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Inverse scattering transform
Inverse scattering transform
from Wikipedia
The 3-step algorithm: transform the initial solution to initial scattering data, evolve initial scattering data, transform evolved scattering data to evolved solution

In mathematics, the inverse scattering transform (or nonlinear Fourier transform) is a method that solves the initial value problem for a nonlinear partial differential equation using mathematical methods related to wave scattering.[1]: 4960  The direct scattering transform describes how a function scatters waves or generates bound-states.[2]: 39–43  The inverse scattering transform uses wave scattering data to construct the function responsible for wave scattering.[2]: 66–67  The direct and inverse scattering transforms are analogous to the direct and inverse Fourier transforms which are used to solve linear partial differential equations.[2]: 66–67 

Using a pair of differential operators, a 3-step algorithm may solve nonlinear differential equations; the initial solution is transformed to scattering data (direct scattering transform), the scattering data evolves forward in time (time evolution), and the scattering data reconstructs the solution forward in time (inverse scattering transform).[2]: 66–67 

This algorithm simplifies solving a nonlinear partial differential equation to solving 2 linear ordinary differential equations and an ordinary integral equation, a method ultimately leading to analytic solutions for many otherwise difficult to solve nonlinear partial differential equations.[2]: 72 

The inverse scattering problem is equivalent to a Riemann–Hilbert factorization problem, at least in the case of equations of one space dimension.[3] This formulation can be generalized to differential operators of order greater than two and also to periodic problems.[4] In higher space dimensions one has instead a "nonlocal" Riemann–Hilbert factorization problem (with convolution instead of multiplication) or a d-bar problem.

History

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The inverse scattering transform arose from studying solitary waves. J.S. Russell described a "wave of translation" or "solitary wave" occurring in shallow water.[5] First J.V. Boussinesq and later D. Korteweg and G. deVries discovered the Korteweg-deVries (KdV) equation, a nonlinear partial differential equation describing these waves.[5] Later, N. Zabusky and M. Kruskal, using numerical methods for investigating the Fermi–Pasta–Ulam–Tsingou problem, found that solitary waves had the elastic properties of colliding particles; the waves' initial and ultimate amplitudes and velocities remained unchanged after wave collisions.[5] These particle-like waves are called solitons and arise in nonlinear equations because of a weak balance between dispersive and nonlinear effects.[5]

Gardner, Greene, Kruskal and Miura introduced the inverse scattering transform for solving the Korteweg–de Vries equation.[6] Lax, Ablowitz, Kaup, Newell, and Segur generalized this approach which led to solving other nonlinear equations including the nonlinear Schrödinger equation, sine-Gordon equation, modified Korteweg–De Vries equation, Kadomtsev–Petviashvili equation, the Ishimori equation, Toda lattice equation, and the Dym equation.[5][7][8] This approach has also been applied to different types of nonlinear equations including differential-difference, partial difference, multidimensional equations and fractional integrable nonlinear systems.[5]

Description

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Nonlinear partial differential equation

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The independent variables are a spatial variable and a time variable . Subscripts or differential operators () indicate differentiation. The function is a solution of a nonlinear partial differential equation, , with initial condition (value) .[2]: 72 

Requirements

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The differential equation's solution meets the integrability and Fadeev conditions:[2]: 40 

Integrability condition:
Fadeev condition:

Differential operator pair

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The Lax differential operators, and , are linear ordinary differential operators with coefficients that may contain the function or its derivatives. The self-adjoint operator has a time derivative and generates a eigenvalue (spectral) equation with eigenfunctions and time-constant eigenvalues (spectral parameters) .[1]: 4963 [2]: 98 

and

The operator describes how the eigenfunctions evolve over time, and generates a new eigenfunction of operator from eigenfunction of .[1]: 4963 

The Lax operators combine to form a multiplicative operator, not a differential operator, of the eigenfunctions .[1]: 4963 

The Lax operators are chosen to make the multiplicative operator equal to the nonlinear differential equation.[1]: 4963 

The AKNS differential operators, developed by Ablowitz, Kaup, Newell, and Segur, are an alternative to the Lax differential operators and achieve a similar result.[1]: 4964 [9][10]

Direct scattering transform

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The direct scattering transform generates initial scattering data; this may include the reflection coefficients, transmission coefficient, eigenvalue data, and normalization constants of the eigenfunction solutions for this differential equation.[2]: 39–48 

Scattering data time evolution

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The equations describing how scattering data evolves over time occur as solutions to a 1st order linear ordinary differential equation with respect to time. Using varying approaches, this first order linear differential equation may arise from the linear differential operators (Lax pair, AKNS pair), a combination of the linear differential operators and the nonlinear differential equation, or through additional substitution, integration or differentiation operations. Spatially asymptotic equations () simplify solving these differential equations.[1]: 4967–4968 [2]: 68–72 [6]

Inverse scattering transform

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The Marchenko equation combines the scattering data into a linear Fredholm integral equation. The solution to this integral equation leads to the solution, u(x,t), of the nonlinear differential equation.[2]: 48–57 

Example: Korteweg–De Vries equation

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The nonlinear differential Korteweg–De Vries equation is [11]: 4 

Lax operators

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The Lax operators are:[2]: 97–102 

and

The multiplicative operator is:

Direct scattering transform

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The solutions to this differential equation

may include scattering solutions with a continuous range of eigenvalues (continuous spectrum) and bound-state solutions with discrete eigenvalues (discrete spectrum). The scattering data includes transmission coefficients , left reflection coefficient , right reflection coefficient , discrete eigenvalues , and left and right bound-state normalization (norming) constants.[1]: 4960 

Scattering data time evolution

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The spatially asymptotic left and right Jost functions simplify this step.[1]: 4965–4966 

The dependency constants relate the right and left Jost functions and right and left normalization constants.[1]: 4965–4966 

The Lax differential operator generates an eigenfunction which can be expressed as a time-dependent linear combination of other eigenfunctions.[1]: 4967 

The solutions to these differential equations, determined using scattering and bound-state spatially asymptotic Jost functions, indicate a time-constant transmission coefficient , but time-dependent reflection coefficients and normalization coefficients.[1]: 4967–4968 

Inverse scattering transform

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The Marchenko kernel is .[1]: 4968–4969 

The Marchenko integral equation is a linear integral equation solved for .[1]: 4968–4969 

The solution to the Marchenko equation, , generates the solution to the nonlinear partial differential equation.[1]: 4969 

Examples of integrable equations

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See also

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Citations

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References

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Further reading

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Revisions and contributorsEdit on WikipediaRead on Wikipedia
from Grokipedia
The inverse scattering transform (IST) is a nonlinear analogue of the , employed to solve the initial-value problems of certain integrable nonlinear evolution equations, such as the Korteweg–de Vries (KdV) equation, by linearizing them through a process. It consists of three main steps: a direct transform that maps the initial potential to data (including discrete eigenvalues and a ), a linear of that data, and an inverse transform that reconstructs the solution at later times using techniques like the Marchenko or Riemann-Hilbert problems. Originally discovered in 1967 by Gardner, Greene, Kruskal, and Miura to exactly solve the KdV equation ut+6uux+uxxx=0u_t + 6uu_x + u_{xxx} = 0, the method revealed the nature of its solutions and established a one-to-one correspondence between rapidly decaying potentials and their data in the context of the associated Schrödinger operator. The term "inverse scattering transform" was coined in 1974 by Ablowitz, Kaup, Newell, and Segur, who generalized it to a broader class of equations, including the , emphasizing its Fourier-like structure for nonlinear problems. IST has become a cornerstone of soliton theory and integrable systems, enabling the exact construction of multi-soliton solutions that emerge unchanged from nonlinear interactions, as well as periodic and other exact solutions for equations modeling phenomena in water waves, optics, and plasma physics. Its formulation relies on the existence of a Lax pair—compatible linear operators whose compatibility condition yields the nonlinear equation—ensuring integrability and conservation laws. Beyond one-dimensional cases, extensions to higher dimensions and discrete systems have been developed, with applications in inverse problems for quantum mechanics and signal processing. The method's power lies in transforming complex nonlinear dynamics into tractable linear algebra, profoundly influencing mathematical physics since its inception.

Historical Development

Origins in Soliton Studies

In August 1834, Scottish engineer John Scott Russell observed a remarkable solitary wave while conducting experiments on canal boat designs along the Union Canal near . As a boat suddenly halted upon hitting an obstruction, a large, rounded swell detached from the bow and propagated forward at a constant speed of about 8-9 miles per hour, maintaining its shape—a 30-foot-long, 1- to 1.5-foot-high hump—over a considerable distance without dispersion or alteration. Russell termed this a "wave of translation," distinguishing it from typical oscillatory waves, and documented his findings through subsequent experiments in a wave tank, confirming the wave's stability and dependence on water depth and amplitude. He reported these observations formally in 1844 to the British Association for the Advancement of Science, sparking initial interest in such nonlinear wave behaviors. The study of water waves in the had roots in earlier linear theories, but Russell's discovery highlighted the role of nonlinear phenomena in producing stable, localized waves. Pioneering work by in the 1780s derived linearized equations for small-amplitude surface waves, yielding the for wave speed gh\sqrt{gh}
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