Rhenium Osmium Chronometer

from Wikipedia, the free encyclopedia

The rhenium osmium chronometer is a method of radiometric age determination .

The isotope 187 Re ( rhenium ) has a half-life of 4.12 · 10 10 years. This long half-life allows the nuclide pair 187 Re and 187 Os ( osmium ) to be used as a chronometer for the r-process . This idea originally came from DE Clayton . 187 Re is generated exclusively in the r process, while 187 Os is primarily generated exclusively in the S process . The S-process frequency of 187 Os can be inferred from the neighboring isotope 188 Os . The remaining 187 Os must have been created by the decay of 187 Re. The ratio of the frequencies of 187 Re and the not primarily generated 187 Os is then correlated with the beginning of r-process events in our galaxy and thus also with the age of our galaxy.

Individual evidence

  1. Smoliar, MI, Walker, RJ and Morgan, JW (1996). Re-Os ages of group IIA, IIIA, IVA, and IVB iron meteorites. Science 271, pp. 1099-1102
  2. Bosch: Observation of bound-state β- decay of fully ionized 187 Re: 187 Re- 187 Os Cosmochronometry . In: Physical Review Letters . 77, No. 26, 1996, pp. 5190-5193. doi : 10.1103 / PhysRevLett.77.5190 .