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Fig. 1. Oxidative remobilization of biogenic uraninite [UO2(s)] in bioreduced sediment suspensions with variable concentrations of Fe(II) addition at pH 4 or 5 (a), 7 (b), and 9 (c). The initial UO2(s) in the system was 16 µmol/L (3808 µg/L).
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