Abstract
Background: Because of its half-life of about 35 million years, is considered as a chronometer for nucleosynthesis events prior to the birth of our sun. The abundance of in the early solar system can be derived from meteoritic data. It has to be compared to theoretical estimates for the production of to determine the time between the last nucleosynthesis event before the formation of the early solar system.
Purpose: The influence of a low-lying short-lived isomer on the nucleosynthesis of is analyzed. The thermal coupling between the ground state and the isomer via so-called intermediate states affects the production and survival of .
Method: The properties of the lowest intermediate state in are known from experiment. From the lifetime of the intermediate state and from its decay branchings, the transition rate from the ground state to the isomer and the effective half-life of are calculated as functions of the temperature.
Results: The coupling between the ground state and the isomer is strong. This leads to thermalization of ground state and isomer in the nucleosynthesis of in any explosive production scenario and almost 100% survival of in its ground state. However, the strong coupling leads to a temperature-dependent effective half-life of which makes the survival very sensitive to temperatures as low as about 8 keV, thus turning at least partly into a thermometer.
Conclusions: The low-lying isomer in does not affect the production of in explosive scenarios. In retrospect this validates all previous studies where the isomer was not taken into account. However, the dramatic reduction of the effective half-life at temperatures below 10 keV may affect the survival of after its synthesis in supernovae, which are the most likely astrophysical sites for the nucleosynthesis of .
- Received 18 March 2016
DOI:https://doi.org/10.1103/PhysRevC.93.065804
©2016 American Physical Society