Elucidating the 3D topology of a cantilevered square cylinder wake using multi-time-delay estimation with FIR-based SPOD
ORAL
Abstract
FIR-based spectral proper orthogonal decomposition (SPOD) (Sieber et al., 2016) is used for remote-sensor based estimation of a highly modulated bluff body wakes. The estimator is trained on individual stereoscopic particle image velocimetry (PIV) planes synchronized with surface pressure measurements. Estimation is then used to reconstruct time-resolved 3D coherent motions with the aim of investigating cycle-to-cycle variations in vortex interactions. The candidate flow is the near turbulent, quasi-periodic near-wake of a cantilevered square cylinder with a height-to-width ratio 4, protruding a thin laminar boundary layer at a Reynolds number of 10600. In a phase-averaged sense, the wake is described as a half-loop shedding pattern, consisting of inter-connected Kármán vortex structures.
We show the benefits of this convolutional SPOD in reconstructing the flow and identifying coherent wake interactions. Unlike phase-averaging, which provides only a representation of the average contributions at the fundamental Kármán shedding frequency (fs) and its harmonics, the present approach also captures slow-varying motions at fL = 0.1fs and inter-harmonic contributions. The slow-varying motion, which arises from shear layer instabilities originating at the obstacle free-end, is shown to modulate intensity of the fundamental vortex-shedding. Inclusion of the inter-harmonic modes allows capturing of shedding disruptions, which in extreme cases manifest as vortex dislocations.
We show the benefits of this convolutional SPOD in reconstructing the flow and identifying coherent wake interactions. Unlike phase-averaging, which provides only a representation of the average contributions at the fundamental Kármán shedding frequency (fs) and its harmonics, the present approach also captures slow-varying motions at fL = 0.1fs and inter-harmonic contributions. The slow-varying motion, which arises from shear layer instabilities originating at the obstacle free-end, is shown to modulate intensity of the fundamental vortex-shedding. Inclusion of the inter-harmonic modes allows capturing of shedding disruptions, which in extreme cases manifest as vortex dislocations.
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Presenters
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Chris Morton
McMaster University
Authors
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Chris Morton
McMaster University
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Ali Mohammadi
University of Calgary
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Robert J Martinuzzi
University of Calgary