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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�
J.
Pliys.
II FYance 4(1994)
1083-1088 JULY1994,
PAGE1083Classification
Physics
Abstracts 47.25Short Communication
Anomalous scaling of velocity structure functions in turbulence:
a new
approach
G. Ruiz Chavarria
(*)
Laboratoire de
Physique (**),
Ecole NormaleSupdrieure
deLyon,
46 Allde d'Italie, 69364Lyon,
France
(Received
13April
1994,accepted
in final form 24May 1994)
Abstract In this letter we report
experimental
evidence about thepossibility
to derive the n-order structure function(in fully developed turbulence)
in termsoflocally averaged dissipation
rate cr and the third order structure function. The results
presented
here are ageneralization
of the 1962 Oboukhovhypothesis
about thescaling
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 notonly
in theregion
where ESS is valid but in a much broader range.The statistical behaviour of three-dimensional
fully developed
turbulence at small scales has beenintensively investigated
in the last five decades. A common way to board thisproblem
isthrough
thevelocity
structure functions. The nth order structure function is defined as:<
bu(r)"
> = <(u(x
+r) viz))"
>where u is the
component
of thevelocity along
the direction of r and < > stands for a statistical average.Kolmogorov's original theory iii predicts
that at verylarge Reynolds
num-bers the
scaling
<bu(r)"
> m~"/3
holds forr in the inertial range
(q
< r <L,
where q =(v3/
< c>)~H
is thedissipative
scale and L is theintegral scale). Many experimental
and theoretical studies do notsupport
theKolmogorov theory [2, 3],
and the deviations areusually
related tointermittency
in the energydissipation.
In 1962 Oboukhov andKolmogorov [4,
5]proposed
an inertial rangescaling
of the n-order structure function which includes theintermittency
in the energydissipation
rate:<
bu(r)"
>mJ <
cf/~
>r"/~ (l)
(*)
On leave from:Departamento
deFisica,
Facultad deCiencias,
UNAM, CiudadUniversitaria,
04510 Mdxico D-F-, Mexico.
(**)
CNRS. URA 1325.1084 JOURNAL DE
PHYSIQUE
II N°7where cr is the average of the energy
dissipation
rate c over a volume of linear dimension r and s =lsv(8u/8x)~
forhomogeneous
andisotropic
turbulence.Equation (I)
alsoimplies
apower law behaviour of <
cll~
> in the inertial range.
In this work a new
scaling
which extendsbeyond
the inertial range is shown. This is the basis toreproduce
anarbitrary velocity
structure function for all scales in terms of <cl/~
>and a universal function
f:
~
n/3
<
bu(r)"
>=
Cn
<cf/~
> rf n~~ (2)
where
Cn
andf
aredimensionless,
the latterbeing
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 thecomputation
of the latter is much moredemanding,
but the twoquantities
exhibit a lineardependence
in a broad range, as shown in reference [6]. The constant D was introduced to normalize thisfunction,
thatis, f
must go to I in the inertial range. On the otherhand,
thecontinuity
invelocity implies
<(bu(r)(3
> mr3
whenr lies in the
vicinity
of theKolmogorov
scale q, then
f
becomesproportional
tor~.
At firstsight
theright
hand side ofequation (2) reproduces
the characteristics of a structure function in tworegions.
The first one isthe
dissipative
range where the power law behaviour iscompletely
dominatedby
the term(r fir In) )"/3,
thequantity
<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 adependence
on
r"/3
anda correction related to the energy
dissipation
rate. At intermediate scales the relation also holds as shownby
theexperimental
data. It must be noticed thatequation (I)
isa
particular
case ofequation (2).
In a
previous
letterby
Benzi et al. [6] an extended selfscaling
is found when a structure function isplotted
versus another one. The selfscaling
is observed on a broadregion
thatbegins approximately
atS~ [3, 6],
earlier than the appearance of any inertial range and atReynolds
numbers for which noscaling
isexpected.
The anomalousexponent ((n)
associated with the n-order structure function is calculated as aslope
in alog-log plot
of <bu(r)"
>versus <
(bu(~)(3
>. Now a selfscaling
broader than that observed in ESS is shown.This letter is intended to discuss a transformation that allows two different
velocity
structure functions to betogether
and also the influence of theintermittency
to be shown in all thescales,
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 50cm~
and 3 mlong.
Turbulence wasgenerated by
acylinder
or ajet,
theintegral
scales L were 10 andN°7 SCALING OF STRUCTURE FUNCTIONS IN TURBULENCE 1085
12.5 cm
respectively.
TheReynolds
numbers based on L were 11 000 for thecylinder
and 300 000 for thejet. Furthermore,
theReynolds
numbers based on theTaylor
scale were 170 and 800respectively (see
Tab.I).
It isinteresting
to notice that theonly
case when a inertialrange was
clearly
detectedcorresponds
to the measurements in thejet (Re
= 300
coo),
as wecan see in
figure I,
where the structure function <(bu(r)(3
> vs.r/~
isplotted
inlog-log
scale. The instantaneous
velocity
was measured with a hot wire whose dimensions aregiven
in table I. The data were
digitalized
with a 16 bitsa/d
converter. Theprobe
wasplaced
at 25 times theintegral
scale downstream. In order tocompute
the structure functions and <sll~
>
the
Taylor hypothesis
wasused, assuming
that the eddies are convectedby
the mean flow. In other words wereplace
rby Ut,
where U is the meanvelocity,
and the derivative8u/8x
is~~P~~~~~
~Yj 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 dataconcerning
two differentReynolds
numbers areplotted:
Re= 11 000
(o)
and Re = 300 000(/h). Only
in the latter case a inertial range isclearly
detected.
In
isotropic
andhomogeneous
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 thischange
does notproduce
any modification in the results [7]. The evaluation ofc)/~
involvesa derivative and an
integral.
The derivativewas calculated
using
a difference schema with the twoneighbouring points
[8]:~
~
~~~
~~2h~~~
~~~~~
lo86 JOURNAL DE
PHYSIQUE
II N°7The function
~"
was
interpolated
with thespline technique
and theintegration
was per- axformed
using
thisinterpolation.
The number of data wasequal
to lo~ for thecylinder
case, whereas in thejet
2.S xlo~
datawere recorded. With this amount of data it is
possible
to evaluate with statistical accuracy until the six order structure function. Infigure
2 the function<
s)/~
> and <s$/~
>(normalized by
<c"/3 >)
areplotted
vs.r/~
inlog-log
scale for the twoReynolds
numbers considered here. The curves go to a constant value when r- j
020
o 15
A o io
£~ v
I
o~o 05
~ a
o.oo
o °
~~~l.0
O-O I-O 20 30 40
Log r/fl a)
O-O A n ~a~
o o °
~§~
0.2 %
A
~&t
V 0.4
I
0106
08
~'~l.0 0 0 0
2.0 30 4.0
Log
r/~b)
Fig.
2.al
<e)/~
>vs.
r/~
andb)
< e$~~ vs.r/~,
TwoReynolds
numbers areconsidered,
Re = 11 000(o)
and Re = 300 000(/h). Generally speaking
<el~~
> goes toa constant value when
r - q, The functions < e~~~ > and < e~~~ > were normalized by <
e~/3
> and <e~/3
>respectively.
N°7 SCALING OF STRUCTURE FUNCTIONS IN TURBULENCE 1087
In
figure
3 the main result of this work isshown, namely
alog-log plot
of <sll~
>
~
n/3
rf
vs. <bu(r)"
> for n= 2 and 6. In all cases the data are
closely
distributed~~~
along
astraight line,
even in thevicinity
of theKolmogorov scale,
and theslope
isalways
very
close
to I. Thisimplies
a directproportionality
between the twoquantities plotted
in thegraphs.
The
possibility
to write the n-ordervelocity
structure function in terms of <sll~
> and2.0
o-o
£_
~
fi~i~
01
~
~~60 Log
<bu~>
&)
1088 JOURNAL DE
PHYSIQUE
II N°7f(r/~) gives
aninsight
in the anomalousscaling. First,
theexponent
of <bu(~)"
> in the inertial range isseparated
in aregular part, given by
theKolmogorov theory of1941,
and acorrection due to
intermittency
in s. A new result concerns the influence ofintermittency
at scaleslying
between thedissipative
and the inertial ranges.According
tofigure
2 theinfluer~je
of <
s)/~
> increases when r decreases. But the same
applies
to the termrf
~~~~
~Only
when r cs ~ the influence of theintermittency
decreases and in thedissipative
range the behaviour of the structure function iscompletely
dominatedby
thecontinuity
invelocity.
In this letter we have shown a
generalization
of the Oboukhovhypothesis
of 1962 thatapplies
at all scales below theintegral
one and even when theReynolds
number is so lowthat no inertial range is
clearly
detected. To do this a functionf(~/~),
notdepending
on theintermittency,
was introduced. Thegeneralization
of the Oboukhovhypothesis permits
us toclarify
the roleplayed by
the energydissipation
at different scales as has beenpointed
out ina
previous paragraph.
All that has beenpointed
here seems to indicate that the main featuresconcerning
the statistics of a turbulent flow arealready presents
at lowReynolds
number andover 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 inincompressible
viscous fluid for verylarge Reynolds
number, DokJ, Akad. Nauk. SSSR 30(1941)
299.[2] Kraichnan
R-H-,
OnKolmogorov'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 inturbulent shear flows, J. Fluid Mecli. 40
(1984)
63.[4] Oboukhov
A-M-,
Somespecific
features ofatmospheric
turbulence, J. Fluid Mecli. 13(1962)
77.[5]
Kolmogorov A-N-,
A refinement ofprevious hypothesis concerning
the local structure of turbu- lence in a viscousincompressible
fluid athigh 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 thedissipation
range offully developed
turbulence,Europliys.
Lent. 24(1993)
275.[7] Thorodsen
S-T-,
Van AttaC-W-, Experimental
evidencesupporting 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