We perform an asymptotic analysis with respect to the parameter of the solution of the scalar advection–diffusion equation , , supplemented with Dirichlet boundary conditions. For small values of ε, the solution exhibits a boundary layer of size in the neighborhood of (assuming ) and an internal layer of size in the neighborhood of the characteristic starting from the point . Assuming that these layers interact each other after a finite time and using the method of matched asymptotic expansions, we construct an explicit approximation satisfying . We emphasize the additional difficulties with respect to the case M constant considered recently by the authors.
Let and . This work is concerned with the scalar advection–diffusion equation
where is the diffusion coefficient and is the transport velocity. For any initial data and Dirichlet condition , there exists a unique solution .
This apparently simple partial differential equation appears in many situation as it is a prototype of models where the diffusion coefficient is small compared to the others. As explained in [8], this model can notably be seen as an embedded system of the Navier–Stokes system with non-characteristic boundary condition and viscosity coefficient equals to ε. It also can be seen as a regularization of a transport equation and for this reason is well employed in numerical analysis (see notably [10,27] and the references therein) when one wants to obtain robust numerical approximation uniformly with respect to ε small. Equation (1) appears in models of miscible displacement of compressible fluids in porous media, with small molecular diffusion and dispersion coefficients, see [6]. Last, it also appears in the context of exact boundary controllability when one wants to steer to zero the solution with a uniform control v: we mention the seminal works [9,14] and the recent papers [19,20].
We are interested in this work with a precise asymptotic description of the solution when ε is small. This problem has been the subject of several studies in the last decades in the case for which the transport velocity is constant and the equation is defined over . We refer to [24,25]. The case of a transport velocity depending only on the time variable has been formally discussed in [21] and deeper analyzed in [26].
Internal (red) and boundary (blue) layer zones for for a constant velocity (left) and non constant velocity (right).
For bounded domains with respect to the space variable, the asymptotic analysis is quite involved as several singular layers may appear in and interact each other. The constant transport velocity case has been analyzed in [3]. More precisely, if we denote the characteristic through as the solution in of
then the violation of the compatibility conditions between and v at the point for which induces a thin inner region (called internal layer) of size in the vicinity of the characteristic where the solution exhibits rapid variations. Thus, if this characteristic gets arbitrarily close to the line in a finite time unique solution of the equation
then the internal layer interacts with the usual boundary layer of size living along and induced by the Dirichlet condition. Figure 1 provides a geometric description of this phenomenon in two cases: the case in Fig. 1-Left for which the function M is constant, i.e. leading to a linear characteristic of equation . The internal layer lives in the red zone and intersects the boundary layer occupying the blue zone in a small neighborhood of the point such that . This case has been extensively studied in [3] (see also [1,2]). Figure 1-Right corresponds to a more general situation for which the function M is not constant. The characteristic starting from the point has the equation .
In this paper, we extend the analysis given in [3] devoted to a constant velocity and perform an asymptotic analysis of the solution of (1). More precisely, assuming the data regular enough, we construct for any small an approximation of the solution such that . We refer to Theorem 3.1 in Section 3 for the precise statement. Compared to [3] where a rate of order is obtained for the constant case, we thus get a rate of order . As we shall see, this is due to the fact that the non constant case under consideration here involves less explicit computations and developments leading to a more tedious analysis, see final comments in Section 5.
The rest of the paper is organized as follows. In Section 2, we set up the matched asymptotic method by considering two terms in the expansion. In particular, we employ fundamental solutions for a parabolic equation with unbounded coefficients to construct an approximation of the solution in the internal layer of size (we refer to Lemma 2.2). The method leads to a so-called composite approximations given by (32). Then, in Section 3 by considering the system satisfied by and using a Gronwall–Bellman type inequality (see Lemma 3.4), we prove an a priori estimate for leading to Theorem 3.1. Some computations are collected in the appendice. In Section 4, we consider some explicit simple examples of transport velocity M and evaluate numerically the norm with respect to ε in agreement with our theoretical estimate. We conclude with some remarks in Section 5.
Matched asymptotic expansions and approximate solutions
In order to construct an asymptotic approximation of the solution of (1), we employ the method of matched asymptotic expansions ([11,15,16,18,22,28]). We also refer to [13] for a recent exposition. The solution exhibits two inner regions: an internal layer located along the characteristic and a boundary layer living along . The internal layer is of size while the boundary layer is of size . The outer region is the subset of consisting of the points far from the internal and boundary layers, it is of size. The occurrence of these three distinct regions require to introduce three distinct asymptotic expansions. The first one, the so-called outer expansion, lives far away from the inner regions and is given by
for some integer . A second one, the so-called first inner expansion, living in the neighborhood of is given by
Last, a third one, the so-called second inner expansion, living along , is given by
where is the unique solution of (3). In particular, these expansions make appear several variables, at different scales, namely, x, t, , and .
We will construct outer and inner expansions which will be valid in the so-called outer and inner regions, respectively. There are intermediate regions between the outer region and the inner regions, with size , . To construct an approximate solution we require that inner and outer expansions coincide in each intermediate region, then some conditions must be satisfied in that region by the corresponding inner and outer expansions. These conditions are the so-called matching asymptotic conditions.
The strategy is as follows. We first identify the functions , , in the outer region. Then, we identify the functions , , of the first inner expansion satisfying the matching conditions (with the ). This allows to define an expansion in the form , valid far away from , as a linear combination of the functions and . Then, we identify the functions , , of the second inner expansion satisfying the matching conditions (with the ). Eventually, we define an expansion , valid in the whole domain , as a linear combination of the functions and , and supposed to be an approximation of . In this work, for simplicity we restrict ourselves to the case as it will allow to get an approximation with rate .
A property of the characteristics
We assume that M is a positive and smooth function in . Let be the characteristic through defined as the solution in of equation (2). Using a classical result of differentiation with respect to a parameter of solutions of a differential equation we get that X is a smooth function of the variables t, x, and s. In particular,
i.e. satisfies the integral equation
We set
Let denote the unique solution of the equation
Differentiating equality (4) with respect to x gives
hence
since .
Outer expansion
Putting into equation , the identification of the powers of ε yields
Taking the initial and boundary conditions into account we define and as functions satisfying the transport equations, respectively,
We find explicit representations of solutions of these equations by using the method of characteristics. We get
and
Inner expansion along the characteristic
We consider the change of variable and function . satisfies the equation
Using the Taylor expansion
then, putting into equation (8), the identification of the powers of ε yields
Obviously, the main difference with respect to the case M constant considered in [3] is the occurrence of some additional unbounded terms with respect to the variable w.
To get the asymptotic matching conditions we write that, for any fixed t and large w,
Rewriting the right-hand side of the above equality in terms of w, t, and using Taylor expansions we have
Therefore, the matching conditions read
where stands for .
Consequently, we obtain that the function must satisfy
In view of (7), we have and . Remark that these limits do not depend on t. Similarly, the function must satisfy
In view of (7), and where is given by (5). Remark that these limits do depend on the variable t.
Representation of the functions and
We express the functions and in term of the fundamental solution of the heat equation.
Fundamental solutions
Let us consider the differential operator
Equation is a parabolic equation with an unbounded coefficient. Linear second order parabolic equations with smooth but unbounded coefficients are studied in [5] (see also [7,12,17]). In [5], the authors consider a second order linear differential operator in the form
and prove the existence of a so-called fundamental solution for . Our operator is obviously of the form of the operator with , , and .
A function defined for and is said to be a fundamental solution of if it has the following properties:
considered as a function of for each fixed , the derivatives of which appear in exist and are continuous;
in ;
If is a continuous function with compact support in then
We shall employ the following lemma.
Letbe a given function in. Assume that f is Hölder continuous on every compact subset of. Thenis a solution of the Cauchy problem
In the particular case of the operator , the solution of the corresponding Cauchy problem has an explicit representation in term of the fundamental solution of the heat equation in defined as follows
with
Precisely, we have the following result.
Letbe the parabolic operator defined by (
12
) and H be the fundamental solution of the heat equation defined by (
13
). Then:
Equationhas a fundamental solution given bywith
Letbe a continuous function inand Hölder continuous with respect to w uniformly for. Letbe a continuous function with compact support in. Then,is a solution of the Cauchy problem
We have
Note also that B is a strictly increasing function so that is equivalent to . Consider the function K defined by (15). We have
For ξ, τ fixed, , , we have by a direct calculation
Then, for any and . If is a continuous function with compact support in we have
Using the change of variable , it holds that
and deduce that
According to Definition 2.1, it follows that the function K given by (15) is a fundamental solution of the equation . Moreover, using that and , we have
implying that
We also have, for any ξ fixed, from which we check that .
Let now U be given by (16). We have
Using again the change of variable , it holds that
We conclude that U given by (16) is a solution of the Cauchy problem (17). □
We now introduce the functions , , defined as functions on and satisfying
We also introduce the functions , , defined on by
Explicit expression of
In order to apply the second part of Lemma 2.2, it remains to choose an initial condition g (for the boundary value problem satisfied by ) so that the corresponding solution given generically by (16) satisfies the asymptotic conditions as (see (10)), i.e. and . The simplest choice, discussed in [3], is given by with
leading to the explicit expression:
Recall that erf is the error function defined by for all , and that the complementary error function is defined by . Using the asymptotic behavior of the error function, we check that satisfies the prescribed asymptotic behavior in (10). Remark also that equals if and if .
Integral representation of
The computation of solution of the boundary value problem (11) posed over is more delicate since, first there is a right side, and second, because the asymptotic limits as depend on the time variable, while the function g in (17) not. This fact requires a special treatment.
Let us consider the function . We have, for ,
Differentiating equation with respect to x yields
with and . Letting , we get
Therefore, for , we have
When has a jump on , the function becomes singular on . This leads to regularize the function as follows. Let such that
We define
Clearly, , for and for . Define
and then as follows
The functiondefined by (
23
) satisfies (
11
), namelyinandfor all t in.
It remains to check the asymptotic condition as . For any , let us consider the integral
In view of (18) and (20), we obtain explicitly
then
For the convergence of the integral in the neighborhood of , we consider the integral , with fixed, and use the change of variable . This gives
The integrand is clearly uniformly bounded in w by with a constant depending only on and t. Moreover, for any fixed v and τ, the integrand tends to 0 as . Using a result of limit passage on integrals depending on a parameter we get .
For the convergence of the integral in the neighborhood of , we consider the integral
Using the change of variable , we get
and conclude as before that and then that .
Consider now the integral
Clearly, is a smooth function on and satisfies for . The change of variable gives
The integrand is uniformly bounded in w by , where depends only on t. Moreover, the integrand tends to 0 as . Then .
We then have
It results from (23) that, for each fixed t, . Since , we conclude that . □
Composite asymptotic approximation outside the boundary layer
We now define a composite approximation of the solution far from the obtained by adding, at each order, the inner and outer expansions and then by subtracting their common part.
At the first order, the common part of and (defined by (7) and (20) respectively) is equal to for and to for . Thus, the first term of the composite approximation outside the boundary layer along is given by
We check that the function is continuous along the characteristic as it satisfies . The second term of the composite approximation is given by
where is defined by (23). Clearly, is also continuous along the characteristic. Then the following quantity is defined to be an asymptotic approximation of , outside the boundary layer along ,
We easily verify the following property.
Assume thatand. Thenbelongs to.
Inner expansion along
We consider the change of variables , , and function . Recall that defined by is the time at which the characteristic starting from the point intersects the right extremity of the domain. We assume that exists. Moreover, since , is unique. The function satisfies the equation
Using the Taylor expansion
and putting into equation (26), the identification of the powers of ε yields
It is important to note that the functions depend on three variables, namely z, t but also τ. As it is standard, the variable is introduced to describe the boundary layer at . Here, the variable allows to take into account the interaction of the internal and boundary layers by making a zoom around the point . If we do not introduce this variable τ, we see notably that solves the same ordinary differential equation than , and the analysis leads to an error estimate (for the norm) of order only. Remark that the variable , as a solution of is not explicit. Therefore, instead of , we could have introduced ; however, we have observed that this leads to some incompatibilities with the matching conditions.
We impose for . To get the asymptotic matching conditions we write that, for any fixed τ, t and large z,
In order to identify at each order the appropriate matching conditions, we need to rewrite the right-hand side of the above equality in terms of z and τ, t being fixed. We have the following equalities , , , , . Writing , , and using Taylor expansions we have
then
It results that
Writing , , and
, and using again Taylor expansions we have
and
We deduce that
with
Therefore, the matching conditions read
We define as a solution of
The solution is
We define as a solution of
Writing that , we obtain, for ,
Asymptotic composite approximation in
We are now in position to define what is supposed to be an asymptotic approximation of the solution . We proceed as before by adding at each order the function , approximation outside the boundary layer along , and the function , approximation in the boundary layer along , then subtracting their common part. At the first order, the composite approximation is given by
i.e. explicitly
Repeating the arguments at the next order, we define
then we define an asymptotic composite approximation of in by
Convergence of the sequence
This section is devoted to prove that the sequence constructed in the previous section provides an approximation of the solution of the advection–diffusion problem (1). Precisely, our main result is as follows.
Letbe the unique solution of (
3
). Assume,,and. Forsmall enough, letbe the solution of (
1
). Then, the functiondefined by (
32
) satisfiesfor some positive constantdepending on the data, v and M but independent of ε.
In order to prove this result we need to establish a number of preliminary results. We define the error as follows:
where is the initial layer corrector defined as a solution of the equation
Preliminary results
From now on, in order to shorten some equations, we shall use the following notation:
Estimate of the initial layer corrector
The following lemma gives an exponential decay property of the initial layer corrector.
Letbe the solution of problem (
34
) and. There exists a constant c independent of ε such that
i) We first check that the initial data is given by
showing that the initial condition gets concentrated in the neighborhood of . Indeed, from (30)–(32) we have
We have from (30)
Using the matching conditions of with , we check that , for and that
It results that for all . These computations lead to (37).
ii-a) We now introduce a cut-off function such that if and if and define, for , the function by . The solution of the linear system (34) can be decomposed as with
In view of the definition of , we see that for all . Then, in view of (37), we check that there exists a constant independent of ε such that for all . By a maximum principle, it follows that
ii-b) Concerning , we check that for all and that for some constant , independent of ε. We now estimate . For that, for any , we check that the function with solves
and satisfies the estimates
with . Gronwall inequality leads to , which is equivalent to
Consequently,
using that (recall that ) and . The value then leads to
for some constant , using that . From inequalities (40) and (42) we deduce (36). The initial layer concentrated in the neighborhood of vanishes exponentially fast with respect to t since the velocity transport is strictly positive. □
Estimate of
Recall that is the differential operator defined by (35). We have the following result proven in Appendice A.1.
Assume hypotheses of Theorem
3.1
. The functiondefined by (
32
) satisfieswithwith,.
From the previous expansions, we get the following estimate for the norm. Details of the proof are given in Appendix A.3.
Assume hypotheses of Theorem
3.1
. Letbe the function defined by (
32
). There exists a constant c independent of ε such that
Gronwall–Bellman type estimate
We now derive a priori estimates for the function . Preliminary, since is not vanishing at and , we define
where and satisfies and , and . The function solves the equation
where , . Recall that is defined by (35).
In order to derive an estimate for , we shall use the following Gronwall–Bellman type inequality (see [23]).
Let,. Ifsatisfieswith, then for,where.
Letbe the function defined by (
44
) andthe function defined by (
32
). There is a constant c independent of ε such that, for each t in,with.
Multiplying equation (45) by and integrating over gives
Applying the Cauchy–Schwarz inequality we obtain
with . Applying Lemma 3.4 with
we obtain (46). □
Estimate of , and ,
We now estimate each term of the right-hand side of (46).
There is a constant c independent of ε such that,,with,.
Let be arbitrary, and , , . We have from (33) that
We have
then we deduce that
By similar arguments to that used in the proof of Lemma 3.3 (point (e.2)), we show that allowing to conclude that .
We also have
Writing , and arguing as above we get that
Similarly as above we have
then conclude that . Inequality (47) follows.
Concerning the second inequality, we have
We have the following estimates, see the proof of Lemma 3.3 (points (c.3), (e.3), and (e.4), respectively),
Then clearly,
We have from (73)
then taking and there holds that
then . We show, as above, that
As in the proof of Lemma 3.3 (point (e.3)), we get . Thus . Similarly , so that (48) follows. Eventually, we easily check that (49) holds. This ends the proof of the lemma. □
We are now in position to finish the proof of Theorem 3.1. It remains to choose the function , satisfying and so as to minimize the terms in the right side of (46), asymptotically with respect to ε. We consider the functions
so that and , for . It follows that, for , and for each ,
Coming back to Lemma 3.5, using the two previous estimates and Lemma 3.3, there holds that
Now, since , we deduce that
Writing and using (49), there holds that
These estimate allow to deduce from (50) that for all . Finally, since , using Lemma 3.1, we derive the estimate
This ends the proof of Theorem 3.1.
Some explicit examples
We explicit in this section some expansion of for some particular case of the function then numerically evaluate the norm of the difference .
The case , in , in
The characteristic starting from is given by where the function solves
and is given by . such that is then given by . Then,
leading to . We obtain that defined by (7) is given by
and
defined by (24) is given by while simply . Then, we get
implying
Consequently, our approximation is given by
Remark that so that . As an illustration, Fig. 2 depicts the function in for with . In particular, observe that does not vanish at and but gets small as ε decreases. Table 1 provides some numerical values of the norm for several values of the parameter ε. The unknown solution of (1) is obtained here using a numerical approximation. We obtain in full agreement with our estimate in Theorem 3.1.
In this case, the function is given by . such that is . Then,
leading to . We obtain that defined by (7) is given by
and
defined by (24) is given by while simply . Then, we get
implying
Consequently, our approximation is given by
with here .
Concluding remarks
We have performed an asymptotic analysis of the solution of an advection–diffusion equation with a small diffusion coefficient . The analysis takes into account the intersection of several singular layers and leads to an approximation in an -neighborhood of the solution for the norm . This analysis extends [3] to non constant, strictly positive transport velocity, leading to much more technical arguments. In particular, the solution in the internal layer (following the characteristic starting form ) solves a parabolic equation with non constant and unbounded coefficients related to the first derivatives of the velocity. The resulting solution is expressed in term of the kernel of the heat equation.
The rate obtained for the final estimate is driven by our approximation in the internal layer, which depends on the non-unique choice of the function . The choice (19) is simple and involves the property in agreement with the fact that . However, it implies that different for when . This gap at the point between and generates an artificial corner layer in the approximation in the neighborhood of the point . This induces an error propagating along the characteristic then affects the quality of the approximation. Precisely, with this simple choice of , the norms of and are of order ε and one respectively (we refer to the proof of Lemma 3.6); this implies an approximation error of order . By analogy with [3, Section 3] devoted to the constant transport case, one may consider the more involved choice
with leading to with
and defined by (20). The new function still satisfies the asymptotic conditions and for all . Moreover, we now observe that
Therefore, this avoids at the first order the corner layer at the point and allows to describe more accurately the discontinuity between the initial and Dirichlet conditions in the neighborhood of the point . In [3] devoted to the constant transport case, this choice leads to an approximation error of order . It remains to check that the choice (52) leads to the same rate in the non constant case.
Beyond this delicate issue related to the corner layer at the point , in order to get a better rate, one would needs as in [3] to consider additional terms in the developments, notably the outer term defined in Section 2.2 not used here, internal layer terms , involving the heat kernel and boundary layer terms and solutions of ordinary differential equations with respect to the variable z. Whether or not we can perform the computations and get a priori estimates with these additional terms is an open issue.
In a future work we plan to study the parabolic system describing the miscible displacement of compressible fluids in a porous medium. The displacement of one compressible fluid by another, completely miscible with the first, in a one-dimensional porous medium , assuming for simplicity that the two fluids have the same compressibility factor z, is described by the following differential system, see for instance [6],
to which initial and boundary conditions are added. The unknowns of system (53), (54) are the functions , and ; p is the pressure, c is the concentration of one of the two components of the fluid mixture, and q is the Darcy velocity. The function is the permeability of the medium, the constant ϕ is the porosity, is the concentration-dependent viscosity of the fluid mixture, is a small term representing the molecular diffusion and dispersion in the porous medium. The viscosity is assumed to be determined by some mixing rule. See [4] for the existence of a weak solution to the one-dimensional equations governing compressible flows of m miscible components in a porous medium. Our aim is to perform an asymptotic analysis of system (53), (54) when d is small and the concentration c satisfies Dirichlet boundary conditions on and .
Footnotes
Acknowledgement
The authors thank the funding by the French government research program “Investissements d’Avenir” through the IDEX-ISITE initiative 16-IDEX-0001 (CAP 20-25).
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