Formation conditions and risk evaluation of glacial debris flow disasters along International Karakorum Highway (KKH) | |
Language | 英语 |
Yang, Zhiquan1,2,3![]() ![]() | |
2011 | |
Source Publication | 5th International Conference on Debris-Flow Hazards Mitigation: Mechanics, Prediction, and Assessment |
Author of Source | R. Genevos ; D.L. Hamlion ; A. Prestinuizi |
Pages | 1031-1037 |
meeting | 5th International Conference on Debris-Flow Hazard Mitigation: Mechanics, Prediction, and Assessment |
Conference Date | 2011 |
Conference Place | Padua |
Country | Italy |
Publisher | American Society of Civil Engineers (ASCE) |
Contribution Rank | 1 |
Abstract | The area of International Karakorum Highway (KKH), a mountain highway connecting northern Pakistan with northwestward China, is an area with dense and frequent glacial debris flow disasters due to the special glacial geology and landform. In this area the three basic conditions inducing glacial debris flow have developed,namely the widely distributed glacial till and ice-snow colluvium, which arise from collapse and landslide, provide the main solid sources of glacial debris flow; the very high and steep slopes, take the landform of steps with a very big gradient, to provide the moving way for glacial debris flow; and the ice-snow melt water from high-mountain, the melt water of glacier avalanche and glacial lake outburst flood provide glacial debris flow for the force to move. The valley-type debris flow is the main type of glacial debris flow occurred in the area, and it can be classified into further three sub-types according to the water source, namely glacierablation type debris flow, glacier-avalanche type debris flow and glacial-lake-outburst- flood type debris flow. Based on in situ investigation and analysis of seven controlling variables of glacial debris flow, such as occurrence frequency, catchment areas, volumes of alluvial fan, estimated outflow of every time, vegetation coverage, slope and altitudeio evaluate the risk degree of 8 chosen representative glacier debris flows along KKH. The comprehensive fuzzy evaluation method is applied to evaluate the risk degree of glacier debris flow and then the evaluation result shows a good correspond with the practical situation, i.e. this method has a valuable application foreground. © 2011 Casa Editrice Universita La Sapienza. |
Keyword | 2008 wenchuan earthquakes 3D laser scanning system Assessment and monitoring Debris flows Development feature Disaster prevention and mitigations Field observations Niujuan Gully |
DOI | 10.4408/IJEGE.2011-03.B-094 |
ISBN | 9788895814469 |
Indexed By | EI |
Accession number | Accession number:20122315082253 |
Citation statistics | |
Document Type | 会议论文 |
Identifier | http://ir.imde.ac.cn/handle/131551/24067 |
Collection | 山地灾害与地表过程重点实验室 |
Corresponding Author | Yang, Zhiquan |
Affiliation | 1.Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Ministry of Water Conservancy, Chengdu, China; 2.Graduate University of Chinese Academy of Sciences, Beijing, China; 3.Key Laboratory of Mountain Hazards and Earth Surface Processes, Chinese Academy of Sciences, Chengdu, 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 | Yang, Zhiquan,Zhu, Yingyan,Zou, D.H. Steve. Formation conditions and risk evaluation of glacial debris flow disasters along International Karakorum Highway (KKH)[C]//R. Genevos, D.L. Hamlion, A. Prestinuizi:American Society of Civil Engineers (ASCE),2011:1031-1037. |
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Formation conditions(464KB) | 会议论文 | 开放获取 | CC BY-NC-SA | View Application Full Text |
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