058:0160 Professor Fred Stern Fall 2009 Chapter 8 1 Chapter 8: Inviscid Incompressible Flow: a Useful Fantasy 8.1 Introduction For high Re external flow about streamlined bodies viscous effects are confined to boundary layer and wake region. For regions where the B.L is thin i.e. favorable pressure gradient regions, Viscous/Inviscid interaction is weak and traditional B.L theory can be used. For regions where B.L is thick and/or the flow is separated i.e. adverse pressure gradient regions more advanced boundary layer theory must be used including viscous/Inviscid interactions. For internal flows at high Re viscous effects are always important except near the entrance. Recall that vorticity is generated in regions with large shear. Therefore, outside the B.L and wake and if there is no upstream vorticity then ω=0 is a good approximation. Note that for compressible flow this is not the case in regions of large entropy gradient. Also, we are neglecting noninertial effects and other mechanisms of vorticity generation. Potential flow theory 1) Determine from solution to Laplace equation 2 0 B.C: at S B : V .n 0 at S : V 0 n Note: F: Surface Function 1 058:0160 Professor Fred Stern Chapter 8 2 Fall 2009 DF F 1 F 0 V .F 0 V .n Dt t F t for steady flow V .n 0 2) Determine V from V and p(x) from Bernoulli equation Therefore, primarily for external flow application we now consider inviscid flow theory ( 0 ) and incompressible flow ( const ) Euler equation: .V 0 DV p g Dt V V .V ( p z ) t V2 V .V V 2 Where : V vorticity 2 fluid angular velocity V 1 ( p V 2 z ) V t 2 If 0 ie V 0 then V : 1 p z B(t ) t 2 Bernoulli’s Equation for unsteady incompressible flow, not f(x) Continuity equation shows that GDE for is the Laplace equation which is 2nd order linear PDE ie superposition principle is valid. (Linear combination of solution is also a solution) V 2 0 1 2 2 0 2 0 2 (1 2 ) 0 21 22 0 2 1 2 0 Techniques for solving Laplace equation: 1) superposition of elementary solution (simple geometries) 2) surface singularity method (integral equation) 3) FD or FE 4) electrical or mechanical analogs 5) Conformal mapping ( for 2D flow) 6) Analytical for simple geometries (separation of variable etc) 2 058:0160 Professor Fred Stern Fall 2009 Chapter 8 3 8.2 Elementary plane-flow solutions: Recall that for 2D we can define a stream function such that: u y v x z vx u y ( x ) ( y ) 2 0 x y i.e. 2 0 Also recall that and are orthogonal. u y x v x y d x dx y dy udx vdy d x dx y dy vdx udy i.e. dy u 1 dx const v dy dx const 8.2 Elementary plane flow solutions Uniform stream u U y x const v 0 x y Ux U y Note: 2 2 0 is satisfied. V Uiˆ i.e. Say a uniform stream is at an angle to the x-axis: 3 058:0160 Professor Fred Stern u U cos Chapter 8 4 Fall 2009 y x v U sin x y After integration, we obtain the following expressions for the stream function and velocity potential: U y cos x sin U x cos y sin 2D Source or Sink: Imagine that fluid comes out radially at origin with uniform rate in all directions. (singularity in origin where velocity is infinite) Consider a circle of radius r enclosing this source. Let vr be the radial component of velocity associated with this source (or sink). Then, form conservation of mass, for a cylinder of radius r, and unit width perpendicular to the paper, L3 Q V d A A S Q 2 r b vr Or , vr Q 2 br m , v 0 r Q Where: m is the convenient constant with unit velocity × length 2 b (m>0 for source and m<0 for sink). Note that V is singular at (0,0) since vr vr In a polar coordinate system, for 2-D flows we will use: 1 V r r 4 058:0160 Professor Fred Stern Chapter 8 5 Fall 2009 And: .V 0 1 1 (rvr ) (v ) 0 r r r i.e.: 1 r r 1 v Tangential velocity r r Such that V 0 by definition. v r Radial velocity Therefore, m 1 r r r 1 v 0 r r vr m ln r m ln x 2 y 2 i.e. m m tan 1 y x Doublets: The doublet is defined as: ψ m( 1 2 ) 1 2 sink source sink source m tan θ tan θ 1 2 tan (θ θ ) tan ( ) 1 2 m 1 tan θ tan θ 1 2 5 058:0160 Professor Fred Stern Chapter 8 6 Fall 2009 r sin r sin ; tan 2 r cos a r cos a r sin r sin 2ar sin tan( ) r cos a r cos a 2 r sin m 1 r sin r a2 r cos a r cos a tan 1 For small value of a 2ar sin 2amy y ) 2 2 2 2 r a r x y2 cos 2am ( Doublet Strength) a 0 lim m tan 1 ( r By rearranging: y 2 ψ 2 x2 (y ) ( )2 2 2 2 x y It means that streamlines are circles with radius R and center at (0, -R) i.e. circles 2 are tangent to the origin with center on y axis. The flow direction is from the source to the sink. 6 058:0160 Professor Fred Stern Chapter 8 7 Fall 2009 2D vortex: Suppose that value of the and for the source are reversal. vr 0 1 K r r r Purely recirculating steady motion, i.e. v f r . integration results in: Kθ ψ K ln r K=constant 2D vortex is irrotational everywhere except at the origin where V and V are infinity. v Circulation Circulation is defined by: For irrotational flow Γ V d s c C closed contour Or by using Stokes theorem: ( if no singularity of the flow in A) Γ V d s V d A .ndA 0 c A A Therefore, for potential flow 0 in general. However, this is not true for the point vortex due to the singular point at vortex core where V and V are infinity. If singularity exists: Free vortex 2 v eˆ rd eˆ 0 2 0 V ds K r K (rd ) 2 K and K r 2 7 058:0160 Professor Fred Stern Chapter 8 8 Fall 2009 Note: for point vortex, flow still irrotational everywhere except at origin itself where V, i.e., for a path not including (0,0) 0 Also, we can use Stokes theorem to show the existence of : V ds ABC V d s C Since AB'C V .d s 0 ABCB' A Therefore in general for irrotational motion: V .d x V d x d d x d dx . ds ds ds dx eˆs ds (V ).eˆs 0 V Where: e s =unit tangent vector along curve x Since e s is not zero we have shown: V i.e. velocity vector is gradient of a scalar function if the motion is irrotational. ( V ds 0 ) The point vortex singularity is important in aerodynamics, since, extra source and sink can be used to represent airfoils and wings and we shall discuss shortly. To see this, consider as an example: an infinite row of vortices: 1 2y 2x 1 K ln ri K ln (cosh cos ) 2 a a 2 i 1 Where ri is radius from origin of ith vortex. Equally speed and equal strength (Fig 8.11 of Text book) 8 058:0160 Professor Fred Stern For y Fall 2009 Chapter 8 9 a the flow approach uniform flow with K y a +: below x axis -: above x axis Note: this flow is just due to infinite row of vortices and there isn’t any pure uniform flow u Vortex sheet: From afar (i.e. y a ) looks that thin sheet occurs which is a velocity discontinuity. 2K strength of vortex sheet a 2K d u l dx u u dx (u l u u )dx dx a d i.e. =Circulation per unit span dx Note: There is no flow normal to the sheet so that vortex sheet can be used to simulate a body surface. This is beginning of airfoil theory where we let (x ) to represent body geometry. Define Vortex theorem of Helmholtz: (important role in the study of the flow about wings) 1) The circulation around a given vortex line is constant along its length 2) A vortex line cannot end in the fluid. It must form a closed path, end at a boundary or go to infinity. 3) No fluid particle can have rotation, if it did not originally rotate Circular cylinder (without rotation): In the previous we derived the following equation for the doublet: 9 058:0160 Professor Fred Stern Chapter 8 10 Fall 2009 y Doublet sin x y r When this doublet is superposed over a uniform flow parallel to the x- axis, we get: 2 2 1 U 1 r sin 2 r U r Where: doublet strength which is determined from the kinematic body boundary condition that the body surface must be a stream surface. Recall that for inviscid flow it is no longer possible to satisfy the no slip condition as aresult of the neglect of viscous terms in PDEs. U r sin sin The inviscid flow boundary condition is: F: Surface Function DF F 1 F 0 V .F 0 V n 0 (for steady flow) Dt t F t Therefore at r=R, V.n=0 i.e. vr 0 r R . F F eˆr eˆ F r eˆr V vr eˆr v eˆ , n F Fr2 F2 V n vr 1 U 1 cos =0 2 r U r U R2 If we replace the constant by a new constant R2, the above equation becomes: U R2 r sin 2 r This radial velocity is zero on all points on the circle r=R. That is, there can be no velocity normal to the circle r=R. Thus this circle itself is a streamline. U 1 We can also compute the tangential component of velocity for flow over the circular cylinder. From equation, R2 v U 1 2 sin r r On the surface of the cylinder r=R, we get the following expression for the tangential and radial components of velocity: v 2U sin 10 058:0160 Professor Fred Stern Chapter 8 11 Fall 2009 vr 0 How about pressure p? look at the Bernoulli's equation: p p 1 2 1 vr v 2 U 2 2 2 After some rearrangement we get the following non-dimensional form: vr 2 v 2 p p C p r , 1 1 U 2 U 2 2 For the circular cylinder being studied here, at the surface, the only velocity component that is non-zero is the tangential component of velocity. Using v 2U sin , we get at the cylinder surface the following expression for the pressure coefficient: C p 1 4 sin 2 Where is the angle measured from the rear stagnation point (at the intersection of the back end of the cylinder with the x- axis). Cp Cp over a Circular Cylinder 1.5 1 0.5 0 -0.5 0 -1 -1.5 -2 -2.5 -3 -3.5 30 60 90 120 150 180 210 240 270 300 330 360 Theta, Degrees From pressure coefficient we can calculate the fluid force on the cylinder: 1 F ( p p )nds U 2 C p ( R, )nds 2 A A ds ( Rd )b b=span length 2 1 F U 2 bR (1 4sin 2 )(cos iˆ sin ˆj )d 2 0 11 058:0160 Professor Fred Stern Lift Fall 2009 Chapter 8 12 2 F ˆj = (1 4 sin 2 ) sin d 0 (due to symmetry of flow 1 1 0 U 2 bR U 2 bR 2 2 around x axis) 2 Drag F iˆ = (1 4 sin 2 ) cos d 0 (dÁlembert paradox) CF 1 1 0 U 2 bR U 2 bR 2 2 We see that C L C D 0 is due to symmetry of Cp. But how realistic is this potential flow solution. We started explain that viscous effects were confined to thin boundary layer and it has negligible effect on the inviscid flow for high Rn flow about streamlined bodies. A circular cylinder is not a streamlined body (like as airfoil) but rather a bluff body. Thus, as we shall determine now the potential flow solution is not realistic for the back portion of the circular cylinder flows ( 90) . For general: CD CD C DSKIN FRICTION CL FORM DRAG CD : drag due to viscous modification of pressure destruction FORM DRAG CDSKIN FRICTION : Drag due to viscous shear stress Streamlined Body : CDSK CD FO Bluff Body :CD FO CDSK Circular cylinder with circulation: The stream function associated with the flow over a circular cylinder, with a point vortex of strength placed at the cylinder center is: sin U r sin ln r r 2 From V.n=0 at r=R: U R 2 Therefore, U r sin U R 2 sin ln r r 2 The radial and tangential velocity is given by: R2 1 vr U 1 2 cos r r R2 U 1 2 sin r r 2 r On the surface of the cylinder (r=R): R2 1 vr U 1 2 cos 0 r R v 12 058:0160 Professor Fred Stern Chapter 8 13 Fall 2009 v 2U sin r 2 R Next, consider the flow pattern as a function of . To start lets calculate the stagnation points on the cylinder i.e.: v 2U sin 0 2 R K sin /2 4 U R 2U R K Note: K 2 U R So, the location of stagnation point is function of . K U R 2 U R 0 ( sin 0 ) 1( sin 0.5 ) 2 ( sin 1 ) >2( sin 1 ) s (stagnation point) 0,180 30,150 90 Is not on the circle but where vr v 0 For flow patterns like above (except a), we should expect to have lift force in –y direction. Summary of stream and potential function of elementary 2-D flows: In Cartesian coordinates: 13 058:0160 Professor Fred Stern Chapter 8 14 Fall 2009 u y x v x y In polar coordinates: 1 vr r r 1 v r r Flow Uniform Flow Source (m>0) Sink (m<0) Doublet U x m ln r cos r Vortex 90 Corner flow Solid-Body rotation K 1 / 2 A( x 2 y 2 ) Doesn’t exist U y m sin r - K ln r Axy 1 2 r 2 These elementary solutions can be combined in such a way that the resulting solution can be interpreted to have physical signification;that is. Represent the potential flow solution for various geometers. Also, methods for arbitrary geometries combine uniform stream with distribution of the elementary solution on the body surface. Some combination of elementary solutions to produce body geometries of practical importance Body name Elemental combination Flow Patterns Rankine Half Body Uniform stream+source Rankine Oral Uniform stream+source+sink Kelvin Oral Uniform stream+vortex point 14 058:0160 Professor Fred Stern Chapter 8 15 Fall 2009 Circular Cylinder without circulation Uniform stream+doublet Circular Cylinder with circulation Uniform stream+doublet+vortex Keep in mind that this is the potential flow solution and may not well represent the real flow especially in region of adverse px. The Kutta – Joukowski lift theorem: Since we know the tangential component of velocity at any point on the cylinder (and the radial component of velocity is zero), we can find the pressure field over the surface of the cylinder from Bernoulli’s equation: p vr2 v2 p U 2 2 2 2 Therefore: 2 U 1 2 1 2 2 p p U 2U sin p U 2 U 2 sin 2 sin 2 2 2 2 R 2 8 R R A B sin C sin 2 where 1 2 2 A p U 2 2 2 8 R U B R C 2 U 2 Calculation of Lift: Let us first consider lift. Lift per unit span, L (i.e. per unit distance normal to the plane of the paper) is given by: L pdx pdx Lower upper 15 058:0160 Professor Fred Stern Chapter 8 16 Fall 2009 On the surface of the cylinder, x = Rcos. Thus, dx = -Rsind, and the above integrals may be thought of as integrals with respect to . For the lower surface, varies between and 2. For the upper surface, varies between and 0. Thus, 2 0 L R A B sin C sin sin d R A B sin C sin 2 sin d 2 Reversing the upper and lower limits of the second integral, we get: 2 2 L R A B sin C sin 2 sin d R A sin B sin 2 C sin 3 d BR 0 0 Substituting for B ,we get: L u This is an important result. It says that clockwise vortices (negative numerical values of ) will produce positive lift that is proportional to and the free stream speed with direction 90 degrees from the stream direction rotating opposite to the circulation. Kutta and Joukowski generalized this result to lifting flow over airfoils. Equation L u is known as the Kutta-Joukowski theorem. Drag: We can likewise integrate drag forces. The drag per unit span, D, is given by: D pdy pdy Front rear Since y=Rsin on the cylinder, dy=Rcosd. Thus, as in the case of lift, we can convert these two integrals over y into integrals over . On the front side, varies from 3/2 to /2. On the rear side, varies between 3/2 and /2. Performing the integration, we can show that D0 This result is in contrast to reality, where drag is high due to viscous separation. This contrast between potential flow theory and drag is the dÁlembert Paradox. The explanation of this paradox are provided by Prandtl (1904) with his boundary layer theory i.e. viscous effects are always important very close to the body where the no slip boundary condition must be satisfied and large shear stress exists which contributes the drag. Lift for rotating Cylinder: We know that L U therefore: L CL 1 U 2 (2 R) U R 2 16 058:0160 Professor Fred Stern Define: v Average CL 1 2 Chapter 8 17 Fall 2009 2 1 v d 2 R Note: Γ V d s V d A V Rd 0 c c c 2 v U averagfe Velocity ratio: a U Theoretical and experimental lift and drag of a rotating cylinder Experiments have been performed that simulate the previous flow by rotating a circular cylinder in a uniform stream. In this case v R which is due to no slip boundary condition. - Lift is quite high but not as large as theory (due to viscous effect ie flow separation) - Note drag force is also fairy high Fletttern (1924) used rotating cylinder to produce forward motion. 17 058:0160 Professor Fred Stern Fall 2009 Chapter 8 18 18 058:0160 Professor Fred Stern Fall 2009 Chapter 8 19 19 058:0160 Professor Fred Stern Fall 2009 Chapter 8 20 8.3 Method of Images The method of image is used to model “slip” wall effects by constructing appropriate image singularity distributions. Plane Boundaries: 2-D: m 2 2 ln x 1 y 2 x 1 y 2 2 1 1 2 2 2 2 3-D: M x 1 y 2 z 2 x 1 y 2 z 2 Similar results can be obtained for dipoles and vortices: 20 058:0160 Professor Fred Stern Chapter 8 21 Fall 2009 Spherical and Curvilinear Boundaries: The results for plane boundaries are obtained from consideration of symmetry. For spherical and circular boundaries, image systems can be determined from the Sphere & Circle Theorems, respectively. For example: Flow field Source of strength M at c outside sphere of radius a, c>a Dipole of strength at l outside sphere of radius a, l>a Source of strength m at b outside circle of radius a, b>a Image System 2 Sources of strength ma at a and line c c sink of strength m extending from center a 2 of sphere to a c 3 2 dipole of strength a at a l l 2 equal source at a and sink of same b strength at the center of the circle 21 058:0160 Professor Fred Stern Fall 2009 Chapter 8 22 Multiple Boundaries: The method can be extended for multiple boundaries by using successive images. (1) For example, the solution for a source equally spaced between two parallel planes w( z ) m ln z 4n a ln z 4n 2 a m 0 , 1, 2 , mln z a ln z 2 a ln z 4 a ln z 6 a ln z 4 a ln z 2 a 22 058:0160 Professor Fred Stern Chapter 8 23 Fall 2009 (2) As a second example of the method of successive images for multiple boundaries consider two spheres A and B moving along a line through their centers at velocities U1 and U2, respectively: Consider the kinematic BC for A: 2 F x, t x yt y 2 z 2 a 2 DF 0 V eˆR U1kˆ eˆR or R U1 cos Dt 2 Ua 3 where 2 cos , R 3 cos R R 2 Similarly for B R U 2 cos ' This suggests the potential in the form U11 U 22 where 1 and 2 both satisfy the Laplace equation and the boundary condition: 1 1 0 cos , R R a R ' R 'b 2 2 cos ' 0, R R a R ' R 'b (*) (**) 1 = potential when sphere A moves with unit velocity towards B, with B at rest 23 058:0160 Professor Fred Stern Chapter 8 24 Fall 2009 2 = potential when sphere B moves with unit velocity towards A, with A at rest If B were absent. 1 0 a3 a3 , cos cos 0 2R2 R2 2 but this does not satisfy the second condition in (*). To satisfy this, we introduce the image of 0 in B, which is a doublet 1 directed along BA at A1, the inverse point of A with respect to B. This image requires an image 2 at A2, the inverse of A1 with respect to A, and so on. Thus we have an infinite series of images A1, A2, … of strengths 1 , 2 , 3 etc. where the odd suffixes refer to points within B and the even to points within A. Let f n AAn & AB c b2 a2 b2 , f2 , f3 c ,… f1 c c f2 c f1 a3 b3 b3 ,… 1 0 3 , 2 1 3 , 3 2 3 c f1 c f 2 radius 3 where 1 = image dipole strength, 0 = dipole strength sistance 3 cos cos cos 1 0 2 1 2 1 2 2 2 with a similar development procedure for 2. R R1 R2 Although exact, this solution is of unwieldy form. Let’s investigate the possibility of an approximate solution which is valid for large c (i.e. large separation distance) 2c c2 R '2 R 2 c 2 2cr cos R 2 1 cos 2 R R 1 1 c c 1 2 cos 2 R' R R R 2 1 2 1 R R 1 2 cos 2 c c c 2 1 2 24 058:0160 Professor Fred Stern Chapter 8 25 Fall 2009 Considering the former representation first defining 1 1 1 2u 2 R' R By the binomial theorem valid for x 1 1 x 2 1 c and u cos R 1 2 0 1 x 2 x 2 3 x 3 , 0 1 and n 1 3 2n 1 2 4 2n Hence if 2u 2 1 2 1 0 1 2u 2 2 2 P0 u P1 u P2 u 2 After collecting terms in powers of , where the Pn are Legendre functions of the first kind (i.e. Legendre polynomials which are Legendre functions of the first kind of order zero). Thus, 1 1 R R2 R C : 2 P1 cos 3 P2 cos R' c c c 1 1 c c2 R C : 2 P1 cos 3 P2 cos R' R R R Next, consider a doublet of strength at A 1 3 c R 2 c 2 2cR cos R 2 c 2 2cR cos 2 Thus, 1 2 RP1 cos 3R 2 P2 cos cos R c : 2 R '2 c3 c c cos R '2 R cos c 1 2c 3c 2 R c : 2 P1 cos 3 P2 cos 4 P3 cos R R R 1 2 Going back to the two sphere problem. If B were absent 1 a3 cos 2R2 R' using the above expression for the origin at B and near B 1 , RR’, ' c 25 058:0160 Professor Fred Stern Chapter 8 26 Fall 2009 1 a3 a 3 R ' P1 cos a3 2 cos 2 3 2R c 2 c 3 a cos R c3 which can be cancelled by adding a term to the first approximation, i.e. 1 a3 cos 1 a3b3 cos ' 1 2 R2 2 c3 R '2 to confirm this 1 a3 a3R 'cos ' 1 a3b3 cos 1 2 2c c3 2 c3 R 1 ' a 3 cos ' a 3b3 cos ' ( R b) 3 0 hot 3 R ' c3 c R' Similarly, the solution for f2 is 2 1 b3 cos ' 1 a 3b3 cos 2 2 R' 2 c3 R 2 These approximate solutions are converted to c 3 . To find the kinetic energy of the fluid, we have 1 K n dS n dS 2 S A SB 1 K A11U12 A12U1U 2 A22U 22 n dS 2 2 S A SB A11 1 A 1 dS A , A22 2 2 dS B , A12 2 1 dS A 1 1 dS B n n n n A B B where dS 2 R 2 sin d 2 2 2 a 3b3 A11 a 3 , A12 , A22 b 3 , 3 3 3 c 3 3 1 2 a b 1 K M '1 U12 U1U 2 M '2 U 22 : using the approximate form of the potentials 3 4 c 4 1 1 where M '1 U12 , M '2 U 22 : masses of liquid displaced by sphere. 4 4 8.4 Complex variable and conformal mapping 26 058:0160 Professor Fred Stern Chapter 8 27 Fall 2009 This method provides a very powerful method for solving 2-D flow problems. Although the method can be extended for arbitrary geometries, other techniques are equally useful. Thus, the greatest application is for getting simple flow geometries for which it provides closed form analytic solution which provides basic solutions and can be used to validate numerical methods. Function of a complex variable Conformal mapping relies entirely on complex mathematics. Therefore, a brief review is undertaken at this point. A complex number z is a sum of a real and imaginary part; z = real + i imaginary i 1 The term i, refers to the complex number i 1, i 1, i i, i 1 2 so that; 3 4 Complex numbers can be presented in a graphical format. If the real portion of a complex number is taken as the abscissa, and the imaginary portion as the ordinate, a twodimensional plane is formed. z = real +i imaginary = x + iy y, imaginary x, real -A complex number can be written in polar form using Euler's equation; z = x + iy = rei = r(cos + isin) Where: r2 = x2 + y2 - Complex multiplication: z1z2 = (x1+iy1)(x2+iy2) = (x1x2 - y1y2) + i(x1y2 + y1x2) r1e i1 r2 e i 2 r1r2 e i (1 2 ) - Conjugate: z = x + iy z x iy z.z x 2 y 2 -Complex function: w(z) = f(z)= (x,y) + i (x,y) 27 058:0160 Professor Fred Stern Fall 2009 Chapter 8 28 If function w(z) is differentiable for all values of z in a region of z plane is said to be regular and analytic in that region. Since a complex function relates two planes, a point can be approached along an infinite number of paths, and thus, in order to define a unique derivative f(z) must be independent of path. PP1( y 0) : w w1 w 1 i 1 ( i ) z z1 z x1 x dw x i x dz 1 Note : w1 1 ( x x, y ) i 1 ( x x, y ) w w2 w 2 i 2 ( i ) PP 2( x 0) : z z2 z i ( y2 y ) dw i y y dz 2 dw to be unique and independent of path: dz x y and y x Cauchy Riemann Eq. For Recall that the velocity potential and stream function were shown to satisfy this relationship as a result of their othogonality. Thus, complex function w i represents 2-D flows. xx yx yy xy i.e. xx yy 0 and similarly for Therefore if analytic and regular also harmonic, i.e., satisfy Laplace equation. 28 058:0160 Professor Fred Stern Fall 2009 Chapter 8 29 Application to potential flow w( z ) i Complex potential where : velocity potential, : stream function dw x i x u iv ur iu e i Complex velocity dz r ' e i ' re i ( ) where r ' r (magnification) and ' (rotation) Triangle about z0 is transformed into a similar triangle in the ζ-plane which is magnified and rotated. Implication: -Angles are preserved between the intersections of any two lines in the physical domain and in the mapped domain. -The mapping is one-to-one, so that to each point in the physical domain, there is one and only one corresponding point in the mapped domain. For these reasons, such transformations are called conformal. 29 058:0160 Professor Fred Stern Fall 2009 Chapter 8 30 Usually the flow-field solution in the ζ-plane is known: W ( ) ( , ) i ( , ) Then w( z) W f z ( x, y) i ( x, y) or & Conformal mapping The real power of the use of complex variables for flow analysis is through the application of conformal mapping: techniques whereby a complicated geometry in the physical z-domain is mapped onto a simple geometry in the ζ-plane (circular cylinder) for which the flow-field solution is known. The flow-field solution in the z-plane is obtained by relating the ζ-plane solution to the z-plane through the conformal transformation ζ=f(z) (or inverse mapping z=g(ζ)). Before considering the application of the technique, we shall review some of the more important properties and theorems associated with it. Consider the transformation, ζ=f(z) where f(z) is analytic at a regular point Z0 where f’(z0)≠0 δζ= f’(z0) δz r ' e i ' , z rei , f ' z 0 e i The streamlines and equipotential lines of the ζ-plane (Φ, Ψ) become the streamlines of equipotential lines of the z-plane (, ψ). 30 058:0160 Professor Fred Stern 2z 2 0 2z 2 0 Chapter 8 31 Fall 2009 i.e. Laplace equation in the z-plane transforms into Laplace equation is the ζ-plane. The complex velocities in each plane are also simply related dw dw d dw ' f ( z) dz d dz d dw dW ( z ) u iv (U iV ) f '( z ) ( f ( z )) dz d i.e. velocities in two planes are proportional. Two independent theorems concerning conformal transformations are: (1) Closed curves map to closed curves (2) Rieman mapping theorem: an arbitrary closed profile can be mapped onto the unit circle. More theorems are given and discussed in AMF Section 43. Note that these are for the interior problems, but we equally valid for the exterior problems through the inversion mapping. Many transformations have been investigated and are compiled in handbooks. The AMF contains many examples: 1) Elementary transformations: az b , ad bc 0 a) linear: w cz d b) corner flow: w Az n 2 c) Jowkowsky: w c d) exponential: w e e) w z s , s irational n 2) Flow field for specific geometries a) circle theorem b) flat plate c) circular arc d) ellipse e) Jowkowski foils f) ogive (two circular areas) 31 058:0160 Professor Fred Stern Fall 2009 Chapter 8 32 g) Thin foil theory [solutions by mapping flat plate with thin foil BC onto unit circle] h) multiple bodies 3) Schwarz-Cristoffel mapping 4) Free-streamline theory The techniques of conformal mapping are best learned through their applications. Here we shall consider corner flow. A simple example: Corner flow 1. In ζ-plane, let W ( ) i.e. uniform stream 2. Say f ( z ) z 3. w( z ) W ( f ( z )) z i.e. corner flow Note that 1-3 are unit uniform stream. w( z ) Uz n UR n cos iUR n sin n , where z Re i i.e. UR n cos n , UR n sin n UR n sin n =const.=streamlines UR n cos n =const.=equipotentials dw dW d nUz n 1 nUR n 1ei ( n 1) (nUR n 1 cos n inUR n 1 sin n )e i dz d dz (ur iu )ei 32 058:0160 Professor Fred Stern Chapter 8 33 Fall 2009 u r nUR n1 cos n u nUR n1 sin n 2n u 0 , u 0 2n n u 0 , u 0 0 r r i.e. w( z ) Uz n represents corner flow: n=1uniform stream, n=290° corner 8.5 Introduction to Surface Singularity methods (also known as Boundary Integral and Panes Methods) Next, we consider the solution of the potential flow problem for an arbitrary geometry. Consider the BVP for a body of arbitrary geometry fixed in a uniform stream of an inviscid, incompressible, and irrotational fluid. The surface singularity method is founded on the symmetric form of Greens theorem and what is known as Greens function. G G dV 2 V 2 G G dS n n S S S B S S (1) where Φ and G are any two scalar field in V (control volume bounded by s infinity S body and S inserted to reder the domain simply connected) and for our application. Φ= velocity potential G= Green’s function 33 058:0160 Professor Fred Stern Chapter 8 34 Fall 2009 Say, 2 G ( x x0 ) in V+V’ (i.e. entire domain) where δ is the Dirac delta function. G0 on S∞ Solution for G (obtained Fourier Transforms) is: G ln r , r x x0 , i.e. elementary 2-D source at x x0 of unit strength, and (1) becomes G G dS n n S SB First term in integrand represents source distribution and second term dipole distribution, which can be transformed to vortex distribution using integration by parts. By extending the definition of Φ into V’ it can be shown that Φ can be represented by distributions of sources, dipoles or vortices, i.e. GdS : source distribution, : source strength S SB or S SB G dS : dipole distribution, : dipole strength n Also, it can be shown that a source distribution representation can only be used to represent the flow for a non-lifting body; that is, for lifting flow dipole or vortex distributions must be used. As this stage, let’s consider the solution of the flow about a non-lifting body of arbitrary geometry fixed in a uniform stream. Note that since G0 on S∞ Φ already satisfy the condition S∞. The remaining condition, i.e. the condition is a stream surface is used to determine the source distribution strength. Consider a source distribution method for representing non-lifting flow around a body of arbitrary geometry. 34 058:0160 Professor Fred Stern Chapter 8 35 Fall 2009 V U : total velocity U : uniform stream, : perturbation potential due to presence of body U U (cos iˆ sin ˆj ) : note that for non-lifting flow must be zero (i.e. for a symmetric foil 0 or for cambered filed oLift ) K 2 ln rds : source distribution on body surface SB Now, K is determined from the body boundary condition. U n V n 0 i.e. U n n 0 or n i.e. normal velocity induced by sources K stream ln rds U n n SB 2 must cancel uniform This singular integral equation for K is solved by descretizing the surface into a number of panels over which K is assumed constant, i.e. we write ni where rij x M no. of panels j 1 Si ln rij dSi U ni , i=1,M, j=1,M x j z i z j =distance from ith panel control point to rj position 2 i Kj 2 2 vector along jth panel. Note that the integral equation is singular since 1 rij ln rij ni rij ni 35 058:0160 Professor Fred Stern Chapter 8 36 Fall 2009 at for rij 0 this integral blows up; that is, when i=j and we trying to determine the contribution of the panel to its own source strength. Special care must be taken. It can be shown that the limit does exist at the integral equation can be written ki 2 ni M K j Ki 2 i 1 2 j i where S j Si ln rij dS i ki 2 1 rij dS j U ni ij nij r Si rij 1 rij 1 1 rij 1 i rij ni n xi n zi 2 xi x j n xi z i z j n zi rij ni rij rij xi z i rij where rij2 xi x j z i z j 2 2 36 058:0160 Professor Fred Stern Fall 2009 Chapter 8 37 Consider the ith panel S i cos i iˆ sin i ˆj , ni S i ˆj sin i iˆ cos i ˆj n xi sin i , n zi cos i K ln rds U n n SB 2 r j r j 0 S S i , r j 0 : origin of jth panel coordinate system, S Si : distance along jth panel V U 37 058:0160 Professor Fred Stern Chapter 8 38 Fall 2009 K 2 ln rds SB K ln rds U n n SB 2 V n 0 Ki M K j 2 i 1 2 j i 1 rij dS j U ni U sin i , ni sin i iˆ cos i ˆj ij nij r Si 1 rij dS j I j and RHS i U sin i , then ij nij r Let Si xi x j n xi zi z j n zi Ki M K j dS j I j RHS i , I j 2 2 2 i 1 2 x x z z Sj i j i j j i x x S n n z z S n n dS x x S n z z S n x x n z z n S n n n n x x z z 2S n x x n z z S Ii li i j0 j zj xi i j0 li i i 0 j j0 j xj j0 zi j 2 zj i xi j0 i 2 0 j j0 zi xj j xj zi zj xi 2 j0 i CS j D li i 2 0 S 2j 2 AS j B j0 j zi i j0 zj i j0 2 j dS j dS j where A cos j xi x j 0 sin j z i z j 0 B xi x j 0 z i z j 0 2 2 C sin i j D xi x j 0 sin i z i z j 0 cos i li S 1 dS j C i dS j DI i1 CI i 2 where S 2j 2 AS j B 0 0 I j1 depends on if q<0 or >0 where q 4B 4 A2 I j D I j2 li 1 ln AI i1 2 Ki M K j 2 i 1 2 j i x x n z x x z i j xi i 2 Sj i j z j n zi zj 2 i dS j U ni RHS i RHS i U cos sin i sin cos i U sin i 38 058:0160 Professor Fred Stern Chapter 8 39 Fall 2009 Ki M K j I i RHS i : Matrix equation for Ki and can be solved using Standard methods 2 i 1 2 j i such as Gauss-Siedel Iteration. In order to evaluate Ij, we make the substitution x j x j 0 S j S xj rj rj0 S j S j z j z j 0 S j S xj where Sj= distance along the jth panel 0 S j l i S xj n zi cos j S zj n xi sin j After substitution, Ij becomes B A 2 xi x j 0 z i z j 0 2 2 cos 2 j xi x j 0 sin 2 j z i z j 0 2 cos j sin j xi x j 0 z i z j 0 2 2 xi x j 0 1 cos 2 j z i z j 0 1 sin 2 j 2 2 2 q 4 B A 2 4 xi x j 0 sin i z i z j 0 cos i i.e. q>0 and as a result, 2S 2 A 1 S A 2 I j1 tan 1 i tan 1 i where q 2 B A 2 2 E E E q q 2 C 1 I j DI j1 C ln AI j1 D CAI j1 ln l0i 2 2 D CA tan 1 li A tan 1 A C ln l j z 2 Al j B E E E 2 B where Si2 2 AS j B Therefore, we can write the integral equation in the form 39 058:0160 Professor Fred Stern Chapter 8 40 Fall 2009 Ki M K j I j U sin i 2 i 1 2 j i 1 2 kj 2 I j Ij 2 1 2 kj K = RHS i i which can be solved by standard techniques for linear systems of equations with GaussSiedel Iteration. Once Ki is known, V U And p is obtained from Bernoulli equation, i.e. V V p 1 2 U Mentioned potential flow solution only depend on is independent of flow condition, i.e. U∞, i.e. only is scaled On the surface of the body Vn=0 so that V2 C p 1 S2 where VS V S =tangential surface velocity U VS S U S S U cos i QS S where U S i U cos iˆ sin ˆj cos iiˆ sin i ˆj VSi U S i S S S M S i j 1 j i K 2 ln rds SB ln r dS 2 S Kj ji lj j : j=i term is zero since source panel induces no tangential i flow on itself. ( lj ln r ji dS j J j ) S i ln rij 1 rij 1 i rij S i S i rij S rij rij rij 1 S S zi 2 xi x j S xi z i z j S zi xi z i xi rij where S xi cos i , S zi sin i 1 rij 40 058:0160 Professor Fred Stern VS C pi 1 i U li x li 0 Fall 2009 2 K , V U cos i i J j j 1 2 i j xi x j n xi z i z j n zi 1 rij dS j dS j 2 2 rij S S j x i x j z i z j J ij Chapter 8 41 x j 0 S j S xj S xi z i z j 0 S j S zxj S zi i x x j 0 S j S xj z i z j 0 S j S zj 2 i 2 dS j where S xi cos i , S zi sin i , xi x j 0 S j S xj z i z j 0 S j S zj S 2j 2 AS j B 2 x 2 x j cos i z i z i 0 sin i S j S xj S xi S zj S zi cos j cos i sin j sin i i i S 0 CS j D 2 j AS j C dS i D xi x j 0 cos i z i z j 0 sin i 1 C cos i j DI j1 CI j 2 DI j1 C ln AI j1 2 2 C D AC 1 l j A C l j 2 Al j B 1 A J j D AC I j1 ln tan tan ln 2 E E E 2 B D AC xi x j 0 cos i z i z j 0 sin i xi x j 0 cos i z i z j 0 sin i cos j i x x cos z z sin sin sin cos cos x x cos sin sin cos cos cos z z sin sin sin cos cos sin x x cos 1 cos sin sin cos z z sin 1 sin cos cos sin x x sin cos sin sin cos z z cos sin i j0 i i j0 i i j i j 2 i j0 i i j j i i 2 i j0 i i j i j j 2 i j0 i j i j j 2 i j0 i where i j0 j j i i j j i j j i j0 j i cos j cos i sin j D AC sin i j E 41 058:0160 Professor Fred Stern Fall 2009 Chapter 8 42 42 058:0160 Professor Fred Stern Fall 2009 Chapter 8 43 43 058:0160 Professor Fred Stern Fall 2009 Chapter 8 44 44 058:0160 Professor Fred Stern Fall 2009 Chapter 8 45 45 058:0160 Professor Fred Stern Fall 2009 Chapter 8 46 46 058:0160 Professor Fred Stern Fall 2009 Chapter 8 47 47 058:0160 Professor Fred Stern Fall 2009 Chapter 8 48 48 058:0160 Professor Fred Stern Fall 2009 Chapter 8 49 49 058:0160 Professor Fred Stern Fall 2009 Chapter 8 50 50