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American Mineralogist; May-June; v. 94; no. 5-6; p. 771-776; DOI: 10.2138/am.2009.3173
© 2009 Mineralogical Society of America
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Inverse spinel structure of Co-doped gahnite

Jasminka Popovic1,*, Emilija Tkalcec2, Biserka Grzeta1, Stanislav Kurajica2 and Boris Rakvin3

1 Division of Materials Physics, Ruder Boskovic Institute, P.O. Box 180, HR-10002 Zagreb, Croatia
2 Faculty of Chemical Engineering and Technology, University of Zagreb, Marulicev trg 19, HR-10000 Zagreb, Croatia
3 Division of Physical Chemistry, Ruder Boskovic Institute, P.O. Box 180, HR-10002 Zagreb, Croatia

Correspondence: * E-mail: jpopovic{at}irb.hr

Powder ZnAl2O4 (gahnite) samples doped with 0–100 at% Co were obtained by a sol-gel technique. X-ray powder diffraction was used to characterize the samples. Gahnite samples are cubic with the normal spinel structure, space group FdFormulam. Cobalt doping caused a nonuniform increase of unit-cell parameter. The structure of the gahnite samples was refined by the Rietveld method. The location of Co2+ was determined by EPR spectroscopy. Cobalt doping of gahnite induces the inverse spinel structure at only 4 at% Co, and the inversion parameter increases with Co2+ doping level. Metal-oxide distances in the (Al,Co)O6 octahedra dominantly influence the unit-cell parameter of Co-doped gahnite.

Key Words: Co-doped gahnite • spinel structure • X-ray powder diffraction • Rietveld method







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