Abstract
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 Fd3̄m. 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
© 2015 by Walter de Gruyter Berlin/Boston
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Articles in the same Issue
- Closure temperatures of intracrystalline ordering in anatectic and metamorphic hercynite, Fe2+Al2O4
- Arsenate substitution in hydroxylapatite: Structural characterization of the Ca5(PxAs1–xO4)3OH solid solution
- The crystal chemical role of Zn in alunite-type minerals: Structure refinements for kintoreite and zincian kintoreite
- Application of precession electron diffraction to the characterization of (021) twinning in pseudo-hexagonal coesite
- Structure, thermodynamic, and transport properties of molten Mg2SiO4: Molecular dynamics simulations and model EOS
- High-pressure behavior of åkermanite and gehlenite and phase stability of the normal structure in melilites
- Synchrotron-based speciation of chromium in an Oxisol from New Caledonia: Importance of secondary Fe-oxyhydroxides
- Meurigite-Na, a new species, and the relationship between phosphofibrite and meurigite
- The role of silver on the stabilization of the incommensurately modulated structure in calaverite, AuTe2
- Hydrogen zoning in zinc-bearing staurolite from a high-P, low-T diasporite (Samos, Greece): A combined EMP-SIMS-FIB-FTIR study
- Dmitryivanovite: A new high-pressure calcium aluminum oxide from the Northwest Africa 470 CH3 chondrite characterized using electron backscatter diffraction analysis
- Crystal chemistry of hydrous forsterite and its vibrational properties up to 41 GPa
- The geothermobarometric potential of tourmaline, based on experimental and natural data
- Inverse spinel structure of Co-doped gahnite
- Advances in understanding the structure of borosilicate glasses: A Raman spectroscopy study
- The occurrence of tetrahedrally coordinated Al and B in tourmaline: An 11B and 27Al MAS NMR study
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- Two types of metamorphic monazite with contrasting La/Nd, Th, and Y signatures in an ultrahigh-pressure metapelite from the Pohorje Mountains, Slovenia: Indications for pressure-dependent REE exchange between apatite and monazite?
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- Letter. Tistarite, Ti2O3, a new refractory mineral from the Allende meteorite
- Letter. Davisite, CaScAlSiO6, a new pyroxene from the Allende meteorite
- Letter. The 4500 cm–1 infrared absorption band in hydrous aluminosilicate glasses is a combination band of the fundamental (Si,Al)-OH and O-H vibrations