Diffusion of Na+. Cs+, Co2+ and Sr2+ in bentonite compacted to a dry densit
y of 1800 kg m(-3) and saturated with groundwaters and aqueous solutions of
differing ionic strength have been studied experimentally using the throug
h diffusion technique. Sorption experiments have been carried out under a w
ide range of pH and concentration of supporting electrolyte.
The dependence of the apparent diffusivity of Na+, Cs+ and Sr2+, mainly sor
bed by ion exchange, on the sorption intensity is accommodated by a model e
ncompassing diffusion of the sorbed cations within the electrical double la
yer next to the mineral surface in addition to diffusion in the pore water.
The apparent diffusivity of Co2+, sorbed by surface complexation reactions
, corresponds to complete immobilization on sorption. (C) 1999 Elsevier Sci
ence B.V. All rights reserved.