A series of experiments were carried out to quantify the interception
of rain-borne caesium by crops of grass (Lolium perenne), broad beans
(Vicia faba) and wheat (Triticum aestivum) under rainfall intensities
typical of those encountered in the U.K. (1-18 mm h(-1)). The fraction
of contamination deposited on the vegetation decreased with time, as
the plant surface approached a saturation level of contamination. Surf
ace contamination was dependent upon the total amount of rainfall rath
er than the rainfall intensity. The total surface water storage capaci
ty of wheat and beans was determined, and found to approach a saturati
on level as total rainfall increased in a manner similar to the measur
ed contamination levels. Total accumulation of caesium from aqueous so
lution onto bean leaves was found to increase linearly with time over
the range of concentrations tested (0.0001-10 mM), the rate of accumul
ation increasing with concentration according to a power law. The comb
ination of results obtained suggests that deposition of rain-borne con
taminants could be modelled appropriately by a water storage capacity
term and a ''chemical term'' derived from the contaminant concentratio
n and its affinity for a particular plant surface. (C) 1997 Elsevier S
cience Ltd.