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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Published in:Journal of Glaciology
Main Authors: ILIESCU, DANIEL, MURDZA, ANDRII, SCHULSON, ERLAND M., RENSHAW, CARL E.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2017
Subjects:
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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spelling 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
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