The Isotope Displacement in Hyperfine Structure

G. Breit
Phys. Rev. 42, 348 – Published 1 November 1932
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Abstract

With Goudsmit's extension of Landé's formula for (1r3) it is possible to explain the order of magnitude of the isotope displacements in Hg, Tl, Pb arc and spark spectra on the hypothesis of small changes in nuclear radii. The nuclear radius is supposed to be proportional to the 13 power of the atomic weight. The effective nuclear charge is supposed to be distributed with a roughly uniform density through the interior of the nucleus. The spectra Hg I, Hg II, Tl I, Tl II, Pb II, are in agreement with the above theory. The larger displacements are due to the addition or removal of a 6s or 7s electron to the electron configuration. The direction of the shift is in agreement with the supposition that the nuclear radius increases with atomic weight, the heavier isotope having the looser binding for the s and p12 electrons. In order to explain the shifts of the 6p2, 6p7s, 6p8s, d6p, 6p8p configurations of PbI it is supposed that in this case the displacements are due principally to changes in the penetration to the nucleus of the 6s2 subgroup. These changes are presumably caused by differences in screening of the two 6s electrons from the nucleus as the valence electron is excited from the 6p state to the ionization limit.

  • Received 12 September 1932

DOI:https://doi.org/10.1103/PhysRev.42.348

©1932 American Physical Society

Authors & Affiliations

G. Breit

  • Department of Physics, New York University

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Issue

Vol. 42, Iss. 3 — November 1932

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