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-Reference-Cited by-同舟云学术

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

Published:2000-10 Issue:9 Volume:15 Page:1399-1416
ISSN:0883-2927
Container-title:Applied Geochemistry
language:en
Short-container-title:Applied Geochemistry

Author:

Abraitis P.K.,Livens F.R.,Monteith J.E.,Small J.S.,Trivedi D.P.,Vaughan D.J.,Wogelius R.A.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Pollution,Environmental Chemistry

Reference53 articles.

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3. Secondary phase formation during nuclear waste-glass dissolution;Abrajano;Clays and Clay Minerals,1990

4. Ball, J.W., Nordstrom, D.K., 1991. WATEQ4F — User’s manual with revised thermodynamic data-base and test cases for calculating speciation of major, trace and redox elements in natural waters. US Geological Survey Open-File Report 90–129

5. Dissolution rate of a basalt glass in silica-rich solutions: implications for long-term alteration;Berger;Geochim. Cosmochim. Acta,1994

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