Strengthening ice through cyclic loading
ABSTRACT New experiments reveal that the flexural strength of fresh water, columnar-grained ice loaded normal to the columns may be increased by about a factor of two upon reversed cyclic loading at a frequency of ~0.1 Hz at stress amplitudes of 1.3–2.6 MPa. The effect is explained in terms of a red...
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Language: | English |
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Cambridge University Press (CUP)
2017
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Online Access: | http://dx.doi.org/10.1017/jog.2017.32 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143017000326 |
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crcambridgeupr:10.1017/jog.2017.32 2024-09-09T19:49:01+00:00 Strengthening ice through cyclic loading ILIESCU, DANIEL MURDZA, ANDRII SCHULSON, ERLAND M. RENSHAW, CARL E. 2017 http://dx.doi.org/10.1017/jog.2017.32 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143017000326 en eng Cambridge University Press (CUP) http://creativecommons.org/licenses/by/4.0/ Journal of Glaciology volume 63, issue 240, page 663-669 ISSN 0022-1430 1727-5652 journal-article 2017 crcambridgeupr https://doi.org/10.1017/jog.2017.32 2024-06-19T04:04:37Z ABSTRACT New experiments reveal that the flexural strength of fresh water, columnar-grained ice loaded normal to the columns may be increased by about a factor of two upon reversed cyclic loading at a frequency of ~0.1 Hz at stress amplitudes of 1.3–2.6 MPa. The effect is explained in terms of a reduction in deformation-induced stress concentration through the activation of grain boundary sliding, which is evident through boundary decohesion. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 63 240 663 669 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
description |
ABSTRACT New experiments reveal that the flexural strength of fresh water, columnar-grained ice loaded normal to the columns may be increased by about a factor of two upon reversed cyclic loading at a frequency of ~0.1 Hz at stress amplitudes of 1.3–2.6 MPa. The effect is explained in terms of a reduction in deformation-induced stress concentration through the activation of grain boundary sliding, which is evident through boundary decohesion. |
format |
Article in Journal/Newspaper |
author |
ILIESCU, DANIEL MURDZA, ANDRII SCHULSON, ERLAND M. RENSHAW, CARL E. |
spellingShingle |
ILIESCU, DANIEL MURDZA, ANDRII SCHULSON, ERLAND M. RENSHAW, CARL E. Strengthening ice through cyclic loading |
author_facet |
ILIESCU, DANIEL MURDZA, ANDRII SCHULSON, ERLAND M. RENSHAW, CARL E. |
author_sort |
ILIESCU, DANIEL |
title |
Strengthening ice through cyclic loading |
title_short |
Strengthening ice through cyclic loading |
title_full |
Strengthening ice through cyclic loading |
title_fullStr |
Strengthening ice through cyclic loading |
title_full_unstemmed |
Strengthening ice through cyclic loading |
title_sort |
strengthening ice through cyclic loading |
publisher |
Cambridge University Press (CUP) |
publishDate |
2017 |
url |
http://dx.doi.org/10.1017/jog.2017.32 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143017000326 |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology volume 63, issue 240, page 663-669 ISSN 0022-1430 1727-5652 |
op_rights |
http://creativecommons.org/licenses/by/4.0/ |
op_doi |
https://doi.org/10.1017/jog.2017.32 |
container_title |
Journal of Glaciology |
container_volume |
63 |
container_issue |
240 |
container_start_page |
663 |
op_container_end_page |
669 |
_version_ |
1809918383370534912 |