“…Na‐silicates have shown an Arrhenius evolution (below 500°C) with
values approaching 30 kJ/mol for both the molar ratios
11 (as shown in Figure S3), which has been previously observed for glass melts
39,40 . The existence of a single
is a consequence of an equilibrium where silanols are released first followed by their conversion into solvating water molecules which then leave the system due to evaporation
11 . K‐ and Li‐silicates, on the other hand, tend to show multiple activation energies.…”