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Autothermotaxis of volatile drops

Pallav Kant1,2,*, Mathieu Souzy1,3,†, Nayoung Kim1,‡, Devaraj van der Meer1,§, and Detlef Lohse1,4,¶

  • 1Physics of Fluids Group, Max Planck Center Twente for Complex Fluid Dynamics, University of Twente, 7500 AE Enschede, The Netherlands
  • 2Bullard Laboratories, Department of Earth Science, University of Cambridge, CB3 0EZ United Kingdom
  • 3INRAE, Aix Marseille Univ, UMR RECOVER, 3275 Rte de Cézanne, CS 40061, 13182 Aix-en-Provence, Cedex5, France
  • 4Max Planck Institute for Dynamics and Self-Organization, Am Fassberg 17, 37077 Göttingen, Germany

  • *kantpallav88@gmail.com
  • mathieu.souzy@inrae.fr
  • nayoungkim516@gmail.com
  • §d.vandermeer@utwente.nl
  • d.lohse@utwente.nl

Phys. Rev. Fluids 9, L012001 – Published 31 January, 2024

DOI: https://doi.org/10.1103/PhysRevFluids.9.L012001

Abstract

When a drop of a volatile liquid is deposited on a uniformly heated wettable, thermally conducting substrate, one expects to see it spread into a thin film and evaporate. Contrary to this intuition, due to thermal Marangoni contraction, the deposited drop contracts into a spherical-cap-shaped puddle, with a finite apparent contact angle. Strikingly, this contracted droplet, above a threshold temperature, well below the boiling point of the liquid, starts to spontaneously move on the substrate in an apparently erratic way. We describe and quantify this self-propulsion of the volatile drop. It arises due to spontaneous symmetry breaking of thermal Marangoni convection, which is induced by the nonuniform evaporation of the droplet. Using infrared imaging, we reveal the characteristic interfacial flow patterns associated with Marangoni convection in the evaporating drop. A scaling relation describes the correlation between the moving velocity of the drop and the apparent contact angle, both of which increase with the substrate temperature.

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synopsis

Hot Surfaces Make Droplets Move Erratically

Published 31 January, 2024

A droplet of a volatile liquid can move on a uniformly heated surface thanks to a nonuniform evaporation effect that drives an unstable fluid flow within the droplet.

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