Potential Difference of Inverted Hemispherical Shell

AI Thread Summary
The discussion centers on calculating the potential difference between the north pole and the center of an inverted hemispherical shell with a uniform surface charge density σ. The correct answer is confirmed as (Rσ/2ε0)(√2 - 1), but the user struggles with verifying this result using Poisson's Equation. It is noted that Poisson's Equation involves volume charge density, which complicates the application since the interior of the hemisphere has zero charge density. An alternative approach suggested is to calculate the electric field directly and integrate it from the pole to the center. This highlights the challenges in using traditional methods for surface charge problems.
Jonathan K
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The problems states: An inverted hemispherical bowl of radius R carries a uniform surface charge density σ. Find the potential difference between the north pole and the center.

I was able to do the problem and got the correct answer the book gives, which is (Rσ/2ε0)(√2 - 1). My professor, however asks that we do an assessment, or check, of our answer for every problem. This is where I am having troubles. I figured I could use Poisson's Equation to show that the Laplacian of the answer is -σ/ε0, but I can't seem to get this. Any other ideas?
 
Jonathan K said:
The problems states: An inverted hemispherical bowl of radius R carries a uniform surface charge density σ. Find the potential difference between the north pole and the center.

I was able to do the problem and got the correct answer the book gives, which is (Rσ/2ε0)(√2 - 1). My professor, however asks that we do an assessment, or check, of our answer for every problem. This is where I am having troubles. I figured I could use Poisson's Equation to show that the Laplacian of the answer is -σ/ε0, but I can't seem to get this. Any other ideas?
Well, sice no one else has responded in a week ..for what it's worth, probably not much ...

Poisson's equation is ∇2V = -ρ/ε with ρ = volume, not surface, density, so your units would be incorrect.

Also, the entire volume inside the hemisphere has ρ = 0. But I don't see that solving for ∇2V = 0 would be pleasant, since V varies not only along the z axis (assuming the hemisphere axis is the z axis and the bottom rests symmetrically on the x-y plane), but also with x and y (or similar problem if you went cylindrical or spherical.) The only alternative that comes to mind is solving for the E field directly and integrating from the pole to the bottom center.
 
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