Know that for a transverse wave, the direction of vibration is at right angles to the direction of propagation and understand that electromagnetic radiation, water waves and seismic S-waves (secondary) can be modeled as transverse

3.1 General Properties of Waves

Learning Objective

Students will be able to:

  • State that in a transverse wave the direction of vibration is at right angles (90°) to the direction of propagation.
  • Model electromagnetic radiation, water‑surface waves and seismic S‑waves (secondary waves) as transverse waves.
  • Distinguish transverse from longitudinal waves and predict which media can support each type.

What Is a Wave?

A wave is a disturbance that carries energy from one location to another without the permanent transport of matter. The disturbance may be:

  • a displacement of particles in a material medium (e.g., a rope, air, water), or
  • a variation of a field, such as the electric‑magnetic (EM) field.

Wave Terminology

SymbolQuantityDefinition
λWavelengthDistance between two successive points that are in the same phase (e.g., crest‑to‑crest or trough‑to‑trough).
fFrequencyNumber of complete cycles that pass a fixed point each second (unit: hertz, Hz).
TPeriodTime for one complete cycle; \(T=\dfrac{1}{f}\) (seconds).
AAmplitudeMaximum displacement of the medium (or field) from its equilibrium position.
vWave speedRate at which the wave propagates; \(v=f\lambda\) (m s⁻¹).
kWave‑numberSpatial frequency; \(k=\dfrac{2\pi}{\lambda}\) (rad m⁻¹).
ωAngular frequencyTemporal frequency; \(ω=2\pi f\) (rad s⁻¹).

Mathematical Description of a Sinusoidal Wave

For a wave travelling in the +x direction the displacement (or field strength) y at position x and time t can be written as

\[

y(x,t)=A\sin\!\big(kx-\omega t\big)

\]

kx gives the spatial variation (how the wave looks along the x‑axis).

ωt gives the time variation (how the wave evolves).

The negative sign indicates propagation in the +x direction; a plus sign would describe a wave moving in the –x direction.

Worked Example – Speed of a Rope Wave

Given: frequency \(f=5\;\text{Hz}\), wavelength \(λ=0.40\;\text{m}\).

Find: wave speed \(v\).

\[

v = f\lambda = (5\;\text{Hz})(0.40\;\text{m}) = 2.0\;\text{m s}^{-1}

\]

Transverse Waves

A transverse wave is one in which the particles of the medium (or the fields) oscillate perpendicular to the direction in which the wave travels.

Rope being flicked – propagation to the right, particle motion up and down

Rope wave: arrows show propagation (→) and particle vibration (↑).

Common Transverse Waves

  • Electromagnetic (EM) radiation – Light, radio waves, X‑rays, etc. The electric field E and magnetic field B oscillate at right angles to each other and to the direction of travel.
  • Water‑surface waves – Particles move in (approximately) circular orbits: a dominant up‑and‑down motion (transverse) combined with a small forward‑backward component (longitudinal).
  • Seismic S‑waves (secondary or shear waves) – Ground particles move side‑to‑side or up‑and‑down, perpendicular to the direction the wave front travels. S‑waves cannot travel through fluids because fluids cannot sustain shear stress.

Longitudinal Waves

In a longitudinal wave the particles vibrate parallel to the direction of propagation. The disturbance consists of alternating regions of compression (high density) and rarefaction (low density).

Sound wave in air – particle motion back and forth along the direction of travel

Sound wave in air: particle motion (←→) is along the direction of travel (→).

  • Examples: Sound in air, compression waves in a slinky, seismic P‑waves (primary).

Transverse vs. Longitudinal – Quick Comparison

FeatureTransverseLongitudinal
Particle vibration directionPerpendicular to propagationParallel to propagation
Typical examplesLight, water‑surface waves, S‑wavesSound in air, P‑waves, spring compression
Medium requirementCan travel in vacuum (EM) or any elastic solid/fluid (mechanical)Requires a material medium that can be compressed
Energy transport mechanismOscillating fields or shear deformationCompression‑rarefaction cycles

Key Behaviour of All Waves

  • Reflection – Wave returns into the original medium when it meets a boundary. Angle of incidence = angle of reflection.
  • Refraction – Change in direction when a wave passes into a medium where its speed is different. Described by Snell’s law

    \[

    n{1}\sin\theta{1}=n{2}\sin\theta{2}

    \]

    where \(n\) is the refractive index.

  • Diffraction – Bending of waves around obstacles or through apertures comparable in size to the wavelength.

Practical Illustration – Ripple‑Tank Experiment (IGCSE Practical)

  1. Generate circular waves with a point source (vibrating rod).
  2. Place a narrow slit in the tank. Observe straight‑line wave fronts beyond the slit – diffraction.
  3. Introduce a rectangular barrier at an angle. Reflected wave fronts demonstrate reflection.
  4. Insert a glass plate partially immersed in the water. The change in wave speed causes the wave fronts to bend – refraction.

By measuring the distance between successive crests (λ) and knowing the vibrator frequency (f), students can calculate the wave speed using \(v=fλ\), reinforcing the wave‑speed relationship.

Key Points to Remember

  1. The vibration direction of a transverse wave is at right angles (90°) to its direction of travel.
  2. Electromagnetic radiation is a transverse wave that does not need a material medium.
  3. Water‑surface waves are mainly transverse; particle motion is roughly circular.
  4. S‑waves are shear waves; they cannot propagate through liquids or the Earth’s outer core.
  5. Reflection, refraction and diffraction are observable for both transverse and longitudinal waves, and the ripple‑tank provides a visual demonstration.

Common Misconceptions

  • “All waves are the same.” – Waves differ in particle motion (transverse vs. longitudinal) and in the media that can support them.
  • “Light needs air to travel.” – Light is an EM transverse wave; it travels through vacuum as well as through transparent media.
  • “Water particles travel with the wave.” – In surface waves each particle moves in a small orbit; the net horizontal displacement is negligible.
  • “S‑waves can pass through the Earth’s outer core.” – The outer core is liquid and cannot sustain shear stress, so S‑waves are blocked (they are shadowed in seismograms).

Practice Questions

  1. Identify the wave type (transverse or longitudinal) for each phenomenon:

    (a) A guitar string vibrating.

    (b) A sound wave in air.

    (c) A radio broadcast.

    (d) A ripple on a pond.

  2. Explain why seismic S‑waves cannot travel through the Earth’s outer core.
  3. Draw a labelled sketch of a transverse wave on a rope, showing the direction of propagation and the direction of particle vibration.
  4. A ripple‑tank source produces waves of frequency 2 Hz. The measured wavelength is 0.30 m. Calculate the wave speed.
  5. Using Snell’s law, determine the angle of refraction when a light ray passes from air (n = 1.00) into water (n = 1.33) at an incidence angle of 30°.