移行金属ヒドリドの形成ギャップとその崩壊に関する見解
Hiroshi Mizoguchi1, Sang-Won Park1,2, Hideo Hosono1,2
1International Center for Materials Nanoarchitectonics (WPI-MANA), National Institute for Materials Science (NIMS), 1-1 Namiki, Tsukuba, Ibaraki 305-0044, Japan.
Journal of the American Chemical Society
|July 21, 2021
まとめ
遅い移行金属 (LTM) は希少にヒドリドを形成する. インターメタリックの負の電荷イオンによって影響されるラットスの柔らかさは,水素吸収の鍵であり,新しい材料の開発を可能にします.
科学分野:
- 材料科学
- 化学について
- 物理学
背景:
- 遅い移行金属 (LTM) は通常,標準条件下では水化物を形成しないが,パラジウム (Pd) は顕著な例外である.
- LaNi5のような水素 (H) 貯蔵インターメタリック (IM) の形成には,低電子陰性金属とLTMを組み込むことが含まれます.
研究 の 目的:
- LTMの水素 (H) 吸収能力を支配する重要な性質を調査する.
- LTM と H ストレージ IM に H を挿入する鍵のパラメータとして格子柔らかさを確立する.
主な方法:
- LTMのH吸収特性に関する試験
- 水素化プロセスにおける負の電荷のLTMイオンの役割の分析.
主要な成果:
- パラジウム (Pd) の格子柔らかさは,Hの挿入を容易にするユニークなパラメータとして特定されました.
- 負の電荷を持つLTMイオンは,Niδ-によって示され,LaNi5で,H溶液を可能にする格子軟化を引き起こすことが判明した.
結論:
- 格子軟化がLTMにおける水素吸収の重要な要因である.
- 格子柔らかさの概念は,新しい水素貯蔵インターメタリックの開発を導くことができます.
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