1. Introduction
Self-sustained oscillations arising from the coupling between acoustics and the underlying flow field have been an active topic of research for several decades. These oscillations, commonly referred to as aeroacoustic instabilities, have garnered significant attention due to their profound impact on various engineering systems. Such instabilities can induce large-amplitude pressure oscillations, leading to extreme sound pressure levels and severe structural vibrations (Chanaud & Powell Reference Chanaud and Powell1965; Hirschberg & Rienstra Reference Hirschberg and Rienstra2004; Ziada Reference Ziada2010).
1.1. Previous studies on aeroacoustics of orifices and cavities in ducts
A classical example of self-sustained aeroacoustic instability is the generation of sound by the impingement of a shear layer on a solid structure. This phenomenon has been widely studied in various subcategories such as edge tones or cavity tones (Rockwell & Naudascher Reference Rockwell and Naudascher1979). Aeroacoustic instabilities also occur in pipelines, combustion chambers, safety relief valves, heat exchanger tube bundles, air conditioning systems and turbomachinery applications (Baines Reference Baines2005). Such a wide scope of fluid systems where such instabilities are encountered and the potential downsides on their occurrence underscore the importance of understanding and mitigating them in practical scenarios.
In aviation and automotive applications, the flow within the engine ducts is typically restricted (Heywood Reference Heywood1988). Such structural flow obstructions within the ducts can significantly affect both aeroacoustic behaviour and flow-induced vibrations. A common obstruction in these systems is the flow through an orifice. Vortical structures are formed due to shear layer instabilities at the orifice lip. For instance, in segmented solid rocket motors (Brown et al. Reference Brown, Dunlap, Young and Waugh1981), incorporating inert substances (called inhibitors) to fill the gaps between segments leads to restrictions in the flow field resulting in vortex shedding across the inhibitors.
The occurrence of periodic vortex generation and lock-in with duct acoustic modes has been extensively discussed in the literature for confined flows (Anderson Reference Anderson1954, Reference Anderson1955; Stubos et al. Reference Stubos, Benocci, Palli, Stoubos and Olivari1999; Karthik, Chakravarthy & Sujith Reference Karthik, Chakravarthy and Sujith2008). The vortices generated by an orifice can lead to acoustic disturbances on downstream impingement. If the flow is confined between two orifice plates, a cavity flow is generated between the orifice plates and the downstream impingement happens typically on the front wall of the second orifice plate. The generated acoustic disturbances propagate upstream and can be enhanced through diffraction at the edge of the orifice. Consequently, the shear layer near the detachment point becomes disturbed, and this disturbance travels downstream, initiating a self-sustaining process (Culick & Magiawala Reference Culick and Magiawala1979). In summary, restrictor-generated vortices can cause acoustic disturbances and perturbations in the shear layer that can propagate downstream and become self-sustaining.
Gloerfelt & Lafon (Reference Gloerfelt and Lafon2008) simulated sound generation by a slit-shaped diaphragm in a square duct at low Mach numbers. Their findings identified the breakdown of coherent structures before wall reattachment as the primary mechanism responsible for sound generation. Bauerheim, Boujo & Noiray (Reference Bauerheim, Boujo and Noiray2020) conducted a comprehensive numerical study to investigate the behaviour of deep cavities subjected to low-Mach-number flows. Their research focused on the dynamic interplay between the flapping of the shear layer, vortex shedding and their interaction with the acoustic field. They observed a transition from a flapping shear layer with moderate acoustic levels to vortex shedding with comparatively higher acoustic levels.
Through experimental investigations and theoretical analysis, Bourquard et al. (Reference Bourquard, Faure-Beaulieu and Noiray2021) developed a new model to explain aeroacoustic instability in deep cavities. In their work, Bourquard et al. (Reference Bourquard, Faure-Beaulieu and Noiray2021) proposed a theoretical framework that depicts the aeroacoustic system as comprising two linearly stable oscillators. These oscillators exhibit linear reactive coupling, nonlinear damping and nonlinear resistive coupling, and they also observed that the aeroacoustic system experiences only supercritical Hopf bifurcations, distinguishing it from many other flow-generated vibration problems.
In disagreement with previous findings on the relationship between vortical and acoustic disturbances, Jou & Menon (Reference Jou and Menon1990) reported that vortices act independently of the acoustic modes of the conduit. The amplification of the acoustic disturbance associated with the phase and shedding frequency of vortices from the restrictors was studied, leading to the development of a semiempirical correlation for the critical Strouhal number as a function of the restrictor size (Stubos et al. Reference Stubos, Benocci, Palli, Stoubos and Olivari1999).
Recent studies have explored the dynamics of aeroacoustic systems through the lens of dynamical systems theory (Boujo et al. Reference Boujo, Bourquard, Xiong and Noiray2020; Bourquard et al. Reference Bourquard, Faure-Beaulieu and Noiray2021; Bhavi, Pavithran & Sujith Reference Bhavi, Pavithran and Sujith2024). Self-sustained oscillations associated with whistling sounds are identified as limit cycles (Nair & Sujith Reference Nair and Sujith2016), while low-amplitude aperiodic acoustic pressure oscillations characterize stable operation in aeroacoustic systems. Typically, system dynamics are analysed by varying a control parameter, transitioning from steady operation to aeroacoustic instability. Nair & Sujith (Reference Nair and Sujith2016) demonstrated that during the transition from stable operation to instability, the system enters a state of intermittency, marked by bursts of periodic oscillations interspersed with intervals of aperiodicity. By analysing unsteady acoustic pressure oscillations in this intermittent phase, they identified precursors to aeroacoustic instabilities.
Other studies have also reported intermittency in flow through orifices and grazing flows. Numerical simulations by Kamin, Mathew & Sujith (Reference Kamin, Mathew and Sujith2019) revealed that inlet turbulent flow fluctuations excite the intermittent growth and breakup of the jet shear layer, resulting in intermittency. Previous research has demonstrated that the whistling frequency in an aeroacoustic system with flow through orifices shifts as the control parameter (flow velocity) is varied (Rockwell Reference Rockwell1983; Karthik et al. Reference Karthik, Chakravarthy and Sujith2008). Bhavi et al. (Reference Bhavi, Pavithran and Sujith2024), in their recent study, identified three distinct scenarios for such frequency changes: a direct and abrupt transition between two limit cycle oscillations; a transition via intermittent state; a transition occurring through an aperiodic state.
1.2. Control strategies for various hydrodynamic and acoustic instabilities
There are two primary methods for controlling acoustic instabilities: passive and active. Passive control strategies involve using various techniques to increase the damping of the system by making specific modifications to the system design (Richards, Straub & Robey Reference Richards, Straub and Robey2003; Noiray et al. Reference Noiray, Durox, Schuller and Candel2007). Active control is classified into two types based on the presence of real-time feedback from the sensor to the actuator. Active closed-loop control is when feedback is present, and active open-loop control is when feedback is absent.
The open-loop control of flows exhibiting oscillator-like behaviour is a significant topic in fluid mechanics. Oscillators refer to flows with inherent unsteadiness marked by a distinct, well-defined frequency that remains largely unaffected by low-level external disturbances (Huerre & Rossi Reference Huerre and Rossi1998). Examples of such oscillator flows include bluff-body configurations like cylinders and open cavities. Sipp (Reference Sipp2012) focuses on open-loop control strategies that specifically target modifications to the properties of the wake rather than the boundary layer. The primary objective of such control is either to suppress the natural frequency of the flow or, if suppression is unfeasible, to shift this frequency to a desired value. Richards et al. (Reference Richards, Thornton, Robey and Arellano2004) noted that the open-loop control approach is most effective when the system operates near its stability limit, indicating that the ability of open-loop control to manage highly nonlinear oscillations may be limited. Acoustic forcing has also proven to be a successful approach to reducing the strength of acoustic oscillations (Li & Juniper Reference Li and Juniper2013b ; Kushwaha et al. Reference Kushwaha, Worth, Dawson, Gupta and Li2022). Open-loop control mitigates thermoacoustic instabilities by applying external periodic forcing to the system without relying on real-time feedback from the combustor. This approach offers a simpler and more cost-effective alternative to closed-loop systems. Large-amplitude limit-cycle oscillations are suppressed by introducing harmonic excitation at a frequency distinct from the system’s natural frequency (Mondal, Pawar & Sujith Reference Mondal, Pawar and Sujith2019; Roy et al. Reference Roy, Mondal, Pawar and Sujith2020).
1.3. Forced synchronization in hydrodynamic and acoustic instabilities
When a self-sustained oscillator is subjected to periodic forcing with a specific frequency that is not its natural frequency, it can adjust its oscillation frequency to match the frequency of the external forcing – a phenomenon known as synchronization (Pikovsky, Rosenblum & Kurths Reference Pikovsky, Rosenblum and Kurths2001). Various natural systems have been observed to exhibit this behaviour, such as fireflies, circadian rhythms, clapping spectators, triode circuits and pacemakers (Pikovsky & Maistrenko Reference Pikovsky and Maistrenko2012).
Forced synchronization refers to the phenomenon in which harmonic forcing and self-sustained limit-cycle oscillations are considered as two oscillators that are coupled in a unidirectional manner (Pikovsky et al. Reference Pikovsky, Rosenblum and Kurths2001). This implies that the forcing influences the limit-cycle oscillations, not vice versa. The natural frequency of limit-cycle oscillations becomes synchronized with the frequency of external forcing (
$f_n=f_f$
), and the phase difference between them is constrained to a narrow range centred around a specific average value (Pikovsky et al. Reference Pikovsky, Rosenblum and Kurths2001).
The typical behaviour of an oscillator undergoing forced synchronization can be divided into two states: locking and suppression. When the oscillator synchronizes through locking, the spectral peak associated with the natural frequency shifts towards the forcing frequency as the forcing amplitude increases. However, for synchronization through suppression, the spectral amplitude associated with the natural frequency of the oscillator gradually decreases and eventually vanishes as the forcing amplitude increases (Balanov et al. Reference Balanov, Janson, Postnov and Sosnovtseva2009; Li & Juniper Reference Li and Juniper2013; Mondal et al. Reference Mondal, Pawar and Sujith2019; Roy et al. Reference Roy, Mondal, Pawar and Sujith2020; Kushwaha et al. Reference Kushwaha, Worth, Dawson, Gupta and Li2022).
Locking has been studied in different flow scenarios, including cylinder wakes (Koopmann Reference Koopmann1967; Van, Charles & Gharib Reference Van, Charles and Gharib1987; Karniadakis & Triantafyllou Reference Karniadakis and Triantafyllou1989), and low-density jets (Sreenivasan, Raghu & Kyle Reference Sreenivasan, Raghu and Kyle1989; Juniper, Li & Nichols Reference Juniper, Li and Nichols2009). Barbi et al. (Reference Barbi, Favier, Maresca and Telionis1986) deliberately subject a wake to external excitation at its natural frequency by means of acoustics or mechanical ways. Their investigation explores the wake response under various conditions. When unforced, the wake exhibits periodic oscillations, i.e. a limit cycle. With weak external forcing, the wake oscillates quasiperiodically, with a shift in natural frequency. Under strong forcing, the wake synchronizes with the external stimulation. Notably, the minimum forcing amplitude for synchronization is asymmetric with respect to the natural frequency, as highlighted in studies by Blevins (Reference Blevins1985) and Barbi et al. (Reference Barbi, Favier, Maresca and Telionis1986).
Harmonically forcing the limit cycle leads to various complex phenomena such as frequency entrainment, pulling and pushing (Balusamy et al. Reference Balusamy, Li, Han, Juniper and Hochgreb2015). Frequency entrainment is observed in reacting and non-reacting low-density jets (Juniper et al. Reference Juniper, Li and Nichols2009). In another study on a low-density, self-excited, non-reacting jet, Li & Juniper (Reference Li and Juniper2013b ) acoustically forced the low-density jet. The system response was asymmetric around the natural frequency of the oscillator, and synchronization was achieved for forcing frequency around the natural frequency of the self-excited jet (Li & Juniper Reference Li and Juniper2013b ).
Periodic forcing of the system close to its instability frequency leads to amplitude suppression via synchronous quenching. Amplitude suppression when forcing the system far from the instability frequency is known as asynchronous quenching (Roy et al. Reference Roy, Mondal, Pawar and Sujith2020). In the study conducted by Bellows, Hreiz & Lieuwen (Reference Bellows, Hreiz and Lieuwen2008), it was observed that a swirl-stabilized combustor experienced an amplitude reduction of around 65 % when the combustor was forced to operate close to its natural frequency. Similarly, a laminar combustor (Roy et al. Reference Roy, Mondal, Pawar and Sujith2020) also showed an amplitude reduction of 90 %, indicating the efficacy of the open-loop active control method. In the case of synchronous quenching, as the forcing frequency is close to the natural mode, the response amplitude is usually increased through resonance phenomenon (Odajima, Nishida & Hatta Reference Odajima, Nishida and Hatta1974; Abel, Ahnert & Bergweiler Reference Abel, Ahnert and Bergweiler2009).
Recently, asynchronous quenching was reported in combustors (Mondal et al. Reference Mondal, Pawar and Sujith2019; Roy et al. Reference Roy, Mondal, Pawar and Sujith2020) and globally unstable jets (Kushwaha et al. Reference Kushwaha, Worth, Dawson, Gupta and Li2022). An asynchronous quenching mechanism stabilizes the natural mode of a self-excited oscillator to a fixed point through periodic external forcing applied at a detuned, off-resonance frequency sufficiently far from the natural frequency (Minorsky Reference Minorsky1967). Typically, asynchronous quenching significantly reduces the response amplitude of the system – often to less than 20 % of its uncontrolled natural amplitude – without amplifying the forcing signal (Guan et al. Reference Guan, Gupta, Kashinath and Li2019a , Reference Guan, He, Murugesan, Li, Liu and Lic ). This reduction results from the destabilization of the original limit-cycle attractor asymptotically by external forcing (Minorsky Reference Minorsky1967).
In the context of cylinder wakes, Olinger (Reference Olinger1993) demonstrated that a forced Landau–Stuart model effectively replicates numerous aspects of quasiperiodicity and lock-in. This includes the occurrence of lock-in beyond a threshold forcing amplitude and a proportional rise in amplitude with frequency detuning. Various other modelling approaches include using oscillator equations to model the forced limit cycle (Juniper et al. Reference Juniper, Li and Nichols2009; Li & Juniper Reference Li and Juniper2013b
,
Reference Li and Juniperc
). A theoretical study was recently conducted on the lock-in phenomenon occurring in vortex-shedding combustors by Britto & Mariappan (Reference Britto and Mariappan2019). They observed that lock-in is achieved via a quasiperiodic route when the forcing amplitude increases. However, as the amplitude was further increased, de-lock-in was also observed. They also examined various routes through which the system transitions from a higher-order
$p:1$
lock-in state to a
$1:1$
lock-in state through lock-in and de-lock-in events.
1.4. Motivation and contributions of the present study
It is well known that cavity flows can develop self-sustained acoustic oscillations at discrete natural frequencies, which are determined by the geometry and flow conditions of the system. These oscillations result from the interaction between vortex shedding and acoustic feedback within the cavity, leading to limit cycle behaviour. The strategy of open-loop control has also been studied previously for self-excited aeroacoustic systems. However, there is no clear demonstration of the types of amplitude suppression or the dynamical regimes available to an aeroacoustic system at a fundamental level. There is also limited understanding on the optimal forcing regimes for effective amplitude suppression or the potential downsides to forcing at suboptimal regimes or even to the possibility of de-lock-in. There are also no simple phenomenological models that can effectively capture all the rich features reported in various aeroacoustic systems due to the limited understanding of the influence of modal parameters on the observed phenomena. These then form the motivation for us to explore lock-in behaviour in a prototypical aeroacoustic system.
In the present study, we harmonically force the flow through a cavity bound by two circular orifice plates at its natural limit cycle state across a spectrum of forcing frequencies. We study various transition regimes at these frequencies as the forcing amplitude is increased towards lock-in and investigate the possibility of de-lock-in. Next, we formulate a reduced-order phenomenological model (ROPM) from first principles based on vortex–acoustic interaction to reproduce various transitions observed in experiments. Based on the findings from experiments and model behaviour, we discuss the optimal regime in which open-loop active control is most effective by investigating the power transfer between the forced and natural modes during harmonic forcing at various forcing amplitudes.
The structure of the paper is as follows: § 2 provides an overview of the experimental set-up and the methodology employed. In § 3, various regimes identified on harmonically forcing a double-orifice cavity flow at its limit cycle state are explained in detail. Modal power transfer between various modes of forcing and effectiveness of control is presented in § 4. In § 5, a ROPM based on vortex dynamics is developed to capture and explain the experimental results. Finally, § 6 presents the key conclusions derived from this study.
2. Experiments and analysis
The experimental set-up consists of a plenum chamber with a length of 420 mm and a diameter of 300 mm, as illustrated in figure 1. Connected to the plenum chamber is a square duct with a cross-section of 75 mm
$\times$
75 mm and a length of 750 mm. At the end of the duct are two orifice plates with a thickness of 15 mm and a gap of 50 mm between the two plates. The orifice is circular with a diameter of 25 mm generating a cavity flow between the orifice plates. A screw compressor provides the air supply, and airflow is regulated by an Alicat 500 MCR mass flow controller, which has an uncertainty range of
$\pm$
0.8
$\%$
of the reading and 0.20
$\%$
of full-scale flow measurements.
The flow is forced harmonically using an Ahuja 16
$\Omega$
impedance AU-60 speaker. The speaker is located 150 mm from the end of the settling chamber. The harmonic signal from the MATLAB signal generator is fed to the power amplifier (Crown XLI 800), and the gain is adjusted to a value of one unit for all experiments. The speaker is connected in parallel to the amplifier. The damping in the system was measured without flow prior to each experiment to ensure that it remained within
$32.6 \pm {3}\,\rm s^{-1}$
by estimating the exponential decay rate of acoustic waves in the experimental chamber.
Acoustic measurements
$p'$
are obtained using a PCB-378C10 microphone (with a sensitivity of
$1 \rm mV\,(kPa^{-1})^{-1}$
and a
$\pm$
0.8
$\%$
uncertainty) placed behind the first orifice plate (745 mm from the settling chamber). The location of the microphone is sufficiently distant from a pressure node and the speaker to ensure reliable data acquisition (DAQ). An analogue to digital card (NI-6143,16 bits) is used to acquire the signals from the piezoelectric transducer at a sampling rate of 20 kHz for 5 s.
The fast Fourier transform technique is utilized to estimate the frequency components of the dynamic pressure (
$p'$
) time series. We sample the datasets at a frequency of 20 kHz to avoid any spectral leakage and accurately capture the limit-cycle signal of the unforced system the frequency of which was estimated to be 150.6 Hz. The sampling frequency is high enough to satisfy the Nyquist criterion for frequencies in a reasonable neighbourhood of this natural frequency (Hearn & Metcalfe Reference Hearn and Metcalfe1995). We collected 1 00 000 data points at each forcing condition, equivalent to around 753 oscillation cycles at the natural frequency. The fast Fourier transform algorithm employed a bin size of 0.2 Hz for frequency resolution, leading to 65 537 bins.
The experimental set-up consists of a plenum chamber connected to a duct with two orifice plates at its end. It includes a speaker for forcing, an amplifier, a microphone, a signal conditioner and a mass flow controller, all integrated and managed through a DAQ system installed on a personal computer (PC). All dimensions are in millimetres.

Various synchronization states are discerned through the behaviour of the instantaneous phase difference (
$\Delta \phi$
=
$\phi _{r} -\phi _{f}$
) between the response signal (
$p^{\prime}_{r}$
) and the forcing signal
$p^{\prime}_{f}$
. The instantaneous phases are obtained by applying the Hilbert transform to the respective signals. The Hilbert transform calculates the phase angle of each complex-valued signal using the arctangent function.
In the phase-locked state, the instantaneous phases and frequencies of the forcing and response signals satisfy
$\Delta \phi =0$
and
$\Delta \omega =0$
(Pikovsky et al. Reference Pikovsky, Rosenblum and Kurths2001). However, in the phase-trapped state, the relative phase between the forcing signal and the response signal exhibits a bounded oscillatory pattern, leading to the synchronization of the mean frequencies of the signals without achieving instantaneous phase lock-in; i.e.
$\Delta \phi \neq 0$
and
$\Delta \omega =0$
(see figure 2
c). Phase-drifting (or phase-slipping) refers to the continuous increase or decrease over time of the unwrapped relative phase between the forcing and response signals. When the forcing frequency is less than the natural frequency, the phase difference between the response and the forcing signals will increase over time. This happens because the system’s natural oscillation frequency is faster than the forcing frequency (see figure 2
a). Similarly, when the forcing frequency is more than the natural frequency, the phase difference between the response and the forcing signals will increase over time as can be seen in figure 2(b).
We perform a transverse intersection of the trajectory of evolution of the response signal using techniques of dynamical systems theory and analyse the resulting intercepts to gain insights into the system’s topology and geometry. This method, known as a one-sided Poincaré map, reveals unique characteristics of different nonlinear responses. To illustrate, a limit cycle, represented by a closed trajectory, appears as a single blob on the map. Detailed information on obtaining the phase trajectory and one-sided Poincaré maps from the experimental data is presented in Appendix A.1.
(a) Phase-drifting (
$f_f/f_n\gt 1$
), (b) phase-drifting (
$f_f/f_n\lt 1$
), (c) phase-trapping and (d) lock-in.

3. Results and discussion
It is essential to analyse the flow system’s natural oscillation state to examine the oscillatory behaviour of a system subjected to external perturbations. From previous studies on the same system (Singh, Mukherjee & Nair Reference Singh, Mukherjee and Nair2024), the various qualitatively different flow regimes for variations in the mass flow rate (mean velocity through the orifice plate
$u_0$
) in the unforced system were identified. At low mean flow velocities (
$u_0$
= 0.5–1
$\mathrm{m\,s^{- 1}}$
), a hydrodynamic mode is present with very low amplitudes that corresponds to pure vortex shedding. As mean velocity is further increased (
$u_0$
= 1.1–2.2
$\mathrm{m\,s^{- 1}}$
), an interaction between the hydrodynamic and acoustic modes is observed in the pressure spectra. As the mean velocity increases further (
$u_0$
= 2.3–4
$\mathrm{m\,s^{- 1}}$
), the vortex shedding mode locks-in with the acoustic mode, leading to large-amplitude limit cycle behaviour. The system traces the same path in both forward and backward variation of flow velocity without any hysteresis.
For the external harmonic forcing experiments reported in this study, we consider an operating with mean velocity
$u_0$
= 2.6
$\mathrm{m\,s^{- 1}}$
where we have self-sustained limit cycle oscillations for the unforced system characterized by a dominant frequency
$f_n$
of 150.6 Hz and its harmonics. This operating condition is sufficiently away from any critical points of transition of the unforced system.
We perform external forcing experiments for various forcing frequencies
$f_f$
and forcing amplitudes
$\sigma _f$
. To estimate the forcing amplitude, we measure the pressure fluctuations
$p^{\prime}$
at the location of the transducer at the forcing frequency without flow. The forcing amplitude is then calculated as
$\sigma _f=u^{\prime}_{rms}/u_0$
, where
$u^{\prime}_{rms}$
is calculated using the acoustic relationship for harmonic waves from the estimated root-mean-square (r.m.s.) of measured pressure fluctuations
$p^{\prime}$
without flow.
For a chosen forcing frequency, we systematically increase the forcing amplitude of the unforced flow system until lock-in is observed. Once lock-in is achieved at the specified forcing frequency for a given amplitude, the forcing is turned off, allowing the system to return to its natural limit-cycle state. This whole process is repeated for multiple forcing frequencies between
$0.49\leqslant f_f/f_n \leqslant 1.48$
. Repeatability was ensured in the measurements by performing the same set of experiments five times.
Four qualitatively different regimes are observed in the transition to lock-in over the studied range of frequencies: (i) synchronous quenching regime (0.9
$\leqslant$
$f_f$
/
$f_n$
$\leqslant$
1.1); (ii) asynchronous quenching regime (0.67
$\leqslant$
$f_f$
/
$f_n$
$\leqslant 0.88$
and 1.13
$\leqslant$
$f_f$
/
$f_n$
$\leqslant$
1.48); (iii) de-lock-in regime (
$ 0.55 \leqslant f_f /f_n \leqslant 0.65$
); (iv)
$1:2$
lock-in regime (
$ 0.49 \leqslant f_f /f_n \leqslant 0.51$
).
(a) Pressure time series, (b) frequency spectrum, (c) phase difference plots and (d) one-sided Poincaré maps for various system dynamics on varying the forcing amplitude in synchronous quenching regime (
$f_f=147.6$
Hz, or
$f_f/f_n=0.98$
).

3.1. Synchronous quenching regime
$(0.9 \leqslant f_f /f_n \leqslant 1.1)$
Forcing near the natural frequency demonstrates synchronous quenching at lock-in. Results for harmonic forcing at
$f_f$
= 147.6 Hz (
$f_f/f_n =0.98$
) are presented in figure 3. When the forcing amplitude is zero (
$\sigma _f$
= 0), a single natural frequency, represented by a sharp peak in the spectral domain of the signal, at
$f_n$
= 150.6 Hz, is observed (see figure 3
bi). This peak is followed by less prominent peaks at higher harmonics, indicating that the limit cycle oscillations are not perfectly sinusoidal. The Poincaré map also shows the presence of a small filled blob (figure 3
d i), which confirms that vortex shedding occurs periodically in the limit cycle state.
Figure 3(a ii,b ii,c ii,d ii) represents the dynamics when the system is forced at low amplitudes (
$\sigma _f$
= 0.009). The interplay between the forcing and natural frequencies gives rise to sidebands resulting from nonlinear wave-triadic interactions. These sidebands indicate a Neimark–Sacker bifurcation (or torus-birth bifurcation) leading to quasiperiodic behaviour (Nayfeh & Balachandran Reference Nayfeh and Balachandran2008). Poincaré map reveals a closed loop, signifying the transition to a stable ergodic
$T^2$
torus attractor (see figure 3
dii). Two incommensurate modes at
$f_f$
and
$f_n$
and their linear combinations in the pressure spectra confirm the presence of quasiperiodicity; see figures 3(bii) and 3(biii). The size of the torus increases as the forcing amplitude increases (
$\sigma _f$
= 0.015) (see figure 3
d iii).
The presence of phase-drifting is evident in the phase difference plots shown in figures 3(c ii) and 3(c iii). In the regimes and for the forcing amplitudes resulting in phase-drifting, the frequency of the vortex shedding process is drifting in a nonlinear albeit regular manner. This leads to the observed temporal evolution of phase difference between forcing and the response pressure signals with extended intervals during which phase difference remains nearly constant, punctuated by brief episodes of rapid increase for
$f_f\lt f_n$
. The phase variation becomes constant when the vortex-shedding frequency of the forced system approaches the forcing frequency. This in turn leads to an increase in the amplitude of the response. The amplitude starts to drop when the vortex shedding frequency eventually drifts away from the forcing frequency towards its natural frequency. The range of drifting of the vortex shedding frequency is always bounded between
$f_f$
and
$f_n$
; that is, for
$f_f \lt f_n$
, the frequency drift is always between
$f_f$
on the lower end and
$f_n$
on the higher end. This leads to the continuous monotonic increase in phase during phase-drifting for
$f_f \lt f_n$
, as can be seen in figure 3(c ii).
As the forcing strength increases, there is no change in the modulation frequency of the response signal (figure 3 a iii) or the time interval between the slips in phase (figure 3 c iii). This indicates that vortex shedding process exhibits a suppression-type behaviour and not a locking-type behaviour as the natural frequency in the pressure spectrum is not pushed (or pulled) towards the forcing frequency. The amplitude of the response signal is much larger at time instances when the frequency of the response signal drifts towards the forcing frequency through a resonance-type behaviour.
Eventually, the vortex shedding process locks-in completely to the forcing frequency abruptly when the forcing amplitude reaches a critical value, see figure 3(a iv,b iv, c iv,d iv). The system dynamics visualized on the Poincaré map (figure 3
d iv) confirms this abrupt transition as the torus structure transforms into a compact blob, indicating the collapse of the phase trajectory to a different periodic orbit. This abruptness of the breakdown indicates that a saddle-node bifurcation has occurred; in other words, the torus attractor has become resonant and the phase difference between the response signal and the forcing signal reaches a constant value (figure 3
c iv). When the vortex shedding process is forced above its natural frequency; i.e.
$f_f \gt f_n$
in the synchronous quenching regime, similar trends are observed (not shown for brevity). The only notable difference is that during phase-drifting, the phase variation shows near-constant epochs punctuated by a rapid decrease with an overall decreasing trend instead of an increasing one.
More importantly, one should note that lock-in does not eliminate the torus attractor; instead, it now has stable periodic orbits on its surface (Balanov et al. Reference Balanov, Janson, Postnov and Sosnovtseva2009; Li & Juniper Reference Li and Juniper2013a
). A sharp reduction in amplitude can also be observed (
$\sim$
38 % r.m.s. amplitude suppression in the presented case) on comparing the pressure time series of the unforced flow and that obtained at lock-in (figure 3
a iv). The observed transitions and dynamics agree well with similar experiments on other flow systems (Li & Juniper Reference Li and Juniper2013b
).
(a) Pressure time series, (b) frequency spectrum, (c) phase difference plots, (d) one-sided Poincaré maps for various system dynamics on varying the forcing amplitude in asynchronous quenching regime (
$f_f/f_n=0.86$
) and (e) torus growth during phase-drifting and subsequently shrinking during phase-trapping.

3.2. Asynchronous quenching regime
$(0.67 \leqslant f_f /f_n \leqslant 0.88$
and
$1.13 \leqslant f_f /f_n \leqslant 1.41)$
Forcing far from the natural frequency results in asynchronous quenching at lock-in. Results for a forcing frequency
$f_f=129.8\, \rm Hz$
(
$f_f/f_n=0.86$
) are presented in figure 4 for various forcing amplitudes. When the forcing amplitude is set to zero (
$\sigma _f$
= 0, figure 4
a i,b i,c i,d i) or has low values (
$\sigma _f$
= 0.073, figure 4
a ii,b ii,c ii,d ii), the dynamics is similar to that obtained in the synchronous quenching regime. A transition from limit cycle to
$T^2$
quasiperiodicity representing dynamics over a torus happens via a torus-birth bifurcation as earlier with the dynamics characterized by phase-drifting. The only difference is that since the difference in natural and forcing frequencies are much larger; slipping is not as noticeable as in the synchronous quenching regime. As the forcing amplitude increases, the size of the torus increases, as is observed in the synchronous quenching regime (figure 4
e i,e ii,e iii).
As the amplitude of external forcing is increased further (
$\sigma _f=0.076$
), phase difference becomes bounded and no longer slips, as can be seen in figure 4(c iii). This marks the onset of phase-trapping dynamics. Phase-trapping indicates that the frequency of the vortex shedding process maintains an average value around the forcing frequency. The vortex shedding frequency drifts both above and below the forcing frequency in a regular manner at the beat frequency
$|f_n-f_f|$
, unlike what was observed for phase-drifting. As a result, we have frequency lock-in without phase lock-in for this forcing amplitude.
Eventually, as the forcing amplitude reaches a value
$\sigma _f=0.128$
, complete lock-in is achieved with the phase difference between the response signal and the forcing signal reaching a constant value (figure 4
c iv). As the forcing amplitude is increased towards lock-in after the phase is trapped, the size of the torus starts shrinking gradually and collapses to a point at lock-in (figure 4
eiv,ev,evi). This progressive reduction in the torus size indicates that one is approaching another Neimark–Sacker bifurcation, this time leading to the death of a torus (or a torus-death bifurcation). Phase trapping was also reported in forced-jet (Li & Juniper Reference Li and Juniper2013b
,
Reference Li and Juniperc
) and Rijke tube experiments (Mondal et al. Reference Mondal, Pawar and Sujith2019). Although the specific mechanism and fluid mechanical details are different for these experiments of global hydrodynamic instability and thermoacoustics from our system, there appears to be a universality underlying the transitions in these systems. As the forcing amplitude increases beyond the first instance of phase-trapping towards lock-in, the departures above and below the forcing frequency are minimized, and the system smoothly transitions to lock-in. Similar trends are observed for
$f_f/f_n\gt 1$
except that the lock-in happens for lower forcing amplitudes than for
$f_f/f_n\lt 1$
. This asymmetry is discussed in greater detail in §§ 3.5 and 4.
The spectra of the response signal (figure 4
b) again make it clear that we have a suppression mechanism at lock-in and not a locking mechanism. We have a clear suppression of natural frequency in favour of the forcing frequency as the forcing amplitude increases with no frequency pulling or pushing. It should also be noted that the reduction in amplitude (or suppression) at lock-in is more significant in the asynchronous quenching regime (up to 61.5 % r.m.s. amplitude suppression) when compared with the reduction in amplitude in the synchronous quenching regime (
$\sim$
38 % suppression).
3.3. De-lock-in regime
$(0.55 \leqslant f_f /f_n \leqslant 0.65)$
A regime of de-lock-in is observed when the system is forced at frequencies between the subharmonic
$ (0.49 \leqslant f_f /f_n \leqslant 0.51)$
and the asynchronous quenching regimes
$(0.55 \leqslant f_f /f_n \leqslant 0.65)$
for
$f_f /f_n \lt 1$
. In this regime, as the forcing amplitude is increased beyond the lock-in state, the system delocks; i.e. the phase starts drifting with the re-emergence of natural frequency in the spectra of the response signal. This behaviour is critically distinct from the dynamics in the synchronous and asynchronous quenching regimes where de-lock-in is not observed even at large forcing amplitudes.
In the works of Anishchenko, Nikolaev & Kurths (Reference Anishchenko, Nikolaev and Kurths2008), Guan, Murugesan & Li (Reference Guan, Murugesan and Li2018), three distinct pathways of de-lock-in were delineated concerning the transition from a lock-in state in a periodically forced oscillator.
-
(i) Route 1. The period-one fixed point, representing the lock-in state, undergoes a sequence of period-two bifurcations, ultimately leading to the disappearance of the lock-in state.
-
(ii) Route 2. The stable and unstable period-one fixed points amalgamate, giving rise to a saddle-node bifurcation. This process results in the dissolution of the lock-in state.
-
(iii) Route 3. The stable and unstable manifolds of the period-one fixed point reach a point of tangency, thereby forming a homoclinic orbit. This specific configuration leads to the de-lock-in phenomenon.
(a) Pressure time series, (b) frequency spectrum, (c) phase difference plots (d) and one-sided Poincaré maps for various system dynamics on varying the forcing amplitude in de-lock-in regime (
$f_f/f_n=0.65$
).

The results for harmonic forcing at
$f_f=98.5 \,\textrm{Hz}$
(
$f_f/f_n=0.65$
) are presented in figure 5. For forcing amplitudes up to lock-in; i.e.
$0 \leqslant \sigma _f \leqslant 0.62$
, the dynamics follows a similar pattern to that observed in the synchronous quenching regime (see figure 5
a i–iii,b i–iii,c i–iii,d i–iii). Phase-drifting is evident (figure 5
c i) with the trajectory represented by a quasiperiodic
$T^2$
torus that emerges through a Neimark–Sacker bifurcation and collapses abruptly to a periodic orbit through a saddle-node bifurcation at lock-in. The lock-in results in the phase difference between the forcing and response signals approaching a constant value with the natural mode completely suppressed.
As the amplitude increases to a certain critical value above the lock-in amplitude (
$\sigma _f=0.82$
), the frequency of the natural mode reappears in the spectra of the response signal, and the phase difference starts to drift nonlinearly. The primary difference between the phase-drifting and de-lock-in dynamics is that the phase drift has no apparent regularity. Another noticeable feature is the presence of a subharmonic of the natural frequency in the spectra of the response signal, which was absent for all lower values of forcing amplitude. The subharmonic is an indicator of vortex merging, which may be responsible for the observed nonlinearity in the phase drift. The presence of the subharmonic also confirms that de-lock-in is happening via a period-doubling bifurcation indicating route
$1$
as the pathway to de-lock-in (figure 5
a iv,biv).
Using a low-order theoretical model for periodically forced vortex shedding, Britto & Mariappan (Reference Britto and Mariappan2019) showed that de-lock-in can occur when a system is forced at a frequency away from the natural vortex shedding frequency at forcing amplitudes much higher than that required for lock-in. Their model shows that de-lock-in typically occurs at the boundary between two distinct lock-in regimes. Our study provides experimental evidence which confirms these findings as de-lock-in is observed in the boundary between
$1:1$
and
$1:2$
lock-in regimes.
In the de-lock-in regime, there is up to a 34.2 % reduction in r.m.s. amplitude of the response signal when external harmonic forcing is applied at lock-in. However, the resurgence of the natural mode
$f_n$
for higher forcing amplitudes beyond lock-in renders this regime ineffective for active control in practical systems. Moreover, the signal amplitude greatly exceeds that of the unforced state during de-lock-in (figure 5
a iv), making such control action counterproductive.
(a) Pressure time series, (b) frequency spectrum, (c) phase difference plots (d) and one-sided Poincaré maps for various system dynamics on varying the forcing amplitude in
$1:2$
lock-in regime (
$f_f/f_n=0.49$
).

3.4. The
$1:2$
lock-in regime
$ (0.49 \leqslant f_f /f_n \leqslant 0.51)$
Periodically forcing the cavity-flow system close to the subharmonic of the natural frequency (
$f_f \sim f_n/2$
) leads to
$1:2$
lock-in. Figure 6 shows the results for a forcing frequency
$f_f=73.9\, \textrm{Hz}$
(
$f_f/f_n=0.49$
). At low forcing amplitudes (
$\sigma _f=0.11$
) where the modal power at
$2f_f$
is lower than that at
$f_n$
(see figure 6
b ii), we get an ergodic
$T^2$
quasiperiodicity that emerges from the unforced base state through a Neimark–Sacker bifurcation (see figure 6
a i–d i,a ii–d ii). The forcing frequency excites higher harmonics (
$2f_f=147.8$
Hz) that compete with the natural vortex shedding mode of the system. Therefore, we observe phase-drifting in a manner comparable to that observed in the synchronous quenching regime (figure 6
cii).
When the forcing amplitude increases to an extent where the modal power at
$2f_f$
is larger than that at
$f_n$
(for instance,
$\sigma _f=0.35$
, also see figure 6
b iii), ergodic
$T^3$
quasiperiodicity is observed in the Poincaré map (see figure 6
d iii) as a densely filled irregular structure with two hollow regions. The presence of
$f_f/3$
in addition to
$f_f/2$
can be confirmed from spectra as well in support of the observed quasiperiodic behaviour; see figure 6(biii).
The presence of subharmonic
$f_f/3$
implies that occasionally three vortices merge instead of two, giving rise to complex dynamics. Such three-frequency regimes have been reported previously in Rayleigh–Benard convection (Gollub & Benson Reference Gollub and Benson1980). Phase-drifting is still evident with the same regularity as observed for low forcing amplitudes where
$T^2$
quasiperiodicity is observed, indicating the absence of frequency pulling (or pushing). However, phase-drifting happens with a much steeper slope in this three-frequency
$T^3$
quasiperiodic regime.
As the forcing amplitude increases to
$\sigma _f=0.51$
, vortex shedding process locks-in to the forcing frequency, and the
$T^3$
torus bifurcates to a period-two limit cycle. We observe two blobs in the Poincaré map which also confirm period-two oscillations (figure 6
d iv). The presence of period-two oscillations at lock-in is an indicator of sustained vortex-merging where vortices shedding at the natural frequency merge together to form larger vortices effectively halving the frequency of the shedding process. This leads to the spectral representation observed in figure 6(b iv) where the modal power at the forcing frequency is lower than that at twice the modal frequency, effectively acting as a subharmonic. In short, lock-in is made possible by the presence of higher harmonics of the forcing frequency which are close to the natural vortex shedding frequency.
The dimensionality of
$T^2$
and
$T^3$
tori are confirmed using a correlation dimension framework (see Appendix A.2, figure 22c). Previous studies have indicated that low-amplitude harmonic forcing of a two-frequency quasiperiodic oscillator can result in
$T^3$
quasiperiodicity (Guan et al. Reference Guan, Gupta, Wan and Li2019b
). Our findings reveal that
$T^3$
quasiperiodicity can also be induced by the high-amplitude forcing of a limit cycle near its subharmonic frequency.
Generally, higher-order tori (in this case
$T^3$
) are known to be unstable and prone to transition to chaos with small perturbations via the Ruelle–Takens–Newhouse route (Anishchenko et al. Reference Anishchenko, Safonova, Feudel and Kurths1994). However, many experimental observations have also reported a stable higher-order torus regime (Barbi et al. Reference Barbi, Favier, Maresca and Telionis1986; Borkowski et al. Reference Borkowski, Perlikowski, Kapitaniak and Stefanski2015). In our case, a stable
$T^3$
torus dynamics is present at least over a small range of forcing amplitudes. As forcing amplitude increases towards lock-in, the vortex shedding process transitions to sustained periodic vortex merging, leading to period-two oscillations.
It has also been reported previously by Guan et al. (Reference Guan, Yin, Yang and Li2024) that period-two oscillations may transition to chaos at higher forcing amplitudes and can lead to de-lock-in. In our studies, even after increasing forcing amplitudes after lock-in, de-lock-in and chaos are not observed. The absence of chaos was confirmed using the 0–1 chaos test (Gottwald & Melbourne Reference Gottwald and Melbourne2004) and autocorrelation function (see Appendix A.3, figure 23).
There is up to a 30.2 % reduction in r.m.s. amplitude of response pressure signal when forcing in the
$1:2$
lock-in regime. However, harmonic forcing in this regime is not optimal for effective control of the unforced high-amplitude limit cycle, as much higher forcing amplitudes are required in comparison with the synchronous and asynchronous quenching regimes. Secondly, there exists a perturbation-sensitive three-frequency regime, which may complicate control action.
3.5. Synchronization map (Arnold tongue)
The concept of a synchronization map (or ‘Arnold tongue’) was first introduced by Vladimir Arnold (Arnold Reference Arnold2009) in his work on circle maps and torus mappings. These tongues describe regions in the parameter space of coupled oscillator systems where phase lock-in or synchronization occurs. Arnold tongues are typically observed as wedge-shaped (or V-shaped) regions in a two-dimensional parameter space. Inside these regions, the system’s frequency locks to a rational ratio of the driving frequency and the centre of the wedge is located precisely at this ratio.
In our discussions so far, we have presented the response dynamics of acoustic pressure oscillations by systematically varying the forcing amplitude (
$\sigma _f$
) and the normalized forcing frequency (
$f_f /f_n$
) which constitute the two-dimensional parameter space in our study. The minimum forcing amplitude at which the system locks-in for various forcing frequencies represents the boundary of the synchronization map in this two-dimensional parameter space. The complete synchronization map corresponding to the four regimes investigated is shown in figure 7. Alongside the
$1:1$
lock-in wedge, a
$1:2$
lock-in wedge is also present over the range of frequencies explored.
Synchronization map (Arnold tongue) obtained from experiments. Four regimes identified, i.e. synchronous quenching, asynchronous quenching,
$1:2$
lock-in and de-lock-in.

Synchronous quenching is observed for
$ 0.9 \leqslant f_f /f_n \leqslant 1.10$
with lock-in happening via phase-drifting through a saddle-node bifurcation. The Arnold tongue appears to have a linear, mildly asymmetric variation on either side of
$f_f/f_n=1$
in the synchronous quenching regime. When forcing far from the natural mode, that is,
$ 0.67 \leqslant f_f /f_n \leqslant 0.88$
and
$ 1.13 \leqslant f_f /f_n \leqslant 1.49$
, we observe asynchronous quenching where lock-in occurs via phase-trapping and torus-death bifurcation. The Arnold tongue is no longer linear, with noticeable asymmetry on either side of the
$f_f/f_n=1$
point.
This asymmetric behaviour has also been reported in several other studies (Li & Juniper Reference Li and Juniper2013a ; Kashinath, Li & Juniper Reference Kashinath, Li and Juniper2018; Guan et al. Reference Guan, Gupta, Kashinath and Li2019a ). Li & Juniper (Reference Li and Juniper2013a ) note that the asymmetric nature of the synchronization map is a characteristic of flow rather than a specific attribute of lock-in. They also found that higher frequencies lead to increased peak acceleration. However, we did not observe peak acceleration (frequency pulling or pushing) despite the observed asymmetry, suggesting that a different mechanism is possibly at play.
The fluid mechanics behind the asymmetry in the Arnold tongue can be reasoned from the asymmetry in the vortex distribution for
$f_f/f_n \gt 1$
and
$f_f/f_n \lt 1$
. External forcing in the
$f_f/f_n \gt 1$
regimes can cause vortices to roll-up and shed earlier than possible by the natural mode, thereby dominating the flow field with smaller vortices at the forcing frequency when compared with vortices shed at the natural mode. This increased distribution of smaller vortices can increase the tendency of lock-in for smaller forcing amplitudes. External forcing on the other side of the Arnold tongue (
$f_f/f_n \lt 1$
) results in vortices taking a longer time to roll up and shed, resulting in fewer larger vortices in the flow field in comparison with those shed at the natural frequency for smaller forcing amplitudes. The dynamical reason behind the asymmetry observed in our case is discussed further in § 4.
In the transition region from
$1:1$
to
$1:2$
lock-in, a small region exists where increasing the forcing amplitude further after lock-in leads to de-lock-in, with the reappearance of the natural mode and a nonlinear phase drift. One can also observe a significant jump in the minimum lock-in amplitude at
$ f_f /f_n = 0.60$
. This abrupt jump indicates the presence of a region characterized by bistability and hysteresis and aligns with a well-known characteristic of a cusp catastrophe, as described in Thompson & Stewart (Reference Thompson and Stewart2002). The cusp catastrophe occurs when alterations in one or two control parameters, specifically forcing frequency
$f_f$
and the forcing amplitude
$\sigma _f$
, cause the system to fall down the fold curve on the catastrophe surface. Such a jump phenomenon has been observed in various nonlinear systems, such as electronic circuits (Giannakopoulos & Deliyannis Reference Giannakopoulos and Deliyannis2001), turbulent premixed combustors (Bellows et al. Reference Bellows, Hreiz and Lieuwen2008) and diffusion flames. Such a jump in the left-hand branch of the Arnold tongue was observed in diffusion flames (Li & Juniper Reference Li and Juniper2013a
). Li & Juniper (Reference Li and Juniper2013a
) observe the jump prior to
$3:4$
lock-in whereas in our studies, the jump phenomenon occurs before the subharmonic
$1:2$
lock-in.
The width of the Arnold tongue at the
$1:2$
forcing regime is narrower than at the
$1:1$
regime. This reduction in width arises because, in the
$1:1$
forcing, phase entrainment is comparatively easier to achieve as saddle-node bifurcation approaches (Pikovsky et al. Reference Pikovsky, Rosenblum and Kurths2001; Balanov et al. Reference Balanov, Janson, Postnov and Sosnovtseva2009) than in other
$p:q$
forcing regimes. In the
$1:2$
forcing regime, the system transitions to lock-in via period-doubling bifurcation through various higher-order tori (
$T^2$
and
$T^3$
, see figure 6), which are more difficult to sustain than period-one oscillations.
Finally, the right-hand branch of the Arnold tongue (
$ f_f /f_n \gt 1$
) appears to saturate to a constant value (
$\sigma _f=0.211$
) for
$f_f /f_n \geqslant 1.25$
. This saturation behaviour was also observed by Kashinath et al. (Reference Kashinath, Li and Juniper2018) in their numerical study on the periodic forcing of a ducted premixed flame.
Normalized reduction in response amplitude (r.m.s.) in various regimes compared with the unforced amplitude.

The reduction in r.m.s. amplitude of the response pressure data (
$\delta p^{\prime}_{rms}=p^{\prime}_{u,rms}-p^{\prime}_{r,rms}$
) at lock-in normalized by the measured r.m.s. value of the pressure data obtained from the unforced system (
$p^{\prime}_{u,rms)}$
for all the four regimes is presented in figure 8. The boundary between synchronous and asynchronous quenching regimes is clearly distinguishable with a sharp reduction in amplitude noticeable across the boundaries towards asynchronous quenching. This corresponds to the qualitative transition in the nature of lock-in from an abrupt one (saddle-node) for synchronous quenching to a smooth one (torus death) for asynchronous quenching. There is also a clear delineation between asynchronous quenching and de-lock-in regimes for
$f_f\lt f_n$
indicative of re-emergence of abrupt transition at lock-in. The boundary between de-lock-in and
$1:2$
lock-in regime is less defined and cannot be identified purely on the basis of amplitude reduction. Overall, asynchronous quenching appears to result in maximal amplitude suppression through lock-in.
As informative as figure 8 is in estimating the control effectiveness, it does not contain information regarding the forcing power required to achieve the suppression. To understand the same, we need to look at the power transfer between the natural and the forcing frequency in the response signal as the forcing amplitude increases, which is discussed in the next section.
4. Modal power variation
To study modal power variation in the various regimes identified, we first calculate the spectral power of four key components: the natural mode power (
$P_n$
); the forced mode power (
$P_f$
) (and its harmonics or subharmonics where relevant); cumulative power (
$P_n$
+
$P_f$
); the total signal power (
$P_t$
), normalized by the power of unforced oscillations (
$P_{n,u}$
). These powers are represented as functions of the forcing power, normalized by the power required at lock-in
$(\sigma _f/\sigma _{f,loc})^2$
. A process similar to bandpass filtering is performed around each frequency to obtain the modal power. This procedure involves integrating the power spectral density around each mode to isolate their contributions. The total power is obtained by integrating the power spectral density across the entire bandwidth. We ensure that the calculated total power matches (within a tolerance of 0.5
$\%$
) the power of the mean squared fluctuations, as required by Parseval’s theorem (Porat Reference Porat2008).
The spectral power of the oscillations as a function of the forcing power for the system in the synchronous quenching regime (
$f_f=141.94$
Hz) and asynchronous quenching regime (
$f_f=129.8$
Hz) on the left-hand side of the Arnold tongue (
$f_f/f_n \lt 1$
) are presented in figures 9(a) and 9(b), respectively. For low forcing amplitudes corresponding to phase-drifting dynamics, a linear decrease in the power of the natural mode (
$P_n$
) and a simultaneous linear increase in the power of the forced mode (
$P_f$
) is observed in both regimes. However, the total signal power is lower than the power of the unforced system.
The linear variations indicate that with each increment in forcing amplitude, a fixed portion of the power is withdrawn from the natural mode. The influence of external forcing on the natural mode suggests the presence of nonlinear interactions, although the power transfer out of the natural mode is linear. Nonlinear mechanisms that can lead to a reduction in
$P_n$
are ones that diminish the natural mode’s ability to extract energy from the base flow, enhance dissipation or transfer energy from the natural mode to its sidebands.
The power increment in forcing frequency remains linear for all forcing amplitudes even beyond lock-in. A similar linear increase in
$P_f$
is observed by Sreenivasan et al. (Reference Sreenivasan, Raghu and Kyle1989) and Kyle & Sreenivasan (Reference Kyle and Sreenivasan1993) in both self-excited and convectively unstable jets. Despite the linear increase in
$P_f$
, the combined power (
$P_n$
+
$P_f$
) decreases linearly for small forcing amplitudes because
$P_n$
diminishes more rapidly than
$P_f$
grows. This decrease is especially pronounced in the asynchronous quenching regime.
For forcing amplitudes close to lock-in in the synchronous quenching regime, while
$P_f$
increases linearly,
$P_n$
decreases in a highly nonlinear and abrupt manner. This deviation from linearity indicates the activation of a second mechanism that enables additional power transfer from the natural mode on approaching the saddle-node bifurcation.
For forcing amplitudes close to lock-in in the asynchronous quenching regime, while
$P_f$
increases linearly,
$P_n$
starts decreasing much more as the dynamics transitions to phase-trapping. Finally, there is an abrupt drop in modal power
$P_n$
as system enters lock-in.
After lock-in, cumulative power as well the total power is dictated by
$P_f$
and its harmonics as the modal power in the natural mode is suppressed completely at lock-in in both the regimes. In the asynchronous quenching regime, the reduction in total power is up to
$74.3\,\%$
at lock-in, whereas in the synchronous quenching regime, the reduction is up to
$56.3\,\%$
. Increasing the forcing amplitude beyond lock-in increases the total signal power; however, this power remains well below the total power of the unforced system, especially in the asynchronous quenching regime.
Spectral power of natural frequency (
$P_ n$
), forcing frequency (
$P_ f$
),
$P_ n$
+
$P_ f$
and total signal power (
$P_ t$
) normalized by unforced system power (
$P_{n,u}$
). These powers are represented as functions of the forcing power and normalized by the lock-in amplitude
$(\sigma _f/\sigma _{f,loc})^2$
for (a) synchronous quenching (
$f_f/f_n$
= 0.94) and (b) asynchronous quenching (
$f_f/f_n$
= 0.86) on the left arm of the Arnold tongue.

Spectral power of natural frequency (
$P_ n$
), forcing frequency (
$P_ f$
),
$P_ n$
+
$P_ f$
and total signal power (
$P_ t$
) normalized by unforced system power (
$P_{n,u}$
). These powers are represented as functions of the forcing power and normalized by the lock-in amplitude
$(\sigma _f/\sigma _{f,loc})^2$
for (a) synchronous quenching (
$f_f/f_n$
= 1.02) and (b) asynchronous quenching (
$f_f/f_n$
= 1.17) on the right arm of the Arnold tongue.

In figure 10, spectral power for forcing performed on the right-hand side of the Arnold tongue (
$f_f/f_n \gt 1$
) are shown for the synchronous (figure 10
a) and asynchronous (figure 10
b) regimes. For low forcing amplitudes corresponding to phase-drifting dynamics,
$P_f$
increases linearly and
$P_n$
appears nearly invariant in the synchronous quenching regime with negligible variation. This near invariance hints at the negligible influence of forcing on dynamics at the natural mode. As a consequence, there is negligible transfer of energy away from the natural mode which leads to an increase in the total signal power to values above the power of the unforced system.
A linear decrease in
$P_n$
is more apparent in the asynchronous quenching regime for low forcing amplitudes corresponding to during phase-drifting dynamics leading to a near constant value of total signal power for low forcing amplitudes. In other words, energy supplied externally is dissipated more efficiently in the asynchronous quenching regime.
For forcing amplitudes close to lock-in, there is an abrupt large decrease in
$P_n$
in the synchronous regime as is observed for
$f_f/f_n \lt 1$
. However, there is a more pronounced nonlinearity in the variation of the
$P_f$
for these forcing amplitudes. This indicates that dynamics at the natural frequency is able to influence the dynamics at the forcing frequency in this range of amplitudes which was not the case for
$f_f/f_n \lt 1$
.
The dynamics in the asynchronous quenching regime is further complicated by the presence of two clear abrupt drops in
$P_n$
corresponding to transitions to phase-trapping dynamics and lock-in. Transition to phase-trapping leads a much larger drop in
$P_n$
in this case than was observed for
$f_f/f_n\lt 1$
. There is a nonlinearity in the variation of
$P_f$
close to lock-in as was observed in the synchronous quenching regime.
The abrupt drops in
$P_n$
bring the total signal power to values lower than that observed for unforced system resulting in amplitude suppression at lock-in. On increasing the forcing amplitude beyond lock-in, one can observe a rapid rise in the total power for both synchronous and asynchronous quenching regimes, to values well beyond that observed for the unforced system. This overshoot or amplification was absent for forcing on the left-hand side of the Arnold tongue (
$f_f/f_n \lt 1$
) where the increase in total power after lock-in is much more gradual.
In the case of synchronous quenching, the amplification is termed as resonant amplification; for asynchronous quenching, it is called non-resonant amplification. For resonant amplification, the shoot-up after lock-in happens at nearly the same levels as the levels at which the modal power at the forcing frequency increases. However, for non-resonant amplification, the shoot-up after lock-in is much more drastic and happens at much higher levels than the levels at which the modal power at the forcing frequency increases. This feature is particularly distinct from the variation of modal power on the left-hand side of the Arnold tongue where the increase in total power was always proportional to the variation of the modal power at the forcing frequency after lock-in. This amplification, possibly due to the asymmetry in the vortex distribution as discussed in the previous section, is responsible for the observed asymmetry of the Arnold map on either side of the natural frequency.
The reduction in total power at lock-in within the synchronous quenching regime reaches up to 38 % for cases where
$f_f/f_n \gt 1$
, which is comparatively smaller than the reduction observed for
$f_f/f_n \lt 1$
(57.3 %). Similarly, in the asynchronous quenching regime, the total power reduction at lock-in reaches 44 % when
$f_f/f_n \gt 1$
, again demonstrating a comparatively smaller reduction than in cases where
$f_f/f_n \lt 1$
(78.3 %).
In figure 11, the power transfer across all significant modes is shown for forcing on either side of the Arnold tongue in the
$1:2$
lock-in regime. When external harmonic forcing is applied to the system near the subharmonic frequency,
$P_n$
decreases with a concurrent rise in
$P_f$
as forcing amplitude increases. In contrast to synchronous and asynchronous quenching regimes, a rise in the power of the second harmonic of the forced mode (
$P_{2f}$
) is also observed with an increase in the forcing amplitude during phase-drifting dynamics before lock-in. Another significant observation is the presence of subharmonics at
$f_f/2$
and
$f_f/3$
corresponding to
$T^3$
quasiperiodicity. The modal power at
$f_f/3$
increases linearly until lock-in when it abruptly disappears as period-two oscillations set in.
Resonant amplification of the total signal power is also observable for forcing amplitudes beyond lock-in for forcing on the right-hand side of the Arnold tongue centred at the subharmonic of the natural frequency (see figure 11
b). The amplification is resonant as forcing results in the excitation of the first harmonic (
$2f_f$
) of the forcing frequency which is located closely to the right of the natural frequency (
$f_n$
). Forcing on the left-hand side of this Arnold tongue does not result in amplification (see figure 11
a). This indicates that amplification is a phenomenon dictated by the forcing frequency or its harmonics being larger than the natural frequency.
Spectral power of natural frequency (
$P_ n$
), forcing frequency (
$P_ f$
),
$P_ n$
+
$P_ f$
, subharmonics (
$P_ {f/2}, P_ {f/3}$
) and total signal power (
$P_ t$
) normalized by unforced system power (
$P_{n,u}$
). These powers are represented as functions of the forcing power and normalized by the lock-in amplitude
$(\sigma _f/\sigma _{f,loc})^2$
for (a) subharmonic lock-in without resonant amplification (
$f_f=73.5\, \textrm{Hz}$
), (b) subharmonic lock-in with resonant amplification (
$f_f=76.2\, \textrm{Hz}$
).

Spectral power of natural frequency (
$P_ n$
), forcing frequency (
$P_ f$
),
$P_ n$
+
$P_ f$
, subharmonic (
$P_ {n/2}$
) and total signal power (
$P_ t$
) normalized by unforced system power (
$P_{n,u}$
). These powers are represented as functions of the forcing power and normalized by the lock-in amplitude
$(\sigma _f/\sigma _{f,loc})^2$
for de-lock-in regime (
$f_f=98.5\, \textrm{Hz}$
).

In the de-lock-in regime, the primary difference from the
$1:2$
lock-in regime for forcing amplitudes until lock-in is the absence of three-frequency dynamics (no modal power at
$f_f/3$
) and a much smaller increase in the energy content of the harmonic
$2f_f$
(figure 12). At higher amplitudes beyond lock-in, de-lock-in can be observed as an increase in the power of the natural mode. Some energy also gets transferred to the subharmonic (
$f_n/2$
) of the natural frequency resulting in complex dynamics. Resonant amplification of total power is observed due to the excitation of the harmonic
$2f_f\gt f_n$
of the forcing frequency as described for the
$1:2$
lock-in regime.
The reduction in total power at lock-in is up to 30.3 % for the
$1:2$
lock-in forcing regime and up to 28.3 % for the de-lock-in regime. The decrease in overall power at lock-in is less compared with asynchronous and synchronous quenching regimes, suggesting that these regimes are unsuitable for optimal control. In the de-lock-in regime, there is the possibility of de-lock-in at higher amplitude ratios with complex dynamics, which makes it risky for control purposes. In the
$1:2$
lock-in regime, there is the presence of a three-frequency regime with subharmonics which complicates control action. In addition, there is also a possibility of resonant amplification.
In summary, to suppress self-sustained oscillations in the cavity flow by external forcing, we need the forcing frequency (
$f_f$
) to be sufficiently detuned from the natural frequency (
$f_n$
) to result in asynchronous quenching. Secondly, we have to ensure that
$f_f/f_n \lt 1$
so that amplification is avoided. And finally, we have to ensure that the detuning is not so large as to end up in other
$p:q$
lock-in regimes or de-lock-in regimes. These conditions pose a strict constraint on the optimal frequency range for effective control action.
In open-loop control, asynchronous quenching emerges as a promising approach for suppressing limit-cycle oscillations. However, a significant limitation of this method is that it necessitates prior knowledge of
$f_n$
, which can be difficult to determine in systems where even brief excursions into a high-amplitude limit-cycle regime may result in catastrophic mechanical or thermal damage. Furthermore, this challenge is compounded by the potential for
$f_n$
to drift due to variations in operating conditions or system parameters.
For robust control, it is desirable to develop a method for suppressing limit-cycle oscillations that is less dependent on the detuning between forced and natural modes. Specifically, a strategy is needed that facilitates both asynchronous and synchronous quenching while avoiding any amplification of the forcing signal.
5. Phenomenological model
Consider a double orifice plate configuration in a duct of length
$L$
that forms a cavity of length
$L_c$
. Flow enters the cavity, forming vortices as the free shear layer develops from the first orifice. These vortices advect downstream with the flow and impinge on the second orifice location, leading to pressure fluctuations of dipole type (Matveev Reference Matveev2005). These pressure fluctuations travel upstream with the speed of sound to the first orifice location, exciting the free shear layer, which, under appropriate flow conditions, also excites the longitudinal acoustic mode of the duct, leading to self-sustained oscillations or a limit cycle. In what follows, a simplified mathematical model is presented to capture this mechanism. The model is inspired by the work of Matveev & Culick (Reference Matveev and Culick2003) and incorporates elements from van der Pol and Duffing oscillators to capture the observed dynamics.
Certain assumptions are incorporated to facilitate a clear mathematical representation, which is reasonable for the flow field under consideration. Specifically, one-dimensional acoustic theory is employed for the duct (treated as open–open) due to the dominance of longitudinal acoustic modes. Additionally, a low Mach number assumption is made so that the effects of mean flow (treated as a constant inside the cavity) in the wave equation can be neglected. Further, the cavity length
$L_c$
is considered small compared with the acoustic wavelength (compact source assumption). The effects of turbulence or flow unsteadiness on vortex advection are ignored, and only the acoustic fluctuations are considered when describing vortex dynamics. Similarly, the only source term in the wave equation arises from the circulation generated by the vortices. Finally, the effects of viscosity and heat transfer on the wave equation are neglected. The momentum and energy equations for the flow may then be written as
and
where
$p^{\prime}$
,
$u^{\prime}$
are acoustic pressure and velocity fluctuations,
$p_{0}$
,
$\rho _{0}$
are mean pressure and density,
$\gamma$
is the ratio of specific heat and
$\Gamma$
is the circulation strength of the vortex. The motivation for the forcing term comes from the expression of the lift generated by a circulation distribution (this is different from the form described in Matveev & Culick Reference Matveev and Culick2003) and the parameter
$x_c=L-Lc$
. Circulation is assumed to be purely time-dependent as it is obtained by spatially integrating the velocity field over a closed contour. Subtracting the time derivative of (5.2) from that of (5.1), the resulting expression can be written as
We employ the Galerkin projection method (Zinn & Lores Reference Zinn and Lores1971) to spatially average the wave equation to obtain ordinary differential equations for the fundamental acoustic mode. The acoustic variables (
$u^{\prime}$
and
$p^{\prime}$
) are expanded using basis functions that meet the boundary conditions of the system as follows:
where
$k=\pi /L$
. Substituting (5.4), (5.5) in (5.3), and spatially integrating over the length of the duct, we obtain second-order ordinary differential equations for the time coefficient
$\eta$
of the acoustic mode,
Damping can be modelled, taking inspiration from the van der Pol oscillator to account for linear and nonlinear damping effects as was done in Noiray & Schuermans (Reference Noiray and Schuermans2013) and Guan et al. (Reference Guan, Gupta, Kashinath and Li2019a
). To model the sudden jump phenomenon observed in experiments in the transition region of
$1:1$
to
$1:2$
lock-in, an additional cubic stiffness term is added as in the Duffing oscillator. Kashinath et al. (Reference Kashinath, Li and Juniper2018) and Guan et al. (Reference Guan, He, Murugesan, Li, Liu and Li2019c
) have previously employed this strategy to capture the jump phenomena in a ducted flame near
$3:4$
lock-in regime.
Schematic representation of the vortex shedding and impingement from double orifice cavity set-up and its active control by harmonic acoustic perturbations.

The final oscillator equation for acoustics then becomes
A value of
${\rm \mu} =0.2$
is selected, which generates an unforced self-excited waveform consistent with experimental observations. The value of
$\zeta =0.95$
is chosen to capture the asymmetry of the Arnold tongue. This approach is different from conventional modelling employed for van der Pol oscillators. The parameter
$\kappa =({2\pi }/{L^2})\sin ^2(({\pi }/{L})x_c)$
represents the coupling factor for vortex–acoustic interaction, which is obtained as 1.25. The cubic-stiffness parameter
$\beta$
is chosen as 0.1 by matching the frequency (
$f_f/f_n=0.60$
) at which the amplitude-response curve peaks in the experiments.
In (5.7)
$\Gamma$
, which represents circulation, appears as a driving (or damping term) that needs to be modelled. When a vortex begins to form, its circulation is zero. As the vortex develops,
$\Gamma$
grows. The vortex detaches once the circulation achieves a critical value and gets advected away from the source location. Therefore, the rate of change of circulation at the leading edge of the cavity at the first orifice can be expressed as follows:
In this equation, the first term represents the growth rate of circulation at the step as defined in Matveev & Culick (Reference Matveev and Culick2003), and the second term represents the rate at which circulation is lost as the shear layer advects downstream. The coefficient
$\alpha$
characterizes the fraction of the mean velocity (
$u_{0}$
) at which the shear layer advects away from the first orifice. Experimental studies suggest that
$\alpha =0.45$
can be appropriate for the present study (Dotson, Koshigoe & Pace Reference Dotson, Koshigoe and Pace1997). Using Galerkin expansion and substituting the value of
$u^{\prime }$
from (5.5) into (5.8), we obtain the rate of change of circulation in terms of the acoustic modes as
where
$a = ({0.5}/{k})\cos ^2( {(\pi }/{L})x_c)$
,
$b = ({(1-\alpha )u_0L}/{\pi })\cos (({\pi }/{L})x_c)$
and
$c = (0.5- \alpha )u^2_0$
. The values of
$a$
,
$b$
and
$c$
are obtained as 0.56, 0.45 and 0.675 on substituting values from experiments.
The parameters
$a$
,
$b$
and
$c$
, which dictate vortex dynamics can be directly related to the physical parameters
$u_0$
,
$L$
and
$L_c$
. Parameter
$a$
captures the nonlinear contribution of acoustic velocity fluctuations to the circulation growth. The value of
$a$
determines the lock-in amplitude. This parameter
$a$
can also broaden the lock-in range, allowing synchronization over a wider frequency band. Parameter
$b$
represents the rate at which circulation is lost as the shear layer advects downstream. Experimental results presented in the previous sections demonstrate that all harmonics, including the even harmonics, are present in the response signals, which conventional van der Pol equation cannot reproduce (only odd harmonics are captured by van der Pol equation). This is typically remedied by introducing additional term
$\dot {\eta }^2$
in the oscillator equation as is done in Rayleigh–van der Pol oscillators. In our system of equations
$\dot {\eta }^2$
term appears indirectly through circulation in (5.7), and parameter
$b$
dictates the relative strength of the even harmonics. This approach, where the Rayleigh term appears as an integrated effect, is necessary to observe the nonlinear phase drift present during de-lock-in. Parameter
$c$
which incorporates the effect of mean velocity and decay due to vortex advection, acts as a bifurcation parameter in the unforced oscillator. On varying
$c$
(flow rate), the system transitions from near-zero amplitudes to self-sustained limit cycle oscillations in the absence of forcing.
Equations (5.7) and (5.9) constitute a system of coupled oscillator equations, hereafter referred to as ROPM. The fast equation (5.7) representing acoustics contains features of van der Pol and Duffing oscillators. The slow equation (5.9) represents the dynamics of vortex generation and advection at the location of the first orifice plate. For harmonically forced dynamics, we add a sinusoidal forcing term to the right-hand side of (5.7) to obtain
where
$\sigma _f$
denotes the non-dimensional amplitude and
$f_f$
denotes the forcing frequency.
Understanding the sensitivity of model parameters which cannot be explicitly determined and the sequential procedure of tuning them is of utmost importance in reproducing experimental results. The parameter
${\rm \mu}$
, which governs both linear and nonlinear damping and determines the unforced system behaviour has to be within the range of 0.1–0.3 so that qualitative behaviour of the model remains the same (Thompson & Stewart Reference Thompson and Stewart2002). For instance, values of
${\rm \mu}$
above this range results in steepened limit cycles.
After adjusting the value of
${\rm \mu}$
, we adjust the cubic stiffness parameter
$\beta$
according to the frequency at which the maximum amplitude in the response curve is observed during the experiments. The value of
$\beta$
, if maintained within a low range (−0.05
$\leqslant$
$\beta$
$\leqslant$
0.2), results in the properties of a soft cubic spring.
Then, the value of
$\zeta =0.95$
is chosen to match the asymmetry of the Arnold tongue seen in experiments. When
$\zeta \leqslant 1.5$
, it correctly captures the asymmetry observed in experiments. The value of
$\zeta$
above 1.5 results in the steepening of the right arm of the Arnold tongue and affects the saturation behaviour observed in the synchronization map.
Here ROPM fundamentally differs from existing models utilized for modelling coupled vortex–acoustic interaction. First, it builds upon Matveev’s model by introducing terms that account for vortex advection. Second, the model avoids discontinuities associated with vortex shedding and impingement present in Matveev’s model. Finally, the model provides a phenomenological pathway based on experimental observations to arrive at a model that contains elements of van der Pol and Duffing oscillators.
The system of coupled oscillators was solved using multistep variable-order algorithm (Shampine & Reichelt Reference Shampine and Reichelt1997). When the forcing term is set to zero, the model gives a solution equivalent to a unforced limit-cycle state with frequency
$f_n$
observed in experiments. The forcing amplitude (
$\sigma _f$
) and forcing frequency
$f_f$
are systematically varied to study the impact of forcing on the limit cycle solution.
5.1. Comparison of model results with experiments
Synchronous quenching is observed when the oscillator (ROPM) is forced near the natural frequency, i.e.
$f_f/f_n = 0.98$
. As the forcing amplitude increases, phase-drifting is observed before lock-in, similar to what is observed in the experiments (figure 3). In figure 14, it is evident that the torus suddenly collapses to a blob on the Poincaré map, indicating saddle-node bifurcation. The model correctly captures side-bands obtained in experiments mainly due to the ability of the model to capture second harmonics. The model also exhibits a suppression-type behaviour and not a locking-type behaviour as the natural frequency in the pressure spectrum is not pushed (or pulled) towards the forcing frequency. This observation is in agreement with experiments.
In figure 15, we present a comparison of four indicators, similar to those shown in figure 14, for our phenomenological model forced far from the natural frequency (
$f_f/f_n = 0.86$
) where asynchronous quenching was observed in experiments. As the forcing amplitude (
$\sigma _f$
) increases, we observe a decrease in the amplitude of the natural mode without any concurrent pulling of the natural frequency towards the forcing frequency (
$f_f$
). For low forcing amplitudes, phase-drifting is present which transitions to phase-trapping prior to lock-in. The torus grows during the phase-drifting dynamics and shrinks in size once dynamics enters phase-trapping (figure 15
e). Hence, we have a Neimark–Sacker bifurcation in the opposite direction leading to torus death, leading the dynamics from
$T^2$
quasiperiodicity to
$1:1$
lock-in as the forcing amplitude increases.
(a) Pressure time series, (b) frequency spectrum, (c) phase difference plots (d) and one-sided Poincaré maps for various system dynamics on varying the forcing amplitude in synchronous quenching regime (
$f_f/f_n=0.98$
), obtained from ROPM.

(a) Pressure time series, (b) frequency spectrum, (c) phase difference plots, (d) one-sided Poincaré maps for various system dynamics on varying the forcing amplitude in asynchronous quenching regime (
$f_f/f_n=0.86$
) and (e) torus growth during phase-drifting and subsequently shrinking during phase-trapping, obtained from ROPM.

(a) Pressure time series, (b) frequency spectrum, (c) phase difference plots (d) and one-sided Poincaré maps for various system dynamics on varying the forcing amplitude in de-lock-in regime (
$f_f/f_n=0.65$
), obtained from ROPM.

As we reduce the forcing frequency towards
$1:2$
lock regime, a window of de-lock-in appears. As the amplitude of forcing (
$\sigma _f=0.089$
) increases from the unforced state, we can observe quasiperiodic behaviour and the appearance of a torus is evident in the Poincaré map (figure 16
d ii). Phase-drifting is observed prior to lock-in. As we further increase the amplitude, we can observe a sudden collapse of the torus to a blob, leading the system to lock-in via saddle-node bifurcation. On further increasing the forcing amplitude after lock-in (
$\sigma _f=0.65$
), we can observe that phase delocks via nonlinear phase-drifting, which matches the observations in experiments. The route to de-lock-in involves period-doubling bifurcation from the lock-in state indicated by the presence of a frequency component at
$f_n/2$
, similar to that observed in experiments.
The ROPM also correctly captures the subharmonic (
$1:2$
) lock-in phenomena observed in the experiments. We forced the system slightly above and below the natural subharmonic frequency. In figure 17, the natural mode is forced at
$f_f/f_n=0.48$
, and the forcing amplitude is progressively increased until lock-in is observed. When the forcing amplitude is small (
$\sigma _f=0.18$
), we can observe various peaks at
$f_n$
and
$f_f$
that lead to phase-drifting and formation of a
$T^2$
torus. When forcing strength is increased further, a three frequency regime corresponding to a higher-order
$T^3$
torus is observed as in experiments. This transition from
$T^2$
to
$T^3$
quasiperiodicity happens when the modal strength at
$2f_f$
exceeds the strength at
$f_n$
. At lock-in, dynamics exhibits period-two oscillations as indicated by the signal and two blobs in the Poincaré map (figure 17(d iv).
(a) Pressure time series, (b) frequency spectrum, (c) phase difference plots (d) and one-sided Poincaré maps for various system dynamics on varying the forcing amplitude in
$1:2$
lock-in regime (
$f_f/f_n=0.49$
), obtained from ROPM.

5.1.1. Synchronization map obtained from ROPM
The synchronization map obtained from the ROPM is compared with the one obtained in the experiment in figure 18.
Comparison of synchronization map (Arnold tongue) obtained from the experiments, discrete map (Britto & Mariappan Reference Britto and Mariappan2019) and ROPM. Zoomed inset shows a comparison of lock-in boundary in the de-lock-in region for experiments (red dashed line) and model (blue dashed line).

The model correctly predicts the onset of the transition from the saddle-node bifurcation region to the torus-death bifurcation regimes of the torus. The model also predicts asymmetry in the Arnold tongue and the saturation of the right-hand branch for
$f_f/f_n\gt 1$
.
The jump in forcing amplitude at
$f_f /f_n$
= 0.6 is captured with the addition of the cubic stiffness parameter
$\beta$
in the model. However, the model tends to overestimate the lock-in amplitude at the jump location when compared with experimental findings. The presence of second subharmonics in the unforced state was found to be crucial in capturing essential dynamics of
$1:2$
lock-in and even predicting comparable trends for lock-in amplitude as in experiments (figure 18). This is a striking improvement over other existing models available to study vortex–acoustic interaction.
Recently, (Britto & Mariappan Reference Britto and Mariappan2019) used a discrete map equation approach to model vortex shedding; the results of this discrete map are also presented in figure 18. The discrete model correctly predicts the map in the synchronous quenching regime; however, the model fails to predict the experimental observations in the region of asynchronous quenching. This is because the discrete map equation (Britto & Mariappan Reference Britto and Mariappan2019) contains only a single equation to generate a synchronization map and cannot account for the complexity in dynamics far away from the forcing frequency. The presented oscillator model, however, offers great flexibility in solving synchronization problems as key parameters, which are physically motivated, can be adjusted to match the experimental results.
5.1.2. Modal power variation obtained from ROPM
The spectral power variation at the dominant modes on the left-hand (
$f_f/f_n=0.96$
Hz) side of the Arnold tongue obtained from ROPM in the synchronous and asynchronous quenching regimes is presented in figures 19(a) and 19(b), respectively. There is a linear reduction in power of natural mode for low forcing amplitudes in both regimes. Close to lock-in there is a single drastic in the synchronous quenching regime, whereas an additional drop in
$P_n$
is observed in the asynchronous quenching regime due to the transition to phase-trapping dynamics prior to lock-in. Power remains below the unforced system’s power for forcing amplitudes larger than that required for lock-in.
Spectral power of natural frequency (
$P_ n$
), forcing frequency (
$P_ f$
),
$P_ n$
+
$P_ f$
and total signal power (
$P_ t$
) normalized by unforced system power (
$P_{n,u}$
). These powers are represented as functions of the forcing power and normalized by the lock-in amplitude
$(\sigma _f/\sigma _{f,loc})^2$
for synchronous quenching (a) left-hand side (
$f_f/f_n=0.96$
) and (b) left-hand side (
$f_f/f_n=0.86$
), for asynchronous quenching (c) right-hand side (
$f_f/f_n=1.02$
) of the Arnold tongue and (d) right-hand side (
$f_f/f_n=1.17$
) of the Arnold tongue obtained from ROPM.

The spectral power variation at the dominant modes on the right (
$f_f/f_n=1.02$
Hz) side of the Arnold tongue obtained from ROPM in the synchronous and asynchronous quenching regimes is presented in figures 19(c) and 19(d), respectively. Amplification (both resonant and non-resonant) is observed in experiments after lock-in, and the total signal power goes beyond that of the unforced system’s power even for low forcing amplitudes, as observed in experiments. The model also correctly captures the mild nonlinearity in
$P_f$
near lock-in.
Spectral power of natural frequency (
$P_ n$
), forcing frequency (
$P_ f$
),
$P_ n$
+
$P_ f$
, subharmonics (
$P_ {f/2}$
,
$P_ {f/3}$
) and total signal power (
$P_ t$
) normalized by unforced system power (
$P_{n,u}$
). These powers are represented as functions of the forcing power and normalized by the lock-in amplitude
$(\sigma _f/\sigma _{f,loc})^2$
for (a) de-lock-in (
$f_f/f_n=0.65$
) and (b) subharmonic regime (
$f_f/f_n=0.48$
) obtained from ROPM.

Figure 20 shows the power transfer across all modes for the sub-
$1:2$
lock-in and de-lock-in regimes. For low forcing amplitudes, there is minimal reduction of
$P_n$
and the total power remains nearly invariant. The variation of
$P_{f_f}$
is linear. However, there is an increase in the spectral power (
$P_{2f}$
) as the forcing amplitude increases in a nonlinear manner.
In the
$1:2$
lock-in regime, there is a three-frequency regime indicated by the spectral contents of
$P_{f_f/2}$
and
$P_{f_f/3}$
. At lock-in, the spectral content of
$P_{f_f/3}$
drops to zero and we have period-two oscillations. In the de-lock-in regime, at high forcing amplitudes beyond lock-in, de-lock-in can be observed as a slight increase in the power of the natural mode can be observed (figure 20
a). Resonant amplification is observed in the de-lock-in regime and on the right arm of the Arnold tongue of the
$1:2$
lock-in regime. All these observations match the trends seen in experiments.
To summarize, we have shown that the model presented can capture essential features of synchronization phenomena at least in cavity flow systems involving vortex–acoustic interaction.
6. Conclusions
In the present study, the effects of external harmonic forcing on self-sustained oscillations in the flow through a duct with a double orifice cavity are investigated. Four qualitatively different regimes are observed over the range of forcing frequencies investigated: (i) synchronous quenching regime (0.9
$\leqslant$
$f_f$
/
$f_n$
$\leqslant$
1.1); (ii) asynchronous quenching regime (0.67
$\leqslant$
$f_f$
/
$f_n$
$\leqslant 0.88$
and 1.13
$\leqslant$
$f_f$
/
$f_n$
$\leqslant$
1.41); (iii) de-lock-in regime (
$ 0.55 \leqslant f_f /f_n \leqslant 0.65$
); (iv)
$1:2$
lock-in regime (
$ 0.49 \leqslant f_f /f_n \leqslant 0.51$
).
In the synchronous quenching regime, as the forcing strength increases, dynamics transitions to lock-in via phase-drifting through a saddle-node bifurcation. The forcing causes the vortex shedding process to slow down for
$f_f/f_n\lt 1$
(or speed up for
$f_f/f_n\gt 1)$
to match the forcing frequency resulting in a continuous drifting of the phase without trapping. In the asynchronous quenching regime, phase-trapping dynamics is observed before lock-in that happens via a torus-death bifurcation. The vortex shedding frequency drifts both above and below the forcing frequency maintaining an average value around the forcing frequency during phase-trapping.
A transition from
$1:1$
lock-in to
$1:2$
lock-in occurs via a region of de-lock-in whereupon the system delocks on increasing the forcing amplitude to large values beyond that required for lock-in. The delocked system exhibits a nonlinear phase drift dictated by the forcing frequency, natural frequency and its subharmonic. The shed vortices occasionally merge resulting in energy transfer from the natural mode to the subharmonic. In the
$1:2$
lock-in regime, lock-in results in period-two oscillations through vortex merging. The dynamics leading to lock-in contains a three-frequency regime where subharmonics of the forcing frequency (
$f_f/2$
,
$f_f/3$
) are observed.
An asymmetry in the synchronization map is observed on forcing either side of the natural frequency, which becomes more pronounced in the asynchronous quenching regime. This asymmetry results in a lower forcing amplitude required at lock-in for
$f_f/f_n\gt 1$
. This asymmetry potentially stems from the asymmetry of the shed vortex distribution on forcing either side of the natural frequency. There is also an observed saturation of the lock-in amplitude for
$f_f/f_n\gt 1$
over the range of frequencies investigated.
For
$f_f/f_n\gt 1$
, amplification is observed, either resonant or non-resonant depending on whether the forcing frequency is close to (synchronous quenching regime) or far from (asynchronous quenching regime) the natural frequency. This amplification results in the total power of the system exceeding the unforced system’s power on increasing the forcing amplitudes further beyond lock-in. Resonant amplification is also observed on the right-hand arm of the synchronization map in the
$1:2$
lock-in regime and the de-lock-in regime. In these latter cases, amplification happens through the excitation of the harmonic
$2f_f$
of the forcing frequency which is slightly larger than the natural frequency.
The region for optimal control is identified as the asynchronous quenching regime on the left-hand side of the Arnold tongue (
$f_f/f_n\lt 1$
) where up to 61.5 % decrease in the r.m.s. amplitude of pressure fluctuations is obtained when compared with the unforced system. In this regime, amplitude suppression is smooth (without complex dynamics or abrupt transitions) and without amplification.
A ROPM that captures vortex–acoustic interaction dynamics is developed to explain the experimental observations. The model captures the boundaries and the dynamics in various regimes, such as phase-drifting, phase-trapping and nonlinear phase-drifting. It predicts the routes to lock-in accurately as well in various regimes. The model also identifies nonlinear damping as the cause of asymmetry in the synchronization map and correctly captures saturation in the synchronization map for large detuning of forcing frequency for
$f_f\gt f_n$
. The model captures the jump in lock-in amplitudes observed in the de-lock-in regime as the dynamics transitions from
$1:1$
to
$1:2$
lock-in, although the lock-in amplitudes are overpredicted. The model accuracy with experiments is principally due to the availability of even harmonics which enables it to capture all the spectral sidebands in various regimes. This distinctive feature addresses a critical limitation in previous models, such as the van der Pol and Duffing oscillators, which could not generate self-sustained oscillations with second harmonics.
Using experiments and phenomenological modelling, this study has identified regions where open-loop active control strategy is most effective and areas where it may inadvertently exacerbate oscillations. This nuanced understanding enables a more targeted application of control methods, maximizing their efficiency while minimizing potential counterproductive effects. Additionally, we addressed critical questions concerning the observed bifurcation routes, the asymmetry in forcing on either side of the natural frequency of the unforced system, power transfer between modes at various forcing frequencies and the essential building blocks required to construct an effective ROPM based on first principles. These findings provide valuable insights and a robust framework to further advance control strategies to mitigate instabilities in complex fluid systems.
Declaration of interests
The authors report no conflict of interest to disclose.
Appendix A.
A.1. Construction of one-sided Poincaré maps
Using Takens’ delay embedding theorem (Takens Reference Takens1981), we may embed a time series
$x_{1}, x_{2}, \ldots , x_{N}$
observed at certain values of the control parameters in the system of interest in a phase space of higher dimension by selecting an appropriate time delay
$\tau$
and embedding dimension (
$d$
). The built delay coordinate vectors are
$x(j), x(j+\tau ), x(j+2\tau ), x(j+3\tau ), x(j + (d-1)\tau )$
where
$j = 1, 2, \ldots , N (d-1)$
. A graph of these vector components shows the development of the dynamics of the system as a trajectory in the phase space. To achieve this reconstruction and construct the Poincaré map, the optimum time delay
$\tau _{opt}$
and the minimum embedded dimension
$d_{0}$
need to be estimated.
The optimal time lag can be determined by computing the average mutual information, as proposed by Fraser & Swinney (Reference Fraser and Swinney1986). Average mutual information quantifies the average amount of information related to
$x(j+\tau )$
that can be expected based on knowledge of
$x(j)$
. The calculation for average mutual information is as follows:
\begin{equation} I(\tau ) = \sum \limits _{t=1}^{N} Q[x(j_i) \cap x(j_i + \tau )] \log _{2}{\frac {Q[x(j_i) \cap x(j_i + \tau )]}{Q[x(j_i)]Q[x(j_i + \tau )]}} \end{equation}
where
$N$
is sample size and
$Q$
is the probability that
$x$
has the value of
$x(j_i)$
and
$Q[x(j_i) \cap x(j_i + \tau )]$
indicates joint probability. The optimum time delay
$\tau _{opt}$
is identified as the value of
$\tau$
for which
$I(\tau )$
reaches its first local minimum.
An optimized version of the false nearest-neighbour method, known as Cao’s method (Cao Reference Cao1997), is employed to determine the least embedding dimension
$d_0$
. False neighbours, which refer to points in the phase space that diverge from their nearest neighbours as the embedding dimension increases, are identified using this method. By systematically increasing the embedding dimension, Cao’s approach monitors the number of false neighbours associated with each point in the phase space. Consequently, once the optimal time delay is established, the measure
$A(j, d)$
can be constructed as follows:
In the phase space, where
$j = 1, 2, \ldots , (N - {\rm d}\tau _{opt})$
, we define
$n(j, d)$
as the index of the point closest to the point
$x_i$
. The distance between two points is calculated by the Euclidean norm, denoted
$||.||$
. By averaging the false neighbours, we obtain a measure that depends solely on the embedding dimension and the optimal time lag as
\begin{equation} e(d) = \frac {1}{N - {\rm d}\tau _{{opt}}} \sum _{j=1}^{N - X_{{\rm d}\tau _{opt}}} A(j, d). \end{equation}
With increase in
$d$
increase in
$e(d)$
can be quantified using
$e_1(d)$
defined as
The process of ascertaining the minimum embedding dimension necessary for the input signal
$x(j)$
involves identifying the smallest value of
$d$
beyond which
$e_1(d)$
achieves saturation.
Once the phase space is identified and the trajectory estimated from the time series, we can cut this trajectory in the transverse direction using an appropriately chosen hyperplane to simplify the visualization of dynamics by projecting it on to a lower dimension. This hyperplane (or surface for a three-dimensional phase space) is known as the Poincaré map. If we consider only the intersection of the trajectory in one direction, it is labelled a one-sided Poincaré map.
The section must be transverse, meaning it is not tangent to the trajectories at the intersection points. To construct an appropriate Poincaré map, the transverse plane (or section) in phase space is typically chosen to intersect all possible trajectories of the dynamical system at least once per cycle. This ensures that the map effectively captures the recurrent behaviour of the system. For each crossing of the Poincaré map, we record the trajectory coordinates in the section’s reduced space and plot successive intersection points ensuring that the direction sense is maintained on intersection. These points reveal system dynamics in a reduced space and can be used to identify various transitions.
One-sided Poincaré map for trajectories representing (a) a periodic limit cycle, (b) period-two oscillations, (c) evolution on a
$T^2$
torus and (d) a
$T^3$
torus.

A blob or a fixed point on the one-sided Poincaré map represents the limit cycle; two fixed points correspond to period-two oscillations and so on. A closed ring is observed for
$T^2$
quasiperiodicity and two closed rings for
$T^3$
quasiperiodicity as can be seen in figure 21.
A stroboscopic map, which is relatively simpler to plot and routinely used in forced synchronization problems gives the same qualitative results as the Poincaré map. However, for our data sets, visualization of dynamics is much poorer in the stroboscopic maps for complex dynamics (especially in understanding bifurcations) and hence is avoided.
A.2. Correlation dimension
The correlation dimension serves as a topological indicator of the fractal dimensionality of an attractor. It quantifies the structure of the attractor, with a value of one indicating a limit cycle, two a
$T^2$
quasiperiodic attractor, three a
$T^3$
quasiperiodic attractor and so on. Non-integer values of correlation dimension are seen for strange attractors.
Correlation dimension (a) periodic limit cycle with
$\overline {D}_c=1$
, (b)
$T^2$
torus with
$\overline {D}_c=2$
and (c)
$T^3$
torus with
$\overline {D}_c=3$
obtained for various forced configuration obtained from experiments.

In our study, we employ the Grassberger and Procaccia algorithm (Grassberger & Procaccia Reference Grassberger and Procaccia1983) to compute the correlation dimension. The correlation sum assesses the probability of two points in the state vector occurring within a specified Euclidean distance, denoted as
$R$
. We calculate the local slope of the correlation sum (
${D}_c$
) and find its average (
$\overline {D}_c$
) to calculate the correlation dimension of a signal. We estimate correlation dimension to confirm the dimensionality of higher-order tori obtained in experiments. Correlation dimension for a periodic limit cycle with
$\overline {D}_c=1$
,
$T^2$
torus with
$\overline {D}_c=2$
and
$T^3$
torus with
$\overline {D}_c=3$
are shown in figure 22.
For a given embedded time series
$\{x^{\prime}_i(d)\}_{j=1}^{N - (d - 1)\tau }$
, the correlation sum
$E_N(d, R)$
is defined as
\begin{equation} E_N(d, R) = \frac {2}{N(N - 1)} \sum _{j=1}^N \sum _{i=j+1}^N H\big(R - \big\|x^{\prime}_j(d) - x^{\prime}_i(d)\big\|\big) \end{equation}
where
$N$
is the total number of points in the embedded time series,
$d$
is the embedding dimension,
$R$
is the threshold distance, H is the Heaviside function, defined as
\begin{equation} H = \begin{cases} 1, & \big(R - \big\|x^{\prime}_j(d) - x^{\prime}_i(d)\big\|\big) \gt 0, \\ 0, & \big(R - \big\|x^{\prime}_j(d) - x^{\prime}_i(d)\big\|\big)\leqslant 0, \end{cases} \end{equation}
$\|x^{\prime}_j(d) - x^{\prime}_i(d)\|$
is the distance between state vectors
$x^{\prime}_j(d)$
and
$x^{\prime}_i(d)$
in the chosen norm.
The correlation sum quantifies the probability of pairs of state vectors
$(x^{\prime}_i(d), x^{\prime}_j(d))$
whose distance is within the threshold
$R$
. It is expected to follow a power-law behaviour in a specific region. Its local slope in this scaling region is defined as
The average value of the local slopes
$\overline {D_c}(d, R)$
in the scaling region is estimated as the correlation dimension.
A.3. The 0–1 test for chaos
The 0–1 chaos test distinguishes chaotic behaviour in dynamical systems through a binary outcome (Gottwald & Melbourne Reference Gottwald and Melbourne2004). It involves computing a test statistic,
$K$
, which asymptotically approaches either 0 or 1. The result of
$K\approx 1$
indicates chaos, marked by a strong sensitivity to initial conditions and an absence of predictability over long time spans. Conversely,
$K\approx 0$
suggests regular, non-chaotic dynamics, often associated with periodic or quasiperiodic behaviour. This test is computationally efficient and robust, making it a valuable tool to identify chaos in various complex systems.
(a) One-sided Poincaré maps displaying various system dynamics as the forcing amplitude is increased in the
$1:2$
lock-in regime (
$f_f/f_n=0.49$
). A dense trajectory is visible at higher forcing amplitudes beyond lock-in without de-lock-in. (b) The 0–1 chaos test constant (
$K$
) indicating absence of chaos. The system is also not in de-lock-in as the natural frequency does not reappear in dynamics.

Figure 23 displays various system dynamics on a Poincaré map as the forcing amplitude is increased in the
$1:2$
lock-in regime (
$f_f/f_n=0.49$
). A dense trajectory is visible at higher forcing amplitudes beyond lock-in which can be confused for chaos. As can be seen in figure 23(b), the 0–1 chaos test constant
$K$
has low values close to zero for all forcing amplitudes showing the absence of chaos.








































































































