3.1. Analysis of Pressure and Mach Number Variation Within the Nozzle
Plots in
Figure 7a illustrate the variation of static pressure (
P) along the nozzle length for the three
PR cases. The three plots demonstrate the presence of a “classic” trend associated with nozzle flow comprising expansion, sudden shock compression, and recovery [
35]. The expansion occurs within the converging section, as well as some distance beyond the throat. However, due to the presence of overexpansion, shock waves are generated within the diverging section for all the cases, leading to a sudden increase in the
P value between ports
P17 and
P22. It can also be seen that as
PR increases, pressure measured at port
P1 increases. This leads to
P being higher for increased
PR within the entire converging section. It can also be seen that the generation of shock-wave compression for the higher
PR occurs at a later distance from the throat. This leads to the generation of a steeper pressure gradient for higher
PR, which would further indicate the presence of increased flow separation for higher
PR, leading to increased impact of flow separation on the shock-wave structure. The plot pertaining to
PR1.81 demonstrates the presence of two spikes in
p values, leading to the presence of two humps. This is characteristic of a
-foot shock structure [
59]. Due to the increased separation shock intensity for higher
PR, the flow downstream of the first shock remains supersonic, leading to the development of expansion fans and compression shocks. Due to this, the pressure recovery is delayed significantly for higher
PR. However, beyond these bumps, the value of
P starts recovering. The convergence of
p values at
for all three cases, despite differences in the downstream compression shock position and the delayed onset of pressure recovery for higher
PR, further indicates that a higher
PR results in a stronger adverse pressure gradient, leading to increased flow separation intensity. This increased flow separation instability feeds the complex SBLI dynamics.
Plots in
Figure 7b present the
Ma variation along the nozzle for three cases. These values were calculated by applying isentropic relations to the aforementioned
p values. The value of
Ma associated with the three cases increases within the converging section and up to a finite distance downstream of the throat, beyond which it starts to reduce due to the formation of shock waves, and ultimately converges to similar values at port
P30.
Ma reduction is steeper and occurs at a lower
Ma for lower
PR values, as they are dominated by inviscid normal shock-wave phenomena resulting in a steeper flow deceleration. It is also noticeable that the higher
PR amounts to higher
Ma values within the nozzle, followed by a slower deceleration beyond the shock wave. The higher
amounts to increased bulk momentum of the incoming flow, which has a significant impact on the origin of SBLIs, and hence the underlying unsteady interactions. The presence of two bumps for
PR1.81 is again indicative of an increased impact of the separation shock, leading to the formation of oblique shocks, and hence the gradual shock-induced deceleration.
3.2. Schlieren Image-Based Flow Structure Analysis of Nozzle Flow for Different Pressure Ratios
In order to shed more light on the large-scale oscillations of shock waves, this section presents a preliminary analysis of the comparison of the flow structure corresponding to the three wind tunnel conditions. This is achieved by comparing the time-sequence Schlieren images at four successive time samples (
to
, where
is the sampling rate of the images). The subfigures in
Figure 8 illustrate the presence of varying SBLI dynamics leading to discrete Mach disk lengths, the
-foot structure, and the accompanying flow separation region and coherent vortical structures linked thereto, which is on par with the physics elaborated in [
46,
59,
60]. It was also noted that this complex shock-wave structure presented streamwise oscillations within the divergent section. The aim of this research was to carry out spectral characterization of these different events and enhance fundamental understanding related to these low-frequency shock-wave oscillations. As noted in the figures, shock-wave structures consist of an inviscid normal shock (also called the Mach disk) near the top surface (indicated as
A in
Figure 8b), a prominent
-foot shock structure (indicated as
B) comprising a leading separation shock (bright white line:
C,
Figure 8c) and a reflection wave (downstream dark line:
D) linked with the lower region followed by shear-layer separation region (
E). The two shock waves (
C and D) merge with the Mach disk at the triple point (
F). The varying intensities of these shock-wave structures lead to varying flow separation dynamics downstream.
The time-sequence images for
PR1.44, that is,
Figure 8a,d,g,j, indicate that the lower ratio leads to SBLIs being dominated by the inviscid Mach disk structure occurring closer to the throat. This led to increased and earlier pressure increment beyond the shock wave for
PR1.44, as indicated earlier in
Figure 7a. Owing to the thinner boundary layer at this portion, as well as the weaker shock wave, the effect pertaining to the shock-wave impinging on the boundary layer is minimal, and hence the
-foot structure is visibly small-scale. It was also contemplated from the time-sequence images that this normal shock wave was more stable. Thus, the weaker shock wave at this
PR leads to a more stable shock wave [
12]. Due to the presence of this normal shock wave, downstream flow is dominated by subsonic flow aerodynamics and forms a fully separated shear-layer downstream. Due to the relatively lower velocity gradient between the shear layer and the post-shock core flow, density variations leading to Kelvin–Helmhotz (KH) instabilities are less intense, resulting in minimal density fluctuations downstream of the shock. The flow downstream is mainly dominated by non-linearities associated with shear-layer eddies. Notwithstanding these attributes, this case still presented streamwise oscillations of the shock-wave structure.
As
PR increases to
, this flow interaction becomes more complex, and the time-resolved images illustrate the presence of incipient separation [
61], leading to the formation of FSS, wherein the flow downstream of the shock wave close to the surfaces lacks flow reattachment [
15], and a prominent
-foot structure originates. Due to the increased energy of higher
PR flow, the shock wave originates at a later distance (
Figure 8b) downstream of the throat, wherein the attached boundary layer is thicker. These observations are similar to the ones observed by Papamoschou [
35]. Higher
PR leads to increased momentum of the incoming flow, which results in a fuller profile, leading to a more downstream position of the SBLIs [
7]. Furthermore, higher
PR leads to the development of a stronger shock wave, resulting in an increased adverse pressure gradient that interacts with the underlying boundary layer to create a separation bubble upstream of the Mach disk that ultimately results in the formation of an oblique separation shock. The flow downstream of this oblique wave interacts with the shear layer. Due to the heightened velocity differences between these two regions, KH instability fluctuations are more intense in this case (
Figure 8e:
F).
Figure 8e further indicates the origin of an additional stronger shock wave from the triple point, downstream of the separation shock, called the reflection shock (
G). Its intensity increases as flow develops with time (compare
Figure 8e:
G and
Figure 8h:
H). This leads to increased KH interactions at the foot of the
-foot structure. Moreover,
Figure 8k shows the presence of a white line originating from the triple point, called the slip line (
I), which is a result of slow-moving flow downstream of the normal shock interacting with the faster flow downstream of the reflection shock leading to increased flow intermixing, and hence the intense density variations appear as line originating at the triple point. Distance between the first separation shock and the trailing reflection shock is called the separation length scale [
7] and is notated as
. Notably, the shear-layer separation is exacerbated for this case, leading to increased density fluctuations downstream. Moreover, flapping of the shear layer was more appreciable at this
PR.
As
PR increased to
PR1.81,
-shock-wave intensity increased and occurred at a later distance from the throat. Due to the overall shock-wave intensity increment, flow separation downstream of the Mach disk is exacerbated, leading to increased interactions and the
-foot structure becoming more intense. In fact,
Figure 8c,f,i,l illustrate the presence of a small
-structure even at the upper portion of the whole structure (See
J in
Figure 8i). Fluctuations pertaining to
were observed to be more significant at this
PR, which would indicate increased oscillations within the separation region, as well as global instability associated with vortex shedding. This subsequently leads to a more intense reflection shock for this case. Thus, increased
PR led to increased interactions between the different regions related to SBLIs, which would indicate the increased influence of high-frequency KH instabilities associated with mixing between the core supersonic flow and shear layer, as well as the eddies associated with slip line formation (See
K in
Figure 8i,l). The increased flow interactions are corroborated by the presence of increased density fluctuations downstream of the separation shock for
PR1.81. The increased influence of turbulent eddies on the overall flow pattern would indicate the presence of increased impact of high-frequency turbulent eddies on the frequency spectrum, which will be further emphasized using spectral analysis in a later section. Similarly to
PR1.44, this case also exhibited the presence of low-frequency large-scale oscillations of the shock-wave structure with respect to the separation-shock foot. In a nutshell, the higher the
PR, the more prominent the impact of separation and reflection shocks will be, leading to a more prominent
shock-wave structure. An illustration depicting the evolution of flow structure as
PR increases within the studied nozzle is provided in the schematics presented in
Figure 9. The lower
PR (
Figure 9a) flow was dominated by normal shock component occurring at an earlier position within the nozzle, whereas the higher
PR flow is dominated by a more complex
-foot shock structure emanating at a latter distance, leading to increased flow inter-mixing, and hence a more complex downstream flow structure, including reflected shocks, slip lines, increased shear-layer separation and KH vortices.
Thus, we can say that increasing the
PR led to increased interactions between the different components, leading to a significant impact on the overall structure of these SBLIs. Moreover, these heightened complex interactions between the shock wave and underlying boundary layer led to the formation of shock trains (
L in
Figure 8l), a bigger separation region (
M in
Figure 8l), increased flapping of the shear layer (
N), as well as increased vortices downstream of the shock wave, as indicated by the
O region in
Figure 8l. Large-scale low-frequency oscillations associated with nozzle flows were established for all the cases. In order to provide critical insights into these quasi-periodic oscillations and reconcile the causes of this unsteadiness, a detailed spectral analysis was carried out, which is illustrated in the following sections.
3.3. Spectral Analysis of Pressure Data Obtained Using High-Frequency Transducers
Critical understanding regarding the aforementioned unsteadiness was initiated by comparing the FFT plots of time-sequence pressure data obtained using the high-frequency transducers
P1AC (
Figure 10a) and
P3AC (
Figure 10b), with the former being closer to the throat, and the latter being further downstream of the throat (See
Figure 3) and placed on the upper wall. An experimental study carried out by Bourgoing et al. [
62] demonstrated the presence of similar frequency peaks across the upper and lower ends of an asymmetric
wave. Moreover, it is well established that reflected shock waves generate an upward deflection of flow [
6], which is the reason why shear layer and prominent
-foot reflections on the lower surface will be measured by transducers placed on the opposite wall. Thus, deductions drawn from the spectral analysis of transducers placed on the upper wall will also be qualitatively similar to the lower surface flow. Through a succinct analysis of the underlying frequency components, FFT analysis leads to enhanced understanding related to oscillations that contribute significantly to the global energy spectra of unsteadiness interactions contained within the time-domain signals of pressure transducer data. Considering the number of samples being 6000 and a sampling rate (
) of 6000 per second, the resolution in the frequency domain was 1 Hz. As per the Nyquist criterion, the maximum frequency discernible through this sampling was
, that is, 3 kHz. Considering the placement of transducers on the top-surface, the spectral plots obtained using the transducer data would be dependent on the fluctuations due to Mach disk gradient, shock-wave location, as well as reflected fluctuation from the lower surface interactions.
For the three
PR cases,
Figure 10a shows that
P1AC detects the presence of three distinct peaks associated with pressure oscillations and a fourth small pulsating peak between 985 and 1068 Hz. A 2020 experiment on the compression corner by Shanguang et al. demonstrated the presence of similar three peaks residing between 100 to 1000 Hz, which provides further context to the validity of these results. The first frequency peak lies between 242 and 293 Hz, the second between 501 and 569 Hz, and the third between 814 and 933 Hz. These ranges will be termed as frequency band −1 (FB1), frequency band −2 (FB2), and frequency band −3 (FB3), respectively. The most dominant frequency, which resides within the range of 500–600 Hz, is in concordance with the 0.4 kHz–2 kHz range, as estimated by Brusniak & Dolling, 1994 [
63]. It is also evident that the corresponding frequency and power of these peaks increase significantly between
PR1.44 and
PR1.6. However, as the
PR changes from 1.6 to 1.81, this frequency increment is markedly lower. In fact, the peak frequency value for FB1 reduces from
PR1.6 to
PR1.81. It was noted earlier that the flow associated with
PR1.44 is dominated by the inviscid normal shock-wave structure, whereas the latter two were associated with increased separation shock impact leading to increased impact of the oblique shocks on the overall flow structure. Normal shock leads to exacerbated adverse pressure gradient conditions, amounting to a heightened scale of the associated vortices, which amounts to lower-frequency oscillations. The flow corresponding to
-foot interactions is associated with smaller-scale oscillations, leading to higher-frequency turbulence flow eddies. Owing to the diverse nature of the underlying flow physics, frequency differences between the former two cases are significantly steep. On the other hand, the flow structure related to
PR1.6 and
PR1.81 is similar, leading to mitigated differences between their respective peak frequency values. The subtle increment in frequency value between
PR1.6 and
PR1.81 for FB2 and FB3 is attributed to increased bulk momentum, leading to increased incoming turbulence, and hence a higher frequency [
26]. Peaks pertaining to FB4 are presented only for
PIAC. This would indicate the presence of a localized driving mechanism related to FB4 oscillations. The close proximity of shock waves to
P1AC could lead to acoustic reflection, small-scale vortices, or small-scale flapping of the shear layer, which are associated with high-frequency oscillations. Considering the dependence of these phenomena on the incoming flow momentum, higher
PR amounts to a significantly increased frequency value of peaks associated with FB4.
It is also noticeable that the overall magnitude of FB2, FB3, and FB4 increases between
PR1.44 and
PR1.6, whereas it reduces from
PR1.6 to
PR1.81. This could be associated with the relative placement of the transducer with respect to the shock-wave interaction. As mentioned earlier, the complex interaction region moves downstream as
PR increases. The transition from
PR1.4 to
PR1.6 leads to a shock wave moving closer to the
P1AC, leading to increased magnitudes of the detected FB2, FB3, and FB4 peak oscillations. On the other hand, between
PR1.6 and
PR1.81, the interaction regions move further downstream. The reduced magnitude indicates that the transducer moves upstream at some of the time-stamps, leading to a reduction of the averaged magnitude of these pulsations. The magnitude related to FB1 increases between
PR1.44 and
PR1.6, whereas it remains similar in magnitude between
PR1.6 and
PR1.81. This indicates the presence of a low-frequency large-scale phenomenon within the flow, for which the amplitude varies significantly between the first two, whereas it remains the same between the last two cases. This indicates that this modulation is related to large-scale instabilities within the separated shear layer that lead to flapping of the shear layers [
64], which could be related to the shedding of vortices and separation-layer breathing. At higher
PR, this global instability increases, leading to an elevated scale of separation-layer oscillations, and hence the lowered-frequency value of the associated FB1 peak. Thus, transducer data placed closer to the throat, wherein the effect of shock-wave unsteadiness would be the maximum, illustrates the presence of three primary peaks, which will be further corroborated using shock-wave position data FFT. The plots also demonstrate that as the effect of
-foot increases, small-scale oscillations associated with broadband frequency pulsations become more prominent, and are showcased as increased high-frequency spectrum magnitudes. Therefore, higher
PR values imply a greater impact of flow separation, which results in a broader and more attenuated oscillation spectrum.
Spectral plots pertaining to port
P3AC in
Figure 10b display unique characteristics pertaining to pressure wave oscillations. The pressure waves recorded at this location will be influenced by large-scale streamwise oscillations of shock waves, small-scale high-frequency turbulent oscillations related to flow separation, shear layer, as well as acoustic disturbances. Frequencies pertaining to the first three peaks occur at the same frequency value compared to those existing at
P1AC. This is indicative of increased correlation of the associated oscillations across the two locations. It is also noteworthy that the magnitude of FB1 and FB2 peaks is lower at
P3AC compared to
P1AC. Thus, downstream of the shock, increased mixing due to separation-induced SBLIs leads to attenuated power of these two modes of oscillations, which is indicative of their association with the overall interaction dynamics. It is also noteworthy that the amplitude of FB1 increases as
PR increases, which provides further credence to this modulation being associated with the separation-induced vortex shedding phenomena (to be clarified using wavelet analysis in a later section). The amplitude of FB3 is higher at this location. Thus, the effect of high-frequency oscillations is higher at this location, which would indicate the dependence of these oscillations on the shear-layer oscillations, including flapping, which becomes more intense and thicker as the flow moves downstream of the interaction region [
64]. Thus, the impact of high-frequency overtones attributed to mixing-layer flow eddies present at this location increases, leading to increased frequency and amplitude scales. These observations emphasize the relation of low-frequency peaks with large-scale oscillations of the interactions, whereas the higher-frequency peaks were related to the turbulence characteristics linked with incoming turbulence or the shear-layer separation dynamics. Notably, these revelations are similar to those observed by Pirozolli et al. in [
65], wherein similar assertions were drawn for flow across an impinging shock configuration.
The FFT plots demonstrate the presence of multiple spectral peaks ranging between 240 to 990 Hz, with a lower power value within the diverging section. The lower two peaks are indicated to be related to the overall shock structure interaction and their oscillations, whereas the third and fourth peaks are indicative of their relation with the shear-layer instabilities. The plots also demonstrate the presence of increased correlation between the pressure data at the throat and diverging section, which is indicative of dependence of the downstream fluctuations on the throat location. To gain further insights into these unsteadiness events, detailed spectral analysis of shock-wave position data, as well as interaction regions, has been carried out in the succeeding sections.
3.4. Spectral and Statistical Analysis of Shock-Wave Position Data Derived Using Lagrangian Approach
Spectrum plots obtained using pressure data are constrained by the fact that it does not represent the complete flow-field, leading only to an external overview of the underlying unsteadiness [
3]. In order to increase the validity of these plots and also increase understanding related to shock-wave dynamics,
Figure 11 plots the spectral power density (
) of the frequency spectrum derived by carrying out an FFT of the non-dimensionalized shock-wave position with respect to the mean position of the shock wave. Data pertaining to the shock-wave position was obtained using the image processing technique described earlier in
Section 2.4. The acquired FFT plot was further smoothed using the variable moving average technique described earlier in
Section 2.5. However, moving average parameters were adjusted to improve clarity of the plots pertaining to this data and are described in
Table 6.
It can be seen that most of the spectral power pertaining to oscillations associated with shock-wave position data resides within 173 Hz to 1000 Hz, with powers reducing above and below these frequencies. Analogous to the FFT plot pertaining to pressure fluctuations described above, these plots also display the presence of three prominent frequency peaks for the three cases, with frequency values lying within the same range as that mentioned earlier. The first band (FB1) lies within 242 Hz to 297 Hz, the second (FB2) within 485–580 Hz, and the third one (FB3) within 767–920 Hz (See
Table 7). Moreover, similar to pressure FFT plots, the frequency value of these peaks is commensurate with the
PR value, with a higher
PR leading to a higher-frequency value. This increment is higher at ≈14% within
PR1.44 to
PR1.6, which reduces to an increment of 6.1% between
PR1.6 and
PR1.81. It can be ascertained that the frequency range estimated by the pressure data, as well as shock-wave position data, is very close to each other, which provides validity to the presence of these three primary oscillations dominating the entire flow field. Furthermore, this provides credibility to the accuracy of the employed Schlieren images to capture the overall flow unsteadiness.
Given the increased impact of flow-field parameters, including upstream and downstream conditions, on shock-wave position, spectral plots pertaining to shock-wave position data indicate the presence of many more low-amplitude frequency peaks, which were not visible within the pressure data FFT. The FFT plot pertaining to
PR1.44 illustrates the presence of an additional peak at 8 Hz and several small peaks below 100 Hz, which are not visible in the other two cases. The predominant normal shock interaction leading to mitigated flow separation for
PR 1.44 increases the influence of upstream flow turbulence [
7] on the shock-wave position. Considering the emphasized role of upstream high-frequency flow in driving low-frequency oscillations [
24], the detected low-frequency peaks could be attributed to the upstream-boundary-layer unsteadiness that results in a subtle ‘breathing effect’, causing small shifts in the shock location that are too subtle to be detected by the transducers. This will be further corroborated using the statistical analysis of amplitude related to these oscillations in a later analysis, as well as coherence and spatial FFT analysis. Notably, the power of oscillations below the range of FB1 is significantly lower for higher
PR cases, further indicating the increased impact of high-frequency turbulent eddies and high-frequency shear-layer unsteadiness on the overall shock-wave flow oscillations.
The shock-wave position data were further processed to obtain imperative statistical data related to these oscillations. The bar plots corresponding to the mean (
), minimum (
), and maximum (
) positions of the detected shock wave from the throat have been discussed in this study. These values have been non-dimensionalized using the throat diameter and notated as
. As noted in
Figure 12a,
increases as
PR increases owing to the increased bulk momentum of the incoming flow field, leading to convection of SBLIs in the downstream direction [
22]. This is further corroborated by the presence of a smaller upstream value of the shock-wave position (
) for lower
PR. The value of
shock-wave position also presents similar trends between
PR1.6 and
PR1.81. However,
PR1.44 presents a higher value compared to
PR1.61. Due to the extended spatial range of the shock-wave position for higher
PR, relative to the throat, standard deviation (
) also subtly increases for higher
PR (
Figure 12b). Paradoxically, the non-dimensionalized amplitude of oscillations (
) about the mean position of the shock wave demonstrates a lower value as
PR increases (
Figure 12c). This reduction in amplitude is in line with the established literature [
16]. For
PR1.44, the flow is dominated by the inviscid normal shock-wave component, leading to a more stable compression, while oscillating with higher amplitudes, which further leads to a deeper downstream position of the shock wave (
Figure 12a). On the other hand, for higher
PR flow, the presence of
-foot structure amounts to improved feedback between the various interaction regions, leading to a more unstable shock-wave structure, and hence smaller
. The distinction associated with a stark difference between the parameters related to
PR1.4 and
PR1.6, compared to the subdued variation between
PR1.6 against
PR1.81, was discerned from the FFT plots of shock-wave position data also. This is again associated with the increased influence of separation bubble pulsation for
PR1.6 and
PR1.81, which was significantly lower for
PR1.44. Thus,
PR variation impacts the overall convective and feedback forcing functions related to SBLIs, leading to varied flow interactions and, hence, the oscillations. To enhance understanding related to interaction dynamics within the different regions, detailed spectral analysis using wavelet transform (or CWT) and spatial FFT has been illustrated in the succeeding sections.
3.5. Wavelet Transform of Pressure Data
The spectral analysis described heretofore provides a global overview of dominant pulsations within the flow. This section makes use of the aforementioned CWT (
Section 2.6) methodology implemented on the pressure transducer data. Output from this transformation, that is, modulus of the Morlet transform,
, has been presented as excerpts of the scalogram contour distribution plots in
Figure 13. In the subfigures, the abscissa corresponds to time, the ordinate represents the frequency scale, and the color of the region presents the oscillation power of a particular frequency. Hence, blue corresponds to a lower
, whereas yellow represents maximum
. Notably, the first row (
Figure 13a–c) corresponds to the scalogram plot upstream of the throat (
P2AC), the second row (
Figure 13d–f) represents the region near the throat (
P1AC), and the third row images (
Figure 13g–i) are related to the scalograms obtained using a pressure transducer placed downstream of the throat (
P3AC). The value of
PR increases from the left column to the right column. Contrary to FFT, scalogram excerpts exhibit intermittent modulation in amplitude, frequency, as well as temporal scales owing to the inherent shock-wave movement. Owing to the shock-wave motion unsteadiness, energy bursts related to the three dominant modulations do not emanate at all times, but intermittently, leading to commensurate time-evolving modulation of the pressure transducer data. Thus, CWT provides a comprehensive oversight of the shock-wave motion responsible for the low-frequency and large-time scale perturbations, and would further provide insights into the associated interactions.
Comprehensive differences between the upstream (
P2AC) and downstream (
P1AC–
P3AC) spectral plots can be inferred from these plots. Pressure transducer,
P2AC (
Figure 13a–c), placed upstream of the throat, illustrates significant variation among the three
PR cases. This port is associated with attached turbulent-boundary-layer flow. The presence of high-frequency, time-filling modulation beyond 1 kHz corroborates the presence of an attached turbulent boundary layer at this location. The presence of intermittency at this frequency modulation is proof of the intermittent character of incoming turbulent-boundary-layer flow. The bandwidth, magnitude, and consistency of this oscillation increase with
PR, attributed to increased incoming turbulent-boundary-layer momentum. Apart from this high-frequency modulation,
P2AC plots further illustrate the presence of modulation within the frequency band corresponding to FB2. The wavelet transform of
P2AC for
PR1.44 illustrates the presence of time-filling modulation around 500 Hz, which is close to the peak frequency of shock-wave pulsation, as determined in
Figure 10 and
Figure 11. Thus, this modulation is present across the entire duration for
PR1.44, whereas it is limited to the first 0.4 s for
PR1.6 and
PR1.81. Notably, the intermittency is lower at this frequency compared to the intermittency observed earlier for high-frequency oscillations. Transonic flow through a nozzle has been associated with the presence of upstream acoustic feedback in earlier studies [
66,
67], with the upstream influence being higher for normal shocks. Thus, normal shock-wave oscillation that generates within the FB2 band for
PR1.44, creates an acoustic feedback leading to time-filling oscillations of the wall upstream of the throat. However, as
PR increases, the shock waves move downstream, separation and shear-layer intensity increase, and the shock wave becomes more oblique, leading to ameliorated upstream movement of the acoustic feedback. The initial energy bursts could be attributed to the presence of most upstream location interaction, leading to increased acoustic feedback (evident in
Figure 13d). The synergized increment of power associated with these initial energy bursts at FB2, compared to the increased pulsating power of the spectrum plots at
P1AC (compare
Figure 13b with
Figure 13e or
Figure 13c with
Figure 13f), further corroborates the increased impact of acoustic feedback from the moving shock waves. For all the cases, there is a time-filling low power modulation at around 50 Hz, which could be attributed to the incoming noise-related pressure fluctuations emanating from the roots blower motor.
Pressure data measured by
P1AC will be a result of coupled interactions between the large-scale shock-wave motion, separation bubble dynamics, as well as high-frequency shear-layer eddies and flapping. Owing to these unsteadiness interactions, scalogram excerpts pertaining to
P1AC (
Figure 13d–f) display increased spectral power magnitude, a broadband frequency modulation, and variable intermittency across the various spectrum bands, attributed to spatial and temporal fluctuations associated with the shock waves. It can also be gleaned that the overall bandwidth of respective frequency modulations becomes wider, and their magnitude increases with
PR increment (compare
Figure 13d with
Figure 13f). Thus, the enhanced incoming turbulence flow leads to broadband modulation of the pressure waves. The intermittent bursts associated with
PR1.44 (
Figure 13d) within the dominant FB2 band (around 500 Hz) exhibit a sparser and inconsistent modulation compared to the consistent and time-filling scalogram described earlier for
P2AC (
Figure 13a). The sparseness of frequency modulation increases from
PR1.44 to
PR1.6. Spectral peaks display increased variability for
PR1.6, owing to the shock-wave motion being closer to this transducer. Thus, when the shock wave moves closer to the transducer, the amplitude increases. As it moves away, this amplitude decreases because of the increased influence of other interactions, which are associated with lower frequencies. Although the intermittency of FB2 is similar for
PR1.81 (
Figure 13f), the magnitude of this peak is reduced at this
PR. This corroborates the reduced magnitude of the spectral peak within FB2 for
PR1.81, as described earlier in
Figure 10a. The downstream location of the shock wave with respect to the transducer for higher
PR leads to a lowered amplitude of the associated oscillation.
Spectral plots pertaining to FFT in
Figure 10 demonstrated the presence of an additional oscillatory phenomenon within FB1 (close to 250 Hz). The wavelet analysis in this section provides key insights into the time evolution of these oscillations. Its spectral power, frequency scale, as well as temporal scale, increased as
PR increased. An interesting quasi-periodic trend pertaining to reciprocal exchange of spectral power between FB1 and FB2 can be observed at this location, especially for
PR1.6 and
PR1.81. The dominant shock motion pulse (FB2) exchanges energy with a lower-frequency oscillation (FB1), which could be associated with large-scale vortex shedding phenomena. Thus, as the separation bubble size increases, the spectral power of this instability increases, which ultimately dampens the shock motion, leading to reduced amplitude of the shock motion spectrum. This energy exchange phenomenon is significantly reduced for
PR1.44 (
Figure 13d), owing to the presence of normal shock dominance, leading to an assuaged impact of these vortices. It is also noteworthy that the temporal scale of FB1 and FB2 oscillations is commensurate with each other. For instance, in
Figure 13e, the broad temporal scale of FB2 at 0.08 s and 0.28 s is followed by the broad temporal scale of FB1 fluctuations. On the other hand, the narrow energy bursts of FB2 between 0.5 s to 0.65 s are accompanied by intermittent narrow time FB1 peaks. This see-saw energy exchange phenomenon is observed for
PR1.81 (
Figure 13f). These results, along with the FFT plot of pressure data above, underline the presence of increased interdependence between the separation-zone breathing and the shock-wave motion, which corroborates the assertions drawn out by Pasquariello et al. [
31]. It can also be noted that as
PR increases, the overall magnitude of FB1 oscillations is higher, whereas it decreases for FB2 oscillations. Thus, as
PR increases, the overall separation-bubble breathing enhances, leading to increased frequency of the associated global instability and higher spectral magnitude occurring over wider time-filling intervals. On the other hand, due to the further downstream location of shock waves for
PR1.81, the overall impact of shock motion on
P1AC is reduced. Increased
PR leads to increased turbulence across the interaction due to vortex shedding within the shear layer. The impact of KH vortices, as depicted earlier in the Schlieren images, also increases as the separation shock impact enhances. This leads to the presence of intermittent modulations across higher frequencies extending beyond 1000 Hz (
Figure 13d,e). This band residing within FB3 is associated with the shear-layer flapping, whose magnitude increases as
PR increases. It can be discerned that the overall spread is wider for
PR1.81 compared to
PR1.6, indicating the broadband nature of turbulent fluctuations. The consistent intermittence of modulations pertaining to FB3 is further indicative of its relation to the turbulent interactions associated with SBLIs observed in this study.
As flow moves from
P1AC to
P3AC (
Figure 13g–i), the magnitude pertaining to FB3 oscillations becomes wider in the frequency scale, whereas it retains the same bandwidth for the other two bands. This is expected, as the flow associated with
P3AC will be linked with heightened turbulence-layer impact due to shear-layer thickening and vortex shedding. In fact, the presence of intermittent modulation around 960 Hz at this transducer for
PR1.44 (
Figure 13g), which was absent in the case of
P1AC scalogram, as seen in
Figure 13d, is associated with the shear layer at this location, leading to turbulent interactions. The magnitude of this high-frequency oscillation increases as
PR increases because of the increased bulk momentum. Similar energy bursts as well as reciprocal exchange of spectral power between FB1 and FB2 oscillations pertaining to
PR1.66 (
Figure 13h) and
PR1.81 (
Figure 13i) are observed at this location. A subtle reduction in relative amplitude pertaining to FB1 is observed at this location compared to
P1AC, because the downstream location leads to a mitigated impact of the separation-region instabilities. However, increasing the
PR at this location (
Figure 13i) leads to increased magnitude for FB1 oscillations because of the heightened flow separation characteristics of higher
PR.
These plots eloquently illustrate the presence of varying intermittency, modulation in the temporal and frequency scales, as well as local high-energy pulses of varying temporal scales for different events [
6]. Thus, the complex SBLI is a sum of numerous sparse events characterized by intermittency on the temporal scale, coupling between the different pulsations, as well as modulations associated with the shock motion and separation-layer breathing.
3.6. Spectral Analysis of Different Regions Within the Nozzle Flow at Different PR Values: Spatial FFT
After acquiring the temporal understanding related to these shock-wave oscillations on a global level, further insights regarding the underlying fluctuations within different sub-regions of SBLI are carried out in this section. This method involved carrying out an FFT analysis of time-resolved pixel intensities within specific regions called spatial FFT. For more details regarding this method, refer to the earlier section,
Section 2.7.
Figure 14 illustrates spectral energy plots derived by carrying out an ensemble-averaged FFT of grayscale values pertaining to different locations indicated earlier in
Figure 5. As noted previously, ensemble averaging was carried out by making use of five different pixel locations within a specific region. The overall frequency resolution for this study was 5 Hz. Identifiers pertaining to different locations, that is, upstream Boundary Layer (BL), downstream BL, inviscid shock wave, reflected shock wave, and separation zone between the
-foot oblique waves, are provided earlier in
Figure 5 and presented again in the subfigure legends of
Figure 14.
It can be seen from
Figure 14a through
Figure 14c that the pulsating power of the separation region is the highest, whereas it is similar for the shock wave and
-foot region in all the cases. The spectral energy of these three regions is significantly higher compared to the upstream and downstream BL. This is expected as the unsteadiness associated with SBLIs is mainly linked with these interaction regions. Upstream and downstream regions are mostly the driving mechanism behind the low-frequency shock-wave oscillations, with the relative dominance based on the inherent separation intensity [
13]. Notably, trends indicating similarity between the upstream–downstream BL signals, as well as between shock-wave-
foot signals, with the latter presenting higher magnitude, were observed earlier in a 2021 experimental study by Ligrani et al. [
14]. This provides credence to the validity of spectral trends captured in this analysis. In line with the earlier established stark difference in flow unsteadiness associated with
PR1.44 compared to
PR1.6 and
PR1.81, spectral plots presented in this section also exhibit the same trend.
In the case of
PR1.44 (
Figure 14a), the downstream and upstream BL spectral energy distribution plots exhibit minimal divergence beyond 80 Hz, with the exception of a pronounced peak in the downstream spectrum near 460 Hz (similar to the FB1 peak observed earlier for shock-wave motion). While a corresponding peak is also evident in the upstream spectrum at this frequency, its amplitude is notably lower. Other than this localized deviation, the spectral characteristics across both regions present correspondence with each other. Given the increased effect of upstream BL (identified as (d)), on shock waves for lowered separation, spectral plots pertaining to the shock-wave region (a) display significant correspondence with the upstream spectral energy trend, especially at 460 Hz. The upstream data further displays trends similar to the shock wave up to 80 Hz, which is indicative of the low-frequency acoustic signals associated with pulsating separation bubble being present at both locations (which was indicated earlier in the FFT of shock-wave position data also). Moreover, both plots display the presence of spectral bursts around 460 Hz. Plots pertaining to downstream BL and separation zone display the dominant frequency peak at the same values, as the separation region associated with normal shock interaction flow is linked with pulsating separation layer rather than the shear-layer flapping effect. This results in uniform subsonic flow downstream of the shock wave, leading to similar spectral dynamics of the separation zone and the downstream boundary layer. The separation-zone plot demonstrates the presence of three peaks with frequency ranges analogous to the peaks observed earlier in the FFT plots of pressure data (
Figure 10) as well as shock-wave position data (
Figure 11). Thus, the separation region spectral energy distribution is directly linked with oscillations pertaining to shock-wave motion at this
PR. Due to the normal shock-wave structure, the separation region fluctuates in sync with the shock-wave oscillations. The presence of similar spectral energy (both in magnitudes or overall pattern) across the shock wave and
-foot region is attributed to the reduced influence of
-foot waves in the case of
PR1.44, leading to similar trends across the two regions. The increased difference between the shock wave (a) and the upstream BL (d) regions at higher frequencies indicates a lack of feedback between the separation region and the upstream BL at high frequencies.
As
PR increases,
PR1.6 and
PR1.81 upstream BL plots in
Figure 14b and
Figure 14c, respectively, show increased magnitudes. This plot comes closer to the shock-wave-
foot signals. In fact, the frequency-wise variation of upstream BL and shock waves displays similar trends, especially within the range of 200 Hz to 600 Hz. This similarity is maximum in the case of
PR1.81. As
PR increases, the separation zone and
-foot magnitude also increase. This leads to increased feedback impact between the upstream and separation-zone regions, and hence the spectral plots display concurrence with regard to frequency-wise variations between the shock wave and upstream BL plots in this frequency range. The spectral energy for upstream BL in the case of
PR1.44 was mainly limited to frequencies below 60 Hz, beyond which it dropped suddenly. However, as
PR increased, the overall spectral energy was distributed across a wider spectrum, owing to increased momentum and hence turbulence. Owing to increased incoming turbulence, the spectral energy of the separation region also increased. This increased separation region intensity leads to increased vortex shedding, shear-layer flapping, as well as KH vortices. Thus, the overall spectrum for the separation region becomes more broadband for higher
PR. In fact, the separation region plot in
Figure 14c displays the maximum peak value at around 256 Hz, which was indicated earlier in the wavelet analysis (
Figure 13) to be due to global instability associated with vortex shedding within the separation bubbles. Due to the increased
PR, the impact of low-frequency noise (less than 60 Hz), separation region instabilities (200–500 Hz), as well as high-frequency vortical and turbulent eddies (more than 950 Hz) also increase. Increased spectral energy of upstream BL also contributes to the increased high-frequency oscillations in the separation region, an effect which increases as
PR increases. The separation zone has dominant high-frequency peaks at
PR1.44, whereas the low-medium frequency pulsations become more and more dominant at higher
PR. Due to the combined impact of increased incoming turbulence and interaction turbulence, higher-frequency pulsations present a wider bandwidth for higher PR.
Broader differences can be observed between the shock waves and
-foot at lower frequencies, which tail off at higher frequencies. Notably, the low-frequency signals are associated with large-scale oscillations.
-foot signals are influenced by low-frequency oscillations pertaining to separation-bubble instabilities and shock-location unsteadiness, which lead to their elevated spectral power, amounting to increased disparity in relation to the shock-wave spectral plot. At higher frequencies, which are mostly affected by small-scale turbulence structures like KH vortices or shear-layer eddies, the frequency spectrum is more isotropic and affects the two regions uniformly. This accounts for their comparable spectral plots at high frequencies. The pulsating power of the
-foot is closest to the separation zone plot at around 500 Hz for
PR1.6 and
PR1.81 cases. This would indicate that the pulsating power of the underlying separation bubble, at different
PR, would directly impact the spectrum of separation shocks [
32]. Spectra pertaining to shock waves and upstream BL indicate concurrent frequency-wise variations, indicating comparable oscillation dynamics. This similarity further confirms the presence of increased feedback between the upstream BL and shock-wave regions for higher
PR.
Downstream BL plots display similar trends across the three PR cases. However, the coupling of different interactions results in different peaks, as well as variations in the high-frequency spectrum. For
PR1.44 and
PR1.6, downstream BL displays the presence of peaks placed closer to each other. However, as
PR increases to 1.81 (
Figure 14c), these peaks become more widespread while increasing the magnitude for pulsations within the high-frequency FB3 spectrum. At
PR1.44, this peak occurs in sync with the separation region peak due to flow being associated with subsonic flow, leading to propagation of information from the normal shock wave to the downstream BL, and hence similar pulsation dynamics. On the other hand, for
PR1.6 and
PR1.81, this region became affected by the separation-layer breathing (near 220 Hz) or shear-layer unsteadiness (around 500 Hz), as well as shear-layer entrainment [
23]. The spectral power of these large-scale instability interactions is higher compared to the underlying higher-frequency small-scale pulsations embedded within the downstream BL. Due to the combined effect of these factors, the downstream BL displays a wider range of frequency-wise perturbations for higher
PR. It is also noteworthy that the peaks related to downstream BL at
PR1.44 were linked with oscillations pertaining to shock position (around 500 Hz). However, as
PR increased, this peak magnitude was reduced significantly due to increased coupling of other flow interactions. Moreover, the presence of an increased separation region mixing, the magnitude of lower-frequency pulsations also starts increasing. In fact, the downstream BL plot pertaining to
PR1.81 in
Figure 14c displayed the presence of an additional peak at a much lower frequency (170 Hz), which could be attributed to the shear layer-driven breathing of the separation zone, leading to lowered frequency [
23]. The plots pertaining to the separation zone further exhibit the presence of modulations below 100 Hz for higher
PR, which could be related to the separation-region breathing effect. This shall be corroborated further using coherence analysis in a later section.
Overall, the spatial FFT analysis across PR1.44, PR1.6, and PR1.81 presented in this section reveals a clear shift from high-frequency-dominated separation dynamics at lower PR to increased low-frequency pulsations and broader spectral bandwidth at higher PR. This is driven by stronger upstream turbulence and enhanced separation-bubble breathing. With increasing PR, upstream boundary layer, shock wave, -foot, and separation-zone spectra become more correlated, while downstream-boundary-layer peaks diversify due to evolving influences from shear-layer unsteadiness, entrainment, and large-scale instability structures. These trends emphasize the strengthening of the feedback mechanism and turbulence coupling within the studied SBLI as PR rises.
3.7. Coherence and Time-Lag Analysis Between Different Regions Within the Nozzle for Different PR
The current section discusses frequency-wise correlation between different interaction regions using magnitude-squared coherence and time-lag quantities. These results would examine the correlation between various frequency-specific events discussed during the previous sections. An earlier study carried out by Ligrani et al. [
14] assessed correlation variation within different regions to understand the unsteadiness related to normal shock waves. Considering the distinct flow characteristics for oblique waves compared to normal shock waves, as elaborated by Dussauge et al. [
12], this section aims to expand the understanding related to the correlation between different regions for
SBLIs characterized by varying
PR conditions that would shed further insights into the underlying flow physics.
Figure 16 compares the coherence between the shock wave and the downstream BL pixels (
). At
PR1.44,
Figure 15a indicates the presence of increased coherence (
) of the order of
at 500 Hz, which was indicated earlier to be the primary shock-wave oscillation frequency. The associated
value presented in
Figure 24a indicates a positive time lag, which conveys the convective attribute of the associated event. Thus, the shock-wave oscillations are transmitted directly to the downstream BL at
PR1.44, leading to the concurrent FFT spectrum for downstream and shock-wave signal indicated above in
Figure 14a. In fact, the presence of coherence ranging beyond
, as well as positive
for all frequencies (
Figure 23a,
Figure 24a and
Figure 25a), further backs up the direct correlation of shock-wave signal with downstream BL fluctuations at
PR1.44. However, as
PR increases, this concurrence is significantly lowered, leading to mitigated coherence between the shock wave and downstream BL signals beyond 100 Hz. In fact, the coherence becomes more widespread, amounting to increased coherence values at higher frequencies. Thus, the downstream flow is affected by small-scale, high-frequency events like KH vortices. The presence of positive
at
PR1.81, indicated in
Figure 24b and
Figure 25b pertaining to a-b interaction, further confirms the convective attribute of these oscillations at high frequency and higher
PR. A downstream BL event that affects the shock-wave oscillation is called the shear-layer entrainment effect, which leads to recharge of the shear-layer instabilities in the downstream direction, leading to flapping of the shear layer. The presence of increased coherence at a frequency close to 180 Hz in
Figure 15c further supports that this phenomenon is related to downstream-boundary-layer fluctuations. Explanation regarding the coherence peaks at frequencies below 100 Hz and above 980 has been included later.
Significant coherence between shock wave and upstream BL events (
) for
PR1.44 in
Figure 16a is indicated by the presence of high
(
) at 290 Hz and 530 Hz. Time lag (
) estimates display a negative value for events pertaining to 100 Hz to 280 Hz (
Figure 23a), whereas at 500 Hz, this value becomes positive, as seen in
Figure 24a. The low-frequency oscillations attributed to “breathing” follow a convective upstream BL → downstream BL path, whereas the subsonic flow downstream leads to high-frequency oscillations becoming easily transmitted to the upstream BL from the shock wave. This was again indicated in the scalogram plot pertaining to wavelet analysis of pressure data, wherein the plot pertaining to
PR1.44 displayed the presence of time-filling energy bursts related to 500 Hz (
Figure 13a). At higher
PR values, the effect of oblique shock waves and shear layer increases. Thus, the increased flow-separation intensity leads to heightened convective vortex shedding in the downstream direction. The presence of negative
(
Figure 23b and
Figure 24b) further emphasizes the presence of convective features related to these oscillations (FB1 and FB2).
The coherence between shock wave and
-foot signals designated as
in
Figure 17 is strongly related to the coupling of motions related to these complex flow attributes. At low
PR (
Figure 17a), due to the dominance of normal shocks, motions associated with them are tightly coupled, leading to increased influence of the large-scale (low-frequency) oscillations associated with shock-wave motion. This is indicated by the delayed shortfall of coherence, which occurs at lower frequencies for higher
PR. This leads to increased mean coherence for
PR1.44 compared to
PR1.6 and
PR1.81. At higher
PR, the coherence is influenced by the oscillations associated with high-frequency, low-scale oscillations in the separation region. This amounts to increased impact of the high-frequency components, leading to increased fluctuations of coherence at higher frequencies. Associated
exhibits a negative value for all the frequency ranges apart from FB3 pulsations in both the
PR cases. The presence of negative
for the low-medium frequency bands (
Figure 23a and
Figure 24b) indicates the relevance of shock-wave oscillations on the oscillations of
-shock oscillations, which are associated with separation region oscillations, especially for higher
. The value of
within FB3 (800–900 Hz), as seen in
Figure 25a,b, presents positive values for both cases. Thus, the high-frequency oscillations associated with turbulence bursts follow a convective mechanism from the shock towards the
-foot waves.
Figure 18,
Figure 19,
Figure 20 and
Figure 21 discuss the coherence between the separation zone (e) and the other regions (a), b, c and d). At
(
Figure 18a),
exhibits a significant coherence of
at around 500 Hz. It also has significant peaks at the frequencies close to the dominant peaks of shock-wave oscillations detected earlier, that is, within FB1 and FB3 bands, which indicates a strong correlation between shock-wave and separation-zone oscillations. At higher
, the separation zone becomes more complex, and hence the peaks become less prominent due to increased intermixing (
Figure 18b,c) and the effect of global instabilities. Despite the lowered peak values, the overall
fluctuations indicate a pattern similar to FFT plots mentioned earlier for shock-wave position data, with maximum coherence at FB2 (≈24%), and subdued peaks (≈18–20%) for oscillations lying within FB1 and FB3. The presence of negative
in
Figure 23b,
Figure 24b and
Figure 25b at all frequencies for both cases (except
PR1.44: 100–200 Hz) indicates a prominent feedback phenomenon between the separation zone and to shock wave governing the primary oscillation peaks. The presence of positive
at FB1, for
PR1.44, is related to the presence of increased normal shock impact, leading to mitigation of separation breathing effect at this
PR, with the flow being mainly dominated by pulsating global instabilities related to large-scale oscillations.
Owing to the increased influence of separation-zone unsteadiness on the overall shock-structure instabilities, further assessment regarding coherence and time-lag evaluations pertaining to oscillations in the separation zone (e) with respect to other regions that—namely, downstream BL (b),
-foot (c) and upstream BL (d)—is discussed in
Figure 19,
Figure 20 and
Figure 21, respectively. Coherence
presents the maximum coherence (>70%) within FB2, followed by subdued local maximum coherence peaks at FB1 and FB3 bands of oscillations. Similar heightened coherence was found for the shock wave versus the downstream BL earlier in
Figure 15. The presence of positive
(
Figure 23a,
Figure 24a and
Figure 25a) indicates that these events occur at the separation zone and then are transmitted to the downstream location without much deterioration. Thus, owing to the normal-shock structure, tight coupling between the shock wave, downstream BL, and separation zone exists; hence, the underlying unsteadiness of the structure is defined by the downstream motion of the shock-wave instability. Global instability associated with coherent structure within the separation region is the driving mechanism related to these shock-wave oscillations at
PR1.44. As
PR increases (
Figure 19b,c), the value of frequency associated with maximum
increases. However, the amplitude of this peak reduces as the overall unsteadiness becomes more widespread and is influenced by high-frequency oscillations related to shear-layer turbulence, as well as KH vortices. Interestingly, the plots also present the local coherence peaks close to 165 Hz. This frequency pulse was indicated earlier for the downstream BL in the spatial FFT plot of
Figure 14, associated with downstream BL flapping. Thus, contrary to the
PR1.44 case, flow unsteadiness at
PR1.6 and
PR1.81 is influenced by pulsation of the separation region, shear-layer fluctuations, as well as global instabilities. The presence of negative
in
Figure 23b,
Figure 24b and
Figure 25b is indicative of the increased feedback from the downstream shear-layer boundary layer for higher
PR.
The presence of alignment between the frequency peaks of FFT (
Figure 11) plot pertaining to shock-wave position data and the coherence estimation, as shown in
Figure 19a, provides further credence to the fact that coherence estimates in this section are forced by the flow physics rather than visual artifacts.
Although the peak coherence between the separation zone and
-foot events (
) at
PR1.44 is reduced to
, the separation zone exhibits increased correlation with respect to
-foot events analogous to shock waves presented earlier in
Figure 18. This validates the increased interaction dynamics between events pertaining to
-foot and separation-zone oscillations. In line with
described above,
also presents an increase in the value of frequency, where coherence is maximum as
PR increases (
Figure 20b,c). It can also be seen that the overall plot demonstrates the presence of higher
up to an extended range of oscillations beyond 100 Hz for
PR1.44, which indicates the presence of increased influence of low-frequency separation bubble pulsation on the
-foot structure. The value of
becomes more widespread as the
increases, which is coincident with the trends observed earlier for
. Hence, the interaction dynamics between the shock wave and the
-foot are influenced by increased shear-layer flapping, as well as global instabilities leading to higher-frequency oscillations. The presence of negative
presented in the time-lag plots further confirms that these oscillations, especially the high-frequency oscillations, originate at the
-foot and then reach the separation zone.
Figure 21 and
Figure 22 compare the magnitude-squared coherence of the separation zone and downstream BL fluctuations with upstream BL,
that is and
, respectively. In the case of
, the plots demonstrate the presence of peak coherence values (
) within FB2, with the frequency value increasing from
PR.1.44 to
PR1.6, while retaining similar values between
PR1.6 and
PR1.81. At lower
PR values, the overall
is mainly influenced by the global instability of the shock-wave oscillations within FB2, whereas at higher
(
Figure 21b,c), there is increased coherence peaks at values lower than the prominent peak due to increased shock pulsation effect corresponding to lower frequencies. The presence of positive
for all the cases suggests the presence of upstream movement of these oscillations from the separation zone. Increased
leads to increased spectral energy of the incoming flow, leading to downstream placement of shock waves; hence, the effect of shear-layer oscillations, vortex shedding, flapping effect, and pulsation bubble increases.
It has been postulated by Pirozzoli et al., 2010 [
65] that the upstream BL acts as a forcing mechanism to sustain the low-frequency breathing of the separation region pertaining to SBLIs.
Figure 22a elaborates the presence of increased
of
at around 500 Hz (main shock-oscillation frequency). Thus, the shock wave’s large-scale oscillation impacts the upstream and downstream locations similarly at this frequency for
PR1.44. The normal shock-wave structure enables convective and feedback flow of disturbances from the breathing separation bubble in both directions. The presence of negative
further emphasizes the seeding of this oscillation in the separation zone. As the
PR increases, the effect of other oscillations also increases, leading to a more uniform
distribution beyond 100 Hz (
Figure 22b,c). This negative
is presented for almost all the cases, further emphasizing its source of origin being downstream of the upstream BL. A distinct peak close to 150 Hz can be observed at
PR1.81, which is concurrent with the peak observed earlier in
Figure 14c, related to the separation-layer breathing effect, which is transmitted to both directions, leading to this peak. The presence of positive
at this frequency for
PR1.44 (
Figure 22a) indicates that this low-frequency oscillation acts as a driving force for this breathing at such a lower
PR, whereas at higher
PR, the upstream BL is mainly influenced by the feedback phenomena, which is higher because of increased global instability of the separation bubble.
Coherence associated with oscillations below 100 Hz presented an increase in magnitude-squared coherence across different regions at lower
PR. This indicates a stronger upstream influence of pulsating bubbles on the acoustic feedback, leading to increased impact of these oscillations originating within the interaction. As
increases, the impact of this acoustic feedback reduces and the influence of high-frequency oscillations increases. Consequently, the drop in coherence is delayed with higher
PR for much of the cases. These trends are applicable across all the coherence plots. However,
in
Figure 22c exhibits the presence of increased coherence values (more than
) for higher
with a negative
(
Figure 25b). This occurs because the increased
amounts to increased low-frequency oscillations in both directions owing to increased separation bubble pulsation. These pulsations lead to comparable coherence in both directions, leading to increased low-frequency coherence for downstream BL versus upstream BL at higher
PR.
3.9. Spectral Analysis of Numerical Pressure Data
To investigate the unsteady behavior of shock-induced pressure fluctuations, FFT was applied to the numerically derived time-resolved static pressure signals obtained from four monitoring locations: P20, P26 (corresponding to the experimental transducer P1AC), P26y (directly beneath P26 on the lower wall), and P3AC, a perpendicular plane near the end of the diverging section that monitors the area-weighted average of static pressure. P20 was selected because, for lower PRs (particularly PR1.44), the shock does not extend far enough downstream to influence P26, ensuring that the signal remained within the effective shock oscillation zone. Additionally, P20 consistently exhibited stronger oscillation amplitudes, making it well-suited for visualizing the frequency characteristics of the flow.
Figure 27 presents the amplitude spectra for
PR1.44,
PR1.6, and
PR1.81. Part (a) shows P20, P26y, and P1AC, which exhibit very similar frequency distributions. P26y reproduces nearly identical spectra to
P1AC despite lying beneath the shear layer, confirming the presence of the same dominant frequencies on both the upper and lower sides of the asymmetric
-wave structure. Part (b) presents the spectra from the
P3AC plane, which closely resemble those in part (a), consistent with the experimental results in
Figure 10. For
PR1.44, three distinct frequency regions are observed between 250 and 900 Hz, with peaks at 265 Hz, 510 Hz, and 800 Hz. For
PR1.6, the frequencies shift upward while maintaining three regions: peaks near 280 Hz, two peaks around 545 Hz, and multiple peaks near 905 Hz. For
PR1.81, the three regions show a single peak at 305 Hz, another at 660 Hz, and multiple peaks around 970 Hz. Notably, for the first frequency region across all
PR cases, the numerical results exhibit an increasing trend in peak frequency, whereas the experimental observations show a slight decrease in frequency for
PR1.6.
The consistent trends of increasing dominant frequency and amplitude with rising PR highlight the intensification of shock motion and its interaction with the boundary layer, producing broader and more energetic spectra. The agreement of numerical and experimental results in both frequency and amplitude confirms that the simulations effectively capture the key unsteady flow features and coherent oscillations throughout the interaction region.
3.10. Numerical Shock-Wave Dynamics Analysis
To complement the spectral analysis, the temporal evolution of the shock-wave position was tracked in the numerical simulations for all three pressure ratios. The axial position of the shock front was extracted in time and analyzed to identify its minimum and maximum extent relative to the throat. The results, presented in
Figure 28, indicate that the range of shock motion increases with rising
PR: for
PR1.44, the shock oscillates between
m and
m downstream of the throat; for
PR1.6, the range extends from
m to
m; and for
PR1.81, from
m to
m. The negative minimum value for
PR1.44 indicates that the shock occasionally moves slightly upstream of the throat, likely due to weak separation and local flow instabilities at lower pressure ratios. Although these upstream excursions are not observed in the experiments, where all positions remain downstream of the throat, the overall trend of increasing downstream shift with
PR is captured.
Further insight into the unsteady behavior of the shock was obtained by analyzing its axial position in the frequency domain using FFT. The amplitude spectra of the shock position over time are shown in the right panel of
Figure 28. Similarly to the FFT of static pressure signals, the shock position spectra exhibit multiple distinct frequency regions for each pressure ratio, reflecting the dominant oscillatory modes of the shock system.
Statistical parameters of the numerically derived shock motion were extracted from the time-resolved position data.
Table 9 presents the mean position, minimum, and maximum positions, standard deviation, and oscillation amplitude of the shock wave, normalized by the throat height. The mean shock position increases monotonically with
PR, consistent with the experimentally observed downstream migration. However, unlike the experimental data, where the standard deviation increases with
PR, the numerical results show a decreasing trend:
drops from 0.46 at PR
to 0.24 at PR
. This discrepancy may result from inherent smoothing and numerical dissipation in the URANS simulations, which dampen short-scale fluctuations that are present in experiments. Similarly, the oscillation amplitude decreases with increasing
PR, from 1.85 to 1.05, reflecting the reduced range of large-scale shock excursions both in the experiment and in the numerical models.
The negative minimum shock position observed for PR1.44 highlights the sensitivity of the shock to upstream flow perturbations under weak separation conditions. In contrast, higher PR cases exhibit strictly positive minimum positions, indicating that the shock remains fully downstream of the throat. Overall, the numerical results reproduce the main characteristics of the shock motion, capturing the downstream shift in the mean position and the general reduction in oscillation amplitude with increasing pressure ratio, while differences in standard deviation trends compared to experimental observations are likely due to the smoothing effects of the numerical scheme. These simulations will act as a benchmark for future detailed numerical evaluations pertaining to SBLIs in the context of over-expanded flow through a typical convergent–divergent nozzle.
It is important to emphasize that the physical mechanisms underlying the low-frequency oscillations remain not fully understood. In particular, scaling laws for their frequency have yet to be firmly established. Therefore, direct comparisons with the experimental results currently lack a solid theoretical foundation. The adjustable experimental rig utilized in this paper holds significant potential for advancing this understanding and establishing such scaling laws through systematic studies. Hence, the numerical study carried out at this stage presented a qualitative comparison only. Owing to the preliminary stage of numerical evaluations, this paper presented results obtained using a moderate computational framework: URANS, avoiding the need for an extremely fine mesh or extensive CPU time. The primary aim of these simulations was to determine whether such a simplified model could qualitatively reproduce the observed low-frequency shock-wave oscillations and capture the general structure of the shock and boundary-layer separation. Encouragingly, the results show a strong overall agreement with the experimental data.
It is envisaged that as the experimental campaign progresses and more parametric data become available, the numerical modeling approach will also be refined using higher-fidelity techniques such as Detached Eddy Simulation (DES), Large Eddy Simulation (LES), and Scale-Adaptive Simulation (SAS) techniques, which will result in a more detailed quantitative comparison between simulations and experimental results. Such analysis in the future will provide valuable insights not only into the flow physics but also into the performance and limitations of the numerical models.