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Physics 1887

On the Relative Motion of the Earth and the Luminiferous Ether

Albert A. Michelson & Edward W. Morley

They looked for the wind of the ether — and found, to exquisite precision, nothing.

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In depth · the introduction

For a century, physicists were sure light needed an invisible sea to travel through. Two Americans built the most careful ruler ever made to feel the current of that sea — and felt nothing at all.

The big idea

In the 1800s, everyone agreed light was a wave. But waves wave in something: sound waves in air, ocean waves in water. So light must wave in something too — a transparent stuff filling all of space, called the luminiferous ether. If it was really there, the Earth racing around the Sun at about 30 kilometres a second should feel an “ether wind” blowing past it, just as you feel air rush by when you stick your hand out of a moving car.

Michelson and Morley set out to feel that wind. They split a beam of light into two, sent the halves down two arms set at right angles, bounced them off mirrors, and let them recombine. If the ether wind sped one beam up and slowed the other, the recombined light would show a tell-tale pattern of stripes — and rotating the whole machine would make the stripes shift. They built an instrument delicate enough to catch a wind twenty times fainter than expected. The stripes never moved.

How it came about

Albert Michelson was obsessed with measuring light. In 1881, working in Germany, he built a first version of his interferometer and got a puzzling near-zero result — but his calculation had an error, and the test wasn't sensitive enough to be sure. Back in Cleveland, he teamed up with the chemist Edward Morley, and together they rebuilt the experiment on an enormous scale.

Their masterpiece was as much engineering as physics. To kill vibration, they mounted the optics on a slab of sandstone and floated it on a pool of liquid mercury, so the whole heavy table could be spun as smoothly as a record on a turntable — one slow turn every six minutes. They watched the stripes hour after hour, season planned after season. Again and again: nothing. The most anticipated wind in physics simply wasn't blowing.

Why it mattered

A famous “nothing” can be more powerful than a discovery. The ether had been the bedrock assumption of physics, and this experiment showed there was no detectable ether wind — which meant something was deeply wrong with the comfortable picture of light moving through a fixed, invisible medium.

It took nearly twenty years to digest. The puzzle helped force a radical idea into the open: that the speed of light is the same for everyone, no matter how they move, and that space and time themselves must bend to keep it so. That idea is Einstein's special relativity, and the Michelson–Morley null result is the experiment most often cited as clearing its path.

A way to picture it

Think of two identical swimmers in a river, racing equal distances and back. One swims straight across the current and returns; the other swims upstream and then back down. Even at the same swimming speed, the current delays them by different amounts — the up-and-down swimmer always loses more time. So if there were an ether “current” flowing past the Earth, the two light beams should return slightly out of step, and you'd see it in the stripes. Michelson and Morley ran the race over and over, turning the pool every which way — and the two swimmers always tied. There was no current.

A schematic Michelson interferometer floated on mercury: a light source, a beam splitter, two perpendicular arms with end mirrors, and a fringe screen. Slide an assumed ether wind from zero up to the Earth's orbital speed; as the table turns, the stripes slide by the amount classical theory predicts — but at zero wind they stay perfectly still.

Where it sits

This experiment sits at a hinge in the history of physics. Behind it lies the great wave theory of light built by Fresnel and Maxwell, which seemed to demand an ether. Ahead of it lies Einstein's 1905 relativity, which threw the ether out and made the speed of light absolute. Michelson's interferometer itself never retired: shrunk for the laboratory it became a precision tool, and grown to four-kilometre arms it became LIGO, the instrument that in 2015 caught gravitational waves — listening for a ripple in space far fainter than the ether wind they once failed to find.

The original document
Original source text

The ether hypothesis

A. A. Michelson & E. W. Morley · American Journal of Science · 1887 · §1
The discovery of the aberration of light was soon followed by an explanation according to the emission theory. The effect was attributed to a simple composition of the velocity of light with the velocity of the earth in its orbit.
On the undulatory theory, according to Fresnel, first, the ether is supposed to be at rest except in the interior of transparent media, in which secondly, it is supposed to move with a velocity less than the velocity of the medium in the ratio (n² − 1)/n², where n is the index of refraction.
[ … ]
If the earth were a transparent body, it might perhaps be conceded, in view of the experiments just cited, that the intermolecular ether was at rest in space, notwithstanding the motion of the earth in its orbit; but we have no right to extend the conclusion from these experiments to opaque bodies.

The apparatus on mercury

§ The interferometer, floated to turn freely and continuously
The stone is about 1.5 meter square and 0.3 meter thick. It rests on an annular wooden float, 1.5 meter outside diameter, 0.7 meter inside diameter, and 0.25 meter thick. The float rests on mercury contained in the cast-iron trough.
The apparatus was revolved very slowly (one turn in six minutes) and observations of the fringes were made continually as the stone turned. By this means an accumulation of errors was avoided, and the displacement, if any, could be detected at once.
The distance D was about eleven meters, or 2×10⁷ wave-lengths of yellow light; hence the displacement to be expected was 0.4 fringe.

The null result

§ Comparing the observed shift with the shift predicted by a stationary ether
The actual displacement was certainly less than the twentieth part of this, and probably less than the fortieth part.
Considering the motion of the earth in its orbit only, this displacement should be 2D × v²/V² = 2D × 10⁻⁸. The distance D was about eleven meters; hence the displacement to be expected was 0.4 fringe — and yet it could not be found.
It appears, from all that precedes, reasonably certain that if there be any relative motion between the earth and the luminiferous ether, it must be small; quite small enough entirely to refute Fresnel's explanation of aberration.
The experiment will therefore be repeated at intervals of three months, and thus all uncertainty will be avoided.
Albert A. Michelson & Edward W. Morley · Cleveland, Ohio · 1887