Study on the Hydration Properties of two Polymorphs of Sr4Al6SO16

Abstract Sr4Al6SO16 is a kind of anhydrous sulfoaluminate that belongs to the sodalite family. In this paper, we demonstrate the effect of Fe3+ ions addition on the hydration properties of two polymorphs of Sr4Al6SO16 (namely pure orthorhombic and cubic). In solid-state reaction of orthorhombic Sr4Al6SO16, excessive 5 wt.% SrSO4 was used to compensate for the loss of sulfur. Results indicate that the hydration rate of cubic phase is faster than that of orthorhombic phase at early stage, but the heat release of the latter is more concentrated. The reason why the cubic phase has a faster earlier hydration kinetics may be due to the incorporation of Fe3+ ions and the formation of SrFe12O19 impurity phase, which increases the defects in the structure and activates the crystal lattice. Both polymorphs react with water to form the reaction products first, and then no crystalline phase hydration product was precipitated after 72 h. In contrary to the XRD, amorphous AH3 was clearly detected in TGA analyses in hydrated samples, probably due to poor crystallinity which cannot be detected by XRD. In addition, both polymorphs contain a lot of impurity phases, and their amounts are calculated using the Rietveld method. Moreover, the addition of Fe3+ ions is not only beneficial to adjust the cubic phase content, but also facilitates the relative particle growth. This work provides a useful platform for employing the Fe3+ ions to regulate the hydration properties of Sr4Al6SO16.