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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Main Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
National Research Council of Canada. Institute for Marine Dynamics
1987
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Subjects: | |
Online Access: | 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 |
Summary: | 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 |
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