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都江堰八一沟8·13泥石流的形成条件分析

覃怡 郑洪春

南水北调与水利科技2013,Vol.11Issue(4):101-104,4.
南水北调与水利科技2013,Vol.11Issue(4):101-104,4.DOI:10.3724/SP.J.1201.2013.04101

都江堰八一沟8·13泥石流的形成条件分析

Initiation Conditions for the 8·13 Debris Flows in Bayi Gully of Dujiangyan

覃怡 1郑洪春1

作者信息

  • 1. 四川大学水利水电学院,成都610065
  • 折叠

摘要

Abstract

The large number of collapse and landslide triggered by the 2008 Wenchuan earthquake had caused a lot of casualties.After the earthquake,the deposits from the collapse and landslide became the primary source for debris flows,which greatly increased the occurrence of earthquake-induced hazards.In order to carry out the hazards prevention work,this paper selected the 8.13 debris flows in the Bayi Gully as the example to investigate its initiation conditions.Field investigation and remote sensingmeasures were used,and three fundamental conditions to initiate the debris flows were analyzed including landform,soil source,and water source.The results suggested the initiation conditions were favor for the occurrence of debris flows.Additionally,theanalytical method applied in this paper can provide references for the study of debris flows under similar conditions.

关键词

八一沟/泥石流/形成条件

Key words

Bayi Gully/ debris flows/ initiation condition

分类

天文与地球科学

引用本文复制引用

覃怡,郑洪春..都江堰八一沟8·13泥石流的形成条件分析[J].南水北调与水利科技,2013,11(4):101-104,4.

基金项目

国家自然科学基金资助项目(51079093) (51079093)

四川省科技支撑计划项目(2011SZ0190) (2011SZ0190)

南水北调与水利科技

OA北大核心CSCDCSTPCD

2096-8086

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