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    An Experimental Study of Low-Frequency Wave Dispersion and Attenuation in Water Saturated Sandstones

    Access Status
    Fulltext not available
    Authors
    Mikhaltsevitch, Vassili
    Lebedev, Maxim
    Gurevich, Boris
    Date
    2013
    Type
    Conference Paper
    
    Metadata
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    Citation
    Mikhaltsevitch, V. and Lebedev, M. and Gurevich, B. 2013. An Experimental Study of Low-Frequency Wave Dispersion and Attenuation in Water Saturated Sandstones, in American Society of Civil Engineers (ed), Proceedings of the 5th BIOT Conference of Poromechanics, Jul 10-12 2013, pp. 135-144. Vienna: American Society of Civil Engineers.
    Source Title
    Poromechanics V: Proceedings of the Fifth Biot Conference on Poromechanics
    Source Conference
    Fifth Biot Conference on Poromechanics
    DOI
    10.1061/9780784412992.016
    ISBN
    978-0-7844-1299-2
    School
    Department of Exploration Geophysics
    URI
    http://hdl.handle.net/20.500.11937/8362
    Collection
    • Curtin Research Publications
    Abstract

    The elastic and anelastic parameters of dry and distilled water-saturated sandstones with low (~7.8 mD) and high (~590 mD) permeabilities were measured at various confining pressures and room temperature (22° C). The both sandstones were quarried in Donnybrook, Western Australia. The experiments were performed with a new laboratory apparatus utilizing stress-strain relationship, which was developed to measure the complex Young's moduli of rocks at seismic (1-100 Hz) and teleseismic (≤1 Hz) frequencies, confining or uniaxial pressures from 0 to 70 MPa, and strain amplitudes 10-8-10-7. The measurements in water-saturated sandstones reveal a prominent peak of attenuation in the sample with low permeability at frequency ~0.8 Hz, whereas the attenuation in the high permeable sample remains similar to the attenuation measured under dry conditions. These results demonstrate that for low-permeability rocks seismic frequencies do not necessarily correspond to the low frequency limit of acoustic wave dispersion.

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