Solution of Poisson's Equation

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Discussion Overview

The discussion revolves around the solution of Poisson's equation in electrostatics, specifically exploring the differences between a proposed double integral approach and the use of Green's functions. Participants examine the implications of these methods in both one-dimensional and multi-dimensional contexts.

Discussion Character

  • Exploratory
  • Technical explanation
  • Mathematical reasoning
  • Debate/contested

Main Points Raised

  • One participant questions why the solution for Poisson's equation in 1D is not simply a double integral, suggesting it leads to a quadratic relation, while noting that the actual solution involves Green's functions yielding a 1/r relation.
  • Another participant clarifies that in 1D, the equation simplifies to a second derivative form, which can be solved by integrating twice with respect to x.
  • A participant introduces the concept of the Coulomb potential as the solution for point charges and explains how continuous charge distributions can be treated as sums of infinitesimal charges, leading to the integral form of the potential.
  • There is a question regarding the origin of the 4π in the denominator of the Coulomb potential, prompting a discussion about its derivation from the Green's function approach.
  • A detailed explanation is provided on how to derive the Green's function for the Laplace operator, including the use of spherical coordinates and Gauss's Law to determine the constant in the Green's function.

Areas of Agreement / Disagreement

Participants express differing views on the methods for solving Poisson's equation, particularly regarding the appropriateness of the double integral approach versus the Green's function method. There is no consensus on a single preferred method, and the discussion remains open-ended.

Contextual Notes

Participants acknowledge that the derivation of the Green's function involves specific assumptions about symmetry and boundary conditions, which may not apply universally. The discussion highlights the complexity of transitioning from one-dimensional to multi-dimensional solutions.

DirecSa
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We all know that Poissson's equation in electrostatic is:

$$\nabla^2\phi=-\frac{\rho}{\epsilon_0}$$

My question is: why the solution, let's say for 1D, is not just double integral as follows:
$$\phi=\iint -\frac{\rho}{\epsilon_0} d^2x$$

which gives x square relation. But the actual solution comes from using Green's function and it gives the relation one over r (1/r). I need the connection between these things how they come to this and not that...

Thank you!
 
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It should be
$$\Delta \phi=-\frac{1}{\epsilon_0} \rho.$$
In 1 dimension the equation simply reads
$$\phi''=-\frac{1}{\epsilon_0} \rho,$$
and this you get a solution by simply integrating twice wrt. ##x##.

However in more than 1 dimension you need the Green's function, and it's easy to find from physical arguments in this case: For the point charge ##q## at position ##\vec{x}'## the potential is of course the Coulomb potential
$$\phi_{\text{C},\vec{x}'}(\vec{x})=\frac{q}{4 \pi \epsilon_0|\vec{x}-\vec{x}'|}.$$
Now you can consider the continuous charge distribution, described by the charge density ρ, as consisting of an infinite number of infinitesimal charges ##\mathrm{d} q=\mathrm{d}^3 x' \rho(\vec{x}')##, located around ##\vec{x}'##, and because the Poisson equation is linear you get the total potential by summing or, since we have a continuous charge distribution, rather integrating, over the Coulomb potentials of all these charges, i.e.,
$$\phi(\vec{x})=\int_{\mathbb{R}^3} \mathrm{d}^3 x' \rho(\vec{x}') \frac{1}{4 \pi \epsilon_0 |\vec{x}-\vec{x}'|}.$$
Formally the charge density of a point charge is
$$\rho_{\text{P},\vec{x}'}(\vec{x})=q \delta^{(3)}(\vec{x}-\vec{x}').$$
and that's why the Coulomb potential is the Greens' function of the operator ##-\Delta## in the sense that from this it follows that
$$-\Delta \phi_{\text{C},\vec{x}'}(\vec{x}')=-\Delta \frac{q}{4 \pi \epsilon_0 |\vec{x}-\vec{x}'|} = \frac{q}{\epsilon_0} \delta^{(3)}(\vec{x}-\vec{x}').$$
These hand-waving physical arguments can of course be made mathematically rigorous.
 
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Thank you so much, now it is more clear for me. And also I added the minus. Maybe just a question regarding the 4pi in the denominator.. does it come from a physical definition or mathematical concept?
 
That comes from finding the Green's function. The idea is not so difficult. You need to solve for
$$-\Delta G(\vec{x})=\delta^{(3)}(\vec{x}).$$
The right-hand side is obviously rotation symmetric. That's why we can conclude that ##G## should depend on ##r=|\vec{x}|## only. Now using the Laplace operator in sphercical coordinates, this leads to
$$-\frac{1}{r} [r G(r)]''=0 \quad \text{for} \quad r \neq 0.$$
You get the general solution by just integrating twice (it's effectively a 1D problem due to this symmetry!):
$$(r G)''=0 \; \Rightarrow r G=A+B r \; \Rightarrow \; G=\frac{A}{r} + B$$
with integration constants ##A## and ##B##. First we want to have ##G \rightarrow 0## for ##r \rightarrow \infty##. This implies ##B=0##. Thus you have
$$G(r)=\frac{A}{r}.$$
To get ##A## we integrate ##\Delta G(r)## over a sphere of radius ##a## around the origin and use Gauss's Law,
$$\int_{S_a} \mathrm{d}^3 r \Delta G(r) = \int_{\partial S_a} \mathrm{d}^2 \vec{f} \cdot \vec{\nabla} G(r).$$
The surface normal vector in spherical coordinates is
$$\mathrm{d}^2 \vec{f} = a^2 \sin \vartheta \mathrm{d} \vartheta \mathrm{d} \varphi \vec{e}_r.$$
The gradient is
$$\vec{\nabla} G(r)=G'(r) \vec{\nabla} r = G'(r) \vec{e}_r=-\frac{A}{r^2} \vec{e}_r$$
and thus
$$\int_{S_a} \mathrm{d}^3 r \Delta G(r) = -\int_0^{\pi} \mathrm{d} \vartheta \int_0^{2 \pi} \mathrm{d} \varphi a^2 \sin \vartheta \frac{A}{a^2} = -4 \pi A.$$
On the other hand ##\Delta G(r)=-\delta^{(3)}(\vec{r})## and thus
$$\int_{S_a} \mathrm{d}^3 \Delta G(r)=-1 \; \Rightarrow \; -4 \pi A=-1 \; \Rightarrow \; A=\frac{1}{4 \pi}.$$
Thus the Green's function of ##-\Delta## is
$$G(r)=\frac{1}{4 \pi r},$$
which is what we wanted to prove.
 
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very grateful, thank you a lot :)
 

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