A comprehensive laboratory study is presented on the solid-phase speci
ation of ionic radiocaesium in bottom sediments (riverine, lacustrine,
estuarine) covering some 75 samples of widely differing textural prop
erties and originating from various locations in Europe. Sediments are
characterised in terms of cation exchange capacities, exchangeable po
tassium and ammonium and specific radiocaesium sorption properties. It
is shown that radiocaesium is quantitatively retained in the specific
sorption sites associated with the micaceous clay minerals in the sed
iments. The practical consequences of this finding are discussed in te
rms of a predictive equation allowing forecasting of radiocaesium leve
ls in the watercolumn or in the interstitial fluid of the sediment.