On the existence and structures of almost axisymmetric solutions to -D Navier-Stokes equations
Abstract.
In this paper, we consider -D Navier-Stokes equations with almost axisymmetric initial data, which means that by writing in the cylindrical coordinates, then and are small in some sense (recall axisymmetric means these three quantities vanish). Then with additional smallness assumption on , we prove the global existence of a unique strong solution , and this solution keeps close to some axisymmetric vector field. We also establish some refined estimates for the integral average in variable for .
Moreover, as and here depend on , it is natural to expand them into Fourier series in variable. And we shall consider one special form of , with some small parameter to measure its swirl part and oscillating part. We study the asymptotic expansion of the corresponding solution, and the influences between different profiles in the asymptotic expansion. In particular, we give some special symmetric structures that will persist for all time. These phenomena reflect some features of the nonlinear terms in Navier-Stokes equations.
Keywords: Navier-Stokes equations, axisymmetric, asymptotic expansions.
1. Introduction
1.1. The general setting
The 3-D incompressible Navier-Stokes equations (N-S) reads:
| (1.1) |
where stands for the velocity field and the scalar pressure of the fluid. This system describes the motion of viscous incompressible fluid. And it is worth mentioning that except the case for initial data with some special structure, it is still a big open problem whether or not the system (1.1) has a unique global solution with large initial data.
Now let us write in the cylindrical coordinates as
| (1.2) |
where denotes the cylindrical coordinates in so that , and
Notice that in the cylindrical coordinates, there holds
| (1.3) |
Then we can reformulate (1.1) in the cylindrical coordinates as
| (1.4) |
where denotes the material derivative.
For the special case when all the components in (1.2) do not depend on , precisely
then this will be called axisymmetric. It is a celebrated result that for the more special axisymmetric without swirl case, which means , Ladyzhenskaya [6] and independently Ukhovskii and Yudovich [11] proved the existence of weak solutions along with the uniqueness and regularities of such solutions. And later Nečas et al. [8] gave a simpler proof. Their proofs deeply rely on the fact that satisfies
| (1.5) |
so that any norm of is conserved.
However, for the arbitrary axisymmetric initial data whose swirl part is non-trivial, we do not have the structure as that in (1.5) any more. To the best of our knowledge, so far we can only establish the global existence of strong solutions when is sufficiently small, and this smallness needs to depend on other components of or , as the strategy is to view this case as a small perturbation of the no swirl case. There are numerous works concerning this situation, here we only list [1, 2, 3, 4, 7, 9, 12, 13] for example.
Here we do not limit us in considering axisymmetric solutions, but this geometric symmetry still plays a crucial role. Let us also introduce satisfying the following axisymmetric N-S:
| (1.6) |
where is the integral average of in variable, precisely
| (1.7) |
By definition, there holds for any smooth function . Then one has
This guarantees the initial data in (1.6) is indeed compatible with the divergence-free condition.
1.2. Main results.
There are three main results in this paper. The first one concerns the global well-posedness of (1.4) with initial data that are close to some axisymmetric vector fields in some sense. To state this precisely, let us introduce the following norms:
| (1.8) |
where is a part of the whole gradient given by (1.3).
Theorem 1.1.
Remark 1.1.
(i) We mention that is axisymmetric when vanishes, and it is well-known that in this situation, the corresponding solution persists axial symmetry for all time.
In view of this, the smallness condition (1.10) actually tells us that is close to some axisymmetric vector field. That is what we mean “almost axisymmetric”. Moreover, it is reasonable to expect that this solution keeps close to some axisymmetric vector field for all time.
To verify this feature quantitatively, we mention that one natural way to axisymmetrize a solution to N-S, is to axisymmetrize the initial data, and then solve N-S with this axisymmetrized initial data, in this way we get . Then in view of the smallness condition (1.10), interpolating between the two estimates in (1.11) gives
which means that is indeed close to the axisymmetric vector field .
(ii) Furthermore, (1.12) shows that after taking average in , will become much smaller. Hence there must be some cancellations in this process, precisely the positive part of almost balance its negative part. This provides us more details on how approaches . One can see this more clearly by expanding into Fourier series in variable, see Remark 1.3 below.
With Theorem 1.1 at hand, now let us turn to study the asymptotic expansion of solutions to N-S with almost axisymmetric initial data. As we know, a regular enough function can be expanded into Fourier series in variable. And by virtue of the assumptions of Theorem 1.1, here we only consider initial data in the following special form 11 1 In this part, we use and to denote the profiles of the initial data, while the subscript is used to denote the -th Fourier coefficients, so that there would be no confusion.:
| (1.13) |
where is some small positive constant to be determined later, and the profiles satisfy
| (1.14) |
and
| (1.15) |
| (1.16) |
It is not difficult to verify that the constraints (1.15), (1.16) meet the divergence-free condition . And thanks to Parseval’s identity, (1.14) guarantees that and . Precisely, we have
and the other norms can be derived similarly. In particular, this implies that the smallness conditions in Theorem 1.1 can be satisfied provided is sufficiently small, and this smallness needs to rely on the norms of profiles appearing in (1.14).
Then Theorem 1.1 guarantees the existence of a unique global strong solution to N-S with initial data (1.13). As we know, a strong solution to N-S would become analytic for any positive time, thus can be expanded into Fourier series in variable in the following form:
| (1.17) |
where can be or , and the profiles do not rely on .
Unlike the Euclidean coordinates, and are not constant vectors. As a result, the convergence of in Sobolev spaces is in general not equivalent to the convergence of each component of . In view of this, it is optimal to verify the validity of the expansion (1.17) in sense. And our first result concerning the asymptotic expansion states as follows:
Theorem 1.2.
Remark 1.2.
The following result concerns the odevity in this asymptotic expansion. We mention that this persistence of odevity deeply reflects some nonlinear structures of N-S.
Theorem 1.3.
Remark 1.3.
One can see from the proof in Section 5 that, here actually satisfies axisymmetric N-S with initial data . Thus corresponds to the in Theorem 1.1, and we can obtain from the expression (1.20) that
and
which indicates that is in general much smaller than , just as what we have mentioned at the end of Remark 1.1. Here we can see that the reason is the cancellations of the oscillating terms, which is the main terms in .
Let us end this section with some notations which will be used throughout this paper.
Notations. We shall use to denote an universal constant which may change from line to line. The notation means , and means both and hold. For a Banach space B, we shall use the shorthand for . We use (resp. ) to denote inhomogeneous (resp. homogeneous) based Sobolev spaces.
2. Preliminary
2.1. Poincaré-type inequality
Lemma 2.1.
For any and , the operator defined in (1.7) satisfies
| (2.1) |
Proof.
Let us first consider the case when . By applying Hölder’s inequality, we get
To prove the second inequality of (2.1), we first write
As a result, we can obtain
Clearly this gives the second inequality of (2.1) for .
As for the case when , we have the following formulas:
and
which hold for any . This completes the proof of this lemma. ∎
2.2. Properties for axisymmetric functions.
Let us first recall the well-known Biot-Savart law, which asserts that any divergence-free velocity field can be uniquely determined by its vorticity . Moreover, for any and any , there holds
| (2.2) |
For the special case when the velocity field is axisymmetric without swirl, namely
then we can use to represent . Moreover, there holds:
Lemma 2.2.
If in addition , then we have the following estimates:
| (2.3) |
| (2.4) |
Proof.
Lemma 2.3.
Let be divergence-free, and the corresponding vorticity . Then we have
| (2.6) | ||||
2.3. A stability result for N-S
In this subsection, we shall give a stability result for N-S. There are numerous works concerning this problem, here we only list two classical results [5, 10].
Proposition 2.1.
Let be a global strong solution to N-S with initial data , and there exists some positive constants and such that
| (2.8) |
Then there exists some small positive constant such that whenever satisfies
| (2.9) |
then N-S with as initial data also has a global strong solution . Moreover, this solution satisfies for that
| (2.10) |
and
| (2.11) |
Proof.
Step 1. The proof of (2.10). Let us denote , then we can find
| (2.12) |
for some properly chosen . By taking inner product of (2.12) with , we obtain
After subtracting on both sides, then applying Gronwall’s inequality leads to
| (2.13) |
While by taking inner product of (2.12) with , we have
Then by using Young’s inequality to the last term, we get
| (2.14) |
On the other hand, by the local well-posedness result, the following set is not empty:
Let us take . If , then for any , we can use the estimate (2.13) and the smallness condition (2.9) with sufficiently small to deduce
By substituting this into (2.14), and then using Gronwall’s inequality, we achieve
which contradicts to the definition of . Thus there must be , and we have
| (2.15) |
Step 2. The proof of (2.11). Let us denote and , which satisfy
| (2.16) |
By taking inner product of (2.16) wit , we get
| (2.17) |
The terms on the right-hand side can be handled as follows:
and by using the Biot-Savart law that
and by using integration by parts together with the divergence-free condition that
Now by substituting the above three estimates into (2.18), and using the relation that
we get
Then Gronwall’s inequality together with the bounds (2.8) and (2.10) leads to
| (2.18) |
Now interpolating between (2.15) and (2.18) gives
which is exactly the desired estimate (2.11). This completes the proof of this proposition. ∎
3. The proof of Theorem 1.1
The purpose of this section is to prove Theorem 1.1 by using perturbation method.
3.1. Global solvability of (1.6)
Let us first introduce the velocity field satisfying the following axisymmetric without swirl N-S:
| (3.1) |
Proposition 3.1.
Proof.
The first estimate (3.2) is nothing but the energy equality and the fact that
Next, the Biot-Savart law tells us that we can use to represent . Hence we can reformulate the System (3.1) as
| (3.4) |
Then it is not difficult to verify that satisfies
| (3.5) |
For a strong solution of N-S, the decay property at infinity implies , while the smoothness implies . As a result, we have
In view of this, the energy estimate of in (3.5) gives
| (3.6) |
By using (2.2) and Lemma 2.1, we have
where . Substituting this into (3.6) gives
| (3.7) |
Proposition 3.2.
Proof.
By using Lemma 2.1 and the fact that , we have
and
These together with the bounds (3.2), (3.3) and the smallness condition (1.9), we get that
where we used the fact that
So that the condition (2.9) in Proposition 2.1 is fulfilled. Thus (1.6) has a unique global strong solution such that
which together with (3.3) leads to the desired estimate (3.11).
The estimate (3.10) follows from the Basic energy equality of Navier-Stokes equations. Thus, we complete the proof of the proposition. ∎
3.2. The proof of Theorem 1.1
The goal of this subsection is to prove Theorem 1.1.
The proof of Theorem 1.1.
We divide the proof into two steps.
Step 1. Global solvability of (1.4). The strategy is still to use Proposition 2.1. To do this, we need to analyse the difference between and , which reads as follows:
and
Then by using Lemma 2.1 and the notation we can obtain
| (3.12) |
| (3.13) |
In view of the estimates (3.10)-(3.13) and the smallness condition (1.10), the condition (2.9) of Propostion 2.1 holds for and . Then by using Proposition 2.1 again, (1.4) has a unique global strong solution in , satisfying
| (3.14) | ||||
In particular, the above estimates together with interpolation inequality and the smallness condition (1.10) implies
which means that is indeed close to an axisymmetric solution.
Step 2. Error estimates of
Step 2.1. Equations for . We first get, by applying to (1.4) that
| (3.15) |
where we have used the fact that for any regular enough function , there holds
Then by denoting , and in view of (1.6) and (3.15), we deduce
| (3.16) |
where with
We mention that here indeed vanishes, but we still write them to derive a symmetric form. In this way, we can handle these terms by using the following key observation: for any functions and any axisymmetric functions , there holds
| (3.17) |
On the other hand, noting that are axisymmetric, we have
As a result, there holds
| (3.18) |
For notation simplification, let us introduce . Obviously there holds
Then by using (3.17), we have
Similar formulas hold for the other terms in . And we can write
| (3.19) | ||||
On the other hand, by using (3.18), we have
| (3.21) |
Step 2.2. -estimate for . Taking inner product of (3.16) with gives rise to
| (3.22) |
Thanks to the formula (3.19) and Lemma 2.1, we obtain
which along with Young’s inequality implies
| (3.23) |
While by virtue of (3.20), (3.21), Lemma 2.1 and Lemma 2.3, we get
Then by using Young’s inequality, we deduce
| (3.24) |
Now by substituting (3.23) and (3.24) into (3.22), we obtain
Then by using Gronwall’s inequality and the fact that , we achieve
Recall that , by using (3.10), (3.11) and (3.14), we obtain
| (3.25) |
This together with the smallness assumption (1.10) gives
which is exactly the first inequality of (1.12).
Step 2.3. -estimate for . Taking inner product of (3.16) with gives rise to
| (3.26) |
In view of the formulas (3.19)-(3.21), we can use Lemmas 2.1 and 2.3 to get
which together with Young’s inequality leads to
By substituting this into (3.26), we infer
Then by applying Gronwall’s inequality and using the fact that , we deduce
Notice that , then we can use (3.10), (3.11) and (3.14) to obtain
| (3.27) |
This together with the smallness assumption (1.10) gives
which is exactly the second inequality of (1.12).
Till now, we have completed the proof of Theorem 1.1. ∎
4. The proof of Theorem 1.2
As we have mentioned in Subsection 1.2, for any initial data given by (1.13), Theorem 1.1 guarantees the existence of some positive constant such that for any , (1.1) has a unique global solution .
By virtue of the classical result that any strong solution to N-S will become analytic at positive time, hence we can expand this solution into Fourier series in variable as
| (4.1) |
Correspondingly, we can expand the pressure into
| (4.2) |
In the following, we shall give the explicit formulas for the profiles in the expansion (4.1), and verify the validity of this expansion in sense. For notation simplification, we shall use to denote the order term in the expansion of , i.e.
| (4.3) |
and does not rely on .
4.1. The order terms
We make the following Ansatz : , where and satisfy the following axisymmetric without swirl N-S:
| (4.4) |
To verify this ansatz, we first deduce from Proposition 3.1 that
| (4.5) |
Here and in all that follows, denotes some positive constant depending only on the norms of the profiles of appearing in (1.14), and may be different in each appearance.
On the other hand, in view of the expression (1.13) for initial data, we have
By using Parseval’s identities, there holds
| (4.6) |
Then for sufficiently small , by virtue of (4.5), (4.6) and Proposition 2.1, we obtain
| (4.7) |
Notice that the system (4.4) does not rely on , and thus its solution also does not rely on . This together with the estimate (4.7) guarantees the validity of our Ansatz , namely is indeed the order term in the expansion of .
In particular, we have shown that vanishes, and for every , the -th Fourier coefficient does not contain order terms, just the same as the initial data (1.13).
4.2. Derivation of the order terms in the Euclidean coordinates
Let us temporarily go back to the Euclidean coordinates, and consider as a whole part.
We make the following Ansatz : is a solution to the linearization of the perturbed Navier-Stokes system around , precisely
| (4.8) |
To verify this ansatz, we first get, by taking inner product of (4.8) with that
Subtracting on both sides, and then applying Gronwall’s inequality gives
| (4.9) |
While following similar derivation as (2.18), we deduce
| (4.10) |
On the other hand, let us consider , which satisfies
| (4.11) |
where can be obtained by taking divergence operator to the first equation in (4.11).
In the following, we shall derive and estimate for . Notice that if there is no external force term in (4.11), then this type of system has already been studied in Proposition 2.1. So here we only focus on the estimate for this external force term.
Firstly, we have
and in view of the bound (4.9), there holds
Then a similar procedure as the proof of Proposition 2.1 leads to
| (4.12) |
Similarly, we have
and
In view of the bounds (4.9) and (4.10), there holds
Then a similar procedure as the proof of Proposition 2.1 leads to
| (4.13) |
Now in view of the estimates (4.12) and (4.13), together with the interpolation inequality , we achieve
| (4.14) |
In view of the estimate (4.14) for the remainder , and the fact that determined by (4.8) does not rely on , we have verified our Ansatz .
Remark 4.1.
Exactly along the same line, we can prove by induction that for any , is a solution to the following linearized system:
And the remainder term satisfies
4.3. Verification of
Noticing that is axisymmetric without swirl, it is not difficult to deduce from (4.8) that satisfies
| (4.15) |
where , and the divergence-free condition here follows from
By taking inner product of (4.15) with , we get
| (4.16) |
where we used the fact that and then the following equality
5. The proof of Theorem 1.3
As the initial data (1.19) considered here is a special case of (1.13), Theorem 1.1 guarantees the existence of a unique global solution for sufficiently small . And this solution can be expanded as (1.18). Hence the aim in the following is to show that and remain even in , while keeps odd in for all time, namely
5.1. Verification of
5.2. Verification of
In view of (5.1), we can write
| (5.2) |
and the corresponding pressure
And from the proof of Subsection 4.2, we know that satisfies (4.8).
Then it is crucial to notice that is axisymmetric without swirl, which makes the couplings between each component of in not so strong. In fact, by rewriting (4.8) according to the basis , it is not difficult to find that we can decompose and into two parts: and respectively, where
and
such that and satisfy the following self-contained system:
| (5.3) |
while and satisfy the following self-contained system:
| (5.4) |
Then by taking inner product of (5.4) with , we obtain
| (5.5) | ||||
It is worth mentioning that, not the same as the most cases in doing estimates in PDE, the constant in this inequality is very important. Precisely, we have
On the other hand, by using Sobolev’s embedding theorem and Young’s inequality, we get
where in the last step we have used the fact that , so that
By substituting the above estimates into (5.5), we deduce
Then by applying Gronwall’s inequality, and using the fact that
which is guaranteed by (4.5), and initially , we obtain that
In another word, we can further reduce the expansion for in (5.2) to be
| (5.6) |
where and are determined by (5.3).
5.3. Verification of , for any
We shall prove this result by the induction method. Assume that for any and any ,
i.e., has the following form
| (5.7) |
then our aim is to show that can also be written as this form, i.e.
Indeed, due to Remark 4.1, we know that in the Euclidean coordinates, satisfies
| (5.8) |
This system has zero-valued initial data. However, due to the external force term , the solution in general does not vanish.
Noticing that has the form (5.7) for , we can get
| (5.9) |
In particular, we can see that and is even in , while is odd in . As a result, this external force does not appear in the equations for for . Thus the equations for are exactly the same as that for (see (5.4)) stated as follows:
Then the same procedure as what we have done at the end of Subsection 5.2 shows that for , indeed vanishes for all time, i.e.
Let us turn to study the -th Fourier coefficients . In view of the expression (5.9), and the following identities
and the fact that is axisymmetric without swirl, we can obtain
| (5.10) |
and
| (5.11) |
where are the external force terms given by
In particular, this reflects the fact that if two profiles have same frequency, then their product would contribute to the average of in variable.
Taking inner product of (5.10) with , it is easy to get that
Therefore, can also be written in the following form:
This completes the proof of Theorem 1.3 by induction.
Acknowledgments. Y. Liu is supported by NSF of China under grant 12101053, and the Fundamental Research Funds for the Central Universities under Grant 310421118. L. Xu is supported by NSF of China under grant 11671383 and 12171019.
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