Titlebook: Laminar-Turbulent Transition; Symposium, Novosibir V. V. Kozlov Conference proceedings 1985 Springer-Verlag, Berlin, Heidelberg 1985 fluid

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Secondary Instability of Plane Shear Flows — Theory and Applicationalysis. Results for subharmonic and fundamental (peak-valley splitting) modes in plane Poiseuille flow and in the Blasius boundary layer are consistent with experimental data and prove the theory’s scope for understanding, classification, and prediction of the observed secondary phenomena.

Debility

Resonant Interactions in Shear Flowshe same time, interest arose in resonance (triads and quartets) among surface waves in water (Phillips [4], McGoldrick [5]) and among surface and internal waves in stratified fluid (Ball [6], Thorpe [7], Davis & Acrivos [8]). Meanwhile, similar advances were taking place in other fields, notably non

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Three-Dimensional Numerical Simulation of Laminar Turbulent Transition and its Control by Periodic D-Stokes equations using a spectral method. The classical peak-valley splitting mode of secondary instability is considered. Detailed comparison with experiments has demonstrated very satisfactory agreement up to the 1-spike stage. Visualizations of the development of three-dimensional flow structure

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Instability and Turbulent Bursting in the Boundary Layeron-linear, convectively driven, cross streamwise periodic disturbance of the resulting flow is then studied and finally, the stability of the resulting localized shearing layers is studied. It is found that at large Reynolds number, the primary disturbance amplitude is about 8% and the secondary dis

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Ballad

Subtransitions in the Transition Zonereakdown. An analysis of experimental data based on this expression shows that when there are rapid and substantial changes in the geometry of the spot dependence cone, the transition zone reveals corresponding changes that may be best viewed as subtransitions. Examples offered include: plane bounda