A study on uptake of neutral and dissociating organic compounds from soil s
olution into roots, and their subsequent translocation, was undertaken usin
g model simulations. The model approach combines the processes of lipophili
c sorption, electrochemical interactions, ion trap, advection in xylem and
dilution by growth. It needs as input data, apart from plant properties, lo
g K-ow, pK(a) and the valency number of the compound, and pH and chemical c
oncentration in the soil solution. Equilibrium and dynamic (steady-state) m
odels were tested against measured data from several authors, including non
-electrolytes as well as weakly acidic and weakly basic compounds. Deviatio
ns from the measured values led to further development of the model approac
h: sorption in the central cylinder may explain the small transpiration str
eam concentration factor of lipophilic compounds. For non-electrolytes, the
model predicted uptake and translocation with high accuracy. For acids and
bases, the tendency of the results was satisfactory. The dynamic model and
the equilibrium approach gave similar results for the root concentration f
actor. The calculation of the transpiration stream concentration factor was
more accurate with the dynamic model, but still gave deviations up to fact
or of ten or more. The dominating process for monovalent weak electrolytes
was found to be the ion trap effect. (C) 2000 Society of Chemical Industry.