特集 地球科学 高圧下における金属‐鉱物の反応と核の組成
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- 鈴木 敏弘
- 学習院大学理学部化学科
書誌事項
- タイトル別名
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- Feature Articles on Earth Science. Metal-mineral Reaction under High Pressure and Its Implications for Composition of the Core.
抄録
In the last decade, reaction of metals and silicate minerals under high pressure and temperature have been studied extensively. These investigations have revealed that the solubility of hydrogen, oxygen and silicon in metallic iron are enhanced by high pressure, and these elements were added to the candidates of the light elements in the earth's core. Pressure effect on partition coefficients of elements between metallic iron and mantle minerals have also been examined by high pressure experiments. These experimental investigations have successively provided important information for the studies of formation and composition of the earth's core. Some difficulties, however, still remain in the high pressure experimental techniques for metal-mineral reaction, such as the reaction of the sample and its container.
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 3 (1), 34-40, 1994
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
- 1390282679358578688
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- NII論文ID
- 130001598635
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- ISSN
- 13481940
- 0917639X
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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
- Crossref
- CiNii Articles
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- 抄録ライセンスフラグ
- 使用不可