S. Paterson et al., A MODEL OF ORGANIC-CHEMICAL UPTAKE BY PLANTS FROM SOIL AND THE ATMOSPHERE, Environmental science & technology, 28(13), 1994, pp. 2259-2266
A three-compartment mass balance model of a plant is developed to quan
tify the uptake of organic chemicals from soil and the atmosphere. The
compartments are as follows: root, stem, and foliage. The processes i
nvolved are diffusion and bulk flow of chemical between soil and root;
transport within the plant in the phloem and transpiration streams be
tween root, stem, and foliage; exchange between foliage and air and be
tween soil and air; metabolism and growth. The model is applied to the
uptake of Bromacil by the soybean from hydroponic solution, yielding
results which compare favorably with experimental data. Illustrative a
pplications to three other chemicals (2,4-D, dichlorobenzonitrile, and
hexachlorobiphenyl) from soil are described showing that chemicals pr
esent in soil may reach foliage by evaporation from soil with subseque
nt foliar absorption and by transpiration, the proportions being deter
mined by the chemical's Henry's law constant and octanol-water partiti
on coefficient. The intent is to provide a method by which chemical co
ncentrations in various plant tissues can be estimated from informatio
n on chemical properties, concentrations in soil and air, and plant ph
ysiology. Applications and data requirements for validation are discus
sed.