Difference between revisions of "Green Function Methods for Floating Elastic Plates"
Line 67: | Line 67: | ||
\end{matrix}</math></center> | \end{matrix}</math></center> | ||
<center><math>\begin{matrix} | <center><math>\begin{matrix} | ||
− | \left(\frac{ | + | \left(\frac{\mbox{ for } \;\;\;\; \mbox{ at } z = 0 \;\;\; \mbox{ for } x = \pm b. |
\end{matrix}</math></center> | \end{matrix}</math></center> | ||
+ | |||
+ | We will consider now the case where <math>k_y=0</math>, although the solutions presented | ||
+ | here can be generalised to the case when <math>k_y\neq 0</math>. Under this assumption | ||
+ | the equations reduce to | ||
+ | |||
+ | <center><math> | ||
+ | \phi(x) = \phi^{i}(x) + \int_{-b}^{b}G(x,\xi) | ||
+ | \left( | ||
+ | \alpha\phi(\xi) - \phi_z(\xi) | ||
+ | \right)d \xi | ||
+ | </math></center> | ||
+ | |||
+ | <center><math>\begin{matrix} | ||
+ | \left( \beta \frac{\partial^4}{\partial x^4} | ||
+ | - \gamma\alpha + 1\right)\frac{\partial \phi}{\partial z} - \alpha\phi = 0 \;\;\;\; | ||
+ | \mbox{ at } z = 0, \;\;\; -b \leq x \leq b, | ||
+ | \end{matrix}</math></center> | ||
+ | <center><math>\begin{matrix} | ||
+ | \frac{\partial^3}{\partial x^3} \frac{\partial\phi}{\partial z}= 0 \;\;\;\; \mbox{ at } z = 0 \;\;\; x = \pm b, | ||
+ | \end{matrix}</math></center> | ||
+ | <center><math>\begin{matrix} | ||
+ | \frac{\partial^2}{\partial x^2} \frac{\partial\phi}{\partial z} = 0\mbox{ for } \;\;\;\; \mbox{ at } z = 0 \;\;\; \mbox{ for } x = \pm b. | ||
+ | \end{matrix}</math></center> | ||
+ | |||
+ | == Transformation using a Green function for the plate == | ||
+ | |||
+ | We can find a function which satisfies |
Revision as of 06:53, 21 December 2006
Introduction
The problem of a two-dimensional Floating Elastic Plate was solved using a Free-Surface Green Function by Newman 1994 and Meylan and Squire 1994. We describe here both methods (which are closely related). A related paper was given by Hermans 2003 and we extended to multiple plates in Hermans 2004.
Equations of Motion
We begin with the equations of motion in non-dimensional form for a single Floating Elastic Plate which occupies the region [math]\displaystyle{ -b\leq x\leq b }[/math]. The full derivation of these equation is presented in Eigenfunction Matching Method for Floating Elastic Plates. We assume that the plate is infinite in the [math]\displaystyle{ y }[/math] direction, but we allow the wave to be incident at an angle which we do by introducing a wavenumber [math]\displaystyle{ k_y }[/math]. These means that the total potential is given by
The free-surface is at [math]\displaystyle{ z=0 }[/math] and the sea floor is at [math]\displaystyle{ z=-h }[/math]
where [math]\displaystyle{ \alpha = \omega^2 }[/math] and
Transformation Using the Green function
We use the Free-Surface Green Function for two-dimensional waves incident at an angle which we denote by [math]\displaystyle{ G(x,\zeta) }[/math] since we are only interested in its value at [math]\displaystyle{ z=0. }[/math] Using this we can transform the system of equations to
We will consider now the case where [math]\displaystyle{ k_y=0 }[/math], although the solutions presented here can be generalised to the case when [math]\displaystyle{ k_y\neq 0 }[/math]. Under this assumption the equations reduce to
Transformation using a Green function for the plate
We can find a function which satisfies