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    Waves in Partially Saturated Medium Due to Surface Loads

    Source: Journal of Engineering Mechanics:;1988:;Volume ( 114 ):;issue: 010
    Author:
    A. J. Philippacopoulos
    DOI: 10.1061/(ASCE)0733-9399(1988)114:10(1740)
    Publisher: American Society of Civil Engineers
    Abstract: A two‐layered continuum in which the underlying half‐space is a fluid‐saturated porous (two‐phased) medium is considered. A comprehensive analysis is made of the disturbance produced in this continuum by time harmonic normal point loads acting at the surface. Integral solutions for the surface displacements are derived. Viscoelastic‐type behavior is assumed for the layer, while the behavior of the half‐space follows Biot's small strain theory for poro‐viscoelastic media. Attenuation of the dilatational and the shear waves in the layer and in the skeletal frame of the fluid‐saturated porous half‐space is assumed. Although the numerical applications presented are restricted to hysteretic attenuation, general‐type, frequency‐dependent attenuation models can be also employed by taking advantage of the frequency‐wave number domain formulation presented. In addition, dissipation due to viscous resistance of the pore fluid is included in the solution. Plots are displayed showing comparisons with conventional solutions for “dry” cases. In these plots, the influence of the pore fluid on the wave propagation is shown.
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      Waves in Partially Saturated Medium Due to Surface Loads

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    https://yetl.yabesh.ir/yetl1/handle/yetl/77497
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    contributor authorA. J. Philippacopoulos
    date accessioned2017-05-08T22:19:13Z
    date available2017-05-08T22:19:13Z
    date copyrightOctober 1988
    date issued1988
    identifier other%28asce%290733-9399%281988%29114%3A10%281740%29.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/77497
    description abstractA two‐layered continuum in which the underlying half‐space is a fluid‐saturated porous (two‐phased) medium is considered. A comprehensive analysis is made of the disturbance produced in this continuum by time harmonic normal point loads acting at the surface. Integral solutions for the surface displacements are derived. Viscoelastic‐type behavior is assumed for the layer, while the behavior of the half‐space follows Biot's small strain theory for poro‐viscoelastic media. Attenuation of the dilatational and the shear waves in the layer and in the skeletal frame of the fluid‐saturated porous half‐space is assumed. Although the numerical applications presented are restricted to hysteretic attenuation, general‐type, frequency‐dependent attenuation models can be also employed by taking advantage of the frequency‐wave number domain formulation presented. In addition, dissipation due to viscous resistance of the pore fluid is included in the solution. Plots are displayed showing comparisons with conventional solutions for “dry” cases. In these plots, the influence of the pore fluid on the wave propagation is shown.
    publisherAmerican Society of Civil Engineers
    titleWaves in Partially Saturated Medium Due to Surface Loads
    typeJournal Paper
    journal volume114
    journal issue10
    journal titleJournal of Engineering Mechanics
    identifier doi10.1061/(ASCE)0733-9399(1988)114:10(1740)
    treeJournal of Engineering Mechanics:;1988:;Volume ( 114 ):;issue: 010
    contenttypeFulltext
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