“…Iron phyllosilicates or iron-containing clay minerals have been studied for their oxidation-reduction reactions Heller-Kallai, 1976a, 1976b;Russell et al, 1979;Stucki et al, 1984aStucki et al, , 1984bWu et al, 1989), their catalytic and adsorption properties (Fanale and Cannon, 1979;Heller-Kallai et al, 1984;Wang and Huang, 1989), and their magnetic properties (Coey et aL, 1982;Gangas et al, 1985). Because iron has two common oxidation states (ferrous and ferric), and a ferric ion shows two common coordination numbers (fourfold and sixfold), the crystallization of iron silicates and iron-containing phyllosilicates is complex and difficult to control (Roy and Roy, 1954;Harder, 1973Harder, , 1977Harder, , 1989Petit and Decarreau, 1990).…”