Abstract
The ground-state electric quadrupole moment of has been measured by means of -ray-detected nuclear magnetic resonance spectroscopy using a spin-polarized beam produced in the projectile fragmentation reaction. The obtained moment, , is in agreement with conventional shell model calculations within the valence space. Previous results on the magnetic moment also support the validity of the model in this isotope, and thus it is concluded that is located outside of the island of inversion.
- Received 16 October 2008
DOI:https://doi.org/10.1103/PhysRevC.79.027301
©2009 American Physical Society