Green's Fnt. For 2-D Helmholtz Eqn.

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SUMMARY

The Green's function for the two-dimensional Helmholtz equation, defined by the equation ∇² G + k² G = δ(x) with outgoing wave boundary conditions, is confirmed to be a Hankel function of the first kind. The solution approach involves transforming the problem into polar coordinates, simplifying the partial differential equation (PDE) to a Bessel equation. The Bessel transform is utilized instead of the Fourier transform, and residue techniques are applied to evaluate the integral representation of G, mirroring the method used in the one-dimensional case.

PREREQUISITES
  • Understanding of the Helmholtz equation in two dimensions
  • Familiarity with Bessel functions and their properties
  • Knowledge of polar coordinates and their application in PDEs
  • Experience with residue theorem in complex analysis
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  • Study the properties and applications of Hankel functions of the first kind
  • Learn about Bessel transforms and their use in solving differential equations
  • Explore the residue theorem and its applications in evaluating integrals
  • Review the one-dimensional Helmholtz equation solutions for comparative analysis
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Mathematicians, physicists, and engineering students focusing on partial differential equations, particularly those interested in wave propagation and mathematical methods in physics.

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Homework Statement



Show that the Green's function for the two-dimensional Helmholtz equation,

2 G + k2 G = δ(x)

with the boundary conditions of an outgoing wave at infinity, is a Hankel function of the first kind.

Here, x is over 2d.

Homework Equations



The eigenvalue expansion?

The Attempt at a Solution



Unfortunately I am not sure where to start. I have solved the one dimensional case with the same boundary conditions, but I have no experience with PDE's (aside from Schrodingers). Since I have provided no attempt, anything would be of help, including references where I can find some help. Afrken isn't helping very much, and google hasn't turned out much information either. The 3-dimensional case is easily found, but I'm not sure it translates directly. Thank's in advance
 
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Working in polar coordinates, from symmetry consideration, G(r,θ)=G(r), so that the PDE reduces to ODE (Bessel equation), which can be solved similarly as the 1D case, except that instead of using Fourier transform, use Bessel transform, and evaluate the integral representation of G using residue techniques (shifting the poles according to radiation condition), as was done in the 1D case.
 
This approach worked, thank you for your help!
 

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