CREEP OF FLOATING ICE SHEET.

Theory was developed for a finite length line load on an elastic plate on elastic foundation. When the solution for a finite thickness plate failed to give convergent expressions for the bending moments under the load, the solution was reduced to the case of a thin plate for which a convergent solut...

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Bibliographic Details
Main Author: Garbaccio,Donald H.
Other Authors: SCIENCE ENGINEERING ASSOCIATES INC SAN MARINO CALIF
Format: Text
Language:English
Published: 1967
Subjects:
Ice
Online Access:http://www.dtic.mil/docs/citations/AD0654742
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0654742
id ftdtic:AD0654742
record_format openpolar
spelling ftdtic:AD0654742 2023-05-15T16:37:26+02:00 CREEP OF FLOATING ICE SHEET. Garbaccio,Donald H. SCIENCE ENGINEERING ASSOCIATES INC SAN MARINO CALIF 1967-04 text/html http://www.dtic.mil/docs/citations/AD0654742 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0654742 en eng http://www.dtic.mil/docs/citations/AD0654742 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Snow Ice and Permafrost (*SEA ICE CREEP) LOADS(FORCES) ELASTIC PROPERTIES VISCOELASTICITY NUMERICAL ANALYSIS MECHANICAL PROPERTIES Text 1967 ftdtic 2016-02-18T20:14:57Z Theory was developed for a finite length line load on an elastic plate on elastic foundation. When the solution for a finite thickness plate failed to give convergent expressions for the bending moments under the load, the solution was reduced to the case of a thin plate for which a convergent solution was obtained. The correspondence principle was applied to obtain the linear viscoelastic problem. An approximate method of Laplace transform inversion was used to obtain the time dependent behavior of the creeping plate. Numerical results are presented. Theory was developed using the Hankel and Laplace transforms for a plate of finite thickness with circular symmetrical loading which was later reduced to a uniform load over a circular area. The solution is presented in a form where numerical calculations can easily be made with a digital computer. Owing to the complexity of the problem the nonlinear creep behavior of floating ice sheets was limited to a thin plate with circular symmmetry deforming with a power creep law. No numerical results were obtained but a suggested method of solution is outlined. (Author) Text Ice Ice Sheet permafrost Sea ice Defense Technical Information Center: DTIC Technical Reports database Laplace ENVELOPE(141.467,141.467,-66.782,-66.782)
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Snow
Ice and Permafrost
(*SEA ICE
CREEP)
LOADS(FORCES)
ELASTIC PROPERTIES
VISCOELASTICITY
NUMERICAL ANALYSIS
MECHANICAL PROPERTIES
spellingShingle Snow
Ice and Permafrost
(*SEA ICE
CREEP)
LOADS(FORCES)
ELASTIC PROPERTIES
VISCOELASTICITY
NUMERICAL ANALYSIS
MECHANICAL PROPERTIES
Garbaccio,Donald H.
CREEP OF FLOATING ICE SHEET.
topic_facet Snow
Ice and Permafrost
(*SEA ICE
CREEP)
LOADS(FORCES)
ELASTIC PROPERTIES
VISCOELASTICITY
NUMERICAL ANALYSIS
MECHANICAL PROPERTIES
description Theory was developed for a finite length line load on an elastic plate on elastic foundation. When the solution for a finite thickness plate failed to give convergent expressions for the bending moments under the load, the solution was reduced to the case of a thin plate for which a convergent solution was obtained. The correspondence principle was applied to obtain the linear viscoelastic problem. An approximate method of Laplace transform inversion was used to obtain the time dependent behavior of the creeping plate. Numerical results are presented. Theory was developed using the Hankel and Laplace transforms for a plate of finite thickness with circular symmetrical loading which was later reduced to a uniform load over a circular area. The solution is presented in a form where numerical calculations can easily be made with a digital computer. Owing to the complexity of the problem the nonlinear creep behavior of floating ice sheets was limited to a thin plate with circular symmmetry deforming with a power creep law. No numerical results were obtained but a suggested method of solution is outlined. (Author)
author2 SCIENCE ENGINEERING ASSOCIATES INC SAN MARINO CALIF
format Text
author Garbaccio,Donald H.
author_facet Garbaccio,Donald H.
author_sort Garbaccio,Donald H.
title CREEP OF FLOATING ICE SHEET.
title_short CREEP OF FLOATING ICE SHEET.
title_full CREEP OF FLOATING ICE SHEET.
title_fullStr CREEP OF FLOATING ICE SHEET.
title_full_unstemmed CREEP OF FLOATING ICE SHEET.
title_sort creep of floating ice sheet.
publishDate 1967
url http://www.dtic.mil/docs/citations/AD0654742
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0654742
long_lat ENVELOPE(141.467,141.467,-66.782,-66.782)
geographic Laplace
geographic_facet Laplace
genre Ice
Ice Sheet
permafrost
Sea ice
genre_facet Ice
Ice Sheet
permafrost
Sea ice
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/AD0654742
op_rights APPROVED FOR PUBLIC RELEASE
_version_ 1766027723128438784