Adsorption of strontium on illite type clay has been studied as a function
of shaking time, the ratio of solution volume to weight of clay and the con
centration of adsorbate, using Sr-90 as a tracer. The adsorption experiment
s were carried out using the batch method and initial Sr2+ ion concentratio
ns ranged from 10(-6) to 10(-1) M. The influence of Ca2+ and Ba2+ cations o
n Sr adsorption were also studied. These effects are correlated with the io
nic radii of alkaline earth ions present in the solution. The Freundlich an
d Dubinin Radushkevich (D-R) isotherm have been applied to the data and the
parameters of the isotherm equations were calculated. The mean energy of a
dsorption, E was also calculated from the adsorption energy constant, K and
maximum capacity X-m values were determined from linearized D-R equation.
From empirical Freundlich parameters a site distribution function was calcu
lated.