Articles

Time-periodic Poiseuille-type solution with minimally regular flow rate.

Kristina Kaulakyte
Institute of Applied Mathematics, Faculty of Mathematics and Informatics, Lituania
Nikolajus Kozulinas
Institute of Applied Mathematics, Faculty of Mathematics and Informatics, Lituania
Konstantin Pileckas
Institute of Applied Mathematics, Faculty of Mathematics and Informatics, Lituania

Time-periodic Poiseuille-type solution with minimally regular flow rate.

Nonlinear Analysis: Modelling and Control, vol. 26, núm. 5, pp. 947-968, 2021

Vilniaus Universitetas

Recepción: 23 Diciembre 2020

Revisado: 06 Julio 2021

Publicación: 01 Septiembre 2021

Abstract: The nonstationary Navier–Stokes equations are studied in the infinite cylinder II=. under the additional condition of the prescribed time-periodic flow rate (flux) F(t). It is assumed that the flow rate F belongs to the space , only. The time-periodic Poiseuille solution has the form , where is a solution of an inverse problem for the time-periodic heat equation with a specific over-determination condition. The existence and uniqueness of a solution to this problem is proved.

Keywords: Navier–Stokes equations, cylindrical domain, time-periodic Poiseuille-type solution, inverse problem, minimal regularity.

1 Introduction

Mathematical modelling is very useful in many practical applications. For example, in medicine, it can be helpful by choosing the optimal strategy of medical treatment. In such modelling, very important issues are multiscale mathematical models of the blood circulation in a network of vessels. The full 3D computations are nowadays very time consuming and may be applied only for small parts of the blood circulation system. Therefore, a new trend is related to the creation of hybrid dimension models that combine the 1D reduction in the regular zones (mostly in straight vessels) with 3D zooms in small zones of singular behaviour. This method of asymptotic partial decomposition of a do- main was proposed by Panasenko (see [12]) and developed in [1316]. It mathematically justifies a size of zoomed areas and prescribes asymptotically exact junction conditions. These hybrid-dimension models require significantly smaller computational resources.

The 1D Poiseuille-type flows in straight vessels play a very important role in hybrid- dimension models.

The steady-state Poiseuille flow in an infinite straight pipe of constant cross-section σ was invented by Jean Louis Poiseuille in 1841 (see [2,11,24]). The Poiseuille flow is described by the fact that the associated velocity field has only one nonzero component directed along the xn-axis of Π, which depends only on , and the pressure function is linear. The Poiseuille-type solutions can be also defined in the nonstationary case (see [7, 1721, 23, 26]). Moreover, in [14] the behaviour of the nonstationary Poiseuille flow was studied in a thin cylinder (with the cross-section of radius ε), and the asymptotics of it as was found.

In the time-periodic case, such flow is usually called Womersley’s flow (see [28]). The time-periodic Poiseuille-type solutions were studied in [3] and [8]. The time periodic solutions for the full Navier–Stokes problem were considered in many papers (see, e.g., [46]). Notice that the time-periodic case is very important because of applications to hemodynamics.

In mentioned above papers the Poiseuille-type solutions were studied in the case when data is sufficiently regular. However, in real applications, one usually does not have data defined by smooth functions, and it is important to study the case of minimal regularity of data. The nonstationary Poiseuille-type solution with a prescribed initial condition and given flow rate F(t) belonging to was studied in [22], where a new class of weak solutions was introduced, and the unique existence of the solution in such class was proved. The goal of the present paper is to extend the result obtained in [22] to the case of time-periodic Poiseuille-type solutions.

Let us consider the time-periodic Navier–Stokes problem describing the motion of a viscous incompressible fluid in the infinite cylinder II:


where u is the fluid velocity, p is the pressure function, and is the constant kinematic viscosity of the fluid.

We look for the solution u of (1) in Π satisfying the additional condition of prescribed flow rate (flux) F(t):


where

The solution of problem (1) has the following expression:


with an arbitrary function p0(t). Putting (2) into (1), we obtain the following problem on the cross-section σ


where and q(t) are unknown functions, is the Laplace operator with respect to .

The Poiseuille flow can be uniquely determined either prescribing the pressure drop q(t) or the flow rate F(t). In the first case the problem is reduced to the standard time- periodic problem for the heat equation for unknown velocity with time- periodic forcing q(t). Problems of such type are well studied (see, e.g., [9]). However, in the real word applications the pressure is unknown, and only the flow rate (flux) of the fluid is given. Therefore, it is necessary to prescribe the additional condition


In this case the solution of problem (3), (4) is a pair of functions , and one has to solve for and q(t) more complicated inverse parabolic problem: for given F(t), to find a pair of functions solving problem (3) with satisfying the flux condition (4).

Thus, in the second case the relation between q(t) and F(t) depends on the solution of the inverse problem (in the stationary case the flux F and the pressure gradient q are proportional, and the problem remains very simple). The solvability of the time-periodic problem with the assumption that the flux F(t) is from the Sobolev space was proved by Beirão da Veiga [3], and in [8] an elementary relationship between the pressure drop q(t) and the flux F(t) was found. However, in applications and numerical computations, the data usually is not regular. Therefore, in this paper, we study problem (3), (4) assuming only that .

Problem (3), (4) can be reduced to the case when all involved functions have zero mean values. Let us denote by the mean value of a function H. Let be a solution of the following problem on σ (the stationary Poiseuille solution corresponding to the flux ):

The solution of (5) can be represented in the form , where


and


Let us represent the solution in the form


Then, obviously, , and is the solution of the problem


where . So, without loss of generality, we assume , that is .

Below, we deal with a weak solution of problem (3), (4). The reasoning about the reduction to the case of functions with zero mean values remains valid for weak solutions as well, and we will study only this case.

The rest of the paper is organized in the following way. In Section 2, function spaces are defined and the main result is formulated. In Section 3 the Galerkin approximations of the solution are constructed, and in Section 4 a priori estimates for these approximations are proved. In Section 5 the main result of the paper, that is the existence and the uniqueness of the solution, is proved.

2 Notation and formulation of main result

2.1 Function spaces

Below, we will use the following notation. If G is the domain in means, as usual, the set of all infinitely differentiable functions in G, and is the subset of functions from with compact supports in G. We use the usual (see [1,9]) notation for Lebesgue and Sobolev spaces: , and . The norm of an element u in the function space V is denoted by is the Bochner space of functions u such that for almost all , and the norm


is finite

Let us consider the set of smooth periodic functions defined on the interval . Let be a Lebesgue space on the interval . We extend the functions from to the whole line R by putting for any t. To emphasize that functions are periodically extended to R, we used notation . Let . Clearle is a closure of in

- norm, and it is a proper subspace of . Let be the closure of the set in -norm. Since function f from coincides with a continuous function on a set whose complement is of measure zero, we may assume that . Let be dual of .

For any function , denote by its primitive:


Clearly, .

If , then . Moreover,


and is a period function:


Thus, . Note that functions defined by (9) with various t0 differ from each other by a constant.

Note that the L2-limit of a sequence ) is not necessary a primitive of some function from . We will prove that an element possesses a primitive in the distributional sense.

Lemma 1.Any functional can be represented in the form


with the uniquely determined .

Proof. Obviously, the functional given by formula (10) obeys the estimate


and hence, .

Let us take an arbitrary functional and show that it can be represented in the form (10). Consider the operator due to periodicity, . Since for any , the equality holds with


we have , and the operator ∂ is an isomorphism from to , where the bounded operator is given by (11).

For , define the functional . Clearly


Hence, there exists a uniquely defined such that


Thus


and is represented in the form (10).

Remark 1. Note that if the functional h can be represented in the form = with and arbitrary , then H(t)= . Therefore, also in the case of a general functional h, for the distributional primitive H, we use the notation .

2.2 Formulation of main result

Definition of a weak solution

Let . By a weak solution of problem (8) we understand a pair such that satisfies the flux condition


and the pair satisfies the integral identity


for any test function such that .

For a regular solution , taking into account that , identity (13) can be easily obtained multiplying equation (8)1 by η, integrating over σ and over the interval and integrating by parts with respect to and t. On the other hand, by uniqueness of such weak solution (see Theorem 1 below) it follows that for , the solution coincides with the regular one, that is . Thus, the proposed definition is an extension of the concept of weak solutions.

Theorem 1.Let . Then problem (8) admits a unique weak solution (V, s). Then there holds the estimate


where the constant c depends only on σ.

Remark 2. Since and all primitives of the function differ from each other by a function independent of t, the integral identity (13) remains valid for any primitive function SV, and we can assume, for example, that SV is taken to be zero at the point

Theorem 1 will be proved applying some version of Galerkin approximations (see Sections 3 and 4). Notice that in order to get estimates of approximate solutions , we have used primitive functions defined over the integrals with specially chosen points and . Thus, estimate (14) is valid only for the primitive function SV obtained as a limit of the sequence

3 Construction of Galerkin approximations

Let and be eigenfunctions and eigenvalues of the Laplace operator:


Note that and . The eigenfunctions are orthogonal in , and we assume that are normalized in . Then


Moreover, is a basis in and .

We look for an approximate solution of problem (8) in the form


The coefficients and the function are obtained by solving the following linear problems


which, in virtue of the orthonormality of functions , are equivalent to ordinary differential equations for the functions :


where . Note that .

The solution of problem (17) has the form


where


It is easy to see that .

Substituting expression (18) into (15), we obtain


Now the flux condition yields


Thus, for the function , we derived Fredholm integral equation of the first kind:


It is well known (see, e.g., [10, 25]) that such equations, in general, are ill-posed in L2 setting. In order to regularize equation (19), we consider the following Fredholm integral equation of the second kind:


where α later will tend to 0, i.e., instead of problem (16), (19), we study the regularized problem


where


Lemma 2.Let . Then equation (20) admits a unique solution .

Proof. First, we show that equation (20)is well defined in the space .Obviously, if F is periodic and is the solution of (20), then also is a periodic function. Assume that mean value . Then


Since


the second term in (22) is equal to and from (22) it follows that


and thus, .

From this it follows that the mean value also vanishes: .

It is well known that Fredholm integral equations of the second kind satisfy the Fredholm alternative (e.g., [27]). So, it is enough to prove the uniqueness of the solution to (20). Let . By construction


and the homogeneous equation (20) gives


Multiplying (21) by , summing by k from 1 to N and integrating over the interval yield


Integrating by parts with respect to t and taking into account the time-periodicity of , we obtain


Thus, for a.a. , and the lemma is proved.

4 A priori estimates of Galerkin approximations

Let the pair be the solution of problem (21) and be the solution of problem (6). Consider the integral . Since the mean value , we have


Therefore, there exists such that . By periodicity we also have

Let define the notation , define the notationSince the mean value of F nabishes, we hace . Moreover,

Lemma 3. The following estimate


holds with a constant c independent of α and N.

Proof. Define. Multiplying (21) by summing the obtained relation from k = 1 to k = N and integrating them over the interval , we obtain


Using the relation


and (21), we derive


Therefore, (24) can be written as


Then



Calculating similarly two integrals J1 and J2 on the left-hand side of (25), we derive that


Hence, relation (25) takes the form


Now multiply (21) by , sum from k = 1 till k = N and integrate over the interval :


Evaluating each of the three integrals in (27) and having in mind that mean values of participating functions are zero, we obtain


From (26) and (28) it follows that


and


Let us estimate the integral . Let be a solution of problem (6). Remind that the flux of U0 is nonzero, (see (7)). Since is a basis in , U0 can be expressed as a Fourier series in :


Let us multiply relations (21) by ak and sum them over k. This gives


On the other hand, multiplying (6) by and integrating by parts in σ, we obtain


Substituting (32) into (31) yields


i.e.,


Integrating (33) with respect to t from τ to , we obtain


Here we have used the choice of the point t, that is


and hence,


From (34) it follows that


Substituting (35) into (29) yields


and choosing ε sufficiently small, we obtain


Estimates (36) and (35) give


Finally, from (30) and (37) it follows that


The constants in (36)–(38) are independent of α and N.

5 Convergence of Galerkin approximations. Proof of Theorem 1

5.1 Proof of existence

The constructed approximate solutions satisfy equalities (21). Multiplying these relations by arbitrary functions such that , summing over k from k = 1 to , integrating with respect to t and then integrating by parts, we obtain the integral identity


for test functions η having the form .

Recall that obey a priori estimate (23) with a constant c independent of α and N.

Since all functions in (23) are -periodic, inequality (23) is equivalent to


Let us fix N and choose a subsequences and such that l converges weakly in to some converges weakly in to SV(N)5, while converges weakly in to s(N). The last convergence means that


where , and , and is a primitive of s(N) in the distributional sense.

Obviously, for the limit functions V(N) and Ss(N), estimate (40) remains valid with a constant c independent of N. In (39), taking and passing to the limit as , we get


Let us show that satisfy the flux condition


Integrating equation (21) for from t to 2π yields


Obviously, the sequence is bounded in . So we may assume, without loss of generality, that is weakly convergent to in . Then the sequence of primitives for all , and hence, . From (43) we have


Therefore,


and differentiating this equality with respect to t, we get (42).

Now we choose a subsequence such that converges weakly in to some converges weakly in ; to SV and converges weakly in to s. In (41) ,passing to the limit over the subsequence as yields


Exactly as above, we can prove that satisfies the flux condition (12). However, the integral identity (44) is proved, up to now, only for test functions η, which can be represented as the sums: with such that . After we have passed to the limit in (41) as , the subscript M in these sums can be arbitrary large natural number. Such sums are dense in the space. This can be proved exactly in the same way as it is done in the book [9] for the case of an initial boundary value problem. Thus, they also are dense in the subspace , and therefore, (41) remains valid for all This proves that satisfies the integral identity (13), and thus, it is a weak solution of problem (8). Estimate (14) for follows from estimate (40) for the approximate solutions.

5.2 Proof of uniqueness

Assume that . Since , we take


Obviously, . Putting this η into identity (13), we obtain


Since


by Fubini’s theorem and the time-periodicity of the function we have




Therefore, from (45) it follows that


Then, and hence, . Integrating over σ, we get


Thus, , and since, we conclude that, that is for a.a. and t.

This implies . From identity (13) it follows that


In (46), we take , where is arbitrary, and is the solution of problem (6). Recall that . Then (46) takes the form


Thus, Ss(t)=const. Since ,i.e. the mean value of Ss(t) is equal to zero, we get that Ss(t) = 0. Therefore, the functional s=0.

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