• ISSN 1008-505X
  • CN 11-3996/S

江苏省耕地土壤有机质时空演变特征及主要驱动因素

Spatial and temporal evolution of soil organic matter in cultivated land across Jiangsu Province and its driving factors

  • 摘要:
    目的 探究耕地土壤有机质含量演变及其驱动机制,为研究区耕地质量保护与提升提供理论依据。
    方法 基于2010年和2020年全国测土配方施肥数据,运用地统计学方法和GIS空间分析技术,分析江苏省耕地土壤有机质含量的时空演变规律及其影响因素。
    结果 1)2010—2020年,江苏省耕地土壤有机质含量整体呈上升趋势,全省均值由2010年的19.83 g/kg增加至25.15 g/kg,升高26.83%。2)有机质空间分布呈里下河和太湖农区较高、沿江和宁镇扬丘陵农区中等、徐淮和沿海农区较低的格局。3)10年间,里下河、沿江、徐淮农区有机质含量增长最多,年均增长量分别为0.59 g/kg、0.48 g/kg、0.47 g/kg,其次是宁镇扬丘陵和沿海农区,年均增长量分别为0.39 g/kg、0.33 g/kg,太湖农区年均增长最少,为0.28 g/kg。4)10年来,有机质含量受到成土母质、土壤质地等自然因素影响逐渐减弱,施肥、秸秆还田、建设用地扩张等人为因素扰动影响增强,并在局部呈现有机质含量的下降趋势。
    结论 江苏省2010—2020年耕地土壤有机质含量整体呈上升趋势,且里下河和太湖农区有机质含量较高、沿江和宁镇扬丘陵农区中等、徐淮和沿海农区较低的空间格局基本不变。变化幅度上,里下河、沿江、徐淮农区有机质含量增长量最多,其次是宁镇扬丘陵和沿海农区,太湖农区有机质含量增长最少。江苏省耕地土壤有机质含量主要受成土母质、土壤质地等自然因素影响,但2010年以后,人为因素扰动影响更为显著,肥料施用和秸秆还田是江苏省耕地土壤有机质含量提高的主要因素,建设用地扩张侵占、土壤盐碱化和单一种植模式是局部区域耕地土壤有机质含量下降的诱因。

     

    Abstract:
    Objectives To investigate the spatial and temporal evolution of soil organic matter(SOM) content in cultivated land and its driving mechanism, providing a theoretical basis for cultivated land quality protection and improvement in Jiangsu Province.
    Methods Using national soil testing and fertilizer application datasets from 2010 and 2020, geostatistical methods and GIS spatial analysis techniques were applied to analyze the spatial and temporal evolution of SOM content in cultivated land across Jiangsu Province and identify the main influencing factors.
    Results 1) The provincial average SOM content increased from 19.83 g/kg in 2010 to 25.15 g/kg in 2020, representing a rise of 26.83%. 2) Spatially, SOM content was higher in the Lixiahe and Taihu Lake agricultural regions, moderate in the Riverside and Ning-Zhen-Yang Hilly agricultural regions, and lower in the Xu-Huai and Coastal agricultural regions. 3) Over the past 10 years, the highest average annual SOM content increase was observed in the Lixiahe (0.59 g/kg), Riverside (0.48 g/kg) and Xu-Huai (0.47 g/kg) agricultural regions, followed by the Ning-Zhen-Yang Hilly (0.39 g/kg) and Coastal agricultural regions (0.33 g/kg). The Taihu Lake agricultural region showed the smallest average annual increase (0.28 g/kg). 4) Natural factors, such as parent material and soil texture, had limited influence on SOM content over the past decade, whereas anthropogenic factors, including fertilizer application, straw returning to the field, and construction land expansion, exerted increasing impacts, causing SOM content declines in some local areas.
    Conclusions From 2010 to 2020, SOM content in cultivated land across Jiangsu Province showed an overall upward trend, with the spatial pattern remaining largely unchanged: higher SOM content in the Lixiahe and Taihu Lake agricultural regions, moderate levels in the Riverside and Ning-Zhen-Yang Hilly agricultural regions, and lower levels in the Xu-Huai and Coastal agricultural regions. In terms of the magnitude of change, the Lixiahe Riverside and Xu-Huai agricultural regions experienced the greatest increases in SOM content, followed by the Ning-Zhen-Yang Hilly and Coastal agricultural regions, while the Taihu Lake agricultural region saw the least increase. The SOM content in cultivated land across Jiangsu Province is primarily influenced by natural factors such as parent material and soil texture. However, after 2010, the impact of human disturbances became more pronounced. Fertilizer application and straw returning to the field were the main factors contributing to the increase in SOM content in cultivated land across Jiangsu Province, while construction land expansion, soil salinization, and monoculture practices were the main causes of the decline in SOM content in certain local areas.

     

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