Structural and magnetic properties of the CaFe2 − xMnxO4 solid solution
Abstract
Substitution of Mn for Fe in the orthorhombic compound CaFe2O4 has been achieved by solid-state reactions at 1100 °C in air up to the composition Ca(Fe1.6Mn0.4)O4. The evolution of cell and atomic parameters was determined from X-ray powder data using the Rietveld method. The results show that the presence of the Jahn–Teller ion Mn3+ distorts the Fe1 octahedral site and that Mn most probably occupies the Fe2 site. With increasing Mn content, the magnetism evolves from antiferromagnetic to ferrimagnetic, with Curie temperature (TC) values (194–209 K) well above the Néel temperature of CaFe2O4 (160 K). A correlation between the evolution of TC and the deviation of the Fe2–O–Fe2 angle from 90° is established.