Abstract

We explore experimentally whether axisymmetry breaking can be exploited for the open-loop control of a prototypical hydrodynamic oscillator, namely a low-density inertial jet exhibiting global self-excited axisymmetric oscillations. We find that when forced transversely or axially at a low amplitude, the jet always transitions first from a period-1 limit cycle to $\mathbb {T}^2$ quasiperiodicity via a Neimark–Sacker bifurcation. However, we find that the subsequent transition, from $\mathbb {T}^2$ quasiperiodicity to $1:1$ lock-in, depends on the spatial symmetry of the applied perturbations: axial forcing induces a saddle-node bifurcation at small detuning but an inverse Neimark–Sacker bifurcation at large detuning, whereas transverse forcing always induces an inverse Neimark–Sacker bifurcation irrespective of the detuning. Crucially, we find that only transverse forcing can enable both asynchronous and synchronous quenching of the natural mode to occur without resonant or non-resonant amplification of the forced mode, resulting in substantially lower values of the overall response amplitude across all detuning values. From this, we conclude that breaking the jet axisymmetry via transverse forcing is a more effective control strategy than preserving the jet axisymmetry via axial forcing. Finally, we show that the observed synchronization phenomena can be modelled qualitatively with just two forced coupled Van der Pol oscillators. The success of such a simple low-dimensional model in capturing the complex synchronization dynamics of a multi-modal hydrodynamic system opens up new opportunities for axisymmetry breaking to be exploited for the open-loop control of other globally unstable flows.

Highlights

  • Open jet flows are ubiquitous in nature and engineering

  • To assess the symmetry of the vortical structures in the jet, we show in figures 7(g–i) the dominant spatial modes extracted via dynamic mode decomposition (DMD; Schmid 2010; Rowley & Dawson 2017) of the in-plane velocity field (u, v) measured with particle image velocimetry (PIV)

  • In the transversely forced jet, we find markedly different behaviour: synchronous quenching of the natural mode still occurs (Pn∗ → 0), the forced mode is not amplified to a degree sufficient to cause Pt∗ to exceed Pt, implying the absence of resonant amplification

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Summary

Introduction

Open jet flows are ubiquitous in nature and engineering. Over the years, their spatiotemporal stability and dynamics have been studied extensively (Huerre & Monkewitz 1990; Schmid & Henningson 2001; Drazin & Reid 2004). If the jet discharges from a round non-swirling nozzle with thin shear layers, its dynamics will be dominated by axisymmetric (bulging) oscillations with azimuthal wavenumber m = 0, which can arise via a supercritical or subcritical Hopf bifurcation (Sreenivasan, Raghu & Kyle 1989; Monkewitz et al 1990; Kyle & Sreenivasan 1993; Hallberg & Strykowski 2006; Zhu, Gupta & Li 2017, 2019). Such self-excited oscillations are desirable in some situations because they can aid mixing and transport.

Forced synchronization and its amplitude suppression mechanisms
Axial forcing of globally unstable jets
Transverse forcing of jets
Contributions of the present study
Experimental set-up
Jet nozzle and velocity measurements
Acoustic pressure field
A B CDE y
Low-dimensional model
Natural jet dynamics
Forced jet response
Synchronization maps
Amplitude suppression and symmetry breaking of the wavemaker region
Bifurcation routes to lock-in
Axial forcing: the jet at position A
Transverse forcing: the jet at position E
Asynchronous quenching
Synchronous quenching
Findings
Conclusions
Full Text
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