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基于GIS和RUSLE的昕水河流域土壤侵蚀特征与多情景模拟OA

Characteristics of soil erosion and multi-scenario simulation based on GIS and RUSLE in Xinshui River Basin

中文摘要英文摘要

[目的]本研究旨在探究长时间序列下土地利用变化对土壤侵蚀时空变化的影响,预测 2030年土地利用空间分布情况.[方法]采用 GIS 空间分析技术与 RUSLE模型,对黄河中游昕水河流域土壤侵蚀时空变化开展量化分析.在此基础上结合 PLUS模型对 3种情境(基准发展、耕地保护和生态保护情景)下 2030年土地利用情况进行模拟.[结果]1)1995-2020年,昕水河流域林地面积呈上升趋势,由 8.85×104 hm2 升至 1.16×105 hm2.耕地与草地面积有所下降;2020年,耕地、草地面积分别为 9.48×104 hm2 和 2.16×105 hm2,分别下降3.27%与 11.48%.建设用地面积不断上升,由 1995年的 773.23 hm2 增至 2.99×103 hm2.2)流域土壤侵蚀模数表现出先上升后下降趋势.2015年,昕水河流域土壤侵蚀模数由 76.37 t/(hm2·a)降至 64.24 t/(hm2·a),2020年增至 97.31 t/(hm2·a).流域中度及以下侵蚀面积增加,但中度侵蚀以上高强度土壤侵蚀面积明显下降.微度侵蚀面积逐年增加,由 2.41×105 hm2 升至 2.58×105 hm2.3)在基准发展、耕地保护和生态保护情景下,昕水河流域林地与建筑用面积均呈现出上升趋势.在生态保护情境下,建设用地上升数量最低.[结论]昕水河流域近25 a林草覆盖度不断提高,土壤侵蚀强度呈下降趋势.

[Objective]This study aims to investigate the impact of long-term land use changes on the spatiotemporal variation of soil erosion and to predict the spatial distribution of land use in 2030.[Methods]This study employed GIS spatial analysis techniques and the RUSLE model to quantitatively analyze the spatiotemporal variation of soil erosion in the Xinshui River Basin in the middle reaches of the Yellow River.On this basis,the PLUS model was utilized to simulate and visualize the land use distribution in 2030 under three scenarios:baseline development,farmland protection,and ecological protection.[Results]1)The area of forestland in the Xinshui River Basin showed an increasing trend from 1995 to 2020,rising from 8.85×104 hm2 to 1.16×105 hm2.The areas of farmland and grassland decreased to 9.48×104 hm2 and 2.16×105 hm2 in 2020,which were 3.27%and 11.48%lower than those in 1995,respectively.The construction land area continuously increased from 773.23 hm2 in 1995 to 2.99×103 hm2 in 2020.2)The soil erosion modulus in Xinshui River Basin showed a trend of first decreasing and then increasing.It decreased from 76.37 t/(hm2·a)to 64.24 t/(hm2·a)in 2015,and then increased to 97.31 t/(hm2·a)in 2020.The area of moderate and lower erosion increased,while the area of high-intensity soil erosion above moderate erosion decreased significantly.The area of slight erosion increased from 2.41×105 hm2 in 1995 to 2.58×105 hm2 in 2020.3)Under the baseline development,farmland protection,and ecological protection scenarios,both forestland and construction land area in the Xinshui River Basin showed an increasing trend.Among them,the increase in construction land area was the smallest under the ecological protection scenario.[Conclusions]In the Xinshui River Basin,the coverage of forest and grass has been continuously increasing,and the intensity of soil erosion has shown a decreasing trend over the past 25 years.

池金洺;巴梦茜;闫亭舟;朱洪盛;于洋

北京林业大学水土保持学院,100083,北京||北京林业大学 山西吉县森林生态系统国家野外科学观测研究站,100083,北京||国家林业和草原局产业发展规划院,100010,北京北京林业大学水土保持学院,100083,北京||北京林业大学 山西吉县森林生态系统国家野外科学观测研究站,100083,北京北京林业大学水土保持学院,100083,北京北京林业大学水土保持学院,100083,北京北京林业大学水土保持学院,100083,北京||北京林业大学 山西吉县森林生态系统国家野外科学观测研究站,100083,北京

农业科技

昕水河流域土壤侵蚀修正通用土壤流失方程斑块生成土地利用变化模拟模型

Xinshui River Basinsoil erosionRevised Universal Soil Loss Equationpatch-generating land use simulation model

《中国水土保持科学》 2026 (4)

84-93,10

国家重点研发计划"生物与工程措施结合的水土流失精准控制技术与示范"(2023YFF1305101) National Key Research and Development Plan"Precision Control Technology and Demonstration for Soil and Water Loss Combining Biological and Engineering Measures"(2023YFF1305101)

10.16843/j.sswc.2025185

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