“…Another possibility is that the phase transformation is controlled by diffusion of alkaline and alkali ions in glass. Extensive literature search results showed that the activation energies needed for the diffusivity of Ca, Sr, Ba, K, B, and Si in silicate glasses are in the range of 175-295, [22][23][24][25] 165-255, 26 -28 175, 29 165-215, 30 -32 345, 33,34 and 320 -550 kJ/mol, 24 respectively. Only the activation energies of alkaline and alkali ions are close to those needed for the formation of cristobalite and pseudowollastonite, indicating a diffusion-controlling mechanism.…”