Glass transition and viscosity of hydrated silica glasses

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Authors

  • S. Zietka
  • J. Deubener
  • H. Behrens
  • R. Müller

Research Organisations

External Research Organisations

  • Clausthal University of Technology
  • BAM Federal Institute for Materials Research and Testing
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Details

Original languageEnglish
Pages (from-to)380-387
Number of pages8
JournalPhysics and Chemistry of Glasses: European Journal of Glass Science and Technology Part B
Volume48
Issue number6
Publication statusPublished - Dec 2007

Abstract

The viscosity of silica glasses with different water contents was measured by penetration of sapphire microspheres in the range from 1012- 1014.7 Pas at ambient pressure. Commercial silica glasses were used together with hydrous silica glasses, which were prepared by melting glass powder plus water in an internally heated pressure vessel at 2-3 kbar and 1350-1450°C. The temperature dependence of the viscosity of silica glasses with total water contents Cw, of 5.4×10-4, 7.0×10-4, 1.00×10-2, and 1.55×10 -2 (Cw, in mass fractions) can be described by Arrhenius equations. From the results, the linear dependence of the T12 isokom (K) with the logarithm of the water content was determined as T 12=192-409 logCw. The analysis of the compositional dependence of the T12 isokom in the H2O-Na 2O-SiO2 system reveals a temperature depression of up to 200 K for mixed water- and sodium-bearing glasses compared to H 2O-SiO2 and Na2O-SiO2 glasses with same molar silica content. From these findings we conclude that protons may contribute significantly to the mixed alkali effect in glasses.

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Glass transition and viscosity of hydrated silica glasses. / Zietka, S.; Deubener, J.; Behrens, H. et al.
In: Physics and Chemistry of Glasses: European Journal of Glass Science and Technology Part B, Vol. 48, No. 6, 12.2007, p. 380-387.

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T1 - Glass transition and viscosity of hydrated silica glasses

AU - Zietka, S.

AU - Deubener, J.

AU - Behrens, H.

AU - Müller, R.

PY - 2007/12

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N2 - The viscosity of silica glasses with different water contents was measured by penetration of sapphire microspheres in the range from 1012- 1014.7 Pas at ambient pressure. Commercial silica glasses were used together with hydrous silica glasses, which were prepared by melting glass powder plus water in an internally heated pressure vessel at 2-3 kbar and 1350-1450°C. The temperature dependence of the viscosity of silica glasses with total water contents Cw, of 5.4×10-4, 7.0×10-4, 1.00×10-2, and 1.55×10 -2 (Cw, in mass fractions) can be described by Arrhenius equations. From the results, the linear dependence of the T12 isokom (K) with the logarithm of the water content was determined as T 12=192-409 logCw. The analysis of the compositional dependence of the T12 isokom in the H2O-Na 2O-SiO2 system reveals a temperature depression of up to 200 K for mixed water- and sodium-bearing glasses compared to H 2O-SiO2 and Na2O-SiO2 glasses with same molar silica content. From these findings we conclude that protons may contribute significantly to the mixed alkali effect in glasses.

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