The magnetic feature of a faceted double perovskite Nd2FeCrO6, synthesized by the solid-state reaction method, is investigated. Nd2FeCrO6 exhibits an orthorhombic structure with Fe and Cr ions in 3+ oxidation states. These ions are shifted away from the centre of FeO6/CrO6 octahedral sublattice, indicating distortion. The Isomer shift in the Mössbauer spectrum correlates with the 3+ oxidation state of Fe, and the existence of magnetic fraction leading to magnetic frustration in Nd2FeCrO6 is established. The superexchange Fe3+ -O- Fe3+ and Cr3+ -O- Cr3+ interactions favour antiferromagnetic ordering, while Fe3+ -O- Cr3+ interactions promote weak ferromagnetic ordering. The low-temperature magnetic study traces negative magnetization in FC mode for the applied external fields of 100Oe and 1000Oe, attributed to the paramagnetic effect of Nd3+ ions aligning antiparallel to the ferromagnetic component of the |Fe+Cr| sublattice internal field. Also, the negative magnetization of FC mode is found to be field-dependent. The deviation of the B2g phonon around the magnetic ordering temperature TN~250K provides evidence of spin-phonon coupling. This variation in the B2g phonon is analysed in terms of the full width at half maximum (FWHM), peak position, intensity, and height.
Read full abstract