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Collective dynamics and patterns of rapid granular fluid and amplitude equation Physics of Granular Flows YITP, Kyoto University, Japan June 24 - 6 July 2013 Priyanka Shukla 2 July 2013 Department of Mathematics and Statistics, IISER


  1. Collective dynamics and patterns of rapid granular fluid and amplitude equation Physics of Granular Flows YITP, Kyoto University, Japan June 24 - 6 July 2013 Priyanka Shukla 2 July 2013 Department of Mathematics and Statistics, IISER Kolkata, Nadia, India

  2. Outline of Talk Part 1  Introduction: collective dynamics & patterns  Amplitude equation in granular fluid Part 2  Problem description: 3D Couette flow  Weakly nonlinear analysis: Amplitude Eqn.  Numerical methods  Results  Conclusions

  3. Introduction When a system is driven by external forcing, it becomes unstable beyond some critical value of the control parameter Spatio-temporal instabilities arises Collective dynamics of unstable system, far from equilibrium, yields patterned states (Cross & Hohenberg, Rev Mod Phys 1993) Classification depending on external forcing Aranson & Tsimring, Rev Mod Phys. 2006 Vibration Gravity Shear

  4. Patterns in vibration driven granular matter Phenomena *Clustering *Surface wave *Localized structure *Convection Uniform configuration to Clustering Coexistence of dilute and dense region Top view of a submonolayer of Freely cooling granular gas grains on a vibrated plate (Goldhirsch and Zanetti, 1993) (Olafsen and Urbach, 1998)

  5. Uniform granular layer to surface wave and localized structure Surface wave Localized structure oscillon Pattern for various values of frequency and acceleration: stripes, squares, hexagons, spiral, interfaces, and oscillons (Umbanhower et al. 1996)

  6. Convection Non-uniform Configuration Bouncing state (Hayakawa, Yue, & Hong, 1995) convection Density inversion (Khain & Meerson, 2003) Leidenfrost state (Eshuis et al 2010) Leidenfrost (Eshuis et al 2005) Convection (Eshuis et al 2010)

  7. Patterns in shear driven granular matter Phenomena *Shearbanding *Segregation *Density wave *Clustering Shearbanding Gradient Banding: Bands of different shear rates, along the gradient direction, coexist     0 . 05 0 . 3   0 . 8 Tan & Goldhirsch 1997 (Alam 2003) (Alam 2003)

  8. Circular Couette geometry Shear-Banding in ‘Dense’ Granular Flow (Savage & Sayed 1984; Mueth et.al. 2000 ) Shear-bands are narrow and localized near Mueth et al. 2000 moving boundary. Fast particles (yellow) near the inner wall appear to move smoothly while the orange and red particles display more irregular and intermittent motion Vorticity Banding: Bands of different shear stress, along the vorticity direction, coexist Conway & Glasser, (2004)    0 0 . 05 , 0 . 6 e Three bands of particles along the vorticity direction

  9. Conway & Glasser, (2004) Clustering & Density wave Reason Inelastic collisions Fluctuations Generate regions of high density Instability Dense cluster, plug..

  10. Amplitude (order parameter) equation Describe the slow modulation in space and time near the onset of instability Gives a qualitative insight of pattern formation • Growth of the perturbation about the spatially uniform state • Saturation of the growth by nonlinearity • Dispersion and effect of spatial distortions

  11. Order Parameter model for Granular patterns Vibration Complex Ginzburg-Landau Equation Patterns in vibrated bed can be predicted by the complex Ginzburg-Landau Eqn (‘ çubic ’) (Tsimring and Aranson 1997, PRL) Phenomenological model Phenomena *Turbulance *Nonlinear Waves, *Phase transitions, *Superconductivity, *Superfluidity, etc.

  12. Generalized Swift Hohenberg Equation Generalized Swift-Hohenberg equation describes primary pattern forming bifurcation: square, strips and oscillons (Crawford and Riecke 1999)     2         2 1 ( ) R N  t                     3 5 3 2 2 2 ( ) .( ) ( ) N b b 1 2 1 2 (Swinney 1996) The magnitude of epsilon describes squares, strips, hexagons, oscillons, etc. patterns Subcritical Complex Ginzburg- Landau Equation (‘ quintic ’)        0 . 192 , 4 , 0 . 3 , 0 . 4 c c c 1 3 4 Localized pulse solution, amplitude surface (Thual and Fauve, J. Phys. 1988)

  13. Shukla P., Meer D. V ., Lohse D. & Alam M., 2013, Preprint Stuart-Landau Equation (Eshuis et al 2010) Experiment (Eshuis et al 2010) Particle Simulation Leidenfrost State leads to convection via a supercritical bifurcation Nonlinear Stability Theory (supercritical)    6 . 2 , 164 , 4 . 0 , F L a mm   52 ( 174 ) f Hz or S

  14. Shear Complex Ginzburg-Landau (CGL) Equation Slow evolution of the spatial structure of shearband using two dimensional CGL ( Saitoh K. & Hayakawa H., 2011) Unbounded domain Stuart- Landau (‘order parameter’) Equation Bounded domain Form of perturbation References Instability Shukla & Alam PRL 2009; Shukla & Alam, JFM, 2011a Shukla & Alam, JFM, 2011b Shukla & Alam, JFM, 2011b Shukla & Alam, JFM, 2013 Alam & Shukla, JFM, 2013

  15. Problem Description Schematic diagram of 3D plane Couette flow The plane Couette flow is unsable due to various stationary and travelling wave instabilities Scaling: Gap between the walls, Average velcocity, and inverse of total shear rate

  16. Granular Hydrodynamic Equations (Savage, Jenkins, Goldhirsch , …) Balance Equations Navier-Stokes Order Constitutive Model Stress Tensor … Granular Heat Flux Dissipation term or sink of energy

  17. Uniform shear flow  Steady No Slip & Zero heat flux B.C.  Fully developed Uniform Shear Solution  Parallel  0 ( )  Unidirectional f     0 0 2 ( ) . ( ) . y const T y const  0 ( ) f 5  0 ( ) u y y  X  Base Flow Perturbation Uniform shear flow (USF)   0 ' X X X Disturbance Eqns Normal mode sol Linear problem  '  X  X '     ' ...  LX N N [ 1 ; 1 ] ( 0 ) [ 1 ; 1 ] ' LX LX c X  2 3  t t

  18. Weakly Nonlinear Analysis Slow/ Active/ Unslaved Fast/ Passive/ Slaved Growing or neutrally stable Decaying mode …dependent Amplitudes are independently determined Bounded Discrete Amplitude Slow modes with positive, zero, Amplitude or slightly negative growth rates spectrum Eq. (ODE) System equation Landau 1944, Stuart & Watson, 1960 Envelope Slow modes: slowly varying Unbounded Continuous envelope of fast varying patterns. Eq. (PDE) System spectrum Newell & Whitehead, 1969

  19. Derivation of Amplitude Equation Notation: Slow mode: S ; Fast Mode: F Coordinate of ‘ S ’ : amplitude of discrete modes of ‘ S ’ Amplitude Order Parameter (gives degree of order/disorder, and structure of the system) Near the onset, the amplitudes of the passive modes in the set ‘ F’ quickly relax to a manifold, called the center manifold ‘ F = F(S) ’ . On center manifold, the amplitudes will evolve on a time scale proportional to inverse of linear growth rate. Coefficient contains relevant Amplitude eqn. information about the system Easier to solve than original Product of active amplitude microscopic eqns.

  20. Separation of mode Center manifold Amplitude equation Newell, Passot & Lega, Annu. Rev. Fluid Mech. 1993

  21. Center Manifold Reduction Separation of mode (Carr 1981; Shukla & Alam, PRL 2009) Center manifold     Disturbance     ' L X N  j   Eqn t Step 1  j 2 Amplitude equation  Inner product with adjoint eigenfunction of the linear  .  ( 0 ) i k x c t E e problem Step 2  Separating the like-power terms in amplitude,  Yields an amplitude eqn Eigenvalue First Landau Coeff Step 3   ( 2 ) ( 2 ) ( 2 ) c a ib Stuart-Landau Equation

  22. Determination of Landau Coefficients All fast modes are determined algebraically as a balance between each linearly decaying fast mode and its regeneration by nonlinear interactions involving members of S. Enslaved Equation represents all non-critical modes Regeneration of F mode by nonlinear interactions of members of S

  23. Amplitude Expansion Method (Stuart & Watson 1960; Shukla & Alam, JFM 2010a )   θ  ( k ) i k Co-ordinate Transformation X' X (y , A) e c.c.        ( , , , ) ( , )  x z t k x k z t (k) (k) [k; n] X (y) A X (y) x z     ( , ) ( ) t A t dA      1 (0) (1) 2 (2)  A a Aa A a  ( ) A A t dt    y y θ Θ d ω   dA A : Real amplitude        ω   (0) (1) 2 (2)  t b Ab A b     t t dA dt     [k; n] [n 1] [1;1] δ L X c X G kn k1 kn [  1 ] n Landau coefficient      c [n 1] [n 1] [n 1] c a ib           [n m] [n m] {k; n} δ G ma ikb X E /(1 ) F kn kn k0 kn    (0) (0) L (na ikb )I L Solution Procedure: kn k Solvability Condition 1/2   [1;1] (0) [1;1] L X c X G Ydy 11 1n   1/2  [n 1] 1/2  c [0;2] L X G , 02 02  [1;1] X Ydy    [1;1] (2) [1;1]  L X c X G [2;2] L X G , 13 13  22 22 1/2

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