Spatial characteristics of the rainfall induced landslides in the Chinese Loess Plateau

被引:30
|
作者
Huo, Aidi [1 ,2 ]
Yang, Lei [1 ,2 ]
Peng, Jianbing [3 ]
Cheng, Yuxiang [3 ]
Jiang, Cheng [2 ]
机构
[1] Changan Univ, Key Lab Subsurface Hydrol & Ecol Effects Arid Reg, Minist Educ, Xian, Shaanxi, Peoples R China
[2] Changan Univ, Sch Water & Environm, Xian, Shaanxi, Peoples R China
[3] Changan Univ, Coll Geol Engn & Geometr, Xian 710054, Shaanxi, Peoples R China
来源
HUMAN AND ECOLOGICAL RISK ASSESSMENT | 2020年 / 26卷 / 09期
基金
中国国家自然科学基金;
关键词
Landslides hazards; precipitation; spatial variation characteristics; trend change; Chinese Loess Plateau; GROUNDWATER QUALITY RESEARCH; SURFACE-WATER; SPECIAL FOCUS;
D O I
10.1080/10807039.2020.1728517
中图分类号
X176 [生物多样性保护];
学科分类号
090705 ;
摘要
The Chinese Loess Plateau (CLP) is still undergoing development. Nearly one-third of the geological disasters take place in this region in China each year. Prior to assessing the spatial characteristics of the rainfall-induced landslides in the CLP, it is fundamental to establish a detailed landslide inventory map. This study utilizes GLDAS (Global Land Data Assimilations Systems) rainfall distribution data in the CLP based on yearly, monthly, and the daily precipitation data from 57 rain gauge stations. Geostatistics analysis and Geographic Information System technique combined with information on geological disasters within the region were used to study the spatial characteristics and trend variations of rainfall and geological disaster distribution in the region. The results indicate that a positive relationship exists between geological disaster and the average annual rainfall, correlation coefficient reaches 0.82, with zonality disasters (account for more than 90%) in the loess gullies, hills, and ridges. Seven zones of loess landside distribution were identified based on their landside densities. The spatial distribution of the geological disasters is characterized by a "linear and zone" shape in the CLP. These results provide a useful reference for the study of the mechanism of water-induced loess landslides.
引用
收藏
页码:2462 / 2477
页数:16
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