ATR-FTIR spectroscopic characterization of coexisting carbonate surface complexes on hematite |
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Authors: | John R. Bargar James D. Kubicki James A. Davis |
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Affiliation: | 1 Stanford Synchrotron Radiation Laboratory, 2575 Sand Hill Road, MS69, Menlo Park, CA 94025, USA 2 Penn State University, Department of Geosciences, 308 Deike Building, University Park, PA 16802, USA 3 Stanford Linear Accelerator Center, 2575 Sand Hill Road, MS68, Menlo Park, CA 94025, USA 4 U.S. Geological Survey, Water Resources Division, 345 Middlefield Road, MS 465, Menlo Park, CA 94025, USA |
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Abstract: | The speciation of carbonate adsorbed to hematite in air-equilibrated aqueous solutions has been studied using ATR-FTIR spectroscopy. Samples were measured over a range of pH conditions, at 0.1 M NaCl and at low ionic strength, and in H2O and D2O solutions to permit a multispecies analysis of the data. Second-derivative analyses and fits to the spectra indicate the presence of two major and two minor surface-bound carbonate species. The two major complexes coexist at near-neutral pH and low ionic strength. One of these two complexes is relatively sensitive to ionic strength, being displaced at 0.1 M NaCl, whereas the other is not. Comparison of experimental to DFT/MO-calculated frequencies suggest these two major species to be (a) a monodentate binuclear inner-sphere carbonate surface complex, and (b) a fully or partially solvated carbonate (CO32−) species that is symmetry broken and appears to reside in the structured vicinal water layers at the hematite-water interface, retained by hydrogen bonding and/or other forces. Minor carbonate complexes include diffuse layer CO32− and an unidentified inner-sphere species. Both of the dominant species observed here are likely to be significant controls of the surface charge and sorptive properties of Fe-oxides. |
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