文摘
The sorption and diffusion behavior of 8 × 10−6 M Np(V) in Opalinus Clay (OPA) with synthetic pore water (pH 7.6) as mobile phase was studied under ambient conditions by batch and diffusion experiments, respectively. The Kd value determined by batch experiments with OPA suspensions is equal to 0.025 ± 0.005 m3/kg. The diffusion-accessible porosity ε of intact OPA as determined by through- and out-diffusion experiments with tritiated water (HTO) is equal to 0.15 ± 0.01. The diffusion coefficient De and the rock capacity factor α of 22Na+ in OPA were measured by through-, out-, and in-diffusion experiments and asserted the reliability of these diffusion techniques. For the diffusion of Np(V) in synthetic pore water, the capillary method gave Dw = (6.0 ± 1.0) × 10−10 m2/s. Due to the strong sorption of Np(V) on OPA, the diffusion of Np(V) was investigated by the in-diffusion technique. The diffusion parameters for Np(V) in OPA are De = (6.9 ± 1.1) × 10−12 m2/s and α = 243 ± 4. This corresponds to Kd = 0.10 ± 0.01 m3/kg for the sorption of Np(V) in intact OPA.