Direction of Oscillation: In a longitudinal wave, the particles of the medium oscillate back and forth parallel to the direction of energy transfer.
Structural Features: These waves are characterized by compressions (regions where particles are close together, resulting in high pressure) and rarefactions (regions where particles are spread apart, resulting in low pressure).
Polarization: Longitudinal waves cannot be polarized because their oscillation is already restricted to the same axis as the wave's travel.
Examples: Sound waves in air, ultrasound, and primary (P) seismic waves are classic examples of longitudinal waves.
Displacement (): The distance and direction of a particle from its equilibrium position at any given time.
Amplitude (): The maximum displacement of a particle from its equilibrium position; it is directly related to the energy carried by the wave.
Wavelength (): The distance between two consecutive points that are in phase, such as from crest to crest or compression to compression.
Frequency (): The number of complete oscillations passing a fixed point per unit time, measured in Hertz ().
Period (): The time taken for one complete cycle of the wave to pass a point, related to frequency by .
Wave Speed (): The speed at which energy is transmitted through the medium, calculated using the fundamental wave equation:
The Wave Equation:
| Feature | Transverse Waves | Longitudinal Waves |
|---|---|---|
| Oscillation Direction | Perpendicular to energy transfer | Parallel to energy transfer |
| Components | Crests and Troughs | Compressions and Rarefactions |
| Polarization | Can be polarized | Cannot be polarized |
| Medium | Can travel in solids and vacuum (EM) | Requires a medium (solids, liquids, gases) |
| Example | Light, Radio, String vibrations | Sound, Ultrasound, Slinky pulses |
Graph Interpretation: Be careful when reading displacement-time vs. displacement-distance graphs. A displacement-time graph for a single point looks identical for both transverse and longitudinal waves; you must check the description of particle motion to distinguish them.
Phase Identification: Points are 'in phase' if they are at the same stage of their cycle (e.g., both at a crest). The distance between any two adjacent points in phase is exactly one wavelength ().
Units Check: Always ensure frequency is in and wavelength is in meters () before calculating wave speed in . Common traps include giving frequency in or wavelength in .
Polarization as a Test: If a question asks how to prove a wave is transverse, the answer is usually to demonstrate that it can be polarized.