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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Main Author: Jones, S. J.
Format: Report
Language:English
Published: National Research Council of Canada. Institute for Ocean Technology 2006
Subjects:
Online Access:https://dx.doi.org/10.4224/8895008
https://nrc-publications.canada.ca/eng/view/object/?id=db2dacd4-05da-46ac-9c84-991baaacfc3d
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spelling 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
institution Open Polar
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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
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