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Science

Waves, sound and hearing

When a school announcement reaches the back of a room, air from the loudspeaker has not travelled all the way into every listener’s ear. A disturbance travels through air, carrying energy and information. Follow that disturbance from its source to the brain.

By PLS Foundation · · 5 min read, plus practice

By the end of this lesson: Distinguish particle motion from wave motion, calculate wavelength and echo distance, and explain the main stages of hearing using a labelled paper model.

Read this topic on its own, or follow Physics: heat, waves, light and electricity

The core idea

A mechanical wave transfers a disturbance through interacting matter. Sound in air is a longitudinal pressure wave; frequency, amplitude and wavelength describe different features, while hearing converts vibrations into nervous signals.

1. Follow the disturbance, not one particle

A wave is a travelling disturbance, or a pattern built from such disturbances. In a mechanical wave, nearby parts of a material exert forces on one another. A displacement at one location therefore influences the next, transferring energy. The material need not travel with the pattern. In an ideal small sound wave, air particles move back and forth around their local equilibrium positions, while the sound travels across the room. Wind, by contrast, is a bulk flow of air. A transverse wave has particle motion perpendicular to its travel direction; a longitudinal wave has particle motion parallel to that direction. These names compare two directions, not two speeds.

Sources: NCERT: Waves ↗

2. Draw compressions and rarefactions

A vibrating source alternately pushes nearby air together and allows it to spread apart. Regions of slightly higher pressure and density are compressions; regions of lower pressure and density are rarefactions. Their propagation is sound in air. On paper, represent air with dots: crowded bands alternate with more spread-out bands. The band pattern moves forward even though a marked dot merely oscillates locally. A pressure-versus-position graph can look like a smooth up-and-down curve, but that does not mean air moves up and down. Its vertical axis represents pressure variation. Sound needs a material medium, so an ideal vacuum cannot carry ordinary sound waves.

Sources: NCERT: Waves ↗

3. Give each wave quantity its own job

Frequency f counts complete oscillations per second and is measured in hertz, Hz. Period T is the time for one oscillation, in seconds: T = 1/f. Wavelength λ, pronounced lambda, is the distance between successive points at the same stage of a repeating pattern, such as neighbouring compressions, in metres. Amplitude describes the maximum departure of a chosen quantity from equilibrium; displacement amplitude and pressure amplitude have different units. Frequency is strongly related to perceived pitch. Amplitude influences sound intensity and perceived loudness, but loudness also depends on frequency and the listener. Making a sound louder does not automatically raise its pitch.

Give each wave quantity a different job

QuantityMeaningIllustrative value
Frequency fCycles per second250 Hz
Period TTime for one cycle1/250 s = 4 ms
Wavelength λDistance between adjacent compressions1.36 m
Wave speed vPattern travel per secondfλ = 340 m/s
Air particles oscillate locally along the travel direction. The pressure pattern travels one wavelength in one period; a single particle does not travel that distance with it.

Sources: NCERT: Waves ↗

4. Connect speed, wavelength and reflection

In one period, a repeating travelling wave advances one wavelength. Therefore v = λ/T = fλ, where v is wave speed in m/s. For small sound waves, speed depends mainly on the medium and its conditions, including temperature; it is not simply set by how loudly the source vibrates. At a stationary boundary, transmitted waves retain the source frequency while speed and wavelength can change. Some energy can reflect. An echo is a distinguishable reflected sound; repeated overlapping reflections produce reverberation. Materials that absorb some sound energy can reduce reverberation in classrooms. Echo calculations must include the outward and return path, not only the distance to the reflecting surface.

Sources: NCERT: Waves ↗ · OpenStax: Speed of Sound, Frequency, and Wavelength ↗

5. Convert vibration into a signal

The outer ear channels sound toward the eardrum. Its vibration moves the middle-ear bones, which transmit vibrations to the fluid-filled cochlea in the inner ear. Fluid movement produces a travelling wave along an internal membrane. Sensory hair cells respond; bending their tiny projections changes ion flow through channels and produces electrical responses. Signals then pass through the auditory nerve to the brain, where sound is interpreted. Different cochlear regions respond most strongly to different frequencies. This sequence crosses several forms of motion and signalling; a sound wave does not remain an airborne pressure wave inside a nerve. A labelled paper flowchart is sufficient to study these stages without producing loud sounds.

Sources: NIH NIDCD: How Do We Hear? ↗

6. Worked example: a repeating pressure pattern

Illustrative classroom calculation: a source has frequency 250 Hz and the sound speed is given as 340 m/s. The speed is a model value for the stated conditions, not a universal constant. Wavelength λ = v/f = 340/250 = 1.36 m. Period T = 1/250 = 0.004 s, or 4 milliseconds; 1 millisecond is 0.001 s. During those 4 milliseconds the pattern moves 1.36 m. An air particle does not travel 1.36 m with it. Doubling frequency while keeping the medium and speed unchanged would halve the wavelength, because twice as many repeating patterns must pass per second.

Sources: NCERT: Waves ↗

7. Worked example: an echo on paper

A hypothetical sound pulse returns to its starting point 0.40 s after reflecting from a stationary wall. Assume a straight path, negligible wind and a constant sound speed of 340 m/s. The total path is vt = 340 × 0.40 = 136 m. If the wall is distance d away, the path is d outward plus d back, so 2d = 136 m and d = 68 m. Using 136 m as the wall distance would count the return journey twice. If the receiver were somewhere else, the two legs would not generally be equal, so this simple divide-by-two rule would need reconsideration.

Sources: NCERT: Waves ↗ · OpenStax: Speed of Sound, Frequency, and Wavelength ↗

PUT IT INTO PRACTICE

Apply it and check your reasoning

  1. On paper, use hypothetical f = 500 Hz and v = 340 m/s. Calculate λ and T, writing the units at each step.
  2. Draw adjacent compressions one wavelength apart and mark a single particle’s back-and-forth direction. Predict what happens to wavelength if frequency doubles at the same speed.
  3. Check: λ = 0.68 m and T = 0.002 s = 2 ms. At 1000 Hz the wavelength is 0.34 m. Particle oscillation is parallel to sound travel, but its local displacement is not the wavelength.

Check your understanding

Why does a sound wave differ from wind?

Sound is a propagating pressure disturbance with local oscillation; wind is bulk movement of air. Both can be present together.

Does a drawn crest prove that sound in air is transverse?

No. Check the vertical-axis quantity. A pressure graph shows pressure rising and falling, not sideways particle displacement.

Can two sounds have the same pitch but different loudness?

Yes. Similar frequencies can occur with different amplitudes and intensities. Pitch and loudness describe different perceptual features.

Why is an echo distance usually smaller than speed multiplied by return time?

That product gives the entire travelled path. When source and receiver share a position, the wall distance is half the outward-and-return path.

Does the auditory nerve carry moving air to the brain?

No. Sensory cells convert mechanical stimulation into electrical signalling, which the nervous system transmits and interprets.

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