Contribution of zeolite-seeded experiments to the understanding of glass resumption of alteration
Résumé
Understanding the origin and the consequences of glass alteration regimes is necessary for the prediction of nuclear glass
durability. The so-called “stage 3” or “resumption of alteration regime” of glasses used to sequester nuclear waste by vitrification, is
characterized by a sudden acceleration of glass alteration rate arising from the precipitation of secondary minerals, mainly zeolites.
To study this process, a promising approach is developed, based on seeding by synthesized zeolite seeds. This study quantitatively
links the alteration of a six-oxide reference borosilicate glass (ISG) and the precipitation of zeolites that affects concentrations of key
species—in particular aluminum—and thus the glass dissolution rate. The characterization of stage 3—easier at alkaline pH—can
now be extended to pH conditions more representative of those found in a geological repository thanks to seeding that reduces, or
even eliminates, the latency period preceding a resumption of glass alteration. The resumption occurrence and glass dissolution
rate are related with temperature and pH. This study shows that the detrimental effect of zeolite precipitation decreases with
decreasing pH and temperature, until it is no longer detectable at a pH around 9 imposed by the dissolution of the ISG glass. Even
for both high temperature and high pH, the resumption rate is lower than the initial alteration rate, which remains the fastest kinetic regime
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