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Although it is generally recognized that goethite surfaces present in natural environments have carbonate species adsorbed, knowledge of their effect on the reactivity of goethite toward other anions remains limited. Accordingly, the effect of CO 3 on the adsorption of SeO 4 and SO 4 on goethite is determined. Carbonate promotes the adsorption of SeO 4 and SO 4 between pH 6 and 8. The maximum effect occurs at relatively low CO 3 concentrations (0.2 m M ), and the promotive effect decreases and eventually becomes competitive with further increase in CO 3 adsorption. Acetate (AcO) and formate also appear to promote adsorption of SeO 4 and SO 4 . Based on existing Fourier transformed dsorption of SeO 4 and SO 4 Based on existing Fourier transformed infrared (FTIR) spectroscopic data and new electrophoretic mobility data, CO 3 may promote the adsorption of other oxyanions by forming extra reactive protonated sites that coexist with the adsorbed CO 3 . Acetate and formate presumably interact through the same mechanism. Goethite surfaces present in natural environments may have substantial amounts of CO 3 adsorbed. Depending on the CO 3 levels, this may enhance, decrease, or have a neutral effect on the adsorption of moderate affinity anions such as SeO 4 and SO 4 . Accordingly, the combined effects of promotive and competitive interactions may render CO 3 less competitive overall than was commonly presumed. Similarly, the presence of AcO and formate may be less competitive with other anions due also to their promotive interaction effect.
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Wijnja et al. (2002) studied this question.
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