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AMS 691 Special Topics in Applied Mathematics Lecture 3 James Glimm Department of Applied Mathematics and Statistics, Stony Brook University Brookhaven National Laboratory

AMS 691 Special Topics in Applied Mathematics Lecture 3

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Partial Differential Equations (PDEs) and Laws of Physics Many laws of physics are expressed in terms of partial differential equations Many types and varieties of partial differential equations. Often nonlinear. Usually to be solved numerically, with some insight from theory We have looked at nonlinear hyperbolic conservation laws. One basic class of physical laws. A broader classification: hyperbolic, parabolic, elliptic This is not the entire universe of PDEs, but is representative of many. Most common PDEs from physics will be one of these or a combination Combination: many problems are put together by combining subproblems.

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Page 1: AMS 691 Special Topics in Applied Mathematics Lecture 3

AMS 691Special Topics in Applied

MathematicsLecture 3

James GlimmDepartment of Applied Mathematics

and Statistics,Stony Brook University

Brookhaven National Laboratory

Page 2: AMS 691 Special Topics in Applied Mathematics Lecture 3

Partial Differential Equations (PDEs) and Laws of Physics

Many laws of physics are expressed in terms of partial differential equations

Many types and varieties of partial differential equations.

Often nonlinear. Usually to be solved numerically, with some insight from theory

We have looked at nonlinear hyperbolic conservation laws. One basic class of physical laws.

A broader classification: hyperbolic, parabolic, ellipticThis is not the entire universe of PDEs, but is representative of many.Most common PDEs from physics will be one of these or a combination

Combination: many problems are put together by combining subproblems.

Page 3: AMS 691 Special Topics in Applied Mathematics Lecture 3

Research Issues

Many PDEs areNonlinearMultiple equations combined (multiphysics)To be solved numericallyMultiscale, meaning that many different length scales are

coupled

Because nonlinear, numerical solutions are neededBecause multiscale, numerical solutions are difficult, and require

large scale computationsBecause multiphysics, accuracy and stability of coupling is important

Page 4: AMS 691 Special Topics in Applied Mathematics Lecture 3

Hyperbolic EquationsThe wave equation is the basic example of a hyperbolic equation.

2 0Rewrite as a first order system

0( ) 0

Differentiate first equation with respect to t, second equation with respect to x, and add:Get ( ) . Equation for isentopic gas dynamic

tt

t x

t x

tt xx

U c U

v uu p v

v p v

2

2 2

s.

Linearize: - '( )Solutions (1 space dimension): ( ), ( )

Substitute, get '' '' 0General solution: specify Cauchy data , at 0. Find

( ) ( ) (= general solution) from Caucht

p v c vU x ct U x ct

c U c UU U t

f x ct g x ct

y data.Reference: Smoller Shock Waves and Reaction Diffusion EquationsChapter 3, 17

Page 5: AMS 691 Special Topics in Applied Mathematics Lecture 3

Nonlinear Hyperbolic Conservation Laws

2

2

Wave equation:0 1

00

0 1 acoustic matrix

0Nonlinear:

( ) 00; ( ) /

Linearize: independent of

t x

t

t

U Uc

Ac

U F UU A U A F U U

A U

Page 6: AMS 691 Special Topics in Applied Mathematics Lecture 3

Parabolic, Elliptic EquationsHyperbolic processes govern wave motionParabolic equations govern diffusion processes,Elliptic equations govern time independent phenomena,

either hyperbolic or parabolic

Multiphysics: hyperbolic + parabolic (+ elliptic)Some processes are combined wave motion and diffusionSome processes may be time independent, while others are not.

Mathematical theory and numerical methods for parabolic/elliptic arevery different from those for hyperbolic

Since we have two or three types of terms in a single equation, we needmultiple solution methods.

Multiscale (example): parabolic term has small coefficient, important in thin layers only.

Page 7: AMS 691 Special Topics in Applied Mathematics Lecture 3

Typical equation forms2

2Elliptic: = 0

Parabolic: (heat or diffusion equation)Physical diffusion processes:Thermal, mass concentration, momentumThermal diffusion in the energy equationMass diffusion in a specie

i i

t

UUx

U U

s concentration equationMomentum diffusion (viscosity) in the momentum equation

Page 8: AMS 691 Special Topics in Applied Mathematics Lecture 3

Parabolic equationsFundamental solution: Gaussian and erf (= indefinite integral of Gaussian)

22 /( )

( )

2( )

( , ) fundamental solution of heat equation2

2( , 0) ( ) Dirac delta function at

( , ) = constant on parabolas ( ) / .

Diffusive information propagates

x y ty

y y

y

tf x t e

f ftf x t x x y

f x t x y t const

0

0 ( )

0

like General solution, with initial data ( ) is

( ) ( ) ( , )

( ) ( , ) solution of parabolic Riemann problem

(data = 1, y > 0)

y

x

tf x

f x f y f x t

efr x f y t dy

Page 9: AMS 691 Special Topics in Applied Mathematics Lecture 3

Fluid Transport• The Euler equations neglect dissipative

mechanisms• Corrections to the Euler equations are given by

the Navier Stokes equations• These change order and type. The extra terms

involve a second order spatial derivative (Laplacian). Thus the equations become parabolic. Discontinuities are removed, to be replaced by steep gradients. Equations are now parabolic, not hyperbolic. New types of solution algorithms may be needed.

Page 10: AMS 691 Special Topics in Applied Mathematics Lecture 3

Numerical Solution forHyperbolic + Parabolic:

Operator Splitting( )

At every time step, solve two equations in succession:( ) 0

First step with hyperbolic methods; second step with parabolic methods

t

t

t

U F U U

U F UU U

Page 11: AMS 691 Special Topics in Applied Mathematics Lecture 3

Fluid Transport• Single species

– Viscosity = rate of diffusion of momentum• Driven to momentum or velocity gradients

– Thermal conductivity = rate of diffusion of temperature• Driven by temperature gradients: Fourier’s law

• Multiple species– Mass diffusion = rate of diffusion of a single species in

a mixture• Driven by concentration gradients• Exact theory is very complicated. We consider a simple

approximation: Fickean diffusion

Page 12: AMS 691 Special Topics in Applied Mathematics Lecture 3

Comments• Why study the Euler equations if the Navier-

Stokes equations are more exact (better)?– Often too expensive to solve the Navier-Stokes

equations numerically– Often the Euler equations are “nearly” right, in that

often the transport coefficients are small, so that the Euler equations provide a useful intellectual framework

– Often the numerical methods have a hybrid character, part reflecting the needs of the hyperbolic terms and part reflecting the needs of the parabolic part.

Page 13: AMS 691 Special Topics in Applied Mathematics Lecture 3

Navier-Stokes Equationsfor Compressible Fluids

( ) is a (2+D)x(2+D) block diagonal matrix,

entries only in the momentum andenergy equations.For multiple species, also entries foreach species concentration equation.

tU F U U

Page 14: AMS 691 Special Topics in Applied Mathematics Lecture 3

Incompressible Navier-Stokes Equation (3D)

( )tv v v P v

Page 15: AMS 691 Special Topics in Applied Mathematics Lecture 3

Turbulent mixing for a jet in crossflow and plans

for turbulent combustion simulations

Page 16: AMS 691 Special Topics in Applied Mathematics Lecture 3

The Team/Collaborators• Stony Brook University

– James Glimm– Xiaolin Li– Xiangmin Jiao– Yan Yu– Ryan Kaufman– Ying Xu– Vinay Mahadeo– Hao Zhang– Hyunkyung Lim

• College of St. Elizabeth– Srabasti Dutta

• Los Alamos National Laboratory– David H. Sharp– John Grove– Bradley Plohr– Wurigen Bo– Baolian Cheng

Page 17: AMS 691 Special Topics in Applied Mathematics Lecture 3

Outline of Presentation• Problem specification and dimensional analysis

– Experimental configuration– HyShot II configuration

• Plans for combustion simulations– Fine scale simulations for V&V purposes– HyShot II simulation plans

• Stanford simulation results

Page 18: AMS 691 Special Topics in Applied Mathematics Lecture 3

Scramjet Project

– Collaborated Work including Stanford PSAAP Center, Stony Brook University and University of Michigan

Page 19: AMS 691 Special Topics in Applied Mathematics Lecture 3

Proposed Plan on UQ/QMU• Decompose the large complex system into

several subsystems

• UQ/QMU on subsystems

• Assemble UQ/QMU of subsystems to get the UQ/QMU for the full system

• Sub-system analysis goal: UQ/QMU for the essential subsystem --- combustor

Page 20: AMS 691 Special Topics in Applied Mathematics Lecture 3

Proposed Plan on UQ/QMU (continued)

• Our hypothesis is that an engineered system has a natural decomposition into subsystems, and the safe operation of the full system depends on a limited number of variables in the operation of the subsystems.

• For the scramjet, with its supersonic flow velocity, a natural time like decomposition is achieved, with each subsystem getting information from the previous one and giving it to the next.

• In this context, we hope that the number of variables to be specified at the boundaries between subsystems will be not too large. To show this in the scramjet context will be a research program, and central to the success of our objectives.

• We call the boundaries between the subsystems to be gates. Or rather the boundary and the specification of the criteria to be satisfied there is the gate.