Upload
eleanor-hanson
View
12
Download
0
Embed Size (px)
DESCRIPTION
DNS and Structure-Based Modeling of Rotated Shear Flows: Implications for Accretion Disks?. S. C. Kassinos Stanford University/University of Cyprus. ESF PESC Exploratory Workshop: Frontiers for Computational Astrophysics Wengen, Switzerland 26-30 September 2004. - PowerPoint PPT Presentation
Citation preview
University of Cyprus
DNS and Structure-Based Modeling of Rotated Shear Flows: Implications
for Accretion Disks?
S. C. Kassinos
Stanford University/University of Cyprus
ESF PESC Exploratory Workshop:
Frontiers for Computational Astrophysics
Wengen, Switzerland 26-30 September 2004
Also supported by AFOSR Grant No. F49620-99-0138
University of Cyprus
Motivation
Strongly rotating flows are challenging to turbulence models.
Most well-known models have been calibrated against 20-year-old LES!
Surprising lack of modern high resolution simulations of these flows.
Objectives
Create a modern high resolution DNS database of homogeneous turbulence that is sheared or strained in rotating frames.
Modeling
DNS results are used to validate a new type of model that was developed before the results were available.
University of Cyprus
Outline
Flow configuration
Results that could be of relevance to accretion
Direct Numerical Simulation (DNS): what are the open issues
Structure-Based Modeling: what are the open issues
Structure-Based Modeling: why is it different (better)?
Future steps
Discussion
University of Cyprus
Discussion focus
DNS: +more accurate physics – limited to low Reynolds numbers
We discuss results from Direct Numerical Simulations (DNS) and one-point turbulence modeling based on RANS
Turbulence models: +calibrated for high Reynolds numbers –often questionable physics
University of Cyprus
Flow Configurations
DNS configurations
rate shear
rate rotation frame Sf -+
counter-rotating frame
co-rotating frame
University of Cyprus
frame co-rotating frame counter-rotating
0
00
? ???
Flow physics: spanwise rotation
rate shear
rate rotation frame Sf
t t
k k kk k
ttt
decay decayexponentialalgebraic algebraic
- +
University of Cyprus
How does equilibrium vary if at all withP ?
P
1
t
turbulence thrives
turbulence dies
Flow physics: basic question
University of Cyprus
DNS Code Description
Governing equations solved in coords deforming with the mean flow to allow Fourier pseudo-spectral methods with periodic B.C.’s.
Time advance is based on a third-order Runge-Kutta method.
Aliasing errors due to periodic remeshing are removed.
Mean shear skews the computational grid, but periodic remeshing allows the simulation to progress to large total shear.
The code is implemented in Vectoral using MPI and has been ported to the ASCI Red and a 48-node Linux cluster.
Accuracy, grid independence and scalability have been tested.
University of Cyprus
Reynolds Decomposition
ijjjjiijiji uupuuu ,,,, )(3
11
pPpuUu iii ,
kikkkiii RUP
Dt
DU,,,
1
continuity: 0, iiumomentum:
averaging? jiij uuR
University of Cyprus
ijij ΩS ,
,k
2ij
ij
Rr
k
one-point model ijR
mean deformation
rate
turbulence scales
Directional intensity of velocity fluctuations
Standard Assumption (RST)
University of Cyprus
ijij ΩS ,
,k
2ij
ij
Rr
k
one-point model ijR
mean deformation
rate
turbulence scales
Directional intensity of velocity fluctuations
Standard Assumption (RST)
Is this enough information for consistent accuracy?
University of Cyprus
ijij ΩS ,
,k
2ij
ij
Rr
k
one-point model ijR
mean deformation
rate
turbulence scales
Directional intensity of velocity fluctuations
Standard Assumption (RST)
Is this enough information for consistent accuracy?
ONLY FOR SIMPLE CASES!!
University of Cyprus
What Other Information?
Most turbulent kinetic energy organized in large structures.
The statistical description of the energy-containing structures is another degree of freedom in addition to .
Velocity magnitude
5123 DNS of rotated shear flow
ijR
University of Cyprus
One-point turbulence structure tensors
1X
,1 ,0 ,0 111111 frd
1X
0 1, ,0 111111 frd
0d means eddy-alignment in the x direction.
means all velocity fluctuations organized in jetal motion in x direction.
1r
means all large-scale circulation organized in vortical motion around x direction.
1f
University of Cyprus
Importance of Structure in Dynamics
Two fields with same , but different structure have different dynamics.
No dynamical effect of rapid frame rotation.
Rapid frame rotation modifies one-point state of the turbulence.
ijR
ijR
University of Cyprus
One-point turbulence structure tensors
kijijk
njniij
jninij
ΨuQ
ΨΨF
ΨΨD
,
,,
,,
Turbulent streamfunction:
0 , - , ,,, iiikkipqipqi ΨΨΨu
dimensionality
circulicity
stropholysis
describes the elongation and orientation of energy-containing eddies.
describes the distribution of large-scale circulation in the turbulence field.
contains information about the breaking of reflectional symmetry by mean/frame rotation.
Like the pressure, carries non-local information'jΨ
University of Cyprus
One-point turbulence structure tensors
Near-wall streaks in fully-developed channel flow
09.0 ,84.0 ,03.0 :5.3 111111 frdy
skin friction
University of Cyprus
ijij ΩS ,
, k
ijkQ
one-point model ijkQ
mean deformation
rate
turbulence scales
Results support this as a more
fundamentally based approach
Directional intensity of velocity fluctuations and morphology of large eddies
Structure-Based Modeling (SBM) Assumption
University of Cyprus
ijk
exactterms
dQ= .... + rotational randomization model
dt
...
, , ijk ij ij ij
d
dt
Q R D F
Structure-Based Formulation
University of Cyprus
ijk
exactrotational randomization model term
2
s
1 3 (( )dQ
= .... dt
- ( ))RFij ijm mk mkk ij mj mmk ik jF DQ R DQ
Coefficients set by matching standard homogeneous flows with mean and frame rotation (shear, elliptic, axisymmetric strain+rotation, plane strain+rotation). Then validated in fully developed channel flow and rotating pipe flow.
Relative narrow range supported by match:
1 2 3 0.5 0.7 0 0.4 almost negligible
Differential SBM
, , ijk ij ij ijQ R D F
University of Cyprus
(For details see Phys. Fluids, 14(7), April 2002)
At high Re, LSE model constants are evaluated by an asymptotic analysis for decaying turbulence in stationary and rotating frames.
2 2
*
production by se
* 2
lf-stretc transfer to small hingand cross-scal scale voticity
does not vae stretching
(vanishes for 2D-2Cnish for 2D-2C
produc
)
t
( )P ij jT iC f S
dC
dt
2 2
vanishes for 2D-2C(forward/inv
ion by mean strain
erse cascade balance)
* *
,
, wh
, model const
ere
9
ant
3
s
ik kj j
i ji
T
j
P
i
k d
d
C C
r
f
f
The High Re Large-Scale Enstrophy (LSE) Equation
University of Cyprus
Results (preliminary): equilibrium P/
P
DNS
SBM
predictions using standard model eqn. (SSG, v2f, …)
SBM using the large-scale enstrophy equation agrees with DNS.
standard model seriously in error!
From a practical point of view, the most important info are the values of where crosses 1 (that we can answer). P
University of Cyprus
Results (preliminary): equilibrium P/
P
University of Cyprus
Results (preliminary): equilibrium P/
P
University of Cyprus
Results: evolution histories of structure tensors
normalized Reynolds stress normalized dimensionality normalized circulicity
Level of agreement between DNS and SBM typical for other . solid lines: DNS dashed lines: SBM using large-scale enstrophy.
University of Cyprus
Results: Reynolds stress tensor at St = 9 vs.
University of Cyprus
Results: evolution histories of structure tensors
normalized Reynolds stress normalized dimensionality normalized circulicity
Level of agreement between DNS and SBM typical for other . solid lines: DNS dashed lines: SBM using large-scale enstrophy.
11
22
12
33
11
12
11
12
33
University of Cyprus
Results: structure tensors at St = 9 vs.
symbols: DNS solid lines: SBM using large-scale enstrophy.
normalized Reynolds stress normalized dimensionality normalized circulicity
University of Cyprus
DNS configurations for MHD turbulence
frame rotation rate
shear ratef S
B
B
2(B )
ext
extshear
B
MS
20
0
(B )
ext
extu
B
LN
u
uLRm
Stuart NumberMagnetic Reynolds No.
University of Cyprus
MHD Results (preliminary): equilibrium P/
P
University of Cyprus
Evolution of Energies
2 10 50 MNRm
0.75 1.0
University of Cyprus
Production over dissipation
2 10 50 MNRm
0.75 1.0 2 2
University of Cyprus
v-field C221
v-field C221W2
v-field C221W2-B=0
Results: moderate shear timescale
25.0 2 10 1 MNRm
0 B03 f 0 B03 f 0 B03 f
BB
horizontal slabs vertical slabsstreamwise eddies
University of Cyprus
Results: scale-dependent anisotropy
Reminiscent of the observations of Cho and Lazarian (2003) in high Rm compressible MHD turbulence
University of Cyprus
But…
DNS is for low Reynolds number periodic flow in a box.
Model predictions are for high-Reynolds number limit.
Establish if possible Reynolds number dependence
Conclusion
SBM with large-scale enstrophy in excellent agreement with DNS!
Future Plans
DNS seems predicts that turbulence is suppressed for . 2 3 DNS seems predicts that MHD turbulence with spanwise B can survive .50, (1), 10, 2m mR P O N M
10243 Or bigger DNS would help! (both Re effects and eddy containment issues