Diffusion coefficients of Fe were measured in glass melts with the basic compositions 5Na2O·xMgO·(15-x)CaO·yAl2O3·(80-y)SiO2 with x = 5, 10 and y = 0, 5, 7.5, 10 or 15. The melts were doped with 0.25mol%Fe2O3 and studied in the temperature range from 1000 to 1600C by using square-wave voltammetry. The voltammograms exhibited distinct peaks attributed to the reduction of Fe3+ to Fe2+, from which peak currents mixed diffusion coefficients of Fe were calculated. Diffusion coefficients in all melt compositions which did not show crystallization could be fitted to Arrhenius equation. The diffusivities measured in different melt compositions were related to the same viscosity, i.e. not the same temperature. Increasing the alumina concentration from 5 to 10mol% resulted in an increase of the viscosity corrected diffusivities. At further increasing alumina concentrations, the diffusivities get smaller again. This could be explained by the stabilizing effect of Na+ and Ca2+ on FeO4- and AlO4--tetrahedra, which strengthens the incorporation of Fe3+ into the glass structure.

The Effect of Mixed Alkaline Earths on the Diffusivity and the Incorporation of Iron into 5Na2O-xMgO-(15-x)CaO-yAl2O3-(80-y)SiO2 Melts. A.Wiedenroth, C.Rüssel: Journal of Non-Crystalline Solids, 2003, 330[1-3], 90-8