The reduction of U(VI) on corroded iron under anoxic conditions

Summary The corrosion of iron and the interaction between corroded iron and U(VI) in anoxic conditions were investigated. The anoxic conditions were obtained by flushing an 99.97% Ar-0.03% CO2 gas mixture through the test vessel, in which an oxygen trap and six reaction bottles containing synthetic groundwater (10 mM NaCl and 2 mM HCO3 −.) were placed. The dark-green coloured corrosion product, formed on iron surface after three months corrosion in synthetic groundwater solutions, was identified by powder X-ray diffraction to be carbonate green rust, Fe4 IIFe2 III(OH)12CO3. The iron foil that reacted in a solution (10 ppm U(VI), 10 mM NaCl and 2 mM HCO3 −) for three months was analysed by SEM-EDS. The result shows that: (i) an uneven layer of carbonate green rust (1-5 µm thick) formed on the metallic iron; (ii) a thin (0.3 µm) uranium-rich layer deposited on top of the carbonate green rust layer; and (iii) some UO2 crystals (3-5 µm sized) on the thin uranium layer. The experimental results proved that the U(VI) removal capacity of metal iron is not hindered by formation of a layer of carbonate green rust on the iron. Tests with cast iron and pure iron indicate that they have similar U(VI) removal capacities. At the end of experiment, U concentrations in solution approached the solubility of UO2(s), 10−8 M. The stability of the carbonate green rust at the experimental conditions, pH, Eh, [Fe2+] and [HCO3 −], is discussed.