THE LAWS OF THE ABSORPTION OF LIGHT IN CRYSTALS.

By H. BECQUEREL.

1. The absorption spectrum observed through a crystal varies with the

direction of the rectilinear luminous vibration which propagates itself in

this crystal. 2. The bands or rays observed through the same crystal have,

in the spectrum, fixed positions, their intensity alone varying. 3. For a

given band or ray there exist in the crystal three rectangular directions

of symmetry, according to one of which the band generally disappears, so

that for a suitable direction of the luminous vibrations the crystal no

longer absorbs the radiations corresponding to the region of the spectrum

where the band question appeared. These three directions may be called the

principal directions of absorption, relative to this band. 4. In the

orthorhombic crystals, by a necessary consequence of crystalline symmetry,

the principal directions of absorption of all the bands coincide with the

three axes of symmetry. We may thus observe three principal absorption

spectra. In uniaxial crystals the number of absorption spectra is reduced

to two. 5. In clinorhombic crystals one of the principal directions of

absorption of each crystal coincides with the only axis of symmetry; the

two other principal rectangular directions of each band may be found

variously disposed in the plane normal to this axis. Most commonly these

principal directions are very near to the principal corresponding

directions of optical elasticity. 6. In various crystals the characters of

the absorption phenomena differ strikingly from those which we might expect

to find after an examination of the optical properties of the crystal. We

have just seen that in clinorhombic crystals the principal absorption

directions of certain bands were completely different from the axis of

optical elasticity of the crystal for the corresponding radiations. If we

examine this anomaly, we perceive that the crystals manifesting these

effects are complex bodies, formed of various matters, one, or sometimes

several, of which absorb light and give each different absorption bands.

Now, M. De Senarmont has shown that the geometric isomorphism of certain

substances does not necessarily involve identity of optical properties, and

in particular in the directions of the axes of optical elasticity in

relation to the geometric directions of the crystal. In a crystal

containing a mixture of isomorphous substances, each substance brings its

own influence, which may be made to predominate in turn according to the

proportions of the mixture. We may, therefore, admit that the molecules of

each substance enter into the crystal retaining all the optical properties

which they would have if each crystallized separately. The principal

directions of optical elasticity are given by the resultant of the actions

which each of the component substances exerts on the propagation of light,

while the absorption of a given region of the spectrum is due to a single

one of these substances, and may have for its directions of symmetry the

directions which it would have in the absorbing molecule supposing it

isolated. It may happen that these directions do not coincide with the axes

of optical elasticity of the compound crystal. If such is the cause of the

anomaly of certain principal directions of absorption, the bands which

present these anomalies must belong to substances different from those

which yield bands having other principal directions of absorption. If so,

we are in possession of a novel method of spectral analysis, which permits

us to distinguish in certain crystals bands belonging to different matters,

isomorphous, but not having the same optical properties. Two bands

appearing in a crystal with common characters, but presenting in another

crystal characters essentially different, must also be ascribed to two

different bodies.

* * * * *

[Continued from SUPPLEMENT, No. 585, page 9345.]

Scientific American Supplement, No. 586, March 26, 1887 · 第 41 / 50 题