Abstract
Low-frequency unsteadiness of a reattaching shear layer was studied in the flow behind a backward-facing step. Spectral data from a hot-wire probe showed that a substantial fraction of the measured turbulence intensity occurs at frequencies significantly lower than the large eddy passing frequency. Several thermal tuft probes were used simultaneously to identify the source of the low-frequency disturbances. It was concluded that the reattaching free shear layer undergoes a non-periodic, roughly two-dimensional, vertical motion. The motion causes the impingement point of the reattaching shear layer to drift slowly up- and downstream over a range of approximately two step heights. The likely cause of the low-frequency motion is an instantaneous imbalance between the entrain-ment rate from the recirculation zone and the reinjection rate near reattachment.
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Abbreviations
- F :
-
Frequency [Hz]
- h :
-
Step height = 5.08 cm
- U 0 :
-
Inlet free stream velocity
- x :
-
Streamwise coordinate
- x R :
-
Time mean reattachment location
- γ:
-
Percent of time that flow is in downstream direction
- θ:
-
Momentum thickness
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© 1982 Springer-Verlag Berlin Heidelberg
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Eaton, J.K., Johnston, J.P. (1982). Low Frequency Unsteadyness of a Reattaching Turbulent Shear Layer. In: Bradbury, L.J.S., Durst, F., Launder, B.E., Schmidt, F.W., Whitelaw, J.H. (eds) Turbulent Shear Flows 3. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-95410-8_16
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DOI: https://doi.org/10.1007/978-3-642-95410-8_16
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