Direct numerical simulation of the effect of inlet isotropic turbulence on centrifugal instabilities over a curved wall. (30th September 2018)

• Record Type: Journal Article
• Authors: Sharma, S.; Ducoin, A.
• Is Part Of: Computers & fluids. Volume 174(2018)
• Page Start: 1
• Page End: 13
• Publication Date: 2018-09-30
• Subjects: Laminar to turbulent transition -- Görtler vortices -- Von Kármán energy spectrum -- Direct numerical simulation; Fluid dynamics -- Data processing -- Periodicals; 532.050285
• DOI: 10.1016/j.compfluid.2018.07.018
• Languages: English
• ISSNs: 0045-7930

Abstract

Highlights: The initial development of instabilities can be receptive to inflow conditions. In that case, this induces a sharper transition to turbulence along the curved wall. The secondary instabilities seems less receptive to inflow conditions. Abstract: The Direct Numerical Simulations (DNS) are carried out in order to capture the flow instabilities and transition to turbulent flow over a curved wall. The simulations are performed using the open source code NEK5000, which solves the incompressible Navier–Stokes equations using high order, spectral element method. The primary objective is to investigate the effect inlet isotropic turbulence, and the development of centrifugal instabilities induced during laminar to turbulent transition. Free-stream turbulence intensities of 0.1% and 1% amplitude have been investigated. The obtained results are compared with existing numerical and experimental reference studies. The investigation of the flow supports the fact that the Görtler vortices show up, which trigger the transition to turbulence. This mechanism appears to be very sensitive to the inlet conditions. It is observed that it occurs earlier as the turbulence intensity increases, with a sharper transition, characterized by a more random longitudinal streaks distribution in the span-wise direction due to the non uniform, atmospheric turbulence prescribed at the inlet. The decreased turbulence intensity leads to more uniform distribution of the streaks and a longer transitional region along the plate. The characteristic frequency of secondary instability is found to be less receptive to the inflow conditions.