“…Two hypotheses can be proposed to explain the last point: either the dissolution of the chromia layer, or the formation rate become respectively greater and lower than expected from the extrapolation of lower temperature values. For the first hypothesis, data on solubility and diffusion of chromium in molten silicates, so as silica-based liquids viscosity are pretty well known [10,11,13,21,22]. In each case, an Arrhenius type law describes the evolution of these parameters with temperature.…”