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    Steady Flow in Porous, Elastically Deformable Materials

    Source: Journal of Applied Mechanics:;1987:;volume( 054 ):;issue: 004::page 794
    Author:
    K. H. Parker
    ,
    R. V. Mehta
    ,
    C. G. Caro
    DOI: 10.1115/1.3173119
    Publisher: The American Society of Mechanical Engineers (ASME)
    Abstract: The steady, one-dimensional flow of an incompressible fluid through a deformable porous material is studied theoretically and experimentally. The theoretical model is essentially that of Biot. Assuming that the stiffness and permeability of the matrix are functions of the local strain gradient, the governing equations can be solved and analytical solutions are presented for several simple constitutive relationships. The stiffness and permeability properties of one particular foam are measured and then used to predict the rate of fluid flow and the distortion of the matrix as a function of the applied pressure difference across the material. Comparison of the predictions of the model with experimental observations indicates good qualitative agreement.
    keyword(s): Flow (Dynamics) , Permeability , Stiffness , Pressure , Fluid dynamics , Porous materials , Equations , Functions , Gradients AND Incompressible fluids ,
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      Steady Flow in Porous, Elastically Deformable Materials

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/102005
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    contributor authorK. H. Parker
    contributor authorR. V. Mehta
    contributor authorC. G. Caro
    date accessioned2017-05-08T23:24:00Z
    date available2017-05-08T23:24:00Z
    date copyrightDecember, 1987
    date issued1987
    identifier issn0021-8936
    identifier otherJAMCAV-26288#794_1.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/102005
    description abstractThe steady, one-dimensional flow of an incompressible fluid through a deformable porous material is studied theoretically and experimentally. The theoretical model is essentially that of Biot. Assuming that the stiffness and permeability of the matrix are functions of the local strain gradient, the governing equations can be solved and analytical solutions are presented for several simple constitutive relationships. The stiffness and permeability properties of one particular foam are measured and then used to predict the rate of fluid flow and the distortion of the matrix as a function of the applied pressure difference across the material. Comparison of the predictions of the model with experimental observations indicates good qualitative agreement.
    publisherThe American Society of Mechanical Engineers (ASME)
    titleSteady Flow in Porous, Elastically Deformable Materials
    typeJournal Paper
    journal volume54
    journal issue4
    journal titleJournal of Applied Mechanics
    identifier doi10.1115/1.3173119
    journal fristpage794
    journal lastpage800
    identifier eissn1528-9036
    keywordsFlow (Dynamics)
    keywordsPermeability
    keywordsStiffness
    keywordsPressure
    keywordsFluid dynamics
    keywordsPorous materials
    keywordsEquations
    keywordsFunctions
    keywordsGradients AND Incompressible fluids
    treeJournal of Applied Mechanics:;1987:;volume( 054 ):;issue: 004
    contenttypeFulltext
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