不同施肥处理下旱地红壤金属元素对细菌、真菌及原生生物丰度的影响

Effects of metals on the abundances of bacteria, fungi, and protists in dryland red soil under different fertilization treatments

  • 摘要: 土壤金属含量和形态直接影响土壤健康、植物生长和生态系统的平衡。为探究不同施肥处理下旱地红壤金属对细菌、真菌及原生生物丰度的影响, 本研究基于旱地红壤长期施肥定位试验, 设置不施肥(CK)、施化肥(NPK)、施有机肥(OM)及化肥和有机肥混合施用(NPKOM) 4种处理, 通过测定土壤化学性质、金属含量及细菌、真菌和原生生物的丰度, 结合相关性分析揭示不同施肥处理下影响细菌、真菌及原生生物丰度的关键金属元素及其作用机制。结果表明: 与CK处理相比, OM和NPKOM处理显著提高了细菌、真菌及原生生物的丰度, 而NPK处理仅增加细菌和真菌的丰度, 对原生生物丰度无显著影响。此外, OM和NPKOM处理显著提高了土壤Mg、Ca含量, 降低了Al、Fe含量。相关性分析表明, 原生生物丰度与土壤pH及有机碳、全磷、Mg和Ca含量呈显著正相关, 而与土壤Al、Fe含量呈显著负相关。这种差异可归因于有机肥的添加可能通过促使Al3+和Fe3+形成有机-铁铝复合物导致Al、Fe含量降低, 为微生物提供更多栖息地与养分, 或通过提高Ca、Mg含量增加了微生物的代谢效率及附着位点, 进而增加细菌、真菌及原生生物的丰度。综上, 施用有机肥可以通过降低Al、Fe及增加Mg、Ca含量, 进而增加细菌、真菌及原生生物的丰度。研究结果可为优化旱地红壤施肥策略提供重要理论依据。

     

    Abstract: Fertilization can cause significant alterations in the chemical properties of soil, with these changes in turn influencing soil metal content and distribution. Moreover, the levels and patterns of these metals can have a direct influence on soil health, plant growth, and ecosystem balance. In this study, performed at the Red Soil Research Institute in Jinxian County, Nanchang City, Jiangxi Province, we investigated the effects of heavy metals on the abundances of bacteria, fungi, and protists in a long-term fertilization plot for dryland red soil, in which we set up the following four treatments: no fertilization, application of chemical fertilizer, application of organic fertilizer, and combined application of chemical and organic fertilizers. By measuring the chemical properties and the contents of heavy metals in soil and the abundances of bacteria, fungi and protists, and performing correlation analysis, we sought to identify the key metals influencing the abundance of these organisms under different fertilization treatments, and the associated mechanisms of action. The results revealed that compared with no fertilization, organic fertilizer and combined chemical and organic fertilizer treatments significantly increased the abundances of bacteria, fungi, and protists, whereas the chemical fertilizer treatment only increased the abundances of bacteria and fungi, it had no significant effects on that of protists. In addition, compared with no fertilization, the organic fertilizer and combined chemical and organic fertilizer treatments significantly increased the contents of Mg and Ca elements in the soil, while reduced the contents of Al and Fe. Further correlation analysis revealed that the abundance of protists was significantly positively correlated with soil pH, and contents of organic carbon, total phosphorus, and Mg and Ca, and negatively correlated with soil Al and Fe contents. Correlation analysis also revealed that the abundances of bacteria, fungi, and protists were significantly positively correlated with soil total phosphorus, total nitrogen, organic matter, available potassium, available phosphorus, dissolved organic carbon, nitrate nitrogen, and ammonium nitrogen contents. Our findings indicated that the abundances of bacteria and protists were significantly positively correlated with soil Mg and Ca contents. However, their abundances were significantly negatively correlated with soil Al and Fe contents, which could be attributed to the fact that the addition of organic fertilizer may cause reductions in the Al and Fe contents of soil by inducing the formation of organic iron-aluminum composites. This would accordingly provide a greater range of habitats and more abundant nutrient supply for microorganisms, which in turn would promote increases in the abundances of bacteria, fungi and protists, whereas by promoting increases in the contents of Ca and Mg. The addition of organic fertilizer may indirectly enhance the metabolic efficiency and surface attachment sites of microorganisms, ultimately leading to increases in the abundances of bacteria, fungi, and protists. In conclusion, by contributing to reductions in the contents of Al and Fe, and increasing the contents of Mg and Ca, the application of organic fertilizers can increase the abundances of bacteria, fungi and protists. Our findings in this study provides an important theoretical basis for optimizing fertilization strategies for dryland red soil and contribute to elucidating the response mechanisms of soil microorganisms to metal elements.

     

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