Abstract
It is known that acids leach out metal ions from the outermost layer of glass, leaving a skeleton film. We found that the refractive index of such a film nf changes with the relative humidity p⁄p0, and studied nf vs. p⁄p0 relations for some dense flint and dense crown glasses. The following conclusions are derived from the analysis of nf vs. p⁄p0 curves: (1) The refractive index of the skeleton ns (>nf) is always greater than that of fused silica, indicating that metal ions are still contained in the skeleton. (2) The porosity of the film ranges from 0.05 to 0.21, and the mean pore radius from 6Å to 23Å, depending on the composition of glass as well as the leaching conditions.