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Electromagnetic Waves — Notes

3 sections 3 min readBeta

1. Displacement current

The puzzle: for a loop round the wire of a charging capacitor, Ampere’s law ∮B⃗⋅dl⃗=μ0I\oint \vec B\cdot d\vec l = \mu_0 I gives μ0I\mu_0 I for a flat surface pierced by the wire but zero for a surface passing through the gap, where no charge flows.

Maxwell’s fix: a changing electric flux acts like a current, the displacement current Id=ε0dΦEdtI_d = \varepsilon_0\dfrac{d\Phi_E}{dt}. In the gap ΦE=q/ε0\Phi_E = q/\varepsilon_0, so Id=dq/dt=II_d = dq/dt = I: the total current is continuous.

Ampere–Maxwell law: ∮B⃗⋅dl⃗=μ0Ic+μ0ε0dΦEdt\oint \vec B\cdot d\vec l = \mu_0 I_c + \mu_0\varepsilon_0\dfrac{d\Phi_E}{dt}. A changing electric field produces a magnetic field (the counterpart of Faraday’s law).

Formulas

  • Displacement current
    Id=ε0dΦEdtI_d = \varepsilon_0\dfrac{d\Phi_E}{dt}
  • Ampere–Maxwell law
    ∮B⃗⋅dl⃗=μ0(Ic+ε0dΦEdt)\oint \vec B\cdot d\vec l = \mu_0\left(I_c + \varepsilon_0\dfrac{d\Phi_E}{dt}\right)

Key terms

Displacement current

The term ε₀ dΦE/dt that acts like a current wherever the electric flux is changing.

2. Electromagnetic waves and their characteristics

  • Source: accelerated (e.g. oscillating) charges. A charge at rest gives only E; steady motion gives E and steady B; acceleration radiates. The wave’s frequency equals the frequency of oscillation of the charge.
  • Self-sustaining: a changing E makes B and a changing B makes E, so the disturbance travels; no medium is needed.
  • Plane wave along x: Ey=E0sin⁡(kx−ωt)E_y = E_0\sin(kx - \omega t), Bz=B0sin⁡(kx−ωt)B_z = B_0\sin(kx - \omega t): E and B are perpendicular to each other and to the direction of travel (transverse), and in phase; E⃗×B⃗\vec E \times \vec B is along the direction of travel.
  • Speed: c=1/μ0ε0≈3.0×108c = 1/\sqrt{\mu_0\varepsilon_0} \approx 3.0 \times 10^8 m s⁻¹ in vacuum, the same for all frequencies; in a medium v=1/με<cv = 1/\sqrt{\mu\varepsilon} < c.
  • E0/B0=cE_0/B_0 = c; c=fλc = f\lambda; k=2π/λk = 2\pi/\lambda, ω=2πf\omega = 2\pi f.
  • EM waves carry energy and momentum (they exert radiation pressure).
E × B points along the direction of travel (checked).
  • E / E₀
  • B / B₀ (same phase)
E₀ = cB₀; the fields reach their peaks at the same places.

Formulas

  • EM wave relations
    c=1μ0ε0,E0=cB0,c=fλc = \dfrac{1}{\sqrt{\mu_0\varepsilon_0}},\qquad E_0 = cB_0,\qquad c = f\lambda

Key terms

Transverse wave

A wave whose oscillations are perpendicular to its direction of travel.

3. The electromagnetic spectrum

In order of decreasing wavelength (increasing frequency and photon energy); the edges are approximate:

BandWavelengthProduced byUses
Radio> 0.1 moscillating currents in aerialsAM/FM radio, TV, mobile phones
Microwave0.1 m – 1 mmmagnetron, klystronradar, ovens (2.45 GHz), satellite links, Wi-Fi
Infrared1 mm – 700 nmhot bodies, molecular vibrationsremote controls, night vision, physiotherapy; greenhouse effect
Visible700 – 400 nmelectron transitions in atomsvision, photography
Ultraviolet400 nm – 1 nmSun, arc lampssterilisation, LASIK; absorbed by the ozone layer
X-rays1 nm – about 1 pmfast electrons hitting a metal targetmedical imaging, crystal structure
Gamma raysbelow about 1 pmradioactive nucleicancer therapy, sterilising equipment
Band edges are approximate; the bands overlap slightly in practice.

Key terms

Electromagnetic spectrum

The full range of EM waves arranged by wavelength or frequency.

Ozone layer

Upper-atmosphere layer that absorbs most of the Sun’s ultraviolet.

Exam tips

  • Displacement current: describe the two surfaces with one boundary, then Id=ε0 dΦE/dtI_d = \varepsilon_0\,d\Phi_E/dt.
  • Transverse nature: E ⟂ B ⟂ direction of travel; E and B in phase; E × B gives the direction.
  • c=1/μ0ε0c = 1/\sqrt{\mu_0\varepsilon_0}, E0=cB0E_0 = cB_0, c=fλc = f\lambda.
  • Spectrum: order, one source and two uses for each band; convert f to λ before naming a band.