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A large landslide in Zigui County, Three Gorges area

机译:三峡地区Zi归县的大型滑坡

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摘要

On 13 July 2003, a landslide with a volume of approximately 20 x 10(6) m(3) occurred on the left bank of the Qinggan River, Zigui County, Hubei Province, China. As a result, 14 people died and 10 people are missing. A landslide dam was formed, blocking the Qinggan River. A channelized diversion was constructed for prevention of upstream flooding and damage downstream caused by dam breaching. The landslide was a typical translational rockslide in weathered shale and sandstone, a block of which slipped down along the bedding plane. It is estimated that the landslide was caused by the combined effect of the following factors: (i) a bedding plane between incompetent weathered shale and competent sandstone that daylights at or is shallowly buried at the bottom of the Qinggan River; (ii) a thin layer of clayey soil acting as the slip plane that is likely a preexisting shear surface; (iii) excavation of the shale as raw material for brick fabricating on the slope; and (iv) a combination of prolonged rainfall and reservoir impounding.
机译:2003年7月13日,中国湖北省Zi归县清干河左岸发生了体积约为20 x 10(6)m(3)的滑坡。结果,有14人死亡,10人失踪。形成了滑坡坝,阻塞了青干河。为了防止上游水灾和因大坝破坏而对下游造成的破坏,修建了通道化的分流。滑坡是风化的页岩和砂岩中的典型平移岩石滑坡,其中一部分沿顺层平面滑落。据估计,滑坡是由以下因素共同作用引起的:(i)不合格的风化页岩和有效砂岩之间的顺层平面,日光在青干河底部或浅埋在青干河的底部; (ii)薄薄的黏土层作为滑动面,可能是预先存在的剪切面; (iii)在页岩上挖掘页岩作为制造砖的原料; (iv)延长降雨和蓄水库的结合。

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