Von Kármán swirling flow
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Von Kármán swirling flow is a flow created by a uniformly rotating infinitely long plane disk, named after
Theodore von Kármán Theodore von Kármán ( hu, ( szőllőskislaki) Kármán Tódor ; born Tivadar Mihály Kármán; 11 May 18816 May 1963) was a Hungarian-American mathematician, aerospace engineer, and physicist who was active primarily in the fields of aeronaut ...
who solved the problem in 1921. The rotating disk acts as a fluid pump and is used as a model for centrifugal fans or compressors. This flow is classified under the category of steady flows in which
vorticity In continuum mechanics, vorticity is a pseudovector field that describes the local spinning motion of a continuum near some point (the tendency of something to rotate), as would be seen by an observer located at that point and traveling along wi ...
generated at a solid surface is prevented from diffusing far away by an opposing convection, the other examples being the Blasius boundary layer with suction, stagnation point flow etc.


Flow description

Consider a planar disk of infinite radius rotating at a constant angular velocity \Omega in fluid which is initially at rest everywhere. Near to the surface, the fluid is being turned by the disk, due to friction, which then causes centrifugal forces which move the fluid outwards. This outward radial motion of the fluid near the disk must be accompanied by an inward axial motion of the fluid towards the disk to conserve mass.
Theodore von Kármán Theodore von Kármán ( hu, ( szőllőskislaki) Kármán Tódor ; born Tivadar Mihály Kármán; 11 May 18816 May 1963) was a Hungarian-American mathematician, aerospace engineer, and physicist who was active primarily in the fields of aeronaut ...
noticed that the governing equations and the boundary conditions allow a solution such that u/r, v/r and w are functions of z only, where (u,v,w) are the velocity components in cylindrical (r,\theta,z) coordinate with r=0 being the axis of rotation and z=0 represents the plane disk. Due to symmetry, pressure of the fluid can depend only on radial and axial coordinate p=p(r,z). Then the continuity equation and the incompressible
Navier–Stokes equations In physics, the Navier–Stokes equations ( ) are partial differential equations which describe the motion of viscous fluid substances, named after French engineer and physicist Claude-Louis Navier and Anglo-Irish physicist and mathematician Geo ...
reduce to : \begin & \frac r + \frac = 0 \\ pt& \left(\frac\right)^2 - \left(\frac\right)^2 + w \frac = - \frac \frac + \nu \frac \\ pt& \frac + w \frac = \nu \frac \\ pt& w \frac = -\frac \frac + \nu \frac \qquad \Rightarrow \qquad \frac p \rho = \nu \frac - \frac w^2 + f(r) \end where \nu is the kinematic viscosity.


No rotation at infinity

Since there is no rotation at large z\rightarrow \infty, p(r,z) becomes independent of r resulting in p =p(z). Hence f(r)=\text and \partial p/\partial r =0. Here the boundary conditions for the fluid z>0 are : u =0, \quad v = \Omega r, \quad w =0, \quad p = p_0 \quad \text z=0 : u =0, \quad v = 0\quad \text z\rightarrow \infty Self-similar solution is obtained by introducing following transformation, : \eta = \sqrtz, \quad u = r \Omega F(\eta), \quad v = r \Omega G(\eta) , \quad w = \sqrt H(\eta) , \quad p = p_0 + \rho \nu \Omega P(\eta) , where \rho is the fluid density. The self-similar equations are : \begin 2F + H' & = 0 \\ F^2 - G^2 + F'H & = F'' \\ 2FG + G'H & = G'' \\ P' + HH' - H'' & = 0 \end with boundary conditions for the fluid \eta>0 are : F =0, \quad G = 1, \quad H =0, \quad P = 0 \quad \text \eta=0 : F =0, \quad G = 0\quad \text \eta\rightarrow \infty The coupled ordinary differential equations need to be solved numerically and an accurate solution is given by Cochran(1934). The inflow axial velocity at infinity obtained from the numerical integration is w = -0.886 \sqrt, so the total outflowing volume flux across a cylindrical surface of radius r is 0.886 \pi r^2 \sqrt. The tangential stress on the disk is \sigma_ = \mu (\partial v/\partial z)_ =\rho \sqrt r G'(0) . Neglecting edge effects, the torque exerted by the fluid on the disk with large (R \gg \sqrt) but finite radius R is :T = 2 \int_0^R 2 \pi r^2 \sigma_ \, dr = \pi R^4 \rho \sqrt G'(0). The factor 2 is added to account for both sides of the disk. From numerical solution, torque is given by T = - 1.94 R^4 \rho \sqrt. The torque predicted by the theory is in excellent agreement with the experiment on large disks up to the Reynolds number of about Re=R^2 \Omega/\nu = 3\times 10^5, the flow becomes turbulent at high Reynolds number.


Rigid body rotation at infinity

This problem was addressed by George Keith Batchelor(1951). Let \Gamma be the angular velocity at infinity. Now the pressure at z\rightarrow\infty is \frac\rho \Gamma^2 r^2. Hence f(r)=\frac\rho \Gamma^2 r^2 and \partial p/\partial r =\Gamma^2.
Then the boundary conditions for the fluid z>0 are : u =0, \quad v = \Omega r ,\quad w =0 \quad \text z=0 : u =0, \quad v = \Gamma r \quad \text z\rightarrow \infty Self-similar solution is obtained by introducing following transformation, : \eta = \sqrtz, \quad \gamma = \frac, \quad u = r \Omega F(\eta), \quad v = r \Omega G(\eta) , \quad w = \sqrt H(\eta) . The self-similar equations are : \begin 2F + H' & = 0 \\ ptF^2 - G^2 + F'H & = F''- \gamma^2 \\ pt2FG + G'H & = G'' \end with boundary conditions for the fluid \eta>0 is : F =0, \quad G = 1, \quad H =0 \quad \text \eta=0 : F =0, \quad G = \gamma\quad \text \eta\rightarrow \infty The solution is easy to obtain only for \gamma>0 i.e., the fluid at infinity rotates in the same sense as the plate. For \gamma<0 , the solution is more complex, in the sense that many-solution branches occur. Evans(1969) obtained solution for the range -1.35<\gamma<-0.61. Zandbergen and Dijkstra showed that the solution exhibits a square root singularity as \gamma^-\rightarrow -0.16053876 and found a second-solution branch merging with the solution found for \gamma\rightarrow -0.16053876. The solution of the second branch is continued till \gamma^-\rightarrow 0.07452563, at which point, a third-solution branch is found to emerge. They also discovered an infinity of solution branches around the point \gamma^-\rightarrow 0. Bodoyni(1975) calculated solutions for large negative \gamma, showed that the solution breaks down at \gamma^-=-1.436. If the rotating plate is allowed to have uniform suction velocity at the plate, then meaningful solution can be obtained for \gamma\leq-0.2 . For 0<\gamma<\infty, \ \gamma\neq 1 (\gamma=1 represents solid body rotation, the whole fluid rotates at the same speed) the solution reaches the solid body rotation at infinity in an oscillating manner from the plate. The axial velocity is negative w<0 for 0\leq\gamma<1 and positive w>0 for 1<\gamma<\infty. There is an explicit solution when , \gamma-1, \ll 1.


Nearly rotating at the same speed, , \gamma-1, \ll 1

Since both boundary conditions for G are almost equal to one, one would expect the solution for G to slightly deviate from unity. The corresponding scales for F and H can be derived from the self-similar equations. Therefore, :G = 1+ \hat G, \quad H = \hat H, \quad F = \hat F \qquad , \hat F, ,, \hat G, ,, \hat H, \ll 1 To the first order approximation(neglecting \hat F^2,\hat G^2, \hat H^2), the self-similar equation becomes : \begin 2\hat F + \hat H' & = 0 \\ 1 + 2\hat G & = \gamma^2 -\hat F'' \\ 2\hat F & = \hat G'' \end with exact solutions : \begin F(\eta) &= - (\gamma-1) e^ \sin\eta, \\ G(\eta) &= 1+(\gamma-1) (1-e^\cos\eta),\\ H(\eta) &= (\gamma-1) -e^ (\sin\eta + \cos\eta) \end These solution are similar to an
Ekman layer The Ekman layer is the layer in a fluid where there is a force balance between pressure gradient force, Coriolis force and turbulent drag. It was first described by Vagn Walfrid Ekman. Ekman layers occur both in the atmosphere and in the ocean ...
solution.


Non-Axisymmetric solutions

The flow accepts a non-axisymmetric solution with axisymmetric boundary conditions discovered by Hewitt, Duck and Foster. Defining \eta = \sqrtz, \quad \gamma = \frac, \quad u = r \Omega '(\eta) + \phi(\eta)\cos 2\theta \quad v=r\Omega (\eta)-\phi(\eta)\sin 2\theta \quad w = -2\sqrtf(\eta), and the governing equations are : \begin f+2ff''-f'^2-\phi^2+g^2&=\gamma^2,\\ g''+2(fg'-f'g)&=0,\\ \phi''+2(f\phi'-f'\phi)&=0, \end with boundary conditions :f(0)=f'(0)=\phi(0)=g(0)-1=f'(\infty)=\phi(\infty)=g(\infty)-\gamma=0. The solution is found to exist from numerical integration for -0.14485\leq\gamma\leq0.


Bödewadt flow

Bödewadt flow describes the flow when a stationary disk is placed in a rotating fluid.


Two rotating coaxial disks

This problem was addressed by George Keith Batchelor(1951),
Keith Stewartson Keith Stewartson (20 September 1925 – 7 May 1983) was an English mathematician and fellow of the Royal Society. Early life The youngest of three children, Stewartson was born to an English baker in 1925. He was raised in Billingham, County Dur ...
(1952) and many other researchers. Here the solution is not simple, because of the additional length scale imposed in the problem i.e., the distance h between the two disks. In addition, the uniqueness and existence of a steady solution are also depend on the corresponding Reynolds number Re = \Omega h^2/\nu.
Then the boundary conditions for the fluid 0 are : u =0, \quad v = \Omega r,\quad w =0 \quad \text z=0 : u =0, \quad v = \Gamma r, \quad w=0 \quad \text z=h. In terms of \eta, the upper wall location is simply \eta=\sqrth=Re^. Thus, instead of the scalings : \begin \eta=\sqrtz, \quad \gamma=\frac, \quad u = r\Omega F'(\eta), \quad v= r\Omega G(\eta), \quad w =-2\sqrtF(\eta) \end used before, it is convenient to introduce following transformation, : \begin \xi = Re^ \eta, \quad f = Re^ F, \quad g = G \end so that the governing equations become : \begin Re^ f + 2ff''-f'^2 + g^2 = \lambda,\\ Re^ g'' + 2(fg'-f'g)=0 \end with six boundary conditions : f' =0, \quad g = 1 ,\quad f =0 \quad \text \xi=0 : f' =0, \quad g = \gamma, \quad f=0 \quad \text \xi=1. and the pressure is given by :\frac = \frac\lambda r^2 \Omega^2 - 2\nu\Omega (Re f^2 + f'). Here boundary conditions are six because pressure is not known either at the top or bottom wall; \lambda is to be obtained as part of solution. For large Reynolds number Re\gg 1, Batchelor argued that the fluid in the core would rotate at a constant velocity, flanked by two boundary layers at each disk for \gamma\geq 0 and there would be two uniform counter-rotating flow of thickness \xi=1/2 for \gamma=-1. However, Stewartson predicted that for \gamma=0,-1 the fluid in the core would not rotate at Re\gg 1, but just left with two boundary layers at each disk. It turns out, Stewartson predictions were correct. There is also an exact solution if the two disks are rotating about different axes but for \gamma=1.


Applications

Von Kármán swirling flow finds its applications in wide range of fields, which includes rotating machines, filtering systems, computer storage devices, heat transfer and mass transfer applications, combustion-related problems, planetary formations, geophysical applications etc.


References


Bibliography

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