The oxidation products of Fe(OH)(2) formed in the presence of Co2+, Cu2+ an
d Cr3+ were characterized by various means. Co2+ and Cu2+ produced pure Fe3
O4 by inhibiting the generation of alpha-FeOOH, whilst Cr3+ promoted the al
pha-FeOOH formation and interfered with the Fe3O4 formation. The Fe3O4 part
icles produced with Co2+ exhibited high Fe2+ content, electrical conductivi
ty and stability to oxidation. Mossbauer spectroscopy demonstrated that the
excess Fe2+ replaced for Fe3+ in B-sites of Fe3O4. A small quantity of met
al Fe formed in addition to Fe3O4 on adding Co2+. (C) 1999 Elsevier Science
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