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Asymptotic scaling laws for periodic turbulent boundary layers and their numerical simulation up to $\textit{Re}_{\boldsymbol{\theta}}\text{ = 8300}$

Published online by Cambridge University Press:  29 September 2025

Andrew Wynn*
Affiliation:
Department of Aeronautics, Imperial College London, South Kensington Campus, London SW7 2AZ, UK
Saeed Parvar
Affiliation:
Department of Aeronautics, Imperial College London, South Kensington Campus, London SW7 2AZ, UK
Joseph O’Connor
Affiliation:
EPCC, Bayes Centre, University of Edinburgh, 47 Potterrow, Edinburgh EH8 9BT, UK
Ricardo A.S. Frantz
Affiliation:
Arts et Métiers Institute of Technology, CNAM, DynFluid, HESAM Université, F-75013, Paris, France
Sylvain Laizet
Affiliation:
Department of Aeronautics, Imperial College London, South Kensington Campus, London SW7 2AZ, UK
*
Corresponding author: Andrew Wynn, a.wynn@imperial.ac.uk

Abstract

We provide a rigorous analysis of the self-similar solution of the temporal turbulent boundary layer, recently proposed by Biau (2023 Comput. Fluids 254, 105795), in which a body force is used to maintain a statistically steady turbulent boundary layer with periodic boundary conditions in the streamwise direction. We derive explicit expressions for the forcing amplitudes which can maintain such flows, and identify those which can hold either the displacement thickness or the momentum thickness equal to unity. This opens the door to the first main result of the paper, which is to prove upper bounds on skin friction for the temporal turbulent boundary layer. We use the Constantin–Doering–Hopf bounding method to show, rigorously, that the skin-friction coefficient for periodic turbulent boundary layer flows is bounded above by a uniform constant which decreases asymptotically with Reynolds number. This asymptotic behaviour is within a logarithmic correction of well-known empirical scaling laws for skin friction. This gives the first evidence, applicable at asymptotically high Reynolds numbers, to suggest that Biau’s self-similar solution of the temporal turbulent boundary layer exhibits statistical similarities with canonical, spatially evolving, boundary layers. Furthermore, we show how the identified forcing formula implies an alternative, and simpler, numerical implementation of periodic boundary layer flows. We give a detailed numerical study of this scheme presenting direct numerical simulations up to a momentum Reynolds number of $\textit{Re}_\theta = 2000$ and implicit large-eddy simulations up to $\textit{Re}_\theta = 8300$, and show that these results compare well with data from canonical spatially evolving boundary layers at equivalent Reynolds numbers.

Information

Type
JFM Papers
Creative Commons
Creative Common License - CCCreative Common License - BY
This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (https://creativecommons.org/licenses/by/4.0/), which permits unrestricted re-use, distribution and reproduction, provided the original article is properly cited.
Copyright
© The Author(s), 2025. Published by Cambridge University Press
Figure 0

Figure 1. A schematic overview of the proposed boundary layer thickness control scheme. The idea is to force either $\delta ^\ast$ or $\theta$ to converge to a reference value of $1$, by choice of the nonlinear control laws $K$ and $F$. The symbol $\varSigma$ denotes the summation of two signals in the feedback loop.

Figure 1

Table 1. Simulation details for the DNS and ILES of (4.1).

Figure 2

Table 2. The DNS and LES grid resolutions, and figure formatting conventions.

Figure 3

Figure 2. Temporal variation of the forcing amplitude $f$, momentum thickness $\theta$, displacement thickness $\delta ^\ast$ and friction velocity $u_\tau$. Data from the present DNS using $f_{\textit{DNS}}$ are shown with solid lines ($\textit{Re}_\theta =1000$; $\textit{Re}_\theta =2000$) and from implementation of Biau’s method in Xcompact3d with dotted lines ($\textit{Re}_\theta =1000$; $\textit{Re}_\theta =2000$).

Figure 4

Figure 3. A comparison of DNS of the current method with that of Biau (2023): (a) mean streamwise velocity $u^+$; (b) r.m.s. velocities and pressures at $\textit{Re}_\theta =1000$; (c) r.m.s. velocities and pressures at $\textit{Re}_\theta =2000$. Data from Biau (2023) are shown with markers ($\mathbf{\times }$$\textit{Re}_\theta =1000$; $\textit{Re}_\theta =2000$), from the present DNS using $f_{\textit{DNS}}$ with solid lines ($\textit{Re}_\theta =1000$; $\textit{Re}_\theta =2000$) and from the implementation of Biau’s method in Xcompact3d with dotted lines ($\textit{Re}_\theta =1000$; $\textit{Re}_\theta =2000$).

Figure 5

Table 3. A comparison of flow statistics between periodic boundary layer and spatially evolving boundary layer simulations.

Figure 6

Figure 4. The scaling of (a) $\textit{Re}_{\tau }$ and $\textit{Re}_{\delta ^\ast }$; and (b) $C_{\!f}$ and $H_{12}$ with $\textit{Re}_{\theta }$. The markers indicate: () for both DNS data from Schlatter & Orlu (2010) and LES data from Eitel-Amor et al. (2014); ($\blacktriangledown$) for DNS data from Sillero et al. (2013); and ($\square$) data from the present method.

Figure 7

Figure 5. Profiles of (a) $u^+$; (b) $u_{\textit{rms}}^+$; (c) $v_{\textit{rms}}^+$; and (d) $w_{\textit{rms}}^{+}$. Reference data are shown with markers: () for both the DNS of Schlatter & Orlu (2010) and the LES of Eitel-Amor et al. (2014); ($\blacktriangledown$) for the DNS of Sillero et al. (2013). Results with the present method are shown with solid lines. The colour convention is explained in § 5.

Figure 8

Table 4. Linear regression coefficients $\alpha ,\beta$ and correlation statistics $R^2$ for fits of the peak value of the squared r.m.s. velocity, $u^{2+}_{\textit{rms}},v^{2+}_{\textit{rms}}$ and $w^{2+}_{\textit{rms}}$ to the line $\alpha \ln {(\textit{Re}_\tau )} + \beta$. Fits are reported to data from the present study; the combined data of Schlatter & Orlu (2010), Eitel-Amor et al. (2014); and the data of Sillero et al. (2013).

Figure 9

Figure 6. (a) Mean Reynolds shear stress; and (b) r.m.s. pressure profiles. Reference data are shown with markers: () for both the DNS of Schlatter & Orlu (2010) and the LES of Eitel-Amor et al. (2014); ($\blacktriangledown$) for the DNS of Sillero et al. (2013). Results with the present method are shown with solid lines.

Figure 10

Figure 7. Turbulent kinetic energy budgets for (a) $\textit{Re}_\theta =1000$ and (b) $\textit{Re}_\theta = 6500$. Reference data are shown with markers: () for both the DNS of Schlatter & Orlu (2010) and the LES of Eitel-Amor et al. (2014); ($\blacktriangledown$) for the DNS of Sillero et al. (2013). Results with the present method are shown with solid lines.

Figure 11

Figure 8. Profiles of the r.m.s. vorticity components (a) $\omega _{x_{\textit{rms}}}$; (b) $\omega _{y_{\textit{rms}}}$; and (c) $\omega _{z_{\textit{rms}}}$, for $\textit{Re}_\theta =1000$ to $8300$. Reference data are shown with markers: () for both the DNS of Schlatter & Orlu (2010) and the LES of Eitel-Amor et al. (2014); ($\blacktriangledown$) for the DNS of Sillero et al. (2013). Results with the present method are shown with solid lines.

Figure 12

Figure 9. Contours of constant $Q^+$ for selected snapshots of a periodic turbulent boundary layer at (a) $\textit{Re}_\theta =1000, Q^+ = 0.01$; (b) $\textit{Re}_\theta =6500, Q^+ = 0.004$. The colour bar indicates non-dimensional streamwise velocity $u$. Each panel shows a section of the respective spatial domains described in table 1.