Two-point correlation in wall turbulence according to the attached-eddy hypothesis
H. Mouri

TL;DR
This paper theoretically investigates two-point velocity correlations in wall turbulence using the attached-eddy hypothesis, deriving general forms without extra assumptions and analyzing related spectra and transfer rates.
Contribution
It derives the most general forms of correlation functions in wall turbulence based solely on the attached-eddy hypothesis, avoiding additional assumptions.
Findings
Derived general forms of two-point correlation functions.
Analyzed energy spectra and transfer rate correlations.
Provided a framework for assessing the attached-eddy hypothesis.
Abstract
For the constant-stress layer of wall turbulence, two-point correlations of velocity fluctuations are studied theoretically by using the attached-eddy hypothesis, i.e., a phenomenological model of a random superposition of energy-containing eddies that are attached to the wall. While the previous studies had invoked additional assumptions, we focus on the minimum assumptions of the hypothesis to derive its most general forms of the correlation functions. They would allow us to use or assess the hypothesis without any effect of those additional assumptions. We also study the energy spectra and the two-point correlations of the rate of momentum transfer and of the rate of energy dissipation.
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Two-point correlation in wall turbulence according to the attached-eddy hypothesis
Hideaki Mouri
Meteorological Research Institute, Nagamine, Tsukuba 305-0052, Japan
Abstract
For the constant-stress layer of wall turbulence, two-point correlations of velocity fluctuations are studied theoretically by using the attached-eddy hypothesis, i.e., a phenomenological model of a random superposition of energy-containing eddies that are attached to the wall. While the previous studies had invoked additional assumptions, we focus on the minimum assumptions of the hypothesis to derive its most general forms of the correlation functions. They would allow us to use or assess the hypothesis without any effect of those additional assumptions. We also study the energy spectra and the two-point correlations of the rate of momentum transfer and of the rate of energy dissipation.
1 Introduction
This is a theoretical study about wall turbulence that is formed in a pipe, in a channel, or over a plate. As shown in figure 1, we set a smooth wall at the - plane, set the mean stream along the direction, and use , , and to denote velocity fluctuations in the streamwise, spanwise, and wall-normal directions at a height from the wall. The mean streamwise velocity itself is not studied here. If the turbulence is stationary and at a high Reynolds number, it has a layer with some constant value of for the mean rate of momentum transfer, i.e., for the Reynolds stress . Here is the mass density, is the friction velocity, and denotes the ensemble average.
For this constant-stress layer, there is a phenomenological model of a random superposition of energy-containing eddies that are attached to the wall, i.e., the attached-eddy hypothesis ([Townsend 1976]). The velocity fields of the eddies are set to have an identical shape with a common characteristic velocity , while their sizes are distributed without any characteristic size. Actually, the constant-stress layer has a characteristic constant in units of velocity but has no characteristic constant in units of length. If the size distribution of the attached eddies is given so as to reproduce the constantness of , a logarithmic law is predicted for the variance of the streamwise velocity fluctuations as
[TABLE]
Since this prediction has been confirmed in experiments of a variety of wall turbulence ([Hultmark et al. 2012, Marusic et al. 2013]), the attached-eddy hypothesis has turned out to be a reliable model.
The important application of such a hypothesis would be to the two-point correlations or equivalently to the energy spectra of the velocity fluctuations. Besides numerical works based on a particular model of the eddies (e.g., [Marusic 2001]), there are some theoretical studies (e.g., [Perry & Chong 1982, Davidson et al. 2006]). They have invoked, however, additional assumptions such as for the similarity ([Perry & Abell 1977]). We rather focus on the minimum assumptions of the attached-eddy hypothesis that have led to the law of equation (1). These assumptions are yet sufficient to constrain the correlation functions and to clarify their most general forms, which would offer an opportunity to use or assess the hypothesis without any effect of the additional assumptions. We also study the energy spectra and the two-point correlations of some other quantities. They are to be compared with the existing models of the wall turbulence.
2 Basic setting of the hypothesis
Here is a summary of the attached-eddy hypothesis ([Townsend 1976]). The turbulence is set homogeneous in the streamwise and spanwise directions. For the case of a boundary layer, we assume that it has been well developed and hence it is negligibly dependent on the streamwise position . Since this hypothesis is for the constant-stress layer, the value of the kinematic viscosity is not essential. The limit is taken so as to ignore the viscous length with respect to the height . Then, a free-slip condition, i.e., and , is imposed on the wall at .
The attached eddies are extending from the wall into the flow but are bounded in each of the directions. Regardless of the size of the eddies, they have an identical shape with a common characteristic velocity . That is, if \mbox{\boldmath{x}}_{\rm e}=(x_{\rm e},y_{\rm e},h_{\rm e}) lies at the highest position of an eddy (see figure 1), its velocity field \mbox{\boldmath{v}}_{\rm e} is given for a position \mbox{\boldmath{x}}=(x,y,z) as
[TABLE]
The condition at is . No more assumption is required about the functional form of .
The sizes of the attached eddies are distributed continuously from to . Here corresponds to the height of the wall turbulence, i.e., pipe radius, channel half-width, or boundary layer thickness. The asymptotic laws for are regarded as those for the constant-stress layer. On the wall, the eddies are distributed randomly and independently. They could even overlap one another. We do not assume any more about the distribution of the eddies, although some previous studies had assumed a particular hierarchy in that distribution (e.g., [Perry & Chong 1982]).
From the random and independent distribution of the attached eddies, it follows that the entire velocity field is a superposition of those of the individual eddies. Any two-point correlation over a streamwise distance \mbox{\boldmath{r}}_{l}=\mbox{\boldmath{r}}_{x}=(r,0,0) at a height is the sum of those within the individual eddies of various sizes from to ,
[TABLE]
The subscripts and denote either of , , or such that and denote either of , , or . As justified later, the number density of the attached eddies at size per unit area of the wall is , where is a constant. By using in place of \langle v_{i}(\mbox{\boldmathx}+\mbox{\boldmathr}_{x})v_{j}(\mbox{\boldmathx})\rangle,
[TABLE]
Since the streamwise and spanwise sizes of each eddy have been set finite, the integral is always finite. Together with the wall condition of equation (2b), which yields a condition for in case of , equation (3) serves as the basis of the attached-eddy hypothesis.
To justify the distribution of the eddy size , the constantness of is reproduced in the limit . That is, for in equation (3a),
[TABLE]
We have used and . The condition of equation (2b) yields with a constant at . If lies in this range of as shown in figure 2, the integral is equal to . The constant is dominant in the limit . To fix the value as , we require , i.e., N_{\rm e}\varpropto 1/|\mbox{\boldmath{f}}|^{2} in equation (3) for a given shape of .
The velocity variances such as that in equation (1) are obtained via the same manner. As shown in figures 2 and 2, the wall condition of equation (2b) yields
[TABLE]
Here and are constants. The result for the constant-stress layer is
[TABLE]
Here , , and are constants. The law for has been confirmed with – and in a variety of wall turbulence ([Hultmark et al. 2012, Marusic et al. 2013]). We rely on the other laws as well. They do hold in the wall turbulence, albeit not yet certain about the values of , , and ([Sillero et al. 2013, Lee & Moser 2015]).
3 Velocity correlation along a wall-parallel line
Two-point velocity correlations along a wall-parallel line are studied at a height in the constant-stress layer. Although the line has been set streamwise, the same discussion is applicable to the case of a spanwise line. We make use of the correlation length
[TABLE]
This is expected to be well-defined in the attached-eddy hypothesis, where any correlation is determined by the individual eddies that are not dependent on one another and are of finite size. From equation (3a) with and ,
[TABLE]
While is dependent on alone, is dependent on alone.111 Although equation (8a) could be rewritten so that is another function of , it is not considered here because is not a characteristic of the constant-stress layer. That is, and are to be determined respectively by and through and .
We require to be finite. If were not finite, it would follow that is not determined and is not well-defined in the attached-eddy hypothesis. The finiteness is also required for because the streamwise size of an eddy is finite as compared with its wall-normal size. For the undermost layer of such an eddy , there is a constant in relation to equation (8b),
[TABLE]
The asymptotic form of is given in equation (5). By substituting the resultant form of into equation (8a), along with given in equation (6), we obtain in the limit . The minimum value for to be finite is adopted as the leading order to determine the asymptotic form of in equation (9). It determines the asymptotic form of in the constant-stress layer via a manner similar to that for the variance in equation (6).
The individual cases of , , and are as follows. Only a leading-order behaviour for is studied about and , e.g., about in equation (6a).
For the streamwise velocity , we adopt in equation (9) and use equation (5) to obtain in the limit . This is applied for as
[TABLE]
On the other hand, from equation (6a),
[TABLE]
By substituting them into equation (8a), we confirm that is finite. If , it would diverge as . The above asymptotic form of is equivalent through and to
[TABLE]
Thus, in this limit is independent of but is only a function of , say, . It is independent of if is fixed as . The correlation function in the constant-stress layer is thereby derived from
[TABLE]
The result is
[TABLE]
To relate these correlations continuously to the variances in equation (6), we require and . Especially if is existent and is dependent on , then is existent and is dependent on .
The functions and are to reflect the internal structures of the individual eddies. Since is due to eddies of sizes up to the height of the turbulence, it is multiplied by and is existent only for the wall-parallel velocities and that are not blocked by the wall. There is also due to eddies of sizes comparable to the height , existent for all the velocities , , and .
The functional forms of equation (10) hold for distances down to those in the inertial range. Below this range, there lies the dissipation range where the kinematic viscosity is important. Since we have taken the limit , those forms do not hold. The velocity fluctuations in the dissipation range are regarded to have been coarse-grained at a length scale in the inertial range (see also §6.2).
Lastly, we reconsider the correlation lengths in the constant-stress layer , by substituting equation (10) into equation (7) with ,
[TABLE]
They tend to increase with an increase in the height . However, and are not proportional to the height because of the factor . This is not the case for , which is exactly proportional to the height .
4 Velocity correlation along a wall-normal line
Two-point velocity correlations are also studied over a wall-normal distance \mbox{\boldmath{r}}_{l}=\mbox{\boldmath{r}}_{z}=(0,0,-r) in the range of . According to the attached-eddy hypothesis (see §2), the correlation function is given by
[TABLE]
Here is identical to . The correlation length is defined by using an integration from to as
[TABLE]
From equation (12a) with and ,
[TABLE]
We require and to be finite (see §3). Then, since is finite in the limit , its asymptotic form is identical to that of in equation (9). For the constant-stress layer , the correlation function is derived via the same manner as for those in equation (10),
[TABLE]
The result is
[TABLE]
Here and are functions of with or with . The functional forms of these correlations are summarized in table 1.
5 Energy spectrum along a wall-parallel line
From the velocity correlation along a wall-parallel line , the energy spectrum at a streamwise wavenumber is obtained as
[TABLE]
The substitution of equation (10) into equation (16) leads to the energy spectra of the attached-eddy hypothesis in the constant-stress layer ,
[TABLE]
Here, we have defined and with . The functional forms are the same even if the wavenumber is spanwise.
There is another model for the energy spectrum ([Perry & Abell 1977]). Within a range of wavenumber , some similarity is assumed among eddies of the streamwise size so that depends only on and , i.e., . If the range of the similarity is from to , where and are constants, it follows that is dependent on as in the case of equation (6a). The same law of is assumed for .
Since equation (6) originates in the attached-eddy hypothesis, the energy spectra of the hypothesis have been related to the law of ([Perry & Chong 1982]). This law is also used to constrain the functional forms of the correlations of the hypothesis ([Davidson et al. 2006]). However, the existence of such a law remains controversial (e.g., [Vallikivi et al. 2015]). The law of is in fact not consistent with the attached-eddy hypothesis. At any height , we find in equation (17) that and are dominated by and . Their spectral shapes are not allowed to yield another factor of for the variances and . Furthermore, the eddies of the streamwise size are not identical to the attached eddies, which have various sizes but could contribute to the same streamwise wavenumber at each of the height . It is coincidental for equation (6) to be derived from these two.
The similarity law of could yet approximate the internal structures of the attached eddies, i.e., or in equation (17), if the range of the similarity is not from but is from . At the height , the premultiplied spectrum is known to exhibit an energy-containing broad plateau (e.g., [Vallikivi et al. 2015]). This could be approximated by the law of through . From equation (16),
[TABLE]
There is an asymptotic relation about the cosine integral function,
[TABLE]
Thus, the correlation function could exhibit approximate dependence on in a range of , which is actually seen in the wall turbulence ([Davidson et al. 2006, Chung et al. 2015], see also [Davidson & Krogstad 2014]).
6 Other correlations
Having studied the velocity correlations in table 1 by using the minimum assumptions of the attached-eddy hypothesis, some other correlations are studied by adding assumptions that are consistent with the hypothesis. Their functional forms are summarized in table 2.
6.1 Kinetic energy and momentum transfer rate
To obtain a moment \langle v_{i}^{m}(\mbox{\boldmathx}+\mbox{\boldmathr}_{l})v_{j}^{m}(\mbox{\boldmathx})\rangle of some order , the corresponding cumulants for eddies of each size are integrated from to . Any cumulant of a sum of random variables is equal to the sum of cumulants of the variables if they are independent of one another (e.g., [Monin & Yaglom 1971]). The moment of the sum is not equal to the sum of the moments, except for low-order central moments such as and , defined for \langle v_{i}(\mbox{\boldmathx}+\mbox{\boldmathr}_{l})v_{j}(\mbox{\boldmathx})\rangle in equations (3) and (12), which serve also as cumulants. Although a combination of those integrals could yield \langle v_{i}^{m}(\mbox{\boldmathx}+\mbox{\boldmathr}_{l})v_{j}^{m}(\mbox{\boldmathx})\rangle, it tends to be a complicated combination and tends to depend on an uncertain value of . There is a more practical approach.
We set many eddies at each position on the wall, by increasing the number of the eddies . According to the central limit theorem (e.g., [Monin & Yaglom 1971]), the resultant velocity field is approximated to be Gaussian and to be determined by \langle v_{i}(\mbox{\boldmathx}+\mbox{\boldmathr}_{l})v_{j}(\mbox{\boldmathx})\rangle alone. The other cumulants are all negligible. This is known as a good approximation for the constant-stress layer of the wall turbulence ([Fernholz & Finley 1996, Meneveau & Marusic 2013]).222 The boundary layer actually exhibits and , for which the Gaussian value is ([Fernholz & Finley 1996]).
The odd-order moments are all equal to [math] in such a Gaussian field, while any even-order moment is equal to a sum of products of the above correlations. In particular,
[TABLE]
The correlation of the kinetic energy per unit mass , , or in the direction , , or is thereby related to that of the velocity in equation (10) or (15),
[TABLE]
From equation (20), we also obtain
[TABLE]
Since the wall condition of equation (2b) yields for (see §2), the correlations \langle u(\mbox{\boldmathx}+\mbox{\boldmathr}_{l})w(\mbox{\boldmathx})\rangle and \langle w(\mbox{\boldmathx}+\mbox{\boldmathr}_{l})u(\mbox{\boldmathx})\rangle depend only on in the limit (see §3). By also using equation (10) or (15) for \langle u(\mbox{\boldmathx}+\mbox{\boldmathr}_{l})u(\mbox{\boldmathx})\rangle and \langle w(\mbox{\boldmathx}+\mbox{\boldmathr}_{l})w(\mbox{\boldmathx})\rangle, the correlation function of the rate of momentum transfer per unit mass is derived for the constant-stress layer as
[TABLE]
As for the functions and , we require and . The fluctuations of are dependent on those of , which are in turn dependent on the factor . This is also the case for the correlation along a spanwise line.
6.2 Energy dissipation rate
Since the attached-eddy hypothesis is a model for the energy-containing eddies, it has not been applied to the rate of energy dissipation per unit mass \varepsilon(\mbox{\boldmathx}). There is nevertheless a possibility for this application, if we add an assumption and if we ignore fluctuations at the smallest length scales.
The dissipation fields of the individual eddies \varepsilon_{\rm e}(\mbox{\boldmathx}) are assumed to have some identical shape with a common characteristic rate ,
[TABLE]
We have the corresponding Kolmogorov length , which is not proportional to the eddy size . Thus, equation (23) does not hold for fluctuations in the dissipation range around that scale . Such fluctuations are regarded to have been coarse-grained at a length scale in the inertial range.
We set the condition at to be , although the last result is the same even in case of . The dissipation rate \varepsilon(\mbox{\boldmathx}) is averaged at a height as
[TABLE]
By using with for a given shape of (see §2) and also by using in place of \langle\varepsilon(\mbox{\boldmathx})\rangle,
[TABLE]
For , we have (see figure 2). The mean rate of energy dissipation in the constant-stress layer is
[TABLE]
To determine the coefficient for , the above constant is set equal to the inverse of the von Kármán constant, . It corresponds to a result of the local equilibrium approximation ([Townsend 1961]), where the constant-stress layer is under an equilibrium between local rates of production and dissipation of the turbulence kinetic energy.333 For the actual constant-stress layer, it is considered that the local rate of energy dissipation is –% of the local rate of energy production ([Lee & Moser 2015]).
The correlation function over a streamwise distance \mbox{\boldmathr}_{l}=\mbox{\boldmathr}_{x}=(r,0,0) at a height is given by
[TABLE]
For , we have (see figure 2). Via a manner similar to that for the velocity correlations (see §3),
[TABLE]
and hence
[TABLE]
Here is a function of with . Since the rate of an eddy is inversely proportional to its size , the entire rate is independent of that originates in eddies of sizes much larger than the height . On the other hand, from , we have . If were too large, the fluctuations of the entire rate would be negligible. They are actually not negligible even over large distances in the wall turbulence (e.g., [Mouri et al. 2006]).
7 Concluding discussion
Two-point velocity correlations have been studied theoretically for the constant-stress layer of wall turbulence on the basis of the attached-eddy hypothesis, i.e., a phenomenological model of a random superposition of energy-containing eddies that are attached to the wall ([Townsend 1976]). While the shapes of the eddies are set identical to one another with a common characteristic velocity , their sizes are distributed up to a finite value in each of the directions.
From the random distribution and the finite sizes of the attached eddies, it follows that the correlation lengths defined in equations (8) and (14) are always existent. We have used this fact to derive the most general forms of the correlation functions in equations (10) and (15) and of the energy spectra in equation (17). The results are summarized in table 1.
The correlation functions \langle v_{i}(\mbox{\boldmathx}+\mbox{\boldmathr}_{l})v_{i}(\mbox{\boldmathx})\rangle are made from due to eddies of sizes comparable to the height and from due to eddies of sizes larger than the height . We have obtained only for the wall-parallel velocities and that are not blocked by the wall. It is multiplied by because the size of the large eddies is up to the height of the turbulence.
These results are not consistent with the results of the previous studies, e.g., the spectra in the form of ([Perry & Chong 1982]). While we have focused on the minimum assumptions of the attached-eddy hypothesis, the previous studies had invoked additional assumptions. They are in fact not consistent with the hypothesis, aside from which is more reliable as a model for the wall turbulence.
Without any confounding effect of such additional assumptions, our results would offer an opportunity to assess the extent to which the attached-eddy hypothesis is consistent with the actual wall turbulence. However, at present, the direct numerical simulations are not at Reynolds numbers that are high enough to attain a layer of the strictly constant stress ([Sillero et al. 2013, Lee & Moser 2015]). The experiments are yet based mostly on Taylor’s frozen-eddy hypothesis. Improvements are desirable for the simulations and for the experiments.
There are nevertheless some experimental implications. It is known that the value of is common to a variety of flows ([Marusic et al. 2013]). This commonness is expected for the entire function , which reflects the undermost layers of the attached eddies that are insensitive to the flow configuration. The value of is not common, and so is not the entire function . We expect these implications to apply further to the other velocities and .
The two-point correlation of the wall-normal velocity is determined by the attached eddies of sizes comparable to the height of the two points. If such eddies are actually dominant in the wall turbulence ([Adrian 2007]), their internal structures would be clarified in that correlation, especially about whether the shape of the eddy is independent of its size. This is not the case for the correlations of the wall-parallel velocities and , which are affected by the larger eddies.
By adding assumptions that are consistent with the attached-eddy hypothesis, we have derived the correlations of some other quantities. That is, if the velocity field is Gaussian, the correlation functions of the kinetic energies , , and and that of the momentum transfer rate are given in equations (21) and (22). If the energy dissipation rate of an attached eddy is proportional to , the correlation function of the entire rate is given in equation (27). The results are summarized in table 2.
The logarithmic law such as that in equation (1) has been found also for the variance of the pressure fluctuations ([Jiménez & Hoyas 2008, Sillero et al. 2013]). If this law is due to the attached eddies, the two-point correlation \langle p(\mbox{\boldmathx}+\mbox{\boldmathr}_{l})p(\mbox{\boldmathx})\rangle is expected to have a functional form that is identical to those of the wall-parallel velocities and given in equations (10) and (15).
Lastly, we note that these results would allow us to use the attached-eddy hypothesis in its most general form. An example is the coarse-graining to characterize or model the wall turbulence, say, the atmospheric boundary layer in a particular class of numerical simulations ([Wyngaard 2004]). Over a streamwise length , we coarse-grain a quantity as
[TABLE]
Through a relation (e.g., [Monin & Yaglom 1971]), the variance of is dependent on the two-point correlation of ,
[TABLE]
and hence
[TABLE]
If the two-point correlation is a function of alone as for , , and in tables 1 and 2, the variance is a function of alone. The remaining variances depend also on . Such a constraint would in turn constrain the theory or model on that coarse-graining. Thus, for this and other various studies of wall turbulence, useful would be the general forms of the correlation functions derived here from the minimum assumptions of the attached-eddy hypothesis.
Acknowledgments
This work was supported in part by KAKENHI Grant No. 25340018. The author is grateful to anonymous referees for stimulating comments.
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