IMHE OpenIR  > Journal of Mountain Science  > Journal of Mountain Science-2017  > Vol14 No.6
The formation of the Wulipo landslide and the resulting debris flow in Dujiangyan City, China
CHEN Xing-zhang; CUI Yi-fei
Corresponding AuthorCUI Yi-fei
2017-06
Source PublicationJournal of Mountain Science
ISSN1672-6316
Volume14Issue:6Pages:1100-1112
Subtype期刊论文
AbstractThe Wulipo landslide, triggered by heavy rainfall on July 10, 2013, transformed into debris flow, resulted in the destruction of 12 houses, 44 deaths, and 117 missing. Our systematic investigation has led to the following results and to a new understanding about the formation and evolution process of this hazard. The fundamental factors of the formation of the landslide are a high-steep free surface at the front of the slide mass and the sandstone-mudstone mixed stratum structure of the slope. The inducing factor of the landslide is hydrostatic and hydrodynamic pressure change caused by heavy continuous rainfall. The geological mechanical model of the landslide can be summarized as "instability - translational slide - tension fracture - collapse" and the formation mechanism as "translational landslide induced by heavy rainfall". The total volume of the landslide is 124.6×104 m3, and 16.3% of the sliding mass was dropped down from the cliff and transformed into debris flow during the sliding process, which enlarged 46.7% of the original sliding deposit area. The final accumulation area is found to be 9.2×104 m2. The hazard is a typical example of a disaster chain involving landslide and its induced debris flow. The concealment and disaster chain effect is the main reason for the heavy damage. In future risk assessment, it is suggested to enhance the research on potential landslide identification for weakly intercalated slopes. By considering the influence of the behaviors of landslide-induced debris flow, the disaster area could be determined more reasonably.
KeywordLandslide Debris Flow Disaster Chain Effect Heavy Rainfall Geological Hazard Area Wenchuan Earthquake
DOI10.1007/s11629-017-4392-1
Indexed BySCI
Language英语
Citation statistics
Cited Times:35[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.imde.ac.cn/handle/131551/18730
CollectionJournal of Mountain Science_Journal of Mountain Science-2017_Vol14 No.6
Recommended Citation
GB/T 7714
CHEN Xing-zhang,CUI Yi-fei. The formation of the Wulipo landslide and the resulting debris flow in Dujiangyan City, China[J]. Journal of Mountain Science,2017,14(6):1100-1112.
APA CHEN Xing-zhang,&CUI Yi-fei.(2017).The formation of the Wulipo landslide and the resulting debris flow in Dujiangyan City, China.Journal of Mountain Science,14(6),1100-1112.
MLA CHEN Xing-zhang,et al."The formation of the Wulipo landslide and the resulting debris flow in Dujiangyan City, China".Journal of Mountain Science 14.6(2017):1100-1112.
Files in This Item:
File Name/Size DocType Version Access License
8.pdf(8728KB)期刊论文作者接受稿开放获取CC BY-NC-SAView Application Full Text
Related Services
Recommend this item
Bookmark
Usage statistics
Export to Endnote
Google Scholar
Similar articles in Google Scholar
[CHEN Xing-zhang]'s Articles
[CUI Yi-fei]'s Articles
Baidu academic
Similar articles in Baidu academic
[CHEN Xing-zhang]'s Articles
[CUI Yi-fei]'s Articles
Bing Scholar
Similar articles in Bing Scholar
[CHEN Xing-zhang]'s Articles
[CUI Yi-fei]'s Articles
Terms of Use
No data!
Social Bookmark/Share
File name: 8.pdf
Format: Adobe PDF
All comments (0)
No comment.
 

Items in the repository are protected by copyright, with all rights reserved, unless otherwise indicated.