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The 2 September 2014 Shanshucao landslide, Three Gorges Reservoir, China

机译:2014年9月2日,中国三峡水库山书草滑坡

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摘要

A Shanshucao landslide, large displacement landslide, took place on 2 September 2014, at 13:19 in Zigui County, Hubei Province, central China, which was about 42 km from the Three Gorges Dam. It was located on the left bank of Luogudong River, which was a secondary tributary of the Yangtze River. Just as the well-known Qianjiangping landslide, this landslide was considered to be one of the longest displacement consequent slope failures, which was characterized by red layer rock landslide. This event has become an outstanding and valuable reference for landslide study and is of particular importance for understanding the influence of the stability of the slope in the Three Gorges Reservoir Area. The geomorphological and geological conditions of the landslide were investigated to identify and characterize previously discontinuous and slide stratum bed. The hydrogeological and geomechanical features were also analyzed. It was found that the landslide was triggered by both the long and heavy rainfall and the rising water level of the reservoir at high speed.
机译:2014年9月2日13:19,在中国中部湖北省Zi归县发生了山书草滑坡,即大位移滑坡,距三峡大坝约42公里。它位于罗古洞河左岸,罗古洞河是长江的次要支流。正如著名的钱江坪滑坡一样,该滑坡被认为是位移最长的滑坡之一,其特征是红层岩石滑坡。该事件已成为滑坡研究的杰出和有价值的参考,对于理解三峡库区斜坡稳定性的影响尤其重要。研究了滑坡的地貌和地质条件,以识别和表征先前不连续的滑层地层。还分析了水文地质和地质力学特征。结果发现,滑坡是由长时间的降雨和暴雨以及水库高速上升的水位引起的。

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