Skip to Main Content
Skip Nav Destination
GEOREF RECORD

Physics and chemistry of silicate glasses and melts

Bjorn Mysen
Physics and chemistry of silicate glasses and melts (in Ninth international symposium on Experimental mineralogy, petrology and geochemistry, Peter Ulmer (convener))
European Journal of Mineralogy (October 2003) 15 (5): 781-802

Abstract

Property and structure data from binary and ternary silicate and aluminosilicate melts and glasses often reveal simple and systematic relationships to composition and temperature. Properties whose dominant structural control is the abundance of fully polymerized Q (super 4) -species, exhibit smooth variations with silica content. Such properties include activation energies associated with transport. Properties that depend on the type and abundance of coexisting structural species in depolymerized melts, either show smooth functional relationships to melt polymerization, NBO/T, or exhibit pronounced minimum or maximum values at intermediate NBO/T-values. The former properties include those, which are related to the availability of configurational states. The latter group includes those whose behavior is controlled by the energetics of mixing of the individual structural species. An example is enthalpy of mixing. Crystal-liquid element partition coefficients also exhibit behavior governed by thermodynamics of mixing of the structural species of the melt. Aluminum in most silicate melts is in tetrahedral coordination at ambient pressure and substitutes for silicon. The Al (super 3+) <--> Si (super 4+) substitution lowers (Si,Al)-O-(Si,Al) bond energy. In principle, the value of properties that depends on bridging oxygen bond strength, decreases, therefore, with increasing Al/(Al+Si). Properties that depend on the proportion of polymerized and depolymerized Q (super n) -species in the melt can show minima or maxima in relationships to Al/(Al+Si) because the abundance of the Q (super n) -species in depolymerized silicate melts depends on the bulk melt Al/(Al+Si). Transport properties fall in this category. It is possible that Al-distribution between Q (super n) -species in depolymerized aluminosilicate melts depends on temperature. It is likely, therefore, at least for high-temperature viscosity, its temperature-dependence is non-Ahrrenian. Other melt transport properties that are functionally related to viscous flow (e.g., diffusivity, electrical, and thermal conductivity) may also show non-Ahrrenian temperature-dependence at high temperature.


ISSN: 0935-1221
EISSN: 1617-4011
Serial Title: European Journal of Mineralogy
Serial Volume: 15
Serial Issue: 5
Title: Physics and chemistry of silicate glasses and melts
Title: Ninth international symposium on Experimental mineralogy, petrology and geochemistry
Author(s): Mysen, Bjorn
Author(s): Ulmer, Peterconvener
Affiliation: Carnegie Institution of Washington, Geophysical Laboratory, Washington, DC, United States
Affiliation: ETH Zurich, Institute for Mineralogy, Zurich, Switzerland
Pages: 781-802
Published: 200310
Text Language: English
Publisher: Schweizerbart'sche Verlagsbuchhandlung (Naegele u. Obermiller), Stuttgart, Federal Republic of Germany
Meeting name: Ninth international symposium on Experimental mineralogy, petrology and geochemistry
Meeting location: Zurich, CHE, Switzerland
Meeting date: 20020324March 24-27, 2002
References: 98
Accession Number: 2004-020035
Categories: General geophysics
Document Type: Serial Conference document
Bibliographic Level: Analytic
Illustration Description: illus. incl. 1 table
Country of Publication: Germany
Secondary Affiliation: GeoRef, Copyright 2017, American Geosciences Institute.
Update Code: 200406

or Create an Account

Close Modal
Close Modal