Induction of Marangoni convection in pure water drops

被引:53
|
作者
Kita, Yutaku [1 ,2 ]
Askounis, Alexandros [1 ,2 ]
Kohno, Masamichi [1 ,2 ,3 ]
Takata, Yasuyuki [1 ,2 ,3 ]
Kim, Jungho [4 ]
Sefiane, Khellil [5 ]
机构
[1] Kyushu Univ, Dept Mech Engn, Nishi Ku, 744 Motooka, Fukuoka 8190395, Japan
[2] Kyushu Univ, Int Inst Carbon Neutral Energy Res WPI I2CNER, Nishi Ku, 744 Motooka, Fukuoka 8190395, Japan
[3] Japan Sci & Technol Agcy, CREST, Nishi Ku, 744 Motooka, Fukuoka 8190395, Japan
[4] Univ Maryland, Dept Mech Engn, College Pk, MD 20742 USA
[5] Univ Edinburgh, Sch Engn, Kings Bldg,Mayfield Rd, Edinburgh EH9 3BF, Midlothian, Scotland
基金
英国工程与自然科学研究理事会; 日本科学技术振兴机构;
关键词
THERMOCAPILLARY CONVECTION; SESSILE DROPLET; EVAPORATION; FLOW; PATTERNS; SURFACE;
D O I
10.1063/1.4966542
中图分类号
O59 [应用物理学];
学科分类号
摘要
We report on experimental observations/visualization of thermocapillary or Marangoni flows in a pure water drop via infrared thermography. The Marangoni flows were induced by imposing a temperature gradient on the drop by locally heating the substrate directly below the center with a laser. Evidently, a temperature gradient along the liquid-air interface of ca. 2.5 degrees C was required for the Marangoni flows to be initiated as twin vortices and a subsequent gradient of ca. 1.5 degrees C to maintain them. The vortices exhibited an oscillatory behavior where they merged and split in order for the drop to compensate for the non-uniform heating and cooling. The origin of these patterns was identified by comparing the dimensionless Marangoni and Rayleigh numbers, which showed the dominance of the Marangoni convection. This fact was further supported by a second set of experiments where the same flow patterns were observed when the drop was inverted (pendant drop). Published by AIP Publishing.
引用
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页数:4
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