The self-diffusion of Na was studied at temperatures ranging from 300 to 1200C by using a 22Na radiotracer. It was found that the diffusivity depended upon the temperature and the composition and ranged from 10-11 to 10-5cm2/s. The Arrhenius plots were non-linear over the entire temperature range but could be divided into 3 sections (table 124). One section was below the glass transition temperature, one was between the transition temperature and 700C, and the third was situated above 700C. This behavior suggested a change from a pure jump mechanism in the glass to a mechanism which was governed by the free volume of the glass melt. There were also some indications of the occurrence of a mixed alkali effect whose magnitude varied with temperature and composition.
M.Braedt, G.H.Frischat: Physics and Chemistry of Glasses, 1988, 29[5], 214-8
Table 124
Diffusion of Na in xNa2O-(1-x)Rb2O•3SiO2 Glasses
x | Temperature (C) | Do (cm2/s) | E (kJ/mol) |
0 | below 520 | 17.7 | 149 |
0 | 520 to 700 | 0.5 | 126 |
0 | above 700 | 0.039 | 105 |
0.25 | below 463 | 1.0 | 126 |
0.25 | 463 to 700 | 0.4 | 122 |
0.25 | above 700 | 0.032 | 101 |
0.5 | below 448 | 3.6 | 130 |
0.5 | 448 to 700 | 0.8 | 120 |
0.5 | above 700 | 0.035 | 96 |
0.75 | below 441 | 0.099 | 103 |
0.75 | 441 to 700 | 1.4 | 118 |
0.75 | above 700 | 0.0079 | 75 |
1 | below 478 | 0.002 | 67 |
1 | 478 to 700 | 0.16 | 93 |
1 | above 700 | 0.0092 | 71 |