introduction to modeling fluid dynamics

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The UNIVERSITY of NORTH CAROLINA at CHAPEL HILL Introduction to Modeling Fluid Dynamics 1

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Introduction to Modeling Fluid Dynamics. Different Kind of Problem. Can be particles, but lots of them Solve instead on a uniform grid. Particle Mass Velocity Position. Fluid Density Velocity Field Pressure Viscosity. No Particles => New State. No Particles => New Equations. - PowerPoint PPT Presentation

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The UNIVERSITY of NORTH CAROLINA at CHAPEL HILL

Introduction to Modeling Fluid Dynamics

1

The UNIVERSITY of NORTH CAROLINA at CHAPEL HILL

2

Different Kind of Problem• Can be particles, but lots of

them• Solve instead on a uniform

grid

The UNIVERSITY of NORTH CAROLINA at CHAPEL HILL

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No Particles => New StateParticle• Mass• Velocity• Position

Fluid• Density• Velocity Field• Pressure• Viscosity

The UNIVERSITY of NORTH CAROLINA at CHAPEL HILL

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No Particles => New Equations

Navier-Stokes equations for viscous, incompressible liquids.

fuuuu

u

pt 1

0

2

The UNIVERSITY of NORTH CAROLINA at CHAPEL HILL

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What goes in must come out

Gradient of the velocity field= 0 Conservation of Mass

fuuuu

u

pt 1

0

2

The UNIVERSITY of NORTH CAROLINA at CHAPEL HILL

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Time derivative

Time derivative of velocity field Think acceleration

fuuuu

u

pt 1

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au

t

The UNIVERSITY of NORTH CAROLINA at CHAPEL HILL

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Advection term

Field is advected through itself Velocity goes with the flow

fuuuu

u

pt 1

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The UNIVERSITY of NORTH CAROLINA at CHAPEL HILL

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Diffusion term

Kinematic Viscosity times Laplacian of uDifferences in Velocity damp out

fuuuu

u

pt 1

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The UNIVERSITY of NORTH CAROLINA at CHAPEL HILL

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Pressure term

Fluid moves from high pressure to low pressureInversely proportional to fluid density,

ρ

fuuuu

u

pt 1

0

2

The UNIVERSITY of NORTH CAROLINA at CHAPEL HILL

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External Force Term

Can be or represent anythyingUsed for gravity or to let animator “stir”

fuuuu

u

pt 1

0

2

The UNIVERSITY of NORTH CAROLINA at CHAPEL HILL

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Navier-Stokes

How do we solve these equations?

fuuuu

u

pt 1

0

2

The UNIVERSITY of NORTH CAROLINA at CHAPEL HILL

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Discretizing in space and time

• We have differential equations

• We need to put them in a form we can compute

• Discetization – Finite Difference Method

The UNIVERSITY of NORTH CAROLINA at CHAPEL HILL

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Discretize in Space

X Velocity

Y Velocity

Pressure

Staggered Grid vs Regular

The UNIVERSITY of NORTH CAROLINA at CHAPEL HILL

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Discretize the operators

• Just look them up or derive them with multidimensional Taylor Expansion

• Be careful if you used a staggered grid

The UNIVERSITY of NORTH CAROLINA at CHAPEL HILL

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Example 2D Discetizations

-1 0 1

1

-1

1 -4 1

1

1

Divergence Operator

Laplacian Operator

The UNIVERSITY of NORTH CAROLINA at CHAPEL HILL

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Make a linear system

It all boils down to Ax=b.

dddd nnxnnx

b

b

x

x

x

2

1

2

1

??

??

???

The UNIVERSITY of NORTH CAROLINA at CHAPEL HILL

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Simple Linear System

• Exact solution takes O(n3) time where n is number of cells

• In 3D k3 cells where k is discretization on each axis

• Way too slow O(n9)

The UNIVERSITY of NORTH CAROLINA at CHAPEL HILL

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Need faster solver

• Our matrix is symmetric and positive definite….This means we can use♦ Conjugate Gradient

• Multigrid also an option – better asymptotic, but slower in practice.

The UNIVERSITY of NORTH CAROLINA at CHAPEL HILL

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Time Integration

• Solver gives us time derivative

• Use it to update the system state

U(t+Δt)

U t

U(t)

The UNIVERSITY of NORTH CAROLINA at CHAPEL HILL

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Discetize in Time

• Use some system such as forward Euler.

• RK methods are bad because derivatives are expensive

• Be careful of timestep

The UNIVERSITY of NORTH CAROLINA at CHAPEL HILL

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Time/Space relation?

• Courant-Friedrichs-Lewy (CFL) condition

• Comes from the advection term

u

xt

The UNIVERSITY of NORTH CAROLINA at CHAPEL HILL

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Now we have a CFD simulator

• We can simulate fluid using only the aforementioned parts so far

• This would be like Foster & Metaxas first full 3D simulator

• What if we want it real-time?

The UNIVERSITY of NORTH CAROLINA at CHAPEL HILL

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Time for Graphics Hacks

• Unconditionally stable advection♦ Kills the CFL condition

• Split the operators♦ Lets us run simpler solvers

• Impose divergence free field♦ Do as post process

The UNIVERSITY of NORTH CAROLINA at CHAPEL HILL

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Semi-lagrangian Advection

CFL Condition limits speed of information travel forward in time

Like backward Euler, what if instead we trace back in time?

p(x,t) back-trace

The UNIVERSITY of NORTH CAROLINA at CHAPEL HILL

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Divergence Free Field

• Helmholtz-Hodge Decomposition♦ Every field can be written as

• w is any vector field• u is a divergence free field• q is a scalar field

quw

The UNIVERSITY of NORTH CAROLINA at CHAPEL HILL

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Helmholtz-Hodge

STAM 2003

The UNIVERSITY of NORTH CAROLINA at CHAPEL HILL

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Divergence Free Field

• We have w and we want u

• Projection step solves this equation

q

q

q

2

2

w

uw

uw

qwu

The UNIVERSITY of NORTH CAROLINA at CHAPEL HILL

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Ensures Mass Conservation• Applied to field before

advection• Applied at the end of a step

• Takes the place of first equation in Navier-Stokes

The UNIVERSITY of NORTH CAROLINA at CHAPEL HILL

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Operator Splitting

• We can’t use semi-lagrangian advection with a Poisson solver

• We have to solve the problem in phases

• Introduces another source of error, first order approximation

The UNIVERSITY of NORTH CAROLINA at CHAPEL HILL

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Operator Splitting

0 u

uu u2 p1 ftu

The UNIVERSITY of NORTH CAROLINA at CHAPEL HILL

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Operator Splitting

1. Add External Forces

2. Semi-lagrangian advection

3. Diffusion solve

4. Project field

f

uu

u20 u

The UNIVERSITY of NORTH CAROLINA at CHAPEL HILL

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Operator Splitting

u2f

uu

W0 W1 W2 W3 W4

u(x,t)

u(x,t+Δt)

0 u

The UNIVERSITY of NORTH CAROLINA at CHAPEL HILL

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Various Extensions

• Free surface tracking• Inviscid Navier-Stokes• Solid Fluid interaction

The UNIVERSITY of NORTH CAROLINA at CHAPEL HILL

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Free Surfaces

• Level sets ♦ Loses volume♦ Poor surface detail

• Particle-level sets♦ Still loses volume♦ Osher, Stanley, & Fedkiw, 2002

• MAC grid♦ Harlow, F.H. and Welch, J.E., "Numerical

Calculation of Time-Dependent Viscous Incompressible Flow of Fluid with a Free Surface", The Physics of Fluids 8, 2182-2189 (1965).

The UNIVERSITY of NORTH CAROLINA at CHAPEL HILL

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Free Surfaces

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MAC Grid Level Set

The UNIVERSITY of NORTH CAROLINA at CHAPEL HILL

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Inviscid Navier-Stokes

• Can be run faster• Only 1 Poisson Solve needed• Useful to model smoke and

fire♦ Fedkiw, Stam, Jensen 2001

The UNIVERSITY of NORTH CAROLINA at CHAPEL HILL

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Solid Fluid Interaction

• Long history in CFD• Graphics has many papers on

1 way coupling♦ Way back to Foster & Metaxas, 1996

• Two way coupling is a new area in past 3-4 years♦ Carlson 2004

The UNIVERSITY of NORTH CAROLINA at CHAPEL HILL

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Where to get more info

• Simplest way to working fluid simulator (Even has code)♦ STAM 2003

• Best way to learn enough to be dangerous♦ CARLSON 2004

The UNIVERSITY of NORTH CAROLINA at CHAPEL HILL

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ReferencesCARLSON, M., “Rigid, Melting, and Flowing Fluid,” PhD Thesis, Georgia Institute of Technology, Jul. 2004.

FEDKIW, R., STAM, J., and JENSEN, H. W., “Visual simulation of smoke,” in Proceedings of ACM SIGGRAPH 2001, Computer Graphics Proceedings, Annual Conference Series, pp. 15–22, Aug. 2001.

FOSTER, N. and METAXAS, D., “Realistic animation of liquids,” Graphical Models and Image Processing, vol. 58, no. 5, pp. 471–483, 1996.

HARLOW, F.H. and WELCH, J.E., "Numerical Calculation of Time-Dependent Viscous Incompressible Flow of Fluid with a Free Surface", The Physics of Fluids 8, 2182-2189 (1965).

LOSASSO, F., GIBOU, F., and FEDKIW, R., “Simulating water and smoke with an octree data structure,” ACM Transactions on Graphics, vol. 23, pp. 457–462, Aug. 2004.

OSHER, STANLEY J. & FEDKIW, R. (2002). Level Set Methods and Dynamic Implicit Surfaces. Springer-Verlag.

STAM, J., “Real-time fluid dynamics for games,” in Proceedings of the Game Developer Conference, Mar. 2003.