Using 3D geological modelling and geochemical mixing models to characterise alluvial aquifer recharge sources in the upper Condamine River catchment, Queensland, Australia
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Approach integrates 3D geological modelling with EMMA and mixing calculations

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Successful characterisation of alluvial recharge sources and controlling factors

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Four end-members identified: rainfall and groundwater inflow from adjacent aquifers

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High contribution rates of mountain front recharge to alluvial hydrochemistry

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Mixing, evapotranspiration and water-rock interaction control groundwater evolution

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