Abstract
We present results from stopped beam rare isotope spectroscopic investigations at the GSI (RISING) experiment based on the detection of -ray transitions following the decay of Pd. A comparison between the measured low-lying level scheme of Rh and the prediction from shell-model calculations reveals the important roles of the and orbitals in explaining the structural features. The low values of the Gamow-Teller strengths can be attributed to the influence of the neutron-proton interaction, which gives rise to an increased seniority mixing for the nuclear states, thereby leading to a fragmentation of the strength to several daughter levels. These results provide further strong indications that Pd resides in the middle of a structural transition region in the Pd isotopes as the line is approached.
- Received 25 July 2012
DOI:https://doi.org/10.1103/PhysRevC.86.041301
©2012 American Physical Society