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    Frost Action in a Hydrophobic Material

    Source: Journal of Cold Regions Engineering:;1993:;Volume ( 007 ):;issue: 004
    Author:
    J. D. Sage
    ,
    M. Porebska
    DOI: 10.1061/(ASCE)0887-381X(1993)7:4(99)
    Publisher: American Society of Civil Engineers
    Abstract: Two series of reversed freezing tests were performed on two hydrophobic and two hydrophilic particulate materials. The tests were conducted to study the role of the adsorbed water film in the freezing and heavy process. The results demonstrate that it is possible to grow ice crystals and ice lenses in a hydrophobic material. During these reversed freezing tests, growth of ice crystals and frost heave occurred in both the hydrophobic and hydrophilic materials. Ice lenses formed as the temperature in the samples approached thermal equilibrium at 358 hours into the test. The coalescence of individual needlelike ice crystals, approximately 1 cm in length, were observed in the hydrophobic material. The experimental data suggest that frost heave occurs from the regeneration of water films on the surface of ice crystals during growth.
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      Frost Action in a Hydrophobic Material

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    contributor authorJ. D. Sage
    contributor authorM. Porebska
    date accessioned2017-05-08T21:13:49Z
    date available2017-05-08T21:13:49Z
    date copyrightDecember 1993
    date issued1993
    identifier other%28asce%290887-381x%281993%297%3A4%2899%29.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/43574
    description abstractTwo series of reversed freezing tests were performed on two hydrophobic and two hydrophilic particulate materials. The tests were conducted to study the role of the adsorbed water film in the freezing and heavy process. The results demonstrate that it is possible to grow ice crystals and ice lenses in a hydrophobic material. During these reversed freezing tests, growth of ice crystals and frost heave occurred in both the hydrophobic and hydrophilic materials. Ice lenses formed as the temperature in the samples approached thermal equilibrium at 358 hours into the test. The coalescence of individual needlelike ice crystals, approximately 1 cm in length, were observed in the hydrophobic material. The experimental data suggest that frost heave occurs from the regeneration of water films on the surface of ice crystals during growth.
    publisherAmerican Society of Civil Engineers
    titleFrost Action in a Hydrophobic Material
    typeJournal Paper
    journal volume7
    journal issue4
    journal titleJournal of Cold Regions Engineering
    identifier doi10.1061/(ASCE)0887-381X(1993)7:4(99)
    treeJournal of Cold Regions Engineering:;1993:;Volume ( 007 ):;issue: 004
    contenttypeFulltext
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