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Waves
Waves transfer energy without transferring matter. This is shown in the sea, where buoys stay still despite waves passing by them – the waves move, but not the particles
Wavelength
The distance between the same points on two consecutive waves
Amplitude
The distance from equilibrium line to the maximum displacement (crest or trough)
Frequency
The number of waves that pass a single point per second
Period
The time taken for a whole wave to completely pass a single point
Wavefront
The plane in which the wave travels (i.e. the direction of the wave)
velocity
frequency × wavelength = v = fλ
Wave speed
Wave speed (metre/second, m/s) = frequency (hertz, Hz) × wavelength (metre, m)
Relationships
Increase frequency, velocity increases; Wavelength increases, velocity increases; Period is inversely proportional to frequency; Smaller period, higher frequency, greater velocity
Transverse waves
Has peaks and troughs; Vibrations are at right angles to the direction of travel e.g. Light, seismic S waves, water waves
Longitudinal waves
Has compressions and rarefactions; Vibrations are in the same direction as the direction of travel e.g. Sound waves, seismic P waves
Refraction
If passing into a more optically denser medium the wave refracts at the boundary, changes direction bending towards the normal, speed decreases, wavelength decreases, frequency stays constant
Reflection
Waves reflect off a flat surface; Angle of incidence = angle of reflection; Light reflects if opaque object is not absorbed
Transmission
Waves pass through transparent material; More transparent more light passes through
Absorption
Light absorbed by electrons and not reemitted if matches energy levels; Absorbed frequencies converted to heat over time
Wavelength effects
Substances may absorb, transmit, refract or reflect waves depending on wavelength e.g. glass transmits visible light, reflects UV
Ultrasound
Sound wave >20 000Hz frequency used in sonar, foetal scanning
Infrasound
Sound wave <20Hz frequency used to explore Earth's core