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The formation of the magnetic structure of charge ordered 3D and layered manganites: The crucial role of the orbital structure. / Gontchar, L.; Nikiforov, A.
In: Czechoslovak Journal of Physics, Vol. 52, No. S1, 2002, p. A245-A248.

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@article{d929bcc0f2514f0e859c1de97be179fb,
title = "The formation of the magnetic structure of charge ordered 3D and layered manganites: The crucial role of the orbital structure",
abstract = "The manganites with general formulae R0.5A0.5MnO3 (3D-manganite), R0.5A1.5MnO4 (layered manganite), and RA2Mn2O7 (bilayer manganite), where R3+ is rare-earth ion, A2+ 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.",
author = "L. Gontchar and A. Nikiforov",
year = "2002",
doi = "10.1007/s10582-002-0059-3",
language = "English",
volume = "52",
pages = "A245--A248",
journal = "Czechoslovak Journal of Physics",
issn = "0011-4626",
publisher = "Springer Netherlands",
number = "S1",

}

RIS

TY - JOUR

T1 - The formation of the magnetic structure of charge ordered 3D and layered manganites: The crucial role of the orbital structure

AU - Gontchar, L.

AU - Nikiforov, A.

PY - 2002

Y1 - 2002

N2 - The manganites with general formulae R0.5A0.5MnO3 (3D-manganite), R0.5A1.5MnO4 (layered manganite), and RA2Mn2O7 (bilayer manganite), where R3+ is rare-earth ion, A2+ 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.

AB - The manganites with general formulae R0.5A0.5MnO3 (3D-manganite), R0.5A1.5MnO4 (layered manganite), and RA2Mn2O7 (bilayer manganite), where R3+ is rare-earth ion, A2+ 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.

UR - https://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcAuth=tsmetrics&SrcApp=tsm_test&DestApp=WOS_CPL&DestLinkType=FullRecord&KeyUT=000175031700059

UR - http://www.scopus.com/inward/record.url?partnerID=8YFLogxK&scp=0036948716

U2 - 10.1007/s10582-002-0059-3

DO - 10.1007/s10582-002-0059-3

M3 - Conference article

VL - 52

SP - A245-A248

JO - Czechoslovak Journal of Physics

JF - Czechoslovak Journal of Physics

SN - 0011-4626

IS - S1

ER -

ID: 43770770