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Boundary integral formulation for flows containing an interface between two porous media

Published online by Cambridge University Press:  28 February 2017

E. Ahmadi*
Affiliation:
Department of Mathematics and Center for Computational Science, Tulane University, New Orleans, LA 70118, USA
R. Cortez
Affiliation:
Department of Mathematics and Center for Computational Science, Tulane University, New Orleans, LA 70118, USA
H. Fujioka
Affiliation:
Center for Computational Science, Tulane University, New Orleans, LA 70118, USA
*
†Email address for correspondence: ellie.ahmadi.2016@gmail.com

Abstract

A system of boundary integral equations is derived for flows in domains composed of a porous medium of permeability $k_{1}$ , surrounded by another porous medium of different permeability, $k_{2}$ . The incompressible Brinkman equation is used to describe the flow in the porous media. We first apply a boundary integral representation of the Brinkman flow on each side of the dividing interface, and impose continuity of the velocity at the interface to derive the final formulation in terms of the interfacial velocity and surface forces. We discuss relations between the surface stresses based on the additional conditions imposed at the interface that depend on the porosity and permeability of the media and the structural composition of the interface. We present simulated results for test problems and different interface stress conditions. The results show significant sensitivity to the choice of the interface conditions, especially when the permeability is large. Since the Brinkman equation approaches the Stokes equation when the permeability approaches infinity, our boundary integral formulation can also be used to model the flow in sub-categories of Stokes–Stokes and Stokes–Brinkman configurations by considering infinite permeability in the Stokes fluid domain.

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Papers
Copyright
© 2017 Cambridge University Press 
Figure 0

Figure 1. Schematic of the Brinkman–Brinkman problem.

Figure 1

Figure 2. Schematic plot of the problem where a porous region described by the Brinkman equations is surrounded by a viscous fluid. The regions in the examples in this section are either circular or elliptical. The background flow is uniformly constant and equal to $\boldsymbol{u}^{\infty }=(20,0)^{t}$. The velocity profiles will be shown across the vertical lines.

Figure 2

Figure 3. Velocity profiles: effects of porosity on the velocity field in a domain with circular interface. Continuity of the velocity and the normal stress along with ‘OTW’ jump condition on the tangential stress are imposed at the interface. On the vertical axes, $\unicode[STIX]{x1D6FA}_{2}$ corresponds to $-1\leqslant y\leqslant 1$. The parameter $\unicode[STIX]{x1D6FC}$ is defined by $\unicode[STIX]{x1D6FC}=\sqrt{\unicode[STIX]{x1D719}/Da}$.

Figure 3

Figure 4. Velocity fields for various values of porosity $\unicode[STIX]{x1D719}$ and $Da$. The parameter $\unicode[STIX]{x1D6FC}$ is defined by $\unicode[STIX]{x1D6FC}=\sqrt{\unicode[STIX]{x1D719}/Da}$.

Figure 4

Figure 5. A $45^{\circ }$ rotated elliptical interface: velocity profiles associated with different values of the porosity and the permeability across the line $x=0$ are plotted. On the vertical axes, $\unicode[STIX]{x1D6FA}_{2}$ corresponds to $-1.265\leqslant y\leqslant 1.265$. The parameter $\unicode[STIX]{x1D6FC}$ is defined by $\unicode[STIX]{x1D6FC}=\sqrt{\unicode[STIX]{x1D719}/Da}$.

Figure 5

Figure 6. Velocity fields are shown in (a,c,e,g) and their corresponding streamlines in (b,d,f,h). The parameter $\unicode[STIX]{x1D6FC}$ is defined by $\unicode[STIX]{x1D6FC}=\sqrt{\unicode[STIX]{x1D719}/Da}$. (a,b) $\unicode[STIX]{x1D719}_{2}=0.9$, $Da=10$, $\unicode[STIX]{x1D6FD}=0.05$, (c,d) $\unicode[STIX]{x1D719}_{2}=0.5$, $Da=0.05$, $\unicode[STIX]{x1D6FD}=0.05$, (e,f) $\unicode[STIX]{x1D719}_{2}=0.1$, $Da=0.002$, $\unicode[STIX]{x1D6FD}=0.05$, (g,h) $\unicode[STIX]{x1D719}_{2}=0.01$, $Da=0.0001$, $\unicode[STIX]{x1D6FD}=0.05$.

Figure 6

Figure 7. Hydrodynamic force on a porous disc as a function of dimensionless permeability.

Figure 7

Figure 8. Horizontal velocity profiles corresponding to a circular porous region $\unicode[STIX]{x1D6FA}_{2}$ surrounded by a different porous region $\unicode[STIX]{x1D6FA}_{1}$. The parameters used are $\unicode[STIX]{x1D719}_{1}=0.6$, $\unicode[STIX]{x1D6FC}_{1}=2.45$ and $\unicode[STIX]{x1D719}_{2}=0.4$, $\unicode[STIX]{x1D6FC}_{2}=2.83$. The panels show the profiles obtained by using different values of the jump coefficient $\unicode[STIX]{x1D6FD}$.

Figure 8

Figure 9. Brinkman–Brinkman system with $(\unicode[STIX]{x1D6FC}_{1},\unicode[STIX]{x1D719}_{1})=(3.16,0.2)$, $(\unicode[STIX]{x1D6FC}_{2},\unicode[STIX]{x1D719}_{2})=(10,0.01)$ and $\unicode[STIX]{x1D6FD}=0.4$.

Figure 9

Figure 10. Brinkman–Brinkman system with $(\unicode[STIX]{x1D6FC}_{1},\unicode[STIX]{x1D719}_{1})=(3.16,0.2)$, $(\unicode[STIX]{x1D6FC}_{2},\unicode[STIX]{x1D719}_{2})=(0.85,0.8)$ and $\unicode[STIX]{x1D6FD}=0.9$.