“…These findings suggest that the oxidation of the Si-CH 3 groups in the silicone preceramic polymer, which starts above 350°C, 21 was at least partly responsible for the formation of the cracks, since it is a very exothermic reaction. 22,23 As described in the following paragraph, this formulation did not form hardystonite, but wollastonite, as the main ceramic phase; nonetheless, this result showed the potential of using a heat treatment in inert atmosphere that could be applied to other silicate ceramic systems. It is also relevant to notice that the volume change associated with the formation of hardystonite (from a stoichiometric amount of SiO 2 , ZnO, and CaO) is À10.2 vol%, while for wollastonite (from a stoichiometric amount of SiO 2 and CaO) is À9.2 vol%.…”