“…By June, both reservoirs have anoxic hypolimnions beginning at depths of 6 m. As these anoxic waters develop, 137 Cs and Fe concentrations increase. For Pond B,137 Cs concentrations in both the surface waters and the hypolimnion increase by a factor of 2Â (Alberts et al, , 1987, and the Fe inventories in the hypolimnion increase by a factor of >15Â (Pinder et al, 1992). The increases in the surface waters reflect mixing across the thermocline, and has been estimated to involve approximately 0.2% of the hypolimnion per day (Hinton and Pinder, 2001).…”