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矮子沟泥石流影响因素及运动参数分析

Research on Influential Factors and Dynamic Characteristics of a Debris Flow in Aizi Gully

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【作者】 贺拿陈宁生朱云华杨建元

【Author】 HE Na1,2,CHEN Ning-sheng1,ZHU Yun-hua1,2,YANG Jian-yuan3(1.Key Laboratory of Mountain Hazards and Surface Process,Chengdu Institute of Mountain Hazards and Environment,M.W.R,C.A.S,Chengdu,Sichuan 610041,China;2.University of Chinese Academy of Sciences,Beijing 100049,China;3.East China Construction Engineering Co.,Ltd.of Zhejiang,Hangzhou,Zhejiang 310030,China)

【机构】 中国科学院 水利部成都山地灾害与环境研究所,山地灾害与地表过程重点实验室中国科学院大学浙江华东建设工程有限公司

【摘要】 通过对矮子沟流域进行现场勘查,收集相关气象及水文等资料,获取矮子沟流域的地形地貌特征、不良地质体分布规律、地震活动等数据,结合矮子沟流域的地质条件及降雨特征,对矮子沟泥石流的影响因素进行分析,探讨矮子沟泥石流的形成过程。在此基础上选取五个典型断面结合经验公式进行运动参数的分析计算,经计算沟口处断面的泥石流的流速为7.54 m/s,流量为948.63 m3/s,此次泥石流总量为60.08万m3,这些运动参数可以为矮子沟泥石流防治方案的选择及防治工程的设计提供参考。

【Abstract】 After the field survey in Aizi gully and relevant data collection,the data about the morphology,bad geology distribution rules and earthquake activity history in Aizi gully are obtained,and combined with the geological conditions and rainfall characteristics of the gully,the influential factors for a debris flow of the gully are analyzed,then the forming process of the debris flow of the gully is discussed.Based on the analysis mentioned above,five typical cross-sections are selected together with empirical formula so as to calculate the related dynamic parameters.Through the calculation,it is obtained that the velocity and discharge at the outlet are 7.54 m·s-1 and 948.63 m3·s-1 respectively,and the total volume of this debris flow is 60.08×104 m3.All these dynamic parameters could play an important role in the selection of prevention measures and the design of prevention projects for the debris flow of Aizi gully.

【基金】 十二五国家科技支撑计划课题(2011BAK12B02);国家自然科学基金青年科学基金项目(41201555);中国科学院重点部署项目(KZZD-EW-05-01)
  • 【文献出处】 水利与建筑工程学报 ,Journal of Water Resources and Architectural Engineering , 编辑部邮箱 ,2013年01期
  • 【分类号】P642.23
  • 【被引频次】7
  • 【下载频次】154
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