IB Physics SL Topic C.2 — Modelling Waves Paper 1 & 2 Longitudinal sound ~7 min read

Sound Waves

Sound is the everyday longitudinal wave. A vibrating source pushes and pulls on the air, sending out a train of squashed and stretched regions that your ear reads as noise — and its frequency and amplitude become the pitch and volume you hear.

📘 What you need to know

How Sound Travels

When a loudspeaker cone (or a voice, or a guitar) vibrates, it repeatedly pushes the nearby air together and then lets it spring back apart. That creates a moving pattern of compressions (air squeezed to high density and pressure) and rarefactions (air stretched to low density and pressure). The pattern races outward to your ear, even though each air particle only jiggles back and forth on the spot.

λcompression (high density) rarefaction (low density)
The speaker sends compressions (dots bunched, high pressure) and rarefactions (dots spread, low pressure) through the air to the ear; the wavelength runs from one compression to the next.

The Spectrum of Sound

Sound covers a continuous range of frequencies, but human ears only pick up a slice of it. That slice — the audible range — runs from about 20 Hz to 20 kHz. Below it lies infrasound (used by elephants and whales); above it lies ultrasound (used by bats and in medical scanning).

INFRASOUND AUDIBLE RANGE ULTRASOUND20 Hz 20 kHz f < 20 Hz f > 20 kHz frequency increasing
Frequency rises left to right: infrasound (below 20 Hz), the human audible range (20 Hz–20 kHz), then ultrasound (above 20 kHz).

Pitch and Volume

Two features of the wave map onto two things you notice about a sound. The frequency sets the pitch: a high frequency (short wavelength) sounds high, a low frequency sounds low. The amplitude sets the volume: a big amplitude sounds loud, a small amplitude sounds quiet.

small amplitude → quiet large amplitude → loud low frequency → low pitch high frequency → high pitch
Top: same pitch, different volume (amplitude). Bottom: same volume, different pitch (frequency). Amplitude → loudness, frequency → pitch.

The Speed of Sound

In air at room temperature, sound travels at roughly 340 m s⁻¹. Two things change that. First, temperature: warmer air means faster-moving particles that pass the vibration on more quickly, so sound speeds up. Second, the state of the medium: sound is fastest in solids, where tightly packed particles hand the oscillation straight to their neighbours, and slowest in gases, where the spread-out particles are far less efficient.

Wave equation (for sound too) v = fλ
Quick recap: sound is longitudinal (needs a medium), heard from 20 Hz to 20 kHz; frequency sets pitch, amplitude sets volume, and it moves ~340 m s⁻¹ in air — fastest in solids.
WE 1

Middle C has a frequency of 256 Hz. Sound travels at 340 m s⁻¹ in air.

Calculate the wavelength of this note in air.

Use the wave equation Rearrange v = fλ to λ = v/f λ = 340 ÷ 256 λ ≈ 1.3 m A low note like this has a wavelength longer than you are tall.
WE 2

A bat emits a sound of wavelength 3.4 mm in air, where the speed of sound is 340 m s⁻¹.

(a) Calculate the frequency. (b) State whether a human could hear it.

Part (a) λ = 3.4 mm = 3.4 × 10⁻³ m, and f = v/λ f = 340 ÷ (3.4 × 10⁻³) f = 100 000 Hz = 100 kHz Part (b) 100 kHz is well above 20 kHz, so it’s ultrasound No — a human cannot hear it

💡 Top tips

⚠ Common mistakes

Up next: the other great family of waves — Electromagnetic Waves — which are transverse, need no medium at all, and all race along at the speed of light.

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