Shear Turbulence. Fabian Waleffe. Depts. of Mathematics and Engineering Physics. Wisconsin
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1 Shear Turbulence Fabian Waleffe Depts. of Mathematics and Engineering Physics, Madison University of Wisconsin
2 Mini-Symposium on Subcritical Flow Instability for training of early stage researchers
3 Mini-Symposium on Subcritical Flow Instability for training of early stage researchers... by late stage researchers?!
4 Mini-Symposium on Subcritical Flow Instability for training of early stage researchers Instability?... by late stage researchers?!
5 Mini-Symposium on Subcritical Flow Instability for training of early stage researchers Instability?... by late stage researchers?! Subcritical instability?
6 Mini-Symposium on Subcritical Flow Instability for training of early stage researchers Instability?... by late stage researchers?! Subcritical instability? Transition to turbulence?
7 Mini-Symposium on Subcritical Flow Instability for training of early stage researchers Instability?... by late stage researchers?! Subcritical instability? Transition to turbulence? What is turbulence?
8 Incompressible flow: Navier-Stokes equations 3D velocity field u(x, t): u = 0 t u + (uu) + p = 1 R 2 u R: Reynolds number
9 Simple geometries, simple flow? Pipe, Channel u = (1 y 2 ) ˆx R 2, 000 Plane Couette u = y ˆx R 350
10 Channel flow for R 2, not simple! Front Top Side Green, M. A., Rowley, C. W. & Haller, G. Detection of Lagrangian coherent structures in three-dimensional turbulence, J. Fluid Mech., 572, 2007,
11 Instability?
12 Instability? NSE: du dt = f (u; R)
13 Instability? NSE: du = f (u; R) dt Equilibrium u 0 : 0 = f (u 0 ; R)
14 Instability? du NSE: = f (u; R) dt Equilibrium u 0 : 0 = f (u 0 ; R) ( ) d(u u Linear stability: 0 ) f = (u u dt u 0 ) 0
15 Instability? du NSE: = f (u; R) dt Equilibrium u 0 : 0 = f (u 0 ; R) ( ) d(u u Linear stability: 0 ) f = (u u dt u 0 ) u u 0 = ve λt, 0 ( ) f u 0 v = λv, Instability if R(λ) > 0, typically for R > R c
16 Linear instability stable R c unstable R
17 Nonlinear bifurcation u u 0 stable R c unstable R
18 Bifurcations R c R Supercritical, NL stabilizes da dt = (R R c)a A 3
19 Bifurcations R c R Supercritical, NL stabilizes da dt = (R R c)a A 3 R c R Subcritical, NL de -stabilizes, da dt = (R R c)a+a 3
20 Bifurcations R c R Supercritical, NL stabilizes da dt = (R R c)a A 3 R c R Subcritical, NL de -stabilizes, da dt = (R R c)a+a 3 R c R Higher order NL stabilization? da dt = (R R c)a+a 3 A 5
21 Supercritical or subcritical?
22 Supercritical or subcritical? Nonlinearity decides: da dt = (R R c)a ± A 3
23 Supercritical or subcritical? Nonlinearity decides: NSE: du dt da dt = (R R c)a ± A 3 dv = f (u; R) dt = L(v; u 0, R) + N(v, v)
24 Supercritical or subcritical? Nonlinearity decides: NSE: du dt da dt = (R R c)a ± A 3 dv = f (u; R) dt = L(v; u 0, R) + N(v, v) v, N(v, v) = 0 d v, v dt = v, L(v) = v, L T (v)
25 Supercritical or subcritical? Nonlinearity decides: NSE: du dt da dt = (R R c)a ± A 3 dv = f (u; R) dt = L(v; u 0, R) + N(v, v) v, N(v, v) = 0 d v, v dt = v, L(v) = v, L T (v) sufficient for supercritical: L = L T
26 Supercritical or subcritical? Nonlinearity decides: NSE: du dt da dt = (R R c)a ± A 3 dv = f (u; R) dt = L(v; u 0, R) + N(v, v) v, N(v, v) = 0 d v, v dt = v, L(v) = v, L T (v) sufficient for supercritical: L = L T necessary for subcritical: L L T
27 Linear stability: L L T... Back to shear flows
28 Back to shear flows Linear stability: L L T... Hard! Confusing!
29 Back to shear flows Linear stability: L L T... Hard! Confusing! Need inflection point for inviscid ( R = ) instability (Rayleigh 1880)
30 Back to shear flows Linear stability: L L T... Hard! Confusing! Need inflection point for inviscid ( R = ) instability (Rayleigh 1880) Viscosity can lead to instability! (Prandtl, Heisenberg, Tollmien, Lin)
31 Back to shear flows Linear stability: L L T... Hard! Confusing! Need inflection point for inviscid ( R = ) instability (Rayleigh 1880) Viscosity can lead to instability! (Prandtl, Heisenberg, Tollmien, Lin)... but only in BL and Channel, not pipe and plane Couette... and weak instability seems unrelated to natural transition
32 Back to shear flows Linear stability: L L T... Hard! Confusing! Need inflection point for inviscid ( R = ) instability (Rayleigh 1880) Viscosity can lead to instability! (Prandtl, Heisenberg, Tollmien, Lin)... but only in BL and Channel, not pipe and plane Couette... and weak instability seems unrelated to natural transition Who said: Subtle is the Lord, but malicious s/he is not.?!
33 Shear turbulence turbulence?! u u 0 stable stable?! R c R
34 Shear turbulence turbulence?! u u 0 transition?! stable stable?! R c R
35 Streaks in turbulent shear flows... R 10 9? (OK, some convection too... )
36 Streaks in turbulent channel flow... Skin friction (Kim, Moin, Moser JFM 2007)
37 Characteristic near-wall coherent structure Derek Stretch, CTR Stanford, 1990 Streaks + staggered quasi-streamwise vortices: why?
38 Self-Sustaining Process (SSP) advection of mean shear Streaks O(1) instability of U(y,z) Streamwise Rolls O(1/R) nonlinear self interaction Streak wave mode (3D) O(1/R) WKH 1993, HKW 1995, W 1995, 1997
39 SSP theory SSP method (1) Add F forcing of streamwise rolls to NSE R2 O( 1 R ) rolls, O(1) streaks ( Full NSE, Newton s method) PRL 1998, JFM 2001, PoF 2003
40 SSP theory SSP method (1) Add F forcing of streamwise rolls to NSE R2 O( 1 R ) rolls, O(1) streaks (2) Find F c subcritical bifurcation point (streak instability) ( Full NSE, Newton s method) PRL 1998, JFM 2001, PoF 2003
41 SSP theory SSP method (1) Add F forcing of streamwise rolls to NSE R2 O( 1 R ) rolls, O(1) streaks (2) Find F c subcritical bifurcation point (streak instability) (3) Continue to F = 0. Ta da! ( Full NSE, Newton s method) PRL 1998, JFM 2001, PoF 2003
42 SSP theory SSP method (1) Add F forcing of streamwise rolls to NSE R2 O( 1 R ) rolls, O(1) streaks (2) Find F c subcritical bifurcation point (streak instability) (3) Continue to F = 0. Ta da! (4) (optional) Recall: Subtle is the Lord, but malicious s/he is not. ( Full NSE, Newton s method) PRL 1998, JFM 2001, PoF 2003
43 Laminar Couette flow: u=0 & u= Wx Fr
44 SSP: Streamwise Rolls create Streaks Wx Fr
45 SSP: Rolls create Streaks Wx Fr
46 SSP: Rolls create Streaks Wx Fr
47 SSP in action: Subcritical Bifurcation from Streaks Wx Fr
48 SSP in action: Subcritical Bifurcation from Streaks Wx Fr
49 SSP in action: Subcritical Bifurcation from Streaks Wx Fr
50 SSP in action: Subcritical Bifurcation from Streaks Wx Fr
51 SSP in action: Subcritical Bifurcation from Streaks Wx Fr
52 SSP in action: Subcritical Bifurcation from Streaks Wx Fr
53 SSP in action: Subcritical Bifurcation from Streaks Wx Fr
54 SSP in action: Subcritical Bifurcation from Streaks Wx Fr
55 SSP in action: Subcritical Bifurcation from Streaks Wx Fr
56 SSP: Self-Sustained! 3D Lower branch Wx Fr
57 SSP: Self-Sustained! 3D Lower branch Wx Fr
58 SSP: Bifurcation from Streaks Wx Fr
59 SSP: Bifurcation from Streaks Wx Fr
60 SSP: Self-Sustained! 3D Upper branch Wx Fr
61 SSP: Self-Sustained! 3D Upper branch Wx Fr
62 Homotopy Free-Free Couette (FFC) Rigid-Free Poiseuille (RFP) µ = 0 1 BC : (1 µ) du dy + µu = 0 Flow : ( 1 U L (y) = y + µ 6 y 2 ) 2
63 FFC RFP
64 FFC RFP
65 FFC RFP
66 FFC RFP
67 FFC RFP
68 Poiseuille traveling wave!
69 Poiseuille traveling wave!
70 Optimum Traveling Wave: 100 +! min R τ = 2h + = 44 for L + x = 274, L + z = 105 just right!
71 Out-of-the-blue-sky DRAG R Lower branch does NOT bifurcate from laminar flow! RRC (α, γ) = (1, 2), (1.14, 2.5), up to R asymptotics
72 Vortex visualization ω x 2Q= 2 p = Ω ij Ω ij S ij S ij
73 Upper and Lower branches 0.6 max(q), (α, γ) = (1.14, 2.5).
74 Upper and Lower branches 0.6 max(q), (α, γ) = (1.14, 2.5).
75 Upper and Lower branches 0.6 max(q), (α, γ) = (1.14, 2.5).
76 Upper and Lower branches 0.6 max(q), (α, γ) = (1.14, 2.5).
77 Upper and Lower branches 0.6 max(q), (α, γ) = (1.14, 2.5).
78 Upper and Lower branches 0.6 max(q), (α, γ) = (1.14, 2.5).
79 Upper and Lower branches 0.6 max(q), (α, γ) = (1.14, 2.5).
80 Upper and Lower branches 0.6 max(q), (α, γ) = (1.14, 2.5).
81 Upper and Lower branches 0.6 max(q), (α, γ) = (1.14, 2.5).
82 Upper and Lower branches 0.6 max(q), (α, γ) = (1.14, 2.5).
83 Upper and Lower branches 0.6 max(q), (α, γ) = (1.14, 2.5).
84 Structure of LBS, R advection of mean shear Streamwise Rolls O(1/R) Streaks O(1) exp ( i α x) mode O(1/R) instability of U(y,z) nonlinear self-interaction u ū ˆx = [u 0 ū, v 0, w 0 ](y, z) + e iαx u 1 (y, z) y max z rms R
85 Structure of LBS, R = advection of mean shear Streamwise Rolls O(1/R) Streaks O(1) exp ( i α x) mode O(1/R) instability of U(y,z) nonlinear self-interaction u = [u 0, v 0, w 0 ](y, z) + e iαx [u 1, v 1, w 1 ](y, z) y u 0 (y, z), v 0 (y, z) w 1 (y, z) z y z critical layer!
86 LB eigenvalues, (α, γ) = (1.14, 2.5), (1, 2), R = Only 1 unstable eig!
87 Stability of LBS real(λ) R
88 LB Transition (α, γ) = (1.14, 2.5), (1, 2), R = Dissipation Rate Dissipation Rate Energy Input Rate Energy Input Rate Dissipation Rate Dissipation Rate Energy Input Rate Energy Input Rate
89 Lower branch R = max(q), R = 1000, (α, γ) = (1.14, 2.5).
90 Two states of fluid flow? Turbulent Laminar
91 Separatrix, transition threshold Turbulent Laminar
92 Unstable Coherent States! Turbulent Laminar
93 PCF data (R = 400) 5 4 Dissipation Rate Energy Input Rate Periodic solutions in HKW (1.14, 1.67) by Viswanath, JFM 2007 & Gibson (TBA)
94 Visualizing State Space ( 10 5 dof s) 0.1 u NB u LM a a a RRC, R=400, Gibson, Halcrow, Cvitanovic, JFM to appear arxiv.org/
95 Visualizing State Space (PCF, R=400) u UB 0.1 u LB τ z u UB u LM a 3 0 τ xz u LB τ x u UB τ xz u UB 0 a a 1 RRC, R=400, Gibson, Halcrow, Cvitanovic, JFM to appear arxiv.org/
96 Conclusions Go nonlinear, young men and women!
97 Conclusions Go nonlinear, young men and women! Instabilities? bifurcations! coherent flows!
98 Conclusions Go nonlinear, young men and women! Instabilities? bifurcations! coherent flows! Laminar or turbulent? lots, and lots of coherent too!
99 Conclusions Go nonlinear, young men and women! Instabilities? bifurcations! coherent flows! Laminar or turbulent? lots, and lots of coherent too! Go coherent, young men and women!
100 Conclusions Go nonlinear, young men and women! Instabilities? bifurcations! coherent flows! Laminar or turbulent? lots, and lots of coherent too! Go coherent, young men and women! Bypass transition = instability of streaks? NO! instability of Lower Branch States!
101 Conclusions Go nonlinear, young men and women! Instabilities? bifurcations! coherent flows! Laminar or turbulent? lots, and lots of coherent too! Go coherent, young men and women! Bypass transition = instability of streaks? NO! instability of Lower Branch States! Lower Branch = Gate to Turbulence!
102 Upper and Lower branches no-slip Couette 5 4 Dissipation Rate Energy Input Rate Steady State & turbulent (by Jue Wang & John Gibson) in RRC, R = 400, (α, γ)=(0.95,1.67)
103 Upper branches Turbulence (no-slip Couette) y 0 y U RMS solid: Turbulent (avg t=2000), dash: fixed point Mean and RMS velocity profiles
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