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Phys. Rev. Lett. 93, 172501 (2004) [4 pages]

New Half-Life Measurement of 182Hf: Improved Chronometer for the Early Solar System

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C. Vockenhuber1,*, F. Oberli2, M. Bichler3, I. Ahmad4, G. Quitté2, M. Meier2, A. N. Halliday2, D.-C. Lee5, W. Kutschera1, P. Steier1, R. J. Gehrke6, and R. G. Helmer6
1Vienna Environmental Research Accelerator (VERA), Institut für Isotopenforschung und Kernphysik, Universität Wien, Währinger Strasse 17, A-1090 Wien, Austria
2Department of Earth Sciences, ETH-Zentrum, Sonneggstrasse 5, CH-8092 Zürich, Switzerland
3Atominstitut der Österreichischen Universitäten, Stadionallee 2, A-1020 Wien, Austria
4Physics Division, Argonne National Laboratory, 9700 S. Cass Avenue, Argonne, Illinois 60439, USA
5Institute of Earth Sciences, Academia Sinica, Nankang, Taipei 115, Taiwan, Republic of China
6Idaho National Engineering and Environmental Laboratory, 2525 Fremont Avenue, Idaho Falls, Idaho 83415, USA

Received 27 May 2004; published 20 October 2004

The decay of 182Hf, now extinct, into stable 182W has developed into an important chronometer for studying early solar system processes such as the accretion and differentiation of planetesimals and the formation of the Earth and the Moon. The only 182Hf half-life measurements available were performed 40 years ago and resulted in an imprecise half-life of (9±2)×106   yr. We redetermined the half-life by measuring the specific activity of 182Hf based on two independent methods, resulting in a value of t1/2(182Hf)=(8.90±0.09)×106   yr, in good agreement with the previous value, but with a 20 times smaller uncertainty. The greatly improved precision of this half-life now permits very precise intercalibration of the 182Hf182W isotopic system with other chronometers.

© 2004 The American Physical Society

URL:
http://link.aps.org/doi/10.1103/PhysRevLett.93.172501
DOI:
10.1103/PhysRevLett.93.172501
PACS:
21.10.Tg, 27.70.+q, 91.35.Nm, 96.35.Cp

*Electronic address: christof.vockenhuber@univie.ac.at