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- 井上 徹
- 愛媛大学理学部生物地球圏科学科
書誌事項
- タイトル別名
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- Water in the Earth's Interior. Is the mantle transition zone a water reservoir?
- カイセツ チキュウ ナイブ ノ ミズ マントル センイソウ ワ ミズ ノ リザバー カ
- Is the mantle transition zone a water reservoir?
- マントル遷移層は水のリザバーか?
この論文をさがす
抄録
H2O is an important volatile material in the Earth, and it affects the physical properties (e. g. density, elastic velocity, viscosity, rheobgical property, diffusion, electrical conductivity and melting temperature) of the Earth's materials. Recently, it has been darified that significant amounts of H2O can be accommodated in β and γ phases of olivine, which means that the mantle transition zone has the potential of being a water reservoir in the Earth. In this paper, I review the H2O contents, lattice parameters and elastic properties of hydrous β and γ phases, the effect of H2O on the phase transformation of olivine, and the possibilities of water transportation into the mantle transition zone are discussed on the basis of these experimental data.
収録刊行物
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- 高圧力の科学と技術
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高圧力の科学と技術 10 (2), 124-133, 2000
日本高圧力学会
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詳細情報 詳細情報について
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- CRID
- 1390282679359120256
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- NII論文ID
- 10004668716
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- NII書誌ID
- AN10452913
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- COI
- 1:CAS:528:DC%2BD3cXltFyqu74%3D
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- ISSN
- 13481940
- 0917639X
- http://id.crossref.org/issn/0917639X
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- NDL書誌ID
- 5358051
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- 本文言語コード
- ja
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- データソース種別
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- JaLC
- NDL
- Crossref
- CiNii Articles
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- 抄録ライセンスフラグ
- 使用不可