中文摘要：

The evolution of low-speed streaks in the turbulent boundary layer of the minimum channel flow unit at a low Reynolds number is simulated by the direct numerical simulation(DNS) based on the standard Fourier-Chebyshev spectral method.The subharmonic sinuous(SS) mode for two spanwise-aligned low-speed streaks is excited by imposing the initial perturbations.The possibilities and the physical realities of the turbulent sustaining in the minimal channel unit are examined.Based on such a flow field environment,the evolution of the low-speed streaks during a cycle of turbulent sustaining,including lift-up,oscillation,and breakdown,is investigated.The development of streamwise vortices and the dynamics of vortex structures are examined.The results show that the vortices generated from the same streak are staggered along the streamwise direction,while the vortices induced by different streaks tilt toward the normal direction due to the mutual induction effect.It is the spatial variations of the streamwise vortices that cause the lift-up of the streaks.By resolving the transport dynamics of enstrophy,the strength of the vortices is found to continuously grow in the logarithmic layer through the vortex stretching mechanism during the evolution of streaks.The enhancement of the vortices contributes to the spanwise oscillation and the following breakdown of the low-speed streaks.

英文摘要：

The evolution of low-speed streaks in the turbulent boundary layer of the minimum channel flow unit at a low Reynolds number is simulated by the direct numer- ical simulation （DNS） based on the standard Fourier-Chebyshev spectral method. The subharmonic sinuous （SS） mode for two spanwise-aligned low-speed streaks is excited by imposing the initial perturbations. The possibilities and the physical realities of the turbulent sustaining in the minimal channel unit are examined. Based on such a flow field environment, the evolution of the low-speed streaks during a cycle of turbulent sus- taining, including lift-up, oscillation, and breakdown, is investigated. The development of streamwise vortices and the dynamics of vortex structures are examined. The results show that the vortices generated from the same streak are staggered along the streamwise direction, while the vortices induced by different streaks tilt toward the normal direction due to the mutual induction effect. It is the spatial variations of the streamwise vortices that cause the lift-up of the streaks. By resolving the transport dynamics of enstrophy, the strength of the vortices is found to continuously grow in the logarithmic layer through the vortex stretching mechanism during the evolution of streaks. The enhancement of the vortices contributes to the spanwise oscillation and the following breakdown of the low-speed streaks.