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Ilcre v, c, :tntl k tlrnol,c 1.I1t: tlrnsity, sl>rc:ilic Itc::rt, :mi contlucl,ivit.y of Ihc lluitl<br />
rc!spwlivrly; 0 in tltc! tlilli~rcnc:c? I)ct,wco~~ Ihc loonl t,t:llll)onrt,r~rc: ant1 (,hat at :t vory<br />
1;rrgc tlisI.:~t~(:c fron~ t11c I)otly, wl~orc: IJlc: l.c:tnpcr:~l,~~rc:, 7', is c:onsl,ant ant1 cq~~:rl lso<br />
'/, i. c . 0 - - '/ - '/',,,. 'I'llt: vcloc(ity lic:ltl w(z, y) :rt1!1 ~(z, y) in oqn. (4.12) is ;~.ssurnctl<br />
to I)c known. 'L'hc t,ernpnrat~~rc: distribution on the I~ountlarics of Lhc botly tlcfinetl<br />
b?~ '/I,, 3 7', is prrsc:ril)ctl nrttl in the sirnplcst cnsc it is constant wit11 respect Lo<br />
sl)nct: and t.imc 1)111., gcncrnlly spcalting, it varies wit11 both. I'rom the pl~ysioal poinl.<br />
of view cqn. (4.12) roprosents the 11c:rt 1):~lanc:c Ihr an clcn~cnt,ary volut~~e. 'l'hc Icfh-<br />
Ilantl sitlc represents t.11~ qu:mt,it,y of heat, c:xcl~:~~~gotl I)y convcc:tiorl, whereas the<br />
rigl~t-ll:rnd side is the ~~~;~n(.it.v of 11r:lt t:xt:I~:~n~cd 11y con(I~t(:tion. T11c frit:l.ion:~l hcatl<br />
gcneratcd in tile fluid is ncglcetctl. Tf 7',, > T,, tho prol)lom is that of detcrrnining<br />
1.ltc tcmperatl~rc field around a hot body which is cooled. By inspection it is scrn<br />
that cqn. (4.12) is of the same form as eqn. (4.6) for the vorticity w. In fact thcy<br />
hccomc itlentiral if the vorticity is replaced by thc tcmpcraturc tliffercncc and t.hc<br />
kincmatic viscosity v by t,hc ratio kip c known as thc thcrmal diffusivity. 'l'hc bountlary<br />
conclit,ion 0 - 0 at a largc distance from thc body corresponds to the condition<br />
tr, = 0 for the undisturbed p,nrnllcl stmam also at a largc distance from the body.<br />
llcncc we may expect that thc solutions of the two equations, i. e. the dislribntion<br />
of vorticity antl that of tcmpcraturc around the body will be similar in chnrnctcr.<br />
Now, tllc tcmpcratlrre dist,riI)ution around the body may be pcrccivcd intnitivrly,<br />
to a ccrtnin cxlcnt. In the limiting ca.sc of zero velocity (fluid at rosl) the inflncncc of<br />
tilo I~eatccl 11otly will extend ~~niforrnly on all ~itics. With very small velocit,ics tho<br />
fluid arountl the hody will still he affectcd by it in all directions. With incrcnsing<br />
velocity of flow, howcvcr, it is clcarly seen that the rcgion affected by the higher<br />
tempcreturc of the body shrinks more and more into a narrow zone in the immetlint,c<br />
vicini1.y of the body, antl into a tail of hcatcd fluid bchind it., 1Pig. 4.3.<br />
. -<br />
-.__ -- -<br />
--__<br />
Fig. 4.3. Annlogy betfween trnlperntuw<br />
and vorticity di~tribution ill tho neigh-<br />
bol~rhd of R body plnml in a strerrrn<br />
of fl\lid<br />
a), b) IAndCq of rrgion or iw.rrhsrd trmprrsture<br />
n) for ~rnnll vclucitlrs<br />
---------__..______<br />
Ir) fur Inrge vrlucitirn uf flow<br />
'rllc so111l.ion of eqn. (4.1 2) ni~rst-, a.s mcnt,ionkd, be of a chn.ra.cter similar t.o that<br />
for vorticit,y. At snlall velocities (viscous forces hrge compared with inertia forces)<br />
t.hcro is vorticity in ihc whole region of llow around the body. On the other hand<br />
for' largc vcloeitics (V~SCOIIS forccs smnll compnrctl wibh ir~ctl~in forccs), we may<br />
rx-prct, i field of flnw in which vorticity is confined to a small Iaycr along the surfacc<br />
of the I)otly antl in a wake behind thc boily, whereas thc rest of the fcld of flow<br />
c. 'l'ho limiting caw nf vory ~nlnll V~RCOIIR li~rtm 79<br />
remains, practically speaking, free from vortioity (scc Vig. 4.1). 11, is, I.l~ercforc,<br />
to be cxpected that in the limiting case of very small viscons forces, i. e. nt 1;rrgc:<br />
Itcynolds numbers, the solutions of the Nevicr-S(.okcs cq~~:~t~ions arc SO ('otlsti(.~tt.rtl<br />
as 1.0 permit a suldivision of the ficld of flow inl,o an cxtcrn:~I rrgion wlti(*ll is fr~o<br />
from vorticity, and a thin layer near the I)otly togcthcr with a wakc I~(:llit~tl it.. I11<br />
1.11~: first, region tho Ilow mny Im oxpnctctl 1.0 sntisfy OIO ctl~~~rtions of I'ri(:(,iot~ltw<br />
flow, the potcr~t~ial llow theory bcing uscd for ih cvalnation, whcrcas in tllc sc~-otr(l<br />
region vorticity is inherent, and, thcrcfore, the Navicr-Stoltcs cq~iations m~~st. hn<br />
uscd for its evaluation. Viscous forccs are importm~t, i. c. of thc santc ortlcr 91'<br />
mngnitt~tlc n.9 inertia forces, only in tl~c scc:ontl region known :is thc bou~tdrtr?y Irr?yrr.<br />
This concept of a boundary layer was introduced into the scicncc of fluid mechanics<br />
by L. Prantitl at the beginning of thc present ccntury: it has proved t,o he vcry<br />
fruitful. The subdivision of the field of flow into tho frictionless oxtcrnnl Ilow iwtl<br />
the cssentinlly viscous boundary-laycr flow pcrmitkd thc reduction of the rnnt,llcmatical<br />
difficnlties inllorent in the Nnvicr-Stokes cqnatior~s to snch an extent, that<br />
it, lmmne possible to integrate them for a large numbcr of cascs. The tloscript.ion<br />
of t,l~csc methods of integration forms t.hc subject of the boundary-laycr thnory prcscntctl<br />
in the following chapters.<br />
From a nt~mcrical analysis of the available soluteions of the Navicr-Stokc~s<br />
cq~~ations it is also poasiblo to show directly that in tho limiting case of vcry lnrgc<br />
Reynolds numbers there exists a thin boundary laycr in which the influcncc of viscosit,y<br />
is conccntratcd. We shall rcvcrt to this topic in Chnp. V.<br />
The previously discussed limiting case in which viscous forcrs heavily outweigh<br />
inertia force3 ((creeping motion, i. e., very small Reynolds number) results in a considerable<br />
mathematical simplification of the Navier-Stokes equations. By omitting<br />
the inertia terms their order is not rcduced, but they become linear. 'J'hc second<br />
limiting case, when inertia forces outweigh viscous forces (boundary layer, i e. very<br />
large Reynolds numbem) present8 greatrr mathematical difficulties than creeping<br />
motion For, if we simply substitute v = 0 in the Navior-Stokcs equations (3.32),<br />
or in the stream-function equation (4.10), wc thereby suppress the derivatives of Lltr<br />
highest order and with the simpler equation of lowcr order it is impossible to satisfy<br />
sirr~ultancously all boundary conditions of the cornpleto tliKrrcntial equnt~ous.<br />
However, this does not signify that the solutions of sucll an equation, sin~ldificd by<br />
t.he elimination of viscous terms, lose their physical meaning. Moreover, it is possil~lc<br />
to prove that this solut,ion agrees with the &mplete solutionof the full ~ svic~:-~toke~<br />
cq11nt.ions nlmost. everywhere in t,he limiting case of vrry large Reynoltls nrtmb~rs.<br />
Tho exception is confincd to n thin lnycr near the wall - the bountlnry In.yc;r. l'h~ls,<br />
thr complete nolution of t.hc Nnvicr-Stmkcs cqtralions c:nn I)c tl~orrgl~l of nrc t:onrcisI,ing<br />
of two sointions, thc so-cnllctl "outcr" solution which is ohtninctl with the nid of<br />
Eulor's equations of motion, and a so-callcd "inner" or bonndnry-1n.yc.r solnt.ion<br />
which is valid only in the thin layer adjacent to the wall. The "inner" solut,ion<br />
satisfies thc so-called houndary-layer eqmtions which are dctlncctl from tho Navicr-<br />
Stokes equations by ~oortlinat~e stretching nnti pwqsagc to tho limit R + m, n.s will<br />
be shown in Chnp. VII. The outer and inncr solutions must he malchcd t,o ench other<br />
by exploiting the condition that thcrc must exist nn overlapping rrgion in which<br />
bbth s&tions are valid.