In the performance assessment of the geological disposal of radioactive wastes, the retardation of radionuclide migration is generally evaluated by using the sorption distribution coefficient (
Kd). The
Kd values would, however, be influenced by the colloidal substance in aqueous phase because these colloids may have the potential abilities to sorb the radionuclides. In this study, Cs-137, bentonite colloids and quartz sands were used for the batch-type sorption tests in order to investigate the influence of colloids on the sorption behavior of radionuclides. The
Kds of Cs-137 onto quartz sands (
Kd1) and onto bentonite colloids (
Kd2) were determined from the distributed amounts among solid phase, colloidal phase and aqueous phase, which were distinguished by the pore size of filters used for separations of the experimental solutions. Under these experimental conditions, distribution of Cs-137 in the coexistence of quartz sands and bentonite colloids was able to be estimated from
Kd1 and
Kd2, which were obtained from other sorption tests carried out in the presence of sands and colloids, respectively. Thus selecting a relevant pore size for filtration would be available for evaluation of colloidal influence on radionuclide sorption onto the solids.
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