Stokes theorem over a hemisphere

In summary, the conversation discusses the evaluation of an integral over the open surface of a hemisphere in 3-D Cartesian space, given a specified vector field and constant. The conversation also mentions the use of Stokes' theorem to switch the integral from the surface of the hemisphere to the surface of the circle on the bottom, but with conflicting results. Further discussion reveals that the line integral and the integral of the curl over the surface give different results, and a method involving replacing 2a^2 with 2x^2+2y^2 is proposed, but ultimately deemed invalid. The correct integral is found to be 4x^2+4y^2.
  • #1
hughb
7
0

Homework Statement


The vector field F is defined in 3-D Cartesian space as
F = y(z^2−a^2)i + x(a^2− z^2)j,
where i and j are unit vectors in the x and y directions respectively, and a is a
real constant.
Evaluate the integral

Integral:(∇ ×F)·dS, where S is the open surface of the hemisphere
x^2+ y^2+ z^2= a^2, z ≥ 0 :
(i) by direct integration over the surface S
(ii) using Stokes’ theorem


Homework Equations


Stokes Theorem


The Attempt at a Solution


I've calculated the integral over the surface and the line integral around the boundary curve, and both answers are 2*pi*a^4. However, my problem is that when i try to use stokes theorem to switch the integral from the surface of the hemisphere to the surface of the circle on the bottom of the hemisphere, via stokes theorem, my answer is half the correct answer.

(∇ ×F).dS = 2a^2 (as z = 0 on circle). 2a^2 = 2x^2+2y^2.

The integral of 2x^2+2y^2 over the surface of the circle is 2*pi*integral(r^3 dr) between 0 and a, which just comes out as pi*a^4.

I'm not sure where I'm going wrong here, maybe the integrand should be a^2 r dr?? But the field varies over the surface of the circle so i don't think this is right??
 
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  • #2
I don't understand what you mean by "However, my problem is that when i try to use stokes theorem to switch the integral from the surface of the hemisphere to the surface of the circle on the bottom of the hemisphere, via stokes theorem, my answer is half the correct answer." The given surface is "the open surface of the hemisphere". There is no "bottom" to be included. And when you say "my answer is half the correct answer", what is the "correct answer".

"I've calculated the integral over the surface and the line integral around the boundary curve, and both answers are 2*pi*a^4." Isn't that all you are asked to do?
 
  • #3
Ok, so I can answer the question, that's fine. But for peace of mind, i tried to check my solutions by switching the integral of the curl of F from the surface of the hemisphere, to the circlular base of the hemisphere as allowed by Stokes theorem. The two integrals should be the same, however, I can't get them to match up.
 
  • #4
hughb said:
Ok, so I can answer the question, that's fine. But for peace of mind, i tried to check my solutions by switching the integral of the curl of F from the surface of the hemisphere, to the circlular base of the hemisphere as allowed by Stokes theorem. The two integrals should be the same, however, I can't get them to match up.

As you correctly got 2a^2 for the function you want to integrate over the disk, why don't you just use that? Don't change it to 2x^2+2y^2. That not correct.
 
  • #5
But 2a^2 is the same as 2x^2+2y^2, but the integral over the area of the circle isn't, if i stick with the 2a^2 and integrate that, then i wouldn't be integrating the field over the disk properly would I? As the field varies over the disk, surely I can't just integrate the constant 2a^2 over the disk, but have to switch to 2x^2+2y^2?
 
  • #6
hughb said:
But 2a^2 is the same as 2x^2+2y^2, but the integral over the area of the circle isn't, if i stick with the 2a^2 and integrate that, then i wouldn't be integrating the field over the disk properly would I? As the field varies over the disk, surely I can't just integrate the constant 2a^2 over the disk, but have to switch to 2x^2+2y^2?

2a^2=2x^2+2y^2+2z^2 is only true on the surface of the hemisphere. It's not true inside of the hemisphere where the surface of the disk is. And in fact it's really easy to integrate 2a^2 over the surface of the disk. It's a constant. Just factor it out and multiply by the area of the disk, pi*a^2.
 
  • #7
Ok, if they aren't the same thing, then when I calculate the direct integral of the curl of F over the hemisphere via projection onto the xy plane, my integral is: 2*pi∫2x^2+2y^2+2a^2 dxdy between 0 and a. The way i calculated this was to let 2a^2 = 2x^2+2y^2 and integrate, giving the correct answer, however, is this a valid method, to replace the 2a^2 this time, but not when i calculate the integral over the disk? If i don't replace the 2a^2, i get the wrong answer.
 
  • #8
hughb said:
Ok, if they aren't the same thing, then when I calculate the direct integral of the curl of F over the hemisphere via projection onto the xy plane, my integral is: 2*pi∫2x^2+2y^2+2a^2 dxdy between 0 and a. The way i calculated this was to let 2a^2 = 2x^2+2y^2 and integrate, giving the correct answer, however, is this a valid method, to replace the 2a^2 this time, but not when i calculate the integral over the disk? If i don't replace the 2a^2, i get the wrong answer.

When you are doing the line integral around the boundary circle, you can use that a^2=x^2+y^2. But that's the only place that it's true. It's not true in the disk and even on the hemisphere it's only true if z=0.
 
  • #9
But this means that the line integral and the integral of the curl over the surface give different results, 2*pi*a^4 for the line integral and 3*pi*a^4 for the surface integral.
 
  • #10
hughb said:
But this means that the line integral and the integral of the curl over the surface give different results, 2*pi*a^4 for the line integral and 3*pi*a^4 for the surface integral.

The quantity I get to integrate dxdy is 2x^2+2y^2+2a^2-2z^2. That reduces to 4x^2+4y^2 which gives the the correct answer. You are right that 2x^2+2y^2+2a^2 would not. Can you show how you got to that point?
 
  • #11
Aha, I think i see where I'm going wrong, I had what you had for the integral, but then assumed z^2=0 as i was projecting onto the plane, is this not the case then? Even if the integral is on the xy plane, does the z component still have to be accounted for?
 
  • #12
hughb said:
Aha, I think i see where I'm going wrong, I had what you had for the integral, but then assumed z^2=0 as i was projecting onto the plane, is this not the case then? Even if the integral is on the xy plane, does the z component still have to be accounted for?

You are integrating over a region in the xy plane, but the quantity you are integrating is evaluated on the hemisphere, where z is not zero.
 
  • #13
Brilliant, I see it, thank you so much - that had been bothering me for days!
 

Related to Stokes theorem over a hemisphere

1. What is Stokes theorem over a hemisphere?

Stokes theorem over a hemisphere is a mathematical theorem in vector calculus that relates the surface integral of a vector field over a hemisphere to the line integral of the same vector field along the boundary of the hemisphere.

2. How is Stokes theorem applied over a hemisphere?

To apply Stokes theorem over a hemisphere, we first need to parameterize the surface of the hemisphere and the boundary curve. Then, we can calculate the surface integral and line integral using the parameterization and use Stokes theorem to relate the two integrals.

3. What are the conditions for Stokes theorem to be applicable over a hemisphere?

The conditions for Stokes theorem to be applicable over a hemisphere are that the vector field must be continuously differentiable on the surface of the hemisphere and its boundary curve, and the surface and boundary must be oriented in a consistent manner.

4. Can Stokes theorem be applied to any surface and boundary?

No, Stokes theorem is applicable only to specific types of surfaces and boundaries, such as a hemisphere, where the conditions mentioned above are met. It cannot be applied to arbitrary surfaces and boundaries.

5. What is the significance of Stokes theorem over a hemisphere?

Stokes theorem over a hemisphere is an important tool in vector calculus, as it allows us to relate surface integrals to line integrals, making it easier to calculate and understand the behavior of vector fields in three-dimensional space.

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