Solution of Poisson's Equation

In summary, the solution to Poissson's equation in electrostatic is found by integrating over a sphere of radius ##a## around the origin. 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 of this vector is ##\vec{\nabla} G(r)=-G'(r) \vec{\nabla} r = G'(r) \vec{e}_r=-\frac{A}{r^2} \vec{
  • #1
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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  • #2
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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  • #3
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?
 
  • #4
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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  • #5
very grateful, thank you a lot :)
 

1. What is Poisson's Equation?

Poisson's Equation is a mathematical equation that describes the relationship between the distribution of electric charge in a region and the resulting electric potential in that region. It is commonly used in electrostatics and electromagnetism.

2. What is the solution of Poisson's Equation?

The solution of Poisson's Equation is the electric potential in a given region, which is determined by the distribution of electric charge in that region. It is a scalar field that describes the magnitude and direction of the electric potential at every point in the region.

3. How is Poisson's Equation solved?

Poisson's Equation can be solved using various mathematical methods, such as separation of variables, Green's function, and finite difference methods. The specific method used depends on the boundary conditions and the complexity of the problem.

4. What are the applications of Poisson's Equation?

Poisson's Equation has many applications in physics and engineering, particularly in the fields of electrostatics, electromagnetism, and fluid dynamics. It is used to model and solve problems related to electric fields, gravitational fields, and fluid flows.

5. What are the limitations of Poisson's Equation?

Poisson's Equation assumes that the electric potential is a continuous function, which may not always be the case in real-world applications. It also does not take into account the effects of quantum mechanics or special relativity, making it unsuitable for certain scenarios. Additionally, it can only be applied to linear systems, meaning that it cannot accurately describe highly nonlinear systems.

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