Biogeochemical constraints on the origin of methane in an alluvial aquifer: Evidence for the upward migration of methane from underlying coal measures
- Publication Type:
- Journal Article
- Citation:
- Biogeosciences, 2017, 14 (1), pp. 215 - 228
- Issue Date:
- 2017-01-17
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Geochemical and microbiological indicators of methane (CH4) production, oxidation and migration processes in groundwater are important to understand when attributing sources of gas. The processes controlling the natural occurrence of CH4in groundwater must be understood, especially when considering the potential impacts of the global expansion of coal seam gas (CSG) production on groundwater quality and quantity. We use geochemical and microbiological data, along with measurements of CH4isotopic composition (δ13C-CH4), to determine the processes acting upon CH4in a freshwater alluvial aquifer that directly overlies coal measures targeted for CSG production in Australia. Measurements of CH4indicate that there is biogenic CH4in the aquifer; however, microbial data indicate that there are no methanogenic archaea in the groundwater. In addition, geochemical data, particularly the isotopes of dissolved inorganic carbon (DIC) and dissolved organic carbon (DOC), as well as the concentration of SO42-, indicate limited potential for methanogenesis in situ. Microbial community analysis also shows that aerobic oxidation of CH4occurs in the alluvial aquifer. The combination of microbiological and geochemical indicators suggests that the most likely source of CH4, where it was present in the freshwater aquifer, is the upward migration of CH4from the underlying coal measures.
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