Two models of time-dependent Cs-137 adsorption and fixation by soil we
re fitted to solution activity data from incubated organic upland soil
s, over a period of 709 days. Both model fits were highly (p < 0.01) o
r very highly (p < 0.001) significant. Both models differentiated betw
een specifically adsorbed and nonspecifically adsorbed 'labile' radioc
esium. Transfer to a nonlabile pool was either by a kinetic step (mode
l I) or a diffusive process (model II). Although fits for model II wer
e comparatively worse in some soils, the second model had the dual adv
antage of being more mechanistic in structure and requiring fewer para
meters. Parameters estimated for models I and II compared favorably wi
th those derived experimentally; some dependence on soil mica was evid
ent. Model I was used to predict the change in bioavailability of radi
ocesium in soils following documented inputs from Windscale (1957), fa
llout from weapons testing (1960s), and the Chernobyl release (1986).
For all but one of the five organic soils, long-term predictions of re
lative bioavailability generated by model I were similar to the limite
d range of published values for Cs-137 uptake by vegetation. It is con
cluded that the Cs fixation models presented account for a substantial
part of the change in availability of Cs-137 observed in field studie
s.