Abstract. In acid mine drainage conditions uranium(VI) adsorbs on goethite and schwertmannite, forming surface complexes with the ferric iron polyhedra and sulfate, respectively. The structure of these surface species was identified by EXAFS.
lntroductionThe ferric oxide Schwertmannite is commonly formed in acid mine drainage waters (pH-range from 2.8 to 4.5) in the presence of high sulfate concentrations (Comell and Schwertmann 1996). Because ofits large specific surface area it may influence the migration of uranium(VI) by sorption processes. By mixing the acid sulfate-rich leachate of the uranium mine Königstein (Saxony) with ground water schwertmannite, as identified by IR-spectroscopy, was precipitated and uranium as a part of the acid sulfate-rich leachate was sorbed on the formed precipitates (Jenk 1996). The aim of this study was to get structural information about the formed uranium(VI) surface complexes by Extended X-ray Absorption Fine Structure (EXAFS) spectroscopy. We include Goethite in our investigations as a reference to compare and interpret the schwertmannite data.
ExperimentalSampies for EXAFS analysis (Table 1) were prepared under N2 atmosphere using 200 mg of Schwertmannite or goethite with initial uranium(VI) concentrations of lxl0-5 (pH 6.5) to 5x10· 5 M (pH 4.2). The ionic strength was adjusted to 0.02 N Na2S04 or 0.01 N NaC104, respectively. Uranium LIII edge EXAFS spectra were recorded at room temperature in fluorescence mode at the Rossendorf beamline