IV. Kinematics of Fluid Motion Contents 1. Specification of Fluid Motion 2. Material Derivatives 3. Geometric Representation of Flow 4. Terminology 5. Motion and Deformation of Fluid Element 6. Rotational and Potential Flows 7. Continuity Equation 1. Specification of Fluid Motion Lagrangian View Study fluid motion by tracing the motion of fluid particles Identify a representative fluid particle Determine its position instantaneously Determine the velocity and acceleration Determine other physical quantities t = 0 r x t = t r r P osition r r r r = r (t ; x ) Velocit y r r ¶r u = ¶t 2r Accelerat ion r ¶ r a = ¶t2 Eulerian View Study fluid motion by investigating the temporal and spatial variation of the flow field Velocit y r r r v = v (x , t ) Acceleration r r r a = a (x , t ) 2. Material Derivatives Definition The rate of change one observed when following the motion of a fluid particle t+ t ( x+ x, y+ y, z+ z ) t ( x,y,z ) t t B xi , t t t t B (x + D x , y + D y , z + D z , t + D t ) = B (x , y , z , t ) + DB ¶B Dx ¶ B Dy ¶ B Dz ¶ B = + + + Dt ¶t Dt ¶ x Dt ¶ y Dt ¶ z ¶B ¶B ¶B ¶B ® + u + v + w ¶t ¶x ¶y ¶z DB Dt Dt Material Derivative D ¶ ¶ ¶ ¶ = + u + v + w Dt ¶t ¶x ¶y ¶z Local / Temporal Advective / Spatial Acceleration of Fluid particles r r r r r r Du ¶u ¶u ¶u ¶u a = = + u + v + w Dt ¶t ¶x ¶y ¶z ¶u ¶u ¶u ¶u ìï ïï ax = + u + v + w ¶ t ¶ x ¶ y ¶z ïï ïï ïí a = ¶ v + u ¶ v + v ¶ v + w ¶ v ïï y ¶t ¶x ¶y ¶z ïï ïï a = ¶ w + u ¶ w + v ¶ w + w ¶ w ïïî z ¶t ¶x ¶y ¶z 3. Geometric Representation of Flow Pathline A pathline is the trajectory of a fluid particle t3 t2 t1 t0 Mathematical representation r r r ér r r dr ét ; x ù = u êx (x , t ), t ù = u êë ú ú û ë û dt dx dy dz r = r = r = dt u éêt ; x ùú v éêt ; x ùú w éêt ; x ùú ë û ë û ë û Streamline A streamline is a line whose tangent always represents the direction of velocity Mathematical representation r r r u (x , t )´ dr = 0 dx dy dz = = u (x , y, z , t ) v (x , y , z , t ) w (x , y , z , t ) Example Find the pathline and streamline of the following flow field: ìï u = t + x ïí ïïî v = t + y Pathline ìï dx = t + x ïï dt ïï í ïï dy ïï = t + y ïî dt ìï u = t + x ü ïï ïí ý ïîï v = t + y ïïþ ìï u = C 1e t - 1 ïï í ïï v = C e t - 1 2 ïî ìï x = a ïí ïï y = b î ü ïï (t = 0 )ý ïï þ ìï du - 1= u ïï dt ïï í ïï dv ïï - 1= v ïî dt ìï x = C 1e t - t - 1 ïï í ïï y = C e t - t - 1 2 ïî ìï x = (a + 1 )e t - t - 1 ïï í ïï y = (b + 1 )e t - t - 1 ïî Streamline dx dy = t + x t + y x + t = C (y + t ) Streamline is identical to pathline if the velocity is invariable with time In general, streamlines will not intercross and will not end at a solid wall, etc. 4. Terminology Discharge and Mass flux Q = r n r u M = òS r r u ×n dS òS r r r u ×n dS V = Q S Streamtube, Stream filament, Total flow Fluid system and Control volume t+ t t z y x Fluid system and Control volume Steady flow and Unsteady flow ¶ = 0 ¶t St eady flow ¶ ¹ 0 ¶t Unst eady flow Steady flow and Unsteady flow Uniform flow and Non-uniform flow ¶ ¶ ¶ u + v + w = 0 ¶x ¶y ¶z Uniform flow ¶ ¶ ¶ u + v + w ¹ 0 ¶x ¶y ¶z Non-uniform flow The streamlines of a uniform flow is necessarily straight lines and parallel to each other r u ×Ñ = 0 r u ^ Ñ Gradually-varying flow and Rapidly-varying flow u ¶ ¶ ¶ + v + w @0 ¶x ¶y ¶z Gradually-varying flow • Curvature of all streamlines are small • Streamlines are nearly parallel 5. Motion and Deformation of Fluid Elements t+ t t Motion of a fluid element can be decomposed into Translation Rotation Deformation The translation is described by Velocity r u r u The rotation is described by Angular velocity r w r w v 2 ¶u = ¶y ¶v v1= ¶x v z ö 1æ ¶ v ¶ u ÷ = çç ÷ ÷ 2 çè¶ x ¶ y ø The angular velocity r 1 r w= Ñ´ u 2 The deformation is described by Rat e of st rain ée ù e e ê 11 12 13 ú eij = êêe21 e22 e23 ú ú ê ú e e e êë 31 32 33 ú û t+ t ö÷ 1æ ¶ u ¶ v e12 = çç + ÷ 2 çè ¶ y ¶ x ø÷ t ¶u e11 = ¶x Rate of strain é ¶u ê ê ¶x ê ê æ 1 ¶v [E ]= êê çç + ê2 çè¶ x ê ê1 æ¶ w + ê çç êêë2 è ¶ x ¶ u ö÷ ÷ ¶ y ø÷ ö ¶u÷ ÷ ¶ z ø÷ ö 1 æ¶ u ¶ w öù 1æ ¶ u ¶ v ÷ çç ÷ ú çç + + ÷ ÷ ÷ 2 çè ¶ y ¶ x ø 2 è ¶ z ¶ x ø÷úú ö÷úú ¶v 1æ ¶ v ¶ w çç + ÷ ú ç ¶y 2 è¶ z ¶ y ø÷ú ú ö ú 1æ ¶w çç¶ w + ¶ v ÷ ú ÷ ÷ ç úúû 2 è¶ y ¶z ø ¶z Helmholtz’s theorem of velocity decomposition r r r r r ¶u ¶u ¶u u = u0 + Dx + Dy + Dz ¶x ¶y ¶z r r r = u 0 + (D r ×Ñ )u r r r r = u 0 + w ´ D r + [E ]×D r r u r u0 r Dr Translation r r r r r u = u 0 + w ´ D r + [E ]×D r Rotation Deformation 6. Rotational and Potential Flows r Ñ´ u ¹ 0 Rot at ional flow r Ñ´ u = 0 Irrot at ional flow Physical Interpretation r 1 r w= Ñ´ u 2 Example ìï ur = 0 ïí ïï u q = k r î ìï u = ky ïí ïï v = 0 î is irrot at ional flow is rot at ional flow r Ñ´ u = 0 f exists so that r u = Ñf Velocity Potential Irrotational flow Potential flow 7. Continuity Equation Conservation of Mass: Mass in a closed system is invariant rw + 1 ¶rw Dz 2 ¶z rv + ru - 1 ¶ru Dx 2 ¶x ru + z y rv - 1 ¶rv Dy 2 ¶y 1 ¶rv Dy 2 ¶y x rw - 1 ¶rw Dz 2 ¶z 1 ¶ru Dx 2 ¶x Net outflow of mass through the surface of the control volume æ ö æ ö÷ 1 ¶ru ççr u + 1 ¶ r u D x ÷ ç D y D z D t r u D x DyDzDt ÷ ÷ ç ÷ ÷ è ø è ø 2 ¶x 2 ¶x æ ö÷ æ ö÷ 1 ¶rv 1 ¶rv ç ç + çr v + Dy÷ D x D z D t - çr v Dy÷ DxDzDt ÷ ÷ çè ç 2 ¶y 2 ¶y ø è ø æ ö æ ö÷ 1 ¶rw 1 ¶rw ÷ ç ç + çr w + Dz÷ D x D y D t - çr w Dz÷ DxDyDt ÷ ÷ è ø è ø 2 ¶z 2 ¶z æ¶ r u ¶ r v ¶ r w ÷ ö r ù ç é = ç + + D x D y D z D t = ëÑ ×(r u )ûD x D y D z D t ÷ ÷ çè ¶ x ¶y ¶z ø Decrease of mass within the control volume ¶r DxDyDzDt ¶t Mass Conservation r ù ¶r é D x D y D z D t = ëÑ ×(r u )ûD x D y D z D t ¶t r ¶r + Ñ ×(r u ) = 0 ¶t For incompressible fluid r Ñ ×u = 0 r Ñ ×u = e11 + e22 + e33 = ev Bulk expansion Continuity Equation for Steady Total Flows Se S o Net out flow = ò r r n ×u dS + So Qo = Qe ò Se r r n ×u dS = Qo - Qe = 0 (AoV o = AV e e) So n u dS n u dS 0 Se Qo Qe Q Vo Ao Ve Ae Continuity Equation for Potential Flows r Ñ ×u = Ñ ×(Ñ f ) = Ñ 2f = 0 ¶ 2f ¶ 2f ¶ 2f + + = 0 2 2 2 ¶x ¶y ¶z