Structural relaxation in silicate glasses and melts: High-temperature Raman spectroscopy

Wim J. Malfait and Werner E. Halter
Phys. Rev. B 77, 014201 – Published 3 January 2008

Abstract

By combining both isothermal and rate heating experiments, structural relaxation times were determined in the glass transition range with in situ, high-temperature Raman spectroscopy. The obtained relaxation times agree well with the shear relaxation times obtained from viscosity data. Thus, the time scale for viscous flow is the same as the time scale of the rearrangement of the silicate network structure toward chemical equilibrium. This demonstrates that Si—O bond breaking is the primary control on silicate melt viscosity.

  • Figure
  • Figure
  • Figure
  • Figure
  • Figure
  • Figure
  • Received 8 June 2007

DOI:https://doi.org/10.1103/PhysRevB.77.014201

©2008 American Physical Society

Authors & Affiliations

Wim J. Malfait and Werner E. Halter

  • Institute for Isotope Geochemistry and Mineral Resources, ETH Zurich, 8092 Zurich, Switzerland

Article Text (Subscription Required)

Click to Expand

References (Subscription Required)

Click to Expand
Issue

Vol. 77, Iss. 1 — 1 January 2008

Reuse & Permissions
Access Options
Author publication services for translation and copyediting assistance advertisement

Authorization Required


×
×

Images

×

Sign up to receive regular email alerts from Physical Review B

Log In

Cancel
×

Search


Article Lookup

Paste a citation or DOI

Enter a citation
×