高岭石强化煤厌氧发酵产甲烷实验研究

    Experimental study on methane production in anaerobic fermentation of coal enhanced by kaolinite

    • 摘要: 强化煤制微生物甲烷技术是实现煤层气高效增产的有效措施。为进一步拓展其强化手段,探究高岭石强化煤厌氧发酵产气的潜力及促进机制,以长焰煤为底物构建厌氧发酵系统,通过对生物甲烷产量、发酵前后残煤表面官能团、中间关键液相产物、微生物群落结构以及产甲烷代谢路径等进行测试和分析,探讨了高岭石对煤厌氧发酵产甲烷的促进效应。结果表明:在以煤为底物的厌氧发酵系统中添加质量分数0.5%的高岭石,可有效强化整个厌氧发酵过程,提高甲烷的阶段产气量及累计产量;添加高岭石后,残煤表面的羰基碳(C=O)、羧基碳(COO−)相对质量分数分别下降48.95%、46.26%,说明高岭石有效促进了微生物对煤的降解;从厌氧发酵初期到产气高峰期,在添加高岭石的系统中,细菌群落的水解菌群和产氢产乙酸菌群活性增强,提高了复杂有机物的水解效率并为产甲烷菌群提供了更充足的底物及营养物质;高岭石层间缝隙能缓解溶液中挥发性脂肪酸的积累,为产甲烷菌提供更稳定安全的代谢环境,使产气高峰期溶液pH值升高、屠场杆状菌属(Macellibacteroides)活性增强;氢营养型产甲烷的甲烷杆菌属(Methanobacterium)能够获得更充足的二氧化碳和氢气作为底物,其活性得到增强;在乙酸营养型为主的对照组中,二氧化碳和氢气的利用率低,但在添加高岭石后,这些底物能够被甲烷菌更充分地利用,从而显著提高了甲烷的产量。

       

      Abstract: Enhancing microbial methane production from coal is an effective way to increase production of coalbed methane. In order to expand its strengthening means and explore the potential of kaolinite-enhanced anaerobic fermentation of coal gas production and its promoting mechanism, an anaerobic fermentation system was constructed with long-flame coal as the substrate. By testing and analyzing biomethane gas production, surface functional groups of residual coal before and after fermentation, intermediate key liquid phase products, microbial community structure and methanogenic metabolic pathway, the promoting effect of kaolinite on methane produced by anaerobic fermentation was investigated. The results show that adding kaolinite with a mass fraction of 0.5% to the coal-based anaerobic fermentation system can effectively strengthen the entire anaerobic fermentation process and improve the staged and cumulative methane production. The relative mass fraction of carbonyl carbon (C=O) and carboxyl carbon (COO−) on the surface of the residual coal decreased by 48.95% and 46.26%, respectively, after the addition of kaolinite, indicating that kaolinite effectively promoted the degradation of coal by microorganisms. From the early stage of anaerobic fermentation to the peak of gas production, the activities of hydrolytic bacteria and hydroacetic acid bacteria in the bacterial community in the kaolinite system were enhanced, which improved the hydrolysis efficiency of complex organic compounds in the early stage and provided more adequate substrates and nutrients for methanogenic bacteria. The gap between the layers of kaolinite can ease the accumulation of volatile fatty acids in the solution and provide a more stable and safe metabolic environment for methanogens. During the peak period of gas production, the pH value in the solution increases and Macellibacteroides is more active in the kaolinite group. The hydrogenotrophic methanogenic Methanobacterium gained more sufficient carbon dioxide and hydrogen as substrates, enhancing their activity. In the acetate-utilizing control group, the utilization efficiency of carbon dioxide and hydrogen was relatively low. However, after the addition of kaolinite, these substrates were more efficiently utilized by the methanogens, leading to a significant increase in methane production.

       

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