1. Introduction
The main object of study in this paper is the following Rayleigh-Stokes problem for a generalized second-grade fluid with a time-fractional derivative model:
where
is a fixed constant, the initial data
and the source term
are given functions,
, and
is the Riemann-Liouville fractional derivative of order
defined by (see, e.g., [
1]):
Here
is the gamma function. Usually problem (
1) is considered in the domain
,
, with a sufficiently smooth boundary
. Problem (
1) is also called
the forward problem.
Equation (
1) when
is also called the Haller equation. Such equations arise when describing the movement of soil moisture (see, for example, in [
2], formulas (1.4) and (1.84) on p. 137 and 158, [
3], formula (9.6.4) on p. 255, and [
4], formula (2.6.1) on p. 59).
In recent years, much attention has been paid to the Rayleigh-Stokes problem (
1) because of its importance for applications (see, e.g., [
5,
6]). This problem plays an important role in the study of the behavior of some non-Newtonian fluids. The fractional derivative
is used in equation (
1) to describe the viscoelastic behavior of the flow (see e.g., [
7,
8]).
In order to get an idea of the behavior of the solution of this model, a number of authors have shown considerable interest in obtaining an exact solution in some special cases; see e.g., [
7,
8,
9]. To find the exact solution to the problem, Shen et al. [
8] used the sine Fourier transform and then applied the fractional Laplace transform. For the case of homogeneous initial and boundary conditions in a rectangular domain, Zhao and Yang [
9] obtained exact solutions using the Fourier method. Note, here the eigenfunctions are written out explicitly. The authors of the above papers wrote out a formal solution, and the questions of the regularity of the solution were not specially studied.
Questions of the regularity of the solution were studied in the fundamental work Bazhlekova et al. [
10]. The authors proved the Sobolev regularity of the homogeneous problem both for smooth and non-smooth initial data
, including
.
The exact solutions obtained in the above papers include infinite series and special functions such as generalized Mittag-Leffler functions and are therefore inconvenient for numerical solution. In addition, explicit solutions are available only for a limited class of problem settings. Therefore, it is very important to develop efficient and maximally accurate numerical algorithms for the problem (
1). Numerous works of specialists are devoted to this issue. An overview of the work in this direction is contained in the above work [
10]. See also recent papers [
11,
12] and references therein.
Quite a lot of works are devoted to the study of the inverse problem of determining the right-hand side of the Raleigh-Stokes equation (see, e.g., [
13,
14,
15] and the bibliography therein). However, the case when the right-hand side has the general form
has not yet been considered by anyone. In all known works, the right-hand side can be represented as
, where
is a given function, and
is a function to be determined. Since this inverse problem is an ill-posed problem in the sense of Hadamard, various regularization methods are proposed in the above papers. Also in these papers, the proposed regularized methods were tested by simple numerical experiments to check the error estimate between the desired solution and the regularized solution.
Note that such an inverse problem is ill-posed in the Hadamard sense also for the subdiffusion equation (see, e.g., [
16,
17,
18]).
In the case when the initial condition
in problem (
1) is replaced by
, then the resulting problem is called
the backward problem. The backward problem for the Rayleigh-Stokes equation is of great importance and it consists in determining the previous state of the physical field (for example, at t = 0) based on its current information (see, e.g., [
19,
20] and the bibliography therein). However, this problem (as well as the inverse problem of finding the right-hand side of the equation) is not stable. In other words, a small change in
leads to a large change in the original data. The authors of the above works proposed various regularization methods and tested these methods using numerical experiments.
Let us list the main findings of this paper.
- (1)
We will give a mathematically justified solution to the forward problem. A formal formula for the solution in the form of eigenfunction expansions was given in the paper [
10], cited above (see also [
15,
19,
20]), but the convergence of the series itself and the differentiated series has not been investigated.
- (2)
We will pay special attention to the backward problem, since in previous papers (see, e.g., [
19,
20]) the authors considered only the case
. And this is connected with the method used in these works: if the dimension of the space is less than four, then for the eigenvalues
of the Laplace operator with the Direchlet condition, the series
converges. In our reasoning, no conditions are imposed on the spectrum of the operator.
- (3)
It is well known that in order to choose the only solution of differential equations that simulates some phenomenon, the initial condition is used. However, there are also processes in which, instead of initial conditions, it is necessary to use non-local conditions, for example, an integral over time intervals, or a connection between the solution values at different points in time, for example, at the initial moment and at the final moment of time. Of course, non-local conditions take into account some additional information and therefore they more accurately model some of the details of natural phenomena.
In the present paper we consider problem (
1) with a non-local time condition:
In the case of classical diffusion equations (i.e.,
), such a non-local problem has been studied by many researchers (see, for example, [
21,
22,
23]). It should also be noted that various non-local boundary value problems for parabolic equations are reduced to a problem with condition (
3) (see [
24], Chapter 1). In the case when it is required that at the final time the temperature of the physical field differs from the initial temperature by the value
, we come to the study of just such a non-local problem.
It turns out that the non-local problem is well-posed. In other words, a solution to a non-local problem exists and is unique. Moreover, the solution depends continuously on the function in the non-local condition.
Thus, the problem of determining the previous state of the physical field on the basis of current information is an ill-posed problem. However, if, without knowing the initial and present states, we want them to differ by the value , then such a problem turns out to be correct.
The remainder of this paper is composed of seven sections and Conclusion. In
Section 3, we give exact formulations of the problems under study. In the next section, we introduce the Hilbert space of “smooth” functions with the help of the degree of the elliptic operator under consideration, and recall some properties of function
, introduced in [
10].
Section 4 is devoted to the study of the main problem (
1) with operator
A instead of the Laplace operator. Here, conditions are given on the right-hand side of the equation and on the initial function, under which the solution of problem (
1) is found in the form of eigenfunction expansions. In
Section 5, we study the backward problem. As noted above, this problem is not well-posed according to Hadamard. Nevertheless, this section shows that if we consider
in the class of smooth functions, then stability is preserved.
Section 6 studies the conditional stability of the backward problem. The next two sections are devoted to the study of problem (
1) with the non-local time condition (
3).
2. Problem Statements
The method of our research is the method of separation of variables. Therefore, only eigenfunctions and eigenvalues are needed from the Laplace operator in the Rayleigh-Stokes problem (
1). With this in mind, instead of the Laplace operator
in problem (
1), we consider an abstract positive operator.
Thus, consider an arbitrary unbounded positive self-adjoint operator
A in the Hilbert space
H. Let
A have a complete in
H system of orthonormal eigenfunctions
and a countable set of positive eigenvalues
. Let
be the scalar product and
be the norm in
H. For a vector-valued functions (or simply functions)
, we define the Riemann-Liouville fractional derivative of order
in the same way as (
2) (see, e.g., [
25]). Finally, let
stand for a set of continuous in
functions
with values in
H.
Consider the following Rayleigh-Stokes problem
where
is a fixed constant,
and
and
is equal to 0 or 1. If
then this problem is called
the backward problem and if
, then it is called
the non-local problem. We will consider both of these cases.
In a recent paper [
26], the authors considered the subdiffusion equation with the Caputo-Fabrizio derivative on a
N-dimensional sphere with a non-local condition
. The motives for studying non-local boundary values are given. Cases
and
are studied separately. The solution limit at
is also studied.
In the present paper, various initial problems are considered. The solution of these problems is defined in a standard way: all vector functions and their derivatives included in the equation and in the initial conditions must be continuous in the variable
t, and all the corresponding equalities should be understood as the equality of the vectors from
H at each point
t. As an example, we give the definition of a solution to problem (
4).
Definition 1. We call a function the solution of the non-local Rayleigh-Stokes problem (4), if and it satisfies conditions (4). To solve problem (
4) in the case when
, we divide it into two auxiliary problems:
and
where
is a given function.
Problems (
5) and (
6) are a special case of problem (
4), so solutions to problems (
5) and (
6) are defined similarly to Definition 1.
If
and
and
are solutions of the formulated problems, then it is easy to check that the solution to problem (
4) has the form
. Therefore, it suffices to consider auxiliary problems.
Remark 1. We note that, as operator A one can take, for example, the Laplace operator with the Dirichlet condition in an arbitrary N (not only )—dimensional domain with a sufficiently smooth boundary. For our reasoning, it is sufficient that operator A has the properties listed above.
In [
27,
28], a similar non-local problem with an arbitrary parameter
was studied in detail for subdiffusion equations with Riemann-Liouville and Caputo derivatives. For the classical diffusion equation with the parameter
, it was first considered in [
21,
22,
23].
3. Preliminaries
In this section, using the degree of operator
A, we introduce the Hilbert space and recall the main properties of function
introduced in [
10] (see also [
19]), which we will use further.
Let
be an arbitrary real number. We introduce the power of operator
A, acting in
H according to the rule (note, operator
A is positive and therefore
for all
k)
Here and everywhere below, for the vector
, the symbol
will denote the Fourier coefficients of this vector:
. The domain of definition of this operator is determined from condition
and has the form:
For elements of
we introduce the norm
With this norm, the linear-vector space becomes a Hilbert space.
Let
be a solution of the following Cauchy problem
The solution of such an equation is expressed in terms of the generalized Wright function (see e.g., A.A. Kilbas et. al [
1], Example 5.3, p. 289). But function
, the solution of this Cauchy problem, is studied in detail in Bazhlekova, Jin, Lazarov, and Zhou [
10]. See also Luc, Tuan, Kirane, Thanh [
19], where very important lower bounds are obtained.
We also note the work of Pskhu [
29], where a more general Cauchy problem than (
7) was studied. From the results of this paper one can obtain a representation for the solution of the Cauchy problem (
7), which is very convenient for further research.
The authors of [
10], in particular, proved the following lemma.
Lemma 1. Let be a solution of the Cauchy problem (7). Then - 1.
,
- 2.
,
- 3.
,
- 4.
It should only be noted that in paper [
10], instead of assertion 2, a more general proposition was proved. But the assertion 2 in our lemma easily follows from the representation of function
, also obtained in [
10]:
where
The following assertion is also implicitly contained in [
10]. But in view of its importance in our reasoning, we present a proof.
Lemma 2. The Cauchy problemhas the only solution Proof. Since
, then
(change the order of integration)
(change of variables:
)
Thus, given that
is a solution to the Cauchy problem (
7), we obtain
□
Corollary 1. The Cauchy problemhas the only solution We also need the following properties of function .
Lemma 3. There is a constant , such that Proof. Therefore, by the definition of
,
(change of variables:
)
□
One can also obtain an estimate for with a smaller singularity at .
Lemma 4. There is a constant , such that Proof. Again by the definition of
one has
□
Now, by combining these two estimates, we can obtain the following statement, which we also apply further.
Lemma 5. There is a constant , such that for any ε, , we have Proof. Let
. Apply Lemmas 3 and 4 to get
□
In the future, instead of
, we will have eigenvalues
of operator
A. The next lower bound for
was obtained in Luc, N.H., Tuan, N.H., Kirane, M., Thanh, D.D.X [
19]. For the convenience of the reader, we present this proof.
Lemma 6. The following estimate holds for all and :where Proof. Since the modulo of trigonometric functions does not exceed one and
, then
It should be noted that the improper integral converges. Indeed,
□
4. Forward Problem
Consider the following Cauchy problem:
where
is a given vector of
H. We also call this problem
the forward problem.Theorem 1. Let and . Then for any problem (13) has a unique solution The estimate of the coercive type is valid with some constants C and : Moreover, the estimateis valid, where is a constant depending on T. As noted in the introduction, the Cauchy problem (
13) in the case when
A is the Laplace operator in the
N-dimensional domain (
) has been considered by many authors. So the authors of [
10] establish the Sobolev regularity of the homogeneous problem for both smooth and non smooth initial data
. In particular, the authors proved an estimate similar to (
15) (see estimate (2.16), note that in this paper
).
Formula (
14) for solving problem (
13) is formally given in the same article of Bazhlekova, Jin, Lazarov, and Zhou [
10], but since this paper is devoted to the study of a homogeneous problem, the question for which
and
it gives a solution to problem (
13) is not considered. Note that functions
and
must be such that, for example, the series (
14) allows term-by-term differentiation with respect to the variable
t.
The formula is also contained in papers [
15], Equation (2.2), [
19], Equation (2.6) and [
20], Equation (
8). Again, since these works are devoted to the study of other problems, the above issues were not considered.
Proof. According to the method of separation of variables, we expand the functions
and
in terms of the system of eigenfunctions
with coefficients
and
correspondingly. The solution of problem (
5) will be sought in the form of a series
with unknown coefficients
.
It is easy to verify that functions
are solutions of the Cauchy problem (
11) with the right-hand side
, the initial condition
and with the parameter
. Therefore (see (
10))
Thus, series (
14) is a formal solution to problem (
13). It remains to show that the series itself and the series obtained after differentiation also converge. Let us get started with this task.
By Parseval’s equality, the first assertion of the Lemma 1, and Hölder’s inequality, we have
Now consider the series after differentiation. Apply Parseval’s equality to obtain
Generalized Minkowski inequality and Lemma 5 imply
Similarly, apply Parseval’s equality and Lemma 5 with
to get
Therefore, it follows from the above
and
Note that , .
Thus, it has been shown that the function defined by the series (
14) is indeed a solution to problem (
5).
Obviously, (
15) follows from the established estimates.
As for the uniqueness of the solution of problem (
5), it follows from completeness of the set of eigenfunctions
in
H. Indeed, suppose the problem has two solutions
and
. Then the difference
is a solution of the homogeneous problem:
Let
be any solution of this problem. Consider the Fourier coefficients
. It is not hard to see, that
is a solution of the Cauchy problem
Corollary 1 implies that for all k. Since the set of eigenfunctions complete in H, then .
It remains to prove estimate (
16). Let
be a partial sum of the series (
14). Then
Apply Parseval’s equality and estimate 3 of Lemma 1 to obtain
Similarly,
(apply generalized Minkowski inequality)
The last two estimates imply (
16).
The theorem is completely proven. □
5. Backward Problem
In the present paragraph we consider the following
backward problem:
where
is a given vector of
H. It should be specially emphasized that for the backward problem the parameter
in the Rayleigh-Stokes equation plays an important role. If this parameter is equal to zero, then we get the classical diffusion equation, for which the backward problem is strongly ill-posed: not for any
(even not for any
) there is a solution, and if it exists, then a small change in
leads to a very strong change in the solution (see e.g., Chapter 8.2 of [
30]). In the next Theorem 2, we show that the parameter
“ennobles” the backward problem for the Rayleigh-Stokes equation and its solution already exists for all
.
Nevertheless the solution to problem (
18) is also unstable, as is the solution to the classical diffusion equation (i.e.,
). Indeed, let
and take
as a initial condition in problem (
13). Then the unique solution to problem (
13) is (see Theorem
13)
This function is a unique solution of the backward problem (
18) with
.
Therefore, on the one hand,
and it tends to zero as
(even
for any
), and on the other hand, according to Lemma 6,
However, the situation changes if we consider the norm of in the space ; note that norm is unbounded as .
Theorem 2. Let and . Then for any problem (18) has a unique solution. Moreover there exists a constant , depending on and T, such that Let . Then there exist constants , such that Note that in work [
31] the backward problem for the subdiffusion equation
was studied. It is shown that an estimate similar to (
20) is valid only with the norm
. However, if we take the derivative in the sense of Caputo in the subdiffusion equation, then the estimate (
20) with the norm
is valid (see ([
32])).
Proof. Let us take a solution (
14) with an unknown initial function
and use condition
to determine this unknown function. Then the Fourier coefficients of
has the form
and the unique formal solution of the backward problem can be written as
According to Theorem 1, this formal solution will indeed be a unique solution to the backward problem if the condition is satisfied. Let us check this condition.
Again this lemma and estimate 3 of Lemma 1 imply (see (
17))
Thus
and therefore, function
defined above is indeed a solution to the backward problem ((
13).
Let us pass to the proof of estimate (
19). We note right away that in order to estimate the norm in
H, by virtue of the Parseval equality, it is sufficient to estimate a series of Fourier coefficients.
Application of Lemmas 1 and 6 gives
Apply Lemma 6 for
in the denominator, estimate (1) of Lemma 1 for
in the numerator, and finally estimate (3) of Lemma 1 for
under the integral sign (see (
17)). Then
Similarly, by virtue of estimate (3) of Lemma 1 we obtain
As for estimate (
20), its left part follows from the just proved estimate (
19), while the right part is contained in (
16). □
As noted in the introduction, statements similar to Theorem 2 were known earlier (see, e.g., [
19,
20] and the bibliography therein). In these papers, operator
A is the Laplace operator with the Dirichlet condition in the domain
,
.
Let us make a few remarks:
- 1.
The left side of the estimate (
20) means that a small change of
in the norm
entails a small change in the norm
of the initial data.
- 2.
The right side of this estimate asserts the unimprovability of the left side, i.e., it is impossible to replace the norm with the norm with any .
- 3.
For the classical diffusion equation (i.e.,
), the statement of Theorem 2 naturally does not hold, since
(see the definition of this constant in Lemma 6). It should also be noted that if we consider the backward problem for the classical diffusion equation, then for its solution estimates of the type (
20) on the scales of spaces
are generally impossible (see, e.g., Chapter 8.2 of [
30]).
6. Conditional Stability
Following work Luc, Huynh, O’Regan and Can [
20], in this section we consider the problem of conditional stability of the backward problem. In other words, suppose that the initial data
satisfies the following a priori estimate:
where
and
are positive constants, and consider a class of functions that satisfy this condition.
So what does conditional stability mean? We saw above that the solution to problem (
18) is not stable, i.e., a small change in
leads to a large change in the original data
. If for some class of functions
(see (
22)) stability takes place, then the problem is called conditionally stable.
The following statement is true:
Theorem 3. Let satisfy condition (22). Then there is a constant C depending on and T such, that This theorem for the case of the Laplace operator with the Dirichlet condition in
N,
,—dimensional domain was proved in the above paper [
20] (note that the condition of the theorem in [
20] is slightly different). Note that in this case the estimates
hold for the eigenvalues of the Laplace operator, and the proof in [
20] is based on the convergence of the series
The proof of Theorem 3 repeats the proof of [
20] with a slight change. For the convenience of the reader, we present this proof.
We emphasize that the assertion of Theorem 3 is valid without any conditions on the spectrum of operator A.
Proof. Apply the Hölder inequality with parametrs
and
to obtain
Finally estimate 1 of Lemma 1 and the Hölder inequality give
The last two estimates imply estimate (
22). □
9. Conclusions
In many papers, explicit solutions of the simplest Rayleigh-Stokes problems are constructed. In [
10], the regularity of the solution was studied for the first time and a formal formula for solving an in-homogeneous problem in a three-dimensional domain was given. Also, the backward problem was studied by the authors in domains of dimension less than four. Some proofs of these results essentially use the fact that the dimension of the domain under consideration is
.
In this paper, all these questions are investigated for the case of an abstract operator instead of the Laplace operator in the Rayleigh-Stokes problem. In addition, a new non-local problem for equation Rayleigh-Stokes is considered and it is shown that, unlike the backward problem, it is well-posed. As the operator A, we can take the Laplace operator with the Dirichlet condition in an arbitrary N-dimensional domain with a sufficiently smooth boundary. It should be specially emphasized that our reasoning does not depend on the behavior of the eigenvalues of the operator under consideration.
We considered problem (
4) for two
values: 0 and 1. It is ill-posed for
and well-posed for
. Of course, it would be interesting to indicate, as in works [
27,
28], the boundary value
separating the two types of behavior of the “semi-inverse” problem under consideration? But for this it is necessary to study the behavior of the derivative
, which has not been possible so far.
In this connection, we note that in [
27,
28] a similar question was studied for the subdiffusion equations. It turns out that in all values
the non-local problem is well-posed, and if
then for the existence of a solution to the problem, the functions
and
must be orthogonal to some eigenfunctions of operator
A.