I. Techer et al., Dissolution kinetics of basaltic glasses: control by solution chemistry and protective effect of the alteration film, CHEM GEOL, 176(1-4), 2001, pp. 235-263
Basaltic glasses are considered as natural analogs for industrial nuclear a
luminoborosilicate glasses. Alteration experiments were conducted in closed
and open systems at 90 degreesC with a synthetic basalt glass doped with 1
% lithium (dissolution tracer). The evolution of the alteration kinetics ov
er time was assessed by comparison of reaction progress at different degree
s in closed system experiments. The maximum dissolution rate (initial rate,
r(0)) was comparable to the value observed For an SON68-type nuclear glass
; the basaltic glass alteration rate subsequently dropped by four orders of
magnitude. The kinetic models currently proposed in the literature to acco
unt for the alteration kinetics of basaltic glasses, nuclear glasses or alu
minosilicate minerals are based on the concept of chemical affinity: the ch
emical affinity alone is assumed to control the dissolution kinetics. When
applied to the experimental data for the closed system tests with basaltic
glass, these models failed to account for the low measured rates. An inhibi
ting effect of dissolved silica was then investigated through open system b
asaltic glass alteration experiments with silicon-enriched solutions. The b
asaltic glass dissolution rate dropped by a factor not exceeding 200 (or ab
out two orders of magnitude) compared with r(0) at the high imposed silicon
concentrations (130 ppm). A protective effect of the alteration film was a
dvanced to account for the four-orders-of-magnitude rate drop observed in c
losed system experiments, based notably on an examination of natural basalt
ic glasses ranging in age from several thousand to a few million years. The
mean alteration rates can be estimated from the measured palagonite thickn
esses, taking into account the age of the natural glasses: the rates were c
omparable to those measured in the laboratory for high reaction progress. (
C) 2001 Elsevier Science B.V. All rights reserved.