Glass dissolution as a function of pH and its implications for understanding mechanisms and future experiments

Author:

Strachan Denis

Funder

Pacific Northwest National Laboratory

U.S. Department of Energy Office of Fossil Energy

US Department of Energy by Battelle Memorial Institute

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference85 articles.

1. Thermodynamic and kinetic constraints on reaction rates among minerals and aqueous solutions I. Theoretical considerations;Åagaard;Am. J. Sci.,1982

2. 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;Abraitis;Appl. Geochem.,2000

3. Single-pass flow-through experiments on a simulated waste glass in alkaline media at 40 C. I. Experiments conducted at variable solution flow rate to glass surface area ratio;Abraitis;J. Nucl. Mater.,2000

4. Bates, J.K., Bradley, C.R., Buck, E.C., Cunnane, J.C., Ebert, W.L., Feng, X., Mazer, J.J., Wronkiewicz, D.J., Sproull, J., Bourcier, W.L., McGrail, B.P., Altenhofen, M.K., 1994. High-level waste borosilicate glass: A compendium of corrosion characteristics. Vol I, Report No. DOE-EM-0177 (Vol 1). US Department of Energy, Washington, DC.

5. Bates, J.K., Bradley, C.R., Buck, E.C., Cunnane, J.C., Ebert, W.L., Feng, X., Mazer, J.J., Wronkiewicz, D.J., Sproull, J., Bourcier, W.L., McGrail, B.P., Altenhofen, M.K., 1994. High-level waste borosilicate glass: A compendium of corrosion characteristics. Vol II, Report No. US Department of Energy, Washington, DC.

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