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河北省元氏县佃户营泥石流灾害形成机理及预报方法的研究

Research on the Forming Mechanism and Forecasting of Debris Flow at Dianhuying,Yuanshi County,Hebei Province

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【作者】 王维早杨涛许强

【Author】 WANG Wei-zao1,2,3,YANG Tao2,XU Qiang1(1.State Key Laboratory of Geohazard Prevention and Geoenvironment Protection,Chengdu University of Technology,Chengdu 610059,China;2.College of Economics,Shijiazhuang University, Shijiazhuang 050031,China;3 Key Laboratory of Water Resources Sustainable Utilization and Exploitation,Shijiazhuang 050031,China)

【机构】 成都理工大学"地质灾害防治与地质环境保护"国家重点实验室石家庄经济学院河北省水资源可持续利用与开发重点实验室

【摘要】 元氏县佃户营是河北省太行山区主要泥石流地质灾害频发区,在现场勘察调查的基础上,对元氏县佃户营泥石流的成因进行了详细的研究,研究表明:元氏县佃户营泥石流形成的物源条件、降雨条件和地势条件均满足泥石流的形成条件,且形成条件充分。在前人研究的基础上,对元氏县佃户营的降雨条件加以分析和研究,从降雨方面给出该泥石流发生的概率。对该泥石流沟的物源及该泥石流发生后的残留物质做颗粒试验,通过实验结合前人的研究成果,从颗粒级配方面,给出了该泥石流的发生概率。

【Abstract】 The Taihang Mountain,Yuanshi County,Hebei Province,is the primary area where debris flow always occurs.Based on the survey at the debris flow site,the formation conditions of debris flow were evaluated.Results showed that the material factor,rainfall factor,and physical features satisfied the formation conditions of debris flow in the valley.The formation conditions are sufficient.The authors analyzed and studied rainfall and its relations with the occurrence of this debris flow on the basis of previous studies.The occurrence probability of this debris flow was worked out from rainfall.A kernel experiment on the provenance of this debris flow ditch and its leftover was made.The occurrence probability of this debris flow is worked out from kernel experimentation and previous research.

【基金】 河北省科学技术研究与发展指导计划项目(07276772)
  • 【文献出处】 地球与环境 ,Earth and Environment , 编辑部邮箱 ,2011年01期
  • 【分类号】P642.23
  • 【被引频次】5
  • 【下载频次】203
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