Stokes's theorem in spherical coordinates

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Problem:

Say we have a vector function ##\vec{F} (\vec{r})=\hat{\phi}##.

a. Calculate ##\oint_C \vec{F} \cdot d\vec{\ell}##, where C is the circle of radius R in the xy plane centered at the origin

b. Calculate ##\int_H \nabla \times \vec{F} \cdot d\vec{a}##, where H is the hemisphere above the xy plane with boundary curve C.

c. Calculate ##\int_D \nabla \times \vec{F} \cdot d\vec{a}##, where D is the disk in the xy plane bounded by C.

(Verify Stokes's theorem in both cases.)

Solution:

First off, isn't it unnecessary to say verify Stokes's theorem in both cases? If we calculate a line integral, and then a surface integral bounded by the same curve, Stokes's theorem states that they're the same, yes?

Moving on...

a. We have [tex]\vec{F} \cdot d\vec{\ell}=(0,0,1)(dr, d\theta, rsin\theta \ d\phi)=rsin\theta \ d\phi[/tex]

So [tex]\oint_C \vec{F} \cdot d\vec{\ell} = Rsin\theta \int_0^{2 \pi} d\phi= 2 \pi R sin \theta[/tex]

Is this correct?

b. We have ##F_r=F_{\theta}=0## and ##F_{\phi}=1##, so for the curl I find [tex]\nabla \times \vec{F}=(\frac{1}{r}tan\theta, 0, -\frac{1}{r})[/tex]

I think this is right so far. But in calculating ##\int_H \nabla \times \vec{F} \cdot d\vec{a}##, I'm not sure what to use as ##d\vec{a}##. Any help? Thanks in advance.
 
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wifi said:
Problem:

Say we have a vector function ##\vec{F} (\vec{r})=\hat{\phi}##.

a. Calculate ##\oint_C \vec{F} \cdot d\vec{\ell}##, where C is the circle of radius R in the xy plane centered at the origin

b. Calculate ##\int_H \nabla \times \vec{F} \cdot d\vec{a}##, where H is the hemisphere above the xy plane with boundary curve C.

c. Calculate ##\int_D \nabla \times \vec{F} \cdot d\vec{a}##, where D is the disk in the xy plane bounded by C.

(Verify Stokes's theorem in both cases.)

First off, isn't it unnecessary to say verify Stokes's theorem in both cases? If we calculate a line integral, and then a surface integral bounded by the same curve, Stokes's theorem states that they're the same, yes?

"Verify Stoke's theorem" means "observe that the line integral is indeed equal to the surface integrals"

Moving on...

a. We have [tex]\vec{F} \cdot d\vec{\ell}=(0,0,1)(dr, d\theta, rsin\theta \ d\phi)=rsin\theta \ d\phi[/tex]

So [tex]\oint_C \vec{F} \cdot d\vec{\ell} = Rsin\theta \int_0^{2 \pi} d\phi= 2 \pi R sin \theta[/tex]

Is this correct?

No. The circle in question is [itex]r = R[/itex], [itex]\theta = \pi/2[/itex] and [itex]\phi \in [0, 2\pi)[/itex]. Thus the element of line length is [itex]\mathrm{d}\vec{l} = R\hat\phi \mathrm{d}\phi[/itex], and the integral is
[tex] \oint_C \vec F \cdot \mathrm{d}\vec{l} = \int_0^{2\pi} R\mathrm{d}\phi[/tex]

b. We have ##F_r=F_{\theta}=0## and ##F_{\phi}=1##, so for the curl I find [tex]\nabla \times \vec{F}=(\frac{1}{r}tan\theta, 0, -\frac{1}{r})[/tex]

I get [itex]\nabla \times \vec F = r^{-1}\tan\theta \hat r - r^{-1}\hat\theta[/itex].


I think this is right so far. But in calculating ##\int_H \nabla \times \vec{F} \cdot d\vec{a}##, I'm not sure what to use as ##d\vec{a}##. Any help? Thanks in advance.

[itex]d\vec a[/itex] is the normal to the surface in question times the element of area. Given the choice of parametrization of the line integral, it's the normal with the non-negative [itex]\hat z[/itex] component.
 
pasmith said:
No. The circle in question is [itex]r = R[/itex], [itex]\theta = \pi/2[/itex] and [itex]\phi \in [0, 2\pi)[/itex]. Thus the element of line length is [itex]\mathrm{d}\vec{l} = R\hat\phi \mathrm{d}\phi[/itex], and the integral is
[tex] \oint_C \vec F \cdot \mathrm{d}\vec{l} = \int_0^{2\pi} R\mathrm{d}\phi[/tex]

Ah, I see. So it's simply the perimeter of a circle. Makes sense. [tex]\int_0^{2\pi} R\mathrm{d}\phi = 2\pi R[/tex]

pasmith said:
I get [itex]\nabla \times \vec F = r^{-1}\tan\theta \hat r - r^{-1}\hat\theta[/itex].

Whoops, yeah that's what I meant.

pasmith said:
[itex]d\vec a[/itex] is the normal to the surface in question times the element of area. Given the choice of parametrization of the line integral, it's the normal with the non-negative [itex]\hat z[/itex] component.

Well in class my prof used ##r^2sin \theta d\theta d \hat{\phi}##. Is that correct? If so, I would like to understand why that's the case.

Thanks, pasmith.
 
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wifi said:
Well in class my prof used ##r^2sin \theta d\theta d \hat{\phi}##. Is that correct? If so, I would like to understand why that's the case.
No, that's not correct. ##d\vec{a}## points in the direction normal to the surface. For the hemisphere, this would be radially outward, so ##d\vec{a}## points in the ##\hat{r}## direction. The magnitude of the area element is ##R^2\sin\theta\,d\theta\,d\phi##.
 
vela said:
No, that's not correct. ##d\vec{a}## points in the direction normal to the surface. For the hemisphere, this would be radially outward, so ##d\vec{a}## points in the ##\hat{r}## direction. The magnitude of the area element is ##R^2\sin\theta\,d\theta\,d\phi##.

That makes perfect sense. So it's ##d\vec{a}=R^2sin \ \theta \ d\theta \ d\phi \ \hat{r}##, right?
 
So when I calculate ## \int_H \nabla \times \vec{F} \cdot d\vec{a} ## does ##r \rightarrow R## in ##\nabla \times \vec{F}=(\frac{1}{r}tan \ \theta, -\frac{1}{r}, 0)##? (ie. is it ##\nabla \times \vec{F}=(\frac{1}{R}tan \ \theta, -\frac{1}{R}, 0)##?)
 
Okay. I have to integrate ##sin \ \theta \ tan \ \theta##. This is going to be a mess...
 
Uh oh, on wolfram alpha it's saying this integral does not converge. Something has to be wrong.
 
## \int_H \nabla \times \vec{F} \cdot d\vec{a} = \int (\frac{1}{R}tan \ \theta, -\frac{1}{R},0) \cdot (R^2 sin \ \theta \ d\theta \ d\phi, 0, 0) = \int_0^{2 \pi} \int_0^{\pi} R sin \ \theta \ tan \theta \ d\theta \ d\phi ##. Yes?
 
Yeah I get ##\int_0^{2 \pi} \int_0^{\pi} R cos \ \theta \ d\theta \ d\phi = 2 \pi R##.

Hopefully I can get part c. with no difficulty. I'll keep you posted.
 
So, for the disk we have ## d\vec{A}= - R^2 sin \ \theta \ d\theta \ d \phi \ \hat{\theta}##?
 
wifi said:
Yeah I get ##\int_0^{2 \pi} \int_0^{\pi} R cos \ \theta \ d\theta \ d\phi = 2 \pi R##.
That integral as written should evaluate to ##4\pi R.##

wifi said:
So, for the disk we have ## d\vec{A}= - R^2 sin \ \theta \ d\theta \ d \phi \ \hat{\theta}##?
Nope. For one thing, r isn't constant over the disk. What should the magnitude of the area element be? Which way should it point?
 
vela said:
That integral as written should evaluate to ##4\pi R.##

Ah, ##\theta## should range from 0 to pi/2. Then the integral is correct.

vela said:
Nope. For one thing, r isn't constant over the disk. What should the magnitude of the area element be? Which way should it point?

I'm not sure about the magnitude, but it should point in the +z direction.
 
##d\vec{A}=-rdrd\phi \hat{\theta}##. Using this in the integral (with r:0 to R and Φ:0 to 2π), I get ##2 \pi R##, as expected. Is this correct?
 
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