Abstract
Different types of naturally occuring minerals have been investigated in respect of the sorption of various radioisotopes. The present work deals with column studies of the sorption of 89Sr and 60Co oh four natural bentonites, collected from localities. Columns of cross section of 1.47 cm2 were used for the determination of the breakthrough capacities for both Sr and Co. The applicability of Glueckauf plate theory to the systems was tested. It was found that HETP is constant for a given system of column and cationic species, which proves the applicability of the theory. From this, it follows that the data obtained for the short laboratory colums can be used to predict the breakthrough behavior for longer columns.