Abstract
The manganites with general formulae R 0.5 A 0.5 MnO 3 (3D-manganite), R 0.5 A 1.5 MnO 4 (layered manganite), and RA 2 Mn 2 O 7 (bilayer manganite) where R 3+ is rare-earth ion, A 2+ is alkaline-earth ion, are known as charge ordered compounds at low temperatures with some R and A. In present work, it is shown how the charge ordering and crystal structure form the orbital and magnetic ones. The model of orbitally-dependent superexchange and single-ion anisotropy is used. Also we assume an ideal insulating state of the crystals. The model presented in this work allows to explain the CE- and A- magnetic structures in the terms of charge and orbital structures.
Similar content being viewed by others
References
F. Damay, Z. Jirak, M. Hervieu et al.: JMMM 190 (1998) 221.
P. G. Radaelli, D. E. Cox, M. Marezio et al.: Phys. Rev. B 55 (1997) 3015; J. Blasco, J. Garcia, J. M. de Teresa et al.,: J. Phys. Condens. Matter 9 (1997) 10321.
B. J. Sterblieb, J. P. Hill, U. C. Wildgruber et al.: Phys. Rev. Lett. 76 (1996) 2169.
C. D. Ling, J. E. Millburn, J. F. Mitchell et al.: Phys. Rev. B 62 (2000) 15096.
L. E. Gontchar, A. E. Nikiforov, S. E. Popov: JMMM 223 (2001) 175.
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Gontchar, L.E., Nikiforov, A.E. The formation of the magnetic structure of charge ordered 3D and layered manganites: The crucial role of the orbital structure. Czech J Phys 52 (Suppl 1), A245–A248 (2002). https://doi.org/10.1007/s10582-002-0059-3
Received:
Accepted:
Issue Date:
DOI: https://doi.org/10.1007/s10582-002-0059-3