“…It was indicated that significant constriction and tortuosity were resulted. However, the iodide ion diffusion in the interstitial water at a steady-state flux NA can be described by ( 7) where D; and D, are the respective pore diffusivities in interstitial and surface water, s; and s, are the respective porosities available for diffusion in interstitial and surface water, and 'IC; and 'IC, are the respective ionic concentration gradients in interstitial and surface water. Assuming ( 8) where kd is the distribution coefficient, ()the fraction of surface water available for diffusion, and Pc the clay dry density, Eq.…”