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Analysis of seepage field and stability of clinosol slope under rainfall infiltration

机译:降雨渗透下临床坡渗流场和稳定性分析

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In order to research on slope seepage field and slop stability under rainfall infiltration, this paper combines finite element with limit equilibrium theory to study. The results show that under rainfall, pore water pressure of the slope crest and slope toe in slope wash is greatly influenced by rainfall; Change in the volume moisture content is more sensitive than pore water pressure, volumetric moisture content of each location is increasing quickly at the initial stage of rain, volumetric moisture content in the lower locations is the first to reach saturated due to the continued supply and gravity of the rain; The slope stability reduces with rainfall infiltration, the greater the rainfall intensity, the more obvious decline the slope safety factor.
机译:为了在降雨渗透下研究坡渗流场和斜坡稳定性,本文将有限元与极限平衡理论相结合。结果表明,在降雨下,坡缘和坡脚趾坡脚趾坡脚趾的孔隙水压受降雨量的影响很大;体积水分含量的变化比孔隙水压力更敏感,每个位置的体积水分含量在雨中初始阶段越来越快,较低位置的体积水分含量是由于持续供应和重力而达到饱和的雨;边坡稳定性随着降雨渗透而减少,降雨强度越大,坡度安全系数越明显。

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