“…8 and 9, its effect was insignificant for the crystallization of the cuspidine phase. In the previous study of the CaO-SiO 2 -R 2 O (R=Li, Na, or K) 14) and CaO-SiO 2 -CaF 2 15) systems, the crystalline phase tended to change from CaO-SiO 2 to dicalcium silicate, or cuspidine, as the cationic radius of the added materials increased. Merwinite is a magnesium substitute of dicalcium silicate, so when merwinite was considered as one of the dicalcium silicates, the tendency of the crystalline phase was similar to that in the present and previous studies.…”