Biogeosciences, 14, 215–228, 2017 www.biogeosciences.net/14/215/2017/ doi:10.5194/bg-14-215-2017 © Author(s) 2017. CC Attribution 3.0 License. Biogeochemical constraints on the origin of methane in an alluvial aquifer: evidence for the upward migration of methane from underlying coal measures Charlotte P. Iverach1,2, Sabrina Beckmann3, Dioni I. Cendón1,2, Mike Manefield3, and Bryce F. J. Kelly1 1Connected Waters Initiative Research Centre, UNSW Australia, UNSW Sydney, NSW, 2052, Australia 2Australian Nuclear Science and Technology Organisation, New Illawarra Rd, Lucas Heights, NSW, 2234, Australia 3School of Biotechnology and Biomolecular Sciences, UNSW Australia, UNSW Sydney, NSW, 2052, Australia Correspondence to: Charlotte P. Iverach (
[email protected]) Received: 26 August 2016 – Published in Biogeosciences Discuss.: 5 September 2016 Revised: 12 December 2016 – Accepted: 24 December 2016 – Published: 17 January 2017 Abstract. Geochemical and microbiological indicators of 1 Introduction methane (CH4/ production, oxidation and migration pro- cesses in groundwater are important to understand when at- Interest in methane (CH4/ production and degradation pro- tributing sources of gas. The processes controlling the natural cesses in groundwater is driven by the global expansion of occurrence of CH4 in groundwater must be understood, es- unconventional-gas production. There is concern regarding pecially when considering the potential impacts of the global the potential impacts of gas and fluid movement, as well as expansion of coal seam gas (CSG) production on ground- depressurisation, on groundwater quality and quantity in ad- water quality and quantity. We use geochemical and micro- jacent aquifers used to support other industries (Atkins et al., biological data, along with measurements of CH4 isotopic 2015; Heilweil et al., 2015; Iverach et al., 2015; Moritz et al., 13 composition (δ C-CH4/, to determine the processes acting 2015; Owen et al., 2016; Zhang and Soeder, 2016).