AN X-RAY-POWDER DIFFRACTION STUDY OF SYNTHETIC (FE,MN)(2)TIO4 SPINEL

Citation
Ik. Sedler et al., AN X-RAY-POWDER DIFFRACTION STUDY OF SYNTHETIC (FE,MN)(2)TIO4 SPINEL, European journal of mineralogy, 6(6), 1994, pp. 873-885
Citations number
39
Categorie Soggetti
Mineralogy
ISSN journal
09351221
Volume
6
Issue
6
Year of publication
1994
Pages
873 - 885
Database
ISI
SICI code
0935-1221(1994)6:6<873:AXDSOS>2.0.ZU;2-1
Abstract
The (Fe,Mn)(2)TiO4 spinel solid solution was synthesized in steps of 1 0 mole % at 950 degrees C, 1 bar total pressure and log f(O2) of -16.3 0. Electron microprobe analysis indicates that all synthesized Fe-Mn t itanate spinels are homogeneous but contain an additional small magnet ite component in solid solution. The magnetite content is 6.8 mole % f or ulvospinel and decreases with increasing manganese. As stoichiometr ic (Fe,Mn)(2)TiO4 oxide mixtures were used as starting material, addit ional Fe-Mn ilmenite occurs in the run products as a result of the Fe3 O4 solution in spinel. Powder X-ray diffraction data, collected in the range 15-160 degrees 2 theta with CuK alpha radiation, indicate that the solid solution is continuous at 950 degrees C with all members hav ing the cubic crystal structure (space group Fd3m). Unit cell dimensio ns, oxygen positional factors, and isotropic displacement factors for Fe-Mn ulvospinel members were refined using the Rietveld method. The u nit cell dimension increases linearly from 8.53374(8) Angstrom for ulv ospinel to 8.68063(7) A for the Mn-endmember. The degree of inversion was estimated from X-ray powder data in three different ways, of which the method of optimizing the Rg factor in the Rietveld refinement pro cedure is considered as the most accurate one. The results indicate th at the whole Fe-Mn ulvospinel solid solution is 82-92 % inverse at 950 degrees C. A change in degree of inversion with composition is not ob vious from the data. The oxygen parameter u ranges from 0.2601(2) to 0 .2615(2) within the solid solution. Calculated tetrahedral-oxygen bond lengths increase from 1.999(3) Angstrom for Fe2TiO4 to 2.046(3) Angst rom for Mn2TiO4, whereas the octahedral-oxygen bond lengths increase f rom 2.050(2) Angstrom to 2.079(2) Angstrom with X(Mn). Estimated effec tive ionic radii of Fe2+ and Mn2+ in spinel are slightly larger in IV- fold coordination and slightly smaller in VI-fold coordination than va lues reported in previous studies.