Difference between revisions of "Green Function Methods for Floating Elastic Plates"
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using a [[Free-Surface Green Function]] by [[Newman 1994]] and [[Meylan and Squire 1994]]. We describe | using a [[Free-Surface Green Function]] by [[Newman 1994]] and [[Meylan and Squire 1994]]. We describe | ||
here both methods (which are closely related). | here both methods (which are closely related). | ||
− | A related paper was given by [[Hermans 2003]]and we extended to | + | A related paper was given by [[Hermans 2003]] and we extended to |
multiple plates in [[Hermans 2004]]. | multiple plates in [[Hermans 2004]]. | ||
Revision as of 08:48, 19 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