Abstract
The isotope shifts and hyperfine-structure-splitting constants of the and transitions of have been measured by collinear laser-ion-beam spectroscopy for the accelerator-produced isotopes and , and for the naturally occurring isotopes and . The magnetic moments of the ground states of the isotopes and have been determined to be and , respectively, and the quadrupole moments to be and . The ratio of the magnetic dipole coupling constants of the level has shown a hyperfine anomaly with respect to the NMR ratio of the nuclear factors. The change in the mean-square nuclear charge radius determined from the isotope shift between and is . This value is smaller than the predictions made by the finite-range droplet model or by the Hartree-Fock plus BCS calculation.
- Received 15 August 2003
DOI:https://doi.org/10.1103/PhysRevC.68.054328
©2003 American Physical Society