塔里木河流域典型植棉区耕地土壤养分空间分布及综合肥力评价

Spatial distribution and comprehensive fertility evaluation of soil nutrients in typical cotton-growing areas of the Tarim River Basin

  • 摘要:
    目的 揭示塔里木河流域耕地土壤养分空间分布特征,定量评价土壤综合肥力水平,为区域精准施肥和耕地质量提升提供理论依据。
    方法 以沙井子垦区、塔南片区和塔北片区0~20 cm耕层土壤为研究对象,测定有机质、碱解氮、有效磷、速效钾及pH。采用描述性统计法分析土壤养分空间变异特征,运用克里金插值法绘制土壤养分空间分布图,采用内梅罗综合指数开展土壤肥力综合评价。
    结果 研究区内土壤有机质整体处于缺乏水平,碱解氮整体达中等及以上水平,有效磷、速效钾含量整体均处于丰富及以上水平;各养分指标空间异质性显著,土壤综合肥力主要受有机质限制;沙井子垦区、塔南片区、塔北片区综合肥力指数分别为1.39、1.25、1.32,肥力等级均为一般。
    结论 塔里木河流域典型植棉区耕地土壤养分空间差异显著,土壤肥力受有机质匮乏制约,生产中应优化氮磷钾养分投入结构,加强有机培肥与耕地保育管理。

     

    Abstract:
    Objective To reveal the spatial distribution characteristics of soil nutrients in cultivated land of the Tarim River Basin, quantitatively evaluate the comprehensive soil fertility level, and provide a theoretical basis for regional precision fertilization and cultivated land quality improvement.
    Methods Soil samples in the 0–20 cm plow layer were collected from the Shajingzi Reclamation Area, Tarim South Area and Tarim North Area. Soil organic matter, alkali-hydrolyzable nitrogen, available phosphorus, available potassium and pH were determined. Spatial variability of soil nutrients was analyzed by descriptive statistics, spatial distribution maps of soil nutrients were drawn by Kriging interpolation, and comprehensive soil fertility was evaluated by the Nemerow comprehensive index method.
    Results Soil organic matter in the study area was generally deficient; alkali-hydrolyzable nitrogen was at a medium or higher level; available phosphorus and available potassium were at an abundant or higher level. Spatial heterogeneity of all nutrient indicators was significant, and comprehensive soil fertility was mainly limited by organic matter. The comprehensive fertility indices of the Shajingzi Reclamation Area, Tarim South Area and Tarim North Area were 1.39, 1.25 and 1.32, respectively, all graded as moderate.
    Conclusion Soil nutrients in cultivated land of typical cotton-growing areas in the Tarim River Basin show significant spatial differences, and soil fertility is restricted by insufficient organic matter. In agricultural production, the input structure of nitrogen, phosphorus and potassium should be optimized, and organic fertilization and cultivated land conservation management should be strengthened.

     

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