Pk. Sinha et al., A COMPARATIVE-STUDY ON INDIGENOUSLY AVAILABLE SYNTHETIC ZEOLITES FOR REMOVAL OF STRONTIUM FROM SOLUTIONS BY ION-EXCHANGE, Radiochimica Acta, 73(3), 1996, pp. 157-163
Removal of strontium ions from solutions by Sr-Na exchange, using indi
genously available synthetic zeolites, has been studied. Batch tests i
ndicated that the time required for equilibrium was 4 hours under stir
red condition. The percent removal and the distribution coefficient (K
-d) values for Sr were determined at different concentrations, ranging
from traces of Sr (solution of Sr-90-nitrate) to 50 mM Sr-nitrate. Tw
o zeolites viz., 4A and 13X, were observed to provide high removal of
Sr, while the other two, AR-1 (a synthetic mordenite) and ZSM-5, were
not as effective. The nature of diffusion of Sr ions. controlling the
exchange reaction, was studied by drawing Bt-t plots (B, diffusional f
requency and t, time). Linear plots, obtained for 13X and 4A, at 50 mM
Sr(NO3)(2) concentration, indicated that the process tvas controlled
by diffusion through the particles. At lower concentrations of Sr and
for the other two zeolites. the plots were non-linear and the process
might be controlled by film diffusion. The equilibrium studies, carrie
d out using isonormal solutions of Sr and Na ions at a total Sr+Na con
centration of 0.1 N, indicated a marginal selectivity for Sr, in case
of 4A and 13X. The corrected selectivity coefficient (K-c) values were
calculated and Kielland plots were drawn. Column trials with 1.5 ml b
eds of the granular zeolites and a simulated waste solution containing
Sr-90, indicated that 4A and 13X could remove about 90-92% of Sr, at
a flow rate of 60 bed volumes per hour (BV/h). The removal increased t
o 97%, when the flow rate was reduced to 12 BV/h. The third zeolite AR
-1 provided lower removal of Sr in both the cases. When another simula
ted alkaline waste solution, containing high salt content (3M NaNO3),
in addition to Sr-90 and Cs-137, was treated using a mixed zeolite col
umn (4A + AR-1), the removal of both the Sr and Cs isotopes was about
55-65%.