{"title":"Influence of Al or Cr substitution on structure and magnetic properties of barium hexaferrites prepared by hydrothermal method","authors":"A.Yu. Mironovich , V.G. Kostishin , H.I. Al-Khafaji , E.S. Savchenko , A.I. Ril , R.I. Shakirzyanov , M.A. Sysoev","doi":"10.1016/j.jmmm.2025.172896","DOIUrl":null,"url":null,"abstract":"<div><div>In this study, BaFe<sub>12-x</sub>Cr<sub>x</sub>O<sub>19</sub> and BaFe<sub>12-x</sub>Al<sub>x</sub>O<sub>19</sub> (x = 0.0, 0.1, 0.3 and 0.4) powders were prepared by a hydrothermal method followed by annealing. The incorporation of Cr and Al in the hexaferrite structure was confirmed by elemental analysis and the results of Rietveld refinement of X-ray diffraction patterns, which revealed a decrease in the lattice volume with increasing x. Based on Mössbauer spectroscopy and magnetic measurements, the lack of Fe<sup>3+</sup> was observed in the 12k site for BaFe<sub>12-x</sub>Al<sub>x</sub>O<sub>19</sub> samples and in the 12k, 4f<sub>1</sub> and 4f<sub>2</sub> sites for BaFe<sub>12-x</sub>Cr<sub>x</sub>O<sub>19</sub> samples. With increasing substitution, the magnetic parameters of Al-substituted hexaferrites varied slightly, possibly due to limited incorporation of Al<sup>3+</sup>. At the same time, a significant decrease in H<sub>c</sub> was observed for Cr-substituted samples (5629 Oe for x = 0 and 2092 Oe for x = 0.4). Electron microscopy revealed that the substitution of Fe<sup>3+</sup> with Al<sup>3+</sup> had no significant effect on crystallite morphology. The substitution of Fe<sup>3+</sup> with Cr<sup>3+</sup> leads to the thinning and widening of the plate-like grains of hexaferrite. This could be one of the reasons for the decrease in coercivity.</div></div>","PeriodicalId":366,"journal":{"name":"Journal of Magnetism and Magnetic Materials","volume":"619 ","pages":"Article 172896"},"PeriodicalIF":2.5000,"publicationDate":"2025-02-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Magnetism and Magnetic Materials","FirstCategoryId":"88","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0304885325001271","RegionNum":3,"RegionCategory":"材料科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"MATERIALS SCIENCE, MULTIDISCIPLINARY","Score":null,"Total":0}
引用次数: 0
Abstract
In this study, BaFe12-xCrxO19 and BaFe12-xAlxO19 (x = 0.0, 0.1, 0.3 and 0.4) powders were prepared by a hydrothermal method followed by annealing. The incorporation of Cr and Al in the hexaferrite structure was confirmed by elemental analysis and the results of Rietveld refinement of X-ray diffraction patterns, which revealed a decrease in the lattice volume with increasing x. Based on Mössbauer spectroscopy and magnetic measurements, the lack of Fe3+ was observed in the 12k site for BaFe12-xAlxO19 samples and in the 12k, 4f1 and 4f2 sites for BaFe12-xCrxO19 samples. With increasing substitution, the magnetic parameters of Al-substituted hexaferrites varied slightly, possibly due to limited incorporation of Al3+. At the same time, a significant decrease in Hc was observed for Cr-substituted samples (5629 Oe for x = 0 and 2092 Oe for x = 0.4). Electron microscopy revealed that the substitution of Fe3+ with Al3+ had no significant effect on crystallite morphology. The substitution of Fe3+ with Cr3+ leads to the thinning and widening of the plate-like grains of hexaferrite. This could be one of the reasons for the decrease in coercivity.
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