The study in deformation and destruction mechanism of Qianjiangping landslide in Three Gorges Reservoir area

Rihong Yang, Zhihua Wang, Jin-zhong Yang, Zuguo Wang
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Abstract

The advanced digital image processing technique was used in the high resolution remote sensing images processing, aero photos before landslide happened and the Quick Bird image after landslide were processed. The technique of digital landslide, 3D visualization and man-machine interactive interpretation were used to analyze the geomorphologic features of remote sensing images. From the characteristic of the deposit, it is deduced that the paleo-landslide was a deep and consequent rock landslide with large-scale deposit, the entire deposit of "7.13" landslide is similar to the paleo-landslide, and the displaced volume is 15×106m3. Based on the geology theory, this paper synthetically compared the effect of landslide between the rainfall and the water level rising. It is concluded that the main inducing factors is the first stage storage of the Three Gorges and the continuous rainfall is triggering factor. Synthetically analyzing the process of slide and the characteristic of deposit, it is deduced that the middle and front part of Qianjiangping landslide is push-type sliding while the back part is drag sliding, the pattern of deformation and destruction is front verge leading sliding-drag.
三峡库区钱江坪滑坡变形破坏机制研究
采用先进的数字图像处理技术对高分辨率遥感图像、滑坡发生前的航空照片和滑坡发生后的Quick Bird图像进行处理。采用数字滑坡技术、三维可视化技术和人机交互解译技术对遥感影像进行地貌特征分析。根据矿床特征推断,该古滑坡为深部顺性大型滑坡,“7.13”滑坡整体与古滑坡相似,位移量为15×106m3。以地质理论为基础,综合比较了降雨与水位上升对滑坡的影响。认为三峡一期库容是主要诱发因素,连续降雨是诱发因素。综合分析滑坡过程和沉积特征,推断黔江坪滑坡中、前段为推滑型,后段为拖滑型,变形破坏模式为前缘导滑-拖滑型。
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