Radionuclide soil-to-crop transfer was analysed in large undisturbed soil m
onoliths installed in lysimeters under controlled climatic conditions. The
soils were representative of large agricultural areas in the European Union
: Loamy-sand Orthic Podzol from Belgium, Loamy-sand Fluvisol from France, L
oamy Calcic Luvisol from Spain, Silty-loam Orthic Luvisol from Germany, and
Sandy-loam Eutric Fluvisol from the UK. On the lysimeters, winter barley w
as sown for two consecutive years on artificially contaminated soils simula
ting a post-accidental situation, 1 and 2 years after radionuclide depositi
on. The amount (Bq m(-2)) of Cs-137 and Sr-90 that accumulated in the crop
was higher in the loamy-sand soils, regardless of the total radionuclides (
MBq m(-2)) or available fraction content in the soil. The Orthic Podzol pro
duced the highest Cs-137 crop accumulation, and the Loamy-sand Fluvisol the
highest Sr-90 accumulation. Concentration ratios (CR) showed similar resul
ts, but with higher Sr-90 transfer for the Podzol than for the Loamy-sand F
luvisol. The activity concentration of radionuclides in the plants was nega
tively correlated with crop yield, indicating that high crop productivity p
roduced a general dilution effect in radionuclide concentration activity in
plants. The relative radionuclide crop accumulation expressed in Bq m(-2)
was predicted from the soil availability parameters, that is the available
Cs-137 fraction divided by the distribution coefficient (K-D) and by the K
concentration in soil solution, and the available Sr-90 divided by the cati
onic exchange capacity (CEC). These predictions could not be obtained when
using the CR, as this does not fully account for the crop growing condition
s which influence radionuclide uptake by the crop. (C) 1999 Elsevier Scienc
e Ltd. All rights reserved.