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Turbulent flows over superhydrophobic surfaces: flow-induced capillary waves, and robustness of air–water interfaces

Published online by Cambridge University Press:  27 November 2017

Jongmin Seo ,
Ricardo García-Mayoral  and
Ali Mani Open the ORCID record for Ali Mani [Opens in a new window]
Jongmin Seo
Affiliation:
Center for Turbulence Research, Stanford University, Stanford, CA 94305, USA
Ricardo García-Mayoral
Affiliation:
Center for Turbulence Research, Stanford University, Stanford, CA 94305, USA Department of Engineering, University of Cambridge, Cambridge CB2 1PZ, UK
Ali Mani*
Affiliation:
Center for Turbulence Research, Stanford University, Stanford, CA 94305, USA
*
†Email address for correspondence: [email protected]
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Abstract

Superhydrophobic surfaces can retain gas pockets within their microscale textures when submerged in water. This property reduces direct contact between water and solid surfaces and presents opportunities for improving hydrodynamic performance by decreasing viscous drag. In most realistic applications, however, the flow regime is turbulent and retaining the gas pockets is a challenge. In order to overcome this challenge, it is crucial to develop an understanding of physical mechanisms that can lead to the failure of superhydrophobic surfaces in retaining gas pockets when the overlying liquid flow is turbulent. We present a study of the onset of failure in gas retention by analysing direct numerical simulations (DNS) of turbulent flows over superhydrophobic surfaces coupled with the deformation of air–water interfaces that hold the gas pockets. The superhydrophobic surfaces are modelled as periodic textures with patterned slip and no-slip boundary conditions on the overlying water flow. The liquid–gas interface is modelled via a linearized Young–Laplace equation, which is solved coupled with the overlying turbulent flow. A wide range of texture sizes and interfacial Weber numbers are considered in this study. Our analysis identifies flow-induced upstream-travelling capillary waves that are coherent in the spanwise direction as one mechanism for failure in retention of gas pockets. To confirm physical understanding of these waves, a semianalytical inviscid linear analysis is developed; the wave speeds obtained from the space–time correlations in the DNS data were found to match with the predictions of the semianalytical model. The magnitude of the pressure fluctuations due to these waves was found to increase with decreasing surface tension, and increase with a much stronger dependence on the slip velocity, when all numbers are reported in wall units. Based on a fitted scaling, a threshold criterion for the failure of superhydrophobic surfaces is developed that is based on estimates of the onset condition required for the motion of contact lines. The second contribution of this work is the development of boundary maps that identify stable and unstable zones in a parameter space consisting of working parameter and design parameters including texture size and material contact angle. We provide a brief description of previously identified failure modes of superhydrophobic surfaces, namely the stagnation pressure and shear-driven drainage mechanisms. In an overlay map, the stable and unstable zones due to each mechanism are presented. For various input conditions, we provide scaling laws that identify the most critical mechanism limiting the stability of gas retention by superhydrophobic surfaces.

JFM classification

Waves/Free-surface Flows: Capillary waves Flow Control: Drag reduction Turbulent Flows: Turbulent Flows
Type
JFM Papers
Information
Journal of Fluid Mechanics , Volume 835 , 25 January 2018 , pp. 45 - 85
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Copyright
© 2017 Cambridge University Press 

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Seo et al. supplementary movie 1

Instantaneous pressure field at y=0, for Re_Tau=197.5, L+=155, and We_L=0.002.

Download Seo et al. supplementary movie 1(Video)
Video 4.2 MB

Seo et al. supplementary movie 2

Instantaneous pressure field at y=0, for Re_Tau=197.5, L+=38, and We_L=0.004.

Download Seo et al. supplementary movie 2(Video)
Video 3.3 MB