NASA NACA-TN-4018-1957 Influence of turbulence on transfer of heat from cylinders《湍流对汽缸热量传递的影响》.pdf
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1、, - %NATIONALADVISORYCOMMITTEEFOR AERONAUTICSTECHNICAL NOTE 4018k2AE! CC3PI: %?m 1AFWL “”ETHNICAL LW3WWWWLAFJWWB t N 9 M+INFLUENCE OF TURBULENCE ON TRANSFEROF HEAT FROM CYLINDERSBy J.Kesth and P. F. MaederBrown UniversityWashingtonOctober 1957.8“ltY,Provided by IHSNot for ResaleNo reproduction or ne
2、tworking permitted without license from IHS-,-,-.,TECH LIBRARY KAFB, NMlH NATIONALADVISORYcolmITTEE FOR AERONAU2 IllllllllllllllilllllllllllulitlJb7iOg“ TECHNICAL NOTE 4018 .-INFLUENCE OF TWWULENCE ON TRANSFEROF HEAT FROM CYLINDERSBy J. Kestin and P.This report deals with the problemturbulence on th
3、e transfer of heat fromF. Maederof the influence of free-streama cylinder in forced convectionat very low Mach numbers but at large Reynolds nunibers. In particular,an attempt is made to determine whether the sole influence of tuxhlenceis to s”ft the point of lsminar separation in mibcritical flow,
4、or thepoint of transition in supercritical flow, and thus effect a change inthe rate of heat transfer. It is shown that this is not the case andthat varying the free-stream turbulence affects local rates of heattransfer.The results are presented in the form of curves of R against Xand against (where
5、 is Nusselt number, = is Reynoldsnumber, and is Stanton number, all basedon mean properties); eachcurve has been plotted for a constant value of turbulence intensity, thetemperature effects having been elhinatedby the use of integral meanvalues of the thermodynamic properties of the fluid over the b
6、oundarylayer. The eerimental results unmistakably demonstrate that in thesubcritical range the Nusselt nuniberis not independent of the intensityof turbulence.An attempt to correlate the variation of the Nusselt nuniberat con-stant Reynolds and Prandtl nuniberswith the Taylor parameter A doesnot lea
7、d to a useful result. Thus, the intensity of turbulence seemsto be the prhsry parameter, at least in the small range of scale valuesL= 0.162 to 0.574 centimeter covered.This paper presents a survey of related analytical and experimentalwork and shows that the present tentative conclusions find ample
8、 supportin previous investigations. It is also pointed out that an oscilhtionin the free stream has a different effect on the velocity profile andon the temperature profile in the boundary -yer which may cause depar-tures from Reynolds analogy, inasmuch as the latter is proved for steadyflow only. H
9、ence, it is thought that the Reynolds analogy is a limitinglaw for zero turbulence intensity.Provided by IHSNot for ResaleNo reproduction or networking permitted without license from IHS-,-,-2 -. NACA TN 4018. .-4. INTRODUCTION -”It has been known for some time that eerimental results on thetransfer
10、 of heat reported by different observers show divergenceswhichexceed the respective experimentalerrors. Tt is clear that a system-atic influence is at work, and the present report shows that in therange of turbulent flow the structure of the turbulent stream exertsa profound influence on the rate of
11、 heat transfer in otherwise similarflows. A dimensional argument of the shnplest kind can be used to showthat this may be so.It will be recalled that in the elementary derivation of the lawsof similarity which apply in forced convection (refs. 1 to 4) the exter-nal flow is always described by specif
12、ying only one velocity Um, thefree-stream velocity. This constitutesan adequate description incases when the external flow is laminar or, in other words, when itsturbulence intensity e = O. However, when the external flow is tur-bulent, the laws of similarity implyl in addition, a similarity in ther
13、andom fluctuations in the streams. Present-day experimental evidenceseems to show that an adequate degree of similarity is achieved whenthe intensity of turbulenceand the scale of turbulenceJwL= G(y) dJ- (2)0are fixed in value. rHere (u )2 denotes the root mean square of thelongitudinalvelocity fluc
14、tuation, G(y) is theG= 1%gcorrelationfactor(3)for fluctuations U1 and U2 occurring at a distance y apart. Theintensity of turbulence is a measure of the amplitude of the random fluc-tuations in the stream, and the scale of turbulence serves as a roughmeasure of the size of eddies present in the stre
15、am.-.Provided by IHSNot for ResaleNo reproduction or networking permitted without license from IHS-,-,-lUlC14TN 4018 30The preceding description of the turbulent free stream disregardsthe frequency of the rsadom fluctuations, it being implied, as is wellknown from the TolJmien-Schlichtingtheory of t
16、he origin of turbulence(ref. ), that the random fluctuations cover a wide range of frequenciesof which a given band is amplified at a given Reynolds nuniber(4)The remaining frequencies are dsmped out and need not be considered.A clear understanding of the influence of turbulence on the rateof heat t
17、ransfer is very importsnt in my engineering applications.It may lead to methods of controlling the rates of heat transfer fromsolid bodies to fluid streams, whether in the direction of increasingthem, for example in boilers or heat exchangers, and thus improvingtheir efficiency or in the direction o
18、f reducing them in order to pro-tect the metal walls from deteriorating and burning out at high tem-peratures. The problem is also important in the calibration of high-temperature probes, inasmuch as the correction factors to be appliedto them depend to a great extent on the rate of heat transfer fr
19、om thestream to the probe.Probably the greatest experimental effort has been spent in meas-uring mesm coefficients of heat transfer from cylinders in crossflow.This case is, perhaps, not of the greatest importance so far as applica-tions in aerosmics are concerned, but it constitutesthe simplestexpe
20、rimental arrangement. Since, in addition, the experimental materialavailable for comparison is abundant, it seems reasonable to begin theinvestigationwith this case.-This investigation has been conducted under the sponsorship adwith the financial assistance of the National Advisory Committee forAero
21、nautics. The authors are indebted to Professor L. S. G. Kov PV2dynamic headresistanceReolds mmiberReynolds numbergas constant1=based on mean propertiesstandard resistancefrontal areaStanton ntierStanton numberwall thiclmessbased on mea propertiestotal temperatureatmospheric temperaturetemperature me
22、asured in settling chambersurface temperaturetemperature of body,of cylinderfree-stream temperaturetime.potential velocityProvided by IHSNot for ResaleNo reproduction or networking permitted without license from IHS-,-,-6 NMX l?N4018Um tree-stream velocityuouvVmvVowwWow=X,yaEeAAvvPvUlongitudinalvelo
23、city componentlongitudinalvelocity component in steady-state solutionfluctuating longitudinalvelocity componentvoltagemeasured voltagetransverse velocity componenttransverse velocity Component h steady-state solutionvelocitymeasured velocityvelocity along center linefree-stream velocitycoordinates o
24、f cylindricalbodymean coefficient,ofheat transferintensity of turbulencetemperature ratioTaylor parsmeter (eq. (6)wavelength of sound wavedynamic viscositykinematic viscositydensity of fluidangle at which transition occurs on “cylinderfrequency of oscillationa71a15a71a15.Provided by IHSNot for Resal
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