Guodong Ai1,*, Linbo Tang1, Pengfei Li1, Jianglin Li1, Kelin Guo2, Wentao Long1, Yixuan Yang1
1 Mineral Resources Survey Institute of Hunan Province, Changsha, 410129,China
2 Ecology Geological Survey and Monitoring Institute of Hunan Province, Changsha, 410119,China
Corresponding Author: Guodong Ai
Abstract: In July 2024, Typhoon “Gaemi” struck Zixing City, Hunan Province, triggering an extreme rainstorm with a maximum 24-hour rainfall of 642.5 mm, breaking the historical record in Hunan Province. The heavy rainfall induced a large number of geological disasters, mainly shallow landslides and slope debris flows, showing a significant “landslide --- debris flow --- flood” chain reaction characteristic. Based on the emergency investigation report of the “7·27” geological disaster in Zixing City and the post-disaster review report, combined with survey data from 706 geological disaster sites, this paper systematically analyzes the disaster mechanism and chain process of special strata such as granite and shallow metamorphic rocks under extreme rainfall conditions. The results show that special strata, with intense weathering and loose structure, are prone to high-altitude, shallow, and clustered landslides under short-term heavy rainfall; landslide masses mix with surface runoff during movement, transform into debris flows, further block river channels to form barrier lakes, trigger secondary flood disasters, and form multi-hazard compound chains. This paper reveals the causes of chain reactions from geological conditions, rainfall characteristics, topography, and human activities, and proposes an integrated disaster prevention and mitigation suggestion of “identification --- monitoring --- warning --- governance”, providing a scientific basis for disaster prevention and control under similar geological and climatic conditions.
Keywords: Extreme rainstorm; Special strata; Landslide; Chain reaction; Geological disaster; Zixing City
References
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