| Author | Search for: Parsons, B. L.; Search for: Snellen, J. B.; Search for: Hill, B. |
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| Format | Text, Article |
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| Subject | sea ice; crack velocity; bifurcation |
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| Abstract | 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. |
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| Publication date | 1987 |
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| Publisher | National Research Council of Canada. Institute for Marine Dynamics |
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| Series | |
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| Reprint of | |
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| Language | English |
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| Peer reviewed | Yes |
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| NRC number | NRC-IOT-5198 |
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| NPARC number | 8896289 |
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| Export citation | Export as RIS |
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| Report a correction | Report a correction (opens in a new tab) |
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| Record identifier | 3559920a-d814-45e1-93cc-7b3031bb6420 |
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| Record created | 2009-04-22 |
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| Record modified | 2023-01-06 |
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