Solved: Green's Functions - Kirchhoff Diffraction Theory

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In summary, Green's function is a function that is proportional to the Laplacian of a three dimensional object.
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[SOLVED] Green's Functions

Homework Statement


The basic equation of the scalar Kirchhoff diffraction theory is:

[tex]\psi(\vec r_1) = \frac{1}{4\pi}\int_{S_2}\left[\frac{e^{ikr}}{r}\nabla \psi(\vec r_2) - \psi(\vec r_2)\nabla (\frac{e^{ikr}}{r})\right] \cdot d\vec S_2[/tex]

where [itex]\psi[/itex] satisfies the homogeneous (three-dimensional) Helmholtz equation and [itex]r = |\vec r_1 - \vec r_2|[/itex]. Derive the above equation, assuming that [itex]\vec r_1[/itex] is interior to the closed surface [itex]S_2[/itex]


Homework Equations


Helmholtz Equation

[tex](\nabla^2 + k^2)\psi = 0[/tex]

Modified Helmholtz Equation

[tex](\nabla^2 - k^2)\psi = 0[/tex]

Has Green's Function

[tex]G(\vec r_1, \vec r_2) = \frac{\mathrm{exp}(-k|\vec r_1 - \vec r_2|)}{4\pi|\vec r_1 - \vec r_2|}[/tex]

Green's Function of three-dimensional Laplacian ([itex]\nabla^2[/itex]) is proportional to

[tex]G(\vec r_1, \vec r_2) \propto \int \mathrm{exp}(i\vec k\cdot(\vec r_1 - \vec r_2))\frac{d^3k}{k^2}[/tex]

The Attempt at a Solution



We have [itex]\psi[/itex] as a solution of the equation

[tex](\nabla_1{}^2 + k^2)\psi(\vec r_1) = (\nabla_1{}^2 - k^2)\psi(\vec r_1) + 2k^2\psi(\vec r_1) = 0[/tex]

or

[tex]\nabla_1{}^2 \psi(\vec r_1) = -k^2\psi(\vec r_1)[/tex]

Which gives that

[tex](\nabla_1{}^2 - k^2)\psi(\vec r_1) = -2k^2\psi(\vec r_1) = 2\nabla_1{}^2 \psi(\vec r_1)[/tex]

So we can write the solution in terms of the Green's function for the modified Helmholtz Equation

[tex]\psi(\vec r_1) & = & \int_{V_2}G(\vec r_1, \vec r_2)2\nabla_1{}^2\psi(\vec r_1) dV_2[/tex]

And then I don't know how to take it from there to the solution. It doesn't look like it should be too hard, but I don't know how to do it.

Any help would be greatly appreciated.

Thanks in advance,
Devin
 
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  • #2
Noone can help?
 
  • #3
Anyone, this is due tomorrow :(
 
  • #4
Ok, I got a little further, still not sure how to finish it though...

I then apply Green's theorem to the RHS and get

[tex]\psi(\vec r_1) = 2\int_{S_2}(G(\vec r_1, \vec r_2)\nabla_2\psi(\vec r_2) - \psi(\vec r_2)\nabla_2G(\vec r_2, \vec r_2))dS_2 + 2\int_{V_2}\psi(\vec r_2)\nabla_2{}^2G(\vec r_1, \vec r_2)dV_2[/tex]

But we know that

[tex]\nabla_2{}^2G(\vec r_1, \vec r_2) = k^2G(\vec r_1, \vec r_2) - \delta(\vec r_1, \vec r_2)[/tex]

So the equation becomes

[tex]3\psi(\vec r_1) = 2\int_{S_2}(G(\vec r_1, \vec r_2)\nabla_2\psi(\vec r_2) - \psi(\vec r_2)\nabla_2G(\vec r_2, \vec r_2))dS_2 + 2k^2\int_{V_2}\psi(\vec r_2)G(\vec r_1, \vec r_2)dV_2[/tex]

The first term is close to what I need, it is

[tex]\frac{1}{2\pi}\int_{S_2}\left[\frac{e^{-kr}}{r}\nabla\psi(\vec r_2) - \psi(\vec r_2)\nabla\frac{e^{-kr}}{r}\right]\cdot dS_2[/tex]

But I don't know how to change that negative to an [itex]i[/itex], or how to get rid of the extra term, or how to get rid of the extra factor of 2/3.
 
  • #5
Ok, for the second term, we have

[tex] k^2\psi(\vec r_2) = -\nabla_2{}^2\psi(\vec r_2)[/tex]

And then

[tex] \int_{V_2}2\nabla_2{}^2\psi(\vec r_2)G(\vec r_1, \vec r_2)dV_2 = \psi(\vec r_1)[/tex]

So we bring it over to the other side, and divide by 4 to get

[tex]\psi(\vec r_1) = \frac{1}{8\pi}\int_{S_2}\left[\frac{e^{-kr}}{r}\nabla\psi(\vec r_2) - \psi(\vec r_2)\nabla\frac{e^{-kr}}{r}\right]\cdot d\vec S_2[/tex]

Which is only off by a factor of 1/2, and has those negatives instead of [itex]i[/itex]'s in the exponent.
 
  • #6
Figured it out, the method I was using was the wrong one.
 
  • #7
I still can't mark my threads as solved...
 

FAQ: Solved: Green's Functions - Kirchhoff Diffraction Theory

What is the concept of Green's Functions in Kirchhoff Diffraction Theory?

Green's Functions are mathematical tools used to solve differential equations in physics, particularly in the field of diffraction. In Kirchhoff Diffraction Theory, Green's Functions are used to describe the propagation of waves through a medium and how they are affected by obstacles or apertures.

How are Green's Functions used in solving Kirchhoff Diffraction problems?

Green's Functions are used to convert the complex problem of diffraction into a simpler problem of solving a linear differential equation. They represent the response of the medium to a point source, and by convolving this function with the source term, the solution to the diffraction problem can be obtained.

Can Green's Functions be used for any type of diffraction problem?

Green's Functions are most commonly used in the context of Kirchhoff Diffraction Theory, which is based on the scalar wave equation. However, they can also be applied to other types of diffraction problems, such as those involving vector waves or electromagnetic waves.

What are the advantages of using Green's Functions in diffraction problems?

Green's Functions offer a systematic and efficient approach to solving diffraction problems. They allow for the separation of variables and can be used to find the solution for any given source distribution. Additionally, they can be combined with other mathematical techniques, such as Fourier transforms, to solve more complex diffraction problems.

Are there any limitations to using Green's Functions in Kirchhoff Diffraction Theory?

Green's Functions are based on certain assumptions, such as the scalar wave equation and the validity of the Kirchhoff approximation. These assumptions may not hold true in all diffraction scenarios, which can limit the accuracy of the solutions obtained using Green's Functions. Additionally, Green's Functions may become more complex to use when dealing with non-homogeneous or anisotropic media.

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