Emergency response to the reactivated Aniangzhai landslide resulting from a rainstorm-triggered debris flow, Sichuan Province, China

被引:1
|
作者
Bo Zhao
Haiquan Zhang
Liao Hongjian
Weile Li
Lijun Su
Wenxiu He
Lu Zeng
Haokun Qin
Megh Raj Dhital
机构
[1] Chinese Academy of Sciences,Key Laboratory of Mountain Hazards and Earth Surface Processes, Institute of Mountain Hazards and Environment
[2] Sichuan Metallurgical Geological Survey and Design Group Co.,School of Human Settlements and Civil Engineering
[3] Ltd,State Key Laboratory of Geohazard Prevention and Geoenvironment Protection
[4] Xian Jiaotong University,Central Department of Geology
[5] Chengdu University of Technology,undefined
[6] CAS Center for Excellence in Tibetan Plateau Earth Sciences,undefined
[7] China-Pakistan joint Research Center on Earth Sciences,undefined
[8] University of Chinese Academy of Sciences,undefined
[9] Tribhuvan University,undefined
来源
Landslides | 2021年 / 18卷
关键词
Reactivated Aniangzhai landslide; Rainstorm; Debris flow; Emergency monitoring;
D O I
暂无
中图分类号
学科分类号
摘要
On June 17, 2020, an unexpected rainstorm struck the Meilong valley, which is located in Danba County, Sichuan Province, China. The cumulative rainfall of this short-duration event reached 38.1–42.4 mm and triggered the Meilong debris flow. The Meilong debris flow rushed into the valley and forced the Xiaojinchuan (XJC) River to flow along the foot of the ancient Aniangzhai (ANZ) landslide. Intense erosion reactivated the ancient ANZ landslide, producing a reactivated area of 0.62 km2. Subsequently, emergency investigation and monitoring were conducted to monitor its deformation because unstable landslide conditions could pose a serious threat to the safety of lives and property downstream. Emergency monitoring over 20 days (June 23, 2020–July 12, 2020) indicated that the reactivated deposit decelerated and entered the constant deformation state; careful attention should be paid to this reactivated deposit.
引用
收藏
页码:1115 / 1130
页数:15
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