Quantifying recharge to the Pilliga Sandstone aquifer, Great Artesian Basin Australia: learnings from combining 14C, 36Cl and 81Kr

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dc.contributor.authorSucknow, AOen_AU
dc.contributor.authorRaiber, Men_AU
dc.contributor.authorDeslandes, Aen_AU
dc.contributor.authorGerber, Cen_AU
dc.contributor.authorMartinez, Jen_AU
dc.contributor.authorYang, GMen_AU
dc.contributor.authorJiang, Wen_AU
dc.contributor.authorMeredith, KTen_AU
dc.date.accessioned2023-11-17T04:00:42Zen_AU
dc.date.available2023-11-17T04:00:42Zen_AU
dc.date.issued2022-07-12en_AU
dc.date.statistics2023-03-30en_AU
dc.description.abstractThe Pilliga Sandstone in the Coonamble Embayment in New South Wales, Australia, is part of the Great Artesian Basin (GAB), an aquifer system that underlies 22% of the Australian continent and is one of the main freshwater resources of inland Australia. Despite its significance, groundwater recharge to the Pilliga Sandstone is insufficiently constrained. Better quantifying recharge is particularly important because of competing interests between agriculture and other industries. The petroleum industry proposes to extract coal seam gas from the Gunnedah Basin underlying the Pilliga Sandstone. Groundwater flow in the Pilliga Sandstone is from the outcrops in the East (light blue in the Figure) to the West. Here we present results of a multi-tracer study (hydrochemistry, 2H, 3H, 3He/4He, 13C, 18O, 14C, 36Cl, 40Ar/36Ar, 85Kr, 81Kr, 87Sr/86Sr and noble gases) that were complemented in the northern part of the project area by geophysical investigations (seismic and ground-based electromagnetics). The project area shows a distinct southern flow path (Figure) for which groundwater velocity and therefore recharge could be quantified using 14C and 36Cl, where the rates were further improved by 81Kr. In the northern area the application of 14C and 36Cl was unsuccessful because of an admixture of waters from the underlying Gunnedah Basin. Groundwaters in that basin, containing the formations targeted for the CSG exploration, show very high total dissolved inorganic carbon (up to 300mMol/L) and chloride concentrations (up to 2000mg/L). Further groundwater from the Gunnedah Basin and intermediate layers to the Pilliga Sandstone has 40Ar/36Ar ratios up to 432, the highest values found in Australian groundwater so far, probably indicating partial release from old sediments by intruding dykes as indicated by a correlation with 3He/4He. Small volumes of admixtures of this water discharge into the Pilliga Sandstone and overprint the age information of the 14C and 36Cl values. Given the success of 81Kr in constraining flow rates for the southern flow path, there is great potential for 81Kr to also improve flow rate estimates in the northern flow area, but access to bores at intermediate distances of the northern flow path have to-date been denied.en_AU
dc.identifier.citationSucknow, A. O., Raiber, M., Deslandes, A., Gerber, C., Martinez, G., Yang, G.-M., Jiang, W., & Meredith, K. (2022). Quantifying recharge to the Pilliga Sandstone aquifer, Great Artesian Basin Australia: learnings from combining 14C, 36Cl and 81Kr. Poster presented to 2022 Goldschmidt Conference, 10-15 July, 2022, Honolulu, Hawaii, USA and Online. Retrieved from: https://conf.goldschmidt.info/goldschmidt/2022/meetingapp.cgi/Paper/10724en_AU
dc.identifier.conferenceenddate2022-07-15en_AU
dc.identifier.conferencename2022 Goldschmidt Conferenceen_AU
dc.identifier.conferenceplaceHonolulu, Hawaii & Onineen_AU
dc.identifier.conferencestartdate2022-07-10en_AU
dc.identifier.urihttps://conf.goldschmidt.info/goldschmidt/2022/meetingapp.cgi/Paper/10724en_AU
dc.identifier.urihttps://apo.ansto.gov.au/handle/10238/15206en_AU
dc.language.isoenen_AU
dc.publisherGoldschmidten_AU
dc.subjectGroundwater rechargeen_AU
dc.subjectAquifersen_AU
dc.subjectArtesian basinsen_AU
dc.subjectNew South Walesen_AU
dc.subjectAustraliaen_AU
dc.subjectFresh wateren_AU
dc.subjectTracer techniquesen_AU
dc.titleQuantifying recharge to the Pilliga Sandstone aquifer, Great Artesian Basin Australia: learnings from combining 14C, 36Cl and 81Kren_AU
dc.typeConference Posteren_AU
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