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奉节县石王庙滑坡位于重庆市奉节县康乐镇,分布于长江一级支流梅溪河左岸斜坡地带,属侵蚀、剥蚀成因低山河谷地貌,地下水主要由上层滞水及基岩裂隙水组成,是在老岩质崩滑堆积体上发育的次生滑坡。在详述滑坡外貌、地质结构及变形破坏特征的基础上,运用传递系数法进行了滑坡稳定性分析,对多种工况下的稳定性进行验算,同时结合滑坡现状进行了定量分析,结果表明,在持续暴雨条件下滑坡稳定性下降,为滑坡的防治提供了重要依据。
Located in Kangle Town, Fengjie County, Chongqing, the Shiwangmiao landslide in Fengjie County is located in the slope belt on the left bank of the Meixi River, a tributary of the Yangtze River. It belongs to the low mountain valley landscape of erosion and erosion. The groundwater mainly consists of stagnant water in the upper layer and fissure water in bedrock. It is a secondary landslide developed on old rock mass collapse accumulation. Based on the detailed description of the landslide appearance, the geological structure and the deformation and failure characteristics, the landslide stability analysis is carried out by using the transfer coefficient method, the stability under various working conditions is checked, and the landslide status is quantitatively analyzed. The results show that , The stability of the landslide decreases under the continuous rainstorm, which provides an important basis for the prevention and control of the landslide.