Ice Stresses in Reservoirs: Effect of Water Level Fluctuations

dc.contributor.author	E. Stander
dc.date.accessioned	2017-05-08T21:14:09Z
dc.date.available	2017-05-08T21:14:09Z
dc.date.copyright	June 2006
dc.date.issued	2006
dc.identifier.other	%28asce%290887-381x%282006%2920%3A2%2852%29.pdf
dc.identifier.uri	http://yetl.yabesh.ir/yetl/handle/yetl/43780
dc.description.abstract	Ice stress, temperature, and forebay elevation data were collected over two winter seasons from the La Gabelle reservoir, located in south-central Quebec, Canada. These data suggest that large compressive stresses can develop within confined ice sheets by the repetitive opening and freezing of shore parallel fissures. These fissures typically develop in reservoirs whose forebay elevation varies cyclically about a mean value. Stresses associated with rising water levels were on the order of
dc.publisher	American Society of Civil Engineers
dc.title	Ice Stresses in Reservoirs: Effect of Water Level Fluctuations
dc.type	Journal Paper
dc.journal.volume	20
dc.journal.issue	2
dc.journal.title	Journal of Cold Regions Engineering
dc.identifier.doi	10.1061/(ASCE)0887-381X(2006)20:2(52)
dc.tree	Journal of Cold Regions Engineering:;2006:;Volume ( 020 ):;issue: 002
dc.contenttype	Fulltext