Strengthening ice through cyclic loading

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...

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Main Authors: DANIEL ILIESCU, ANDRII MURDZA, ERLAND M. SCHULSON, CARL E. RENSHAW
Format: Article
Language:English
Published: Cambridge University Press 2017-08-01
Series:Journal of Glaciology
Subjects:
Online Access:https://www.cambridge.org/core/product/identifier/S0022143017000326/type/journal_article
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author DANIEL ILIESCU
ANDRII MURDZA
ERLAND M. SCHULSON
CARL E. RENSHAW
author_facet DANIEL ILIESCU
ANDRII MURDZA
ERLAND M. SCHULSON
CARL E. RENSHAW
author_sort DANIEL ILIESCU
collection DOAJ
description 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.
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spelling doaj.art-4e27d5a08de443f5baa1b0a85f19d7932023-03-09T12:40:27ZengCambridge University PressJournal of Glaciology0022-14301727-56522017-08-016366366910.1017/jog.2017.32Strengthening ice through cyclic loadingDANIEL ILIESCU0ANDRII MURDZA1ERLAND M. SCHULSON2CARL E. RENSHAW3Ice Research Laboratory, Thayer School of Engineering, Dartmouth College, Hanover, NH 03755, USAIce Research Laboratory, Thayer School of Engineering, Dartmouth College, Hanover, NH 03755, USAIce Research Laboratory, Thayer School of Engineering, Dartmouth College, Hanover, NH 03755, USAIce Research Laboratory, Thayer School of Engineering, Dartmouth College, Hanover, NH 03755, USANew 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.https://www.cambridge.org/core/product/identifier/S0022143017000326/type/journal_articleice engineeringice physicsice rheology
spellingShingle DANIEL ILIESCU
ANDRII MURDZA
ERLAND M. SCHULSON
CARL E. RENSHAW
Strengthening ice through cyclic loading
Journal of Glaciology
ice engineering
ice physics
ice rheology
title 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_short Strengthening ice through cyclic loading
title_sort strengthening ice through cyclic loading
topic ice engineering
ice physics
ice rheology
url https://www.cambridge.org/core/product/identifier/S0022143017000326/type/journal_article
work_keys_str_mv AT danieliliescu strengtheningicethroughcyclicloading
AT andriimurdza strengtheningicethroughcyclicloading
AT erlandmschulson strengtheningicethroughcyclicloading
AT carlerenshaw strengtheningicethroughcyclicloading