N. Maes et al., Determination of the diffusion coefficient of ionic species in boom clay by electromigration: Feasibility study, RADIOCH ACT, 82, 1998, pp. 183-189
Migration studies are necessary for the performance assessment of a geologi
cal disposal of HLW. Classical diffusion experiments on Boom Clay take long
time because of the excellent retention characteristics. To accelerate the
migration of ionic species, an electrical field is used to reduce the expe
rimental time drastically. The electromigration technique has also the adva
ntage that the apparent molecular diffusion coefficient can be derived by t
wo independent methods. First, it can be calculated from the dispersion coe
fficient, knowing the dispersion length and convection velocity The dispers
ion length for Boom Clay was experimentally determined as 8.5 10(-5) m. Sec
ondly, from the Einstein relation between the velocity of the migrating spe
cies and the apparent molecular diffusion coefficient. But corrections are
necessary for electro-osmotic flow. The electro-osmotic mobility was experi
mentally determined as 1.4 10(-9) m(2)/Vs. Both methods were used to determ
ine the apparent molecular diffusion coefficient of Sr-85. Both methods res
ult in an apparent molecular diffusion coefficient of 6.3-7.8 10(-12) m(2)/
s which is validated by pure diffusion experiments. The feasibility of the
technique is further demonstrated for Na-22, I-131 and I-ITO. The excellent
agreement with the apparent molecular diffusion coefficients obtained by c
lassical diffusion tests clearly demonstrates the feasibility of the electr
omigration technique for the determination of diffusion coefficients.