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由于黄腊石滑坡群的复活,在三峡大坝正式蓄水之后,结合不同的降雨过程和不同的长江水位分析了石榴树包滑坡的稳定性变化以及因滑坡而引起的涌浪对其上下游的重要城镇和建筑物的影响。
Due to the revival of the Huanglashi landslide group, the stability changes of the Shulinshubao landslide and the importance of the surging caused by the landslide to its upstream and downstream are analyzed after the Three Gorges Dam formally charged with different rainfall processes and different Yangtze River water levels The impact of towns and buildings.