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在波纹表面上形成冰核

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
PubMed
概括

波纹表面的异质冰核,如Cu{511},促进了冰膜的生长. 纳米级波纹稳定水层,增强冰核和影响气候模型.

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科学领域:

  • 表面科学
  • 物理化学
  • 环境科学

背景情况:

  • 异质冰核对于大气和气候建模至关重要.
  • 从表面的初始水层了解三维冰的增长仍然不完整.
  • 在核化大冰中表面的效率尚未完全理解.

研究的目的:

  • 为了研究波纹,水友/疏水表面的水重组.
  • 从第一层水中阐明冰膜形成的机制.
  • 确定表面波纹在冰核化效率中的作用.

主要方法:

  • 在波纹Cu511表面上模拟水的行为.
  • 分析水道网络的形成和重组.
  • 与平面研究进行比较.

主要成果:

  • 波纹Cu ((511) 上的水形成一个带的六角湿层,其中包括H键供应点和受体点.
  • 这一第一层水放松成冰状的布局, 稳定下一层冰.
  • 与平面相比,纳米级的表面波纹显著增强了冰核.

结论:

  • 波纹表面为多层冰的生长提供了有利的模板.
  • 表面波纹是影响冰核效率的关键因素.
  • 这一发现对了解气候和材料科学中的自然和人工表面有意义.