Mechanical Wave Generation

Interactive exploration of how mechanical waves are generated and propagated

Transverse Wave Generation

Vibration perpendicular to propagation direction

Wave Source (Hand) Wave Propagation → Particle Vibration ↑↓

Transverse Wave Formula

y = A·sin(kx - ωt)

Particles vibrate perpendicular to wave direction

Characteristics

  • Crests and Troughs
  • Particle motion ⊥ wave propagation
  • Examples: Rope waves, water waves

Longitudinal Wave Generation

Vibration parallel to propagation direction

Wave Source (Hand) Wave Propagation → Compression ↔ Rarefaction

Longitudinal Wave Formula

y = A·sin(kx - ωt) (displacement in x-direction)

Particles vibrate parallel to wave direction

Characteristics

  • Compressions and Rarefactions
  • Particle motion ∥ wave propagation
  • Examples: Sound waves, spring waves

Wave Parameters Control

Controls vibration speed of wave source
Controls maximum displacement of particles
Controls how fast the wave pattern propagates
Slow motion to observe wave details

Real-time Wave Parameters

Frequency (f) 1.0 Hz
Period (T = 1/f) 1.00 s
Wavelength (λ = v/f) 100 px
Angular Frequency (ω = 2πf) 6.28 rad/s
Wave Number (k = 2π/λ) 0.063 rad/px
Wave Speed (v = ω/k) 100 px/s

Understanding Mechanical Waves

Wave Generation

Mechanical waves require a source of vibration (like a moving hand) and a medium to propagate through (like rope or spring). The source creates periodic disturbances that travel through the medium.

Particle Motion vs Wave Motion

Particles in the medium only vibrate about their equilibrium positions; they do not travel with the wave. The wave pattern travels, but particles stay in place!

Types of Mechanical Waves

Transverse waves: particles vibrate perpendicular to wave direction (ropes, water surface). Longitudinal waves: particles vibrate parallel to wave direction (sound, springs).

Wave Parameters

Frequency (f): vibrations per second. Amplitude (A): maximum displacement. Wavelength (λ): distance between identical points. Wave speed (v): how fast the pattern moves (v = λ·f).

Energy Transfer

Waves transfer energy from one place to another without transferring matter. The vibrating source transfers energy to neighboring particles, which then transfer it further.

Real-world Applications

Sound waves (longitudinal) for communication, seismic waves for earthquake detection, ocean waves for surfing, string instruments for music production, and ultrasound for medical imaging.

Transverse vs Longitudinal Waves

Characteristic Transverse Wave Longitudinal Wave
Particle Direction Perpendicular to wave Parallel to wave
Wave Features Crests & Troughs Compressions & Rarefactions
Examples Rope waves, water waves, light Sound waves, spring waves
Propagation Medium Solids, liquid surface Solids, liquids, gases

Key Insights

🌊

Waves Transfer Energy, Not Matter

The wave pattern moves across the medium, but individual particles only vibrate in place. Watch the marked particle to see this clearly!

🔄

Source Frequency = Wave Frequency

The frequency at which the source vibrates determines the frequency of the entire wave. Change the source vibration rate, and the whole wave pattern changes accordingly.

Wave Speed Depends on Medium

The speed of wave propagation is determined by the properties of the medium (tension, density, elasticity), not by how fast the source vibrates.

📐

Wavelength Changes with Frequency

When frequency increases, wavelength decreases (λ = v/f). Higher frequency waves are more closely spaced, while lower frequency waves are more spread out.