Published by Patrick Mutisya · 14 days ago
Know that for a longitudinal wave the direction of vibration is parallel to the direction of propagation and understand that sound waves and seismic P‑waves (primary waves) can be modelled as longitudinal.
The speed \$v\$ of a wave is related to its frequency \$f\$ and wavelength \$\lambda\$ by
\$v = f \lambda\$
For longitudinal waves in a gas, the speed of sound can be expressed as
\$v = \sqrt{\frac{\gamma\,R\,T}{M}}\$
where \$\gamma\$ is the adiabatic index, \$R\$ the universal gas constant, \$T\$ the absolute temperature, and \$M\$ the molar mass of the gas.
| Property | Transverse Wave | Longitudinal Wave |
|---|---|---|
| Particle displacement | Perpendicular to propagation | Parallel to propagation |
| Typical examples | Light, water surface waves, string vibrations | Sound in air, seismic P‑waves, compression waves in springs |
| Regions of disturbance | Crests and troughs | Compressions and rarefactions |
| Medium requirement | Can travel in solids, liquids, or gases (e.g., light is electromagnetic) | Requires a material medium (solid, liquid, or gas) |
When a source vibrates (e.g., a speaker diaphragm), it pushes adjacent air molecules together, creating a compression. The molecules then move apart, forming a rarefaction. This alternating pattern travels outward, while individual air molecules oscillate back and forth along the same line as the wave travels.
P‑waves are the fastest seismic waves generated by earthquakes. They propagate through the Earth’s interior by compressing and expanding the material in the direction of travel, exactly as a longitudinal wave does. Because they can move through solids, liquids, and gases, P‑waves are the first to be recorded by seismographs.