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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Published in:Geophysical Research Letters
Main Authors: Murdza, Andrii, Schulson, Erland M., Renshaw, Carl E., Polojarvi, Arttu
Other Authors: Department of Energy and Mechanical Engineering, Solid Mechanics, Dartmouth College, Aalto-yliopisto, Aalto University
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2022
Subjects:
Online Access:https://aaltodoc.aalto.fi/handle/123456789/116966
https://doi.org/10.1029/2022GL099771
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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
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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
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doi:10.1029/2022GL099771
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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