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Uranium isotopes reveal the enrichment and attenuation processes of groundwater uranium in floodplain aquifers
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DOI：10.1016/j.watres.2026.126623.png)
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Abstract
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• Uranium isotopes were used to trace U fate along redox gradients. • U concentrations decreased systematically along groundwater flow paths. • Isotopic fractionation distinguished adsorption from reductive immobilization. • The contribution of U reduction to attenuation was quantitatively constrained. • Microbially mediated U(VI) reduction was the dominant U attenuation pathway.
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12.4
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3.0W
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15.7W
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