Study of Features of the Composition, Magnetic, and Crystal Structure of Barium Hexaferrite BaFe12- xTixO19

被引:13
作者
Korovushkin, V. V. [1 ]
Trukhanov, A. V. [1 ,2 ]
Kostishin, V. G. [1 ]
Isaev, I. M. [1 ]
Shchetinin, I. V. [1 ]
Durov, N. M. [1 ]
Mironovich, A. Yu. [1 ]
Minkova, I. O. [1 ]
Astapovich, K. A. [2 ]
机构
[1] Natl Univ Sci & Technol MISIS, Moscow 119049, Russia
[2] Natl Acad Sci Belarus Mat Sci, Sci & Prod Ctr, Minsk 220072, BELARUS
基金
俄罗斯科学基金会;
关键词
hexaferrites; heterovalent substitution; titanium; Mossbauer spectroscopy; magnetic properties; X-ray diffraction; simultaneous thermal analysis; MOSSBAUER; FERRITES;
D O I
10.1134/S1063783420050145
中图分类号
O469 [凝聚态物理学];
学科分类号
070205 ;
摘要
The features of the composition, crystal, and magnetic structure of Ti-substituted barium hexaferrite BaFe12 - xTixO19 (0.25 <= x <= 1.5) are studied by Mossbauer spectroscopy, vibration magnetometry, X-ray diffraction, and simultaneous thermal analysis. Bounded heterovalent isomorphism implemented by the scheme 2Fe(3+) -> Ti4+ + Fe2+ while retaining the charge balance is established when Fe3+ ions are partially substituted with Ti4+ ions. An increase in the 3d-electron density and the presence of Fe2+ in BaFe12 - xTixO19 samples with x = 1.5 is detected by Mossbauer spectroscopy. The heterovalent isomorphic substitution limit is determined to be within 0.75 < x < 1.0. Using Mossbauer spectroscopy and X-ray diffraction, the formation of titanium-contained phases at x = 1.0 whose content increases with the degree of substitution is shown. The data on the preferential distribution of substituent ions (Ti4+) in the barium hexaferrite structure at the 12k and 2b sites are presented.
引用
收藏
页码:891 / 901
页数:11
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