Sodium Diffusion in SiO 2 Glass

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Abstract
Diffusion of the radioactive tracer 22 Na in a commercial SiO 2 glass was investigated from 170° to 1000°C. The temperature dependence curve had discontinuities at about 573° and 250°C. The resulting Arrhenius equations are D = 3.44 × 10 2 exp(‐21.1 kcal/RT) cm 2 /sec between 1000° and 573°C, D = 0.398 exp(‐25.8 kcal/RT) cm 2 /sec between 573° and 250°C, and D = 2.13 exp(‐28.3 kcal/RT) cm 2 /sec between 250° and 170°C. The two anomalies are discussed in terms of “quartz‐like” and “cristobalite‐like” precrystalline elements in the structure of the glass. Comparison of the Na diffusion in SiO, glass with that in soda‐silica and soda‐lime‐silica glasses shows that SiO 2 glass occupies a boundary position with respect to these systems. A possible diffusion mechanism is discussed.

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