Marangoni convection in an evaporating water droplet
•Marangoni flow in an autonomously evaporating pure water drop into the air is measured using particle tracking velocimetry.•No external heating is used to stimulate the Marangoni flow.•A mathematical model representing the evaporating drop is developed and solved numerically.•The experimental veloc...
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Published in | International journal of heat and mass transfer Vol. 181; p. 122042 |
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Main Authors | , , , |
Format | Journal Article |
Language | English |
Published |
Oxford
Elsevier Ltd
01.12.2021
Elsevier BV |
Subjects | |
Online Access | Get full text |
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Summary: | •Marangoni flow in an autonomously evaporating pure water drop into the air is measured using particle tracking velocimetry.•No external heating is used to stimulate the Marangoni flow.•A mathematical model representing the evaporating drop is developed and solved numerically.•The experimental velocities in the center of the droplet were found to be 10 mm/s which is significant compared to those typically reported.•The simulated velocities in the center of the droplet were found to be even larger (almost twice as large as those measured).
The existence of Marangoni flow in an evaporating pure water drop has remained an open question. In this study, we report the occurrence of Marangoni convection within a water drop resting on a copper rod as it evaporates into the air. Through careful preparation of the test liquid suspension, we have observed convective structures inside the water drop. We also developed a mathematical model representing the evaporation system and solved it numerically to further strengthen support for the experimental data. Our study is different from previous studies on droplet evaporation in the sense that we allowed the droplet to evaporate spontaneously in the normal laboratory condition without heating the substrate. The substrate was neither externally heated nor did radiation from the illumination light stimulate a Marangoni flow. The velocities in the midsection of the droplet were measured using particle tracking velocimetry in both the sessile and pendant configurations. The typical velocities in the center of the droplet were found to be 10 mm/s experimentally and even higher velocities (about double that) were predicted by the mathematical model. This high value stands out among the thermocapillary-driven flows observed in an autonomously evaporated drop of water under ambient conditions.
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ISSN: | 0017-9310 1879-2189 |
DOI: | 10.1016/j.ijheatmasstransfer.2021.122042 |