+ All Categories
Home > Documents > II Nonlinear wave equations

II Nonlinear wave equations

Date post: 14-Jan-2016
Category:
Upload: millie
View: 53 times
Download: 0 times
Share this document with a friend
Description:
II Nonlinear wave equations. 2.1 Introduction. Introduction Solitary waves Korteweg-deVries (KdV) equation Nonlinear Schrodinger equation. Introduction Linear wave equations. Simplest (second order) linear wave equation u tt – c 2 u xx = 0 D’Alembert’s solution - PowerPoint PPT Presentation
34
II Nonlinear wave equations • Introduction Solitary waves Korteweg-deVries (KdV) equation Nonlinear Schrodinger equation 2.1 Introduction
Transcript
Page 1: II Nonlinear wave equations

II Nonlinear wave equations

• Introduction• Solitary waves• Korteweg-deVries (KdV) equation• Nonlinear Schrodinger equation

2.1 Introduction

Page 2: II Nonlinear wave equations

• Simplest (second order) linear wave equation

utt – c2uxx = 0

• D’Alembert’s solution

u(x,t) = f(x-ct) + g(x+ct)f, g arbitrary functionsDispersionlessDissipationlessDispersion relation = ck

IntroductionLinear wave equations

Page 3: II Nonlinear wave equations

IntroductionLinear wave equations

• Simplest Linear

ut – cux = 0 or ut + cux = 0

u(x,t) = f(x+ct) or u(x,t) = f(x-ct)• Simplest Dispersive, Dissipationless

ut + cux + auxxx = 0

u(x,t) = exp[i(kx – t)]

= ck - ak3 • Simplest Nondispersive, Dissipative

ut + cux - auxx = 0

u(x,t) = exp[i(kx – t)]

= ck – iak2

Page 4: II Nonlinear wave equations

IntroductionNonlinear wave equations

• Simplest Nonlinearut + (1+u)ux = 0u(x,t) = f(x-(1+u)t)Sharpens at leading and trailing edges (shock formation)

• Korteweg deVries (KdV) Equation (1895)

ut + (1+u)ux + uxxx = 0

Solitary wave/soliton behaviour

Dispersion and tendency to shock formation in balance

o

2 x-ct -x ( 2

c sech

2

c t)u(x,

Page 5: II Nonlinear wave equations

2.2 Solitary waves

Over one hundred and fifty years ago, while conducting experiments to determine the most efficient design for canal boats, a young Scottish engineer named John Scott Russell (1808-1882) made a remarkable scientific discovery.Here is an extract fromJohn Scott Russell’s ‘Report on waves’ 

Page 6: II Nonlinear wave equations

Solitary wavesRussell’s report on waves

 “I was observing the motion of a boat which was rapidly drawn along a narrow channel by a pair of horses, when the boat suddenly stopped - not so the mass of water in the channel which it had put in motion; it accumulated round the prow of the vessel in a state of violent agitation, then suddenly leaving it behind, rolled forward with great velocity, assuming the form of a large solitary elevation, a rounded, smooth and well-defined heap of water, which continued its course along the channel apparently without change of form or diminution of speed. I followed it on horseback, and overtook it still rolling on at a rate of some eight or nine miles an hour, preserving its original figure some thirty feet long and a foot to a foot and a half in height. Its height gradually diminished, and after a chase of one or two miles I lost it in the windings of the channel. Such, in the month of August 1834, was my first chance interview with that singular and beautiful phenomenon which I have called the Wave of Translation”.

Page 7: II Nonlinear wave equations

• The wave of translation (or solitary wave) observed by John Scott Russell is described by a nonlinear wave equation known as the Korteweg-deVries (KdV) equation.

• We review various possible types of nonlinearity in wave equations before studying two specific equations – the KdV and the nonlinear Schrodinger (NLS) equations.

0 u 6uu -u xxxxt

2.3 Korteweg deVries (KdV) equation

Page 8: II Nonlinear wave equations

'wave.dat'

0 20 40 60 80 100 120 14000.511.522.533.54

-0.20

0.20.40.60.81

1.21.41.61.8

Korteweg deVries (KdV) equation Numerical solution (strong dispersive term)

Page 9: II Nonlinear wave equations

'wave.dat'

0 20 40 60 80 100 120 14000.511.522.533.54

-0.200.20.40.60.811.2

1.41.61.82

Korteweg deVries (KdV) equation Numerical solution (weak dispersive term)

Page 10: II Nonlinear wave equations

Korteweg deVries (KdV) equation Effect of nonlinear term ut = -(1+u)ux

The sequence of plots at t = 0, t and 2t illustrate how a pulse forms and splits off from theleading edge of a smooth front.

2 4 6 8 10

-1

-0.5

0.5

1

1.5

ux(0)

-(1+u(0))ux(0)u(0)

2 4 6 8 10

-1

-0.5

0.5

1

1.5

ux(t)

-(1+u(t))ux(t)u(t)

2 4 6 8 10

-1

-0.5

0.5

1

1.5

u(2t)

Page 11: II Nonlinear wave equations

Korteweg deVries (KdV) equation Effect of dispersive term ut = - uxxx

2 4 6 8 10

-1

-0.5

0.5

1

1.5

u(0)-uxxx(0)

2 4 6 8 10

-1

-0.5

0.5

1

1.5

u(0) u(t)

2 4 6 8 10

-1

-0.5

0.5

1

1.5

u(2t)

Combined effects of nonlinear and dispersive terms

Page 12: II Nonlinear wave equations

Korteweg deVries (KdV) equation Soliton simulations

These simulations come from Klaus Brauer's webpage (Osnabrück)

Page 13: II Nonlinear wave equations

Korteweg deVries (KdV) equationSolution for PBC and sinusoidal initial conditions

This animation by K. Takasaki shows the sinusoidal initial state breaking up into a soliton train. Zabusky and Kruskal (1966).

Page 14: II Nonlinear wave equations

Korteweg deVries (KdV) equation Analytic solution

•KdV equation

•Let the solution be u = u(x,t) and consider a change of variables = x – ct and = t

•Call the function in new variables f()

•The change in u or f brought about by translations (dx, dt) or () is

dt ddt c -dx d d f d f df

dt tu dx

xu du

0u6uuu xxxxt

Page 15: II Nonlinear wave equations

• If we convert the change in f brought about by translations through (dx, dt) into changes in f brought about by translations through (dx, dt)

•Since u and f represent the same function the same translation (dx, dt) must produce the same change in either. Hence

Korteweg deVries (KdV) equation Analytic solution

dt fc- f dx f df

dt f dt c -dx f df

fc- f tu

f xu

Page 16: II Nonlinear wave equations

Korteweg deVries (KdV) equation Analytic solution

• When transforming the pde from (x, t) to () we must make the replacements

• In the (x, t) variables a soliton moves along the x axis as time advances

•In the () variables a soliton is stationary in time provided we choose c in the transformation to be the soliton velocity

c- t

x

Page 17: II Nonlinear wave equations

•The conventional form for the KdV equation is  •Travelling wave solutions have the form

  c is the wave velocity

 •Substituting for u in the KdV equation and setting the time derivative to zero we obtain     

Korteweg deVries (KdV) equation Analytic solution

0 f 6ff -cf-

0 u 6uu -u xxxxt

ct - x )f( t)u(x,

Page 18: II Nonlinear wave equations

Korteweg deVries (KdV) equation Analytic solution

B Af f2

c f f

2

1

B Af f2

1 f -f

2

c-

Afd f 3f -cf-fd

A f 3f -cf-

0 f 6ff -cf-d

232

232

2

2

•Integrate twice wrt

Page 19: II Nonlinear wave equations

Korteweg deVries (KdV) equation Analytic solution

• A and B are constants of integration. In order to have a localised traveling wave packet, we impose boundary conditions: all tend to zero as || goes to infinity.

• To ensure these conditions we set A = B = 0. Solutions also exist at zeros of the polynomial in f.

• The solution with A = B = 0 obeys

• Rearrange to

f,ff,

c 2ff f 22

d c 2ff

df

Page 20: II Nonlinear wave equations

Korteweg deVries (KdV) equation Analytic solution

dc

2-

tanhc sech 2

c-

tanh sech cd

becomes c 2ff

df

22

2

• Make change of variable

2sech 2

c- f

c

x

c

2 o

• Last term on rhs is constant of integration

Page 21: II Nonlinear wave equations

Korteweg deVries (KdV) equation Analytic solution

• Rearrange to

• Make back substitution

o

2 x-ct -x ( 2

c sech

2

c f

tanh sech - sech d

d

ee

2 sech

o x- 2

c

Page 22: II Nonlinear wave equations

2.4 Nonlinear Schrödinger equation

• The naming of the nonlinear Schrödinger (NLS) equation becomes obvious when it is compared to the time-dependent Schrödinger equation from quantum mechanics

• The NLS can be derived for wave packets localised in k space for systems where the dispersion relation depends on wave intensity ) (k,

2

0 ψ V xxψ2m

tψi

0 ψψ Q xxψ P tiψ2

2

Page 24: II Nonlinear wave equations

Nonlinear Schrödinger equationDerivation from dispersion relation

...

...)k(kk

ω

2!

1 )k(k

k

ω ω- ω

2

2

2o

o

2

2

o

o

o

2o

• The NLS is derived from the dispersion relation for the envelope function which has a slow time variation cf the carrier waves

• Suppose that the dispersion relationship isMake a Taylor expansion of this about ko and zero intensity

) (k, 2

Page 25: II Nonlinear wave equations

Nonlinear Schrödinger equationDerivation from dispersion relation

2

oψ,

o

2ψ2

o,

o

2

2

2

o,

og

oo

ω

ω Q

ωk

ω 2P

ωk

ω

v

k– k K ω - ω Ω

• Let

• Then the Taylor expanded dispersion relation becomes

22g Q PK K v

Page 26: II Nonlinear wave equations

Nonlinear Schrödinger equationDerivation from dispersion relation

• Consider a wavepacket constructed from a small group of waves in slow variables X = x, T = t <<1

vecarrier wa*ddK -

)]T

- KX

exp[i( )(K, T)(X,

t)]-xexp[i(k* ddK -

)]T

- KX

exp[i( )(K,

ddk -

t)] -exp[i(kx )(k, t)(x,

oo

• The latter is the envelope function in ‘slow’ variables X,T

Page 27: II Nonlinear wave equations

Nonlinear Schrödinger equationDerivation from dispersion relation

T i

i

T

X iK

iK

X

T)(X,iK

ddK -

)]T

- KX

exp[i( )(K,iK

ddK -

)]T

- KX

exp[i( )(K,X

T)(X,X

Page 28: II Nonlinear wave equations

Nonlinear Schrödinger equationDerivation from dispersion relation

22g Q PK K v

• The dispersion relation

becomes

22XX

2XgT

222

g

QPvi- i

QX

i-PX

i- vT

i

g

g

v T

X

T Tv-X• Make further change of variables

Page 29: II Nonlinear wave equations

Nonlinear Schrödinger equationDerivation from dispersion relation

22XX

2XgT QPvi- i

becomes

0qi

0QPi

2

2

• This is the conventional form for the NLS equation. It has an envelope solution with a sech profile. (See handout)

Page 30: II Nonlinear wave equations

31-nn

3n1n1nn1nn )u(u)u(uAK)uu2K(uum

Nonlinear Schrödinger equationApplication to lattice dynamics

• Hooke’s Law plus additional nonlinear term

3

42

AKr -Krdr

dU(r)- F(r)

r4

AK Kr

2

1 U(r)

• Equation of motion

• Solution and dispersion relation

2

kasinR6A1

2

kasin

m

K2ω

c.c. t)]-exp[i(kna Ru

22

n

Page 31: II Nonlinear wave equations

Nonlinear Schrödinger equationApplication to lattice dynamics

• We have just seen that introduction of a nonlinear term in the force law for a 1-D chain of atoms leads to a dispersion relation which depends on |R|2. At the website below, use the monatomic chain applet to see some of these localised modes.

•Intrinsic localised modes in lattice dynamics of crystals

0.5 1 1.5 2 2.5 3

k

0.2

0.4

0.6

0.8

1

2

kasin

m

K2ω

2

kasinR6A1

2

kasin

m

K2ω 22

Page 32: II Nonlinear wave equations

Nonlinear Schrödinger equationApplication to lattice dynamics

• Click on monatomic 1-D chains and then on the link in the title to the page (works best with Internet Explorer)

•You will find stationary ILM with

• envelope function (c.f. solutions of NLS equation) is composed of groups of waves centred on the Brillouin zone boundary (k = ) (group velocity zero)

• moving ILM composed of groups of waves centred away from the Brillouin zone boundary (group velocity nonzero)

Page 33: II Nonlinear wave equations

Nonlinear Schrödinger equationApplication to lattice dynamics

• You will also find

• molecular dynamics simulations showing ILM in 3-D crystals (click on 3-D Ionic crystals)

•Simulations showing ILM in 1-D chains of interacting spins

Page 34: II Nonlinear wave equations

Nonlinear Schrödinger equationApplication to optical communications

• Read the introductory articles on

• Solitons in optical communications by Ablowitz et al.

• Historical aspects of optical solitons by Hasegawa

• Soliton propagation in optical fibres


Recommended