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    Direct laboratory observation of patchy saturation and its effects on ultrasonic velocities

    132517_13156_009LebedevTomsClennellGurevich.pdf (293.0Kb)
    Access Status
    Open access
    Authors
    Lebedev, Maxim
    Toms-Stewart, Julianna
    Clennel, B.
    Pervukhina, M.
    Shulakova, V.
    Paterson, L.
    Muller, T.
    Gurevich, Boris
    Wenzlau, F.
    Date
    2009
    Type
    Journal Article
    
    Metadata
    Show full item record
    Citation
    Lebedev, Maxim and Toms-Stewart, Julianna and Clennell, Ben and Pervukhina, Marina and Shulakova, Valeriya and Paterson, Lincoln and Muller, Tobias and Gurevich, Boris and Wenzlau, Fabian. 2009. Direct laboratory observation of patchy saturation and its effects on ultrasonic velocities. The Leading Edge 28. (1): pp. 24-28.
    Source Title
    The Leading Edge
    DOI
    10.1190/1.3064142
    ISSN
    1070485X
    Faculty
    Department of Exploration Geophysics
    Faculty of Science and Engineering
    WA School of Mines
    Remarks

    Published by the Society of Exploration Geophysicists

    © 2009 Society of Exploration Geophysicists

    The link to the journal’s home page is at : http://segdl.aip.org/tle

    URI
    http://hdl.handle.net/20.500.11937/46299
    Collection
    • Curtin Research Publications
    Abstract

    Maximizing the recovery of known hydrocarbon reserves is one of the biggest challenges facing the petroleum industry today. Optimal production strategies require accurate monitoring of production-induced changes of reservoir saturation and pressure over the life of the field. Time-lapse seismic technology is increasingly used to map these changes in space and time. However, until now, interpretation of time-lapse seismic data has been mostly qualitative. In order to allow accurate estimation of the saturation, it is necessary to know the quantitative relationship between fluid saturation and seismic characteristics (elastic moduli, velocity dispersion, and attenuation). The problem of calculating acoustic properties of rocks saturated with a mixture of two fluids has attracted considerable interest (Gist, 1994; Mavko and Nolen-Hoeksema, 1994; Knight et al., 1998. For a comprehensive review of theoretical and experimental studies of the patchy saturation problem see Toms et al., 2006).

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