“…The concern is the unintended incorporation of carbonate. Many synthesis routes include the use of organic materials or carbonates in the starting materials. ,,,,,− ,,,,,,, Indeed, carbonate is occasionally observed in synthetic apatites and britholites, even though it is presumably volatile and expected to degas as CO 2 during calcining. ,,,,, Evidently, some carbonate is stabilized and retained in the crystal lattice . As starting materials are usually prepared stoichiometrically, this leads to the problem of excess Si, which could then either precipitate as a silica polymorph (SiO 2 either quartz or tridymite), or bond with other components in the system to form other byproduct phases (e.g., CaSiO 3 wollastonite).…”