Fracture of a slope by percolating
Lu XB(鲁晓兵); Zhang XH(张旭辉); Hu KH; Chen XQ; Lu, XB (reprint author), Chinese Acad Sci, Inst Mech, Lab Hydraul & Ocean Engn, Beijing 100080, Peoples R China
会议录名称GEOMECHANICS AND GEOTECHNICS: FROM MICRO TO MACRO, VOLS 1 AND 2
2011
页码925-931
会议名称International Symposium on Geomechanics and Geotechnics - From Micro to Macro
会议日期OCT 10-12, 2010
会议地点Shanghai, PEOPLES R CHINA
摘要A theoretical analysis based on a pseudo-three-phase media is presented, and the instability of a slope causing the debris flow is studied. The occurrence of fractures (or water films) in saturated soils in two cases is analyzed. The first case is that the water is forced to percolate through the soil upwards. A perturbation method is used in this case to obtain an approximate solution to explain the formation mechanism of cracks. The second case is about the cracks in liquefied soils. Numerical analysis and theoretical analysis are processed for this case. The formation of fractures in saturated grain accumulation under gravity is due to the blocking by redeposit of finer grains. The formation of fractures presents a sliding surface for landslides and debris flow.
关键词Fracture Slope Percolation Debris Flow Mechanism Liquefaction Sand
WOS记录号WOS:000291373800138
课题组名称LMFS海洋土力学(LHO)
ISBN号978-0-415-61295-1
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收录类别CPCI-S ; EI
语种英语
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文献类型会议论文
条目标识符http://dspace.imech.ac.cn/handle/311007/45218
专题水动力学与海洋工程重点实验室(2009-2011)
通讯作者Lu, XB (reprint author), Chinese Acad Sci, Inst Mech, Lab Hydraul & Ocean Engn, Beijing 100080, Peoples R China
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Lu XB,Zhang XH,Hu KH,et al. Fracture of a slope by percolating[C]GEOMECHANICS AND GEOTECHNICS: FROM MICRO TO MACRO, VOLS 1 AND 2,2011:925-931.
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