Abstract
SPECTROSCOPIC investigations on the scattering of light in crystals show very plainly that their vibration spectra have a discrete structure manifesting itself as a set of lines with sharply defined frequency shifts. That a similar discrete structure is also to be seen in the infra-red absorption spectra of crystals when examined under appropriate conditions is shown by a remarkable investigation by Barnes and Brattain1. These authors examined the case of magnesium oxide, which is a crystal of the cubic class with a structure similar to that of rock-salt. Plates obtained by cleavage from flawless transparent single crystals of large size were employed, and the absorption spectra of a whole series of such plates from the very thinnest obtainable to the thickest were investigated. The rock-salt spectrometer used in the study covered the wave-length range 1–15·6 μ., and the galvanometer deflexions were amplified 150 times by a photo-electric relay system. The resulting data showed the presence of some forty absorption lines in the wave-length range 6–15·5 μ. In the absorption curves reproduced with their paper, these lines are so sharply defined that their positions can be measured with high precision.
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References
Phys. Rev., 48, 582 (1935).
Proc. Ind. Acad. Sci., 18, 237 (1943).
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RAMAN, C. Infra-Red Absorption Spectra of Crystals. Nature 161, 165–166 (1948). https://doi.org/10.1038/161165b0
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DOI: https://doi.org/10.1038/161165b0
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