The 102 Landslide: human-slope interaction in SE Tibet over a 20-year period
文献类型:期刊论文
作者 | Shang, Yanjun1; Hyun, Chang-Uk2; Park, Hyeong-Dong3; Yang, Zhifa1; Yuan, Guangxiang4 |
刊名 | ENVIRONMENTAL EARTH SCIENCES
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出版日期 | 2017 |
卷号 | 76期号:1 |
关键词 | Large Scale Landslide Moraine Tibet Debris Flow Sands Sliding Slope Remediation |
ISSN号 | 1866-6280 |
DOI | 10.1007/s12665-016-6365-z |
文献子类 | Article |
英文摘要 | The evolution of large- scale landslides should be studied because, over long periods of time, primary remediation measures may suffer reduced efficiency or have to be adjusted many times. The 102 Landslide in southeast Tibet, which originally formed in 1991 with a volume of 5.1 million m(3) and still exhibits post- failure activity, provides a distinctive case study. The landslide evolved from earthquake destruction and unloading, rainfall- triggered sliding, and debris flow to sands sliding slopes. The NE ringed scarp receded by 38.96 m during a five- year period (2003-2008). The total recession was 160 m with a total area of 2500 m (2) during a 17-year period (1991-2008). Although several types of remediation measures were applied and were temporarily effective, the normal function of the Sichuan-Tibet Highway was affected by landslide reactivation from time to time. Actual effects of the engineering measures such as retaining walls, prestressed anchor cables, and drainage ditches confirm that hasty governance of this type of large-scale landslide is generally unfeasible over long time periods. Finally, an approach involving a tunnel running backward from the front face has been adopted as a permanent solution to large-scale moraine slope failures: This engineering practice has been in progress since April 2012. This paper describes the evolution of the 102 Landslide, the engineering interventions to mitigate the effects of the landslide on the Sichuan-Tibet Highway, and the choice of tunneling as a final mitigation measure. The present study concludes that approaches that allow escape from developing geohazards should always be the initial choice. |
WOS关键词 | MASS MOVEMENTS ; HIGHWAY ; FAILURE ; CHINA |
WOS研究方向 | Environmental Sciences & Ecology ; Geology ; Water Resources |
语种 | 英语 |
WOS记录号 | WOS:000392286300047 |
出版者 | SPRINGER |
资助机构 | Chinese Natural Science Foundation Committee(41372324) ; Brain Korea 21 Plus Project ; Research Institute of Energy and Resources, Seoul National University ; Chinese Natural Science Foundation Committee(41372324) ; Brain Korea 21 Plus Project ; Research Institute of Energy and Resources, Seoul National University ; Chinese Natural Science Foundation Committee(41372324) ; Brain Korea 21 Plus Project ; Research Institute of Energy and Resources, Seoul National University ; Chinese Natural Science Foundation Committee(41372324) ; Brain Korea 21 Plus Project ; Research Institute of Energy and Resources, Seoul National University |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/53145] ![]() |
专题 | 地质与地球物理研究所_中国科学院页岩气与地质工程重点实验室 |
通讯作者 | Hyun, Chang-Uk |
作者单位 | 1.Chinese Acad Sci, Key Lab Engn Geomech, Inst Geol & Geophys, Beijing 100029, Peoples R China 2.KIOST, Korea Polar Res Inst, Inchon 21990, South Korea 3.Seoul Natl Univ, Dept Energy Resources Engn, Seoul 151744, South Korea 4.North China Univ Water Resources & Elect Power, Zhengzhou 450011, Peoples R China |
推荐引用方式 GB/T 7714 | Shang, Yanjun,Hyun, Chang-Uk,Park, Hyeong-Dong,et al. The 102 Landslide: human-slope interaction in SE Tibet over a 20-year period[J]. ENVIRONMENTAL EARTH SCIENCES,2017,76(1). |
APA | Shang, Yanjun,Hyun, Chang-Uk,Park, Hyeong-Dong,Yang, Zhifa,&Yuan, Guangxiang.(2017).The 102 Landslide: human-slope interaction in SE Tibet over a 20-year period.ENVIRONMENTAL EARTH SCIENCES,76(1). |
MLA | Shang, Yanjun,et al."The 102 Landslide: human-slope interaction in SE Tibet over a 20-year period".ENVIRONMENTAL EARTH SCIENCES 76.1(2017). |
入库方式: OAI收割
来源:地质与地球物理研究所
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