Using the vector identity ∇⋅(E×B)=B⋅(∇×E)−E⋅(∇×B):
∇⋅(E×B)=−μ0J⋅E−μ0ε0∂t∂(2E2)−∂t∂(2B2)
Dividing by μ0 and rearranging:
−∇⋅S=J⋅E+∂t∂u
Where S=μ01E×B is the Poynting vector and u=21(ε0E2+μ0B2) is the energy density.
Interpretation: The rate of energy leaving a volume equals the work done on charges plus The rate of increase of field energy. In integral form:
−∮SS⋅dA=dtd∫VudV+∫VJ⋅EdV
5.5 EM Wave Propagation: Worked Examples
Intensity. For a plane wave, the time-averaged Poynting vector is:
⟨S⟩=2μ0cE02k^=21ε0cE02k^
Example: Radiation pressure
A plane wave normally incident on a perfectly absorbing surface exerts a radiation pressure. The momentum flux of the wave is ⟨S⟩/c per unit area, so:
Pabs=c⟨S⟩=2ε0E02
For a perfectly reflecting surface, the momentum transfer is doubled:
Pref=c2⟨S⟩=ε0E02
A 1 kW/m2 beam (like sunlight near Earth) exerts a pressure of about 3.3μPa on a Perfect absorber. ■
Example: Polarization of EM waves
Linear polarization.E=E0cos(kz−ωt)x^. The field Oscillates in a fixed direction.
Circular polarization. Two orthogonal linear polarizations with a phase difference of π/2:
E=E0cos(kz−ωt)x^±E0sin(kz−ωt)y^
The tip of E traces a circle. The + sign gives left-circular polarization (LCP) and the − sign gives right-circular polarization (RCP).
Elliptical polarization. The general case with arbitrary amplitudes and phase:
E=E0xcos(kz−ωt)x^+E0ycos(kz−ωt+δ)y^
■
5.6 EM Waves in Conductors
In a conductor with conductivity σOhm’s law gives J=σE. Substituting into the Ampere-Maxwell law:
∇×B=μ0σE+μ0ε0∂t∂E
For a monochromatic wave E=E0e−iωtThis leads to a complex Wave number:
k~2=μ0ε0ω2+iμ0σω
Writing k~=k+iκ where k is the real part (wave number) and κ is the Imaginary part (attenuation constant):
E(z,t)=E0e−κzcos(kz−ωt)
The field decays exponentially. The skin depth is the distance over which the amplitude Falls by a factor of 1/e:
δ=κ1
For a good conductor (σ≫ε0ω):
δ=μ0σω2
Example: Skin depth in copper at 60 Hz and 1 MHz
Copper: σ=5.96×107 S/m, μr≈1.
At f=60 Hz (ω=2π×60 rad/s):
δ=4π×10−7×5.96×107×2π×602≈8.5mm
At f=1 MHz (ω=2π×106 rad/s):
δ=4π×10−7×5.96×107×2π×1062≈65μm
The skin depth decreases as 1/fSo higher-frequency signals are confined to thinner Surface layers. ■
5.7 Waveguides
Electromagnetic waves can be guided by hollow conducting pipes (waveguides). Consider a Rectangular waveguide with dimensions a (width) and b (height).
TE modes (transverse electric, Ez=0, Bz=0). The lowest-order mode is \mathrm{TE_}{10}With fields:
Ey=E0sin(aπx)cos(kgz−ωt)
Bx=−ωkgE0sin(aπx)cos(kgz−ωt)
Bz=ωaπE0cos(aπx)sin(kgz−ωt)
Where the guide wave number is kg=(ω/c)2−(π/a)2.
Cutoff frequency. Waves propagate only when ω>ωc where:
ωc,mn=cπ(am)2+(bn)2
For the \mathrm{TE_}{10} mode: fc=2ac.
Phase and group velocities. In a waveguide, the phase velocity exceeds c:
vp=kgω=1−(ωc/ω)2c>c
The group velocity (signal velocity) is less than c:
vg=dkgdω=c1−(ωc/ω)2<c
They satisfy vpvg=c2.
:::caution Common Pitfall The phase velocity in a waveguide exceeds cBut this does not violate special relativity. No information or energy travels faster than c; the signal velocity is the group velocity vg<c. The phase velocity is the speed of the wave crests, which is a purely Kinematic quantity.
5.8 Electric Dipole Radiation
An oscillating electric dipole is the simplest source of electromagnetic radiation.
Consider a dipole p(t)=p0cos(ωt)z^. In the radiation zone (r≫λ), the fields are:
E=−4πμ0p0ω2rsinθcos[ω(t−r/c)]θ^
B=−4πcμ0p0ω2rsinθcos[ω(t−r/c)]ϕ^
The fields fall off as 1/r (not 1/r2 as for static fields), which is characteristic of Radiation.
Radiation pattern. The intensity varies as sin2θWith maximum radiation in the Equatorial plane (θ=π/2) and zero along the dipole axis (θ=0,π).
Total radiated power. Integrating the Poynting vector over a sphere:
P=12πcμ0p02ω4
Larmor formula. For a point charge q undergoing acceleration a:
P=6πε0c3q2a2
This is the non-relativistic limit and is valid whenever v≪c.
Derivation: Power radiated by an oscillating dipole
The time-averaged Poynting vector magnitude in the radiation zone: