Leidenfrost Effect as a Directed Percolation Phase Transition

Pierre Chantelot and Detlef Lohse
Phys. Rev. Lett. 127, 124502 – Published 17 September 2021
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Abstract

Volatile drops deposited on a hot solid can levitate on a cushion of their own vapor, without contacting the surface. We propose to understand the onset of this so-called Leidenfrost effect through an analogy to nonequilibrium systems exhibiting a directed percolation phase transition. When performing impacts on superheated solids, we observe a regime of spatiotemporal intermittency in which localized wet patches coexist with dry regions on the substrate. We report a critical surface temperature, which marks the upper bound of a large range of temperatures in which levitation and contact coexist. In this range, with decreasing temperature, the equilibrium wet fraction increases continuously from zero to one. Also, the statistical properties of the spatiotemporally intermittent regime are in agreement with that of the directed percolation universality class. This analogy allows us to redefine the Leidenfrost temperature and shed light on the physical mechanisms governing the transition to the Leidenfrost state.

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  • Received 11 June 2021
  • Accepted 16 August 2021

DOI:https://doi.org/10.1103/PhysRevLett.127.124502

© 2021 American Physical Society

Physics Subject Headings (PhySH)

Fluid DynamicsStatistical Physics & Thermodynamics

Authors & Affiliations

Pierre Chantelot1,* and Detlef Lohse1,2,†

  • 1Physics of Fluids Group, Max Planck Center Twente for Complex Fluid Dynamics, MESA+ Institute, and J. M. Burgers Center for Fluid Dynamics, University of Twente, P.O. Box 217, 7500AE Enschede, Netherlands
  • 2Max Planck Institute for Dynamics and Self-Organisation, Am Fassberg 17, 37077 Göttingen, Germany

  • *p.r.a.chantelot@utwente.nl
  • d.lohse@utwente.nl

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Issue

Vol. 127, Iss. 12 — 17 September 2021

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