| Citation: | ZHU Ying，GAN Jianjun，LU Qirui，et al. Analysis of rainfall induced-movement of landslide debris flows in granite residual soil: A case study of Yuanshan Village, Huangmei County, Hubei Province[J]. Bulletin of Geological Science and Technology，2025，44（3）：268-279 doi: 10.19509/j.cnki.dzkq.tb20240564
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The landslide in Yuanshan Village, Huangmei County, Hubei Province, represents a granite residual soil avalanche debris flow with complex and abrupt movement dynamics influenced by geological conditions. This study investigates the kinematic mechanisms of such landslide-debris flows in mid-low mountainous areas by analyzing the motion process of this specific event.
Through the field geological survey, the movement process of the landslide debris flow was analyzed based on UAV aerial photography, digital elevation model (DEM), on-site investigation, geological data analysis, and numerical simulations.
The results show that the maximum accumulation thickness of the avalanche is 6 m during the movement process. The peak velocity reaches 17 m/s at
This study can provide a reference for the prevention and control of similar disasters.
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