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湖北省巴东县桐木园山坡型泥石流的形成机理及预警指标——以2003—03—31强降雨过程为例
引用本文:张永双,吴树仁,赵越,何锋,石菊松,罗菊英.湖北省巴东县桐木园山坡型泥石流的形成机理及预警指标——以2003—03—31强降雨过程为例[J].地质通报,2003,22(10):833-838.
作者姓名:张永双  吴树仁  赵越  何锋  石菊松  罗菊英
作者单位:1. 中国地质科学院地质力学研究所,北京,100081
2. 湖北省巴东县气象局,湖北,巴东,444300
基金项目:科技部重点专项资金项目(No.2001DIA20027),国家自然科学基金项目(No.40102025)
摘    要:2003年3月31日,巴东县在连续强降雨作用下出现多处山体斜坡地质灾害,造成大量房屋破坏和人员伤亡。通过现场综合调查,笔者认为灾害比较严重的桐木园斜坡灾害体发球典型的山坡型泥石流,着重剖析了该山坡型泥石流的变形特征及其成灾机理,并探讨了斜坡浅表层松散岩土体快速变形的临界降雨阀值和预指标。

关 键 词:山坡型泥石流  成灾机理  强降雨过程  预警指标  湖北  巴东县
文章编号:1671-2552(2003)12-0833-06
修稿时间:2003年5月15日

Formation mechanism of debris flow on the Tongmuyuan slope andits early warming index--A case study of the hard rain processon March 31, 2003 in Badong County, Hubei Province
ZHANG Yongshuang,WU Shuren,ZHAO YueHE Feng,SHI Jusong,LUO Juying.Formation mechanism of debris flow on the Tongmuyuan slope andits early warming index--A case study of the hard rain processon March 31, 2003 in Badong County, Hubei Province[J].Geologcal Bulletin OF China,2003,22(10):833-838.
Authors:ZHANG Yongshuang  WU Shuren  ZHAO YueHE Feng  SHI Jusong  LUO Juying
Abstract:Several slope geohazards induced by continuous rainstorm occurred in Badong County on March 31, 2003, which resulted in destruction of many houses and casualties. On the basis of field investigation, the authors believe that the severe hazard mass on the Tongmuyuan slope belongs to a typical slope-type debris flow, i.e. the debris flow on slope. Its deformation characteristics and corresponding formation mechanisms are analyzed and the critical rain threshold value and early warning indices for predicting the rapid deformation of loose rock-soil masses on the shallow slope surface are discussed.
Keywords:debris flow on slopes  hazard formation mechanism  rain intensity  early warning  
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