3.2.2 Refraction of light
- Syllabus
- 0625–2026–2027
- Topic
- 3.2.2
- Level
- —
At the point where a ray meets a boundary, the normal is an imaginary line drawn at right angles to the boundary.
| Term | Meaning |
|---|---|
| incident ray | ray travelling towards the boundary |
| refracted ray | transmitted ray travelling in the second region |
| angle of incidence, i | angle between the incident ray and the normal |
| angle of refraction, r | angle between the refracted ray and the normal |
Draw the normal through the exact point of incidence and place the centre of a protractor there. Measure i in the first region and r in the second region, both from the normal.
If the incident ray makes 50∘ with the boundary, then i=90∘−50∘=40∘.
An angle drawn against the boundary is not i or r; it is the complement of the corresponding angle to the normal.
A narrow ray and a traced transparent block make the change of direction at each boundary measurable.
| Step | Method |
|---|---|
| 1 | place a rectangular, triangular or semicircular transparent block on plain paper and trace its outline |
| 2 | direct one narrow ray from a ray box at a chosen face and mark two points on the incident path and two on the emergent path |
| 3 | remove the block, join the marked points with a ruler and reconstruct the path through the outline |
| 4 | draw a normal at every boundary crossing and measure the angles from each normal |
| 5 | repeat with a different incidence angle and with blocks of different shapes |
The ray bends towards the normal when it enters a region in which it travels more slowly and away from the normal when it enters one in which it travels faster. A ray entering along the normal does not change direction. A parallel-sided block gives an emergent ray parallel to the incident ray but shifted sideways; a non-parallel face can change the final direction.
Changing the block shape changes the orientation of its boundaries; it does not by itself change the refractive behaviour of the material. Keep the ray narrow and mark points far enough apart for accurate ruler lines.
Refraction is a change in wave direction caused by a change in wave speed at a boundary between two regions.
| Passage across the boundary | Ray direction | Other wave properties |
|---|---|---|
| into a region where light travels more slowly | bends towards the normal, so r<i | frequency stays constant; wavelength decreases |
| into a region where light travels faster | bends away from the normal, so r>i | frequency stays constant; wavelength increases |
| along the normal, i=0∘ | does not bend | speed and wavelength may still change |
At the first face of a parallel-sided block the ray bends towards the normal; at the second, parallel face it bends away by the matching amount. The emerging ray is parallel to the incident ray but laterally displaced.
The ray bends at the boundary, not gradually throughout a uniform material. Frequency is fixed by the source and does not change when the ray crosses the boundary.
The critical angle c is the angle of incidence in the region where light travels more slowly for which the refracted ray in the faster region is at 90∘ to the normal.
At i=c, the refracted ray travels along the boundary. The critical angle is measured from the normal inside the slower region, not from the boundary and not in the faster region.
| Incident angle in the slower region | What happens at the boundary |
|---|---|
| i<c | a transmitted ray refracts into the faster region, with some reflection possible |
| i=c | the transmitted ray travels along the boundary |
| i>c | no transmitted ray emerges; total internal reflection occurs |
The ray at the critical angle is not an example of total internal reflection because a transmitted ray still exists along the boundary.
Internal reflection is light reflected back into its original transparent region; total internal reflection (TIR) is the limiting case in which all the light is reflected and no refracted ray crosses the boundary.
TIR requires both conditions: light approaches a boundary from a region where it travels more slowly into one where it travels faster, and its angle of incidence is greater than the critical angle.
| Experimental move | Observation |
|---|---|
| send a narrow ray into the curved face of a semicircular block along a radius | it reaches the flat face without bending at the curved face |
| increase i at the flat block–air boundary | the refracted ray moves farther from the normal and the internally reflected ray remains |
| set i=c | the refracted ray runs along the flat surface |
| increase to i>c | the refracted ray disappears and only the internally reflected ray remains |
A swimmer can see the water surface act like a mirror for rays striking it at sufficiently large angles. Right-angle glass prisms can also turn a ray through 90∘ by TIR, as used in optical viewing devices.
A large incidence angle alone is not enough: light approaching from the faster region cannot undergo TIR at that boundary.
For a wave passing from region 1 into region 2, the relative refractive index is the ratio of its speed before the boundary to its speed after the boundary.
n=v2v1
v1 is the wave speed in the incident region and v2 is its speed in the refracting region. For light travelling from air into a material, v1≈3.0×108m s−1 and n≈c/v.
If light travels at 3.0×108m s−1 in air and 2.0×108m s−1 in glass, then n=(3.0×108)/(2.0×108)=1.5.
Refractive index has no unit because it is a ratio of two speeds with the same unit. Reversing the direction swaps the speed ratio, so identify regions 1 and 2 before substituting.
For light travelling from air into a transparent material, refractive index connects the two angles measured from the normal.
n=sinrsini
i is the angle in air and r is the angle in the material for this form of the equation. Check that both are measured from the normal, and put the calculator in degree mode.
For i=46∘ and r=26∘, n=sin46∘/sin26∘=1.64 (3 s.f.). To find an unknown angle, first isolate its sine and then apply sin−1.
Do not replace sini/sinr with i/r. If the ray travels from the material into air, the angle in air still belongs in the numerator when calculating the material's refractive index.
For light at a material–air boundary, the material's refractive index n and its critical angle c are related because the refracted angle is 90∘ at the critical condition.
n=sinc1
To find the critical angle, rearrange to sinc=1/n, so c=sin−1(1/n). Use degree mode and give the angle with appropriate precision.
For glass with n=1.56, c=sin−1(1/1.56)=39.9∘. At exactly this incidence angle, the refracted ray travels along the glass–air boundary.
This equation is for the critical boundary between the material and air. TIR occurs only for incidence from the material side with i>c, not at i=c.
An optical fibre carries information as pulses of visible or infrared light along a transparent core.
The core has a higher refractive index than the surrounding cladding. A suitably launched ray meets the core–cladding boundary from the slower core at an incidence angle greater than the critical angle, so repeated total internal reflection keeps it inside the core.
| Stage | Role in telecommunications |
|---|---|
| transmitter | converts information into a timed pattern of light pulses |
| fibre | guides the pulses over distance by repeated TIR |
| detector | converts the received pulse pattern into an electrical signal that can be decoded |
Optical fibres can carry large amounts of data at high rates with little signal loss, so they are used for internet, telephone and cable-television links.
The fibre does not trap every possible ray. If a ray reaches the core boundary below the required incidence angle, some light escapes into the cladding and the transmitted signal weakens.