New insights into the occurrence of the catastrophic Zhaiban slope debris flow that occurred in a dry valley in the Hengduan Mountains in southwest China | |
Tian, Shufeng5,6; Chen, Ningsheng4,6; Rahman, Mahfuzur3; Hu, Guisheng4,6; Peng, Taixin5,6; Zhang, Yong2; Liu, Mei1 | |
刊名 | LANDSLIDES |
2022-01-14 | |
页码 | 11 |
关键词 | Slope debris flow Open tunnel Hollow regions Dry-wet cycle Hengduan Mountains |
ISSN号 | 1612-510X |
DOI | 10.1007/s10346-021-01824-0 |
英文摘要 | In 2019, the catastrophic Zhaiban slope debris flow (ZSDF) crushed an open road tunnel in Ganluo County, Sichuan Province, China, causing seven deaths and interrupting traffic flow for 16 days. We analyzed the characteristics of the ZSDF disaster by undertaking a comprehensive on-site investigation, evaluating the internal and external dynamic characteristics, and conducting a numerical simulation. The formation mechanism of typical slope debris flows in the arid valley area of the Hengduan Mountain was revealed, and the material foundations for generating the ZSDF were identified as internal dynamic effects on the slope (including thrust faults and folds), historical earthquake occurrences, and external dynamic effects from an extreme dry and wet cycle (with a low frequency of once in 55 years). Soil failure occurred in a hollow catchment region at the top of the gully (covering an area of 74,084 m(2)) under a heavy rainfall of 33.4 mm/h, and large boulders (average radius of 2.43 m) were pulled along the gully and down the steep slope gradient, thereby providing the large amount of kinetic energy required for the ZSDF. Large boulders and soil masses remain in gullies on slopes within the study area, providing the high possibility of future slope debris flows under heavy rainfall. The results also suggest the use of large-gradient flumes on top of open tunnels in the arid valley area of the Hengduan Mountains to provide optimum protection against slope debris flow. |
资助项目 | National Natural Science Foundation of China[U20A20110] ; National Natural Science Foundation of China[41861134008] ; Youth Innovation Promotion Association CAS[2020367] ; National Key Research and Development Program of China[2018YFC1505202] |
WOS关键词 | WENCHUAN EARTHQUAKE ; LANDSLIDES ; RAINFALL |
WOS研究方向 | Engineering ; Geology |
语种 | 英语 |
出版者 | SPRINGER HEIDELBERG |
WOS记录号 | WOS:000742973200002 |
资助机构 | National Natural Science Foundation of China ; Youth Innovation Promotion Association CAS ; National Key Research and Development Program of China |
内容类型 | 期刊论文 |
源URL | [http://ir.imde.ac.cn/handle/131551/56400] |
专题 | 成都山地灾害与环境研究所_山地灾害与地表过程重点实验室 |
通讯作者 | Chen, Ningsheng; Hu, Guisheng |
作者单位 | 1.Xihua Univ, Sch Emergency Sci, Chengdu 610039, Peoples R China 2.Anyang Inst Technol, Sch Civil & Architectural Engn, Anyang 455000, Peoples R China 3.Int Univ Business Agr & Technol IUBAT, Dept Civil Engn, Dhaka 1230, Bangladesh 4.Acad Plateau Sci & Sustainabil, Xining 810016, Peoples R China 5.Univ Chinese Acad Sci, Beijing 100049, Peoples R China 6.Chinese Acad Sci, Key Lab Mt Hazards & Surface Proc, Inst Mt Hazards & Environm, Chengdu 610041, Peoples R China |
推荐引用方式 GB/T 7714 | Tian, Shufeng,Chen, Ningsheng,Rahman, Mahfuzur,et al. New insights into the occurrence of the catastrophic Zhaiban slope debris flow that occurred in a dry valley in the Hengduan Mountains in southwest China[J]. LANDSLIDES,2022:11. |
APA | Tian, Shufeng.,Chen, Ningsheng.,Rahman, Mahfuzur.,Hu, Guisheng.,Peng, Taixin.,...&Liu, Mei.(2022).New insights into the occurrence of the catastrophic Zhaiban slope debris flow that occurred in a dry valley in the Hengduan Mountains in southwest China.LANDSLIDES,11. |
MLA | Tian, Shufeng,et al."New insights into the occurrence of the catastrophic Zhaiban slope debris flow that occurred in a dry valley in the Hengduan Mountains in southwest China".LANDSLIDES (2022):11. |
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