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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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 |
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1766027755942576128 |