becomes larger, and the stability of the slope gradually decreases. The farther the initial location of rainfall infiltration is from the shoulder of the slope, the shorter the rain-induced fissure extension length is and the better the stability of the slope is. The research results provide reference for the engineering treatment of rock slope under rainfall conditions.
基于零厚度黏结单元的降雨入渗岩质边坡稳定性分析
岩质边坡中常存在大量节理、裂隙等水通道。在短期强降雨或连续降雨条件下,大量雨水进入坡体,极易诱发岩质边坡滑坡灾害。因此,研究降雨入渗作用下岩质边坡的稳定性具有重要意义。基于ABAQUS数值模拟平台,通过嵌入零厚度内聚元,实现降雨条件下岩质边坡变形与破坏的连续-不连续模拟,并以向量法安全系数为指标,重点研究降雨强度、降雨持续时间和降雨入渗位置对边坡稳定性的影响。结果表明:随着降雨强度和降雨持续时间的增加,边坡裂缝深度逐渐变大,边坡稳定性逐渐降低;降雨入渗初始位置离坡肩越远,雨致裂缝扩展长度越短,边坡稳定性越好。研究结果可为降雨条件下岩质边坡的工程处理提供参考。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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