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Failure mechanism of a slow-moving landslide on September 27, 2020, in Chang Nong Village, Guangxi, China

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Abstract

A recent slow-moving landslide occurred on September 27, 2020, in Chang Nong Village (24°21′ 25” N, 109°09′ 27″ E), Guangxi Province, China. The precursor activity of the landslide started approximately 5 months before landslides with cut slope construction work at the toe part of a mountain. Given this precursor, engineers set a counterweight berm at the slope’s toe for expanding toe weight to avoid further deformation. However, the measure had a negative effect on the stability of landslides, as the stabilizing berm blocked off natural groundwater channels located at the slope toe, leading to further deformation of landslides. Fortunately, monitoring of the creeping downslope movements of the landslide mass began, and an early warning was issued before the event. Thus, no casualties were caused by the slow-moving landslide; however, 72 houses were destroyed. In order to deduce the Chang Nong Village landslide failure mechanism, the geological characteristics, slope excavation schemes, rainfall data statistics, and landslide deformation patterns were systematically investigated based on unmanned aerial vehicle (UAV) photography, field investigation, displacement monitoring, and laboratory testing. The results show that colluvial stratigraphic structures and poor rock mass properties are the internal factors that induced landslides. The combined effects of prolonged heavy rainfall and the repeated fluctuation of groundwater caused by improper activities, including toe excavation and counterweight filling, are external factors that directly triggered the landslide. This case discusses how improper engineering treatment influences groundwater changes in landslide areas and supports the importance of prevention measures for colluvium landslides.

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Acknowledgments

The authors would like to thank Mr. Yang and Mr. Luo for assisting in mechanical tests. The authors would like to thank the editor and anonymous reviewers for their valuable comments that substantially improved this paper.

Funding

This work was developed within the scope of the Anhui Province Transport Technology Progress Plan (202130 and JKKJ-2021-20), and this work was funded by the Opening Fund of Key Laboratory of Geological Survey and Evaluation of Ministry of Education (Grant No. GLAB2019 ZR05) and the Fundamental Research Funds for the Central Universities.

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Correspondence to Zhi Zhou.

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Zhang, J., Zhou, Z., Lin, F. et al. Failure mechanism of a slow-moving landslide on September 27, 2020, in Chang Nong Village, Guangxi, China. Landslides 18, 2575–2592 (2021). https://doi.org/10.1007/s10346-021-01688-4

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  • DOI: https://doi.org/10.1007/s10346-021-01688-4

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