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730 XXIV. Prec turhi~lent. flowu; jcta and wnkes<br />
in tjhe tlownst.ream direction. Concurrently the jet spreads out and its vclocity de-<br />
creases, but the total momentum remains constant*. A comprehensive account of the<br />
problems of free jets was given by S.I. Pai [26]. See also the book by G.N. Abrnmo-<br />
vich [ll.<br />
A wake is formed behind a solid body which is bcing dragged through fluid<br />
at rest, Fig. 24.1 c, or hehind a solid body which has hcen placed in a stream of fluid.<br />
The velocities in a wnkc arc smaller than those in thc main stream and the losses<br />
in the vclocity in thc wakc amount to a loss of momcnta~m which is due to thc drag<br />
on the hody. Thc sprcad of thc wakc increases as tllc distancc from thc body is<br />
increased and the cliffcrenccs between the velocity in the wake and that outside<br />
I)ecomc smaller.<br />
Qnalitativcly such flows resemble similar flows in the laminar region (Chaps. IX<br />
and XI), but thcrc arc large quantitative differences which are due to the very much<br />
larger turbulcnt friction. Free turbulent flows are much more amenable to mathc-<br />
matical analysis than turbulcnt, flows along walls because turbulent friction is much<br />
larger than lnrninar friction in the wholc region under consitlcration. Consequently,<br />
laminar friction may bc wholly neglected in problcms involving free turbulent flows,<br />
which is not tho c.wc in flows along solid walls. It, will be rccalled that in thc lattcr<br />
case, by cont.mst,, laminar frict.ion must always bc taken into account in thc imrnc-<br />
diatc ncigl~bourhood of thc wall (i. c. in thc laminar sub-lnycr), and that causrs great<br />
mathematical tlifficultics.<br />
Furtlirrmorc, it will ho noted that prol)l~ms in frec turbulent flow arc of n<br />
houndmy-hycr nature, mcaning that tho region of space in which a solntion is being<br />
sought docs not cxtcntl far in a transverse direction, as comparctl with the main<br />
dirc~t~ion of flow, and that tho transverse grndjcnts arc large. Conscqucntly it is<br />
permissible to study such prol)lcms with the aid of the boundary-layer equations.<br />
In tlic two-tlimrnsiond iwomprrssit)lc flow tlicsc are<br />
Ilcrc T t1c:notcs t.hc I~url~~~lcnt shmring sl.rcss. l'hc pressure term has bccn droppcd<br />
in the cqrmtion of motion because in all problems to be considered it is permissible<br />
to assume, at Icast to n firsL approximation, that the prcssnrc remains constant. In<br />
the case of wakcs this assumption is satisfictl only from a certain distance from the<br />
tmtly onwartls.<br />
In ordm to be in a po.sit.ion t,o intrgratc the systcrn of equations (2.1.1) and<br />
(24.2), it is necessary to exprem the tnrbulcnt shearing stress in terms of the paramctcm<br />
of tho main ~Iow. ~t present suct~ an rIimin&tiort can only 110 aotticvcd witti<br />
the aid of sorni-cnipiricd ~~snmptions. 'LY~csc liavc already bcen ciiscuwcd in Chap.<br />
XlX. In this conncxion it is possible to make use of I'rantltl's mixir~g lcngtll tl~cory,<br />
eqn. (19.7):<br />
or of ite extension<br />
b. Estimation of tho incre-c in width ntid or tho dccre,wo in vrlocity<br />
where the mixing lcngths 1 and lI are b be rcgartl~rt na purely local functionst. They<br />
must be suitably dcalt with in each particular case. Further, it is possible to use<br />
Prandtl's hypothesis in eqn. (19.10), namcly<br />
t,=o& aa- ~ I L<br />
,ag - e xl b (urn,, - %,in)<br />
731<br />
(24.5)<br />
where h tlenotcs thc width of the mixing zone and x, is an empirical constant. Morc-<br />
over<br />
is the virtual kinematic viscosity, nssumcd constant ovcr thc wholc width and, IICIICC,<br />
independent of y. In adclition it is possible to use von IChrmh's Ilypothcsis, cqn.<br />
(19.19) and that due to G. I. Taylor, cqn. (19.15~~).<br />
Whcn cithcr of thc nssnmpthns (24.3), (24.4) or (24.5) is uscd it is fonncl that<br />
the rcsolts differ from cach otlicr only compnmtivcly littlo. ?'he bcsl rncnsuro of<br />
ngrccmcnt with cxpcrimcntal rcsnlta is furnished by thc awnml)tion in ccln. (24.5)<br />
and, in addition, the resulting cqnations arc morc convenicrit to solvc:. I'or I.l~c:sc:<br />
reasons we shall express a prcfercncc for this hypothcsis. Ncvcrtl~clcss, sonlo cxar~lplcs<br />
will be st~~diccl with the aid of thc l~y~otlicscs in cqns. (24.3) and (24.4) in ortlcr to<br />
cxhibit tho diffcrcnccs in tltc rcsulta whcn clifhrcnt, l~ypoblicscs arc IIRCCI. Morcovt~r.<br />
the mixing Icngth formula, cqn. (24.3), has rcndcrctl such valuablc service in the<br />
theory of pipe flow that it is useful to tcst ib applicability to thc typo of glow under<br />
consideration. It will be recalled that, among others, the universal logarit~limic<br />
velocity dist,ribution law has bcen dcduccd from it.<br />
b. Estimation of the increase in width anal of the clecrcnoc in vclneity<br />
Bcrorc proceeding to intcgratc cqns. (24.1) ant1 (24.2) fnr scvcrd parth11:rr<br />
cascs wc first propose to make estimatiotis of onlcra of magr~it~utlc. In this way wo<br />
shall bc able to form an idea of the typc of law wl~ich govcrns thc increase in the<br />
width of thc mixing zone and of the decrcasc in the 'hcight' of the ~clocit~y ~~roAlo<br />
with increasing distancc x. The followit~g accourlt will bc based on one first givrt~<br />
by I,. Prantltl [27].<br />
When dealing with problems of turbulcrlt jck and wakes it is usu;dly assumed<br />
that the mixing lcngth 1 is proportional to the width of jct, 0, because in this way<br />
wr are led to 11sdu1 rcsults. Hcnce we put<br />
t This extension was not diucu~acd in Chnp. XTX bccnuuc it is usrd only very rnraly.