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11/14/2014 PHY 711  Fall 2014 -- Lecture 34 11/14/2014 PHY 711  Fall 2014 -- Lecture 34

11/14/2014 PHY 711 Fall 2014 -- Lecture 34 - PowerPoint Presentation

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11/14/2014 PHY 711 Fall 2014 -- Lecture 34 - PPT Presentation

1 PHY 7 11 Classical Mechanics and Mathematical Methods 101050 AM MWF Olin 103 Plan for Lecture 34 Chapter 10 in F amp W Surface waves Nonlinear contributions and soliton ID: 636393

phy 2014 711 lecture 2014 phy lecture 711 fall surface equation equations terms linear derivatives order velocity soliton waves

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Slide1

11/14/2014

PHY 711 Fall 2014 -- Lecture 34

1

PHY

7

11 Classical Mechanics and Mathematical Methods

10-10:50 AM MWF Olin 103

Plan for Lecture

34:

Chapter 10 in F & W: Surface waves

-- Non-linear contributions and

soliton

solutionsSlide2

11/14/2014

PHY 711 Fall 2014 -- Lecture 34

2Slide3

11/14/2014

PHY 711 Fall 2014 -- Lecture 34

3

p

0

h

z

x

z

y

General problem

including

non-

linearities

Surface waves in an incompressible fluidSlide4

11/14/2014

PHY 711 Fall 2014 -- Lecture 34

4

p

0

h

z

x

z

ySlide5

11/14/2014

PHY 711 Fall 2014 -- Lecture 34

5

p

0

h

z

x

z

y

z=0

Non-linear effects in surface waves:Slide6

11/14/2014

PHY 711 Fall 2014 -- Lecture 34

6

Detailed analysis of non-linear surface waves

[Note

that these

derivations

follow

Alexander

L. Fetter and John Dirk

Walecka

,

Theoretical

Mechanics of Particles and

Continua (McGraw Hill, 1980), Chapt. 10

.]

The surface of the fluid is described by

z=

h+z(

x,t). It is assumed that the fluid is contained in a structure (lake, river, swimming pool, etc

.) with a structureless bottom defined by the z =

0 plane and filled to an equilibrium height of z = h.Slide7

11/14/2014

PHY 711 Fall 2014 -- Lecture 34

7

Defining equations for

F

(

x,z,t

)

and

z

(

x,t

)

Bernoulli equation (assuming

irrotational

flow) and gravitation

potential energySlide8

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PHY 711 Fall 2014 -- Lecture 34

8

Boundary conditions on functions –

Zero velocity at bottom of tank:

Consistent vertical velocity at water surfaceSlide9

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PHY 711 Fall 2014 -- Lecture 34

9

Analysis assuming water height

z

is

small relative to

variations in the direction of wave

motion

(x)

Taylor’s expansion about

z

=

0:

Note that the zero vertical velocity at the bottom ensures that all odd derivatives

vanish

from

the

Taylor expansion . In addition, the Laplace equation allows us to convert all even derivatives with respect to

z

to derivatives with respect to x.Slide10

11/14/2014

PHY 711 Fall 2014 -- Lecture 34

10

Check linearized equations and their solutions:

Bernoulli equations --

Using Taylor's expansion results to lowest orderSlide11

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PHY 711 Fall 2014 -- Lecture 34

11

Analysis of non-linear equations --

keeping

the lowest order nonlinear terms and include up

to 4th

order derivatives in the linear terms.

The expressions keep the lowest order nonlinear terms and include up

to 4th

order derivatives in the linear terms

.Slide12

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PHY 711 Fall 2014 -- Lecture 34

12

Note that the wave

“speed”

c

will be consistently determinedSlide13

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PHY 711 Fall 2014 -- Lecture 34

13

Integrating and re-arranging coupled equationsSlide14

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PHY 711 Fall 2014 -- Lecture 34

14

Integrating and re-arranging coupled equations – continued --

Expressing modified surface velocity equation in terms of

h

(u):Slide15

11/14/2014

PHY 711 Fall 2014 -- Lecture 34

15

Solution of the famous

Korteweg

-de

Vries

equation

Modified surface

amplitude

equation in terms

of

h

Soliton

solutionSlide16

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PHY 711 Fall 2014 -- Lecture 34

16

Relationship

to “standard”

form

of

Korteweg

-de

Vries

equationSlide17

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PHY 711 Fall 2014 -- Lecture 34

17

More detailsSlide18

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PHY 711 Fall 2014 -- Lecture 34

18

Soliton

solution

SummarySlide19

11/14/2014

PHY 711 Fall 2014 -- Lecture 34

19

Some links:

Website

http://www.ma.hw.ac.uk/solitons/

Photo of canal

soliton

http://www.ma.hw.ac.uk/solitons/