Analysis of condition of startup of gully debris flow after earthquake—The hydraulic mechanism of instability of loose deposits in rainfall
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Analysis of condition of startup of gully debris flow after earthquake—The hydraulic mechanism of instability of loose deposits in rainfall
Vol. 33, Issue 10, (2012)
作者机构:
1. 中国科学院 水利部成都山地灾害与环境研究所,成都,610041
2. 中国矿业大学 深部岩土力学与地下工程国家重点实验室,江苏,徐州,221008
3. 成都理工大学 地质灾害防治与地质环境保护国家重点实验室,成都,610041
作者简介:
基金信息:
DOI:
CLC:U418.5+6
Online First:19 October 2012,
Published:2012
稿件说明:
移动端阅览
WU Yong, HE Si-ming, PEI Xiang-jun, et al. Analysis of condition of startup of gully debris flow after earthquake—The hydraulic mechanism of instability of loose deposits in rainfall[J]. 2012, 33(10).
DOI:
WU Yong, HE Si-ming, PEI Xiang-jun, et al. Analysis of condition of startup of gully debris flow after earthquake—The hydraulic mechanism of instability of loose deposits in rainfall[J]. 2012, 33(10).DOI:
Analysis of condition of startup of gully debris flow after earthquake—The hydraulic mechanism of instability of loose deposits in rainfall
Because large quantities of loose deposits were accumulated in gully after “5•12” Earthquake
the occurrence probability of gully debris flow is enhanced greatly in rainfall. However
due to the special conditions of provenance and disaster environment
the traditional theory cannot be used to expound the mechanism of gully debris flow and prevent the disaster effectively as ever after the event. Here
based on hydrology
the hydrological model of ground water table in loose deposits is established first. Then by aid of hydraulic theory
the change of hydraulic characteristics and the variation of hydraulic power with the rising of groundwater level are analyzed. Furthermore
the calculation formulas of hydrodynamic and hydrostatic pressure are also proposed. Finally
by applying infinite slope theory in calculation of sliding force
anti-sliding force and residual sliding force acting on each segment
the failure mechanism of accumulation body is illustrated clearly with an example. The result indicates the failure of loose deposits in rainfall is the result of increase of the hydraulic power with the rising of groundwater level. Those deposits which have small coefficient
gentle slope
narrow-deep gully and large basin would be easy to fail because of its high hydraulic pressure generating in rainstorm
and the failure modes can be divided into two types according to residual sliding force as pushing failure and hauling failure.
Engineering vulnerability assessment for bridges and tunnels harmed by debris flow hazards
Experiment study of fractal feature and relationship between fractal dimension and permeability coefficient of gravelly soil in debris flow source area
Debris flow susceptibility analysis based on theories of minimum entropy and uncertainty measurement
Screening of debris flow risk factors and risk evaluation based on rank correlation
Experimental study on shear characteristics of mudstone under combined action of stress-dry-wet cycles
Related Author
XU Lin-rong
CHEN Shu-yang
CAO Lu-lai
HE Na
CHEN Ning-sheng
ZHU Yun-hua
YANG Jian-yuan
YANG Cheng-lin
Related Institution
School of Civil Engineering, Central South University
East China Construction Engineering Corporation of Zhejiang
School of Civil Engineering,Henan Polytechnic University
University of Chinese Academy of Sciences
Key Laboratory of Mountain Hazards and Surface Process, Institute of Mountain Hazards and Environment, Chinese Academy of Sciences and Ministry of Water Resources