Waves and superposition: models, interference and diffraction

Key idea: Use signed displacement and phase consistently across time and space, then apply superposition to standing waves, interference and diffraction without confusing their distinct conditions.

  • H2 Physics 9478 · 2027
  • Internally reviewed by MiniEducation Team
  • Recorded selected-response study loop available

Before you start: Oscillations objective chainQuantities & Measurement objective chain

By the end, you can

  • Model mechanical and electromagnetic progressive waves, interpret time and position graphs, and use wave quantities, phase and energy transfer.
  • Apply intensity–amplitude and inverse-square relationships, and use polarisation and Malus' law for electromagnetic waves.
  • Apply superposition and explain standing-wave experiments, boundary conditions, nodes, antinodes and sound-wavelength measurement.
  • Analyse coherent two-source interference and Young double-slit fringes using phase and path difference.
  • Use diffraction gratings, single-slit first minima and the Rayleigh criterion with their distinct aperture spacings and assumptions.

Starting-point self-check

1. Check your starting point

Attempt all seven groups without notes and mark the first graph axis, phase conversion, boundary condition or aperture spacing you could not justify. Use the recorded topic diagnostic above when you want scoring and a personalised repair plan.

Intensity, amplitude and inverse-square spreading 10(g)–(h)

Question 1

An isotropic point source radiates 12.0 W without loss. Find intensity at 4.00 m and at 8.00 m, then state the intensity change if wave amplitude halves.

Check the model response

I = P/(4πr²). At 4.00 m, I = 12.0/[4π(4.00)²] = 5.97 × 10⁻² W m⁻². Doubling distance gives 1.49 × 10⁻² W m⁻². Since I ∝ A², halving amplitude quarters intensity.

repair

2. Repair the eleven common breaks

Use only the repair matching an error, then redraw the axes, signed displacement, boundary conditions, rays or aperture before retrying.

Intensity, amplitude and inverse-square spreading 10(g)–(h)

Check this idea

Misconception: Halving amplitude halves intensity.

Repair: For a progressive wave, I ∝ A², so halving amplitude reduces intensity to one quarter.

Check this idea

Misconception: Every measured intensity obeys an inverse-square law.

Repair: The model requires point-source spreading without energy loss. Absorption, directional emission or nearby boundaries break the simple relation.

worked example

3. Follow seven worked models

Follow how each solution fixes the graph type, energy-spreading model, transmission axis, boundary condition, path difference or aperture before calculating.

Intensity, amplitude and inverse-square spreading 10(g)–(h)

Model 1

An isotropic source has intensity 0.318 W m⁻² at 5.00 m. Find its power and the amplitude factor at 10.0 m.

Check the model response

P = I4πr² = 0.318(4π)(5.00²) ≈ 100 W. At double distance, intensity is one quarter. Since amplitude is proportional to √I, amplitude is one half.

guided practice

4. Guided practice

Use each hint only to select the graph interval, spreading surface, polarisation reference, mode shape, interference condition or aperture equation.

Intensity, amplitude and inverse-square spreading 10(g)–(h)

Question 1

A point source gives 6.0 × 10⁻³ W m⁻² at 2.0 m. Find intensity at 5.0 m and the amplitude ratio A₅/A₂.

Hint: Use I₂/I₁ = (r₁/r₂)², then amplitude ∝ √I.

Check the model response

I₅ = 6.0 × 10⁻³(2.0/5.0)² = 9.6 × 10⁻⁴ W m⁻². A₅/A₂ = √(I₅/I₂) = 2.0/5.0 = 0.40.

independent practice

5. Independent practice

Solve without repair notes and state the graph, source, boundary, coherence and aperture assumptions used.

Intensity, amplitude and inverse-square spreading 10(g)–(h)

Question 1

Without absorption, intensity falls from 0.80 to 0.20 W m⁻². State the distance and amplitude factors.

Check the model response

The intensity factor is 1/4. From I ∝ 1/r², distance doubles. From I ∝ A², amplitude halves.

Practice exit check

6. Practice assessment

Use this as extra closed-book practice, then complete the separate recorded assessment in your plan.

Intensity, amplitude and inverse-square spreading 10(g)–(h)

Question 1

Define wave intensity. A lossless isotropic source radiates 50 W; find intensity at 10 m and the intensity and amplitude factors at 30 m relative to 10 m.

Check the model response

Intensity is power transferred per unit area. I₁₀ = 50/[4π(10)²] = 3.98 × 10⁻² W m⁻². Tripling distance reduces intensity to 1/9 and amplitude to 1/3.

Re-test practice

7. Delayed re-test practice

Return after at least three days and solve these fresh contexts without reopening earlier responses. The recorded plan enforces the delay and uses a separate re-test family for selected-response skill-group evidence.

Intensity, amplitude and inverse-square spreading 10(g)–(h)

Question 1

A point-source wave has amplitude A and intensity I at radius r. State both quantities at radius 4r, assuming lossless spreading.

Check the model response

I ∝ 1/r², so intensity becomes I/16. Since intensity is proportional to amplitude squared, amplitude becomes A/4.

Continue with established practice

Use the established six-question structured set after the delayed re-test, then use the combined Waves & Superposition quiz and Standing Wave Explorer for mixed graphical and experimental transfer.

Open Waves structured practice