(a) Prove that the average magnetic field, over a sphere of radius R, due to steady currents inside the sphere, is
Bave=4πμ0R32m , (5.93)
where m is the total dipole moment of the sphere. Contrast the electrostatic result, Eq. 3.105. [This is tough, so I’ll give you a start:
Bave=34πR31∫Bdτ .
Eave=−4πϵ01R3p(3.105)
Write B as (∇ × A), and apply Prob. 1.61(b). Now put in Eq. 5.65, and do the surface integral first, showing that
∫ᴫ1da=34πr′ .
A(r)=4πμ0∫ᴫJ(r′)dτ′(5.65)
(see Fig. 5.65). Use Eq. 5.90, if you like.]
m=21∫(r×J)dτ(5.90)
(b) Show that the average magnetic field due to steady currents outside the sphere is the same as the field they produce at the center.
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Note that J depends on the source point r′, not on the field point r. To do the surface integral, choose the (x, y, z) coordinates so that r′lies on the z axis (see diagram).
Thenᴫ=R2+(z′)2−2Rz′cosθ , whileda=R2sinθdθdϕr^ .
By symmetry, the x and y components must integrate to zero; since the z component of r^is cosθ, we have