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Results 1-10 of 18 (Search time: 0.007 seconds).
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Issue DateTitleAuthor(s)
24-Aug-2014Comparison of oxygen isotope records from radiocarbon dated groundwater and U-Th dated flowstoneAdler, L; Treble, PC; Meredith, KT; Baker, AA; Hellstrom, JC
10-Jul-2013Stable isotope (δ13C and δ15N) studies in aquatic ecosystems: response to different conditionsMazumder, D; Walsh, C; Williams, RJ; Jenkins, K; Sives, C; Hollins, SE; Meredith, KT; Doyle, T
8-Jun-2014Using trace element and halide isotopes to understand salinization mechanisms of groundwaters from an arid aquiferMeredith, KT; Hollins, SE; Tomascak, P; Moriguti, T; Frape, S; Nakamura, E
1-Jan-2015Use of stable and radioactive isotopes to unravel surface water groundwater interactions in developed catchmentAndersen, MS; Rau, GC; Meredith, KT; McCallum, AM; Acworth, RI
1-Jan-2012Using 14C and 3H to delineate a recharge 'window' into the Perth Basin aquifers, North Gnanagara groundwater system, Western AustraliaMeredith, KT; Cendón, DI; Pigois, JP; Hollins, SE; Jacobsen, GE
1-Jul-2013The lithium, boron and strontium isotopic systematics of groundwaters from an arid aquifer system: implications for recharge and weathering processesMeredith, KT; Moriguti, T; Tomascak, P; Hollins, SE; Nakamura, E
19-Jan-2012Modelling evaporative losses from the Darling River during drought using δ2H and δ18OHughes, CE; Hollins, SE; Crawford, J; Meredith, KT; Cendón, DI
15-Dec-2016A nine-year record of groundwater environmental tracer variations in a weathered sandstone plateau aquiferCendón, DI; Hankin, SI; Hughes, CE; Meredith, KT; Peterson, MA; Scheiber, L; Shimizu, Y
15-Dec-2018Rainfall isotope variations over the Australian continent – implications for hydrology and isoscape applicationsHollins, SE; Hughes, CE; Crawford, J; Cendón, DI; Meredith, KT
24-Nov-2019What’s going on down (under) there? Unravelling biochemical flows under differential rainfall periods in a Western Australian calcreteSaccò, M; Blyth, AJ; Meredith, KT; Smith, C; Hua, Q; Mazumder, D; Humphreys, WF; White, N; Grice, K

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