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.