Ja. Alonso et al., Preparation, crystal structure, and magnetic and magnetotransport properties of the double perovskite Ca2FeMoO6, CHEM MATER, 12(1), 2000, pp. 161-168
Ca2FeMoO6 perovskite has been prepared in polycrystalline form by controlle
d reduction of previously decomposed citrate precursors. This material has
been studied by X-ray and neutron powder diffraction (NPD), scanning electr
on microscopy, thermal analysis, and magnetic and magnetotransport measurem
ents. The crystal structure is monoclinic, space group P2(1)/n, with a = 5.
4150(1), b = 5.5224(1.), c = 7.7066(2) Angstrom, and beta = 89.969(8)degree
s at room temperature (RT). The crystal contains alternating FeO6 and MoO6
octahedra, considerably tilted due to the relatively small size of the Ca2 cations. Low-temperature (2 K) NPD data show evidence for a ferrimagnetic
coupling between the Fe3+ and Mo5+ sublattices, with ordered magnetic momen
ts of 3.2(1) and -0.76(6) mu(B), respectively. The Curie temperature is 380
K. Both magnetism and transport indicate a large component of itinerancy f
or downspin Feta, electrons. The carrier density measured by the Hall effec
t is 0.031 holes per formula unit at 100 K. A magnetoresistance of 80% has
been observed at RT for 9T, significantly larger than that reported for oth
er A(2)FeMoO(6) perovskites, A = Sr, Ba.