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Direct observation of magnetic Friedel oscillation at Fe(001) surface
https://repo.qst.go.jp/records/84765
https://repo.qst.go.jp/records/847652d6a671a-d1fe-4723-9374-af1c256877b9
Item type | 学術雑誌論文 / Journal Article(1) | |||||
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公開日 | 2021-09-01 | |||||
タイトル | ||||||
タイトル | Direct observation of magnetic Friedel oscillation at Fe(001) surface | |||||
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 | |||||
アクセス権 | ||||||
アクセス権 | metadata only access | |||||
アクセス権URI | http://purl.org/coar/access_right/c_14cb | |||||
著者 |
Takaya, Mitsui
× Takaya, Mitsui× Seiji, Sakai× Songtian, Li× Tetsuro, Ueno× Tetsu, Watanuki× Kobayashi, Yasuhiro× Masuda, Ryo× Makoto, Seto× Akai, Hisazumi× Takaya, Mitsui× Seiji, Sakai× Songtian, Li× Tetsuro, Ueno× Tetsu, Watanuki× Makoto, Seto |
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抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | Surface magnetism of Fe (001) was investigated by the in situ iron-57 probe layer method with a synchrotron Mössbauer source. The observed layer-by-layer internal hyperfine field shows a marked reduction at the surface and an oscillatory behavior with increasing depth in the individual layers below the surface. The calculated layer-by-layer hyperfine interactions (hyperfine field, isomer shift, and quadrupole shift) were consistent with the experimental results. The results give direct evidence for the magnetic Friedel oscillations, penetrating several layers from the Fe (001) surface. | |||||
書誌情報 |
Hyperfine Interactions 巻 242, p. 37, 発行日 2021-11 |
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出版者 | ||||||
出版者 | Springer Nature | |||||
ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 0304-3843 | |||||
DOI | ||||||
識別子タイプ | DOI | |||||
関連識別子 | 10.1007/s10751-021-01772-0 | |||||
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識別子タイプ | DOI | |||||
関連識別子 | https://doi.org/10.1007/s10751-021-01772-0 |