高级检索

采煤沉陷区自然恢复驱动下农田土壤微生物固碳潜力演变特征

Evolution of microbial carbon sequestration potential in farmland soil driven by natural restoration in coal mine subsidence area

  • 摘要: 在全球碳中和目标的大背景下,土壤固碳作为陆地生态系统碳循环的关键环节,其研究备受关注。采煤沉陷区作为典型的人为干扰生态系统,土壤结构破坏、肥力下降及微生物群落失衡等问题突出。近年来,针对采煤沉陷区人工修复对土壤固碳潜力和菌群结构的影响已被广泛关注,但自然恢复过程中农田土壤微生物固碳潜力的演变特征尚不清楚。为此,研究以采煤沉陷区为研究对象,系统采集不同自然恢复时间的采煤塌陷区农田土壤样品,综合运用高通量测序技术、结构方程模型和分子生态网络分析等方法,分析固碳菌群结构动态变化规律及其与土壤固碳潜力的内在联系。研究结果表明,自然恢复可帮助采煤沉陷区农田土壤理化性质和酶活性的有效恢复,自然恢复过程中农田土壤的固碳潜力主要受变形菌门(Proteobacteria)和酸杆菌门(Acidobacteria)控制。农田土壤受损程度随着自然恢复时间不断缓解,pH和有机质(SOM)含量的变化调控了过氧化氢酶(CAT)和β-葡糖苷酶(BG)活性,从而干预了ProteobacteriaAcidobacteria中的固碳基因丰度,进而影响了农田土壤固碳潜力。与未塌陷土壤相比,自然恢复初期,固碳菌群与环境因子的互作网络相对简单,生态系统稳定性较弱;而随着恢复进程推进,土壤受损程度不断缓解,网络中的节点数量显著增加,节点间的连接更加紧密,垂构连通度和聚类系数持续升高,表明生态系统的复杂性和稳定性逐步增强。研究首次系统揭示了采煤沉陷区自然恢复过程中农田土壤固碳潜力的演变特征及调控机制,为全面评估自然恢复的生态效益提供了新视角。研究结果不仅丰富了采煤沉陷区生态修复领域的理论基础,也为我国碳中和目标的实现提供了科学依据,对指导采煤沉陷区土地资源可持续利用和生态环境修复提供了参考。

     

    Abstract: Under the global goal of carbon neutrality, soil carbon sequestration—as a critical component of the terrestrial ecosystem carbon cycle—has garnered significant attention. Coal mining subsidence areas, as typical human-impacted ecosystems, are characterized by soil structural degradation, reduced fertility, and imbalances in microbial communities. Although the effects of artificial restoration on soil carbon sequestration potential and microbial community structure in these areas have been extensively studied, the evolutionary characteristics of soil microbial carbon sequestration potential during natural recovery remain poorly understood. To address this knowledge gap, this study selected coal mining subsidence areas as the research object and systematically collected soil samples from farmlands at various stages of natural recovery. High-throughput sequencing technology, structural equation modeling, and molecular ecological network analysis were comprehensively applied to investigate the dynamic changes in carbon-sequestering microbial community structures and their intrinsic relationships with soil carbon sequestration potential. Results indicated that natural recovery effectively restored the physicochemical properties and enzyme activities of farmland soils in coal mining subsidence areas. During the recovery process, the soil carbon sequestration potential was primarily influenced by Proteobacteria and Acidobacteria. As natural recovery progressed and soil damage gradually diminished, variations in pH and soil organic matter (SOM) content regulated the activities of catalase (CAT) and β-glucosidase (BG), thereby affecting the abundance of carbon sequestration-related genes in Proteobacteria and Acidobacteria, which in turn influenced the overall carbon sequestration potential. At the early stage of natural recovery, the interaction network between microbial communities involved in carbon sequestration and environmental factors was relatively simple, indicating low ecosystem stability. However, as recovery advanced, the complexity and stability of the system increased, evidenced by a growing number of network nodes, stronger inter-node connections, and higher vertical connectivity and clustering coefficients. This study, for the first time, systematically elucidated the evolutionary patterns and regulatory mechanisms of soil carbon sequestration potential in farmland soils during the natural recovery of coal mining subsidence areas. These findings provide new insights into the comprehensive evaluation of ecological benefits associated with natural recovery processes. The results not only enrich the theoretical foundation of ecological restoration in coal mining subsidence areas but also offer crucial scientific support for achieving China's carbon neutrality goals. Furthermore, they hold significant practical value for guiding sustainable land use and ecological restoration efforts in such regions.

     

/

返回文章
返回