Comparison of the strength of iceberg and other freshwater ice and the effect of temperature
Based on literature results, the temperature of an iceberg around the Grand Banks of Newfoundland is shown to vary from -2°C at the surface to approximately -20°C at depth. This temperature variation affects the strength of the ice. The strength of iceberg ice is shown to be 1.7 times less than othe...
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National Research Council of Canada. Institute for Ocean Technology
2006
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ftdatacite:10.4224/8895008 2023-05-15T17:22:00+02:00 Comparison of the strength of iceberg and other freshwater ice and the effect of temperature Jones, S. J. 2006 https://dx.doi.org/10.4224/8895008 https://nrc-publications.canada.ca/eng/view/object/?id=db2dacd4-05da-46ac-9c84-991baaacfc3d en eng National Research Council of Canada. Institute for Ocean Technology https://dx.doi.org/10.4224/8895008 Technical report Text article-journal ScholarlyArticle 2006 ftdatacite https://doi.org/10.4224/8895008 https://doi.org/10.4224/8895008 2021-11-05T12:55:41Z Based on literature results, the temperature of an iceberg around the Grand Banks of Newfoundland is shown to vary from -2°C at the surface to approximately -20°C at depth. This temperature variation affects the strength of the ice. The strength of iceberg ice is shown to be 1.7 times less than other freshwater ice at a strain-rate of 10-³s-¹, probably due to pre-existing cracks. Using an activation energy of 80kJ/mol., the uniaxial compressive strength of iceberg ice is shown to vary from 5 MPa at -2°C near the surface, to 8 MPa at -20°C, at 10-20m depth. : Technical Report (National Research Council of Canada. Institute for Ocean Technology), No. NRC-ITO-6318 Report Newfoundland DataCite Metadata Store (German National Library of Science and Technology) Canada |
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Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
description |
Based on literature results, the temperature of an iceberg around the Grand Banks of Newfoundland is shown to vary from -2°C at the surface to approximately -20°C at depth. This temperature variation affects the strength of the ice. The strength of iceberg ice is shown to be 1.7 times less than other freshwater ice at a strain-rate of 10-³s-¹, probably due to pre-existing cracks. Using an activation energy of 80kJ/mol., the uniaxial compressive strength of iceberg ice is shown to vary from 5 MPa at -2°C near the surface, to 8 MPa at -20°C, at 10-20m depth. : Technical Report (National Research Council of Canada. Institute for Ocean Technology), No. NRC-ITO-6318 |
format |
Report |
author |
Jones, S. J. |
spellingShingle |
Jones, S. J. Comparison of the strength of iceberg and other freshwater ice and the effect of temperature |
author_facet |
Jones, S. J. |
author_sort |
Jones, S. J. |
title |
Comparison of the strength of iceberg and other freshwater ice and the effect of temperature |
title_short |
Comparison of the strength of iceberg and other freshwater ice and the effect of temperature |
title_full |
Comparison of the strength of iceberg and other freshwater ice and the effect of temperature |
title_fullStr |
Comparison of the strength of iceberg and other freshwater ice and the effect of temperature |
title_full_unstemmed |
Comparison of the strength of iceberg and other freshwater ice and the effect of temperature |
title_sort |
comparison of the strength of iceberg and other freshwater ice and the effect of temperature |
publisher |
National Research Council of Canada. Institute for Ocean Technology |
publishDate |
2006 |
url |
https://dx.doi.org/10.4224/8895008 https://nrc-publications.canada.ca/eng/view/object/?id=db2dacd4-05da-46ac-9c84-991baaacfc3d |
geographic |
Canada |
geographic_facet |
Canada |
genre |
Newfoundland |
genre_facet |
Newfoundland |
op_relation |
https://dx.doi.org/10.4224/8895008 |
op_doi |
https://doi.org/10.4224/8895008 https://doi.org/10.4224/8895008 |
_version_ |
1766108188429516800 |