In this paper, temporal decay estimates for weak solutions to the three dimensional generalized Navier–Stokes equations are established firstly. With these estimates at disposal, algebraic time decay for higher order Sobolev norms of small initial data solutions are obtained. The decay rates are optimal in the sense that they coincide with ones of the corresponding generalized heat equation.
The incompressible Navier–Stokes equations can be written as
where , , , the vector field denotes the velocity of the fluid, is the pressure of the fluid and the positive ν is the viscosity coefficient.
Whether or not weak solutions of (1.1) decay to zero in as time tends to infinity was posed by Leray in his pioneering paper [11,12]. Kato [8] gave the first affirmative answer for strong solutions with small data to system (1.1). Algebraic decay rates for weak solutions to system (1.1) were first obtained by Schonbek [18], in which she proved that there exists a Leray–Hopf weak solution of (1.1) in three space dimension with arbitrary data in which satisfies
where the constant C only depends on the and norms of the initial data. Later the method in [18] was extended by Schonbek [19], Kajikiya and Miyakawa [7] and Wiegner [25]. It was shown that the rate of decay for Leray–Hopf solutions of (1.1) in three space dimension with large data in , is the same as for solutions of the heat equation, that is
where the constant C only depends on the and norms of the initial data. It is referred to [2,3,5,10,15,24] for more studies.
In this paper, we consider the large-time behavior of solutions to the Cauchy problem for the incompressible generalized Navier–Stokes equations in three space dimension
Here is defined through Fourier transform (see [21])
It is known that if is a solution to the three-dimensional generalized Navier–Stokes equations, then for any , the scaling solution also solves the generalized Navier–Stokes equations. The corresponding energy is
It follows that as when . In this sense, we say that the three-dimensional generalized Navier–Stokes equations is supercritical if , critical for and subcritical with . So far, it has been proved that when , the three-dimensional generalized Navier–Stokes equations has a global and unique regular solution (see [13] or [26]). However, when , the three-dimensional fractional Navier–Stokes system is still supercritical and their global well-posedness theories remain open. Meanwhile, the Navier–Stokes equations with fractional dissipation have been studied from a mathematical viewpoint and some interesting results have been obtained. Tao [22] showed the global regularity for a logarithmically supercritical hyper-dissipative Navier–Stokes system. In [9], it was shown that the Hausdorff dimension of the space singular set at time of first blow up for smooth solution to the three-dimensional fractional Navier–Stokes equations is at most as .
In this paper, we will focus on the asymptotic behavior of solution of (1.2) in the supercritical case, that is, when . Motivated by [18], [19] and [20], we will show that the weak solutions to (1.2) which are to be constructed in the end of the paper, subject to large initial data, decay in at a uniform algebraic rate. The decay estimates for the higher order Sobolev norms whose global in time existence is guaranteed for sufficiently small initial data [27] will also be established. Our main results can be stated as follows.
Assume. Then for divergence-free vector-field with, the Cauchy problem (1.2) admits a weak solution such thatwhere the constant C depends on α, the andnorms of the initial data.
Here and in the following the -norm of a function f is denoted by and the - norm by . We will also set for simplicity.
The rate of decay in (1.3) is the same as that of the solutions to the generalized heat equation with the same initial data (see Lemma 3.1 in [17]).
Assumeand divergence-free vector-fieldwith p satisfying one of the conditions:Then, for (the set of positive integers) there exists a such that the small global-in-time solution satisfiesfor all, where the constant C depends on m, α and.
In Theorem 1.2, the restrictions on p are based on Theorem 1.1 which requires that the lower bound of p is . However, in Theorem 1.2, for technical reason, we have a little bit more restrictions on the upper bound of p. Precisely, in the case of , p is chosen to satisfy . The point in the proof is to show in (3.14). In the case of , p is chosen to satisfy . The point in the proof is to show in (3.11). While in the case , the restriction on p is the same as in Theorem 1.1.
Similar results have been established respectively in [4] for the classical Navier–Stokes equations and in [20] for the Hall-magnetohydrodynamic equations.
Our results extend the corresponding ones in [18,19] and [20] to the supercritical cases and the Fourier splitting method due to M. Schonbek with appropriate modification will be applied. In comparison with [18–20], new ingredients in our proof are as follows. Firstly, in the proof of Theorems 1.1 and 1.2, we choose as a test function with γ being a constant to be determined. In fact, γ has to be adjusted according to the change of α in order to get the optimal decay (see (2.13)). This is different from the one in [18,19] in which and (the dimension of the space) are fixed. Secondly, in the proof of Theorem 1.2, we firstly establish decay estimates for s-order Sobolev norms in Proposition 3.3
However, the decay rates are not optimal. Then, we establish a unified inequality for
which is different from Lemma 3.2. of [19], in which
with
Thirdly, based on (1.4), we will use an iterative scheme. By induction for m, we get the optimal decay estimates for high order Sobolev norms.
The paper unfolds as follows: Section 2 is devoted to the proof of Theorem 1.1 whereas Section 3 deals with the proof of Theorem 1.2. The existence of weak solutions is postponed in the final section of the paper.
Proof of Theorem 1.1
In this section, we will prove Theorem 1.1. The following are two key lemmas.
Let u be a smooth solution to the Cauchy problem (1.2) with initial data,. Then there exists a constant depending only onsuch that
Taking the Fourier transform of the first equation of (1.2) yields
where
Multiplying (2.2) by the integrating factor gives
Integrating in time from 0 to t, we obtain
Hence
To complete the proof we need to establish an estimate for . Taking the divergence operator on the first equation of (1.2) yields
Note that the Fourier transform is a bounded map from into . It follows that
Similarly, for the convective term, we have by using the divergence free condition
Combining the above two estimates, we have
By inserting (2.5) into (2.4) and using the boundedness of the norm of the solution, we obtain
□
Letwith, then whereand the constant C depends on γ, α and thenorm of.
Let be the Fourier transform. By Riesz theorem, if , we have and
where . Therefore, we get by the Hölder inequality
Combining (2.8) and (2.9) yields
Since and the volume of is , we thus get
□
In the rest of this section, we first present a formal argument by the Fourier-splitting method (see [18]).
By taking -inner product on bothsides of the first equation of (1.2) with u, we get
Applying the Plancherel theorem to the above equation yields
Let
where γ is a constant to be determined. Then
Multiplying (2.11) by the integrating factor yields
Using (2.10), we get . Hence
To complete the proof we will use Lemmas 2.1 and 2.2 to estimate the right-hand side of (2.12). Indeed, by plugging (2.1) into the right-hand side of (2.12) and using (2.6) we have
Integrating the last inequality in time from 0 to t yields
Case 1: Assume . Since , we have . Hence, by choosing , we have
Case 2: Assume . If , one has . Hence, by choosing we have
If , one has . Hence, by choosing we have
Now we will improve the rate in (2.14). To this end, motivated by [19], we will use the preliminary decay rate of (2.14) to show that
and then a bootstrap argument will lead to the higher decay rate in (2.14). Replacing H by its upper bound in (2.5) and using the decay rate in (2.14), on one hand, for , for and we have
On the other hand, for we have
Hence by (2.3), (2.16) and (2.17)
This combined with (2.12) yields
Integrating the last inequality in time yields
By choosing γ suitably large, we have
Case 3: Assume and . Similar to the proof of (2.12), (2.13) and (2.14), we have
By using (2.18), we have
Thanks to (2.3), we have . By plugging the last inequality into (2.12) again, we obtain
Integrating the last inequality in time and choosing γ suitably yield
Similar to the proof of (2.12), (2.13) and (2.15), we know that in the case of and
Therefore, combining the three cases yields the formal proof of Theorem 1.1.
We apply the a prior estimates to the approximate solutions constructed in the Appendix part to make the above proof rigorous. Let us recall that is a solution of the approximate equation
where is the spectral cutoff defined by
and P is the Leray projector over divergence-free vector-fields.
It is shown that the converge strongly in to a weak solution of the generalized three-dimensional Navier–Stokes equation (1.2) in the Appendix part. Hence the decay of will imply the decay of the weak solution of (1.2). □
Proof of Theorem 1.2
In this section, we start with the following small data global regularity result (Theorem 4.3 in [27]).
Ifwithandfor some suitable constant, then the IVP (1.2) has a global and unique solutionsatisfyingand
Here with , and is a Besov space, which can be seen in [16] for more details.
By the fact that coincides with , it follows from Theorem 3.1 that the Cauchy problem (1.2) has a global and unique solution in the usual Sobolev space with if we choose
We can also obtain that
In fact, by Theorem 4.3 in [27], one has
By the hypothesis on initial condition , we can suppose that is the first time such that
Then for any , we have
This combined with (3.2) implies that is a non-increasing function of t for . Then
which contradicts with . Therefore,
Using (3.2) again yields
for some . In particular, choosing , , we can get (3.1).
Let,with. Then, for any and for anywe havewhere C depends only on.
Since , we have
The result of Lemma 2.1 leads to the desired (3.3). □
The following are decay estimates for high order Sobolev norms.
Assume. Let ,andwith. Then, there exists a such that for anythe global-in-time solution established in Theorem3.1satisfyingwhere C depends on α and.
We adopt to the Fourier-splitting method again. The Fourier transform of (3.1) can be written as
In a similar fashion as the proof of Theorem 1.1, we have
As a consequence, by using the result of Lemma 3.2, there exists a such that for any , we have
Arguing as for proving (1.3), we get that for any
Thus, the proof is finished. □
To prove Theorem 1.2, we need the following product and commutator estimates.
Letand. Then whereand,.
The proof is referred to Lemma 3.1 in [6] and the details are omitted here.
For any , applying on both sides of the first equation of (1.2), multiplying the resulting equation by and integrating by part, we obtain
By the Hölder inequality and (3.5),
Inserting the Gagliardo–Nirenberg inequality
into (3.8) and using the Young inequality, we get
The Gagliardo–Nirenberg inequality yields
In view of Theorem 1.1 and Proposition 3.3, we have for any
Plugging (3.10) into (3.9), one has for
When , we can also establish the same estimate as (3.11). Indeed, by divergence free condition, (3.7) can be written as
As a result, using the Hölder inequality and commutator estimate (3.5)–(3.6), we have
Combining the estimates of Theorem 1.1 and Proposition 3.3 and using the Gagliardo–Nirenberg inequality yield for any and
Hence, it is now clear that for ,
Let
Then,
Inserting (3.15) with suitable l into (3.11), we get
To complete the proof of Theorem 1.2 in the case of , we use the induction for m. Assume
then we have after inserting the above assumption into (3.16)
Integrating (3.17) in time from to t yields
Hence, by choosing suitable l we can get
We now consider the case when . Since , we have for any Therefore, we get by Remark 3.1
By choosing in (3.8) and using the Young inequality, we get
This combined with
yields
In the same way as proving (3.10), we can obtain
Since ,
Therefore, there exists some T such that for all , the right-hand side of (3.20) can be bounded by . We thus get
This together with (3.19) yield for any
Inserting (3.15) with suitable l into the last inequality yields that
Adopting to similar procedure as above, we can also obtain (3.18). Theorem 1.2 is proved. □
Footnotes
Acknowledgement
The authors express their gratitude to the anonymous referee for his/her valuable suggestions to improve the presentations of the paper.
Existence of weak solutions
In this section we show that the generalized Navier–Stokes equations with have a global weak solution corresponding to any prescribed initial data.
We start with a definition of weak solutions for (1.2) with initial data . Let be arbitrarily fixed.
The following theorem states that there exists global-in-time weak solutions of (1.2).
We will use the Friedrichs method to prove Theorem A.1. Before proof, let us recall the following Picard theorem [14] and Bernstein inequality [1].
References
1.
H.Bahouri, J.-Y.Chemin and R.Danchin, Fourier Analysis and Nonlinear Partial Differential Equations, Grundlehren Math. Wiss., Vol. 343, Springer, 2011.
2.
W.Borchers and T.Miyakawa, decay for the Navier–Stokes flows in unbounded domains with application to exterior stationary flows, Arch. Rat. Mech. Anal.118 (1992), 273–295.
3.
A.Carpio, Large-time behavior in incompressible Navier–Stokes equations, SIAM J. Math. Anal.27 (1996), 449–475.
4.
D.Chae and M.Schonbek, On the temporal decay for the Hall-magnetohydrodynamic equations, J. Differential Equations255 (2013), 3971–3982.
5.
J.Heywood, The Navier–Stokes equations: On the existence, regularity and decay of solutions, Indiana University Math. J.29 (1980), 639–681.
6.
N.Ju, Existence and uniqueness of the solution to the dissipative 2D quasi-geostrophic equations in the Sobolev space, Commun. Math. Phys.251 (2004), 365–376.
7.
R.Kajikiya and T.Miyakawa, On decay of weak solutions of the Navier–Stokes equations in , Math. Z.192 (1986), 135–148.
8.
T.Kato, Strong -solutions of the Navier–Stokes equation in , with applications to weak solutions, Math. Z.187 (1984), 471–480.
9.
N.H.Katz and N.Pavlović, A cheap Caffarelli–Kohn–Nirenberg inequality for the Navier–Stokes equation with hyper-dissipation, Geom. Funct. Anal.12 (2002), 355–379.
10.
H.Kozono and T.Ogawa, Two dimensional Navier–Stokes flow in unbounded domains, Math. Ann.297 (1993), 1–31.
11.
J.Leray, Étude de diverses équations integrales non lineaires et de quelques problémes que pose l’hydrodynamique, J. Math. Pure Appl.9 (1933), 1–82.
12.
J.Leray, Sur le mouvement d’un liquide visqueux emplissant l’espace, Acta Math.63 (1934), 193–248.
13.
J.-L.Lions, Quelques méthodes de résolution des problèmes aux limites non linéaires, Dunod, Gauthier-Villars, Paris, 1969.
14.
A.J.Majda and A.L.Bertozzi, Vorticity and Incompressible Flow, Cambridge University Press, 2001.
15.
P.Maremonti, Some results on the asymptotic behavior of Hopf weak solutions to the Navier–Stokes equations in unbounded domains, Math. Z.210 (1992), 1–22.
16.
C.Miao, J.Wu and Z.Zhang, Littlewood–Paley Theory and Applications to Fluid Dynamics Equations, Monographs on Modern Pure Mathematics, Vol. 142, Science Press, Beijing, 2012.
17.
C.Miao, B.Yuan and B.Zhang, Well-posedness of the Cauchy problem for the fractional power dissipative equations, Nonlinear Analysis68 (2008), 461–484.
18.
M.Schonbek, decay for weak solutions of the Navier–Stokes equations, Arch. Rat. Mech. Anal.88 (1985), 209–222.
19.
M.Schonbek, Large time behavior of solutions to the Navier–Stokes equations, Comm. Partial Differential Equations11 (1986), 733–763.
20.
M.Schonbek and M.Wiegner, On the decay of high-order norms of the solutions of Navier–Stokes equations, Proc. Roy. Soc. Edinburgh Sect. A126 (1996), 677–685.
21.
E.Stein, Singular Integrals and Differentiability Properties of Functions, Princeton University Press, Princeton, USA, 1970.
22.
T.Tao, Global regularity for a logarithmically supercritical hyperdissipative Navier–Stokes equation, Analysis and PDE3 (2009), 361–366.