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L3: The Navier-Stokes equations II: Topology Prof. Sauro Succi.

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Presentation on theme: "L3: The Navier-Stokes equations II: Topology Prof. Sauro Succi."— Presentation transcript:

1 L3: The Navier-Stokes equations II: Topology Prof. Sauro Succi

2 Topological Fluid Dynamics

3 Deformation/Strain rate/Rotation *These are inverse time scales=internal bootstrap frequencies* The deformation tensor governs/encodes the local flow topology

4 Deformation: kinematics Deformation

5 Differential forms

6

7 Deformation/Strain rate/Rotation *These are inverse time scales=internal bootstrap frequencies* Strain rate: shear dissipation Compression: bulk dissipation Rotation: No Dissipation

8 Whiteboard Example: Compute S,D,Omega, div for Couette, Poiseuille, Rigid rotation, Irrotational vortex, Elongational (torture) flow

9 Radial Flow

10 Vortex Flow

11 Elongational Flow

12 Velocity-Vorticity Degree of local rotation Eliminates pressure Useful for nearly-inviscis flows

13 Rotational/Irrotational

14 Rotational/Potential Flow Potential ~ Inviscid Potential & Incompressible Analytic function: very useful for 2D low-viscous hydrodynamics

15

16 Kelvin theorem

17 Turbo-jungle vorticity

18 What’s vorticity good for? Pressure-free! Vortex stretching: Take curl of both sides and use identity To obtain:

19 Enstrophy Vorticity Stretch: Finite-time blow-up? 2d Beltrami flows:

20 What’s vorticity good for? Pressure-free! Vortex Collection: Long-range (electrostatic) interactions

21 Helicity Swirl motion, Dynamo 1d 2d Beltrami flows:

22

23

24 2d: Vorticity-Streamfunction Two-dimensional Potential-->Irrotational: Built-in incompressibility:

25 Potential Flow: 2D Conformal mapping:

26 Body-fitted coordinates

27 2d: Enstrophy conserved Vortex stretching identically zero: Enstrophy is conserved:

28 2d turbulence: Vorticity-Stream Two-dimensional: spectral methods Nonlinear depletion: coherent structures (vortices)

29 Coherent structures Non-linear depletion Cascade blocking; Long-lived metastable states Enstrophy cascade: REGULAR!

30 Ideal 2d: Hamiltonian Symplectic dynamics: Borrow a lot from particle dynamics! Hamiltonian streaming + vortex mergers/breakup

31 Enstrophy: inverse cascade Cascade blocking; Long-lived metastable states Enstrophy cascade: REGULAR! Energy cascade: SINGULAR

32 End of Lecture


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