Abstract
Abundant water and unstable loess are favorable factors for initiating landslides; landslides induced by hidden layer instability in a residential area would cause marked damage. On March 27, 2021, a landslide caused by loess interlayer instability occurred in Dege County, Sichuan Province, China. In total, 20 houses were damaged, and the lives of 1100 residents were threatened. This study explores the failure mechanism of the landslide caused by loess interlayer instability through field investigation, laboratory tests, and circular slide stability analysis. The results show that (1) Dege landslide is a small thrust-type landslide caused by the instability of loess hidden under colluvium; (2) precipitation convergence by hollow landform and domestic water leakage increased the moisture content of the loess interlayer; domestic water leakage occupied 91.7%; (3) the loess interlayer zone has high porosity, strong collapsibility, and high clay mineral content, which causes softening by water; and (4) multiple water sources reduced the anti-sliding force by approximately 3.3%, and newly building load increased the sliding force by approximately 15.9%. The combination of multiple water sources and building load led to landslide failure. This study provides new insights into the hidden loess interlayer landslide in mountainous urban areas of western China and can be a reference for landslide prevention and mitigation.
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source and distribution of the water in the landslide
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Data availability
The datasets used or analyzed during the current study are available from the corresponding author on reasonable request.
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This study was supported by the National Natural Science Foundation of China [grant number U20A20110]; and the National Natural Science Foundation of China [grant number 41861134008].
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Peng, T., Chen, N., Hu, G. et al. Failure mechanism of Dege landslide in western China, March, 2021: the loess interlayer and multiple water resources. Landslides 19, 2189–2197 (2022). https://doi.org/10.1007/s10346-022-01910-x
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DOI: https://doi.org/10.1007/s10346-022-01910-x