A pulse travels while the string stays in place
Briefly move a taut string sideways. The disturbance travels along it while each small material segment is displaced transversely. The speed of the travelling shape depends on how strongly neighbouring segments pull on each other and how much mass must be accelerated.[1]
The model requires Newton’s force law, mass per length, and small slopes. Tension is a force in newtons. Linear mass density tells you how many kilograms occupy one metre of the taut string; it is neither total mass nor density per volume.[1]
Specify tension and mass per unit length
applies to a uniform string; L is its length in the considered taut state.[1]
denotes longitudinal tension magnitude in newtons. is linear mass density in , not density per volume in . Total mass alone does not fix it: a shorter string with the same mass contains more mass per length. Varying thickness or composition can change local linear density, so a single constant speed is not automatic.
The formula describes a transverse disturbance propagating along the string. An element moves mainly across the string; its speed additionally depends on frequency and amplitude. Tension supplies restoring action while string mass resists transverse acceleration.
Small slope is the geometric approximation
Let describe small transverse motion about a nearly straight string. Local slope must have magnitude much smaller than 1. Then and length changes are higher-order effects. The linear model treats tension and mass per projected length as constant.[1]
Small amplitude alone is insufficient at very short wavelength; the relevant product is Ak.
A hypothetical 1 mm amplitude at gives . The same amplitude at gives , outside the small-slope approximation. This comparison separates geometric scale from absolute displacement.
Balance transverse forces on a short element
Isolate an element between x and x + Δx. Tensions point outward along the local tangents. In the linear model their horizontal magnitudes are FT, giving transverse resultant FT[∂xy(x+Δx) − ∂xy(x)]. For a smooth shape this becomes FT∂2xy Δx. Element mass is .[1]
Apply Newton’s law to transverse motion; Δx cancels.
A smooth travelling disturbance solves the equation when .
The positive speed magnitude is therefore a square root. Direction is selected by or g(x+vt). The force-to-mass ratio follows from the model assumptions; it is not a universal formula for any rope, bending vibration or slack string.
Double speed requires four times the tension
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Mass units, rearrangements and scaling
Solving for μ needs ; taking the square root gives m/s.
1 g/m equals 0.001 kg/m. If mass is measured in grams and length in centimetres, convert them separately. Quadrupling tension at fixed μ doubles v; quadrupling μ at fixed tension halves v. Doubling speed requires four times the tension when μ is unchanged.
For and , . Increasing real tension can lengthen the string and change mass per length. Keeping fixed is therefore an explicit model condition, not an automatic property of every experiment.
Here, string tension means tensile force in newtons. Mechanical normal stress is instead force per cross-sectional area, , in pascals. Without the appropriate area, a value in pascals cannot be inserted as tension; linear mass density does not supply that area either.[6][1]
Two original calculations: transit time and retensioning
A uniform string sample
- Given
- A uniform sample in the considered state has mass 12.0 g over 2.40 m. FT = 72 N; a transverse disturbance travels 1.50 m; flexible linear model.
- Find
- Find μ, v and one-way transit time.
Approach: The uniform taut sample determines density. The pulse travels a one-way path.
Substitute the given values with matching units.
Take the square root of tension divided by linear density.
Divide stationary distance by speed.
Result: μ = 5.00 g/m, v = 120 m/s and transit time 12.5 ms.
Check: reproduces tension. checks the one-way path. An echo covering the same outward and return paths would require , twice as long.
Increase speed by a factor of 1.5
- Given
- μ = 0.00350 kg/m remains fixed in the model; initial tension 35.0 N; desired speed 150 m/s. The same source stays at f = 50 Hz.
- Find
- Find new tension and both wavelengths.
Approach: Keep density fixed but change tension: square the speed factor first.
Substitute the given values with matching units.
Insert desired speed into the rearranged equation.
Find wavelengths at the same frequency.
Result: New tension is arithmetically 78.75 N, a factor of 2.25; wavelength increases from 2 to 3 m.
Check: confirms the speed factor. Both wavelengths reproduce their speeds at . Source frequency is fixed here; natural frequencies of a string fixed at both ends would instead rise with speed.
Driving and natural frequencies play different roles
A travelling harmonic wave with supplied frequency has . The material model sets speed, while the source sets frequency. A length fixed at both ends instead has natural frequencies . Greater tension shifts these upwards if length and mass density stay unchanged. Source frequency and natural frequency are therefore different specifications.[2]
For an ideal flexible string fixed at both ends,
Not every driving frequency is a natural frequency. A real driven system also responds away from resonance, generally with different amplitude and phase. Boundaries, excitation position and losses determine that response; speed alone does not give resonance amplitude.
A standing wave on a string fixed at both ends adds boundary conditions to this propagation speed. Its discrete natural frequencies belong to the vibrating length; they replace neither a freely specified driving frequency nor the small-slope check.[2][1]
Explore further: measurement uncertainty and inference
A simple one-way measurement gives . An out-and-back echo instead covers . Timing zero must match launch of the disturbance; instrument delay is not an extra string path. Also check whether the reading identifies one clean pulse or several overlapping reflections. The third example shows the effect of a known delay explicitly.
Weigh a representative length of the actual string. A wound string cannot be described by a guessed core density; μ includes all moving mass per length. A heavy sensor or attached mass may change boundaries and reflect waves. Such additions cannot silently be absorbed into one uniform μ.
The wave relation for speed, wavelength and frequency gives for a travelling harmonic wave. A transit measurement instead tracks an identifiable pulse over its actual path. Phase and group speed agree in the ideal nondispersive string model; frequency alone cannot reconstruct unknown reflection paths.[5][1]
Flexibility, losses and dispersion limit the model
Real strings have bending stiffness. At short wavelengths its contribution can alter the tension-only model and cause dispersion. Large slopes, spatially varying tension, nonuniform linear density, and nonlinear extension also exceed alone. The simple result requires a nearly straight, taut, ideal flexible string undergoing small transverse motion.[1][3]
The ideal model is nondispersive: and phase and group speeds agree. Losses or real stiffness can alter pulse shape and mode spacing. With zero tension the taut-string assumption is lost; a formal zero speed does not replace a model of a slack cord.
A round-trip time determines tension
Inferring tension squares the speed. A modest timing error can therefore appreciably alter the inferred tension. This echo example separates instrument delay from actual travel time.[1][4]
A round-trip time determines tension
- Given
- A uniform taut string has length 2.00 m and mass 8.00 g. A small transverse pulse travels to the reflecting end and back. The instrument reads 45.0 ms, including an independently known 5.0 ms delay. Other paths and reflection delays are excluded in this ideal model.
- Find
- Calculate propagation speed and tension; assess the error if the delay is not removed.
Approach: first obtain actual travel time, then use the doubled path and taut-string mass density.
Substitute consistent SI units.
Without correction, a smaller speed and its square would be used.
Result: The model gives and . Omitting the correction would underestimate tension by approximately 20.99%.
Check: Check: and . The delay must be known independently; one travel-time reading cannot determine both tension and an unknown delay.
Five solved exercises
Calculate · Foundation
FT = 50 N and μ = 0.00200 kg/m. Find v.
Show hint
has units m2/s2.
Learning goal: Calculate speed from tension and line density.
Show solution and calculation
Approach: the positive square root gives speed magnitude.
.
Check: reproduces tension.
Rearrange · Application
A uniform 3.00 m sample has mass 9.00 g; measured speed is 80.0 m/s in the ideal model. Find FT.
Show hint
Calculate μ in kg/m first.
Learning goal: Infer tension using specimen mass.
Show solution and calculation
Approach: divide mass by taut length first, then infer tension from speed squared.
, .
Check: . Length refers to the measured taut state.
Transfer · Application
FT stays fixed while μ rises from 4 to 9 g/m. How does v change?
Show hint
Compare using the square root of a ratio.
Learning goal: Apply square-root scaling for changed density.
Show solution and calculation
Approach: constant tension cancels in the ratio.
.
Speed falls by one third; would incorrectly assume linear rather than square-root dependence.
Interpret · Application
A small transverse wave on an ideal string has FT=80 N and μ=0.005 kg/m. Marked material points move up and down. Does every point move along the string at propagation speed? Calculate that speed and explain the distinction.
Show hint
Wave speed tracks a phase feature rather than a material particle.
Learning goal: Distinguish transverse particle motion from propagation speed.
Show solution and calculation
Approach: The string model gives approximately 126.491 m/s for phase propagation.
Material points oscillate transversely with their own time-dependent velocities set by amplitude and frequency.
Tension and line density alone do not give that speed.
Rapid pattern propagation does not imply comparable longitudinal flow of string material.
Error analysis · Application
A sinusoidal wave has amplitude A=2 cm and wavelength 10 cm. Someone treats the linear string speed as exact because 2 cm looks small. Check maximum slope and assess the small-slope assumption.
Show hint
Compare amplitude to wavelength through kA, not to an arbitrary length.
Learning goal: Check small slope before applying linear wave speed.
Show solution and calculation
Approach: Maximum slope of a sine profile is wave number times amplitude.
Here it is about 1.25664, nowhere near much less than one.
The linear small-slope derivation is not justified; tension and geometry can change dynamically.
An apparently small centimetre value alone cannot justify exactness.
In brief
Sources for this explanation
Quanta · Updated October 2, 2026
- OpenStax UP1 §16.3: Wave Speed on a Stretched String
- OpenStax UP1 §16.6: Standing Waves and Resonance
- MIT OCW 8.03SC: phase/group velocity and dispersion
- OpenStax University Physics 1 §16.2: Pulses and wave functions
- OpenStax University Physics Volume 1 §16.1: Traveling Waves
- OpenStax University Physics Volume 1 §12.3: Stress, Strain, and Elastic Modulus
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This explanation, 3 worked examples and 5 exercises are available in German and English. Structure, source references and mathematical notation undergo automated checks. Calculations, model assumptions and both language versions receive a separate AI review.
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Editorial responsibility, sources and methodsChange history
- Distinguished tensile force from mechanical stress and added relevant wave connections; preserved all existing calculations, exercises, figures and model limits.
- Distinguished propagation from material motion; added echo inference with a known instrument delay and a tension–speed curve. Preserved previous calculations, model limits, and all five exercises.
- Added two exercises; labelled all five by task type, difficulty and learning goal.
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Quanta. Wave speed on a stretched string. Updated October 2, 2026. https://quanta-study.de/en/formula-sheet/wellengeschwindigkeit-saite
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