3D Direct Numerical Simulation of Flat-Plate
and
Analysis of Transition to Turbulence



 


The general aim of this project is to get a more complete understanding of wall-generated turbulence from a detailed investigation of numerical data for the process of laminar-turbulent boundary-layer transition. For this purpose, as a first step a parallelized version of a boundary-layer transition code is being developed that will allow for the first time a well-resolved direct numerical simulation of the spatial process of laminar-turbulent transition, comprising the stages of initial development of linear disturbances up to the fully developed turbulent boundary layer. These simulations are being run on the new Velocity CLuster


The following sub-pages describe some areas of this work :

 

Numerical Algorithm (Direct Numerical Simulation)

A highly accurate algorithm has been developed to study the process of spatial transition to turbulence. The algorithmic details of the direct numerical simulation of transition to turbulence in a boundary layer based on a formulation in terms of vertical velocity and vertical vorticity are presented. Issues concerning the boundary conditions are discussed. The linear viscous terms are discretized using an implicit Crank-Nicholson scheme, and a low-storage Runge-Kutta method is used for the nonlinear terms. For the spatial discretization, fourth-order compact finite differences have been used, as these have been found to have better resolution compared to explicit differencing schemes of comparable order. The number of grid points that are needed per wavelength is close to the theoretical optimum for any numerical scheme. The resulting time-discretized fourth-order equations are split up into two second-order equations, resulting in Helmholtz- and Poisson-type equations. The boundary conditions for the Laplacian of the vertical velocity are determined using an influence matrix method. A robust multigrid algorithm has been developed to solve the resulting anisotropic elliptical equations. For the outflow boundary, a buffer domain method, which smoothly reduces the disturbances to zero, in conjunction with parabolization of the Navier-Stokes equations has been used. The validation of the results for the DNS solver is done both for linear and weakly nonlinear cases.

High Performance Computing

The spatial transition to turbulence has been simulated using a parallel multigrid strategy. The multigrid has been parallelized using a domain decomposition technique. Linear interpolation, full weight for restriction, and line Gauss-Seidel for smoothing has been used. The parallel computing performance characteristics, speedup and scaled efficiency have been determined. Both the algorithmic and implementation scalability features have resulted in efficient parallelization. Message-passing-interface (MPI) has been used for the communication between the various nodes. The K-mechanism of laminar breakdown has been simulated using direct numerical simulation (DNS) of the Navier-Stokes equation. The typical structures of transition, high shear layer, $\Lambda$-vortex, spikes, and longitudinal vortices have been observed.

Events of Transition (Physics of the flow)

Spatial transition to turbulence for a flat-plate boundary-layer has been simulated using direct numerical simulation. For the case of forced transition, a single frequency disturbance has been introduced, and fundamental breakdown and the characteristic events of a transitional boundary layer have been observed. The main events and structures are the inflectional nature of the disturbance velocity profiles as well as the mean velocity. The presence of a $\Lambda$-vortex, significance of streamwise vorticity, spanwise vorticity, shear layer, and speed of propagation of these structures are discussed in detail as well as their role in the transition process and in the process of breakdown to turbulence.

Resonance theory for transition to turbulence phenomena

The fundamental breakdown to turbulence known as the \emph{K-mechanism} of transition has been simulated under controlled conditions. The important characteristic features of the K-mechanism, namely peak-valley formation, significant spanwise modulation of the velocity, shear layer lift-up, and appearance of spikes have been observed. A possible explanation of the characteristic traits of this K-mechanism has been given using wave-resonance theory. Due to resonance, initially large-amplitude harmonics of a plane 2D wave are generated, and with increasing streamwise distance the harmonics of all the higher spanwise wavenumbers appear gradually and amplify in a deterministic manner. Up to the location of spike formation the amplitudes of the spanwise modes increases, reaching their highest levels just after the appearance of the spikes, while slightly dropping off further downstream.

kiran@mae.cornell.edu