Reduction of pertechnetate [Tc(VII)] by aqueous Fe(II) and the nature of solid phase redox products

다국어 초록 (Multilingual Abstract)

<P><B>Abstract</B></P><P>The subsurface behaviour of <SUP>99</SUP>Tc, a contaminant resulting from nuclear fuels reprocessing, is dependent on its valence (e.g., IV or VII). Abiotic reduction of soluble Tc(VII) by Fe(II)<SUB>(aq)</SUB> in pH 6–8 solutions was investigated under strictly anoxic conditions using an oxygen trap (<7.5×10<SUP>−9</SUP>atmO<SUB>2</SUB>). The reduction kinetics were strongly pH dependent. Complete and rapid reduction of Tc(VII) to a precipitated Fe/Tc(IV) form was observed when 11μmol/L of Tc(VII) was reacted with 0.4mmol/L Fe(II) at pH 7.0 and 8.0, while no significant reduction was observed over 1 month at pH 6.0. Experiments conducted at pH 7.0 with Fe(II)<SUB>(aq)</SUB>=0.05–0.8mmol/L further revealed that Tc(VII) reduction was a combination of homogeneous and heterogeneous reaction. Heterogeneous reduction predominated after approximately 0.01mmol/L of Fe(II) was oxidized. The heterogeneous reaction was more rapid, and was catalyzed by Fe(II) that adsorbed to the Fe/Tc(IV) redox product. Wet chemical and Fe–X-ray absorption near edge spectroscopy measurements (XANES) showed that Fe(II) and Fe(III) were present in the Fe/Tc(IV) redox products after reaction termination. <SUP>57</SUP>Fe-Mössbauer, extended X-ray adsorption fine structure (EXAFS), and transmission electron microscopy (TEM) measurements revealed that the Fe/Tc(IV) solid phase was poorly ordered and dominated by Fe(II)-containing ferrihydrite with minor magnetite. Tc(IV) exhibited homogeneous spatial distribution within the precipitates. According to Tc-EXAFS measurements and structural modeling, its molecular environment was consistent with an octahedral Tc(IV) dimer bound in bidentate edge-sharing mode to octahedral Fe(III) associated with surface or vacancy sites in ferrihydrite. The precipitate maintained Tc(IV)<SUB>aq</SUB> concentrations that were slightly below those in equilibrium with amorphous Tc(IV)O<SUB>2</SUB>·<I>n</I>H<SUB>2</SUB>O<SUB>(s)</SUB>. The oxidation rate of sorbed Tc(IV) in the Fe/Tc precipitate was considerably slower than Tc(IV)O<SUB>2</SUB>·<I>n</I>H<SUB>2</SUB>O<SUB>(s)</SUB> as a result of its intraparticle/intragrain residence. Precipitates of this nature may form in anoxic sediments or groundwaters, and the intraparticle residence of sorbed/precipitated Tc(IV) may limit <SUP>99</SUP>Tc remobilization upon the return of oxidizing conditions.</P>