RESOURCES AND ENVIRONMENT IN THE YANGTZE BASIN >> 2017, Vol. 26 >> Issue (05): 789-796.doi: 10.11870/cjlyzyyhj201705017

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VARIATION OF HAZARD AREAS OF TYPICAL RAINSTORM DEBRIS FLOW ALLUVIAL FANS

LI Yan-ji1,2,3, YAN Chun-da4, HU Kai-heng1,2, WEI Li1,2,3   

  1. 1. Key Laboratory of Mountain Hazards and Earth Surface Processes, Chinese Academy of Sciences, Chengdu 610041, China;
    2. Institute of Mountain Hazards and Environment, Chinese Academy of Sciences & Ministry of Water Conservancy, Chengdu 610041, China;
    3. University of Chinese Academy of Sciences, Beijing 100049, China;
    4. Yunnan Kunming Dongchuan Geology Disaster Protection Center, Kunming 654100, China
  • Received:2016-11-04 Revised:2017-01-07 Online:2017-05-20
  • Supported by:
    National Program on Key Basic Research Project (2015CB452704);National Natural Science Foundation of China (41371039);the Open Foundation of Key Laboratory of Mountain Hazards and Earth Surface Processes, Chinese Academy of Sciences

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Abstract: Based on the Landsat images during 1987 to 2014, this paper interpreted the hazard areas of debris flow fans, analyzed their evolution characteristics in the Jiangjia and Dabaini catchments in Xiaojiang Basin, and further discussed the variation of influenced area in Jiangjia and Dabaini catchments, as well as their influential factors of the variation. It revealed that (1) the damaging ranges of debris flow fans have shrunk during the recent 30 years; (2) the development of debris flow fans in Dabaini basin was at the mature stage with lower amplitude of shrinkage, while in Jiangjiagou basin, their development were at the over-mature stage with higher amplitude of shrinkage and stable situation; (3)water, sediment provenance and human activities are the main factors of that influence variation of debris flow fans.

Key words: rainstorm debris flow, alluvial fans, evolution, TM images, OLI images

CLC Number: 

  • P642.23
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