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“8·13”碱坪沟泥石流形成机理及特征研究
引用本文:褚胜名,余斌,李丽,马煜,吴雨夫,亓星.“8·13”碱坪沟泥石流形成机理及特征研究[J].中国水土保持,2011(8):52-54.
作者姓名:褚胜名  余斌  李丽  马煜  吴雨夫  亓星
作者单位: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,四川,成都,610059
基金项目:教育部创新团队发展计划项目
摘    要:2010年8月13日在强降雨的作用下,四川省都江堰市龙池镇碱坪沟沟床启动并带动沟道两侧固体物质运动,形成大规模泥石流,冲毁沟口农家乐、龙池公路及沟口一处居民供水设施。碱坪沟泥石流是典型的震区沟谷型泥石流,通过分析泥石流的形成机理及容重、流速、流量、冲出量等动力学参数,得出泥石流的危险范围和威胁对象,并根据沟道中大量崩滑体等各类物源的堆积情况,在降雨作用下对其再次暴发泥石流的可能性进行了分析预测,还根据沟口现场堆积情况提出了防治建议。

关 键 词:地震灾区  泥石流  形成机理  特征  碱坪沟

Forming Mechanism and Characteristics of Debris Flow Happened on August 13,2010 in Jianping Gully
CHU Sheng-ming,YU Bin,LI Li,et al..Forming Mechanism and Characteristics of Debris Flow Happened on August 13,2010 in Jianping Gully[J].Soil and Water Conservation In China,2011(8):52-54.
Authors:CHU Sheng-ming  YU Bin  LI Li  
Institution:CHU Sheng-ming,YU Bin,LI Li,et al.(State Key Laboratory of Geo-Hazard Prevention and Geo-Environment Protection,Chengdu University of Technology,Chengdu,Sichuan 610059,China)
Abstract:After the bed was activated,the solid material on both sides of Jianping Gully was driven,forming a large-scale debris flow in Longchi Township of Dujiangyan City in Sichuan on August 13,2010,under the action of heavy rain.The debris flow washed away farm tourism facilities,Longchi highway and drinking water supply facilities at the mouth of gully.This is a typical gully-type debris in the earthquake-stricken region.Through analysis on the forming mechanism and dynamic parameters of volume weight,velocity,d...
Keywords:earthquake-stricken region  debris flow  forming mechanism  characteristic  Jianping Gully  
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