Abstract
Powder neutron diffraction and magnetometry studies have been conducted to investigate the crystallographic and magnetic structure of . The compound stabilizes in the orthorhombic crystal symmetry in the measured temperature range of 5 to 380 K, with a transition to antiferromagnetic order at K. The spin cycloid present for BiFeO is found to be absent with 50% Mn cation substitution, leading to -type antiferromagnetic order with an enhanced out-of-plane canted ferromagnetic component, evident from measurable weak-ferromagnetic hysteresis. Structural modifications do not solely explain this behavior, indicating that modified electron exchange interactions must be taken into account. A classical spin simulation was developed to investigate the effect of random substitution in a disordered pseudocubic perovskite. The calculations took into account the nearest-neighbor, next-nearest-neighbor, and Dzyaloshinskii-Moriya interactions, along with the local spin anisotropy. Using this framework to extend the established Hamiltonian model for BiFeO, we show that only certain types of perturbations at a magnetic defect and the surrounding molecular fields trigger a simultaneous collapse of cycloidal order and the emergence of the long-range weak-ferromagnetic component. By adopting values for the Mn molecular fields appropriate for MnO ( rare earth), simulations of BiMnFe exhibit the key magnetic properties of our experimental observations.
3 More- Received 7 November 2013
- Revised 6 March 2014
DOI:https://doi.org/10.1103/PhysRevB.89.144422
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