2025 Vol. 41, No. 1
Article Contents

XIE Yang-Long, QI Xin, GAO Peng, WANG Ying-Hao. 2025. Comparative Analysis of Slope Geological Hazard Susceptibility Assessment Based on Multiple Evaluation Models: A Case Study of Wuhan, China. South China Geology, 41(1): 185-196. doi: 10.3969/j.issn.2097-0013.2025.01.015
Citation: XIE Yang-Long, QI Xin, GAO Peng, WANG Ying-Hao. 2025. Comparative Analysis of Slope Geological Hazard Susceptibility Assessment Based on Multiple Evaluation Models: A Case Study of Wuhan, China. South China Geology, 41(1): 185-196. doi: 10.3969/j.issn.2097-0013.2025.01.015

Comparative Analysis of Slope Geological Hazard Susceptibility Assessment Based on Multiple Evaluation Models: A Case Study of Wuhan, China

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  • The susceptibility evaluation of geological disasters is an indispensable part of disaster prevention and mitigation. It is of great significance to select effective evaluation methods and models for the susceptibility evaluation of geological disasters. This paper takes the slope geological disasters (collapse and landslide) in Wuhan city as the research object, selects 9 evaluation factors such as slope, slope direction, elevation, engineering geological rock group and vegetation coverage, and uses the information method (IV), the determination coefficient method (CF) and the random forest model (RF) to evaluate the susceptibility of geological disasters, and then uses the receiver operating characteristic curve (ROC) to test the accuracy of the evaluation model and compare the evaluation results of the three models. The results show that: (1) The three models can correctly reflect the development characteristics of slope geological disasters in the study area. The high-prone areas and extremely high-prone areas are concentrated in the mountainous areas in the northern, central and western parts of the study area and the eroded accumulation hilly areas formed by river denudation and leveling. The low-prone areas account for the vast majority and are mainly distributed in the plain areas around the banks and lakes of the Yangtze River and most of the low-mountain plain areas. (2) The AUC area of the three models from high to low is IV > CF > RF. The zoning results obtained by the IV and CF models have high similarity, and the disaster point density of the extremely high-prone areas of the two models is higher than that of the RF model. (3) Slope, elevation, engineering geological rock group and slope structure type are the most important factors in the evaluation system, indicating that the development factors of slope geological disasters in the study area are mainly related to topography and lithology.

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