Journal of Applied Mathematics

Journal of Applied Mathematics / 2014 / Article

Research Article | Open Access

Volume 2014 |Article ID 101685 |

Liselott Flodén, Anders Holmbom, Marianne Olsson Lindberg, Jens Persson, "Homogenization of Parabolic Equations with an Arbitrary Number of Scales in Both Space and Time", Journal of Applied Mathematics, vol. 2014, Article ID 101685, 16 pages, 2014.

Homogenization of Parabolic Equations with an Arbitrary Number of Scales in Both Space and Time

Academic Editor: Carlos Conca
Received05 Sep 2013
Revised18 Dec 2013
Accepted23 Dec 2013
Published24 Feb 2014


The main contribution of this paper is the homogenization of the linear parabolic equation exhibiting an arbitrary finite number of both spatial and temporal scales. We briefly recall some fundamentals of multiscale convergence and provide a characterization of multiscale limits for gradients, in an evolution setting adapted to a quite general class of well-separated scales, which we name by jointly well-separated scales (see appendix for the proof). We proceed with a weaker version of this concept called very weak multiscale convergence. We prove a compactness result with respect to this latter type for jointly well-separated scales. This is a key result for performing the homogenization of parabolic problems combining rapid spatial and temporal oscillations such as the problem above. Applying this compactness result together with a characterization of multiscale limits of sequences of gradients we carry out the homogenization procedure, where we together with the homogenized problem obtain local problems, that is, one for each spatial microscale. To illustrate the use of the obtained result, we apply it to a case with three spatial and three temporal scales with , , and .

1. Introduction

In this paper, we study the homogenization of where and . Here , where is an open bounded subset of with smooth boundary and is periodic with respect to the unit cube in in the first variables and with respect to the unit interval in the remaining variables. The homogenization of (1) consists in studying the asymptotic behavior of the solutions as tends to zero and finding the limit equation which admits the limit of this sequence as its unique solution. The main contribution of this paper is the proof of a homogenization result for (1), that is, for parabolic problems with an arbitrary finite number of scales in both space and time.

Parabolic problems with rapid oscillations in one spatial and one temporal scale were investigated already in [1] using asymptotic expansions. Techniques of two-scale convergence type, see, for example, [24], for this kind of problems were first introduced in [5]. One of the main contributions in [5] is a compactness result for a more restricted class of test functions compared with usual two-scale convergence, which has a key role in the homogenization procedure. In [6], a similar result for an arbitrary number of well-separated spatial scales is proven and the type of convergence in question is formalized under the name of very weak multiscale convergence.

A number of recent papers address various kinds of parabolic homogenization problems applying techniques related to those introduced in [5]. [7] treats a monotone parabolic problem with the same choices of scales as in [5] in the more general setting of -convergence. In [8], the case with two fast temporal scales is treated with one of them identical to a single fast spatial scale. These results with the same choice of scales are extended to a more general class of differential operators in [9] and in [10], the two fast spatial scales are fixed to be , , while only one fast temporal scale appears. Significant progress was made in [11], where the case with an arbitrary number of temporal scales is treated and none of them has to coincide with the single fast spatial scale. A first study of parabolic problems where the number of fast spatial and temporal scales both exceeds one is found in [12], where the fast spatial scales are , and the rapid temporal scales are chosen as , , and . Similar techniques have also been recently applied to hyperbolic problems. In [13] the two fast spatial scales are well separated and the fast temporal scale coincides with the slower of the fast spatial scales and in [14] the set of scales is the same as in [8, 9]. Clearly all of these previous results include strong restrictions on the choices of scales. Our aim here is to provide a unified approach with the choices of scales in the examples above as special cases. The homogenization procedure for (1) covers arbitrary numbers of spatial and temporal scales and any reasonable choice of the exponents and defining the fast spatial and temporal scales, respectively. The key to this is the result on very weak multiscale convergence proved in Theorem 7 which adapts the original concept in [6] to the appropriate evolution setting. Let us note that techniques used for the proof of the special case with , in [10] do not apply to the case with arbitrary numbers of scales studied here.

The present paper is organized as follows. In Section 2 we briefly recall the concepts of multiscale convergence and evolution multiscale convergence and give a characterization of gradients with respect to this latter type of convergence under a certain well-separatedness assumption. In Section 3 we consider very weak multiscale convergence in the evolution setting and give the key compactness result employed in the homogenization of (1), which is carried out in Section 4. In this final section, we also illustrate how this general homogenization result can be used by applying it to the particular case governed by where .

Notation. is the space of all functions in that are -periodic repetitions of some function in . We denote for , , , , for , , , , and . Moreover, we let ,  , and , , be strictly positive functions such that and go to zero when does. More explanations of standard notations for homogenization theory are found in [15].

2. Multiscale Convergence

Our approach for the homogenization procedure in Section 4 is based on the two-scale convergence method, first introduced in [2] and generalized to include several scales in [16]. Following [16], we say that a sequence in ()-scale converges to if for any and we write This type of convergence can be adapted to the evolution setting; see, for example, [12]. We give the following definition of evolution multiscale convergence.

Definition 1. A sequence in is said to ()-scale converge to if for any . We write

Normally, some assumptions are made on the relation between the scales. We say that the scales in a list are separated if for and that the scales are well-separated if there exists a positive integer such that for .

We also need the concept in the following definition.

Definition 2. Let and be lists of well-separated scales. Collect all elements from both lists in one common list. If from possible duplicates, where by duplicates we mean scales which tend to zero equally fast, one member of each such pair is removed and the list in order of magnitude of all the remaining elements is well-separated, the lists and are said to be jointly well-separated.

In the remark below, we give some further comments on the concept introduced in Definition 2.

Remark 3. To include also the temporal scales alongside with the spatial scales allows us to study a much richer class of homogenization problems such as all the cases included in (1). For a more technically formulated definition and some examples, see Section  2.4 in [17]. Note that the lists and of spatial and temporal scales, respectively, in (1) are jointly well-separated for any choice of and .

Below we provide a characterization of evolution multiscale limits for gradients, which will be used in the proof of the homogenization result in Section 4. Here is the space of all functions in such that the time derivative belongs to ; see, for example, Chapter 23 in [18].

Theorem 4. Let be a bounded sequence in and suppose that the lists and are jointly well-separated. Then there exists a subsequence such that where , and for .

Proof. See Theorem 2.74 in [17] and the appendix of this paper.

3. Very Weak Multiscale Convergence

A first compactness result of very weak convergence type was presented in [5] for the purpose of homogenizing linear parabolic equations with fast oscillations in one spatial scale and one temporal scale. A compactness result for the case with oscillations in well-separated spatial scales was proven in [6], where the notion of very weak convergence was introduced. It states that for any bounded sequence in and the scales in the list well-separated it holds up to subsequence that for any and , where is the same as in the right-hand side of the original time independent version of the gradient characterization in Theorem 4, that is found in [16]. In Theorem 7 below we present a generalized result including oscillations in time with a view to homogenizing (1). First we define very weak evolution multiscale convergence.

Definition 5. We say that a sequence in   -scale converges very weakly to if for any ,   and . A unique limit is provided by requiring that We write

The following proposition (see Theorem 3.3 in [16]) is needed for the proof of Theorem 7.

Proposition 6. Let be a function such that and assume that the scales in the list are well-separated. Then is bounded in .

We are now ready to state the following theorem which is essential for the homogenization of (1); see also Theorem 7 in [19] and Theorem 2.78 in [17].

Theorem 7. Let be a bounded sequence in and assume that the lists and are jointly well-separated. Then there exists a subsequence such that where, for , and, for ,   are the same as in Theorem 4.

Proof. We want to prove that for any ,   and , for some suitable subsequence. First we note that any can be expressed as for some (see, e.g., Remark 3.2 in [7]). Furthermore, let and observe that because of the -periodicity of . By (18), the left-hand side of (17) can be expressed as Integrating by parts with respect to , we obtain To begin with, we consider the first term. Passing to the multiscale limit using Theorem 4, we arrive up to subsequence at and due to (20) all but the last term vanish. We have
Moreover, (8) means that the second term of (22) up to a subsequence approaches where the last equality is a result of (20).
It remains to investigate the last term of (22). We write
Clearly, is bounded in for by Proposition 6. Observing that is assumed to be bounded in , this means that, for any integer , there are constants such that Hence, all the terms in the sum (26) vanish as as a result of the separatedness of the scales. Then (24) is all that remains after passing to the limit in (22). Finally, integrating (24) by parts, we obtain which is the right-hand side of (17).

Remark 8. The notion of very weak multiscale convergence is an alternative type of multiscale convergence. It is remarkable in the sense that it enables us to provide a compactness result of multiscale convergence type for sequences that are not bounded in any Lebesgue space. In fact, it deals with the normally forbidden situation of finding a limit for a quotient, where the denominator goes to zero while the numerator does not. The price to pay for this is that we have to use much smaller class of admissible testfunctions. In the set of modes of multiscale convergence usually applied in homogenization that we find in Definition 1 and Theorem 4, very weak multiscale convergence provides us with the missing link. As we will see in the homogenization procedure in the next section Theorems 4 and 7 give us the cornerstones for the homogenization procedure that allows us to tackle all appearing passages to limits in a unified way by means of two distinct theorems and without ad hoc constructions. Moreover, Theorem 7 provides us with appropriate upscaling to detect microoscillations in solutions of typical homogenization problems, which are usually of vanishing amplitude, while the global tendency is filtered away as a result of the choice of test functions. See [12].

4. Homogenization

We are now ready to give the main contribution of this paper, the homogenization of the linear parabolic problem (1). The gradient characterization in Theorem 4 and the very weak compactness result from Theorem 7 are crucial for proving the homogenization result, which is presented in Section 4.1. An illustration of how this result can be used in practice is given in Section 4.2.

4.1. The General Case

We study the homogenization of the problem where ,  , , and where we assume that(A1).(A2) for all , all and some .Under these conditions, (29) allows a unique solution and for some positive constant ,

Given the scale exponents and , we may define some numbers in order to formulate the theorem below in a convenient way. We define (the number of temporal scales faster than the square of the spatial scale in question) and (indicates whether there is nonresonance or resonance), , as follows.(i)If ,then , if for some , then , and if , then .(ii)If for some , that is we have resonance, we let ; otherwise, .Note that from the definition of we have in fact in the definition of that in the case of resonance.

Finally, we recall that the lists and are jointly well-separated.

Theorem 9. Let be a sequence of solutions in to (29). Then it holds that where is the unique solution to with Here and , , are the unique solutions to the system of local problems for , where is independent of .

Remark 10. In the case , we naturally interpret the integration in (34) as if there is no local temporal integration involved and that there is no independence of any local temporal variable.

Remark 11. Note that if,for example, is independent of the function space that belongs to simplifies to and when is also independent of , we have that and so on.

Proof of Theorem 9. Since is bounded in and the lists of scales are jointly well-separated, we can apply Theorem 4 and obtain that, up to a subsequence, where , , and , .
To obtain the homogenized problem, we introduce the weak form of (29) where and , and letting , we get using Theorem 4 We proceed by deriving the system of local problems (34) and the independencies of the local temporal variables. Fix and choose with ,   for ,  ,   and for . Here and will be fixed later. Using this choice of test functions in (36), we have where, for and , the interpretation should be that the partial derivative acts on and , respectively, and where the and terms are defined analogously. We let and using Theorem 4, we obtain
and extracting a factor in the first term, we get Suppose that and (which also guarantees that as required above); then, by Theorems 7 and 4, we have left which is the point of departure for deriving the local problems and the independency.
We distinguish four different cases where is either zero (nonresonance) or one (resonance) and is either zero or positive.
Case  1. Consider and . We choose and . This means that since and . This implies that (42) is valid. We get where we let and obtain by means of Theorems 7 and 4 By the Variational Lemma, we have a.e. in for all and by density for all . This is the weak form of the local problem in this case. In what follows Theorems 7 and 4, the variational lemma and the density argument are used in a corresponding way.
Case  2. Consider and . We again choose and . We then have since and and which implies that we may again use (42). We get and, passing to the limit, By the variational lemma a.e. for all and , which is the weak form of the local problem in this second case.
Case  3. Consider and . Let be fixed and successively be . Choose which immediately yields that . Furthermore, by the restriction of and the definition of .
Thus we have from (42) We let tend to zero and obtain and we have left