• Aucun résultat trouvé

Onset of oscillatory flows in double-diffusive convection

N/A
N/A
Protected

Academic year: 2021

Partager "Onset of oscillatory flows in double-diffusive convection"

Copied!
17
0
0

Texte intégral

(1)

HAL Id: hal-01886729

https://hal.archives-ouvertes.fr/hal-01886729

Submitted on 3 Oct 2018

HAL is a multi-disciplinary open access

archive for the deposit and dissemination of

sci-entific research documents, whether they are

pub-lished or not. The documents may come from

teaching and research institutions in France or

abroad, or from public or private research centers.

L’archive ouverte pluridisciplinaire HAL, est

destinée au dépôt et à la diffusion de documents

scientifiques de niveau recherche, publiés ou non,

émanant des établissements d’enseignement et de

recherche français ou étrangers, des laboratoires

publics ou privés.

Onset of oscillatory flows in double-diffusive convection

Kassem Ghorayeb, Hicham Khallouf, Abdelkader Mojtabi

To cite this version:

Kassem Ghorayeb, Hicham Khallouf, Abdelkader Mojtabi. Onset of oscillatory flows in

double-diffusive convection. International Journal of Heat and Mass Transfer, Elsevier, 1999, 42 (4),

pp.629-643. �10.1016/S0017-9310(98)00204-X�. �hal-01886729�

(2)

OATAO is an open access repository that collects the work of Toulouse

researchers and makes it freely available over the web where possible

Any correspondence concerning this service should be sent

to the repository administrator:

tech-oatao@listes-diff.inp-toulouse.fr

This is an author’s version published in:

http://oatao.univ-toulouse.fr/20646

To cite this version:

Ghorayeb, K. and Khallouf, Hicham and Mojtabi, Abdelkader

Onset of oscillatory flows in double-diffusive convection.

(1999) International Journal of Heat and Mass Transfer, 42

(4). 629-643. ISSN 0017-9310

Official URL:

http://doi.org/10.1016/S0017-9310(98)00204-X

(3)

 Corresponding author

Onset of oscillatory ~ows in double!di}usive convection

K[ Ghorayeb

a\

\ H[ Khallouf

b

\ A[ Mojtabi

c

aReservoir En`ineerin` Research Institute\ 734 Pa`e Mill Road\ Palo Alto\ CA 83293\ U[S[A[ bM[I[P[\ U[F[R[\ M[I[G[\ 007 route de Narbonne\ 20951 Toulouse Cedex\ France

cU[M[R[\ 4491 IMFT!CNRS!UPS\ U[F[R[\ M[I[G[\ 007 route de Narbonne\ 20951 Toulouse Cedex\ France

Abstract

A numerical study is presented of unsteady double!di}usive convection in a square cavity with equal but opposing horizontal temperature and concentration gradients[ The boundary conditions along the vertical side!walls are imposed in such a way that the buoyancy ratio N  GrS:GrTis equal to −0\ where GrSand GrTare the solutal and thermal Grashof numbers\ respectively[ In this situation\ steady!state convective ~ow is stable up to a threshold value Grc0of the thermal Grashof number which depends on the Lewis number Le[ Beyond Grc0\ oscillatory convective ~ows occur[ Here we study the transition\ steady!state ~owÐoscillatory ~ow\ as a function of the Lewis number[ The Lewis number varies between 1 and 34[ Depending on the values of the Lewis number\ the oscillatory ~ow occurring for GrTslightly larger than Grc0is either centro!symmetric " for Le − 06# or asymmetric single frequency ~ow " for Le ¾ 06#[ For larger values of the thermal Grashof number\ the two regimes occur for _xed values of GrTand Le[ Furthermore\ computations show that Grc0reaches a minimum equal to 3[64×093for Le ¼ 6[ Þ 0887 Elsevier Science Ltd[ All rights reserved[

Nomenclature

C dimensionless concentration D solutal di}usivity

Grc0 critical value of the thermal Grashof number cor! responding to the onset of the oscillatory motion GrS solutal Grashof number

GrT thermal Grashof number ` gravitational acceleration Le Lewis number

N buoyancy ratio Nu Nusselt number P dimensionless pressure

P dimensionless period of oscillation Pr Prandtl number

RaT thermal Rayleigh number

Rac critical value of the thermal Rayleigh number cor! responding to the onset of convection

Sc Schmidt number Sh Sherwood number t dimensionless time T dimensionless temperature

U dimensionless velocity vector u horizontal component of the velocity

x\ z dimensionless horizontal and vertical coordinates[ Greek symbols

bC coe.cient of solutal expansion bT coe.cient of thermal expansion x thermal di}usivity

dC solutal boundary layer dT thermal boundary layer n kinematic viscosity r density

C stream!function[

0[ Introduction

The behavior of a ~uid subjected to the gradient of two properties with di}erent di}usivities is called {double! di}usive convection| ð0Ł[ Although {double!di}usive con! vection| covers a wide range of phenomena such as ocean! ography\ geology and crystal growth "Schmidt ð1Ł\ Wil! cox ð2Ł\ Turner ð3Ł and Huppert and Turner ð4Ł#\ we shall restrict ourselves to the investigation of the structure of the steady and unsteady ~ows in a square cavity with

(4)

horizontal heat and mass gradients due to constant tem! peratures and concentrations along the vertical side! walls\ respectively[

Double!di}usive convection in cavities with horizontal thermal and solutal gradients was the subject of several works in the two last decades since it is related closely to some physical processes such as the horizontal Bridgman crystal growth technique "Kamotani et al[ ð5Ł#[ During the growth of a crystal\ the profound in~uence of the transport processes in the ~uid phase on the structure and the quality of the solid phase requires a good under! standing of the buoyancy convective ~ows in this prob! lem[

Aside from the aspect ratio of the cavity\ double di}us! ive convection involves four dimensionless parameters] the Prandtl number Pr\ the Schmidt number Sc\ and the solutal and thermal Grashof numbers GrSand GrT\ respectively "all of the parameters will be de_ned in sec! tion 1#[ However\ the qualitative behavior of the double! di}usive induced ~ow depends mainly on the buoyancy ratio N  GrS:GrT"bCDC#:"bTDT# and the Lewis num! ber Le  Sc:Pr  x:D where D\ x\ bC\ bT\ DC\ and DT are the solutal and thermal di}usivities\ the coe.cients of solutal and thermal expansion\ and the di}erences of concentrations and temperatures between the vertical side!walls\ respectively[ The question of the e}ect of the Lewis number and the buoyancy ratio on the ~ow struc! ture when the temperature and the concentration are imposed along the vertical side!walls has been widely discussed by Bergeon et al[ ð6Ł\ Ghorayeb ð10Ł\ and Bennacer ð11Ł[

Two situations are generally considered depending on the sign of the buoyancy ratio N[ The solutal and thermal buoyancy contributions can cooperate "N × 9# or be opposite to each other "N ³ 9#[ In both cases\ mono!cell and multi!cell ~ows have been experimentally observed and numerically computed\ depending on the range of parameters considered[ It should be mentioned that\ a better agreement between experimental and numerical results has been observed when the solutal and thermal buoyancy forces cooperate than the case when they oppose to each other[ This may perhaps be due to the unsteady convective motions which are generally observed in the {opposing case| "Jiang et al[ ð7Ł\ Weaver and Viskanta ð8Ł\ Ghorayeb ð10Ł and Bergeon et al[ ð6Ł#[ This paper is concerned with the numerical investi! gation of the onset of double!di}usive oscillatory ~ows in a square cavity when the ratio N of solutal to thermal Grashof numbers is equal to −0[ This situation has been previously studied by Krishnan ð15Ł\ Gobin and Bennacer ð09Ł\ Xin et al[ ð01\ 13Ł\ Ghorayeb ð10Ł\ Ghorayeb and Mojtabi ð02Ł\ Bergeon et al[ ð6Ł\ Nishimura et al[ ð03^ 16Ð 17Ł\ and Zou and Zebib ð04Ł[ The choice N  −0 would be di.cult to attain experimentally[ However\ we believe that the study of this particular situation provides a step! ping stone to a better understanding of much more

realistic situations in which N di}ers from −0[ In such a situation\ convective motions are induced by the di}er! ence between the thermal and the solutal di}usivities\ x and D\ respectively[

When N is equal to −0\ the purely di}usive solution is stable up to a critical value Racof the thermal Rayleigh number RaT "RaT Pr GrT#[ Linear analysis has been performed in order to evaluate this critical Rayleigh num! ber Rac[ Gobin and Bennacer ð09Ł established that in an in_nite vertical layer\ the stability of the motionless solution only depends on RaT"Le−0#[ They showed\ fol! lowing the analysis carried out by Thorpe et al[ ð00Ł\ that Rac 5011:"Le−0#[ The analytical solution they obtained only satis_es the impermeability condition at the vertical side!walls[ Ghorayeb and Mojtabi ð02Ł and Xin et al[ ð01\ 13Ł re_ned this analysis and established that RaT 5498:"Le−0#\ corresponding to the critical dimensionless wave number kc 1[42[ More precisely\ Ghorayeb and Mojtabi ð02Ł considered vertical two! dimensional bounded boxes of various _nite extension[ Their results show the evolution of the critical Rayleigh number with the aspect ratio[ Using direct numerical simulations of convective solutions\ they observed the existence of a wide variety of steady one!cell and multi! cell solutions for a _xed aspect ratio and Rayleigh number[ Recently\ Bergeon et al[ ð6Ł considered\ using a continuation method\ the mechanisms by which stable solutions lose stability or by which unstable solutions regain stability[ They also studied the in~uence of the cavity inclination on the stability and bifurcating solu! tions[ They found that the bifurcation at Racis either transcritical or pitchfork depending on the aspect ratio and the inclination of the cavity[

For the vertical square cavity\ Rac"Le−0# is equal to 06 061 and the bifurcation at Racis transcritical ð6\ 01Ð 02\ 13Ł[ Two branches of steady solutions emerge at RaT Rac"Fig[ 0#] the supercritical and the sub!critical ones[ Both solutions are centro!symmetric[ When we increase the thermal Grashof number beyond some value "GrT 2924 for Le  00\ for example#\ only one branch of solution remains stable "the sub!critical solution#[ The supercritical branch undergoes a pitchfork bifurcation and\ consequently\ loses stability[ The other branch of solution "the sub!critical branch\ designated by squares on Fig[ 0# remains stable up to a critical value of the thermal Grashof number Grc0[ At Grc0\ it undergoes a Hopf bifurcation[ Thus\ the steady state ~ow loses stab! ility and an oscillatory convective ~ow appears[ The value of Grc0 depends on the Lewis number[ Krishnan ð15Ł studied this transition for Pr  0 and Le  2[050 in a square cavity[ He established that the transition convec! tive steady ~owÐoscillatory ~ow occurs for GrT Grc0 5[14×093[ The oscillatory solution\ which appears at Grc0\ breaks the centro!symmetry and is a single frequency oscillatory ~ow[

(5)

Fig[ 0[ Behavior of the extremum value of the dimensionless stream function as a function of the Rayleigh number for a square cavity\ for both the supercritical regime "circles# and the sub!critical regime "squares#[ The zoom shows the supercritical regime in more detail[ The dashed branch designates predictive mapping of the unstable solution branch ð02Ł[

the in~uence of the Lewis number on the steady ~owÐ oscillatory ~ow transition[ We _nd that the nature of the oscillatory ~ow occurring for GrT× Grc0depends on the Lewis number[ The oscillatory regime can be centro! symmetric or not\ depending on the values of the Lewis number and the Grashof number[ In this paper we con! sider the range "1Ð34# of the Lewis number[ The Prandtl number is set equal to 0 in a square cavity[ All the numeri! cal simulations are performed for a square cavity[ Very recently\ Nishimura et al[ ð16Ł studied the e}ect of the buoyancy ratio on the transition steady stateÐoscillatory state in a cavity of aspect ratio A  1 for Pr  0\ Le  1 and GrT 09

4

[ This study shows that oscillatory ~ows occur not only for N  −0\ but also for N $ ð−0[011Ð 9[8Ł[ The authors also reported hysteresis of steady and oscillatory states in the range N $ ð−0[011Ð0[933Ł[ In two previous papers ð16Ð17Ł\ the authors studied the same problem for the same range of parameters except for the aspect ratios^ they considered cavities with aspect ratios A 0 ð16Ł and A  9[4 ð17Ł[They reported that no oscil! latory ~ows occur for those aspect ratios under the above ~ow conditions[ This is in agreement with our result^ for A 0\ Le  1\ our numerical simulations show that the transition steady stateÐoscillatory state occurs at Grc0 0[14×094[ Zhou and Zebib ð04Ł have studied the onset of double!di}usive oscillatory ~ows in a similar situation "crystal growth by physical vapor transport pro! cess where the horizontal velocity along the vertical side! walls is proportional to the solutal ~ux#[ This study shows that the critical Grashof number depends on both the Lewis number and the aspect ratio of the cavity ð04Ł[

Our study is restricted to a range of the Grashof num! ber where the oscillatory regime is found to be single

frequency[ However\ as it was found by Krishnan ð15Ł\ when we increase the Grashof number\ the oscillatory regime undergoes two further bifurcations leading to states with incommensurate second and third frequencies[ A typical power spectrum before broad band noise begins to grow contains three linearly distinct frequencies and several linear combinations of these frequencies[ This behavior is the same as that reported by Gollub and Benson ð05Ł for the RayleighÐBenard con_guration[ This important feature of the ~uid behavior is not studied here[ Our interest is only focused on understanding the onset of the oscillatory ~ow as a function of the Lewis number[

The paper is organised as follows] the next section outlines the mathematical formulation of the problem and the numerical method used to investigate it[ The results are presented in the following section[ We _rst study the structure of the steady state solution occurring before the transition steady stateÐoscillatory state[ Then\ the in~uence of the Lewis number on both the values of the Grashof number corresponding to this transition\ and the structure of the oscillatory ~ow are studied[

1[ Mathematical formulation and numerical method 1[0[ Mathematical formulation

The system of equation is assumed to be unsteady state with no heat generation\ viscous dissipation\ chemical reactions or thermal radiation[ The OberbeckÐBous! sinesq approximation is assumed to be valid^ thermo!

(6)

physical properties are constant except in the buoyancy term where]

r"T\ C#  r9"0−bT"T−T9#−bC"C−C9##[

Here] r9 r"T9\ C9#\ bT"−0:r9#"1r:1T#C and bC"−0:r9#"1r:1C#Tare the density at temperature T9 and concentration C9\ the thermal expansion coe.cient\ and the solutal expansion coe.cient\ respectively[ The conservation equations for momentum\ mass\ energy and species in dimensionless form are the following] 1U 1t ¦"U = 9#U  −9P¦9 1U−"Gr TT¦GrSC#k\ "0# 9 = U  9\ "1# 1T 1t¦U = 9T  0 Pr9 1 T\ "2# 1C 1t¦U = 9C  0 Sc9 1C\ "3# where GrT `bTDTL 2

n1 is the thermal Grashof number\ GrS

`bCdCL2

n1 is the solutal Grashof number\ Pr n

xis the Prandtl number and\ Sc n

Dis the Schmidt number[

D\ x\ n and `\ are the solutal di}usivity\ the thermal di}usivity\ the kinematic viscosity\ and the gravity accel! eration\ respectively[ The corresponding boundary con! ditions "Fig[ 1# are]

Fig[ 1[ De_nition|s scheme[

U 9 "x  9\ x  0\ [z and z 9\ z  0\ [x#\ "4# T  C 0 "x  9\ [z#\ "5# T  C 9 "x  0\ [z#\ "6# 1T 1z 1C 1z9 "z  9\ z  0\ [x#[ "7# In the above equations\ lengths are nondimensionalized by L\ velocity by n:L\ time by L1:n\ temperature by DT  T1−T0and concentration by DC  C1−C0[ T0\ C0\ T1\ and C1are the temperature and the concentration at x 9 and x  L\ respectively[ We assume that bT× 9 and bC³ 9 "r increases with C and decreases with T# and that T0× T1and C0× C1[ These assumptions lead to] GrT×9 and GrS³9[ The buoyancy ratio N  GrS: GrT −0 and the aspect ratio A is set equal to 0[

Equations "0#Ð"3# together with the boundary con! ditions "4#Ð"7# are symmetric with respect to the follow! ing centro!symmetry operator]

2

U"x\ z# T"x\ z# C"x\ z#

3

:

2

−U"0−x\ 0−z# −T"0−x\ 0−z# −C"0−x\ 0−z#

3

[ "8#

As reported by Ghorayeb and Mojtabi ð02Ł\ and Bergeon et al[ ð6Ł\ all of the stable solutions observed numerically in the square cavity are symmetric with respect to the above operator[

1[1[ Numerical scheme

The numerical method used here is based on the pro! jection di}usion algorithm developed by Batoul et al[ ð06Ł for solving two!dimensional unsteady incompressible NavierÐStokes equations[ The temporal integration con! sists of a semi!implicit second!order _nite di}erences approximation[ The linear "viscous# terms are treated implicitly by the second!order Euler backward scheme\ while a second!order explicit AdamsÐBashforth scheme is used to approximate the non!linear "advective# parts[ A high!accuracy spectral method\ namely the Chebyshev collocation method\ with the GaussÐLobatto zeros as collocation points\ is used for the spatial discretization ð12Ł[ The code has been used by Labrosse et al[ ð19Ł to study the transition to unsteadiness of natural convection ~ow in a di}erentially heated cavity[ The results obtained by those authors agree extremely well with previous stud! ies[ Furthermore\ the results we present in this work are in good agreement with those obtained by Krishnan ð15Ł using a _nite element numerical code[

2[ Results and discussion

The study aims to compute the critical Grashof number Grc0beyond which the steady state convective ~ow loses stability in a square cavity[ The nature of the oscillatory

(7)

~ows occurring for GrT× Grc0is also studied[ The ~ow structure and the heat and mass transfers depend on the Lewis number[ Our study is performed for values of the Lewis number between 1 and 34[ However\ our numerical simulations show that for Le × 06\ Grc0and the oscil! lation frequency vary linearly with Le[

The study is performed using 20×20 and 30×30 meshes for Le ¾ 10 and Le × 10\ respectively[ Table 0 shows the mesh in~uence on the Nusselt number Nu\ the Sherwood number Sh\ and the stream function in the middle of the cavity for Le  10 and GrT 5[4×09

3 "slightly lower than Grc0#[ This table shows that the results obtained for the 20×20 mesh di}ers by less than 9[4) from those obtained for the 30×30 mesh[ With regard to the time step\ it varies between 09−3Ð4×09−4depend! ing on the values of Le and GrT[ Our numerical simu! lations show that\ in the whole range of parameters we studied\ further re_nement of grid size and time step results in less than 9[4) of uncertainty both in terms of heat and mass transfers\ and the oscillation frequency[

In order to compute the critical Grashof number which corresponds to the steady ~owÐoscillatory ~ow tran! sition\ we progressively increase GrT with a given step dGrTuntil the steady state loses stability[ We compute the solution for GrT¦dGrTstarting with initial conditions corresponding to GrT[ Once the oscillatory ~ow is obtained\ we progressively decrease GrTwith small step dGrT starting this time with the oscillatory regime as initial condition for the numerical simulations[ It should be noted that\ the lower =GrT−Grc0=\ the higher the tran! sition time is[ The closer one gets to the critical Grashof number\ the slower the oscillations decay or grow[ For instance\ the critical Grashof number is obtained with less than 1) accuracy[

2[0[ Steady state ~ow structure"GrT³ Grc0#

The experimental and numerical studies using large Lewis number binary ~uids show a very thin solutal boundary layer[ Suppose that the vertical side!walls of the cavity are maintained at temperatures "con! centrations# T0and T1"C0and C1# respectively[ The ther! mal "solutal# boundary layer dT"dC# near the wall x  9\

Table 0

Resolution e}ect] Le  10\ GrT 5[4×093"slightly lower than Grc0# M Nu Sh C "center# 10 2[48269 8[883 −8[2155 20 2[53660 09[79 −8[3633 30 2[53305 09[67 −8[3532 40 2[53332 09[66 −8[3536

for instance\ is de_ned as the distance across which the temperature "concentration# varies from T0 "C0# to "T0¦T1#:1 ""C0¦C1#:1#[ dT"dC# depends evidently on z[ Our numerical simulations show that the thermal and solutal boundary layer thicknesses are minimum for z 9[1 " for the square cavity#[ We designate\ subsequently\ the boundary layer thickness that cor! responding to z ¼ 9[1[ When the Lewis number is larger than 0\ the ratio dT:dCis thus larger than 0[ This ratio becomes more important when Le increases[ The con! centration outside the vertical solutal boundary layer is almost constant[ The small solutal gradient outside the thin solutal boundary layer leads to thermally driven buoyancy forces in the core of the cavity[ Wang et al[ ð14Ł suggested that the ratio of the thermal to the solutal boundary layer thicknesses is of the order of]

dT dc

"=N=Le#0:3[ "09# This result is e}ectively observed in several numerical and experimental studies "Kamotani et al[ ð5Ł^ Lee and Hyun ð07Ł^ Hyun and Lee ð08Ł#[ It con_rms the result obtained by the thermo!solutal boundary layer analysis for a ~uid in which the thermal buoyancy force dominates the solutal one ð11Ł "i[e[\ the density variations in the ~uid are mainly caused by thermal buoyancy forces#[ However\ the thermo!solutal boundary layer analysis shows that\ in the opposite case\ where the solutal buoy! ancy force dominates the thermal buoyancy force\ one obtains ð11Ł

dT dC

 Le0:2[ "00#

These results are obtained for large Lewis number[ For N  −0\ the case we study\ we investigated the in~uence of the Lewis number on the thermal and solutal boundary layers[ It should _rstly be mentioned that the mesh we use "GaussÐLabatto collocation points# is par! ticularly suitable for the study where thin boundary layers occur[ Figure 2 shows both the iso!concentration lines and the mesh for "Le  10\ GrT 58 999# "Grc0 69 999# where four collocation points are in the solutal boundary layer[ Figures 3 and 4 show the solutal and thermal boundary layers as a function of the Lewis number[ The corresponding Grashof numbers are slightly lower than the critical Grashof numbers[ Figure 4 shows that\ the thermal boundary layer is not signi_cantly in~uenced when the Lewis number varies "the Prandtl number is set equal to −0#[ We _nd\ in the range of parameters we study\ that]

dT dC

 Le9[2546[ "01# Figure 5 shows dT:dCnumerically obtained and the ana! lytical approximation obtained by eqns "09# and "00#[ On a logÐlog graph\ dT:dC increases linearly with Le[ The

(8)

Fig[ 2[ Solutal boundary layer for Le  10\ GrT 58 999\ 20×20 mesh[ Four collocation points are in the boundary layer[

slope of this linear curve is 9[2546[ This result di}ers by less than 09) from the results obtained by equation "00#[ 2[1[ Oscillatory re`imes

Figure 6 summarizes the principal results concerning Grc0and the structure ~ow for GrT×Grc0[ Grc0depends on the value of the Lewis number[ The curve X1OX3 designates the critical Grashof number as a function of the Lewis number[ For the values of "Le\ GrT# below this curve we obtain a steady state convective ~ow[ Grc0 reaches a minimal value equal to 3[14×093

for Le ¼ 6[ The point O "Le  06\ GrT 5[3×09

3

# divides this curve into two parts[ For Le × 06\ Grc0varies almost linearly as function of Le[ The "+# on the curve OX1designates the value reported by Krishnan ð15Ł for the transition steady ~owÐoscillatory ~ow[ This value agrees very well with our results[ It should be noted that the steady state convective ~ow "GrT³ Grc0# is shown to be centro!sym! metric for all values of Le considered in this study[ However\ the oscillatory ~ow is either centro!symmetric or not depending on the values of "Le\ GrT#[ With regard to the nature of the oscillatory ~ow obtained for the values of "Le\ GrT# above the curve X1OX3\ three zones of the oscillatory ~ow structure can be distinguished "Fig[ 6#[

2[1[0[ Sb] centro!symmetry breakin` re`ime

This region is bounded by the curves OX0and OX1[ The ~ow in this region breaks the centro!symmetry[ The ~ow structure on a half of a period is symmetric to that corresponding to the other half of the period with respect to the middle of the cavity[ Let P be the oscillation period

for some couple "Le\ GrT# in this zone[ the ~ow at the time t of this period is symmetric\ with respect to the middle of the cavity\ to that corresponding to the time t¦P:1[ We designate by {temporal symmetry| the last ~ow behavior[ It should be mentioned that Krishnan ð15Ł has only observed the centro!symmetry breaking solution[ Figure 7 shows the ~ow structure during a per! iod for Le  00\ GrT 3[64×09

3"Gr

c0 3[56×09 3#[ The temporal symmetry is clearly shown on this _gure[ The ~ow in this zone is a single!frequency one[

2[1[1[ Sc] centro!symmetric re`ime

The oscillatory ~ow obtained for the values of "Le\ GrT# bounded by the curves OX2and OX3is centro! symmetric[ However\ temporal symmetry does not occur[ Figure 8 shows the ~ow structure during a period for Le 10\ GrT 6[9×09

3

"Grc0 5[8×09 3

#[ 2[1[2[ Sbc] multiple oscillatory ~ows

For the values of "Le\ GrT# which are above the curve X0OX2 "Sbczone#\ our numerical simulations show that both centro!symmetry oscillatory ~ow and symmetry breaking oscillatory ~ow occur for _xed values of "Le\ GrT#[ There are multiple oscillatory ~ows[ This depends on the initial conditions of the numerical simu! lation[ The symmetry properties of a solution in this region are the same of that corresponding to the initial conditions of this numerical simulation[ Figures 09 and 00 show the ~ow structure during a period for both the centro!symmetric oscillatory solution and the symmetry breaking oscillatory solution obtained for "Le  00\ GrT 6[9×093# and "Le  10\ GrT 8[9×093#\ respec! tively[ Figure 01"a# shows how the oscillatory solution loses the centro!symmetry property when the numerical simulation is performed for "Le\ GrT# in the "Sb# zone starting with initial conditions corresponding to a centro! symmetric solution in the Sbczone[ The opposite case is shown in Fig[ 01"b# which shows how the oscillatory solution becomes centro!symmetric when the numercial simulation is performed for "Le\ GrT# in the "Sc# zone starting with initial conditions corresponding to a centro! symmetry breaking solution in the Sbczone[ Figure 02"aÐ f# shows the behavior of the Nusselt number as function of time\ the power of the specter as function of the frequency\ and the Sherwood number as function of the Nusselt number for Le  00\ GrT 6[9×09

3 "left# and Le 10\ GrT 8[9×09

3

"right#[ We can see that the oscillation frequency for the centro!symmetric solution is larger than the oscillation frequency for the centro! symmetry breaking solution[ We can also see that the amplitude of the oscillation is larger for the centro!sym! metry breaking solution than that of the centro!sym! metric solution[

2[1[3[ Remarks and discussion

In Figs 7 and 8\ small solutal blobs are pinched o} "contour C  9[4 in Fig[ 7 and contours C  9[3 and

(9)

Fig[ 3[ Solutal boundary layer for Le  1\ 6\ 04\ 06\ 14\ and 24 corresponding to GrT 0[1×094\ 3[0×093\ 4[8×093\ 5[3×093\ 6[0×093\ and 7[14×093\ respectively "values slightly lower than Gr

c0#[ The meshes used are 20×20 and 30×30 for Le ¾ 10 and Le × 10\ respectively[

(10)

Fig[ 4[ Thermal boundary layer for Le  1\ 6\ 05\ 06\ 14\ and 24 corresponding to GrT 0[1×094\ 3[0×093\ 4[8×093\ 5[3×093\ 6[0×093\ and 7[14×093\ respectively "values slightly lower than Gr

c0#[ The meshes used are 20×20 and 30×30 for Le ¾ 10 and Le × 10\ respectively[

(11)

Fig[ 5[ dT:dCis presented as function Le "top#[ +\ dashed\ and dot!dashed lines designate our numerical results and the curves dT:dC Le0:2and dT:dC Le0:3obtained by the thermo!solutal boundary layer analysis\ respectively[ The _gure in bottom pre! sents the same curves in a logÐlog graph[ The curve plotted in the solid line designates dT:dC Le9[2546[

Fig[ 6[ Various zones of oscillatory ~ows as function of "GrT\ Le#[ Below X1OX3] steady state centro!symmetric regime[ X1OX3is the threshold of this regime[ Sb] symmetry breaking oscillatory regime[ Sc] centro!symmetric oscillatory regime[ Sbc "above X0OX2#] coexistence of both oscillatory regimes for _xed "GrT\ Le#[ + indicates the steady stateÐoscillatory state threshold obtained by Krishnan ð15Ł for Le  2[050[

Fig[ 7[ Flow structure during eight moments of a period[ Con! tours of the stream!function\ concentration and temperature _elds are shown[ Le  00\ GrT 3[64×093\ Resolution is 20×20\ time step is 09−3[

(12)

Fig[ 8[ Flow structure during eight moments of a period[ Con! tours of the stream!function\ concentration\ and temperature _elds are shown[ Le  10\ GrT 6[9×093\ Resolution is 20×20\ time step is 09−3[

C 9[5 in Fig[ 8#[ These blobs appear only over a small part of the time cycle[ Over the remainder part of the oscillation period\ they are dissipated away by the e}ect of solutal di}usion[ Those _gures designate the ~ow for Grashof numbers slightly greater than the critical Grashof number[ The size of these blobs is shown to be closely related to the Lewis number and the Grashof number[ This size increases with Le[ With an increasing Grashof number\ the solutal blobs become bigger and present throughout the time cycle "Figs 09 and 00#[ The number of blobs also increases with the Grashof number[ The presence of the solutal blobs has been reported by Krishnan ð15Ł\ to be the cause of the oscillatory ~ow in the ~uid[

3[ Conclusion

Numerical simulations of unsteady double!di}usive convection in a square cavity\ with equal and opposing buoyancy forces due to horizontal thermal and con! centration gradients were carried out[ The presented results exhibit the in~uence of the Lewis number on the transition steady state convective ~owÐoscillatory ~ow\ and the oscillatory ~ow structure occurring beyond this transition[ The range "1Ð34# of the Lewis number has been studied[ The convective steady state ~ow is centro! symmetric regardless of the value of Le[ However\ the oscillatory ~ow which occurs after the transition steady stateÐoscillatory state is either centro!symmetric or asym! metric depending on the value of the Lewis number[ Furthermore\ it is found that\ depending on the values of "Le\ GrT"× Grc0##\ results show three situations of the oscillatory ~ow[ The _rst is where only the asymmetric oscillatory ~ow occurs[ The second is where only the centro!symmetric oscillatory ~ow occurs[ The third is where both oscillatory ~ows occur for _xed values of "Le\ GrT#[ In the range of "Le\ GrT# studied\ the oscillatory ~ow is shown to be single frequency[ Computations have been repeated for _ner mesh and time step[ This should con_rm the quantitative and qualitative validity of our results[

Acknowledgements

This work has been carried out with the support of the Centre Nationale d|Etudes Spatiales "CNES#\ France[ Computations were carried out on the DEC ALPHA 1099 3:164 of the Laboratoire de Mathematiques pour l|Industrie et la Physique "MIP#[ The authors thank A[ Bergeon and R[ Sani for fruitful discussions[

(13)

Fig[ 09[ Flow structure during eight moments of a period[ Contours of the stream!function\ concentration\ and temperature _elds are shown\ the symmetry!breaking solution "left# and the centro!symmetric solution "right#[ Le  00\ GrT 6[9×093\ Resolution is 20×20\ time step is 09−3

(14)

Fig[ 00[ Flow structure during eights moments of a period[ Contours of the stream!function\ concentration\ and temperature _elds are shown\ the symmetry!breaking solution "left# and the centro!symmetric solution "right#[ Le  10\ GrT 8[9×093\ Resolution is 20×20\ time step is 4×09−4[

(15)

Fig[ 01[ u"9[0218\ 9[4# as function of the time[ Resolution is 20×20\ time step is 09−3[ "a#] numerical simulation for "Le  00\ GrT 49 999# "Sbzone#[ The initial condition corresponds to a centro!symmetric ~ow for "Le  00\ GrT 44 999 × Grc0# "Sbczone[ "b#] numerical simulation for "Le  10\ GrT 64 999# "Sczone#[ The initial condition corresponds to a centro!symmetric ~ow for "Le  10\ GrT 74 999# "Sbczone#[

(16)

Fig[ 02[ Behavior of the Nusselt number as function of the time t "a and b# and of the power of the specter of the oscillations as a function of the frequency "c and d#[ The dashed and solid lines designate the centro!symmetric ~ow and the centro!symmetry breaking ~ow\ respectively[ "e and f# designate Sh as function of Nu during a period[  and e correspond to the eight moments of a period plotted in Figs 09 and 00\ respectively[ Resolution is 20×20\ time step is 09−3and 09−4for Le  00 and Le  10\ respectively[

(17)

References

ð0Ł J[S[ Turner\ Double!di}usive phenomena\ Annu[ Rev[ Fluid Mech[ 5 "0863# 26Ð45[

ð1Ł R[W[ Schmidt\ Double di}usion in oceanography\ Annu[ Rev[ Fluid Mech[ 15 "0883# 144Ð174[

ð2Ł W[R[ Wilcox\ Transport phenomena in crystal growth from solution\ Prog[ Crystal Growth and Charact[ 15 "0882# 042Ð083[

ð3Ł J[S[ Turner\ Multicomponent convection\ Annu[ Rev[ Fluid Mech[ 06 "0874# 00Ð33[

ð4Ł H[E[ Huppert\ J[S[ Turner\ Double!di}usive convection\ J[Fluid Mech[ 095 "0870# 188Ð218[

ð5Ł Y[ Kamotani\ L[W[ Wang\ S[ Ostrach\ H[D[ Jiang\ Exper! imental study of natural convection in shallow enclosures with horizontal temperature and concentration gradients\ Int[ J[ Heat Mass Transfer 17 "0874# 054Ð062[

ð6Ł A[ Bergeon\ K[ Ghorayeb\ A[ Mojtabi\ Double di}usive instability in an inclined cavity\ to appear in Phys[ Fluids[ ð7Ł H[D[ Jiang\ S[ Ostrach\ Y[ Kamotani\ Unsteady ther!

mosolutal transport phenomena due to opposed buoyancy forces in shallow enclosures\ J[ Heat Transfer 002 "0880# 024Ð039[

ð8Ł J[A[ Weaver\ R[ Viskanta\ Natural convection in binary gases due to horizontal thermal and solutal gradients\ J[ Heat Mass Transfer 002 "0880# 030Ð036[

ð09Ł D[ Gobin\ R[ Bennacer\ Double di}usion in a vertical ~uid layer] Onset of the convective regime\ Phys[ Fluids 5 "0# "0883# 48Ð56[

ð00Ł S[A[ Thorpe\ P[P[ Hutt\ R[ Soulsby\ The e}ect of horizontal gradients on thermohaline convection\ J[ Fluid Mech[ 27 "0858# 264Ð390[

ð01Ł S[ Xin\ P[ Le Quere\ L[S[ Tucherman\ Bifurcation analysis of double!di}usive convection with opposing horizontal thermal and solutal gradients\ Phys[ Fluids 09 "3# "0887# 749Ð747[

ð02Ł K[Ghorayeb\ A[ Mojtabi\ Double di}usive convection in a vertical rectangular cavity\ Phys[ Fluids 8 "7# "0886# 1228Ð 1237[

ð03Ł T[ Nishimura\ M[ Wakamutsu\ A[ Morega\ Oscillatory double!di}usive convection in a rectangular enclosure with combined horizontal temperature and concentration gradi! ents\ Int[ J[ Heat Mass Transfer 30 "0887# 0590Ð0500[ ð04Ł H[ Zhou\ A[ Zebib\ Oscillatory double di}usive convection

in crystal growth\ J[ Crystal Growth 024 "0883# 476Ð482[ ð05Ł J[ P[ Gollub\ D[V[ Benson\ Many routes to turbulent con!

vection\ J[Fluid Mech[ 099 "0879# 338Ð369[

ð06Ł A[ Batoul\ H[ Khallouf\ G[ Labrosse\ Une methode de resolution directe "pseudo!spectrale# du probleme de Stokes 1D:2D instationnaire[ Application a la cavite entra(¼! nee carree\ C[R[A[S[ Paris 208 serie II "0883# 0344Ð0350[ ð07Ł J[W[ Lee\ J[M[ Hyun\ Double!di}usive convection in a

rectangle with opposing horizontal temperature and con! centration gradients\ In[ J[ Heat Mass Transfer 22 "0889# 0508Ð0521[

ð08Ł J[M[ Hyun\ J[W[ Lee\ Double!di}usive convection in rec! tangle with cooperating horizontal gradients of tem! perature and concentration\ Int[ J[ Heat Mass Transfer 22 "0889# 0594Ð0507[

ð19Ł G[ Labrosse\ E[ Eric\ H[ Khallouf\ M[ Betrouni\ A direct "pseudo!spectral# solver of the 1D:2D Stokes problem] transition to unsteadiness of nature convection ~ow in a di}erentially heated cubical cavity\ Num[ Heat Transfer part B 20 "2# "0886# 150Ð164[

ð10Ł K[ Ghorayeb\ Etude des ecoulements de convection ther! mosolutale en cavite rectangulaire\ Ph[D[ Thesis\ Univ! ersite Paul Sabatier\ Toulouse\ France "0886#[

ð11Ł R[ Bennacer\ Convection naturelle thermosolutale] simu! lation numerique des transferts et des structures d|ec! oulement\ Ph[D[ Thesis\ Universite Pierre et Marie Curie\ Paris\ France "0882#[

ð12Ł H[ Khallouf\ Simulation numerique de la convection thermo!vibrationnelle par une methode spectrale\ Ph[D[ Thesis\ Universite Paul Sabatier\ Toulouse\ France "0884#[ ð13Ł S[ Xin\ P[ Le Quere\ L[S[ Tucherman\ Double di}usion in a square cavity] on the nature of the bifurcation at convection onset\ Notes et Documents LIMSI "0885# 85Ð096[ ð14Ł L[W[ Wang\ Y[ Kamotani\ S[ Ostrach\ Experimental study

of natural convection in shallow horizontal cavity with di}erent end temperatures and concentrations\ Report FATS:TR!70!053\ Case Western University\ "0872#[ ð15Ł R[ Krishnan\ A numerical study of the instability of double

di}usive convection in a square enclosure with a horizontal temperature and concentration gradients\ ASME National Heat Transfer Conference\ Philadelphia 0878 "ASME\ New York\ 0878#\ 246Ð257[

ð16Ł T[ Nishimura\ T[ Imoto\ M[ Wakamatsu\ A numerical study of the structure of double!di}usive natural con! vection in a square cavity\ Proc[ of 3th ASME:JSME Ther! mal Eng[ Conference 0 "0884# 082Ð199[

ð17Ł T[ Nishimura\ T[ Imoto\ M[ Wakamatsu\ A numerical study of double!di}usive natural convection in a rec! tangular enclosure _lled with binary gas\ Trans[ JSME Ser[ B 51 "0885# 160Ð166[

Figure

Figure 6 summarizes the principal results concerning Gr c0 and the structure ~ow for Gr T ×Gr c0 [ Gr c0 depends on the value of the Lewis number[ The curve X 1 OX 3 designates the critical Grashof number as a function of the Lewis number[ For the values o

Références

Documents relatifs

Il inter- vient pour les médicaments contre le cancer dont le remboursement a été refusé par le système de santé publique britannique en raison d’un prix trop élevé ou

la seconde partie de

The interaction of natural convection with surface radiation in a differentially heated square cavity filled with air is considered under large temperature differences.. The study

1 2 ﺢﻠﻄﺼﺼﻤﻟ ﻲﻠﻋ ﺲﻧﻮﯾ ﺪﻤﺤﻣ ﺚﺣﺎﺒﻟا ﺎھﺎﻨﺒﺘﯾ ﺔﻤﺟﺮﺗ ﻲھو Utterance ﺔﯾﺰﯿﻠﺠﻧﻹﺎﺑ ، نﺎﻤﺣﺮﻟا ﺪﺒﻋ ﺚﺣﺎﺒﻟا ّنأ ﻦﯿﺤﻓ ﻢﺟﺮﺘﯾ ﺢﻟﺎﺻ جﺎﺤﻟا Utterance ﺔﯿﺴﻧﺮﻔﻟﺎﺑ ﻲھو لﻮﻘﻟﺎﺑ ا

[5] Antonio Bucciarelli, Alberto Carraro, Thomas Ehrhard & Giulio Man- zonetto (2012): Full Abstraction for Resource Lambda Calculus with Tests, throught Taylor

In this way, the definition of the direct kinematic model of the SCARA robot requires the identification of 4 parameters, for each rotational joint, which describe the

We support that it may have undergone highly turbulent RDDC, either in the overturning compositional convection (unstably stratified) or in the finger regime associated with

L’accès à ce site Web et l’utilisation de son contenu sont assujettis aux conditions présentées dans le site LISEZ CES CONDITIONS ATTENTIVEMENT AVANT D’UTILISER CE SITE WEB.