Green's function for problems involving linear isotropic media

  • #1
spin_100
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TL;DR Summary
Is there a way to tackle problems involving linear isotropic dielectric media with permittivity separated by a boundary directly using an appropriate green's function? I am studying electrodynamics from Jackson's electrodynamics and after learning about the power of using green's function to solve boundary value problems, I was wondering if there is something similar to this for dielectric media. I have shown my approach here but I am stuck at a point.
I am considering a simple problem of a sphere of isotropic dielectric media (permittivity ## \epsilon ## and Radius ##R##) placed in a uniform electric field ## E_0 ## (z-direction). The problem is from Griffiths Chapter 4, example 7.
Since, it is a linear dielectric material, ## D = \epsilon E ## Since there is a discontinuity in ## \epsilon ##
We can model ## \epsilon (r) = \epsilon \theta (R-r) + \epsilon_0 \theta (r-R)##
Taking the divergence of D and since there are no free charges. (external charges) we get $$ 0 = \epsilon(r) \nabla \cdot E + \delta (R-r) ( \epsilon_0 - \epsilon ) E \cdot r$$

Then, we get the possion's equation $$ \nabla \cdot E = - \delta (R-r) ( \epsilon_0 - \epsilon ) E \cdot r $$ After that I don't know how to proceed further. I solved for the potential using an appropriate green's function but the result I am getting is wrong.
 
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  • #2
You can get the Green's function using the image-charge concept. The Green's ##G(\vec{x},\vec{x}')## function is given by the solution of the problem having a "unit charge" at ##\vec{x}'##. Then you need an image charge (distinguishing the cases when ##\vec{x}'## is inside or outside the sphere). The case of a homogeneous electric field is given by taking two charges ##\pm Q## to infinity and moving them to ##\pm \infty \vec{e}_z## (for the asymptocally constant electric field in the ##z## direction).

You can also solve the problem with the asymptotically constant electric field by making a multipole-expansion ansatz. From symmetry it's a priori clear that you only need to go to the dipole order.
 
  • #3
vanhees71 said:
You can get the Green's function using the image-charge concept. The Green's ##G(\vec{x},\vec{x}')## function is given by the solution of the problem having a "unit charge" at ##\vec{x}'##. Then you need an image charge (distinguishing the cases when ##\vec{x}'## is inside or outside the sphere). The case of a homogeneous electric field is given by taking two charges ##\pm Q## to infinity and moving them to ##\pm \infty \vec{e}_z## (for the asymptocally constant electric field in the ##z## direction).

You can also solve the problem with the asymptotically constant electric field by making a multipole-expansion ansatz. From symmetry it's a priori clear that you only need to go to the dipole order.
Please provide a reference where such a method is discussed.
 

FAQ: Green's function for problems involving linear isotropic media

What is Green's function in the context of linear isotropic media?

Green's function is a mathematical tool used to solve differential equations that describe physical phenomena in linear isotropic media. It represents the response of the system to a point source, allowing for the solution of complex boundary value problems by superimposing the effects of simpler solutions.

How is Green's function constructed for a given problem in linear isotropic media?

Green's function is constructed by finding a solution to the governing differential equation with a delta function source term. This involves solving the equation subject to appropriate boundary conditions to ensure that the solution is physically meaningful and satisfies the properties of the medium.

What are the applications of Green's function in linear isotropic media?

Green's function is widely used in various fields such as acoustics, electromagnetism, elasticity, and heat conduction. It helps in solving problems related to wave propagation, stress analysis, temperature distribution, and more by providing a fundamental solution that can be used to build more complex solutions.

What are the advantages of using Green's function in solving physical problems?

Using Green's function simplifies the process of solving differential equations by converting the problem into an integral equation. This approach allows for the superposition of solutions, making it easier to handle complex boundary conditions and source distributions. It also provides a clear physical interpretation of the response of the system to external influences.

Can Green's function be used for nonlinear or anisotropic media?

Green's function is specifically designed for linear and isotropic media. For nonlinear or anisotropic media, the approach needs to be modified, and different techniques or approximations are required. In such cases, numerical methods or perturbation techniques are often employed to obtain approximate solutions.

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