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Boundary Lyer Theory

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482 XVT. Origin of tmbulcncc I c. Effort of oscillnhg frrc? st,rcn~n on t.rnnnit,ion 483<br />

process of transition from ltbmin~r to turbulent flow is the conseq~~cnce of an inshbility<br />

in t.1~ laminar flow, enilnciatcd by 0. Reynolds, is hereby completely vindicated.<br />

It. certsinly represents a posaiblr: and observahlr: mechanism of transition. The question<br />

as to whet.11~~ it pints a complet,e picture of the process and whethcr it constit~ltes<br />

the onhy nloahanism oneountcrcd in naturo is still at prtxent an open one. The latter<br />

cjt~:st.iotis now oconpy t.hc at.tcnt.ion of many research workcr*.<br />

e. Effect of oscillnting free stream on transition<br />

Aftrr it hntl bccn dincoverccl with 1.11~ aid of the oxprin~cnt drmrihed earlier thnt. the intensit.y<br />

of turbulenc:c of tho cxternnl stream, thnt. is thnt the preaence of an irreguhr tittle-dependent<br />

flnrtnntion in t,he free strcnm, cxert.ed a strong inflnence on transition, it was natural to nndertnke<br />

st,ndicu on t,ho chct of regular fluctnnt.ion in the free stream on tratlsi6ion. The effect of a<br />

nnperin~ponrd flnct,unt.ion of smnll nmplit,udc (E < 1) in an cxternnl stream U(z, 1) of the form<br />

on tho ~trtwt,urc of n lntninnr bonndnry lnyer w~ diucnwed in SBCB. XV n 3 nnd XV e 3.<br />

Sincc the Il*ynolils rlnrnbrr nt. trnnnition clrrrmnr*r ronnidorsl~l~ RR tho in tan nit^ of turbnlcnrc<br />

inrrrnru, it iu plnllniblc Lo suppoue Lhnt n ainlilnr erect nhould occur a8 the amplitude d u =<br />

~111 of the periodic cxternnl stream is 111;de to increw. The effect of an oscillation euperimposed<br />

on the external strcntn on thc transition of a hminnr boundary layer was clarified experimentally<br />

by J.H. Obren~ski nntl A.A. Fejer [63a] arr well aa by J.A. Miller and A.A. Fejer [60a]. Them<br />

inveetigntionu conwntrated attention, in the first place, on the boundary layer on a flat plate<br />

(Bl~ius profile). In this cnse, the velocity clintribution in the externnl stream is<br />

Hcrc {J, is the tin~c-avcrngc of thc frco-strcnm velocity which is independent of z, dU is the<br />

nn~plitudc of the temporal Rnctuntion in the external stream, and n denotea ita circular frequency.<br />

'rho mcnsurcn~enb rcported in 163~1 werc performed in an incompressible stream with<br />

and with frequencies of n = 4 Lo 62 sec-1.<br />

Them very carcful experin~entnl invent.iptions yielded the following emntial reaults:<br />

(a) The c-riticnl Rrynolds nnmbcr of tho start of transition, R,,fr = Urn zw/v dcpends only on the<br />

arnplitudc AU/Um of the external fluctuation.<br />

(h) Thc dimcnsionlr.s trnnuition length, thnt in the distance between the start of trnnuition and<br />

itn ronil,lrtion, R,,f - RZsc, depcntls only on the frequency of the externnl oscillationt.<br />

(c) '1.11~ record showing the varintion of velocity with time demonutratm that the line of transition<br />

is chnrart~rized by n regular and intermittent transition. The meaaurementa led to the conclusion<br />

thnt trnnnition rnn hc t~rscribrcl by the following "non-steady" hynoldu numbw:<br />

Sinrc thr rhnrnrlrrirtic length of tho cxtrrnal, oscillnt.ing stzrnm iu C - llm/n, it, iu po~sible to<br />

cxprrw the ~~non.~tt~ntly" I~tyold~ nnmbcr in thc form<br />

uz (A u/rrm)<br />

RNC =<br />

2nvn r'<br />

llrre All/l?, in the rlitnenuionlr~~ nn~plitude of tile impredsed oscillntion and ns/lJ: is itR dimensionlr~u<br />

frrqrrt-~~t*y. 'I'hr n~mnnrrn~rnb showd tlint the llcynolds number Rz.t, = 11, ~tr/v nt<br />

- --<br />

t Start of t.rnnnition nt R,,(, .- (1, .rl,/v -- lower curve in Fig. 16.10. Complct,ion of t,ranuition<br />

nt. R,,I, - 11, .rl./l* - nppcr ctrrvc it1 Fig. I ti. 16. Over the t1iut.nncc from zt, to xr it is observed<br />

thnt Ihr intr:r~~~ittr:r~cy fndor incrcnucu fro111 p = 0 to y = 1; this is interprctcd by t,hc statenwnt<br />

thnt in t.liin zone we ohnerve "trannitional t~~rbulcnce".<br />

the point of t8rnnuit~ion warr always con~itlcrnbly reduced con~pnrctl wit,l~ that for nhtionnry llow<br />

when t,hc %on-st.eatlyV Reynolds number am Inrge, i. c. whcn RNS > 27000. In t.l~c.sc: rxpcriincnt.s.<br />

t.rn.nnit.ion on tho flnt p1nt.c in ut.nlionnry Ilow s(.nrl.ctl nt. R,,,, -- 1.8 x 10". At.t.or,li~lg to<br />

Fig. I(i.l(i. thin vnluo of Rz.1, cor~.cnp~ntI~. np~)rt~~in~nLoly. t.o n tnrl~rtlet~co itrlr11nit.y of T 0.230/,,<br />

in the cxtnrnnl nt.rennt.<br />

So far, n nnt,isfnctory theory of ut,nbilit,y for houndnry lnyors in t,hc prcocnco of nn oxt.crrinl<br />

o~cillnting utrcntu doen not cxiut {I I a]. 011servnt.ion of intern~ittnnt t,nrl~ulcncc i r ~ t.11(! I~rrwt%tlrr of<br />

n frro-st,rcntn oncillntion ~IIOWR thtl its freqrroncy fl, is of thc antnc ortlor of n~np~it.~~clo nn thnt, of<br />

nntnrnl. neutrnl disturbnncer of the Tollrnie~l-Scl~licl~ti~~g typo fro111 ntnhilit.y t,l~eor.y; sm also<br />

I'ig. Ifl.18. The freqnenry, ,I, of 1.l~ oscillnt~ing flow invcst.igntml Irwc \vnn ~ninllrr 11y 11 I':u:tor of<br />

ahont 100 t.hnn thnt in t.hc nnl.urnl, nc~rtrnl tlint.nrbnnccs.<br />

A review of Ilte prorcns of trnnsition in thr prcnrnrc of frrc-strrnnl o~rillilt~io~ln uils rrrrntly<br />

prrhlinhrd hy ILJ. l,ochrkc, M.V. Morkovin, nntl A.A. Fcjcr 14HhJ<br />

(G) Conlcscencc. of 1.11rLulcnt spot.s ink) :I fr11l.y t1cvc~lopc:tl t.~~rl)~tlt*~rt. I)OIIII~~:LI.~ 1:13't~.<br />

In most CRRCR, t,hc t,rnnsit.ion frotn t,r~t.l)ulc:nt spvt,s (.o I.ully tlevclopotl (,III~IIII~W~I~ is<br />

associated with the furrnntion of a separat.ion bubblr, ns nlrwtly ~nont.ionctl in c:otlncxion<br />

wit,ll Fig. 10.10. At, tho present, time, only stngcs (1 ), (2) ant1 (3) nrr :~mrnnt)le t.o :L<br />

t,hcoretical analysis. The complete clnrification of the ~~~nnining stngrbn will rrq11i1.e<br />

rn~lch ntltlit,i~)nnl t.l~corc~t~icid resenrcl~ work.<br />

(1) Stnbtr now<br />

(2) I~'11~1nI~lr '~f~ll~~~l~~~~-H~~l~li~~l~li~~u<br />

WIWR 01--x I?,,,,<br />

Q 099 9 9<br />

lominor I- Ironsilion<br />

A,,,,<br />

R c<br />

JdTig. 16.23. Itlcnlizcd sltclrh of t.rnnsil.ion zone ill lhr I)O~III~~ILT~ 1:1~t:r 011 11 Ililt l~llltP 111 Z~.I.O i11t.i.<br />

clcncc after P. M. While 11073

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