On the solution of the coupled steady-state dual-porosity-Navier-Stokes fluid flow model with the Beavers-Joseph-Saffman interface condition11footnotemark: 1
Abstract
In this work, we propose a new analysis strategy to establish an a priori estimate of the weak solutions to the coupled steady-state dual-porosity-Navier-Stokes fluid flow model with the Beavers-Joseph-Saffman interface condition. The most advantage of our proposed method is that the a priori estimate and the existence result are independent of small data and the large viscosity restriction. Therefore the global uniqueness of the weak solution is naturally obtained.
keywords:
weak solution, dual-porosity-Navier-Stokes, Beavers-Joseph-Saffman interface condition, a priori estimate, existence, global uniqueness1 Introduction
Coupled free flow and porous medium flow systems play an important role in many practical engineering fields, e.g., the flood simulation of arid areas in geological science [20], filtration treatment in industrial production [28, 37], petroleum exploitation in mining, and blood penetration between vessels and organs in life science [19]. Specifically, the systems are usually described by Navier-Stokes equations (or Stokes equations) coupled with Darcy’s equation, and there are amounts of achievements such as [12, 13, 10, 16, 26, 36, 48]. However, the standard Darcy’s equation describes fluids flowing through only a single porosity medium, which is not accurate to deal with the complicated multiple porous media similar to naturally fractured reservoir. Actually, the naturally fractured reservoir is comprised of low permeable rock matrix blocks surrounded by an irregular network of natural microfractures, and further they have different fluid storage and conductivity properties [43, 47]. In 2016, Hou et al. [31] proposed and numerically solved a coupled dual-porosity-Stokes fluid flow model with four multi-physics interface conditions. The authors used the dual-porosity equations over Darcy’s region to describe fluid flowing through the multiple porous medium. Recently, several related research on the above model can be found in the literatures [2, 3, 24, 29, 44]. In particular, Gao and Li [24] proposed a decoupled stabilized finite element method to solve the coupled dual-porosity-Navier-Stokes fluid flow model in the numerical field.
The steady-state dual-porosity-Navier-Stokes fluid flow model has distinct features and difficulties in mathematical analysis. Many numerical methods have been studied for the well-known stationary or time-dependent Navier-Stokes/Darcy model with Beavers-Joseph or Beaver-Joseph-Saffman interface condition, including coupled finite element methods [6, 11, 21, 22, 49], discontinuous Galerkin methods [17, 26, 27], domain decomposition methods [12, 20, 21, 30, 38], and decoupled methods based on two-grid finite element [10, 23, 48, 49]. In spite of the above great contributions to numerical simulation, the existence of a weak solution to the coupled dual-porosity-Navier-Stokes fluid flow model with Beavers-Joseph-Saffman interface condition for general data keeps unresolved. In many literatures [6, 10, 17, 20, 21, 22, 26, 27, 30, 49], a priori estimates and existence of a weak solution need suitable small data and/or large viscosity restrictions, and therefore only local uniqueness can be established when the data satisfy additional restrictions. In [26], the authors pointed out that the difficulty for a priori estimates and existence with general data is stemmed from the transmission interface condition, which does not completely compensate the nonlinear convection term from the Navier-Stokes equations in the energy balance.
Therefore in this paper, stemming from resolving steady-state Navier-Stokes equations with mixed boundary conditions in [32], we shall establish a new a priori estimate of the weak solutions by coupling the model problem with a designed auxiliary problem in order to completely compensate the nonlinear convection term from the Navier-Stokes equations. In addition, we shall also prove existence of a weak solution without small data or large viscosity restriction. As a result, the global uniqueness of the weak solution is naturally obtained.
The rest of this paper is organized as follows. In Section 2, we specify the steady-state dual-porosity-Navier-Stokes fluid flow model with Beavers-Joseph-Saffman interface condition and provide its Galerkin variational formulation. In Section 3, we establish a new a priori estimate of the weak solutions by coupling the model problem with an auxiliary problem, which is designed subject to the model problem. Finally, in Section 4, we prove existence of the weak solution without small data and/or large viscosity restriction by the Galerkin method and Brouwer’s fixed-point theorem, and global uniqueness of all variables by the inf-sup condition and Babus̆ka–Brezzi’s theory.
2 Model specification
2.1 Setting of the problem
In this section, we consider the steady-state dual-porosity-Navier-Stokes fluid flow model in a bounded open polygonal domain with four physically valid interface conditions.

The domain consists of a fluid flow region and a dual-porous medium region , with interface (see Figure 1). Both and are open, regular, simply connected, and bounded with Lipschitz continuous boundaries , respectively. Here, , . The unit normal vector of the interface pointing from to (from to ) is denoted by (resp. ), and the corresponding unit tangential vectors are denoted by , . In two-dimensional case, if we write , then .
(2.1) |
where is the stress tensor, is the kinetic viscosity, is the velocity deformation tensor, denotes the fluid velocity in , denotes the kinematic pressure in , and denotes a general body force term that includes gravitational acceleration. As usual, we write formally:
The filtration of an incompressible fluid through porous media is often described using Darcy’s law. So in dual-porous medium domain , the flow is governed by a traditional dual-porosity model, which is composed of matrix and microfracture equations as follows:
(2.2) |
where , denote the matrix and microfracture flow pressure, is the dynamic viscosity, , are the intrinsic permeability of the matrix and microfracture regions, is the shape factor characterizing the morphology and dimension of the microfractures, is the sink/source term for the microfractures, and the term describes the mass exchange between matrix and microfractures.
Based on the fundamental properties of the dual-porosity fluid flow model and traditional Stokes–Darcy flow model, Hou et al. [31] introduced four physically valid interface conditions as follows to couple appropriately the dual-porosity-Stokes model, which are also adapted to our problem.
-
1.
No-exchange condition between the matrix and the conduits/macrofractures:
(2.3) -
2.
Mass conservation:
(2.4) -
3.
Balance of normal forces:
(2.5) - 4.
In (2.3)–(2.6), is the Beavers-Joseph constant depending on the properties of the dual-porous medium, represents the intrinsic permeability that satisfies the relation , is the identity matrix, and is the fluid density.
2.2 Galerkin variational formulation
Throughout this paper we use the following standard function spaces. For a Lipschitz domain , , we denote by the Sobolev space with indexes , of real-valued functions defined on , endowed with the seminorm denoted by and norm denoted by [1]. When , is denoted as and the corresponding seminorm and norm are written as and , respectively. In addition, with we denote the -dimensional Hausdorff measure of .
To perform the variational formulation, we define some necessary Hilbert spaces given by
We also need the trace space (resp. ), which is a nonclosed subspace of (resp. ) and has a continuous zero extension to (resp. ) [14, 15, 20]. For the trace space and its dual space , we have the following continuous imbedding result [15]:
(2.7) |
One can see more details in [15, 34, 45] and the references therein. For any bounded domain , denotes the inner product on , and denotes the inner product (or duality pairing) on the boundary . We also consider the following product Hilbert space with norm
In addition, based on the following formula:
we introduce the trilinear form given by ,
(2.8) |
Hence, the Galerkin variational formulation of the coupled problem (2.1)–(2.6) is proposed that: to find such that
(2.9) |
where , , the bilinear forms and are defined as
Remark 2.1.
We note that the term vanishes in (2.8) if .
Remark 2.2.
For the sake of clarity, in our analysis we shall adopt homogenous boundary conditions. In addition, for the general Dirichlet boundary conditions:
the standard homogenization technique and the lifting operators employed in [20] can be used to obtain an equivalent system with the homogeneous Dirichlet boundary conditions.
3 An a priori estimate
In this section, we shall propose an a priori estimate for possible solutions of (2.9).
3.1 Some technique inequalities
Firstly, throughout this paper we use to denote a generic positive constant independent of discretization parameters, which may take different values in different occasions. Then, based on general Sobolev inequalities, the trace theorem and the Sobolev embedding theorem [1], we have that for any bounded open set with Lipschitz continuous boundary and for all ,
(3.1) | ||||
(3.2) | ||||
(3.3) |
which can be also found in [17, 26]. We also need Poincaré inequality and Korn’s inequality [15] that for all and for all ,
(3.4) | ||||
(3.5) | ||||
(3.6) |
Moreover, for the trilinear form , the following lemma holds with the help of [4, 8], (3.1), (3.4) and (3.6).
Lemma 3.1.
For any functions , , , we have
(3.7) | ||||
(3.8) |
Proof 1.
First, let us recall the standard interpolation inequality [4, 8]: for any bounded open set with Lipschitz continuous boundary , and ,
(3.9) |
In (3.9), we set , and
-
1.
if , , , we then have
(3.10) -
2.
if , , , we then have
(3.11)
Hence, the results (3.7) and (3.8) then follow from Hölder inequality, (3.1), (3.4), (3.6), (3.10) and (3.11) when or .
3.2 The equivalent problem
Let us introduce the following divergence-free space:
and we consider the new product Hilbert space:
which equipped with the same norm as .
Thanks to [26], it provides a lower constant bound depending only on to guarantee the following inf-sup condition:
(3.12) |
Hence, by (3.12) and the same argument in [25], the Galerkin variational formulation (2.9) is equivalent to the following problem: to find such that
(3.13) |
3.3 Discretization and an auxiliary problem
Let be a quasi-uniform regular triangulation of the domain , , respectively. If assuming that the two meshes and coincide along the interface , then we can define , which is also a quasi-uniform regular triangulation of . The diameter of element is denoted as , and we set the mesh parameter .
Then we denote by a finite element space defined on . The discrete space can be naturally restricted to , so we set . Following the same technique, we establish other finite element spaces and . We assume that is a stable finite element space pair. Further we define the following vector-valued Hilbert space on :
In addition, we need a finite element subspace defined on given by
Similarly, we have
where is a weakly divergence-free finite element space on , and any function has an implicit restriction that because of the continuity of across the interface .
According to [26], the difficulty of obtaining an a priori estimate of the Navier-Stokes/Darcy fluid flow model comes from the energy unbalance due to the nonlinear convection term in (2.1). It motivates us to construct an auxiliary discrete Galerkin variational problem defined on with compatible boundary conditions, so that the auxiliary problem can compensate the nonlinear convection term in the energy balance of the Navier-Stokes equations.
To fix ideas, we first define a lifting operator as follows: for any with such that
Then, we introduce the Scott-Zhang interpolator satisfying the following properties [42]:
(3.14) | ||||
(3.15) |
Now, with the mesh parameter , the interpolator and any given , we consider the following auxiliary discrete Galerkin variational problem: to find with such that for all ,
3.4 An a priori estimate of weak solutions
We realize that (3.13) and (3.16) can form a larger coupled system because of the convection term and the constraint for the unknown variable over the interface , and we also stress that the new coupled system has no energy exchange via the interface . It implies that (3.16) is subjected to (3.13) but any possible solution of (3.13) has nothing to do with the auxiliary problem (3.16).
Theorem 3.2.
Assume that the data in the auxiliary discrete problem (3.16) satisfy small enough and . If problem (3.13) exists a possible solution , we then have the following a priori estimate that
(3.18) |
where
Here we stress that there are no assumptions for the data and physical parameters of the model problem.
Proof 2.
We denote by a possible solution of problem (3.13), and denote by the solution of problem (3.16). Then, we assume that there is a positive finite constant such that . Taking in (3.13), and noting that the terms and are non-negative, we have
(3.19) |
In addition, we note that in , and the by the definition of . Hence, the identity (2.8) can also be applied to the second term in the left hand of (3.16), that is for all ,
(3.21) |
It follows from (3.2), (3.3), (3.4), (3.6), (3.14), (3.15), Hölder inequality and the triangle inequality that
(3.22) |
As follows, we now define the dual norms of and , which are denoted as and , respectively.
Hence, by using Hölder inequality and Young’s inequality, we have
(3.23) |
In addition, based on the imbedding result (2.7), the standard trace theorem [1], Hölder inequality, Korn’s inequality, Young’s inequality, (3.15) and the following inverse inequality [39]: for any polynomial on ,
we have
(3.24) |
Finally, with the assumptions that is small enough such that , and satisfies , gathering (3.19), (3.21), (3.22), (3.23) and (3.24) yields (3.18), where
4 Existence and global uniqueness of the solution
In this section, we shall use the technique of the Galerkin method to verify that problem (3.13) has at least one weak solution, and then we can prove the global uniqueness of the weak solution due to the a priori estimate (3.18) obtained in Section 3.
4.1 The solvability of the conforming Galerkin approximation problem
We denote by the product finite element space . Then, we consider the following conforming Galerkin approximation problem of (3.13): to find such that ,
(4.1) |
To show the solvability of (4.1), stemming from Theorem 3.2, we shall consider the following constructed coupled discrete system: to find such that
(4.2) | |||||
(4.3) | |||||
(4.4) |
where is a positive constant specified later, , and in by the definition of the lifting operator . Furthermore, it follows the head statements of Section 3.4 that if is a solution of problem (4.2)–(4.4), then will solve (4.1).
Lemma 4.1.
If problem (4.1) exists a possible solution , we have the following a priori estimate that
(4.5) |
where is defined in Theorem 3.2.
Proof 3.
The proof is quite close to the proof of Theorem 3.2. To avoid repeating, we just present the differences. Since , we have
and thus the term (3.22) vanishes here. As a result, some subtle differences occur to the following estimate:
Thus, for any given mesh parameter , the result (4.5) follows the assumption that .
Now we start to verify the solvability of problem (4.2)–(4.4). For any , following the similar technique proposed in [32], we denote , , and
where with in the domain . Then, we denote by the product space , and define a mapping as: for each such that ,
(4.6) |
Clearly, define a mapping from into itself, and a zero of is a solution of the coupled system (4.2)–(4.4). Further we introduce the Brouwer’s fixed-point theorem:
Lemma 4.2.
[18] Let be a nonempty, convex, and compact subset of a normed vector space and let be a continuous mapping from into . Then has at least one fixed point.
Based on Lemma 4.1, we define a subset of as:
where is defined in Theorem 3.2. Then, taking in (4.6), and following the steps of proving Theorem 3.2 and Lemma 4.1, we obtain that
Hence, it follows Lemma 4.2 that there is at least one zero of in the ball centered at the origin.
Gathering all the above results, we conclude the following theorem:
4.2 Existence and global uniqueness
It stems from Theorem 4.3 and the conforming property that there exists a 3-tuple function in the Hilbert space , and a uniformly bounded subsequence such that
(4.8) |
Furthermore, the Sobolev imbedding implies that the above convergence results are strong in for any whenever or . In particular, by extracting another subsequence, still denoted by , we obtain
(4.9) |
Theorem 4.4.
If the data satisfies that
(4.10) |
the problem (3.13) then admits a unique solution in such that
where is defined in Theorem 3.2.
Proof 4.
(4.11) |
because of (4.8). Then, for the trace bilinear term , it follows from Hölder inequality, (3.2), and (3.4)–(3.6) that
Since the uniform boundedness of shown in (4.7) and the strong -convergence result (4.9), we derive that
which implies that is a solution of (3.13).
Finally, we assume that there are two solutions to (3.13). Then, there differences , and satisfy that ,
(4.15) |
we obtain
(4.16) |
Hence, if we assume (4.10) holds, then (4.16) shows the unique solution to (3.13) based on a priori estimate (3.18).
In order to prove the existence and uniqueness of the solution to the model problem (2.9), we shall use the inf-sup condition (3.12) and the Babus̆ka–Brezzi’s theory [5, 9, 25, 46].
Theorem 4.5.
Under the assumption (4.10) of Theorem 4.4, the model problem (2.9) admits a unique solution such that
(4.17) | ||||
(4.18) |
where is defined in Theorem 3.2.
Proof 5.
For the solution to (3.13), the following mapping:
defines an element of the dual space , and furthermore, vanishes on . As a result, the inf-sup condition (3.12) implies that there exists exactly one such that
(4.19) |
Therefore the fact and (4.19) show that the model problem (2.9) admits a unique solution . Finally, the result (4.18) is a straightforward application of the inf-sup condition (3.12) with the help of (4.15) and (4.17).
References
- [1] R. Adams, J. Fournier, Sobolev Spaces, Acadamics Press, New York, 2003.
- [2] M. A. Al Mahbub, X.-M. He, N. J. Nasu, C. Qiu, H. Zheng, Coupled and decoupled stabilized mixed finite element methods for nonstationary dual–porosity–Stokes fluid flow model, Int. J. Numer. Methods. Eng. 120 (6) (2019) 803–833. doi:10.1002/nme.6158.
- [3] M. A. Al Mahbub, F. Shi, N. J. Nasu, Y. Wang, H. Zheng, Mixed stabilized finite element method for the stationary Stokes–dual–permeability fluid flow model, Comput. Methods Appl. Mech. Engrg. 358 (2020) 112616. doi:10.1016/j.cma.2019.112616.
- [4] T. Aubin, Nonlinear Analysis on Manifolds. Monge-Ampère Equations, Grundlehren der mathematischen Wissenschaften 252, Springer-Verlag New York, NY, 1982. doi:10.1007/978-1-4612-5734-9.
- [5] I. Babus̆ka, The finite element method with Lagrangian multipliers, Numer. Math. 20 (1973) 179–192. doi:10.1007/BF01436561.
- [6] L. Badea, M. Discacciati, A. Quarteroni, Numerical analysis of the Navier-Stokes/Darcy coupling, Numer. Math. 115 (2010) 195–227. doi:10.1007/s00211-009-0279-6.
- [7] G. Beavers, D. Joseph, Boundary conditions at a naturally permeable wall, Journal of Fluid Mechanics 30 (1) (1967) 197–207. doi:10.1017/S0022112067001375.
- [8] J. Bergh, J. Löfström, Interpolation Spaces: An Introduction, Grundlehren der mathematischen Wissenschaften 223, Springer-Verlag Berlin Heidelberg, Berlin, 1976. doi:10.1007/978-3-642-66451-9.
- [9] F. Brezzi, On the existence, uniqueness and approximation of saddle-point problems arising from Lagrangian multipliers, RAIRO Anal. Numer. R2 (1974) 129–151. doi:10.1051/m2an/197408R201291.
- [10] M. Cai, M. Mu, J. Xu, Numerical solution to a mixed Navier–Stokes/Darcy model by the two-grid approach, SIAM J. Numer. Anal. 47 (5) (2009) 3325–3338. doi:10.1137/080721868.
- [11] L. Cao, Y. He, J. Li, D. Yang, Decoupled modified characteristic FEMs for fully evolutionary Navier-Stokes-Darcy model with the Beavers-Joseph interface condition, Journal of Computational and Applied Mathematics 383 (2021) 113128. doi:10.1016/j.cam.2020.113128.
- [12] Y. Cao, Y. Chu, X. He, M. Wei, Decoupling the Stationary Navier-Stokes-Darcy System with the Beavers-Joseph-Saffman Interface Condition, Abstract and Applied Analysis 2013 (2013) 136483. doi:10.1155/2013/136483.
- [13] Y. Cao, M. Gunzburger, X. He, X. Wang, Robin–Robin domain decomposition methods for the steady-state Stokes–Darcy system with the Beavers–Joseph interface condition, Numer. Math. 117 (4) (2011) 601–629. doi:10.1007/s00211-011-0361-8.
- [14] Y. Cao, M. Gunzburger, X. Hu, F. Hua, X. Wang, W. Zhao, Finite element approximations for Stokes–Darcy flow with Beavers–Joseph interface conditions, SIAM. J. Numer. Anal. 47 (6) (2010) 4239–4256. doi:10.1137/080731542.
- [15] Y. Cao, M. Gunzburger, F. Hua, X. Wang, Coupled Stokes–Darcy model with Beavers–Joseph interface boundary condition, Commun. Math. Sci. 8 (1) (2010) 1–25. doi:10.4310/CMS.2010.v8.n1.a2.
- [16] W. Chen, M. Gunzburger, S. Dong, X. Wang, Efficient and long-time accurate second-order methods for Stokes-Darcy system, SIAM J. Numer. Anal. 51 (5) (2013) 2563–2584. doi:doi:10.1137/120897705.
- [17] P. Chidyagwai, B. Rivière, On the solution of the coupled Navier–Stokes and Darcy equations, Comput. Methods Appl. Mech. Engrg. 198 (47) (2009) 3806–3820. doi:10.1016/j.cma.2009.08.012.
- [18] D. Cioranescu, V. Girault, K. R. Rajagopal, Mechanics and Mathematics of Fluids of the Differential Type, Advances in Mechanics and Mathematics, vol. 35. Springer International Publishing, Cham, Switzerland, 2016. doi:10.1007/978-3-319-39330-8.
- [19] C. D’Angelo, P. Zunino, Robust numerical approximation of coupled Stokes’ and Darcy’s flows applied to vascular hemodynamics and biochemical transport, ESAIM: Mathematical Modelling and Numerical Analysis 45 (3) (2011) 447–476. doi:10.1051/m2an/2010062.
- [20] M. Discacciati, Domain decomposition methods for the coupling of surface and groundwater flows, Ph.D. thesis, Ecole Polytechnique Fédérale de Lausanne, Switzerland, 2004. doi:10.5075/epfl-thesis-3117.
- [21] M. Discacciati, A. Quarteroni, Navier-Stokes/Darcy Coupling: Modeling, Analysis, and Numerical Approximation, Rev. Mat. Complut. 22 (2) (2009) 315–426. doi:10.5209/rev_REMA.2009.v22.n2.16263.
- [22] M. Discacciati, R. Oyarzúa, A conforming mixed finite element method for the Navier–Stokes/Darcy coupled problem, Numer. Math. 135 (2017) 571–606. doi:10.1007/s00211-016-0811-4.
- [23] J. Fang, P. Huang, Y. Qin, A two-level finite element method for the steady-state Navier-Stokes/Darcy model, J. Korean Math. Soc. 57 (4) (2020) 915–933. doi:10.4134/JKMS.j190449.
- [24] L. Gao, J. Li, A decoupled stabilized finite element method for the dual-porosity-Navier–Stokes fluid flow model arising in shale oil, Numer. Methods Partial Differential Eq. (2020) 1–18. doi:10.1002/num.22718.
- [25] V. Girault, P. A. Raviart, Finite element methods for Navier–Stokes equations, Springer-Verlag, Berlin, 1986. doi:10.1007/978-3-642-61623-5.
- [26] V. Girault, B. Rivière, DG Approximation of Coupled Navier–Stokes and Darcy Equations by Beaver–Joseph–Saffman Interface Condition, SIAM J. Numer. Anal. 47 (3) (2009) 2052–2089. doi:10.1137/070686081.
- [27] V. Girault, G. Kanschat, B. Rivière, On the Coupling of Incompressible Stokes or Navier-Stokes and Darcy Flows Through Porous Media. In: J. Ferreira, S. Barbeiro, G. Pena, M. Wheeler(eds) Modelling and Simulation in Fluid Dynamics in Porous Media. Springer Proceedings in Mathematics & Statistics, vol 28. Springer, New York, NY, 2013. doi:10.1007/978-1-4614-5055-9_1.
- [28] N. Hanspal, A. Waghode, V. Nassehi, R. Wakeman, Numerical analysis of coupled Stokes/Darcy flows in industrial filtrations, Transport in Porous Media 64 (1) (2006) 73. doi:10.1007/s11242-005-1457-3.
- [29] X. He, N. Jiang, C. Qiu, An artificial compressibility ensemble algorithm for a stochastic Stokes-Darcy model with random hydraulic conductivity and interface conditions, International Journal for Numerical Methods in Engineering 121 (4) (2020) 712–739. doi:10.1002/nme.6241.
- [30] X. He, J. Li, Y. Lin, J. Ming, A domain decomposition method for the steady-state Navier-Stokes-Darcy model with Beavers-Joseph interface condition, SIAM J. Sci. Comput. 37 (5) (2015), 264–290. doi:10.1137/140965776.
- [31] J. Hou, M. Qiu, X. He, C. Guo, M. Wei, B. Bai, A dual–porosity–Stokes model and finite element method for coupling dual–porosity flow and free flow, SIAM J. Sci. Comput. 38 (5) (2016) B710–B739. doi:10.1137/15M1044072.
- [32] Y. Hou, S. Pei, On the weak solutions to steady Navier-Stokes equations with mixed boundary conditions, Mathematische Zeitschrift 291 (2019) 47–54. doi:10.1007/s00209-018-2072-7.
- [33] I. P. Jones, Low Reynolds number flow past a porous spherical shell, Mathematical Proceedings of the Cambridge Philosophical Society 73 (1) (1973) 231–238. doi:10.1017/S0305004100047642.
- [34] R. Li, J. Li, Z. Chen, Y. Gao, A stabilized finite element method based on two local Gauss integrations for a coupled Stokes–Darcy problem, Journal of Computational and Applied Mathematics 292 (15) (2016), 92–104. doi:10.1016/j.cam.2015.06.014.
- [35] A. Mikelić, W. Jäger, On the interface boundary condition of Beavers, Joseph, and Saffman, SIAM Journal on Applied Mathematics 60 (4) (2000) 1111–1127. doi:10.1137/S003613999833678X.
- [36] M. Mu, X. Zhu, Decoupled schemes for a non-stationary mixed Stokes-Darcy model, Mathematics of Computation 79 (270) (2010) 707–731. doi:10.1090/S0025-5718-09-02302-3.
- [37] V. Nassehi, Modelling of combined Navier-Stokes and Darcy flows in crossflow membrane filtration, Chemical Engineering Science 53 (6) (1998) 1253–1265. doi:10.1016/S0009-2509(97)00443-0.
- [38] C. Qiu, X. He, J. Li, Y. Lin, A domain decomposition method for the time-dependent Navier-Stokes-Darcy model with Beavers-Joseph interface condition and defective boundary condition, Journal of Computational Physics 411 (2020) 109400. doi:10.1016/j.jcp.2020.109400.
- [39] B. Rivière, Discontinuous Galerkin methods for solving elliptic and parabolic equations. Theory and implementation, Front. Appl. Math. 35, SIAM, Philadelphia, 2008. doi:10.1137/1.9780898717440.
- [40] H. G. Roos, M. Stynes, L. Tobiska, Robust numerical methods for singularly perturbed differential equations. Convection–Diffusion–Reaction and Flow Problems, 2nd ed., Springer Ser. Comput. Math. 24, Springer, Berlin, 2008. doi:10.1007/978-3-540-34467-4.
- [41] P. G. Saffman, On the boundary condition at the surface of a porous medium, Studies in Applied Mathematics 50 (2) (1971) 93–101. doi:10.1002/sapm197150293.
- [42] L. Scott, S. Zhang, Finite element interpolation of nonsmooth functions satisfying boundary conditions, Math. Comp. 54 (190) (1990) 483–493. doi:10.1090/S0025-5718-1990-1011446-7.
- [43] K. Serra, A. C. Reynolds, R. Raghavan, New pressure transient analysis methods for naturally fractured reservoirs, Journal of Petroleum Technology 35 (12) (1983) 2271–2283. doi:10.2118/10780-PA.
- [44] L. Shan, J. Hou, W. Yan, J. Chen, Partitioned time stepping method for a dual–porosity–Stokes model, J. Sci. Comput. 79 (1) (2019) 389–413. doi:10.1007/s10915-018-0879-3.
- [45] L. Shan, H. Zheng, Partitioned time stepping method for fully evolutionary Stokes–Darcy flow with Beavers–Joseph interface conditions, SIAM J. Numer. Anal. 51 (2) (2013) 813–839. doi:10.1137/110828095.
- [46] R. Temam, Navier–Stokes Equations: Theory and Numerical Analysis, 3rd Edition, North-Holland, Amsterdam, 1984. doi:10.1090/chel/343.
- [47] J. E. Warren, P. J. Root, The behavior of naturally fractured reservoirs, Society of Petroleum Engineers Journal 3 (3) (1963) 245–255. doi:10.2118/426-PA.
- [48] J. Zhao, T. Zhang, Two-grid finite element methods for the steady Navier-Stokes/Darcy model, East Asian Journal on Applied Mathematics 6 (1) (2016) 60–79. doi:10.4208/eajam.080215.111215a.
- [49] L. Zuo, Y. Hou, Numerical analysis for the mixed Navier–Stokes and Darcy Problem with the Beavers–Joseph interface condition, Numer. Methods Partial Differential Eq. 31 (2015) 1009–1030. doi:10.1002/num.21933.