Magnetic and dipole moments in indium doped barium hexaferrites
Creators
- 1. SSPA "Scientific and practical materials research centre of NAS of Belarus", 220072 Minsk, P. Brovki str., 19 (Belarus)
- 2. South Ural State University, 454080 Chelyabinsk, Lenin Prospect, 76 (Russian Federation)
- 3. National University of Science and Technology MISiS, 119049 Moscow, Leninsky Prospekt, 4 (Russian Federation)
- 4. Donetsk Institute of Physics and Technology named after O.O. Galkin of the NAS of Ukraine, Prospect Nauky, 46, Kyiv 03680 (Ukraine)
- 5. Joint Institute for Nuclear Research, 141980 Dubna, Joliot-Curie str., 6 (Russian Federation)
Description
Highlights: • Structure vs. temperature for BaFe12−xInxO19 x = 0.1, 1.2 was investigated. • Atomic coordinates and lattice parameters were Rietveld refined. • Exchange interactions vs. structure were investigated. • Magnetic and dipole moments at different position per iron ion were defined. • Spontaneous polarization for these compositions was established at 300 K. Crystal and magnetic structure of the doped BaFe12−xInxO19 samples were refined by the results of investigations using high resolution neutron powder diffraction and vibration sample magnetometry at different temperatures. The refinements were realized in frame of two space groups. The P63/mmc (No 194) centrosymmetric nonpolar and P63mc (No 186) noncentrosymmetric polar space groups were used. The unit cell parameters, ionic coordinates, thermal isotropic factors, occupation positions, bond lengths and bond angles, microstrain values were established. The magnetic and dipole moments were also defined. It is established that the In3+ cations may be located only in the Fe1 – 2a and Fe2 – 2b crystallographic positions with equal probability for the sample with lowest substitution level x = 0.1. At the x = 1.2 substitution level about half of the In3+ cations occupies the Fe5 – 12 k positions. For the last sample the remaining half of the In3+ cations is equiprobably located in the Fe1 – 2a and Fe2 – 2b positions. The spontaneous polarization was established for these compositions at 300 K. It is studied the influence of the type of substitutive cation and structural parameters on the Fe3+(i) – O2− – Fe3+(j) (i, j = 1, 2, 3, 4, 5) indirect superexchange interactions with temperature. With substitution level increase the superexchange interactions between the magnetic positions inside and outside the sublattices are broken which leads to a decrease in the value of their magnetic moments.
Availability note (English)
Available from http://dx.doi.org/10.1016/j.jmmm.2018.02.078Additional details
Identifiers
- DOI
- 10.1016/j.jmmm.2018.02.078;
- PII
- S0304885317338416;
Publishing Information
- Journal Title
- Journal of Magnetism and Magnetic Materials
- Journal Volume
- 457
- Journal Page Range
- p. 83-96
- ISSN
- 0304-8853
- CODEN
- JMMMDC
INIS
- Country of Publication
- Netherlands
- Country of Input or Organization
- International Atomic Energy Agency (IAEA)
- INIS RN
- 53034638
- Subject category
- S36: MATERIALS SCIENCE;
- Descriptors DEI
- BARIUM; BOND ANGLE; BOND LENGTHS; CRYSTALLOGRAPHY; CRYSTALS; DOPED MATERIALS; EXCHANGE INTERACTIONS; FERRITES; HEXAGONAL LATTICES; INDIUM IONS; IRON IONS; LATTICE PARAMETERS; MAGNETIC MOMENTS; NEUTRON DIFFRACTION; POLARIZATION; SPACE GROUPS
- Descriptors DEC
- ALKALINE EARTH METALS; CHARGED PARTICLES; COHERENT SCATTERING; CRYSTAL LATTICES; CRYSTAL STRUCTURE; DIFFRACTION; DIMENSIONS; ELEMENTS; FERRIMAGNETIC MATERIALS; INTERACTIONS; IONS; IRON COMPOUNDS; LENGTH; MAGNETIC MATERIALS; MATERIALS; METALS; OXYGEN COMPOUNDS; SCATTERING; SYMMETRY GROUPS; THREE-DIMENSIONAL LATTICES; TRANSITION ELEMENT COMPOUNDS
Optional Information
- Copyright
- Copyright (c) 2018 Elsevier B.V. All rights reserved.