Intuition Why this page exists
The parent note gave you the tools: v = f λ , v = T / μ , the travelling wave y = A sin ( ω t − k x ) , and particle velocity. But tools only stick when you've swung them at every kind of nail . Below we first list every case class this topic can throw at you, then work one example per class — so no exam scenario is new to you.
Before we start, one reminder of the symbols we reuse (all built in the parent):
A = amplitude , the biggest displacement a particle reaches (metres).
ω = angular frequency (radians per second), and f = ω /2 π (cycles per second, hertz).
k = angular wave number (radians per metre), and λ = 2 π / k (metres per cycle).
v = ω / k = f λ = speed the pattern moves.
v p = ∂ y / ∂ t = speed a single particle moves up/down.
φ = phase constant (radians): a fixed head-start added inside the sine, y = A sin ( ω t − k x + φ ) . It just shifts where the wave sits at t = 0 ; it never changes A , ω , k , or v .
T = tension in a string (newtons): the pull along the string that acts as the restoring force. (Not to be confused with a period; on this page T always means tension.)
μ = linear mass density of a string (kilograms per metre): mass per unit length, the inertia the restoring pull has to move.
For bulk media: Y = Young's modulus, B = bulk modulus (both in pascals, Pa ), ρ = mass density (kg/m 3 ) — the elastic and inertial properties of a solid/fluid.
See Mechanical waves — transverse and longitudinal for how each of these was born, and Simple Harmonic Motion for why the sine appears at all.
Cell
Case class
What's tricky
Example
C1
Read a + x wave equation
extract every quantity, get sign of travel right
Ex 1
C2
Read a − x wave equation
sign flip sin ( ω t + k x ) → direction reversed
Ex 2
C3
Particle velocity & the slope link
don't confuse v p with v ; sign of v p at a chosen instant
Ex 3
C4
Speed from medium (string)
v = T / μ , and scaling under × tension
Ex 4
C5
Speed from medium (solid vs fluid)
pick Y / ρ vs B / ρ ; which wave types are allowed
Ex 5
C6
Degenerate / zero inputs
A = 0 , f = 0 , T = 0 , k = 0 — what "wave" survives?
Ex 6
C7
Limiting behaviour
f → ∞ (λ → 0 ), μ → ∞ (v → 0 )
Ex 7
C8
Real-world word problem
echo / distance, must model then compute
Ex 8
C9
Exam-style twist
build the equation from graph + given direction
Ex 9
C10
Nonzero phase constant φ
read/build y = A sin ( ω t − k x + φ )
Ex 10
Every numeric answer below is machine-checked in the verify block.
A wave is y = 0.05 sin ( 400 t − 8 x ) (SI units). Find A , ω , f , k , λ , v , and the direction of travel.
Forecast: Guess — is λ bigger or smaller than 1 metre? Is the wave going left or right?
Step 1. Compare 0.05 sin ( 400 t − 8 x ) to the standard form A sin ( ω t − k x ) .
Why this step? The standard form is a template: each slot has a physical meaning, so lining them up hands us every quantity at once.
A = 0.05 m , ω = 400 rad/s , k = 8 rad/m
Step 2. Frequency: f = 2 π ω = 2 π 400 = 63.7 Hz .
Why this step? ω counts radians per second; dividing by 2 π (radians per full cycle) converts to cycles per second.
Step 3. Wavelength: λ = k 2 π = 8 2 π = 0.785 m .
Why this step? k counts radians per metre; 2 π radians is one full spatial cycle = one wavelength.
Step 4. Speed: v = k ω = 8 400 = 50 m/s .
Why this step? A crest is where the phase ω t − k x stays fixed; keeping it fixed forces x to advance at ω / k .
Step 5. Direction: the form is ω t − k x (a minus ), so the wave moves in + x .
Why this step? To keep phase constant as t grows, x must grow too — the pattern slides in the + x direction.
Verify: cross-check v = f λ = 63.7 × 0.785 = 50 m/s ✓ — matches Step 4. Units: ( Hz ) ( m ) = m/s ✓.
y = 0.01 sin ( 200 t + 5 x ) (SI). Find v and the direction of travel.
Forecast: The only change from Ex 1's form is a plus sign. Does that change the speed , the direction , or both?
Step 1. Compare to A sin ( ω t + k x ) : ω = 200 , k = 5 .
Why this step? Same template idea — but now the phase is ω t + k x .
Step 2. Speed magnitude: v = k ω = 5 200 = 40 m/s .
Why this step? Speed is always ∣ ω / k ∣ ; the sign lives in the direction , not the magnitude.
Step 3. Direction: to hold phase ω t + k x constant as t grows, x must shrink , so the wave moves in − x .
Why this step? A plus sign means "the delay runs backwards" — the pattern travels toward decreasing x .
Verify: the plus sign changed only the direction, not the speed (40 m/s , a plain magnitude). Units of ω / k = ( rad/s ) / ( rad/m ) = m/s ✓.
This figure shows a snapshot of the Ex 1 wave frozen at t = 0 (white curve, displacement y up the page vs position x across it). The yellow dot marks the particle at x = 0 , sitting on the rest line y = 0 . The pink arrow points straight up from it — that's the particle velocity v p , showing this particle is climbing at that instant. The separate blue arrow points along + x — that's the wave velocity, the whole pattern sliding sideways. Two different arrows, two different motions: read them as "the dot bobs along pink; the shape marches along blue."
For y = 0.05 sin ( 400 t − 8 x ) (the Ex 1 wave), find (a) the maximum particle speed, and (b) the particle velocity at x = 0 , t = 0 .
Forecast: The wave moves at 50 m/s (Ex 1). Guess: is a particle's up-down speed bigger or smaller than that?
Step 1. Particle velocity is v p = ∂ t ∂ y . Differentiate y = A sin ( ω t − k x ) with respect to t (holding x fixed):
v p = A ω cos ( ω t − k x )
Why this step? "How fast does one particle move up/down?" is exactly the rate of change of its displacement in time — that's the time-derivative, one particle at a time.
Step 2. Maximum particle speed = A ω because cos maxes at 1 :
v p , m a x = A ω = 0.05 × 400 = 20 m/s
Why this step? The cosine can't exceed 1 ; the biggest speed happens as the particle whips through its rest line (crest/trough are where it momentarily stops).
Step 3. At x = 0 , t = 0 : v p = A ω cos ( 0 ) = 20 m/s (moving up , positive).
Why this step? Plug the instant in. Look at the yellow dot in the figure: at this instant the particle sits at y = 0 and is climbing — maximum upward speed.
Step 4 (sanity, the slope link — derived here, not assumed). Differentiate the same y = A sin ( ω t − k x ) with respect to x (holding t fixed) to get the snapshot's slope:
∂ x ∂ y = − A k cos ( ω t − k x )
Compare it to the time-derivative ∂ y / ∂ t = A ω cos ( ω t − k x ) from Step 1. Divide one by the other: ∂ y / ∂ x ∂ y / ∂ t = − A k cos A ω cos = − k ω = − v . Rearranged:
v p = ∂ t ∂ y = − v ∂ x ∂ y
Why this step? This is the "slope link": a particle's up-down speed equals − v times the local steepness of the frozen shape. The minus sign is the physics — where the snapshot slopes downward to the right, the wave sliding into that point pushes the particle up . Plugging back reproduces v p = A ω cos , so the two routes agree.
Verify: v p , m a x = 20 m/s is smaller than the wave speed 50 m/s here — but note they measure different things (up-down vs pattern). Units: ( m ) ( rad/s ) = m/s ✓.
A string has linear mass density μ = 4 × 1 0 − 3 kg/m and tension T = 100 N . (a) Find v . (b) If tension is quadrupled to 400 N , find the new v .
Forecast: Quadruple the tension — does v quadruple, double, or something else?
Step 1. Transverse string speed: v = μ T .
Why this step? Speed is a tug-of-war: restoring pull T (the tension, up) over inertia μ (mass per length, down). The square root balances their units to give m/s.
Step 2. v = 4 × 1 0 − 3 100 = 25000 = 158 m/s .
Why this step? Direct substitution of the given medium properties.
Step 3. Quadruple T : v new = 4 × 1 0 − 3 400 = 100000 = 316 m/s .
Why this step? Since v ∝ T , multiplying T by 4 multiplies v by 4 = 2 .
Verify: 316/158 = 2 exactly ✓ — the turned a × 4 into a × 2 . Units: ( N ) / ( kg/m ) = m 2 / s 2 = m/s ✓.
(a) A steel rod: Young's modulus Y = 2.0 × 1 0 11 Pa , density ρ = 8000 kg/m 3 . Find the longitudinal wave speed. (b) Water: bulk modulus B = 2.2 × 1 0 9 Pa , ρ = 1000 kg/m 3 . Find the sound speed. (c) Which of these media can carry a transverse bulk wave?
Forecast: Steel is far stiffer than water. Guess: is steel's speed ~2×, ~5×, or ~10× water's?
Step 1. Solid rod uses Young's modulus Y : v = Y / ρ .
Why this step? A rod stretched along its length resists with Y ; that's the restoring elasticity for a longitudinal rod wave.
v steel = 8000 2.0 × 1 0 11 = 2.5 × 1 0 7 = 5000 m/s
Step 2. Fluid uses bulk modulus B : v = B / ρ .
Why this step? A fluid has no shear stiffness, only resistance to compression — that's B .
v water = 1000 2.2 × 1 0 9 = 2.2 × 1 0 6 = 1483 m/s
Step 3. Transverse bulk waves: only the steel can carry them.
Why this step? Transverse motion needs shear rigidity. Solids have it; the fluid (water bulk) does not — exactly the parent's rule. See Sound waves for why fluid sound is longitudinal.
Verify: 5000/1483 = 3.37 — steel is ~3.4× faster ✓. Units of both: ( Pa ) / ( kg/m 3 ) = m/s ✓.
Discuss (a) A = 0 , (b) f = 0 , (c) tension T = 0 on a string, (d) k = 0 . What "wave" survives each?
Forecast: Which of these four still leaves something moving?
Step 1. A = 0 : y = 0 ⋅ sin ( ω t − k x ) = 0 for all x , t .
Why this step? Amplitude scales the whole displacement; zero amplitude = flat medium = no wave at all . Every particle stays home.
Step 2. f = 0 : then ω = 2 π f = 0 , so y = A sin ( − k x ) , frozen in time.
Why this step? Zero frequency means nothing oscillates in time — you get a static bent shape , not a travelling wave. No energy propagates.
Step 3. T = 0 : v = T / μ = 0 = 0 .
Why this step? With no tension there is no restoring force, so a disturbance can't be pulled onward — speed collapses to zero ; a "kink" just sits there.
Step 4. k = 0 : then λ = 2 π / k → ∞ and y = A sin ( ω t ) — no spatial variation , every particle oscillates in step (in phase).
Why this step? Zero wave number means the "wave" has infinite wavelength — no crests or troughs anywhere along x , so the whole medium bobs together like a single SHM oscillator. It's the opposite degenerate limit to f = 0 : here time varies but space doesn't. Nothing propagates (no phase lag between points), so it isn't a travelling wave either.
Verify: four degeneracies, four distinct failures of propagation — via A → 0 (flat), ω → 0 (frozen in time), v → 0 (can't be carried), k → 0 (no spatial pattern). 0 = 0 ✓ and 2 π / k → ∞ as k → 0 ✓.
On a fixed string (speed v = 200 m/s fixed by the medium): (a) as f → ∞ , what happens to λ ? Compute λ at f = 100 , f = 1000 , f = 10000 Hz . (b) If instead μ → ∞ at fixed T , what happens to v ?
Forecast: Which quantity shrinks toward zero in each limit?
Step 1. From v = f λ with v fixed: λ = v / f .
Why this step? Medium fixes v ; the source picks f ; so λ is forced to adjust — it's the dependent variable here.
Step 2. Compute:
λ 100 = 100 200 = 2 m , λ 1000 = 0.2 m , λ 10000 = 0.02 m
Why this step? As f → ∞ , λ = v / f → 0 — waves crowd tighter and tighter while their speed never changes.
Step 3. μ → ∞ limit: v = T / μ → 0 .
Why this step? An infinitely heavy string has infinite inertia, so a fixed restoring tension can barely accelerate it; the disturbance is passed on ever more slowly, and in the limit the wave crawls to a standstill (v → 0 ).
Verify: each × 10 in f gave a ÷ 10 in λ (2 → 0.2 → 0.02 ) ✓ — clean inverse proportionality, and v stayed 200 m/s throughout.
You clap facing a cliff and hear the echo 1.2 s later. Sound speed in air = 340 m/s . How far away is the cliff?
Forecast: Will you divide the total distance by 2, or multiply by 2? (The sound makes a round trip.)
Step 1. Total path travelled by the sound = v × t = 340 × 1.2 = 408 m .
Why this step? Distance = speed × time; the medium fixes v , the stopwatch gives t .
Step 2. That path is there and back , so the cliff distance is half:
d = 2 408 = 204 m
Why this step? The echo returns, so the wave covered the cliff distance twice — divide by 2 to get the one-way distance.
Verify: round trip = 2 × 204 = 408 m , and 408/340 = 1.2 s ✓ — plugging back reproduces the given time. Units: ( m/s ) ( s ) = m ✓.
This figure is a snapshot of the wave you're about to build: displacement y (up) vs position x (across), amplitude A = 0.03 m marked by the blue vertical arrow from the rest line to a crest, and the wavelength λ = 0.5 m marked by the pink double-arrow spanning crest to crest (two yellow dots). The yellow arrow near the bottom shows the required travel direction (− x ). Everything you need to fill the template A sin ( ω t ± k x ) is read straight off this picture.
A transverse wave has amplitude A = 0.03 m , wavelength λ = 0.5 m , frequency f = 20 Hz , travelling in the − x direction. Write y ( x , t ) and find v .
Forecast: Given − x travel, will your equation contain − k x or + k x ?
Step 1. Angular frequency: ω = 2 π f = 2 π ( 20 ) = 40 π ≈ 125.66 rad/s .
Why this step? The standard form needs ω , not f ; convert cycles/s to radians/s with 2 π .
Step 2. Wave number: k = λ 2 π = 0.5 2 π = 4 π ≈ 12.57 rad/m .
Why this step? The form needs k (radians per metre), obtained from wavelength.
Step 3. Direction − x ⇒ use ω t + k x (from Ex 2's rule). So:
y ( x , t ) = 0.03 sin ( 40 π t + 4 π x ) m
Why this step? A plus sign inside makes phase constant require decreasing x — i.e. travel toward − x , as required.
Step 4. Speed: v = f λ = 20 × 0.5 = 10 m/s .
Why this step? In one period the pattern advances one wavelength, so v = f λ — independent of direction.
Verify: cross-check v = ω / k = 40 π /4 π = 10 m/s ✓ — matches f λ . The figure shows the snapshot with λ = 0.5 m marked crest-to-crest.
A wave is y = 0.04 sin ( 50 t − 2 x + 2 π ) (SI). (a) Find A , ω , k , v . (b) What is y at x = 0 , t = 0 , and why is it not zero? (c) Rewrite this wave using cosine.
Forecast: With that extra + 2 π inside, will A , ω , k , or v change compared with a φ = 0 wave?
Step 1. Compare to the full form A sin ( ω t − k x + φ ) : read off A = 0.04 , ω = 50 , k = 2 , φ = 2 π .
Why this step? The phase constant φ is just one more slot in the template — the largest new idea here is recognising it as a fixed head-start, not a rate.
Step 2. Speed and everything geometric are untouched: v = k ω = 2 50 = 25 m/s .
Why this step? φ is a constant; it drops out when you track a crest (phase = const still gives v = ω / k ). So φ shifts where the wave starts, never how fast it goes.
Step 3. At x = 0 , t = 0 : y = 0.04 sin ( 0 − 0 + 2 π ) = 0.04 sin 2 π = 0.04 m .
Why this step? Without φ the wave would sit at y = 0 at the origin; the 2 π head-start advances it a quarter-cycle, so it starts at a crest (y = A ) instead. That's exactly what a phase constant does — it sets the starting point.
Step 4. Cosine form: since sin ( θ + 2 π ) = cos θ , we get y = 0.04 cos ( 50 t − 2 x ) .
Why this step? A + 2 π phase shift is the difference between sine and cosine — showing that "which trig function" and "what φ " are the same choice, not two different physics.
Verify: A , ω , k , v match the φ = 0 case's method exactly (v = 25 m/s ); only the t = 0 starting value moved from 0 to 0.04 m ✓. And 0.04 sin ( 50 t − 2 x + 2 π ) = 0.04 cos ( 50 t − 2 x ) is an identity ✓.
Recall Scenario matrix — cover the answers
Sign inside the sine is minus (ω t − k x ) ::: wave travels in + x
Sign inside the sine is plus (ω t + k x ) ::: wave travels in − x
Maximum particle speed ::: A ω
Quadruple the tension changes v by factor ::: 4 = 2
Fluid bulk cannot carry which wave type ::: transverse (no shear rigidity)
A = 0 , f = 0 , T = 0 , k = 0 each kill propagation via ::: A → 0 (flat), ω → 0 (frozen), v → 0 (uncarried), k → 0 (no spatial pattern)
As f → ∞ at fixed v , λ ::: → 0
Echo: divide the round-trip distance by ::: 2
A phase constant φ changes ::: only where the wave sits at t = 0 , not A , ω , k , v
"Minus moves plus, plus moves minus." A minus sign inside sin ( ω t ∓ k x ) sends the wave toward + x ; a plus sends it toward − x .
Related deep tools: Wave equation , Superposition and Interference , Standing waves & resonance , Doppler effect .