The singular limit of the thin film Muskat problem is performed when the density (and possibly the viscosity) of the lighter fluid vanishes and the porous medium equation is identified as the limit problem. In particular, the height of the denser fluid is shown to converge towards the solution to the porous medium equation and an explicit rate for this convergence is provided in space dimension . Moreover, the limit of the height of the lighter fluid is determined in a certain regime and is given by the corresponding initial condition.
The thin film Muskat problem is the strongly coupled degenerate parabolic system
which describes the motion of two thin fluid layers on an impermeable horizontal bottom, identified with the hyperplane , under the influence of gravity. Here is the thickness of the layer which has density and viscosity and is the thickness of the layer with density and viscosity . In particular, (1.1) is a model for the spreading of two fluid blobs of different fluids on an impermeable surface. We assume that , the positive constants in (1.1) being given by the relations
The system (1.1) is derived in [11,12,25] in a one-dimensional setting and most of the analysis devoted so far to this problem, which we review now, is restricted to the one-dimensional case . The well-posedness of (1.1) in the setting of classical solutions is addressed in [11], while non-negative global weak solutions are constructed, by different approaches, in [3,9,10,13,14]. The rich dynamics described by the thin film Muskat problem (1.1) is very well illustrated by the laboratory experiments described in [25], but also by the numerical simulations reported in [1,2,15]. Besides, from a mathematical point of view, many of these experimental and numerical observations are rigorously established. In particular, non-negative weak solutions to (1.1) possess finite speed of propagation and solutions emanating from certain initial data feature the waiting time phenomenon, see [14]. However, the finite speed of propagation property for a single fluid phase, that is, when only (or ) is compactly supported, is still an open problem. When the system (1.1) is posed on , the large time behavior of weak solutions is investigated in [15]. More precisely, it is shown that solutions starting from even initial data converge towards the (unique) even self-similar solution, a property which is in perfect agreement with the laboratory experiments reported in [25]. It is worthwhile to mention, as a special feature of the one-dimensional thin film Muskat problem (1.1), that, depending on the values of the parameters R and μ, there may exist a continuum of self-similar solutions which are not symmetric, see [15], and every weak solution to (1.1) converges to one of these special solutions for large times. Determining which self-similar solutions are attained in the large time limit is still an open problem, but numerical simulations performed in [15] seem to indicate that some of these non-symmetric self-similar solutions attract certain non-negative weak solutions. The dynamics is much simpler in dimension , as there exists only one self-similar solution to (1.1) which is radially symmetric and a global attractor, see [2].
Though the thin film Muskat problem is formally derived as the singular limit of the Muskat problem when letting the thickness of the fluid layers vanish [11], it is rather immediate to notice that (1.1) can be viewed as a two-phase generalization of the well-known porous medium equation
see [6,24]. Indeed, when , f solves, up to a multiplicative factor which can be scaled out, the equation (1.2). The goal of this paper is to establish the latter observation rigorously by performing the singular limit
with μ kept constant or even letting , to recover the porous medium equation (1.2) in the limit, see Theorem 1.2–Theorem 1.5 below. In order to present our results, we first quantify how (and possibly also ) vanishes by setting
with , , and a positive constant (we will let ). For this choice of the parameters R and μ, the system (1.1) becomes
We supplement (1.4) with initial data
where
We next recall that the system (1.1) is a gradient flow for the energy functional
with respect to the 2-Wasserstein distance, see [13], a similar property being available for the porous medium equation (1.2) as observed earlier in [20,21]. Additionally, the entropy functional
is also non-increasing along solutions to (1.1). The gradient flow structure and the time monotonicity of (1.7) are used in [13] to construct non-negative global weak solutions to (1.1). The next theorem just recalls the statement of [13, Theorem 1.1] and provides also the corresponding results in the case , as the strategy used in [13] can be adapted to establish Theorem 1.1 in arbitrary space dimension .
Let,, and assume (
1.3
). Then, there exists a pairsuch that
,,
with,
andis a weak solution to (
1.4
)–(
1.5
) in the sense thatfor alland. In addition,satisfy the following estimates:for almost all.
From now on and are fixed in and , , denotes the solution to the evolution problem (1.4)–(1.5) provided by Theorem 1.1. In our first main result, see Theorem 1.2 below, we establish the convergence of the family found in Theorem 1.1 towards a weak solution to the porous medium equation (1.2) as along a suitable sequence.
Let,, and assume (
1.3
). There exists a sequencewithand a functionwithsuch thatinfor allas. Moreover, f is a weak solution to the porous medium equation (
1.2
) determined by the initial conditionin the sense that it satisfies (
1.9
) andfor alland.
Even though there are several uniqueness results available for the porous medium equation (1.2) in the literature, see [4,5,8,19,22,24] and the references therein, uniqueness of a weak solution to (1.2) in the sense of Theorem 1.2 does not seem to be dealt with and is thus reported below when the space dimension satisfies , see Theorem 1.3. In fact, Theorem 1.3 improves Theorem 1.2 in space dimension by providing rates for the convergence of the whole family as towards the solution f to the porous medium equation.
Let,, and assume (
1.3
). Then, the porous medium equation (
1.2
) with initial datahas a unique solution f in the sense of Theorem
1.2
and there exists a positive constantsuch that
On the one hand, the occurrence of the -norm in Theorem 1.3 is not surprising, as it is well-known that the porous medium equation (1.2) has a gradient flow structure in [7]. Also, the -norm is instrumental in some uniqueness proofs [8,22]. On the other hand, the dimension-dependent exponent of ε featured in (1.11) is connected to the low regularity assumed on the solutions to (1.2) and (1.4). Under the additional assumption that an ε-independent -bound is available for the solutions to (1.2) and (1.4), the outcome of Theorem 1.3 can be improved as follows.
Let,, and assume (
1.3
). Ifand if there exists a positive constant κ such thatthen there exists a positive constantsuch that
The boundedness (1.12) is well-known for the solution to the porous medium equation (1.2), as the comparison principle ensures that for . Such a bound is far from being obvious for solutions to (1.1) and we refer to [16,17] for results in that direction.
Finally, in Theorem 1.5 we establish the convergence of the family towards the initial condition in the regime where .
Let,, and assume (
1.3
). Then, there exists a positive constantsuch that
The outline of the paper is as follows. In Section 2 we deduce from Theorem 1.1 a handful of estimates for the solutions to the problem (1.4)–(1.5) which form the basis of the proof of the convergence result stated in Theorem 1.2. Section 3 is next devoted to the proofs of Theorem 1.3 and Corollary 1.4, which use the estimates from Section 2, a duality technique, and Gronwall’s lemma. Finally, in Section 4, we establish Theorem 1.5, using once more the estimates established in Section 2.
To begin with, we derive from Theorem 1.1 estimates for solutions to the evolution problem (1.4)–(1.5), see Lemma 2.1. These estimates, together with Lemma 2.2 and a classical compactness result [23, Corollary 4], enable us to establish the convergence of along a sequence towards the solution to the porous medium equation (1.2), see Lemma 2.3. We conclude the section with the proof of Theorem 1.2. In the following we use the shorthand notation
Since and
the estimates (i)–(ii) directly follow from the definition of and the energy inequality, see Theorem 1.1(b).
In order to prove (iii), let us consider, for each , the function defined by
We point out that is continuously differentiable and has compact support, hence it can be approximated in the -norm by functions in . Moreover, the properties of the solutions to the problem (1.4)–(1.5) listed in Theorem 1.1 enable us to show that
Hence, using , , as test functions in (1.8), these convergences yield in the limit that
In particular, it follows from (1.3) and Theorem 1.1(b) that there exists a constant such that
Taking advantage of [13, Lemma A.1], we find a positive universal constant such that
which, together with (2.1) and the entropy estimate in Theorem 1.1(a), shows that
Since and for , we conclude, together with (1.3), that there exists a constant with the property that
and (iii) follows from the above inequality.
Next, a classical consequence of Theorem 1.1 (see Lemma 3.1 below for a related result) ensures that solves (1.4) in distributional sense; that is,
where the fluxes and are given by
The estimates (i)–(ii) from Theorem 1.1, along with Hölder’s inequality, lead us to
which shows that is bounded in . This property immediately implies (iv) by a duality argument.
Finally, the bound (v) is a straightforward consequence of (2.1). □
The next step is the continuity and compactness of some embeddings involving weighted -spaces, which will serve when establishing the convergence of the family (along a suitable sequence ).
Given, the embeddingis continuous.
The embeddingis compact.
The claim (i) with is obvious. For , Hölder’s inequality leads us to
and (i) follows.
With respect to (ii), let be a bounded sequence in and set
Owing to the compactness of the embedding of in for any , where we set , it follows from a standard Cantor diagonal procedure that there exist a function and a subsequence of (not relabeled) such that in for all and
Choosing such that when , Sobolev’s embedding and (2.4) then lead us to
for all and . Letting first and then , we deduce that in . Finally, for ,
Arguing as before completes the proof of (ii). □
We now use the estimates derived in Lemma 2.1 and the previous result to deduce the following convergences.
Let,, and assume (
1.3
). Then, there exist a sequencewithand a functionfor allsuch that
inand infor all;
infor all;
in;
infor all.
Let be fixed. In view of Lemma 2.1(i), (iii), and (v), we obtain the boundedness of in and in , as well as that of in . Hence, the family is bounded in . Since
and the first embedding is compact according to Lemma 2.2(ii), we infer from a classical compactness result, see [23, Corollary 4], and a Cantor diagonal argument that there exist a sequence and a function f such that in and in for all . Note that Lemma 2.1(i) now immediately implies that .
Next, the convergence (ii) is a straightforward consequence of Lemma 2.1(iii) and the just established Lemma 2.3(i), from which we also deduce that for all .
Recalling Lemma 2.1(iv), the convergence in (after possibly extracting a further subsequence) follows from Lemma 2.3(i) and the reflexivity of .
With respect to (iv), due to Lemma 2.1(ii), we may assume that there is such that
Moreover, the bounds in Lemma 2.1(iii), along with Lemma 2.3(ii), imply that
while Lemma 2.3(i) leads us to
Combining the last two convergences we find
Recalling (2.5), we conclude that and therewith establish (iv). □
Let and f be as found in Lemma 2.3. As a direct consequence of Lemma 2.1(v) and Lemma 2.3(i), which in particular implies that in for almost all , we deduce that for all . Taking also into account that it follows that a.e. in for all . Moreover, in view of Lemma 2.3(i) and (iv), it is straightforward to pass to the limit in (1.8a) with and obtain
for all and all , thereby establishing (1.10).
Finally, choosing with
as test function in (1.10), we find that for all . Therefore for all . □
Estimating the error
In this section we restrict our arguments to the case when the space dimension satisfies . The main goal is to provide an estimate for the error with , cf. Theorem 1.3. In particular, we also prove that the porous medium equation (1.2) with initial data has a unique solution as defined in Theorem 1.2. Hence, this improves Theorem 1.2 in the sense that now the whole family converges for towards the corresponding solution to the porous medium equation. In order to prepare the proof of Theorem 1.3, which we postpone to the end of the section, we first introduce some notation. We recall that is an isomorphism for all and
Theorem 1.3 then amounts to estimate the norm , where
Testing the equations (1.8a) and (1.10) by , with and using the self-adjointness of the operator , we arrive at
where . Hence, letting
we have and, subtracting the above identities, we deduce that
As a consequence of (3.1), Theorem 1.1, and Theorem 1.2, we obtain the following result.
Letand. Thenandfor all.
The proof relies on the classical result which allows one to approximate a continuous time-dependent function by a sequence of piecewise constant functions with respect to time. We thus omit it here. □
The next lemma provides an integral identity, cf. (3.4), which is obtained when formally testing with in (3.3). This identity is the starting point in the proof of Theorem 1.3.
For alland,
Since with , we have . Let denote the even reflection of with respect to the boundary of and choose . We then define as the convolution where is a standard mollifier on . We first note that there exists a positive integer with the property that for all and . Using as a test function in (3.3), we get
To pass to the limit in the term on the right-hand side of (3.5) we recall that
by Lemma 2.1(i)–(ii), Theorem 1.3, and Hölder’s inequality. Moreover, the regularity of , the restriction to space dimension , and Sobolev’s embedding ensure that , from which we deduce that in for all when letting . We therewith get
To deal with the first term on the left-hand side of the equality (3.5), we note that in for and all , and therefore we may assume that
To pass to the limit in the second term on the left-hand side of (3.5), we note that Lemma 2.3(iii) guarantees that . Since , we have and this implies that lies in . It follows that in and therefore in as . Taking also into account that , due to Lemma 2.3(i)–(ii) and the continuous embedding of in , we may now pass to the limit in (3.5) to conclude that the identity
is satisfied for almost all . Now, owing to (3.2),
in . Combining the above two identities, we end up with
for almost every . Choosing a suitable approximating sequence for the constant function 1, we infer from the above identity, after passing to the limit and using the relation , that (3.4) holds true (for all due to the fact that ). □
We are now in a position to establish our second main result, see Theorem 1.3.
Given , it follows from (3.4) that
where
Below we estimate the terms and separately in order to obtain an integral inequality to which we may apply Gronwall’s inequality and conclude in this way our claim (1.11).
The term. Using Hölder’s and Young’s inequalities, we find
The first term on the right-hand of (3.7) is clearly controlled by the left-hand side of (3.6) and we are thus left with estimating the second term. In view of the continuous embedding (recall that ), we infer from Hölder’s inequality that
Hence, in view of Theorem 1.2 and Lemma 2.1(i), we have
The term. In order to estimate , we first observe that embeds continuously in due to . We then infer from Gagliardo–Nirenberg’s inequality [18] that
where
Hölder’s inequality and (3.9) now imply that
Taking advantage of Young’s inequality, we then get
Consequently, since ,
Using Hölder’s inequality and (2.2), we further have
Furthermore, by Gagliardo–Nirenberg’s inequality and Lemma 2.1(i),
which implies, together with (2.2) and the property , that
Recalling the definition of a, we conclude that
for all .
Applying Gronwall’s lemma. Gathering (3.6), (3.7), (3.8), and (3.10), we arrive at
Recalling (2.2), a direct application of Gronwall’s inequality now leads us to the desired estimate (1.11).
Uniqueness of the solution to (
1.2
). If and are two solutions to (1.2) corresponding to the same initial data , then we can perform similar computations as those leading to (3.11) to obtain that
and Gronwall’s lemma then implies . □
We complete this section with the proof of Corollary 1.4.
Keeping the notation introduced in the proof of Theorem 1.3, it readily follows from (1.12) and (3.7) that
Using again (1.12) along with (2.2) and Hölder’s and Young’s inequality, we find
Combining (3.6), (3.12), and (3.13) gives
and applying Gronwall’s lemma completes the proof. □
The limiting behavior of
In this section we establish our last main result stated in Theorem 1.5. Before going on, we point out that all the estimates for the family provided by Theorem 1.1 involve the function multiplied by a positive power of ε when , see Lemma 2.1, except the conservation of mass , which stems from , . Nevertheless, exploiting this property, we establish below the convergence of towards the initial condition for , without any restriction on the space dimension .
To start, we use (1.8b) and the continuous embedding to deduce that
for all and , where we recall that . Consequently we have
and it remains to estimate the norm .
Recalling that , , Gagliardo–Nirenberg’s inequality yields
Taking now advantage of (2.2), we get
and Hölder’s inequality leads us to
Recalling from (2.2) that
we obtain, by using once more Hölder’s inequality and the definition of , that
which proves the claim. □
Footnotes
Acknowledgements
Part of this work was carried out while PhL enjoyed the hospitality and support of DFG Research Training Group 2339 “Interfaces, Complex Structures, and Singular Limits in Continuum Mechanics – Analysis and Numerics” at Fakultät für Mathematik, Universität Regensburg.
References
1.
A.Ait Hammou Oulhaj, A finite volume scheme for a seawater intrusion model with cross-diffusion, in: Finite Volumes for Complex Applications VIII – Methods and Theoretical Aspects, Springer Proc. Math. Stat., Vol. 199, Springer, Cham, 2017, pp. 421–429.
2.
A.Ait Hammou Oulhaj, C.Cancès, C.Chainais-Hillairet and Ph.Laurençot, Large time behavior of a two phase extension of the porous medium equation, Interfaces Free Bound.21 (2019), 199–229. doi:10.4171/IFB/421.
3.
J.Alkhayal, M.Jazar and R.Monneau, Global weak solutions for a degenerate parabolic system modelling seawater intrusion in confined aquifers, Appl. Anal.99 (2020), 1749–1764. doi:10.1080/00036811.2018.1544622.
Ph.Bénilan, M.G.Crandall and M.Pierre, Solutions of the porous medium equation in under optimal conditions on initial values, Indiana Univ. Math. J.33 (1984), 51–87. doi:10.1512/iumj.1984.33.33003.
6.
J.Boussinesq, Recherches théoriques sur l’écoulement des nappes d’eau infiltrées dans le sol et sur le débit de sources, J. Math. Pures Appl.10 (1904), 5–78.
7.
H.Brézis, Monotonicity methods in Hilbert spaces and some applications to nonlinear partial differential equations, in: Contributions to Nonlinear Functional Analysis, Proc. Sympos., Math. Res. Center, Univ. Wisconsin, Madison, Wis., 1971, pp. 101–156. doi:10.1016/B978-0-12-775850-3.50009-1.
8.
H.Brézis and M.G.Crandall, Uniqueness of solutions of the initial-value problem for , J. Math. Pures Appl.58 (1979), 153–163.
9.
G.Brüll and R.Granero-Belinchón, On the thin film Muskat and the thin film Stokes equations, J. Math. Fluid Mech.21 (2019), Paper No. 31, 31 pp. doi:10.1007/s00021-019-0431-8.
10.
J.Escher, Ph.Laurençot and B.-V.Matioc, Existence and stability of weak solutions for a degenerate parabolic system modelling two-phase flows in porous media, Ann. Inst. H. Poincaré Anal. Non Linéaire28 (2011), 583–598. doi:10.1016/j.anihpc.2011.04.001.
11.
J.Escher, A.-V.Matioc and B.-V.Matioc, Modelling and analysis of the Muskat problem for thin fluid layers, J. Math. Fluid Mech.14 (2012), 267–277. doi:10.1007/s00021-011-0053-2.
12.
M.Jazar and R.Monneau, Derivation of seawater intrusion models by formal asymptotics, SIAM J. Appl. Math.74 (2014), 1152–1173. doi:10.1137/120867561.
13.
Ph.Laurençot and B.-V.Matioc, A gradient flow approach to a thin film approximation of the Muskat problem, Calc. Var. Partial Differential Equations47 (2013), 319–341. doi:10.1007/s00526-012-0520-5.
14.
Ph.Laurençot and B.-V.Matioc, Finite speed of propagation and waiting time for a thin film Muskat problem, Proc. Roy. Soc. Edinburgh Sect. A147 (2017), 813–830. doi:10.1017/S030821051600038X.
15.
Ph.Laurençot and B.-V.Matioc, Self-similarity in a thin film Muskat problem, SIAM J. Math. Anal.49 (2017), 790–842.
16.
Ph.Laurençot and B.-V.Matioc, Bounded weak solutions to a class of degenerate cross-diffusion systems, arXiv:2201.06479.
17.
Ph.Laurençot and B.-V.Matioc, Bounded weak solutions to the thin film Muskat problem via an infinite family of Liapunov functionals, to appear in Trans. Amer. Math. Soc., arXiv:2110.01234.
18.
L.Nirenberg, On elliptic partial differential equations, Ann. Scuola Norm. Sup. Pisa Cl. Sci. (3)13 (1959), 115–162.
19.
F.Otto, -contraction and uniqueness for quasilinear elliptic-parabolic equations, J. Differ. Equations131 (1996), 20–38. doi:10.1006/jdeq.1996.0155.
20.
F.Otto, Dynamics of labyrinthine pattern formation in magnetic fluids: A mean-field theory, Arch. Rational Mech. Anal.141 (1998), 63–103. doi:10.1007/s002050050073.
21.
F.Otto, The geometry of dissipative evolution equations: The porous medium equation, Comm. Partial Differential Equations26 (2001), 101–174. doi:10.1081/PDE-100002243.
22.
M.Pierre, Uniqueness of the solutions of with initial datum a measure, Nonlinear Anal., Theory Methods Appl.6 (1982), 175–187. doi:10.1016/0362-546X(82)90086-4.
23.
J.Simon, Compact sets in the space , Ann. Mat. Pura Appl. (4)146 (1987), 65–96. doi:10.1007/BF01762360.
24.
J.L.Vázquez, The Porous Medium Equation, Clarendon Press, Oxford, 2007.
25.
A.W.Woods and R.Mason, The dynamics of two-layer gravity-driven flows in permeable rock, J. Fluid Mech.421 (2000), 83–114. doi:10.1017/S0022112000001567.