Please use this identifier to cite or link to this item: https://apo.ansto.gov.au/dspace/handle/10238/12318
Title: Residence times of bank storage and return flows and the influence on river water chemistry in the upper Barwon River, Australia
Authors: Howcroft, W
Cartwright, I
Cendón, DI
Keywords: Storage
Water
Watersheds
Tritium
Chlorine 36
Geologic deposits
Rivers
Australia
Isotopes
Data
Drainage
Storms
Ground water
Issue Date: Feb-2019
Publisher: Elsevier B. V.
Citation: Howcroft, W., Cartwright, I., & Cendón, D. I. (2019). Residence times of bank storage and return flows and the influence on river water chemistry in the upper Barwon River, Australia. Applied Geochemistry, 101, 31-41. doi:10.1016/j.apgeochem.2018.12.026
Abstract: Documenting the sources and residence times of water that contributes to streamflow is important for understanding processes in river catchments. The residence times of bank storage and return flow and its influence on river water chemistry in the upper Barwon River of southeast Australia were investigated using stable (18O, 2H, and 13C) and radioactive (3H and 36Cl) isotopes, major ion geochemistry, river discharge data, and electrical conductivity (EC)-discharge hysteresis. Elevated 3H activities following high winter flows indicate that bank storage and return flow contributes to river discharge for at least several months. However, EC-discharge hysteresis patterns suggest that individual storm events make additional contributions to bank storage and return flow throughout the year over periods of a few weeks. 3H activities in the upper Barwon River are >1.75 TU throughout the year, suggesting that the contribution of older regional groundwater, which has 3H activities <0.04 TU, is relatively minor in comparison to bank return flows. However, downstream trends in total dissolved solids (TDS) concentrations, δ13C values and R36Cl values demonstrate that regional groundwater inflows deliver solutes to the river. Estimates of regional groundwater inflows are mainly in the range 8–33% of total stream flow. The R36Cl values of river water in the upper Barwon catchment are between 37 and 46, which are significantly higher than those of modern rainfall (∼20). The high R36Cl values may reflect retardation of bomb-pulse 36Cl due to plant uptake and recycling in the soil zone, which suggests Cl residence times of up to ∼60 years. The results of this study demonstrate that river water is comprised of both young and old water and that managing rivers and near-river environments should include careful consideration of both inputs. © 2018 Elsevier Ltd.
URI: https://doi.org/10.1016/j.apgeochem.2018.12.026
https://apo.ansto.gov.au/dspace/handle/10238/12318
ISSN: 0883-2927
Appears in Collections:Journal Articles

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