202 Drag and Moment in Viscous Potential Flow D. D. Joseph, T. Y. Liao and H. H. Hu Department of Aerospace Engineering and Mechanics University of Minnesota Minneapolis, Minnesota 55455 May 1992 We consider solutions of the Navier-Stokes equations in which the velocity is given by the gradient of a potential. We show that the drag on bodies and bubbles is the same in viscous and inviscid potential flow. The lift on two-dimensional bodies is given by the usual Kutta condition but the moment about the origin of the stresses acting on the body is given by MI + 2 where is the viscosity, is the circulation and MI is the usual moment for an inviscid fluid. 211 1 Viscous and Viscoelastic Potential Flow Daniel D. Joseph and Terrence Y. Liao Department of Aerospace Engineering and Mechanics University of Minnesota, Minneapolis, MN 55455 January 12, 1993 Abstract Potential flows of incompressible fluids admit a pressure (Bernoulli) equation when the divergence of the stress is a gradient as in inviscid fluids, viscous fluids, linear viscoelastic fluids and second-order fluids. We show that the equation balancing drag and acceleration is the same for all these fluids independent of the viscosity or any viscoelastic parameter and that the drag is zero in steady flow. The unsteady drag on bubbles in a viscous (and possibly in a viscoelastic) fluid may be approximated by evaluating the dissipation integral of the approximating potential flow because the neglected dissipation in the vorticity layer at the traction-free boundary of the bubble gets smaller as the Reynolds number is increased. Using the potential flow approximation, the drag D on a spherical gas bubble of radius a rising with velocity U(t) in a linear viscoelastic liquid of density and shear modules G(s) is given by D 2 3 a3 Ý U 12 a G(t )U( )d t _ and in a second-order fluid by D a 2 3 a2 12 1 _ _ _ _ Ý U 12 a U where 1 < 0 is the coefficient of the first normal stress and is the viscosity of the fluid. Because 1 is negative, we see from this formula that the unsteady normal stresses oppose inertia; that is, oppose the acceleration reaction. When U(t) is slowly varying, the two formulas coincide. For steady flow, we obtain D 12 a U for both viscous and viscoelastic fluids. In the case where the dynamic contribution of the interior flow of the bubble cannot be ignored as in the case of liquid bubbles, the dissipation method gives an estimation of the rate of total kinetic energy of the flows instead of the drag. When the dynamic effect of the interior flow is negligible but the density is important, this formula for the rate of total kinetic energy leads to D ( a )VBg ex aVB Ý U where a is the density of the fluid (or air) inside the bubble and VB is the volume of the bubble. Classical theorems of vorticity for potential flow of ideal fluids hold equally for viscous and viscoelastic fluids. The drag and lift on two-dimensional bodies of arbitrary cross section in viscoelastic potential flow are the same as in potential flow of an inviscid fluid but the moment M in a linear viscoelastic fluid is given by M MI 2 G(t ) ( ) t _ d where MI is the inviscid moment and (t) is the circulation, and M MI 2 2 1 t in a second-order fluid. When (t) is slowly varying, the two formulas for M coincide. For steady flow, they reduce to M MI 2 which is also the expression for M in both steady and unsteady potential flow of a viscous fluid. Potential flows of models of a viscoelastic fluid like Maxwell's are studied. These models do not admit potential flows unless the curl of the divergence of the extra-stress vanishes. This leads to an over-determined system of equations for the components of the stress. Special potential flow solutions like uniform flow and simple extension satisfy these extra conditions automatically but other special solutions like the potential vortex can satisfy the equations for some models and not for others. 270 Breakup of a liquid drop suddenly exposed to a high-speed airstream by Daniel D. Joseph, J. Belanger & G.S. Beavers University of Minnesota, Minneapolis, MN 55455 This paper is dedicated to Gad Hetsroni, on the occasion of his 65th birthday, to honor his many contributions to the understanding of multiphase flows. Abstract The breakup of viscous and viscoelastic drops in the high speed airstream behind a shock wave in a shock tube was photographed with a rotating drum camera giving one photograph every 5s. From these photographs we created movies of the fragmentation history of viscous drops of widely varying viscosity, and viscoelastic drops, at very high Weber and Reynolds numbers. Drops of the order of one millimeter are reduced to droplet clouds and possibly to vapor in times less than 500 s. The movies may be viewed at http://www.aem.umn.edu /research/Aerodynamic_Breakup. They reveal sequences of breakup events which were previously unavailable for study. Bag and bag-and-stamen breakup can be seen at very high Weber numbers, in the regime of breakup previously called “catastrophic.” The movies allow us to generate precise displacement-time graphs from which accurate values of acceleration (of orders 104 to 105 times the acceleration of gravity) are computed. These large accelerations from gas to liquid put the flattened drops at high risk to Rayleigh-Taylor instabilities. The most BREAKUP OF A LIQUID DROP SUDDENLY EXPOSED TO A HIGH-SPEED AIRSTREAM unstable Rayleigh-Taylor wave fits nearly perfectly with waves measured on enhanced images of drops from the movies, but the effects of viscosity cannot be neglected. Other features of drop breakup under extreme conditions, not treated here, are available on our Web site. 284 Accepted for publication in J. Fluid Mech. 1 Viscous potential flow analysis of Kelvin-Helmholtz instability in a channel By T. FUNADA1 AND D. D. JOSEPH2 1Department 2Department of Digital Engineering, Numazu College of Technology, Ooka 3600, Numazu, Shizuoka, Japan of Aerospace Engineering and Mechanics, University of Minnesota, Minneapolis, MN 55455, USA (Received ?? and in revised form ??) We study the stability of strati.ed gas-liquid .ow in a horizontal rectangular channel using viscous potential .ow. The analysis leads to an explicit dispersion relation in which the e.ects of surface tension and viscosity on the normal stress are not neglected but the e.ect of shear stresses are neglected. Formulas for the growth rates, wave speeds and neutral stability curve are given in general and applied to experiments in air-water .ows. The e.ects of surface tension are always important and actually determine the stability limits for the cases in which the volume fraction of gas is not too small. The stability criterion for viscous potential .ow is expressed by a critical value of the relative velocity. The maximum critical value is when the viscosity ratio is equal to the density ratio; surprisingly the neutral curve for this viscous .uid is the same as the neutral curve for inviscid .uids. The maximum critical value of the velocity of all viscous .uids is given by inviscid .uids. For air at 20.C and liquids with density ρ = 1 g/cm3 the liquid viscosity for the critical conditions is 15 cp; the critical velocity for liquids with viscosities larger than 15 cp are only slightly smaller but the critical velocity for liquids with viscosities smaller than 15 cp, like water, can be much lower. The viscosity of the liquid has a strong a.ect on the growth rate. The viscous potential .ow theory .ts the experimental data for air and water well when the gas fraction is greater than about 70%. 294 Rayleigh-Taylor Instability of Viscoelastic Drops at High Weber Numbers D.D. Joseph*, G.S. Beavers*, T. Funada** *University of Minnesota, Minneapolis, MN 55455 ** Numazu College of Technology, Ooka 3600, Numazu, Shizuoka, Japan 410-8501 Abstract Movies of the breakup of viscous and viscoelastic drops in the high speed airstream behind a shock wave in a shock tube have been reported by Joseph, Belanger and Beavers [1999]. A Rayleigh-Taylor stability analysis for the initial breakup of a drop of Newtonian liquid was presented in that paper. The movies, which may be viewed at http://www.aem.umn.edu/ research/Aerodynamic_Breakup, show that for the conditions under which the experiments were carried out the drops were subjected to initial accelerations of orders 104 to 105 times the acceleration of gravity. In the Newtonian analysis of Joseph, Belanger and Beavers the most unstable Rayleigh-Taylor wave fits nearly perfectly with waves measured on enhanced images of drops from the movies, but the effects of viscosity cannot be neglected. Here we construct a Rayleigh-Taylor stability analysis for an Oldroyd B fluid using measured data for acceleration, density, viscosity and relaxation time 1. The most unstable wave is a sensitive function of the retardation time 2 which fits experiments when 2/1= O(10-3). The growth rates for the most unstable wave are much larger than for the comparable viscous drop, which agrees with the surprising fact that the breakup times for viscoelastic drops are shorter. We construct an approximate analysis of Rayleigh-Taylor instability based on viscoelastic potential flow which gives rise to nearly the same dispersion relation as the unapproximated analysis. 300 Capillary/C-InstabSh03-27.tex 1 Viscous Potential Flow Analysis of Capillary Instability T. Funada and D.D. Joseph University of Minnesota Aug 2001 Draft printed March 28, 2002 This paper is dedicated to Klaus Kirchg¨assner on the occasion of his 70th birthday. Contents 1 Introduction 1 2 Governing equations and dimensionless parameters 3 2.1 Linearized disturbance equations . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 3 2.2 Dispersion relation for fully viscous flow (FVF) . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4 2.3 More viscous fluid outside . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 4 2.4 Dispersion relation for viscous potential flow (VPF) . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 5 3 Growth rate curves, vs. 6 4 Maximum growth rates and wavenumbers, and vs. 11 5 vs. for IPF 16 6 Conclusions and discussion 16 _ k _m km pJ _ mI km Abstract Capillary instability of a viscous fluid cylinder of diameter surrounded by another fluid is determined by a Reynolds number , a viscosity ratio and a density ratio . Here is the capillary collapse velocity based on the more viscous liquid which may be inside or outside the fluid cylinder. Results of linearized analysis based on potential flow of a viscous and inviscid fluid are compared with the unapproximated normal mode analysis of the linearized Navier-Stokes equations. The growth rates for the inviscid fluid are largest, the growth rates of the fully viscous problem are smallest and those of viscous potential flow are between. We find that the results from all three theories converge when is large with reasonable agreement between viscous potential and fully viscous flow with . The convergence results apply to two liquids as well as to D J = V D_`= _` _a= _` ` = _a=_` m= V = = _` J J > O( 10) liquid and gas. 1 Introduction Capillary instability of a liquid cylinder of mean radius leading to capillary collapse can be described as a neckdown due to surface tension in which fluid is ejected from the throat of the neck, leading to a smaller neck and greater neckdown capillary force as seen in the diagram in figure 1.1. The dynamical theory of instability of a long cylindrical column of liquid of radius under the action of capillary force was given by Rayleigh (1879) following earlier work by Plateau (1873) who showed that a long cylinder of liquid is unstable to disturbances with wavelengths greater than . Rayleigh showed that the effect of inertia is such that the wavelength corresponding to the mode of maximum instability is exceeding very considerably the circumference of the cylinder. The idea that the wave length associated with fastest growing growth rate would become dominant and be observed in practice was first put forward by Rayleigh (1879). The analysis of Rayleigh is based on potential flow of an inviscid R R 2_R _ _ = 4:51 _ 2R; 305 J. Fluid Mech. (2004), vol. 505, pp. 365–377. c _ 2004 Cambridge University Press DOI: 10.1017/S0022112004008602 Printed in the United Kingdom 365 The dissipation approximation and viscous potential .ow By D. D. JOSEPH AND J. WANG Department of Aerospace Engineering and Mechanics, University of Minnesota, Minneapolis, MN 55455, USA (Received 18 June 2003 and in revised form 1 February 2004) Dissipation approximations have been used to calculate the drag on bubbles and drops and the decay rate of free gravity waves on water. In these approximations, viscous e.ects are calculated by evaluating the viscous stresses on irrotational .ows. The pressure is not involved in the dissipation integral, but it enters into the power of traction integral, which equals the dissipation. A viscous correction of the irrotational pressure is needed to resolve the discrepancy between the zero-shear-stress boundary condition at a free surface and the non-zero irrotational shear stress. Here we show that the power of the pressure correction is equal to the power of the irrotational shear stress. The viscous pressure correction on the interface can be expressed by a harmonic series. The principal mode of this series is matched to the velocity potential and its coe.cient is explicitly determined. The other modes do not enter into the expression for the drag on bubbles and drops. They vanish in the case of free gravity waves. 315 J. Fluid Mech. (2003), vol. 479, pp. 191–197. c _ 2003 Cambridge University Press DOI: 10.1017/S0022112002003634 Printed in the United Kingdom 191 Viscous potential .ow By D. D. JOSEPH Department of Aerospace Engineering and Mechanics, University of Minnesota, MN 55455, USA joseph@aem.umn.edu (Received 6 September 2002 and in revised form 10 December 2002) Potential .ows u = 佫φ are solutions of the Navier–Stokes equations for viscous incompressible .uids for which the vorticity is identically zero. The viscous term μ佫2u = μ佫佫2φ vanishes, but the viscous contribution to the stress in an incompressible .uid (Stokes 1850) does not vanish in general. Here, we show how the viscosity of a viscous .uid in potential .ow away from the boundary layers enters Prandtl’s boundary layer equations. Potential .ow equations for viscous compressible .uids are derived for sound waves which perturb the Navier–Stokes equations linearized on a state of rest. These linearized equations support a potential .ow with the novel features that the Bernoulli equation and the potential as well as the stress depend on the viscosity. The e.ect of viscosity is to produce decay in time of spatially periodic waves or decay and growth in space of time-periodic waves. In all cases in which potential .ows satisfy the Navier–Stokes equations, which includes all potential .ows of incompressible .uids as well as potential .ows in the acoustic approximation derived here, it is neither necessary nor useful to put the viscosity to zero. 319 J. Fluid Mech. (2003), vol. 488, pp. 213–223. c _ 2003 Cambridge University Press DOI: 10.1017/S0022112003004968 Printed in the United Kingdom 213 Rise velocity of a spherical cap bubble By DANIEL D. JOSEPH University of Minnesota, Aerospace Engineering and Mechanics, 110 Union St. SE, Minneapolis, MN 55455, USA (Received 23 October 2002 and in revised form 26 February 2003) The theory of viscous potential .ow is applied to the problem of .nding the rise velocity U of a spherical cap bubble (see Davies & Taylor 1950; Batchelor 1967). The rise velocity is given by U √gD =. 8 3 ν(1 + 8s) _gD3 + √2 3 _1 . 2s . 16sσ ρgD2 + 32v2 gD3 (1 + 8s)2_1/2 , where R = D/2 is the radius of the cap, ρ and ν are the density and kinematic viscosity of the liquid, σ is surface tension, r(θ) = R(1 + sθ2) and s = r__(0)/D is the deviation of the free surface from perfect sphericity r(θ) = R near the stagnation point θ = 0. The bubble nose is more pointed when s < 0 and blunted when s > 0. A more pointed bubble increases the rise velocity; the blunter bubble rises slower. The Davies & Taylor (1950) result arises when s and ν vanish; if s alone is zero, U √gD =. 8 3 ν _gD3 + √2 3 _1 + 32ν2 gD3 _1/2 , showing that viscosity slows the rise velocity. This equation gives rise to a hyperbolic drag law CD = 6+32/Re, which agrees with data on the rise velocity of spherical cap bubbles given by Bhaga & Weber (1981). 324 J. Fluid Mech. (2004), vol. 511, pp. 201–215. c _ 2004 Cambridge University Press DOI: 10.1017/S0022112004009541 Printed in the United Kingdom 201 Potential .ow of a second-order .uid over a sphere or an ellipse By J. WANG AND D. D. JOSEPH Department of Aerospace Engineering and Mechanics, University of Minnesota, Minneapolis, MN 55455, USA (Received 9 May 2003 and in revised form 10 March 2004) We study the potential .ow of a second-order .uid over a sphere or an ellipse. The normal stress at the surface of the body is calculated and has contributions from the inertia, viscous and viscoelastic e.ects. We investigate the e.ects of Reynolds number and body size on the normal stress; for the ellipse, various angles of attack and aspect ratios are also studied. The e.ect of the viscoelastic terms is opposite to that of inertia; the normal stress at a point of stagnation can change from compression to tension. This causes long bodies to turn into the stream and causes spherical bodies to chain. For a rising gas bubble, the e.ect of the viscoelastic and viscous terms in the normal stress is to extend the rear end so that it tends to the cusped trailing edge observed in experiments.