Sine Waves
Shake the end in SHM and every point copies it, a little later.
Lesson at a glanceShow the key points
- If the end moves as A sin ωt, the wave is y = A sin ω(t − x/v) (15.6): every particle performs SHM of amplitude A and frequency ν, with a phase lag ωx/v.
- Particle velocity ∂y/∂t = Aω cos ω(t − x/v) (15.7) is completely different from the constant wave velocity v.
- Wavelength λ = vT (15.8): the smallest separation of particles in the same phase; v = νλ (15.9); wave number k = 2π/λ.
- Crests (positive displacement) and troughs (negative) are λ apart.
- Equivalent forms: A sin(ωt − kx), A sin 2π(t/T − x/λ), A sin k(vt − x); a phase constant φ can be added (15.13).
Keep moving the end of the string up and down in simple harmonic motion and the whole string comes alive with a sine wave, the shape behind almost every wave in physics.
From a shaking end to a sine wave
If the end x = 0 performs SHM, (15.5), with period T = 2π/ω and frequency ν = 1/T, the wave that travels out is
Every particle of the string performs SHM with the same amplitude and frequency, but each copies the motion of a particle to its left after a delay x/v. When one particle reaches its top, a particle just ahead is still rising and one just behind is already coming down.
The velocity of the particle at x (x held fixed, so a partial derivative) is
Wavelength, frequency and speed
A particle a distance vT further along copies the first after a delay of exactly one period, which makes no difference: they move in perfect step (same phase). This separation is the wavelength.
Other ways to write it
These all assume t = 0 when the end crosses its mean position going up. A different choice of t = 0 adds a phase constant: (15.13). With φ = π/2 (end at its top at t = 0) this becomes ; with φ = π, (15.15).
A wave on a string is y = (3.0 mm) sin[(2.0 cm⁻¹)x − (40 s⁻¹)t]. Find its amplitude, wave number, wavelength, frequency, period and speed, and the greatest speed of a particle.
- 1: every particle does SHM, each lagging the one before.
- 2Particle velocity ∂y/∂t ≠ wave velocity v.
- 3, , , , so .
- 4Equivalent forms A sin(ωt − kx), A sin 2π(t/T − x/λ); a phase constant depends on the choice of t = 0.
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