Author
Listed:
- Xiangyang Feng
(School of Public Policy and Management, China University of Mining and Technology, Xuzhou 221116, China)
- Zhaoqi Wu
(School of Public Policy and Management, China University of Mining and Technology, Xuzhou 221116, China)
- Zihao Wu
(School of Public Policy and Management, China University of Mining and Technology, Xuzhou 221116, China
Present address: Room A512, School of Public Policy & Management School of Emergency Management, China University of Mining and Technology, No.1 Daxue Street, Tongshan District, Xuzhou 221116, China.)
- Junping Bai
(Xinjiang Power Transmission and Transformation Co., Ltd., Urumqi 830000, China)
- Shixiang Liu
(Zhongdihuaan Science and Technology Co., Ltd., Urumqi 830000, China)
- Qingwu Yan
(School of Public Policy and Management, China University of Mining and Technology, Xuzhou 221116, China)
Abstract
Landslides frequently occur in the Xinjiang Uygur Autonomous Region of China due to its complex geological environment, posing serious risks to human safety and economic stability. Existing studies widely use machine learning models for landslide susceptibility prediction. However, they often fail to capture the threshold and interaction effects among environmental factors, limiting their ability to accurately identify high-risk zones. To address this gap, this study employed a gradient boosting decision tree (GBDT) model to identify critical thresholds and interaction effects among disaster-causing factors, while mapping the spatial distribution of landslide susceptibility based on 20 covariates. The performance of this model was compared with that of a support vector machine and deep neural network models. Results showed that the GBDT model achieved superior performance, with the highest AUC and recall values among the tested models. After applying clustering algorithms for non-landslide sample selection, the GBDT model maintained a high recall value of 0.963, demonstrating its robustness against imbalanced datasets. The GBDT model identified that 8.86% of Xinjiang’s total area exhibits extremely high or high landslide susceptibility, mainly concentrated in the Tianshan and Altai mountain ranges. Lithology, precipitation, profile curvature, the Modified Normalized Difference Water Index (MNDWI), and vertical deformation were identified as the primary contributing factors. Threshold effects were observed in the relationships between these factors and landslide susceptibility. The probability of landslide occurrence increased sharply when precipitation exceeded 2500 mm, vertical deformation was greater than 0 mm a −1 , or the MNDWI values were extreme (<−0.4, >0.2). Additionally, this study confirmed bivariate interaction effects. Most interactions between factors exhibited positive effects, suggesting that combining two factors enhances classification performance compared with using each factor independently. This finding highlights the intricate and interdependent nature of these factors in landslide susceptibility. These findings emphasize the necessity of incorporating threshold and interaction effects in landslide susceptibility assessments, offering practical insights for disaster prevention and mitigation.
Suggested Citation
Xiangyang Feng & Zhaoqi Wu & Zihao Wu & Junping Bai & Shixiang Liu & Qingwu Yan, 2025.
"Landslide Susceptibility Mapping in Xinjiang: Identifying Critical Thresholds and Interaction Effects Among Disaster-Causing Factors,"
Land, MDPI, vol. 14(3), pages 1-25, March.
Handle:
RePEc:gam:jlands:v:14:y:2025:i:3:p:555-:d:1606884
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