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An investigation of the scales in transitional boundary layers under high free-stream turbulence conditions

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Abstract

The scales in a transitional boundary layer subject to high (initially 8%) free-stream turbulence and strong acceleration (K as high as 9×10−6) were investigated using wavelet spectral analysis and conditional sampling of experimental data. The boundary layer shows considerable evolution through transition, with a general shift from the lower frequencies induced by the free-stream unsteadiness to higher frequencies associated with near-wall-generated turbulence. Within the non-turbulent zone of the intermittent flow, there is considerable self-similarity in the spectra from the beginning of transition to the end, with the dominant frequencies in the boundary layer remaining constant at about the dominant frequency of the free-stream. The frequencies of the energy-containing scales in the turbulent zone change with streamwise location and are significantly higher than in the non-turbulent zone. When normalized on the local viscous length scale and velocity, however, the turbulent zone spectra also show good self-similarity throughout transition. Turbulence dissipation occurs almost exclusively in the turbulent zone. The velocity fluctuations associated with dissipation are isotropic, and their normalized spectra at upstream and downstream stations are nearly identical. The distinct differences between the turbulent and non-turbulent zones suggest the potential utility of intermittency based transition models in which these zones are treated separately. The self-similarity noted in both energy containing and dissipation scales in both zones suggests possibilities for simplifying the modeling for each zone.

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Notes

  1. Results based on the turbulent zone wavelet spectra agreed well with those of Fig. 20 up to the peak, but then continued to increase monotonically at higher frequencies. Comparison of the composite flow wavelet and Fourier spectra revealed very good agreement over nearly all frequencies, including all those associated with the energy containing scales described in the sections above. Some small differences were always present in the high frequency tails of the spectra, however, with the magnitudes of the wavelet spectra always slightly higher than those of the Fourier spectra. While insignificant in terms of energy, the difference was significant in terms of dissipation. A different wavelet than the Mexican Hat may have produced better results, but since virtually all the dissipation occurs in the turbulent zone, the composite flow Fourier spectra can be normalized using the local intermittency at each station to give the time averaged turbulent zone contribution.

Abbreviations

C :

dilation factor

FSTI:

free-stream turbulence intensity

f :

frequency in Hz

f fs :

frequency in Hz of free-stream v spectra peak

K :

(ν /U 2)(dU /dx), acceleration parameter

PSD:

power spectral density

Re x :

U x/ν, Reynolds number

Re λ :

\(\overline {u^{'2} } \sqrt {15/(\nu \varepsilon )} ,\)

Re θ :

momentum thickness Reynolds number

t :

time

U :

local free-stream velocity

u :

instantaneous streamwise velocity

u :

instantaneous streamwise fluctuating velocity

u τ :

\(\sqrt {\tau _{{\rm w}} /\rho} \)

-uv:

instantaneous turbulent shear stress

v :

instantaneous wall normal velocity

v :

instantaneous wall normal fluctuating velocity

w :

wavelet function

x :

streamwise coordinate, distance from leading edge

y :

cross-stream coordinate, distance from wall

y + :

yuτ /ν, distance from wall in wall coordinates

Γ:

intermittency function

γ:

intermittency, time average of Γ (fraction flow is turbulent)

γ pk:

peak intermittency in profile

δ99.5:

99.5% boundary layer thickness

ε:

turbulence dissipation rate

ν:

kinematic viscosity

ρ:

density

τ w :

wall shear stress

θ:

momentum thickness

-:

(overbar) time average

∞:

free-stream

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Correspondence to Ralph J. Volino.

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Volino, R.J. An investigation of the scales in transitional boundary layers under high free-stream turbulence conditions. Exp Fluids 38, 516–533 (2005). https://doi.org/10.1007/s00348-005-0945-0

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