IMHE OpenIR  > 山地灾害与地表过程重点实验室
横断山区泥石流空间格局和激发雨量分异性研究
Alternative TitleSpatial pattern of debris-flow catchments and the rainfall amount of triggering debris flows in the Hengduan Mountains region
胡凯衡1,2; 魏丽1,2,3; 刘双1,2; 李秀珍1,2
2019
Source Publication地理学报
ISSN0375-5444
Volume74Issue:11Pages:2303-2313
SubtypeArticle
Contribution Rank1
Abstract地形、降雨等环境因子决定了泥石流的时空分布特征,理解泥石流与这些因子的关系有助于区域泥石流灾害风险评估与防灾减灾工作。以横断山区为研究区域,选取降水、气候、地貌、地质、土地覆盖、土壤厚度、高差势能以及湿度指数等因子,利用地理探测器和灰度关联分析等方法,探讨了环境因子与泥石流沟空间分布的关系以及降水特征与泥石流灾害的时间关联性。结果表明,湿度指数是决定泥石流沟空间格局的最主要因子,其次是高差势能和土壤厚度,多年平均分布的降水特征对泥石流沟分布的影响较小。泥石流灾害事件与降水特征的时间关联具有较大的区域异质性。泥石流发生地的激发雨量、湿度指数、高差及土壤厚度的统计分布在不同地貌、地质和气候单元中有明显差异。这表明泥石流预警不仅需要考虑雨量等激发因子,还必须考虑其他影响因素的空间差异性。
Other AbstractEnvironmental factors determine the spatial and temporal distribution of debris flows. Understanding the relationship between debris flows and their effective factors is important for debris flows risk assessment at regional scale. In this paper, geographic detectors and gray correlation analysis are used to explore the relationship between 11 influencing factors, including precipitation, climate, landforms, geology, land cover type, soil thickness and topographic wetness, and the spatial distribution of debris flows-prone catchments, as well as the spatial and temporal correlation between precipitation and debris flows disasters in the Hengduan Mountains region. The results show that the topographic wetness index is the most dominant factor controlling the spatial distribution of the catchments, followed by topographic relief and soil thickness. Temporal correlation between debris flows disasters and precipitation characteristics has large regional heterogeneity. The rainfall characteristics of debris flows disaster events in different regions exhibit significant difference. The frequency of debris flows with rainfall, topographic wetness, topographic relief and soil thickness in the Hengduan Mountains region varies significantly in different zones, which indicates that not only the rainfall but also the other factors controlling the spatial pattern of debris flows should be reflected in debris flows early warning model in the region.
Keyword泥石流灾害 环境因子 降雨特征 地理探测器 灰色关联分析
DOI10.11821/dlxb201911008
Indexed ByEI ; CSCD
Language中文
CSCD IDCSCD:6597017
EI Accession NumberAccession number:20195007811391
Citation statistics
Document Type期刊论文
Identifierhttp://ir.imde.ac.cn/handle/131551/31251
Collection山地灾害与地表过程重点实验室
Corresponding Author胡凯衡
Affiliation1.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.中国科学院大学
First Author Affilication中国科学院水利部成都山地灾害与环境研究所
Corresponding Author Affilication中国科学院水利部成都山地灾害与环境研究所
Recommended Citation
GB/T 7714
胡凯衡,魏丽,刘双,等. 横断山区泥石流空间格局和激发雨量分异性研究[J]. 地理学报,2019,74(11):2303-2313.
APA 胡凯衡,魏丽,刘双,&李秀珍.(2019).横断山区泥石流空间格局和激发雨量分异性研究.地理学报,74(11),2303-2313.
MLA 胡凯衡,et al."横断山区泥石流空间格局和激发雨量分异性研究".地理学报 74.11(2019):2303-2313.
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