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    Ice Stresses in Reservoirs: Effect of Water Level Fluctuations

    Source: Journal of Cold Regions Engineering:;2006:;Volume ( 020 ):;issue: 002
    Author:
    E. Stander
    DOI: 10.1061/(ASCE)0887-381X(2006)20:2(52)
    Publisher: American Society of Civil Engineers
    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
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      Ice Stresses in Reservoirs: Effect of Water Level Fluctuations

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    https://yetl.yabesh.ir/yetl1/handle/yetl/43780
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    contributor authorE. Stander
    date accessioned2017-05-08T21:14:09Z
    date available2017-05-08T21:14:09Z
    date copyrightJune 2006
    date issued2006
    identifier other%28asce%290887-381x%282006%2920%3A2%2852%29.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/43780
    description abstractIce 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
    publisherAmerican Society of Civil Engineers
    titleIce Stresses in Reservoirs: Effect of Water Level Fluctuations
    typeJournal Paper
    journal volume20
    journal issue2
    journal titleJournal of Cold Regions Engineering
    identifier doi10.1061/(ASCE)0887-381X(2006)20:2(52)
    treeJournal of Cold Regions Engineering:;2006:;Volume ( 020 ):;issue: 002
    contenttypeFulltext
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