Antiferromagnet–ferromagnet transition in the cobaltites
Магнетизм
DOI (Low Temperature Physics):
https://doi.org/10.1063/1.4736615
Ключові слова:
antiferromagnet, oxygen vacancies, spin state transition, layered perovskite.Анотація
The three series oxygen-deficient cobaltites La0.5Ba0.5CoO3–δ, LnBaCo2O5.5 and Sr2YCo4O10.5 have been studied. It has been shown that La0.5Ba0.5CoO3 is an insulating ferromagnet whereas La0.5Ba0.5CoO2.75 is a pure antiferromagnet in which the oxygen vacancies are disordered. The oxygen-vacancies ordering leads to appearance of the ferromagnetic component apparently due to a formation of the noncollinear magnetic structure. The antiferromagnet–“ferromagnet” transition is accompanied by a giant magnetoresistance. It is suggested that in the ferromagnetic oxidized compounds Co3+ and Co4+ ions adopt intermediate spin state whereas for antiferromagnetic (Co4+-free) compositions Co3+ ions have high-spin state (pyramids CoO5) and dominant low-spin state (octahedra CoO6). In both ferromagnetic and antiferromagnetic compounds the superexchange via oxygen plays an essential role in a formation of the magnetic properties.
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Опубліковано
2012-05-17
Як цитувати
(1)
I.O. Troyanchuk, M.V. Bushinsky, D.V. Karpinsky, and V.A. Sirenko, Antiferromagnet–ferromagnet transition in the cobaltites: Магнетизм, Low Temp. Phys. 38, (2012) [Fiz. Nizk. Temp. 38, 833-841, (2012)] DOI: https://doi.org/10.1063/1.4736615.
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