Abstract
The ground-state quadrupole moments of , , , , , , , , and were determined by measuring the quadrupole hyperfine-splitting energies of muonic x rays. The results are b for , b for , b for , b for , b for , b for , b for , b for , and b for . The present quadrupole moments, compared with values obtained from electronic-atom hyperfine measurements, show that the Sternheimer correction factors used in the rare-earth electronic-atom analysis are unreliable. Systematics of deformation parameters calculated from the present quadrupole moments for odd- nuclei, and from values of Coulomb excitation measurements for even- nuclei, also indicate that the largest deformation change so far known exists between and . Except at the onset of nuclear deformation, the deformation parameters of the odd- nuclei are quite consistent with those of the even- neighbors.
- Received 15 November 1983
DOI:https://doi.org/10.1103/PhysRevC.29.1830
©1984 American Physical Society