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    Water Film in Liquefied Sand and Its Effect on Lateral Spread

    Source: Journal of Geotechnical and Geoenvironmental Engineering:;1999:;Volume ( 125 ):;issue: 010
    Author:
    Takeji Kokusho
    DOI: 10.1061/(ASCE)1090-0241(1999)125:10(817)
    Publisher: American Society of Civil Engineers
    Abstract: A 1D saturated sand layer of 2 m in thickness, in which a silt seam is sandwiched, is liquefied by an instant shock. It is found that a water film is easily formed beneath the silt seam with a thickness as thin as a few millimeters just after liquefaction in loose sand and that the film lasts longer than the post-liquefaction settlement. The effect of the water film on pore-pressure distribution and sand settlement is intensively studied. 1
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      Water Film in Liquefied Sand and Its Effect on Lateral Spread

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    http://yetl.yabesh.ir/yetl1/handle/yetl/51618
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    contributor authorTakeji Kokusho
    date accessioned2017-05-08T21:26:31Z
    date available2017-05-08T21:26:31Z
    date copyrightOctober 1999
    date issued1999
    identifier other%28asce%291090-0241%281999%29125%3A10%28817%29.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/51618
    description abstractA 1D saturated sand layer of 2 m in thickness, in which a silt seam is sandwiched, is liquefied by an instant shock. It is found that a water film is easily formed beneath the silt seam with a thickness as thin as a few millimeters just after liquefaction in loose sand and that the film lasts longer than the post-liquefaction settlement. The effect of the water film on pore-pressure distribution and sand settlement is intensively studied. 1
    publisherAmerican Society of Civil Engineers
    titleWater Film in Liquefied Sand and Its Effect on Lateral Spread
    typeJournal Paper
    journal volume125
    journal issue10
    journal titleJournal of Geotechnical and Geoenvironmental Engineering
    identifier doi10.1061/(ASCE)1090-0241(1999)125:10(817)
    treeJournal of Geotechnical and Geoenvironmental Engineering:;1999:;Volume ( 125 ):;issue: 010
    contenttypeFulltext
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