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Estimating the time required for water to travel through headwater catchments from where it recharges to where it discharges into streams (the transit time) is important for understanding catchment behaviour. This study uses tritium (3H) activities of stream water to estimate the mean transit times of water in the upper Latrobe and Yarra catchments, southeast Australia, at different flow conditions...
In arid central Australia, the ∼1.14Mkm 2 endorheic Lake Eyre Basin (LEB) experiences sporadic floods, and contains saline shallow groundwater. In this basin, where on-ground physical and chemical data are very sparse, new observations of major ion chemistry, stable isotopes (δ 2 H, δ 18 O, δ 13 C), radiogenic isotopes ( 3 H, 14 C), and remote sensing...
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