Waves & Sound · Lecture Lecture · § 1 / 8
1 / 8
Class XI · Physics · Unit 10 · Lecture

Waves & Sound

The complete lecture — every idea comes alive in the live panel on the right as you read, drawn from real life: a stone dropped in a Clifton pond, a shaken rope, a singing sitar, an ambulance racing past. Press ▶ and let the narration carry you through; or scroll, and the dark stage keeps pace.

A wave is a travelling disturbance that carries energy and momentum through a medium without any net transport of the medium itself. Drop a stone into a still pond at Clifton: rings of ripples race outward across the surface, yet a leaf floating nearby only bobs up and down in place. The energy crosses the pond; the water stays.

  • Mechanical waves — need a material medium: water ripples, sound, waves on a string, seismic waves.
  • Electromagnetic waves — need no medium: light, radio and X-rays cross empty space at 3 × 10⁸ m/s.
  • Progressive wave — crests move forward, handing energy from particle to particle.

Each particle of the medium performs simple harmonic motion about its own mean position (in metres of displacement); only the pattern moves on. The amplitude A is the greatest displacement from the mean, and the energy a wave carries is proportional to A².

Exam point: a wave transfers energy, not matter. A cork or leaf on water ripples never travels with the wave — it oscillates about a fixed point.

Shake one end of a rope up and down: humps and dips (crests and troughs) run along the rope while each rope particle moves only up and down — this is a transverse wave, particle motion perpendicular to the wave. Now push and pull a Slinky along its own length: bunched coils (compressions) and stretched coils (rarefactions) chase each other along — a longitudinal wave, particle motion parallel to the wave.

TransverseLongitudinal
Particle motion⊥ to wave∥ to wave
Patterncrests & troughscompressions & rarefactions
Examplesrope, sitar string, water surface, lightsound in air, Slinky push-pulse
Exam point: sound in air is always longitudinal — a gas has no sideways (shear) rigidity to carry a transverse wave.
  • Wavelength λ — crest-to-crest (or compression-to-compression) distance; one full wave (m).
  • Period T & frequency f — time for one vibration (s); f = 1/T vibrations per second (Hz).
  • Wave speed v — distance the pattern travels per second (m/s).
The wave equationin one period T the wave advances exactly one wavelength → v = λ/T
v = f λ — true for water, sound and light alike

A struck sitar string pushes the surrounding air into a compression, then leaves a rarefaction as it swings back; these pressure pulses travel out as a longitudinal sound wave. Sound needs a medium — pump the air from a bell jar and the ringing bell falls silent. Speed of sound ≈ 331 + 0.61T m/s (T in °C), about 343 m/s at 20 °C; solids > liquids > gases.

worked — a tabla note
f = 250 Hz, v = 340 m/s. Find λ and T.
λ = v/f = 340/250 = 1.36 m · T = 1/f = 4 ms

Three things describe any sound: loudness follows amplitude (intensity ∝ A²), pitch follows frequency, and quality (timbre) follows the waveform — the mix of overtones that makes a flute and a sitar on the same note sound different. Loudness is measured on the logarithmic decibel (dB) scale: 0 dB threshold, ~60 dB talk, ~120 dB pain.

Doppler effect: relative motion between source and observer changes the apparent frequency. An ambulance racing along Sharea Faisal bunches its wavefronts as it approaches — shorter λ, higher pitch — and stretches them as it recedes — longer λ, lower pitch. The siren itself never changes; only the spacing of the wavefronts reaching your ear does.

Exam trap: pitch ↔ frequency, loudness ↔ amplitude — never swap them. Doppler needs motion along the line joining source and observer.

Principle of superposition: where waves overlap, the resultant displacement is the sum of the individual displacements; the waves then pass on unchanged. Drop two stones in the pond and their rings cross — along some lines crests pile on crests, along others crest fills trough.

  • Constructive — crest on crest (in phase): A = A₁ + A₂, louder. Path difference = .
  • Destructive — crest on trough (out of phase): A = |A₁ − A₂| → silence if equal. Path difference = (n + ½)λ.

Two loudspeakers on one signal make loud-and-quiet bands across a room; two ripple-tank dippers draw the same pattern in water. Noise-cancelling headphones are deliberate destructive interference — proof that sound is a wave, because particles could never cancel.

Sound two notes of slightly different frequencies together and they slide in and out of phase: in phase → loud, out of phase → quiet. This periodic throb of loudness is a beat.

Beat frequencyf_beat = |f₁ − f₂| throbs per second (distinct only below ~10 Hz)

Tuning by beats: a sitar or tabla player sounds the instrument against a harmonium note or tuning fork. Beats heard → out of tune; the player tightens or loosens the string until the throbbing slows and vanishes — zero beats means perfectly in tune. Piano tuners do exactly the same.

worked — tuning a sitar string
440 Hz fork + string → 4 beats/s; tightening slows the beats. Original f?
f = 440 ± 4; tightening raised f and beats fell → f was below → 436 Hz

Two identical waves travelling in opposite directions (a wave and its reflection) superpose into a stationary wave: the pattern stops travelling and a plucked guitar or sitar string vibrates in fixed loops.

  • Node (N) — permanently still point; adjacent nodes are λ/2 apart.
  • Antinode (A) — maximum swing, midway between nodes; N→A = λ/4.
  • No net energy transfer — energy stays trapped, sloshing inside each loop.
String fixed at both ends (length L)L = n(λ/2) → fₙ = n·v / 2L = n f₁, n = 1, 2, 3 …
v = √(F/m): tighter string → higher pitch (how a string is tuned)

Resonance & the tube practical: drive a body at its natural frequency and it responds with large amplitude. A struck fork (known f) hums over a tube while the water falls; the air column booms at L₁ ≈ λ/4 and L₂ ≈ 3λ/4, giving λ = 2(L₂ − L₁) and v = 2f(L₂ − L₁).

worked — sitar string fundamental
L = 0.60 m, m = 1.0 × 10⁻³ kg/m, F = 90 N. f₁?
v = √(90/10⁻³) = 300 m/s → f₁ = v/2L = 300/1.2 = 250 Hz

Every idea in this chapter is one sentence: a wave moves energy through a medium while the matter stays put — from the pond's ripples to the air carrying a qawwali.

  • Wave = energy transfer, no matter transfer; particles do SHM about fixed positions.
  • Transverse ⊥ (rope, water, light); longitudinal ∥ (sound) — compressions & rarefactions.
  • v = fλ; v_string = √(F/m); v_sound ≈ 331 + 0.61T m/s ≈ 343 m/s at 20 °C.
  • Loudness ↔ amplitude, pitch ↔ frequency, quality ↔ waveform.
  • Constructive nλ, destructive (n+½)λ; beats f_b = |f₁−f₂| → tuning.
  • Stationary: nodes λ/2 apart, fₙ = nf₁; resonance tube v = 2f(L₂−L₁); Doppler: approach → higher, recede → lower.
🌊 Live panelWaves & Sound
Scroll the lecture — this panel animates each idea as you reach it.