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Physics (AS & A Level) 9702 · Chapter 7

Waves

Wave terms, using a CRO, v = f lambda, intensity, transverse and longitudinal waves, the Doppler effect for a moving source, the electromagnetic spectrum, and polarisation with Malus's law.

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7.1 Progressive waves

A progressive wave transfers energy from one place to another without transferring matter. You can see this on ropes, on springs and on water in a ripple tank.

Wave terms

TermMeaning
Displacement xxdistance of a point from its rest position
Amplitude AAmaximum displacement
Wavelength λ\lambdadistance between neighbouring points in phase, such as crest to crest
Period TTtime for one complete oscillation
Frequency ffnumber of oscillations per unit time, f=1/Tf = 1/T
Speed vvdistance a wavefront travels per unit time
Phase differencehow far one oscillation is ahead of another, in degrees or radians. One whole wavelength is 360° or 2π2\pi rad

Using a CRO

A cathode-ray oscilloscope displays voltage against time.

  • The time-base setting (such as 2 ms/div) is the time per horizontal division. Measure the divisions for one cycle, multiply, and that is the period. Then f=1/Tf = 1/T.
  • The y-gain setting (such as 5 V/div) is the voltage per vertical division. Amplitude is the divisions from the centre to a peak, multiplied by the y-gain.

The wave equation

In one period TT, a wave travels one wavelength. So v=λ/Tv = \lambda/T, and since f=1/Tf = 1/T:

v=fλv = f\lambda

Intensity

Intensity is the power per unit area, at right angles to the direction of travel, I=P/AI = P/A, measured in W m⁻². For a progressive wave:

I∝A2I \propto A^2

Doubling the amplitude makes the intensity four times as large. From a point source spreading out equally, I=P/(4πr2)I = P/(4\pi r^2).

7.2 Transverse and longitudinal waves

TransverseLongitudinal
Oscillationsat right angles to the direction of energy transferparallel to the direction of energy transfer
Exampleslight, water ripples, waves on a ropesound, a pushed slinky
Featurescrests and troughscompressions and rarefactions
Can be polarised?yesno

A transverse wave with wavelength and amplitude marked, and a longitudinal wave with compressions and rarefactions

A transverse wave with wavelength and amplitude marked, and a longitudinal wave with compressions and rarefactions

Reading wave graphs

Two graphs look alike, and you must check the axis:

  • Displacement against distance is a snapshot of the wave. It gives the wavelength.
  • Displacement against time shows one point as time passes. It gives the period.

For a longitudinal wave, a graph of displacement against distance is still a sine curve, even though the particles move along the wave's direction. Compressions are where neighbouring particles move towards a point.

7.3 Doppler effect for sound waves

When a source of sound moves relative to a stationary observer, the observed frequency differs from the frequency the source emits. Coming towards you, the wavefronts are bunched up, so you hear a higher frequency. Going away, they are spread out, so you hear a lower one.

fo=fs vv±vsf_o = \frac{f_s\, v}{v \pm v_s}

where vv is the speed of sound and vsv_s is the speed of the source. Use minus when the source approaches (the observed frequency goes up) and plus when it recedes.

7.4 Electromagnetic spectrum

All electromagnetic waves are transverse and travel at the same speed in free space, c=3.00×108c = 3.00 \times 10^{8} m/s.

RegionApproximate wavelength range
Radio wavesabove 0.1 m (can be 10⁶ m)
Microwaves10−310^{-3} m to 0.1 m
Infrared7×10−77 \times 10^{-7} m to 10−310^{-3} m
Visible light400 nm to 700 nm
Ultraviolet10−810^{-8} m to 4×10−74 \times 10^{-7} m
X-rays10−1310^{-13} m to 10−810^{-8} m
Gamma raysbelow 10−1110^{-11} m

The X-ray and gamma-ray ranges overlap because they are named by how they are made, not just their wavelength.

7.5 Polarisation

Polarisation can only happen to transverse waves. In a plane-polarised wave, the oscillations are all in one plane that contains the direction of travel. Unpolarised light has oscillations in many planes.

A polarising filter only transmits the component of the oscillations along its transmission axis. So the amplitude after the filter is A0cos⁡θA_0\cos\theta. Since intensity depends on amplitude squared:

I=I0cos⁡2θI = I_0\cos^2\theta

This is Malus's law, where θ\theta is the angle between the wave's plane of polarisation and the transmission axis.

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