Uniform estimates on the velocity in Rayleigh–Bénard convection
Manuel NúñezCitation: Journal of Mathematical Physics46, 033102 (2005); doi: 10.1063/1.1855400
View online: https://doi.org/10.1063/1.1855400
View Table of Contents: http://aip.scitation.org/toc/jmp/46/3
Uniform estimates on the velocity in Rayleigh–Bénard
convection
Manuel Núñeza兲
Departamento de Análisis Matemático, Universidad de Valladolid, 47005 Valladolid, Spain 共Received 17 March 2004; accepted 23 November 2004; published online 8 February 2005兲
The kinetic energy of a fluid located between two plates at different temperatures is easily bounded by classical inequalities. However, experiments and numerical simulations indicate that when the convection is turbulent, the volume of the do-mains in which the speed is large, is rather small. This could imply that the maxi-mum of the speed, in contrast with its quadratic mean, does not admit an a priori upper bound. It is proved that, provided the pressure remains bounded, a uniform estimate for the speed maximum does indeed exist, and that it depends on the maxima of certain ratios between temperature, pressure, and velocity. © 2005 American Institute of Physics. 关DOI: 10.1063/1.1855400兴
I. INTRODUCTION
The study of thermal convection of a fluid powered by the difference of temperature between two plates, known as Rayleigh–Bénard convection, has been an extensively studied subject for a long time. Computer modeling and physical experiments have produced an enormous wealth of information: for recent reviews, see Refs. 1 and 2. Perhaps unavoidably, there has not been a comparable volume of rigorous studies, if we except the study of the stability of different patterns 共Ref. 3, pp. 23–95兲. It is well known that when the difference of temperature between the top and bottom plates exceeds a certain amount, usually measured in terms of the Rayleigh constant R, convection sets in. Near the onset, convection cells occur; with increasing R, and depending also on the ratio between viscosity and thermal diffusivity共the Prandtl number兲more complex patterns appear and bifurcations to chaotic states may occur. The same may be said of the temperature: for a colorful illustration, starting with regular rolls, see e.g., Ref. 4.
The standard mathematical model of Reyleigh–Bénard convection is given by the Boussinesq approximation to the equations of motion, which we repeat here for convenience. We will consider a d-dimensional domain U of the form⍀⫻关0 , h兴, and as usual we will assume that the tempera-ture is constant at the lower and upper lids, T = T0at⍀⫻兵0其 and T = Th⬍T0 at⍀⫻兵h其. The rest
of the boundary conditions will be discussed later. Let us denote by v the fluid velocity, T the temperature,the kinematic viscosity,the thermal diffusivity, andthe kinetic pressure. Then the nondimensionalized Boussinesq approximation共see, e.g., Ref. 5兲to the equations of motion is
v
t =⌬v − v · ⵜv − ⵜ+共T − Th兲ed, 共1兲
T
t =⌬T − v · ⵜT, 共2兲
a兲Electronic mail: mnjmhd@am.uva.es
46, 033102-1
ⵜ· v = 0. 共3兲
eddenotes the vertical unit vector. Traditionally the differenceof the actual temperature with the
linear one between the lids共associated to pure heat conduction兲is used,
= T − T0+xd,
共4兲 =T0− Th
h .
is also changed to+xd2/ 2 −共T0− Th兲xd共which we denote again by兲. The final system is
v
t =⌬v − v · ⵜv − ⵜ+ed, 共5兲
t =⌬− v · ⵜ+vd, 共6兲
ⵜ· v = 0. 共7兲
Boundary conditions are usually the following ones: the upper and lower plates are taken either rigid, where we assume a no-slip condition and v vanishes there, or stress free, in which casevd= 0
and the vertical derivatives of the remaining components of the velocity are also zero,dvi= 0. The
lateral walls are assumed rigid and conducting, so that v and vanish there.
Let us state some classical results, since T satisfies 共2兲, which is a scalar parabolic equation without terms in T, it also satisfies the maximum and minimum principles共see, e.g., Ref. 6兲. That means that T lies always between T0and Th, which makes excellent physical sense. Thereforeis
uniformly bounded. By multiplying 共5兲by v, integrating in U and making use of the boundary conditions, one gets
1
2 d
dt
冕
Uv2dV +
冕
U兩ⵜv兩2dV =
冕
U
vddV艋储储⬁Vol共U兲2储vd储2, 共8兲
where Vol共U兲denotes the volume共area in dimension two兲of U. Since with our boundary condi-tions a Poincaré inequality holds, there exists a positive constant c such that
c
冕
U
兩v2兩dV艋
冕
U
兩ⵜv兩2dV. Thus, by standard inequalities,
1
2 d
dt储v储2
2
+ c 2 储v储2
2艋 1
22c2储储⬁
2
Vol共U兲, 共9兲
which implies that储v储2 is bounded for all time.
As in many other turbulent situations, modeling of the chaotic phase of convection shows a tendency of the flow to concentrate the velocity in regions of small volume.7Thus the bounded-ness of the kinetic energy does not provide an a priori bound upon the maximum of the speed. It is true that physically it seems obvious that this maximum cannot grow without limit, but never-theless it is interesting to obtain rigorous estimates in terms of the main magnitudes of the
problem. Our only hypothesis will be the boundedness of the pressure 关or, to be specific, of /共1 +v兲兴.
II. ANALYSIS OF THE MOMENTS OF THE VELOCITY
Let us start with the momentum equation
v
t =⌬v − v · ⵜv − ⵜ+ed, 共10兲 and for p = 1 , 2…, let
Fp=
冕
U
vpdV, 共11兲
wherev=兩v兩 represents the modulus of v. Fpis a function of time. Sincev2= v · v,
v2p
t = 2pv
2p−2v ·v
t.
Therefore
1
2pF ˙
2p=
冕
Uv2p−2v ·v
tdV,
and taking into account the momentum equation,
1
2pF ˙
2p= −
冕
Uv2p−2共v · ⵜv兲· v dV +
冕
Uv2p−2v ·⌬v dV +
冕
U共v2p−2v
d−v2p−2v · ⵜ兲dV.
共12兲
In the first place,
冕
Uv2p−2共v · ⵜv兲· v dV =
冕
U
1
2pv · ⵜv
2pdV = 0. 共13兲
As for the dissipative term,
冕
Uv2p−2v ·⌬v dV =
冕
U
兺
j共ⵜ·共vjv2p−2ⵜvj兲− ⵜvj· ⵜ共v2p−2vj兲兲dV
=1 2
冕
Uv2p−2v
2
nd−
冕
U冉
v2p−2兩ⵜv兩2+p − 1 2 v
2p−4兩ⵜ
v2兩2
冊
dV. 共14兲It is understood that the last term 共multiplied by p − 1兲 vanishes when p = 1; there are never negative powers ofv. As for the boundary integral, it also vanishes, sincev2/n vanishes in all
冕
U共v2p−2vd−v2p−2v · ⵜ兲dV. 共15兲
Since
−
冕
U
v2p−2v · ⵜdV = −
冕
U
v2p−2v · n d+
冕
U共p − 1兲v2p−4v · ⵜv2dV, 共16兲
and again the boundary integral vanishes, the term in共16兲is
冕
U共v2p−2vd+共p − 1兲v
2p−4v · ⵜ
v2兲dV, 共17兲
with the same meaning as before when p = 1. We may bound共17兲in several ways. We first choose
冏
冕
Uv2p−2vd+共p − 1兲v2p−4v · ⵜv2dV
冏
=冏
冕
U 1 +v共vdv
2p−2+
vdv2p−1兲+共p − 1兲
1 +v共v
2p−4
+v2p−3兲v ·ⵜv2dV
冏
艋
冐
1 +v冐
⬁冕
U共v2p−2+v2p−1兲兩vd兩dV +共p − 1兲
冐
1 +v
冐
⬁ ⫻冕
U
共v2p−4+v2p−3兲兩v · ⵜv2兩dV
艋
冐
1 +v冐
⬁冕
U共v2p−1+v2p兲dV +共p − 1兲
冐
1 +v冐
⬁ ⫻冕
U
共v2p−3+v2p−2兲兩ⵜv2兩dV. 共18兲
From now on we will denote
␣=
冐
1 +v冐
⬁,=
冐
1 +v冐
⬁.Notice that they are functions of t. Thus
1
2pF ˙
2p艋−
冕
Uv2p−2兩ⵜv兩2dV −共p − 1兲
2
冕
Uv2p−4兩ⵜv2兩2dV +␣
冕
U共v2p−1+v2p兲dV
+共p − 1兲
冕
U
共v2p−3+v2p−2兲兩ⵜv2兩dV. 共19兲
For our first estimate we will not make use of the first dissipative term. We have
␣
冕
U
共v2p−2+v2p−1兲dV艋␣共F2p−1+ F2p兲. 共20兲
As for the second term, by using Cauchy–Schwarz and Young’s inequalities,
共p − 1兲
冕
U
共vp−1+vp兲vp−2兩ⵜv2兩dV艋共p − 1兲
冉
冕
U
共vp−1+vp兲2dV
冊
1/2
冉
冕
Uv2p−4兩ⵜv2兩2dV
冊
1/2
艋共p − 1兲21
冕
U共vp−1+vp兲2dV
+共p − 1兲 4
冕
Uv2p−4兩ⵜ
v2兩2dV
艋共p − 1兲22
共F2p−2+ F2p兲+
共p − 1兲
4
冕
Uv2p−4兩ⵜv2兩2dV.
共21兲 We have proved the recursive inequality
1
2pF ˙
2p艋−
共p − 1兲 4
冕
Uv2p−4兩ⵜv2兩2dV +␣F
2p−1+␣F2p+
2共p − 1兲2
F2p−2+
2共p − 1兲2
F2p.
共22兲 We use now the fact that U has finite volume to bound all the Fkin terms of F2p,
F2p−2艋Vol共U兲1/pF2p 1−1/p
,
共23兲 F2p−1艋Vol共U兲1/2pF2p
1−1/2p
.
Let us begin studying a series of alternatives. It may happen
共A兲 F2p⬍1. Otherwise,
共B兲 F2p−2艋Vol共U兲1/pF2p, F2p−1艋Vol共U兲1/2pF2p.
We will consider the consequences of alternative共B兲. We have
1
2pF ˙
2p+
共p − 1兲 4
冕
Uv2p−4兩ⵜ
v2兩2dV艋
冉
␣共1 + m共U兲1/2p兲+2共p − 1兲2
共1 + Vol共U兲
1/p兲
冊
F 2p,共24兲
and if we call k = 1 + max兵Vol共U兲, 1其,
1
2pF ˙
2p+
共p − 1兲 4
冕
Uv2p−4兩ⵜ
v2兩2dV艋k
冉
␣+2共p − 1兲2
冊
F2p. 共25兲Let us now remember a particular case of the Gagliardo–Nirenberg inequality共Ref. 8, pp. 69 and 70兲. For any function f僆H1共U兲, there exists a constant C depending only on U such that
储f储2d+2艋C共储ⵜf储2+储f储1兲d储f储1 2
. 共26兲
Since共x + y兲d艋2d−1共xd+ yd兲, by taking= max兵2d−1C , 1其,
储f储2d+2艋 共储ⵜf储2d+储f储1d兲储f储12, 共27兲
with艌1. Notice that for f =vp,
储f储2= F2p 1/2
, 储f储1= Fp, ⵜf =
p
2v
2p−2ⵜ
v2, 储ⵜf储22= p
2
4
冕
Uv2p−4兩ⵜ
v2兩2dV. 共28兲
共b1兲 储f储2⬍ 1/共d+2兲储f储1, 共29兲
or
共b2兲 储ⵜf储22艌
冉
储f储2d+2−储f储 1 d+2
储f储12
冊
2/d
. 共30兲
With our election of f, the first alternative means
F2p⬍ 2/共d+2兲Fp 2
. 共31兲
Alternative共b2兲, when taken into共25兲, yields
1
2pF ˙
2p艋−
共p − 1兲 p2
冉
F2p共d+2兲/2−Fpd+2 Fp2
冊
2/d
+ k
冉
␣+2共p − 1兲2
冊
F2p. 共32兲Take now, for p艌2,
␥p=
冉
1 + kd/2冉
p2 共p − 1兲
冊
d/2
冉
␣+ 2共p − 1兲2
冊
d/2
冊
. 共33兲 Notice that␥p艌艌2/共d+2兲艌1. A short calculation will convince us that if F2p⬎␥pFp2
and共b2兲 occurs, then F˙2p艋0. Since alternative共b1兲is included in
共B1兲 F2p艋␥pF2p,
the remaining possibility is
共B2兲 F2p艋0.
Recall that all this assumes共B兲. Therefore the alternatives are共A兲F2p艋1,共B1兲or共B2兲.
III. UNIFORM ESTIMATES IN TIME
Let us consider a time interval关0 ,兴, and let
⌽p共兲= max兵1,max兵Fp共t兲:t僆关0,兴其其
共34兲 ⌫p共兲= max兵␥p共t兲:t僆关0,兴其.
For every t僆关0 ,兴where共A兲or 共B1兲occurs, certainly
F2p共t兲艋 ⌫p共兲⌽p共兲2. 共35兲
Now, if共35兲occurs for every t僆关0 ,兴, obviously
⌽2p共兲艋 ⌫p共兲⌽p共兲2. 共36兲
The other possibility is that for a certain t1僆关0 ,兴,
F2p共t1兲⬎ ⌫p共兲⌽p共兲2, 共37兲
which implies that共B2兲holds, i.e., F˙2p共t1兲艋0. Let共t0, t1兴 be a maximal left interval where共37兲
occurs. We know that F2p is decreasing there. If t0⬎0, F2p共t0兲=⌫p共兲⌽p共兲2, which, since
F2p共t1兲艋F2p共t0兲, contradicts our hypothesis. The only possibility is that共35兲occurs nowhere, i.e.,
t0= 0. In that case, F2pis decreasing in关0 , t1兴and therefore F2p共t1兲艋F2p共0兲. Thus, in every case
⌽2p共兲艋max兵⌫p共兲⌽p共兲2,F2p共0兲其. 共38兲
Since储v共t兲储p= Fp共t兲1/p, if we denote
p共兲= max兵1,max兵储v共t兲储p:t僆关0,兴其其, 共39兲
the 2pth root of共38兲yields
2p共兲艋max兵⌫p共兲1/2pp共兲,储v共0兲储2p其. 共40兲
Hence
4共兲艋max兵⌫2共兲1/42共兲,储v共0兲储4其,
8共兲艋max兵⌫4共兲1/8⌫2共兲1/42共兲,⌫4共兲1/8储v共0兲储4,储v共0兲储8其¯,
共41兲 2n共兲艋兵⌫2n−1共兲1/2
n
⌫2n−2共兲1/2 n−1
¯⌫2共兲1/42共兲,
⌫2n−1共兲1/2 n
⌫2n−2共兲1/2 n−1
¯⌫4共兲1/8储v共0兲储4…,储v共0兲储2n. Let us study the infinite product
⌫2共兲1/4⌫4共兲1/8¯⌫2n−1共兲1/2 n
¯. 共42兲 Recall that
␣共t兲=
冐
共t兲1 +v共t兲
冐
⬁, 共t兲=冐
共t兲1 +v共t兲
冐
⬁. 共43兲Let us denote by␣共兲,共兲 their respective maxima in关0 ,兴. By the expression in 共33兲,
⌫2n共兲艋
冉
1 + kd/2冉
22n 共2n− 1兲冊
d/2
冉
␣共兲+2共2n− 1兲
共兲2
冊
d/2
冊
艋
冉
1 +冉
22n+2k冉
␣共兲 +共兲2
2
冊冊
d/2冊
艋 冉
1 +冉
22n+2k冉
␣共兲 +共兲2
2 + 1
冊冊
d/2冊
. 共44兲The addition of 1 to the parentheses is intended to ensure that
x =
冉
22n+2k冉
␣共兲 +共兲2
2 + 1
冊冊
d/2艌1.
Since for those x, log共1 + x兲艋1 + log x holds,
log⌫2n共兲艋log+ 1 + d
2
冉
log k +共2n + 2兲log 2 + log冉
␣共兲 + 共兲2
2 + 1
冊冊
.Hence the sum of the logarithms of⌫2n satisfies
兺
n=1
⬁ 1
2n+1log⌫2n共兲艋 1
2
冉
1 + log+ d2log k
冊
+ d 2log 2兺
n=1⬁ 2n + 2
2n+1 + d 4log
冉
␣共兲 +
共兲2
2 + 1
冊
.共45兲
Thus, since the sum of the series兺共2n + 2兲/ 2n+1is 3,
兿
n=1
⬁
⌫2n共兲1/2 n+1
艋23d/2共e兲1/2kd/4
冉
␣共兲 +共兲2
2 + 1
冊
d/4, 共46兲
兿
n=1 m
⌫2n共兲1/2 n+1
. 共47兲
Since, on the other hand,
储v共0兲储p艋储v共0兲储⬁Vol共U兲1/p艋k储v共0兲储⬁, 共48兲 we find
2n共兲艋23d/2共e兲1/2kd/4
冉
␣共兲 +共兲2
2 + 1
冊
d/4max兵2共兲,k储v共0兲储⬁其. 共49兲
It is well known that储v储p→储v储⬁as p→⬁, so that2n共兲→max兵1 ,储v共t兲储⬁: t僆关0 ,兴其. Also,2共兲 represents the maximum of the kinetic energy in关0 ,兴, which we denote by E共兲. Calling M the universal constant written in共49兲, we obtain our main estimate
max兵储v共t兲储⬁:t僆关0,兴其艋M
冉
1 max关0,兴冐
共t兲 1 +v共t兲
冐
⬁+1 2max
关0,兴
冐
共t兲 1 +v共t兲
冐
⬁2
+ 1
冊
d/4
⫻max兵E共兲,k储v共0兲储⬁其. 共50兲
IV. COMMENTS AND EXTENSIONS OF THE ESTIMATES
In principle it could look as if the estimates in terms of and divided by 1 +vare unnec-essary, since if vis bounded so are and. While there is no conceptual gain in taking these magnitudes divided by 1 +v, the estimate 共50兲 is in fact finer than one involving only 储储⬁ and 储储⬁. It can be far better if the regions whereand/orare larger coincide with regions of high velocity. In particular, high temperature deviation propels the fluid faster, so it is likely that /共1 +v兲is considerably smaller than .
When the flow is chaotic, the temperature may become irregular. Therefore it is possible that some primitive of共e.g., a function⌰such that for some coordinate j,j⌰=兲may have a better behavior than the temperature deviation: portions whereis positive may compensate with others where it is negative to obtain a smooth result. We will see that储v储⬁may also be bounded in terms of⌰/共1 +v兲. The method follows the steps of the previous one: the term
冕
Uv2p−2vddV 共51兲
may be written as
冕
U共j⌰兲v2p−2vddV = −
冕
U⌰j共v2p−2vd兲dV = −
冕
U⌰共v2p−2jvd+ 2共p − 1兲v2p−4vdv ·jv兲dV.
共52兲
This may be bounded by
共2p − 1兲
冕
U
冏
⌰ 1 +v
冏
共v2p−2+
v2p−1兲兩ⵜv兩dV艋共2p − 1兲
冐
⌰ 1 +v冐
⬁冕
U共v2p−2+v2p−1兲兩ⵜv兩dV. 共53兲
Using now the Cauchy–Schwarz inequality, the term is bounded by
共2p − 1兲2
冐
⌰ 1 +v冐
⬁1
2
冕
U共v2p−2+
v2p兲dV +
冕
U
v2p−2兩ⵜv兩2dV. 共54兲 The last term may now be cancelled with the first of the dissipative terms共which we did not use in our previous proof兲and we are left with
共2p − 1兲2
冐
⌰ 1 +v冐
⬁2 1
2共F2p−2+ F2p兲. 共55兲
The rest of the proof is analogous to the previous one. We are left with a bound of the form
max兵储v共t兲储⬁:t僆关0,兴其艋M
冉
1 2max关0,兴
冐
⌰共t兲 1 +v共t兲
冐
⬁2
+ 1 2max
关0,兴
冐
共t兲 1 +v共t兲
冐
⬁2
+ 1
冊
d/4
⫻max兵E共兲,k储v共0兲储⬁其. 共56兲 Notice, however, that now a factor of the form 1 /2 appears before the maximum norm of ⌰/共1 +v兲, and this is squared, while before we had only 1 /and the power of/共1 +v兲was one. This may be important when the viscosity is low.
V. CONCLUSIONS
While the kinetic energy of the flow in Rayleigh–Bénard convection may be easily bounded by classical inequalities, the maximum of the velocity is harder to handle. As soon as the flow becomes chaotic small islands or filaments of high velocity are observed, which makes compatible the boundedness of the square mean of the velocity共the kinetic energy兲with the existence of large velocity peaks. It is proved here that, provided the pressure remains uniformly bounded, so does the velocity, and its maximum may be estimated by the maxima of the temperature deviation and pressure divided by one plus the velocity modulus. Other estimates may be made in terms of certain means of the temperature, which may be considerably smaller than the temperature itself if its distribution is irregular. The bounds depend on certain powers, depending on the dimension, of the previously mentioned magnitudes and the flow viscosity.
1
A. V. Getling, Rayleigh-Bénard Convection: Structures and Dynamics共World Scientific, Singapore, River Edge, London, 1998兲.
2
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