Stable isotope tracing of water exchange along a dryland river

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dc.contributor.authorGibson, JJen_AU
dc.contributor.authorSadek, MAen_AU
dc.contributor.authorStone, DJMen_AU
dc.contributor.authorHughes, CEen_AU
dc.contributor.authorHankin, SIen_AU
dc.contributor.authorCendón, DIen_AU
dc.contributor.authorHollins, SEen_AU
dc.date.accessioned2022-01-24T03:43:32Zen_AU
dc.date.available2022-01-24T03:43:32Zen_AU
dc.date.issued2006-08-27en_AU
dc.date.statistics2021-12-24en_AU
dc.description.abstractDeuterium and oxygen-18 enrichment in river water during its transit along the Barwon-Darling River, a dryland region in southeastern Australia, is found to occur systematically along evaporation lines with slopes of close to 4 in 2H–18O space. This is largely consistent with expected trends for an open-water dominated evaporating system. When combined with reach balance assessments and derived runoff ratios, this strongly suggests that the enrichment signal and its variability is acquired during the process of evaporation from the river channel itself, as enhanced by the presence of abundant weirs, dams and other storages, rather than reflecting inherited enrichment signals from soil water evaporation in the watershed. Using a steady-state isotope mass balance analysis based on monthly 18O and 2H, we use the isotopic evolution of river water to re-construct a picture of net exchange between the river and its contributing area along eight reaches of the river from July 2002 to December 2003, including the duration of a minor flood event. As expected for a flood-driven dryland system, considerable temporal variability in exchange is predicted. For 65% of all reach-months evaluated the river was apparently gaining water along its course; about 10% of these times it was also undergoing substantial volumetric drawdown. Overall, a broad systematic decline in the percentage of gaining intervals is noted from the upstream to downstream reaches, with most reaches gaining water substantially more than half of the time. One reach, known to be an intensive cotton-growing area, was found to be fairly balanced between gaining and losing periods. While a more detailed analysis is required to carefully verify the quantities of water exchange, a first assessment of monthly runoff ratios for the reach catchments suggests that the inflow estimates are reasonable. The technique, while requiring additional quantitative ground-truthing, demonstrates potential as a non-invasive tool for detecting and quantifying water diversions, one that can be easily incorporated within existing water quality monitoring activities. © 2006 Published by Elsevier Ltd.en_AU
dc.identifier.citationGibson, J. J., Sadek, M. A., Stone, D. J. M., Hughes, C., Hankin, S., Cendón, D. I., Hollins, S. E. (2006). Stable isotope tracing of water exchange along a dryland river. Paper presented to the 16th Annual V.M. Goldschmidt Conference : Geochemistry downunder, Melbourne Exhibition and Convention Centre, Melbourne, Australia,27 August- 1 September 2006. In Geochimica et Cosmochimica Acta, 70(18, Supplement), A201. doi:10.1016/j.gca.2006.06.406en_AU
dc.identifier.conferenceenddate1 September 2006en_AU
dc.identifier.conferencename6th Annual V.M. Goldschmidt Conference (Goldschmidt 2006) - 'Geochemistry downunder',en_AU
dc.identifier.conferenceplaceMelbourne, Australiaen_AU
dc.identifier.conferencestartdate27 August 2006en_AU
dc.identifier.issn0016-7037en_AU
dc.identifier.issueS18en_AU
dc.identifier.journaltitleGeochimica et Cosmochimica Actaen_AU
dc.identifier.paginationA201en_AU
dc.identifier.urihttps://doi.org/10.1016/j.gca.2006.06.406en_AU
dc.identifier.urihttps://apo.ansto.gov.au/dspace/handle/10238/12712en_AU
dc.identifier.volume70en_AU
dc.language.isoenen_AU
dc.publisherGoldschmidten_AU
dc.subjectDeuteriumen_AU
dc.subjectOxygenen_AU
dc.subjectRiversen_AU
dc.subjectAustraliaen_AU
dc.subjectEvaporationen_AU
dc.subjectDamsen_AU
dc.subjectWater reservoirsen_AU
dc.subjectWatershedsen_AU
dc.subjectWateren_AU
dc.subjectEvaporationen_AU
dc.subjectFloodsen_AU
dc.titleStable isotope tracing of water exchange along a dryland riveren_AU
dc.typeConference Abstracten_AU
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