Identifying the contribution of regional groundwater to the baseflow of a tropical river (Daly River, Australia)

Brian Smerdon, W. Payton Gardner, Glenn Harrington, Steven Tickell

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    49 Citations (Scopus)


    A mixture of older regional-scale groundwater flow and relatively modern local-scale groundwater was identified as the source of baseflow to a perennial river in a tropical savanna. Multiple environmental tracers, including 222Rn, CFCs, SF 6, and 4He were measured in the river, groundwater, and springs along a 60km segment of the Daly River in the Northern Territory of Australia. At the location where a group of springs intersected the river, groundwater discharge contained elevated 4He and very low concentrations of CFCs and SF 6. This influx of regional-scale groundwater could be detected at downstream locations in the river and was used to parameterize a one-dimensional model for estimating the groundwater discharge flux. Upstream and downstream of the springs, the source of baseflow is composed of waters containing SF 6 and CFCs from local-scale groundwater sources adjacent to the river. Within 1km of the river, a redox fence was detected, with reducing conditions leading to degradation of CFCs that could have masked detecting the contribution of local-scale sources. This study confirmed the applicability of a new technique using 4He to identify regional-scale groundwater flow contributions to rivers, and demonstrated that multi-tracer studies are needed to identify the locations, rates, and sources of baseflow.

    Original languageEnglish
    Pages (from-to)107-115
    Number of pages9
    JournalJournal of Hydrology
    Publication statusPublished - 25 Sept 2012


    • Baseflow
    • Environmental tracers
    • Regional groundwater
    • Springs
    • Surface water-groundwater interaction


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