Technical Note Natural convection driven in CO2 near its critical point under terrestrial gravity conditions

Technical Note Natural convection driven in CO2 near its critical point under terrestrial gravity conditions

\ PERGAMON International Journal of Heat and Mass Transfer 31 "0888# 660Ð663 Technical Note Natural convection driven in CO1 near its critical point...

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\ PERGAMON

International Journal of Heat and Mass Transfer 31 "0888# 660Ð663

Technical Note Natural convection driven in CO1 near its critical point under terrestrial gravity conditions Hisao Azumaa\ Shoichi Yoshiharaa\ Mitsuru Onishia\ Koji Ishiib\ Shunsuke Masudab\ Toru Maekawab\ a

National Aerospace Laboratory\ 6!33!0\ Jindaiji!Hi`ashi!Machi\ Chofu\ Tokyo 071\ Japan b Toyo University\ 1099\ Kujirai\ Kawa`oe\ Saitama 249\ Japan Received 29 January 0887

Nomenclature ` gravitational acceleration P pressure T temperature Tc critical temperature[ Greek symbols aP coe.cient of volume expansion kT isothermal compressibility r density[

0[ Introduction The speci_c heat and the isothermal compressibility increase greatly as a ~uid system approaches its critical point and\ therefore\ the thermal di}usivity becomes very small[ It had been believed that thermal energy cannot be transferred near the critical point because of this small thermal di}usivity[ However\ a fast heat transfer was observed even under microgravity conditions in which buoyancy convection was suppressed ð0Ł[ This problem was analysed by Onuki et al[ ð1Ł and Boukari et al[ ð2Ł from a thermodynamical point of view and by Zappoli et al[ ð3Ł\ Zappoli ð4Ł\ and Zappoli and Carles ð5Ł from a thermo~uid mechanical point of view[ It is now known that temperature propagates as acoustic waves near the critical point[ Ishii et al[ ð6Ł analysed the temperature propagation near the critical point theoretically and

 Corresponding author[ Tel[] 9970 381 28 0213^ fax] 9970 381 22 8668^ e!mail] trmkwÝeng[toyo[ac[jp 9906Ð8209:87 ,08[99 Þ 0887 Elsevier Science Ltd[ All rights reserved PII] S 9 9 0 6 Ð 8 2 0 9 " 8 7 # 9 9 1 4 5 Ð 6

made clear the e}ect of the direction of gravity and the wave number of perturbation on the temperature propa! gation mode[ However\ the convective mode induced in near!critical ~uids under gravitational conditions has not yet been investigated either experimentally or theor! etically[ In this paper\ we investigate natural convection driven in near!critical CO1 experimentally under 0` conditions[ In Section 1\ the experimental apparatus and procedure are described[ In Section 2\ the result of the experiment is shown and the e}ect of the gravitational direction and the system temperature on the convective mode is discussed[ In the _nal section\ the result of the exper! imental analysis is summarised[

1[ Experimental apparatus and procedure The outline of the experimental system is shown in Fig[ 0[ The cylindrical test cell\ 59 mm in diameter and 39 mm long\ was made of aluminium[ A cylindrical cavity\ 16 mm in diameter and 39 mm long\ was made in the cell and sandwiched between two glass windows\ 19 mm in diameter and 09 mm thick[ CO1 was introduced into the test cell until the density reached the critical value ð7Ł and the system temperature was raised to the set value by a precise temperature controller[ The system temperature was controlled to an accuracy of 9[990 K and the ~uid temperature was measured by a thermistor[ Another ther! mistor was set at the centre of the test cell and heated for 1[9 s by circulating an electric current[ The heated part of the thermistor is shown in Fig[ 1[ The thermistor was covered with a polyimide _lm\ the length and diameter of which were\ respectively\ 3 mm and 9[27 mm[ The

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Fig[ 0[ Schematic diagram of the experimental system[ CO1 was introduced until the density reached the critical value[ The sys! tem temperature was controlled by a heater[ One spot in the test cell was heated by a thermistor set at the centre[ The temperature _eld was visualised by the shadowgraph method[

power of heat input was 9[4 mW[ The temperature _eld was visualised using the shadowgraph technique and rec! orded on a video tape[ Experiments were carried out in both supercritical and subcritical regions near the critical point[

2[ Result and discussion The temperature _eld visualised by the shadowgraph method is shown in Fig[ 2[ When the di}erence between the initial system temperature and the critical temperature\ T−Tc\ was −9[914 K "Fig[ 2"a## and 9[926 K "Fig[ 2"d##\ buoyancy convection was driven in the anti!gravitational direction and no convection was induced in the gravi! tational direction[ On the other hand\ when T−Tc  −9[901 K "Fig[ 2"b## and 9[993 K "Fig[ 2"c##\ convection was driven in both anti!gravitational and gravitational directions[ The temperature propagation in the anti! gravitational direction is due to the buoyancy e}ect[ Con! vection in the gravitational direction was observed only when −9[901 K ³ T−Tc ³ 9[904 K[ The time variation of the displacement of the tem! perature front in both gravitational and anti!gravi! tational directions after the heat input is shown in Fig[ 3[ The front of buoyancy convection moves in the anti! gravitational direction and the e}ect of the initial system temperature on the speed of the temperature front is not signi_cant[ On the other hand\ the initial system temperature has a strong e}ect on the speed of the tem!

Fig[ 2[ Temperature _eld visualised by the shadowgraph method[ "a#\ "d#] Buoyancy convection was driven in the anti! gravitational direction[ "b#\ "c#] Convection was driven in the gravitational direction when the system temperature was very close to the critical temperature[

perature front and the time delay of the onset of con! vection in the case of convection driven in the gravi! tational direction[ The temperature propagation speed was calculated from Fig[ 3 and the dependence of the speed on the initial system temperature is shown in Fig[ 4[ The temperature propagation speed in the anti!gravitational direction is higher than that in the gravitational direction[ The tem! perature propagation speed in the gravitational direction becomes maximum at the critical temperature\ while the speed in the anti!gravitational direction is almost uniform[ Another signi_cant feature is that the temperature front does not start moving in the gravitational direction immediately after the heat input[ The dependence of the

Fig[ 1[ Heated part of thermistor[

Technical Note

Fig[ 3[ Displacement of temperature front[ Ž\ T−Tc  ¦03 mK^ \ T−Tc  ¦00 mK^ R\ T−Tc  ¦4 mK^ r\ T−Tc  ¦1 mK^ ž\ T−Tc  9 mK^ \ T−Tc  −6 mK^ E\ T−Tc  −00 mK[ A thermistor set at the centre of the test cell was heated when the time was zero[ There is no signi_cant e}ect of the system temperature on buoyancy convection[ The onset of convection in the gravitational direction is delayed and the propa! gation speed is di}erent depending on the system temperature[

Fig[ 4[ Speed of temperature front[ \ The speed of the tem! perature front in the anti!gravitational direction[ ž\ The speed of the temperature front in the gravitational direction[ The propagation speed of the temperature front in the gravitational direction becomes maximum at the critical temperature[

delay time on the initial temperature of the system is shown in Fig[ 5[ The delay time of the onset of convection in the gravitational direction becomes minimum at the critical temperature and longer as the system temperature deviates from the critical temperature\ whereas the delay time of the onset of buoyancy convection is almost constant[ We carried out various experiments altering the power of the heat but the basic characteristics of convection driven in the gravitational direction was the same as those explained above A volumetric force r` acts on ~uid under 0` conditions\ where r is the density of ~uid and ` is the gravitational acceleration[ Density change Dr is dependent on both temperature and pressure changes\ DT and DP[ Dr 

0 1 1r 1T

P

DT¦

0 1 1r 1P

T

DP  −raPDT¦rkTDP

"0#

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Fig[ 5[ Delay time of the onset of convection[ \ The delay time of the onset of convection in the anti!gravitational direction[ ž\ The delay time of the onset of convection in the gravitational direction[ The delay time of the onset of convection in the gravi! tational direction becomes minimum at the critical temperature\ whereas that in the anti!gravitational direction is almost constant[

where aP and kT are\ respectively\ the coe.cient of vol! ume expansion and the isothermal compressibility[ When ~uid is heated\ both temperature and pressure rise and therefore buoyancy force raPDT` acts in the anti!gravi! tational direction and compression force rkTDP` acts in the gravitational direction[ When a ~uid system is very close to its critical point\ the isothermal compressibility becomes very large and therefore convection may possibly be driven in the gravitational direction[ The mechanism of the onset of convection in the gravi! tational direction is an open question[ The dependence of the speed of convection and the delay of the onset of convection on the system temperature must be explained[ A more detailed theoretical investigation of the mech! anism of the convection based on eqn "0# will be carried out in the future[

3[ Conclusion We investigated natural convection induced in CO1 near its critical point under 0 g conditions experimentally[ Through this study\ the following results were obtained^ "0# convection was driven in the gravitational direction when the system was close to the critical point\ "1# the temperature propagation speed in the gravitational direc! tion was lower than that in the anti!gravitational direc! tion\ "2# the temperature propagation speed in the gravi! tational direction became maximum at the critical temperature and "3# the onset of convection in the gravi! tational direction was delayed after the heat input[ The delay time became minimum at the critical temperature[

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Acknowledgement We would like to thank Prof[ J[ Straub\ Technical University of Munich\ for his constructive comments[

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References ð0Ł J[ Straub\ L[ Eicher\ A[ Haupt\ Dynamic temperature propa! gation in a ~uid near its critical point observed under micro! gravity during the German spacelab mission D!1\ Phys[ Rev[ E40 "5# "0884# 4445Ð4452[ ð1Ł A[ Onuki\ H[ Hao\ R[A[ Ferrell\ Fast adiabatic equilibration in a single!component ~uid near the liquid!vapor critical point\ Phys[ Rev[ A30 "3# "0889# 1145Ð1148[ ð2Ł H[ Boukari\ J[N[ Shaumeyer\ M[E[ Briggs\ R[W[ Gammon\

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Critical speeding up in pure ~uids\ Phys[ Rev[ A30 "3# "0889# 1159Ð1152[ B[ Zappoli\ A[ Durand!Daubin\ Heat and mass transport in a near supercritical ~uid\ Phys[ Fluids 5 "4# "0883# 0818Ð 0825[ B[ Zappoli\ P[ Carles\ The thermo!acoustic nature of the critical speeding Up\ Eur[ J[ Mech[ B:Fluids 03 "0# "0884# 30Ð54[ B[ Zappoli\ S[ Amiroudine\ P[ Carles\ J[ Ouazzani\ Ther! moacoustic and buoyancy!driven transport in a square side! heated cavity _eld with a near!critical ~uid\ J[ Fluid Mech[ 205 "0885# 42Ð61[ K[ Ishii\ T[ Maekawa\ H[ Azuma\ S[ Yoshihara\ M[ Onishi\ E}ect of gravitational acceleration on temperature wave propagation in a critical ~uid\ Appl[ Phys[ Lett[ 61 "0# "0887# 05Ð07[ H[L[ Swinney\ D[ Henry\ Dynamics of ~uids near the critical point] decay rate of order!parameter ~uctuations\ Phys[ Rev[ A7 "4# "0862# 1476Ð1506[