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contributor authorJ. C. Doering
contributor authorL. E. Bekeris
contributor authorM. P. Morris
contributor authorK. E. Dow
contributor authorW. C. Girling
date accessioned2017-05-08T21:14:04Z
date available2017-05-08T21:14:04Z
date copyrightMarch 2001
date issued2001
identifier other%28asce%290887-381x%282001%2915%3A1%2860%29.pdf
identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/43705
description abstractA counterrotating flume housed in a cold room was used to study anchor ice growth. The rate of anchor ice growth was monitored and quantified over time using a digital image processing system. The laboratory experiments were conducted over Froude numbers ranging from 0.18 to 0.76 using air temperatures of −15 and −20°C. The data suggest that the rate of anchor ice growth and the density of the resulting anchor ice have a dependence on the Froude number. The rate of anchor ice growth is observed to be a maximum at a Froude number of approximately 0.27. The qualitatively observed density of the anchor ice increases with increasing Froude number. The release of anchor ice is related to the Reynolds number; anchor ice was released for Reynolds number less than approximately 42,000, but remains attached for larger Reynolds numbers.
publisherAmerican Society of Civil Engineers
titleLaboratory Study of Anchor Ice Growth
typeJournal Paper
journal volume15
journal issue1
journal titleJournal of Cold Regions Engineering
identifier doi10.1061/(ASCE)0887-381X(2001)15:1(60)
treeJournal of Cold Regions Engineering:;2001:;Volume ( 015 ):;issue: 001
contenttypeFulltext


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