A. Michelson and E. Morley. On the Relative Motion of the Earth and the Luminiferous Ether. // American Journal of Science - Third series - Vol. XXXIV, No. 203. - Nov. 1887.

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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 v elociy

less than the velocity of the medium in the ratio ~ \ where


n is the index of refraction. These two hypotheses give a complete and satisfactory explanation of aberration. The second hypothesis, notwithstanding its seeming improbability, must be considered as fully proved, first, by the celebrated experiment of Fizeau,* and secondly, by the ample confirmation of our own work.f The experimental trial of the first hypothesis forms the subject of the present paper.

If the earth were a transparent body, it might perhaps be conceded, in view of the experiments just cited, that the inter-molecular ether was at rest in space, notwithstanding the motion of the earth in iis orbit; but we have no right to extend the conclusion from these experiments to opaque bodies. But there can hardly be question that the ether can and does pass through metals. Lorentz cites the illustration of a metallic barometer tube. When the tube is inclined the ether in the space above the mercury is certainly forced out, for it is im-compressible4 But again we have no right to assume that it makes its escape with perfect freedom, and if there be any resistance, however slight, we certainly could not assume an opaque body such as the whole earth to offer free passage through its entire mass. But as Lorentz aptly remarks: “quoi qui’l en soit, on fera bien, & mon avis, de ne pas se laisser guider, dans une question aussi importante, par des considerations sur le degr£ de probability ou de simplicity de l’une ou de 1’autre hypothese, mais de s’addresser a ^experience pour apprendre a connaitre l’etat, de repos ou de mouvement, dans lequel se trouve Tether a la surface terrestre.”§

In April, 1881, a method was proposed and carried out for testing the question experimentally.!

In deducing the formula for th^ quantity to be measured, the effect of the motion of the earth through the ether on the path of the ray at right angles to this motion was overlooked.^"

* Comptes Rendus, xzxiii, 349, 1851; Pogg. Ann. Erganzungsband, iii, 457, 1853; Ann. Chim. Phys., Ill, lvii, 385, 1859.

f Influence of Motion of the Medium on the Yelocity of Light. This Journal, III, ixxi, 377. 1886.

% It may be objected that it may escape by the space between the mercury and the walls; but this could be prevented by amalgamatitf^ the walls.

§ Archives Neerlandaises, xxi, 2me livr.

(The relative motion of the earth and the luminiferous ether, by Albert A. Michelson, this Jour., Ill, xxii, 120. 1

It may be mentioned here that the error was pointed out to the author of the >former paper by M. A. Potier, of Paris, in the winter of 1881.

The discusssion of this oversight and of the entire experiment forms the subject of a very searching analysis by H. A. Lorentz,* who finds that this effect can by no means be disregarded. In consequence, the quantity to be measured had in fact but one-half the value supposed, and as it was already barely beyond the limits of errors of experiment, the conclusion drawn from the result of the experiment might well be questioned; since, however, the main portion of the theory remains unquestioned, it was decided to repeat the experiment with such modifications as would insure a theoretical result much too large to be masked by experimental errors. The theory of the method may be briefly stated as follows:

Let sa, fig. 1, be a ray of light which is partly reflected in ah, and partly transmitted in a<?, being returned by the mirrors b and c, along ba and ca. ba is partly transmitted along ad,

and ca is partly reflected along ad. If then the paths ab and ac are equal, the two rays interfere along ad. Suppose now, the ether being at rest, that the whole apparatus moves in the direction sc, with the velocity of the earth in its orbit, the direc-

* De l’lnfluence du M.ouvement de la Terre sur lea Phen. Lum. Archives N6er-landaises, xxi, 2m® livr., 1886.

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