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Chapter 10: Sound Waves — Characteristics and Applications

Science · CBSE Class 9 · NCERT ‘Exploration’ · Notes & Solutions

Sound Waves: Characteristics and Applications — Detailed Notes

Sound is a form of energy that produces the sensation of hearing. This chapter covers how sound is produced, how it travels, its wave nature, its characteristics, and its applications.

10.1 Production of sound

Sound is produced by vibrations (periodic to-and-fro motion) of an object — a plucked rubber band, a struck tuning fork, vibrating vocal cords in the larynx, an air column in a flute. The vibrating object is the source. When the vibration stops, the sound stops.

10.2 Propagation — sound needs a medium

Sound travels through solids, liquids and gases (a medium), but not through vacuum. The bell-jar experiment shows the sound fades as air is pumped out. That is why astronauts in space (near vacuum) cannot hear each other directly and use radio devices.

10.3 Sound waves

A vibrating source pushes air to make a high-density region (compression, C) and pulls back to make a low-density region (rarefaction, R). A travelling series of compressions and rarefactions is a sound wave. The particles only vibrate about their mean positions — they do not travel with the wave; it is the energy that is transferred. Sound is a longitudinal wave (particles vibrate parallel to the direction of propagation) and a mechanical wave (needs a medium). (In a transverse wave, particles vibrate perpendicular to propagation, e.g. light — which needs no medium.)

10.5 Graphical representation

Plotting density vs distance gives a wave: the maximum-density point is a crest (compression), the minimum-density point is a trough (rarefaction), about the average-density line.

10.6 Characteristics of a sound wave

• Wavelength (λ) — distance between two consecutive crests (or troughs); SI unit metre. • Frequency (ν) — number of oscillations per second; SI unit hertz (Hz). • Time period (T) — time for one oscillation; T = 1/ν. • Amplitude — the maximum change in density (bigger amplitude = more energy = louder). • Intensity — sound energy per unit area per unit time (decreases with distance as energy spreads). • Speed (v): v = λ × ν.

Speed of sound is fastest in solids, slower in liquids, slowest in gases (≈340 m s⁻¹ in air, ≈1500 in water, ≈5000 in steel). It increases with temperature and humidity (≈331 m s⁻¹ at 0 °C, ≈344 m s⁻¹ at 22 °C in air). For a given medium the speed is fixed — changing the frequency changes the wavelength, not the speed.

10.6.4 Human perception

Pitch = how we perceive frequency (high frequency → shrill/high pitch). Loudness = how we perceive amplitude (measured in decibels, dB). Audible range of humans = 20 Hz to 20,000 Hz. Below 20 Hz = infrasonic; above 20 kHz = ultrasonic. Timbre distinguishes the same note on different instruments.

10.7 Reflection of sound

Sound obeys the laws of reflection. An echo is a reflected sound heard separately — possible only if the reflected sound arrives at least 0.1 s after the original, so the reflecting surface must be at least 17 m away (distance = v×t/2 = 340×0.1/2). Reverberation is the persistence of sound by multiple reflections in a hall.

10.8 Ultrasound & infrasound applications

Ultrasound (>20 kHz): ultrasonography (imaging organs), breaking kidney stones, cleaning parts, detecting flaws in metals, SONAR (measuring sea depth / locating submarines). Echolocation — bats, dolphins locate objects using reflected ultrasound. Infrasound (<20 Hz): detecting earthquakes, volcanic eruptions, storms (elephants, whales use it).

Key Terms

vibration, medium, vacuum, compression, rarefaction, longitudinal/mechanical wave, crest, trough, wavelength (λ), frequency (ν), time period (T), amplitude, intensity, speed (v = λν), pitch, loudness, decibel, audible range, infrasonic, ultrasonic, echo, reverberation, echolocation, SONAR.

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