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    Bounds for seismic dispersion and attenuation in poroelastic rocks

    173609_41719_Bounds for seismic dispersion and attenuation in poroelastic rocks.pdf (617.4Kb)
    Access Status
    Open access
    Authors
    Gurevich, Boris
    Makarynska, Dina
    De Paula, Osni
    Date
    2011
    Type
    Conference Paper
    
    Metadata
    Show full item record
    Citation
    Gurevich, Boris and Makarynska, Dina and De Paula, Osni. 2011. Bounds for seismic dispersion and attenuation in poroelastic rocks, in Society of Exploration Geophysics (ed), SEG/San Antonio 2011, Sep 18 2011, pp. 2155-2160. San Antonio, Texas: SEG
    Source Title
    SEG Technical Program Expanded Abstracts
    Source Conference
    SEG/San Antonio 2011
    DOI
    10.1190/1.3627636
    ISSN
    1949-4645
    School
    Department of Exploration Geophysics
    Remarks

    ©2011 Society of Exploration Geophysicists

    URI
    http://hdl.handle.net/20.500.11937/3392
    Collection
    • Curtin Research Publications
    Abstract

    Recently, Hashin-Shtrikman bounds for bulk and shear moduli of elastic composites have been extended to the moduli of composite viscoelastic media. Since viscoelastic moduli are complex, the viscoelastic bounds form a closed curve on a complex plane. We apply these general viscoelastic bounds to a particular case of a porous solid saturated with a Newtonian fluid. Our analysis shows that for poroelastic media, the viscoelastic bounds for the bulk modulus are represented by a semi-circle and a segment of the real axis, connecting formal HS bounds (computed for an inviscid fluid). Furthermore, these bounds are independent of frequency and realizable. We also show that these viscoelastic bounds account for viscous shear relaxation and squirt-flow dispersion, but do not account for Biot's global flow dispersion.

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