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...
Published in: | Geophysical Research Letters |
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Main Authors: | , , , |
Other Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Wiley
2022
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Subjects: | |
Online Access: | https://aaltodoc.aalto.fi/handle/123456789/116966 https://doi.org/10.1029/2022GL099771 |
_version_ | 1828685479336214528 |
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author | Murdza, Andrii Schulson, Erland M. Renshaw, Carl E. Polojarvi, Arttu |
author2 | Department of Energy and Mechanical Engineering Solid Mechanics Dartmouth College Aalto-yliopisto Aalto University |
author_facet | Murdza, Andrii Schulson, Erland M. Renshaw, Carl E. Polojarvi, Arttu |
author_sort | Murdza, Andrii |
collection | Aalto University Publication Archive (Aaltodoc) |
container_issue | 17 |
container_title | Geophysical Research Letters |
container_volume | 49 |
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 |
format | Article in Journal/Newspaper |
genre | Arctic Sea ice |
genre_facet | Arctic Sea ice |
geographic | Arctic |
geographic_facet | Arctic |
id | ftaaltouniv:oai:aaltodoc.aalto.fi:123456789/116966 |
institution | Open Polar |
language | English |
op_collection_id | ftaaltouniv |
op_doi | https://doi.org/10.1029/2022GL099771 |
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 PURE FILEURL: https://research.aalto.fi/files/88419649/Geophysical_Research_Letters_2022_Murdza_Rapid_Healing_of_Thermal_Cracks_in_Ice.pdf PURE LINK: http://www.scopus.com/inward/record.url?scp=85137980211&partnerID=8YFLogxK https://aaltodoc.aalto.fi/handle/123456789/116966 doi:10.1029/2022GL099771 |
op_rights | openAccess |
publishDate | 2022 |
publisher | Wiley |
record_format | openpolar |
spelling | ftaaltouniv:oai:aaltodoc.aalto.fi:123456789/116966 2025-04-06T14:45:27+00:00 Rapid Healing of Thermal Cracks in Ice Murdza, Andrii Schulson, Erland M. Renshaw, Carl E. Polojarvi, Arttu Department of Energy and 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 Wiley 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 PURE FILEURL: https://research.aalto.fi/files/88419649/Geophysical_Research_Letters_2022_Murdza_Rapid_Healing_of_Thermal_Cracks_in_Ice.pdf PURE LINK: http://www.scopus.com/inward/record.url?scp=85137980211&partnerID=8YFLogxK https://aaltodoc.aalto.fi/handle/123456789/116966 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 2025-03-10T01:16:29Z 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 Arctic Sea ice Aalto University Publication Archive (Aaltodoc) Arctic Geophysical Research Letters 49 17 |
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 |
title | 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_short | Rapid Healing of Thermal Cracks in Ice |
title_sort | rapid healing of thermal cracks in ice |
topic | ice cracks healing fracture SEA-ICE OCEAN WAVES BEHAVIOR |
topic_facet | ice cracks healing fracture SEA-ICE OCEAN WAVES BEHAVIOR |
url | https://aaltodoc.aalto.fi/handle/123456789/116966 https://doi.org/10.1029/2022GL099771 |