Size And Rate Effects on the Fracture of Sea Ice.

This report contains the details of the experimental study as well as the theory applied to study the rate and size effect on the fracture of sea ice. To study the fracture of ice, experiments were carried out on a semi-circular bend fracture geometry. The test program formed a lab scale study to co...

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Bibliographic Details
Main Author: Dempsey, John P.
Other Authors: CLARKSON UNIV POTSDAM NY
Format: Text
Language:English
Published: 1996
Subjects:
Ice
Online Access:http://www.dtic.mil/docs/citations/ADA321958
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA321958
id ftdtic:ADA321958
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spelling ftdtic:ADA321958 2023-05-15T15:06:21+02:00 Size And Rate Effects on the Fracture of Sea Ice. Dempsey, John P. CLARKSON UNIV POTSDAM NY 1996-05 text/html http://www.dtic.mil/docs/citations/ADA321958 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA321958 en eng http://www.dtic.mil/docs/citations/ADA321958 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Snow Ice and Permafrost *FRACTURE(MECHANICS) *SEA ICE STRESS STRAIN RELATIONS LOAD DISTRIBUTION TENSILE STRENGTH MICROSTRUCTURE STRESS ANALYSIS DEFORMATION VISCOELASTICITY ICE MECHANICS CRACK PROPAGATION SALINITY AXIAL LOADS POLYCRYSTALLINE CREEP STRENGTH Text 1996 ftdtic 2016-02-19T19:40:22Z This report contains the details of the experimental study as well as the theory applied to study the rate and size effect on the fracture of sea ice. To study the fracture of ice, experiments were carried out on a semi-circular bend fracture geometry. The test program formed a lab scale study to complement the in-situ large-scale sea ice fracture tests. The ice used was shipped back in the form of cores from the arctic tests. Two directions of fracture, parallel to the c-axis (optical axis) and perpendicular to the c-axis are studied. To examine the rate effect, a Reversed Direct Stress (RDS) device was modified to suit rectangular shaped test specimens. The details of modifications are given. Ice samples were subjected to creep-recovery loading and allowed to recover. The resultant time dependent deformations were analyzed using nonlinear viscoelastic theory. Experimental results as well as the details of the nonlinear viscoelastic models are given. Text Arctic Ice permafrost Sea ice Defense Technical Information Center: DTIC Technical Reports database Arctic
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Snow
Ice and Permafrost
*FRACTURE(MECHANICS)
*SEA ICE
STRESS STRAIN RELATIONS
LOAD DISTRIBUTION
TENSILE STRENGTH
MICROSTRUCTURE
STRESS ANALYSIS
DEFORMATION
VISCOELASTICITY
ICE MECHANICS
CRACK PROPAGATION
SALINITY
AXIAL LOADS
POLYCRYSTALLINE
CREEP STRENGTH
spellingShingle Snow
Ice and Permafrost
*FRACTURE(MECHANICS)
*SEA ICE
STRESS STRAIN RELATIONS
LOAD DISTRIBUTION
TENSILE STRENGTH
MICROSTRUCTURE
STRESS ANALYSIS
DEFORMATION
VISCOELASTICITY
ICE MECHANICS
CRACK PROPAGATION
SALINITY
AXIAL LOADS
POLYCRYSTALLINE
CREEP STRENGTH
Dempsey, John P.
Size And Rate Effects on the Fracture of Sea Ice.
topic_facet Snow
Ice and Permafrost
*FRACTURE(MECHANICS)
*SEA ICE
STRESS STRAIN RELATIONS
LOAD DISTRIBUTION
TENSILE STRENGTH
MICROSTRUCTURE
STRESS ANALYSIS
DEFORMATION
VISCOELASTICITY
ICE MECHANICS
CRACK PROPAGATION
SALINITY
AXIAL LOADS
POLYCRYSTALLINE
CREEP STRENGTH
description This report contains the details of the experimental study as well as the theory applied to study the rate and size effect on the fracture of sea ice. To study the fracture of ice, experiments were carried out on a semi-circular bend fracture geometry. The test program formed a lab scale study to complement the in-situ large-scale sea ice fracture tests. The ice used was shipped back in the form of cores from the arctic tests. Two directions of fracture, parallel to the c-axis (optical axis) and perpendicular to the c-axis are studied. To examine the rate effect, a Reversed Direct Stress (RDS) device was modified to suit rectangular shaped test specimens. The details of modifications are given. Ice samples were subjected to creep-recovery loading and allowed to recover. The resultant time dependent deformations were analyzed using nonlinear viscoelastic theory. Experimental results as well as the details of the nonlinear viscoelastic models are given.
author2 CLARKSON UNIV POTSDAM NY
format Text
author Dempsey, John P.
author_facet Dempsey, John P.
author_sort Dempsey, John P.
title Size And Rate Effects on the Fracture of Sea Ice.
title_short Size And Rate Effects on the Fracture of Sea Ice.
title_full Size And Rate Effects on the Fracture of Sea Ice.
title_fullStr Size And Rate Effects on the Fracture of Sea Ice.
title_full_unstemmed Size And Rate Effects on the Fracture of Sea Ice.
title_sort size and rate effects on the fracture of sea ice.
publishDate 1996
url http://www.dtic.mil/docs/citations/ADA321958
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA321958
geographic Arctic
geographic_facet Arctic
genre Arctic
Ice
permafrost
Sea ice
genre_facet Arctic
Ice
permafrost
Sea ice
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/ADA321958
op_rights APPROVED FOR PUBLIC RELEASE
_version_ 1766337983819022336