Abstract

We apply steady-state capillary-controlled upscaling in heterogeneous environments. A phase may fail to form a connected path across a given domain at capillary equilibrium. Moreover, even if a continuous saturation path exists, some regions of the domain may produce disconnected clusters that do not contribute to the overall connectivity of the system. In such cases, conventional upscaling processes might not be accurate since identification and removal of these isolated clusters are extremely important to the global connectivity of the system and the stability of the numerical solvers. In this study, we address the impact of percolation during capillary-controlled displacements in heterogeneous porous media and present a comprehensive investigation using random absolute permeability fields, for water-wet, oil-wet and mixed-wet systems, where J-function scaling is used to relate capillary pressure, porosity and absolute permeabilities in each grid cell. Important information is revealed about the average connectivity of the phases and trapping at the Darcy scale due to capillary forces. We show that in oil-wet and mixed-wet media, large-scale trapping of oil controlled by variations in local capillary pressure may be more significant than the local trapping, controlled by pore-scale displacement.

Highlights

  • The flow of one or more fluids in porous rocks at the field scale is modelled using Darcy’s law

  • Relative permeability is a dimensionless quantity, which indicates the average connectivity of a rock for a given phase when it partially saturates that rock (Muskat 1937)

  • A revised steady-state upscaling algorithm is introduced accounting for the trapping of fluids in a large-scale invasion percolation displacement

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Summary

Introduction

The flow of one or more fluids in porous rocks at the field scale is modelled using Darcy’s law. The capillary pressure, on the other hand, is the difference in pressure between two fluid phases at equilibrium (Leverett 1941). This definition of capillary pressure is precise at the pore scale at fluid–fluid interfaces, it becomes less accurate for large scales where the capillary pressure may be undefined once a phase loses its connectivity across a given domain. The capillary pressure will still be defined though at the pore scale at the interface of some disconnected fluid regions For such cases, the corresponding relative permeability value for the disconnected phase is precisely zero, and only one phase is flowing inside that domain

Importance of Upscaling
Steady-state Upscaling
Darcy-scale Saturation-Dependent Functions
Theory of Large-scale Trapping of Fluids
Revised Procedure
Filling Cells at a Given Capillary Pressure
Phase Mobility Index γp
Phase Connectivity Index ψp
Large-scale Invasion Percolation with Trapping
Average Relative Permeability Algorithm
Validation
Illustrative Examples
Findings
10 Conclusions
Full Text
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