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:
Ice
Online Access:http://www.dtic.mil/docs/citations/AD0635581
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0635581
id ftdtic:AD0635581
record_format openpolar
spelling ftdtic:AD0635581 2023-05-15T16:37:28+02:00 INTERACTION THEORY FOR A FLOATING ELASTIC SHEET OF FINITE LENGTH WITH GRAVITY WAVES IN WATER OF FINITE DEPTH (INCLUDING A COMPARISON WITH EXPERIMENTAL DATA). Hendrickson, James A. SCIENCE ENGINEERING ASSOCIATES INC SAN MARINO CALIF 1966-04 text/html http://www.dtic.mil/docs/citations/AD0635581 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0635581 en eng http://www.dtic.mil/docs/citations/AD0635581 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS 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 Text 1966 ftdtic 2016-02-18T19:15:18Z 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) Text Ice permafrost Defense Technical Information Center: DTIC Technical Reports database
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic 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
spellingShingle 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
Hendrickson, James A.
INTERACTION THEORY FOR A FLOATING ELASTIC SHEET OF FINITE LENGTH WITH GRAVITY WAVES IN WATER OF FINITE DEPTH (INCLUDING A COMPARISON WITH EXPERIMENTAL DATA).
topic_facet 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
description 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)
author2 SCIENCE ENGINEERING ASSOCIATES INC SAN MARINO CALIF
format Text
author Hendrickson, James A.
author_facet Hendrickson, James A.
author_sort Hendrickson, James A.
title INTERACTION THEORY FOR A FLOATING ELASTIC SHEET OF FINITE LENGTH WITH GRAVITY WAVES IN WATER OF FINITE DEPTH (INCLUDING A COMPARISON WITH EXPERIMENTAL DATA).
title_short INTERACTION THEORY FOR A FLOATING ELASTIC SHEET OF FINITE LENGTH WITH GRAVITY WAVES IN WATER OF FINITE DEPTH (INCLUDING A COMPARISON WITH EXPERIMENTAL DATA).
title_full INTERACTION THEORY FOR A FLOATING ELASTIC SHEET OF FINITE LENGTH WITH GRAVITY WAVES IN WATER OF FINITE DEPTH (INCLUDING A COMPARISON WITH EXPERIMENTAL DATA).
title_fullStr INTERACTION THEORY FOR A FLOATING ELASTIC SHEET OF FINITE LENGTH WITH GRAVITY WAVES IN WATER OF FINITE DEPTH (INCLUDING A COMPARISON WITH EXPERIMENTAL DATA).
title_full_unstemmed INTERACTION THEORY FOR A FLOATING ELASTIC SHEET OF FINITE LENGTH WITH GRAVITY WAVES IN WATER OF FINITE DEPTH (INCLUDING A COMPARISON WITH EXPERIMENTAL DATA).
title_sort interaction theory for a floating elastic sheet of finite length with gravity waves in water of finite depth (including a comparison with experimental data).
publishDate 1966
url http://www.dtic.mil/docs/citations/AD0635581
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0635581
genre Ice
permafrost
genre_facet Ice
permafrost
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/AD0635581
op_rights APPROVED FOR PUBLIC RELEASE
_version_ 1766027755942576128