The kinetics and mechanisms of simulated British Magnox waste glass dissolution as a function of pH, silicic acid activity and time in low temperature aqueous systems
Pk. Abraitis et al., The kinetics and mechanisms of simulated British Magnox waste glass dissolution as a function of pH, silicic acid activity and time in low temperature aqueous systems, APPL GEOCH, 15(9), 2000, pp. 1399-1416
Dissolution of a simulated British Magnox waste glass is governed by two pH
-dependent processes. At low pH, dissolution is governed by reactions occur
ring predominantly at non-Si sites and residual Si-rich gels develop at the
glass surface as B, Al and modifier cations are selectively leached. Here,
extensive proton promoted hydrolysis of B-O and Al-O bonds is coupled with
hydration and ion exchange processes. Hydrolysis of siloxane bonds governs
the rate of dissolution at high pH and the glass dissolves congruently as
the silicate network breaks down extensively. Differences in the surface ch
emistries and morphologies of glass samples reacted in strongly acidic and
highly alkaline media reflect the net effects of these processes. The rate
of the congruent dissolution process is influenced by the activity of silic
ic acid, The results are compared with published data for other glass formu
lations and are discussed in the context of proposed kinetic dissolution mo
dels. (C) 2000 Elsevier Science Ltd. All rights reserved.