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    基于RUSLE模型的冀北山地丘陵区土壤侵蚀特征及保护建议

    Soil erosion characteristics and protection suggestions in mountainous and hilly areas of Northern Hebei based on RUSLE model

    • 摘要:
      研究目的 土壤侵蚀是威胁全球陆地生态系统的关键问题,京津冀水源涵养区作为华北生态屏障,其山地丘陵区因采矿活动与生态保护的矛盾,土壤侵蚀问题日益突出。本研究以冀北山地丘陵区的平泉市为对象,基于RUSLE模型与GIS技术,结合2000—2023年多源数据,定量分析土壤侵蚀时空演变特征及其支流差异性。
      研究方法 研究运用RUSLE模型和GIS计算土壤流失量及空间分布,通过多源数据量化各侵蚀因子,分析土壤侵蚀的时空演变及支流差异。
      研究结果 平泉市土壤侵蚀以微度和轻度为主,时间上呈“政策抑制—矿业恶化—规划缓解”阶段性。高强度侵蚀集中于瀑河中游矿区、老哈河上游矿点与陡坡区,与坡长坡度因子高值区契合;青龙河、老牛河流域因植被保护侵蚀稳定。流域差异受矿业活动和植被覆盖主导,地形、土地利用和降雨共同作用。
      结论 平泉市土壤侵蚀机制具有独特性,属于“人类工程活动主导型”,矿业活动驱动强度远超国内外非资源型流域。高强度侵蚀与矿业热点区、陡坡地形耦合,验证了“生态修复边际效益衰减”与“采矿活动滞后影响”的双重机制。研究成果为京津冀水源涵养区协调“生态保护与矿业发展”提供了科学支撑。

       

      Abstract:
      This paper is the result of ecological geological survey engineering.
      Objective Soil erosion poses a critical threat to the global terrestrial ecosystem. As an ecological barrier in North China, the water conservation zone of the Beijing–Tianjin–Hebei region confronts increasingly acute soil erosion in its mountainous and hilly areas, primarily driven by the conflict between mining activities and ecological protection. This study takes Pingquan City, located in the mountainous-hilly region of northern Hebei, as the research case. By integrating the RUSLE model with GIS technology and multi-source datasets from 2000 to 2023, it quantitatively analyzes the spatial-temporal evolution of soil erosion and examines differences among its tributaries.
      Methods This study employs the RUSLE model and GIS to calculate soil loss and its spatial distribution. By quantifying each erosion factor through multi-source data, the spatial-temporal evolution of soil erosion and differences among tributaries is analyzed.
      Results Soil erosion in Pingquan City is dominated by slight and mild degrees, showing a phased pattern of "policy suppression-mining deterioration-planning mitigation" over time. High-intensity erosion is concentrated in the middle reaches of the Pu River mining area, the upper reaches of the Laoha River mining sites, and steep slope areas, which coincide with the high-value areas of slope length and gradient factors; the Qinglong River and Laoniu River basins have stable erosion due to vegetation protection. The differences among basins are dominated by mining activities and vegetation cover, with topography, land use, and rainfall acting together.
      Conclusions Pingquan City exhibits a unique soil erosion mechanism characterized as "human engineering activity-dominated", where the driving intensity of mining activities far exceeds that of non-resource-based basins at home and abroad. The coupling of high-intensity erosion with mining hotspots and steep terrain verifies the dual mechanisms of "diminishing marginal benefits of ecological restoration" and "lagging impacts of mining activities". The research findings provide scientific support for coordinating "ecological protection and mining development" in the water conservation area of the Beijing–Tianjin–Hebei region.

       

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