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HAL Id: jpa-00248029

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Anomalous scaling of velocity structure functions in turbulence: a new approach

G. Ruiz Chavarría

To cite this version:

G. Ruiz Chavarría. Anomalous scaling of velocity structure functions in turbulence: a new ap- proach. Journal de Physique II, EDP Sciences, 1994, 4 (7), pp.1083-1088. �10.1051/jp2:1994186�.

�jpa-00248029�

(2)

J.

Pliys.

II FYance 4

(1994)

1083-1088 JULY

1994,

PAGE1083

Classification

Physics

Abstracts 47.25

Short Communication

Anomalous scaling of velocity structure functions in turbulence:

a new

approach

G. Ruiz Chavarria

(*)

Laboratoire de

Physique (**),

Ecole Normale

Supdrieure

de

Lyon,

46 Allde d'Italie, 69364

Lyon,

France

(Received

13

April

1994,

accepted

in final form 24

May 1994)

Abstract In this letter we report

experimental

evidence about the

possibility

to derive the n-order structure function

(in fully developed turbulence)

in terms

oflocally averaged dissipation

rate cr and the third order structure function. The results

presented

here are a

generalization

of the 1962 Oboukhov

hypothesis

about the

scaling

in the inertial range. The results are in accor-

dance with the Extended Self

Similarity (ESS),

a concept

recently

introduced in the literature.

In fact we

reproduce

the n-order structure function not

only

in the

region

where ESS is valid but in a much broader range.

The statistical behaviour of three-dimensional

fully developed

turbulence at small scales has been

intensively investigated

in the last five decades. A common way to board this

problem

is

through

the

velocity

structure functions. The nth order structure function is defined as:

<

bu(r)"

> = <

(u(x

+

r) viz))"

>

where u is the

component

of the

velocity along

the direction of r and < > stands for a statistical average.

Kolmogorov's original theory iii predicts

that at very

large Reynolds

num-

bers the

scaling

<

bu(r)"

> m

~"/3

holds for

r in the inertial range

(q

< r <

L,

where q =

(v3/

< c

>)~H

is the

dissipative

scale and L is the

integral scale). Many experimental

and theoretical studies do not

support

the

Kolmogorov theory [2, 3],

and the deviations are

usually

related to

intermittency

in the energy

dissipation.

In 1962 Oboukhov and

Kolmogorov [4,

5]

proposed

an inertial range

scaling

of the n-order structure function which includes the

intermittency

in the energy

dissipation

rate:

<

bu(r)"

>

mJ <

cf/~

>

r"/~ (l)

(*)

On leave from:

Departamento

de

Fisica,

Facultad de

Ciencias,

UNAM, Ciudad

Universitaria,

04510 Mdxico D-F-, Mexico.

(**)

CNRS. URA 1325.

(3)

1084 JOURNAL DE

PHYSIQUE

II N°7

where cr is the average of the energy

dissipation

rate c over a volume of linear dimension r and s =

lsv(8u/8x)~

for

homogeneous

and

isotropic

turbulence.

Equation (I)

also

implies

a

power law behaviour of <

cll~

> in the inertial range.

In this work a new

scaling

which extends

beyond

the inertial range is shown. This is the basis to

reproduce

an

arbitrary velocity

structure function for all scales in terms of <

cl/~

>

and a universal function

f:

~

n/3

<

bu(r)"

>

=

Cn

<

cf/~

> r

f n~~ (2)

where

Cn

and

f

are

dimensionless,

the latter

being

related to the third order structure function that is:

~

f ~))

"

<)>

~

~~i~~

~ ~~~

In order to define

f(r/~)

we have used <

(bu(r)(~

> rather than <

bu(r)3

> because the

computation

of the latter is much more

demanding,

but the two

quantities

exhibit a linear

dependence

in a broad range, as shown in reference [6]. The constant D was introduced to normalize this

function,

that

is, f

must go to I in the inertial range. On the other

hand,

the

continuity

in

velocity implies

<

(bu(r)(3

> m

r3

when

r lies in the

vicinity

of the

Kolmogorov

scale q, then

f

becomes

proportional

to

r~.

At first

sight

the

right

hand side of

equation (2) reproduces

the characteristics of a structure function in two

regions.

The first one is

the

dissipative

range where the power law behaviour is

completely

dominated

by

the term

(r fir In) )"/3,

the

quantity

<

sll~

>

going

to a constant value when small scales are considered.

The second one is the inertial range where the power law behaviour is

composed

of a

dependence

on

r"/3

and

a correction related to the energy

dissipation

rate. At intermediate scales the relation also holds as shown

by

the

experimental

data. It must be noticed that

equation (I)

is

a

particular

case of

equation (2).

In a

previous

letter

by

Benzi et al. [6] an extended self

scaling

is found when a structure function is

plotted

versus another one. The self

scaling

is observed on a broad

region

that

begins approximately

at

S~ [3, 6],

earlier than the appearance of any inertial range and at

Reynolds

numbers for which no

scaling

is

expected.

The anomalous

exponent ((n)

associated with the n-order structure function is calculated as a

slope

in a

log-log plot

of <

bu(r)"

>

versus <

(bu(~)(3

>. Now a self

scaling

broader than that observed in ESS is shown.

This letter is intended to discuss a transformation that allows two different

velocity

structure functions to be

together

and also the influence of the

intermittency

to be shown in all the

scales,

not

only

in the inertial range.

Table 1.

R

R, L(cm) ~(~m)

11000 170 10 440

300000 800 12.S 100

Sonde size : Diameter 25 pm.

Length

0.25 mm.

The

experimental set-up

consists of a wind tunnel with a cross section 50 x 50

cm~

and 3 m

long.

Turbulence was

generated by

a

cylinder

or a

jet,

the

integral

scales L were 10 and

(4)

N°7 SCALING OF STRUCTURE FUNCTIONS IN TURBULENCE 1085

12.5 cm

respectively.

The

Reynolds

numbers based on L were 11 000 for the

cylinder

and 300 000 for the

jet. Furthermore,

the

Reynolds

numbers based on the

Taylor

scale were 170 and 800

respectively (see

Tab.

I).

It is

interesting

to notice that the

only

case when a inertial

range was

clearly

detected

corresponds

to the measurements in the

jet (Re

= 300

coo),

as we

can see in

figure I,

where the structure function <

(bu(r)(3

> vs.

r/~

is

plotted

in

log-log

scale. The instantaneous

velocity

was measured with a hot wire whose dimensions are

given

in table I. The data were

digitalized

with a 16 bits

a/d

converter. The

probe

was

placed

at 25 times the

integral

scale downstream. In order to

compute

the structure functions and <

sll~

>

the

Taylor hypothesis

was

used, assuming

that the eddies are convected

by

the mean flow. In other words we

replace

r

by Ut,

where U is the mean

velocity,

and the derivative

8u/8x

is

~~P~~~~~

~Y

j I

40

20

~ O-O

j~

~i

~l

20 fi

~ A

a

40 ~

~ o o

~~l

-0 O-o 1.0 2 0 S-O 40

Log r/q

Fig.

1.

Log

< (bu~( > vs.

Log (r/~).

The data

concerning

two different

Reynolds

numbers are

plotted:

Re

= 11 000

(o)

and Re = 300 000

(/h). Only

in the latter case a inertial range is

clearly

detected.

In

isotropic

and

homogeneous

turbulence:

cr =

~~"

(8u/8x)~dz (4)

r

~

For

experimental

convenience we take a one-dimensional average rather than a three- dimensional one.

According

to other authors this

change

does not

produce

any modification in the results [7]. The evaluation of

c)/~

involves

a derivative and an

integral.

The derivative

was calculated

using

a difference schema with the two

neighbouring points

[8]:

~

~

~~~

~

~2h~~~

~~

~~~

(5)

lo86 JOURNAL DE

PHYSIQUE

II N°7

The function

~"

was

interpolated

with the

spline technique

and the

integration

was per- ax

formed

using

this

interpolation.

The number of data was

equal

to lo~ for the

cylinder

case, whereas in the

jet

2.S x

lo~

data

were recorded. With this amount of data it is

possible

to evaluate with statistical accuracy until the six order structure function. In

figure

2 the function

<

s)/~

> and <

s$/~

>

(normalized by

<

c"/3 >)

are

plotted

vs.

r/~

in

log-log

scale for the two

Reynolds

numbers considered here. The curves go to a constant value when r

- j

020

o 15

A o io

£~ v

I

o~

o 05

~ a

o.oo

o °

~~~l.0

O-O I-O 20 30 40

Log r/fl a)

O-O A n ~a~

o o °

~§~

0.2 %

A

~&t

V 0.4

I

01

06

08

~'~l.0 0 0 0

2.0 30 4.0

Log

r/~

b)

Fig.

2.

al

<

e)/~

>

vs.

r/~

and

b)

< e$~~ vs.

r/~,

Two

Reynolds

numbers are

considered,

Re = 11 000

(o)

and Re = 300 000

(/h). Generally speaking

<

el~~

> goes to

a constant value when

r - q, The functions < e~~~ > and < e~~~ > were normalized by <

e~/3

> and <

e~/3

>

respectively.

(6)

N°7 SCALING OF STRUCTURE FUNCTIONS IN TURBULENCE 1087

In

figure

3 the main result of this work is

shown, namely

a

log-log plot

of <

sll~

>

~

n/3

rf

vs. <

bu(r)"

> for n

= 2 and 6. In all cases the data are

closely

distributed

~~~

along

a

straight line,

even in the

vicinity

of the

Kolmogorov scale,

and the

slope

is

always

very

close

to I. This

implies

a direct

proportionality

between the two

quantities plotted

in the

graphs.

The

possibility

to write the n-order

velocity

structure function in terms of <

sll~

> and

2.0

o-o

£_

~

f

i~i~

01

~

~~60 Log

<bu~>

&)

(7)

1088 JOURNAL DE

PHYSIQUE

II N°7

f(r/~) gives

an

insight

in the anomalous

scaling. First,

the

exponent

of <

bu(~)"

> in the inertial range is

separated

in a

regular part, given by

the

Kolmogorov theory of1941,

and a

correction due to

intermittency

in s. A new result concerns the influence of

intermittency

at scales

lying

between the

dissipative

and the inertial ranges.

According

to

figure

2 the

influer~je

of <

s)/~

> increases when r decreases. But the same

applies

to the term

rf

~

~~~

~

Only

when r cs ~ the influence of the

intermittency

decreases and in the

dissipative

range the behaviour of the structure function is

completely

dominated

by

the

continuity

in

velocity.

In this letter we have shown a

generalization

of the Oboukhov

hypothesis

of 1962 that

applies

at all scales below the

integral

one and even when the

Reynolds

number is so low

that no inertial range is

clearly

detected. To do this a function

f(~/~),

not

depending

on the

intermittency,

was introduced. The

generalization

of the Oboukhov

hypothesis permits

us to

clarify

the role

played by

the energy

dissipation

at different scales as has been

pointed

out in

a

previous paragraph.

All that has been

pointed

here seems to indicate that the main features

concerning

the statistics of a turbulent flow are

already presents

at low

Reynolds

number and

over a broader range than the inertial one.

Acknowledgements.

The author thanks S.

Ciliberto,

R.

Benzi,

C.

Baudet,

J.F. Pinton and R. Labbe for their valuable comments.

References

iii Kolmogorov

A-N-, The local structure of turbulence in

incompressible

viscous fluid for very

large Reynolds

number, DokJ, Akad. Nauk. SSSR 30

(1941)

299.

[2] Kraichnan

R-H-,

On

Kolmogorov's

inertial range theories, J. Fluid Mech. 62

(1974)

305.

[3] Anselmet

F., Gagne

Y.,

Hopfinger

E-J- and Antonia R-A-,

High-order

structure functions in

turbulent shear flows, J. Fluid Mecli. 40

(1984)

63.

[4] Oboukhov

A-M-,

Some

specific

features of

atmospheric

turbulence, J. Fluid Mecli. 13

(1962)

77.

[5]

Kolmogorov A-N-,

A refinement of

previous hypothesis concerning

the local structure of turbu- lence in a viscous

incompressible

fluid at

high Reynolds number,

J. Fluid Mecli. 13

(1962)

82.

[6] Benzi R., Ciliberto S., Baudet C., Ruiz Chavarria G. and

Tripiccione R.,

Extended self similarity in the

dissipation

range of

fully developed

turbulence,

Europliys.

Lent. 24

(1993)

275.

[7] Thorodsen

S-T-,

Van Atta

C-W-, Experimental

evidence

supporting Kolmogorov's

refined simi-

larity

hypothesis, PJiys.

Fluids A 4

(1992)

2592.

[8] Kuznetzov

V-R-, Praskovsky

A-A-, SabeInikov V-A-, Fine-scale turbulence structure of intermit-

tent shear flows, J. Fluid Mecli. 243

(1992)

595.

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