Classification and Initiation Conditions of Debris Flows in Linzhi Area,Tibet

HU Gui-sheng; CHEN Ning-sheng; DENG Ming-feng; WANG Yuan-huan

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Classification and Initiation Conditions of Debris Flows in Linzhi Area,Tibet

- Classification and Initiation Conditions of Debris Flows in Linzhi Area,Tibet
- Bulletin of Soiland Water Conservation Vol. 30, Issue 2, Pages: 193-197(2011)
- 作者机构：
  
  1. 中国科学院山地灾害与地表过程重点实验室
  2. 中国科学院水利部成都山地灾害与环境研究所
  3. 中国科学院研究生院
- 作者简介：
- 基金信息：
- DOI：
  CLC：
- Published：2011
- 稿件说明：
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HU Gui-sheng, CHEN Ning-sheng, DENG Ming-feng, et al. Classification and Initiation Conditions of Debris Flows in Linzhi Area,Tibet[J]. Bulletin of Soiland Water Conservation, 2011, 30(2): 193-197.
DOI：

HU Gui-sheng, CHEN Ning-sheng, DENG Ming-feng, et al. Classification and Initiation Conditions of Debris Flows in Linzhi Area,Tibet[J]. Bulletin of Soiland Water Conservation, 2011, 30(2): 193-197. DOI：

摘要

西藏林芝地区是我国泥石流灾害最为严重的地区之一

特别是近年来受全球气候变化的影响

冰川融化速度加快

冰川融水型泥石流灾害频频发生

危害极其严重。自2009年7月中旬开始

对该地区林芝、米林、波密、察隅4县30条泥石流沟做了系统调查。在研究该区域20条较具代表性泥石流沟的基础上

结合该区域已有研究资料

按泥石流形成的激发条件将其分为降雨型泥石流

冰川降雨型泥石流

冰崩、雪崩型泥石流

冰湖、堰塞湖溃决型泥石流共4类。进而从地形地貌、物源、水源及气温等方面分析了其形成条件。并在此基础上提出了针对性防灾建议。

Abstract

Linzhi area of Tibet is one of the most dangerous regions threatened by debris flows in China.Under the influence of global warming

the melting rate of glacier has accelerated in this area

leading to frequent initiations of glacier-melting debris flows

which is severely hazardous.Since the middle of July

2009

the authors had carried out systematic investigations regarding approximately thirty debris flow gullies in counties of Linzhi

Milin

Bomi and Chayu in Linzhi area.Based on analysis of the twenty typical debris flow gullies and related historic documents

debris flows were divided into four classes according to initial water conditions

namely

rainfall-induced debris flow

glacier-rainfall-induced debris flow

avalanche-induced debris flow

and lake-outburst-induced debris flow.The initiation conditions were analyzed regarding landform

soil source

water source and air temperature.Specific advices based on the analysis were recommended for disaster prevention.

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Related Author

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WANG Yong

YU Shu-jiao

FENG Hang-jian

YANG Cheng-lin

CHEN Ning-sheng

DENG Ming-feng

DENG Hu

Related Institution

Institute of Geology and Minerals of Zhejiang Province

Key Lab of Mountain Hazards and Surface Processes,Institute of Mountain Hazards and Environment, Chinese Academy of Sciences

College of Earth Science,Chengdu University of Technology

The Institute of Exploration Technology, CAGS

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