Mossbauer Study of Fe2+ in the Low Temperature Phase of Fe3O4
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- Umemura Shizuo
- Department of Physics, Faculty of Science, The University of Tokyo
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- Iida Shuichi
- Department of Physics, Faculty of Science, The University of Tokyo
書誌事項
- タイトル別名
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- Mössbauer Study of Fe<SUP>2+</SUP> in the Low Temperature Phase of Fe<SUB>3</SUB>O<SUB>4</SUB>
- Mossbauer Study of Fe2 + in the Low Tem
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Mössbauer spectra of the low temperature phase of single crystal magnetite were measured with a magnetic field along various directions in (1\bar10) plane after cooled in the magnetic field along [112]. Measured spectra were found to be sensitive to the direction of the applied magnetic field. As the result of detailed analysis two kinds of Fe2+ ions (Fe2+–I and II) were clearly recognized and the principal Z-axis of EFG was found to be along [100] or [010] for Fe2+–I and [001] for Fe2+–II. Since the observed anisotropy of the internal magnetic field is well described by EFG observed, angular momentum of each Fe2+ ion is suggested to be quenched.
収録刊行物
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- Ｊｏｕｒｎａｌ ｏｆ ｔｈｅ Ｐｈｙｓｉｃａｌ Ｓｏｃｉｅｔｙ ｏｆ Ｊａｐａｎ
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Ｊｏｕｒｎａｌ ｏｆ ｔｈｅ Ｐｈｙｓｉｃａｌ Ｓｏｃｉｅｔｙ ｏｆ Ｊａｐａｎ 47 (2), 458-467, 1979
一般社団法人 日本物理学会
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詳細情報 詳細情報について
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- CRID
- 1390001204185423104
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- NII論文ID
- 210000088280
- 110001964647
- 130003896031
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- NII書誌ID
- AA00704814
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- BIBCODE
- 1979JPSJ...47..458U
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- COI
- 1:CAS:528:DyaE1MXlsVyqurc%3D
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- ISSN
- 13474073
- 00319015
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- NDL書誌ID
- 2059332
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- 本文言語コード
- en
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- データソース種別
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- JaLC
- NDL
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- 使用不可