IMHE OpenIR  > 山地学报
Alternative TitleDigital Simulation of Guanling Long Distance Landside Clastic Flow
倪振强1,2,3; 阿发友1,2,3; 孔纪名1,2; 崔云1,2,3; 田述军1,2,3
Corresponding Author孔纪名
Source Publication山地学报
Contribution Rank1
Other AbstractLong landside debris flow is a geological disaster with great size, exceptional speed, long distance movement, great energy, and the unusually high mobility and other characteristics. Becuause of these features with the geological disaters are often very shory time, which are dangerous. Guanling "6.28" long distance landside debris flow caused serious casualties and property losses, Analyze the failure mechanism, through the numerical simulation method, to simulate the formation of landslide. We got that the large-scale landslide deformation obtained is a complex mechanical mechansim of geological processes, soil landslide and rock slide interaction, showing a complexand progressive destruction of property; the coordination mechanism of locked section and the creeping segment; landsilde debris flow got in the geological disaster chain formation mechanism. Analysis results have certain significance for impoving the umderstanding on long distance landslide debris debris, and it will be a tyical and academic significance and also provide a reference for other similar type of mountain hazards mechainism.
Keyword灾害 远程滑坡 碎屑流 形成机理 数值模拟
Indexed By其他
Document Type期刊论文
Corresponding Author孔纪名
First Author Affilication中国科学院水利部成都山地灾害与环境研究所
Corresponding Author Affilication中国科学院水利部成都山地灾害与环境研究所
Recommended Citation
GB/T 7714
倪振强,阿发友,孔纪名,等. 关岭滑坡-碎屑流形成机理数值模拟[J]. 山地学报,2011,29(S):28-34.
APA 倪振强,阿发友,孔纪名,崔云,&田述军.(2011).关岭滑坡-碎屑流形成机理数值模拟.山地学报,29(S),28-34.
MLA 倪振强,et al."关岭滑坡-碎屑流形成机理数值模拟".山地学报 29.S(2011):28-34.
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