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Homogenization of Smoluchowski Equations in Thin Heterogeneous Porous Domains

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01 September 2023

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06 September 2023

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Abstract
We carry out in a thin heterogeneous porous layer, the multiscale analysis of Smoluchowski's discrete diffusion-coagulation equations describing the evolution density of diffusing particles that are subject to coagulate in pairs. Assuming that the thin heterogeneous layer is made of microstructures that are uniformly distributed inside, we obtain in the limit an upscaled model in lower space dimension. We also prove a corrector-type result very useful in numerical computations. In view of the thin structure of the domain, we appeal to a concept of two-scale convergence adapted to thin heterogeneous media to achieve our goal.
Keywords: 
Subject: Computer Science and Mathematics  -   Applied Mathematics

1. Introduction and the main results

The use of Smoluchowski equation has proved very efficient in modelling several natural and physical phenomena in Chemistry, in Astrophysics, in Aerosol science, in Physics, in Engineering and in Biological sciences, just to cite a few. Some applications arise in the modeling of the polymerization in Chemistry, the motion of a system of particles that are suspended in a gas, the behavior of fuel mixtures in engines (in Engineering science), the formation of stars and planets (in Physics) and in the modeling of red blood cell aggregation. In this work, we are particularly interested in its application to aggregation and diffusion of particles.
More precisely, we are concerned with Smoluchowski equation modelling Alzheimzer’s disease (AD) which is a system of partial differential equations aiming at describing the evolving densities of diffusing particles subject to coagulate in pairs. Recently, the crucial role of Smoluchowski equations in the multiscale modeling of the evolution of AD at different scales has been considered in [1,2,3,4] where the authors proposed a suitable mathematical model for the aggregation and diffusion of β -amyloid (A β ) in the brain affected by AD at a microscale (that is, at the size of a single neuron) and at primary step of the disease when small amyloid fibrils are free to move and merge. We also refer to [5,6,7,8] for some other works in the same direction. In the model considered in [2], a tiny part of the cerebral tissue is viewed as a bounded domain Ω R 3 which is perforated by removing from it a set of periodically distributed holes of size ε (the neurons). Moreover the production of A β in monomeric form at the level of neuron membranes is modeled by a non homogeneous Neumann condition on the boundary of the porosities.
In the current work, we consider the model stated in [2], but this time in a thin porous layer. This is motivated by the fact that Alzheimer’s disease particularly affects the cerebral cortex (responsible for language and information processing) and hippocampus (essential for memory), which represent very thin layers of brain tissue and contain thousands millions of neurons. Here we describe a very small layer of the brain tissue by a highly heterogeneous thin porous layer in which the heterogeneities are due to the number of millions of neurons that the brain tissue can contain. To be more precise, our model problem at the micro level is stated below.
Let Ω be a bounded open Lipschitz connected subset in R 2 . For 0 < ε < 1 be freely fixed, we set
Ω ε = Ω × ( ε , ε ) = ( x ¯ , x 3 ) R 3 : x ¯ Ω and ε < x 3 < ε .
We denote by Z = Y × I the reference layer cell, where Y = ( 0 , 1 ) 2 and I = ( 1 , 1 ) . Let Z f Z be a compact set in Z with smooth boundary, which represents a generic neuron, and let Z s = Z Z f be the supporting cerebral tissue (often call the solid part in the literature of porous media).
Let us set a notation that will be used throughout the work. Let 0 < ε 1 . For any set S R 3 and any k Z 3 ( Z denoting the integers), we set
S ε , k = x R 3 : x = ε ( k + y ) for y S .
With this in mind, let K ε = { k Z 2 × { 0 } : Z ε , k Ω ε } , and set T ε = k K ε Z f ε , k . We define the thin porous layer by
Ω ε = Ω ε T ε ( points in Ω ε lying off T ε ) .
The boundary of Ω ε is divided into two parts: the outer boundary D Ω ε = Ω ε and the inner boundary Γ ε = T ε . We also denote by Γ = Z f , so that Γ ε = k K ε Γ ε , k . Finally we denote by ν the outward unit normal to Γ ε . We assume that Ω ε is connected and that Z s > 0 , where Z s stands for the Lebesgue measure of Z s in R 3 . The ε -model reads as follows: for m = 1 , u 1 ε solves the PDE
u 1 ε t div ( d 1 u 1 ε ) + u 1 ε j = 1 M a 1 , j u j ε = 0 in Q ε = 0 , T × Ω ε u 1 ε ν = 0 on 0 , T × Ω ε u 1 ε ν = ε ψ ε on 0 , T × Γ ε u 1 ε ( 0 , x ) = 0 in Ω ε ;
for 1 < m < M , u m ε solves the PDE
u m ε t div ( d m u m ε ) + u m ε j = 1 M a m , j u j ε = f m ε in Q ε u m ε ν = 0 on 0 , T × Ω ε u m ε ( 0 , x ) = 0 in Ω ε ;
and for m = M , u M ε solves the equation
u M ε t div ( d M u M ε ) = g ε in Q ε u M ε ν = 0 on 0 , T × Ω ε u M ε ( 0 , x ) = 0 in Ω ε ,
where
f m ε = 1 2 j = 1 m 1 a j , m j u j ε u m j ε , g ε = 1 2 j + k M j < M , k < M a j , k u j ε u k ε and ψ ε ( t , x ) = ψ ( t , x ¯ , x ε ) ( ( t , x ) Q ε ) .
We assume that:
(H1)
the coefficients a i , j are positive constants and satisfy a i , j = a j , i ( 1 i , j M ) with a M , M = 0 , and that the diffusion coefficients d i are positive constants that become smaller as j is large;
(H2)
The function ψ ε is defined by ψ ε ( t , x ) = ψ ( t , x ¯ , x ε ) ( ( t , x ) Q ε ), where ψ C 1 ( [ 0 , T ] ; C 1 ( Ω ¯ ; C p e r 1 ( Y ; C 1 ( I ) ) ) ) with 0 ψ 1 and ψ ( 0 , x ¯ , y ) = 0 for ( x ¯ , y ) Ω × Z .
In (H2), C p e r 1 ( Y ; C 1 ( I ) ) denotes the space of functions in C l o c 1 ( R 2 ; C 1 ( I ) ) that are Y-periodic. In (1)-(3), stands for the usual gradient operator while div denotes the divergence operator with respect to the variable x; T is a positive number representing the final time. The unknowns are the vectors value functions u ε : Q ε R M , u ε = ( u 1 ε , . . . , u M ε ) where the coordinate u m ε 0 ( 1 m < M ) stands for the concentration of m-clusters, that is clusters made of m identical elementary particles, while u M ε takes into account aggregation of more than M 1 monomers. It is worth noting that the meaning of u M ε is different from that of u m ε ( m < M ) as it aims at describing the sum of densities of all the large assemblies. It is assumed that the large assemblies exhibit all the same coagulation properties and do not coagulate with each other. We also assume that the only reaction allowing clusters to form large clusters is a binary coagulation mechanism, while the movement of clusters leading to aggregation arises only from a diffusion process described by the constant diffusion coefficient d m ( 1 m M ). The kinetic coefficient a i , j arises from a reaction in which an ( i + j ) -cluster is formed from an i-cluster and a j-cluster. Therefore, they can be interpreted as coagulationrates. Finally, f m ε ( 1 < m < M ) represents the formation of m-clusters by coalescence of smaller clusters and g ε accounts for the formation of a large clusters by coalescence of others large one that have the same coagulation properties.
Our main aim in this work is to investigate the limiting behavior as ε 0 , of the solution u ε to (1)-(3) under the assumptions (H1)-(H2). This falls within the scope of the multiscale analysis through the homogenization theory in thin porous domains.
Most structures in nature exhibit multiscale features both in space and time. In biological sciences, modeling and simulation have proven to be useful and necessary in describing and explaining many biological processes. To meet the challenge of their complexity, and in order to model numerically such features and capture as correct as possible these multiscale phenomena, mathematical modeling and theoretical concepts combined with the development of efficient algorithms and simulation tools must be emphasized and promoted. One such mathematical concept that has seen a tremendous development during the past 50 years is the theory of homogenization. Roughly speaking, homogenization consists in replacing the generally complicated study of heterogeneous and composite phenomena, often modeled by (nonlinear) partial differential equations (PDE) with variable coefficients, by the study of equivalent homogeneous phenomena having the same overall properties, but modeled by PDE with non oscillating coefficients, which is ideal for numerical analysis, interpretation and predictions. Hence the important role of this step. Homogenization offers a rigorous mathematical framework allowing the modeling and analysis of composites in various environments. This is especially the case when the environment is represented by a domain which is the union (or the complement of the union) of subdomains of very small size, say, a domain containing infinite many holes as the one under consideration in this work. That is why the macroscopic model that will be derived in this work is more relevant in practice than the microscopic one.
There is a huge literature on homogenization in fixed or porous media. A few works deal with the homogenization theory in thin heterogeneous domains; see e.g. [9,10,11,12,13,14,15]. As for the homogenization in thin heterogeneous porous media, very few results are known up to now. We may cite [9,10,11,12,14]. Concerning the Smoluchowski equation as stated in this work, to the best of our knowledge, the only work dealing with its homogenization is the paper [2] in which the considered domain is a uniformly perforated one that is not thin. Our contribution in this work is twofold: 1) the domain Ω ε is a thin heterogeneous porous layer. This renders the homogenization procedure not easy to handle. Indeed, to achieve our goal in Theorem 1 below, we make use of the partial mean integral operator M ε (see below for its definition) associated to the extension operator while in [2], even the extension operator is not used; 2) we prove in Theorem 2 a corrector-type result allowing us to approximate each u m ε by a function of the form v m ε ( t , x ) = u m ( t , x ¯ ) + ε u m 1 ( t , x ¯ , x / ε ) where the functions u m and u m 1 do not depend on ε . We summarize our main results below.
Theorem 1.
Assume that(H1)-(H2)hold. For any ε > 0 , let u ε = ( u m ε ) 1 m M be the unique solution of(1)-(3)in the class ( C 1 + α 2 , 2 + α ( Q ε ) ) M , ( α ( 0 , 1 ) ). Let also M ε and E ε denote respectively the partial mean integral operator and the extension operator defined by(37)(see SectionSection 3) and in Lemma1(see SectionSection 2). Then, as ε 0 , one has, for any 1 m M ,
M ε E ε u m ε u m in L 2 ( Q ) - strong ,
M ε E ε u m ε x ¯ u m in L 2 ( Q ) 2 - weak ,
M ε E ε u m ε t u m t in L 2 ( Q ) - weak ,
where u = ( u m ) 1 m M [ L ( Q ) L 2 ( 0 , T ; H 1 ( Ω ) ) H 1 ( 0 , T ; L 2 ( Ω ) ) ] M is the unique solution of the system(8)-(10)below:
θ u 1 t div x ¯ d 1 A x ¯ u 1 + θ u 1 j = 1 M a 1 , j u j = d 1 ψ ˜ in Q = ( 0 , T ) × Ω A x ¯ u 1 · n = 0 on ( 0 , T ) × Ω u 1 ( 0 , x ¯ ) = 0 in Ω ;
If 1 < m < M ,
θ u m t div x ¯ d m A x ¯ u m + θ u m j = 1 M a m , j u j θ 2 j = 1 M a j , m j u j u m j = 0 in Q A x ¯ u m · n = 0 on ( 0 , T ) × Ω u m ( 0 , x ¯ ) = 0 in Ω ;
and
θ u M t div x ¯ d M A x ¯ u m θ 2 j + k M j < M , k < M a j , k u j u k = 0 in Q A x ¯ u M · n = 0 on ( 0 , T ) × Ω u M ( 0 , x ¯ ) = 0 in Ω .
Moreover u ( C 1 + α 2 , 2 + α ( Q ) ) M and is such that
u m > 0 in Q , m = 1 , . . . , M .
In(8)-(10), n is the outward unit normal to Ω and the matrix A = I 2 + y ¯ ω , where I 2 is the 2 × 2 identity matrix and ω = ( ω i ) i = 1 , 2 with ω i being the unique solution (up to addition of a function v i H # 1 ( Y ; H 1 ( I ) ) such that v i = 0 in Z s ) in H # 1 ( Y ; H 1 ( I ) ) = { u H p e r 1 ( Y ; H 1 ( I ) ) : Z s u d y = 0 } of the cell problem
div y ( e i + y ω i ) = 0 in Z s , ( e i + y ω i ) · ν = 0 on Γ , ω i ( . , y 3 ) is Y - periodic ,
where here, ν stands for the outward unit normal to Γ and e i is the ithvector of the canonical basis in R 3 ; the function ψ ˜ and θ are defined respectively by ψ ˜ ( t , x ¯ ) = Γ ψ ( t , x ¯ , y ) d σ ( y ) , ( t , x ¯ ) Q and θ = Z s (the Lebesgue measure of Z s in R 3 .
The partial mean integral M ε considered in Theorem 1 is defined, for a function ϕ by
M ε ϕ ( t , x ¯ ) = 1 2 ε ε ε ϕ ( t , x ¯ , ζ ) d ζ for ( t , x ¯ ) Q .
The system (8)-(10) is the upscaled model arising from the ε -model (1)-(3). It is posed in a 2 dimensions space, leading to an expected dimension reduction problem as it is usually the case for the homogenization theory in thin domains. Moreover the Neumann boundary behavior in (1) plays now the role (in the upscaled model) of the source term in the leading equation in (8), so that, in the case of (1), the limiting equation does not have the same form as the original equation posed in the ε -model. For (9) and (10), apart from the diffusion term, they are similar to the ε -equations in (2) and (3).
Now, let ω i ( i = 1 , 2 ) and u m ( 1 m M ) be as in Theorem 1. We set
u m 1 ( t , x ¯ , y ) = j = 1 2 ω j ( y ) u m x j ( t , x ¯ ) ω ( y ) · x ¯ u 1 ( t , x ¯ ) for ( t , x ¯ , y ) Q × Z ,
where ω = ( ω 1 , ω 2 ) . We have that u m 1 L 2 ( Q ) H # 1 ( Y ; H 1 ( I ) ) , where H # 1 ( Y ; H 1 ( I ) ) stands for the space of functions u in H l o c 1 ( R 2 ; H 1 ( I ) ) that are Y-periodic and satisfy Z s u ( y ) d y = 0 .
With this in mind, the second main result is a corrector-type result and reads as follows.
Theorem 2.
For each 1 m M , assume that u m 1 defined by(13)belongs to L 2 ( 0 , T ; H 1 ( Ω ) ) C # 1 ( Y ; H 1 ( I ) ) where C # 1 ( Y ; H 1 ( I ) ) = { u C l o c 1 ( R 2 ; H 1 ( I ) ) : u is Y-periodic and Z s u d y = 0 } . Then as ε 0 , one has
ε 1 2 u m ε u m ε ( u m 1 ) ε L 2 ( 0 , T ; H 1 ( Ω ε ) ) 0
where ( u m 1 ) ε ( t , x ) = u m 1 ( t , x ¯ , x / ε ) for ( t , x ) Q ε .
The result in Theorem 2 allows us to approximate u m ε in Q ε by a function v m ε of the form v m ε ( t , x ) = u m ( t , x ¯ ) + u m 1 ( t , x ¯ , x / ε ) for ( t , x ) Q ε . Theorem 2 is new in the literature of the homogenization of Smoluchowski equation and is very important as far as the quantitative homogenization theory of such kind of equations is concerned.
The plan of the work is as follows. We investigate in Section 2 the well posedness of (1)-(3) and provide useful uniform estimates. Section 3 deals with the treatment of the concept of two-scale convergence for thin heterogeneous domains. We prove therein some compactness results that will be used in the homogenization process. With the help of the results obtained in Section 3, we pass to the limit in (1)-(3) in Section 4 where we prove the first main result of the work, viz. Theorem 1. We also prove Theorem 2 in the same section, and close the work with a conclusion.

2. Well posedness and uniform estimates

The current section deals with the existence and uniqueness of the solution to (1)-(3), alongside with some useful a priori estimates. We begin with the following theorem.
Theorem 3.
Assume that(H1)-(H2)hold true. For any ε > 0 , the system(1)-(3)possesses a unique weak solution u ε = ( u m ε ) 1 m M ( C 1 + α 2 , 2 + α ( Q ε ) ) M ( α ( 0 , 1 ) be fixed) such that
u m ε ( t , x ) > 0 for ( t , x ) Q ε , m = 1 , . . . , M .
Furthermore there exists ε 0 > 0 such that, for all 1 m M ,
u m ε L ( Q ε ) C ,
u m ε L 2 ( Q ε ) C ε 1 2 ,
u m ε t L 2 ( Q ε ) C ε 1 2 ,
and
ψ ε L 2 ( ( 0 , T ) × Γ ε ) C ψ L 2 ( 0 , T ; C ( Ω ¯ × Γ ) ) ,
for all 0 < ε ε 0 , where C > 0 is independent of m and ε.
Proof. 
The well posedness of (1)-(3) has been addressed in [1,2,4,16]. We are concerned here only with the uniform estimates (15)-(17), the estimate (18) being a classical result arising from the trace result. We just emphasize that since Γ ε = O ( 1 ) ( Γ ε stands for the Lebesgue measure of Γ ε ), no scaling is needed in the left-hand side of (18). Now, as for (15), we follows exactly the same lines of reasoning as in [2] to obtain it. It remains to check (16) and (17). We first consider (16). We distinguish the cases m = 1 and 1 < m M .
We start with m = 1 . Multiplying (1) 1 by u 1 ε and integrating over Ω ε , next using the divergence theorem, we get
1 2 d d t u 1 ε L 2 ( Ω ε ) 2 + d 1 u 1 ε L 2 ( Ω ε ) 2 + Ω ε u 1 ε 2 j = 1 M a 1 , j u j ε d x = ε d 1 Γ ε ψ ( t , x ¯ , x ε ) u 1 ε ( t , x ) d σ ε ( x ) ε d 1 2 ψ ε ( t ) L 2 ( Γ ε ) 2 + ε d 1 2 u 1 ε ( t ) L 2 ( Γ ε ) 2 ,
where the last inequality above stems from Hölder’s and Young’s inequalities. We use a well-known trace inequality to deduce the existence of a positive constant C 1 independent of ε such that
ε u 1 ε ( t ) L 2 ( Γ ε ) 2 C 1 Ω ε u 1 ε ( t ) 2 d x + ε 2 Ω ε u 1 ε ( t ) 2 d x .
Therefore, integrating (19) over ( 0 , t ) ( t ( 0 , T ] ) and taking into account (18) and (20), we are led to
u 1 ε ( t ) L 2 ( Ω ε ) 2 + d 1 ( 2 ε 2 C 1 ) 0 t u 1 ε ( s ) L 2 ( Ω ε ) 2 d s C 1 d 1 0 t u 1 ε ( s ) L 2 ( Ω ε ) 2 d s + ε d 1 C ψ L 2 ( 0 , T ; C ( Ω ¯ × Γ ) ) .
We therefore infer the boundedness of u 1 ε in L ( Q ε ) associated to (21) that there exists ε 0 > 0 such that (16) holds for m = 1 and u 1 ε L ( 0 , T ; L 2 ( Ω ε ) ) 2 C ε 1 2 for all 0 < ε ε 0 , where ε 0 is chosen such that 2 ε 2 C 1 1 , that is, ε 0 C 1 1 2 .
For 1 < m < M , we proceed as for m = 1 and multiply (2) 1 by u m ε and integrate over Ω ε ; then one obtains
1 2 d d t u m ε ( t ) L 2 ( Ω ε ) 2 + d m u m ε L 2 ( Ω ε ) 2 + Ω ε u m ε 2 j = 1 M a m , j u j ε d x = Ω ε f m ε u m ε d x f m ε L 2 ( Ω ε ) u m ε L 2 ( Ω ε ) 2 .
Integrating over ( 0 , t ) for t ( 0 , T ] , we get
u m ε ( t ) L 2 ( Ω ε ) 2 + 2 d m 0 t u m ε ( s ) L 2 ( Ω ε ) 2 d s 2 f m ε L 2 ( Q ε ) u m ε L 2 ( Q ε ) 2 .
Using (15), we get at once
u m ε L ( 0 , T ; L 2 ( Ω ε ) ) 2 + u m ε L 2 ( Q ε ) 2 C ε 1 2 .
Finally, the proof of (16) for m = M is obtained exactly as the one for the case 1 < m < M mutatis mutandis (replace f m ε by g ε ).
Let us now prove (17). We proceed as above by distinguishing three cases.
For m = 1 , we multiply (1) 1 by u 1 ε / t and use (1) 2 -(1) 3 to get
Ω ε u 1 ε t 2 d x + d 1 2 t Ω ε u 1 ε 2 d x = ε d 1 Γ ε ψ ε u 1 ε t d σ ε ( x ) Ω ε u 1 ε u 1 ε t j = 1 M a 1 , j u j ε d x .
But
Ω ε u 1 ε u 1 ε t j = 1 M a 1 , j u j ε d x u 1 ε t L 2 ( Ω ε ) u 1 ε j = 1 M a 1 , j u j ε L 2 ( Ω ε ) 1 2 u 1 ε t L 2 ( Ω ε ) 2 + 1 2 u 1 ε j = 1 M a 1 , j u j ε L 2 ( Ω ε ) 2 .
Thus
u 1 ε t L 2 ( Ω ε ) 2 + d 1 t u 1 ε L 2 ( Ω ε ) 2 2 ε d 1 Γ ε ψ ε u 1 ε t d σ ε ( x ) + u 1 ε j = 1 M a 1 , j u j ε L 2 ( Ω ε ) 2 .
Integrating (22) over ( 0 , t ) and using the boundedness property (15), we obtain after integration by parts,
0 t u 1 ε s ( s ) L 2 ( Ω ε ) 2 d s + d 1 u 1 ε ( t ) L 2 ( Ω ε ) 2 C ε + 2 ε d 1 Γ ε ψ ε u 1 ε d σ ε ( x ) 2 ε d 1 0 t Γ ε ψ ε s ( s ) u 1 ε ( s ) d σ ε ( x ) d s ,
where we have used the fact that ψ ( 0 , x ¯ , y ) = 0 . Now, we use the inequality (20); then (23) becomes
0 t u 1 ε s ( s ) L 2 ( Ω ε ) 2 d s + d 1 u 1 ε ( t ) L 2 ( Ω ε ) 2 C ε + ε d 1 ψ ε L 2 ( Γ ε ) 2 + u 1 ε L 2 ( Γ ε ) 2 + ε d 1 0 t ψ ε s ( s ) L 2 ( Γ ε ) 2 + u 1 ε ( s ) L 2 ( Γ ε ) 2 d s C ε + C ε ψ L ( 0 , T ; C ( Ω ¯ × Γ ) ) 2 + ψ t L 2 ( 0 , T ; C ( Ω ¯ × Γ ) ) 2 + C u 1 ε L 2 ( Ω ε ) 2 + C d 1 ε 2 u 1 ε ( t ) L 2 ( Ω ε ) 2 + C u 1 ε L 2 ( Ω ε ) 2 + C ε 2 u 1 ε L 2 ( Q ε ) 2 .
It follows that
0 t u 1 ε s ( s ) L 2 ( Ω ε ) 2 d s + d 1 ( 1 C ε 2 ) u 1 ε ( t ) L 2 ( Ω ε ) 2 C ε ,
where in (24), we took advantage of (15) and (16). Hence, choosing ε ε 0 sufficiently small so that 1 C ε 2 0 , we get (17) for m = 1 .
The proof of (17) in the case when 1 < m M follows the same lines of reasoning as above, but is much easier. It is therefore left to the reader. This completes the proof. □
The following result whose proof can be found in [17] will be useful in the sequel.
Lemma 1.
There exists a bounded linear operator E ε : H 1 ( Ω ε ) H 1 ( Ω ε ) such that, for all v H 1 ( Ω ε ) , E ε v = v in Ω ε and
E ε v L 2 ( Ω ε ) C v L 2 ( Ω ε ) + ε v L 2 ( Ω ε ) ,
and
E ε v L 2 ( Ω ε ) C v L 2 ( Ω ε )
for a positive constant independent of both ε and v.
By virtue of Lemma 1, we may define the extension operator from L 2 ( 0 , T ; H 1 ( Ω ε ) ) into L 2 ( 0 , T ; H 1 ( Ω ε ) ) by:For v L 2 ( 0 , T ; H 1 ( Ω ε ) ) we have
( E ε v ) ( t ) = E ε ( v ( t ) ) for a . e . t ( 0 , T ) .
Then accounting of Lemma 1 and Theorem 3, we have
sup 1 m M E ε u m ε L ( Ω ε T ) + E ε u m ε L 2 ( 0 , T ; H 1 ( Ω ε ) ) C ε 1 2 ,
where C > 0 is independent of ε and
Ω ε T = ( 0 , T ) × Ω ε .
We also need an estimate on u m ε / t in L 2 ( Ω ε T ) . To that end, we proceed as in [18] and consider the restriction operator R ε : L 2 ( Ω ε ) L 2 ( Ω ε ) , R ε v = v Ω ε (the restriction of v to Ω ε ). Then it is a fact that R ε is a bounded linear operator as
R ε v L 2 ( Ω ε ) v L 2 ( Ω ε ) v L 2 ( Ω ε ) .
Now, if R * : L 2 ( Ω ε ) L 2 ( Ω ε ) denotes the adjoint operator of R ε , then for v L 2 ( 0 , T ; L 2 ( Ω ε ) ) = L 2 ( Q ε ) , we define R ε * v by:
( R ε * v ) ( t ) = R ε * ( v ( t ) ) for a . e . t ( 0 , T ) .
Then one has
R ε * u , v = 0 T R ε * ( u ( t ) ) , v ( t ) d t = 0 T u ( t ) , R ε ( v ( t ) ) d t
for all u L 2 ( Q ε ) and v L 2 ( Ω ε T ) . It is therefore easy to see that R ε * v = χ Ω ε v for all v L 2 ( Q ε ) , or equivalently
R ε * v = χ Ω ε E ε v for all v L 2 ( Q ε ) ,
where χ Ω ε stands for the characteristic function of Ω ε in Ω ε .
Lemma 2.
Let the assumptions of Theorem3hold. It holds that
χ Ω ε E ε u m ε t L 2 ( Ω ε T ) C ε 1 2 for all 0 < ε ε 0 ,
where C > 0 is independent of ε, and ε 0 is defined in Theorem3.
Proof. 
First, we have R ε * t u m ε = χ Ω ε t E ε u m ε , where t = / t . Thus it is sufficient to show that
R ε * t E ε u m ε L 2 ( Ω ε T ) C ε 1 2 .
So, let φ L 2 ( Ω ε T ) ; then
R ε * t E ε u m ε , φ = t E ε u m ε , R ε φ t E ε u m ε L 2 ( Q ε ) R ε φ L 2 ( Q ε ) t u m ε L 2 ( Q ε ) φ L 2 ( Ω ε T ) C ε 1 2 φ L 2 ( Ω ε T ) .
Whence the result. □

3. Two-scale convergence in thin heterogeneous domains

The two-scale convergence for thin heterogeneous domains has been introduced in [19] and extended to thin porous surfaces in [12,17]. The notations used in this section are the same as in the previous ones. Especially, the domain Ω ε is defined as above, that is, Ω ε = Ω × ( ε , ε ) . When ε 0 , Ω ε shrinks to the "interface" Ω 0 = Ω × { 0 } . We know that Q ε = ( 0 , T ) × Ω ε and Ω ε T = ( 0 , T ) × Ω ε , and we set Q = ( 0 , T ) × Ω 0 , I = ( 1 , 1 ) , Y = ( 0 , 1 ) 2 and finally Z = Y × I . Let 1 p < ; by L p e r p ( Y ; L p ( I ) ) we denote the space of functions in L l o c p ( R 2 ; L p ( I ) ) that are Y-periodic. Accordingly we define W p e r 1 , p ( Y ; W 1 , p ( I ) ) as the subspace of W l o c 1 , p ( Y ; W 1 , p ( I ) ) made of periodic Y-periodic functions, and we set
W # 1 , p ( Y ; W 1 , p ( I ) ) = u W p e r 1 , p ( Y ; W 1 , p ( I ) ) : Z u ( y ¯ , y 3 ) d y = 0 ,
which is a Banach space equipped with the norm
u # = Z u p d y 1 / p , u W # 1 , p ( Y ; W 1 , p ( I ) ) .
Any x in R 3 writes ( x ¯ , x 3 ) or ( x ¯ , ζ ) where x ¯ = ( x 1 , x 2 ) . We identify Ω 0 with Ω so that the generic element in Ω 0 is also denoted by x ¯ instead of ( x ¯ , 0 ) .
We are now able to define the two-scale convergence for thin heterogeneous domains and for thin boundaries.
Definition 1.
(a) A sequence ( u ε ) ε > 0 L p ( Ω ε T ) ( 1 p < ) is
(i) 
weakly two-scale convergent in L p ( Ω ε T ) to u 0 L p ( Q ; L p e r p ( Y ; L p ( I ) ) ) if whenever ε 0 , one has
1 ε Ω ε T u ε ( t , x ) f t , x ¯ , x ε d x d t Q × Z u 0 ( t , x ¯ , y ) f ( t , x ¯ , y ) d y d x ¯ d t
for any f L p ( Q ; C p e r ( Y ; L p ( I ) ) ) ( 1 / p = 1 1 / p ); we denote this by " u ε u 0 in L p ( Ω ε T ) -weak 2 s ";
(ii) 
strongly two-scale convergent in L p ( Ω ε T ) towards u 0 L p ( Q ; L p e r p ( Y ; L p ( I ) ) ) if, as ε 0 , one has u ε u 0 in L p ( Ω ε T ) -weak 2 s and
ε 1 p u ε L p ( Q ε ) u 0 L p ( Q ; L p e r p ( Y ; L p ( I ) ) ) ;
we denote this by " u ε u 0 in L p ( Ω ε T ) -strong 2 s ".
(b) A sequence ( u ε ) ε > 0 in L p ( ( 0 , T ) × Γ ε ) is weakly two-scale convergent in L p ( ( 0 , T ) × Γ ε ) towards u 0 L p ( Q × Γ ) if, whenever ε 0 , one has
( 0 , T ) × Γ ε u ε ( t , x ) f t , x ¯ , x ε d σ ε ( x ) d t Q × Γ u 0 ( t , x ¯ , y ) f ( t , x ¯ , y ) d σ ( y ) d x ¯ d t
for all f L p ( 0 , T ; C ( Ω ¯ × Γ ) ) that is Y-periodic in y ¯ ; we denote this by " u ε u 0 in L p ( ( 0 , T ) × Γ ε ) -weak 2 s ".
Remark 1.
It is easy to see that if u 0 L p ( Q ; C p e r ( Y ; L p ( I ) ) ) then (29) is equivalent to
ε 1 p u ε u 0 ε L p ( Ω ε T ) 0 as ε 0 ,
where u 0 ε ( t , x ) = u 0 ( t , x ¯ , x / ε ) for ( t , x ) Ω ε T .
We start with the following important result that should be used in the sequel; see [20] for the proof.
Lemma 3.
Let ψ L p ( 0 , T ; C ( Ω ¯ × Γ ) ) that is Y-periodic in y ¯ . Then, letting ψ ε ( t , x ) = ψ ( t , x ¯ , x / ε ) for ( t , x ) ( 0 , T ) × Γ ε , we have
(i) 
ψ ε L p ( ( 0 , T ) × Γ ε ) ψ L p ( 0 , T ; C ( Ω ¯ × Γ ) ) ;
(ii) 
0 T Γ ε ψ ( t , x ¯ , x / ε ) d σ ε ( x ) d t Q × Γ ψ ( t , x ¯ , y ) d x ¯ d σ ( y ) d t .
Throughout the work, the letter E will stand for any ordinary sequence ( ε n ) n 1 with 0 < ε n 1 and ε n 0 when n . The generic term of E will be merely denote by ε and ε 0 will mean ε n 0 as n . This being so, we have the following compactness results.
Theorem 4.
(i)Let ( u ε ) ε E be a sequence in L p ( Ω ε T ) ( 1 < p < ) such that
sup ε E ε 1 / p u ε L p ( Ω ε T ) C
where C is a positive constant independent of ε. Then up to a subsequence E of E, the sequence ( u ε ) ε E weakly two-scale converges in L p ( Ω ε T ) to some u 0 L p ( Q ; L p e r p ( Y ; L p ( I ) ) ) .
(ii)Let ( u ε ) ε E be a sequence in L p ( ( 0 , T ) × Γ ε ) such that
u ε L p ( ( 0 , T ) × Γ ε ) C ,
C > 0 being independent of ε. Then we may find a subsequence E of E such that the sequence ( u ε ) ε E weakly two-scale converges in L p ( ( 0 , T ) × Γ ε ) towards some function u 0 L p ( Q × Γ ) .
In Theorem 4 above, the proof of part (i) can be found in [21] while the proof of part (ii) can be found in [20] (see also [12,17]).
Theorem 5.
Let ( u ε ) ε E be a sequence in L p ( 0 , T ; W 1 , p ( Ω ε ) ) ( 1 < p < ) such that
sup ε E ε 1 / p u ε L p ( Ω ε T ) + ε 1 / p u ε L p ( Ω ε T ) C
where C > 0 is independent of ε. Then up to a subsequence E extracted from E, we may find a vector function ( u 0 , u 1 ) with u 0 L p ( 0 , T ; W 1 , p ( Ω ) ) and u 1 L p ( Q ; W # 1 , p ( Y ; W 1 , p ( I ) ) ) such that, when E ε 0 , we have
u ε u 0 in L p ( Ω ε T ) - weak 2 s ,
u ε x i u 0 x i + u 1 y i in L p ( Ω ε T ) - weak 2 s for i = 1 , 2 ,
and
u ε x 3 u 1 y 3 in L p ( Ω ε T ) - weak 2 s .
For the proof of Theorem 5, we refer to [21].
Remark 2.
If we set
x ¯ u 0 = u 0 x 1 , u 0 x 2 , 0 ,
then (31) and (32) are equivalent to
u ε x ¯ u 0 + y u 1 in L p ( Ω ε T ) 3 - weak 2 s .
The following result is sharper than its homologue in Theorem 5.
Theorem 6.
Let ( u ε ) ε E be a sequence in L 2 ( 0 , T ; H 1 ( Ω ε ) ) such that
sup ε E ε 1 2 u ε L 2 ( 0 , T ; H 1 ( Ω ε ) ) + u ε H 1 ( 0 , T ; L 2 ( Ω ε ) ) C ,
where C is a positive constant independent of ε. Finally, suppose that the embedding H 1 ( Ω ) L 2 ( Ω ) is compact. Then up to a subsequence E of E, there is a vector function ( u , u 1 ) ( L 2 ( 0 , T ; H 1 ( Ω ) ) H 1 ( 0 , T ; L 2 ( Ω ) ) ) × L 2 ( Q ; H # 1 ( Y ; H 1 ( I ) ) ) such that, as E ε 0 ,
u ε u in L 2 ( Ω ε T ) - strong 2 s ,
u ε x ¯ u + y u 1 in L 2 ( Ω ε T ) 3 - weak 2 s ,
and
t u ε t u in L 2 ( Ω ε T ) - weak 2 s .
Proof. 
First, owing to Theorem 5, we derive the existence of a subsequence E of E and of a vector function ( u , u 1 ) L 2 ( 0 , T ; H 1 ( Ω ) ) ) × L 2 ( Q ; H # 1 ( Y ; H 1 ( I ) ) ) such that, as E ε 0 ,
u ε u in L 2 ( Ω ε T ) - weak 2 s ,
u ε x ¯ u + y u 1 in L 2 ( Ω ε T ) 3 - weak 2 s ,
and
t u ε t u in L 2 ( Ω ε T ) - weak 2 s .
It remains to prove (34). To that end, we set
M ε u ε ( t , x ¯ ) = 1 2 ε ε ε u ε ( t , x ¯ , x 3 ) d x 3 for ( t , x ¯ ) Q .
Then we easily see that M ε u ε L 2 ( 0 , T ; H 1 ( Ω ) ) H 1 ( 0 , T ; L 2 ( Ω ) ) with
sup ε E M ε u ε L 2 ( 0 , T ; H 1 ( Ω ) ) + M ε u ε H 1 ( 0 , T ; L 2 ( Ω ) ) C .
Then from (38), we derive the existence of a subsequence of E still denoted by E and of a function u 0 L 2 ( 0 , T ; H 1 ( Ω ) ) H 1 ( 0 , T ; L 2 ( Ω ) ) such that, as E ε 0 ,
M ε u ε u 0 in L 2 ( 0 , T ; L 2 ( Ω ) ) - strong .
We recall that (39) stems from the compactness of the continuous embedding L 2 ( 0 , T ; H 1 ( Ω ) ) H 1 ( 0 , T ; L 2 ( Ω ) ) L 2 ( 0 , T ; L 2 ( Ω ) ) .
Now, from the Poincaré-Wirtinger inequality, it holds that
ε 1 2 u ε M ε u ε L 2 ( 0 , T ; L 2 ( Ω ε ) ) C ε u ε L 2 ( 0 , T ; L 2 ( Ω ε ) ) ,
so that
ε 1 2 u ε M ε u ε L 2 ( 0 , T ; L 2 ( Ω ε ) ) 0 as E ε 0 .
Thus the inequality
ε 1 2 u ε u 0 L 2 ( Ω ε T ) ε 1 2 u ε M ε u ε L 2 ( Ω ε T ) + ε 1 2 M ε u ε u 0 L 2 ( Ω ε T )
associated to the equality
ε 1 2 M ε u ε u 0 L 2 ( Ω ε T ) = 2 M ε u ε u 0 L 2 ( Q )
yield (with the help of (39) and (40))
ε 1 2 u ε u 0 L 2 ( Ω ε T ) 0 as E ε 0 .
This shows that u ε u 0 in L 2 ( Ω ε T ) -strong 2 s , and so u 0 = u . The proof is complete. □
The next result and its corollary are proved exactly as their homologues in [22] (see also [23]).
Theorem 7.
Let 1 < p , q < and r 1 be such that 1 / r = 1 / p + 1 / q 1 . Suppose that ( u ε ) ε E L q ( Ω ε T ) weakly two-scale converges in L q ( Ω ε T ) towards u 0 L q ( Q ; L p e r q ( Y ; L q ( I ) ) ) and ( v ε ) ε E L p ( Ω ε T ) strongly two-scale converges in L p ( Ω ε T ) towards v 0 L p ( Q ; L p e r p ( Y ; L p ( I ) ) ) . Then ( u ε v ε ) ε E is weakly two-scale convergent in L r ( Ω ε T ) to u 0 v 0 .
Corollary 1.
Assume the sequences ( u ε ) ε E in L p ( Ω ε T ) and ( v ε ) ε E in L p ( Ω ε T ) L ( Ω ε T ) (with 1 < p < , p = p / ( p 1 ) ) satisfy:
(i) 
u ε u 0 in L p ( Q ε ) -weak 2 s ;
(ii) 
v ε v 0 in L p ( Q ε ) -strong 2 s ;
(iii) 
( v ε ) ε E is bounded in L ( Q ε ) .
Then u ε v ε u 0 v 0 in L p ( Q ε ) -weak 2 s .

4. Derivation of the homogenized problem: Proofs of the main results

4.1. Preliminary results

In this subsection, we aim at providing further important convergence results that will be very useful in the sequel. In that order, it is to be noted that Ω ε can alternatively be defined as follows: Ω ε = k K ε Z s ε , k , where K ε = { k Z 2 × { 0 } : Z ε , k Ω ε } with Ω ε = Ω × ( ε , ε ) and Z ε , k = { ε ( k + y ) : y Z } . We set Λ ε = k K ε Z s 1 , k , a periodic repetition of the set Z s . We denote by χ ε the characteristic function function of Λ ε in Ω ε : χ ε χ Λ ε . Then it holds that
Ω ε = { x Ω ε : χ ε ( x ε ) = 1 } ,
so that χ Ω ε ( x ) = χ ε ( x ε ) for x Ω ε .
Lemma 4.
Let ( u ε ) ε > 0 be a sequence in L p ( Ω ε T ) ( p > 1 a real number) which is weakly two-scale convergent in L p ( Ω ε T ) to u 0 L p ( Q ; L p e r p ( Y ; L p ( I ) ) ) . Then, as ε 0 ,
u ε χ ε u 0 χ Z s in L p ( Ω ε T ) - weak 2 s .
If further the two-scale convergence is strong, then(41)holds in the strong two-scale sense.
Proof. 
Set v ε ( t , x ¯ , ζ ) = u ε ( t , x ¯ , ε ζ ) for ( t , x ¯ , ζ ) Ω 1 T . Then since u ε u 0 in L p ( Ω ε T ) -weak 2 s , it holds that u ε L p ( Ω ε T ) C ε 1 / 2 ( C > 0 being independent of ε ), so that v ε L p ( Ω 1 T ) C . Hence, up to a subsequence, v ε v 0 in L p ( Ω 1 T ) in the usual classical two-scale weak sense, where v 0 L p ( Q × I ; L p e r p ( Y ) ) . Next, let f C ( Q ¯ ; C p e r ( Y ; C ( I ¯ ) ) ) . Passing to the limit (in the subsequence determined above) in the obvious equality
1 ε Ω ε T u ε ( t , x ) f t , x ¯ , x ε d x d t = Ω 1 T v ε ( t , x ¯ , ζ ) f t , x ¯ , x ¯ ε , ζ d x ¯ d ζ d t ,
we get at once u 0 = v 0 .
This being so, choosing f as above, one has
1 ε Ω ε T u ε ( t , x ) χ ε x ε f t , x ¯ , x ε d x d t = Ω 1 T v ε ( t , x ¯ , ζ ) χ Λ 1 x ¯ ε , ζ f t , x ¯ , x ¯ ε , ζ d x ¯ d ζ d t J ε .
Owing to the usual two-scale concept, we obtain, as ε 0 ,
J ε Ω 1 T × Y u 0 ( t , x ¯ , y ¯ , ζ ) χ Z s ( y ¯ , ζ ) f ( t , x ¯ , y ¯ , ζ ) d x ¯ d y ¯ d ζ d t ,
where in (42) we have used the fact that u 0 = v 0 proved above. This concludes the proof. □
The following result will be crucial in the homogenization process. From now on, we set χ s = χ Z s , the characteristic function of Z s in Z.
Proposition 1.
Let ( u m ε ) 1 m M be the solution of(1)-(3). Given any ordinary sequence E, there exist a subsequence E of E and functions ( u m , u m 1 ) 1 m M with u m L 2 ( 0 , T ; H 1 ( Ω ) ) H 1 ( 0 , T ; L 2 ( Ω ) ) and u m 1 L 2 ( Q ; H # 1 ( Y ; H 1 ( I ) ) ) , such that, as E ε 0 ,
χ ε u m ε χ s u m in L 2 ( Ω ε T ) - strong 2 s ,
χ ε u m ε χ s ( x ¯ u m + y u m 1 ) in L 2 ( Ω ε T ) 3 - weak 2 s ,
and
χ ε t u m ε χ s t u m in L 2 ( Ω ε T ) - weak 2 s .
Proof. 
Since E ε u m ε = u m ε in Q ε , we have
χ ε u m ε = χ ε E ε u m ε .
Next, appealing to (25) and (28), we are in a condition to apply Theorem 6: Given a sequence E, we may find a subsequence E of E together with a vector function ( u m , u m 1 ) ( L 2 ( 0 , T ; H 1 ( Ω ) ) H 1 ( 0 , T ; L 2 ( Ω ) ) ) × L 2 ( Q ; H # 1 ( Y ; H 1 ( I ) ) ) such that, as E ε 0 ,
E ε u m ε u m in L 2 ( Ω ε T ) - strong 2 s ,
E ε u m ε x ¯ u m + y u m 1 in L 2 ( Ω ε T ) 3 - weak 2 s ,
and
E ε t u m ε t u m in L 2 ( Ω ε T ) - weak 2 s .
Applying Lemma 4 and accounting of (46), we are done. □

4.2. Passage to the limit

Assume that the functions u m and u m 1 are as in Proposition 1. Let φ C 1 ( Q ¯ ) and φ 1 C 1 ( Q ¯ × I ¯ ; C p e r 1 ( Y ) ) , and define
Φ ε ( t , x ) = φ ( t , x ¯ ) + ε φ 1 ( t , x ¯ , x ε ) for ( t , x ) Ω ε T .
We Φ ε as test function in the variational form of (1)-(3):
1 ε Q ε u 1 ε t Φ ε d x d t + d 1 ε Q ε u 1 ε · Φ ε d x d t + 1 ε Q ε u 1 ε j = 1 M a 1 , j u j ε Φ ε d x d t = 0 T Γ ε ψ ( t , x ¯ , x ε ) Φ ε ( t , x ) d t d σ ε ( x ) ;
For 1 < m < M ,
1 ε Q ε u m ε t Φ ε d x d t + d m ε Q ε u m ε · Φ ε d x d t + 1 ε Q ε u m ε j = 1 M a m , j u j ε Φ ε d x d t = 1 2 ε Q ε j = 1 m 1 a j , m j u j ε u m j ε Φ ε d t d x ;
and
1 ε Q ε u M ε t Φ ε d x d t + d M ε Q ε u M ε · Φ ε d x d t = 1 2 j + k M , j < M , k < M 1 ε Q ε a j , k u j ε u k ε Φ ε d x d t .
Let us first deal with (50). We note that it is equivalent to
1 ε Ω ε T χ ε u 1 ε t Φ ε d x d t + d 1 ε Ω ε T χ ε u 1 ε · Φ ε d x d t + 1 ε Ω ε T χ ε u 1 ε j = 1 M a 1 , j u j ε Φ ε d x d t = 0 T Γ ε ψ ( t , x ¯ , x ε ) Φ ε ( t , x ) d t d σ ε ( x ) .
We have that
Φ ε ( t , x ) = x ¯ φ ( t , x ¯ ) + y φ 1 ( ( t , x ¯ , x ε ) + ε x ¯ φ 1 ( ( t , x ¯ , x ε ) .
Thus we may apply Proposition 1 to proceed to the passage to the limit in the first two terms of the left-hand side of (53), using Φ ε as test function in the two-scale concept. Concerning the right-hand side of (53), we use Lemma 3 to pass to the limit therein. We end up with the last term on the left-hand side where the limit passage therein is more involved. Indeed, we use there the strong two-scale convergence of χ ε u 1 ε towards χ s u 1 associated to the weak two-scale convergence of χ ε u j ε ( 1 j M ) towards χ s u j to get from Corollary 1 that, for 1 j M , we have, as E ε 0 ,
χ ε u 1 ε u j ε = ( χ ε u 1 ε ) ( χ ε u j ε ) χ s u 1 u j in L 2 ( Ω ε T ) - weak 2 s .
Therefore, using in that term the test function Φ ε and taking into account all the process described above after (53), we are led, as E ε 0 in (53), to
Q × Z χ s u 1 t φ d x ¯ d y d t + d 1 Q × Z χ s ( x ¯ u 1 + y u 1 1 ) · ( x ¯ φ + y φ 1 ) d x ¯ d y d t + Q × Z χ s u 1 j = 1 M a 1 , j u j φ d x ¯ d y d t = Q × Γ ψ φ d x ¯ d σ ( y ) d t ( φ , φ 1 ) C 1 ( Q ¯ ) × C 1 ( Q ¯ × I ¯ ; C p e r 1 ( Y ) ) .
We use the same process as for (53) to pass to the limit in (51) and in (52), and we obtain:
For 1 < m < M ,
Q × Z χ s u m t φ d x ¯ d y d t + d m Q × Z χ s ( x ¯ u m + y u m 1 ) · ( x ¯ φ + y φ 1 ) d x ¯ d y d t + Q × Z χ s u m j = 1 M a m , j u j φ d x ¯ d y d t = 1 2 Q × Z χ s j = 1 m 1 a j , m j u j u m j φ d x ¯ d y d t for all ( φ , φ 1 ) C 1 ( Q ¯ ) × C 1 ( Q ¯ × I ¯ ; C p e r 1 ( Y ) ) ;
and
Q × Z χ s u M t φ d x ¯ d y d t + d M Q × Z χ s ( x ¯ u M + y u M 1 ) · ( x ¯ φ + y φ 1 ) d x ¯ d y d t = 1 2 j + k M , j < M , k < M Q × Z χ s a j , k u j u k φ d x ¯ d y d t for all ( φ , φ 1 ) C 1 ( Q ¯ ) × C 1 ( Q ¯ × I ¯ ; C p e r 1 ( Y ) ) .
We have proved the following result.
Theorem 8.
The functions ( u m , u m 1 ) 1 m M determined by Proposition1solve the variational problems(55),(56)and(57).
Our next goal is to derive the system whose ( u m ) 1 m M is solution to. To that end, we start by uncoupling each of the equations (55)-(57). We first consider (55) and we see that it is equivalent to the following system consisting of (58) and (59) below:
Q × Z χ s ( x ¯ u 1 + y u 1 1 ) · y φ 1 d x ¯ d y d t = 0 φ 1 C 1 ( Q ¯ × I ¯ ; C p e r 1 ( Y ) ) ,
Q × Z χ s u 1 t φ d x ¯ d y d t + d 1 Q × Z χ s ( x ¯ u 1 + y u 1 1 ) · x ¯ φ d x ¯ d y d t + Q × Z χ s u 1 j = 1 M a 1 , j u j φ d x ¯ d y d t = Q × Γ ψ φ d x ¯ d σ ( y ) d t φ C 1 ( Q ¯ ) .
Let us first consider Eq. (58) and choose therein φ 1 under the form φ 1 ( t , x ¯ , y ) = ϕ ( t , x ¯ ) η ( y ) with ϕ C 0 ( Q ) and η C p e r ( Y ) C 1 ( I ¯ ) ; then (58) becomes
Z χ s ( x ¯ u 1 + y u 1 1 ) · y η d y = 0 η C p e r ( Y ) C 1 ( I ¯ ) .
To solve (60), we rather consider the variation problem
Z χ s ( e j + y ω j ) · y η d y = 0 η C p e r ( Y ) C 1 ( I ¯ ) ,
where e j ( j = 1 , 2 , 3 ) denotes the jth vector of the canonical basis of R 3 . Then (61) is equivalent to the cell problem
div y ( e j + y ω j ) = 0 in Z s , ( e j + y ω j ) · ν = 0 on Γ ω j ( . , y 3 ) is Y - periodic ,
where ν stands for the outward unit normal to Γ . It is an easy task to see that (62) possesses a solution in the space
H # 1 ( Y ; H 1 ( I ) ) = u H p e r 1 ( Y ; H 1 ( I ) ) : Z s u d y = 0
that is unique up to addition of a function v j such that v j = 0 in Z s . Now, multiplying (61) by u 1 / x j ( j = 1 , 2 ) and summing up the resulting equations, then comparing the latter sum with (60) yields at once
u 1 1 ( t , x ¯ , y ) = j = 1 2 ω j ( y ) u 1 x j ( t , x ¯ ) ω ( y ) · x ¯ u 1 ( t , x ¯ ) ,
where ω = ( ω 1 , ω 2 ) .
Next, going back to (59) and replacing there u 1 1 by the expression obtained in (63), we get
Q Z χ s d y u 1 t φ d x ¯ d t + d 1 Q Z χ s ( I 2 + y ¯ ω ) d y x ¯ u 1 · x ¯ φ d x ¯ d t + Q Z χ s d y u 1 j = 1 M a 1 , j u j φ d x ¯ d t = Q Γ ψ ( . , . , y ) d σ ( y ) φ d x ¯ d t for all φ C 1 ( Q ¯ ) ,
where I 2 is the identity 2 × 2 matrix.
This being so, we set
θ = Z χ s d y = Z s > 0 , A = I 2 + y ¯ ω and ψ ˜ ( t , x ¯ ) = Γ ψ ( ( t , x ¯ , y ) d σ ( y ) .
Then A is a 2 × 2 symmetric positive definite matrix. Indeed it is a fact that the entries of A have the form
A i j = Z s ( e i + y ω i ) · ( e j + y ω j ) d y , 1 i , j 2 ;
this stems from (61) where we show that it is still valid for η H # 1 ( Y ; H 1 ( I ) ) and the choose therein η = ω i . With the above notations in (65), we see that (64) is equivalent to the problem
θ u 1 t div x ¯ ( d 1 A x ¯ u 1 ) + θ u 1 j = 1 M a 1 , j u j = d 1 ψ ˜ in Q A x ¯ u 1 · n = 0 on ( 0 , T ) × Ω u 1 ( 0 , x ¯ ) = 0 in Ω .
Proceeding as we did for (55), we easily show that (56) and (57) are equivalent to the variational formulations of the following PDEs:
For 1 < m < M , (56) is equivalent to
θ u m t div x ¯ ( d m A x ¯ u m ) + θ u m j = 1 M a m , j u j θ 2 j = 1 m 1 a j , m j u j u m j = 0 in Q A x ¯ u m · n = 0 on ( 0 , T ) × Ω u m ( 0 , x ¯ ) = 0 in Ω ;
and for m = M , (57) is equivalent to
θ u M t div x ¯ ( d M A x ¯ u M ) θ 2 j + k M , j < M , k < M a j , k u j u k = 0 in Q A x ¯ u M · n = 0 on ( 0 , T ) × Ω u M ( 0 , x ¯ ) = 0 in Ω .
The system (66)-(68) is the homogenized model arising from the microscale ε -problem (1)-(3). It is posed in a 2 dimensional space, leading to a dimension reduction problem. We see from [2] that (66)-(68) possesses a unique solution. We are now in a position to prove Theorem 1.

4.3. Proof of Theorem 1

The proof of (5)-(7) follows easily from (47)-(49) associated to the properties of the operator M ε . The fact that ( u m ) 1 m M solves (8)-(10) has been shown here above in SubSection 4.2. Now, if we proceed as in [1] (see also [2]), we get the well posedness of (8)-(10) in the space ( C 1 + α 2 , 2 + α ( Q ) ) M , and especially, (11) holds true. Indeed, if we set F = ( F 1 , . . . , F M ) where
F 1 ( t , u ) = d 1 ψ ˜ θ u 1 j = 1 M a 1 , j u j , F m ( t , u ) = θ u m j = 1 M a m , j u j θ 2 j = 1 m 1 a j , m j u j u m j for 1 < m < M , F M ( t , u ) = θ 2 j + k M j < M , k < M a j , k u j u k .
Then F satisfies the assumptions of [1, Appendix]. Hence Theorems 7.1 and 7.2 of [1] readily ensure the existence and uniqueness of the solution of (8)-(10) as claimed above. Finally, the fact that the whole sequence [ ( u m ε ) 1 m M ] ε > 0 converges towards ( u m ) 1 m M follows from the uniqueness of the solution (8)-(10). This concludes the proof.

4.4. Proof of Theorem 2

First of all we recall that ( u m 1 ) ε ( t , x ) = u m 1 ( t , x ¯ , x / ε ) for ( t , x ) Q ε . This being so, for 1 m M be freely fixed, let r m ε = u m ε u m ε ( u m 1 ) ε . Then r m ε = u m ε x ¯ u m ( y u m 1 ) ε ε ( x ¯ u m 1 ) ε . Assuming u m 1 L 2 ( 0 , T ; H 1 ( Ω ) ) C # 1 ( Y ; H 1 ( I ) ) , the functions u m 1 , y u m 1 and x ¯ u m 1 belong to L 2 ( Q ; C p e r ( Y ; L 2 ( I ) ) ) , so that they can be used as test functions in the definition of the two-scale convergence (see Definition 1).
This being so, let us first consider the case m = 1 .
We have
d 1 r ε L 2 ( Q ε ) 2 = d 1 Q ε r ε · r ε d x d t .
Thus taking into account (43) (or (47)), proving Theorem 2 amount in showing that ε 1 r ε L 2 ( Q ε ) 2 0 as ε 0 . So, we have
d 1 ε r ε L 2 ( Q ε ) 2 = d 1 ε Ω ε T χ ε ( u 1 ε x ¯ u 1 ( y u 1 1 ) ε ε ( x ¯ u 1 1 ) ε ) · ( u 1 ε x ¯ u 1 ( y u 1 1 ) ε ε ( x ¯ u 1 1 ) ε ) = d 1 ε Ω ε T χ ε u 1 ε · u 1 ε d 1 ε Ω ε T χ ε u 1 ε · ( x ¯ u 1 + ( y u 1 1 ) ε + ε ( x ¯ u 1 1 ) ε ) d 1 ε Ω ε T χ ε ( x ¯ u 1 + ( y u 1 1 ) ε + ε ( x ¯ u 1 1 ) ε ) · u m ε + d 1 ε Ω ε T χ ε ( x ¯ u 1 + ( y u 1 1 ) ε + ε ( x ¯ u 1 1 ) ε ) · ( x ¯ u 1 + ( y u 1 1 ) ε + ε ( x ¯ u 1 1 ) ε ) = I 1 I 2 I 3 + I 4 ,
where in the series of equalities above, we have omitted d x d t in the integrals just for the simplification of the presentation. We use y u 1 1 and x ¯ u 1 1 as test functions to get at once
I 2 Q × Z χ s ( x ¯ u 1 + y u 1 1 ) · ( x ¯ u 1 + y u 1 1 ) d x ¯ d y d t ,
I 4 Q × Z χ s ( x ¯ u 1 + y u 1 1 ) · ( x ¯ u 1 + y u 1 1 ) d x ¯ d y d t
and
I 3 Q × Z χ s ( x ¯ u 1 + y u 1 1 ) · ( x ¯ u 1 + y u 1 1 ) d x ¯ d y d t .
As regard I 1 , one has
I 1 = 1 ε Ω ε T χ ε u 1 ε t u 1 ε 1 ε Ω ε T χ ε u 1 ε j = 1 M a 1 , j u j ε u 1 ε + 0 T Γ ε ψ ( t , x ¯ , x ε ) u 1 ε .
Appealing to (54) and using once more the strong two-scale convergence of χ ε u 1 ε towards χ s u 1 , we get
χ ε u 1 ε u j ε u 1 ε = ( χ ε u 1 ε ) ( χ ε u j ε u 1 ε ) χ s u 1 u j u 1 in L 2 ( Ω ε T ) weak 2 s .
Also, the strong two-scale convergence of χ ε u 1 ε associated to the weak two-scale convergence of χ ε u 1 ε / t gives, owing to Corollary 1,
χ ε u 1 ε t u 1 ε χ s u 1 t u 1 in L 1 ( Ω ε T ) weak 2 s .
Now, for the last term on the right-hand side of (72), we first notice that from the well-known trace inequality
ε 1 2 u 1 ε ( t , . ) L 2 ( Ω ε ) C u 1 ε ( t , . ) L 2 ( Ω ε ) + ε u 1 ε ( t , . ) L 2 ( Ω ε ) ,
we have from (15)-(16)
u 1 ε L 2 ( ( 0 , T ) × Γ ε ) C ,
where C > 0 is independent of ε . It follows from [part (ii) of] Theorem 4 that (up to a subsequence) the trace of u 1 ε on ( 0 , T ) × Γ ε two-scale converges in L 2 ( ( 0 , T ) × Γ ε ) and its two-scale limit can be easily identified (by integration by parts) with the trace of u 1 on Q × Γ , i.e.,
u 1 ε ( 0 , T ) × Γ ε u 1 Q × Γ in L 2 ( ( 0 , T ) × Γ ε ) - weak 2 s .
Thus, using ψ as test function, we get, up to a subsequence,
0 T Γ ε ψ ( t , x ¯ , x ε ) u 1 ε ( t , x ) d σ ε ( x ) d t Q × Γ ψ u 1 d x ¯ d σ ( y ) d t .
Now, in view of the uniqueness of u 1 , the convergence result in (77) holds with the entire sequence ( u 1 ε ) ε > 0 .
Collecting (73), (74) and (77), we obtain
I 1 Q × Z χ s u 1 t u 1 Q × Z χ s Ω ε T χ s u 1 j = 1 M a 1 , j u j u 1 + Q × Γ ψ u 1 d x ¯ d σ ( y ) d t .
Now, if we take u 1 as a test function in the variational form of (66) and accounting of (78), we see that
I 1 Q × Z χ s ( x ¯ u 1 + y u 1 1 ) · ( x ¯ u 1 + y u 1 1 ) d x ¯ d y d t .
Putting together (69), (70), (71) and (79), we get the result in the case m = 1 .
The proof in the case 1 < m M is more easier and follows the same steps as in the case m = 1 . Theorem 2 is therefore proved.
Conclusion 9.
In this work, we have provided the qualitative multiscale analysis of a micro-model of Smoluchowski equations in thin heterogeneous domains. Starting from a 3 dimensions problem, we have proved that the upscaled equation is posed on a 2 dimensions space, leading to a dimension reduction problem. We have also addressed an approximation issue by proving a corrector-type result, showing that the solution u m ε can be approximated by the function v m ε = u m + ε ( u m 1 ) ε in Q ε where u m and u m 1 solve equations that are independent of ε . This is very useful in the numerical computations and opens the door to the quantitative homogenization of (1) which aims at finding the rate of convergence in the approximation of u m ε by v m ε .

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