Turbulent transport for wall shear stress fluctuations
Myoungkyu Lee, Yongyun Hwang
TL;DR
This work analyzes wall shear stress fluctuations in wall-bounded turbulence (Poiseuille and Couette flows) using direct numerical simulations and dimensional analysis within polar-log spectral coordinates. It demonstrates that inner-range dissipation spectra with $\lambda \lesssim 1000\delta_\nu$ are Reynolds-number invariant, while outer-range spectra with $\lambda \gtrsim \delta$ decay with $Re$, causing the total wall dissipation to rise with $Re$ due to intermediate scales $1000\delta_\nu < \lambda < \delta$. The near-wall motions responsible for these dissipation characteristics are shown to be inactive (negligible Reynolds stress) and are sustained by turbulent transport, with both wall-normal and inter-scale transport spectra sharing the same $Re$-scaling and exhibiting energy flux toward the wall and inverse transfer along wall-parallel directions. These findings provide a mechanistic link between outer-scale dynamics and near-wall dissipation, informing models of wall-bounded turbulence and improving understanding of wall-shear fluctuations in engineering applications.
Abstract
Statistical structure and the underlying energy budget of wall shear stress fluctuations are studied in both Poiseulle and Couette flows with emphasis on its streamwise component. Using a dimensional analysis and direct numerical simulation data, it is shown that the spectra of streamwise wall dissipation for $λ\lesssim 1000 δ_ν$ are asymptotically invariant with the Reynolds number ($Re$), whereas those for $λ\gtrsim δ$ decay with $Re$ (here, $λ$ is a nominal wall-parallel wavelength, and $δ_ν$ and $δ$ are the viscous inner and outer length scales, respectively). The wall dissipation increases with $Re$ due to the increasing contribution of the spectra at $1000 δ_ν\lesssim λ\lesssim δ$. The subsequent analysis of the energy budget shows that the near-wall motions associated with these wall dissipation spectra are mainly driven by turbulent transport and are `inactive' in the sense that they contain very little Reynolds shear stress (or turbulence production). As such, turbulent transport spectra near the wall are also found to share the same $Re$-scaling behaviour with wall dissipation, and this is observed in the spectra of both the wall-normal and inter-scale turbulent transports. The turbulent transport underpinning the increase of wall dissipation with $Re$ is characterised by energy fluxes towards the wall, together with inverse energy transfer from small to large length scales along the wall-parallel directions.
