Transcript
Page 1: AMS 691 Special Topics in Applied Mathematics Lecture 5

AMS 691Special Topics in Applied

MathematicsLecture 5

James Glimm

Department of Applied Mathematics and Statistics,

Stony Brook University

Brookhaven National Laboratory

Page 2: AMS 691 Special Topics in Applied Mathematics Lecture 5

Today

Viscosity

Ideal gas

Gamma law gas

Shock Hugoniots for gamma law gas

Rarefaction curves fro gamma law gas

Solution of Reimann problems

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

Total time derivatives

( ) particle streamline

( ) ( ) / velocity

Lagrangian time derivative

= derivative along streamline

Now consider Eulerian velocity ( , ).

On streamline, ( ( ), )

x t

v t dx t dt

D

Dt

vt x

v v x t

v v x t t

Dv

Dt

acceleration of fluid particle

v vv

t x

Page 4: AMS 691 Special Topics in Applied Mathematics Lecture 5

Euler’s EquationForces = 0

inertial force

Pressure = force per unit area

Force due to pressure =

other forces 0

S V

Dv

Dt

Pds Pdx

DvP

Dt

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

Conservation form of equationsConservation of mass

0

Conservation of momentum

other forces

v

t x

v vv

t t tv

v v P vx x

v v vP

t x

Page 6: AMS 691 Special Topics in Applied Mathematics Lecture 5

Momentum flux

( ) 0; flux of U

flux of momentum

stress tensor

Now include viscous forces. They are added to

'

' viscous stress tensor

ik ik i k ik i k

ik ik ik

ik

UF U F

tv v P

P v v v v

P

Page 7: AMS 691 Special Topics in Applied Mathematics Lecture 5

Viscous Stress Tensor

' depends on velocity gradients, not velocity itself

' is rotation invariant; assume ' linear as a function of velocity gradients

Theorem (group theory)

2'

3

C

i k i iik ik

k i i i

v v v v

x x x x

orollary: Incompressible Navier-Stokes eq. constant density

v v vP v

t x

Page 8: AMS 691 Special Topics in Applied Mathematics Lecture 5

Incompressible Navier-Stokes Equation (3D)

( )

0

dynamic viscosity

/ kinematic viscosity

density; pressure

velocity

t v v v P v

v

P

v

Page 9: AMS 691 Special Topics in Applied Mathematics Lecture 5

Two Phase NS Equationsimmiscible, Incompressible

• Derive NS equations for variable density• Assume density is constant in each phase with a jump

across the interface• Compute derivatives of all discontinuous functions using

the laws of distribution derivatives– I.e. multiply by a smooth test function and integrate formally by

parts• Leads to jump relations at the interface

– Away from the interface, use normal (constant density) NS eq.– At interface use jump relations

• New force term at interface– Surface tension causes a jump discontinuity in the pressure

proportional to the surface curvature. Proportionality constant is called surface tension

Page 10: AMS 691 Special Topics in Applied Mathematics Lecture 5

Reference for ideal fluid EOS and gamma law EOS

@Book{CouFri67, author = "R. Courant and K. Friedrichs", title = "Supersonic Flow and Shock Waves", publisher = "Springer-Verlag", address = "New York", year = "1967",}

Page 11: AMS 691 Special Topics in Applied Mathematics Lecture 5

EOS. Gamma law gas, Ideal EOS

0

0

Ideal gas:

/ (molecular weight)

universal gas constant

For an ideal gas, ( )

Tabulated values: ( ) is a polynomial in

and polynomial coefficients are tabulated (NASA tables).

Different gass

PV RT

R R

R

e e T

e T T

es have different tabulated polynomials.

Polytropic (also called Gamma law) gas:

; specific heat at constant volume

For gamma law gas, is independent of . Also

( , ) ; ( )

v v

v

e c T c

c T

P P S A A a S

Page 12: AMS 691 Special Topics in Applied Mathematics Lecture 5

Derivation of ideal EOS

( , ) , ( , )

/ ( ) 0

0

ODE for in , . Solution:

( ); exp( / ). Conclusion: depends on only.

' ( 1/ ); '; ' arbitrary

Substitute and check; O

V S

S V

s V

de TdS PdV P e S V T e S V

R PV T RT P V

Re Ve

e S V

e h VH H S R e VH

Re RVh H R Ve VHh h

DE has unique solution for given initial data. We define

1'( )

Thus depends on VH only. as function of . (This is a thermodynamic

hypothesis.) Thus is invertable; ( ); ( ) (

s

s

T e h VH VHR

T T VH

e VH VH T e h VH h

1

( )).

Thus we write as a function of . Also

'( ) '( ) .

This is the ideal EOS.V

VH T

e T

P e h VH H h H H

Page 13: AMS 691 Special Topics in Applied Mathematics Lecture 5

Gamma

12

2 2 2

The sound speed, by definition, is with

( , ) '( )

acoustic impedence

For an ideal gas,

'( / )c ( , ) ''( )

1 ( ) , where

( ) 1 ; also ( ) 1

c

dP S dh Hc H

d d

c

h HV S H h VH V H

dTR RT T RTde

dT de RT R

de dT T

specific heat at constant volume

Vc

Page 14: AMS 691 Special Topics in Applied Mathematics Lecture 5

2 2 2

2

2 2 2

( ) ''( ) 1

In fact:

'( )/

''( ) so

''( )

1

V V

V V V

dTc T h VH V H R RT

de

h VHe RT P H RT V

V

h VH VH

c h VH V H Ve VRT VP VRT

T e T TRT VR RT PVR R RT

e V e e

Page 15: AMS 691 Special Topics in Applied Mathematics Lecture 5

Proof 2 1dT

c R RTde

2

2

2 2 2

( )

(1) '( )

1'( )

(2) '( ) ''( )

''( ) by (1,2)

''( ) ( )

(1 )

V

V

V V

V V

V V

V V

e h VH

e Hh VH

T h VH VHR

RT h VH H h VH VH

e RT h VH VH

c h VH V H V e RT

dTT e

de

dTVe VR e

dedT

VP VRPdedT

RT Rde

Page 16: AMS 691 Special Topics in Applied Mathematics Lecture 5

Polytropic = gamma law EOS

1

1

( 1)

0

0

Definition: Polytropic: = is proportional to ;

( ) 1 1 .;

( ); 1 1

1 1'( ) ( ) '( )

'( ) ( )

1'( ) ( )

V

V

V V

V

V

e c T T

dTT R Rc const

de

e c T h VH Rc

T h VH VH e h VH c h VH VHR R

Rh VH h VH

c VH

VHh VH h VH h

VH H

H

additive constant in the entropy S

Page 17: AMS 691 Special Topics in Applied Mathematics Lecture 5

10( )'( ) ( 1) vc S SP h VH H e

0

0

( 1)

0

( 1)

0

( 1)

0

/ 1

( )/

( )/ 1

( 1) ( )

( ) ( 1)

; 1

( 1) V

V

V

S RV

S S c

S S c

VHe h

H

HP e V A S

H

HA S

H

H e Rc

P e

e e

Page 18: AMS 691 Special Topics in Applied Mathematics Lecture 5

Specific Enthalpy i = e +PV

2

1

For adiadic changes, 0,

.

For ideal gas, is a function of .

( ) ( ) (1 ( 1))

1 1

= specific heat at constant pressure .

; 1 ;

P

V V V

di VdP Tds

dS

dPdi VdP V d c Vd

d

i T

di d e PV d e RT R R

dT dT dT

c

dec Rc c R

dT

/ ( 1)

/ / ratio of specific heats (assuming ideal gas)1 1 P V

R Rc c

Page 19: AMS 691 Special Topics in Applied Mathematics Lecture 5

Enthalpy for a gamma law gas

( 1) ( 1)

21

2 1

1

( )1 1

( )

i e PV

AV AV

cA S

dPc A S

d

Page 20: AMS 691 Special Topics in Applied Mathematics Lecture 5

Hugoniot curve for gamma law gas

0 0

00 0 0

( )/ ( )/2 1

2 0 00 0

2 20 0 0

Recall

( , ) ( , ) ( , ) ( ) 0;2

1 1; define . ; ( 1)

1 1

12 ( , ) 2 2 ( )( )

1 1 1

( ) ( )

V VS S c S S c

P PH V P V P V P V V

PV e P e

PVPVH V P P P V V

V V P V V P

Rarefaction waves are isentropic, so to study them we studyIsentropic gas dynamics (2x2, no energy equation). is EOS.( )P P

Page 21: AMS 691 Special Topics in Applied Mathematics Lecture 5

Characteristic Curves

1

A conservation law ( ) 0 or

0; / is hyperbolic

if ( ) has all real eigenvalues

A curve ( ), ( ) in 1D space + time is characteristic

if its speed = / ( / )( / ) is an eige

t

t x

U F U

U AU A F U

A A U

x s t s

dx dt dx ds dt ds

nvalue of .

This definition depends on the solution and should hold

on the entire curve. Along the curve,

( , , ) ( , , )

For a characteristi

t x x x

A

U

dU dt dx dt dx dx dtU U A x t U U A x t U I U

ds ds ds ds ds dt ds

c curve, and for = an eigenvector, is a constant.

In general, one component of is constrained by equation along a charactersitic.xU U

U

Page 22: AMS 691 Special Topics in Applied Mathematics Lecture 5

Isentropic gas dynamics, 1D

2 2

2 2

0

Rewrite first equation as

where '( ) and '( )

0;/ /

Eigenvalues of :

State space: , : 0

Characteristic curv

xt x

t x x

xt x x x

t x

Pu uu

u u

u uu c P P c P

u uA

u c u u c u

A u c

u

es (there are two families for 2x2 system):

/: ; Eigenvectors of = transpose =

1T cdx

C u c A Adt

Page 23: AMS 691 Special Topics in Applied Mathematics Lecture 5

2

2

/

/ // /

1 1

T

T

u cA

u

c ccu cA c u

c u

Page 24: AMS 691 Special Topics in Applied Mathematics Lecture 5

Riemann Invariants

Theorem: is a constant on each curve

Proof:

.

/But = = = left eigenvector of for ei

1

t x

x

cu d C

d dU dt dxU U

ds U ds U ds ds

dx dtA I U

U dt ds

cA

U

u

genvalue .

So result is zero if .

Definition: simple wave (= rarefaction wave): is constant inside that wave.

In a simple wave, both of the 's are constant on a charactersitic,

u c

dxu c

dt

C

thus

= constant in a simple wave on a characteristic.

Equation for a simple wave: = constant, 0.

U C

dS

Page 25: AMS 691 Special Topics in Applied Mathematics Lecture 5

Centered Simple WaveA rarefaction whose straight caracteristics ( for right/left rarefaction)

all meet at a point, is called centered. Asuming that this point is the origin,

. This is a simple wave, in that =

C

xu c

t

1

constant. These two equations

define the solution at each space-time point.

For a gamma law gas, and we compute

( ) 2 2.

1 1

Starting from a right state with sound speed

r r

dPc A

d

cu d u c u c

, velocity , we have

two equations to determine , at each point. These equations define the

rarefaction wave curve.

r rc u

u c


Recommended