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Spec mapping (OCR H556 Module 4.5): Describe stationary waves as the superposition of two progressive waves of equal amplitude and frequency travelling in opposite directions; identify nodes and antinodes; derive harmonic frequencies on strings (fn=nv/2L) and in air columns (open–open: all harmonics; open–closed: odd harmonics only). PAG 3 anchor for measurement of the speed of sound or fundamental frequency on a stretched string using Melde's apparatus.
When two progressive waves of the same frequency and amplitude travel in opposite directions through the same region, their superposition produces a wholly different kind of pattern — a stationary wave (also called a standing wave). Rather than travelling through space, the wave appears to be "frozen" in place, with certain points (nodes) where the displacement is always zero and other points (antinodes) where the oscillation is maximum.
Stationary waves are the physics of musical instruments. Every string you have plucked, every pipe you have blown across, and every tuning fork you have struck produces sound by setting up stationary waves. This lesson introduces stationary waves in general, the distinction between nodes and antinodes, and the specific cases of stationary waves on strings (with both ends fixed) and in pipes (open and closed). The OCR A-Level specification expects quantitative treatment using:
f=2L1μT
(fundamental frequency on a stretched string).
Consider a progressive wave travelling to the right along a string, meeting a fixed end. The wave is reflected, with a π phase shift (because a fixed end cannot move, the reflected wave must cancel the incoming displacement). The result is two waves of the same frequency and amplitude, travelling in opposite directions along the same string.
By the principle of superposition, the total displacement at any point is the sum of the two waves' displacements. Mathematically, the two opposing travelling waves combine to give:
y(x,t)=2Asin(kx)cos(ωt)
where k=2π/λ is the wavenumber and ω=2πf the angular frequency of each constituent wave.
The spatial part sin(kx) is independent of time; the temporal part cos(ωt) applies equally to every point. At positions where sin(kx)=0 — called nodes — the displacement is always zero. At positions where sin(kx)=±1 — called antinodes — the amplitude of oscillation is maximum (2A, twice that of either constituent wave).
This is the defining feature of a stationary wave: the pattern is stationary in space — nodes remain nodes and antinodes remain antinodes — while each point between them oscillates in simple harmonic motion at angular frequency ω.
A node is a point on a stationary wave where the displacement is always zero. Nodes form at positions where the two travelling waves permanently cancel.
An antinode is a point where the amplitude of oscillation is maximum. Antinodes form at positions where the two travelling waves permanently reinforce.
Key facts about nodes and antinodes:
This list is worth memorising — it is the bedrock of every stationary-wave question.
A string of length L, fixed at both ends (like a guitar or violin string) can support stationary waves only if the pattern has nodes at both ends, because the fixed ends cannot move.
The only stationary waves that fit are those with a whole number of half-wavelengths between the ends:
L=2nλ,n=1,2,3,…
So the allowed wavelengths are:
λn=n2L
and the corresponding frequencies (using v=fλ) are:
fn=2Lnv,n=1,2,3,…
These are the harmonics of the string.
The fundamental frequency (first harmonic) is the lowest allowed frequency:
f1=2Lv
It corresponds to n=1 — a single "half-wavelength loop" with nodes at each end and one antinode in the middle.
The overtones of a string are the harmonics above the fundamental. In music theory the second harmonic is the first overtone, the third the second overtone, etc.
flowchart LR
Start[Stretched string of length L, both ends fixed]
Start --> Cond[Node at each end]
Cond --> Half[Length must contain integer number of half wavelengths]
Half --> Form[Allowed wavelengths lambda equals 2L over n]
Form --> Freq[Allowed frequencies f equals n v over two L]
Freq --> F1[Fundamental f1 equals v over 2L]
Freq --> Fn[All harmonics n equals 1 2 3 present]
The speed of a transverse wave on a stretched string is:
v=μT
where:
Substituting into f1=v/(2L), the fundamental frequency of a stretched string becomes:
f1=2L1μT
This is the formula you must know. It tells you that the pitch of the string rises:
This is the full physics of how guitars, violins, pianos and harps are tuned and played.
Q. A guitar string has length L=0.65 m, mass per unit length μ=1.0×10−3 kg m−1, and is under tension T=100 N. Calculate the fundamental frequency.
A.
v=μT=1.0×10−3100=1.00×105=316 m s−1
f1=2Lv=2×0.65316=243 Hz
Slightly lower than the 247 Hz of the B3 on a standard guitar — plausibly, a B string that needs a slight tune-up.
Q. For the same guitar string, calculate the frequency of the second harmonic.
A. f2=2f1=2×243=486 Hz.
Q. A string of length L=0.50 m and μ=2.0×10−3 kg m−1 is to produce a fundamental of 300 Hz. Calculate the required tension.
A. From f1=(1/2L)T/μ:
300=2×0.5012.0×10−3T=2.0×10−3T
9.00×104=2.0×10−3T⇒T=180 N
Q. A musician finds her guitar's open A-string sounds at 220 Hz when tuned correctly. After a temperature drop the same string sounds at 208 Hz. By what fraction has the tension changed?
A. f1∝T, so
ToldTnew=(220208)2=0.894
Tension has dropped by about 11% — the typical effect of overnight cold contraction.
A stationary wave on a stretched string stores energy that oscillates between purely kinetic and purely potential forms — but the total energy stays constant. Consider the snapshots of the wave's shape across one period:
So the period of the energy oscillation is T/2, half the period of the displacement oscillation. This is a generic feature of harmonic motion: kinetic and potential energies each oscillate at twice the displacement frequency, π/2 rad out of phase with each other, summing to a constant total.
For a string of length L, linear mass density μ, vibrating in its n-th harmonic with antinode amplitude A, the total energy is
E=41μω2A2L
(where ω=2πfn). You will not be asked to derive this at A-Level, but it tells you that doubling the amplitude quadruples the energy stored — important when discussing loudness of musical instruments or the energy dissipated when a vibrating string stops oscillating.
A real Melde's string driven by an oscillator does not vibrate at exactly one frequency — it responds with significant amplitude across a range of frequencies near each harmonic. This is a resonance curve: a peak in amplitude vs driving-frequency centred on each harmonic fn, with a finite width Δf determined by damping.
The quality factor is defined as
Q=Δffn
A high-Q resonator (low damping) has a very sharp, tall peak — the string only responds significantly within a narrow frequency window of fn. A low-Q resonator (heavily damped) has a broad, shallow peak.
For a Melde's-apparatus demonstration string, Q∼10–100 is typical. Plucked piano strings reach Q∼103; high-quality crystal oscillators in electronics achieve Q∼106 or higher.
This explains a subtle observation from the lab: when you sweep the oscillator frequency through a harmonic, you don't see a sudden snap from "no pattern" to "perfect pattern" and back — the pattern builds smoothly, reaches a peak at fn, then fades. The width of that transition is Δf. For sharp Q resonance the transition is rapid; for weak resonance it is gradual.
The second classical case is stationary waves in a column of air — a pipe. Pipes come in two types, differing in whether the ends are open or closed.
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