Creation and Magnetic Study of Ferrites with Magnetoplumbite Structure Multisubstituted by Al3+, Cr3+, Ga3+, and In3+ Cations

被引:23
|
作者
Zhivulin, Vladimir E. [1 ]
Sherstyuk, Daria P. [1 ]
Zaitseva, Olga, V [1 ]
Cherkasova, Natalia A. [1 ]
Vinnik, Denis A. [1 ]
Taskaev, Sergey, V [2 ]
Trofimov, Evgeny A. [1 ]
Trukhanov, Sergei, V [3 ]
Latushka, Siarhei, I [3 ]
Tishkevich, Daria, I [1 ,3 ]
Zubar, Tatiana, I [1 ,3 ]
Trukhanov, Alex, V [1 ,3 ,4 ]
机构
[1] South Ural State Univ, Lab Single Crystal Growth, 76 Lenin Av, Chelyabinsk 454080, Russia
[2] Chelyabinsk State Univ, Fac Phys, 129 Bratiev Kashirinykh St, Chelyabinsk 454001, Russia
[3] NAS Belarus, SSPA Sci & Pract Mat Res Ctr, Lab Magnet Films Phys, 19 P Brovki Str, Minsk 220072, BELARUS
[4] Natl Univ Sci & Technol MISiS, Dept Elect Mat Technol, Moscow 119049, Russia
基金
俄罗斯科学基金会;
关键词
M-type hexaferrites; structure; high-entropy oxides; magnetization; anisotropy; BA-SR HEXAFERRITES; CRYSTAL-STRUCTURE; EXCHANGE INTERACTIONS; MICROWAVE PROPERTIES; ENTROPY STATE; CO; PERFORMANCE; ANISOTROPY; EVOLUTION; FREQUENCY;
D O I
10.3390/nano12081306
中图分类号
O6 [化学];
学科分类号
0703 ;
摘要
Multisubstituted barium ferrites with a magnetoplumbite structure were obtained by the method of solid-phase reactions with ferritization and pre-firing. Three-charged, mainly diamagnetic cations Al3+, Cr3+, Ga3+, and In3+ were chosen as substituents for the Fe3+ iron cations, the proportion of which in solid solutions did not exceed 50%. The values of the configurational mixing entropy were calculated for all the compositions. A slight deviation of the chemical composition of the obtained solid solutions from the nominal value was established by the energy-dispersive X-ray spectroscopy method. The phase purity and values of the unit cell parameters were refined from X-ray scattering data using full-profile analysis in the Rietveld method. A non-monotonic behavior of the unit cell parameters as a function of the B-sub-lattice average ionic radius of the magnetoplumbite structure was found. A minimum unit cell volume of similar to 667.15 angstrom(3) was found for the composition BaFe6.11Al1.56Cr2.17Ga2.16O19 with a B-sub-lattice average ionic radius of similar to 7.449 angstrom. The average crystallite size varied within 5.5-6.5 mu m. The temperature and field dependencies of the magnetization have been measured. The values of the saturation magnetization, residual magnetization, hysteresis loop squareness, and coercivity at 50 K and 300 K were extracted from the experimental data. Using the Law of Approach to Saturation, the magnetic crystallographic anisotropy coefficient and anisotropy field were calculated. Multisubstitution leads to a significant decrease in such magnetic parameters as the magnetic ordering temperature and spontaneous magnetization at both temperatures. The maximum magnetic ordering temperature of similar to 297.7 K was found for the composition BaFe5.84Ga6.19O19 with a B-sub-lattice average ionic radius of similar to 7.586 angstrom in a field of 500 Oe. A maximum saturation magnetization of similar to 24.7 emu/g was found for the composition BaFe5.84Ga6.19O19 with a B-sub-lattice average ionic radius of similar to 7.586 angstrom at 50 K. A maximum hysteresis loop squareness of similar to 0.72 was found for the composition BaFe6.11Al1.56Cr2.17Ga2.16O19 with an average ionic radius of similar to 7.449 angstrom at 50 K. A maximum magnetic crystallographic anisotropy coefficient of similar to 2.09 x 10(5) Erg/g was found for the composition BaFe6.19Al1.25Cr1.57Ga1.74In1.26O19 with a B-sub-lattice average ionic radius of similar to 7.706 angstrom at 50 K. The frustrated magnetic state including the nano-sized clusters with an average diameter in the range of 50-200 nm was established from the results of measuring the ZFC and FC temperature magnetizations. The interpretation of the obtained experimental data is carried out taking into account the increased stability of high-entropy phases and regular changes in the intensity of the Fe3+(Al3+, Cr3+, Ga3+, In3+)-O2--Fe3+(Al3+, Cr3+, Ga3+, In3+) indirect superexchange interactions as a result of magnetic dilution of the iron sub-lattice in the magnetoplumbite structure.
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页数:18
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