IUPAC-IUGS status report on the half-lives of 238U, 235U and 234U

被引:29
|
作者
Villa, I. M. [1 ,2 ,4 ,5 ]
Bonardi, M. L. [1 ,3 ,6 ,7 ]
De Bievre, P. [1 ,3 ,8 ]
Holden, N. E. [1 ,3 ,9 ]
Renne, P. R. [1 ,2 ,10 ,11 ]
机构
[1] Univ Bern, Inst Geol, Joint IUPAC IUGS Task Grp Isotope Data Geosci, CH-3012 Bern, Switzerland
[2] Int Union Geol Sci, Beijing 100037, Peoples R China
[3] Int Union Pure & Appl Chem, Res Triangle Pk, NC 27709 USA
[4] Univ Bern, Inst Geol, CH-3012 Bern, Switzerland
[5] Univ Milano Bicocca, Ctr Univ Dataz & Archeometria, I-20126 Milan, Italy
[6] Univ Milan, LASA, I-20090 Segrate, Italy
[7] INFN, I-20090 Segrate, Italy
[8] Metrology, Chem, B-2460 Kasterlee, Belgium
[9] Brookhaven Natl Lab, Natl Nucl Data Ctr, Upton, NY 11973 USA
[10] Berkeley Geochronol Ctr, Berkeley, CA 94720 USA
[11] Univ Calif Berkeley, Dept Earth & Planetary Sci, Berkeley, CA 94720 USA
关键词
CA-TIMS METHOD; DECAY CONSTANTS; ISOTOPIC COMPOSITION; ATOMIC WEIGHTS; PB; MASS; FRACTIONATION; GEOCHRONOLOGY; PRECISION; ZIRCON;
D O I
10.1016/j.gca.2015.10.011
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The current state of knowledge on the half-lives of the long-lived U radionuclides has been reviewed by the IUPAC-IUGS joint Task Group "Isotopes in Geosciences". U-238 is assigned a half-life of (4.4683 +/- 0.0096) Ga, i.e. a decay constant lambda(238) = (0.155125 +/- 0.000333) Ga-1. The coverage factor is k = 2 for this and all other estimates presented here. The U-238 half-life can be used as a reference for the half-lives/decay constants of all other isotopic geochronometers. A revision of the half-life of U-235 based on intercomparison of natural geological samples is premature. The improved repeatability of mass spectrometric measurements has revealed Type B uncertainties that had been dismissed as subordinate in the past. The combined uncertainty of these as yet incompletely charted and quantified sources of Type B uncertainty may be no smaller than the currently accepted uncertainty of the alpha counting experiments. A provisional value for the U-234 half-life can be calculated with the assumption of secular equilibrium in the analyzed natural samples. This assumption has not yet been verified independently and its metrological traceability appears sub-optimum. A Type B evaluation suggests that the ca. 0.17% offset between the N(U-234)/N(U-238) number-ratios of the natural samples used to estimate the U-235 half-life and those of the four samples used to estimate the U-234 half-life should be compounded into the standard measurement uncertainty of the latter. The resulting provisional uncertainty interval (k = 2) for the U-234 half-life is (244.55-247.77) ka, corresponding to lambda(234) = (2.8203-2.8344) Ma(-1). (C) 2015 Elsevier Ltd. All rights reserved.
引用
收藏
页码:387 / 392
页数:6
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