INTERACTION THEORY FOR A FLOATING ELASTIC SHEET OF FINITE LENGTH WITH GRAVITY WAVES IN WATER OF FINITE DEPTH (INCLUDING A COMPARISON WITH EXPERIMENTAL DATA).

A theory is developed for the dynamic interaction of a floating elastic plate with incident gravity waves. The theory is two-dimensional and assumes finite dimensions for the plate and a finite depth for the water. The depth of submersion of the plate, however, is neglected. This investigation exten...

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Bibliographic Details
Main Author: Hendrickson, James A.
Other Authors: SCIENCE ENGINEERING ASSOCIATES INC SAN MARINO CALIF
Format: Text
Language:English
Published: 1966
Subjects:
Snow
Ice and Permafrost
Fluid Mechanics
(*FLOATING BODIES
ICE)
(*ICE
HYDRODYNAMICS)
WATER WAVES
STRESSES
ELASTIC PROPERTIES
FLUID DYNAMICS
TWO DIMENSIONAL FLOW
FLUID FLOW
NUMERICAL ANALYSIS
GRAVITY WAVES
Ice
permafrost
Online Access:http://www.dtic.mil/docs/citations/AD0635581
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0635581
Description
Summary:A theory is developed for the dynamic interaction of a floating elastic plate with incident gravity waves. The theory is two-dimensional and assumes finite dimensions for the plate and a finite depth for the water. The depth of submersion of the plate, however, is neglected. This investigation extends the work of previous investigations by considering the two-dimensional, finite depth aspect of the fluid flow. The theory is adapted to a numerical means of analysis and a computer program is developed to calculate the response parameters of the elastic sheet for given input parameters. Numerical results are obtained for a particular plate and water depth for four different input waves. These conditions were chosen to be the same as those for which model tests were performed under a different study. The experimental results and the theory are then compared and shown to be in reasonable agreement. (Author)

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