Abstract

We study three different time integration methods for a dynamic pore network model for immiscible two-phase flow in porous media. Considered are two explicit methods, the forward Euler and midpoint methods, and a new semi-implicit method developed herein. The explicit methods are known to suffer from numerical instabilities at low capillary numbers. A new time-step criterion is suggested in order to stabilize them. Numerical experiments, including a Haines jump case, are performed and these demonstrate that stabilization is achieved. Further, the results from the Haines jump case are consistent with experimental observations. A performance analysis reveals that the semi-implicit method is able to perform stable simulations with much less computational effort than the explicit methods at low capillary numbers. The relative benefit of using the semi-implicit method increases with decreasing capillary number $\mathrm{Ca}$, and at $\mathrm{Ca} \sim 10^{-8}$ the computational time needed is reduced by three orders of magnitude. This increased efficiency enables simulations in the low-capillary number regime that are unfeasible with explicit methods and the range of capillary numbers for which the pore network model is a tractable modeling alternative is thus greatly extended by the semi-implicit method.

Highlights

  • Different modeling approaches have been applied in order to increase understanding of immiscible two-phase flow in porous media

  • Pore network models have proven to be useful in order to reduce the computational cost [5], or enable the study of larger systems, while still retaining some pore-level detail

  • We present three numerical methods that can be utilized to perform stable simulations of two-phase flow in porous media with pore network models of the Aker type

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Summary

INTRODUCTION

Different modeling approaches have been applied in order to increase understanding of immiscible two-phase flow in porous media. One of the advantages of the Aker-type model is that a detailed picture of the fluid configuration is provided at any time during a simulation Dynamic phenomena, such as the retraction of the invasion front after a Haines jump [13,14,15,16], are resolved. We present three numerical methods that can be utilized to perform stable simulations of two-phase flow in porous media with pore network models of the Aker type.

PORE NETWORK MODEL
Link Mobility Model
Capillary Pressure Model
Fluid Interface Interaction Models
Boundary Conditions
TEMPORAL DISCRETIZATION
FORWARD EULER METHOD
Time Step Restrictions
MIDPOINT METHOD
SEMI-IMPLICIT METHOD
IMPLEMENTATION
CASE DESCRIPTIONS
Links-in-Series Test Case
References μw
Convergence Tests
Stability Tests
10. PERFORMANCE ANALYSIS
Findings
11. CONCLUSION
Full Text
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