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    Immiscible Displacement Model for Anisotropic and Correlated Porous Media

    Source: International Journal of Geomechanics:;2007:;Volume ( 007 ):;issue: 004
    Author:
    Franco M. Francisca
    ,
    Pedro Arduino
    DOI: 10.1061/(ASCE)1532-3641(2007)7:4(311)
    Publisher: American Society of Civil Engineers
    Abstract: Immiscible flow governs the macroscopic behavior of aqueous and non-aqueous phase liquids inside the porous media. Ganglia generation and movement of the advancing front during fluid displacement can only be described by means of microscopic models. In this study, a pore network cellular automata is used to simulate the displacement of a nonaqueous phase liquid by water inside a porous media. Pore sizes are generated using random and stochastic fields. The numerical model captures the evolution of interfaces and fluid movement for each pressure applied to the displacing fluid. Observed trends suggest that ganglia size and shape, and fingering are directly related to anisotropy, pore size spatial variability and correlation length. The results show that micro- and mesoscale porous media properties control the nonaqueous phase residual saturation and observed macoscopic behavior.
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      Immiscible Displacement Model for Anisotropic and Correlated Porous Media

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    http://yetl.yabesh.ir/yetl1/handle/yetl/55117
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    contributor authorFranco M. Francisca
    contributor authorPedro Arduino
    date accessioned2017-05-08T21:32:03Z
    date available2017-05-08T21:32:03Z
    date copyrightJuly 2007
    date issued2007
    identifier other%28asce%291532-3641%282007%297%3A4%28311%29.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/55117
    description abstractImmiscible flow governs the macroscopic behavior of aqueous and non-aqueous phase liquids inside the porous media. Ganglia generation and movement of the advancing front during fluid displacement can only be described by means of microscopic models. In this study, a pore network cellular automata is used to simulate the displacement of a nonaqueous phase liquid by water inside a porous media. Pore sizes are generated using random and stochastic fields. The numerical model captures the evolution of interfaces and fluid movement for each pressure applied to the displacing fluid. Observed trends suggest that ganglia size and shape, and fingering are directly related to anisotropy, pore size spatial variability and correlation length. The results show that micro- and mesoscale porous media properties control the nonaqueous phase residual saturation and observed macoscopic behavior.
    publisherAmerican Society of Civil Engineers
    titleImmiscible Displacement Model for Anisotropic and Correlated Porous Media
    typeJournal Paper
    journal volume7
    journal issue4
    journal titleInternational Journal of Geomechanics
    identifier doi10.1061/(ASCE)1532-3641(2007)7:4(311)
    treeInternational Journal of Geomechanics:;2007:;Volume ( 007 ):;issue: 004
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian