1979
DOI: 10.2514/3.7632
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Two-point LDV measurements in a plane mixing layer

Abstract: Investigations into the nature of the large structures in a two-dimensional shear layer were carried out using laser Doppler velocimetry in the GALCIT free-surface water tunnel. By simultaneous measurements of velocity at two points outside the turbulent region, above and below the shear layer, it was possible to measure the strength (total circulation) and location of the vorticity center of the large structures. It was found that structures not in the process of pairing convect downstream with the center of … Show more

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Cited by 26 publications
(9 citation statements)
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“…-0.025h0) the local transverse location at which ( U > = +(U,+ U z ) ; this is consistent with the results of Koochesfahani et al (1979).…”
Section: Discussionsupporting
confidence: 88%
“…-0.025h0) the local transverse location at which ( U > = +(U,+ U z ) ; this is consistent with the results of Koochesfahani et al (1979).…”
Section: Discussionsupporting
confidence: 88%
“…Also, it is interesting to consider the total circulation of the shear layer per unit wavelength; that is, Γ∕λ Γ o;v ∕λ nΓ o;vs ∕λ. Based on the circulation values in Table 1, and λ∕θ 17.8, Γ∕λ 0.95ΔU, which is consistent with Γ∕λ ∼ 1 for shear layers (e.g., see [14]). Figure 9 displays a comparison between the computed and the measured streamwise velocity profiles at 10 different phases of the oscillation cycle (Ψ 0 to 1 in steps of 0.1).…”
Section: Resultssupporting
confidence: 75%
“…The corresponding induced velocity decays at least quadratically with distance, and hence these differences should have minimal, if any, influence on the computed velocity. The negligible influence of higher-order moments on the induced velocity is also discussed in reference [14] for the specific case of a two-stream shear layer.…”
Section: Vortex-array Modelmentioning
confidence: 97%
“…There is also some evidence that, in mixing layers which have developed from laminar initial conditions, the streamwise vortices survive in the post-transition flow with an average spacing which increases in step with that of the spanwise structures (Jimenez, Cogollos & Bernal 1985;Bernal & Roshko 1986;Bell & Mehta 1992). It seems that the structures are not always present however and, even in situations where their presence has been detected (Koochesfahani et al 1979;Hussain & Zaman 1985), velocity correlation measurements show no evidence of the large-amplitude antisymmetric induced fluctuations characteristic of the vortex amalgamations in the pre-transition flow (Browand & Weidman 1976).…”
Section: Introductionmentioning
confidence: 99%