History effects and near-equilibrium in turbulent boundary layers with pressure gradient

TL;DR

This study uses large-eddy simulations to analyze turbulent boundary layers under adverse pressure gradients, revealing how pressure development influences turbulence structures and boundary layer states.

Contribution

It provides new insights into the influence of streamwise pressure development and tests a proposed scaling law in turbulent boundary layers with pressure gradients.

Findings

Non-constant pressure cases approach a unique boundary layer state downstream.

Strong pressure gradients enhance outer-region energy-carrying structures.

Scaling laws may be affected by the development length of the pressure gradient.

Abstract

Turbulent boundary layers under adverse pressure gradients are studied using well-resolved large-eddy simulations (LES) with the goal of assessing the influence of the streamwise pressure development. Near-equilibrium boundary layers were identified with the Clauser parameter $\beta$. The pressure gradient is imposed by prescribing the free-stream velocity. In order to fulfill the near-equilibrium conditions, the free-stream velocity has to follow a power-law distribution. The turbulence statistics pertaining to cases with a constant Clauser pressure-gradient parameter ? were compared with cases with a non-constant pressure distribution at matched ? and friction Reynolds number Re_tau . It was noticed that the non-constant cases appear to approach far downstream a certain state of the boundary layer, which is uniquely characterised by beta? and Re_tau. The investigations on the flat plate were extended to the flow around a wing section. Comparisons with the flat-plate cases at matched Re_tau and ? revealed some interesting features: In turbulent boundary layers with strong pressure gradients in the development history the energy-carrying structures in the outer region are strongly enhanced, which can be detected by the pronounced wake in the mean velocity as well as the large second peak in the Reynolds stresses. Furthermore, a scaling law suggested by Kitsios et al. (2015), proposing the edge velocity and displacement thickness as scaling parameters, was tested on a constant pressure gradient case. The mean velocity and Reynolds stress profiles were found to be dependent on the downstream development, indicating that their conclusion might be the result of a too short constant pressure gradient region.