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🎯⭐ INTERACTIVE LESSON

Electromagnetic Waves

Learn step-by-step with interactive practice!

Electromagnetic Waves - Complete Interactive Lesson

Part 1: Maxwell's Equations Overview

🌐 Maxwell's Equations

Part 1 of 7 — The Four Laws of Electromagnetism


The Four Equations

#NameIntegral Form
1Gauss's Law (E)∮E⃗⋅dA⃗=Qencε0\oint \vec{E} \cdot d\vec{A} = \frac{Q_{enc}}{\varepsilon_0}
2Gauss's Law (B)∮B⃗⋅dA⃗=0\oint \vec{B} \cdot d\vec{A} = 0
3Faraday's Law∮E⃗⋅dl⃗=−dΦBdt\oint \vec{E} \cdot d\vec{l} = -\frac{d\Phi_B}{dt}
4Ampere-Maxwell∮B⃗⋅dl⃗=μ0(I+ε0dΦEdt)\oint \vec{B} \cdot d\vec{l} = \mu_0\left(I + \varepsilon_0 \frac{d\Phi_E}{dt}\right)

Physical Meaning

EquationSays...
Gauss (E)Electric charges create electric fields
Gauss (B)No magnetic monopoles
FaradayChanging B creates E
Ampere-MaxwellCurrents AND changing E create B

🔑 Maxwell's equations unify electricity and magnetism and predict electromagnetic waves.

📝 Worked Example — Gauss's Law with Calculus

A point charge Q=+4.0 nCQ = +4.0 \text{ nC} sits at the center of a sphere of radius r=0.20 mr = 0.20 \text{ m}. Find the electric flux through the sphere, then the field magnitude on its surface.

Step 1 — Apply Gauss's Law. The closed-surface integral gives the enclosed charge over ε0\varepsilon_0:

ΦE=∮E⃗⋅dA⃗=Qencε0=4.0×10−98.85×10−12≈452 N⋅m2/C\Phi_E = \oint \vec{E} \cdot d\vec{A} = \frac{Q_{enc}}{\varepsilon_0} = \frac{4.0 \times 10^{-9}}{8.85 \times 10^{-12}} \approx 452 \text{ N}\cdot\text{m}^2/\text{C}

Step 2 — Exploit spherical symmetry. By symmetry E⃗\vec{E} is radial and constant in magnitude over the surface, so ∮E⃗⋅dA⃗=E∮dA=E(4πr2)\oint \vec{E} \cdot d\vec{A} = E \oint dA = E(4\pi r^2).

Step 3 — Solve for the field. Setting E(4πr2)=Qε0E(4\pi r^2) = \frac{Q}{\varepsilon_0} gives the familiar point-charge result:

E=14πε0Qr2=(8.99×109)(4.0×10−9)(0.20)2≈899 N/CE = \frac{1}{4\pi\varepsilon_0}\frac{Q}{r^2} = \frac{(8.99 \times 10^9)(4.0 \times 10^{-9})}{(0.20)^2} \approx 899 \text{ N/C}

🔑 Gauss's Law is most powerful when symmetry lets you pull EE outside the surface integral.

Concept Check 🎯

Part 2: Displacement Current

🔄 Displacement Current

Part 2 of 7 — Maxwell's Key Insight


The Problem with Ampere's Law

Consider a charging capacitor — current flows in the wire but not between the plates. Ampere's law gives different answers depending on which surface you choose!


Maxwell's Fix: Displacement Current

Id=ε0dΦEdtI_d = \varepsilon_0 \frac{d\Phi_E}{dt}

This changing electric flux acts like a current for purposes of producing a magnetic field.

∮B⃗⋅dl⃗=μ0(I+Id)\oint \vec{B} \cdot d\vec{l} = \mu_0(I + I_d)

🔑 Between capacitor plates, there is no real current — but the changing E⃗\vec{E} creates a magnetic field just as if there were current.

📝 Worked Example — Displacement Current in a Capacitor

A parallel-plate capacitor with circular plates of radius R=5.0 cmR = 5.0 \text{ cm} is charged so the electric field between the plates increases at dEdt=2.0×1012 V/m per s\frac{dE}{dt} = 2.0 \times 10^{12} \text{ V/m per s}. Find the displacement current.

Step 1 — Write the electric flux. For a uniform field perpendicular to plates of area A=πR2A = \pi R^2:

ΦE=EA=E πR2\Phi_E = E A = E\,\pi R^2

Step 2 — Differentiate with respect to time. Since AA is constant, the derivative passes through:

dΦEdt=πR2dEdt\frac{d\Phi_E}{dt} = \pi R^2 \frac{dE}{dt}

Step 3 — Multiply by ε0\varepsilon_0. The displacement current is

Id=ε0dΦEdt=ε0πR2dEdtI_d = \varepsilon_0 \frac{d\Phi_E}{dt} = \varepsilon_0 \pi R^2 \frac{dE}{dt}

Id=(8.85×10−12) π(0.050)2(2.0×1012)≈0.14 AI_d = (8.85 \times 10^{-12})\,\pi (0.050)^2 (2.0 \times 10^{12}) \approx 0.14 \text{ A}

🔑 The displacement current between the plates exactly equals the conduction current in the wire — that is what makes Ampere-Maxwell consistent for any surface.

Concept Check 🎯

Part 3: Electromagnetic Waves

🌊 Electromagnetic Waves

Part 3 of 7 — Light as an EM Wave


EM Wave Properties

c=1μ0ε0=3.0×108 m/sc = \frac{1}{\sqrt{\mu_0 \varepsilon_0}} = 3.0 \times 10^8 \text{ m/s}

PropertyValue
Speedc=3×108c = 3 \times 10^8 m/s (in vacuum)
E⃗⊥B⃗\vec{E} \perp \vec{B}E and B are perpendicular
E⃗⊥v⃗\vec{E} \perp \vec{v}Transverse wave
E/B=cE/B = cRatio of field amplitudes

Energy in EM Waves

Energy density: u=ε0E2=B2μ0u = \varepsilon_0 E^2 = \frac{B^2}{\mu_0}

Intensity: I=12cε0E02I = \frac{1}{2}c\varepsilon_0 E_0^2

Poynting vector: S⃗=1μ0E⃗×B⃗\vec{S} = \frac{1}{\mu_0}\vec{E} \times \vec{B}

🔑 Light is an electromagnetic wave — predicted by Maxwell's equations before being experimentally confirmed by Hertz.

📝 Worked Example — Speed from μ0\mu_0 and ε0\varepsilon_0

Maxwell's equations predict that a plane wave E(x,t)=E0sin⁡(kx−ωt)E(x,t) = E_0 \sin(kx - \omega t) must satisfy the wave equation ∂2E∂x2=μ0ε0∂2E∂t2\frac{\partial^2 E}{\partial x^2} = \mu_0\varepsilon_0 \frac{\partial^2 E}{\partial t^2}. Show the propagation speed and evaluate it.

Step 1 — Take the spatial derivatives. Differentiating twice in xx pulls down k2k^2:

∂2E∂x2=−k2E0sin⁡(kx−ωt)\frac{\partial^2 E}{\partial x^2} = -k^2 E_0 \sin(kx - \omega t)

Step 2 — Take the time derivatives. Differentiating twice in tt pulls down ω2\omega^2:

∂2E∂t2=−ω2E0sin⁡(kx−ωt)\frac{\partial^2 E}{\partial t^2} = -\omega^2 E_0 \sin(kx - \omega t)

Step 3 — Match coefficients. Substituting into the wave equation gives k2=μ0ε0 ω2k^2 = \mu_0\varepsilon_0\,\omega^2, so the speed is

v=ωk=1μ0ε0=1(4π×10−7)(8.85×10−12)≈3.0×108 m/sv = \frac{\omega}{k} = \frac{1}{\sqrt{\mu_0\varepsilon_0}} = \frac{1}{\sqrt{(4\pi \times 10^{-7})(8.85 \times 10^{-12})}} \approx 3.0 \times 10^8 \text{ m/s}

🔑 The wave speed contains only the universal constants μ0\mu_0 and ε0\varepsilon_0 — so every EM wave in vacuum travels at cc, independent of frequency.

Concept Check 🎯

Part 4: EM Spectrum

🌈 The Electromagnetic Spectrum

Part 4 of 7 — Types of EM Radiation


The Spectrum

TypeWavelengthFrequency
Radio> 1 m< 300 MHz
Microwave1 mm – 1 m300 MHz – 300 GHz
Infrared700 nm – 1 mm
Visible400 – 700 nm
Ultraviolet10 – 400 nm
X-ray0.01 – 10 nm
Gamma< 0.01 nm> 101910^{19} Hz

All travel at c=fλc = f\lambda in vacuum.

🔑 All electromagnetic waves are the same phenomenon — oscillating E⃗\vec{E} and B⃗\vec{B} fields. They differ only in frequency.

📝 Worked Example — Wavelength, Frequency, and Photon Energy

A green laser emits light of wavelength λ=532 nm\lambda = 532 \text{ nm}. Find its frequency and the energy of one photon.

Step 1 — Use c=fλc = f\lambda. Solve for frequency:

f=cλ=3.0×108532×10−9≈5.6×1014 Hzf = \frac{c}{\lambda} = \frac{3.0 \times 10^8}{532 \times 10^{-9}} \approx 5.6 \times 10^{14} \text{ Hz}

Step 2 — Apply the Planck relation. Photon energy is E=hfE = hf with h=6.63×10−34 J⋅sh = 6.63 \times 10^{-34} \text{ J}\cdot\text{s}:

E=hf=(6.63×10−34)(5.6×1014)≈3.7×10−19 JE = hf = (6.63 \times 10^{-34})(5.6 \times 10^{14}) \approx 3.7 \times 10^{-19} \text{ J}

Step 3 — Convert to electron-volts. Dividing by 1.6×10−19 J/eV1.6 \times 10^{-19} \text{ J/eV}:

E≈3.7×10−191.6×10−19≈2.3 eVE \approx \frac{3.7 \times 10^{-19}}{1.6 \times 10^{-19}} \approx 2.3 \text{ eV}

🔑 Shorter wavelength means higher frequency and higher photon energy — that is why gamma rays are far more energetic than radio waves.

Concept Check 🎯

Part 5: Energy & Momentum of EM Waves

💡 Energy and Momentum of EM Waves

Part 5 of 7 — Poynting Vector and Radiation Pressure


Poynting Vector

S⃗=1μ0E⃗×B⃗\vec{S} = \frac{1}{\mu_0}\vec{E} \times \vec{B}

∣S⃗∣|\vec{S}| = power per unit area (W/m2)(W/m^{2})

Average intensity: I=12cε0E02=E0B02μ0I = \frac{1}{2}c\varepsilon_0 E_0^2 = \frac{E_0 B_0}{2\mu_0}


Radiation Pressure

SurfacePressure
Perfect absorberP=IcP = \frac{I}{c}
Perfect reflectorP=2IcP = \frac{2I}{c}

EM waves carry momentum: p=Ucp = \frac{U}{c} (for absorbed radiation)

🔑 Light exerts pressure — this is the basis of solar sails and laser propulsion.

📝 Worked Example — Intensity and Radiation Force on a Solar Sail

Sunlight near Earth has intensity I=1.36×103 W/m2I = 1.36 \times 10^3 \text{ W/m}^2. A reflective solar sail of area A=100 m2A = 100 \text{ m}^2 faces the Sun. Find the force on it and the peak electric field of the sunlight.

Step 1 — Radiation pressure on a reflector. A perfect reflector reverses the photon momentum, so

P=2Ic=2(1.36×103)3.0×108≈9.1×10−6 PaP = \frac{2I}{c} = \frac{2(1.36 \times 10^3)}{3.0 \times 10^8} \approx 9.1 \times 10^{-6} \text{ Pa}

Step 2 — Force from pressure. Multiply by the sail area:

F=PA=(9.1×10−6)(100)≈9.1×10−4 NF = P A = (9.1 \times 10^{-6})(100) \approx 9.1 \times 10^{-4} \text{ N}

Step 3 — Peak field from intensity. Invert I=12cε0E02I = \frac{1}{2}c\varepsilon_0 E_0^2:

E0=2Icε0=2(1.36×103)(3.0×108)(8.85×10−12)≈1.0×103 N/CE_0 = \sqrt{\frac{2I}{c\varepsilon_0}} = \sqrt{\frac{2(1.36 \times 10^3)}{(3.0 \times 10^8)(8.85 \times 10^{-12})}} \approx 1.0 \times 10^3 \text{ N/C}

🔑 Radiation force is tiny but continuous; over months it can meaningfully accelerate a low-mass spacecraft.

Concept Check 🎯

Part 6: Problem-Solving Workshop

🛠️ Maxwell Workshop

Part 6 of 7 — Practice


AP Physics C E&M: Maxwell Topics

ConceptWhat to Know
Identify which equation appliesMatch to symmetry and context
Displacement currentId=ε0dΦEdtI_d = \varepsilon_0 \frac{d\Phi_E}{dt}
EM wave speedc=1μ0ε0c = \frac{1}{\sqrt{\mu_0\varepsilon_0}}
E/B ratioE=cBE = cB
Poynting vectorDirection of energy flow
Radiation pressureP=IcP = \frac{I}{c} (absorber), 2Ic\frac{2I}{c} (reflector)

📝 Worked Example — Faraday's Law for an Induced Field

A uniform magnetic field fills a circular region of radius R=0.10 mR = 0.10 \text{ m} and increases at dBdt=0.50 T/s\frac{dB}{dt} = 0.50 \text{ T/s}. Find the induced electric field magnitude at radius r=0.10 mr = 0.10 \text{ m} (the edge).

Step 1 — Write Faraday's Law. Around a circular loop of radius rr, symmetry makes E⃗\vec{E} tangential and constant, so

∮E⃗⋅dl⃗=E(2πr)=−dΦBdt\oint \vec{E} \cdot d\vec{l} = E(2\pi r) = -\frac{d\Phi_B}{dt}

Step 2 — Express the flux. For r≤Rr \le R the loop encloses the full field over area πr2\pi r^2:

ΦB=B πr2⇒dΦBdt=πr2dBdt\Phi_B = B\,\pi r^2 \quad\Rightarrow\quad \frac{d\Phi_B}{dt} = \pi r^2 \frac{dB}{dt}

Step 3 — Solve for EE. Taking magnitudes,

E=r2dBdt=0.102(0.50)=0.025 N/CE = \frac{r}{2}\frac{dB}{dt} = \frac{0.10}{2}(0.50) = 0.025 \text{ N/C}

🔑 Inside the field region E∝rE \propto r; outside it (r>Rr > R) the enclosed flux is fixed at BπR2B\pi R^2, so E∝1/rE \propto 1/r.

Concept Check 🎯

Part 7: Review & Applications

📋 Maxwell's Equations Review

Part 7 of 7 — Final Summary


The Big Picture

Maxwell's four equations describe ALL of classical electromagnetism:

  1. Gauss (E): Charges → E fields
  2. Gauss (B): No magnetic monopoles
  3. Faraday: Changing B → E
  4. Ampere-Maxwell: Currents + changing E → B

Together they predict EM waves traveling at c=1μ0ε0c = \frac{1}{\sqrt{\mu_0\varepsilon_0}}.

🔑 "Maxwell's equations are the most beautiful equations in physics." — Richard Feynman

📝 Worked Example — Synthesis: From Fields to Power

A laser beam in vacuum has peak electric field E0=2.0×103 N/CE_0 = 2.0 \times 10^3 \text{ N/C} and a circular cross-section of radius r=1.0 mmr = 1.0 \text{ mm}. Find its average intensity and total power.

Step 1 — Average intensity from E0E_0. Using the Poynting time-average,

I=12cε0E02=12(3.0×108)(8.85×10−12)(2.0×103)2≈5.3×103 W/m2I = \frac{1}{2}c\varepsilon_0 E_0^2 = \frac{1}{2}(3.0 \times 10^8)(8.85 \times 10^{-12})(2.0 \times 10^3)^2 \approx 5.3 \times 10^3 \text{ W/m}^2

Step 2 — Beam cross-sectional area. A circle of radius rr:

A=πr2=π(1.0×10−3)2≈3.14×10−6 m2A = \pi r^2 = \pi (1.0 \times 10^{-3})^2 \approx 3.14 \times 10^{-6} \text{ m}^2

Step 3 — Power = intensity × area.

P=IA=(5.3×103)(3.14×10−6)≈1.7×10−2 W\mathcal{P} = I A = (5.3 \times 10^3)(3.14 \times 10^{-6}) \approx 1.7 \times 10^{-2} \text{ W}

🔑 This single chain — E0→I→PE_0 \to I \to \mathcal{P} — ties together the field, energy-density, and Poynting-vector ideas from the whole unit.

Concept Check 🎯