横断山区水土流失敏感性时空演变与预测研究OA
Spatiotemporal evolution and prediction of soil erosion sensitivity in Hengduan Mountains
[目的]探究横断山区水土流失敏感性的演变规律,为制定差异化的水土保持与防治策略、保障生态安全提供科学参考.[方法]基于RUSLE模型,分析了2000-2020年横断山区水土流失敏感性的时空变化特征.采用CA-Markov模型预测2025年与2030年水土流失敏感性结果,并利用地理探测器定量分析了水土流失敏感性变化的驱动机制.[结果](1)横断山区水土流失敏感性总体以不敏感为主,且敏感程度呈现缓解趋势.不敏感区域先减后增,轻度敏感区域逐年增加,而中度、重度和极度敏感区域均呈现先增后减的变化规律.水土流失敏感性空间分布差异较为明显,空间变化特征较为一致.总体呈西南高、东北低的空间分布特点.(2)植被覆盖度、年均降水是影响横断山区水土流失敏感性的主要驱动因子.因子交互作用主要表现为非线性增强.相较于其他因子之间的交互作用,植被覆盖度的交互作用影响力更为显著.(3)横断山区未来5~10 a水土流失敏感性整体呈现向好趋势,不敏感和轻度敏感区域面积增加,中度、重度和极度敏感区域面积减小.[结论]横断山区地区水土流失敏感性总体得到有效遏制,水土流失敏感性动态规律显著,植被覆盖度对其变化驱动作用明显.今后,需根据水土流失敏感性程度实施分区治理,有针对性地采取不同水土流失保护与防治策略.
[Objective]This study aims to investigate the evolutionary patterns of soil erosion sensitivity in the Hengduan Mountains,thereby providing scientific references for formulating differentiated soil and water conservation and control strategies and ensuring ecological security.[Methods]Based on the RUSLE model,the spatiotemporal characteristics of soil erosion sensitivity in the Hengduan Mountains from 2000 to 2020 were analyzed.The CA-Markov model was used to predict soil erosion sensitivity in 2025 and 2030,and the geodetector was used to quantitatively analyze the driving mechanisms behind the changes in soil erosion sensitivity.[Results](1)The overall soil erosion sensitivity in the Hengduan Mountains was mainly insensitive,and the degree of sensitivity showed a trend of alleviation.The area of insensitive regions first decreased and then increased,while that of slightly sensitive regions increased year by year.The areas of moderately,highly,and extremely sensitive regions all showed a trend of first increasing and then decreasing.The spatial distribution of soil erosion sensitivity showed notable differences,and the spatial change characteristics were relatively consistent.Overall,it showed a spatial distribution pattern of high sensitivity in the southwest and low sensitivity in the northeast.(2)Vegetation cover and annual average precipitation were the main driving factors affecting soil erosion sensitivity in the Hengduan Mountains.The interaction between factors was primarily manifested as nonlinear enhancement.Compared to the interaction between other factors,the interaction of vegetation cover had a more significant influence.(3)The soil erosion sensitivity in the Hengduan Mountains was projected to show an overall improving trend in the next 5~10 years.The areas of insensitive and slightly sensitive regions were projected to increase,while the areas of moderately,highly,and extremely sensitive regions were projected to decrease.[Conclusion]The soil erosion sensitivity in the Hengduan Mountains is effectively controlled in general,exhibiting a distinct dynamic pattern.The vegetation cover plays a significant role in driving these changes.In the future,it is necessary to implement zonal management based on the degree of soil erosion sensitivity and adopt targeted strategies for soil erosion protection and control.
邓锦山;江飞;麻泽龙;卢鑫;李卓蔓
四川省水利科学研究院,成都 610072四川省水利科学研究院,成都 610072四川省水利科学研究院,成都 610072四川省水利科学研究院,成都 610072四川省水利科学研究院,成都 610072
农业科技
水土流失敏感性时空变化横断山区
soil erosion sensitivityspatiotemporal variationHengduan Mountains
《水土保持研究》 2026 (2)
13-23,11
四川省自然科学基金(24NSFSC3892)四川省公益性科研院所基本科研项目(2025-SKY-ZXKY-04,2025-SKY-ZXKY-01)
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