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 abundance 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)、施无机肥(NPK)、施有机肥(OM)及有机肥无机肥配施(NPKOM) 4种处理, 通过测定土壤金属含量及细菌、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: 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处理显著提高了土壤Mg、Ca含量, 而降低了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 significantly alters soil chemical properties, and these changes in turn influence soil metal content and distribution. The levels and patterns of soil metals directly affect soil health, plant growth and ecosystem balance. To investigate the effects of heavy metals on the abundance of bacteria, fungi and protists in dryland red soil under different fertilization treatments, the present study was based on the long-term fertilization plot for dryland red soil at the Red Soil Research Institute in Jinxian County, Nanchang City, Jiangxi Province, and set up four treatments: no fertilization (CK), inorganic fertilizer (NPK), organic fertilizer (OM), and organic and inorganic mixed application (NPKOM). By measuring the heavy metal content and chemical properties of the soil and the abundance of bacteria, fungi and protists, and combined with the correlation analysis to reveal the key metals affecting the abundance of bacteria, fungi and protists under different fertilization treatments. The correlation analysis was used to reveal the key metal elements and their mechanisms of action that affect the abundance of bacteria, fungi and protists under different fertilization treatments. The results showed that: compared to no fertilization (CK), organic fertilizer (OM) and organic-inorganic (NPKOM) treatments significantly increased the abundance of bacteria, fungi, and protists, whereas the inorganic fertilizer (NPK) treatment only increased the abundance of bacteria and fungi and had no significant effect on the abundance of protists. In addition, compared to no fertilization (CK), the organic fertilizer (OM) and organic-inorganic (NPKOM) treatments significantly increased the content of Mg and Ca elements in the soil, while decreased the content of Al and Fe. Further correlation analysis revealed that the abundance of protists was significantly positively correlated with soil pH, organic carbon, total phosphorus, Mg and Ca content, and negatively correlated with soil Al and Fe content. Further correlation analysis revealed that the abundance of bacteria, fungi and protists was significantly positively correlated with soil total phosphorus, total nitrogen, organic matter, available potassium, available phosphorus, dissolved organic carbon, nitrate nitrogen and ammonium nitrogen. Simultaneously, the abundance of bacteria and protists showed significant positive correlations with soil Mg and Ca content, while exhibiting significant negative correlations with soil Al and Fe content. This difference can be attributed to the fact that organic fertilizer additions may reduce the Al and Fe content by inducing the formation of organic iron aluminum composite, providing more habitats and nutrient supply for microorganisms, which in turn promotes the abundance of bacteria, fungi and protist; whereas organic fertilizer additions indirectly increased the metabolic efficiency and surface attachment sites of microorganisms by increasing the Ca and Mg content, which ultimately led to an increase in the abundance of bacteria, fungi and protist. In conclusion, In conclusion, the application of organic fertilizers can increase the abundance of bacteria, fungi and protist by decreasing the content of Al and Fe, and increasing the content of Mg and Ca. The results of this study can provide an important theoretical basis for optimizing the fertilization strategy of dryland red soil and elucidate the response mechanisms of soil microorganisms to metal elements.

     

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