“…This is in contrast to Ghosh-Dastidar et al [30] who found that the sorption of SeO 2 (g) on hydrated lime at elevated temperatures resulted in the formation of CaSeO 3 under SO 2 (g) deficient conditions, as confirmed by XRD. Likewise, Baur and Johnson [27,28] generated CaSeO 3 , but used neat aqueous experiments and synthetically generated monosulfate, ettringite and calcium silicate hydrate (CSH) phases. While they explicitly sought CaSeO 3 ·H 2 O in XRD spectra, no agreement could be attained for either the available PDF files with their measured XRD spectra (8 • , 16 • and 24 • 2Â), or the experimentally determined solubility product data, leading Baur and Johnson [27] to ultimately conclude that SeO 3 2− was incorporated into AFm phases at high Se concentrations.…”