“…The biogeochemistry of Se in the aquatic system is quite complicated, because Se can exist in four oxidation states (−II, 0, IV, and VI). The major features affecting the movement and solubility of Se are associated with changes in those species (Cooke and Bruland, 1987; Jayaweera and Biggar, 1996; Masscheleyn et al, 1990; Masscheleyn and Patrick, 1993). Selenate is the most oxidized form of Se, and is highly soluble in water (Elrashidi et al, 1987; Mikkelsen et al, 1989b).…”