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    Injection of Fluid Into a Layer of Deformable Porous Medium

    Source: Applied Mechanics Reviews:;1995:;volume( 048 ):;issue: 010::page 722
    Author:
    Steven Barry
    ,
    Geoffrey Aldis
    ,
    Geoffry Mercer
    DOI: 10.1115/1.3005054
    Publisher: The American Society of Mechanical Engineers (ASME)
    Abstract: The flow of fluid from a point source into a layer of deformable porous material is considered. The main applications of this work are to subcutaneous injections and subterranean soil flows. The porous material is assumed to be an isotropic, homogeneous, linearly elastic solid. The governing equations are derived for an axisymmetric geometry using linear poro-elasticity and are applied to the situation of a point source at some height z = z0 with a line sink at a distance r = ρ. These are solved analytically using Hankel transform techniques with the Hankel inversion integrals calculated numerically. Results are given for the pressure contours and the displacement of the solid matrix for a variety of source heights and elastic parameters. These indicate the swelling of the medium and subsequent deformation of the free surface. Results indicate regions where one dimensional models may be applicable.
    keyword(s): Fluids , Porous materials , Flow (Dynamics) , Elasticity , Deformation , Pressure , Displacement , Equations , Geometry AND Soil ,
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      Injection of Fluid Into a Layer of Deformable Porous Medium

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    https://yetl.yabesh.ir/yetl1/handle/yetl/114716
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    contributor authorSteven Barry
    contributor authorGeoffrey Aldis
    contributor authorGeoffry Mercer
    date accessioned2017-05-08T23:46:09Z
    date available2017-05-08T23:46:09Z
    date copyrightOctober, 1995
    date issued1995
    identifier issn0003-6900
    identifier otherAMREAD-25696#722_1.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/114716
    description abstractThe flow of fluid from a point source into a layer of deformable porous material is considered. The main applications of this work are to subcutaneous injections and subterranean soil flows. The porous material is assumed to be an isotropic, homogeneous, linearly elastic solid. The governing equations are derived for an axisymmetric geometry using linear poro-elasticity and are applied to the situation of a point source at some height z = z0 with a line sink at a distance r = ρ. These are solved analytically using Hankel transform techniques with the Hankel inversion integrals calculated numerically. Results are given for the pressure contours and the displacement of the solid matrix for a variety of source heights and elastic parameters. These indicate the swelling of the medium and subsequent deformation of the free surface. Results indicate regions where one dimensional models may be applicable.
    publisherThe American Society of Mechanical Engineers (ASME)
    titleInjection of Fluid Into a Layer of Deformable Porous Medium
    typeJournal Paper
    journal volume48
    journal issue10
    journal titleApplied Mechanics Reviews
    identifier doi10.1115/1.3005054
    journal fristpage722
    journal lastpage726
    identifier eissn0003-6900
    keywordsFluids
    keywordsPorous materials
    keywordsFlow (Dynamics)
    keywordsElasticity
    keywordsDeformation
    keywordsPressure
    keywordsDisplacement
    keywordsEquations
    keywordsGeometry AND Soil
    treeApplied Mechanics Reviews:;1995:;volume( 048 ):;issue: 010
    contenttypeFulltext
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