基于微生物矿化的生态修复措施下边坡土壤理化特性与微生物群落的协同演变研究

The synergistic evolution of soil physicochemical properties and microbial communities in slope soils with the ecological restoration measures based on Microbially Induced Carbonate Precipitation

  • 摘要: 本研究聚焦于基于微生物矿化的生态修复措施对边坡土壤的影响, 重点解析了土壤理化性质与微生物群落的协同演变机制。研究发现, 该生态修复措施(XF)显著改善了土壤理化特性, 与对照组相比, 土壤pH由4.30升至5.20, 有机质含量由8.06 g·kg−1增至15.67 g·kg−1, 全氮由0.32 g·kg−1增至0.53 g·kg−1, 碱解氮由24.37 mg·kg−1增至43.60 mg·kg−1, 有效磷由0.27 mg·kg−1增至15.88 mg·kg−1, 速效钾由70.00 mg·kg−1增至110.67 mg·kg−1, 土壤肥力状况显著提高。α多样性指数显示, XF组微生物群落物种丰富度与均匀度更高, 且β多样性分析进一步证实XF组与对照组微生物群落组成存在显著差异。在微生物群落组成方面, XF组中放线菌门(Actinobacteriota)、γ-变形菌纲(γ-Proteobacteria)、蓝细菌门(Cyanobacteria)和拟杆菌门(Bacteroidota)等呈富集态势。其中, 慢生根瘤菌属(Bradyrhizobium)、伯克霍尔德氏菌-卡巴莱罗尼亚菌-副伯克霍尔德氏菌(Burkholderia-Caballeronia-Paraburkholderia)菌群、中华单胞菌属(Sinomonas)等有益微生物的相对丰度显著增加, 进而增强了有机物分解和碳氮养分循环功能。相比之下, 对照组以绿弯菌门(Chloroflexi)和酸杆菌门(Acidobacteriota)等维持土壤基础功能的土著微生物为主。通过基于距离的冗余分析(distance-based redundancy analysis, db-RDA), 确定有效磷为最关键环境因子, 其解释度高达98.34%。物种与环境因子相关性分析显示, 未分类的B12-WMSP1目下的属与碱解氮呈显著负相关, 分枝杆菌属(Mycobacterium)与碱解氮和有机质含量均呈极显著正相关, JG30-KF-CM45科下未分类属与有效磷呈显著正相关。这些发现阐明了该生态修复措施下边坡土壤理化特性与微生物群落的协同演变规律, 为边坡生态修复工程提供了重要的理论依据与实践指导, 对推动生态修复技术的优化和应用具有重要意义。

     

    Abstract: This study focuses on the impact of ecological restoration measures based on microbial mineralization on slope soils, with an emphasis on elucidating the synergistic evolution mechanisms between soil physicochemical properties and microbial communities. The findings reveal that the ecological restoration measures (XF) significantly improved soil physicochemical characteristics. Compared to the control group, soil pH increased from 4.30 to 5.20, organic matter content rose from 8.06 to 15.67 g·kg−1, total nitrogen increased from 0.32 to 0.53 g·kg−1, available nitrogen increased from 24.37 to 43.60 mg·kg−1, available phosphorus increased from 0.27 to 15.88 mg·kg−1, and available potassium increased from 70.00 to 110.67 mg·kg−1, indicating a significant enhancement in soil fertility. Alpha diversity indices demonstrated that the XF treatment resulted in higher species richness and evenness in the microbial community, and beta diversity analysis further confirmed significant differences in microbial community composition between the XF and control treatments. In terms of microbial community composition, the XF treatment showed enrichment of Actinobacteriota, γ-Proteobacteria, Cyanobacteria, and Bacteroidota. Notably, the relative abundance of beneficial microorganisms such as Bradyrhizobium, Burkholderia-Caballeronia-Paraburkholderia, and Sinomonas significantly increased, thereby enhancing organic matter decomposition and carbon-nitrogen nutrient cycling functions. In contrast, the control group was dominated by indigenous microorganisms, such as Chloroflexi and Acidobacteriota, which maintain basic soil functions. The available phosphorus was determined as the most crucial environmental factor through distance-based redundancy analysis (db-RDA), with an explanatory power as high as 98.34%. Correlation analysis between species and environmental factors revealed that unclassified genera under the B12-WMSP1 order were significantly negatively correlated with available nitrogen, while Mycobacterium showed highly significant positive correlations with available nitrogen and organic matter content. Unclassified genera under the JG30-KF-CM45 family were significantly positively correlated with available phosphorus. These findings elucidate the synergistic evolution patterns of soil physicochemical properties and microbial communities under the ecological restoration measures, providing important theoretical foundations and practical guidance for slope ecological restoration projects. This study holds significant implications for advancing the optimization and application of ecological restoration technologies.

     

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