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Article

A Note on Stokes Approximations to Leray Solutions of the Incompressible Navier–Stokes Equations in ℝn

by
Joyce C. Rigelo
1,
Janaína P. Zingano
2 and
Paulo R. Zingano
2,*
1
Master AI, Inc., 10036 Milla Circle, Austin, TX 78748, USA
2
Departamento de Matemática Pura e Aplicada, Universidade Federal do Rio Grande do Sul, Porto Alegre 91509, RS, Brazil
*
Author to whom correspondence should be addressed.
Fluids 2021, 6(10), 340; https://doi.org/10.3390/fluids6100340
Submission received: 29 July 2021 / Revised: 4 September 2021 / Accepted: 24 September 2021 / Published: 27 September 2021

Abstract

:
In the early 1980s it was well established that Leray solutions of the unforced Navier–Stokes equations in R n decay in energy norm for large t. With the works of T. Miyakawa, M. Schonbek and others it is now known that the energy decay rate cannot in general be any faster than t ( n + 2 ) / 4 and is typically much slower. In contrast, we show in this note that, given an arbitrary Leray solution u ( · , t ) , the difference of any two Stokes approximations to the Navier–Stokes flow u ( · , t ) will always decay at least as fast as t ( n + 2 ) / 4 , no matter how slow the decay of u ( · , t ) L 2 ( R n ) might be.
AMS Mathematics Subject Classification:
35Q30; 76D07 (primary); 76D05 (secondary)

Graphical Abstract

1. Introduction

In this note, we derive an interesting new property regarding the large time behavior of Stokes flows approximating Leray solutions (as constructed by J. Leray in [1]) of the incompressible Navier–Stokes equations
u t + u · u + p = ν u , · u ( · , t ) = 0 ,
u ( · , 0 ) = u 0 L σ 2 ( R n ) ,
in dimension 2 n 4 , where ν > 0 is constant and L σ 2 ( R n ) denotes the space of functions u = ( u 1 , , u n ) L 2 ( R n ) with · u = 0 in the distributional sense. Leray solutions to (1),(2) are mappings u ( · , t ) L ( ( 0 , ) , L σ 2 ( R n ) ) L 2 ( ( 0 , ) , H ˙ 1 ( R n ) ) that are weakly continuous in L 2 ( R n ) for all t 0 and satisfy the Equation (1) in R n × ( 0 , ) as distributions. Moreover, they satisfy the energy estimate [1,2,3,4,5,6]
u ( · , t ) L 2 ( R n ) 2 + 2 ν 0 t D u ( · , s ) L 2 ( R n ) 2 d s u 0 L 2 ( R n ) 2
(for all t 0 ), so that, in particular, u ( · , t ) u 0 L 2 ( R n ) 0 as t 0 . For n 3 , their uniqueness and exact regularity properties are still an open problem, but it is known that at the very least they must be smooth for large t : for some t 0 (depending on the solution) we have u C ( R n × ( t , ) ) , and, for each m 0 ,
u ( · , t ) C ( ( t , ) , H m ( R n ) ) ,
as shown by Leray ([1], p. 246). Actually, we have
t 0.000465 ν 5 u 0 L 2 ( R 3 ) 4 ( if n = 3 )
and
t 0.002728 ν 3 u 0 L 2 ( R 4 ) 2 ( if n = 4 )
(see [7], Theorem A), with t = 0 if n = 2 . For more on solution properties, see e.g., [1,2,3,4,5,6,8,9,10,11]. Here, we are particularly interested in the behavior for t 1 : it is now well known that, for every m 0 ,
lim t t m / 2 D m u ( · , t ) L 2 ( R n ) = 0
(see e.g., [11,12,13,14,15,16,17,18,19,20,21]), where D m u ( · , t ) L 2 ( R n ) denotes the norm of u ( · , t ) in H ˙ m ( R n ) , that is,
u ( · , t ) L 2 ( R n ) 2 = u 1 ( · , t ) L 2 ( R n ) 2 + + u n ( · , t ) L 2 ( R n ) 2
if m = 0 and
D m u ( · , t ) L 2 ( R n ) 2 = i = 1 n j 1 = 1 n j m = 1 n R n D j 1 D j m u i ( x , t ) 2 d x
if m 1 , where D j = / x j . For arbitrary initial values u 0 L σ 2 ( R n ) , the result (7) is all that can be obtained, but stronger additional assumptions may give that, for some α > 0 , we actually have
D m u ( · , t ) L 2 ( R n ) = O ( t α m / 2 )
as t , with the generic limitation α ( n + 2 ) / 4 , see [8,22,23]. (For the exceptional case of faster decaying solutions, see [8,22,24,25].) Another point of interest is the large time behavior of the associated linear Stokes flows. In the case of (1), (2) these are given by solutions v ( · , t ) L ( [ t 0 , ) , L σ 2 ( R n ) ) of the linear heat flow problems
v t = ν v , t > t 0 ,
v ( · , t 0 ) = u ( · , t 0 ) ,
for some given t 0 0 (arbitrary). The solution is given by v ( · , t ) = e ν ( t t 0 ) u ( · , t 0 ) , where e ν τ , τ 0 , is the heat semigroup. If α < ( n + 2 ) / 4 , the error D m ( u v ) ( · , t ) L 2 ( R n ) decays faster than the rate (10), so that the Stokes solutions (11), (12) give a useful approximation to the more complex Navier–Stokes flow u ( · , t ) defined by the Equation (1).
Our contribution in this note is to point out that, for arbitrary Navier–Stokes flows (i.e., for arbitrary initial values u 0 L σ 2 ( R n ) ), two distinct Stokes approximations v ( · , t ) , v ˜ ( · , t ) to u ( · , t ) eventually become very closely similar in that we always have
D m [ v ( · , t ) v ˜ ( · , t ) ] L 2 ( R n ) = O ( t ( n + 2 ) / 4 m / 2 )
for large t. The precise statement reads as follows:
Theorem 1. 
Given 2 n 4 and u 0 L σ 2 ( R n ) , let u ( · , t ) L ( ( 0 , ) , L σ 2 ( R n ) ) L 2 ( ( 0 , ) , H ˙ 1 ( R n ) ) be any Leray solution to the Navier–Stokes equations ( 1 ) . Then, for any 0 t 0 < t ˜ 0 , we have
v ( · , t ) v ˜ ( · , t ) L 2 ( R n ) K ν ( n + 2 ) / 4 u ( · , 0 ) L 2 ( R n ) 2 ( t ˜ 0 t 0 ) ( t t ˜ 0 ) ( n + 2 ) / 4
for all t > t ˜ 0 , where v ( · , t ) = e ν ( t t 0 ) u ( · , t 0 ) and v ˜ ( · , t ) = e ν ( t t ˜ 0 ) u ( · , t ˜ 0 ) are the corresponding Stokes flows associated with the time instants t 0 and t ˜ 0 , respectively, and K = ( 4 π ) n / 4 / e . Moreover, for any m 1 , we have
D m [ v ( · , t ) v ˜ ( · , t ) ] L 2 ( R n ) K ( m , n ) ν ( n + 2 ) / 4 m / 2 u 0 L 2 ( R n ) 2 ( t ˜ 0 t 0 ) ( t t ˜ 0 ) ( n + 2 ) / 4 m / 2
for all t > t ˜ 0 , where the constant K ( m , n ) depends only on m , n (and not on t 0 , t ˜ 0 , ν , u 0 or the solution u ( · , t ) ) .
Remark 1. 
In dimension n 3 it is not known whether Leray’s construction gives all (weak) solutions in the class X = { u ( · , t ) L ( ( 0 , ) , L σ 2 ( R n ) ) L 2 ( ( 0 , ) , H ˙ σ 1 ( R n ) ) : ( 3 ) h o l d s   f o r   a l l   t > 0 } , the so-called Leray-Hopf solutions. In case it does not, it would be interesting to know if Theorem A remains valid for all Leray-Hopf solutions as well.
From (14), (15) and standard Sobolev imbeddings we obtain the following corollary regarding supnorm estimates.
Theorem 2. 
Given 2 n 4 and u 0 L σ 2 ( R n ) , let u ( · , t ) L ( ( 0 , ) , L σ 2 ( R n ) ) L 2 ( ( 0 , ) , H ˙ 1 ( R n ) ) be any Leray solution to the Navier–Stokes equations ( 1 ) . Then, for any 0 t 0 < t ˜ 0 , we have
D m [ v ( · , t ) v ˜ ( · , t ) ] L ( R n ) G ( m , n ) ν ( n + 2 ) / 4 m / 2 n / 4 u ( · , 0 ) L 2 ( R n ) 2 ( t ˜ 0 t 0 ) ( t t ˜ 0 ) ( n + 2 ) / 4 m / 2 n / 4
for all t > t ˜ 0 and every m 0 , where v ( · , t ) = e ν ( t t 0 ) u ( · , t 0 ) and v ˜ ( · , t ) = e ν ( t t ˜ 0 ) u ( · , t ˜ 0 ) , and where G ( m , n ) > 0 is some constant that depends only on ( m , n ) .
Remark 2. 
Earlier versions of (14) and (16) for m = 0 were given in [26,27], but, as the results and analysis there were neither as sharp nor as complete as in the present discussion, they have now become obsolete.
The proof of Theorem 1 is developed in the next section, along with some necessary mathematical preliminaries. We end the discussion with some brief considerations in Section 3.

2. Proof of Theorem 1

We first recall Leray’s construction [1], as it will be needed in the proof of Theorem 1 if n 3 . (If n = 2 , the proof can be done directly from (1) by easily adapting the argument below.) For the construction of his solutions, Leray used an ingenious regularization procedure which we now review. Taking (any) G C 0 ( R n ) nonnegative with R n G ( x ) d x = 1 and setting u ¯ 0 , δ ( · ) C ( R n ) by convolving u 0 ( · ) with G δ ( x ) = δ n G ( x / δ ) , δ > 0 , one defines u δ , p δ C ( R n × [ 0 , ) ) as the (unique, globally defined) classical L 2 solutions of the regularized equations
t u δ + u ¯ δ ( · , t ) · u δ + p δ = u δ , · u δ ( · , t ) = 0 ,
u δ ( · , 0 ) = u ¯ 0 , δ : = G δ u 0 m = 1 H m ( R n ) ,
where u ¯ δ ( · , t ) : = G δ u δ ( · , t ) . As shown by Leray, there is some sequence δ 0 for which we have the weak convergence
u δ ( · , t ) u ( · , t ) as δ 0 , t 0 ,
that is, u δ ( · , t ) u ( · , t ) weakly in L 2 ( R n ) , for every t 0 (see [1], p. 237). This gives u ( · , t ) L ( ( 0 , ) , L σ 2 ( R n ) )   L 2 ( ( 0 , ) , H ˙ 1 ( R n ) ) C w 0 ( [ 0 , ) , L 2 ( R n ) ) , with u ( · , t ) continuous in L 2 at t = 0 and solving the Navier–Stokes Equations (1) in distributional sense. Moreover, the energy inequality (3) is satisfied for all t 0 , so that, in particular,
0 D u ( · , t ) L 2 ( R n ) 2 d t 1 2 ν u 0 L 2 ( R n ) 2 .
A similar estimate for the regularized solutions u δ ( · , t ) is also valid, since we have, from (17), (18) above, that
u δ ( · , t ) L 2 ( R n ) 2 + 2 ν 0 t D u δ ( · , s ) L 2 ( R n ) 2 d s u 0 L 2 ( R n ) 2
for all t > 0 (and δ > 0 arbitrary). Another property shown in [1] is that u C ( R n × ( t , ) ) for some t   0 , with D m u ( · , t ) C ( ( t , ) , L 2 ( R n ) ) for each m 1 , cf.(4). The following result considers the Helmholtz projection of u ( · , t ) · u ( · , t ) into L σ 2 ( R n ) , that is, the divergence-free field Q ( · , t ) L σ 2 ( R n ) given by
Q ( · , t ) : = u ( · , t ) · u ( · , t ) p ( · , t ) , a . e . t > 0 .
Of similar interest is the quantity Q δ ( · , t ) : = u ¯ δ ( · , t ) · u δ ( · , t ) p δ ( · , t ) , which will be important in Theorem 4 below.
Theorem 3. 
For almost every s > 0 (and every s t , with t given in ( 4 ) above), one has
e ν ( t s ) Q ( · , s ) L 2 ( R n ) K 1 ( n ) ν n / 4 ( t s ) n / 4 u ( · , s ) L 2 ( R n ) D u ( · , s ) L 2 ( R n )
and
e ν ( t s ) Q ( · , s ) L 2 ( R n ) K 2 ( n ) ν ( n + 2 ) / 4 ( t s ) ( n + 2 ) / 4 u ( · , s ) L 2 ( R n ) 2
for all t > s , where K 1 ( n ) = ( 8 π ) n / 4 and K 2 ( n ) = ( 4 π ) n / 4 / e .
Proof. 
This is shown in [14], p. 236, using the Fourier transform. Here we give an alternative, direct argument in physical space: Let P be the Helmholtz projection. Since, by definition, P is an orthogonal projection in the Hilbert space of vector fields in L 2 , we have P f L 2 f L 2 for any vector field in L 2 . Hence we have e ν ( t s ) Q ( · , s ) L 2 = e ν ( t s ) P [ u ( · , s ) · u ( · , s ) ] L 2 =   P [ e ν ( t s ) ( u ( · , s ) · u ( · , s ) ) ] L 2 e ν ( t s ) ( u ( · , s ) · u ( · , s ) ) L 2 Γ ( t s ) L 2 u ( · , s ) · u ( · , s ) L 1 , where Γ denotes the heat kernel, so that e ν ( t s ) Q ( · , s ) L 2 Γ ( t s ) L 2 u ( · , s ) L 2 u ( · , s ) L 2 . This is (23). Similarly, e ν ( t s ) Q ( · , s ) L 2   j = 1 n Γ ( t s ) D j [ u j ( · , s ) u ( · , s ) ] L 2 = j = 1 n D j Γ ( t s ) [ u j ( · , s ) u ( · , s ) ] L 2   j = 1 n D j Γ ( t s ) L 2 u j ( · , s ) u ( · , s ) L 1   j = 1 n D j Γ ( t s ) L 2 u j ( · , s ) L 2 u ( · , s ) L 2 , which gives (24), as claimed.  □
In a completely similar way, considering the solutions of the regularized Navier–Stokes Equations (17) and (18), one obtains
e ν ( t s ) Q δ ( · , s ) L 2 ( R n ) K 1 ( n ) ν n / 4 ( t s ) n / 4 u δ ( · , s ) L 2 ( R n ) D u δ ( · , s ) L 2 ( R n )
and
e ν ( t s ) Q δ ( · , s ) L 2 ( R n ) K 2 ( n ) ν ( n + 2 ) / 4 ( t s ) ( n + 2 ) / 4 u δ ( · , s ) L 2 ( R n ) 2
for all t > s > 0 , where the constants K 1 ( n ) , K 2 ( n ) are given in Theorem 3 and Q δ ( · , s ) = u ¯ δ ( · , s ) · u δ ( · , s ) p δ ( · , s ) .
Theorem 4.  
Let u ( · , t ) , t > 0 , be any particular Leray solution to ( 1 ) . Given any pair of starting times t ˜ 0 > t 0 0 , one has
v ( · , t ) v ˜ ( · , t ) L 2 ( R n ) K 2 ( n ) ν ( n + 2 ) / 4 u ( · , 0 ) L 2 ( R n ) 2 ( t ˜ 0 t 0 ) ( t t ˜ 0 ) ( n + 2 ) / 4
for all t > t ˜ 0 , where v ( · , t ) = e ν ( t t 0 ) u ( · , t 0 ) , v ˜ ( · , t ) = e ν ( t t ˜ 0 ) u ( · , t ˜ 0 ) are the corresponding Stokes flows associated with t 0 , t ˜ 0 , respectively, and K 2 ( n ) is given in Theorem 3 above, that is, K 2 ( n ) = ( 4 π ) n / 4 / e .
Proof. 
The following argument combines the Leray’s construction reviewed above with the usual strategy of handling nonlinear terms as a Duhamel-type correction. We begin by writing v ( · , t ) = e ν ( t t 0 ) [ u ( · , t 0 ) u δ ( · , t 0 ) ] + e ν ( t t 0 ) u δ ( · , t 0 ) , t > t 0 , with u δ ( · , t ) given in (17), (18), δ > 0 . Because
u δ ( · , t 0 ) = e ν t 0 u ¯ 0 , δ + 0 t 0 e ν ( t 0 s ) Q δ ( · , s ) d s ,
where u ¯ 0 , δ = G δ u 0 and Q δ ( · , s ) = u ¯ δ ( · , s ) · u δ ( · , s ) p δ ( · , s ) , we get
v ( · , t ) = e ν ( t t 0 ) [ u ( · , t 0 ) u δ ( · , t 0 ) ] + e ν t u ¯ 0 , δ + 0 t 0 e ν ( t s ) Q δ ( · , s ) d s ,
for t > t 0 . A similar expression holds for v ˜ ( · , t ) as well, giving
v ˜ ( · , t ) v ( · , t ) = e ν ( t t ˜ 0 ) [ u ( · , t ˜ 0 ) u δ ( · , t ˜ 0 ) ] e ν ( t t 0 ) [ u ( · , t 0 ) u δ ( · , t 0 ) ] + t 0 t ˜ 0 e ν ( t s ) Q δ ( · , s ) d s
for t > t ˜ 0 . Therefore, given any K R n compact, we get, for each t > t ˜ 0 , δ > 0 :
v ˜ ( · , t ) v ( · , t ) L 2 ( K ) J δ ( t ) + t 0 t ˜ 0 e ν ( t s ) Q δ ( · , s ) L 2 ( K ) d s J δ ( t ) + K 2 ( n ) ν ( n + 2 ) / 4 t 0 t ˜ 0 ( t s ) ( n + 2 ) / 4 u δ ( · , s ) L 2 ( R n ) 2 d s J δ ( t ) + K 2 ( n ) ν ( n + 2 ) / 4 u 0 L 2 ( R n ) 2 ( t ˜ 0 t 0 ) ( t t ˜ 0 ) ( n + 2 ) / 4
by (21) and (26), where K 2 ( n ) = ( 4 π ) n / 4 / e and
J δ ( t ) = e ν ( t t ˜ 0 ) [ u ( · , t ˜ 0 ) u δ ( · , t ˜ 0 ) ] L 2 ( K ) + e ν ( t t 0 ) [ u ( · , t 0 ) u δ ( · , t 0 ) ] L 2 ( K ) .
Taking δ = δ 0 according to (19), we get J δ ( t ) 0 , since, by Lebesgue’s Dominated Convergence Theorem and (19), we have, for any σ , τ > 0 : e ν τ [ u ( · , σ ) u δ ( · , σ ) ] L 2 ( K ) 0 as δ 0 . This gives (27), as claimed.  □
In particular, we obtained (14). This, in turn, gives (15) using well known estimates of the heat operator, or, alternatively, by applying to (14) the direct method introduced in [28] to derive upper estimates in the spaces H ˙ m ( R n ) . This completes the proof of Theorem 1.

3. Concluding Remarks

The main results of this note (namely, Theorems 1 and 2) show the somewhat surprising fact that the difference of any two Stokes approximations to an arbitrarily given Leray solution of the Navier–Stokes system (1), (2) will always decay as t at least as fast as the fastest decaying Leray flows in general, no matter how slow the particular Leray solution at hand might be decaying. This is an interesting theoretical finding about Stokes flows in R n , which are important approximations for Navier–Stokes flows. On the more practical side, it sheds some additional light on the quality of these approximations. For example, it shows that M. Wiegner’s estimates ([20], Theorem (c), p. 305) on the large time size of the error u ( · , t ) e ν t u 0 L 2 ( R n ) apply more generally to the error of any Stokes approximation of u ( · , t ) , and so forth.

Author Contributions

Conceptualization, P.R.Z.; investigation, J.C.R., J.P.Z. and P.R.Z.; writing—original draft preparation, P.R.Z.; writing—review and editing, J.C.R. and J.P.Z. All authors have read and agreed to the published version of the manuscript.

Funding

This research received no external funding.

Conflicts of Interest

The authors declare no conflict of interest.

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Rigelo, J.C.; Zingano, J.P.; Zingano, P.R. A Note on Stokes Approximations to Leray Solutions of the Incompressible Navier–Stokes Equations in ℝn. Fluids 2021, 6, 340. https://doi.org/10.3390/fluids6100340

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Rigelo JC, Zingano JP, Zingano PR. A Note on Stokes Approximations to Leray Solutions of the Incompressible Navier–Stokes Equations in ℝn. Fluids. 2021; 6(10):340. https://doi.org/10.3390/fluids6100340

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Rigelo, Joyce C., Janaína P. Zingano, and Paulo R. Zingano. 2021. "A Note on Stokes Approximations to Leray Solutions of the Incompressible Navier–Stokes Equations in ℝn" Fluids 6, no. 10: 340. https://doi.org/10.3390/fluids6100340

APA Style

Rigelo, J. C., Zingano, J. P., & Zingano, P. R. (2021). A Note on Stokes Approximations to Leray Solutions of the Incompressible Navier–Stokes Equations in ℝn. Fluids, 6(10), 340. https://doi.org/10.3390/fluids6100340

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