Abstract
A linear stability analysis of the single-phase conservation equation in multidimensional porous media is performed, for both weakly compressible and compressible fluids. Non-Newtonian and non-Darcy effects are accounted for using a non-linear Darcy-like form for the superficial velocity, where the mobility tensor is velocity-dependent and proportional to the permeability. It is found that under this hypothesis, flows at an angle with respect to the principal axes of the permeability tensor can be unstable, unless the mobility is a function of the velocity magnitude in terms of the inverse permeability norm. As shown by previous authors, for steady-state incompressible flows this is also the condition ensuring that the governing equation derives from the minimization of a dissipation potential.
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Notes
Although several acceptions exist in the literature, the term “non-Darcy” will here specifically be employed to qualify flows where inertial effects cannot be neglected.
Although the approach would be cumbersome, we mention for completeness that an expression of the form (32) could also be used for weakly compressible fluids provided the appropriate \(Z\) function is chosen (e.g., \(Z = \frac{M}{RT}\frac{p}{\rho _0\left[1+c_\mathrm{f}\left(p-p_0\right)\right]}\) for the fluid considered in Sect. 2.3).
References
Al-Hussainy R., Ramey H.J., Crawford P.B. (1965) The flow of real gases through porous media. SPE Journal 1243A
Auriault, J.L., Royer, P., Geindreau, C.: Filtration law for power-law fluids in anisotropic porous media. Intl. J. Eng. Sci. 4010, 1151–1163 (2002)
Aziz, K., Settari, A.: Petroleum Reservoir Simulation. Applied Science publishers, London (1979)
Bachmat, Y.: Basic transport coefficients as aquifer characteristics. In: I.A.S.H. symposium on hydrology of fractured rocks, vol. 1, Dubrovnik, pp. 63–75 (1965)
Barree, R.D.: Beyond beta factors: a complete model for Darcy, Forchheimer, and trans-Forchheimer flow in porous media. SPE paper 89325 presented at the ATCE held in Houston (2004)
Bear, J.: Dynamics of Fluids in Porous Media. Dover publications, New York (1972)
Bird, R.B., Armstrong, R.C., Hassager, O.: Dynamics of Polymeric Liquids, vol. 1, pp. 171–173. Wiley, New York (1987)
Brinkman, H.C.: A calculation of the viscous force exerted by a flowing fluid on a dense swarm of particles. Appl. Sci. Res. 1(1), 27–34 (1947)
Cannella, W.J., Huh, C., Seright, R.S.: Prediction of xanthan rheology in porous media. SPE paper 18089 presented at the ATCE held in Houston (1988)
Carreau, P.J., De Kee, D., Chhabra, R.P.: Rheology of Polymeric Systems. Hanser Publishers, New York (1997)
CMG: IMEX User’s guide (2010)
Darcy, H.: Les Fontaines Publiques de la Ville de Dijon. Dalmont, Paris (1856)
Delshad, M., Pope, G.A., Sepehrnoori, K.: UTChem version 9.0 technical documentation. CPGE, The University of Texas at Austin (2000)
Firdaouss, M., Guermond, J.-L., Le Quéré, P.: Nonlinear corrections to Darcy’s law at low Reynolds numbers. J. Fluid Mech. 343, 331–350 (1997)
Forchheimer, P.: Wasserbewegung durch Boden. VDIZ 45, 1782–1788 (1901)
Getachew, D., Minkowycz, W.J., Poulikakos, D.: Macroscopic equations of non-Newtonian fluid flow and heat transfer in a porous matrix. J. Porous Media 1(3), 273–283 (1998)
Gilbert, G.T.: Positive definite matrices and Sylvester’s criterion. Am. Math. Monthly 98(1), 44–46 (1991)
Idris, Z., Orgéas, L., Geindreau, C., Bloch, J.-F., Auriault, J.-L.: Microstructural effects on the flow law of power-law fluids through fibrous media. Modeling Simul. Mater. Sci. Eng. 12, 995–1015 (2004)
Ikoku, C.U., Ramey Jr., H.J.: Transient flow of non-Newtonian power-law fluids in porous media. SPE Journal 7139 (1978)
Kalaydjian, F.J-M., Bourbiaux, B.J., Lombard, J-M.: Predicting gas-condensate reservoir performance: how flow parameters are altered when approaching production wells. SPE paper 36715 presented at the ATCE held in Denver (1996)
Kazemi, H.: Pressure transient analysis of naturally fractured reservoirs with uniform fracture distribution. SPE J. 9(4), 451–462 (1969)
Kececioglu, I., Rubinsky, B.: A continuum model for the propagation of discrete phase-change fronts in porous media in the presence of coupled heat flow, fluid flow and species transport processes. Int. J. Heat Mass Transf. 32, 1111–1130 (1989)
Knupp, P.M., Lage, J.L.: Generalization of the Forchheimer-extended Darcy flow model to the tensor permeability case via a variational principle. J. Fluid Mech. 299, 97–104 (1995)
Lake, L.: Enhanced Oil Recovery. Prentice Hall, Englewood Cliffs (1989)
Li, D., Engler, T.W.: Literature review on correlations of the non-Darcy coefficient. SPE paper 70015 presented at the permian basin oil and gas recovery conference held in Midland (2001)
Newman, M.S., Yin, X.Y.: Lattice Boltzmann simulation of non-Darcy flow in stochastically generated 2D porous media geometries. SPE paper 146689 presented at the ATCE held in Denver (2011)
Raghavan, R.: Well Test Analysis. Prentice Hall, Englewood Cliffs (1993)
Russo, Spena F., Vacca, A.: A potential formulation of non-linear models of flow through anisotropic porous media. Transp. Porous Media 45, 407–423 (2001)
Sanchez-Palencia, E.: On the asymptotics of the fluid flow past an array of fixed obstacles. Intl. J. Eng. Sci. 20(12), 1291–1301 (1982)
Schlumberger: Eclipse reservoir simulation software, Technical description (2010)
Slattery, J.C.: Flow of viscoelastic fluids through porous media. AIChE J. 13(6), 1066–1071 (1967)
Sochi, T.: Pore-scale modeling of non-Newtonian flow in porous media. Ph.D. Thesis, Imperial College, London (2007)
Sorbie, K.S.: Polymer-Improved Oil Recovery. Blackie, Glasgow (1991)
Tan, C.T., Homsy, G.M.: Stability of miscible displacements in porous media: rectilinear flow. Phys. Fluids 29(1), 3549 (1986)
Tosco, T., Marchisio, D.L., Lince, F., Sethi, R.: Extension of the Darcy–Forchheimer law for shear-thinning fluids and validation via pore-scale flow simulations. Transp. Porous Media 96, 1–20 (2013)
Valdes-Parada, F.J., Ochoa-Tapia, J.A., Alvarez-Ramirez, J.: On the effective viscosity for the Darcy–Brinkman equation. Physica A 385, 69–79 (2007)
Wang, X., Thauvin, F., Mohanty, K.K.: Non-Darcy flow through anisotropic porous media. Chem. Eng. Sci. 54, 1859–1869 (1998)
Whitaker, S.: The method of volume averaging. In: Theory and Applications of Transport in Porous Media. Kluwer academic publishers, Dordrecht (1999)
Whitaker, S.: Flow in porous media I: a theoretical derivation of Darcy’s law. Transp. Porous Media 1, 3–25 (1986)
Whitaker, S.: The Forchheimer equation: a theoretical development. Transp. Porous Media 25, 27–61 (1996)
Yortsos, Y.C., Hickernell, F.J.: Linear stability of immiscible displacements in porous media. SIAM J. Appl. Maths 49(3), 730–748 (1989)
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Appendices
Appendix
Criteria for Acceptable Mobilities
1.1 Weakly Compressible Case
Within the weakly compressible approximation with gravity, using our definition of fluid potential given by Eq. (23), the closure relationship for the superficial velocity can be cast in the non-Newtonian case as (see Eq. (24)):
Due to our “small” compressibility assumption, we have \(\rho /\rho _0=1+o(1)\) and to leading order
where \(\lambda >0\) is the velocity-dependent mobility factor. To leading order this equation formally also applies to the non-Darcy case. For Eq. (80) to yield a physically solvable flow problem, there must be a bijective mapping between potential gradient and velocity. In other words, for a given velocity there should be a unique potential gradient driving the flow, and conversely. In particular, according to the inverse function theorem, local invertibility is guaranteed provided the Jacobian of
is non-singular. Differentiation of \(\mathbf{f}\) leads to the following Jacobian expression:
where \(\underline{\underline{I}}\) is the identity tensor. For invertibility we require that \(\det (\underline{\underline{\text{ df}}}(\mathbf{u}))\ne 0\), which yields the condition
Clearly, there must exist a continuous path driving the flow velocity from 0 to \(\mathbf{u}\), hence the above expression should remain strictly positive, and since \(\lambda >0\) we can write that for \(v\ge 0\)
i.e.,
Multiplying Eq. (80) on the left by \(\underline{\underline{\kappa }}^{\alpha -1}\) and taking the norm, we obtain
which suggests that \(\left|\underline{\underline{\kappa }}^{\alpha -1}.\mathbf{u}\right|\) can be considered as a function of \(\left|\underline{\underline{\kappa }}^{\alpha }\cdot \nabla \psi \right|\). To verify this, we introduce
and compute
Assuming that \(\mathbf{f}\) defined by Eq. (81) is bijective, it clearly follows that \(g\) is surjective, and according to Eqs. (84) and (88), \(g^{\prime }(v)>0\) and \(g\) is also injective. We conclude that \(g:\mathbb R ^{+}\mapsto \mathbb R ^{+}\) is bijective and \(\left|\underline{\underline{\kappa }}^{\alpha -1}\cdot \mathbf{u}\right|=g^{-1}\left(\left|\underline{\underline{\kappa }}^{\alpha }\cdot \nabla \psi \right|\right)\). Defining
we can now rewrite Eq. (80) as
and Eq. (86) as
Defining
we see that \(h(g(v))=g(v)\tilde{\lambda }(g(v))=g(v)\lambda (v)=v\), therefore \(h^{\prime }(g(v)) = 1/g^{\prime }(v) >0\) and \(h\) is strictly monotone. Since \(h^{\prime }(w) = \tilde{\lambda }(w)+w\tilde{\lambda }^{\prime }(w)\), in addition to inequality (85) we have
i.e.
This second inequality is also the one ensuring that the Jacobian of \(\mathbf{u}=\mathbf{m}(\mathbf{\nabla }\psi )\) (Eq. (90)) is non-singular. Conditions (85) and (94) are illustrated in Fig. (1).
In practice, for a given velocity-dependent mobility function \(\lambda \) (what is typically known from experiments or physical models is the function \(\lambda \), not \(\tilde{\lambda }\)), we can compute \(\tilde{\lambda }\) by integration of the first-order ODE
with the initial condition \(\tilde{\lambda }(0)=\lambda (0)\). We may also write this relationship as
where \(w=g(v)\), i.e.,
1.2 Compressible Case
Without gravity, using our definition of fluid potential given by Eq. (33), the closure relationship for the superficial velocity can be cast in the non-Darcy case as (see Eq. (34)):
By identification with Eq. (80), i.e. “replacing \(\mathbf{u}\) by \(\rho \mathbf{u}\)” and “replacing \(\psi \) by \(M\psi /2RT\)”, we see that the requirements of Eqs. (85) and (94), as well as the property of Eq. (97), still hold.
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Patacchini, L., de Loubens, R. A Class of Physically Stable Non-linear Models of Flow Through Anisotropic Porous Media. Transp Porous Med 97, 409–429 (2013). https://doi.org/10.1007/s11242-013-0132-3
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DOI: https://doi.org/10.1007/s11242-013-0132-3