Since the early twentieth century, there
have been many investigations on the penetration of silica glass by light
gases. In 1926, H. Elsey reported that silica glass has the property of passing
helium but stopping air at room temperature when the pressure is about 100
atmospheres. Although the densities of crystal quartz and vitreous silica
differ only by about 17% (2.65 and 2.20 g/cm3, respectively), the helium
permeability of silica glass is six orders more elevated than that of crystal
quartz. This vast difference has puzzled researchers for decades considering
that silica glass and quartz crystal have the same chemical composition. This
work discusses the mechanism of high helium permeation through silica glass. It
briefly reviews the experimental data and its contradictions with the
continuous random network theory. The research not only sheds light on the
strength of silica glass but also suggests potential implications for other
abnormal properties of silica glass. A recently proposed nanoflake model for
silica glass structure is utilized to explain the origin of glass permeation to
helium. According to the nanoflake model, the formation of nanoflakes not only
brings a one-dimensional medium-range ordering structure into silica glass but
simultaneously creates regions where van der Waals bonds replace the
oxygen-silicon covalent bonds. It is the weakness of van der Waals bonds that
causes the helium mobility in these areas to increase. Accordingly, the
permeation rate of helium through silica glass with fast cooling is expected to
be lower than that of slow- cooling glass. This prediction should be
experimentally verified in the near future.
Author (s) Details
Shangcong Cheng
Molecular Foundry of Lawrence Berkeley National Laboratory, Berkeley, CA
94720, USA.
Please see the book here:- https://doi.org/10.9734/bpi/cmsdi/v6/2707
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