A zirconia-pillared and an alumina-pillared montmorillonite clay were found
to exhibit high K(d)s for trace levels of cesium (2.5 ppb) in the presence
of high concentrations of Ca2+, Mg2+, and Na+ ions with distribution coeff
icients (K(d)s) for Cs-137 exceeding 1 x 10(5) mL/g over a wide range of co
mpeting ion concentrations. An excess of K+ ions, however, caused a dramati
c reduction in the Ca K(d)s for both of the materials. These results were i
n contrast to the parent montmorillonite which exhibited far lower K(d)s fo
r Cs-137, particularly in the presence of high concentrations of Mg2+ and C
a2+. Batch tests in simulated groundwaters showed that both pillared clays
efficiently removed Cs-137 from solution, with the best Kds being approxima
tely 8.5 x 105 mL/g in a potassium-free groundwater. The materials performe
d less well in a groundwater with a high potassium concentration, but still
gave K(d)s similar to commercially available zeolites. The rate of Cs-137
uptake was found to be rapid with both the alumina- and zirconia-pillared c
lays extracting > 90% of the Cs-137 from a 0.1 M NaNO3 solution within 5 mi
nutes.