土壤孔隙度对滑坡易发边坡稳定性的影响分析

The activation of landslide processes most often occurs as a result of water saturation of the soil, which consequently affects both the strength parameters of clay or loam soil and the weight of the mass. The combination of changing factors during water saturation leads to landslide collapse. The article presents the dependence of slope stability on the geometric parameters of the terrain and soil porosity. 滑坡过程的激活通常是由于土壤的水分饱和 从而影响粘土或壤土的强度参数和质量的重量。 水饱和过程中变化因素的组合导致滑坡塌陷。 本文介绍了边坡稳定性对地形几何参数和土壤孔隙度的依赖性。