Open access peer-reviewed chapter - ONLINE FIRST

Extracting Coherent Structures in Near-Wall Turbulence Based on Wavelet Analysis

By Peng Du, Haibao Hu and Xiao Huang

Submitted: December 14th 2019Reviewed: March 5th 2020Published: July 21st 2020

DOI: 10.5772/intechopen.92015

Downloaded: 34

Abstract

To analyze the properties of the coherent structures in near-wall turbulence, an extraction method based on wavelet transform (WT) and a verification procedure based on correlation analysis are proposed in this work. The flow field of the turbulent boundary layer is measured using the hot-film anemometer in a gravitational low-speed water tunnel. The obtained velocity profile and turbulence intensity are validated with traditional boundary layer theory. The fluctuating velocities at three testing positions are analyzed. Using the power spectrum density (PSD) and WT, coherent and incoherent parts of the near-wall turbulence are extracted and analyzed. The probability density functions (PDFs) of the extracted signals indicate that the incoherent structures of turbulence obey the Gaussian distribution, while the coherent structures deviate from it. The PDFs of coherent structures and original turbulence signals are similar, which means that coherent structures make the most contributions to the turbulence entrainment. A correlation parameter is defined at last to prove the validity of our extraction procedure.

Keywords

  • coherent structure
  • wavelet transform
  • correlation analysis
  • turbulence

1. Introduction

Turbulence is a commonly seen but very complicated phenomenon in nature. Numerous tests have proven that turbulence is not a pure random process but contains different scales of fluctuations called coherent structures [1, 2, 3]. These structures significantly contribute to fluid entrainment and mass, momentum, and heat transfer [4, 5]. Therefore, investigating the coherent structures is of great significance to undercover the physics and to realize flow control.

Among the techniques of turbulence analysis, wavelet transform has been proven feasible and power to detect and extract the coherent structures in turbulence [6, 7, 8, 9]. Early works are based on continuous wavelet transform (CWT). Liandrant [10] and Jiang [11, 12] proposed the maximum energy principle, which considered the signal at the maximum energy scale as the burst events in turbulence. Kim [13] identified the coherent structure around a vibrating cantilever based on CWT. However, a drawback of CWT is that it is unable to reconstruct the signal if the mother wavelet is not orthogonal [14, 15, 16]. To solve this problem, Longo [17] used the multiresolution analysis technique based on the discrete wavelet transform (DWT) and extracted the structures in turbulence. DWT has evident advantages compared with CWT since it is invertible and multi-scaled scales can be analyzed. Kadoch [18] combined DWT and direct numerical simulation (DNS), whose results proved that coherent structures preserve the vortical structures with only about 4%of the wavelet coefficients but retain 99.9%of the turbulence energy.

In this work, measurement of the turbulent boundary layer is carried out using hot-film anemometer in a gravitational low-speed water tunnel. A procedure based on the WT and correlation analysis is proposed to extract and verify the coherent and incoherent structure in turbulence.

2. Experimental tests and analysis

2.1 Experimental apparatus

A gravitational low-speed water tunnel was constructed for the experiment. The gravity generated by the water level difference drives the water flow in the tunnel, and the flow can be tested in the experimental section (Figure 1). A maximum water speed of 2.0 m/scan be reached, and the turbulence intensity is less than 2%. The IFA300 hot-wire anemometer was used to measure the turbulence boundary layer flow at a series of positions in the vertical direction (Figure 2). Detailed setups in the experimental section can be observed in Figure 2. A probe penetrates into the flow to measure the flow field. A coordinate frame was used to move the probe in the vertical direction, with a precision of 0.01 mm. During the experiment, the sampling frequency and sampling time were set to 50 kHzand 10.24 s.

Figure 1.

Sketch (left) and photo (right) of the gravitational low-speed water tunnel. (1) Water tank; (2) stabilization section; (3) contraction section; (4) experimental section; (5) electromagnetism flowmeter; (6) water level observation section; (7) water pump; (8) water storage basin; (9) switch valve.

Figure 2.

Sketch of experimental setups. (1) PC; (2) hot-film anemometer; (3) coordinate frame; (4) experimental plate; (5) hot-film probe.

2.2 Verification of turbulent boundary layer flow

By using the experimental setups in Figure 2, the flow velocity of the turbulence boundary layer was measured at a series of positions in the vertical direction. The mean velocity profile and the turbulence intensity distribution at the water speed 0.4 m/scan are analyzed in Figures 3 and 4, which agree with the turbulence boundary layer theory. This means that the flow field in the experimental section is fully developed. Our setups and techniques are ready for turbulent boundary layer tests.

Figure 3.

The profile of mean velocity at the water speed 0.4 m/s.

Figure 4.

Turbulence intensity at the water speed 0.4 m/s.

3. Theoretical background of wavelet transform

WT is a mapping of a time function, in a one-dimensional case, to the two dimensional time-scale joint representation. The temporal aspect of the signal can be preserved. The wavelet transform provides multiresolution analysis with dilated windows. The high-frequency part of the signal is analyzed using narrow windows, and the low-frequency part is done using wide windows. WT decomposes the signal into different frequency components and then studies each component with a resolution matched to its scale. It has advantages over traditional Fourier methods in analyzing physics where the signal contains discontinuities and sharp spikes.

WT of a signal stis defined as the integral transform of ψa,b=1aψtba, which can be expressed as:

Wfab=stψa,bdt=st1aψtbadtE1

where φm,ntis the scaling function, which is defined as φm,nt=2m/2φ2mtn, and where aand bare the scale and position [19].

Scale a and position b should be discretized for applications. Usually we choose a=2mmZa0>1, b=n2mb0>0nZ. When ψtobeys the orthogonal condition ψm,ntψm,ntdt=δm,mδn,n, the functions of the orthogonal basis can be written as:

ψm,nt=12mψtn2m2m=2m/2ψ2mtnE2

The corresponding DWT can be expressed as:

<s,ψm,n>=2m/2stψm,ntdt=2m/2stψ2mtndtE3

The orthogonality of ψm,nteliminates the relevance between the points in wavelet space because of redundancy. The analyzing result of WT can thus reflect the characteristics of the original signal. Based on OWT, the signal stcan be written as:

st=<s,ψm,n>ψm,ntE4

By choosing the scale m0as the critical value, the signal stcan be divided into the approximate and detailed parts:

st=m=m0+1n=<s,ψm,n>ψm,nt+m=m0n=<s,ψm,n>ψm,nt=n=<s,φm,n>φm0,nt+m=m0n=<s,ψm,n>ψm,nt=n=am0nφm0,nt+m=m0n=dmnψm,nt=Am0+m=1mDmE5

where ψm,ntis the wavelet function. φm,ntcan be viewed as a low-pass filter, while ψm,ntas a band-pass filter. The first part of the above equation is the low-frequency approximation of the signal stat the scale 2m0; the high-frequency part is the details of the signal st[15, 20].

For turbulence, the fluctuating velocity of turbulence can be normally divided into two subparts:

s=s˜+sE6

where s˜is the coherent part and sis the incoherent part. The signals s˜and sare statistically independent.

By adopting the multiresolution analysis (Figure 5), the turbulence signal stcan be divided into different frequencies. Coherent structures can thus be reconstructed in a selected frequency domain. Other redundant signals can then be eliminated. Therefore, the frequency range determination and localization of the coherent structures are critical in this process. The frequency can be determined as:

Figure 5.

Sketch of the multiresolution analysis.

f=fcfiaE7

where fsand fcare the sampling frequency and the central frequency of a particular wavelet basis. a is the scale, denoted as 2m(mis a particular level of decomposition) in OWT. It represents the original frequency range of the turbulence signal when m=0(i.e., a=1), f=f0.

4. Extraction and verification of turbulent structures

To extract the coherent structures in turbulence, the signals at the central area of turbulence should be selected. According to previous studies [20, 21, 22], the formation of the coherent structures in turbulence is formed in the area of 0<y+<30, and the self-sustaining of the coherent structures is in the area of 20<y+<60. As a result, three testing positions with the y+20.8, 33.5, and 42.6 were selected, whose fluctuating velocity signals are shown in Figure 6.

Figure 6.

Fluctuating velocity signals at three positions (a) y+=20.8, (b) y+=33.5, (c) y+=42.6.

4.1 Preliminary evaluation of coherent structures

For preliminary evaluations of the coherent structures, CWT is first utilized for the analysis. CWT is a mathematical mapping similar to the Fourier transform [23, 24]. It is linear, invertible, and orthogonal. However, the Fourier transform uses basis functions, including the sines and cosines, which extend to infinity in time, while wavelet basis functions drop towards zero outside a finite domain (compact support). This allows for an effective localization in both time and frequency. CWT uses inner products to measure the similarity between the turbulence signal and the wavelet function, which defines a mapping between the two. CWT compares the turbulence signal to shifted and compressed/stretched versions of the wavelet function. Compressing/stretching is also referred to as dilation or scaling and corresponds to the physical notion of scale. By continuously varying the values of the scale parameter, a, and the position parameter, b, one can obtain the CWT coefficients at last.

In the work, the 5th order of Daubechies wavelet was selected as the basis function, whose central frequency fc is 0.6667 Hz. The calculated CWT coefficients of the three signals are shown in Figure 7, where the quasi-periodic structures (coherent structures) of turbulence can be clearly observed. The modulus of the wavelet coefficients shows that during the vortex breakdown, which is caused by the strong nonlinear flow instability, energy is spread over a wide range of scales. Large-scale structures exhibit anisotropic properties in the flow. Their peaks and troughs appear at the scale about 300, corresponding with a frequency of 0.6667/300 = 0.0022 Hz. These dominant scales will have the highest level of energy in turbulence. At the smaller scales, the vortices break up into intermittent small-scale features. Some organizations are evident here, with periodical and intermittent turbulent bursts. The low-frequency structures will decay to isotropic structures and dissipate in turbulence at last.

Figure 7.

Continuous wavelet transform coefficients at (a) y+=20.8, (b) y+=33.5, (c) y+=42.6.

4.2 Extraction of coherent structures

To obtain the frequency range of coherent structures in turbulence, power spectrum densities of the three selected signals were calculated in Figure 8. The centralized frequencies of the coherent structures are found in the range 0 230 Hz, 0 240 Hz, 0 230 Hz. The rapid attenuation of PSD demonstrates the low noise of our experimental system. Multiresolution analysis of OWT was used to extract the coherent structures in turbulence [9, 25, 26].

Figure 8.

Power spectrum densities at the three positions (a) y+=20.8, (b) y+=33.5, (c) y+=42.6.

WT of a signal is equivalent to local cross-correlation analysis between the signal and wavelet function. OWT carries out the multi-resolution analysis for both decomposition and reconstruction of the original turbulence signal. It is thought of the wavelet coefficients as digital filters as which the original signal is passed through low-pass filters to decompose into low-frequency components and passed through high-pass filters to analyze into high-frequency components.

Using the multiresolution analysis of OWT, the turbulence signal was split into seven scales as in Table 1, which eliminates most of the redundant signals. The frequency range of the approximate signal is mainly in the range 0 260 Hz, which covers most of the coherent structures. In Table 1, the coherent structures are found to take almost 75 %of the whole energy in turbulence.

SignalFrequency/HzEnergy/%
y+=20.8y+=33.5y+=42.6
s0 33,335100100100
A70 26085.649877.067781.3847
D7260 5200.01470.02000.0259
D6520 10420.00620.00860.0129
D51042 20830.00190.00360.0042
D42083 41670.04640.07030.0868
D34167 83,3340.39570.80990.8505
D283,334 16,6683.59935.59745.2322
D116,668 33,33510.241116.422512.4028

Table 1.

Frequency and energy distribution of seven level decompositions.

The extracted signals of each level are shown in Figure 9, where “A7” is the approximate signal, i.e., the coherent structures; where “sD7” is the incoherent structures, which is calculated by:

Figure 9.

Extracted signals in turbulence. (a) Incoherent structure (y+=20.8); (b) coherent structure (y+=20.8); (c) incoherent structure (y+=33.5); (d) coherent structure (y+=33.5); (e) incoherent structure (y+=42.6); (f) coherent structure (y+=42.6).

sD7=sA7=D1+D2++D7,E8

and where “s” is the original signal. “D1 D7” are the detailed signals of each level.

4.3 Verification of extracted signals

To characterize the properties of the extracted signals, the probability density functions (PDFs) were analyzed in Figure 10. It can be observed that the incoherent structures are approximately Gaussian, demonstrating isotropic characteristics. The PDFs of coherent structures deviate from the Gaussian distribution, presenting strong anisotropic characteristics. And the PDFs of the coherent structures resemble that of the original turbulence signals. This means that coherent structures contribute the most to turbulence entrainment.

Figure 10.

Probability density functions at three testing positions (a) y+=20.8, (b) y+=33.5, (c) y+=42.6.

For further validation of the extracted coherent and incoherent structures, correlation analysis was carried out here. A correlation parameter βbetween these structures was defined [27]:

β=vavd¯v2¯=1Nvaivdi1Nvi2E9

where vis the fluctuating velocity signal. The subscripts “a” and “d” represent the coherent and incoherent structures. Nis the number of the sampling points. vavd¯can be regarded as the stress between the coherent and incoherent structures. Value of βrepresents the correlation between coherent and incoherent structures. A large value of βmeans that the coherent structures are divided into detailed signals as incoherent structures, denoting an inappropriate selection of the decomposition level. If the coherent structures are correctly extracted, the correlation parameter βshould be 0. According to Eq. (9), βof our three selected signals at the level 7 are 3.8444×104, 7.2638×104, and 3.2677×104, respectively, demonstrating the low correlation between the extracted coherent and incoherent structures. This proves the validity of the proposed extraction process.

5. Conclusion

The flow field of the turbulence boundary layer was measured using hot-film anemometer in a gravitational low-speed water tunnel. The coherent and incoherent structures in turbulence were separated successfully with an extraction method based on WT. With CWT, the turbulent structures can be observed in various scales. With DWT, multiresolution analysis can be carried out for the decomposition and reconstruction of vortical structures in different scales. The PDF of the incoherent structures was found to obey the Gaussian distribution, while that of the coherent structures deviate from it. The similarity of the PDFs of the coherent structures and the original turbulence signal demonstrate that the coherent structures make most contributions to turbulence. A correlation parameter between coherent and incoherent structures was defined, which proves the successful separation of coherent structure from turbulence.

Acknowledgments

The authors acknowledge the support from the National Natural Science Foundation of China (Grant No. 51879218, 51679203) and Fundamental Research Funds for the Central Universities (Grant No. 3102018gxc007, 3102020HHZY030004).

Conflict of interest

The authors declare no conflict of interest.

Appendix I: complex wavelet transform

The continuous wavelet transform (CWT) has the drawback of redundancy. As the dilation parameter a and the shift parameter b take continuous values, the resulting CWT is a very redundant representation. Therefore, the discrete wavelet transform was proposed to overcome this problem by setting the scale and shift parameters on a discrete set of basis functions. Their discretization is performed by:

a=a0jb=ka0jb0forj,kZE10

where a0>1is the dilation and b00is the translation. The family of wavelets can be expressed as:

ψj,kt=a0j/2ψa0jtkb0E11

and the discrete wavelet decomposition of a signal ftis:

ft=jkDfjkψj,ktE12

where Dfjkis the DWT of the signal ft. The most widely used dilation and shift parameters are a=2and b=1.

The basis function set ψj,kshould be orthonormal such that:

Dfjk=ψj,ktftdt=ψj,ktftE13

The advantage of the DWT is the multi-resolution analysis ability. Although the standard DWT is powerful, it has three major disadvantages that undermine its applications: shift sensitivity, poor directionality, and absence of phase information.

Complex wavelet transform can be used to overcome these drawbacks. It uses complex-valued filtering and decomposes the signal into real and imaginary parts, which can be used to calculate the amplitude and phase information.

For turbulence analysis, the complex wavelet transform should be used since the modulus of the wavelet coefficients allows characterizing the evolution of the turbulent energy in both the time and frequency domains. The real-valued wavelets will make it difficult to sort out the features of the signal or the wavelet. On the contrary, the complex-valued wavelets can eliminate these spurious oscillations. The complex extension of a real signal ftcan be expressed as:

xt=ft+jgtE14

where gtis the Hilbert transform of ftand is denoted as Hftand j=11/2. The instantaneous frequency and amplitude of the signal xtcan then be calculated as:

Magnitudeofxt=ft2+gt2Angle ofxt=tan1gt/ftE15

The complex wavelet transform is able to remove the redundancy for turbulence analysis where the directionality and phase information play important roles.

Notes

Reprinted (adapted) with permission from Chinese Physics B, 2013, 22(7): 074703.

Abbreviations

WTwavelet transform
PSDpower spectrum density
OWTorthogonal wavelet transform
PDFprobability density function
CWTcontinuous wavelet transform
DWTdiscrete wavelet transform
DNSdirect numerical simulation
storiginal turbulence signal
φm,ntscaling function
ascale parameter
bposition parameter
m0critical scale
ψm,ntwavelet function
coherent part of the signal
s′incoherent part of the signal
ffrequency
fssampling frequency
fccentral frequency of particular wavelet basis
y+dimensionless wall distance
A7,D1∼D7detailed signal of each level
vfluctuating velocity signal
βcorrelation parameter

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Peng Du, Haibao Hu and Xiao Huang (July 21st 2020). Extracting Coherent Structures in Near-Wall Turbulence Based on Wavelet Analysis [Online First], IntechOpen, DOI: 10.5772/intechopen.92015. Available from:

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