After placing radioactive waste in a deep underground repository, long-lived radionuclides may be leached from the waste and subsequently transported by groundwater through fractures in the rock mass surrounding the repository. Radionuclides transported by groundwater will diffuse into the rock matrix and be adsorbed on minerals (Fig. 1-12). Although the radionuclides have been released from the repository, their migration is greatly impeded. Further, the concentration of these radionuclides in groundwater is diluted significantly before the nuclides return to our biosphere. These mechanisms greatly mitigate the risks of this method of radioactive waste disposal.
Transport of radionuclides in an intact rock sample was investigated and Fick's diffusion law was confirmed to be applicable to predicting transport behavior. The distance plutonium diffuses in the rock mass in a million-year period, for example, is predicted to be 5 m using the diffusivity value obtained in this study. It became clear that radionuclides diffuse through pore water in rock (pore diffusion), and some radionuclides diffuse in the adsorbed state on mineral surfaces (surface diffusion). This knowledge is used in the long-term performance assessment of radioactive waste disposal. |