Potential Difference of Inverted Hemispherical Shell

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SUMMARY

The discussion focuses on calculating the potential difference between the north pole and the center of an inverted hemispherical shell with radius R and uniform surface charge density σ. The correct answer, confirmed by the original poster, is (Rσ/2ε0)(√2 - 1). The challenge arises in verifying this result using Poisson's Equation, where the poster struggles to apply the equation correctly due to confusion between surface and volume charge densities. A suggestion is made to solve for the electric field directly and integrate from the pole to the center as an alternative approach.

PREREQUISITES
  • Understanding of electrostatics, specifically electric potential and charge distributions.
  • Familiarity with Poisson's Equation and its application in electrostatics.
  • Knowledge of the relationship between surface charge density (σ) and volume charge density (ρ).
  • Basic skills in calculus, particularly integration techniques in three dimensions.
NEXT STEPS
  • Review the derivation and applications of Poisson's Equation in electrostatics.
  • Study the relationship between surface charge density and electric field calculations.
  • Learn how to compute electric fields from charge distributions using integration techniques.
  • Explore advanced topics in electrostatics, such as boundary value problems and potential theory.
USEFUL FOR

Students and professionals in physics or engineering, particularly those focusing on electrostatics, electric fields, and potential theory. This discussion is beneficial for anyone looking to deepen their understanding of charge distributions and their implications in electrostatic 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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