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    Velocity-saturation relation in partially saturated rocks: Modelling the effect of injection rate changes

    Access Status
    Fulltext not available
    Authors
    Liu, J.
    Müller, T.
    Qi, Q.
    Lebedev, Maxim
    Sun, W.
    Date
    2016
    Type
    Journal Article
    
    Metadata
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    Citation
    Liu, J. and Müller, T. and Qi, Q. and Lebedev, M. and Sun, W. 2016. Velocity-saturation relation in partially saturated rocks: Modelling the effect of injection rate changes. Geophysical Prospecting. 64 (4): pp. 1054-1066.
    Source Title
    Geophysical Prospecting
    DOI
    10.1111/1365-2478.12376
    ISSN
    0016-8025
    School
    Department of Exploration Geophysics
    URI
    http://hdl.handle.net/20.500.11937/32691
    Collection
    • Curtin Research Publications
    Abstract

    The relationship between P-wave velocity and fluid saturation in a porous medium is of importance for reservoir rock characterization. Forced imbibition experiments in the laboratory reveal rather complicated velocity–saturation relations, including rollover-like patterns induced by injection rate changes. Poroelasticity theory-based patchy saturation models using a constant fluid patch size are not able to describe these velocity–saturation relations. Therefore, we incorporate a saturation-dependent patch size function into two models for patchy saturation. This recipe allows us to model observed velocity–saturation relations obtained for different and variable injection rates. The results reveal an increase in patch size with fluid saturation and show a reduction in the patch size for decreasing injection rate. This indicates that there can exist a distinct relation between patch size and injection rate. We assess the relative importance of capillarity on velocity–saturation relations and find that capillarity stiffening impairs the impact of patch size changes. Capillarity stiffening appears to be a plausible explanation when a decrease in the injection rate is expected to boost the importance of capillarity.

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