Instantaneous convective heat transfer at the wall: a depiction of turbulent boundary layer structures

TL;DR

This study experimentally visualizes and analyzes the turbulent boundary layer structures affecting wall heat transfer, revealing scale-dependent convective behaviors at different Reynolds numbers using innovative temperature measurement techniques.

Contribution

It introduces a novel experimental method to measure wall heat transfer fluctuations and characterizes the multi-scale turbulent structures in the boundary layer.

Findings

Elongated heat transfer structures resemble near-wall streaks at low Reynolds numbers.

Effective size of heat transfer fluctuations increases with Reynolds number.

Larger structures convect at free-stream velocity, smaller ones at about 10 times friction velocity.

Abstract

We demonstrate the ability to experimentally measure fluctuations of the convective heat transfer coefficient at the wall in a turbulent boundary layer. For this, we measure two-dimensional fields of wall-temperature fluctuations beneath a zero-pressure-gradient turbulent boundary layer, at two moderate friction Reynolds numbers ($Re_\tau \approx 990$ and $Re_\tau \approx 1800$). Spatiotemporal data of wall-temperature are acquired by means of a heated-thin-foil sensor as sensing hardware, and an infrared camera as temperature detector. At low $Re_\tau$ conditions, the fields of the Nusselt number fluctuations are populated by elongated structures comprising streamwise and spanwise length scales comparable to those of near-wall streaks. At higher $Re_\tau$ conditions, the effective width and length of the coherent $Nu$ fluctuations increases. These findings are based on two-point correlations, as well as streamwise-spanwise energy spectra of $Nu$ fluctuations. The convective velocities of the $Nu$ fluctuations are also computed with the available time resolution from the measurements. This allows for resolving the multi-scale nature of convective footprints of wall-bounded turbulence: our experimental data reflect that larger streaks in the footprint convect at velocities in the order of the free-stream velocity, while the more energetic smaller-scale features move at velocities in the order of $10u_\tau$. Measurements of the kind presented here offer a promising method for sensing, as they can be used as input to flow control systems.