- #1
thequirk
- 6
- 0
Here's the problem:
The passage of a thundercloud overhead caused the vertical electric field strength in the atmosphere, measured at the ground, to rise to 0.1 statvolt/cm [E_0].
(a) How much charge didthe thundercloud contain, in esu per cm^2 of horizontal area?
(b) Suppose there was enough water in the thundercloud in the form of 1-millimeter-diameter [convert to cm and divide by two, call this r] drops to make 0.25 cm of rainfall [d], and that it was those drops which carried the charge. How large was the electric field strength at the surface of one of those drops?
Here's what I got:
(a) E_0 = 2πσ, from which we get σ = E_0/(2π)
(b) Here's where I am not sure whether I am doing the right thing or not.
Consider some part of the water at the ground of area A at the top (assuming level water).
Φ = 4πq and Φ = E_0 * A => q = AE_0/(4π)
This is the total charge there is.
On the other hand,
Adρ = AE_0/(4π) <=> ρ = E_0/(4πd)
Then the charge which is carried by one drop is:
Q = (4/3)πρr^3 => Q = (r^3)E_0/(3d)
Since the field at the surface is Q/R^2, we get:
E = R*E_0/(3d)
The passage of a thundercloud overhead caused the vertical electric field strength in the atmosphere, measured at the ground, to rise to 0.1 statvolt/cm [E_0].
(a) How much charge didthe thundercloud contain, in esu per cm^2 of horizontal area?
(b) Suppose there was enough water in the thundercloud in the form of 1-millimeter-diameter [convert to cm and divide by two, call this r] drops to make 0.25 cm of rainfall [d], and that it was those drops which carried the charge. How large was the electric field strength at the surface of one of those drops?
Here's what I got:
(a) E_0 = 2πσ, from which we get σ = E_0/(2π)
(b) Here's where I am not sure whether I am doing the right thing or not.
Consider some part of the water at the ground of area A at the top (assuming level water).
Φ = 4πq and Φ = E_0 * A => q = AE_0/(4π)
This is the total charge there is.
On the other hand,
Adρ = AE_0/(4π) <=> ρ = E_0/(4πd)
Then the charge which is carried by one drop is:
Q = (4/3)πρr^3 => Q = (r^3)E_0/(3d)
Since the field at the surface is Q/R^2, we get:
E = R*E_0/(3d)