Can large-scale oblique undulations on a solid wall reduce the turbulent drag?
File(s)1705.01989v2.pdf (6.69 MB)
Published version
Author(s)
Ghebali, Sacha
Chernyshenko, Sergei I
Leschziner, Michael A
Type
Journal Article
Abstract
Direct numerical simulations of fully-developed turbulent channel flows with
wavy walls are undertaken. The wavy walls, skewed with respect to the mean flow
direction, are introduced as a means of emulating a Spatial Stokes Layer (SSL)
induced by in-plane wall motion. The transverse shear strain above the wavy
wall is shown to be similar to that of a SSL, thereby affecting the turbulent
flow, and leading to a reduction in the turbulent skin-friction drag. The
pressure- and friction-drag levels are carefully quantified for various flow
configurations, exhibiting a combined maximum overall-drag reduction of about
0.5%. The friction-drag reduction is shown to behave approximately
quadratically for small wave slopes and then linearly for higher slopes, whilst
the pressure-drag penalty increases quadratically. Unlike in the SSL case,
there is a region of increased turbulence production over a portion of the
wall, above the leeward side of the wave, thus giving rise to a local increase
in dissipation. The transverse shear-strain layer is shown to be approximately
Reynolds-number independent when the wave geometry is scaled in wall units.
wavy walls are undertaken. The wavy walls, skewed with respect to the mean flow
direction, are introduced as a means of emulating a Spatial Stokes Layer (SSL)
induced by in-plane wall motion. The transverse shear strain above the wavy
wall is shown to be similar to that of a SSL, thereby affecting the turbulent
flow, and leading to a reduction in the turbulent skin-friction drag. The
pressure- and friction-drag levels are carefully quantified for various flow
configurations, exhibiting a combined maximum overall-drag reduction of about
0.5%. The friction-drag reduction is shown to behave approximately
quadratically for small wave slopes and then linearly for higher slopes, whilst
the pressure-drag penalty increases quadratically. Unlike in the SSL case,
there is a region of increased turbulence production over a portion of the
wall, above the leeward side of the wave, thus giving rise to a local increase
in dissipation. The transverse shear-strain layer is shown to be approximately
Reynolds-number independent when the wave geometry is scaled in wall units.
Date Acceptance
2017-09-05
Citation
Physics of Fluids, 29, pp.105102-105102
Start Page
105102
End Page
105102
Journal / Book Title
Physics of Fluids
Volume
29
Copyright Statement
© The Authors
Sponsor
The Royal Society
Innovate UK
Identifier
http://arxiv.org/abs/1705.01989v2
Grant Number
IE130524
113022
Subjects
physics.flu-dyn
physics.flu-dyn