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Introductory Physics Volume Two

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50 Electric Potential 2.7<br />

The change in potential energy of the electron will be:<br />

Use conservation of energy:<br />

∆U = q∆V = (−e)∆V.<br />

∆U + ∆K = −e∆V + ( 1 2 m ev 2 − 0) = 0<br />

√ √<br />

2e∆V 2(1.6 × 10<br />

−→ v = =<br />

−19 C(+9V)<br />

m e 9.11 × 10 −31 kg<br />

= 1.78 × 10 6 m s<br />

Example<br />

Near the surface of the Earth, there is always a background electric<br />

field that averages 100N/C and points down. Assuming the Earth to be<br />

a perfect conductor, how much electric charge is stored on the Earth’s<br />

surface?<br />

Since the electric field points down, we know the Earth’s charge is negative.<br />

So, lets find the magnitude. Use the previous result to determine<br />

the surface charge density:<br />

E = σ ɛ 0<br />

−→ σ = Eɛ 0 .<br />

Multiply this by the Earth’s surface area to get the total charge:<br />

Q E = σ(4πR 2 E) = Eɛ 0 (4πR 2 E) = 453, 000C<br />

Example<br />

<strong>Two</strong> equal and opposite charges are located a distance a apart. Find<br />

the electric field and the electric potential at a) the point directly between<br />

the two charges and b) the point a distance a/2 directly above<br />

the point inbetween the two charges.<br />

+q -q<br />

The electric fields due to each charge point in the same direction at the<br />

center point c:<br />

a<br />

E +<br />

c<br />

+q -q<br />

E -

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