Introductory Physics Volume Two
Introductory Physics Volume Two
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 -