IMHE OpenIR  > 山地灾害与地表过程重点实验室
The characteristics of genesis and evolution of debris flow fans based on fixed point observation
Language英语
Zhang, Jinshan1,2; Shen, Xingju3,4
2011
Source Publication5th International Conference on Debris-Flow Hazards Mitigation: Mechanics, Prediction, and Assessment
Author of SourceR. Genevos ; D.L. Hamlion ; A. Prestinuizi
Pages283-292
meeting5th International Conference on Debris-Flow Hazard Mitigation: Mechanics, Prediction, and Assessment
Conference Date2011
Conference PlacePadua
CountryItaly
PublisherAmerican Society of Civil Engineers (ASCE)
Contribution Rank1
AbstractThe Liziao Gully and Huajiaopo Gully are 2 tributaries of Jiangjia Gully in its middle reaches, a well-known gully for its debris flows of high frequency. The two gullies are extremely similar in features of their drainage basins, including high frequency of debris flows and rapid formulation of debris flow fans. During field studies, process of movement and accumulation of debris flow fan are observed, and sampling and analysis of debris flows with different features are conducted. Terrain of debris flow fans and their longitudinal and transverse profiles are measured prior to and post rainy season each year. By analyzing evolution process, planar features, longitudinal and transverse section, accumulation rate and other parameters of debris fans in the 2 tributary gullies during 2006-2008, following conclusions are obtained: (1) Influenced by geological and lithological features in its drainage basin, Huajiaopo Gully is larger in unit weight and grain size of its debris flow, and its accumulation fan is formulated in Mound-shape. Whereas debris flow in Liziao Gully is smaller in unit weight and grain size, with debris flows moving on the fan and its accumulation is in a linguiform. Further evolution of debris flow fans is finished with Mound-shaped accumulation and channel shifting. (2) In case of accumulation in main channel, debris flow fans in tributary gullies are formed by aggradation and aggradation height is uniformly distributed at upper and lower parts of the fan. (3) Slopes of debris flow fans on both longitudinal and transverse sections are largely determined by fluidic properties of debris flows. The greater the unit weight is, the larger the slope of debris flows on both longitudinal and transverse sections is. © 2011 Casa Editrice Universita La Sapienza.
KeywordDebris flows Discharge estimation Flow depth Jiangjia Gully Reliable methods Surge
DOI10.4408/IJEGE.2011-03.B-102
ISBN9788895814469
Indexed ByEI
Accession numberAccession number:20122315082176
Citation statistics
Document Type会议论文
Identifierhttp://ir.imde.ac.cn/handle/131551/24064
Collection山地灾害与地表过程重点实验室
Corresponding AuthorZhang, Jinshan
Affiliation1.Key Laboratory of Mountain Hazard and Surface Processes, Chinese Academy of Sciences, Sichuan Chengdu 610041, China;
2.Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Ministry of Water Conservancy, Sichuan Chengdu 610041, China;
3.Graduate School of the Chinese Academy of Sciences, Beijing 100049, China;
4.College of Tourism and History and Culture, Southwest University for Nationalities, Sichuan Chengdu 610041, China
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
Zhang, Jinshan,Shen, Xingju. The characteristics of genesis and evolution of debris flow fans based on fixed point observation[C]//R. Genevos, D.L. Hamlion, A. Prestinuizi:American Society of Civil Engineers (ASCE),2011:283-292.
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