E. Valcke et A. Cremers, SORPTION-DESORPTION DYNAMICS OF RADIOCESIUM IN ORGANIC-MATTER SOILS, Science of the total environment, 157(1-3), 1994, pp. 275-283
A systematic study has been carried out on the radiocaesium sorption p
roperties of 25 soils (forest, peat) covering organic matter (OM) cont
ents in the range of 10-97%. Predictions are made for radiocaesium par
titioning between micaceous Frayed Edge Sites (FES) and regular exchan
ge sites (RES) on the basis of specific radiocaesium interception pote
ntials of the soil and overall exchange capacity. It is shown that for
soils with a very high OM content (> 80%), significant fractions are
present in a readily reversible form in the OM phase. In soils of low-
medium OM content (< 40%), only a very minor fraction is present in th
e OM exchange complex. Experimental findings, based on a desorption sc
reening with a variety of desorption agents are in agreement with thes
e predictions. On the basis of a study of sorption kinetics, some addi
tional tools are available for identifying problem soils. In cases of
very high OM content, radiocaesium adsorption is completed within hour
s demonstrating the involvement of the OM sites. In soils for which in
terception occurs in the FES, sorption continues to proceed for period
s of 2-3 weeks. In conclusion, some examples are presented on radiocae
sium desorption using ion exchangers as radiocaesium sinks in promotin
g desorption. For a peaty soil, near quantitative desorption is accomp
lished. For forest soils with OM contents in a range of 10-40%, fixati
on levels of 30-50% are demonstrated.