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    One‐Dimensional Shock and Quasi‐Static Liquefaction of Silt and Sand

    Source: Journal of Geotechnical Engineering:;1994:;Volume ( 120 ):;issue: 010
    Author:
    Jane M. Bolton
    ,
    Deanna S. Durnford
    ,
    Wayne A. Charlie
    DOI: 10.1061/(ASCE)0733-9410(1994)120:10(1874)
    Publisher: American Society of Civil Engineers
    Abstract: This paper summarizes the results of undrained quasi‐static and shock compression tests performed on confined specimens of saturated Bonny Silt, Monterey No. 0/30 sand, and a mixture of the two soils. The tests evaluated pore pressure response and liquefaction potential of sand, silt and silty‐sand subjected to high intensity compressive loading. The quasi‐static tests consisted of load cycles of increasing magnitude and the shock tests consisted of millisecond compressive wave loadings. Shock and quasi‐static induced excess pore pressures were approximately equal when the sand was subjected to equal peak strains. The silt and the mixture exhibited significantly higher increases in excess pore pressure under quasi‐static loading than under shock loading for the same peak strain. The pore‐pressure ratio of the three soil types increased with increasing peak strain, with decreasing effective stress, and with increasing void ratio.
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      One‐Dimensional Shock and Quasi‐Static Liquefaction of Silt and Sand

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    contributor authorJane M. Bolton
    contributor authorDeanna S. Durnford
    contributor authorWayne A. Charlie
    date accessioned2017-05-08T20:37:04Z
    date available2017-05-08T20:37:04Z
    date copyrightOctober 1994
    date issued1994
    identifier other%28asce%290733-9410%281994%29120%3A10%281874%29.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/21340
    description abstractThis paper summarizes the results of undrained quasi‐static and shock compression tests performed on confined specimens of saturated Bonny Silt, Monterey No. 0/30 sand, and a mixture of the two soils. The tests evaluated pore pressure response and liquefaction potential of sand, silt and silty‐sand subjected to high intensity compressive loading. The quasi‐static tests consisted of load cycles of increasing magnitude and the shock tests consisted of millisecond compressive wave loadings. Shock and quasi‐static induced excess pore pressures were approximately equal when the sand was subjected to equal peak strains. The silt and the mixture exhibited significantly higher increases in excess pore pressure under quasi‐static loading than under shock loading for the same peak strain. The pore‐pressure ratio of the three soil types increased with increasing peak strain, with decreasing effective stress, and with increasing void ratio.
    publisherAmerican Society of Civil Engineers
    titleOne‐Dimensional Shock and Quasi‐Static Liquefaction of Silt and Sand
    typeJournal Paper
    journal volume120
    journal issue10
    journal titleJournal of Geotechnical Engineering
    identifier doi10.1061/(ASCE)0733-9410(1994)120:10(1874)
    treeJournal of Geotechnical Engineering:;1994:;Volume ( 120 ):;issue: 010
    contenttypeFulltext
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