YOUNG'S MODULUS FOR SEA ICE
A study is made of the dependence of Young's modulus for small samples of sea ice on their brine content. Young's modulus is determined from the velocity of ultrasonic waves through the samples and the brine content from their salinity and temperature. It is found that, over a range of bri...
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1962
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Online Access: | http://dx.doi.org/10.1139/p62-001 http://www.nrcresearchpress.com/doi/pdf/10.1139/p62-001 |
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crcansciencepubl:10.1139/p62-001 2024-09-15T18:34:43+00:00 YOUNG'S MODULUS FOR SEA ICE Langleben, M. P. 1962 http://dx.doi.org/10.1139/p62-001 http://www.nrcresearchpress.com/doi/pdf/10.1139/p62-001 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Physics volume 40, issue 1, page 1-8 ISSN 0008-4204 1208-6045 journal-article 1962 crcansciencepubl https://doi.org/10.1139/p62-001 2024-08-15T04:09:32Z A study is made of the dependence of Young's modulus for small samples of sea ice on their brine content. Young's modulus is determined from the velocity of ultrasonic waves through the samples and the brine content from their salinity and temperature. It is found that, over a range of brine content of about 0.01 to 0.1 as a fraction of the total volume, Young's modulus decreases linearly with increasing brine content. Its value is 10.0 × 10 10 dyne cm −2 when the brine content is 0 and 6.5 × 10 10 dyne cm −2 for a brine content of 0.1. Article in Journal/Newspaper Sea ice Canadian Science Publishing Canadian Journal of Physics 40 1 1 8 |
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Open Polar |
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Canadian Science Publishing |
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crcansciencepubl |
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English |
description |
A study is made of the dependence of Young's modulus for small samples of sea ice on their brine content. Young's modulus is determined from the velocity of ultrasonic waves through the samples and the brine content from their salinity and temperature. It is found that, over a range of brine content of about 0.01 to 0.1 as a fraction of the total volume, Young's modulus decreases linearly with increasing brine content. Its value is 10.0 × 10 10 dyne cm −2 when the brine content is 0 and 6.5 × 10 10 dyne cm −2 for a brine content of 0.1. |
format |
Article in Journal/Newspaper |
author |
Langleben, M. P. |
spellingShingle |
Langleben, M. P. YOUNG'S MODULUS FOR SEA ICE |
author_facet |
Langleben, M. P. |
author_sort |
Langleben, M. P. |
title |
YOUNG'S MODULUS FOR SEA ICE |
title_short |
YOUNG'S MODULUS FOR SEA ICE |
title_full |
YOUNG'S MODULUS FOR SEA ICE |
title_fullStr |
YOUNG'S MODULUS FOR SEA ICE |
title_full_unstemmed |
YOUNG'S MODULUS FOR SEA ICE |
title_sort |
young's modulus for sea ice |
publisher |
Canadian Science Publishing |
publishDate |
1962 |
url |
http://dx.doi.org/10.1139/p62-001 http://www.nrcresearchpress.com/doi/pdf/10.1139/p62-001 |
genre |
Sea ice |
genre_facet |
Sea ice |
op_source |
Canadian Journal of Physics volume 40, issue 1, page 1-8 ISSN 0008-4204 1208-6045 |
op_rights |
http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining |
op_doi |
https://doi.org/10.1139/p62-001 |
container_title |
Canadian Journal of Physics |
container_volume |
40 |
container_issue |
1 |
container_start_page |
1 |
op_container_end_page |
8 |
_version_ |
1810476669794779136 |