Vector calculus question regarding helmholtz theorem

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The discussion focuses on deriving the functions U(r) and W(r) within the context of the Helmholtz theorem and vector calculus. It explains how to express any vector field as a sum of a potential field and a solenoidal field, leading to the formulation of Poisson's equation. The derivation utilizes the Green's function of the Laplace operator, resulting in the expression for U(x) in terms of the source function D(x). The discussion also highlights the gauge invariance of W, emphasizing the common condition that its divergence equals zero. Overall, the thread provides a detailed mathematical framework for understanding these vector functions in relation to physical fields.
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How to get U(r) and W(r), why are them defined out of nowhere, is that the standard structure of that kind of functions ( what kind of functions are them??) ? T.Y
 

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Use the div and curl equations to derive Poisson's equation for two functions (called U and W) with C and D as the source functions.
 
You can express any vector field as the sum of a potential field (curl free) and a solenoidal field (source free):

\vec{F}(\vec{x})=-\vec{\nabla} U(\vec{x})+\vec{\nabla} \times \vec{W}.

Taking the divergence of this equation, you find

\vec{\nabla} \cdot \vec{F}(\vec{x})=-\Delta U(\vec{x})=D(\vec{x}).

Assuming that all the fields vanish sufficiently quickly at infinity and that they are sufficiently well behaved everywhere, this equation (the Poisson-Laplace equation) is solved with help of the Green's function of the Laplace operator:

U(\vec{x})=\int_{\mathbb{R}^3} \mathrm{d}^3 \vec{x}' \frac{D(\vec{x}')}{4 \pi |\vec{x}-\vec{x}'|}.

The Green's function you find by solving the equation

\Delta_{\vec{x}} G(\vec{x}-\vec{x}')=-\delta^{(3)}(\vec{x}-\vec{x}').

This is done most easily by introducing spherical coordinates for \vec{r}=\vec{x}-\vec{x}' \neq {0}.

This yields together with the condition that the Green's function should vanish at infinity,

G(\vec{r})=\frac{C}{|\vec{r}|}.

The constant C is given by integrating the delta distribution over a ball of radius, R:

-1=-\int_{K_R} \mathrm{d}^3 \vec{r} \delta^{(3)}(\vec{r}) \int_{K_R} \mathrm{d}^3 \vec{r} \Delta G(\vec{r})=\int_{\partial K_R} \mathrm{d} \vec{A} \cdot \vec{\nabla} G(\vec{r})=-4 \pi C.

This means C=1/(4 \pi).

Now taking the curl of the above Helmholtz decomposition of the vector field yields

\vec{\nabla} \times \vec{F}=\vec{\nabla} \times (\vec{\nabla} \times \vec{W})=\vec{\nabla} (\vec{\nabla} \cdot \vec{W})-\Delta \vec{W}=\vec{C}.

Now \vec{W} is only determined up to the gradient of a scalar field, and thus we can demand one auxilliary condition (this is a special case of gauge invariance). Here, the condition

\vec{\nabla} \cdot \vec{W}=0

is most costumary since then we have

\Delta \vec{W}=-\vec{C},

and we can again use the Green's function of the Laplace operator to get

\vec{W}(\vec{x})=\int_{\mathbb{R}^3} \mathrm{d}^3 \vec{x}' \frac{\vec{C}(\vec{x}')}{4 \pi |\vec{x}-\vec{x}'|}.
 
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