Hydrothermal Formation of Ferrite Spinels

Abstract

The possibility of forming spinel-type ferrites MFe2O4 from M(OH)2 or MO and α-FeO(OH) (goethite) or α-Fe2O3 (hematite) under hydrothermal conditions up to 350° has been investigated experimentally for M = Mg, Ca, Mn, Co, Ni, Cu, and Zn. Formation of MFe2O4 was observed for M = Mn (jacobsite), Co, Ni (trevorite), and Zn (franklinite), and was in general favored by high temperatures, high pH, and the presence of NaNO3 or, especially, NaCl in solution. α-FeO(OH) is more reactive than α-Fe2O3, but generally converts to the latter at 220–260°, independently of pH, in neutral or alkaline media. Interpretation of the results is complicated by the ion-exchanging properties and varying degrees of crystallinity of M(OH)2, and by the tendency of M(OH)2 to decompose to MO or to be oxidized at the higher temperatures. Nevertheless, the order of reactivity M = Co ≥ Mn > Ni > Zn > (Mg, Ca, Cu) in MFe2O4 formation is generally valid. The formation of MFe2O4 is limited by kinetic rather than thermodynamic factors for the various M listed (except Cu).