Subsurface Migration of Radioactive Waste Materials by Particulate Transport

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Abstract
The role of suspended particles as carriers of dissolved nuclides from high-level radioactive waste repositories has been investigated. Depending on the concentrations of suspended particles and the nature of the invading water, it has been found that cationic nuclides may be competitively adsorbed on suspended clay particles, the partitioning being largely determined by pH, temperature, and comparative surface areas of particulates and surrounding rocks. Column tests with activated particles have been conducted and showed that the clay particles pass readily through porous mineral columns and are increasingly retained if salinity is increased. Retention in basalt columns is stronger in the presence of high concentrations of sodium and calcium ions and has been explained in terms of van der Waals forces. The range of particulate migration then depends on the condition of the rock surfaces, the persistence of a clay coating, and the total dissolved ion concentration. For adsorbable waste ions, this may represent a pathway comparable in significance to ion-exchange-controlled migration. For some bed materials, the particulate movement displayed a prompt and a delayed component; the nature of the delay mechanism is not fully understood at present.