江西主要植烟区的土壤中量元素含量及影响因素

Contents and Influencing Factors of Medium-element Nutrients in Tobacco-growing Soils of Jiangxi Province

  • 摘要:
    目的 明确江西省植烟区土壤中量元素含量状况及其影响因素,为烟草的合理施肥提供依据。
    方法 采集江西省典型植烟区6种主要土壤类型的69个表层土壤样品,测定土壤基本理化性质,通过分级处理和冗余分析(RDA)对土壤交换性钙镁和有效硫含量的特征进行分析。
    结果 江西省植烟区各类型土壤交换性钙镁含量缺乏严重,其均值分别为1.29 cmol(+) kg−1和0.28 cmol(+) kg−1;不同类型土壤之间交换性钙镁含量差异较大,分别在0.43 ~ 4.42 cmol(+) kg−1和0.11 ~ 0.98 cmol(+) kg−1之间。仅紫泥田中占比16.67%和8.33%的土壤交换性钙镁含量等级为适中,其余各类型土壤均未达适中水平的4 cmol(+) kg−1和0.8 cmol(+) kg−1。土壤有效硫的平均含量为16.76 mg kg−1,处于适中水平,但等级为极缺和缺的点位占比为39.61%,且各类型土壤有效硫变异系数均较大,在33.09%和57.23%之间。RDA分析表明,土壤交换性钙镁含量主要受pH和阳离子交换量(CEC)影响,而土壤类型则通过影响pH和CEC间接影响土壤交换性钙镁含量;土壤有效硫含量与有机质及黏粒含量呈现正相关关系,黏粒含量差异源于成土母质,由潮土发育而来的潮砂泥田中的黏粒含量较其他土壤更低。土壤物理性质主要通过改善土壤孔隙情况来影响其他指标进而影响中量元素有效性。
    结论 针对土壤交换性钙镁普遍缺乏问题可施用钙镁磷肥、熟石灰等方式补充,麻砂泥田可施用有机肥辅助改良。针对有效硫缺乏地区,可施用硫酸钾进行补充,紫泥田和麻砂泥田可施用有机肥辅助改良。

     

    Abstract:
    Objective This study aimed to clarify the content levels and influencing factors of medium elements in soils within tobacco-growing areas of Jiangxi Province, in order to provide a basis for rational fertilization of tobacco.
    Method Sixty-nine topsoil samples were collected from 6 predominant soil types in typical tobacco-growing regions, Jiangxi Province. Key physicochemical properties of each soil type were measured, and the characteristics of exchangeable Ca, Mg, and available S were analyzed through grading classification and redundancy analysis (RDA).
    Result The exchangeable Ca and Mg contents in various soil types of tobacco-growing regions were severely deficient, with average values of 1.29 cmol(+) kg−1 and 0.28 cmol(+) kg−1. Among different soil types, the contents of exchangeable Ca ranged from 0.43 to 4.42 cmol(+) kg−1, while the contents of exchangeable Mg fluctuated from 0.11 to 0.98 cmol(+) kg−1. Only 16.67% of the content of exchangeable Ca and 8.33% of the content of exchangeable Mg in purple clay paddy soils met the moderate thresholds of 4 cmol(+) kg−1 (Ca) and 0.8 cmol(+) kg−1 (Mg), whereas all other soil types fell below these critical levels. The average content of soil available S was 16.76 mg kg−1, indicating a moderate level, but 39.61% of sampling sites were classified as extremely deficient or deficient. The coefficients of variation (CV) for available S across soil types ranged from 33.09% to 57.23%. RDA results indicated that the variation in exchangeable Ca and Mg was mainly driven by pH and cation exchange capacity (CEC), whereas soil type exerted an indirect influence by altering these two factors. Soil available S content exhibited positive correlations with organic matter and clay content. This variation was primarily attributed to parent material, with alluvial sandy loam paddy soils (derived from fluvo-aquic soil) exhibiting significantly lower clay content compared to other soil types. Soil physical properties primarily influence medium element content by improving soil pore structure, which consequently affects related soil parameters.
    Conclusion Amendments such as calcium magnesium phosphate fertilizer or slaked lime can be applied to alleviate the widespread deficiency of exchangeable Ca and Mg. Organic fertilizer application can assist in improving granitic sandy loam paddy soils. Amendments such as potassium sulfate can be used in the available S-deficient area. Organic fertilizer application can also aid improvement in purple clay paddy soils and granitic sandy loam paddy soils.

     

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