Relationships between Landslide Types and Topographic Attributes in a Loess Catchment,China  

作　　者：ZHANG Fanyu CHEN Wenwu LIU Gao LIANG Shouyun KANG Chao HE Faguo 

机构地区：[1]Key Laboratory of Mechanics on Disaster and Environment in Western China(Ministry of Education of China),and Department of Geological Engineering,Lanzhou University,Lanzhou 730000,China [2]Department of Civil and Environmental Engineering,University of Alberta,Edmonton,Alberta,T6G 2W2,Canada

出　　处：《Journal of Mountain Science》2012年第6期742-751,共10页山地科学学报（英文）

基　　金：supported by the National Natural Science Foundation of China (Project No.41072213);the Opening Fund of Key Laboratory of Mechanics on Disaster and Environment in Western China (Lanzhou University) (No. 201207);the Fundamental Research Funds for the Central Universities (No. lzujbky2011-7)

摘　　要：Topographic attributes have been identified as the most important factor in controlling the initiation and distribution of shallow landslides triggered by rainfall.As a result,these landslides influence the evolution of local surface topography.In this research,an area of 2.6 km 2 loess catchment in the Huachi County was selected as the study area locating in the Chinese Loess Plateau.The landslides inventory and landslide types were mapped using global position system(GPS) and field mapping.The landslide inventory shows that these shallow landslides involve different movement types including slide,creep and fall.Meanwhile,main topographic attributes were generated based on a high resolution digital terrain model(5 m × 5 m),including aspect,slope shape,elevation,slope angle and contributing area.These maps were overlaid with the spatial distributions of total landslides and each type of landslides in a geographic information system(GIS),respectively,to assess their spatial frequency distributions and relative failure potentials related to these selected topographic attributes.The spatial analysis results revealed that there is a close relation between the topographic attributes of the postlandsliding local surface and the types of landslide movement.Meanwhile,the types of landslide movement have some obvious differences in local topographic attributes,which can influence the relative failure potential of different types of landslides.These results have practical significance to mitigate natural hazard and understandgeomorphologic process in thick loess area.

关 键 词：Shallow landslides Movement types Topographic attributes Loess catchment GIS 

分 类 号：P208[天文地球—地图制图学与地理信息工程] S162[天文地球—测绘科学与技术]