Determining Wave Speed: To find the velocity of a wave, you must multiply its frequency in Hertz (Hz) by its wavelength in meters (m). This calculation is universal and applies to both light waves in space and sound waves in the atmosphere.
Relating Period and Frequency: The time period () is the duration of one complete cycle and is the mathematical reciprocal of the frequency (). When analyzing waves from a time-based graph, the period is the distance between peaks on the time axis.
Identifying Wave Types: You can identify a wave type by observing the relationship between the source vibration and the energy path. If a rope moves up and down while the wave travels forward, it is transverse; if a spring pulses back and forth in the direction of travel, it is longitudinal.
| Feature | Transverse Waves | Longitudinal Waves |
|---|---|---|
| Oscillation | Perpendicular to travel | Parallel to travel |
| Structure | Peaks and Troughs | Compressions and Rarefactions |
| Vacuum | Possible (EM waves) | Impossible (Mechanical) |
| Mediums | Solids/Liquid surfaces | Solids, Liquids, and Gases |
| Density | Stays constant | Varies locally |
Seismic Differences: In geology, S-waves (secondary) are transverse and cannot travel through liquid layers. P-waves (primary) are longitudinal and move faster, allowing them to pass through both solid and liquid internal structures.
Pressure and Density: Longitudinal waves create areas of high and low pressure, which is why they are often called pressure waves. Transverse waves primarily change the displacement of the medium without creating significant pressure gradients.
Check the Units: Always ensure that frequency is in Hertz (Hz) and wavelength is in meters (m) before using the wave equation. A common mistake is using centimeters for wavelength, which leads to an incorrect speed in m/s unless converted.
Directional Logic: When asked to draw the motion of a particle, look for the direction of energy transfer first. For transverse waves, draw arrows at ; for longitudinal, draw them horizontally along the same line as the wave.
Doppler Nuances: Remember that the Doppler effect is an apparent change in frequency, not an actual change in the source's output. The source continues to emit waves at a constant frequency, but the relative motion causes the observer to perceive a shift.
Memorize Examples: Examiners frequently ask for lists of examples. Keep 'Sound' and 'P-waves' in your longitudinal list, and 'EM waves', 'Water ripples', and 'Guitar strings' in your transverse list.
Matter vs. Energy: A common error is believing that the medium moves with the wave. In reality, particles only oscillate about a fixed position; if the matter moved with the wave, a sound wave would create a constant wind as it traveled.
Vacuum Propagation: Students often forget that sound cannot travel through a vacuum. Because longitudinal waves require particle compressions, the absence of particles in space prevents sound from being heard, unlike light waves.
Wavelength Measurement: Ensure you measure wavelength from the center of one compression to the center of the next for longitudinal waves. Measuring from the start of one to the end of the same compression only gives the width of the compressed region.