“…The latter solid species are more resistant in the soil. Compared to results of relatively short-term deposition (Baumann et al, 1996;Rigol et al, 1999), our soils showing long-term deposition had lower amounts of 137 Cs bound to exchangeable, microbial biomass or organic matter fractions but higher amounts as persistent and residual fractions, which might be due to the well-known ''aging effect'' (Absalom et al, 1996;Spezzano, 2005). Recent study of soils affected by the Chernobyl accident indicate that most of the 137 Cs is in the residual fraction (Hou et al, 2003), which supports this aging phenomenon.…”