The glass-forming regions have been determined in the GeO
2-Na
2O system by quenching the melts in the compositional range of GeO
2=100-25mol% from above the liquidus to below
Tg at various cooling rates,
Q1=1.0×10
-1-
Q7=10
5K/s. Three glass-forming regions were found but the boundary compositions varied with cooling rate. The reciprocal of the critical cooling rate, -log
Q, versus GeO
2 concentration curve shows maxima at concentrations around GeO
2=90, 72 and 35mol%, and minima at GeO
2=85 and 50mol%. The liquidus viscosity, which is highest at GeO
2=100mol%, is maximum at GeO
2=92 and 65mol%, and minimum at GeO
2=78mol%. The slope parameter,
Eη/
TL, is also largest at GeO
2=100mol% and becomes maximum at GeO
2=92 and 65mol%, and minimum at 78mol%. The ratio of the constant
T0 in the Fulcher type equation to the liquidus temperature
TL,
T0/
TL, remains small at 0-0.1 in the composition of GeO
2=100-98mol%, but constant in the range 0.5±0.1 in the composition of GeO
2<98mol%. A comparison was made between the compositional dependence of the viscosity parameters (liquidus viscosity, slope parameter and
T0/
TL) and that of the critical cooling rate. From these data, the magnitude of the structural parameter
ΔSf (the fusion entropy per flow unit) was estimated, and the size of the flow unit was elucidated. Extraordinarily high crystallization tendency was observed in the composition of GeO
2=100-99mol%. It was suspected that this is due to an inhomogeneous nucleation resulting from the nonstoichiometry of GeO
2 including oxygen deficiency.
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