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Coupling pore network and finite element methods for rapid modelling of deformation

Published online by Cambridge University Press:  15 June 2020

Samuel Fagbemi
Affiliation:
Department of Petroleum Engineering, University of Wyoming, Laramie, WY82071, USA
Pejman Tahmasebi*
Affiliation:
Department of Petroleum Engineering, University of Wyoming, Laramie, WY82071, USADepartment of Civil Engineering, University of Wyoming, Laramie, WY82071, USA
*
†Email address for correspondence: ptahmase@uwyo.edu

Abstract

Numerical modelling of deformation in hydromechanical systems can be time-consuming using fully coupled classical numerical methods for large representative porous media samples. In this paper, we present a new two-way coupled partitioned fluid–solid system. The coupled system is applied for simulating geomechanical processes at the pore-scale. We track the deformation of the solid resulting from the drainage of resident fluids in the pores, as well as the evolution of fluid properties from dynamic loading. The finite element method is responsible for capturing the structural deformation in the coupled system while the dynamic pore network is used for modelling multiphase flow in the fluid subsystem. A fictitious fluid–solid interface is created at each pore network-finite element node junction via convex hulling, followed by data exchange using linear interpolation. The results show good agreement with a pre-existing coupled finite volume model and the computations are completed in much less time.

Information

Type
JFM Papers
Copyright
© The Author(s), 2020. Published by Cambridge University Press
Figure 0

Table 1.Comparison of the computational times for various coupled pore-scale solvers on a domain with $120^{3}$ voxels. Note that the review of speeds of coupled solvers includes the preliminary results of this work. Similar step size and different cell sizes were used. Coupled and decoupled solutions were performed using multiphase fluids, while the stand-alone fluid simulations were performed for both multiphase (with FV) and single-phase flow (with FE). The central processing unit, CPU, time is reported in minutes. The FE-DPN*, which is the method implemented in this work, came out fastest by far in all categories; DPN represents dynamic pore network.

Figure 1

Figure 1.A local PN structure.

Figure 2

Figure 2.A subsample or elementary volume used for coupling simulations.

Figure 3

Figure 3.Schematic of the superimposed domains (fluid and solid). (a) The voxelized solid phase along with the PN and (b) discretized finite element domain and PN.

Figure 4

Figure 4.Test points used for convex hulling. The hydrodynamic load is transferred to the solid mesh node points by linear interpolation of node points within the convex hull. Here, $\unicode[STIX]{x1D716}_{i+r_{n}}$ represents the enlarged hull volume to include more points for interpolation. Points enclosed within $\unicode[STIX]{x1D716}_{i+r_{n}}$ are labelled as one. Points outside are zero.

Figure 5

Table 2.Properties used for the coupled simulation.

Figure 6

Figure 5.Drainage evolution in time for a water-wet system (oil is blue and water is red).

Figure 7

Figure 6.Solid deformed as a result of fluids residing in the pores at different pore pressures.

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Figure 7.Hydrodynamic forces and the corresponding deformation induced by nodal pressure in the network at times 1 s, 3 s, 5 s and 15 s, respectively.

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Figure 8.Effects of the number of test points on the capillary pressure solution for drainage in the water-wet system.

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Figure 9.Evolution of (a) solid deformation and (b) the von Mises stress at different flow rates.

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Figure 10.Convergence of pore network extractions.

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Figure 11.Solid deformation resulting from strain rates applied. Results are shown for two FE nodes, with 800 test points and $\unicode[STIX]{x1D750}_{\boldsymbol{i}+\boldsymbol{r}_{\boldsymbol{n}}}=8\times 10^{-5}$.

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Figure 12.(a) Solid boundary conditions used in microscale tests. (b) Pore pressure change.

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Figure 13.Change in PSD with a load increase at fluid injection times 1 s, 4 s, 5 s, 8 s, 10 s and 14 s. There is an apparent shift to the left of the original plot when the solid is compacted in the axial direction, indicating a reduction in the pore radii. At a strain value of 0.01247, there is constriction as well as lateral dilation of some pores due to stress.

Figure 15

Figure 14.The network (a) before deformation and (b) after deformation. The differences between (a) and (b) are noted by white colouring in (b).

Figure 16

Figure 15.Absolute permeability evolution at different times.

Figure 17

Figure 16.The FV geometry, similar to the coupled model used in this work, was obtained using micro-CT imaging technology. To effectively study the effects of external stresses and fluid forces on the sample at the pore-scale, high-porosity Berea sandstone was used. The Berea image was initially filtered to improve the signal-to-noise ratio and then subsequently segmented into binary data, where each domain is represented by 0 or 1. The rock image sample has a pore volume fraction of 21.174 %. The original voxel size of the sample was $1000^{3}$, which was later resized to $120^{3}$ for the simulation.

Figure 18

Figure 17.Verification of results for solid deformation from the finite volume model (FVM) and this work for selected nodal points, at the third time step from the last time $\Vert d_{T-3}\Vert$.