Magnetic Transformations in Phase-Separated Manganite La0.60Sr0.35Ce0.05Mn0.95Со0.05O3+γ

The results of an experimental study of the magnetic properties of La0.60Sr0.35Ce0.05Mn0.95Со0.05O3+γ polycrystalline manganites produced using ceramic technology are presented. According to X-ray and electron microscopy studies, the samples are single phase, have a rhombohedral structure at 300 K, and are characterized by microdistortions and modulated crystallite structures. At temperatures below 140 K, the process of nucleation of the orthorhombic phase begins, and at 90 K, two phases are detected by X-ray diffraction: orthorhombic (space group Pnma) and rhombohedral (R $$\bar {3}$$ c). Magnetometry reveals three temperatures of ~320, 220, and 130 K, at which the magnetic properties of the material change, the latter being characterized by a decrease in the magnetization of the manganite. Magneto-optical imaging makes it possible to identify these transitions with the appearance of magnetic-phase separation of the material, which is associated with inhomogeneities in the composition and structure, and to study the kinetics of phase nucleation.

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Journal
Journal of Surface Investigation X-ray Synchrotron and Neutron Techniques
Published
2024-12-01
DOI
https://doi.org/10.1134/s1027451024701702
Primary Topic
Magnetic and transport properties of perovskites and related materials
Type
article
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article

Magnetic Transformations in Phase-Separated Manganite La0.60Sr0.35Ce0.05Mn0.95Со0.05O3+γ

A. G. Badelin, V. K. Karpasyuk, L. S. Uspenskaya, R. S. Evstigneev
Journal of Surface Investigation X-ray Synchrotron and Neutron Techniques
Magnetic and transport properties of perovskites and related materials
article

Magnetic Transformations in Phase-Separated Manganite La0.60Sr0.35Ce0.05Mn0.95Со0.05O3+γ

A. G. Badelin, V. K. Karpasyuk, L. S. Uspenskaya, R. S. Evstigneev
article en

Abstract

The results of an experimental study of the magnetic properties of La0.60Sr0.35Ce0.05Mn0.95Со0.05O3+γ polycrystalline manganites produced using ceramic technology are presented. According to X-ray and electron microscopy studies, the samples are single phase, have a rhombohedral structure at 300 K, and are characterized by microdistortions and modulated crystallite structures. At temperatures below 140 K, the process of nucleation of the orthorhombic phase begins, and at 90 K, two phases are detected by X-ray diffraction: orthorhombic (space group Pnma) and rhombohedral (R $$\bar {3}$$ c). Magnetometry reveals three temperatures of ~320, 220, and 130 K, at which the magnetic properties of the material change, the latter being characterized by a decrease in the magnetization of the manganite. Magneto-optical imaging makes it possible to identify these transitions with the appearance of magnetic-phase separation of the material, which is associated with inhomogeneities in the composition and structure, and to study the kinetics of phase nucleation.

Journal of Surface Investigation X-ray Synchrotron and Neutron TechniquesVol. 18(6)
Astrakhan Tatischev State University (RU), Osipyan Institute of Solid State Physics RAS (RU)
Openalex Percentile: Top 84%
Magnetic and transport properties of perovskites and related materials
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