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To solve surface charge problems, we break the surface into symmetrical differential “stripes” that match the shape of the surface; here, we’ll use rings, as shown in the figure. Again, by symmetry, the horizontal components cancel and the field is entirely in the vertical direction. The vertical component of the electric field is extracted by multiplying by , so
As before, we need to rewrite the unknown factors in the integrand in terms of the given quantities. In this case,
(Please take note of the two different “ r ’s” here; r is the distance from the differential ring of charge to the point P where we wish to determine the field, whereas is the distance from the center of the disk to the differential ring of charge.) Also, we already performed the polar angle integral in writing down dA .
or, more simply,
which is the expression for a point charge
Check Your Understanding How would the above limit change with a uniformly charged rectangle instead of a disk?
The point charge would be where a and b are the sides of the rectangle but otherwise identical.
As , [link] reduces to the field of an infinite plane , which is a flat sheet whose area is much, much greater than its thickness, and also much, much greater than the distance at which the field is to be calculated:
Note that this field is constant. This surprising result is, again, an artifact of our limit, although one that we will make use of repeatedly in the future. To understand why this happens, imagine being placed above an infinite plane of constant charge. Does the plane look any different if you vary your altitude? No—you still see the plane going off to infinity, no matter how far you are from it. It is important to note that [link] is because we are above the plane. If we were below, the field would point in the direction.
However, in the region between the planes, the electric fields add, and we get
for the electric field. The is because in the figure, the field is pointing in the + x -direction.
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