]^Hh^(AA^^'^ J, NATIONAL ADVISORY COMMITTEE FOR AERONAUTICS TECHNICAL MEMORANDUM 1265 AMPLITUDE DISTRIBUTION AND ENERGY BALANCE OF SMALL DISTURBANCES IN PLATE FLOW By H. Schlichting Translation of *Amplitudenverteilung und Energiebilanz der kleinen Storungen bei der Plattenstromung." Nachrichten von der Gesellschaft der Wissenschaften zu Gottingen, Neue Folge, Band l,No. 4, 1935 Washington April 1950 DOCUMENTS DEPARTMfc-NT 3 ^r ^^"^^ NATIONAL ADVISORY COMMITTEE FOR AERONAUTICS TECHNICAL MEMORANDUM I265 AMPLITUDE DISTRIBUTION AND ENERGHT BALANCE OF SMALL DISTURBANCES IN PLATE FLOW* By H. Schllchting SUMMARY In a previous report by W. Tollmlen, the stability of laminar flow past a flat plate was Investigated by the method of small vibrations, and the wave length \ = 2.n/a., the phase velocity c , and the Reynolds number R of the neutral disturbances established. In connection with this J the present report deals with the average disturbance veloc— \| ities \ u' and \JT and the correlation coefficient \|u'2 X v'2 as function of the wall distance y for two special neutral disturbances (one at the lower and one at the upper branch of the equilibrium curve in the oR plane). The maximum value of the last two q.uantlties lies in the vicinity of the critical layer where the velocity of the basic flow and the phase velocity of the disturbance motion are equal. The energy balance of the disturbance motion is investigated. The transfer of energy from primary to secondary motion occurs chiefly in the neigh- borhood of the critical layer, while the dissipation is a 1 most completely confined to a small layer next to the wall. The energy conversion In the two explored disturbances is as follows: In one oscillation period, half of the total kinetic energy of the disturbance motion on the lower branch of the equilibrium curve is destroyed by dissipation and replaced by the energy transferred from the primary to the secondary motion. For the disturbance on the upper branch of the equilibrium curve, about a fourth of the kinetic energy of the disturbance motion Is dissipated and replaced In one oscillation period. The requirement that the total energy balance for the neutral disturbances be equal to zero is fulfilled with close approximation and affords a welcome check on the previous solution of the characteristic value problem. *"Amplltudenverteilung und Energiebilajiz der kleinen Storungen bel der Plattenstrbmung." Nachrichten von der Gesellschai't der Vis sens cheif ten zu Gottingen, Neue Folge, Band 1, No. k, 1935, PP. ^7-78- NACA TM 1265 1 . Intr oduct i an The numerous efforts, within the last decade, to solve the problem of turhulence (reference l) have at least produced some satisfactory results for a certain class of houndary— layer profiles when their stability was Investigated "by the method of gmal 1 vibrations, with due consideration to the friction of the fluid and the profile curvature (reference 2). Eef erring to Toll mi en (reference 3), who treated the example of laminar flow past a flat plate, the writer investigated several other cases: the Couette flow (reference k) , the amplification of the unstable disturbances in plate flow (reference 5), and the stabilizing effect of a stratification by centrifugal forces (reference 6), and temperature gradients (reference 7) - Every one of the investigations was restricted to the solution of the corresponding characteristic— value problemB, without calculating the characteristic function itself. In that manner, the wave lengths of the imstable, hence "dangerous", disturbances were Identified as function of the Reynolds number. In most cases, only the disturbances situated right at the boimdary, between amplification and damping, were determined. For these, just as much energy is transferred from the primary to the secondary flow, as secondary^notion energy is dissipated by the friction so that the total energy "balance is zero. All the stability studies made up to now were, for reasons of mathematical simplicity, based upon an assumedly plane fundamental flow, which depends only on the coordinate transverse to the direction of the flow, and a plane superposed disturbance motion which propagates in form of a wave motion in the primary— flow direotiono Vhile there is no objection to the limitation to the plane fundamental flow, since it is frequently realized experimentally, objection may be raised to the plane disturbance motion because the disturbances accidentally produced in practice are almost always three— dimensional. Accordingly, it might appear aa if the limitation to two— dimensional disturbances was all too special. However, H. B. Squire (reference 8) recently demonstrated on the Couette flow — this theorem is equally applicable to boundary- layer profiles — that precisely the specific case of the two-dimensional disturbance motion is particularly suitable for the stability study in the following sense: According to Squire, a two— dimensional flow, which is unstable against three-dimensional disturbances at a certain Reynolds number, is unstable against two-dimensional disturbances even at a lower Reynolds number. The two-dimensional disturbances are therefore "more dangerous" for a flow than the three— dimensional o The critical Reynolds number, which is defined as lowest stability limit, is thus obtained precisely from the two— dimensional, not the three— dimensional, disturbances. To gain a deeper insight into the mechanism of the turbulence phenomena from small unstable disturbances, a more detailed knowledge of the properties of these small disturbances is necessary. The present NACA TM 1265 report, therefore, deals first, with the distribution of the amplitude of the disturhance over the flow section, that is, the calculation of the characteristic fimctions and second, with the study of the energy- distribution and energy balance of the disturbance Jiotion. The investi- gations are based upon the disturbances of the laminar flow past a flat plate which are situated exactly at the boundary between amplification and damping (neutral oscillations). Chapter I AMPLITUDE DISTEIBUTION 2. Discussion of the differential equation of disturbance. Let U(y) be the velocity distribution of the fundamental flow (fig. 1) and )|f the flow function of the superposed disturbance motion, which is assumed as a wave motion moving in the x direction (direction of primary flow), whose amplitude (p is solely dependent on y, hence *(x,y,t) = cp(y)ei(°«^^^) = q)(y) 6^°-^^"^*^ a is real and X, = 2jr/a is the wave length of the disturbance; P = Pp + iPj^ and c = P/a are, in general, complex; T = 2Jt/p is the period of oscillation; P^ indicates the amplification or the damping, depending upon whether positive or negative; c = Pp/a. is the phase velocity of the disturbance. For the distiirbance amplitude cp, after introduction of dimenslonless variables from the Navier-Stokes differential equations, it results in a linear-differential equation of the fourth order, the differential equation of the disturbance (U - c)(cp" - a^cp) - U"cp = - ^(cp"" - 2aV + aV) (D (R = Ujjj6/v = Reynolds number, U^j^ = constant velocity outside of the boundary layer, 5 = characteristic length of the boundary— layer profile = boundary— layer thickness, v = kinematic viscosity.) The general solution cp of the disturbance equation is built up from four particular solutions cp^, ..., cpj^ cp = Cjtp^ + C2CP2 + Cf>2 "^ ^^^h ^2) MCA TM 1265 The "boundary conditions cp = qj' =0 for y = and y = (as explained in the report cited in reference (5)) give Cj, = (3a) and for C^, 02^ Co the system of eq.uations C^cpio + C2CP20 + C3CP30 = C-,cp-,„' + C^cp_' + C,cp,^' = ^1^10 '2^20 3^30 Cl%a + C202a = >va = 'Pva' + °^ve.' ^ = 1. 2) W J The subscript indicates the values at the wall y = 0, autecript a the values in the connecting point y = a to the region of constant velocity. From (i+) the equation of the characteristic value problem follows as 9-Lo ^ 20 ^30 ^10' ^20' ^30' la 2a = (5) This equation is discussed in the earlier reports for several cases. It contains^ aside from the constants of the hasic profile, the parameters a, E^ c j and c. . The complex equation (5) is equivalent to two real equations, and, if limited to the case of neutral disturhances ic- = 0), these two equations give, after elimination of c^., one equation "between a and E. This is the equation of the neutral curve in the oR plane, which separates the unsta"ble from the stable disturbance attitudes, and was originaily computed by Tollmien for the plate flow. They ajr-e assumed to be known for the subsequent study (fig. 2). -4?he writer computed the neutral curve for the plate flow cited under reference 5 again and found some differences with respect to Tollmien' s report. The newly obtained values are used in this study. NACA TM 1265 In the following, the amplitude and energy distribution ia computed for two neutral oscillations, one of which lies on the lower, the other on the upper hranch of the eq.uilibrium cijrve (fig. 2) o The parameters of these two neutral oscillations, obtained from the earlier calculation, are indicated in table 1. For the calculation of the integration constants from {h) , we put a^ ^2' ^3 Ci = l (3b) because the amplitude of 'disturbance remains indeterminate up to a constant factor, the intensity factor of the disturbajice motion. Thus, for the other two constants Co = - 2 $ la 2a 9 30 la 9 30 la ^ I - 9 10 (6) The particular solutions <^-,ij) and cpo^^) ^^^ readily obtainable by expansion in series from the so— called frictionless differential eq.uation of disturbance of the second order, which follows from the general equation (l) by omission of the terms on the right-hand side afflicted with the small factor l/oR. The point U = c , where phase velocity of disturbance motion and basic flow velocity agree, and which is termed the critical point y = y,, is a singular point of the frictionless differential equation of disturbance, which plays a prominent part in the investigations. NACA TM 1265 Putting = y ; = y ; ay = a ; a(a — y ) = a^ (7) y^ "^^l a - y^ ^2 ^]£ 1 ^Y 2 ^'^ where subscript k denotes the values at the critical points, the frlctionless solutions for linear velocity distribution read cp-L = a~l sinh(ar]_y-j_) ; cp = cosh(a-^y-|_) (8) and for parabolic velocity distribution ^-^= a^y^ + ^^^^ + a^j^^ + ... U " ^2 " ^0 "^ ^1 ^2 ^ ^2 ^2 + • • • + ^ ^1 ^°S yg ^°^ ^2 ^ ° ^9^ k 92 = tiQ + b^y^ + "b^yg^ + ... + — |- cp^^logjy^l - l^j for yg < U?he Blasius profile of the plate flow la approximated by a linear and a quadratic function (fig. l) , namely ^ y/6 ^ 0.175: U/Ujj, = 1.68 y/6 0.175 ^ y/6 S 1.015: U/U^ = 1 - (1.015 - y/&)^ (7a) y/5 > 1.015: U/U = 1 m For the connection between 6 and the displacement thickness 5* used in figiure 2, 5* = 0.3^15 is applicable. NACA TM 1265 According to earlier data, the coefficients are given by the eq.uations « 2 2 1 °'2 °'2 ai = 1; ag = - -; a3 = — ; ai, = - — , a = - 0.0013 ccg^ + 0.0083 ttg^; a^ = 0.002U ql^ + O.OOO6 ag r, 2 bo =1; b^ = 0; bg = -1 + -|- (10) b = 0.125 + 0.056 a^; bi^ = 0.021 - O.li+1 a,^ + 0.0)+2 a,^ b^ = 0,005 + 0.005 °"^ + 0".00U QL^ bg = 0.0015 + 0.0012 o^ - 0.0038 ci^ + 0.0011+ a.^ The particular solution 9 , with its derivatives, is regular throughout the entire range of flow (—1 ■= /-, ^ 0, '^ jp '^ -t-lj , and can be numerically computed with these data. But the particvilar solution cpp has a singularity, in which cpp' becomes logarithmically infinite in the critical layer y = y, . The more detailed discussion has shown that the friction at the wall, and in a restricted vicinity of the critical layer, must be taken into consideration. The first gives the friction solution CP;,, the other, the friction correction for cp-. Introducing the new variable ,.(.-.,) (=BU,.)^/3 -'-4^ (11) gives (only the greatest terma from (l) for 9(1)) being taken into account) the differential equation i9"" + W" = e^ (12) from which follows the correction for cpo near the critical layer, as well as the third friction— affected solution cp . The calcvilation of these two solutions merits a little closer study. 8 NACA TM 1265 3. The friction solution cp 3 The friction solution 9^ is obtained from the differential eq.uation (l2) when the inhomogeneous terms encum'bered with the small factor 6 are omitted; hence^ from the differential equation + TjCp 3 = Unusual In this equation is that. In contrast to the complete disturbance equation (l) and to the frictlonleas , equation of disturbance^ the dependence of the parameters a^ K, and U' by (U) enters only as scale factor for j, and that it is not at all affected by U^' . As a result J 9 (tj) can be computed once for all entirely independent from the velocity profile^ In this Instance, Tletjens' report (reference 9) constitutes a valuable support. A fundamental system cp and cp 32 = F, of equation (13) is given by 31 = F, r,V2 J 1/3 2^3/2e-Wl^' and T\ 1/2 -1/3 2,3/2 3-lnA (li^) The expansion In series of the Bessel functions V^)=(i (iz/2: 2V 2/ vTo ^'-T^P + V + 1) NACA TM 1265 /^vl/3 1/6 .^- gives, when the constant factors 1—1 (— i) / ^ [ T audi — (—1) \^[ ] ^^® omitted >> F;'(ri) = T, - 13 19 2'.3^«U'7 k'.y-k'^-lO'lZ 6l3^'4-7-10-l3-l6-19 + — ° + i \ .^ 10 .16 F2"(ti) = 1 - l'.3''"-ii 3133.1+. 7. 10 5l35.l+.7.iO'13.l6 .6 J > (15) .12 2'.32'2.5 lil3^.2'5-8.ll + i-^ 15 l'.3'^-2 3'.3^'2-5.8 5I35.2.5.8.11.14 — + • / Owing to the boimdajy condition cpo" = for i^ = + 00 only the solution aggregate P-i^-," + ^r^r^^ approaching zero for great positive real t^ (Pj, Pn ~ integration constants) comes into question. For great t], this can be represented by the Hankel function of the second kind with the subscript — and the argument r^ e ^"/^ , hence by 9," =F ''(ti) = 1/2 ^ (2) H, 1/3 1.3/2 ^-m/k 10 NACA TM 1265 Herewith, the looked— for solution of (13) — the constant factor lieing put as cp '(t) ) = cp _' for the sake of simplicity 3 — is given as expansion in power series near t) = 9 30 and as asymptotic expansion for great t| Integrating between the limits r\ and tj gives ^30 J Tl^ d\ — = 3l / / F^"dTldTl + P2 / I* F2"dTldn + T) - T)^ -D (I6c) ^30 ti\(/V U\U'\o where B and D are additional integration constants dependent on T)^; T\^ is the t\ coordinate at the wall, y = 0; hence hy (ll) 1/3 ^o = -^k/^ = -yk(°«U^') (lla) ■o 'o k The boundary condition 9^'/cp^^' =1 at y = 0, that is, t) = t| , is fulfilled by adding the term 1 in equation (l6b) » •3 -CnCPon' ^s "'^■'^® gliding speed of the frictionless solution at the wall. NACA TM 1265 11 Tietjens computed the integration constants ^-., Po^ ^^ ^ from the fact that at a point t^ = tj, ^ which lies in the range of validity of hoth expansions, asymptotic expansion and power series expansion of the solution of (13) up to and including the third differential quotient must agree. The resixltant equation system, set up and solved hy Tietjens, reads P^F^"' + ^2^2' •^l^l" ^ ^2^2" = ^^1^" r Pl / Fi_"dTi + P Al^ 2 / ^2 F2"dT) + 1 = BF, ' o u O (a) (b) (c) > (IT) 3l ' / F^"dTidTi + P2 / / Fg-dT^dn + n - Ti^ - D = BFi^ (d) The integration constants Pj^, P2, B, and D can also be computed hy a simpler method than Tietjens', with the aid of the transition formula from Hankel's to Bessel's functions, which reads H 1/3 sin ir/3 [^ 1/3 -1/3 This obviates the Joining of the two expansions, makes (I7) superfluous, and {ijh) gives the exact values immediately: !2 = ^-in/6 32/3 ll Pl ^ 3 r(2 and ^=ei'^A3l/3r(^|J3i^| (18) = -1.190 + 0.687i = 0.789(1 + i) h Tollmien, who pointed this out to the writer, had this representation as far back as I929, but summarily took over the data by Tietjens for the sake of simplicity. 12 NACA TM 1265 The factors P and D as fimctlon of r\ can then also he indicated explicitly, namely ,,.|(.-eW3)3V3,(i)./;o,^„,^A/; ^ -1 ° V^n D = -n + p, i 'o 1 > (19) F/'dTldTl + -^ Po po m 1 lli^oli^o F2"dTidTi)- - Bq) (0) with Bcp (0) = ip^ Tahle 2 contains the resiilts of a new calculation of Tiet Jens' value carried out hy these formulas. The differences from Tiet Jens' figures are f>Tl f]r\ insignificant. The values of F^", Fg", / ^^"d.^ = '^i , / ^2"^^^ = ^2*^ / F 'di) = F-,, / Fg'dT) = F2 as function of tj are indicated separateily uo uo as real and imaginary part In tahle 3« Since, according to (15), these quantities are either symmetrical or antisymmetric functions of r\, this tahle can he continued Immediately according to the negative values of r\. For the two neutral oscillations, whose amplitude and energT^ distri— hution is to he computed, it is y\^ = -2.63 and tj^ = -4.05 The corresponding values of e, according to (lla), are given in tahle I. along with the Integration constants P-,, Po, D ohtained hy Interpolation for these t^^ values. This takes care of all the data necessary for computing the friction solution cp^ with its first and second derivative as function of t] hy the equations (l6a, t, and c) . Tahle h gives the thus ohtained values NACA TM 1265 13 ^3 ^3 ^3 of : : as function of ti. The connection between ti and y ^30 ^30 ^30 is, according to eq.uatlon (ll), y = yjj. + eTj In all cases, the friction solution cp^ from the wall toward the Inside of the flow is very quickly damped out; but it still extends a little beyond the critical layer for both oscillations. h. The friction correction of cpg in the intermediate layer The second frlctionless solution 9^ behaves singularly at the critical layer y = y^, namely through equation (9) as jfriy - y]5-)log(y - J-^) , so that cpg' behaves as -— ■< 1 + log(y — yj^-) [• and cpg" behaves a V 1 as . Uk' (y - J^) From the differential equation (l2), in which only the greatest friction terms are taken into account, follows a solution cp^ modified by the friction, which joins the frlctionless solution at some distance from the critical point. For this purpose cpp is expanded In powers of the previously Introduced small quantity e = (oRU, ')~-^/3 ^2 " ^20 + ^^21 "^ ■"• ^^°) ^oQ being chosen equal to unity. From (12) follows the inhomogeneous differential equation for 9^1 with reference to t). 11^ NACA TM 1265 On accoimt of the very small value of e, tj can assume great values even at small y — Jy values. An attempt is made to find such a solution 9o-i " of this equation, which for large t), hut small (y — y^.) joins on to the frictionless solution ^\ V dy \' y - yj. For large t^ there shall he: d Cp^, TT " ^21 ^k dy^ V^ (22) ) The corresponding homogeneous equation appeared earlier in the calculation of cp (equation (13)). It has the fundamental system F-,"(r|) and F "(t)) (equation (l5))- A particular solution of (2l) is -'k V,/„'Vin-F,"/^%,"d, which can he verified easily hy suhstitution, and the general solution of (21) is 21 U,. IF2" r F^"dT, - iF^" r F^-dTi + c^Fi" + C2F2" I (23) The integration constants c and Cp, which can be complex, are evaluated from the boundary conditions. The quantity ^p-i" is complex and shall join the real frictionless value (equation (22)) for large NACA TM 1265 values of t). By decomposition in real and imaginazy parts, the four equations defining the integration constants read ^21r" = ^"(^) = -^2i"Flr' - ^2r"^ll' ^ Fii-'F^r' + F^-Fg,' ■^k ■^ ^ir^lr" - ^li^li" - -2r^2r" " ^2i^: 1 21 T, F^21i" = S"(^) = - F2l"^li' - ^2r"^lr' - Fi.-F^i' - F^-'F^,' (^U) ^ ^ir^li" - -li^lr" ^ ^2r^2i" ^ ^2i^2r" = ° for T| = ±TJ^ From (21), with the "boundary condition (22), it follows that 922j-" is an antisymmetrical, and ^pil" ^ symmetrical function of t\. Moreover, since F^', F^^', F^^", F^." are symmetrical and F^^', F^^' , F^.", 7^" antisymmetrical functions of tj, the following must be true c-Li = C2p = (25a) for reasons of symmetry. The other two constants c , Cp. are obtained by solving the above equation system for t) = tj, . For the present calculation, tj = U was chosen. The series for the Bessel functions are still fairly convergent for t] = ii; but since differences of very large numbers occur, the separate terms in i^k) must be computed to five digits (table 3). For c and Cp. ci^ = 1.2852; C2i = 0.9373 (25b) so that ^^21r" = ^"(^) ^^ "^;;^21i" = ^"(ti) can be calculated. The k k values are given in table 5. l6 NACA TM 1265 The values of cp and - — in the Intermediate layer are obtained immediately by quadratures, namely dcp, '^2r dy = ^|(1 + log €) + a'CTl)| (26a) and ^--v"'^>-v,L.'"'^''^-v«''^' <^«'' A check on this numerical calculation is given "by the fact that dcp2i for — — at transition from large positive to large negative tj the transition substitution for cp_ deduced by Tollmien (reference 3) must result again (compare equation (9))^ which he obtained by discussion of the asymptotic representation of the Hankel functions. Tollmien' s transition substitution gives \ dy /y=+oo \^ dy /y=-~ U^^' the present numerical calculation gives 'dcp_.\ /d.9oA U, " n+00 2i> I 2il + JL. / H"(Ti)dTi dy /y=+~ \ dy /y=-«> U^^' U-o and the graphical integration gives / H"(Tl)dTl Z / H"(Tl)dTl = 3.li^ (27) J -co U-h that is J complete agreement within the scope of mathematical accuracy. NACA TM 1265 17 The intermediate layer near the critical point, which "by the present calculation reaches from atout tj = — ij- to t) = +k, is already so wide at the first neutral oscillation that it reaches up to the wall (wall T) = —2.63); at the second oscillation with t) = —14-005, the "boundaj:y of the intermediate layer is reached exactly at the wall. With this, all data needed for the numerical calculation of the solution cp_, corrected "by the friction with cp ' and 9p"> ^^® available. 5. The numerical values of the integration constants All three particular solutions cp , cp , cp are numerically known. To build up the required solution 9 from it, the numerical values of the integration constants C and C-^ must be accertained (equation (i First of all, equation (2) is rewritten in a more suitable form, namely cpo 9 = cp^ + 0^92 + C^' -^ (2a) where equations (3a) and (3^) were resorted to and 9 was replaced by the quantity 9 /9 _' which follows immediately from the numerical calculations. Comparicon with (6) gives S' = I-^20' - 'lo' - -f 2'20' * '10') '«-' This method of writing has the advantage that the two integration constants Cp and C-,' in (2a) are dependent only on the values of the frictionless solutions 9 and 9 , hence are relatively simple to compute . The values of 9^^^, 9^^, ^la'^ ''2a'' "^la' ^ 2a ^^ "^^® values of C^ and C^ ' thus computed by (6) and (6a) for both neutral oscillations are given in table 1. Table 6 and figures 3 and k give the values of 9^, 9^, 9^', 9^' computed with it, hence the desired amplitude distribution as function of y/&. 18 NACA TM 1265 Outside of the "boundary layer, at y/& > I.OI5 the simple formula 'V 9^=9^' = (29) is valid for the amplitude distrihution. The constant C* is so chosen that the value of cp ' joins the already found value in y/6 = 1 = 015. (Tahle 1.) 6. The average fluctuation velocities and the correction factor (compare reference 10) Changing to the real method of writing M r u' = — = K Jcp^' coa(ax - 3^t) - cp^^' sin(ax - P^t) I U^ (30) V = — s^ r — = KaJ cp^ sin(aix - p^t) + cp^ cos(ca - P^t) U, m K is a freely available intensity factor. According to figures 3 ajid k, the one phase (cp^, or cpp' ) predominates in both neutral oscillations. Tne amplitude distribution of u' and v' can be represented most appropriately by forming, in analogy with the turbulent fluctuation u ,2 U and ^^^•2 U„ ; where the dash velocity, the dlmensionless q^uantities '"'m "m denotes the time average value formation over a period T at a fixed point X, y, or in other words ,.2 _ 1 I'^dt (T = vibration period) t=o NACA TM 1265 19 The result is \u' U m f,W'*^i"-- ,2. C^ u m f2 \|^i CPi (31) and CPl^) (32) The last quantity gives the mean kinetic ener®r of the motion disturbance. (See eq. 36.) These averages, which are independent of x, are represented in figures 5, 6, and 7 and table 7 for both neutral vibrations as functions of y/5. The intensity factor itself was so to O.O5U ^ m \ o in the boundary layer is equal dy = 0.05Uj^| (table l) . The majcimum amplitude chosen that the average value of for both neutral vibrations lies near the critical layer. The correlation factor between u' and v' , which is completely Independent from the intensity of the motion disturbance, can then also be calculated. It Is k(u', v') = u'v'dt = r^ ,2 ^,2 k(u', v') = cpr'^i - ^r^±' \|(9r'^ + cp^'^) (9/ + cpi^) (33) The correlation factor is likewise dependent on y/6 only; Its variation is indicated in figure 8 and table 7. It is negative almost throughout the entire range of the flow, for both neutral vibrations, as is to be expected, since, owing to the positive dU/dy, positive u' Is usually coupled with negative v' and negative u' with positive v' . The maximum value of k is -O.I7 and -O.I9, respectively. It is inter- esting to compare the theoretically established correlation coefficient with Townend's data in a developed turbulent flow (reference ll) . The k values of -O.I6 to -O.18, obtained for the flow in a channel of square 20 - WACA TM 1265 cross section at various distances from the axis, are of the same order of magnitude as those obtained by the present calculation for the incipient turhulence. Chapter II EEERGf DISTRrBUTION 7. The kinetic energT" of the disturbance motion. Having established the amplitude distribution for the two neutral vibrations J the energy of the disturbance motion can be computed. The total kinetic energy of the disturbance motion in a layer of unit height, which, in x direction, extends over a wave length X and in y direc- tion from the wall to infinity is P>X f)oa E = £ / / (u'2 + v'2)dxdy 2 (/x=0 iiy=0 i^v/; cpj.'^ + 9i'^ + a2(cp^2 ^ (p^2) d(y/6) (34) The energy dE of the secondary motion In a strip of width dy and length X is accordingly ^ = f|a,V V"-%'=--"( 0, and for neutral disturbances =0, the integration extending over the entire range of the particular flow. Participating on the variation of the secondary-motion energy are: first, the transfer of kinetic energy from the primary to the secondary flow, or vice versa; second, the pressure variation; and, third, dissipation. For neutral vibrations, the total energy balance is not only equal to zero for the entire space in question, but for every point y of the cross section, the energy 22 MCA TM 1265 increase per vibration period T = 23t/p is also equal to zero. This is easily confinned in the following manner: It is ^ ^(u'2 . V.2) 2jt=0^* dt 2)dt |Lu-2,,,2 + PU 1/0 u' -^^^ + v' I dt = ^x Sx The first term disappears by reason of the periodicity of u' and v' , The same holds true when the last term for u' and v' is entered according to equation (3O) . Thus, the energy increase per vibration period T Is equal to zero at every point x, y for a neutral vibration. It is interesting to see how the several factors enumerated above participate on the energy conversion in a specific case. For both specific cases of neutral disturbance the calculation of the energy- is carried out for a plane basic flow and a plane disturbance motion according to Lorentz (reference 12) Dt |(u'2 . v-2) -pu'v' ^ dy ^(u'p') ^ a(v'p') ^x Sy -(s^-rr^^{i<-^')-i<-4 where ^' = — - — , \i = coefficient of viscosity Sx By NACA TM 1265 23 The first term gives the transfer of energy from the primary to the secondary flow, the second gives the contribution resixlting from the pressure variations, and the third and fourth terms, the loss of energy by dissipation. After integration of this term with respect to y over the total width of the laminar flow from y = to y = " and with respect to x over a wave length X. of the disturbance, the second and foiorth terms disappear, since u' and v' disappear for y = and y = 00 and with respect to x have the period X. Thus, the growth of the energ/ per unit time in a layer of unit height and base area 02, {^, THE KINETIC ENERGY OF THE DISTUKBANCE MOTION u'^ + v'^, AND THE CORRELATION COEFFICIENT k AS FUNCTION OF y/5. EQUATIONS (31), (32), (33) - Concluded Second Neutral Vitratlon y/6 \iu'2 10 ^ .0= V' -^ m m .029 .661 .0655 .1+33 .054 .937 .211+ .869 .121 .071+ 1.038 .359 1.068 .170 .105 1.108 .595 1.218 .191 .157 1.127 1.028 1.262 .11+6 .209 1.086 l.i+U5 1.190 .076 .250 .998 1.755 1.019 .010 .290 .906 2.04 .854 -.015 .370 .686 2.50 .528 -.019 .1^51 .^Ok 2.87 .332 .531 .3^0 3.10 .208 .612 .205 3.26 .11+6 .693 .087 3.35 .118 .77^ .022 3.37 .117 .85U .123 3.33 .121+ .935 .216 3.22 .11+9 1.015 .305 . 3.11 .187 1.1 .292 2.925 .171 1.2 .272 2.72 .11+6 1.3 .252 2.53 .126 l.U .23i+ 2.35 .109 1.5 .218 2.18 .093 38 NACA TM 1265 TABLE 8 THE LOCAL ENERGY" CONVERSION l) = TRANSFER FROM ERIMART TO SECONDARY MOTION, 2) = DISSIPATION EQUATIONS (J+l) AND (I+3) First Neutral Vibration y/& e-^' X lo3 e^' X 103 E d.j '1 E .^^^)2 86.9 ^.78 .050 .268 31.8 .021 -2.1+8 .090 2.150 17.6 .168 -1.37 .130 12.25 10.8 .955 -.81+ .170 23.25 5.73 1.81)+ -.i^5 .209 28 2.6I1 2.18 -.21 .250 27.30 .06 2.13 .290 22.85 .72 1.78 -.05 .370 7.^9 2.20 .581+ -.17 .I151 1.885 2.80 .li+7 -.22 .531 -1.102 2.1+3 -.086 -.19 .612 2.36 -.18 .693 2.12 -.17 .77*+ 1.92 -.15 .851+ 1.75 -.11+ .935 1.61 -.13 1.015 1.50 -.12 NACA TM 1265 39 TABLE 8 THE LOCAL ENERGY CONVERSION l) = TRANSFER FROM ERJMARY TO SECONDARY MOTION, 2) = DISSIPATION [equations (Ul) A1\1D (43)] - Concluded Second Neutral Vibration y/& e^' X 10^ e^' X lo3 l¥<^>i l^(-). 320 -13.31 .029 1 83.6 -.044 -3.48 .054 7. 84 24.3 .326 -1.01 .otV 18.1+5 11.15 .768 -.464 .105 41.5 2.61 1.726 -.109 .157 55.6 .04 2.310 -.002 .209 37.5 .840 1.560 -.035 .250 5.22 2.31 .217 -.096 .290 7-97 2.01 -.331 -.084 .370 -8.44 1.91 -.351 -.079 .451 1.80 -.075 .531 1.38 -.057 .612 1.01 -.042 •693 .819 -.034 .774 .695 -.029 .851+ .608 -.025 .935 .520 -.022 1.015 .458 -.019 ko NACA TM 1265 Figure 1.- Laminar flow past the plate. 0.3 1 0.2 0.1 r ._ E Sfobk ' \ U, nsfable 1 ■^ ^ 1 S^a/>/e ^Theoretical stabili fy limii 6 Um^* ^W^^ Figure 2.- The zone of the stable and unstable disturbances of plate flow. I = first neutral vibration, n - second neutral vibration. NACA TM 1265 kl 1 1 ^ txi 'Ifr fr / + — ■ 1 1 \ X ^' y,-' ao2 t/1 r 1 1 1 > / \ N - Q2 y / X <. '. ^ ^/ 1 ^ X s ' r- 2 ^ X4 1 £ 0.8 ^ ^^ 'OOP 0.2- 1 --0.7 1.0 I 0.5 -0.6 Figures.- Real and imaginary part v ^ '^ ' 0.4t 0.8 ,.2 -_ ^ ,6 Figure 7.- The mean kinetic energy of the disturbance motion u'*^ + v''^/u plotted against the wall distance for both neutral vibrations. m 0.20 0.15 0.10 0.06 '005 1 1 \ ^\ V 1 \ 1 \ i\ V y ^^^ / 0.1 OS \0^ 3 t-"c 5 1 Figure 8,- The correlation coefficient k - ^u'2.v'2 for both neutral vibrations. plotted against y/e kh NACA TM 1265 15.0 10.0 5.0 -2.5 iim.t r" " ' 1 \ll(2) \| V 1(2) - y >^ ^) 0.6 0.8 1 LO Figure 9.- The local energy conversion of the secondary motion for the first and second neutral vibration. I (1), n (1) = energy transfer from primary to secondary flow; I (2), U (2) = dissipation. NACA-Langley - 4-18-50 -950 •p u cd U +^ m 4J ^ XJ S UNIVERSITY OF FLORIDA 3 1262 08105 023 8 ^,^,,„ ..•FLORIDA BoOUMiNTS DEPARTMENT iaO N/.ARSTON SCIENCE LIBRARY P.O. BOX 117011 GAlNiSVILLE, FL 32611-7011 USA