18.06.2013 Views

Boundary Lyer Theory

Boundary Lyer Theory

Boundary Lyer Theory

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

672<br />

XXll. 'l'llc incon~prcssiblc turbulent bol~ndary lnycr 1). 7'110 cnlci~lnLion of two-rlimcnsional lrtrbulont boundary lnynrs 673<br />

involved when differential equation methods are used is substantially larger than in<br />

tho case of integral methods. The former require the use of a very large digital<br />

computer equipped with a large memory, whereas the latter can be done on a small<br />

calcrllator or, even, with the aid of a slide rule.<br />

In the following paragraphs we shall confine ourselves to the des~ript~ion of<br />

methods which rcsult merely in the calculation of time-averaged values of such<br />

variables of the turbulent flow as t,he velocity, the local shearing stress and the region<br />

of separation, because we subscribe to the view that only such mean values are of real<br />

interost to the engineer. Thus we rcfrain from calculating all those quantities that<br />

result from fluctuations, for example the correlation coefficients, the intensity of<br />

turbulence and its scale. Readers interested in these aspects are referred to more<br />

specialized publications, e. g. [lo, 813.<br />

Rcsearch into turbulent boundary layers was considerably advanced by the<br />

Stanford Univcrsity Conference organized by S. J. Kline in 1968. The results achieved<br />

at the time have been published in two large volumes edited by S. J. Kline, M.V.<br />

Morkovin, G. Sovran, D. J. Cockrell, D. E. Coles and E.A. Hirst [64]. In the appended<br />

[79] "morphology" prepared by W. C. Reynolds, the reader will find a de~cription<br />

of 20 integral and 8 differential methods and characterized according to their respective<br />

physical basis (status = of 1967). They differ, principally, in the empirical closure<br />

functions which are introduced in ordcr to malre the system of equations solvable. In<br />

addition, the conference had at its disposal 33 sets of experimental data which served<br />

as testing material for the computational algorithms. About ten years later, W.C.<br />

Reynolds [81] provided once again a summary review of the very large number of<br />

computational schemes; this appeared in his contribution to the Annual Reviews of<br />

Fluid Mechanics of 1976 (cf. the same author's 1974 contribution in Chemical Engineering<br />

[80]). In 1974 there appeared the book by F.M. White [I191 which describes<br />

20 integral and 11 differential procedures. It is difficult, and we shall not attempt, to<br />

select a "best method" from among the very large number proposed so far.<br />

A summary of many of these methods, principally integral ones, was prepared<br />

earlier by A. Walz [116] and J.C. Rotta [86, 871. A review of differedial methods is<br />

conlaincd in P. Bmdshaw's contributions [9, 12, 13, 141. Further, the book by T.<br />

Cebrci and A.M.O. Srnit,l~ [20] and two earlier papers by the same authors [18, 191,<br />

contain good reviews of many calculational procedures. The two earlier reviews by<br />

L. S. C. I$Y .<br />

2. Truckenbrodt's integral method. Before we proceed with the description of the<br />

details of E. Truckenbrodt's [I141 method, we find it helpful for its understanding to<br />

preface it with a few historical remarks. As already mentioned earlier, all computa-<br />

tional algorithms for turbulent boundnry layers rcly on ecrtnin empirical relations.<br />

As time progressed, and, in particular, since thc middlc of t,hc tl~irtics, tho empirical<br />

basis, and hencc also the semi-empirical and theoretical computational proccclurcs,<br />

underwent a process of continuous improvement.<br />

The first method for tho calculntion of t,urbulcnt boundnry Inycrs wit.11 prcssure<br />

gratlicnts was formulated by E. Gruschwitz [40] in 1931. The cxpcrimcntd data on<br />

which this mrthod wns basod wcro Intcr irnprovcd by A. 1

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!