Abstract
In order to resolve a recent discrepancy in the half-life of Fe60, we performed an independent measurement with a new method that determines the Fe60 content of a material relative to Fe55 (t1/2=2.744yr) with accelerator mass spectrometry. Our result of (2.50±0.12)×106yr clearly favors the recently reported value (2.62±0.04)×106yr, and rules out the older result of (1.49±0.27)×106yr. The present weighted mean half-life value of (2.60±0.05)×106yr substantially improves the reliability as an important chronometer for astrophysical applications in the million-year time range. This includes its use as a sensitive probe for studying recent chemical evolution of our Galaxy, the formation of the early Solar System, nucleosynthesis processes in massive stars, and as an indicator of a recent nearby supernova.
| Original language | English |
|---|---|
| Article number | 041101 |
| Number of pages | 6 |
| Journal | Physical Review Letters |
| Volume | 114 |
| Issue number | 4 |
| DOIs | |
| Publication status | Published - 28 Jan 2015 |
Funding
Part of this work was funded by the Austrian Science Fund (FWF) Projects No. AP20434 and AI00428 (FWF and CoDustMas, Eurogenesis via ESF). We thank M. Frohlich (nee Srncik) for production of Fe oxide material.
Austrian Fields of Science 2012
- 104003 Inorganic chemistry
- 103014 Nuclear physics
- 104017 Physical chemistry
Keywords
- EARLY SOLAR-SYSTEM
- NUCLEAR-DATA SHEETS
- PROTOPLANETARY DISK
- IRON-60
- FE-55
- HETEROGENEITY
- RADIONUCLIDES
- FE-60-NI-60
- CHRONOLOGY
- CHONDRITES