Preliminary data of kinetic sorption experiments are presented. Batch sorption experiments with the aim of estimation of distribution coefficient (K d ) values were conducted using natural clay minerals from the Šaltiškiai quarry and two sets of solutions with different caesium concentrations (C(Cs) = 2.30·10−10 mol/l and C(Cs) = 6.80·10 −5 mol/l). Kinetic sorption experiments indicated insignificant variation of sorption parameters depending on the chemical composition of groundwater and clay minerals. Speciation studies showed the high content (up to 70%) of exchangeable caesium in experiments with high caesium concentrations. Results of kinetic tracer experiments and sequential extraction studies revealed differences in sorption mechanisms depending on the Cs concentration. Data obtained from sorption-desorption experiments were used to model sorption process by applying the kinetic 4-box model to describe the cation exchange processes on three sites of clay minerals with distinctly different selectivity. The obtained forward and backward exchange rate constants were used to calculate apparent equilibrium constants, which ranged from 1 to 26 and the highest ones were found for reversible sites.