自动驱动的滴滴运动在它们的结冰点以下
Lizhong Wang1, Guochen Jiang1, Dongyu Zhu2
1Laser Materials Processing Research Center, Key Laboratory for Advanced Materials Processing Technology (Ministry of Education), Joint Research Center for Advanced Materials & Anti-icing of Tsinghua University (SMSE)-AVIC ARI, School of Materials Science and Engineering, Tsinghua University, Beijing, 100084, P. R. China.
Small (Weinheim an der Bergstrasse, Germany)
|June 14, 2023
概括
发现揭示了冰化环境中自动驱动的滴滴运动,随着距离和体积的增加而加速. 这些运动是由结冰过压和毛细血管拉动引发的,不需要外部能量输入,扩大了结条件下的应用.
科学领域:
- 物理 物理学 物理
- 材料科学 材料科学 材料科学
- 流体动力学 流体动力学
背景情况:
- 液体流动性对于许多技术至关重要,但随着温度的下降,阻碍了在寒冷环境中的应用.
- 热力学规定,随着温度下降,液体流动性会减少,导致冰点以下的固化.
研究的目的:
- 在冰化环境中发现和演示自动驱动的滴滴运动.
- 研究这些运动的机制和影响因素.
- 探索冷条件下受控滴滴运动的潜在应用.
主要方法:
- 在受控的冰化环境中观察和证明滴滴运动.
- 运动触发机制的分析,包括自发的过压和毛细血管拉动.
- 研究液体特性,表面结构和压力梯度的影响.
主要成果:
- 在结冰条件下观察到自动驱动的滴滴运动,包括自行深化和曲.
- 随着距离和滴水体积的增加,运动加速.
- 运动是由结冰引起的过压触发的,并由毛细血管力放大.
- 这些现象在各种液体和微纳米结构表面中是通用的.
结论:
- 在冰化环境中自动驱动的滴滴运动是一种新奇的现象.
- 这一发现为在结条件下操纵液体提供了新的可能性.
- 潜在的应用范围包括能源,微流体和在寒冷气候中运行的生物输送系统.
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