Fracture criterion for ice using a dislocation model

The propensity for crack formation on basal and prismatic planes and twin nucleation on two pyramidal planes in hexagonal ice is examined on the basis of fracture theories and anisotropic elastic theories of dislocations. Calculations show that the ease of crack formation is almost the same in the b...

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Bibliographic Details
Main Author: Parameswaran, V. R.
Format: Article in Journal/Newspaper
Language:English
Published: 1982
Subjects:
ice
Online Access:https://nrc-publications.canada.ca/eng/view/ft/?id=91ff5448-65df-4697-a8d0-1c9ddc6804d3
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spelling ftnrccanada:oai:cisti-icist.nrc-cnrc.ca:cistinparc:20378608 2024-09-15T18:15:40+00:00 Fracture criterion for ice using a dislocation model Parameswaran, V. R. 1982 text https://nrc-publications.canada.ca/eng/view/ft/?id=91ff5448-65df-4697-a8d0-1c9ddc6804d3 https://nrc-publications.canada.ca/eng/view/object/?id=91ff5448-65df-4697-a8d0-1c9ddc6804d3 https://nrc-publications.canada.ca/fra/voir/objet/?id=91ff5448-65df-4697-a8d0-1c9ddc6804d3 eng eng issn:0022-1430 Journal of Glaciology, Volume: 28, Issue: 98, Publication date: 1982, Pages: 161–169 report_number:DBR-P-1035 ice glace crackings (breaking) fissuration dislocation elastic analysis domaine élastique stresses contrainte hexagonal ice crack formation basal and prismatic planes article 1982 ftnrccanada 2024-08-05T14:05:07Z The propensity for crack formation on basal and prismatic planes and twin nucleation on two pyramidal planes in hexagonal ice is examined on the basis of fracture theories and anisotropic elastic theories of dislocations. Calculations show that the ease of crack formation is almost the same in the basal and prismatic planes, whereas it is almost impossible to produce mechanical twinning in ice by stress alone. Sur la base des théories de la fracture et des théories élastiques anisotropiques des dislocations on examine les possibilités pour la formation de fissures sur les plans de base et sur les faces pyramidales ainsi que la nucléation des macles sur deux faces pyramidales dans de la glace hexagonale. Les calculs montrent que la formation de fissure est presque aussi facile sur le plan de base et sur les faces prismatiques, alors qu'il est presque impossible de produire des macles dans la glace par le seul exercice d'un effort mécanique. Peer reviewed: Yes NRC publication: Yes Article in Journal/Newspaper Journal of Glaciology National Research Council Canada: NRC Publications Archive
institution Open Polar
collection National Research Council Canada: NRC Publications Archive
op_collection_id ftnrccanada
language English
topic ice
glace
crackings (breaking)
fissuration
dislocation
elastic analysis
domaine élastique
stresses
contrainte
hexagonal ice
crack formation
basal and prismatic planes
spellingShingle ice
glace
crackings (breaking)
fissuration
dislocation
elastic analysis
domaine élastique
stresses
contrainte
hexagonal ice
crack formation
basal and prismatic planes
Parameswaran, V. R.
Fracture criterion for ice using a dislocation model
topic_facet ice
glace
crackings (breaking)
fissuration
dislocation
elastic analysis
domaine élastique
stresses
contrainte
hexagonal ice
crack formation
basal and prismatic planes
description The propensity for crack formation on basal and prismatic planes and twin nucleation on two pyramidal planes in hexagonal ice is examined on the basis of fracture theories and anisotropic elastic theories of dislocations. Calculations show that the ease of crack formation is almost the same in the basal and prismatic planes, whereas it is almost impossible to produce mechanical twinning in ice by stress alone. Sur la base des théories de la fracture et des théories élastiques anisotropiques des dislocations on examine les possibilités pour la formation de fissures sur les plans de base et sur les faces pyramidales ainsi que la nucléation des macles sur deux faces pyramidales dans de la glace hexagonale. Les calculs montrent que la formation de fissure est presque aussi facile sur le plan de base et sur les faces prismatiques, alors qu'il est presque impossible de produire des macles dans la glace par le seul exercice d'un effort mécanique. Peer reviewed: Yes NRC publication: Yes
format Article in Journal/Newspaper
author Parameswaran, V. R.
author_facet Parameswaran, V. R.
author_sort Parameswaran, V. R.
title Fracture criterion for ice using a dislocation model
title_short Fracture criterion for ice using a dislocation model
title_full Fracture criterion for ice using a dislocation model
title_fullStr Fracture criterion for ice using a dislocation model
title_full_unstemmed Fracture criterion for ice using a dislocation model
title_sort fracture criterion for ice using a dislocation model
publishDate 1982
url https://nrc-publications.canada.ca/eng/view/ft/?id=91ff5448-65df-4697-a8d0-1c9ddc6804d3
https://nrc-publications.canada.ca/eng/view/object/?id=91ff5448-65df-4697-a8d0-1c9ddc6804d3
https://nrc-publications.canada.ca/fra/voir/objet/?id=91ff5448-65df-4697-a8d0-1c9ddc6804d3
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_relation issn:0022-1430
Journal of Glaciology, Volume: 28, Issue: 98, Publication date: 1982, Pages: 161–169
report_number:DBR-P-1035
_version_ 1810453597290233856