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Secondary instability of a temporally growing mixing layer

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TLDR
The three-dimensional stability of two-dimensional vortical states of planar mixing layers is studied by direct numerical integration of the Navier-Stokes equations in this article.
Abstract
The three-dimensional stability of two-dimensional vortical states of planar mixing layers is studied by direct numerical integration of the Navier-Stokes equations. Small-scale instabilities are shown to exist for spanwise scales at which classical linear modes are stable. These modes grow on convective timescales, extract their energy from the mean flow and exist at moderately low Reynolds numbers. Their growth rates are comparable with the most rapidly growing inviscid instability and with the growth rates of two-dimensional subharmonic (pairing) modes. At high amplitudes, they can evolve into pairs of counter-rotating, streamwise vortices, connecting the primary spanwise vortices, which are very similar to the structures observed in laboratory experiments. The three-dimensional modes do not appear to saturate in quasi-steady states as do the purely two-dimensional fundamental and subharmonic modes in the absence of pairing. The subsequent evolution of the flow depends on the relative amplitudes of the pairing modes. Persistent pairings can inhibit threedimensional instability and, hence, keep the flow predominantly two-dimensional. Conversely, suppression of the pairing process can drive the three-dimensional modes to more chaotic, turbulent-like states. An analysis of high-resolution simulations of fully turbulent mixing layers confirms the existence of rib-like structures and that their coherence depends strongly on the presence of the two-dimensional pairing modes.

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Citations
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New Trends in Large-Eddy Simulations of Turbulence

TL;DR: In this article, a large-eddy simulation (LES) formalism, along with various subgrid-scale models developed since Smagorinsky's model, is presented, with an emphasis on the generation of coherent vortices.
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Spectral methods for the Navier-Stokes equations with one infinite and two periodic directions

TL;DR: In this paper, the Navier-Stokes equations in boundary layers and mixing layers are solved by two numerical methods which employ rapidly decaying spectral basis functions to approximate the vertical dependence of the solutions.
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Mean flow and turbulence structure over fixed, two-dimensional dunes: implications for sediment transport and bedform stability

TL;DR: In this paper, the authors measured the downstream and vertical components of velocity at more than 1800 points over one dune wavelength and constructed a set of contour maps for all mean flow and turbulence parameters, which are assessed using higher moment measures and quadrant analysis.
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Three-dimensional instability of a plane free shear layer: an experimental study of the formation and evolution of streamwise vortices

TL;DR: In this paper, the three-dimensional development of a plane free shear layer subjected to small sinusoidal perturbations periodically placed along the span is experimentally studied using both laser induced fluorescence and direct interface visualization.
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The three-dimensional evolution of a plane mixing layer - The Kelvin-Helmholtz rollup

TL;DR: In this paper, the Kelvin Helmholtz roll up of three dimensional, temporally evolving, plane mixing layers were simulated numerically, starting from a few low wavenumber disturbances, usually derived from linear stability theory, in addition to the mean velocity profile.
References
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Journal ArticleDOI

On density effects and large structure in turbulent mixing layers

TL;DR: In this article, Spark shadow pictures and measurements of density fluctuations suggest that turbulent mixing and entrainment is a process of entanglement on the scale of the large structures; some statistical properties of the latter are used to obtain an estimate of entrainedment rates, and large changes of the density ratio across the mixing layer were found to have a relatively small effect on the spreading angle.
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Perturbed Free Shear Layers

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Vortex pairing : the mechanism of turbulent mixing-layer growth at moderate Reynolds number

TL;DR: A mixing layer is formed by bringing two streams of water, moving at different velocities, together in a lucite-walled channel as mentioned in this paper, where dye is injected between the two streams just before they are brought together, marking the vorticitycarrying fluid.
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Subharmonics and vortex merging in mixing layers

TL;DR: In this paper, it was shown that the spreading rate of a mixing layer can be greatly manipulated at very low forcing level if the mixing layer is perturbed near a subharmonic of the most-amplified frequency.
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Coherent structures—reality and myth

TL;DR: In this article, a definition of coherent structures in turbulent shear flows is proposed and its implications discussed, and the characteristic coherent structure properties are identified and the analytical and experimental constraints in the eduction of coherent structure are examined.
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