Competitive association to several components of sail through ion exchange
processes influences the fate of organic cations in the environment. To exa
mine these processes, the distributions of aniline and 1-aminonaphthalene b
etween aqueous 5 mM CaCl2 solutions and three different Indiana soils were
evaluated. Solute ratios (Sr) of aniline to 1-aminonaphthalene of 0.4-4.7 w
ere employed, and the soil solutions ranged in pH from 2.7 to 7.5, with all
measurements made 24 h after the introduction of the chemicals to the soil
s. Two previously proposed equilibrium models - the two-site (TS) and distr
ibuted parameter (DP) models - were modified to predict competition. These
models assume instantaneous equilibrium of the following reversible process
es: (i) acid dissociation of the protonated organic base (BHaq+) in the aqu
eous phase; (ii) ion exchange on the soil between the protonated organic ba
se and inorganic divalent cations (DXaq2+ = Ca-aq(2+) + Mg-aq(2+)); and (ii
i) partitioning of the nonionic species of aniline (B-aq) to soil organic c
arbon. The TS model is a general mass action model that does not take into
consideration cation exchange site heterogeneity, whereas the DP model cons
iders association constants to these sites to be distributed in a log-norma
l fashion. To describe competition for cation exchange sites within the DP
model, it was necessary to add a correlation coefficient (rho) that relates
the ion-exchange association constant (K-BH) probability density distribut
ion functions of the two compounds. The value of rho is characteristic of e
ach soil. Results indicate that competition has a greater effect at low pH
values, where ion exchange is the predominant process. For all cases, these
models capture the general trends in the soil-water distribution data of b
oth amines. The DP model also captures the nonlinearity of the 1-aminonapht
halene isotherms at low pH while at the same time capturing the nearly line
ar isotherms of aniline as a competing organic base.