The processes of membrane transport exhibiting permeability coefficien
ts depending on the species activities do not obey the ''independence
principle'' and are assumed to take place by a mechanism of discrete n
ature, analyzable by a kinetic formalism. in this article, we study th
e dependence of the osmotice permeability coefficient on the water act
ivities, from the steady-state analysis of a kinetic model of single-f
ile water transport that simultaneously incorporates the vacancy-media
ted and ''knock-on'' mechanisms into the state diagram. In particular,
we study the relation between the near-equilibrium osmotic permeabili
ty (P-e) and the equilibrium water activity of the compartments (w). T
he analysis and numerical calculations performed for a simple case of
the model show that, for values of the parameters consistent with expe
rimental data, P-e exhibits only a small variation with w within the p
hysiological range in the majority of the situations considered here.
It is not possible to predict, from the study of these simple models,
whether more complicated kinetic diagrams of water transport may be ch
aracterized by permeability coefficients with a more evident dependenc
e on the water activities. Nevertheless, the results obtained here sug
gest that, for the case of physiological water pores, the analysis of
the kinetic dependence of the permeability coefficients on the water a
ctivities may not yield evidence pointing to a discrete nature for the
transport process.