We study the asymptotic behavior of pressure-driven Stokes flow in a thin domain. By letting the thickness of the domain tend to zero we derive a generalized form of the classical Reynolds–Poiseuille law, i.e. the limit velocity field is a linear function of the pressure gradient. By prescribing the external pressure as a normal stress condition, we recover a Dirichlet condition for the limit pressure. In contrast, a Dirichlet condition for the velocity yields a Neumann condition for the limit pressure.
We consider the flow of an incompressible Newtonian fluid in a thin domain in whose characteristic length ε in the l directions is much smaller than those in the other m directions. Such thin structures allow the following representation of the boundary: , where the measure of (Neumann boundary) is of the order while the measure of (Dirichlet boundary) is of order unity. The Dirichlet part is modelled as a solid wall by imposing a no-slip condition for the velocity field. The Neumann part is modelled as a penetrable inlet/outlet boundary, by prescribing the normal stress. Thus, the flow is driven by an external pressure gradient alone, which is applied as a surface force along . That is, no body forces or moving boundaries are contributing to the motion of the fluid, although such effects can be superimposed. Since the flow is assumed to be governed by the Stokes equation, inertial effects are also neglected.
Our aim is to obtain a precise asymptotic description of the flow by letting the thickness parameter ε tend to zero. A dimensional reduction of the problem is accomplished by a technique called two-scale convergence for thin domains, which was developed by Marušić and Marušić-Paloka [11]. This framework offers an elegant approach compared to previous methods which have relied mostly on rescaling techniques.
As a result we obtain a generalized form of the Reynolds–Poiseuille law. The original laws were formulated by Reynolds [16] in the context of lubrication theory (moving boundaries) and Poiseuille [15] who studied flow of water through thin glass tubes and the effects of pressure drop. The first rigorous mathematical derivation of Reynolds work was done by Bayada and Chambat [1]. Starting from the Stokes system and assuming that the velocity field satisfies a Dirichlet condition on the whole boundary, the authors prove that the limit pressure satisfies the classical Reynolds equation with a Neumann condition. In real-life applications, however, it is more common that the Reynolds equation is solved by prescribing the boundary values of the pressure [13]. Under present assumptions we obtain the Reynolds equation with a Dirichlet boundary condition for the pressure, which is in better agreement with engineering practice. Furthermore, this illustrates the general manner in which boundary conditions are preserved for asymptotic limits:
A Dirichlet condition for the velocity field in the original problem, posed in a thin domain, becomes a Neumann condition for the pressure in the limit problem, posed in a domain of unit thickness.
A Neumann condition for the stress tensor in the original problem becomes a Dirichlet condition for the pressure in the limit problem.
A similar result holds for Stokes flow in a porous medium [5].
Let us also mention that there seems to be no precise definition of the term “pressure-driven flow” in the scientific literature. From a physical point of view one can argue that the stress vector (traction) should be continuous across the interface between two similar fluids, see e.g. Lamb [9, Art. 327]. It therefore makes sense to prescribe all components of the stress vector on some part of the boundary provided that the surrounding fluid is of the same constitutive type. The situation is more complicated for the interface between two dissimilar fluids, say a droplet of water surrounded by air, which is characterized by a jump in the density and continuity of the tangential velocity. For a general discussion regarding boundary conditions at fluid-fluid interfaces we refer to Ch. 5 of Panton [12]. Although the pressure of an incompressible fluid has a precise mathematical definition, it does not have a clearly defined physical meaning – one can measure only the normal component of the total stress (including the viscous part). We therefore choose to prescribe the boundary values for the pressure implicitly as a Neumann condition for the stress tensor. As shown in the works of Glowinski [7,8] and Pironneau [14], the resulting boundary value problem is well-posed. In particular, for the mixed boundary value problem both pressure and velocity are uniquely determined. Nevertheless, alternative formulations exist. For example, it is possible to impose an explicit boundary condition for the pressure on one part of the boundary as shown in [3,10], provided that the tangential component of the velocity is prescribed on the same part. Both formulations could be legitimate – the preferred choice depends on the boundary data available. Suppose that one could measure only the average stresses at the inlet and the outlet of a finite pipe connecting two large reservoirs of fluid, where the streamlines bend slightly at both ends of the pipe. Then the normal stress condition seems like the most realistic alternative.
Problem formulation
Thin geometry
Following [11], let ω be a bounded domain in with a Lipschitz boundary and let be a family of domains in such that:
For each , the set is contained in the unit cube in .
There exists such that the ball
of radius α is contained in for each .
The set
forms a Lipschitz domain in .
The boundary of Ω is divided into two disjoint parts
The thin geometry is defined by anisotropic scaling of the domain Ω using the parameter :
In particular, for there are two possible configurations: the thin film and the thin pipe (see Fig. 1 and 2 respectively).
Structure of Ω (thin film).
Structure of Ω (thin pipe).
Function spaces
Let . We shall work mainly with the following spaces
Clearly , both being closed subspaces of . Since has positive surface measure (by assumption) we can equip with the norm
which is equivalent to the usual -norm by Friedrichs’ inequality.
Problem
In we pose the following boundary value problem for the velocity field and the pressure field :
Here is the outward unit normal of and
denotes the symmetric part of the velocity gradient. Thus, (2) becomes the Stokes system, driven by an external pressure , which is implicitly imposed by condition (2c). The scalar function is assumed to depend only on the variable . Such a restriction seems reasonable as it excludes circular or re-entrant flow in the vicinity of . Note also that the system (2) depends only the boundary values of restricted to .
Existence and uniqueness
Let the normalized pressure be defined by
Then a weak formulation of (2) is given by
for all , where . By standard arguments, such as the Korn inequality and the Lax–Milgram theorem, it can be shown that the weak formulation (3) has a unique solution in . For the details we refer to [8, Ch. 4] or [4]. However, to prove the homogenization result (see Theorem 3.4 below) we need careful a priori estimates for the velocity and the pressure. This question is addressed in Section 4.
Main result
The notion of two-scale convergence for thin domains was introduced by Marušić and Marušić-Paloka in [11]. We recall here the definition.
Following the notation in Section 2.1 we say that a sequence in two-scale converges to u in provided that
for all φ in and we write . Moreover, we say that two-scale converges strongly to u if
and we write (strongly).
Next, we introduce the concept of permeability function for thin domains.
The solution ϕ of the boundary value problem
is called the permeability function of Ω. That is, for each , is the solution of
where
The permeability of the domain is defined as
The regularity of the function ϕ, defined by equation (6), depends on the smoothness of the boundary . For the main result to hold it seems that a minimum requirement would be
with . Furthermore, hypothesis (ii) in Section 2.1 is necessary to have . To avoid technicalities, we assume the stronger condition that ϕ belongs to . Indeed, this is the case for Examples 3.1 and 3.2 below (both very important from application point of view). In the general case, however, it is not clear to us if the requirement that is of class is sufficient to ensure -regularity for ϕ.
(Main result).
For eachthe boundary value problem (
2
) has a unique solutionsuch thatwhere the constant C depends only on Ω and. Let ϕ denote the permeability function defined by (
6
). Then the following strong two-scale convergence holds,where u inis defined byand p inis the solution of the boundary value problemwhere a is defined by (
7
).
Note that the Dirichlet boundary condition (9b) for the limit pressure arises from the Neumann condition (2c) for the stress tensor in the original problem. By contrast, if one imposes a non-homogeneous Dirchlet condition for the velocity field on , one ends up with a Neumann condition in (9) (see equation (5.7) in [1]). For practical purposes, the main difference between the two is that the limit pressure is uniquely determined by (9b), whereas it is only defined up to an additive constant for the Neumann problem. The limit velocity u is uniquely defined in both formulations.
Example 1 (Reynolds’ law)
Let and . For simplicity is denoted as x. Suppose ω is a Lipschitz domain in and that is the line segment
where (see Fig. 1 and Fig. 3(a)). Thus, the thickness of the film is given by the function , which is assumed to be bounded from below by the constant . Then the permeability function satisfies
whose solution is given by
Hence, the pressure equation (9) becomes the classical Reynolds equation with a Dirichlet boundary condition:
This equation together with
gives the asymptotic solution for pressure-driven incompressible flow in a thin film of variable thickness .
Fluid domains.
Example 2 (Poiseuille’s law)
Let and . As above, is denoted as x. Suppose is the line segment and that is the disc
where (see Fig. 2 and Fig. 3(b)). The radius is assumed to be bounded from below by the constant α. Switching to polar coordinates, , we see that the permeability function ϕ satisfies
Solving this equation gives
Hence, (9) becomes the classical Poiseuille equation with a Dirichlet boundary condition:
Thus, the last equation together with
gives the asymptotic solution for pressure-driven incompressible flow in a thin circular pipe of length L and of variable radius .
Estimates
Korn inequality
To obtain precise a priori estimates of the velocity field in (3) we need to control the constant in the Korn inequality for the domain as ε tends to zero. The following estimates show how the constant depends on the parameter ε.
Letanddenote the best constants in the inequalitiesfor all. Then there exist constantsanddepending only on Ω andsuch that
For the velocity, the following estimates holdwhereandare the constants in Theorem
4.1
.
By choosing in (3), using , we establish
By the Korn inequality (12), the right-hand side can be estimated as
Thus, we obtain
Applying the Korn inequality anew (to the left side) gives
□
The Bogovskiĭ operator
Let denote the quotient space of by . Thus, consists of equivalence classes of elements modulo the space of divergence free elements. By a result of Bogovskiĭ [2] (see also [4,6,17]) the operator
defined by is an isomorphism, provided that has positive surface measure and non-empty interior. The so called Bogovskiĭ operator
is defined as the inverse of the operator A. It follows that the dual operator
is an isomorphism called the pressure operator (or de Rham–Tartar operator). Subsequently we write to emphasize the dependence of B on the domain . To obtain a -bound for the pressure, we estimate the operator norm
Letdenote the Bogovskiĭ operator. Then there exist positive constantsanddepending only on Ω andsuch that
We would like to point out that the lower bound in Theorem 4.3 for the norm of the Bogovskiĭ operator is not needed to prove the main result, nor is it used anywhere in the analysis. It is included only to show that the norm does indeed “blow up” as and that an upper bound of the form is the best possible.
Pressure estimate
The normalized pressuresatisfies the estimatewhereis the constant in Theorem
4.1
andis the constant in Theorem
4.3
.
Let be defined by
From (3), we see that belongs to . Since
we deduce
Let in be defined by the pressure operator, i.e.
From Theorem 4.3 we infer
□
Two-scale convergence
Convergence result
Since , we have
By Theorems 4.2 and 4.5, the solution of (3) satisfies
for some constant C that does not depend on ε. Indeed, C can be chosen as
For any sequenceinsatisfying the bound (
17
), there existswith, whereandsuch that, up to a subsequence,
wheredenotes the m first components of u anddenotes the l last components of u,
For the sake of completeness we provide the proof which follows the same ideas as in [11]. In view of (17) and Theorem 1 in [11] there exists such that, up to a subsequence,
for any . Furthermore, there exists such that, up to a subsequence,
for any .
Since vanishes on we have
for all such that on . Multiplying (18) with and passing to the limit gives
Choosing we see that u is weakly differentiable w.r.t. to the variable y, with . Hence the trace of u on is well defined. Applying the divergence theorem to (19) we obtain
for all such that on . We conclude that u satisfies the Dirichlet condition on . Convergence of the symmetric part of the gradient follows by linearity. □
Conservation of volume
Letbe as in Lemma
5.1
with the additional condition thatin. Then any subsequential two-scale limitsatisfiesand
The proof is very similar to the proof of [11, Proposition 4]. We include it only for the sake of completeness. The divergence free condition for can be stated as
for all scalar test-functions . It follows that
for all such that on . Multiplying (22) with and passing to the limit we obtain
hence (20).
Choosing such that on in (22) and multiplying with , the limit equation becomes
hence (21). □
Momentum equation
(The thin film equations).
Letand q be as in Lemma
5.1
. Then the first componentand q satisfywhereas the second component.
By taking φ in (3) of the form
we obtain
for all . Letting gives
where is defined in Lemma 5.1. Consequently
for all . Clearly, the last equality is the weak form of the homogenized problem (23).
By taking φ in (3) of the form
where is a smooth function such that , we obtain
Letting gives
By density, this relation is valid also for . Thus, from Korn’s inequality we conclude that , due to the Dirichlet condition on . □
The class of test functionsfor which (
25
) holds can be enlarged towhich consists of allsuch that
,
on,
.
Moreover,belongs to.
Since and can be extended by zero outside , we can write the first term in (25) as
Thus (25) can be written as
This relation holds for all , since is dense in . □
Pressure equation
Let be the permeability function defined by (6). Upon substituting it is readily seen that
is a solution of (23) in the sense of distributions. There remains to prove -regularity for p and to find the boundary value problem that this function satisfies. To this end we take in (26),
where Φ is an arbitrary vector field in . Thus we obtain
Using (6) we obtain
where a is defined by (7) and
Relation (27) proves that q belongs to with
provided that (see Remark 3.3), which is equivalent to
Using the divergence free condition for (Lemma 5.2) we see that belongs to and is a solution of (9). Hence p and u are uniquely determined and we conclude that the convergence holds for the whole sequence.
Strong convergence
There remains to prove the strong two-scale convergence of the velocity and the pressure. By Lemma 1, part (i) of [11] it suffices to prove that
Choosing in (3), we obtain
as . Using (26) with test function (Lemma 5.4) we see that
This proves the strong two-scale convergence
Strong two-scale convergence of the velocity
To prove strong two-scale convergence of , consider the auxiliary problem
For each this problem has a unique solution such that
where the constant C does not depend on ε. The derivation of this inequality is analogous to the derivation of (17), so is the limit process when . We therefore omit all arguments that are similar to those used in Section 5 and state merely the conlusions. Extracting subsequences such that
we find that the limit satisfies
for all and by density (see Lemma 5.4) we have
for all .
Using the weak formulation of (29), with test function , and the strong convergence (28), we can pass to the limit in
as . Choosing in (30), using Lemma 5.2, we deduce
Hence strongly.
Strong two-scale convergence of the pressure
To prove the strong convergence of , we consider another auxiliary problem:
For each this problem has a unique solution such that
where the constant C does not depend on ε. By compactness, as in Lemma 5.1, we can extract a subsequence such that
with on and . Here there is no need to find the limit problem satisfied by , but we need to show that . From the second and fourth equation of (31) it follows that
for all scalar test functions such that on . Multiplying (32) with and passing to the limit we obtain
so in Ω. Choosing such that on in (32) and multiplying with , the limit equation becomes
so
This proves that z belongs to the extended class of test functions defined in Lemma 5.4.
Taking in the weak formulation (3) with , gives
thanks to the strong convergence of as . Choosing in (26) with (note that in this case ), we see that
Hence strongly.
Footnotes
Acknowledgement
The authors wish to thank an anonymous referee for many thoughtful comments and suggestions which significantly improved the final version of this paper.
Proof of Theorem 4.1
First we show how the constant in the Korn inequality behaves under isotropic scaling of the domain. To this end, let denote the cube in of length ε confined between the hyperplanes
For we omit the superscripts.
To estimate the constant in the Korn inequality under anisotropic scaling of the domain we use an extension operator in combination with a covering argument. In view of the assumptions stated in Section 2.1, we can assume, without loss of generality, that
so that . Indeed, due to the Dirichlet condition on , we can extend any by zero to which is confined between the hyperplanes . Moreover, we choose large enough so that the set
satisfies
Extension operator.
Covering argument. For let denote the cube in of length ε centered at z, i.e.
For each , there exists a finite collection of points in such that
Set
Then
for all . Since each cube is a translation of the cube we can use the inequality (35) locally.
Suppose v in . In order to use the extension operator in Lemma A.2, let in be defined by
Thus we obtain
or
Hence
This gives an upper bound for in (12). The estimation of in (13) is completely analogous. □
Proof of Theorem 4.3
The upper bound is proved by a simple scaling argument. For the lower bound we estimate for a special function ψ.
For any , let denote the scaling operator defined by
where and similarly for . Clearly, is invertible with . A simple change of variables shows that maps onto with
Moreover, maps onto with
In particular, acting on through
is well defined in .
References
1.
G.Bayada and M.Chambat, The transition between the Stokes equations and the Reynolds equation: A mathematical proof, Appl. Math. and Optim.14 (1986), 73–93. doi:10.1007/BF01442229.
2.
M.E.Bogovskiĭ, Solution of the first boundary value problem for the equation of continuity of an incompressible medium, Soviet. Math. Doklady20 (1979), 1094–1098.
3.
C.Conca, F.Murat and O.Pironneau, The Stokes and Navier–Stokes equations with boundary conditions involving the pressure, Japan J. Math.20(2) (1994), 279–318. doi:10.4099/math1924.20.279.
4.
J.Fabricius, Stokes flow with kinematic and dynamic boundary conditions, Quart. Appl. Math. (2019), To appear. doi:10.1090/qam/1534.
5.
J.Fabricius, E.Miroshnikova and P.Wall, Homogenization of the Stokes equation with mixed boundary condition in a porous medium, Cogent Mathematics4(1) (2017).
6.
G.P.Galdi, An Introduction to the Mathematical Theory of the Navier–Stokes Equations, Springer, New York, 2011.
7.
R.Glowinski, Numerical Methods for Nonlinear Variational Problems, Springer-Verlag, New York, 1984.
8.
R.Glowinski, Finite Element Methods for Incompressible Viscous Flow, P.G.Ciarlet and J.L.Lions, eds, Handbook of Numerical Analysis, Vol. IX, Numerical Methods for Fluids (Part 3), Elsevier, 2003.
9.
H.Lamb, Hydrodynamics, 6th edn, Cambridge University Press, London, 1932.
10.
S.Marušić, On the Navier–Stokes system with pressure boundary condition, Ann. Univ. Ferrara Sez. VII Sci. Mat.53(2) (2007), 319–331. doi:10.1007/s11565-007-0024-y.
11.
S.Marušić and E.Marušić-Paloka, Two-scale convergence for thin domains and its applications to some lower-dimensional models in fluid mechanics, Asymptotic Analysis23(1) (2000), 23–57.
F.Pérez-Ràfols, R.Larsson and A.Almqvist, Modelling of leakage on metal-to-metal seals, Tribology International94 (2016), 421–427. doi:10.1016/j.triboint.2015.10.003.
14.
O.Pironneau, Finite Element Methods for Fluids, John Wiley & Sons, Ltd., Chichester, 1989.
15.
J.L.M.Poiseuille, Recherches expérimentales sur le mouvement des liquides dans les tubes de très petits diamètres; I. Influence de la pression sur la quantité de liquide qui traverse les tubes de très petits diamètres, C. R. Acad. Sci.11 (1840), 961–967.
16.
O.Reynolds, On the theory of lubrication and its application to Mr. Beauchamp Tower’s experiments, Phil. Trans. Roy. Soc. London A117 (1886), 157–234.
17.
L.Tartar, Topics in Nonlinear Analysis, Publications Mathématiques d’Orsay, Université de Paris-Sud, Orsay, 1978.