The glass-forming regions in the SiO
2-Li
2O system have been determined by cooling the melts containing 35-81mol% SiO
2 from liquidus temperature to room temperature at cooling rates;
Q1=4×10
-2,
Q2=1.4×10
-1,
Q3=4×10
-1,
Q4=3,
Q5=19,
Q6=4.4×10
2 and
Q7≅10
5K/s. In the composition range SiO
2=35-75mol%, the glass-forming region expanded with increasing cooling rate, and the critical cooling rate
Q* decreased with increasing silica content, and reached a minimum at SiO
2=75mol%. Phase separation was observed in the composition range SiO
2>70mol% at cooling rates
Q2-
Q5. However, the region in which the phase separation takes place decreased with increasing cooling rate, yet persisting in high silica compositions. A linear dependence was found in the log-log plot of liquidus viscosity η
L against
Q*. When the log
Q*-logη
L diagrams are compared with the system B
2O
3-Li
2O, the system SiO
2-Li
2O system was found to have a higher liquidus viscosity than B
2O
3-Li
2O system for a given critical cooling rate. The difference in the glass-forming ability between the two systems was analyzed in terms of kinetic parameters based on the crystallization formula, and the poor glass-forming ability in the system SiO
2-Li
2O in comparison with B
2O
3-Li
2O system was elucidated to be due to a smaller fusion entropy in the former. This implies a smaller structural difference upon crystallization of the silicate in comparison with that of the borate.
View full abstract