Abstract
Direct pore scale simulations of two-fluid flow on digital rock images provide a promising tool to understand the role of surface wetting phenomena on flow and transport in geologic reservoirs. We present computational protocols that mimic conventional special core analysis laboratory (SCAL) experiments, which are implemented within the open source LBPM software package. Protocols are described to simulate unsteady displacement, steady-state flow at fixed saturation, and to mimic centrifuge experiments. These methods can be used to infer relative permeability and capillary curves, and otherwise understand two-fluid flow behavior based on first principles. Morphological tools are applied to assess image resolution, establish initial conditions, and instantiate surface wetting maps based on the distribution of fluids. Internal analysis tools are described that measure essential aspects of two-fluid flow, including fluid connectivity and surface measures, which are used to track transient aspects of the flow behavior as they occur during simulation. Computationally efficient workflows are developed by combining these components with a two-fluid lattice Boltzmann model to define hybrid methods that can accelerate computations by using morphological tools to incrementally evolve the pore-scale fluid distribution. We show that the described methods can be applied to recover expected trends due to the surface wetting properties based on flow simulation in Benntheimer sandstone.
Original language | English |
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Pages (from-to) | 871-895 |
Number of pages | 25 |
Journal | Computational Geosciences |
Volume | 25 |
Issue number | 3 |
DOIs | |
State | Published - Jun 2021 |
Funding
J.M. and Z.L. thank Equinor ASA for funding parts of this research through a post-doc project. T.R. thanks Anders Kristoffersen, Einar Ebeltoft, Knut Uleberg and Åsmund Haugen, Equinor, for valuable discussions. An award of computer time was provided by the Department of Energy Director’s Discretionary program and the Frontier Center for Accelerated Application Readiness (CAAR). This research also used resources of the Oak Ridge Leadership Computing Facility, which is a DOE Office of Science User Facility supported under Contract DE-AC05-00OR22725. T.R. acknowledges Equinor ASA for granting permission to publish this paper. J.M. and Z.L. thank Equinor ASA for funding parts of this research through a post-doc project. T.R. thanks Anders Kristoffersen, Einar Ebeltoft, Knut Uleberg and ?smund Haugen, Equinor, for valuable discussions. An award of computer time was provided by the Department of Energy Director?s Discretionary program and the Frontier Center for Accelerated Application Readiness (CAAR). This research also used resources of the Oak Ridge Leadership Computing Facility, which is a DOE Office of Science User Facility supported under Contract DE-AC05-00OR22725. T.R. acknowledges Equinor ASA for granting permission to publish this paper.
Funders | Funder number |
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Einar Ebeltoft | |
Knut Uleberg | |
U.S. Department of Energy | |
Office of Science | DE-AC05-00OR22725 |
Keywords
- Capillary pressure
- Flow simulation
- Porous media
- Relative permeability
- SCAL
- Special core analysis
- Wettability