中国农业气象 ›› 2026, Vol. 47 ›› Issue (9): 1373-1387.doi: 10.3969/j.issn.1000-6362.2026.09.002

• 农业生态环境栏目 • 上一篇    下一篇

黄土水力侵蚀机制与预测模型研究进展

  

  1. 1.长安大学地质工程与测绘学院,西安 710054;2. 自然资源部生态地质与灾害防控重点实验室,西安 710054;3.中铁第一勘察设计院集团有限公司,西安 710043

  • 收稿日期:2025-06-27 出版日期:2026-09-20 发布日期:2026-09-18
  • 通讯作者: 李明昊 E-mail:1271027643@qq.com
  • 基金资助:
    国家自然科学基金项目(42377158)

Research Progress and Prospects on Mechanisms and Prediction Models of Hydraulic Erosion in Loess Regions

  1. 1.College of Geological Engineering and Geomatics,Chang’an University,Xi’an 710054,China;2.Key Laboratory of Ecological Geology and Disaster Prevention,Ministry of Natural Resources,Xi'an 710054;3.China Railway First Survey and Design Institute Group Co.,Ltd,Xi'an 710043

  • Received:2025-06-27 Online:2026-09-20 Published:2026-09-18
  • Supported by:

摘要: :黄土地区地形复杂,降水量时空差异大,且黄土具有大孔隙、水敏性和易崩解等特性,导致水力侵蚀严重。理清黄土水力侵蚀机理与预测模型的研究现状,可为该地区水土保持、地质灾害防治、生态修复及可持续发展等领域的深入研究指明方向。本研究通过检索国内外相关文献,分析多种影响因素对黄土侵蚀机制的作用差异,对比不同模型在黄土地区水力侵蚀过程中的适用性,系统总结黄土水力侵蚀机制与预测模型的研究进展及存在问题。结果表明:(1)黄土水力侵蚀方式分为溅蚀、面蚀和沟蚀,不同侵蚀方式受降水量、地形、植被、黄土性质与人类活动的多因素影响。(2)黄土水力侵蚀主要以降水量和径流为动力驱动,以水土相互作用为基本原理,但黄土侵蚀水力学机制不明,难以支撑水力侵蚀预测模型的构建。(3)黄土水力侵蚀预测模型主要分为经验统计模型和物理成因模型,受限于模拟精度、过程描述以及机理认知的不足,现有模型难以满足水力侵蚀防治需要。未来需加强水力侵蚀监测与研究数据积累,加深黄土水力侵蚀动力学机制研究,为黄土地区生态环境保护与水力侵蚀防治提供参考。

关键词: 黄土, 水力侵蚀, 侵蚀机制, 侵蚀模型

Abstract: The Loess region is characterized by complex topography,significant spatiotemporal variations in precipitation and unfavorable soil properties such as large pores,water sensitivity and easy disintegration of loess, which collectively lead to severe hydraulic erosion.To clarify the current research status of research on the mechanisms and predictive models of loess hydraulic erosion can provide direction for in−depth studies in soil and water conservation,geological hazard prevention,ecological restoration and sustainable development in the region. By reviewing relevant domestic and international literature,the study was to compare the differences of various influencing factors on the mechanism of loess erosion,compare the applicability of different models in simulating hydraulic erosion processes in the loess region,and systematically summarize research progress and existing issues regarding loess hydraulic erosion mechanisms and predictive models.The results showed that:(1)loess hydraulic erosion could be categorized into raindrop splash,sheet erosion and rill erosion,with each type influenced by multiple factors,including precipitation,topography,vegetation,loess properties and human activities.(2) Loess hydraulic erosion was primarily driven by precipitation and runoff,based on the fundamental principle of soil−water interactions. However, the hydraulic mechanisms underlying loess erosion remained unclear, hindering the development of accurate prediction models.(3)Prediction models for loess hydraulic erosion were mainly divided into empirical model and physically−based model.Nevertheless,due to limitations in simulation accuracy,process representation and mechanistic understanding,these models fell short of meeting the needs for hydraulic erosion control.Future efforts should focus on enhancing hydraulic erosion monitoring and data accumulation,deepening research on the dynamic mechanisms of loess hydraulic erosion,and providing a theoretical foundation for ecological conservation and erosion mitigation in loess regions.

Key words: Loess, Hydraulic erosion, Erosion mechanism, Erosion model