Isotope and chemical alteration of coalbed gases during migration from underground coal mine into the atmosphere
Publication date
2026-01-13
Authors
Bezyk, Yaroslav
Szurgacz, Dawid
Górka, Maciej
Strąpoć, Dariusz
Kruszewski, Łukasz
Wachniew, Przemysław
Nęcki, Jarosław
Zimnoch, Miroslaw
Sówka, Izabela
Modelska, Magdalena
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Advisors
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Document Type
Article
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Abstract
Methane release into mine workings and the atmosphere poses a serious environmental and safety risks. This study examines the composition and stable isotope geochemistry of coalbed methane in a hard coal mine of the Upper Silesian Coal Basin (Poland), with emphasis on gas migration pathways from the coal seam through mine workings and ventilation shaft to the atmosphere. Methane concentrations decrease progressively with distance from the active excavation zone toward the exhaust shaft. In addition to CH4 and CO2, the coalbed gas contained notable amounts of nitrogen heterocyclic compounds, sulfur-bearing species, and chlorinated gases, depending on the sampling location and temporal window. Geochemical results reveal a strong link between gas migration and isotopic variability in the underground environment. Zones of methane accumulation, commonly associated with bends in return airways, showed enrichment in 13C, consistent with diffusive fractionation. Variations in CH4 and corresponding isotope effects during coal transport indicate multiple gas origins within the coal seam. Isotope signatures point to predominantly thermogenic CH4 at the active mining level, whereas 13C-depleted methane at the exploited and flooded levels suggests secondary microbial generation. The microbial contribution is likely promoted by infiltrating meteoric waters supplying nutrients for methanogenic archaea, as supported by δ2H, δ18O signatures of mine water, and measurable tritium activity. The absence of enriched δ13C values in CO2 and dissolved inorganic carbon (DIC) further implies mixed thermogenic-microbial gas origin in abandoned mine workings. These findings highlight the combined influence of mining operations, diffusion-desorption processes, microbial activity, and gas mixing on the molecular and isotope composition of coalbed gases transported toward the exhaust shaft. Moreover, isotopic data from downwind emission plumes demonstrate the value of integrating underground measurements with atmospheric observations to trace and quantify methane emissions from coal mining operations.
Keywords
Coal mine methane, Emission plume, Isotope composition, Trace compounds, Upper Silesian Coal basin, Fuel Technology, Geology, Economic Geology, Stratigraphy
Citation
Bezyk, Y, Szurgacz, D, Górka, M, Strąpoć, D, Kruszewski, Ł, Wachniew, P, Nęcki, J, Zimnoch, M, Sówka, I, Modelska, M, Wołkowicz, W, van der Veen, C & Röckmann, T 2026, 'Isotope and chemical alteration of coalbed gases during migration from underground coal mine into the atmosphere', International Journal of Coal Geology, vol. 313, 104922. https://doi.org/10.1016/j.coal.2025.104922