Water solubilities and diffusivities have been measured in melts of binary
alkali silicate compositions. The results are compared to the classic work
of Scholze and co-workers. Water solubilities obtained in the present study
for sodium and lithium silicate melts are similar to those of the earlier
work while there is some question regarding results for a potassium silicat
e melt. Water diffusivities found in the present study are consistently gre
ater than those of the earlier work by a factor of 2 to 3. The activation e
nergies for water diffusion into two sodium silicate melts obtained in the
present study are lower than those of the earlier work for water diffusion
out of melts. The difference in diffusivities may be due to the difference
in diffusion direction but this cannot be established at this time. It is s
hown for the first time that water diffusivity is independent of the partia
l pressure of water vapour in the melting atmosphere. Finally the correlati
on between water diffusivity and melt viscosity proposed by Scholze & Mulfi
nger cannot be applied to the results of this study which raises doubts reg
arding the universality of this model.