Evaporation of water: evaporation rate and collective effects

被引:123
作者
Carrier, Odile [1 ]
Shahidzadeh-Bonn, Noushine [1 ]
Zargar, Rojman [1 ]
Aytouna, Mounir [1 ]
Habibi, Mehdi [1 ,2 ]
Eggers, Jens [3 ]
Bonn, Daniel [1 ]
机构
[1] Univ Amsterdam, Inst Phys, Van der Waals Zeeman Inst, Sci Pk 904, NL-1098 XH Amsterdam, Netherlands
[2] Inst Adv Studies Basic Sci IASBS, Zanjan 4513766731, Iran
[3] Univ Bristol, Dept Math, Univ Walk, Bristol BS8 1TW, Avon, England
关键词
condensation/evaporation; drops; phase change; SESSILE DROPS; DROPLETS; TEMPERATURE; DEPOSITION; CONVECTION; CONTACT;
D O I
10.1017/jfm.2016.356
中图分类号
O3 [力学];
学科分类号
08 ; 0801 ;
摘要
We study the evaporation rate from single drops as well as collections of drops on a solid substrate, both experimentally and theoretically. For a single isolated drop of water, in general the evaporative flux is limited by diffusion of water through the air, leading to an evaporation rate that is proportional to the linear dimension of the drop. Here, we test the limitations of this scaling law for several small drops and for very large drops. We find that both for simple arrangements of drops, as well as for complex drop size distributions found in sprays, cooperative effects between drops are significant. For large drops, we find that the onset of convection introduces a length scale of approximately 20 mm in radius, below which linear scaling is found. Above this length scale, the evaporation rate is proportional to the surface area.
引用
收藏
页码:774 / 786
页数:13
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