Condensation on Highly Superheated Surfaces: Unstable Thin Films in a Wickless Heat Pipe

被引:27
作者
Kundan, Akshay [1 ]
Nguyen, Thao T. T. [1 ]
Plawsky, Joel L. [1 ]
Wayner, Peter C., Jr. [1 ]
Chao, David F. [2 ]
Sicker, Ronald J. [2 ]
机构
[1] Rensselaer Polytech Inst, Howard P Isermann Dept Chem & Biol Engn, Troy, NY 12180 USA
[2] NASA, Glenn Res Ctr, Cleveland, OH 44135 USA
基金
美国国家科学基金会; 美国国家航空航天局;
关键词
DROPWISE CONDENSATION; CONSTANT-AREA; ADIABATIC TIP; MODEL; MICROGRAVITY; EVAPORATION; CAPILLARY; TRANSPORT; STANDARD; DRYOUT;
D O I
10.1103/PhysRevLett.118.094501
中图分类号
O4 [物理学];
学科分类号
0702 ;
摘要
A wickless heat pipe was operated on the International Space Station to provide a better understanding of how the microgravity environment might alter the physical and interfacial forces driving evaporation and condensation. Traditional heat pipes are divided into three zones: evaporation at the heated end, condensation at the cooled end, and intermediate or adiabatic in between. The microgravity experiments reported herein show that the situation may be dramatically more complicated. Beyond a threshold heat input, there was a transition from evaporation at the heated end to large-scale condensation, even as surface temperatures exceeded the boiling point by 160 Kappa. The hotter the surface, the more vapor was condensed onto it. The condensation process at the heated end is initiated by thickness and temperature disturbances in the thin liquid film that wet the solid surface. Those disturbances effectively leave the vapor "superheated" in that region. Condensation is amplified and sustained by the high Marangoni stresses that exist near the heater and that drive liquid to cooler regions of the device.
引用
收藏
页数:6
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