旱改水配施生物有机肥措施下滨海盐渍土微生物群落结构响应特征

Microbial Community Response to Dryland Conversion and Bio-organic Fertilizer Application in Coastal Saline Soils

  • 摘要:
    目的 明确水肥综合改良措施对滨海盐渍土基本性状的影响以及土壤微生物群落结构对改良的响应特征,为滨海地区盐渍土资源的高效利用和开发提供科学依据。
    方法 以天津滨海地区典型盐渍土为研究对象,设计旱田(CK)、旱改水田(W)和旱改水田配施生物有机肥(BW)三个处理,探究不同改良措施对土壤盐碱指标的调控效应,并分析土壤细菌群落结构对环境因子变化的响应特征。
    结果 相较于CK处理,BW处理显著降低土壤电导率(EC)和pH(分别下降4.1%和5.8%),提高了土壤有机碳和速效磷含量(增幅分别为17.2%和17.9%)、土壤脲酶及碱性磷酸酶活性(分别提升25.8%和126%)。BW处理显著增加细菌丰富度,促进酸杆菌门(Acidobacteriota)(相对丰度提升39%)和芽单胞菌门(Gemmatimonadota)等有益菌群富集。功能预测表明BW处理显著提升了脱硫叠球菌科(Desulfosarcinaceae)、硫酸盐还原菌(Desulfocapsaceae)等硫氮转化相关菌群的丰度水平。
    结论 旱改水配施有机肥处理通过降低土壤pH和EC,提高有机碳及速效磷等养分含量,改善滨海盐渍土壤环境,优化土壤氮硫养分转化相关菌群结构,增强生态功能,是可行的盐渍土微生态修复途径。

     

    Abstract:
    Objective The aims were to clarify the response characteristics of comprehensive water-fertilizer improvement measures to basic properties of coastal saline soil and soil microbial community structure, in order to provide a scientific basis for the efficient utilization and development of saline soil resources in coastal areas.
    Method the typical saline soil in Tianjin coastal area was taken as the research object, and three treatments of dry field (CK), dry modified paddy field (W) and dry modified paddy field combined with bio-organic fertilizer (BW) were designed. The effects of different treatments on salt reduction and alkali regulation of coastal saline soil, and the response characteristics of soil bacterial community to environmental changes were analyzed.
    Result Compared with CK, the BW treatment significantly reduced soil EC and pH (by 4.1% and 5.8%, respectively), increased soil organic carbon and available phosphorus content (by 17.2% and 17.9%, respectively), and enhanced soil urease and alkaline phosphatase activities (by 25.8% and 126%, respectively). The BW treatment also significantly increased bacterial richness and promoted the enrichment of beneficial bacterial groups such as Acidobacteriota (relative abundance increased by 39%) and Gemmatimonadota. Functional prediction revealed that the BW treatment significantly enhanced the abundance of microbial taxa involved in sulfur and nitrogen cycling, such as Desulfosarcinaceae and Desulfocapsaceae.
    Conclusion The combination of converting dryland to paddy field with bio-organic fertilizer application improved the coastal saline soil environment by reducing soil pH and EC, increasing nutrient contents such as organic carbon and available phosphorus, optimizing microbial communities associated with nitrogen and sulfur transformation, and enhancing ecological functions. This approach represents a viable strategy for microecological restoration of saline soils.

     

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