Before arguing about whether light is a wave, you need a clear picture of what waves do that particles never do. Throw two handfuls of pebbles through a pair of doorways and you get two piles. Send water waves through the same doorways and you get something stranger: a fan of calm stripes where the water barely moves, alternating with stripes of violent motion. That pattern — interference — together with the spreading of waves through gaps — diffraction — is the fingerprint of a wave. This topic studies both with water, where you can see them, so the rest of the unit can look for the same fingerprints in light.
Superposition in two dimensions
In Grade 11 you added pulses on a string: where two waves overlap, the displacement is the sum of the two separate displacements. A ripple tank does the same thing across a whole surface. Two dippers tap the water in phase — at the same frequency, rising and falling together — so each sends out circular ripples with the same wavelength . Wherever a crest from one source meets a crest from the other, the water rises twice as high (constructive interference). Wherever a crest meets a trough, the water stays nearly flat (destructive interference). Because the sources keep the same timing, these spots do not wander about. They line up into a stable pattern of curved lines called nodal lines (always calm) separated by antinodal lines (always strongly oscillating).
Path difference decides everything
Pick any point in the tank. It is a distance from one source and from the other. The waves leave in phase, so what matters is how much farther one wave travelled than the other: the path difference . If that difference is a whole number of wavelengths (), a crest arrives with a crest and is on an antinodal line. If it is an odd number of half-wavelengths (), a crest arrives with a trough and is on a nodal line.
The perpendicular bisector between the sources is equally far from both, so it is always the central antinodal line (). The first nodal line on either side () has a path difference of half a wavelength, the second () of one and a half, and so on. For a point far away compared with the source separation , the path difference is very nearly , where is the angle measured from the bisector. That gives a way to locate nodal lines by angle, or by their distance from the bisector at a distance from the sources:
| Change | Effect on the pattern | Reason |
|---|---|---|
| Increase the frequency of both sources | More nodal lines, packed closer together | Higher means shorter , so is smaller for each line |
| Move the sources farther apart | More nodal lines, packed closer together | Larger makes smaller |
| Move the sources closer together | Fewer nodal lines, spread wider | Once there are no nodal lines at all |
| Make one source half a cycle out of phase | Nodal and antinodal lines swap places | The bisector now receives a crest and a trough together |
Diffraction: waves bending through openings
Send straight wavefronts at a barrier with a gap and the waves that emerge are not a neat beam the width of the gap: they spread into the shadow region behind the barrier. This bending is diffraction, and it also happens around the edge of a single obstacle. Huygens' principle explains why: every point on a wavefront acts as a tiny source of new circular wavelets, and the next wavefront is where those wavelets overlap. Far from any barrier the sideways wavelets cancel each other out, so the wave carries straight on. At the edges of a gap there are no neighbours on one side to cancel them, so the wave curves around.
- The ratio is large (about 1 or more)
- Waves fan out into nearly semicircular fronts
- Strong bending into the shadow
- Example: sound waves through a doorway
- The ratio is tiny
- Waves pass through as a nearly straight beam
- Only the edges of the beam curve slightly
- Example: light through the same doorway