The kinetics of Potassium adsorption from solution to exchangeable pha
ses was investigated on bentonite samples which were first saturated w
ith calcium in the form of CaCl2. Potassium adsorption time was evalua
ted on Ca-saturated samples using 125, 150, 200 and 250 mugK/ml soluti
ons, equilibrated for 10, 15, 20, 30, 35, 45, 60, 75, 80 and 120 minut
es. Sample pH levels varied between 4.0 and 9.0. Equilibrium in potass
ium exchange was reached faster in lower concentrations and higher pH
values. Four mathematical models (first-order rate, parabolic diffusio
n, Elovich and modified Freundlich equation) were used to describe pot
assium sorption. Comparison of coefficients of determinations (r2), an
d plots indicated that modified Freundlich and parabolic diffusion mod
els provided the best fits of the adsorption data (r2 > 0.979). Consta
nts for the Freundlich equation were estimated and the model was expre
ssed as a function of pH.