Well-posedness and inverse Robin estimate for a multiscale elliptic/parabolic system
Martin Lind, Adrian Muntean, Omar Richardson

TL;DR
This paper proves the well-posedness of a coupled micro-macro parabolic-elliptic system modeling pressures in a porous medium and establishes a local stability estimate for an inverse Robin problem to identify interfacial transfer coefficients.
Contribution
It introduces a rigorous mathematical framework for the well-posedness and inverse stability of a multiscale coupled system in porous media, using advanced energy and regularity techniques.
Findings
Well-posedness of the coupled system established.
Local stability estimate for the inverse Robin problem proved.
Methodology applicable to micro-macro interfacial problems in porous media.
Abstract
We establish the well-posedness of a coupled micro-macro parabolic-elliptic system modeling the interplay between two pressures in a gas-liquid mixture close to equilibrium that is filling a porous media with distributed microstructures. Additionally, we prove a local stability estimate for the inverse micro-macro Robin problem, potentially useful in identifying quantitatively a micro-macro interfacial Robin transfer coefficient given microscopic measurements on accessible fixed interfaces. To tackle the solvability issue we use two-scale energy estimates and two-scale regularity/compactness arguments cast in the Schauder's fixed point theorem. A number of auxiliary problems, regularity, and scaling arguments are used in ensuring the suitable Fr\'echet differentiability of the solution and the structure of the inverse stability estimate.
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Well-posedness and inverse Robin estimate for a multiscale elliptic/parabolic system
Martin Lind
Department of Mathematics and Computer Science
Karlstad University
651 88 Karlstad
Sweden
,
Adrian Muntean
Department of Mathematics and Computer Science
Karlstad University
651 88 Karlstad
Sweden
and
Omar Richardson
Department of Mathematics and Computer Science
Karlstad University
651 88 Karlstad
Sweden
Abstract.
We establish the well-posedness of a coupled micro-macro parabolic-elliptic system modeling the interplay between two pressures in a gas-liquid mixture close to equilibrium that is filling a porous media with distributed microstructures. Additionally, we prove a local stability estimate for the inverse micro-macro Robin problem, potentially useful in identifying quantitatively a micro-macro interfacial Robin transfer coefficient given microscopic measurements on accessible fixed interfaces. To tackle the solvability issue we use two-scale energy estimates and two-scale regularity/compactness arguments cast in the Schauder’s fixed point theorem. A number of auxiliary problems, regularity, and scaling arguments are used in ensuring the suitable Fréchet differentiability of the solution and the structure of the inverse stability estimate.
Key words and phrases:
Upscaled porous media, two-scale PDE, inverse micro-macro Robin problem
2010 Mathematics Subject Classification:
76S05, 35B27, 35R10, 35R30, 86A22
1. Introduction
We are interested in developing evolution equations able to describe multiscale spatial interactions in gas-liquid mixtures, targeting a rigorous mathematical justification of Richards-like equations - upscaled model equations generally chosen in a rather ad hoc manner by the engineering communities to describe the motion of flow in unsaturated porous media. The main issue is that one lacks a rigorous derivation of the Darcy’s law for such flow (see Hornung (2012) (chapter 1) for a derivation via periodic homogenization techniques of the Darcy law for the saturated case).
If air-water interfaces can be assume to be stagnant for a reasonable time span, then averaging techniques for materials with locally periodic microstructures (compare e.g. Chechkin and Piatnitski (1998)) lead in suitable scaling regimes to what we refer here as two-pressure evolution systems. These are normally coupled parabolic-elliptic systems responsible for the joint evolution in time () of a parameter-dependent microscopic pressure evolving with respect to for any given macroscopic spatial position and a macroscopic pressure with for any given . Here denotes the universal constant of gases. The two-scale geometry we have in mind is depicted in Figure 1 below.
To cast the physical problem in mathematical terms as stated in (1), we need a number of dimensional constant parameters ( (gas permeability), (diffusion coefficient for the gaseous species), (atmospheric pressure), (gas density)) and dimensional functions ( (Robin coefficient) and (initial liquid density)). It is worth noting that excepting the Robin coefficient , all the model parameters and functions are either known or can be accessed directly via measurements. Getting grip on a priori values of is more intricate simply because this coefficient is defined on the Robin part of the boundary of , say , where the micro-macro information transfer takes actively place. The Neumann part of the boundary is assumed to be accessible via measurements, while is thought here as unaccessible.
Our aim is twofold:
- (1)
ensure the well-posedness in a suitable sense of our two-pressure system with taken to be known;
- (2)
prove stability estimates with respect to for the inverse micro-macro Robin problem ( is now unknown, but measured values of the microscopic pressure are available on ).
The main results reported here are Theorem 3.1 (the weak solvability of (1)) and Theorem 5.1 (the local stability for the inverse micro-macro Robin problem).
The choice of problem and approach is in line with other investigations running for two-scale systems, or systems with distributed microstructures, like Lind and Muntean (2016); Meier (2008); Peszynska and Showalter (2007). As far as we are aware, this is for the first time that an inverse Robin problem is treated in a two-scale setting. A remotely connected single-scale inverse Robin problem is treated in Nakamura and Wang (2015).
2. Problem formulation
We shall consider the following parabolic-elliptic problem posed on two spatial scales and .
[TABLE]
where the parameters, coefficients and the nonlinear function satisfies the assumptions discussed below (see Section 2.1). The initial condition for follows from the coupling between and .
A prominent role in this paper is played by the micro-macro Robin transfer coefficient , which is selected from the following set
[TABLE]
2.1. Assumptions
- ()
The domains have Lipschitz continuous boundaries. 2. ()
The parameters satisfy . 3. ()
The initial value . 4. ()
where , . 5. ()
There is a structural constant such that
[TABLE]
uniformly in . 6. ()
There is a constant such that
[TABLE] 7. ()
The constant in () satisfies
[TABLE]
where is the Poincaré constant of the domain (see Proposition 2.1 below).
Remark 1*.*
Assumptions ()-() have clear geometrical or physical meanings, while ()-() are technical. The assumption () is only used when deriving uniqueness of the weak solution to (1). Note also that for some special classes of domains, the Poincaré constant can be quantitatively estimated, see e.g. Mikhlin (1981).
2.2. Auxiliary results
In this section, we state some auxiliary results that will be useful in this context.
Proposition 2.1** (Poincaré’s inequality).**
Let be a fixed domain and denote by the smallest constant such that
[TABLE]
hold for all . The constant is called the Poincaré constant of the domain .
Proposition 2.2** (Interpolation-trace inequality).**
Assume that is a Lipschitz domain and . For any we have
[TABLE]
where . In particular,
[TABLE]
The next result provides a useful equivalent norm on .
Proposition 2.3**.**
Let be a domain and where has positive -dimensional surface measure. Then there are constants such that
[TABLE]
We shall also need the following two results, the first a Sobolev-type embedding and the second a simple trace theorem.
Proposition 2.4**.**
Assume that , then and
[TABLE]
Proposition 2.5**.**
Assume that and is Lipschitz continuous. Then
[TABLE]
and
[TABLE]
We have the following existence and regularity results.
Proposition 2.6** (see e.g. Evans (1998)).**
Consider the problem
[TABLE]
If and , then the problem (2) has a unique weak solution .
Proposition 2.7** (see e.g Cazenave (2006)).**
Let be in and consider the problem
[TABLE]
where the nonlinear function satisfies ()-(). Then the problem (3) has a unique weak solution .
Finally, we state the following two classical compactness results, see e.g. Zeidler (1986).
Theorem 2.8** (Aubin-Lions Theorem Aubin (1963)).**
Let . Suppose that is compactly embedded in and that is continuously embedded in . Let
[TABLE]
Then the embedding of into is compact.
Theorem 2.9** (Schauder’s Fixed Point Theorem).**
Let be a nonempty, closed, convex, bounded set and a compact operator. Then there exists at least one such that .
3. Existence and uniquenes of the solution
3.1. Existence of weak solution
The main result of this subsection is the following theorem.
Theorem 3.1**.**
Assume that ()-() hold. Then the problem (1) has at least a weak solution solution .
Proof.
We shall decouple the problem. The first sub-problem is as follows: given and , we let be the weak solution to
[TABLE]
The weak formulation of (5) is: find such that for a.e. and every there holds
[TABLE]
and . Existence and regularity of is provided by Proposition 2.6 (recall that () states that ).
The second sub-problem is: given data , consider the problem
[TABLE]
Let be a free parameter. By the scaling properties of and uniqueness of weak solution, we have that if is the weak solution of (7) with data , then is the weak solution to (7) with data . Hence, if is the weak solution to
[TABLE]
then , again by the scaling properties of . The weak form of (8) is as follows: find such that for a.e. and all , there holds
[TABLE]
Existence and regularity of is guaranteed by Proposition 2.7.
We shall now use a fixed point argument à la Schauder (see Theorem 2.9) to show that there exists a for which the functions of the pair are weak solutions to the sub-problems (5) and (8). Then we recover , a weak solution to (1), by taking and .
Define the operators
[TABLE]
by (the weak solution of (5)) and
[TABLE]
by (the weak solution of (8)). Finally, consider the operator on the space into itself defined by
[TABLE]
To obtain existence of solution, we shall prove that the operator has a fixed point. This will then give . The idea of the proof is to first use the Schauder Fixed Point Theorem (Theorem 2.9 above).
We shall prove that there exist a and a set such that
- (1)
is a compact operator; 2. (2)
is convex, closed, bounded and satisfies .
To obtain compactness of , it is sufficient to demonstrate that is compact and that is continuous. Recall that we have
[TABLE]
However, since we assume that we get that and . Whence,
[TABLE]
where
[TABLE]
By Theorem 2.8,
[TABLE]
Thus, for any bounded set , there holds and since is compactly contained in we have that is precompact in . Hence, is compact.
We continue to prove that is continuous. Assume we have two solutions and . Substituting these both in (3.1) and subtracting, we obtain
[TABLE]
and for , we get
[TABLE]
Using () and (), we obtain that
[TABLE]
By the Poincaré’s inequality, we obtain
[TABLE]
and we conclude the mapping is continuous.
Let be a fixed number that we specify later and let be the collection of functions such that
[TABLE]
For each , the set
[TABLE]
is a convex, closed and bounded. We show that we may select and such that
[TABLE]
Note that is a bounded subset of , with a bound depending only on . In other words,
[TABLE]
Indeed, this follows from the fact that is a compact operator.
We proceed by observing that we may choose such that if is arbitrary and , then
[TABLE]
Let so that . Testing the weak formulation of with and using Cauchy-Schwarz’ inequality and Poincaré’s inequality, we get
[TABLE]
Integrating over and using (11), we obtain after using Poincaré’s inequality
[TABLE]
By taking small enough (depending on ), we obtain (12) whence (10) follows. ∎
Remark 2*.*
Instead of using scaling arguments and Schauder’s fixed point theorem, we could have used alternatively the Schaefer/Leray-Schauder fixed point theorem.
3.2. Uniqueness of weak solutions
We proceed to prove the following uniqueness theorem.
Theorem 3.2**.**
Assume that in addition to the assumptions of Theorem 3.1 the condition () also holds. Then the weak solution to (1) is unique.
Proof.
The weak formulation of the uncoupled problem is: find where and for a.e. the equations
[TABLE]
and
[TABLE]
hold for all and all .
Assume that two pairs of solutions exist: and . Let and . If we substitute the two solutions in (13) and (14) and subtract, we obtain that
[TABLE]
and
[TABLE]
for all and all .
Choosing specific test function , using Young’s inequality with parameter and (), we obtain from (15) the first key estimate
[TABLE]
We focus on (16), which, using test function , yields
[TABLE]
Now, we estimate the right hand side of (18) by using trace inequality and the fact that on . We have
[TABLE]
The second term at the right-hand side of the previous inequality can be estimated by using the trace inequality and Young’s inequality with parameter :
[TABLE]
for some absolute constant . Using the previous estimates and rearranging (18), we obtain
[TABLE]
By Poincare’s inequality, we have
[TABLE]
where is the Poincaré constant of the domain . Using this in (17), we obtain
[TABLE]
By (), we may take small enough such that . Then we obtain
[TABLE]
Whence, it follows from the previous estimate and (19) with that
[TABLE]
By using Grönwall’s inequality and the fact that , it follows that . From (20), we obtain as well. This demonstrates the uniqueness. ∎
4. Energy and stability estimates
We start this section by stating the following energy estimates for our problem.
Proposition 4.1**.**
Assume ()-() and let be a weak solution to
[TABLE]
Then the following energy estimate hold
[TABLE]
The proof of Proposition 4.1 follows by similar arguments as the proof of Theorem 4.2 below, therefore we omit it.
We proceed to study the stability of solutions with respect to some of the parameters involved. Some preliminary remarks:
- •
We do not need to study the stability of the solution with respect to and . Recall that is an universal physical constant, while fix the type of fluid and gas we are considering.
- •
We could investigate the stability of with respect to structural changes into the non-linearity . We omit to do so mainly because our main intent lies in understanding the role of the micro-macro Robin coefficient .
- •
For this stability proof, we decide to use a direct method which relies essentially on energy estimates; see e.g. Muntean (2009).
For , let be two weak solutions corresponding to the sets of data , where denote the initial data, diffusion coefficients and mass-transfer coefficients of the solution . Denote
[TABLE]
Theorem 4.2**.**
Assume that for , belongs to a fixed compact subset of , that and that . Let be weak solutions to (1) corresponding to the choices of data above. Then the estimate
[TABLE]
holds
Proof.
We have for
[TABLE]
and
[TABLE]
for all and .
Subtracting the corresponding equations and then testing with and gives:
[TABLE]
and
[TABLE]
Regarding (24), note that
[TABLE]
Using () and (), we may estimate the right-hand side of (24) and obtain
[TABLE]
Using Poincaré’s inequality, assumptions on and Young’s inequality with parameter , we get
[TABLE]
Choosing , rearranging and using energy estimates for , we obtain
[TABLE]
We proceed to estimate , using (LABEL:eq:beta). Note that
[TABLE]
Hence, it follows that
[TABLE]
We have
[TABLE]
Further,
[TABLE]
Finally,
[TABLE]
We assume that for all , we have
[TABLE]
this can be ensured by taking smooth enough. Hence,
[TABLE]
Taking all the estimates above into consideration, and compensating terms by selecting small , we finally obtain
[TABLE]
Applying Grönwall’s inequality leads to
[TABLE]
and, by integration over ,
[TABLE]
It also follows that
[TABLE]
Further, by (26) and Poincaré’s inequality, we have
[TABLE]
Taking all the above estimates together, we obtain
[TABLE]
which concludes the proof. ∎
5. Local stability for the inverse Robin problem
In this section, we shall study the inverse problem of recovering the micro-macro Robin coefficient from measurement on ; the Neumann part of the boundary. (Usuallly, one thinks of as the inaccessible part of , while is the accessible part.) Our discussion is influenced by the work Jiang and Zou (2016). An alternative way of working could be by following the abstract result in Bourgeois (2013).
Recall that we denote
[TABLE]
the set of admissible Robin coefficients. Denote by the true Robin coefficient of our problem and define the set as
[TABLE]
Below denotes the solution to (1) corresponding to the coefficient . Our main result is the following theorem.
Theorem 5.1**.**
Assume that and on . Then there exists such that
[TABLE]
for every .
Remark 3*.*
The discussion around Theorem 5.1 can be extended to the case of recovering micro-macro Robin coefficient with a genuine two-scale structure, e.g. or . In this case, two-scale measurements are needed. To keep the presentation as simple as possible, we focus our attention on .
In the rest of this section, we prove establish several lemmata. The proof of Theorem 5.1 is given in Section 6.
Lemma 5.2**.**
For any and let be the solution to (1) and the solution to
[TABLE]
where is specified below. Then is continuously Fréchet differentiable and its derivative at is given by .
Proof.
One can observe that the well-posedness of (29) follows by similar arguments as in the previous sections. Take and such that .
Note first that solves
[TABLE]
where . Denote by and
[TABLE]
then solves the problem
[TABLE]
where . Note that the nonlinearities satisfiy the conditions of the energy estimate Proposition 4.1. Thus,
[TABLE]
Whence,
[TABLE]
and it is sufficient to show that the right-hand side above tends to 0 as . Using the interpolation-trace inequality, we obtain
[TABLE]
Furthermore, using Proposition 4.1 and the interpolation-trace inequality again, we obtain
[TABLE]
from which follows that
[TABLE]
The proof of continuity follows by a similar argument, we refer to the discussion in Jiang and Zou (2016). ∎
We proceed now in a similar fashion as in e.g. Choulli (2004); Jiang and Zou (2016).
Let and be the weak solution to the system
[TABLE]
For , define the operator
[TABLE]
by
[TABLE]
Then is a bounded linear operator (boundedness follow from energy estimates).
Lemma 5.3**.**
The operator is bijective and is finite.
Proof.
We prove the surjectivity of . Assume that , we must prove that there exists such that . Using (30), we obtain
[TABLE]
or, equivalently,
[TABLE]
Define
[TABLE]
by
[TABLE]
Then we have
[TABLE]
Note further that , where
[TABLE]
We have seen that is compact and is clearly continuous. Hence, is compact.
We claim now that is not an eigenvalue to . Then, by the Fredholm alternative theorem, is invertible and
[TABLE]
To prove that 1 is not an eigenvalue of , assume that for some . It follows from (31) that , so . Hence, on . Since solves (30) it also solves
[TABLE]
Hence, , but then from the Robin boundary condition of (30), and since , we get . In other words, is not an eigenvalue of . In conclusion, is invertible. Since is bounded, bijective and linear, the open mapping theorem ensures that exists and is bounded. ∎
6. Proof of Theorem 5.1
We are now ready to prove our main result.
Proof of Theorem 5.1.
Let and consider the scaled problem
[TABLE]
Recall that we have . From this it follows that the solution to the above problem satisfies . Note that on . Define the norm on by
[TABLE]
Further, define the mapping
[TABLE]
by . It follows from the fact that is Frechet differentiable with continuous derivative that is a -diffeomorphism. We have
[TABLE]
where is the solution to
[TABLE]
Since , it follows from (30) that and by by (34). It follows that . Since is a -diffeomorphism, there exists a neighbourhood such that for any we have
[TABLE]
(see the discussion in Jiang and Zou (2016)). We have
[TABLE]
Using (33), one obtains the estimate
[TABLE]
By the interpolation-trace inequality, we have
[TABLE]
Further, by the Poincaré inequality,
[TABLE]
Hence, we obtain
[TABLE]
We have
[TABLE]
Since is -dimensional, we have
[TABLE]
by Proposition 2.5 and Proposition 2.4. Further, by Proposition 2.6 and the assumption , we have . Hence,
[TABLE]
By the above estimates, we can rely on
[TABLE]
Using the equivalent norm on given by Proposition 2.3, we obtain
[TABLE]
Set and , then solves
[TABLE]
where .
Using Proposition 4.1 and similar estimates as above, we obtain
[TABLE]
This finally yields the crucial estimate
[TABLE]
Choose such that and use that , then we obtain
[TABLE]
Finally, since , we obtain that
[TABLE]
∎
The reference list from the paper itself. Each links out to its DOI / PubMed record.
- 1Aubin [1963] Jean-Pierre Aubin. Un théoreme de compacité. C R Acad. Sci. Paris , 256(24):5042–5044, 1963.
- 2Bourgeois [2013] L. Bourgeois. A remark on Lipschitz stability for inverse problems. C R Acad Ser Paris , 351:187–190, 2013.
- 3Cazenave [2006] T. Cazenave. An introduction to semilinear elliptic equations . Editora do IM-UFRJ, Rio de Janeiro, 2006.
- 4Chechkin and Piatnitski [1998] G. A. Chechkin and A. L. Piatnitski. Homogenization of boundary-value problem in a locally periodic perforated domain. Applicable Analysis , 71(1-4):215–235, 1998.
- 5Choulli [2004] M. Choulli. An inverse problem in corrosion detection: stability estimates. J. Inverse Ill-posed Probl. , 12(4):349–367, 2004.
- 6Evans [1998] L. C. Evans. Partial Ddifferential Equations . American Mathematical Society, 1998.
- 7Hornung [2012] U. Hornung. Homogenization and Porous Media , volume 6. Springer Science & Business Media, 2012.
- 8Jiang and Zou [2016] D. Jiang and J. Zou. Local Lipschitz stability for inverse Robin problems in elliptic and parabolic systems. Technical Report arxiv:1603.02556 v 1, 2016.
