The leaching of137Cs and90Sr from Surrey Earth montmorillonite and Silver Hill illite has been studied. Three forms of the clays, calcined and uncalcined
and their composites with cement, were leached with four leachants, deionized water, and simulated sea ground and storage
pond waters. Results were expressed as the cumulative fraction of activity leached against the square root of time, and
... [Show full abstract] used
to compute diffusion coefficients. These suggested that all the leaching processes studied were slow (10−22 to 10−18 m2.s−1).