有机肥与白云石粉及生物炭复配对强酸性黄壤酸化特征的影响

Effects of Organic Fertilizer Combined with Dolomite Powder and Biochar on Acidification Characteristics of Strongly Acidic Yellow Soil

  • 摘要:
    目的 探究不同改良材料复配对强酸性黄壤酸化特征的影响,筛选出不同改良剂的最佳配施组合,以期为酸化黄壤的改良提供理论和技术支撑。
    方法 采用室内短期土壤培养试验,设置CK(不施用任何改良材料)、N(单施氮肥)、施用有机肥及其与不同用量生物炭或白云石粉配施共11个处理,分析土壤pH、交换性酸、交换性盐基离子等变化特征。
    结果 与CK相比,N处理pH显著提高了0.46个单位、交换性酸显著提高了8.63%;与N处理相比,施用有机肥交换性盐基离子总量显著提高了120.34%,有机肥配施生物炭或白云石粉土壤pH显著提高了0.15 ~ 0.82个单位、交换性酸显著降低了12.05% ~ 36.25%、交换性盐基离子总量显著提高了228.84% ~ 500.57%,以有机肥 + 高量生物炭 + 高量白云石粉处理改良效果最佳;土壤pH与交换性酸呈极显著负相关,其中与交换性氢的线性相关性更高;土壤pH与交换性盐基离子呈极显著正相关,其中交换性钙起主导作用;改良材料碱度与pH及交换性盐基离子呈极显著线性正相关,与交换性酸呈极显著线性负相关,其中与交换性铝、交换性钾、交换性钙的相关系数较高。
    结论 土壤酸化与交换性酸和交换性盐离子含量关系密切,受交换性钙的影响最大。单施有机肥对强酸性土壤改良效果欠佳,配施白云石粉或生物炭可显著提高酸化改良效果,二者高量配施效果最佳。

     

    Abstract:
    Objective The effects of different modified materials on the acidification characteristics of strongly acidic yellow soil were explored, and the best combination of different modifiers was selected to provide theoretical and technical support for the improvement of acidified yellow soil.
    Method The indoor short-term soil culture experiment was carried out, and 11 treatments were set up, including CK (do not apply any modified materials), N (single application of nitrogen fertilizer), application of organic fertilizer and its combination with different amounts of biochar or dolomite powder. The variation characteristics of soil pH, exchangeable acid and exchangeable base ions were analyzed.
    Result Compared with CK, the pH of N treatment was significantly increased by 0.46 units, the exchangeable acid was significantly increased by 8.63%. Compared with N treatment, the total amount of exchangeable base ions increased by 120.34%, the soil pH of organic fertilizer combined with biochar or dolomite powder was significantly increased by 0.15 - 0.82 units, the exchangeable acid decreased by 12.05% - 36.25%, and the total amount of exchangeable base ions increased by 228.84% - 500.57%. The treatment of organic fertilizer + high amount of biochar + high amount of dolomite powder had the best improvement effect. Soil pH was significantly negatively correlated with exchangeable acid, and the linear correlation with exchangeable hydrogen was higher. Soil pH was significantly positively correlated with exchangeable base ions, in which exchangeable calcium played a leading role. The alkalinity of the modified material was significantly positively correlated with pH and exchangeable base ions, and significantly negatively correlated with exchangeable acid. The correlation coefficients with exchangeable aluminum, exchangeable potassium and exchangeable calcium were higher.
    Conclusion Soil acidification is closely related to the content of exchangeable acid and exchangeable salt ions, and is most affected by exchangeable calcium. The improvement effect of single application of organic fertilizer on strongly acidic soil was not good, and the combination of dolomite powder or biochar could significantly increase the improvement effect of acidification, and the combination of the two is the best.

     

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