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    Morphological evaluation of heterogeneous oolitic limestone under pressure and fluid flow using X-ray microtomography

    Access Status
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    Authors
    Zhang, Y.
    Lebedev, Maxim
    Al-Yaseri, A.
    Yu, H.
    Nwidee, L.
    Sarmadivaleh, Mohammad
    Barifcani, Ahmed
    Iglauer, Stefan
    Date
    2018
    Type
    Journal Article
    
    Metadata
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    Citation
    Zhang, Y. and Lebedev, M. and Al-Yaseri, A. and Yu, H. and Nwidee, L. and Sarmadivaleh, M. and Barifcani, A. et al. 2018. Morphological evaluation of heterogeneous oolitic limestone under pressure and fluid flow using X-ray microtomography. Journal of Applied Geophysics. 150: pp. 172-181.
    Source Title
    Journal of Applied Geophysics
    DOI
    10.1016/j.jappgeo.2018.01.026
    ISSN
    0926-9851
    School
    WASM: Minerals, Energy and Chemical Engineering (WASM-MECE)
    URI
    http://hdl.handle.net/20.500.11937/66907
    Collection
    • Curtin Research Publications
    Abstract

    Pore-scale analysis of carbonate rock is of great relevance to the oil and gas industry owing to their vast application potentials. Although, efficient fluid flow at pore scale is often disrupted owing to the tight rock matrix and complex heterogeneity of limestone microstructures, factors such as porosity, permeability and effective stress greatly impact the rock microstructures; as such an understanding of the effect of these variables is vital for various natural and engineered processes. In this study, the Savonnières limestone as a carbonate mineral was evaluated at micro scales using X-ray micro-computed tomography at high resolutions (3.43 μm and 1.25 μm voxel size) under different effective stress (0 MPa, 20 MPa) to ascertain limestone microstructure and gas permeability and porosity effect. The waterflooding (5 wt% NaCl) test was conducted using microCT in-situ scanning and nanoindentation test was also performed to evaluate microscale geomechanical heterogeneity of the rock. The nanoindentation test results showed that the nano/micro scale geomechanical properties are quite heterogeneous where the indentation modulus for the weak consolidated area was as low as 1 GPa. We observed that the fluid flow easily broke some less-consolidated areas (low indentation modulus) area, coupled with increase in porosity; and consistent with fines/particles migration and re-sedimentation were identified, although the effective stress showed only a minor effect on the rock microstructure.

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