波紋状の表面での氷核化
Chenfang Lin1, Gefen Corem2, Oded Godsi2
1Surface Science Research Centre and Department of Chemistry , University of Liverpool , Liverpool L69 3BX , U.K.
Journal of the American Chemical Society
|October 30, 2018
まとめ
Cu(511のような波紋表面の異質な氷核は,氷膜の成長を促進する. ナノスケールの波紋は水層を安定させ 氷の核形成を促進し 気候モデルに影響を与えます
科学分野:
- 表面科学
- 物理化学
- 環境科学
背景:
- 異質な氷の核化は 大気と気候のモデル化に不可欠です
- 表面上の最初の水層からの3D氷の成長を理解することはまだ不完全です.
- 表面の効率は完全に理解されていません.
研究 の 目的:
- 波紋状の,水性/水害性の表面での水の再構成を調査する.
- 最初の水層から氷膜の形成のメカニズムを解明する.
- 氷核の効率化における表面波紋の役割を決定する.
主な方法:
- 波紋 Cu ((511) 表面での水の振る舞いのシミュレーション
- 水道ネットワークの形成と再構築の分析
- 平面での研究との比較
主要な成果:
- 波紋 Cu ((511) 上の水は,H結合のドナーと受容体の両方を含んだ6角形の潤滑層を形成する.
- この最初の水層は 氷のような配置に落ち着き,その後の氷層を安定させます.
- ナノスケールの表面波紋は平らな表面と比較して氷の核を大幅に強化します.
結論:
- 波紋状の表面は,多層の氷の成長に有利なテンプレートを提供します.
- 表面の波紋は,氷の核化の効率に影響を与える重要な要因です.
- この発見は,気候と材料科学における 自然と人工的な表面の理解に 影響を及ぼします
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