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    1990—2020年湖南省土壤侵蚀时空变化及其驱动机制

    Spatiotemporal variations in soil erosion and its driving mechanisms in Hunan province from 1990 to 2020

    • 摘要:
      目的 作为长江中游的重要生态屏障,湖南省土壤侵蚀时空变化直接关系到区域生态安全格局的构建,对于揭示其驱动机制、维护区域生态安全具有重要意义。
      方法 基于修正通用土壤流失方程(RUSLE)模型,综合运用地理探测器、转移矩阵和空间自相关分析等方法,本研究系统地揭示1990—2020年湖南省土壤侵蚀的时空演变规律及其驱动力机制。
      结果 1)近30年来,湖南省土壤侵蚀以微度和轻度为主(占91.63%),中度及以上仅占8.37%,多年平均土壤侵蚀模数为2091.87 t/(km2·a)。2)土壤侵蚀存在明显的空间聚集特征,“高−高”聚集区主要位于湘西武陵山区、雪峰山脉北麓及罗霄山脉西侧;“低−低”聚集集中在洞庭湖平原、湘江中下游河谷平原及沅水下游冲积平原。3)地貌类型以大起伏山地为主是影响湖南省土壤侵蚀空间格局的主导因子(解释力强度q = 0.056),其与坡度的交互作用对侵蚀格局的驱动作用最为显著(q = 0.069),中度及以上侵蚀面积呈波动变化,主要受区域内多次极端暴雨事件驱动。高风险区具有中高坡度(6.32°~27.80°)、粉粒含量高、海拔557~1980 m、NDVI低(0.559~0.598)等特征。
      结论 湖南省土壤侵蚀总体较轻,土壤侵蚀治理需重点关注湘西及湘东山地中高坡度与粉砂质土壤区域,强化植被恢复与工程措施。该研究结果可为湖南省水土流失防控与生态安全建设提供科学依据。

       

      Abstract:
      Objective As an important ecological barrier in the middle reaches of the Yangtze River, the spatiotemporal variations in soil erosion in Hunan province are directly linked to the construction of regional ecological security patterns, which is of great significance for revealing its driving mechanism and maintaining regional ecological security.
      Methods Based on the Revised Universal Soil Erosion Equation (RUSLE) model, and by comprehensively using methods including geodetector, transfer matrix, and spatial autocorrelation analysis, this study systematically revealed the spatiotemporal evolution patterns of soil erosion and their driving mechanisms in Hunan Province from 1990 to 2020.
      Results 1) Over the past 30 years, soil erosion in Hunan Province was dominated by slight and mild levels (accounting for 91.63%), while the moderate and above levels accounted for only 8.37%. The multi-year average soil erosion modulus was 2 091.87 t/(km2·a). 2) Soil erosion exhibited distinct spatial clustering characteristics. The "high-high" clustering areas were mainly located in the Wuling Mountain area of western Hunan, the northern foothills of the Xuefeng Mountains, and the western side of the Luoxiao Mountains. The "low-low" clustering was concentrated in the Dongting Lake Plain, the valley plain in the middle and lower reaches of the Xiangjiang River, and the alluvial plain of the lower reaches of the Yuanjiang River. 3) The dominant landform type, characterized by large undulating mountains, was the leading factor influencing the spatial patterns of soil erosion in Hunan province (explanatory power q = 0.056), and its interaction with slope gradient has the most significant driving effect on the erosion patterns (q = 0.069). The area of moderate and above erosion exhibited fluctuating changes, mainly driven by multiple extreme rainstorm events within the region. High-risk areas were characterized by medium to high slopes (6.32°−27.80°), high silt content, an altitude of 557−1 980 m, and low NDVI (0.559−0.598).
      Conclusions Soil erosion in Hunan province is generally mild. Soil erosion control should focus on the mountainous areas with medium to high slope gradients and silty soil in western and eastern Hunan, with an emphasis on vegetation restoration and engineering measures. The research findings can provide a scientific basis for the prevention and control of soil erosion and the construction of ecological security in Hunan province.

       

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