Abstract
The diffusion-convection model of 137Cs transport has been used to evaluate the activity-depth profiles of soils in southwestern Nigeria in this study. The experimentally determined depth profiles were fitted into the diffusion-convection equation to obtain the diffusion coefficient D and the convective velocity υ. Results obtained showed that the range of the diffusion coefficient was 0.72 – 1.02 cm2 per year while that of the convective velocity was from 0.07 to 0.16 cm per year. It was observed that the diffusion coefficient is higher than the convective velocity in all the sampling points. The low convective velocities obtained in all the locations may imply that convective rates of the radionuclide within the soil layers are insignificant compared to the diffusion rates. Key words: 137Cs activity, diffusion coefficient, convective velocity, soil depth, radionuclide.
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