Difference between revisions of "Generalized Eigenfunction Expansion for Water Waves for a Fixed Body"

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= Outline of the theory =
 
= Outline of the theory =
  
We consider the case of a rigid body in water of finite depth. We can solve  
+
We consider the case of a rigid body in water of finite depth. The time-dependent equations
 +
of motion are
 +
<math>\nabla^2 \phi = 0</math>
 +
<math>\phi_n + \frac{\omega^2}{g} \phi  = 0, x\in F</math>
 +
<math>\phi_n  = 0, x\in F</math>
 +
 
 +
 
 +
We can solve  
 
the single frequency problem with frequency <math>\omega</math> for an incident wave  
 
the single frequency problem with frequency <math>\omega</math> for an incident wave  
 
travelling from <math>-\infty</math>
 
travelling from <math>-\infty</math>
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to obtain a solution <math>\phi(\omega,x)</math>. This looks like an incident plus reflected
 
to obtain a solution <math>\phi(\omega,x)</math>. This looks like an incident plus reflected
wave as <math>x\to\-infty</math> and like a transmitted
+
wave as <math> x\to -\infty</math> and like a transmitted wave as <math> x\to -\infty</math>.
 +
We call these solutions generalised eigenfunctions.
 +
We then try and expand the solution in terms of this solutions (which we call the generalised
 +
eigenfunctions) because they solve for

Revision as of 05:08, 18 April 2006

This page is under construction.


The theory of generalised eigenfunction is described in Hazard and Lenoir 2002 and Meylan 2002 for the case of a rigid body in water of infinite depth and for a thin plate on water of shallow draft respectively. We will present here the theory for a rigid body in water of finite depth.

Outline of the theory

We consider the case of a rigid body in water of finite depth. The time-dependent equations of motion are [math]\displaystyle{ \nabla^2 \phi = 0 }[/math] [math]\displaystyle{ \phi_n + \frac{\omega^2}{g} \phi = 0, x\in F }[/math] [math]\displaystyle{ \phi_n = 0, x\in F }[/math]


We can solve the single frequency problem with frequency [math]\displaystyle{ \omega }[/math] for an incident wave travelling from [math]\displaystyle{ -\infty }[/math]

[math]\displaystyle{ \phi^i = e^{i \omega x} }[/math]

to obtain a solution [math]\displaystyle{ \phi(\omega,x) }[/math]. This looks like an incident plus reflected wave as [math]\displaystyle{ x\to -\infty }[/math] and like a transmitted wave as [math]\displaystyle{ x\to -\infty }[/math]. We call these solutions generalised eigenfunctions. We then try and expand the solution in terms of this solutions (which we call the generalised eigenfunctions) because they solve for