“…Subsequent desorption of 137 Cs from sediments can occur and contribute to the Cs content of water (Alberts et al, 1979;Evans et al, 1983;Alberts et al, 1987) and biota (Kelly and Pinder, 1996;Holloman et al, 1997;Peles et al, 2000). Cesium desorption is particularly evident in systems with (1) a large proportion of clays such as kaolinite that desorb Cs more readily than 2:1 layered clays such as illite (Comans et al, 1991;Maguire et al, 1992;de Koning et al, 2000;Hinton et al, 2001;Krumhansl et al, 2001) and (2) periods of anoxia associated with the production or release of monovalent cations that compete with Cs C for sorption sites on the sediments (Sholkovitz, 1985;Comans et al, 1989;Dominik and Span, 1992).…”