Experiment Study on Soil Properties of Shennv Stream Landslide in Wu Gorge |
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Authors: | ZHAO Xiantao XIANG Jie TANG Hongmei LIANG Xuezhan and HU Jun |
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Institution: | Institute of Geotechnical Engineering, Chongqing Jiaotong University, Chongqing 400074, P. R .China;Institute of Geotechnical Engineering, Chongqing Jiaotong University, Chongqing 400074, P. R .China;Institute of Geotechnical Engineering, Chongqing Jiaotong University, Chongqing 400074, P. R .China;Institute of Geotechnical Engineering, Chongqing Jiaotong University, Chongqing 400074, P. R .China;Institute of Geotechnical Engineering, Chongqing Jiaotong University, Chongqing 400074, P. R .China |
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Abstract: | Accurate obtainting soil parameters of landslide is the key links for landslide stability evaluation and project management . This article takes Shennv Stream landslide in Chongqing Wushan County as an example, implementing unconsolidated and undrained shear test and mineral composition analysis by X ray diffraction for soil in different elevations of landslide ,conducting sensitivity test for various soil parameters of reservoir landslide change with different water level.Study shows that : Mineral composition of soil mainly contains Calcite, Quartz and clay mineral. Hydrophilic minerals in clay mineral have great effect on stability of landslide. Shear strength decreases by influence of water content on cohesion. Cohesion decreases sharply in a quadratic function relation with water content increasing .When water content comes to 18.21% ,change of cohesion tends to be stable.But the internal friction angle of landslide soil decreases linearly in small amplitude with an increase of water content. Research results may provide some important references for rationally choosing strength parameters of soil in similar landslide. |
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Keywords: | Shennv Stream landslide X ray diffraction direct shear test parameters of shear strength water content |
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