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Macroscopic model for unsteady flow in porous media

Published online by Cambridge University Press:  10 January 2019

Didier Lasseux*
Affiliation:
CNRS, I2M, UMR 5295, Esplanade des Arts et Métiers, 33405 Talence CEDEX, France
Francisco J. Valdés-Parada
Affiliation:
Universidad Autónoma Metropolitana-Iztapalapa, Departamento de Ingeniería de Procesos e Hidráulica, Av. San Rafael Atlixco 186, 09340 Ciudad de México, Mexico
Fabien Bellet
Affiliation:
Laboratoire EM2C, CNRS, CentraleSupélec, Université Paris-Saclay, 3 rue Joliot Curie, 91192 Gif-sur-Yvette CEDEX, France
*
†Email address for correspondence: didier.lasseux@u-bordeaux.fr

Abstract

The present article reports on a formal derivation of a macroscopic model for unsteady one-phase incompressible flow in rigid and periodic porous media using an upscaling technique. The derivation is carried out in the time domain in the general situation where inertia may have a significant impact. The resulting model is non-local in time and involves two effective coefficients in the macroscopic filtration law, namely a dynamic apparent permeability tensor, $\unicode[STIX]{x1D643}_{t}$, and a vector, $\unicode[STIX]{x1D736}$, accounting for the time-decaying influence of the flow initial condition. This model generalizes previous non-local macroscale models restricted to creeping flow conditions. Ancillary closure problems are provided, which allow the effective coefficients to be computed. Symmetry and positiveness analyses of $\unicode[STIX]{x1D643}_{t}$ are carried out, showing that this tensor is symmetric only in the creeping regime. The effective coefficients are functions of time, geometry, macroscopic forcings and the initial flow condition. This is illustrated through numerical solutions of the closure problems. Predictions are made on a simple periodic structure for a wide range of Reynolds numbers smaller than the critical value characterizing the first Hopf bifurcation. Finally, the performance of the macroscopic model for a variety of macroscopic forcings and initial conditions is examined in several case studies. Validation through comparisons with direct numerical simulations is performed. It is shown that the purely heuristic classical model, widely used for unsteady flow, consisting of a Darcy-like model complemented with an accumulation term on the filtration velocity, is inappropriate.

Information

Type
JFM Papers
Copyright
© 2019 Cambridge University Press 
Figure 0

Figure 1. (a) Sketch of a porous medium including a sample of the averaging volume and the characteristic length scales. Here ${\mathcal{V}}_{M}$ denotes the entire domain composed of the homogeneous part (${\mathcal{V}}_{Mh}$) and the region near the boundary ($I(\unicode[STIX]{x2202}{\mathcal{V}}_{M})$), i.e. ${\mathcal{V}}_{M}={\mathcal{V}}_{Mh}\cup I(\unicode[STIX]{x2202}{\mathcal{V}}_{M})$. (b) Position vectors associated with the averaging volume.

Figure 1

Figure 2. Two-dimensional sketch of a periodic structure and a geometrical periodic unit cell of side length $\ell$.

Figure 2

Figure 3. Dynamics of the $xx$-component of the apparent permeability tensor (a–c) and of the $x$-component of vector $\unicode[STIX]{x1D736}$ (d) for the flow problem described in § 4.1. The predictions result from solving the closure problems I and II in the unit cell depicted in figure 2 taking: (a) $\unicode[STIX]{x1D700}=0.4$ and (b) $\unicode[STIX]{x1D700}=0.6$. In (c), results are presented after normalization with the steady value of the apparent permeability. In (d), results are normalized with the initial value of $\unicode[STIX]{x1D6FC}_{x}$.

Figure 3

Figure 4. Solution domain for the DNS consisting of an array of $n$ inline square unit cells of length $\ell$.

Figure 4

Figure 5. Dynamics of the $x$-component of the macroscale velocity vector, normalized by its steady-state value $\langle v_{x}^{\ast }\rangle _{ss}^{\unicode[STIX]{x1D6FD}}$, resulting from the step change on the pressure gradient given in (4.5). In (a), predictions correspond to DNS and the volume averaging method with and without inclusion of the initial flow. In (b), a comparison is shown between predictions from the volume averaging method and the heuristic model. Simulations correspond to a porosity of 0.4 and $Re=10^{6}$.

Figure 5

Figure 6. (a) Dynamics of the decaying macroscopic pressure gradient given in (4.6) taking $t_{m}^{\ast }=8\times 10^{-4}$ and $\unicode[STIX]{x1D714}^{\ast }=1000$. (b) Dynamics of the $x$-component of the macroscale velocity vector, normalized by its initial value $\langle v_{0,x}^{\ast }\rangle ^{\unicode[STIX]{x1D6FD}}$, resulting from the time-decaying macroscopic pressure gradient. Predictions result from performing DNS, and from the solution of the macroscale model obtained by the volume averaging method and the heuristic model. Simulations correspond to a porosity of 0.4 and $Re=10^{6}$.

Figure 6

Figure 7. Dynamics of the $x$-component of the macroscale velocity as a response to a macroscopic pressure gradient pulse given by (4.7). Results from DNS, and from the solution of the macroscale model obtained by the volume averaging method and the heuristic model correspond to a porosity of 0.4 and (a) $Re=10^{3}$ and (b) $Re=10^{6}$.

Figure 7

Figure 8. Dynamics of the $x$-component of the macroscale velocity vector, resulting from a response to an oscillatory change in the macroscopic pressure gradient according to (4.8). Predictions result from performing DNS, from the solution of the macroscale model obtained by the volume averaging method and from the heuristic model. Simulations correspond to a porosity of 0.4 and (a) $Re=10^{3}$ and (b) $Re=10^{6}$.