“…A large number of these studies have shown that metal ions sorb to these oxides through innersphere complexes: Cr(III) to goethite and ferrihydrite (18); Cd to a "two-line ferrihydrite" type of hydrous ferric oxide and to goethite (6); selenate to two-line ferrihydrite and goethite (5); U(VI) to ferrihydrite (19); As(V) and Cr(VI) to goethite (20); Zn to goethite (21); Pb to goethite (22)(23)(24) and to hematite (22); Hg(II) to goethite (25); and Cu and Pb to two-line ferrihydrite (17). In contrast, other studies of iron oxide systems report outersphere types of adsorption mechanisms, where the adsorbate ions retain their waters of hydration; these include ZnEDTA sorption to goethite (21), Sr sorption to HFO (26), PbEDTA sorption to goethite (27), and Sr sorption to goethite (28).…”