High strain-rate compression tests on ice
High-speed uniaxial compression tests were conducted in the strain-rate range 10-1-101 s-1, at -11 C, on freshwater ice and "Baltic" sea ice of mean salinity 2.4 ± 0.7 ppt. Two different testing machines were used to check for machine stiffness effects. The results showed that for both typ...
Published in: | The Journal of Physical Chemistry B |
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1997
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Online Access: | https://doi.org/10.1021/jp963162j https://nrc-publications.canada.ca/eng/view/object/?id=d31b21de-3d53-47c2-9fd1-1ce48fa2770f https://nrc-publications.canada.ca/fra/voir/objet/?id=d31b21de-3d53-47c2-9fd1-1ce48fa2770f |
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ftnrccanada:oai:cisti-icist.nrc-cnrc.ca:cistinparc:8895950 2023-05-15T18:17:03+02:00 High strain-rate compression tests on ice Jones, S. J. 1997 text https://doi.org/10.1021/jp963162j https://nrc-publications.canada.ca/eng/view/object/?id=d31b21de-3d53-47c2-9fd1-1ce48fa2770f https://nrc-publications.canada.ca/fra/voir/objet/?id=d31b21de-3d53-47c2-9fd1-1ce48fa2770f unknown The Journal of Physical Chemistry B, Volume: 101, Issue: 32, Publication date: 1997, Pages: 6099–6101 doi:10.1021/jp963162j report_number:IR-1997-26 article 1997 ftnrccanada https://doi.org/10.1021/jp963162j 2021-09-01T06:18:58Z High-speed uniaxial compression tests were conducted in the strain-rate range 10-1-101 s-1, at -11 C, on freshwater ice and "Baltic" sea ice of mean salinity 2.4 ± 0.7 ppt. Two different testing machines were used to check for machine stiffness effects. The results showed that for both types of ice, the strength, , increased with strain rate, , consistent with a power law, = Am, where A = 8.9 and m = 0.15 for fresh water ice, and A = 6.0 and m = 0.19 for the "Baltic" sea ice. At a strain-rate of 101 s-1, the freshwater ice was a factor of only 1.3 times stronger than the sea ice. Results are compared to literature values at lower strain rates. Peer reviewed: Yes NRC publication: Yes Article in Journal/Newspaper Sea ice National Research Council Canada: NRC Publications Archive The Journal of Physical Chemistry B 101 32 6099 6101 |
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Open Polar |
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National Research Council Canada: NRC Publications Archive |
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ftnrccanada |
language |
unknown |
description |
High-speed uniaxial compression tests were conducted in the strain-rate range 10-1-101 s-1, at -11 C, on freshwater ice and "Baltic" sea ice of mean salinity 2.4 ± 0.7 ppt. Two different testing machines were used to check for machine stiffness effects. The results showed that for both types of ice, the strength, , increased with strain rate, , consistent with a power law, = Am, where A = 8.9 and m = 0.15 for fresh water ice, and A = 6.0 and m = 0.19 for the "Baltic" sea ice. At a strain-rate of 101 s-1, the freshwater ice was a factor of only 1.3 times stronger than the sea ice. Results are compared to literature values at lower strain rates. Peer reviewed: Yes NRC publication: Yes |
format |
Article in Journal/Newspaper |
author |
Jones, S. J. |
spellingShingle |
Jones, S. J. High strain-rate compression tests on ice |
author_facet |
Jones, S. J. |
author_sort |
Jones, S. J. |
title |
High strain-rate compression tests on ice |
title_short |
High strain-rate compression tests on ice |
title_full |
High strain-rate compression tests on ice |
title_fullStr |
High strain-rate compression tests on ice |
title_full_unstemmed |
High strain-rate compression tests on ice |
title_sort |
high strain-rate compression tests on ice |
publishDate |
1997 |
url |
https://doi.org/10.1021/jp963162j https://nrc-publications.canada.ca/eng/view/object/?id=d31b21de-3d53-47c2-9fd1-1ce48fa2770f https://nrc-publications.canada.ca/fra/voir/objet/?id=d31b21de-3d53-47c2-9fd1-1ce48fa2770f |
genre |
Sea ice |
genre_facet |
Sea ice |
op_relation |
The Journal of Physical Chemistry B, Volume: 101, Issue: 32, Publication date: 1997, Pages: 6099–6101 doi:10.1021/jp963162j report_number:IR-1997-26 |
op_doi |
https://doi.org/10.1021/jp963162j |
container_title |
The Journal of Physical Chemistry B |
container_volume |
101 |
container_issue |
32 |
container_start_page |
6099 |
op_container_end_page |
6101 |
_version_ |
1766191064309301248 |