The growth of the initially turbulent mixing layer: A large eddy simulation study

W. A. McMullan*, J. Mifsud, M. Angelino

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

Abstract

This article presents new information on the growth of a mixing layer originating from turbulent upstream conditions, obtained through large eddy simulation. The mixing layer develops from a turbulent high-speed side boundary layer and a laminar low-speed side boundary layer. Validation of the grid resolution, subgrid-scale model, and spanwise domain extent is performed. It is observed that the initially turbulent mixing layer undergoes three distinct phases in its evolution: a sub-shear region, where an internal shear layer develops immediately downstream of the splitter plate trailing edge and entrains the vorticity from the high-speed side boundary layer; a relaxation region, where the mixing layer develops to a point where the influence of the upstream conditions is forgotten; and a fully developed region, where the flow behaves in a self-preserving manner. The simulations display a discrepancy in downstream distances for the mean field, and turbulent stresses, to attain a self-preserving state, respectively, which is attributed to the spanwise integral length scale requiring a longer distance to attain an equilibrium value when compared to its streamwise and vertical counterparts. Large-scale, spanwise-orientated coherent structures are found to be a constituent part of the fully developed flow, and there is an absence of a spatially stationary streamwise structure in the initially turbulent mixing layer. The findings of the simulations are used to reconcile discrepancies found in experiments available in the archival literature.
Original languageEnglish
Article number115194
Number of pages25
JournalPhysics of Fluids
Volume36
Issue number11
Early online date21 Nov 2024
DOIs
Publication statusPublished - Nov 2024

Bibliographical note

Copyright © 2024 Author(s). All article content, except where otherwise noted, is licensed under a Creative Commons Attribution (CC BY) license (https://creativecommons.org/licenses/by/4.0/).

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