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| 基于RS和GIS的雅鲁藏布江林芝-加查段沿线泥石流源地物源分析 | |
| 引用本文： | 王高峰,唐川,王洪德,李为乐,王玉华.基于RS和GIS的雅鲁藏布江林芝-加查段沿线泥石流源地物源分析[J].水土保持通报,2012,32(1):10-13. |
| 作者姓名： | 王高峰 唐川 王洪德 李为乐 王玉华 |
| 作者单位： | 1. 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,四川成都610059／中国地质调查局水文地质环境地质调查中心,河北保定071051 2. 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,四川成都,610059 3. 中国地质调查局水文地质环境地质调查中心,河北保定,071051 4. 河南省基本建设科学实验研究院有限公司,河南郑州,450000 |
| 基金项目： | 国土资源部公益性行业科研专项“青藏高原东南部地质灾害与防灾减灾对策研究”(201111024) |
| 摘 要： | 为研究泥石流灾害对西藏雅鲁藏布江林芝—加查段沿线的影响与危害,利用遥感(RS)和地理信息系统(GIS)开展了该段沿线泥石流源地物源提取及其分布特征的分析。研究结果表明,林芝—加查段沿线泥石流源地物源分布不均匀,物源分布受地层岩性、海拔高程及地形坡度影响。这些泥石流源地物源在冰川融水及冰川型泥石流过后更加发育,积累的松散物质更加丰富,使泥石流源地物源进一步复活并产生大量新物源,从而使沿线泥石流发生频率增高,规模增大。 |
| 关 键 词： | 西藏 雅鲁藏布江 泥石流 源地 遥感 |
| 收稿时间： | 2011/4/27 0:00:00 |
| 修稿时间： | 6/9/2011 12:00:00 AM |
RS and GIS Based Analysis of Material Sources in Debris Flow Origin Areas Along Linzhi-Jiacha Section in Yarlung Zangbo River |
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| WANG Gao-feng,TANG Chuan,WANG Hong-de,LI Wei-le and WANG Yu-hua.RS and GIS Based Analysis of Material Sources in Debris Flow Origin Areas Along Linzhi-Jiacha Section in Yarlung Zangbo River[J].Bulletin of Soil and Water Conservation,2012,32(1):10-13. | |
| Authors: | WANG Gao-feng TANG Chuan WANG Hong-de LI Wei-le and WANG Yu-hua |
| Institution: | 1.State Key Lab of Geo-hazard Prevention and Geo-environment Protection,Chengdu University of Technology,Chengdu 610059, China;2.Center for Hydrogeology and Environmental Geology Survey,China Geology Survey,Baoding,Hebei 071051,China; 3.The Basic Construction of He′nan Province Science Experiment Research Institute Co.,Ltd,Zhengzhou,He′nan 450000,China) |
| Abstract: | In order to study the impacts and hazards of debris flow disaster on the Linzhi—Jiacha section along the Yarlung Zangbo River in Tibet,remote sensing and geographical information systems techniques are used to extract information on the material sources in the debris flow origin areas along the Linzhi—Jiacha section and analyze the distribution characteristics of the material sources.Results from the study showed that the distribution of the material sources in the debris flow origin areas is not uniform due to the influences of formation lithology,altitude,and topographic slope.After glacier melting and glacier type mudflow,the material sources are more developed and the accumulated loose materials are more abundant,which further stimulates the material sources and produces a large amount of new material sources in the debris flow origin areas.Consequently,the frequency of debris flows along the river is raised and the scale of the debris flows is enlarged. |
| Keywords: | Tibet Autonomous Region Yarlung Zangbo River debris flow origin area remote sensing |
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