Proof divergence of vector potential = 0

grantdenbrock
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Homework Statement


I need to show that $$\del*\vec{A(\vec{r})}=\frac{\mu}{4\pi}\int{\frac{\vec{J{vec\r'}}}{\vec{R}}}d\tau=0$$
where A is the vector potential and R refers to "script r" or (r-r') where r is source point of charge and r' is the measurement point. tau refers to a volume integral. I have tried many times now to show this by bringing del into the integrand using product rules and the fact that $$\delR=-\del'R'$$ but cannot make it equal zero. I am not sure if there is something I have overlooked or another method to use but any help or suggestions are much appreciated!

Homework Equations


del*R=-del'R' must be used at some point[/B]

The Attempt at a Solution


My solution thus far goes like this (Sorry My latex is awful so I will just write out my method)
1) bring Del into the integrand
2) using product rule rule of dot products expand into 2 terms each with its own dot product
3) del*J' =0 since del operates on unprimed coordinates
4) J' del*1/R does not equal zero therefore integrand does not equal zero :/[/B]
 
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I should add that its divergence of A, meaning del dot A =0 . Also, I am aware of the other thread regarding this problem however that thread does not contain any useful information or attempt a solution.
 
From what you've said, you should be able to show that
$$ \nabla \cdot \mathbf{A}(\mathbf{x}) = - \frac{\mu}{4\pi} \int \mathbf{J}(\mathbf{x}') \cdot \nabla' \left(\frac{1}{|\mathbf{x}- \mathbf{x}'|} \right) d\mathbf{x}'.$$
The next step would be to integrate by parts and argue that both terms vanish independently subject to reasonable assumptions.
 

You write "... r is source point of charge ..." but don't you mean "source point of current density"? The integral certainly looks like the magnetic vector potential, especially with the μ in it ... based on that assumption I offer the following:

∇⋅A
= 0 is not an identity. It is chosen as a convenience.
We define A as H = ∇ x A.
By Maxwell, ∇ x H = j (j = current density).
So j = ∇ x (∇ x A).
But by a mathematical identity, this can be rewritten as
j = ∇(∇⋅A) - ∇2A
So we choose ∇⋅A = 0, giving
2A = -j
i.e. the Poisson equation, the solution for which is your integral. BTW the denominator in the integrand should read |R|. You can't divide one vector by another, at least not to my knowledge.
 
To solve this, I first used the units to work out that a= m* a/m, i.e. t=z/λ. This would allow you to determine the time duration within an interval section by section and then add this to the previous ones to obtain the age of the respective layer. However, this would require a constant thickness per year for each interval. However, since this is most likely not the case, my next consideration was that the age must be the integral of a 1/λ(z) function, which I cannot model.
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