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    东北黑土区小流域侵蚀沟空间分布特征及驱动因素

    Gully spatial distribution characteristics and their driving factors in The Northeast Black Soil Region

    • 摘要: 侵蚀沟是东北黑土区坡耕地的严重土壤侵蚀表现,已成为粮食和生态安全的重要威胁。本研究在东北黑土区吉林省兴家甸小流域开展侵蚀沟实地调查及其其形态和地形参数统计分析,并采用空间自相关和地理探测器,辨识了网格和子流域尺度的侵蚀沟线密度、面密度和核密度空间分布特征与主控因素。主要获得以下结论:1)小流域内的侵蚀沟规模差异较大,但断面形态、几何形态及地形发育条件较为相似。2)侵蚀沟的空间分布具有明显正向空间自相关关系,局部聚集和热点区域主要集中在小流域的西北部和南部区域,核密度对侵蚀沟分布格局具有良好空间解释力。网格尺度适用于揭示侵蚀沟空间异质性与局部聚集特征,而子流域尺度适用于区域整体侵蚀格局研究。3)土地利用、距居民点距离、距耕地距离、垄作方向、高程、坡度、地表起伏度、地表粗糙度与NDWI等因素为研究流域的的侵蚀沟发育主控因子,其中“高程+土地利用”组合的解释力最高,多数人类活动因子与其他因子组合后解释力均普遍较高。研究结果可为深入理解东北黑土区侵蚀沟空间分布规律与发育机制提供定量证据,也为后续风险预警预测中空间规划与流域综合治理提供参考。

       

      Abstract: Gully erosion is a severe form of soil erosion on sloping farmland in the black soil region of Northeast China, posing a major threat to food security and ecological security. This study conducted field investigations of gullies in the Xingjiadian small watershed of Jilin Province and performed statistical analyses of their morphological and topographic parameters. Spatial autocorrelation analysis and the geographical detector were further applied to identify the spatial distribution characteristics and dominant factors of gully line density, area density, and kernel density at the grid and sub-watershed scales. The main conclusions are as follows: (1) The gullies within the small watershed vary considerably in scale, but their cross-sectional shapes, geometric forms, and topographic development conditions are relatively similar. (2) The spatial distribution of gullies shows a clear positive spatial autocorrelation. Local clusters and hotspot areas are mainly concentrated in the northwestern and southern parts of the watershed, and kernel density provides strong spatial explanatory power for gully distribution patterns. The grid scale is suitable for revealing spatial heterogeneity and local aggregation characteristics of gullies, whereas the sub-watershed scale is more appropriate for analyzing the overall regional erosion pattern. (3) Land use, distance to residence, distance to cropland, ridge direction, elevation, slope, surface relief, surface roughness, and NDWI are identified as the dominant factors influencing gully development. Among these, the combination of “elevation + land use” achieves the highest explanatory power, and combinations involving most human-activity-related factors generally exhibit stronger explanatory effects. The results provide quantitative evidence for understanding the spatial distribution patterns and development mechanisms of gullies in the black soil region of Northeast China and offer references for spatial planning and integrated watershed management in future risk assessment and prediction.

       

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