New insights into the occurrence of the Baige landslide along the Jinsha River in Tibet
文献类型：期刊论文
| 作者 | Tian, Shufeng2,3 ; Chen, Ningsheng3,4; Wu, Hua4; Yang, Chengye4; Zhong, Zheng1; Rahman, Mahfuzur2,3,5
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| 刊名 | LANDSLIDES
 |
| 出版日期 | 2020-05-01 |
| 卷号 | 17期号:5页码:1207-1216 |
| 关键词 | Baige landslide Slope seepage Tectonics Groundwater Rainfall Risk management |
| ISSN号 | 1612-510X |
| DOI | 10.1007/s10346-020-01351-4 |
| 产权排序 | 1 |
| 通讯作者 | Chen, Ningsheng(chennsh@imde.ac.cn) |
| 文献子类 | Article |
| 英文摘要 | The catastrophic Baige landslide occurred on October 10, 2018 in the Tibet Autonomous Region, China, and formed a barrier lake with a direct economic loss of 6.8 billion RMB (~ 963.5 million USD). After the landslide, field investigations were conducted both to support emergency operations and to understand the failure mechanism immediately after the landslide. Detailed field surveys, borehole exploration, discharge measurements, laboratory experiments, and meteorological analyses were employed in this study to explore the mechanisms underlying the Baige landslide. A key influence from the water source in Bogong Gully on the Baige landslide formation was newly found. The results show that the underground of the slope comprises extremely weathered serpentinite, and fresh rock has not yet been revealed in boreholes. The seepage outlets are 450-550 m higher than the Jinsha River and ~ 118 m lower than the bed of Bogong Gully. Water flow in the channel of Bogong Gully is strongly infiltrated, with a flow loss of 62.6%. Seepage into the Bogong Gully, along with the landslide, caused by the local geological structure and lithology, accelerated the extreme weathering of rock masses and promoted landslide formation. Furthermore, extreme annual rainfall also contributed to the occurrence of the Baige landslide by increasing the discharge of the Bogong Gully. Further risk management measures in this area should include increasing the depth of geological explorations and the construction of drainage systems. |
| 电子版国际标准刊号 | 1612-5118 |
| WOS研究方向 | Engineering ; Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000528626300013 |
| 出版者 | SPRINGER HEIDELBERG |
| 源URL | [http://ir.imde.ac.cn/handle/131551/34586]  |
| 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 |
| 作者单位 | 1.Kunming Univ Sci & Technol, Kunming 650504, Peoples R China; 2.Univ Chinese Acad Sci, Beijing 100049, Peoples R China; 3.Chinese Acad Sci, Inst Mt Hazards & Environm, Key Lab Mt Hazards & Surface Proc, Chengdu 610041, Peoples R China; 4.Tibet Univ, Joint Lab Plateau Surface Remote Sensing, Lhasa 850000, Peoples R China; 5.IUBAT, Dept Civil Engn, Dhaka 1230, Bangladesh |
| 推荐引用方式 GB/T 7714 | Tian, Shufeng,Chen, Ningsheng,Wu, Hua,et al. New insights into the occurrence of the Baige landslide along the Jinsha River in Tibet[J]. LANDSLIDES,2020,17(5):1207-1216. |
| APA | Tian, Shufeng,Chen, Ningsheng,Wu, Hua,Yang, Chengye,Zhong, Zheng,&Rahman, Mahfuzur.(2020).New insights into the occurrence of the Baige landslide along the Jinsha River in Tibet.LANDSLIDES,17(5),1207-1216. |
| MLA | Tian, Shufeng,et al."New insights into the occurrence of the Baige landslide along the Jinsha River in Tibet".LANDSLIDES 17.5(2020):1207-1216. |
入库方式： OAI收割
来源：成都山地灾害与环境研究所
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