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绵竹市清平乡塌洞沟泥石流发育特征及成因机制分析

唐梁

人民珠江Issue(6):99-101,3.
人民珠江Issue(6):99-101,3.DOI:10.3969/j.issn.1001-9235.2014.06.028

绵竹市清平乡塌洞沟泥石流发育特征及成因机制分析

Characteristics of Collapse Debris Flow Development in Qingping Village in Mianzhu City and Genetic Mechanisms Analysis

唐梁1

作者信息

  • 1. 成都理工大学环境与土木工程学院,四川 成都 610059; 重庆蜀通岩土工程有限公司,重庆 401147
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摘要

Abstract

Affected by the 5.12 earthquake,the Tadonggou ditch domain generated a lot of loose material source,which has erupted re-peatedly debris flows in heavy rain and other predisposing conditions. Through a detailed investigation of the debris flow,we divided the ditch domain into formation circulation area and stacking area,and study the alluvial deposition characteristics and accumulation characteristics of each section. We also analyzed the formation mechanism of the debris flow.

关键词

塌洞沟/泥石流/发育特征/成因机制

Key words

Tadong ditch/Debris flow/Development characteristics/Formation mechanism

分类

建筑与水利

引用本文复制引用

唐梁..绵竹市清平乡塌洞沟泥石流发育特征及成因机制分析[J].人民珠江,2014,(6):99-101,3.

人民珠江

1001-9235

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