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

Citation
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
Citations number
53
Categorie Soggetti
Earth Sciences
Journal title
APPLIED GEOCHEMISTRY
ISSN journal
08832927 → ACNP
Volume
15
Issue
9
Year of publication
2000
Pages
1399 - 1416
Database
ISI
SICI code
0883-2927(200010)15:9<1399:TKAMOS>2.0.ZU;2-G
Abstract
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.