土质边坡非饱和渗流及其稳定性研究OA北大核心CSTPCD
Study on unsaturated seepage and stability of soil slope
为研究降雨过程及雨停后土质边坡整体渗流场及稳定性变化情况,运用FLAC3D软件对其进行数值模拟分析,并采用室外降雨模拟试验验证模拟结果.研究结果表明:降雨入渗过程中从坡脚开始破坏,主要表现为浅层滑动;降雨停止初期,雨水会继续下渗,湿润峰深度持续下移,安全系数仍有下降的趋势;雨停中后期,随着土体水分的减少,安全系数开始回升;降雨强度与坡度的增大对边坡稳定性不利.研究结论为解决非饱和土流-固耦合问题提供新思路.
In order to study the overall seepage field and stability changes of the soil slopes during rainfall and after the rain stops,numerical simulation analysis is carried out by using FLAC3D,and the simulation results are verified by using outdoor rainfall simulation tests.The results of the study show that rainfall infiltration process from the foot of the slope began to damage,mainly in the form of shallow sliding;during the rainfall cessation of the initial period,the rain will continue to infiltrate,the depth of the wetting peak continues to move downward,and the coefficient of safety still has a tendency to decline;In the mid to late rainy season,the factor of safety begins to pick up as the soil moisture decreases;the increase in rainfall intensity and slope gradient is detrimental to slope stability.The research results provide a new idea for solving the unsaturated soil flow-consolidation coupling problem.
何玉琼;赵鋆嬉;张家明;唐磊;董文杰
昆明理工大学 交通工程学院,云南 昆明 650500昆明理工大学 建筑工程学院,云南 昆明 650500
交通运输
土质边坡非饱和渗流数值分析稳定性分析FLAC3D软件降雨
soil slopesunsaturated seepagenumerical analysisstability analysisFLAC3Drainfall
《辽宁工程技术大学学报(自然科学版)》 2024 (004)
408-416 / 9
国家自然科学基金项目(41807258);云南省交通厅项目(云交科教便[2022]4号)
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