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  1. 原著論文

Magnetic and spin transitions in wüstite: A synchrotron Mössbauer spectroscopic study

https://repo.qst.go.jp/records/47980
https://repo.qst.go.jp/records/47980
9df585a9-b291-4de5-bcb6-245524be3e04
Item type 学術雑誌論文 / Journal Article(1)
公開日 2017-05-23
タイトル
タイトル Magnetic and spin transitions in wüstite: A synchrotron Mössbauer spectroscopic study
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 Hamada, Maki

× Hamada, Maki

WEKO 481639

Hamada, Maki

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Kamada, Seiji

× Kamada, Seiji

WEKO 481640

Kamada, Seiji

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Ohtani, Eiji

× Ohtani, Eiji

WEKO 481641

Ohtani, Eiji

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Mitsui, Takaya

× Mitsui, Takaya

WEKO 481642

Mitsui, Takaya

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Masuda, Ryo

× Masuda, Ryo

WEKO 481643

Masuda, Ryo

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Sakamaki, Tatsuya

× Sakamaki, Tatsuya

WEKO 481644

Sakamaki, Tatsuya

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Suzuki, Nanami

× Suzuki, Nanami

WEKO 481645

Suzuki, Nanami

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Maeda, Fumiya

× Maeda, Fumiya

WEKO 481646

Maeda, Fumiya

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Akasaka, Masahide

× Akasaka, Masahide

WEKO 481647

Akasaka, Masahide

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三井 隆也

× 三井 隆也

WEKO 481648

en 三井 隆也

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抄録
内容記述タイプ Abstract
内容記述 This is a Mossbauer study of wustite at pressures above 200 GPa using synchrotron Mossbauer spectroscopy. Synthetic Fe 0.96 O-wustite was investigated at 91(2), 95(4), 109(2), 114.5(3), 131.1(7), 133.2(2), 155(2), 167(2),
193(2) and 203(1) GPa at 300 K at the SPring-8 BL11XU beamline. The Mossbauer spectrum at 91 GPa consists of both magnetic and nonmagnetic components. The magnetic high-spin component decreases gradually with
increasing pressure from 91 to 203 GPa, while the nonmagnetic low-spin component increases with pressure in the same pressure range. The result suggests that the spin state of Fe in the outer core at pressures above
203 GPa is the low-spin state. If oxygen exists in the core, the low-spin Fe-O bonding is shorter than high-spin Fe-O bonding, suggesting dense Fe-O liquid in the Earth’s outer core. The gradual increase of the density of the metallic liquid with depth by the spin transition of Fe-O bonding in the shallow outer core region will stabilize the outer core against thermal convection.
書誌情報 Physical Review B

巻 93, p. 155165-1-155165-6, 発行日 2016-04
出版者
出版者 アメリカ物理学会
DOI
識別子タイプ DOI
関連識別子 10.1103/PhysRevB.93.155165
関連サイト
識別子タイプ URI
関連識別子 http://journals.aps.org/prb/abstract/10.1103/PhysRevB.93.155165
関連名称 http://journals.aps.org/prb/abstract/10.1103/PhysRevB.93.155165
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