煤厌氧发酵过程中固液气三相物质演化规律

Evolution regularities of solid, liquid and gas phases during coal anaerobic fermentation

  • 摘要: 煤厌氧发酵技术是通过本/异源微生物降解煤有机质定向转化为甲烷、氢气等清洁能源,其核心科学问题在于揭示“煤结构演化−代谢物质传递−微生物群落响应”的多尺度协同作用机制。系统综述了煤厌氧发酵过程中固液气的演化规律,建立了煤厌氧发酵过程中固液气成分联合表征技术体系。固相成分分析包括煤预处理、孔隙结构和分子结构及其模型构建技术等,不同的预处理技术在实验室条件下能够显著提升生物甲烷产量,增幅范围达到24.98%~2 430.00%,但复杂的地质条件下的原位效应需进一步验证。煤储层孔隙系统作为微生物与煤基质界面反应的拓扑载体,其结构特征在厌氧微生物活动的影响下发生显著变化,微孔占比降低12.38%,而中孔和大孔占比分别增大15.84%和352.89%,孔隙度和渗透率增幅分别达到4.73%~64.9%和33.3%~40.0%。煤分子结构表征及模型构建技术研究为生物气化过程中煤表面官能团、碳骨架和化学键断裂位置提供了直接证据。微生物降解作用导致煤中范德华能降低幅度最大,达到8.74%~9.27%,其次是非共价键能和氢键能。液相成分分析主要包括分子生物学和中间代谢物质分析,分子生物学通过分析煤层微生物的多样性特征及其代谢潜力,突破了对本源微生物生命活动的认知瓶颈,为生物甲烷生成路径研究提供新途径,而中间代谢物质(如溶解性有机质、小分子有机酸和糖类等)的表征为代谢产物传递研究提供了重要的数据支撑。甲烷、氢气、二氧化碳等气相组分的定量表征有助于理解生物气化潜力及甲烷生成途径分析,未来可着重突破多场耦合作用机制解析、代谢网络工程改造及动态环境调控等关键技术,为实现煤层气资源的智能化生物转化与工业化应用提供理论支撑。

     

    Abstract: Coal anaerobic fermentation technology utilizes indigenous or exogenous microorganisms to degrade coal organic matter, converting it into clean energy sources such as methane and hydrogen. The core scientific challenge lies in elucidating the multi-scale synergistic mechanisms involving coal structure evolution, metabolite transfer, and microbial community response. This study systematically reviews the evolution law of solid, liquid, and gas during coal anaerobic fermentation and establishes a joint characterization and analysis technology system for the components of coal anaerobic fermentation. The analysis of solid phase components encompasses coal pretreatment, pore structure, molecular structure, and model construction techniques, and different pretreatment techniques have been shown to significantly increase biomethane production under laboratory conditions, ranging from 24.98% to 2430%, but the in-situ effect under complex geological conditions needs to be further verified. As the primary medium for interfacial reactions between microorganisms and the coal matrix, the structural characteristics of the coal reservoir pore system undergo significant changes under anaerobic microbial activity. Specifically, the proportion of micropores decreases by 12.38%, whereas the proportions of mesopores and macropores increase by 15.84% and 352.89%, respectively. Porosity and permeability also exhibit notable increases, ranging from 4.73% to 64.9% and 33.3% to 40.0%, respectively. The research on the characterization of coal molecular structure and model construction techniques has provided direct evidence for the functional groups on the surface of coal, the carbon skeleton, and the positions of chemical bond breakage during the process of biogasification. Microbial degradation was found to reduce Van der Waals energy by 8.74% to 9.27%, followed by decreases in non-covalent bond energy and hydrogen bond energy. Liquid phase component analysis primarily encompasses molecular biology and intermediate metabolite analysis. Molecular biology overcomes the cognitive bottleneck of the life activities of native microorganisms by analysing the diversity characteristics and metabolic potential of coal seam microorganisms, thereby providing a new approach for the study of biological methane generation pathways. Meanwhile, the characterization of intermediate metabolites, such as Dissolved organic matter, low-molecular-weight organic acids, and sugars, offers significant data support for the research on the transmission of metabolites. Furthermore, the quantitative characterization of gas phase components such as methane, hydrogen, and carbon dioxide facilitates the understanding of biogasification potential and methane generation pathway. Future research should prioritize breakthroughs in key technologies, including multi-field coupling mechanism analysis, metabolic network engineering, and dynamic environmental regulation, in order to provide robust theoretical support for the intelligent bioconversion and industrial application of CBM resources.

     

/

返回文章
返回