What Reflection at a Boundary Means
So far we considered waves propagating in an unbounded medium. When a pulse or a wave meets a boundary, it gets reflected. The phenomenon of echo — sound returning from a cliff or wall — is the everyday example of reflection by a rigid boundary. The character of the reflection, however, is not the same for every kind of boundary. Two ideal cases bracket the behaviour: a perfectly rigid boundary, where the end cannot move, and a perfectly free (open) boundary, where the end is completely free to move.
If the boundary is not completely rigid, or is an interface between two different elastic media, the situation is more involved. Part of the incident wave is reflected and part is transmitted into the second medium. When a wave is incident obliquely on the boundary between two media, the transmitted wave is called the refracted wave: the incident and refracted waves obey Snell's law of refraction, while the incident and reflected waves obey the usual laws of reflection. For NEET the two limiting cases — rigid and free — carry almost all the weight, so we treat each in turn.
A single transverse pulse approaches a wall. At a rigid end it returns inverted; at a free end it returns upright. The two diagrams below make the contrast concrete.
Reflection at a Rigid (Fixed) Boundary
Picture a pulse travelling along a stretched string toward an end clamped firmly to a wall. Assuming no absorption of energy by the boundary, the reflected wave has the same shape as the incident pulse, but it suffers a phase change of π (180°) on reflection. A crest returns as a trough.
NCERT gives two complementary reasons for this inversion. The first is a boundary-condition argument: the boundary is rigid, so the disturbance must have zero displacement at all times at that point. By the principle of superposition, the net displacement at the wall can be zero only if the reflected and incident waves differ in phase by π, so that they cancel there. The second is a dynamical argument from Newton's third law: as the pulse arrives at the wall it exerts an upward force on the wall; the wall exerts an equal and opposite (downward) force on the string, and this generates a reflected pulse that differs by a phase of π. Because the displacement is permanently zero at the fixed end, that point is a node.
Rigid end → π phase change → node
Students routinely mix up which boundary inverts the pulse. Tie the three ideas together as one packet: a rigid / fixed / denser boundary forces zero displacement, so the reflected wave is phase-shifted by π and a crest comes back as a trough. The fixed point itself is a node.
Fixed end ⇒ phase reversal of π ⇒ node (zero displacement always).
Reflection at a Free (Open) Boundary
Now suppose the boundary point is not rigid but completely free to move — the textbook model is a string tied to a freely moving ring that slides without friction on a rod. With no constraint forcing the displacement to zero, the reflected pulse has the same phase and amplitude (assuming no energy dissipation) as the incident pulse. A crest returns as a crest, with no inversion.
At the instant the incident and reflected pulses overlap at the free end, their displacements add. The net maximum displacement at the boundary is therefore twice the amplitude of each pulse, so the free end is a point of maximum displacement — an antinode. An example of a non-rigid boundary is the open end of an organ pipe.
At a free boundary there is no inversion. The reflected crest comes back as a crest, and momentarily the displacement at the end reaches 2a.
Rigid vs Free — The Decisive Table
NCERT summarises the whole topic in a single sentence: a travelling wave or pulse suffers a phase change of π on reflection at a rigid boundary and no phase change on reflection at an open boundary. The table fixes every consequence side by side.
| Feature | Rigid / Fixed / Denser end | Free / Open / Rarer end |
|---|---|---|
| Phase change on reflection | π (180°) | 0 (none) |
| A crest returns as | a trough (inverted) | a crest (upright) |
| Displacement at boundary | zero at all times | maximum (twice amplitude) |
| Point formed there | node | antinode |
| Reflected-wave equation | y_r = − a sin(kx + ωt) | y_r = a sin(kx + ωt) |
| Physical example | echo from a cliff; closed end of a pipe | open end of an organ pipe |
The Reflected-Wave Equations
To put the summary mathematically, NCERT writes the incident travelling wave as $y(x,t) = a\sin(kx - \omega t)$. The reflected wave that meets a boundary is obtained by adding the phase shift the boundary imposes.
At a rigid boundary the phase shift is π:
$$y_r(x,t) = a\sin(kx - \omega t + \pi) = -\,a\sin(kx - \omega t)$$
At an open boundary the phase shift is zero:
$$y_r(x,t) = a\sin(kx - \omega t + 0) = a\sin(kx - \omega t)$$
Two cautions are worth holding. First, the reflected wave actually travels in the opposite direction to the incident wave, so when it is used to build a standing wave it is written with the argument $kx + \omega t$; at the rigid end this reads $y_r = -\,a\sin(kx + \omega t)$, exactly as the NCERT summary states. Second, at the rigid boundary the incident and reflected displacements satisfy $y = y_i + y_r = 0$ at the wall at all times — the algebraic statement of the node.
Reflection is a direct application of the principle of superposition of waves: the resultant at the boundary is the algebraic sum of incident and reflected displacements.
Transmission at a Junction of Two Strings
A genuinely rigid or free end is an idealisation. More commonly a wave reaches a junction where the medium changes — for example a light string knotted to a heavy one. Here part of the wave is reflected and part is transmitted into the second medium, and the rule for the reflected part follows the same denser/rarer logic.
When a wave travelling on a string reflects from a denser medium (a heavier string ahead, which behaves like a fixed support in the limit), the reflected part is inverted — a π phase reversal, exactly as at a rigid wall. When it reflects from a rarer medium (a lighter string ahead, tending toward a free end), the reflected part is upright — no phase change. The transmitted wave, whichever way the density steps, always continues in phase with the incident wave; it is never inverted.
Longitudinal waves: "change of type" at a rarer end
For sound (longitudinal waves) the NIOS treatment adds a subtlety. On reflection from a denser medium a compression returns as a compression (no change of type) but with change of sign. On reflection from a rarer medium a compression returns as a rarefaction and a rarefaction as a compression — a "change of type" but no change of sign. Do not blindly apply the transverse crest-to-trough rule to compressions.
Sound at a rarer (open) end ⇒ compression ↔ rarefaction (type flips), phase unchanged.
How Reflection Builds Standing Waves
Reflection at a single boundary is only the first step. The familiar situations — a string fixed at both ends, or an air column closed at one end — involve reflection at two or more boundaries. A wave travelling one way reflects at one end, travels back, reflects at the other end, and so on, until a steady pattern is established. Superposing the incident $y_1 = a\sin(kx - \omega t)$ and reflected $y_2 = a\sin(kx + \omega t)$ waves gives
$$y(x,t) = 2a\,\sin kx\,\cos \omega t$$
in which $kx$ and $\omega t$ appear separately rather than in the combination $kx - \omega t$. This is a standing (stationary) wave, with permanently fixed nodes and antinodes set by the boundary conditions. The full development of normal modes, harmonics and organ-pipe frequencies follows from exactly the rigid-end and free-end conditions established here.
Reflection of Waves in one screen
- A pulse meeting a boundary is reflected; an echo is reflection at a rigid boundary.
- Rigid / fixed / denser end: phase change of π, crest returns as trough, displacement zero, a node forms.
- Free / open / rarer end: no phase change, crest returns as crest, displacement reaches 2a, an antinode forms.
- Reflected equations for incident $a\sin(kx-\omega t)$: rigid → $-a\sin(kx+\omega t)$; open → $a\sin(kx+\omega t)$.
- At a junction: part reflects (denser ⇒ inverted, rarer ⇒ upright), part transmits in phase. For sound, a rarer end flips compression ↔ rarefaction.
- Superposing incident and reflected waves gives the standing wave $y = 2a\sin kx\,\cos\omega t$.