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干旱区地理 ›› 2026, Vol. 49 ›› Issue (4): 778-790.doi: 10.12118/j.issn.1000-6060.2025.292 cstr: 32274.14.ALG2025292

• 灾害研究 • 上一篇    下一篇

基于熵权-随机森林优化赋权法的新源县地质灾害风险评估

刘京会(), 李鑫旭(), 袁旭山, 李艳敏   

  1. 防灾科技学院应急技术与管理学院河北 三河 065201
  • 收稿日期:2025-05-22 修回日期:2025-08-20 出版日期:2026-04-25 发布日期:2026-04-28
  • 通讯作者: 李鑫旭(2000-),男,硕士研究生,主要从事灾害风险评估等方面的研究. E-mail: lxxmail824@163.com
  • 作者简介:刘京会(1975-),女,博士,副教授,主要从事灾害监测与评估等方面的研究. E-mail: liujh@cidp.edu.cn
  • 基金资助:
    第三次新疆综合科学考察(2022xjkk0600)

Geological disaster risk assessment of Xinyuan County based on entropy weight-random forest optimization weighting method

LIU Jinghui(), LI Xinxu(), YUAN Xushan, LI Yanmin   

  1. School of Emergency Technology and Management, Institute of Disaster Prevention, Sanhe 065201, Hebei, China
  • Received:2025-05-22 Revised:2025-08-20 Published:2026-04-25 Online:2026-04-28

摘要:

伊犁河流域地质灾害频发,新源县位于伊犁河谷腹地,是流域内发生最频繁的县市之一。以新源县为研究区,构建包含致灾因子危险性、孕灾环境敏感性与承灾体脆弱性的三维度指标体系,并提出一种结合熵权法与随机森林模型的权重优化方法,结合ArcGIS平台对新源县地质灾害风险进行综合评估。结果表明:(1) 权重优化后,危险性主要由水动力因子主导,敏感性受地形因素影响显著,脆弱性以交通与人口经济特征为主,同时优化后权重在受试者工作特征曲线下的面积较熵权法更高。(2) 危险性、敏感性与脆弱性在空间上呈现明显差异,分别对应地质条件复杂区域、阴坡缓坡区域和人口经济集聚区域。(3) 整体风险空间格局与脆弱性高度一致,高风险区主要集中在镇区与主要道路沿线,中高风险区多位于灾害环境与承灾体叠加区,低风险区分布于生态稳态区或无显著承灾体区。(4) 风险高值区与历史灾害点及典型承灾体空间分布高度重合,验证了评估结果的合理性与可靠性。研究结果揭示了新源县地质灾害风险空间分布格局,为防灾减灾工作提供一定科学依据与理论参考。

关键词: 风险评估, 地质灾害, 熵权法, 随机森林, 新源县

Abstract:

Geological disasters frequently occur in the Ili River Basin, and Xinyuan County is among the most disaster-prone areas. This study focuses on Xinyuan County and establishes a three-dimensional indicator system encompassing the hazard of triggering factors, the susceptibility of disaster-prone environments, and the vulnerability of exposed elements. An optimized weighting scheme was developed by integrating the entropy weight method with the Random Forest model, and the comprehensive geological disaster risk of the county was evaluated using the ArcGIS platform. The results indicate that (1) After weight optimization, hazard was primarily governed by hydrodynamic factors, susceptibility was strongly controlled by topographic factors, and vulnerability was mainly determined by transportation networks and population-economic characteristics. The optimized weights yielded higher area under curve values than those obtained using the traditional entropy weight method. (2) The spatial distributions of hazard, susceptibility, and vulnerability differed significantly, corresponding to areas with complex geological conditions, gentle shaded slopes, and population-economic clusters, respectively. (3) The overall spatial pattern of geological disaster risk closely corresponded to the distribution of vulnerability, with high-risk areas concentrated in town centers and along major roads, medium-high-risk areas mainly located where disaster-prone environments overlapped with exposed elements, and low-risk areas distributed in ecologically stable zones or regions lacking significant exposed elements. (4) High-risk zones exhibited strong spatial consistency with historical disaster points and typical exposed elements, thereby confirming the rationality and reliability of the assessment results. The findings reveal the spatial distribution pattern of geological disaster risk in Xinyuan County and provide a scientific basis and theoretical reference for disaster prevention and mitigation.

Key words: risk assessment, geological disasters, entropy weight method, random forest, Xinyuan County