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Large S isotope and trace element fractionations in pyrite of uranium roll front systems result from internally-driven biogeochemical cycle

Fuel CycleEnvironmental RadiochemistryEnvironmental ChemistryBiogeochemistryEngineeringTrace Element GeochemistryLarge S IsotopeIsotope GeochemistryGeochemistryChemistryTrace Element FractionationsGeochemical CyclingInternally-driven Biogeochemical CycleEarth Science