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...
Main Author: | |
---|---|
Other Authors: | |
Format: | Text |
Language: | English |
Published: |
1967
|
Subjects: | |
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 |