Griffiths 3rd Ed. Page 80 Homework: V(\vec{r}) Wrong?

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In summary, the conversation discusses an apparent inconsistency in Griffiths' E and M book regarding the transformation of a line integral along a path in the reverse direction. The conversation presents a formal path on the z-axis and concludes that there are two sign changes that result in the path integral being equivalent to an ordinary integral. This resolves the inconsistency and confirms that Griffiths was correct. However, the logic behind the transformation may seem unintuitive.
  • #1
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Homework Statement


Please stop reading unless you have Griffith's E and M book (3rd Edition).

Maybe I am nitpicking, but I think the sign is wrong on the last equation on page 80. The formula for the potential was

[tex] V(\vec{r}) = -\int_{O}^{\vec{r}}\vec{E}\cdot d\vec{l} [/tex]

Thus when you come in from z = infinity along the z axis [itex] \vec{E}\cdot d\vec{l} [/itex] becomes E(-dz) right ?

Homework Equations


The Attempt at a Solution

 
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  • #2
Suppose we have a line integral of some vector field along the curve [itex]\vec \gamma (t)[/itex]:

[tex]\Phi = \int_{\vec a}^{\vec b} \vec F \cdot d\vec \ell.[/tex]

Formally, this is given by

[tex]\Phi = \int_{t_a}^{t_b} \vec F \cdot \frac{d\vec \gamma}{dt} \; dt[/tex]

where [itex]d\vec\ell = (d\vec \gamma / dt) \; dt[/itex].

However, suppose we were to integrate [itex]\vec F[/itex] along the same path, but in the reverse direction, from [itex]\vec b[/itex] to [itex]\vec a[/itex]? We would expect to get the negative of our original result. This is identical to taking the path [itex]\vec \gamma (t)[/itex] in the opposite direction,

[tex]\vec \gamma (t) \rightarrow \vec \gamma (-t).[/tex]

But in that case, we also have

[tex]dt \rightarrow -dt[/tex]

and

[tex]\frac{d\vec \gamma}{dt} \rightarrow -\frac{d\vec \gamma}{dt}.[/tex]

Therefore,

[tex]\Phi = -\int_{\vec b}^{\vec a} \vec F \cdot d\vec \ell = -\int_{t_b}^{t_a} \vec F \cdot \left(-\frac{d\vec \gamma}{dt}\right) \; (-dt) = -\int_{t_b}^{t_a} \vec F \cdot \frac{d\vec \gamma}{dt} \; dt.[/tex]

Or in other words, apparently a reversal of path direction,

[tex]t \rightarrow -t[/tex]

results in

[tex]d\vec\ell \rightarrow d\vec\ell.[/tex]

That is, [itex]d\vec\ell[/itex] doesn't transform like an ordinary vector.

So, maybe as an exercise, try to resolve the apparent inconsistency in Griffiths by defining a formal path [itex]\vec\gamma(t)[/itex] which happens to lie on the z-axis. Do the formal substitution to reduce the path integral to an ordinary integral, and you should find that you pick up two sign changes; one from [itex]d\vec\gamma / dt[/itex] and one from [itex]dt[/itex].
 
  • #3
Let [itex]\gamma(t) = (0,0,-t)[/itex].

Then [tex] V(\vec{r}) = -\int_{O}^{\vec{r}}\vec{E(\gamma)}\cdot d\vec{l} = -\int_{t=-\infty}^{-z}\vec{E(\gamma)}\cdot \frac{d\gamma}{dt} dt = -\int_{t=-\infty}^{-z}\vec{E(\gamma)}\cdot \frac{d\gamma}{dt} dt = \int_{t=-\infty}^{-z}\vec{E_z((0,0,-t))} dt = -\int_{t=\infty}^{z}\vec{E_z((0,0,t))} dt [/tex]

[tex]= -(V((0,0,z))-V((0,0,\infty))) = V((0,0,\infty))-V((0,0,z)) [/tex]

So, Griffiths was right. That is so unintuitive! But if you go from z to infinity, then you can just use -dz and integrate from z to infinity ?? Why does that make any sense when you are going "outward"??
 
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FAQ: Griffiths 3rd Ed. Page 80 Homework: V(\vec{r}) Wrong?

1. What is the reason for the mistake in the homework?

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