The migration potentials for Cs-134 in spruce soil columns (undisturbe
d profile) following a surface contamination and also the redistributi
on of the radionuclide through the profile have been investigated. The
radiocaesium bioavailability in the different horizons was estimated
by activity measurements in the soil solution and from extractions mad
e of the solid phase. The calculation of a Kd ratio indicates that ret
ention mechanisms increase very rapidly with depth. Cs-134 speciation
reveals the high affinity of the radionuclide for specific sites on mi
neral components. In spite of its organic nature, the O Ah horizon has
a great efficiency for Cs accumulation; the role of humic clay compon
ents and/or microflora is unforeseen.