Affiliation:
1. Institut für Kernphysik, Universität Münster
Abstract
Abstract
Because of the discrepancies between different determinations of the half-life T of 87Rb and the importance of T for measuring geological ages we decided to compare the separated isotopes. All experimental errors are the same in both cases, and the difference of the counting rates has to be attributed to 87Rb. In this manner we got T = (4.88 + 0.10) • 1010 y
Subject
Physical and Theoretical Chemistry,General Physics and Astronomy,Mathematical Physics
Cited by
5 articles.
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