Abstract
Conventional shell-model calculations of the iron isotopes with are discussed. The calculated level spectra are in good agreement with experiment. The calculations of observables are in reasonable agreement with experiment when added effective charges of are used for both neutrons and protons. The neutron effective charge is significantly different from one appropriate () for . There is a strong state dependence in the effective operator, and calculations of observables are in general disagreement with experiment. An analysis of the structure of ground-state bands and yrast levels is made in terms of a simple rotational model. In all even isotopes, the intrinsic quadrupole moments in the ground-state "band" shrink dramatically with increasing . There is evidence of a band crossing in all three even isotopes, but no evidence is found for an abrupt shape change in the ground-state bands of these nuclei. It is concluded that no simple rotational model gives a good description of the low-lying states of the iron isotopes.
NUCLEAR STRUCTURE , , , , , calculated levels. , , , calculated , , , branching ratios. Shell model, Vervier interaction, Horie-Ogawa interaction, effective operators. Comparison with experiment and rotational model.
- Received 17 April 1979
DOI:https://doi.org/10.1103/PhysRevC.20.830
©1979 American Physical Society