A semiempirical equation relating the foaming temperature to sulphate
concentration was established. Literature data on sulphate solubility
and melt viscosity and the variation of foaming temperature with sulph
ate concentration obtained in a previous study were used to evaluate e
mpirical coefficients involved in the equation. An agreement between t
heory and experiment was attained when bubble nucleation on undissolve
d silica grains and nonuniform distribution of SiO2 within the melt we
re considered. The results show that the rate of dissolution of solid
grains in the melt and the temperature history control sulphate foam f
ormation and retention in glass.