Calculating Total Charge on a Disk with Varying Charge Density

In summary: Sorry that my attempt at answering your question fell so short of what you wanted. I'll be sure to try so much harder in the future.
  • #1
Punkyc7
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Electric charge is distributed over a disk x^2+Y^2<=4 so that the charge density at (x,y) is

o(x,y)= x+y+x^2+y^2

what is the total charge on the disk

so I change to polar and get (rcos +rsin +r^2)rdrdtheta
and my limits go from 0 to 2pi and 0 to 2

for my answer i got 8 pi I am just wondering if that is right
 
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  • #2
What's the question?
 
  • #3
He wants to know if he's correct in his answer.
 
  • #4
Char. Limit said:
He wants to know if he's correct in his answer.

zhermes wants to know what was the question that Punkyc7 was answering when Punkyc7 asked if the answer was correct.

That's a valid inquiry by zhermes.
 
  • #5
I would guess that Punkyc7 was asking if [itex]8\pi[/itex] is the total charge on the disc- though he did not specfically say that.

Punkyc7, I do NOT get [itex]8\pi[/itex]. Show us what you did and we will decide which of us made a mistake.
 
  • #6
my question was it it correct, for the total charge on the disk


any ways

i integrated with respect to r and gotr^4/4+(r^3/3)cos+(+(r^3/3)sin evaluated from 0 to2



so i got 4+8/3 cos +8/3 sin and then i evaluted with respect to theta and got

8pi +8/3 sin-8/3 cos evaluated from 0 to 2pi


sin drops out and -8/3 -(8/3) drops out

so 8 pi that how i got my answer, i guess my question now is where did i go wrong
 
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  • #7
is it in my limits or in my conversion to polar
 
  • #8
The cos(θ) term also drops out.

cos(2π) = cos(0)
 
  • #9
I don't think there's any error. I get 8pi. The sin and cos terms both integrate to zero. So you've got just r^3*dr*dtheta. Looks like 8pi to me.
 
  • #10
Dick said:
I don't think there's any error. I get 8pi. The sin and cos terms both integrate to zero. So you've got just r^3*dr*dtheta. Looks like 8pi to me.
Absolutely correct. To elaborate a little... Punkyc7: if you look at the part of the equation, o(x,y)= x, this will be positive on one half of the disk, and just as much negative on the opposite side of the disk. Therefore the total is zero. The same argument applies to o(x,y) = y. Thus, as SammyS and dick point out, both of those terms fall out of the integral.

Char. Limit said:
He wants to know if he's correct in his answer.
That's outrageously helpful, thanks.
 
  • #11
zhermes said:
That's outrageously helpful, thanks.

Sorry that my attempt at answering your question fell so short of what you wanted. I'll be sure to try so much harder in the future.
 

FAQ: Calculating Total Charge on a Disk with Varying Charge Density

What is charge density over a disk?

Charge density over a disk refers to the amount of electric charge present per unit area on a disk-shaped surface. It is usually denoted by the symbol σ and has units of coulombs per square meter (C/m^2).

How is charge density over a disk calculated?

Charge density over a disk can be calculated by dividing the total amount of charge on the disk by the surface area of the disk. It can also be calculated by taking the limit of the charge per unit area as the area approaches zero.

What factors affect charge density over a disk?

The two main factors that affect charge density over a disk are the amount of charge on the disk and the surface area of the disk. The charge density will increase as the amount of charge increases or as the surface area decreases.

How does charge density over a disk relate to electric field?

Charge density over a disk is directly related to the electric field generated by the disk. The higher the charge density, the stronger the electric field will be. This relationship is described by Gauss's Law.

Can charge density over a disk vary across the surface?

Yes, charge density can vary across the surface of a disk. This is because the charge may not be distributed evenly across the surface, leading to areas of higher or lower charge density. This can also be affected by the shape and orientation of the disk.

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