Oscillations are perpendicular to the direction of energy transfer
Longitudinal wave
Oscillations are parallel to the direction of energy transfer
Transverse waves
Electromagnetic waves
Seismic s-waves
Longitudinal waves
Sound waves
Seismic p-waves
Parts of a longitudinal wave
Compressions and rarefactions
Wave amplitude
Maximum displacement of a point on a wave from its undisturbed position
Wavelength
Distance from a point on a wave to the same position on the adjacent wave, most commonly peak to peak or trough to trough
Wave frequency
Number of waves that pass a given point each second
Unit of frequency
Hertz, Hz
A frequency of 200Hz means 200 waves pass a given point each second
Wave speed
Speed at which the wave moves or at which energy is transferred through a medium
A wave transfers energy
Calculating wave speed
1. Wave Speed = Frequency x Wavelength
2. Speed (m/s), Frequency (Hz), Wavelength (m)
Reflection
When a wave bounces off a surface
How sound waves travel through solids (Higher)
The particles in the solid vibrate and transfer kinetic energy through the material
Frequency range of human hearing (Higher)
20 Hz - 20kHz (1kHz = 1000 Hz)
Ultrasound waves (Higher)
Waves which have a frequency higher than the upper limit of human hearing (20kHz)
Uses of ultrasound waves (Higher)
Medical or industrial imaging
Seismic waves (Higher)
Produced by earthquakes, include both P-waves and S-waves
Difference between P-waves and S-waves (Higher)
waves travel through both solids and liquids, S-waves only travel through solids (not liquids)
Echo sounding (Higher)
Technique used to detect objects in deep water and measure water depth, using high frequency sound waves that are emitted, reflected and detected, with time difference and wave speed used to calculate distances