Problem Irodov 3.350
A parallel-plate capacitor has round disc plates a distance apart, and the gap is filled with a uniform, weakly conducting medium of conductivity and permittivity . An alternating voltage is applied across it. Ignoring edge effects, find the magnetic field strength between the plates at a distance from their common axis.
The disc capacitor edge on: the medium of permittivity and conductivity fills the gap , and the leads carry the voltage across the plates.
- Given
- gap
- distance from the axis
- edge effects neglected
- Find
- between the plates
Solution
Step 1The field and the two current densities
With the edge effects neglected the field between the plates is uniform and normal to them, . The medium carries a conduction current by Ohm’s law, and the changing field adds a displacement current; both are normal to the plates. Each is measured along the direction the field has when :
Differentiating in time:
Step 2The circulation of H round a coaxial circle
The capacitor at an instant chosen with the left plate positive and charging (plate charges not drawn): the conduction current and the displacement current both run across the gap, and circulates round the coaxial circle of radius .
Take a circle of radius about the axis, in a plane between the plates, spanned by the flat disc it bounds. Both current densities are uniform over that disc, so the circulation theorem gives
Here is the component along the circle taken counterclockwise about the field direction at (right-hand rule).
Step 3One oscillation with a phase lead
Two oscillations a quarter period apart add into one. Writing and , the bracket in (3) is a cosine of a sum:
The field grows linearly with and leads the voltage by the phase .
Check
Limits. A perfect insulator () gives and , the field of a pure displacement current in an ordinary capacitor. Direct current () gives and , the field inside a uniform conductor carrying the current density , growing as just like the field inside a straight wire. Units: is .
Remark
The ratio compares the displacement current with the conduction current, and it is times the medium’s charge relaxation time . A medium counts as a conductor at frequencies well below and as a dielectric well above it; for sea water ( S/m, ) the crossover lies near s.
