Skip to content
Marlbridge

Revision Notes

Cambridge O Level Physics: Waves (5054) – Revision Notes

Condensed revision notes on Waves for Cambridge O Level Physics 5054: definitions, equations, light, sound, the EM spectrum, a self-test and common lost marks.

Subject
Physics
Level
O LEVELS
Topic
Waves
Updated

Aligned to Cambridge O Level Physics (5054), 2026-2028. Official specification .

Syllabus page (what it covers and how it is assessed): Cambridge O Level Physics.

Syllabus points this page covers

5054

  • 3.1 General properties of waves
  • 3.2 Light
  • 3.3 Electromagnetic spectrum
  • 3.4 Sound

Found an error? Report a correction.

Need help with this topic? Request a free trial class for O Level Physics (5054).

Short notes on topic 3, Waves, from the Cambridge O Level Physics 5054 syllabus (examined 2026 to 2028), covering sections 3.1 to 3.4. The study guide has the longer explanations and worked examples. Once the self-test below goes well, try the practice questions. Also useful: the Physics course hub, a printable checklist and our free diagnostics.

Equations

Quantity Equation Notes
Wave speed v = fλ Use m/s, Hz and m
Period T = 1/f T in s
Refractive index n = sin i / sin r i in the air, r in the material, both from the normal
Critical angle n = 1 / sin c Rearrange: sin c = 1/n
Linear magnification image length / object length No unit
Echo or sonar distance = v × t / 2 Halve: the pulse goes there and back
Speed of sound by echo v = 2d / t d is the distance to the reflector

3.1 General properties of waves

Definitions to recite.

  • Waves transfer energy without transferring matter.
  • Frequency: the number of wavelengths that pass a point per unit time (Hz).
  • Wavelength: the distance between two consecutive, identical points, such as two consecutive crests.
  • Amplitude: the maximum distance from the mean position.
  • Wavefront: a line joining points at the same stage of vibration.
  • Crest (peak) and trough: highest and lowest points of a transverse wave.
Transverse Longitudinal
Vibration at right angles to the direction of energy transfer Vibration parallel to the direction of energy transfer
Electromagnetic radiation, surface water waves, seismic S-waves (secondary) Sound waves, seismic P-waves (primary)
Crests and troughs Compressions and rarefactions

Wave motion: shaking a rope or spring sends a pulse along it, and each part only vibrates about its rest position. Ripples in water show the same: a floating object bobs and stays put.

Three wave behaviours.

  • Reflection at a plane surface: the wave bounces back.
  • Refraction: a change of direction caused by a change of speed. The frequency stays fixed, so the wavelength changes too.
  • Diffraction through a gap: spreading out. Most when the gap is about one wavelength. Less when the gap is much wider than the wavelength. A longer wavelength spreads more. At an edge a longer wavelength also bends round more.

Ripple tank, one line each.

  • Reflection: a straight barrier turns the wavefronts back.
  • Refraction: shallow water slows the waves, shortens the wavelength and changes direction.
  • Gap: a narrow gap spreads the wavefronts into circles.
  • Edge: the wavefronts curve round the end of a barrier.

Method: v = fλ.

  1. Write down the two known quantities with units.
  2. Convert units first (cm to m, kHz to Hz).
  3. Rearrange: v = fλ, f = v/λ, λ = v/f.
  4. Give the unit.
Top view of a ripple tank at 10 Hz. Wavefronts cross from deep water (wavelength 3.0 cm, speed 0.30 m/s) to a shallow plate (1.2 cm, 0.12 m/s). The wavefronts bunch up and the ray turns towards the normal from 40 degrees to 14.9 degrees.
Over the plate the wave is slower and its wavelength shorter, at the same frequency.
Two side views of ripples a quarter period apart. The crest moves right by a quarter wavelength but a floating cork stays at the same horizontal position and only moves up and down.
The wave moves along but the water only vibrates.
A sine graph of displacement against distance marks wavelength between two crests (0.40 m) and amplitude from rest position to crest. With f = 5 Hz, v = f x wavelength = 2.0 m/s and the period is 0.2 s.
Wavelength is crest to crest; amplitude is from the middle to a crest; v = f x wavelength.
A rope wave moves points up and down at right angles to travel (transverse). A spring wave moves coils back and forth along the direction of travel (longitudinal), bunching into compressions and spreading into rarefactions (Extended names).
Transverse waves vibrate at right angles to the direction of travel; longitudinal waves vibrate along it.
Two cross-sections of the Earth with an earthquake at the top. S-waves travel in straight lines through the mantle but stop at the liquid core, leaving a shadow zone on the far side where no S-waves arrive. P-waves pass through the core and change direction at its boundary.
S-waves cannot cross the liquid core, but P-waves can, which is evidence that part of the core is liquid.

3.2 Light

Reflection

  • The normal is at right angles to the surface. Angles of incidence and reflection are measured from it.
  • Law of reflection: the two angles are equal.
  • Plane mirror image: matches the object in size, sits behind the mirror at the object’s distance in front, and is virtual.
  • Experiment: ray box, mirror, paper. Mark the ray, join the points, measure from the normal, repeat.
  • Image position: pins in line with the image from two directions. The lines cross at the image.
Top view of a ripple tank. Straight wavefronts reflect from a straight barrier and leave at the same 30 degrees on the other side. In a second panel the wavefronts curve round the edge of a barrier into the shadow region.
In a ripple tank a straight barrier returns wavefronts at equal angles, and waves bend round an edge into the shadow.
Top view of wavefronts meeting a barrier with a gap. With a gap of five wavelengths the wavefronts stay mostly straight and bend only at the edges. With a gap of one wavelength they spread as nearly circular arcs. Diffraction is appreciable only when wavelength and gap are comparable.
A gap about one wavelength wide spreads waves strongly; a wide gap hardly does.
Three rays in a glass semicircle: below the critical angle some light leaves, at 41.8 degrees the refracted ray runs along the surface, above it all light is reflected. sin c = 1/n (Extended).
Above the critical angle all the light is reflected back inside the glass.

Refraction

  • Slower medium: ray bends towards the normal. Faster medium: away from the normal.
  • Light through a rectangular block emerges parallel to its original path, shifted sideways. A triangular prism bends the ray towards its base.
  • Experiments: trace the ray through a block on paper at several angles. For internal reflection, aim a ray at the flat face of a semicircular block through the curved face and raise the angle until the refracted ray runs along the face (angle c), then beyond it.
  • Total internal reflection needs both: light travelling in the more dense medium towards the less dense, and i greater than c.
  • At i equal to c, the refracted ray travels along the boundary.
  • Optical fibres use total internal reflection. Used in telecommunications. Advantages: carry a large amount of information and avoid electrical interference. Use these as points, then add the context asked in the question.

Method: refractive index.

  1. Is the ray going into the material (use n = sin i / sin r) or out (use n = sin r / sin i with r now in air)?
  2. Put both angles measured from the normal.
  3. Take sin, divide, then take the inverse sin.
  4. Check: entering a denser medium, r is smaller than i.

Thin lenses

  • Converging lens: parallel beam brought to the principal focus. Diverging lens: parallel beam spreads out.
  • Focal length: lens centre to principal focus. Principal axis: line through the lens centre at right angles to it.
  • Ray diagram: one ray parallel to the axis, through the focus after the lens; one ray through the centre, straight on.
Converging lens, object at Image
More than 2F away Inverted, real, diminished
Between F and 2F Inverted, real, magnified
Less than F away (magnifying glass) Upright, virtual, magnified

A diverging lens always gives a virtual, upright, smaller image.

  • Real image: formed by converging rays. Virtual image: formed by diverging rays.
  • Eye diagrams: a normal eye brings parallel rays to a focus on the retina. In short sight they focus in front of the retina, so a diverging lens spreads them first. In long sight the focus lies behind the retina, so a converging lens is used.
Ray diagram for a converging lens with f = 4 cm. A 2 cm object 6 cm from the lens gives a real, inverted image 4 cm tall 12 cm beyond the lens, magnified by 2.0.
An object between F and 2F gives a real, inverted, magnified image.
Parallel rays meet at the principal focus after a converging lens. After a diverging lens they spread out and appear to come from a principal focus on the incoming side.
A converging lens brings parallel rays to a focus; a diverging lens spreads them as if from a focus.
To-scale ray diagram with f = 120 and object at 300: image forms at 200, real, inverted and diminished.
An object beyond 2F gives a real, inverted, diminished image.
Ray diagram for a convex lens with the object inside the principal focus. The two refracted rays spread out and never meet; dotted lines traced backwards meet 7.5 cm from the lens on the same side as the object, giving a virtual, upright image 5 cm tall, which is 2.5 times larger than the 2 cm object.
Inside the principal focus a convex lens gives a larger, upright, virtual image.
Ray diagram for a concave lens. A ray parallel to the axis bends away from the axis, appearing to come from the principal focus on the object side; the ray through the centre is undeviated. The refracted rays never cross, but dotted lines traced back meet 4 cm from the lens on the object side, giving a virtual, upright image 1 cm tall (one third of the object).
A concave lens only ever makes a virtual, upright, smaller image.
Four schematic eyes in two rows. Long sight: rays from a near object focus behind the retina, and a convex lens in front of the eye brings them to a focus on the retina. Short sight: parallel rays from a distant object focus in front of the retina, and a concave lens in front of the eye moves the focus back onto the retina.
A convex lens corrects long sight and a concave lens corrects short sight.

Dispersion

A prism refracts violet most and red least. Frequency increases: red, orange, yellow, green, blue, indigo, violet. Wavelength increases the other way.

A ray reflects from a mirror with i and r both 55 degrees measured from the normal, with two marked points on the reflected ray. A second panel shows pins lined up with the image of an object pin; the lines drawn back behind the mirror cross at the image, the same distance behind as the object is in front.
Both mirror practicals: measure i and r from the normal, and find the image where lines from the pins cross behind the mirror.
Three views of a ray aimed at the centre of a semicircular block (n = 1.6) at 25 degrees, 38.7 degrees and 55 degrees. At 25 degrees the ray refracts out, at the critical angle it runs along the flat face, and at 55 degrees it is totally internally reflected.
Increase the angle and the refracted ray bends away until it runs along the face at the critical angle, then only reflection remains.
A ray hits a plane mirror at 35 degrees to the normal and reflects at 35 degrees on the other side. The 55 degree angle to the mirror surface is marked as the common wrong measurement.
Angle of incidence equals angle of reflection, both measured from the normal.
An upright object O is 3.5 m from a vertical plane mirror. Two rays from its base reflect so that angle of incidence equals angle of reflection (36.9 and 24.2 degrees), measured from dashed normals. Dashed extensions behind the mirror meet at the image I, 3.5 m behind the mirror: virtual, upright and the same size.
Two rays from O reflect with i = r and their backward extensions meet at the virtual image I, as far behind the mirror as O is in front.
A ray at 45 degrees in air bends towards the normal to 28 degrees in glass (n = 1.5) and leaves parallel, bending away. n = sin i / sin r = 1.50 (Extended).
Light slows and bends towards the normal entering glass, and speeds up and bends away leaving it.
Wavefronts meet an air-glass boundary at 45 degrees. In air (3.00e8 m/s) they are 545 nm apart; in glass (2.00e8 m/s) 364 nm apart, with the same frequency 5.50e14 Hz. The end entering first slows first, so the ray bends towards the normal to 28.1 degrees. n = 3.00/2.00 = 1.50.
Wavefronts bunch closer in the slower medium, so the ray pivots towards the normal while frequency stays fixed.
A ray in a fibre of n = 1.48 meets the wall at 60 degrees, above the 42.5 degree critical angle, and is totally internally reflected again and again. Uses are endoscopes and communications. A 2.0 km fibre gives a transit time of 9.9 microseconds.
Light zigzags along a fibre by total internal reflection because it meets the wall above the critical angle.
White light enters a glass prism and is refracted at both faces. Red is bent least and violet most, in the order red, orange, yellow, green, blue, indigo, violet. The spread is exaggerated for clarity.
White light splits into a spectrum because violet is bent more than red.

3.3 Electromagnetic spectrum

Increasing frequency, decreasing wavelength: radio waves, microwaves, infrared, visible light, ultraviolet, X-rays, gamma rays. Speed: 3.0 × 10⁸ m/s in a vacuum and about the same in air.

Region Uses to learn
Radio Radio and television, astronomy
Microwave Satellite television, mobile phones, Bluetooth, ovens
Infrared Appliances, remote controllers, intruder alarms, thermal imaging, optical fibres
Visible Photography, vision
Ultraviolet Security marking, counterfeit notes, sterilising water
X-rays Medical imaging, security scanners, killing cancer cells, cracks in metal
Gamma Treating cancer, sterilising food and equipment, cracks in metal

Dangers. Excess exposure heats soft tissue and burns. Ionising radiation: ultraviolet (skin cancer, cataracts); X-rays and gamma rays (cell mutation, cancer).

Seven bands from radio to gamma with their uses. Microwaves and infrared heat tissue and can burn; ultraviolet, X-rays and gamma rays are ionising and can cause cancer or cell mutation.
Each band has its own uses; microwaves and infrared heat, while ultraviolet, X-rays and gamma rays are ionising.
Seven regions from radio to gamma, each with a wave of shorter wavelength than the one above (illustrative) and one use. All travel at 3.0 x 10^8 m/s in a vacuum (Extended).
Frequency rises and wavelength falls from radio waves to gamma rays.

3.4 Sound

  • Made by vibrating sources. Longitudinal, with compressions and rarefactions.
  • Audible range for humans: 20 Hz to 20 000 Hz.
  • Cannot travel in a vacuum because there are no particles to pass on the vibration. Demonstration: bell in an evacuated jar.
  • Amplitude gives loudness. Frequency gives pitch.
  • Timbre: the oscilloscope trace shape differs between sources even at the same pitch and loudness.
  • Echo: reflection of sound. Show by directing sound at a hard board and detecting reflection.
  • Speed in air: approximately 330 to 350 m/s. Solids faster than liquids, liquids faster than gases.
  • Ultrasound: frequency above 20 kHz. Uses: cleaning, prenatal and other medical scanning, sonar.

Method: speed of sound in air. Measure the distance to a wall with a long tape. Clap and time the echo with a stopwatch. v = 2d/t. Repeat and average.

Method: echo or sonar depth. Distance travelled = v × t. Divide by 2 for the one-way distance.

Two bell jars each with a bell. With air in the jar sound spreads out and is heard. With the air pumped out the hammer still strikes but no sound is heard, because sound needs particles.
Pump the air out of the jar and the bell is still seen ringing but can no longer be heard.

Must-know distinctions

  • Loudness is amplitude; pitch is frequency.
  • Refraction changes speed and wavelength; frequency stays the same.
  • Real image: can be caught on a screen. Virtual image: cannot.
  • Critical angle belongs to the dense-to-less-dense direction; it does not exist going the other way.
  • Ionising: ultraviolet, X-rays, gamma rays. Heating effect: microwaves and infrared.

Quick self-test

  1. Water waves have a frequency of 12 Hz and a wavelength of 0.25 m. Find the speed.
  2. A note has a frequency of 250 Hz. Find the period.
  3. A ray in air strikes glass (n = 1.5), making 30° with the normal. Find the angle of refraction.
  4. A microwave has a wavelength of 0.12 m. Find its frequency, using 3.0 × 10⁸ m/s.
  5. An image is 9.0 cm tall and the object is 2.0 cm tall. Find the magnification.
  6. A sonar pulse returns after 0.40 s. The speed in water is 1500 m/s. Find the depth.
  7. A ray goes from air into a plastic. The angle of incidence is 60° and the angle of refraction is 35°. Find n.
  8. A ray makes 62° with a plane mirror. Find the angle of reflection.
  9. Calculate the critical angle of a glass with n = 1.5.
  10. Sound at 170 Hz travels at 340 m/s. Find the wavelength.
  11. State why sound cannot pass through a vacuum.
  12. Give the property of a sound wave that sets its pitch.

Answers

  1. v = fλ = 12 × 0.25 = 3.0 m/s.
  2. T = 1/250 = 0.004 s.
  3. sin r = sin 30° / 1.5 = 0.333, so r = 19.5°.
  4. f = v/λ = 3.0 × 10⁸ / 0.12 = 2.5 × 10⁹ Hz.
  5. 9.0 / 2.0 = 4.5.
  6. 1500 × 0.40 / 2 = 300 m.
  7. n = sin 60° / sin 35° = 1.51.
  8. Angle of incidence = 90 − 62 = 28°, so the angle of reflection is 28°.
  9. sin c = 1/n = 0.667, giving c = 41.8°.
  10. λ = 340 / 170 = 2.0 m.
  11. There are no particles to vibrate and pass the energy on.
  12. The frequency.

Where marks are usually lost

  • Using the surface rather than the normal as the line to measure angles from.
  • Leaving out the halving step in echo and sonar questions.
  • Quoting frequency, wavelength or speed without converting kHz, MHz or cm first.
  • Writing that sound “goes faster in air than in water”.
  • Describing the longitudinal wave as “up and down”.
  • Stating total internal reflection without both conditions.
  • Mixing up the order of the electromagnetic spectrum with the order of colours in dispersion.
  • Saying a virtual image is “not there” instead of saying the rays only appear to come from it.

Frequently asked questions

What is the difference between loudness and pitch? Loudness depends on the amplitude of a sound wave, and pitch depends on its frequency.

What is the difference between a real and a virtual image? A real image can be caught on a screen. A virtual image cannot, because the rays only appear to come from it.

Which parts of the electromagnetic spectrum are ionising? Ultraviolet, X-rays and gamma rays are ionising, while microwaves and infrared mainly have a heating effect.

Does sound travel faster in air or in water? Sound travels faster in water than in air. Writing that sound goes faster in air than in water is a common error.

Official syllabus

Source: topic 3, Waves, of the Cambridge International Education O Level Physics 5054 syllabus for 2026 to 2028.

Get free revision emails (optional)

Occasional emails with practice questions, worked explanations and links to free resources for the qualification and subjects you choose. No spam, and you can unsubscribe from any email. The free tools on this site never need an email.

Subjects (optional, up to 6)

Choose a qualification to see its subjects.

Related resources

Related articles

Studying this with a teacher

Working through Physics O LEVELS?

This page is free and stays free. If you would rather be taught it, Marlbridge runs Physics classes one-to-one and in small groups of up to 15, online in your own time zone. The first trial class is free. WhatsApp replies within an hour (8am–11pm Pakistan time, every day); email the same day.