Electric Fields from Linear Charges

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SUMMARY

The discussion focuses on calculating the electric field at the center of a semi-circle of radius R with a uniform charge Q. The key equations used include E = (k*q)/(r^2) and λ = Q/(π*R). Participants emphasize the importance of breaking down the electric field contributions into x and y components, specifically noting that the sine function must be included in the calculations to ensure accuracy. The symmetry of the problem leads to the conclusion that the y-component of the electric field (Ey) is zero, allowing Ex to represent the total electric field at the center.

PREREQUISITES
  • Understanding of electric fields and point charges
  • Familiarity with calculus, particularly integration
  • Knowledge of polar coordinates and their application in physics
  • Proficiency in using the equations for electric field and linear charge density
NEXT STEPS
  • Study the derivation of electric fields from continuous charge distributions
  • Learn about the application of symmetry in electric field calculations
  • Explore the use of polar coordinates in solving physics problems
  • Investigate the impact of charge distribution on electric field strength
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Students and educators in physics, particularly those studying electromagnetism and electric fields, as well as anyone involved in solving problems related to charge distributions and electric forces.

Mark Zhu
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Homework Statement


Am amount of charge Q is uniformly spread over a semi-circle of radius R whose center is located a distance A from the origin. What point charge would have to be placed at the origin so that the E field at the center of the circle is 0? (The open end of the semi-circle is facing away from the origin, and is symmetric about the x axis).

Homework Equations


E = (k*q)/(r^2)
λ = Q/(pi*R)
λ = dq/ds
ds = R*dθ

The Attempt at a Solution


First we break up the entire line of charge into tiny bits of charge 'dq'. We look at a single 'dq' and consider the tiny charge's contribution to the electric field at point 'A' (the center of the semi-circle) in the x and y directions. We integrate 'dEx' and 'dEy' both with respect to 'θ' over the entire semi-circle of charge. Of course, we have to first do a series of substitutions for some of the variables using the above "relevant equations", before we can actually do the two integrations. Then we get 'Ex' and 'Ey', and all is well.

My question is since in this problem 'Ey' turns out to be zero due to symmetry, and so 'Ex' equals 'E', do we even need to break up 'dE' into its x and y components? If not, then in the integral of 'dEx' we could leave out the annoying 'sin θ' thus simplifying the calculation.
 
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Mark Zhu said:
My question is since in this problem 'Ey' turns out to be zero due to symmetry, and so 'Ex' equals 'E', do we even need to break up 'dE' into its x and y components? If not, then in the integral of 'dEx' we could leave out the annoying 'sin θ' thus simplifying the calculation.
You can invoke symmetry and that should be sufficient. However, you can also do the integral for Ey formally and verify that it is zero. Either way is correct.
 
Mark Zhu said:

Homework Statement


Am amount of charge Q is uniformly spread over a semi-circle of radius R whose center is located a distance A from the origin. What point charge would have to be placed at the origin so that the E field at the center of the circle is 0? (The open end of the semi-circle is facing away from the origin, and is symmetric about the x axis).

The Attempt at a Solution


...

My question is since in this problem 'Ey' turns out to be zero due to symmetry, and so 'Ex' equals 'E', do we even need to break up 'dE' into its x and y components? If not, then in the integral of 'dEx' we could leave out the annoying 'sin θ' thus simplifying the calculation.
You must include the "annoying" ##\sin\theta## to get ##E_x ~ .##
 
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tHANKS FOR THE HELPFUL POST!
 
You must include ##\sin\theta## to get the correct expression for ##E_x##. The correct contribution to ##E_x## from each dq includes the ##\sin\theta## term, otherwise you would integrating the wrong contribution from each dq and thus you would getting the wrong result for ##E_x##.

Because the contributions to ##E_y## sum up to zero due to symmetry, this doesn't give you the right "to transfer" the ##E_y## contributions to ##E_x## contributions and thus omit the ##\sin\theta## term.
 
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Thank you for all your great help guys, I understand it now.
 
oh
 
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Tip: Doing this in polar coordinates should help. After you've cart bashed it, try by polars too.
 

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