24 / 2025-03-25 16:32:54
Effect of typical mineral in coal on biogenic coalbed methane production and the response of microbial community
Mineral,Coalbed methan,microbial community structure
摘要待审
Huan He / 中国矿业大学
Qian Zhang / China University of Mining and Technology
Xin Yin Huang / China University of Mining and Technology
Xiao Yu Li / China University of Mining and Technology
Bei Zhang / China University of Mining and Technology
Zai Xing Huang / China University of Mining and Technology
As the world's largest lignite resource holder, China holds significant potential for developing biogenic coalbed methane, yet the mechanistic impacts of inorganic mineral components on microbial methanogenesis remain poorly understood. This study systematically investigates the influence of three typical minerals (pyrite, kaolinite, and calcite) on coal bioconversion processes using density-segregated lignite samples (1.3–1.8 g/cm³) from Shaanxi Daliuta. Microbial consortia enriched from coalbed methane well drainage water were employed for bio-gasification experiments, combined with physicochemical characterization (proximate analysis, XRD, XRF, FTIR) , ELISA and high-throughput sequencing. Results demonstrated that ash and fixed carbon contents critically regulate CH4 production (p<0.05), with Fe, Ti, K, Ca, and Sr concentrations showing strong gas yield correlations. FTIR revealed density-dependent depletion of degradable functional groups (alkyl C-H, hydroxyl/amino, ether bonds). Microbial community analysis identified mineral-driven differentiation between low-ash (1.3–1.5 g/cm³) and high-ash (1.6–1.8 g/cm³) groups, particularly in sulfur-cycling taxa (Desulfobacterota, Geobacter) and methanogens (Methanofollis, p<0.05). Controlled mineral supplementation experiments showed pyrite enhanced volatile fatty acid accumulation (18.7–24.3%) and F420 activity (32.5–41.8%) but suppressed late-stage methanogenesis at >2% dosage, while kaolinite (optimal at 2%) and calcite (via pH modulation) boosted CH4 yields by 45.6%. Mineral-specific restructuring of drainage-derived microbial consortia was observed: pyrite enriched Firmicutes (48.2±3.5%) and Bacteroidota (22.7±2.1%), kaolinite elevated Desulfobacterota (31.4±2.8%), and calcite promoted Proteiniphilum (19.6±1.9%) and Geobacter (15.3±1.2%), with Geobacter's dominance across systems underscoring its role in extracellular electron transfer. These findings elucidate how reservoir-adapted microbial communities interact with mineralogical constraints to govern methanogenic efficiency, providing actionable insights for enhancing in situ coalbed methane recovery through biostimulation strategies.
重要日期
  • 会议日期

    06月10日

    2025

    06月13日

    2025

  • 04月15日 2025

    初稿截稿日期

主办单位
National Natural Science Foundation of China
Geobiology Society
National Committee of Stratigraphy of China
Ministry of Science and Technology
Geological Society of China
Paleontological Society of China
Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences (CAS)
Institute of Vertebrate Paleontology and Paleoanthropology, CAS
International Commission on Stratigraphy
International Paleontological Association
承办单位
State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences (CUG, Wuhan)
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