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    Effective fluid transport properties of deformable rocks

    71771.pdf (529.4Kb)
    Access Status
    Open access
    Authors
    Müller, T.
    Gurevich, Boris
    Date
    2006
    Type
    Conference Paper
    
    Metadata
    Show full item record
    Citation
    Müller, T. and Gurevich, B. 2006. Effective fluid transport properties of deformable rocks, in Proceedings of the International Exposition and 76th Annual Meeting, Oct 1-6 2006, pp. 1957-1961. New Orleans, Louisiana: SEG.
    Source Title
    Society of Exploration Geophysicists - SEG International Exposition and 76tth Annual Meeting 2006, SEG 2006
    DOI
    10.1190/1.2369882
    ISBN
    9781604236972
    School
    WASM: Minerals, Energy and Chemical Engineering (WASM-MECE)
    Remarks

    Use of this publication is subject to SEG terms of use and conditions at https://seg.org/Terms-of-Use

    URI
    http://hdl.handle.net/20.500.11937/71528
    Collection
    • Curtin Research Publications
    Abstract

    Modern reservoir monitoring technologies often make use of diffusion waves in order to estimate the hydraulic conductivity and diffusivity of reservoir rocks. However, most theoretical descriptions for these effective uid transport properties assume that the host rock is elastically rigid. Inhomogeneous poroelastic continua described by Biot's equations of dynamic or quasi-static poroelasticity provide an adequate framework to study the dependence of uid transport properties on the elastic properties of the host rock. Analysis of diffusion wave elds in randomly inhomogeneous poroelastic structures provides new insight into how uctuations of the compressible constituents of the rock affect the effective diffusivity. Using the method of statistical smoothing we derive an effective wave number of the coherent diffusion wave eld. This wave number yields expressions for the effective conductivity and diffusivity of a deformable and inhomogeneous porous medium. These uid transport properties are frequency-dependent. Comparison of the hydraulic conductivity derived here with that estimated from unsteady ow through porous media based on Darcy's law shows that they are identical in the limits of low and high frequencies.

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