Fjørtoft theorem 2026-10-14
For a smooth inviscid parallel shear profile with an exponentially growing mode, let be its velocity at an inflection point. The real and imaginary parts of the integrated Rayleigh equation for inviscid shear flow imply . Consequently somewhere in the channel. This strengthens Rayleigh's inflection-point theorem but is still only a necessary condition, not a sufficient instability criterion.
Let the perturbation velocity and pressure be , with real . Linearizing the Euler equations about the inviscid parallel shear flow gives
Use , to satisfy incompressibility. The first momentum equation gives ; differentiate it and use the second equation. The Rayleigh equation for inviscid shear flow follows:
A growing temporal normal mode has and growth rate .
Rayleigh's inflection-point theorem states that such an instability of a smooth parallel profile requires to change sign somewhere. To prove it, divide by , multiply by , integrate over and integrate the second derivative by parts. Decay removes the endpoint terms, giving
Taking the imaginary part yields
The weighting is nonnegative. A one-signed that is not identically zero cannot satisfy this identity for a nontrivial mode; otherwise the mode vanishes on an interval and uniqueness of the differential equation forces it to vanish throughout. If , the real part of the identity is already a strictly positive integral for a nontrivial decaying mode. This proves the necessary sign-change condition.
Fjørtoft's theorem strengthens this: if is the velocity at an inflection point, instability requires somewhere. This is a necessary condition, not a sufficient criterion. For , and
The possibility of instability is therefore consistent with Fjørtoft's theorem.
For the piecewise-linear approximation, within each of the three regions. The decaying solutions outside and the two independent interior solutions can be written
At each corner, the normal velocity is continuous, so is continuous. Pressure matching at a piecewise-linear shear interface additionally gives , hence . At the slope jumps from to ; at it jumps from to . Substituting the decaying outer solutions gives
Thus the inviscid instability of a piecewise-linear mixing layer has dispersion relation
At , , so the root with positive imaginary part is an explicitly growing mode, with growth rate . More generally the unstable interval is , where the unique solves . This direct calculation establishes instability of the approximation; passing a necessary inflection test alone would not have established it.
Write the perturbation Stokes streamfunction as , with and nonzero . Its radial and axial velocity amplitudes are and . These automatically obey incompressibility. Linearizing the radial and axial Euler equations, with pressure amplitude , gives
Thus
Differentiating the first expression, the terms involving cancel. Equating the two expressions for proves the axisymmetric inviscid pipe stability equation:
At the axis, finite smooth axisymmetric velocity requires , after choosing the irrelevant constant in the streamfunction. At the wall, impermeability gives . There is no tangential no-slip condition in this inviscid problem. A decoupled azimuthal disturbance satisfies and does not introduce a growing discrete mode when .
For real , suppose with , so division by is legitimate. Multiply the ordinary differential equation by , integrate, and apply integration by parts. The endpoint terms vanish by the preceding regularity and wall conditions, leaving
Taking its imaginary part yields
A growing temporal mode therefore requires a sign change of , rather than a sign change of alone. This is the cylindrical counterpart of Rayleigh's inflection-point theorem. If this derivative vanishes identically, the positive first integral rules out a nontrivial growing real-wavenumber mode as well. Isolated zeros without a sign change do not make the second integral vanish for a nonzero regular mode.
For the parabolic Poiseuille flow, is constant. Under the specified exclusion of critical levels, division gives
Setting , or equivalently choosing in , turns this into
It is the Modified Bessel differential equation of order one. Hence . Since tends to a nonzero constant at the axis, it gives a singular radial velocity and must be excluded. The admissible mode shape is therefore
For , direct solution gives after axis regularity, and the wall condition again forces the trivial solution. For nonzero , the nonzero roots of are imaginary. Writing for the zeros of the ordinary Bessel function , the evanescent potential modes of inviscid Poiseuille flow are
Their perturbation vorticity vanishes: . These modes grow exponentially in one axial direction and decay in the other. They can describe end-forced or spatially localized potential fields, but neither sign gives a bounded normal mode on a whole infinite pipe. Moreover, the reduced radial equation contains no : it supplies no temporal eigenvalue condition. An arbitrary imaginary part assigned to here is consequently not evidence for a physical temporal instability.
The real-wavenumber calculation does exclude growing discrete axisymmetric modes of this inviscid profile. It does not establish every form of stability: singular neutral disturbances with in the range of , transient dynamics, non-axisymmetric disturbances, and finite-amplitude transition require separate treatment. The exclusion specifically removes the inviscid continuous spectrum.
With viscosity, linearize the Navier-Stokes equations instead and eliminate pressure to obtain a fourth-order cylindrical counterpart of the Orr-Sommerfeld equation. Impose both and , with appropriate regularity at the axis. The resulting eigenvalue problem involves the Reynolds number and determines complex frequencies, rather than leaving arbitrary. Viscosity supplies diffusion, no-slip boundary layers and critical-layer regularization, so the inviscid sign argument alone no longer decides its spectrum. That observation does not imply that viscous pipe flow must have a growing linear eigenmode; finite-amplitude pipe transition is a different question.
Let and , with chosen for the temporal mode convention. In the inviscid limit, the Orr-Sommerfeld equation reduces to the Rayleigh equation for inviscid shear flow:
The impermeability boundary condition is ; the extra viscous derivative condition is not an independent condition for this reduced second-order equation. For an unstable mode , the denominator has no real zero. Multiply by and apply integration by parts to obtain
Its imaginary part gives
For a nontrivial mode, the weight is nonnegative and is positive except at isolated mode zeros. Thus must take both signs, unless it vanishes identically. The identically zero case also has no unstable nontrivial mode, by the positive first integral in the displayed identity. Therefore the smooth real base-flow profile must have an interior inflection point. This proves Rayleigh's inflection-point theorem; it is a necessary condition, not a sufficiency test.
Let at an inflection point supplied by the preceding identity. Its imaginary part, divided by nonzero , gives . Its real part is
Adding times the zero integral replaces by :
Therefore the integrand's profile factor must be strictly negative somewhere in the open channel:
This is the Fjørtoft theorem. The positive weight and the strictly negative integral establish the strict inequality, not merely a nonpositive value. It is a stronger necessary condition than Rayleigh's inflection-point theorem, and neither condition alone proves instability.
Let be real and twice continuously differentiable, take a nonzero real wave number, and write . Exponential instability requires , in particular , so has no zero on the channel. Divide the Rayleigh equation for inviscid shear flow by , multiply by and integrate. The wall conditions remove the boundary term, giving
Its imaginary part is
The weight is nonnegative and positive wherever the nontrivial eigenfunction does not vanish. A nontrivial solution of this regular second-order equation cannot vanish on an interval. If had one strict sign without changing sign, the integral could not vanish. If were identically zero, the real identity would instead give the contradiction . Thus must take both signs, and continuity gives an interior zero. This proves Rayleigh's inflection-point theorem: an unstable profile must have an inflection point, in fact a sign change of rather than merely an isolated zero without sign change.
Write the Rayleigh equation for inviscid shear flow as
Multiply by , integrate, and use integration by parts:
Its imaginary part is
For an unstable mode , the integral can vanish only if changes sign somewhere in the flow. Thus the velocity profile must have an inflection point. This is Rayleigh's inflection-point theorem; it is necessary, not sufficient, for inviscid instability.