Wave Reflection — Phase Inversion, Fixed Ends and the Law of Reflection

What a wave does at a boundary: why fixed ends flip pulses upside down, free ends reflect them upright, why the angle of incidence equals the angle of…

Quick answer

Reflection is the bouncing of a wave off a boundary back into its original medium. At a fixed end the pulse returns inverted (upside down); at a free end it returns upright.

θi=θr\theta_i = \theta_r

Unit: angles measured from the normal, in degrees

Example: A light ray striking a mirror at 30° from the normal leaves at 30° on the other side of the normal.

What you will learn

  • Describe what happens when a wave reaches a boundary
  • Predict whether a reflected pulse is inverted or upright for fixed and free ends
  • State and apply the law of reflection θi = θr
  • Explain partial reflection at a boundary between two media
  • Give real-world applications of wave reflection

A pulse meets a wall

Send a single pulse down a stretched rope toward a wall and watch what comes back. The pulse does not vanish into the wall — it returns toward you, traveling through the same rope it came down. That return journey is reflection: a wave bouncing off a boundary back into its original medium.

What makes reflection interesting is not that the pulse comes back, but how it comes back. The boundary's nature — rigid or free, head-on or angled — writes itself into the reflected wave.

Fixed end: the inverted reflection

Tie the rope firmly to a wall and send an upward pulse toward it. The reflected pulse comes back downward — inverted, as if flipped through the rope's resting line.

Why? The tied end cannot move, so the arriving pulse yanks upward on the wall, and the wall yanks back downward on the rope (Newton's third law). That downward reaction launches the return pulse upside down. In wave language, a fixed end imposes a phase shift of half a cycle (π\pi radians): crest becomes trough and trough becomes crest.

An upward pulse traveling toward a wall, then returning downward after reflecting from the fixed endλ (wavelength)A (amplitude)direction
A pulse reflecting from a fixed end returns inverted: the wall's reaction flips crest to trough.

Free end: the upright reflection

Now thread the rope's end through a smooth ring that slides freely on a vertical pole — a free end. Send the same upward pulse. This time it returns upward, upright and unflipped.

The free end offers no resistance: the arriving pulse lifts the ring to double height momentarily, and the ring's fall launches the reflected pulse in the original orientation. There is no phase shift — crest stays crest. The same rule governs a sound wave hitting open air or a water wave reaching a gentle beach: softer boundaries reflect upright.

Oblique incidence: the law of reflection

Waves rarely strike boundaries head-on. For a ray hitting a smooth surface at an angle, reflection obeys one clean rule:

θi=θr\theta_i = \theta_r

The angle of incidence θi\theta_i equals the angle of reflection θr\theta_r — and both are measured from the normal, the line perpendicular to the surface at the impact point, with incident and reflected rays on opposite sides of it.

This law holds for light on mirrors, sound on walls, and water waves on harbor barriers alike. It is why you can aim a billiard-style bank shot with a laser pointer — and why concert halls angle their wall panels to throw sound exactly where the audience sits.

Partial reflection at soft boundaries

Real boundaries are rarely perfect walls. When a wave meets the boundary between two media it can enter — like sound passing from air into water — part of the wave reflects and part transmits through. This is partial reflection.

How much reflects depends on the contrast between the media, called the impedance mismatch. Shouting across a canyon gives a strong echo because air and rock are wildly different; a doctor's ultrasound gel exists to reduce the mismatch between the probe and your skin, so more sound enters the body instead of reflecting off it.

Worked mini-example

A pulse travels at 10 m/s10\ \mathrm{m/s} along a rope toward a fixed wall 2 m2\ \mathrm{m} away.

  • Time to reach the wall: t=d/v=2/10=0.20 st = d/v = 2/10 = 0.20\ \mathrm{s}.
  • Time for the round trip back to the starting point: 0.40 s0.40\ \mathrm{s}.
  • The returning pulse is inverted (fixed end) and slightly smaller (some energy lost as heat and sound at the wall).

If the end were free instead, the pulse would return in the same 0.40 s0.40\ \mathrm{s} but upright. Same timing, opposite phase — the boundary type is written into the wave.

Everyday reflections

Reflection is a working tool, not just a textbook demo. Echo sounding maps the seafloor by timing sound pulses reflected off the bottom. Medical ultrasound builds images from reflections at tissue boundaries. Radar and lidar locate aircraft and map terrain with reflected radio waves and laser pulses.

Even architecture leans on it: a whispering gallery is a room shaped so that sound reflects along its walls to a distant listener, and anechoic chambers do the opposite — lining walls with wedges that swallow reflections so engineers can test speakers in pure, reflection-free sound.

Variables and units

SymbolNameUnitMeaning
θiθᵢAngle of incidencedegreesAngle between incoming ray and the surface normal
θrθᵣAngle of reflectiondegreesAngle between reflected ray and the surface normal
vvWave speedm/sSpeed of the wave in the medium

Common mistakes

✗ Every reflection flips the wave upside down.

Only hard, fixed boundaries invert the pulse. Free ends and boundaries with softer media reflect the wave upright — the phase change depends on the boundary type.

✗ The angle of reflection is measured from the surface.

Both the angle of incidence and the angle of reflection are measured from the normal — the line perpendicular to the surface at the impact point.

✗ Waves only reflect from solid walls.

Any boundary between different media reflects part of a wave: air-to-water, warm air to cold air, even different rock layers underground. Seismologists map Earth's interior from such reflections.

Real-world applications

  • Sonar and medical ultrasound send pulses out and read their reflections to map what they cannot see.

  • Radar guns bounce radio waves off cars; the reflected signal reveals the vehicle's speed.

  • Concert-hall designers place reflective and absorptive surfaces so reflections enrich the music instead of muddying it.

Frequently asked questions

Why does a fixed end invert a reflected pulse?

The end cannot move, so when the pulse arrives the rope pulls up on the support and the support pulls back down on the rope (Newton's third law). That reaction launches an inverted pulse back along the rope — equivalent to a phase shift of half a cycle, or π radians.

What is the difference between fixed-end and free-end reflection?

A fixed end returns the pulse upside down (phase shift π); a free end returns it upright (no phase shift). The fixed end is a displacement node — it cannot move — while the free end is free to swing and launches the reflected pulse in the same orientation.

Does reflection change the wave's speed or frequency?

No. An ideal reflection changes neither the speed (set by the medium) nor the frequency (set by the source). Only the direction of travel — and sometimes the phase — changes. Real reflections may lose some energy, reducing the amplitude.

What is partial reflection?

When the boundary is between two media the wave can enter — like air into water — part of the wave reflects and part transmits through. The split depends on how different the two media are (the impedance mismatch): a bigger contrast means a stronger reflection.

How do bats and sonars use reflection?

Bats emit ultrasonic chirps and time the returning echoes to locate insects in the dark; sonar does the same underwater with sound, and radar with radio waves. In each case the reflection's delay gives the distance and any frequency shift gives the target's speed.