Rapid Healing of Thermal Cracks in Ice
The structural integrity of the arctic sea ice cover is under threat owing largely to the combination of thinning and larger waves. Another contributor may be thermal cracking. In concentrating stress, thermal cracks may weaken the cover. Of interest, therefore, is the strength of thermally damaged...
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AMERICAN GEOPHYSICAL UNION
2022
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Online Access: | https://aaltodoc.aalto.fi/handle/123456789/116966 https://doi.org/10.1029/2022GL099771 |
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ftaaltouniv:oai:aaltodoc.aalto.fi:123456789/116966 2024-04-21T08:11:14+00:00 Rapid Healing of Thermal Cracks in Ice Murdza, Andrii Schulson, Erland M. Renshaw, Carl E. Polojarvi, Arttu Department of Mechanical Engineering Solid Mechanics Dartmouth College Aalto-yliopisto Aalto University 2022-09-16 6 application/pdf https://aaltodoc.aalto.fi/handle/123456789/116966 https://doi.org/10.1029/2022GL099771 en eng AMERICAN GEOPHYSICAL UNION Geophysical Research Letters Volume 49, issue 17 Murdza, A, Schulson, E M, Renshaw, C E & Polojarvi, A 2022, ' Rapid Healing of Thermal Cracks in Ice ', Geophysical Research Letters, vol. 49, no. 17, e2022GL099771 . https://doi.org/10.1029/2022GL099771 0094-8276 1944-8007 PURE UUID: 21412095-695e-4114-ab7d-f244233e0b78 PURE ITEMURL: https://research.aalto.fi/en/publications/21412095-695e-4114-ab7d-f244233e0b78 PURE LINK: http://www.scopus.com/inward/record.url?scp=85137980211&partnerID=8YFLogxK PURE FILEURL: https://research.aalto.fi/files/88419649/Geophysical_Research_Letters_2022_Murdza_Rapid_Healing_of_Thermal_Cracks_in_Ice.pdf https://aaltodoc.aalto.fi/handle/123456789/116966 URN:NBN:fi:aalto-202209285762 doi:10.1029/2022GL099771 openAccess ice cracks healing fracture SEA-ICE OCEAN WAVES BEHAVIOR A1 Alkuperäisartikkeli tieteellisessä aikakauslehdessä publishedVersion 2022 ftaaltouniv https://doi.org/10.1029/2022GL099771 2024-03-27T17:56:18Z The structural integrity of the arctic sea ice cover is under threat owing largely to the combination of thinning and larger waves. Another contributor may be thermal cracking. In concentrating stress, thermal cracks may weaken the cover. Of interest, therefore, is the strength of thermally damaged ice. To that end, new experiments were performed on sea ice and on lab-grown saline and salt-free ice that had been cracked by thermal shocking. As expected, the cracks weakened the materials in accord with fracture mechanics. However, within tens to hundreds of seconds of shocking, the strength recovered completely, for the ice had healed. Healing is attributed to thermally activated sintering related to surface diffusion, assisted possibly by the formation of a quasi-liquid layer on crack faces. Whether behavior on the small scale is indicative of behavior on the large scale remains to be determined. Peer reviewed Article in Journal/Newspaper Sea ice Aalto University Publication Archive (Aaltodoc) Geophysical Research Letters 49 17 |
institution |
Open Polar |
collection |
Aalto University Publication Archive (Aaltodoc) |
op_collection_id |
ftaaltouniv |
language |
English |
topic |
ice cracks healing fracture SEA-ICE OCEAN WAVES BEHAVIOR |
spellingShingle |
ice cracks healing fracture SEA-ICE OCEAN WAVES BEHAVIOR Murdza, Andrii Schulson, Erland M. Renshaw, Carl E. Polojarvi, Arttu Rapid Healing of Thermal Cracks in Ice |
topic_facet |
ice cracks healing fracture SEA-ICE OCEAN WAVES BEHAVIOR |
description |
The structural integrity of the arctic sea ice cover is under threat owing largely to the combination of thinning and larger waves. Another contributor may be thermal cracking. In concentrating stress, thermal cracks may weaken the cover. Of interest, therefore, is the strength of thermally damaged ice. To that end, new experiments were performed on sea ice and on lab-grown saline and salt-free ice that had been cracked by thermal shocking. As expected, the cracks weakened the materials in accord with fracture mechanics. However, within tens to hundreds of seconds of shocking, the strength recovered completely, for the ice had healed. Healing is attributed to thermally activated sintering related to surface diffusion, assisted possibly by the formation of a quasi-liquid layer on crack faces. Whether behavior on the small scale is indicative of behavior on the large scale remains to be determined. Peer reviewed |
author2 |
Department of Mechanical Engineering Solid Mechanics Dartmouth College Aalto-yliopisto Aalto University |
format |
Article in Journal/Newspaper |
author |
Murdza, Andrii Schulson, Erland M. Renshaw, Carl E. Polojarvi, Arttu |
author_facet |
Murdza, Andrii Schulson, Erland M. Renshaw, Carl E. Polojarvi, Arttu |
author_sort |
Murdza, Andrii |
title |
Rapid Healing of Thermal Cracks in Ice |
title_short |
Rapid Healing of Thermal Cracks in Ice |
title_full |
Rapid Healing of Thermal Cracks in Ice |
title_fullStr |
Rapid Healing of Thermal Cracks in Ice |
title_full_unstemmed |
Rapid Healing of Thermal Cracks in Ice |
title_sort |
rapid healing of thermal cracks in ice |
publisher |
AMERICAN GEOPHYSICAL UNION |
publishDate |
2022 |
url |
https://aaltodoc.aalto.fi/handle/123456789/116966 https://doi.org/10.1029/2022GL099771 |
genre |
Sea ice |
genre_facet |
Sea ice |
op_relation |
Geophysical Research Letters Volume 49, issue 17 Murdza, A, Schulson, E M, Renshaw, C E & Polojarvi, A 2022, ' Rapid Healing of Thermal Cracks in Ice ', Geophysical Research Letters, vol. 49, no. 17, e2022GL099771 . https://doi.org/10.1029/2022GL099771 0094-8276 1944-8007 PURE UUID: 21412095-695e-4114-ab7d-f244233e0b78 PURE ITEMURL: https://research.aalto.fi/en/publications/21412095-695e-4114-ab7d-f244233e0b78 PURE LINK: http://www.scopus.com/inward/record.url?scp=85137980211&partnerID=8YFLogxK PURE FILEURL: https://research.aalto.fi/files/88419649/Geophysical_Research_Letters_2022_Murdza_Rapid_Healing_of_Thermal_Cracks_in_Ice.pdf https://aaltodoc.aalto.fi/handle/123456789/116966 URN:NBN:fi:aalto-202209285762 doi:10.1029/2022GL099771 |
op_rights |
openAccess |
op_doi |
https://doi.org/10.1029/2022GL099771 |
container_title |
Geophysical Research Letters |
container_volume |
49 |
container_issue |
17 |
_version_ |
1796952950252240896 |