“…According to the surface complexation theory, lowering the pH increases the positive charge of the surface, thus increasing the sorption of the two negative species SeO 2− 3 and HSeO − 3 . If such a mechanism were involved, since biselenite is the major species in solution between pH 4 and 7.5 and the neutral species H 2 SeO 3 is negligible above pH 4 (pK 1 = 2.50 and pK 2 = 8.17, measured in KNO 3 0.1 M), the adsorption of SeO 2− 3 and HSeO − 3 would normally result in a maximum of sorption down to the lowest pH values, as was observed for several oxides and clays (17)(18)(19)(20)(21)(22).…”