| Abstract
| - Heterogeneous oxidation of gas-phase SO2 on different iron oxides was investigated in situ using a Whitecell coupled with Fourier transform infrared spectroscopy (FTIR) and diffuse reflectance infrared Fouriertransform spectroscopy (DRIFTS). The results revealed that adsorbed SO2 could be oxidized on the surfaceof most iron oxides to form a surface sulfate species at ambient temperature. Additional support for thishypothesis was provided by X-ray photoelectron spectroscopy (XPS) measurements and ion chromatogram(IC) analysis. The spectroscopic results further revealed that the surface hydroxyl species on the iron oxideswas the key reactant for this heterogeneous oxidation. Furthermore, the bidentate sulfate species were thepredominant surface species with α-Fe2O3, α-FeOOH, and Fe3O4, while the monodentate surface Fe(III)−sulfato complexes were available in the case of γ-Fe2O3. Using the BET area as the reactive surface area, thesamples showed the varied reactivity in the order of α-Fe2O3> γ-Fe2O3> Fe3O4> β-FeOOH > α-FeOOH.Some preliminary experiments indicated a significant acceleration during SO2 uptake on the surface of α-Fe2O3in the presence of oxygen. In contrast, no significant formation of sulfate was seen on the surface of α-Fe2O3prereduced by H2 at 523 K at the absence of O2, suggesting that the concentration of adsorbed oxygen overcatalyst surfaces may be the key factor contributing to the oxidizing activities. On the basis of these results,the atmospheric implications of these studies on SO2 uptake on Fe-rich mineral aerosol were discussed.
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