• Aucun résultat trouvé

THE BÉNARD INSTABILITY IN A 3He/4He MIXTURE

N/A
N/A
Protected

Academic year: 2021

Partager "THE BÉNARD INSTABILITY IN A 3He/4He MIXTURE"

Copied!
3
0
0

Texte intégral

(1)

HAL Id: jpa-00218359

https://hal.archives-ouvertes.fr/jpa-00218359

Submitted on 1 Jan 1978

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.

THE BÉNARD INSTABILITY IN A 3He/4He MIXTURE

G. Lee, Philippe Lucas, A. Tyler, E. Vavasour

To cite this version:

G. Lee, Philippe Lucas, A. Tyler, E. Vavasour. THE BÉNARD INSTABILITY IN A 3He/4He MIX- TURE. Journal de Physique Colloques, 1978, 39 (C6), pp.C6-178-C6-179. �10.1051/jphyscol:1978679�.

�jpa-00218359�

(2)

JOURNAL DE PHYSIQUE Colloque C6, suppliment au no 8, Tome 39, aolit 1978, page C6- 178

T H E

BENARD

INSTABILITY IN A 3 ~ e / h ~ e MIXTURE

G. Lee, P. Lucas, A. Tyler and E. Vavasour

Department o f Physics, Schuster Laboratory, The University, Manehester MI3 9LP, England

Rdsum6.- Des expdriences sont ddcrites dhontrant que le mglange 3 ~ e / 4 ~ e est un systgme trss versa- tile pour l'gtude de l'instabilitd de Bdnard 1 deux composants qui elle-mcme fournit une sonde pour la mesure du coefficient de thermo-diffusion du mglange.

Abstract.- Experiments are described showing that a liquid 3 ~ e / 4 ~ e mixture is a very versatile sys- tem for investigating the two-component BLnard instability, which itself provides a probe for mea- suring the thermal diffusion ratio of the mixture.

The B6nard instability in a binary mixture has been the subject of considerable interest re- cently / I / because thermal diffusion is an additio- nal mechanism for producing gravitationally unsta- ble density fluctuations besides that of thermal expansion. A liquid 3 ~ e / 4 ~ e mixture is a much more versatile system for investigating this problem

than the fluids hitherto used because of the large variation in the thermal diffusion ratio kT and mass diffusion coefficient D near the X and tricritical points /2,3,4/.

In a convection cell with horizontal rigid boundaries at which the temperature is fixed and in which there is a vertical heat current it is possi- ble to show /5/ that the Rayleigh number R above which instability sets in and defined by

R = ~ 6 ~ k , g d ~ (1+1 /M) / (vDT) (1) can take values between 1708 (DIDT-, M N ) and 720 (D/D~+o, M*) depending on the size of the quan- tity

but 6 is negative. The same applies below TI whe- T

re the analysis pertains essentially to the one- component Bdnard problem with an effective thermal conductivity 131.

We have confined our experiments so far to cylindrical experimental cells containing a 15 mo- lar per cent mixture of 3 ~ e in 4 ~ e which have dia- meter 2.5 cm and spacing 0.2 cm between the two ho- rizontal copper end-plates. Near the X-point our approach has been to fix the temperature of the lower plate and direct a heat current W downward through the upper plate. The boundary conditions are consequently not quite the same as those just described but are not expected to change the range over which R may vary.

Figure 1 shows experimental data on the de- pendence of the temperature AT(W) on the heat cur- rent W into a cell that has a fixed heat leak of 27 k 1.5 pW from the upper plate into the colder helium bath.

M = D~{D(I+A)

L 7 -

~ ~ ~ / ( k ~ 6 ~ f l ) - ~ (2)

10 I I I I I I

Here

B

is the temperature gradient, g is the acce- 9

leration due to gravity, v is the kinematic visco-

4

. * *

4

sity, d is the cell spacing distance,

O .

pBc =

-

(ap I' a ~ ) ~ , ~ , p, c, P and T are the mixture density, mass concentration pressure and tempera- ture respectively,

bT

is the expansion coefficient and A = kT2(a~/ac)T,p/(~~c,p) where A =

v-j-vt,

is the difference in the chemical potentials of the mixture and C

-

is the s~ecific heat. For convec-

C,P w fywl

tive instability to occur R must be positive, which implies that in a dilute mixture near its A-point

Fig. I : Dependence of temperature AT on heat cur- the heat current must be directed downwards so that rent

w

into cell with lower plate maintained at 6 is positive, since kT and 6 are both positive

Article published online by EDP Sciences and available at http://dx.doi.org/10.1051/jphyscol:1978679

(3)

Consequently the heat current through the mixture flows either downward or upward according to whether W is greater than or less than 27 pW respectively.

AT(W) is measured from the ratio of two carbon re- sistance thermometers mounted on the cell plates and is given by AT(W) = 6T(W) + 6To where &T(W) is the temperature difference between the plates and 6T is the magnitude of the temperature difference when W = 0. The data show that the thermal conduc- tivity is enhanced when W>27 pW regardless of whe- ther the mixture is above or below TX implying con-

oscillations were observed with periods of 20-30 minutes and the onset of convection was easily ob-

servable with W = 1 0 pWwhich is to be expected in view of the much smaller size of kT % This regime corresponding to -1<M<O, is one in which thermal oscillations have been observed in ordina- ry fluids by several observers /1,6/.

References

vection occurs for downward heat currents W only, /I/ Schechter,R.S., Velarde,M.G. and Platten,J.K., which are at the most 1.5 wW. Other data without Adv. Chemical Physics

26

(1974) 265

the heat leak show Wc<0.2 pW. /2/ Ahlers,G. and Pobell,F., Phys. Rev. Letters 32 (1974) 144

The small size of Wc is to be expected, for

-

/3/ Lucas,P. and Tyler,A., Journal Low Temp. Phys.

by substituting typical values of thermodynamic

-

27 (1977) 281

and transport parameters near TX into (1) and using /4/ Roe,D. and Meyer,H., Journal Low Temp. Phys.

R = 1708, we find 6T

-

10WK to be the minimum tem-

-

28 (1977) 349

perature difference above which convection may oc- /5/ Lucas,P. and Tyler,A., to be published cur which corresponds to W = 10-'p~. /6/ Caldwall,D.R., Journal Fluid Mech.

74

(1976)

129

Above T the measured thermal conductivity is X /7/ Ahlers,G., Phys. Rev. Letters

&

(1970) 1333 strongly dependent on the heat current through the

mixture as can be seen from the data in figure 2.

Fig. 2 : Dependence of measured thermal conductivi- ty K on T

-

TX for cell which fixed heat current 2 pW(O), 10 pW(0) is flowing. Solid line : non- convective data of Ahlers/7/.

These data were obtained with the heat leak discon- nected so that W is the mixture heat current. We anticipate that these data shoul'd enable us to ob- tain the temperature dependence of k

T'

Finally we have performed some experiments above Tg, the temperature above which 6 T is positi- ve, without the heat leak and with the heat currenp directed vertically upward. In this regim thermal

Références

Documents relatifs

An experimental device, containing three thermal buckles controlled in temperature and greatly instrumented, and two plate heat exchanger, permits to study the

R., Commutative Banach algebras with power series generators, in Radical Banach algebras and automatic continuity, Proceedings Long Beach 1981, Springer-

The purpose of this paper is to derive a model governing the exchange of heat in a composite medium consisting of a background material with very small spherical inclusions of

关 16 兴 , we showed that the influence of cold electrons is much weaker during the second stage of the expansion, so that intense magnetic fields eventually develop in all casesY.

The deficit may be related to a change in summer mortality response, which may be due to public awareness of the dangers of high temperatures, the preventive measures

Instead, there is a maximum from October to December of both air‐sea heat flux (Figure 3a) and mixed layer temperature tendency due to air ‐ sea fluxes (Figure 4b) which thus

Under some appropriate scaling assumptions on the size, volume fraction and heat capacity of the inclusions, the temperature field T ≡ T ( t, x ) of the background material and

Based on the Péclet number evaluated in the core ow eld only, the critical viscosities and the corresponding times for the transition between a diusion and convection regimes