Integral form of Poisson's equation

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Discussion Overview

The discussion revolves around the integral form of Poisson's equation, specifically examining the relationship between the equation ##V(\textbf{r}) = \frac{1}{4 \pi \epsilon_0} \int \frac{1}{|\textbf{r}-\textbf{r}^{'}|}\ \rho(\textbf{r}^{'})\ d \tau^{'}## and its differential form ##\nabla^{2} V = - \frac{1}{\epsilon_0} \rho##. Participants explore mathematical derivations, the role of Green's functions, and the implications of these equations in physics.

Discussion Character

  • Technical explanation
  • Mathematical reasoning
  • Debate/contested

Main Points Raised

  • One participant asserts that the integral form is indeed the correct representation of Poisson's equation and discusses the derivation involving point-like sources and Coulomb's Law.
  • Another participant requests a proof of the relationship involving the Dirac delta function and its connection to the integral form of Poisson's equation.
  • A later reply provides a detailed mathematical formulation of deriving the Green's function for the Laplace operator, including the use of spherical coordinates and integration techniques.
  • Some participants express a desire to study Green's functions further before engaging with the mathematical proofs presented.

Areas of Agreement / Disagreement

Participants generally agree on the validity of the integral form of Poisson's equation, but there is no consensus on the specific steps or methods to derive it, as multiple approaches and interpretations are discussed.

Contextual Notes

Some mathematical steps and assumptions in the derivations remain unresolved, particularly regarding the treatment of the Dirac delta function and the implications of using spherical coordinates in the context of singularities.

Who May Find This Useful

This discussion may be useful for students and professionals interested in mathematical physics, particularly those studying electrostatics, differential equations, and Green's functions.

spaghetti3451
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Is it true that ##V(\textbf{r}) = \frac{1}{4 \pi \epsilon_0} \int \frac{1}{|\textbf{r}-\textbf{r}^{'}|}\ \rho(\textbf{r}^{'})\ d \tau^{'}## is the integral form of Poission equation ##\nabla^{2} V = - \frac{1}{\epsilon_0} \rho##?

Can you trace the steps that lead from one to the other, or at the very least offer some possible way to tackle the proof?
 
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Yes, it is. It is a very important insight, because it provides a simple example for a Green's function. I set ##\epsilon_0=1## (Heaviside-Lorentz units). Then you have to solve
\begin{equation}
\label{1}
\Delta \Phi(\vec{x})=-\rho(\vec{x}).
\end{equation}
Now you can think of the field ##\Phi## as of made up by a field, which is due to very many point-like sources, located at places ##\vec{r}'## with charge
\begin{equation}
\label{2}
\mathrm{d} Q=\mathrm{d}^3 \vec{x}' \rho(\vec{x})'.
\end{equation}
You know the solution for that case, because it's simply the Coulomb Law for a charge siting at ##\vec{r}'##. This makes a contribution to the field of
\begin{equation}
\label{3}
\mathrm{d} \Phi(\vec{x})=\mathrm{d}^3 \vec{x}' \rho{\vec{x}'} \frac{1}{4 \pi |\vec{x}-\vec{x}'|}.
\end{equation}
Now the Poisson equation is a linear differential equation, and thus the total field is just given by "summing" up all the contributions. But since you've a continuous charge distribution this "sum" turns into an integral over the infinitesimal charge increments (\ref{2}), i.e.,
\begin{equation}
\label{4}
\Phi(\vec{x})=\int_{V} \mathrm{d}^3 \vec{x}' \frac{\rho(\vec{x}')}{4 \pi |\vec{x}-\vec{x}'|}.
\end{equation}
This is the physicists' shortcut to the solution.

It ist worthwhile to study the mathematical formalism behind it. I'll explain this tomorrow (lack of time now :-().
 
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Thanks!

I'll read up on Green's functions in the meantime!
 
failexam said:
Is it true that ##V(\textbf{r}) = \frac{1}{4 \pi \epsilon_0} \int \frac{1}{|\textbf{r}-\textbf{r}^{'}|}\ \rho(\textbf{r}^{'})\ d \tau^{'}## is the integral form of Poission equation ##\nabla^{2} V = - \frac{1}{\epsilon_0} \rho##?

Can you trace the steps that lead from one to the other, or at the very least offer some possible way to tackle the proof?

Are you familiar with the Dirac delta function? [tex]\rho ( x ) = \int d^{3} \bar{x} \ \rho ( \bar{x} ) \ \delta^{3} ( x - \bar{x} ) .[/tex]
Can you prove (or do you know) the following relation? [tex]\nabla^{2} | \frac{1}{x - \bar{x}} | = - 4 \pi \ \delta^{3} ( x - \bar{x} ) ,[/tex] where [itex]x[/itex] and [itex]\bar{x}[/itex] are vectors in [itex]\mathbb{R}^{3}[/itex]. These two relations let you go from the differential representation to the integral one and vice versa.
Sam
 
So here's the promised more mathematical formulation. There are two ways to derive the Green's function for the Laplace operator: You can use Fourier transformation to "momentum space" and then do the back transformation or you integrate the defining equation (see the previous posting):

\begin{equation}
\label{1}
\Delta G(\vec{x}-\vec{x}')=-\delta^{(3)}(\vec{x}-\vec{x}'),
\end{equation}

where I already used the translation invariance of the Green's function to write ##G(\vec{x}-\vec{x}')##. So we can as well solve
\begin{equation}
\label{2}
\Delta G(\vec{x})=-\delta^{(3)}(\vec{x}).
\end{equation}
Let's follow the approach to directly integrate the equation. Since everything is radially symmetric around the origin in (\ref{2}), we can introduce spherical coordinates. There's however one caveat: You cannot express the ##\delta## distribution peaked at the origin in these coordinates, because they are singular along the ##z## axis. But for ##\vec{x} \neq 0## you just have
\begin{equation}
\label{3}
\Delta G(\vec{x})=0, \quad \vec{x} \neq 0.
\end{equation}
Now we can look for the radially symmetric solution of this potential equation, i.e., we make the Ansatz ##G(\vec{x})=G(r)## with ##r=|\vec{x}|##. Then we use the Laplace operator in spherical coordinates to get
\begin{equation}
\label{4}
\frac{1}{r} (rG)''=0.
\end{equation}
This you can immediately integrate twice. In the first step you get
\begin{equation}
\label{5}
(r G)'=C_1 =\text{const}.
\end{equation}
Integrating again gives
\begin{equation}
\label{6}
G(r)=C_1+\frac{C_2}{r}.
\end{equation}
Now we want ##G(r) \rightarrow 0## for ##r \rightarrow \infty##, which makes ##C_1=0##.

To determine ##C_2## we must bring in the ##\delta## distribution again. To this end we rewrite ##G## in terms of Cartesian coordinates,
\begin{equation}
\label{7}
G(\vec{x})=\frac{C_2}{\sqrt{x^2+y^2+z^3}}.
\end{equation}
Now we can determine the constant from (\ref{2}). To this end we integrate this equation over a sphere of arbitrary radius ##a## around the origin, using Gauß's integral theorem:
\begin{equation}
\label{8}
\int_{K_a} \mathrm{d}^3 \vec{x} \Delta G(\vec{x}) = \int_{\partial K_a} \mathrm{d}^2 \vec{F} \cdot \vec{\nabla} G(\vec{x}) \stackrel{!}{=} -1.
\end{equation}
Now for ##\vec{r} \neq 0## we have
\begin{equation}
\label{9}
\vec{\nabla} G(r)=(\vec{\nabla} r) G'(r)=-C_2 \frac{\vec{x}}{r^3}.
\end{equation}
In spherical coordinates the normal-surface element of the sphere is
\begin{equation}
\label{10}
\mathrm{d}^2 \vec{F}=\mathrm{d} \vartheta \mathrm{d} \varphi \vec{e}_r r^2 \sin \vartheta.
\end{equation}
Plugging everything into (\ref{8}) gives
\begin{equation}
-4 \pi C_2=-1 \; \Rightarrow \; C_2=\frac{1}{4 \pi},
\end{equation}
leading to the correct result, namely the Coulomb potential for a unit charge at the origin,
\begin{equation}
G(\vec{x})=\frac{1}{4 \pi |\vec{x}|}.
\end{equation}
 
Last edited:
This is some pretty heavy-going mathematics. I'll wait till I study Green's functions from Sadri's textbook and then tackle the proof.
 

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