4.7 Article

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

期刊

LANDSLIDES
卷 18, 期 3, 页码 1115-1130

出版社

SPRINGER HEIDELBERG
DOI: 10.1007/s10346-020-01612-2

关键词

Reactivated Aniangzhai landslide; Rainstorm; Debris flow; Emergency monitoring

资金

  1. Belt & Road international cooperation team for the Light of West program of CAS
  2. National Natural Science Foundation of China [42007273]
  3. Second Tibetan Plateau Scientific Expedition and Research Program [2019QZKK0902]
  4. Special Assistant Researcher Foundation of Chinese Academy of Sciences
  5. China Postdoctoral Science Foundation [2020 M673292]

向作者/读者索取更多资源

An unexpected rainstorm on June 17, 2020 triggered a debris flow and reactivated an ancient landslide in the Meilong valley of Danba County, Sichuan Province, China, with an area of 0.62 km(2). Emergency monitoring over 20 days showed that the reactivated deposit entered a constant deformation state.
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 km(2). 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.

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