Abstract
A recent measurement of the magnitude of quadrupole moment of the ground state of , , finds that . A variety of shell-model calculations, using -shell wave functions, predict and yield quadrupole moments whose magnitudes are approximately half the experimental values. Agreement between theory and experiment is improved when effective charges are used, although the results are still not completely satisfactory. A calculation of the wave functions of the low-lying states of and using a modified version of the Sussex matrix elements in a model space, including all and excitations, has been performed. The resulting value for was —3.46 as compared with the experimental value of ±3.22±0.66 . The effective charge used in the calculation, , reproduced the experimental value of exactly. The calculated magnetic dipole moment of the ground state of is the experimental value is .
- Received 9 May 1984
DOI:https://doi.org/10.1103/PhysRevC.30.1320
©1984 American Physical Society