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dc.contributor.authorSteven F. Daly
dc.date.accessioned2017-05-08T21:13:50Z
dc.date.available2017-05-08T21:13:50Z
dc.date.copyrightMarch 1995
dc.date.issued1995
dc.identifier.other%28asce%290887-381x%281995%299%3A1%2841%29.pdf
dc.identifier.urihttp://yetl.yabesh.ir/yetl/handle/yetl/43589
dc.description.abstractThe stresses induced in ice covers by river waves are investigated as a possible mechanism for causing transverse cracks during breakup. The maximum stress levels that river waves can cause in the ice cover are determined over the entire spectrum of waves that may be present at breakup. The ice cover is analyzed as a continuous elastic plate. For a given wave amplitude, the amplitude of ice-cover bending stress has two possible maximums: one when the wavelength is equal to 2π
dc.publisherAmerican Society of Civil Engineers
dc.titleFracture of River Ice Covers by River Waves
dc.typeJournal Paper
dc.journal.volume9
dc.journal.issue1
dc.journal.titleJournal of Cold Regions Engineering
dc.identifier.doi10.1061/(ASCE)0887-381X(1995)9:1(41)
dc.treeJournal of Cold Regions Engineering:;1995:;Volume ( 009 ):;issue: 001
dc.contenttypeFulltext


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