Airy ordinary differential equation Created 2026-10-05 Updated 2026-10-06
This second-order ordinary differential equation has the independent entire Airy functions and as a standard basis. It is distinct from the dispersive PDE in Airy equation. Its general solution is .
Airy resolvent kernel Created 2026-10-05 Updated 2026-10-06
For , put using the principal cube root and . The decaying Green function for on the real line is
The identities among the three characteristic roots show that and are continuous, while has jump one. Its distributional derivative therefore satisfies . This is the kernel of the resolvent operator , obtained by the time Laplace transform of the Airy equation.
Let solve the Airy ordinary differential equation . For , set and define the displayed similarity solution. Differentiating the profile equation gives , so the chain rule yields
Their sum is zero, proving the Airy equation . Every real linear combination of the two standard Airy functions gives such a solution. This is a solution of the linear dispersive equation; the nonlinear Korteweg-De Vries equation includes an extra term and does not follow from the same arbitrary profile construction.
For the Airy equation with opposite dispersive sign, on , let be the initial Half-range Fourier transform and . Three integrations by parts give the displayed global relation. The spatial transform is holomorphic for , whereas the finite-time spectral boundary transforms are entire functions. The symmetry , , preserves their time exponent.
// Target: analysis.bigb
For the Airy equation on , define and analogously at . Set and . Integrating the local relation with flux proves the displayed global relation. The dispersion relation is invariant under multiplication of by a cube root of unity; the resulting three equations determine the three missing boundary transforms for data .
Linear dispersive Stokes equation Created 2026-10-06 Updated 2026-10-14
The scalar linear partial differential equation is an Airy equation with a first-order transport term. It is a linearization of the Korteweg-De Vries equation with an advective term retained. It is distinct from the viscous incompressible-flow Stokes equation. On the whole line its spatial Fourier transform evolves by .
For the Airy equation, let . Its local relation follows by arranging the flux so that the unwanted spatial derivatives cancel:
Consequently
Thus the dispersion relation and the required flux are given by
The calculation is polynomial in the complex spectral parameter, so the local relation holds for every .
The given Riccati ansatz is . Differentiating it and substituting for shows
It therefore selects in the preceding scaled Painleve equation. Write . The quadratic terms cancel in the ansatz, leaving
Thus every nonzero solution of the indicated Airy equation gives the local mKdV solution
on intervals where . For example , with constants not both zero, has the required equation. This branch is generally complex and meromorphic; the printed ansatz itself includes . A real on a real interval would require simultaneously and , which is impossible on an interval. Hence this particular ansatz does not furnish a nontrivial real-valued mKdV profile.
Take . The Airy equation is . To discuss positivity of this linear operator, use its homogeneous variation domain . Integration by parts gives
The boundary term is zero at both ends. The same calculation with two different functions proves that the associated form is a symmetric bilinear form. Positivity here concerns the homogeneous domain; the condition instead defines an affine set of admissible solutions.
For the variational problem define
and minimize
The Sobolev trace at zero is meaningful in . No derivative boundary value is imposed on this trial space: the Neumann boundary condition will emerge naturally. For , Cauchy-Schwarz inequality and integration give
so . Thus is a bounded, symmetric, coercive bilinear form on the Hilbert space . The Lax-Milgram theorem says that a bounded coercive bilinear form and a bounded linear functional determine a unique weak solution. Apply it to
and set . This is precisely the first variation condition for .
Compactly supported test functions first yield in the sense of distributional derivatives. Since , the solution is in . Integration by parts then leaves for every , hence . The other boundary condition is built into . Conversely a solution of this boundary value problem satisfies the first variation condition. Finally,
This proves existence, uniqueness and the global minimum characterization, including the natural boundary condition. It is the mixed-boundary Airy energy principle.
Define the initial Half-range Fourier transform , and, for each available boundary trace, its finite-time spectral boundary transform
Temporarily let also denote the missing trace. Three integrations by parts in give
Consequently the backward-sign Airy half-line global relation is
The spatial transform is holomorphic below the real axis, while each finite-time is an entire function. Moreover, because .
Suppose the missing derivative has order , and put . Its contribution to the right-hand side is , where , , . Apply the inversion from the preceding part at time and select
The rotated coefficients of that missing trace now equal minus its real-line coefficient. Its entire contribution is therefore
The real-axis pieces cancel. What remains is the boundary of the middle upper sector, outward on and inward on . In this sector , and
is bounded by . The factor decays exponentially throughout the closing arc, overcoming . There are no poles. Thus the Cauchy integral theorem proves the cubic-dispersion elimination of one missing boundary trace and removes every occurrence of the unknown .
For a compact explicit answer, use only the two prescribed traces to form . The three choices are
For each row the solution is
All quantities in this formula are transforms of the given data. On the contour rays is real, so the time exponential is oscillatory; the integrals use the usual limiting interpretation of Fourier inversion. The decay estimate used for elimination belongs to the middle sector, not to or , where can grow.
At , and the preceding inversion recovers . The spectral exponential satisfies the Airy equation with the required minus sign. Differentiating the finite-time amplitudes produces only derivatives of the Dirac delta supported at and zero rotated closed-contour contributions, so the interior equation also holds. Finally, two solutions with the same data have for their difference, so this representation gives zero: each of the three prescribed pairs determines the solution uniquely in the smooth decaying class.
Put and . The constant-shear Orr-Sommerfeld equation gives
Let and . Since and , the equation becomes
This is the Airy ordinary differential equation, yielding the Airy reduction of the Orr-Sommerfeld equation in constant shear. It is distinct from the evolution PDE represented by the existing Airy equation article.
Apply the time Laplace transform to the Airy equation. Extend past in any suitable way and write
For example, setting after makes ; the final solution for is independent of this extension. The Laplace transform of a derivative gives
Take the principal cube root for . The three characteristic roots of the spatial ordinary differential equation are
Since , only has negative real part. Thus spatial decay leaves just one homogeneous exponential, which the single prescribed Neumann boundary condition determines.
The Airy resolvent kernel on the whole real line is
It decays at both ends, is continuous together with its first derivative, and satisfies . Consequently as a distribution. A particular solution is the Green-function representation
Adding the decaying homogeneous mode to impose the boundary derivative gives
Every term is known. If denotes the spatial Laplace transform, then
The Bromwich inversion formula now gives the required integral representation:
Here is to the right of any singularities required by the growth of the data. The usual decay or growth hypotheses are understood for this Laplace transform construction; when absolute inversion is unavailable, the vertical integral is interpreted as the limit of truncated Bromwich contours. The transformed ordinary differential equation verifies the partial differential equation and initial condition, while differentiating at gives exactly and hence . The derivative compatibility makes the two data agree at the corner.
Under the Fourier transform, the operator is the Fourier multiplier operator
Its symbol is purely imaginary because is real. Consequently is skew-adjoint on with common domain and generates the strongly continuous unitary group
The Plancherel theorem gives , so every . Products of the frozen groups are also unitary; hence this is a stable family of semigroup generators with constants .
For ,
Since , the map is continuously differentiable from to . All hypotheses from part f are satisfied, so an evolution family exists on every finite interval .
In this commuting Fourier multiplier operator example the solution operator can also be written explicitly:
Its multiplier has absolute value one, directly confirming strong continuity, the evolution family law, preservation of , and the required derivatives. The equation combines the dispersive Airy equation with a time-dependent linear transport equation.
Differentiating the first auxiliary equation in , the second in , and equating and leaves precisely
so the Airy equation is their compatibility condition.
Multiplication of by gives
Hence
For , the kernel is bounded when ; dominated differentiation makes analytic for . Rapid decrease gives
For real , multiply the time equation by and let . The rapidly decreasing terms on its right vanish, leaving
Therefore
and the Fourier inversion theorem gives
Differentiate the Airy ordinary differential equation to obtain . Combining part (a)'s derivatives yields
To make this vanish for an arbitrary Airy profile, the time powers must agree: , giving . Their common coefficient must then vanish, giving , hence . Therefore
For the two terms cancel exactly:
This is an Airy similarity solution of the linear dispersive equation. The Airy equation here is the linear partial differential equation , the reduced equation specified in the question; it is distinct from the profile's Airy ordinary differential equation. The construction works for every linear combination of its two independent profiles, including zero. No condition at is supplied, and this singular time is excluded. With real cube roots the final formula can also be used separately on .
Quantum bouncer 2026-10-20
A quantum particle above a hard reflecting wall in a linearly increasing potential for . The Schrödinger equation reduces to the Airy equation. Decay at infinity selects , while the wall requires . Thus and the energies are the displayed values. The th state has interior nodes and a decaying tail beyond its classical turning point. A gravitational realization has ; gravitational neutron bound-state transmission tests such confinement experimentally.
Scorer function 2026-10-05
The Scorer functions are particular solutions of inhomogeneous Airy equations: and . They occur when an endpoint participates in an Airy-type transition. The NIST Digital Library of Mathematical Functions gives their standard normalizations.