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Structural properties of magnetite under high pressure studied by Mossbauer spectroscopy
https://sucra.repo.nii.ac.jp/records/12969
https://sucra.repo.nii.ac.jp/records/129695ad0adcd-f321-4d1a-bdad-c8b08cb846dc
名前 / ファイル | ライセンス | アクション |
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A1002312.pdf (88.8 kB)
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Item type | 学術雑誌論文 / Journal Article(1) | |||||
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公開日 | 2007-11-27 | |||||
タイトル | ||||||
タイトル | Structural properties of magnetite under high pressure studied by Mossbauer spectroscopy | |||||
言語 | ||||||
言語 | eng | |||||
資源タイプ | ||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||
資源タイプ | journal article | |||||
著者 |
Kobayashi, Hisao
× Kobayashi, Hisao× Isogai, Ichiro× Kamimura, Takashi× Hamada, Noriaki× Onodera, Hideya× Todo, Sakae× 毛利, 信男 |
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著者 ローマ字 | ||||||
Kobayashi, Hisao | ||||||
著者 ローマ字 | ||||||
Isogai, Ichiro | ||||||
著者 ローマ字 | ||||||
Kamimura, Takashi | ||||||
著者 ローマ字 | ||||||
Hamada, Noriaki | ||||||
著者 ローマ字 | ||||||
Onodera, Hideya | ||||||
著者 ローマ字 | ||||||
Todo, Sakae | ||||||
著者 ローマ字 | ||||||
Mori, Nobuo | ||||||
著者 所属 | ||||||
著者 所属 | ||||||
著者 所属 | ||||||
著者 所属 | ||||||
著者 所属 | ||||||
著者 所属 | ||||||
著者 所属 | ||||||
埼玉大学 | ||||||
著者 所属(別言語) | ||||||
著者 所属(別言語) | ||||||
著者 所属(別言語) | ||||||
著者 所属(別言語) | ||||||
著者 所属(別言語) | ||||||
著者 所属(別言語) | ||||||
著者 所属(別言語) | ||||||
Department of Physics, Saitama University, Saitama | ||||||
書誌情報 |
PHYSICAL REVIEW B 巻 73, 号 10, p. 104110-1-104110-5, 発行日 2006 |
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年月次 | ||||||
2006-3 | ||||||
出版者名 | ||||||
出版者 | American Physical Society | |||||
ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 10980121 | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | We have measured the Mossbauer spectra of magnetite (Fe3O4) under a pressure of up to 18 GPa at room temperature using nonenriched high-quality samples. An analysis of the observed Mossbauer spectra confirms that Fe3O4 does not undergo a magnetic or crystalline structural transition up to 18 GPa at room temperature. In the pressure dependences of the refined hyperfine interaction parameters, however, small but distinct anomalies are found at 7.0 GPa in the center shifts of two crystallographically nonequivalent Fe sites, which are caused by the discontinuous decrease of an oxygen internal coordinate in the cubic inverse spinel structure. We believe that the pressure-induced discontinuous change of the Fe-O bond length is related to the absence of a metal-insulator transition above 7.5 GPa. | |||||
注記 | ||||||
内容記述タイプ | Other | |||||
内容記述 | 出版社版 | |||||
資源タイプ | ||||||
内容記述タイプ | Other | |||||
内容記述 | text | |||||
フォーマット | ||||||
内容記述タイプ | Other | |||||
内容記述 | application/pdf | |||||
作成日 | ||||||
日付 | 2007-11-27 | |||||
日付タイプ | Created | |||||
アイテムID | ||||||
A1002312 |