The relationship between the speed of the wave (), its frequency (), and its wavelength () is governed by the Wave Equation: . This implies that for a wave traveling at a constant speed, frequency and wavelength are inversely proportional.
Frequency () is the number of complete oscillations that pass a point per second, measured in Hertz (Hz). It is the reciprocal of the Period (), which is the time taken for one complete cycle: .
When performing calculations, it is vital to ensure all units are in the SI standard (meters, seconds, Hertz) to avoid errors, especially when dealing with prefixes like micro () or mega (M).
The most critical distinction between wave types is the direction of oscillation. While transverse waves oscillate perpendicularly, longitudinal waves oscillate parallel to the direction of travel.
| Feature | Transverse Waves | Longitudinal Waves |
|---|---|---|
| Oscillation | Perpendicular to travel | Parallel to travel |
| Structure | Crests and Troughs | Compressions and Rarefactions |
| Polarization | Can be polarized | Cannot be polarized |
| Examples | Light, S-waves, Radio | Sound, P-waves, Ultrasound |
Polarization is a unique property of transverse waves. Because they oscillate in a plane perpendicular to travel, their vibrations can be restricted to a single plane (polarized), whereas longitudinal waves, oscillating along the line of travel, have no 'side-to-side' component to restrict.
Transverse waves are typically represented using two types of graphs: Displacement-Distance and Displacement-Time. While both appear sinusoidal, they provide different physical information.
A Displacement-Distance graph acts like a 'snapshot' in time. The distance between two peaks on this graph represents the physical wavelength () of the wave.
A Displacement-Time graph tracks a single point as the wave passes. The time interval between two peaks on this graph represents the time period (), from which frequency can be calculated.
Identify the Axis: Always check the x-axis of a wave graph before extracting values. If the axis is 'Distance', you are finding wavelength; if it is 'Time', you are finding the period. Confusing these is a very common source of lost marks.
Equilibrium Reference: When measuring amplitude, ensure you measure from the center line (equilibrium) to the peak, NOT from the trough to the peak. Measuring trough-to-peak gives you twice the amplitude.
Unit Conversions: Physics problems often provide frequency in kHz or MHz and time in ms or s. Always convert these to base units (, , , ) before using the wave equation.