“…Similarly for SO 4 , leachability at high pH (>11) was increased in aged materials, supposedly due to enhanced dissolution of alumina ferric oxide trisulphate (AFt) and alumina ferric oxide monosulphate (AFm) phases with increased carbonation (Engelsen et al, 2009). Calcium, lithium, strontium and barium presented a similar trend: CDW3 and CDW4 displayed lower leaching, especially at high pH, possibly because of lower solubility of the corresponding carbonates compared with the original sulphate species, as suggested by Müllauer et al (2012). Oxyanion-forming elements, such as V (and Cr and Mo, to a lower extent), showed a sharper V-shape at high pH for CDW1, CDW2 and CDW5, which is typical of fresher materials (Engelsen et al, 2010); the same V-shape was observed for SO 4 , confirming that oxyanions may partly substitute SO 4 in ettringite in fresher samples (Kumarathasan et al, 1990).…”