Preliminary measurements of terminal crack velocity in ice
Direct measurements of ice crack velocity obtained from double cantilever beam fracture toughness specimens gave a terminal velocity of approximately 20 m/s. Fragrant size in ice is not the result of bifurcation but a consequence of the various stress fields developed. Peer reviewed: Yes NRC publica...
Published in: | Cold Regions Science and Technology |
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Format: | Article in Journal/Newspaper |
Language: | English |
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National Research Council of Canada. Institute for Marine Dynamics
1987
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ftnrccanada:oai:cisti-icist.nrc-cnrc.ca:cistinparc:8896289 2023-05-15T18:17:33+02:00 Preliminary measurements of terminal crack velocity in ice Parsons, B. L. Snellen, J. B. Hill, B. 1987 text https://nrc-publications.canada.ca/eng/view/object/?id=3559920a-d814-45e1-93cc-7b3031bb6420 https://nrc-publications.canada.ca/fra/voir/objet/?id=3559920a-d814-45e1-93cc-7b3031bb6420 eng eng National Research Council of Canada. Institute for Marine Dynamics Research Report (National Research Council of Canada. Institute for Marine Dynamics); no. RR-AVR-03, Publication date: 1987 sea ice crack velocity bifurcation article 1987 ftnrccanada 2023-01-08T00:01:31Z Direct measurements of ice crack velocity obtained from double cantilever beam fracture toughness specimens gave a terminal velocity of approximately 20 m/s. Fragrant size in ice is not the result of bifurcation but a consequence of the various stress fields developed. Peer reviewed: Yes NRC publication: Yes Article in Journal/Newspaper Sea ice National Research Council Canada: NRC Publications Archive Cold Regions Science and Technology 13 3 233 238 |
institution |
Open Polar |
collection |
National Research Council Canada: NRC Publications Archive |
op_collection_id |
ftnrccanada |
language |
English |
topic |
sea ice crack velocity bifurcation |
spellingShingle |
sea ice crack velocity bifurcation Parsons, B. L. Snellen, J. B. Hill, B. Preliminary measurements of terminal crack velocity in ice |
topic_facet |
sea ice crack velocity bifurcation |
description |
Direct measurements of ice crack velocity obtained from double cantilever beam fracture toughness specimens gave a terminal velocity of approximately 20 m/s. Fragrant size in ice is not the result of bifurcation but a consequence of the various stress fields developed. Peer reviewed: Yes NRC publication: Yes |
format |
Article in Journal/Newspaper |
author |
Parsons, B. L. Snellen, J. B. Hill, B. |
author_facet |
Parsons, B. L. Snellen, J. B. Hill, B. |
author_sort |
Parsons, B. L. |
title |
Preliminary measurements of terminal crack velocity in ice |
title_short |
Preliminary measurements of terminal crack velocity in ice |
title_full |
Preliminary measurements of terminal crack velocity in ice |
title_fullStr |
Preliminary measurements of terminal crack velocity in ice |
title_full_unstemmed |
Preliminary measurements of terminal crack velocity in ice |
title_sort |
preliminary measurements of terminal crack velocity in ice |
publisher |
National Research Council of Canada. Institute for Marine Dynamics |
publishDate |
1987 |
url |
https://nrc-publications.canada.ca/eng/view/object/?id=3559920a-d814-45e1-93cc-7b3031bb6420 https://nrc-publications.canada.ca/fra/voir/objet/?id=3559920a-d814-45e1-93cc-7b3031bb6420 |
genre |
Sea ice |
genre_facet |
Sea ice |
op_relation |
Research Report (National Research Council of Canada. Institute for Marine Dynamics); no. RR-AVR-03, Publication date: 1987 |
container_title |
Cold Regions Science and Technology |
container_volume |
13 |
container_issue |
3 |
container_start_page |
233 |
op_container_end_page |
238 |
_version_ |
1766191879825653760 |