C.2 SL/HL Concept 2 of 4

Transverse and Longitudinal Waves

Part of C.2 Wave Model · Unit C — IB Physics 2023

2 Lesson 2 of 4 · C.2 Wave Model
Transverse and Longitudinal Waves
Waves fall into two families based on how particles move relative to the direction of energy transfer. This lesson builds the transverse/longitudinal distinction, the shift method for reading particle velocity off a snapshot, where compressions and rarefactions actually sit on a displacement–distance graph, and how mechanical waves differ from electromagnetic ones.

🪢 Hook – flick a rope, watch what actually moves

Pin one end of a rope down and flick the other end up and down once. A hump races away from your hand down the rope's length. But does any piece of rope travel with it? Mark a piece of tape on the rope and watch it — it only moves up and down, then comes back to rest. The hump travels; the rope itself does not.

Transverse wave on a rope showing crests, troughs, and particles moving perpendicular to the direction of travel
Fig 1 — A transverse wave on a rope: particles move up and down while the disturbance travels along the rope.
💡 Diagnostic question (think – then read on) — as the hump in the rope travels to the right, does the taped point on the rope also drift to the right over time? No — averaged over a full cycle, the taped point returns to exactly where it started. It only oscillates vertically; only the wave pattern (and the energy it carries) travels horizontally.

↕️ Transverse waves

A wave is transverse if the displacement of the particles of the medium is at right angles (perpendicular) to the direction of energy transfer.

On a rope, each segment oscillates up and down while the wave pattern propagates horizontally. The highest points are crests; the lowest are troughs. Each particle performs simple harmonic motion with the same frequency as the wave, slightly out of phase with its neighbour.

Examples: waves on strings and ropes, water surface waves, all electromagnetic waves, seismic S-waves.

⚠️ Exam tip — velocity at crests vs equilibrium. At a crest or trough, a particle is momentarily at rest but has maximum acceleration (directed toward equilibrium). At the equilibrium position, it has maximum speed but zero acceleration — straight out of the SHM you met in C.1.

↔️ Longitudinal waves

A wave is longitudinal if the displacement of the particles is parallel to the direction of energy transfer. Longitudinal waves consist of alternating compressions and rarefactions.

Push and pull one end of a slinky spring along its length: coils crowd together (compression), then spread apart (rarefaction), and these regions travel along the spring.

Longitudinal wave on a slinky spring showing compressions where coils bunch together and rarefactions where coils spread apart
Fig 2 — A longitudinal wave on a slinky: compressions (coils bunched) and rarefactions (coils spread apart).
CompressionA region where particles are closer together than at equilibrium — higher density and pressure.
RarefactionA region where particles are further apart than at equilibrium — lower density and pressure.

We can still draw a displacement–distance graph for a longitudinal wave — the displacement axis just represents motion along the direction of travel, not sideways: positive means displaced in the direction of travel, negative means displaced against it.

Displacement-distance graph for a longitudinal wave with compressions and rarefactions marked at the zero-crossing points
Fig 3 — A longitudinal wave as a displacement–distance graph. Compressions and rarefactions sit at the zero-crossings, not the peaks.

🔊 Sound waves

Sound is a longitudinal mechanical wave, produced when a vibrating surface — a loudspeaker cone, vocal cords, a tuning fork — creates alternating compressions and rarefactions in the surrounding air.

Sound wave spreading from a loudspeaker cone, shown as bands of compressed and rarefied air
Fig 4 — A loudspeaker creates compressions and rarefactions of air pressure — a longitudinal sound wave.
  • Medium required: sound cannot travel through a vacuum.
  • Typical speed in air: ~340 m s⁻¹ at room temperature, rising slightly with temperature.
  • Speed in different media: generally fastest in solids, slowest in gases — particles are closer together and inter-particle forces stronger in solids.
  • Audible range: roughly 20 Hz – 20 kHz.
  • Pitch is set by frequency (higher \(f\) → higher pitch); loudness is set by amplitude (greater \(A\) → louder).

To give a sense of scale: at the threshold of hearing (1000 Hz), the pressure variation at the eardrum exceeds atmospheric pressure by just 20 μPa (atmospheric pressure is ~10⁵ Pa) — a molecular displacement of about \(10^{-11}\) m, roughly a tenth of a hydrogen atom's diameter.

📡 Mechanical vs electromagnetic waves

PropertyMechanical wavesElectromagnetic waves
Requires medium?Yes — solid, liquid, or gasNo — can travel through vacuum
What oscillates?Particles of the mediumElectric and magnetic fields
TypeTransverse or longitudinalAlways transverse
Speed in vacuumCannot exist in vacuum\(c = 3.00\times10^{8}\ \text{m s}^{-1}\)
Speed depends on…Medium properties (density, stiffness)Same for all EM waves in vacuum; varies slightly in materials
ExamplesSound, water waves, seismic wavesLight, radio, X-rays, microwaves, gamma rays

📈 Graph mastery – reading wave-snapshot and displacement graphs

Graph typeAxes (X, Y)ShapeWhat to read
Transverse snapshot (shift method)distance / displacementSinusoidal curve, shifted slightly along travel directionEach particle moves vertically toward its position on the shifted curve
Longitudinal displacement–distancedistance / displacementSinusoidal curveCompressions/rarefactions sit at zero-crossings, not peaks

This is a key exam skill for transverse waves: given the wave direction and a snapshot, you can find which way any particle moves next. (1) Draw the wave profile (solid) at the current instant. (2) Draw a copy shifted slightly in the direction of travel (dashed). (3) Each particle moves vertically from its position on the solid curve toward its position on the dashed curve.

Wave snapshot with a solid profile and a slightly shifted dashed profile showing the direction the wave is travelling
Fig 5 — Shift the wave slightly in its travel direction to see where each particle moves next.
Particles marked on a transverse wave with arrows showing the vertical direction each will move next
Fig 6 — Each particle moves vertically toward the shifted (dashed) profile.

✍️ Worked example – locating a compression on a graph

A longitudinal wave travels to the right. A displacement–distance graph shows that at point P (\(x = 20\ \text{cm}\)), the displacement is zero and the curve is transitioning from positive to negative. Is P a compression or a rarefaction?

1
Identify: at a zero-crossing, look at which way the neighbouring particles have moved — toward P (crowding, compression) or away from P (spreading, rarefaction).
2
Data: P is at \(x=20\ \text{cm}\), displacement \(=0\), gradient negative (positive → negative), wave moving right.
3
Reasoning: a negative gradient at zero means the particle just to the left of P has positive displacement (moved right, toward P) and the particle just to the right has negative displacement (moved left, toward P).
4
Answer: particles on both sides of P have moved toward P — higher density there — so P is a compression.
Displacement-distance graph for a longitudinal wave with point P marked at a zero-crossing with negative gradient, identified as a compression
Fig 7 — Point P sits at a zero-crossing with negative gradient — a compression.

🌍 Real-world: seismic waves reveal Earth's structure

Transverse mechanical waves need a restoring force perpendicular to their direction of travel, which requires the medium to sustain shear stress. Gases and liquids have no fixed molecular structure and cannot resist shear — their molecules simply slide past each other — so only longitudinal (compression) waves can propagate through them.

Cross-section of the Earth showing transverse S-waves blocked by the liquid outer core while longitudinal P-waves pass through it
Fig 8 — S-waves (transverse) are blocked by the liquid outer core; P-waves (longitudinal) pass straight through.
✓ Examiner tip: this is why seismic S-waves cannot pass through Earth's liquid outer core while P-waves can — direct evidence that the outer core is liquid.

🚀 HL extension – are water waves really transverse?

We call water surface waves "transverse," but this is a simplification. In deep water, individual water particles actually move in circles (ellipses in shallow water), combining vertical and horizontal motion. The surface appears to move up and down, but the underlying particle motion is more complex — a good example of how a model simplifies reality.

Challenge: if transverse waves need shear stress, why can water — a liquid — support surface waves at all? Answer: it isn't shear stress doing the restoring here — gravity (and surface tension, for very short wavelengths) pulls the raised surface back down, which is why this is a surface effect and not a true bulk-shear transverse wave through the liquid.

⚠️ Trap corner – common mistakes

MisconceptionCorrect view
Compressions and rarefactions sit at the peaks and troughs of the displacement graphThey sit at the zero-crossings — a compression at zero displacement with negative gradient (for a rightward wave), a rarefaction with positive gradient. At the peaks, displacement is maximum but density is approximately normal
Sound is an electromagnetic wave, since it "travels through the air like light does"Sound is a mechanical longitudinal wave and needs a medium; light is electromagnetic and needs none
All electromagnetic waves can be transverse or longitudinal, like mechanical wavesElectromagnetic waves are always transverse — the oscillating electric and magnetic fields are perpendicular to the direction of travel
A louder sound has a higher frequencyLoudness is set by amplitude; frequency sets pitch — the two are independent
⚠️ Most common slip: marking compressions/rarefactions at the peaks of a longitudinal wave's displacement graph instead of the zero-crossings. Always check the gradient at zero, not the height of the curve.
transverse: displacement ⊥ travel longitudinal: displacement ∥ travel crest/trough: v = 0, a = max compression: zero disp., negative gradient (rightward wave) sound: longitudinal, needs medium, ~340 m s⁻¹ in air EM waves: always transverse, c = 3.00×10⁸ m s⁻¹ transverse waves need shear stress → gases/liquids can't carry them
Practice check — multiple choice
1. In a certain wave, particles oscillate parallel to the direction the wave travels. This wave is:
A transverse
B longitudinal
C electromagnetic
D a standing wave
2. On a displacement–distance graph for a longitudinal wave moving to the right, a compression is found where:
A displacement is at its maximum positive value
B displacement is at its maximum negative value
C displacement is zero and the gradient is negative
D displacement is zero and the gradient is positive
3. Which of the following can travel through a vacuum?
A sound waves
B seismic S-waves
C water surface waves
D light (an electromagnetic wave)
4. Which pairing correctly matches a sound wave's properties to what determines them?
A loudness = frequency, pitch = amplitude
B loudness = amplitude, pitch = frequency
C both are determined by amplitude
D both are determined by frequency
Practice check — fill in the blanks

Complete the statements:

A wave is if particle displacement is at right angles to the direction of energy transfer, and if it is parallel. On a displacement–distance graph for a longitudinal wave moving right, a occurs at a zero-crossing with negative gradient. Electromagnetic waves are always .
Exam‑style questions
Exam question · State
Q1. State the key difference between a transverse wave and a longitudinal wave, in terms of particle displacement relative to the direction of energy transfer. [2 marks]
✓ Transverse: particle displacement is perpendicular (at right angles) to the direction of energy transfer.
✓ Longitudinal: particle displacement is parallel to the direction of energy transfer.
Exam question · Apply
Q2. A transverse wave propagates to the right along a string. Three marked points on the string are shown. Indicate the direction each will move in the next instant. [3 marks]
Transverse wave on a string with three marked points labelled to determine their next direction of motion
✓ Shift the wave slightly to the right and move each point vertically toward the shifted profile.
✓ A point just behind a crest moves up; a point just ahead of a crest moves down.
✓ A point at a crest is momentarily stationary.
Exam question · Graph
Q3. A displacement–distance graph for a longitudinal wave travelling to the right is given. Positive displacement means motion to the right. (a) State the wavelength. (b) Mark on the graph one position where a compression occurs and one where a rarefaction occurs. (c) At \(x = 1.0\ \text{m}\) and \(x = 3.0\ \text{m}\), draw arrows showing the direction of particle velocity. [4 marks]
✓ (a) The wavelength is the distance between repeating features, read directly off the graph.
✓ (b) Compression = zero displacement with negative gradient; rarefaction = zero displacement with positive gradient.
✓ (c) Velocity arrows point toward where each particle moves next (use the small-shift method).
Exam question · State / Explain
Q4. State and explain two differences between an electromagnetic wave and a sound wave. [3 marks]
✓ EM waves need no medium and can travel through vacuum; sound requires a medium.
✓ EM waves are transverse (oscillating E and B fields); sound is longitudinal (compressions and rarefactions).
✓ EM waves travel at \(c=3.0\times10^8\ \text{m s}^{-1}\) in vacuum, far faster than sound (~340 m s⁻¹ in air).
Exam question · Explain
Q5. Explain why seismic S-waves (transverse) cannot travel through Earth's liquid outer core, but P-waves (longitudinal) can. What does this tell us about the state of the outer core? [3 marks]
✓ Transverse waves need a medium that can sustain shear stress; liquids cannot resist shear, so S-waves are not transmitted through the liquid outer core.
✓ Longitudinal P-waves rely on compression, which liquids can transmit, so they pass through.
✓ The absence of S-waves through the core is evidence that the outer core is liquid.
Exam question · Deduce
Q6. A displacement–position graph for a longitudinal wave shows four particles P, Q, R and S. The wave travels to the right. P is at maximum negative displacement. Q is at a zero-crossing with negative gradient. R is at maximum positive displacement. S is at a zero-crossing with positive gradient. (a) State the amplitude of the wave. (b) State which particle is at the centre of a compression, and explain. (c) A quarter period later, state the displacement of particle P. [4 marks]
✓ (a) The amplitude is the maximum displacement magnitude shown on the graph.
✓ (b) Q — at a zero-crossing with negative gradient, neighbouring particles move toward Q, crowding together into a compression.
✓ (c) A quarter period later P returns to zero displacement, moving from the extreme toward equilibrium.
Score: 0 pts