Y. Thiry et al., DETERMINATION OF THE PHYSICOCHEMICAL PARAMETERS WHICH INFLUENCE THE CS AVAILABILITY IN FOREST SOILS, Science of the total environment, 157(1-3), 1994, pp. 261-265
The type of soil and humus has to be considered as primordial for the
evaluation of the Cs availability and for its transfer dynamics. Previ
ous studies on the radiocesium distribution through a forest soil prof
ile indicate that the intermediate layer, OAh (organic and mineral par
ticles intimately mixed) accumulates Cs in a more efficient way than t
he deeper mineral layer. Our study on the physico-chemical parameters
influencing Cs retention shows however, that humic compounds do not pa
rticularly influence the Cs retention. On the contrary, the K interact
ion with mineral particles induces a clear increase in the Cs fixation
. This observation suggests that K inducing collapse is responsible fo
r a higher Cs retention. In the OAh layer, an original collapsed state
of the mica structure would benefit the Cs fixation.