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有机肥替代部分化学氮肥对强酸性土壤酸度和铝形态的调控作用

Effects of partial replacement of chemical nitrogen fertilizer with organic fertilizers on soil acidity and aluminum fractions in a strongly acidic soil

  • 摘要: 强酸性土壤普遍存在铝毒障碍,严重制约作物生长和土壤质量提升。有机肥替代部分化学氮肥是阻控土壤酸化的重要措施,但不同来源有机肥的性质差异及其降酸控铝效果尚不清楚。本研究以南方典型强酸性红壤为供试土壤,选取8种不同来源的代表性有机肥开展室内培养试验,比较其主要元素组成和酸碱性质,分析其对土壤酸度和铝形态转化的影响。结果表明,受原料来源和堆腐方式等因素影响,不同有机肥的碳氮含量、可溶性有机碳含量、pH、酸中和容量及盐基离子含量存在显著差异。有机肥改良酸性土壤的效果与其酸中和容量和盐基离子含量显著相关,而与有机肥自身pH无显著相关性。与单施硫酸铵相比,有机肥替代50%化学氮肥均能缓解土壤酸化,提高土壤pH和交换性盐基离子含量,土壤可溶性有机碳含量总体呈增加趋势。同时,有机肥处理降低了可溶性铝和交换性铝等高活性铝形态的含量,并促进羟基结合态铝和无定形铝等相对稳定形态的形成。提高土壤pH是降低活性铝的主要机制。可溶性有机碳参与可溶性单核有机铝的形成,能够降低单核无机铝的含量,但也可能使部分铝保持在可溶性有机络合态,从而延缓可溶性铝向相对稳定的固相铝形态转化。综合比较表明,商品鸡粪和虾肽有机肥的降酸控铝效果较好。商品鸡粪处理使土壤pH提高0.19个单位、可溶性有机碳含量提高18.8%,可溶性铝和交换性铝含量分别降低48.5%和70.5%;虾肽有机肥处理使土壤pH提高0.25个单位,可溶性铝和交换性铝含量分别降低45.6%和69.9%。研究结果可为高效控酸有机肥的筛选及强酸性土壤酸化与铝毒风险协同调控技术的构建提供理论依据。

     

    Abstract: Aluminum toxicity is a widespread constraint in strongly acidic soils, severely limiting crop growth and improvements in soil quality. Partial replacement of chemical nitrogen fertilizer with organic fertilizers is an important practice for mitigating soil acidification. However, the differences in the properties of organic fertilizers from different sources and their effects on soil acidity and aluminum fractions remain unclear. A laboratory incubation experiment was conducted using a typical strongly acidic red soil from southern China, with eight representative organic fertilizers from different sources. Their major elemental compositions and acid base properties were compared, and their effects on soil acidity and the transformation of aluminum fractions were analyzed. The results showed that the organic fertilizers differed significantly in carbon and nitrogen contents, dissolved organic carbon content, pH, acid neutralization capacity, and base cation contents because of differences in feedstock sources and composting methods. The effectiveness of organic fertilizers in ameliorating acidic soil was significantly correlated with their acid neutralization capacity and base cation contents, but not with their own pH. Compared with the sole application of ammonium sulfate, replacing 50% of chemical nitrogen fertilizer with organic fertilizers mitigated soil acidification, increased soil pH and exchangeable base cation contents, and generally increased soil dissolved organic carbon content. Meanwhile, the organic fertilizer treatments reduced the contents of highly active aluminum fractions, including soluble and exchangeable aluminum, and promoted the formation of relatively stable fractions, including hydroxyl bound and amorphous aluminum. Increasing soil pH was the primary mechanism underlying the reduction in active aluminum. Dissolved organic carbon contributed to the formation of soluble monomeric organic aluminum, thereby reducing the content of monomeric inorganic aluminum, but it may also retain some aluminum in soluble organic complexes, thereby delaying the transformation of soluble aluminum into relatively stable solid phase aluminum fractions. Overall, commercial chicken manure and shrimp peptide organic fertilizer were more effective in ameliorating soil acidity and controlling aluminum fractions. Commercial chicken manure increased soil pH by 0.19 units and dissolved organic carbon content by 18.8%, while decreasing soluble and exchangeable aluminum contents by 48.5% and 70.5%, respectively. Shrimp peptide organic fertilizer increased soil pH by 0.25 units and decreased soluble and exchangeable aluminum contents by 45.6% and 69.9%, respectively. These findings provide a theoretical basis for screening organic fertilizers with high efficiency in controlling soil acidity and developing technologies for the coordinated regulation of soil acidification and aluminum toxicity risks in strongly acidic soils.

     

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