Abstract
On March 5, 2020, a shallow loess landslide occurred in Yaoba Village, Songpan County, Sichuan Province, posing a severe threat to the lives and properties of 130 villagers. In this study, the landslide’s essential characteristics were identified through field investigations, and the failure mechanism of the landslide was analyzed through numerical simulations, laboratory experiments, and strength calculations. A new mechanism of the Yaoba loess landslide was proposed. The results show that (1) the minimum induced rainfall required for the landslide from the natural unsaturated state into the saturated state at the lowest thickness of 1.4 m was 177.2 mm. The limited amount of previous rainfall was not sufficient to make the landslide soil saturated and unstable. (2) Snowmelt water infiltration caused by abnormally high temperatures was the leading cause of the landslide failure. Based on the strong hydrodynamic conditions in the area and the confluence through the hollow region upstream of the landslide, abnormally high temperatures caused an increase in snowmelt values up to 219 mm. Snowmelt infiltrated into the slope and increased the water content up to a saturation state at 26.67%, making the shear strength of the soil reach the limit equilibrium state and be unstable. The analysis of the Yaoba landslide in western Sichuan that occurred during a dry spell will improve the early warning of groundwater- and snowmelt-induced shallow loess landslides.
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Funding
This study was financially supported by the National Natural Science Foundation of China (Grant Nos. U20A20110 and 41861134008), and the Youth Innovation Promotion Association CAS (Grant No. 2020367). All financial supports are greatly appreciated.
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Wu, K., Chen, N., Hu, G. et al. Failure mechanism of the Yaoba loess landslide on March 5, 2020: the early-spring dry spell in Southwest China. Landslides 18, 3183–3195 (2021). https://doi.org/10.1007/s10346-021-01703-8
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DOI: https://doi.org/10.1007/s10346-021-01703-8