Existence of planar non-symmetric stationary flows
with large flux in an exterior disk
Abstract. This paper is concerned with the two-dimensional stationary Navier-Stokes system in the domain exterior to the unit disk. The existence of solutions with critical decay is established around some explicit flows with large flux. The solutions are obtained for non-symmetric external forces, and moreover, are unique in a certain class.
1 Introduction
We consider the two-dimensional stationary Navier-Stokes system in the exterior disk :
(NS) |
The unknown functions and are respectively the velocity field and the pressure field. The function is a given external force in . We assume that both and are constants. The vector refers to . The system (NS) describes the motion of a viscous incompressible fluid around the disk rotating at angular velocity and whose surface subjects to a normal suction velocity .
The existence and uniqueness theories for the problem (NS) are generally open. As for the existence, there are two fundamental difficulties. The first one is lack of certain embeddings. Let be smooth and compactly supported in for brevity. Under smallness conditions, adapting the proof by Leray [15] or relying on Fijita [2], we can actually find weak solutions of (NS) having a finite Dirichlet integral, called -solutions. Nevertheless, the bound itself cannot verify the condition at spatial infinity in (NS) in two-dimensional unbounded domains; see Korobkov, Pileckas and Russo [10, 11, 12] for recent progress on this topic. The other one is the logarithmic growth in the Green function of the exterior Stokes system, which is the source of the famous Stokes paradox; see [1, 3, 4, 14] for descriptions. The uniqueness of solutions will be discussed in Remark 1.2 (iii) below.
These issues illustrate a delicate aspect concerning the zero condition at infinity in (NS). Most existing results treating (NS) assume both smallness and symmetry on the data. The latter is useful for making quantities decay in space by cancellation. The reader is referred to Galdi [3, 4], Russo [20], Yamazaki [22, 23, 24] and Pileckas and Russo [19] for the existence of solutions, and to Nakatsuka [18] and [24] for the uniqueness. Relevant numerical simulations are carried out in Guillod and Wittwer [7]. We note that, if another condition were imposed at infinity, the situation would be quite different. Indeed, the recent work by Korobkov and Ren [13] proves the uniqueness in the class of -solutions for plane exterior Navier-Stokes flows converging to a small but non-zero constant vector field at infinity.
In this paper, we examine the problem (NS) from a different angle. Note that, when the external force is trivial, there is an explicit solution given by
(1.1) |
which is invariant under the scaling of the Navier-Stokes equations. A (non-trivial) solution in this class is called scale-critical and it represents the balance between the nonlinear and linear parts of the equations. Given this nature, it is expected that the Navier-Stokes flows around a scale-critical flow differ quantitatively from those around the trivial flow. In fact, Hillairet and Wittwer [9] consider the Navier-Stokes problem in an exterior disk by perturbating the system around . A crucial observation is that the decay of solutions to the corresponding linearized system is improved when is sufficiently large, more precisely, when . This is possible because of the structure of the equation for vorticities. Then, based on iteration to the nonlinear problem with subcritialized nonlinearity, they show the existence of solutions in the form of when . These solutions are driven by inhomogeneous boundary data, on which no symmetries are imposed thanks to the mechanism of the proof.
The result in [9] can be read as the scale-critical flow producing a stabilizing effect in view of spatial decay. In this context, we here consider such an effect of and address the existence of solutions to the problem (NS). Briefly, we will see that the stabilization is effective for any if . As an application, we obtain the Navier-Stokes flows for non-symmetric external forces based on the perturbation. We also describe the asymptotics near spatial infinity in terms of the decay rate of external forces.
Let us introduce some notations to state the main result. For , we define
(1.2) |
which is a Banach space under the norm . Taking advantage of symmetry, we introduce the polar coordinates on as
For given vector field on and , we set
and denote by the projection on the Fourier mode :
(1.3) |
Now the result is stated as follows.
Theorem 1.1
Remark 1.2
-
(i)
As far as the author knows, Theorem 1.1 is the first result obtaining the plane exterior Navier-Stokes flows zero at spatial infinity, non-symmetric and unique in a certain class. In [9] dealing with the case , the uniqueness of solutions seems not to be provided. More to the point, the proof should not be easy since the existence of solutions in [9] is verified by the intermediate value theorem. The inconvenience is closely related to the structure of the zero mode of the linearized system (1.8) below.
- (ii)
- (iii)
-
(iv)
The stability of the flows in Theorem 1.1 is an open problem. The global -stability of is proved by Guillod [6] and the local -stability of by Maekawa [16, 17] without any symmetries on initial perturbations. However, these results essentially rely on the smallness of the coefficients and, therefore, cannot be adapted to the flows in Theorem 1.1, even if the Hardy inequality applies to .
The ingredients of the proof of Theorem 1.1 are the following.
(I) Perturbation. We will construct the solution of (NS) in the form of
(1.6) |
The pair is understood as the perturbation from in response to the external force . Inserting the ansatz (1.6) into (NS) and using the relation
(1.7) |
as well as , we see that solves the perturbed system
() |
Our next task is to prove the existence of solutions to the problem ().
(II) Linear analysis. The linearized system of () around is written as
() |
Since () is invariant under the action of in (1.3), one can study it in each Fourier mode.
As mentioned in Remark 1.2 (ii), the presence of the parameter stabilizes the decay of solutions of (). A sharp contrast with [9] is that this effect is exerted on the zero mode of the velocity . Indeed, while follows from the second and third lines in (), satisfies the ordinary differential equation
(1.8) |
which is independent of . Then, since the Green functions of equation are and , the solution decays subcritically if the data decays fast enough.
The stabilization from displays also in the non-zero modes. However, to prove Theorem 1.1, we need to make precise the relationship between the decay of solutions and that of external forces. For this purpose, we derive the representation formula for the -mode of the velocity using the streamfunction-vorticity variant of the system in [9] and the Biot-Savart law in [16, 17, 5, 8]. When verifying the formula, we essentially use the decay of the vorticity subcritically improved by .
This paper is organized as follows. In Section 2, we collect preliminary results from vector calculus in the polar coordinates. In Section 3, we study the linear problem () decomposed into the Fourier modes. In Section 4, we prove Theorem 1.1.
Notations. We denote by the constant and by the constant depending on . Both of these may vary from line to line. We use the function spaces
and which is the completion of in the -norm. If there is no confusion, we use the same notation to denote the quantities concerning scalar-, vector- or tensor-valued functions. For example, denotes to the inner product on , or .
2 Preliminaries
This section collects useful facts about the vector calculus in the exterior disk .
2.1 Operators in the polar coordinates
The following formulas will be used:
(2.1) |
and
2.2 Fourier series
2.3 Biot-Savart law
For a given , we consider the Poisson equation
The solution is called the streamfunction. Let with and set and . In the polar coordinates, solves the ordinary differential equation
(2.4) |
The decaying solution of (2.4) is given by
(2.5) |
Then the following vector field is called the Biot-Savart law:
(2.6) |
It is straightforward to see that
(2.7) |
If additionally with , one can check that .
We state two propositions related to the Biot-Savart law. The first one is implicitly contained in [16, Proposition 2.6 and Lemma 3.1] and the second one has the same content as [16, Corollary 2.7]. However, we provide slightly more concise proofs for completeness.
Proposition 2.1
Let and . Set . Then, if and for some , we have and in (2.5).
Proof.
Proposition 2.2
Let and . Then, if in the sense of distributions, we have for some .
Proof.
We only need to show that for all . Then the assertion follows from the Helmholtz decomposition in . Note that, for and , by integration by parts we have
Let and set . By Proposition 2.1, is represented by the Biot-Savart law as . Then the definition of in (2.6) implies that the streamfunction is smooth and compactly supported in . Thus the condition that in the sense of distributions leads to
The left-hand side can be rewritten as . Consequently, we have for all . This completes the proof. ∎
3 Linearized problem
In this section, we study the linearized problem
() |
Let . Applying in (1.3) to (), we see that and satisfy
(3.1) | |||
(3.2) |
the divergence-free and the no-slip boundary conditions
(3.3) |
and the condition at infinity
(3.4) |
3.1 Zero mode
Proposition 3.1
Proof.
Let in (LABEL:eq.polar.vr)–(3.4). The first condition in (3.3) leads to that with some constant . Then the second condition leads to , which yields that .
Thus we focus on the angular part . From (LABEL:eq.polar.vtheta) and (3.3), we find that
(3.7) |
The linearly independent solutions of the homogeneous equation of (3.7) are
and their Wronskian is . Hence the solution of (3.7) in is given by
Then we have
By the assumption with and the computations
one can check that satisfies (3.5) and that belongs to and satisfies (3.6). The pressure is obtained by (LABEL:eq.polar.vr). Clearly, is the unique solution of (LABEL:eq.polar.vr)–(3.4). The proof is complete. ∎
3.2 Non-zero modes
By Proposition 3.1, the zero mode of the solution of () decays as fast as desired, if the external force does correspondingly. On the other hand, for the non-zero mode, the decay rate is governed by the Biot-Savart law (2.6). Taking this into account, we will build a solution of the non-zero mode of () satisfying, for ,
(3.8) |
under suitable assumptions on the external force .
For , we define
(3.9) |
This definition of coincides with the one in [9] if . We compute
(3.10) |
Let us set for simplicity. Then we have
(3.11) |
with independent of , and .
Proposition 3.2
Proof.
The proof is divided into two parts. First we show the existence of solutions using the representation formula. Second we verify the uniqueness by Proposition 2.1.
(Existence) Initially, let us assume that . Operating and to the first line of (), we see that satisfies the ordinary differential equation
(3.16) |
By the transformation
we find that solves
(3.17) |
The linearly independent solutions of the homogeneous equation of (3.17) are
and their Wronskian is . Hence the decaying solution of (3.17) is given by
(3.18) |
where the constant is to be determined later and is defined by
(3.19) |
Here we performed integration by parts using . Going back to the equation (3.16), we see that the decaying solution is given by
(3.20) |
Let us determine in (3.18). From , we have . We choose so that in (2.5) is zero, namely,
(3.21) |
Then the Biot-Savart law in (2.6) is written as
(3.22) |
Let us show that, for in (3.22), there is a pressure such that the pair is a solution of (). From and implied by (3.11), we see that in (3.20) is smooth and satisfies for any . This, combined with the choice of in (3.21) and Lemma A.1, ensures that is smooth and satisfies and for any . Accordingly, we can apply Proposition 2.2 because of and
Now, let in (3.19)–(3.22). We will prove the estimates (3.12)–(3.15). For in (3.20) and in (3.21), using Lemma A.1, we have
where (3.11) is used in the second inequality and is independent of , , and . Hence we see from (3.20) that satisfies (3.12). For in (3.22), using (2.1) and (3.12), we have
Hence we see from Lemma A.1 (2) that satisfies (3.13)–(3.15).
It remains to verify that given by (3.22) is a solution of () for general . The condition follows from (3.13)–(3.15) and the choice of in (3.21). By Lemma A.2 and direct computation, one has
(3.23) |
To show that satisfies the weak formulation of (), we take such that . Let denote the smooth solution given by (3.22) replacing by . Also, let be an associated pressure. Then, using (3.23) and linearity of the equations, we have, for any ,
Here we performed integration by parts in the first and last equalities. Consequently, we see that is a weak solution of (). Then, by regarding as the external force, one can prove the local regularity and the existence of an associated pressure by standard theory for the Stokes system; see Sohr [21, Chapter III] for example. This completes the existence part of the proof.
(Uniqueness) Assume that is a solution of () with . By the elliptic regularity, is smooth in . Since satisfies the homogeneous equation of (3.16), due to the summability , we have with some constant . Then Proposition 2.1 implies that and . The latter condition is rewritten as
Thus we have and hence . Then the uniqueness follows from . This completes the uniqueness part of the proof. Hence we conclude. ∎
4 Nonlinear problem
In this section we prove Theorem 1.1 by showing the unique solvability of the system
() |
Let us collect two lemmas needed in the proof. For , we define the Banach space
Lemma 4.1
Proof.
This follows from Propositions 3.1 and 3.2 and an estimate obtained from (3.11):
Indeed, we see from the propositions that there is a weak solution of () satisfying (4.1). Then, as in the proof of Proposition 3.2, we have the local regularity and an associate pressure . The uniqueness of follows from that of for . This completes the proof. ∎
Lemma 4.2
For and , we have
Proof.
The identity
and the Young inequality for sequences imply
This completes the proof. ∎
Proof of Theorem 1.1: Firstly we show the unique solvability of () under smallness conditions on . We define the Banach space
equipped with the norm , and consider the closed subset
For any , by Lemma 4.1, there is a unique solution to the problem
satisfying
(4.2) |
where Lemma 4.2 is applied in the second inequality. Hence, by denoting by , we see that defines a linear map from to itself.
Let us show that is a contraction on if both and are sufficiently small depending on . Then the unique existence of solutions of () follows from the Banach fixed-point theorem. For any , by (4.2), we have
(4.3) |
On the other hand, for any , by Lemma 4.2 again, we have
(4.4) |
Therefore, fixing and so that
(4.5) |
we see that is contractive. Then the Banach fixed-point theorem yields that there is a unique element such that . Thus we obtain a solution of () with unique in .
Appendix A Integral estimates
We summarize the integral estimates used in the proof of Proposition 3.2. The proof only uses elementary calculations and thus we will just state the results. Recall that
Lemma A.1
For , we have the following.
-
(1)
Let . For ,
-
(2)
Let .
-
(i)
If , for ,
-
(ii)
If , for ,
and for ,
-
(iii)
For ,
-
(i)
Lemma A.2
Under the assumption in Proposition 3.2,
Acknowledgements
The author is partially supported by JSPS KAKENHI Grant Number JP 20K14345.
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M. Higaki
Department of Mathematics, Graduate School of Science, Kobe University, 1-1 Rokkodai, Nada-ku, Kobe 657-8501, Japan.
Email: [email protected]