The Adam-Gibbs theory of structural relaxation is presented in terms of the
microscopic parameters controlling viscous flow; Delta mu, the energy barr
ier hindering rearrangement of a single silicate monomer, and z(*) the numb
er of monomers that must simultaneously overcome their barrier in order for
a change in configuration to occur. Independent viscosity, calorimetric an
d spectroscopic data for glasses and melts in the system SiO2-Na2O are used
to show that z(*) at the glass transition has a value of approximately 10
for all of the compositions considered and that microscopic energy barriers
are on the order of several tens of kJ per mole of silicon. Furthermore, t
he variation of configurational entropy of glasses in the system SiO2-Na2O
has been determined from the viscosity and calorimetric data. It is conclud
ed that a stable melt complex with a stoichiometry close to Na2Si3O7 exists
and that medium range order plays an important role in determining the con
figurational entropies, although the details are unclear. Overall, a self-c
onsistent picture of the quantitative links between microscopic and macrosc
opic properties is determined for this simple system, providing an encourag
ing first step towards a fully generalisable predictive model for silicate
melt viscosity. (C) 2001 Elsevier Science B.V. All rights reserved.