Structural studies of charge disproportionation and magnetic order inCaFeO3

Abstract
The crystal and magnetic structures of CaFeO3 have been determined at 300 and 15 K using synchrotron x-ray and neutron powder-diffraction techniques. At 300 K, CaFeO3 adopts the GdFeO3 struture, space group Pbnm with unit-cell dimensions a=5.32630(4), b=5.35270(4), and c=7.53986(6)Å. This structure is distorted from the ideal perovskite structure by tilting of the FeO6 octahedra about [110] and [001]. The average Fe-O distance is 1.922(2) Å, and the Fe-O-Fe angles are 158.4(2)° and 158.1(1)°. At 15 K the crystal structure belongs to space group P21/n with a=5.31182(3), b=5.34775(4), c=7.52058(5)Å and β=90.065(1)°, and contains two distinct Fe sites. The average Fe-O bond length is 1.872(6) Å about the one iron site, and 1.974(6) Å about the second site, with bond valence sums of 4.58 and 3.48, respectively. This provides quantitative evidence for charge disproportionation, 2Fe4+Fe3++Fe5+, at low temperature. The temperature evolution of the lattice parameters indicates a second- (or higher-) order phase transition from the orthorhombic charge-delocalized state to the monoclinic charge-disproportionated state, beginning just below room temperature. The magnetic structure at 15 K is incommensurate, having a modulation vector [δ,0,δ] with δ ∼0.322, corresponding to one of the 〈111〉 directions in the pseudocubic cell. A reasonable fit to the magnetic intensities is obtained with the recently proposed screw spiral structure [S. Kawasaki et al., J. Phys. Soc. Jpn. 67, 1529 (1998)], with Fe moments of 3.5 and 2.5μB, respectively. However, a comparable fit is given by a sinusoidal amplitude-modulated model in which the Fe moments are directed along [010], which leaves open the possibility that the true magnetic structure may be intermediate between the spiral and sinusoidal models (a fan structure).