Characterization of Turbulence in Closed Flow

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alternate ways of defining an internal turbulent. Reynolds number, at least in the case of a closed flow. Among possible non-local, non-intrusive measurements.
J.

Phys.

II

FYance

7

(1997)

Characterization

#cole

J.-F.

Lyon (**),

de

1996,

November

29

revised

Hydrodynamic Turbulent

flows,

PACS.47.32.-y

Rotational

flow

Abstract.

characterize

to on

fluid. of

the

driving

the

We

the

numbers.

then

show

velocity

rms

We

of

state

torque

and

that

Lyon,

June

1997.

France

accepted

and

convection

flow

July 1997)

16

heat

transfer

vorticity

and

the

fluctuations

flow

closed

show

in

that

flow

the

and

that

reveals

it

Finally, we show that the transition once the calculation of fundamental global quantities allows the same the velocity fluctuations, the effective integral length as rms and Kolmogorov's dissipation length ~. That these quantities devices removed from the bulk of the flow is of importance complex geometries and for using corrosive fluids. the

Flow

Chillit

69364

J6

1729

between coaxial rotating disks, at moderate contra global ii. e. spatially averaged) quantities can be used the flow and its degree of turbulence. We first report measurements show how it depends on the is imparted to the momentum manner boundary provide a good estimate at the flow measurements pressure

investigate

We

high Reynolds

Closed

a

PAGE

stability

PACS.47.20.~k

PACS.47.27.-I

to

in

(*) and F.

Pinton

Sup6rieure

Normale

(Received

Turbulence

of

Mordant,

N.

NOVEMBER1997,

1729-1742

volume.

the

has

transition

to

occurred,

the

turbulence

for

characteristics

L*, Taylor's

scale may

turbulence

be

study of fluid

the

of

such

microscale

from

obtained

in

knowledge

A

measuring motion

in

Introduction

1.

turbulence The properties of flows at high Reynolds numbers are usually described experimentally in terms of the scaling properties of the local velocity field, as measured by a small probe documented and has produced placed inside the flow [1-3]. This technique is widely most of turbulent flows. Unfortunately the method is complex, local the existing experimental data on and intrusive; in addition, depending on the flow conditions, it is not always possible to use an probe m situ. Simple examples are flows in which the temperature is very high or anemometer liquids, flows in liquid metals [4], etc. The question then arises corrosive not uniform, flows in of

the

experimental

measureInents.

the

intensity of the

of

characterization

The

problem

is to

turbulence.

always

if

turbulent

a

determine

present.

We

flow

whether note

in

the

that

the

flow is

the

absence

turbulent

knowledge

local

of

and

of the

to

anemometry characterize

integral Reynolds by the values of

here integral determined that it is means diameter experiment (for example, the flow rate and tube in determined flow characteristics if one Turbulent compute an may only be can a pipe flow). internal Reynolds number~ I.e. based on internal flow parameters only. This is the turbulent number

external

is

not

parameters

sufficient

fixed

in

(*) Author for correspondence (**) CNRS URA 1325

@

Les

(ditions

de

Physique

the

(e~mail:

1997

pintonl3physique.ens-lyon.fr)

When

case

local

anemometry

velocity fluctuations rms global measurements to

defining

of

Among

global

are

turbulent

non-intrusive

measurements,

acoustic ary; measurements

by

which

the

where

quantity

V

volume is

average function

an

(fast-varying) g(t) j dg

in

let

f(Re)

r~J

In the

an

of

the

is

of

case

limit

known

in

the

disk

of

radius

a

on

way that the

fact

of

is

the

to

value

Dimensional

is

recovered

integral Reynolds dependent and

the

expressed

internal

quantities

describe

present

surements

in

be

into

section

next

results

our

can

inserted

the

on

3.I; for the

fluid.

number

combined

to

in

as

fl) thus

terms

of

can

be

of the

flow;

our

experimental

e.g.

the

transition

propose

of

f

to

the

that

[5]. We

the

the flow

internal

more

a

from

come

whereas

expected

energetic meaningful

f u)~~. e. g. global that do measurements not urm~[bulk] prm~[at wall].

only;

variables

r~J

r~J

techniques.

measurement

show

and

turbulence

in

velocity

rms

expression

an

related

boundaries

to

le. g.

parameters

that

f depends

that

stress

behavior

and

set-up

observed

been

just

we

measurements,

pressure

proceed with the deduction of internal flow dissipation, Taylor microscale, etc.) and we

via

has

r~J

in

flow

internal

accessed

bulk

characterize

its

be

can

and

via

=

slightly) rugose disks f(Re) Re° behavior.

simply

not

are

motion

It

moment

R~fl Iv. The the experiwith

Re also

varies

a

differences

The

the

torque

observes

rather

one

bulk.

the

in

when T is

point is that such require a probe to be

a

fluctuations

and

j,

thus

j2)

number

the

into

velocity

flow

the

Our

then

of

Section

in

injected

is

energy

related

behavior

We

point

this

to

global

a

high Reynolds numbers. For speed fl angular at constant analysis shows that the mean

very

rotating

R

v.

externally fixed parameters (such (such as urm~). The fluid is set into

variables cost

detail

in

return

the

such

,

Reynolds

itself

is

that

stress

pR5n2fjRe)

smooth, highly polished disks,

of

case

will

function

unknown

f

These

of the flow; it is

surface the condition of the disk. Indeed it geometry, e-gconst., in the limit of very high Reynolds number for (even so

ment's

f(Re)

is

form

We

mean

=

functional

of it.

realization

characteristics

f where

bound-

etc.

11)

large part

a

density p and kinematic viscosity required to drive the disks is given by:

torque

flow

driving mechanism, the ~'spatially averaged" mean

studied.

be

consider

us

the

at

pressure

are:

ways

flow.

closed

a

of

use

alternate

propose

of

case

the

flow

instantaneous

of

fluid

a

we

we

in the

justify

gix,t)d~x,

or

the

whose

time

scaling of j

the

cases

some

example,

of

and

using the

defined

is

=

flow

entire

space

over

of

must

=

In

the

covers

number

article~

this

least

at

of

we

/

gin)

In

measurements

term

N°11

fluctuations

consumption

power

ones,

A.

Reynolds number,

turbulent

non-local,

possible

microscale

the

II

Reynolds

turbulent

a

the

characterize

internal

an

available; Taylor

is

and

PHYSIQUE

DE

JOURNAL

1730

how

the

the

flow.

mea-

We

fluctuations,

for the

We

two

then energy

Reynolds

turbulent

number.

2.

2.I.

Experimental FLow

between

walls different

two

Set-Up

GEOMETRY. coaxial

surround

fluids,

We

use

counter~rotating

the

flow

volume.

air

and

water.

The

the disks

von

of

K6rm6n radius

experimental

R,

a

swirling

flow [6]

variable

distance

set-up is

sketched

in

produced H

apart.

Figure

I.

in

the

gap

Cylindrical We

use

two

CHARACTERIZATION

N°11

OF

TURBULENCE

CLOSED

IN A

FLOW

1731

MOTOR

H

PRESSURE TRANSDUCER

Q2 MOTOR

Fig. I. rotating wall, is

of the experimental set-up in water. equal frequencies. H 20 cm, R 9 cm. located in the mid plane between the disks.

Sketch

at

the

In

.

=

10

=

perpendicular

order

in

of air, R

case

blades, motors,

to

increase

the

rotation

the

In

used

in

order

torque

with smooth

disks

The

controlled

rotation

water

are

or

has

rugosity is

larger a

measured

The

disks

disks

disks

fitted

are

height hb

with are

of

radius of

cm

2

"

by

driven

=

9

=

flR~ Iv

cm,

and

thus is

H

in the

range

set

a

and 45 Hz

450

and

the

to

of 8

vertical

thickness

independent cm

counter-

flush

0.5

cm,

DC

watt

controlled

diameter.

in

The

10~.

=

and increase

0

20

two

40 Hz.

apart,

cm

are

enclosed

in

cm

in

Parvex-Alsthom The

Reynolds

RS420 numbers

motors

achieved

10~.

Experiments are performed with disks whose surface Calibrated waterproof sandpaper is used and rugosity. independently with an optical profilometer Iii. than

a

height. Light disks are cut-off of the the high frequency with a regulated constant water

19.8

maintained

independently by

rotated

with

cm

disks

the

mounted

=

diameter

temperature

frequencies

Re

R

inner

effects

inertia

are

about

by

motion

adjustable from 0 to are enclosed in a cylinder 23.2

are

thus

are

The

measurements.

circulation. at

reduce

to

the

and

cm

surfaces,

into

transducer,

pressure

frequencies of which

of water, disks container, 19.3

case

cylindrical

40

=

disks

entrainment.

by a feed-back loop. The largest Reynolds numbers

.

H

cm,

flow is set

The

=

the

to

The

controlled

is its

emphasize that in both cases, the forcing of the flow is such that the rotation rate of is kept through feed-back that other such loop. This quantities constant a means the by applied the disks fluctuating An the quantities in input time. torque as or energy are experimental study of these fluctuations has recently been done [8]. We

disks

the

2. 2. on

a

MEASUREMENT National

anti-aliasing

TECHNIQUES.

Instruments filters.

NBA2150F

In

each

16-bits

case

the

digitizing

transducers signal from the are card which incorporates the

recorded necessary

PHYSIQUE

DE

JOURNAL

1732

II

N°11

(local) are performed in air using a TSI Velocity subminiature hot-film measurements probe with a sensing element 10 ~m thick and I mm long. Velocities deduced from are voltage the validity using the usual King's law fi a)16, of which measurements (e~ has been checked, and the coefficients a and b obtained from in a calibrated measurements wind tunnel. The position of the probe is adjustable. We have checked that the presence of the probe does not affect the flow by performing identical measurements measurements with the probe support different angles. inclined at

.

=

Pressure PCBHl12A21 piezoelectric transin water done with a 5 mm measurements are ducer, mounted flush with the lateral wall, in the mid-plane the disks. It is between acceleration-compensated and has a low frequency cut-off at -3 dB equal to 50 mHz; its

.

is I

rise-time

flush

mounted

Torque

.

the

EG&G

3.

performed driving

amplifier

read

to

and

its

rise-time

also mm,

is 25 ~s.

experimental apparatus using liquids. One of (strain by a calibrated Lebow torque sensor Signal-to-noise ratio is improved by the use of an gage bridge output. in the

Inotor

1102-3.53Nm).

Model

lock-in

Hz

0.05

is

the

to

piezoelectric PCB103A02, transducer mide-plane. Its active diameter is 2.I

a

and in the

wall

-5%

at

are

connected

is

shaft,

gage

cut-off

by

measured

are

lateral

measurements

disks

air

in

the

with

frequency

low

its

ms.

fluctuations

Pressure

the

Results

We

first

with

the

at

report

which

to

recast

turbulence

to

TORQUE

3.I.

the

sure

The

torque applied of

case

blades,

disk

a

is

and

a

of the

flow.

PRESSURE

AND

driving torque the

is

boundary

flow

they permit transition

the driving torque and show how it depends on the on manner imparted to the fluid. We then show that measurements pressure provide a good estimate of the rms velocity fluctuations in the flow and the torque data the In particular it reveals onto a very simple form.

measurements

moInentuln

on

one

fitted

MEASUREMENTS: of the

blades

with

just equal to very simple

disks

what

of

needed

is

referring

that

the

authors The

thickness

sion

depends that

cannot

In

fluid is

done

the

tribution

in

be

disks

is

on

whether

flow is

the

equation (2) f(Re) observed

turbulent law

in

our

lit&. ~w

experiment

regime Schlichting's

yields

a

boundary layer

or

thickness

c~

The as

turbulent. has

been rotation

using e

fl~.

This

is

~w

the

fluid is

of the

entrainment

the

argument

f

and

at

case

This

where

the

between

in

also

the

when

case

rugosity hb is larger than the boundary high rotation rates as observed by many

whose

decreases

which

laminar

situation,

of fluid

slices

mea-

rates.

'

dependent.

viscosity

boundary layer,

-of the

e

T

the

subtle:

more

layers and is thus

We

equal

at

hb

const.

~w

disks

uia

VARIABLES.

the

motion

into

set

~2~2

~

equation (2), f(Re)

to

smooth

of

case

boundary

the

so

"

the

is

FLow

opposite directions simplest one: in that

in

rotate

to:

sublayer. This is eventually always the [5,9j and again in Figure 2 (asterisks).

viscous

disks

back of the

entrainment

to

leads

calculation

y so

INTERNAL

they height hb

when

skin

Re

increases;

In the

verified rate

in

addition

laminar

regime

(see [10j

of the

empirical

(v/fl)~/~;

through

done

pv(0vjj /0z)

friction

this

for

a

its e

the

involves expres-

/fl

~w

review),

but

disks is always to high.

(-th-power velocity gives f(Re)

c~

dis-

Re~~/~

CHARACTERIZATION

N°11

OF

IN A

TURBULENCE

CLOSED

o.7

(~

FLOW

1733

(a)

o,

QJ

ii~

§ c

~i

~

5

0

10

Rotation

Qi

slope

[Hz]

Q2

io

°

lo

=

35

30

25

20

15

frequency

(~)

2.01

£ E

j~_

~o

.

~ ~

~

.

~

~~-

)

-2

lo

o ~

>

io°

lo'

Fig. of

Torque

2.

smooth

Our

(o)

in

measurement

and

(*, b

rugose

measurements

=

~ with

a

We

1.82.

~w

in

note

We

rotation

not

that

flow

the

disks, the

forcing

the

of the

measurements

on

geometry flow that

in

many

result;

Figure

see

p/fl2

~'~'

~~~

~

2

(circles)

the

gap

between

of the

probe the

the

geometrical container, etc.

bulk

but

the

of the

we

observe:

~~.

observed scalings are in boundary layers are always turbulent.

(power input),

where

'

the

other

case

~

asymptotic

these

rates:

Linear

that

that so

flow

rotation varying equal and opposite coordinates. and 16) logarithmic

with

(a)

this

Re~°

f(Re)

find

2

rates

depends

the

with

~~

~

disks

disks.

~w

Figure

explored Inean

thus

for

water

37 ~Jm)

agreement

in

are

Qi

equency

otation

state

flow.

disks

is

itself

characteristics, The

of the

torque fluid

turbulent. such

as

gives only motion

can

the

entire

This

Indeed

the

in

the

separation

some

only

range state

of

between

indication

be

of does

turn

obtained

on

the

from

JOURNAL

1734

PHYSIQUE

DE

N°11

II

(a) w

~~

~

o

o

Cid

~

-

o

oo

w o

~

£

~

~

o~

~

o~

w~ ~o

~°oooo°°~~~ ~0

Qi

frequency

Rotafion

25

20

15

10

5

~o

o~



wwwwww~

o

o~

~

35

30

[Hz]

Q2

=

(b)

p

slope

2.06

~

~

P

»

/

w

»

g

, -

,

cz C~~

g

~*

fl

w

~ ~

~

slope 1.76

o

~

~W w »

o

o

~w ~

»

o o

~o w



» o

~

o

o

~

smooth

We

of the

variance

asymptotic

regime

Evolution

3.

the

In

water.

lo). (a)

disks

show

that

the

measurements

at

now

pressure

Linear

just

measurement;

recall

of prrrs

for

rw

intensity the

disks

rugose coordinates.

[Hz]

Q2

=

fluctuations

pressure

~~

(b) logarithmic

and

that

the

10~

Qi

frequency

Rotation

in

o

10'

10°

Fig.

o

the

in

(*,

b

=

fluctuations in the velocity wall, in the mid-plane- We equation for the pressure: of

lateral the

AP

~Pv'

~

ll~v)~l

"

~P~j)fl~

mid-plane, 37 ~Jm)

bulk

and

can

that

stress

flow

the

at

~~

prrrs

be

wall, for

~~

~w

obtained

this

is

a

uia

global

13) ,

j

is

a

Poisson

(see [11j Figure varied.

for 3

It is

the

one, an

shows

the

readily

of

term

source

extended

which

involves

the

velocity

level

prms

gradients

of

disks

rotation

the

flow

review).

evolution observed

of the

that,

fluctuation

pressure

contrary

to

torque

measurements,

as

the the

pressure

rate

fluctuations

is

CHARACTERIZATION

N°11

OF

TURBULENCE

CLOSED

IN A

1o°

FLOW

1735

(a)

io.'

-8

-6

2

0

-4

4

(p-P)/P,~ns 0

(b)

~

»

~i

o~

o°°~

»

o

~

~°o@~

o o

0.3

Ul

*

°°

°

.

~j

~

O

O

~z

~

nJ

~'

j~

o

,

w

-0.5

uJ

°o~

*

o

°~o

ww

o

*.

-0.6

o

w

».*

o

-0.8 ~

~

~~

-0.9 ~~

5

0

10

Fig.

Evolution

4.

water,

in

high

and with

disks

Qi

"

Ll2

35

[Hz]

fluctuations. Probability Density of the Measurement Function pressure mid-plane. (a) Comparison of low rotation 2 Hz) rate (dotted line, Q (solid line, ~ 34 Hz). (b) Comparison of the variation of the PDFS' skewness frequency; (o): smooth disks and (*); disks with b 37 ~Jm rugosity.

in

rate

rotation

change

30

25

20

of the

wall

rotation

the

display

the

at

15

frequency

Rotation

the

=

=

=

when going from slow to fast disk At low fl, prms rotation. remains asymptotically as level, while in the limit of large rotation rates it scales turbulent flow [12,13]. Note, that however again the scaling a power law, as expected in a once depends on the between entrainment mechanism, as illustrated by the difference of behavior at

an

smooth This pressure

a

almost

and

of

behavior

constant

rugose

change

of

fluctuations

disks. behavior

is

also

visible

on

at

low fl

(see Fig. 4a):

regime they display the well behavior in the PDFS shape remains rates, the skewness regime. We note that the

known may

about transition

be

seems

tails

by

while

constant to

be

PDFS

the

exponential measured

Density Functions (PDFS) of the Gaussian, while in the turbulent are towards low values [14]. This change of skewness (see Fig. 4b). At low rotation

Probability

the

its

it more

decreases

abrupt

almost when

linearly

rugose

disks

in are

the

turbulent

being

used.

PHYSIQUE

DE

JOURNAL

1736

N°11

II

~~ ~

~~ (

i ~

.35

-)------

1.3

15

25

20

Velocity

5.

tuations

the

at

m/s). (o):

in

height,

at

r

thus

We

prms

cm

observe

now

fluctuations,

urms,

regime, the simplest

turbulent

the

in

g(Re)

where

case

=

wall

a

g(Re)

~

pressure

fluc-

(both

scaled

velocity

recorded

the

at

same

cm.

the

as

of

transition

flow

the

of the

measurement

On

grounds, one Reynolds number.

the

of Re

cc,

~

that

so

pr~s

to

expects the

In

pu)~~.

c~

a

of

variance

dimensional

function const.

from

anemometry

calculated

and

disk

reveals

flow.

arbitrary

an

is

3

[Hz]

hotwire

meaningful

of the

bulk

is

flow

yields

prms

using

lower r

Q2

=

50

45

blades)

with

the

and

cm

the

at

that

fitted

above

11

=

Qi

measurements

cm

h

pressure

show

pu)~~ g(Re)

=

the

the 5

=

(*):

(disks

air

to

h

at

axis.

the

that

We

state.

velocity

the

measured from

in

compared

wall

pressure

5

=

turbulent

fluctuations

rms

lateral

40

35

frequency

Rotation

Fig.

30

It

quasi-Gaussian approximation [15,16], so that the pressure case fluctuations mostly governed by the velocity fluctuations at the integral scale although the are involves the in velocity gradients. its equation term source We have directly tested the proportionality of u)~~ and prms in the experimental set-up in air, simultaneous where and velocity possible. Velocity measurements measurements pressure are made hotwire the flow. different radial and vertical within using positions anemometry, at are (0.22 + 0.03)udisk throughout the 2grRfl where udwk We obtain urms volume, measurement /p (0.32 0.02) when the is the disk rim velocity. On the other hand, we observe + udisk prms has

been

shown

the

to be

the

in

~

=

=

of

recorded

is

pressure

the

at

the

Altogether,

disks.

of the

wall

probe

anemometer

either

and

in the

of

the

of the

center

prms/p

gives

it

(1.45

=

measurement

transducers,

pressure

(see Fig. 5). torque scale (an approach

then

We

reconsider

velocity shown in Figure 6,

teristic as

in

our

where

we

for

fi

using

measurements

volume

already used in [17] ). have plotted f/Vprms us.

The

fi

all

disks

of the

frequencies

rotation

of

Rfl)

behavior

is

radically

the

one

locations

(instead V is

to

nearer

or

0.07)urms, independent

+

charac-

a

as

changed

volume

of

fluid

a

clear

motion). (I)

a

sharp

transition

transition

in

for

values

scaling

can

flow,

be

observed

which

at

becomes

a

critical

value

turbulent

when

p)~~, giving evidence the

velocity

fluctuations

for

exceed

threshold.

certain

(it)

the

of the

range

is

rotation

verified

rate as

soon

such as

that

the

prms

entire

>

flow

p)~~,

the

becomes

scales torque turbulent.

as

prms.

This

a

N°11

CHARACTERIZATION

TURBULENCE

OF

0.12

~

~

)~~ ~

$~'~

~~

CLOSED

~~~l ~ § ~

+~+

X~

IN A

~

~

~

~

~

~

FLOW

1737

*

~~

/#

.~

#

~'

t

0 08

4'

j

i

~

~j~

* w

$$t

# ~

~

+

i~

~

~~

~

#

~ +

~ +

~

#~ w +

#

~

+

~

~

~

~



sq"( Fig. flow,

6.

that

Note

all

threshold

the

for

two

to

access

forcing intensity) the

the

performed

measurements

to

torque,

rotation

power

input (P

the

quantities:

amplitude

of the

quantities

These

velocity allow

integral length scale length 1/.

the

motion:

dissipation

L*

of

shape,

internal

flow

in

the

of the 37

pm.

showing variables

(of

state

course

gives the

and

flow. and

rate

fl,

r

=

of the the

fluctuations

pressure

characteristic

prms/p,

calculation

(*)

pm,

experiment)

fluctuations

the

same

of

a

the

on

23.7

turbulent

of the

the

fluid).

Kolmogorov

geometry

the

term

flow

(#)

pm,

on

in

The

turbulent

of the

scales

global

11.3

recast

of the

the

on

(x)

disks) collapse

transition

depends

pm,

intensity of velocity fluctuations by Vprrrs, where V is the volume

CHARACTERISTICS. and

of the

response

the

8.6

when

torque

of the it

(+)

rugose

or

driving

with

adimensionalized

fundamental

TURBULENCE

3.2.

give

and

universal,

not

scaling

appropriate

smooth

of the

Pr~nS

disk

one

on

is

rugosities:

disks

determination

a

is

torque

(with

behavior

allows

it

The

various

curves

simple

very

alone;

for

applied

torque

the

fi.

by

Measurements

fluid.

the

of

Variation

measured

as

30

25

20

15

of the

characteristic

characteristic

flow, Taylor

of

length

microscale

I

Integral Scale L*. In most experiments L* is identified with a charactersitic scale L experimental set-up (e.g. the grid mesh size in grid-turbulence). It is a fixed parameter, independent of the forcing of the flow, even though its physical meaning is to give the size of the studies which containing eddies. Its evaluation is made more precise in numerical energy define it through the velocity power spectrum: 3.2.1.

of the

f kE(k)dk fE(k)dk

2gr

fi We the

to

propose energy

change of

keep

input the

into

kinetic

the

spirit of this the

definition

Equating

flow.

of

energy

~

structures

)

and

the

power

of size

L*,

~w

~

L* ~w

calculate

L*

consumption one

~~

~

P

to

as

a

of the

characteristic

size of

flow

rate

to

the

of

obtains:

_j f P

3/2

(4)

PHYSIQUE

DE

JOURNAL

1738

N°11

II

0.2 0.18

~ -

0.1

~

0

Fig. 7. consumption

The

correspond calculate

to

Taylor

3.2.2.

Its

flow

This

rates

constant

to

to

that

2

cm

the

energy

It

decreases

at the

transition

7.

We

note

that

disks

and

that

it

This

confirms

value.

set-up.

from

Figure

in

about

of the

diameter

length

inner

R~ which arrangement.

the

in

the

does

not

need

the

to

is

scale

obtained

it

filaments

local

from

j

hotwire

)

maximum

turbulent

the

addition,

In

of enstrophy. Together with urms it motion. intensity of the turbulence, independently has been proposed [17,18] that I is the observed in swirling flows. Traditionally, of the

characteristic

of the

characterizes

vorticity

of the

scale

scale

the

is

number

experimental length characteristic microscale the Taylor

of

I.

gives the

Renolds

a

calculated

displayed

is

experimental

the

in

scale L*, boundary.

rotation

the

than

[Hz]

Q2

"

40

35

measurements.

Microscale

measurement

yields

length

particular

any

smaller

times

at low

remains

it

the

at

frequency

rotation

(20 cm)

threshold,

the

length

fluctuations

disks

the

Integral

disks.

pressure

of the fluid

L* is 10

from

it

smooth the

with

Above

regime

turbulent

and

height

the

from

turbulence.

to

flow

of L*

variation

rapidly

with

Measurement

of the

Lli

frequency

Rotation

30

25

20

15

10

5

using:

anemometry,

(VU)~,

~

lL~~~

computation, the Taylor hypothesis is used to spatial velocity profile [19-21]. We propose of I, but to the velocity gradients from the dissipation, estimate input and the viscous dissipation rate: power and

a

in

the

fixed

present

location

to

the

P

pV The from the are

numerical

values

corresponding comparable to R~

@ ~w

Figure

scattering

ultrasound

behavior

see

~jp~~2

turbulent the is

one

~'~'

~

8a

are

measurements

Reynolds measured

observed

in

the

'~)mS

~2

fl/pV

~

~

close to the

one

turbulent

anemometry

regime.

equating

above

the

time

averaged

j~~

obtained

one

in

[17].

size

and

at

definition

Prms

directly

=

local

measurements

the

retain

fl/V

~

of the filaments core number R~ urmsl/v;

from

time

relate to

observes that

the

similar

conditions

Figure 8b that usual

the

shows values

asymptotic

CHARACTERIZATION

N°11

OF

TURBULENCE

IN A

CLOSED

FLOW

1739

5

i

15

10

Qi

Q2

=

35

30

25

20

frequency

Rotation

[Hz] (b)

12

o

~y~ ~

~

~

Ct~

o

o

i

a~

o

ooooooooooooooo°°

°o~ oo

~5

15

10

Fig.

Measurements

8.

velocity

fluctuations

Reynolds

number

R>

smooth

Iv

itrrrsl

=

/$,

cc

of the

the

smallest

transfer

possible

consumption

power

Length

kinetic

of the

structures

of the

the

Calculation

the

variations

3.2.4.

one

of q with the recovers

Comparison

with

of the

Taylor

microscale

from

the

Taylor-based

flow.

This

of the

in

energy the flow.

scale is

characteristic

turbulent

In

the

number

Re =

rms

turbulent

R~~ Iv.

In

motion

regime

turbulent

of the heat.

to

it is

It

friction,

viscous

gives the

estimated

of

size

from

the

flow:

~3 /PV~

The

lHz]

lb) Evolution of the integral (experimental) Reynolds in

1/.

~

regime,

Q2

expected.

as

Kolmogorov Dissipation

3.2.3. I.e.

with

la)

disks.

dissipation

energy

regime R>

turbulent

the

with

and

Dim

35

30

25

20

frequency

Rotation

the usual Hot-

disks

~~~

~

rotation

relationship Wire

1/4

frequency

)

~w

Measurements.

shown

are

Re~@, To

as

in

observed

establish

Figure 9a. In the in Figure 9b.

further

global

the

calculation

turbulent

of tur-

compared the results we with traditional hot-wire the fluid. anemometry, in the working The dissias (0u/0z)~ pation is estimated from the local velocity C~v where u measurements < >, as EL is the local flow velocity and a localized Taylor hypothesis [21] is used to relate temporal and bulence

small

scales

characteristics

from

have

measurements, setup using air

~w

JOURNAL

1740

PHYSIQUE

DE

N°11

II

40

(a)

~

35

G

o

30 a -

~i

~

~

o

25

o

~

o

o

~

°°o

20

°o~

o

~ooo

o~

15

o~~

~~5

frequency

Rotation

30

25

20

15

IO

Qi

Ooo

35

Q2

"

lHz]

~

o(b) o°

5

2 rn~

°

oo

o

4

go

oo°

~o°

coo°

o

a

il~

~

'~

i~

XXXXXXXXXXrXX

°

~

OXX OX

~

~X

~/

o~ X

R w

10

5

Fig.

Measurement

9.

input

energy

in

the

with

(experimental) Reynolds spatial

derivatives.

sured

dissipation Kolmogorov's

The

The

Re

constant

of the

center

near

number

is also

=

Ce

calculated

with

the

considered

is

disks,

the

from

the

Q2

"

motors

regime

equal

be

to

1/

15

to

as

function

from

of the

the

integral

L*Re~~/~

cc

velocity u is meabe homogeneous.

the

since

consumption

power

calculated

~,

a

expected

flow is

the

length

L*,

scale

turbulent

where

[Hz]

dissipation

integral length

R~~ Iv. In the

between

gap

(a) Kolmogorov

disks.

smooth

(b) Scaling of1/

flow.

Qi

35

30

25

20

15

frequency

Rotation

to

eG

as

"

(Pm~~hanicai) /M.

dissipation scale is then calculated as 1/G,L (v~ leG,L)~@ for several values of frequencies. The results, displayed in Figure 10, show that both methods yield the disk rotation LRe~~@ the correct order of magnitude for 1/. However, the Reynolds number dependence1/ It shows that it is very difficult to obtain a good is only observed for the global measurements. level is fluctuation of EL using local velocimetry in closed flows where the velocity estimate of EL, such for the calculation other alternatives very high (about 35% here). We have tried Karman-Howarth relationship, again the order of magnitude is correct, but not using the as of the Taylor microscale dependence. It also affects the the Reynolds number measurements ~

~w

I

when same

as

it is

estimated

when

derived

expected We the

I

~w

thus turbulence

the

from

from

the

velocity

local

mechanical

Re~~/~ scaling. observe small

that scale

the

global

measurements

characteristics

in

a

the

measurements:

power

input

in the

yield

closed

flow.

a

flow,

correct

order but

and

of

it

magnitude

does

coherent

not

is

exhibit estimation

the

the of

CHARACTERIZATION

N°11

x

OF

TURBULENCE

CLOSED

IN A

10~~

FLOW

1741

~

9

8 ~.73

S

7 ~'~

~'~

~'~

~ -

~

f

5

~ ~

4

~

~ '

T

3 15

10.

Calculation

(o),

fluctuations The

inset

and

data

the

shows

Kolmogorov

of

from

local

dissipation

hotwire

Qi

from

(*)

50

45

[Hz]

Q2

"

length,

measurements

logarithmic

in

~

40

35

frequency

Rotation Fig.

30

25

20

~

consumption position h 11

power

probe

=

and cm,

pressure r

=

3

cm.

coordinates.

Conclusion

4.

behavior of a closed flow investigate the dynamical using global ii. e. spatially averaged) measurements only. These sophisticated simple that probes be and do require measurements not are very introduced bulk of the flow. physical quantities such as the The scaling of relevant in the applied torque or power consumption in terms of internal flow variables (e.g. urms) reveals the turbulent transition regime. It does so much more clearly than the corresponding to the rate). Furthermore, variations with the experimental control rotation parameters (e.g. disks the has occurred, the turbulence be characterized with the knowledge of transition once can of the global Indeed, the and of quantities. the input measurements same pressure power We

have

at

moderate

shown

fluctuations the

as

of

measuring motion

in

wall

it is

possible

sizes

the

in

removed

complex

or

flow,

from

geometries

calculate

to

the of

intensity of the

overall

devices

sufficient

are

to

numbers

fluctuations

motion

the

measures

the

at

velocity

rms

interval

that

here

high Reynolds

to

the

turbulence

fundamental

typical length L* IA yields an

L*, I and

scales estimate

of the

characteristics

1/. inertial

obtained

study of fluid

range,

turbulence.

That

these

quantities

may

be

bulk

flow is of

importance

for

the

of the

and/or using

such

[L*,1/] is the

Then

while

Rj from

fluids.

corrosive

Acknowledgments We

acknowledge

helpful

assisted

The

experimental

set-up

could

expertise of Marc

Moulin

and

us

in

the

discussions

who

measurement not

Franck

Stephan

with

of the have

sand

been

Vittoz.

Many thanks to Sergio Ciliberto rugosity with his optical profilometer.

Fauve. paper

modified

so

many

times

without

the

(patient)

JOURNAL

1742

DE

PHYSIQUE

N°11

II

References

[3]

Lumley J-L-, A Nelkin M., Adu. Phys. 43 (1994) (Cambridge Turbulence Frish U.,

[4]

Magnetohydrodynamics

[1]

[2]

Tennekes

[6] [7] [8] [9]

[10] [11] [12] [13] [14] [15] [16] [17] [18] [19] [20] [21]

and

flows

are

first

course

in

turbulence

(The

MIT

Press, 1971).

143-181. U. of

Press.

1995).

importance

in

a

wide

range

of

ranging from areas, understanding of the

cooling circuits study of heat transfers in nuclear reactors dynamo effect that generates the magnetic field of planets. Nagata S., Mixing, chap-I, (J. Wiley & Sons, 1975). so-called swirling flows", see for instance, Zandbergen these "von Karman For reviews on Ann. Mech. and Dijkstra D., Reu. Fluid P-J19 (1987) 465-491. Commitn. Arecchi F-T-, Bertani D. and Ciliberto S., Opt. 31 (1979) 263. LabbA R., Pinton J.-F. and Fauve S., J. Phys II France 6 (1996) 1099-1100. J.-F. and Fauve S., Phys. Flitids 8 (1996) 914-922. LabbA R., Pinton Schlichting H., Boundary-layer theory (McGraw-Hill, 1979). J.-F., to appear in Non Linear Pinton Dernoncourt B.. LabbA R. and Fauve S., Abry P., Science Today, Beheringer, Ed. (Springer-Verlag, 1996). Abry P., Fauve S., Flandrin P. and Laroche C., J. Phys. II France 4 (1994) 725-733. Cadot O., Douady S. and Couder Y., Phys. Flitids 7 (1995) 630-646. Fauve S., Laroche C. and Castaing B., J. Phys. II France 3 (1993) 271-278. Batchelor G-K-, Proc. Cambridge Phil. Soc. 47 (1951) 359-374. George W-K-, Beuther P-D- and Arndt R-E-A-, J. Flitid Mech. 148 (1984) 155-191. Dernoncourt B., Pinton J.-F. and Fauve S., submitted to Physica D. Conference, Turbulence Hernandez R. and Baudet C., in Proceedings of the Vth European Kluwer, (1996). Taylor G-I-, Proc. Roy. Soc. A. 164 (1928) 476. Fisher M-J- and Davies P-O-A-L-, J. Flitid Mech. 18 (1964) 97-116. Pinton J-F- and LabbA, R., J. Phys. II France 4 (1994) 1461-1468.

the

[5]

H.

to the