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Small-Scale Anisotropy in High Reynolds Number Turbulence
-- Universality of the 2nd Kind --
Y. KanedaNagoya University
August 23rd, 2007, Summer School at Cargèse,Small-Scale Turbulence : Theory, Phenomenology and Applications
Turbulence = a system of huge degree of freedom
A paradigm of Studies of systems of huge degree of freedom
Thermodynamics and Statistical Mechanics for thermal equilibrium state
Analogy with Statistical Mechanics for Near Equilibrium System
I. Two kinds of universalitycharacterizing the macroscopic state of the equilibriumsystemnot only
a) Equilibrium state itself, like Boyle-Charles’ lawbut also
b) Response to disturbance
II . Thermal equilibrium state Universal equilibrium state at small scaleinfluence of external force, mean flow, etc. at small scale
may be regarded as disturbance.How dose the equilibrium state respond to the disturbance ?
Universality of the 2nd Kind
Equilibrium state
at thermal equilibrium state
disturbance
response
Universality in Response to disturbances, near equilibrium state
1905, Einstein, D=μkT,the first example of FD-elation Perrin’s experiment.
1928, Nyquist’s theorem on thermal noise:P(f)=4kT Re(Z(f))
1931, Onsager’s reciprocal theorem:
J = C X, C=TC
generalized flux, generalized force
J = CX
Generalized Flux vs. Generalized Force
e.g.Density Flux vs. Density gradient ; J = C grad ρ
Heat Flux vs. Temperature gradient ; J = C grad T
Electric Current vs. External electric field ; J = σ E = σ grad φ , (I=E/R, Ohm’s law)
---
Momentum Flux vs. Strain rate ;
coupling only between tensors of the same order.
(Newton’s law)
Thermal Equilibrium system
Linear response
Equilibrium state
Disturbance
Xgrad φgrad Tgrad c
Xgrad φgrad Tgrad c
F=CX (Hooke’s law)J = C’ grad φ= σE (Ohm’s law)J = C’’ grad T (Fourier’s law)J = C’’’ grad c (Fick’s law)
F=CX (Hooke’s law)J = C’ grad φ= σE (Ohm’s law)J = C’’ grad T (Fourier’s law)J = C’’’ grad c (Fick’s law)
History:Universality in Response
to disturbances, near equilibrium state
1905, Einstein, D=μkT,the first example of FD-elation Perrin’s experiment.
1928, Nyquist’s theorem on thermal noise:P(f)=4kT Re(Z(f))
1931, Onsager’s reciprocal theorem:J = C X, C=TC
generalized flux, generalized force
1950-60, Nakano, KuboLinear Response Theory
Equilibrium State of Turbulence
Equilibrium state
?
disturbance
response
Turbulence ?
DNS
Series1Series1 Series2Series2
Energy Spectrum a la Kolmogorov (K41)
From Kaneda &Ishihara (2006)
Equilibrium state
a la Kolmogorov K41
disturbance
response
Disturbance
1. Mean Shear2. Buoyancy by Stratification3. Magneto-Hydrodynamic Force
I. Mean Shear
See Ishihara et al. (2002)
Local co-ordinateNS-equation
Effect of mean shear
Turbulent Shear Flow
Local strain rate of mean flow
Effect of Mean FlowHomogenous Mean Shear Flow:
• in the inertial subrange of homogeneous turbulent shear flow;
i ij jU S x=
( ) ( ) ( )ij i jQ u u= −k k k = ?
Let δ(k) =τk/T, (where τk =1/(ε 1/3 k 2/3), T=1/S)
Assume (1) δ <<1, for large enough k(2) expand in powers of δ
k=1/l
Two kind of measures characterizing the universal equilibrium state
0( ) ( ) ( )ij ij ijQ Q C Sαβ αβ= +k k k<ui(k)uj(-k)> =
1) Equilibrium state itself
2) Response to disturbanceSimilar to stress vs. rate of strain relation:
τ ij = Cijαβ Sαβ(justified by the Linear response theory for non-equilibrium system)
Not only
but also
(0) 2 /3 11/3( ) ( )4
Kij ij
CQ k Pεπ
−=k k
ˆ ˆ ˆ( ) , /ij ij i j i iP kk k k kδ= − =k
Anisotropic part
ˆ ˆ( ) ( ) ( ) ( ) ( ) ( ) ( ) ( )ij i j i j ijC a k P P P P b k P k kαβ α β β α α β⎡ ⎤= + +⎣ ⎦k k k k k k1/3 13/3 1/3 13/3( ) , ( )a k A k b k B kε ε− −= =
Only 2 (universal) parameters, A and B
Is this correct? What are the values of A and B?
0( ) ( ) ( )ij ij ijQ Q C Sαβ αβ= +k k k<ui(k)uj(-k)> =
at small scale of turbulent shear flowKolmogorov’s isotropic equilibrium spectrum
response
cf. Lumley(1967) Cambon & Rubinstein (2006)
Method of numerical experiment
max 1k η =
Initial condition: isotropic turbulence
max 241k =
DNS of homogeneous turbulence with the simple shear flow
2
00
Sx⎛ ⎞⎜ ⎟= ⎜ ⎟⎜ ⎟⎝ ⎠
U
Resolution: 5123
ˆ ˆ( ) ( ), ( ) ( )abij ij ij a b ij
p k p kE k Q E k p p Q
= =
= =∑ ∑p pObserve
especially,12 12 12 12 11 22 33
12 11 22 33 12 12 12( ), ( ), ( ), ( ), ( ), ( ), ( ), ( )iiE k E k E k E k E k E k E k E k
Estimate A and B, and check consistency.
0.5,1.0S =
1212 12
4 1 4( ) (7 ) , ( ), ( ) ( ) ,15 2 15iiE k A B E k E k A Bπ πξ ξ= − = − + L 1/3 7 /3k Sξ ε −=
Anisotropic Energy spectrum of homogeneous turbulent shear flow
ˆ ˆ( ) ( ) ( )abij a b i j
p kE k p p u u
=
= −∑ p p
( ) ( ) ( )ij i jp k
E k u u=
= −∑ p p
124( ) (7 )15
E k A Bπ ξ= −
121 4( ) ( )2 15iiE k A Bπ ξ= − +
12 ( )E k
121 ( )2 iiE k−
1 ( )2 iiE k
2
00
Sx⎛ ⎞⎜ ⎟= ⎜ ⎟⎜ ⎟⎝ ⎠
UMean Flow
3312
4( ) (23 ) ,105
E k A Bπ ξ= − L
11 2212 12
4( ) ( ) (13 3 )105
E k E k A Bπ ξ= = −
1/3 7 /3S kξ ε −=
Theoretical predictions:
where
Ishihara, et al. (2002)
Consistency11 22 3312 12 12( ), ( ), ( )E k E k E k− − − 12 12 12
11 22 33( ), ( ), ( )E k E k E k− − −
3312
4( ) (23 )105
E k A Bπ ξ= −
11 2212 12
4( ) ( ) (13 3 )105
E k E k A Bπ ξ= = − 12 1211 22
16( ) ( ) ( 2 )105
E k E k A Bπ ξ= = − +
1233
8( ) ( 3 )105
E k A Bπ ξ= +
Theoretical predictions:
1.02.0
SSt
==
1.02.0
SSt
==
Ishihara et al.(2002)
See also Yoshida et al. (2003)
II. Stratification
See Kaneda & Yoshida (2004)
Boussinesq approximation
Buoyancy by Stratification
Kolmogorov scaling:
Boussinesq Turbulence Scaling
From Kaneda & Yoshida (2004)
Angular dependence
From Kaneda & Yoshida (2004)
From Kaneda & Yoshida (2004)
III. MHD
See Ishida & Kaneda (2007)
MHD approximation
quasi-static approximation
+O(b2)
Magnetic force
Local co-ordinateNS-equation
Effect of mean shear
Turbulent Shear Flow
Local strain rate of mean flow
Response; Anisotropic
Isotropic turbulence( Equilibrium state )
Disturbance : X
External forcedue to the magnetic field
External forcedue to the magnetic field
C XC X
Approximately linear in “X”
response of isotropic turbulence
3 (universal) parameters in the inertial subrange
anisotropic parts
• To detect , define
< f (k) >k= k
Theoretical prediction (1)• Angular dependence
Theoretical prediction (2)• Scale dependence
– Assumptions• are functions of only and in the inertial subrange)(kqi
Comparison between theory and DNS
• Angular dependence– Theory
– DNS
– for the DNS• Every 3°• Shells
– [k0,k1)=[8,16)– [k0,k1)=[16,32)– [k0,k1)=[32,64)– [k0,k1)=[64,128)– [k0,k1)=[128,241)
3°
From Ishida & Kaneda (2007)
Comparison between theory and the DNS
• Angular dependence– Theory
– DNS
From Ishida & Kaneda (2007)
Comparison between theory and DNS
• Scale dependence
Theory
DNS-5/3
-7/3
k-7/3/k-5/3=k-2/3
From Ishida & Kaneda (2007)
anisotropy remains at small scale.
From Vorobev et al.( Phys. Fluids 17, 125105 (2005))
Results in our DNS
approaches to isotropic state. (c(k)→1)
Anisotropy increases.
From Ishida & Kaneda (2007)
Results in our DNS
approaches to isotropic state. (c(k)→1)
Anisotropy increases.
From Ishida & Kaneda (2007)
• Anisotropy : c(k)– DNS
– Our theory
Comparison between theory and the DNS
T=TM=16 magnetic field OFF T=TF=32 magnetic field ON
Comparison with the DNS and the theory
≒0.1~0.2
k-7/3/k-5/3=k-2/3
From Ishida & Kaneda (2007)
Summary -1For turbulence,We don’t know the pdf nor Hamiltonian in contrast to thermal equilibrium state
But we may assume 1) the existence of equilibrium state at small scale
(Universal) Local equilibrium state a la K41,disturbance can be treated as perturbation to theinherent equilibrium state determined by the NS-dynamics
and see
2) the response small disturbancedisturbances tested:
Mean Shear, Stratification, MHD( others, e.g., scalar field under mean scalar gradient).
But3) The anisotropy may remain large even at small scales,
if Re is not high enough, so that the inertial subrange is not wide.
Summary -2
Equilibrium state
?
Disturbance; X
Response: J
Mean shearStratificationMHD
Jij= Δ Qij= Cijkm Xkm
References• Ishida T. and Kaneda Y., (2007)
Small-scale anisotropy in MHD turbulence under a strong uniform magnetic field,Physics of Fluids, Vol.19, No. 7, 2007/07, Art. No. 075104-1_10
• Kaneda Y. and Ishihara T., (2006)High-resolution direct numerical simulation of turbulence,Journal of Turbulence, 7 (20): 1-17.
• Kaneda Y. and Yoshida K., (2004)Small-scale anisotropy in stably stratified turbulence,New Journal of Physics, Vol.6, Page/Article No.34-1_16.
• Yoshida K., Ishihara T. and Kaneda Y., (2003)Anisotropic spectrum of homogeneous turbulent shear flow in a Lagrangian renormalized approximation, Physics of Fluids, Vol.15, No. 8, pp.2385-2397.
• Ishihara T., Yoshida K. and Kaneda Y., (2002)Anisotropic velocity correlation spectrum at small scales in a homogeneous turbulent shear flow,Physical Review Letters, Vol. 88, No. 15, Art. No. 154501-1_4.
The end