Characterization of the intermediate in formation of selenate-substituted ettringite
Precipitation of SeO{sub 4}{sup 2−}-substituted ettringite is an efficient method to immobilize SeO{sub 4}{sup 2−} under alkaline conditions. The effect of SO{sub 4}{sup 2−} on SeO{sub 4}{sup 2−} immobilization was investigated, because SO{sub 4}{sup 2−} is one of the major ions in aqueous and soil environments and it is easily incorporated in ettringite. We aimed to systemically elucidate the formation mechanisms of SeO{sub 4}{sup 2−}-substituted ettringite with and without SO{sub 4}{sup 2−}. When SO{sub 4}{sup 2−} and SeO{sub 4}{sup 2−} coexisted, both oxoanions were immediately coprecipitated with ettringite after adding a Ca source. Although SO{sub 4}{sup 2−} was partially substituted by SeO{sub 4}{sup 2−} in ettringite, no other phases were formed during the process. Without SO{sub 4}{sup 2−}, SeO{sub 4}{sup 2−}-substituted AFm phase was formed as an intermediate, confirmed by X-ray diffraction peak at d 2.878, as well as by scanning electron microscopy with energy dispersive X-ray spectroscopy and zeta potential measurements. It is clear that the incorporation mechanism of SeO{sub 4}{sup 2−} in ettringite is dependent on coexisting SO{sub 4}{sup 2−} in aqueous environments. - Highlights: • SO{sub 4}{sup 2−} is preferentially incorporated in ettringite over SeO{sub 4}{sup 2−}. • Coexisting SO{sub 4}{sup 2−} influences immobilization of SeO{sub 4}{sup 2−}. • SO{sub 4}{sup 2−}–hydrocalumite is proved as an intermediate. • The zeta potential and SEM-EDX support the XRD results.