The Isotope Effect in Band Spectra, Part I

Abstract
Theory of the isotope effect in band spectra of diatomic molecules. — Generalizing previous discussions by Loomis and Kratzer, it is shown that each coefficient in the detailed expressions for the spectral terms (except those involved in νe) of a band spectrum of a diatomic molecule may be written as a quantity independent of mass times some power of 1μ, where, if M and M are the masses of the two nuclei, 1μ=1M+1M. The frequency ν of any line may be considered as the sum of an "electronic," a (positive or negative) "vibrational," and a (positive or negative) "rotational" contribution: ν=νe+νn+νm, where n=vibrational and m=rotationalquantumnumber. From theory and experience in line spectra, νe (if present) should be substantially identical for corresponding band systems of two or more isotopes, so that these should have a common "origin." This leads to the definition of the origin of a band-system: ν=νe; νn=νm=0; and the definition of the origin of a band: ν=νe+νn; νm=0. For two isotopes, ν2=ν2e+ν2n+ν2m=ν1e+ρν1n+ρ2ν1m, approximately, where ρ2=(1μ2)(1μ1). The various bands corresponding to various values of νn should form for each isotope an essentially identical pattern about the origin. The scale of this pattern should, however, be greater for a lighter isotope (vibrational isotope effect), and large separations between corresponding bands of isotopes may result for bands remote from the origin. Two typical band-patterns for a mixture of isotopes are given in Fig. 1. Analogous relations hold with respect to the νm terms (rotational isotope effect) (cf. Fig. 2). An explicit equation for band-l eads is obtained; this contains important mixed and higher power terms in n and n; the corresponding isotope effect is discussed. In studying isotope effects in band spectra, compounds of isotopic elements with other elements of high atomic weight are favorable; a low-temperature light source is very desirable; other practical factors are discussed. Quantitative and semi-quantitative confirmations of the isotope effect already obtained (BO, SiN, CuH, CuCl, CuBr, CuI) lend powerful support to the general quantum theory of band spectra.

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