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Groundwater Dynamics Analysis of Sanmashan Side Slope in the Three Gorges Reservoir Region, China

机译:中国三峡库区三山山边坡地下水动力学分析

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Sanmashan side slope in the Three Gorges reservoir region is located in the center area of the Xincheng district, Fengjie county, China. Based on the analysis of hydrogeological structure of the studied area, one can conclude that a groundwater reservoir form near the side slope area after the impoundment of the Three Gorges Reservoir, which induces large groundwater pressure on the side slope. In particular, large hydrodynamic pressure will occur in the landslide mass under the condition of the reservoir water level descending significantly, which has bad effects on slope stability. Numerical simulation results show that the seepage force on landslide is 43 times of that under normal situation, as the reservoir water level declining dramatically from 175m to 145m. Thus, the influence of hydrodynamic pressure should be considered in the stability calculation.
机译:三峡库区三幡山边坡位于中国奉杰县新城区的中心地区。基于研究区域的水文地质结构的分析,可以得出结论,三峡库蓄水后侧坡面积附近的地下水储存器形成,这在侧坡上诱导大型地下水压。特别地,在储层水位的条件下显着下降的情况下,在山体内压力下发生大的流体动力压力,这对坡度稳定性具有不良影响。数值模拟结果表明,在正常情况下滑坡上的渗漏力是43倍,因为水库水位从175米下降到14.5米。因此,应在稳定性计算中考虑流体动力学压力的影响。

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