Leaching experiments under static conditions have been conducted in water a
t 90 degreesC with a borosilicate and an albite glass to check whether the
kinetics r of the reaction are determined by the affinity A of dissolution
through the law r = r(0)[1 - exp(-A/RT)]. These experiments have been condu
cted with the goal of approaching saturation conditions thanks to the fast
kinetics ensured by a high ratio between the surface area of glass and the
volume of the solution (80 and 343 cm(-1) for the borosilicate and an albit
e glass, respectively). The leaching rates decrease by several orders of ma
gnitude over month-long experiments. The ionic activities as calculated fro
m the concentrations of species in the solution are used to define the chem
ical affinity A = RT ln(K/Q) where Q is the ionic activity product, K the r
eaction equilibrium constant, R the gas constant and T the temperature. The
constant K has been calculated from the Gibbs-free energy of formation of
glasses determined in a another paper. Because the [1 - exp(-A/RT)] term do
es not drop below 0.75, the general rate equation does not account for the
marked decrease of the reaction rate. Although the affinity of dissolution
can be considered to be a rate controlling factor, the decrease of leaching
rate is likely due to the formation of a gel at the glass-solution interfa
ce that constitutes a diffusion barrier limiting the transfer of reacting a
queous species to the glass. (C) 2001 Elsevier Science B.V. All rights rese
rved.