Prandtl–Batchelor Theorem

In fluid dynamics, Prandtl–Batchelor theorem states that ''if in a two-dimensional laminar flow at high Reynolds number closed streamlines occur, then the vorticity in the closed streamline region must be a constant''. A similar statement holds true for axisymmetric flows. The theorem is named after Ludwig Prandtl and George Batchelor. Prandtl in his celebrated 1904 paper stated this theorem in arguments, George Batchelor unaware of this work proved the theorem in 1956. The problem was also studied in the same year by Richard Feynman and Paco Lagerstrom and by W.W. Wood in 1957.

Mathematical proof

At high Reynolds numbers, Euler equations reduce to solving a problem for stream function,

:$\nabla^2\psi = - \omega(\psi), \quad \psi=\psi_o \text \partial D.$

As it stands, the problem is ill-posed since the vorticity distribution $\omega(\psi)$ can have infinite number of possibilities, all of which satisfies the equation and the boundary condition. This is not true if the streamlines are not closed, in which case, every streamline can be traced back to infinity, where $\omega(\psi)$ is assumed to be prescribed. The difficulty arises only when closed streamlines occur inside the flow at high Reynolds number, where $\omega(\psi)$ is not uniquely defined. The theorem asserts that $\omega(\psi)$ is uniquely defined in such cases by examining the limiting process $Re\rightarrow \infty$ properly.

In two-dimensional flows, the only non-zero component lies in the z direction. The steady, non-dimensional vorticity equation in this case reduces to

:$\mathbf \cdot \nabla\mathbf = \frac\nabla^2\omega.$

Integrate the equation over a surface $S$ lying entirely in the region where we have closed streamlines, bounded by a closed contour $C$

:$\int_S\mathbf \cdot \nabla\mathbf\, d\mathbf S = \frac\int_S\nabla^2\omega\, d\mathbf S.$

The integrand in the left-hand side term can be written as $\nabla \cdot (\omega\mathbf u)$ since $\nabla\cdot\mathbf u=0$. By divergence theorem, one obtains

:$\oint_C \omega\mathbf\cdot \mathbf n dl = \frac\oint_C\nabla\omega\cdot \mathbf n dl.$

where $\mathbf n$ is the outward unit vector normal to the contour line element $dl$. The left-hand side integrand can be made zero if the contour $C$ is taken to be one of the closed streamlines since then the velocity vector projected normal to the contour will be zero, that is to say $\mathbf u\cdot \mathbf n=0$. Thus one obtains

:$\frac\oint_C \nabla\omega \cdot \mathbf\ dl = 0$

This expression is true for finite but large Reynolds number since we did not neglect the viscous term before.

Unlike the two-dimensional inviscid flows, where $\omega=\omega(\psi)$ since $\mathbf u\cdot \nabla \omega =0$ with no restrictions on the functional form of $\omega$, in the viscous flows, $\omega\neq \omega(\psi)$. But for large but finite $\mathrm$, we can write $\omega=\omega(\psi) + \rm$, and this small corrections become smaller and smaller as we increase the Reynolds number. Thus, in the limit $\mathrm\rightarrow \infty$, in the first approximation (neglecting the small corrections), we have

:$\frac\oint_C \nabla\omega \cdot \mathbf\ dl = \frac\oint_C \frac\nabla\psi \cdot \mathbf\ dl = 0.$

Since $d\omega/d\psi$ is constant for a given streamline, we can take that term outside the integral,

:$\frac\frac\oint_C \nabla\psi \cdot \mathbf\ dl = 0.$

One may notice that the integral is negative of the circulation since

:$\Gamma = -\oint_C\mathbf u\cdot d\mathbf =-\int_S \omega d\mathbf S = \int_S \nabla^2\psi d\mathbf = \oint_C \nabla \psi \cdot \mathbf dl$

where we used the Stokes theorem for circulation and $\omega=-\nabla^2\psi$. Thus, we have

:$\frac\frac = 0.$

The circulation around those closed streamlines is not zero (unless the velocity at each point of the streamline is zero with a possible discontinuous vorticity jump across the streamline) . The only way the above equation can be satisfied is only if

:$\frac = 0,$

i.e., vorticity is not changing across these closed streamlines, thus proving the theorem. Of course, the theorem is not valid inside the boundary layer regime. This theorem cannot be derived from the Euler equations.Lagerstrom, P. A. (1975). Solutions of the Navier–Stokes equation at large Reynolds number. SIAM Journal on Applied mathematics, 28(1), 202-214.

References

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Fluid dynamics