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    Experimental study on rock mechanical response during CO2injection into limestone reservoir at different conditions

    Access Status
    Fulltext not available
    Authors
    Zhang, Y.
    Lebedev, Maxim
    Sarmadivaleh, Mohammad
    Barifcani, Ahmed
    Iglauer, Stefan
    Date
    2018
    Type
    Conference Paper
    
    Metadata
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    Citation
    Zhang, Y. and Lebedev, M. and Sarmadivaleh, M. and Barifcani, A. and Iglauer, S. 2018. Experimental study on rock mechanical response during CO2injection into limestone reservoir at different conditions.
    Source Title
    52nd U.S. Rock Mechanics/Geomechanics Symposium
    School
    WASM: Minerals, Energy and Chemical Engineering (WASM-MECE)
    URI
    http://hdl.handle.net/20.500.11937/73387
    Collection
    • Curtin Research Publications
    Abstract

    Copyright © 2018 ARMA, American Rock Mechanics Association. CO2 storage in deep saline aquifers is the green technology to mitigate climate change by greenhouse gas emissions. The carbonate reservoir such as limestone is the popular storage site due to widely existed. However, such reservoirs are sensitive to the acidic CO2 fluids and how the geomechanical response for different areas in the storage sites are poorly understand. Thus in this paper, we measured the geomechanical response on Savonnières Limestone samples by UCS test on three different reservoir conditions: near the wellbore – scCO2 flooding, distances with wellbore – CO2 saturated brine flooding, and far from the wellbore – dead brine saturated. The flooding tests were set as a representative reservoir conditions at approximately 1000m depth with 325 K/50oC, 15 MPa confining pressure and 10 MPa pore pressure. The results show that the CO2 saturated brine flooding had largest dissolution effect with lowest maxim unconfined compressive stresses. We thus concluded that the most matrix damaged area by acid fluid dissolution should be some distances around the wellbore but not near the wellbore, and such geomechanical weakening may cause potential geohazard such as layer collapse and fault reactive.

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