范德瓦尔斯在雾和雾中对部分融化的冰核诱导了冰的生长
M Boström1, Y Li2,3, I Brevik4
1Centre of Excellence ENSEMBLE3 Sp. z o. o., Wolczynska Str. 133, 01-919, Warsaw, Poland. mathias.bostrom@ensemble3.eu.
Physical chemistry chemical physics : PCCP
|November 28, 2023
概括
发现了一种由部分融化的冰颗粒启动的新型冰形成过程. 这种受范德瓦尔斯力影响的机制解释了薄冰层的增长,并对雾和大气科学产生了影响.
科学领域:
- 环境科学环境科学
- 食品工程 食品工程
- 大气科学 大气科学
- 天文地质物理学 天文地质物理学
背景情况:
- 冰的核和形成在各种科学领域都至关重要.
- 目前对冰形成机制的理解尚不完整.
研究的目的:
- 介绍和阐明一个新的冰形成过程.
- 为了研究范德瓦尔斯力在冰的增长中的作用.
- 为了提供关于薄冰层形成的见解.
主要方法:
- 从部分融化的冰核中分析冰晶的生长.
- 探索范德瓦尔斯 (Lifshitz) 自由能量和界面应力.
- 基于核的特性建模冰层厚度.
主要成果:
- 确定了一种新的异质/均质冰形成过程.
- 冰晶的生长是从微米大小的部分融化冰颗粒开始的.
- 该过程在部分融化冰面上产生了薄冰层 (纳米到微米).
- 有证据表明,薄冰层形成而不是液态水膜.
结论:
- 这种新的冰形成过程为雾和雾形成提供了新的见解.
- 这些发现在大气和天体地质物理研究中具有潜在的应用.
- 了解界面能量是预测冰层形成的关键.
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