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    基于GIS和RULSE的昕水河流域土壤侵蚀特征与多情景模拟

    Quantitative Analysis of Land Use Changes on Soil Erosion and Mult-scenario Simulation Based on GIS and RUSLE in Xinshui River Basin

    • 摘要: 基于GIS和RULSE的昕水河流域土壤侵蚀特征与多情景模拟 /t/n池金洺1,巴梦茜1, 朱洪盛1,闫亭舟1,于洋1,2*/t/n摘要:目的开展流域土壤侵蚀特征及多情境土地利用模拟对流域可持续管理策略制定具有重要意义。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进行了量化分析,在此基础上结合斑块级土地利用变化模拟模型(Patch-level Land Use Simulation Model, PLUS)对三种情境(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了模拟。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9.48×104hm2、2.16×105 hm2,分别下降3.22%与11.43%。建设用地面积不断上升,由1995年的773.23 hm2增至2.99×103hm2。(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)后,于2020年增至97.31 t/(hm2·a)。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。研究认为:昕水河流域近三十年林草覆盖度不断提高,土壤侵蚀强度呈下降趋势,研究结果可为昕水河流域植被恢复与综合治理提供科学支撑。

       

      Abstract: Objective It is of great significance to carry out soil erosion characteristics and multi-scenario land use simulation in the basin for developing sustainable management strategies. Methods This study quantitatively analyzes the temporal and spatial characteristics of soil erosion in Xinshui River Basin from 1995 to 2020, at the same time, the PLUS model was taken to simulate the 2023 land use type in different scenarios. Results (1) The area of forestland showed a increasing trend from 1995 to 2020, increased from 8.85×104 hm2 to 1.16×105 hm2. The farmland and the grassland decreased. The area of farmland and grassland were 9.48×104 hm2 and 2.16×105 hm2 in 2020, which were 3.22% and 11.43% lower than those in 1995. The area of building land has gradually increased, from 773.23 hm2 in 1995 to 2.99×103 hm2 in 2018. (2) The soil erosion modulus in Xinshui River Basin fluctuated 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 slight erosion land increased from 2.41×105 hm2 in 1995 to 2.58×105 hm2 in 2020. (3) In different simulation scenarios, the forest land building area in Xinshui River Basin showed an decreasing trend, and in the ecological protection scenario, the number of building land increased the least. During the 25 years in Xinshui River Basin, the coverage of forest and grass improved continuously, and the intensity of soil erosion decreased. Conclusion The results of this study provided a basis for the ecological protection and comprehensive management of Xinshui River Basin.

       

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