Assessing connectivity between an overlying aquifer and a coal seam gas resource using methane isotopes, dissolved organic carbon and tritium

dc.contributor.authorIverach, CPen_AU
dc.contributor.authorCendón, DIen_AU
dc.contributor.authorHankin, SIen_AU
dc.contributor.authorLowry, Den_AU
dc.contributor.authorFisher, REen_AU
dc.contributor.authorFrance, JLen_AU
dc.contributor.authorNisbet, EGen_AU
dc.contributor.authorBaker, AAen_AU
dc.contributor.authorKelly, BFJen_AU
dc.date.accessioned2022-10-25T01:42:29Zen_AU
dc.date.available2022-10-25T01:42:29Zen_AU
dc.date.issued2015-11-03en_AU
dc.date.statistics2022-01-11en_AU
dc.description.abstractCoal seam gas (CSG) production can have an impact on groundwater quality and quantity in adjacent or overlying aquifers. To assess this impact we need to determine the background groundwater chemistry and to map geological pathways of hydraulic connectivity between aquifers. In south-east Queensland (Qld), Australia, a globally important CSG exploration and production province, we mapped hydraulic connectivity between the Walloon Coal Measures (WCM, the target formation for gas production) and the overlying Condamine River Alluvial Aquifer (CRAA), using groundwater methane (CH4) concentration and isotopic composition (δ13C-CH4), groundwater tritium (3H) and dissolved organic carbon (DOC) concentration. A continuous mobile CH4 survey adjacent to CSG developments was used to determine the source signature of CH4 derived from the WCM. Trends in groundwater δ13C-CH4 versus CH4 concentration, in association with DOC concentration and 3H analysis, identify locations where CH4 in the groundwater of the CRAA most likely originates from the WCM. The methodology is widely applicable in unconventional gas development regions worldwide for providing an early indicator of geological pathways of hydraulic connectivity. © The Authors.en_AU
dc.identifier.citationIverach, C. P., Cendon, D. I., Hankin, S. I., Lowry, D., Fisher, R. E., France, J. L., Nisbet, E. G., Baker, A., & Kelly, B. F. J. (2015). Assessing connectivity between an overlying aquifer and a coal seam gas resource using methane isotopes, dissolved organic carbon and tritium. Paper presented at the Australian Groundwater Conference, The Shine Dome, Canberra, Australia, 3-5 November 2015, (pp. 197). Retrieved from: https://www.groundwater.com.au/media/W1siZiIsIjIwMTgvMDcvMzEvMDNfNDNfMDBfNzk5X0FHQzIwMTVfQWJzdHJhY3RfYm9va2xldC5wZGYiXV0/AGC2015%20Abstract%20booklet.pdfen_AU
dc.identifier.conferenceenddate5 November 2015en_AU
dc.identifier.conferencenameAustralian Groundwater Conferenceen_AU
dc.identifier.conferenceplaceCanberra, Australiaen_AU
dc.identifier.conferencestartdate3 November 2015en_AU
dc.identifier.urihttps://www.groundwater.com.au/media/W1siZiIsIjIwMTgvMDcvMzEvMDNfNDNfMDBfNzk5X0FHQzIwMTVfQWJzdHJhY3RfYm9va2xldC5wZGYiXV0/AGC2015%20Abstract%20booklet.pdfen_AU
dc.identifier.urihttps://apo.ansto.gov.au/dspace/handle/10238/13921en_AU
dc.language.isoenen_AU
dc.publisherNational Centre for Groundwater Research And Trainingen_AU
dc.subjectAquifersen_AU
dc.subjectCoal seamsen_AU
dc.subjectIsotopesen_AU
dc.subjectMethaneen_AU
dc.subjectCarbonen_AU
dc.subjectTritiumen_AU
dc.subjectQueenslanden_AU
dc.subjectAustraliaen_AU
dc.subjectCarbon 14en_AU
dc.subjectGasesen_AU
dc.subjectGeochemistryen_AU
dc.subjectGround wateren_AU
dc.titleAssessing connectivity between an overlying aquifer and a coal seam gas resource using methane isotopes, dissolved organic carbon and tritiumen_AU
dc.typeConference Abstracten_AU
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