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西藏冻融侵蚀的分级和评价
引用本文:张建国,刘淑珍,杨思全. 西藏冻融侵蚀的分级和评价[J]. 地理学报(英文版), 2007, 17(2): 165-174. DOI: 10.1007/s11442-007-0165-z
作者姓名:张建国  刘淑珍  杨思全
作者单位:[1]School of Geography, Nantong University, Nantong 226007, China [2]Institute of Mountain Hazards and Environment, CAS, Chengdu 610041, China [3]National Disaster Reduction Center, MCA, Beijing 100053, China
基金项目:Key Basic Research Proiect of China, No.2004CCA03600
摘    要:
Freeze-thaw erosion is the third largest soil erosion type after water erosion and wind erosion. Restricted by many factors, few researches on freeze-thaw erosion have so far been done at home and abroad, especially those on the assessment method of freeze-thaw erosion. Based on the comprehensive analysis of impact factors of free-thaw erosion, this paper chooses six indexes, including the annual temperature range, annual precipitation, slope, aspect, vegetation and soil, to build the model for relative classification of freeze-thaw erosion using weighted and additive methods, and realizes the relative classification of the freeze-thaw erosion in Tibet with the support of GIS software. Then a synthetic assessment of freeze-thaw erosion in Tibet has been carried out according to the relative classification result. The result shows that the distribution of freeze-thaw eroded area is very extensive in Tibet, accounting for 55.3% of the total local land area; the spatial differentiation of freeze-thaw erosion with different intensities is obvious; and the difference in distribution among different regions is also obvious.

关 键 词:西藏 冻融侵蚀 分类 评价 GIS
收稿时间:2007-02-08
修稿时间:2007-02-082007-03-16

The classification and assessment of freeze-thaw erosion in Tibet
Zhang Jianguo,Liu Shuzhen,Yang Siquan. The classification and assessment of freeze-thaw erosion in Tibet[J]. Journal of Geographical Sciences, 2007, 17(2): 165-174. DOI: 10.1007/s11442-007-0165-z
Authors:Zhang Jianguo  Liu Shuzhen  Yang Siquan
Affiliation:1. School of Geography, Nantong University, Nantong 226007, China|;2. Institute of Mountain Hazards and Environment, CAS, Chengdu 610041, China|;3. National Disaster Reduction Center, MCA, Beijing 100053, China
Abstract:
Freeze-thaw erosion is the third largest soil erosion type after water erosion and wind erosion. Restricted by many factors, few researches on freeze-thaw erosion have so far been done at home and abroad, especially those on the assessment method of freeze-thaw erosion. Based on the comprehensive analysis of impact factors of free-thaw erosion, this paper chooses six indexes, including the annual temperature range, annual precipitation, slope, aspect, vegetation and soil, to build the model for relative classification of freeze-thaw erosion using weighted and additive methods, and realizes the relative classification of the freeze-thaw erosion in Tibet with the support of GIS software. Then a synthetic assessment of freeze-thaw erosion in Tibet has been carried out according to the relative classification result. The result shows that the distribution of freeze-thaw eroded area is very extensive in Tibet, accounting for 55.3% of the total local land area; the spatial differentiation of freeze-thaw erosion with different intensities is obvious; and the difference in distribution among different regions is also obvious.
Keywords:Tibet   freeze-thaw erosion   GIS   classification and assessment
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