a computational “rheometer” for turbulent flows · 06/02/2020  · imfm applied to turbulent...

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A Computational “Rheometer” for Turbulent Flows Ali Mani Center for Turbulence Research Stanford University Graduate Students: Danah Park, Yasaman Shirian Advanced Modeling & Simulation (AMS) Seminar Series NASA Ames Research Center, February 6, 2020

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Page 1: A Computational “Rheometer” for Turbulent Flows · 06/02/2020  · IMFM Applied to Turbulent Channel Flow at Re τ=180 (3/3) •Eddy diffusivity is highly anisotropic (non-Boussinesq)

A Computational “Rheometer” for Turbulent Flows

Ali Mani

Center for Turbulence ResearchStanford University

Graduate Students: Danah Park, Yasaman Shirian

Advanced Modeling & Simulation (AMS) Seminar SeriesNASA Ames Research Center, February 6, 2020

Page 2: A Computational “Rheometer” for Turbulent Flows · 06/02/2020  · IMFM Applied to Turbulent Channel Flow at Re τ=180 (3/3) •Eddy diffusivity is highly anisotropic (non-Boussinesq)

• Standard eddy diffusivity model and Boussinesq approximation in RANS equation

• Researchers often ask: “how to tune ?”

• We study: “what should the entire operator look like?”

• Motivations: the standard model is not truly predictive for many practical flows

Motivations

Page 3: A Computational “Rheometer” for Turbulent Flows · 06/02/2020  · IMFM Applied to Turbulent Channel Flow at Re τ=180 (3/3) •Eddy diffusivity is highly anisotropic (non-Boussinesq)

Simpler Question: Scalar Transport

• Instantaneous equation of passive scalar transport (Microscopic)

• Averaged equation (Macroscopic)

• Standard eddy diffusivity modelLinear

Page 4: A Computational “Rheometer” for Turbulent Flows · 06/02/2020  · IMFM Applied to Turbulent Channel Flow at Re τ=180 (3/3) •Eddy diffusivity is highly anisotropic (non-Boussinesq)

Macroscopic Forcing Method (MFM)

• Investigate response to forcing

• survives in averaging the equation

• Perform many DNSs to compute in response to different

• Obtain a linear system and rearrange to obtain

• Expensive!

Condition:

Page 5: A Computational “Rheometer” for Turbulent Flows · 06/02/2020  · IMFM Applied to Turbulent Channel Flow at Re τ=180 (3/3) •Eddy diffusivity is highly anisotropic (non-Boussinesq)

Example: A 2D Parallel Flow (1/6)

• Steady, parallel, velocity field

• Example of 2D solution for (“expensive DNS”)

• Quantity of interest

• What 1D equation (“RANS”) can directly predict ?

x1

x2

L2

x1

x2

x1

Page 6: A Computational “Rheometer” for Turbulent Flows · 06/02/2020  · IMFM Applied to Turbulent Channel Flow at Re τ=180 (3/3) •Eddy diffusivity is highly anisotropic (non-Boussinesq)

Example: A 2D Parallel Flow (2/6)

• Dimensionless Microscopic Equation

• Approximate model using method of G. I. Taylor (1953)

macroscopic diffusivity = Deff=1/2valid for large-scale

x1 x1

t

Page 7: A Computational “Rheometer” for Turbulent Flows · 06/02/2020  · IMFM Applied to Turbulent Channel Flow at Re τ=180 (3/3) •Eddy diffusivity is highly anisotropic (non-Boussinesq)

Example: A 2D Parallel Flow (3/6)

• MFM analysis: • Add forcing to the governing equation

• For different find the linear response

• Homogeneity allows analysis in Fourier space

Page 8: A Computational “Rheometer” for Turbulent Flows · 06/02/2020  · IMFM Applied to Turbulent Channel Flow at Re τ=180 (3/3) •Eddy diffusivity is highly anisotropic (non-Boussinesq)

Example: A 2D Parallel Flow (4/6)

• MFM result (steady limit, ω=0) • Remember Taylor/Boussinesq prediction

2

1

ktrans.~1/mixing length

Page 9: A Computational “Rheometer” for Turbulent Flows · 06/02/2020  · IMFM Applied to Turbulent Channel Flow at Re τ=180 (3/3) •Eddy diffusivity is highly anisotropic (non-Boussinesq)

Example: A 2D Parallel Flow (5/6)

• Macroscopic operator (steady limit, ω=0)

• Fitted operator:

Fitted expression

• Not a number but an operator • Suppressed in small-scale limits• Non-local operator

Page 10: A Computational “Rheometer” for Turbulent Flows · 06/02/2020  · IMFM Applied to Turbulent Channel Flow at Re τ=180 (3/3) •Eddy diffusivity is highly anisotropic (non-Boussinesq)

Outline • Go back and relax simplifications

• Unsteady problems

• Molecular diffusivity active in all directions

• Unsteady 3D flows

• Extension from scalar transport to Navier-Stokes

• Extension to non-homogeneous flows

• Computational cost

• An example incorporating all of the above

Page 11: A Computational “Rheometer” for Turbulent Flows · 06/02/2020  · IMFM Applied to Turbulent Channel Flow at Re τ=180 (3/3) •Eddy diffusivity is highly anisotropic (non-Boussinesq)

Example: A 2D Parallel Flow (6/6)

• Solution to the unsteady problem

• Evaluation of performance

real part fitted operator

Page 12: A Computational “Rheometer” for Turbulent Flows · 06/02/2020  · IMFM Applied to Turbulent Channel Flow at Re τ=180 (3/3) •Eddy diffusivity is highly anisotropic (non-Boussinesq)

Extension to Turbulent Flows

• What will happen if velocity is 3D, unsteady, and turbulent?• Test case: Homogeneous Isotropic Turbulence (HIT) at Reλ=40

Fitted operator:

Page 13: A Computational “Rheometer” for Turbulent Flows · 06/02/2020  · IMFM Applied to Turbulent Channel Flow at Re τ=180 (3/3) •Eddy diffusivity is highly anisotropic (non-Boussinesq)

MFM for Navier-Stokes (1/2)

• First obtain DNS (or measurement) of flow field

• Nonlinearity and interpretation of nonlinear term • Apply MFM to a generalized momentum transport equation (GMT)

• Linear system, (N.S. is its special case)• Operator dependent on flow

Page 14: A Computational “Rheometer” for Turbulent Flows · 06/02/2020  · IMFM Applied to Turbulent Channel Flow at Re τ=180 (3/3) •Eddy diffusivity is highly anisotropic (non-Boussinesq)

MFM for Navier-Stokes (2/2)

• Example: MFM + GMT applied to HIT (Reλ=40)

• Turbulent Schmidt number ScT=D0v/D0

c=0.5

Fitted operator:

Page 15: A Computational “Rheometer” for Turbulent Flows · 06/02/2020  · IMFM Applied to Turbulent Channel Flow at Re τ=180 (3/3) •Eddy diffusivity is highly anisotropic (non-Boussinesq)

Impact on Prediction of Practical Flows

• Can the operator already obtained improve prediction of mean velocity profile? • Example: turbulent round jet à self-similar solution • Use Prandtl Mixing Length Model to determine D and l

r

x

Usignificant

improvement

Page 16: A Computational “Rheometer” for Turbulent Flows · 06/02/2020  · IMFM Applied to Turbulent Channel Flow at Re τ=180 (3/3) •Eddy diffusivity is highly anisotropic (non-Boussinesq)

Outline • Go back and relax simplifications

• Unsteady problems

• Molecular diffusivity active in all directions

• Unsteady 3D flows

• Extension from scalar transport to Navier-Stokes

• Extension to non-homogeneous flows

• Computational cost

• An example incorporating all of the above

Page 17: A Computational “Rheometer” for Turbulent Flows · 06/02/2020  · IMFM Applied to Turbulent Channel Flow at Re τ=180 (3/3) •Eddy diffusivity is highly anisotropic (non-Boussinesq)

Extension to Inhomogeneous Flows (1/2)• Example: transport between two walls

• Left/right BC: Dirichlet condition • Top/bottom: periodic condition • Averaging defined in x2

• Steady limit • Macroscopic model is 1D

• MFM Result:

: discrete macroscopic operator D = Eddy diffusivity operatoris a convolution kernel !

Page 18: A Computational “Rheometer” for Turbulent Flows · 06/02/2020  · IMFM Applied to Turbulent Channel Flow at Re τ=180 (3/3) •Eddy diffusivity is highly anisotropic (non-Boussinesq)

Most General Form of Eddy Diffusivity

• Scalar transport

• Momentum transport

• MFM allows precise measurement of D• Expense?

Page 19: A Computational “Rheometer” for Turbulent Flows · 06/02/2020  · IMFM Applied to Turbulent Channel Flow at Re τ=180 (3/3) •Eddy diffusivity is highly anisotropic (non-Boussinesq)

A fast method for computation of kernel moments

Inverse MFM (not presented) Can obtain moments of D at affordable cost

Page 20: A Computational “Rheometer” for Turbulent Flows · 06/02/2020  · IMFM Applied to Turbulent Channel Flow at Re τ=180 (3/3) •Eddy diffusivity is highly anisotropic (non-Boussinesq)

Boussinesq Approximation

If kernel width ~ eddy size << macroscopic length

è Provides a quantitative framework for assessment of the Boussinesq approximation

Page 21: A Computational “Rheometer” for Turbulent Flows · 06/02/2020  · IMFM Applied to Turbulent Channel Flow at Re τ=180 (3/3) •Eddy diffusivity is highly anisotropic (non-Boussinesq)

Example Applicationflow field DNS solution (s=1) macroscopic field

DNS

MFM D0

MFM D2 (non-local)

Can construct approximate kernels by matching higher moments of D(x1,y1)

= 0

Page 22: A Computational “Rheometer” for Turbulent Flows · 06/02/2020  · IMFM Applied to Turbulent Channel Flow at Re τ=180 (3/3) •Eddy diffusivity is highly anisotropic (non-Boussinesq)

Outline

• Go back and relax simplifications

• Unsteady problems

• Molecular diffusivity active in all directions

• Unsteady 3D flows

• Extension from scalar transport to Navier-Stokes

• Extension to non-homogeneous flows

• Computational cost

• An example incorporating all of the above

Page 23: A Computational “Rheometer” for Turbulent Flows · 06/02/2020  · IMFM Applied to Turbulent Channel Flow at Re τ=180 (3/3) •Eddy diffusivity is highly anisotropic (non-Boussinesq)

IMFM Applied to Turbulent Channel Flow at Reτ=180 (1/3)

• Only 9 DNSs required to compute D0jilk

• All 81 coefficients computed versus distance from wall• This is the eddy-diffusivity tensor !

– Represents truncated operator up to the leading (local) term

– Analysis of non-local terms in progress

• Example profile (one out of 81 profiles)

• MFM can measure eddy diffusivityon the centerline !

x2

Page 24: A Computational “Rheometer” for Turbulent Flows · 06/02/2020  · IMFM Applied to Turbulent Channel Flow at Re τ=180 (3/3) •Eddy diffusivity is highly anisotropic (non-Boussinesq)

IMFM Applied to Turbulent Channel Flow at Reτ=180 (2/3)

• Leading order model (D0) is sufficient for RANS prediction of channel flow (nonlocal effects not dominant for this example)

• Error due to neglecting of non-local effects ~ 1.5% (converged)

x2

Page 25: A Computational “Rheometer” for Turbulent Flows · 06/02/2020  · IMFM Applied to Turbulent Channel Flow at Re τ=180 (3/3) •Eddy diffusivity is highly anisotropic (non-Boussinesq)

IMFM Applied to Turbulent Channel Flow at Reτ=180 (3/3)

• Eddy diffusivity is highly anisotropic (non-Boussinesq) • Let’s examine streamwise momentum equation

• Boussinesq approx. prescribes D01111=D0

2121

• Our measurement shows D01111 is ~16 times larger than D0

2121!

• In parallel flows (e.g. channel) the difference does not matter • What about onset of separation?

Page 26: A Computational “Rheometer” for Turbulent Flows · 06/02/2020  · IMFM Applied to Turbulent Channel Flow at Re τ=180 (3/3) •Eddy diffusivity is highly anisotropic (non-Boussinesq)

Final Words

• We developed a rheometer for turbulent flows

• Standard rheometer for laminar flow measures momentum diffusivity • Assumes the underlying Brownian motion (transporter of

momentum) remains unaffected by rheometry • MFM honors this condition for turbulent flows

• MFM informs closure model forms:à anisotropy, non-locality

› Ref: Mani, A. and Park, D., “Macroscopic forcing method: a tool for turbulence modeling and analysis of closures,” Physical Review Fluids

momentum transporter of momentum

Page 27: A Computational “Rheometer” for Turbulent Flows · 06/02/2020  · IMFM Applied to Turbulent Channel Flow at Re τ=180 (3/3) •Eddy diffusivity is highly anisotropic (non-Boussinesq)

Thank you