Clean quartz matters for cosmogenic nuclide analyses: An exploration of the importance of sample purity using the CRONUS-N reference material

被引:5
作者
Corbett, Lee B. [1 ]
Bierman, Paul R. [1 ]
Brown, Thomas A. [2 ]
Caffee, Marc W. [3 ,4 ]
Fink, David [5 ]
Freeman, Stewart P. H. T. [6 ]
Hidy, Alan J. [2 ]
Rood, Dylan H. [7 ]
Wilcken, Klaus M. [5 ]
Woodruff, Thomas E. [3 ]
机构
[1] Univ Vermont, Rubenstein Sch Environm & Nat Resources, Burlington, VT 05405 USA
[2] Lawrence Livermore Natl Lab, Ctr Accelerator Mass Spectrometry, Livermore, CA USA
[3] Purdue Univ, Dept Phys & Astron, W Lafayette, IN USA
[4] Purdue Univ, Dept Earth Atmospher & Planetary Sci, W Lafayette, IN USA
[5] Australian Nucl Sci & Technol Org, Lucas Heights, NSW, Australia
[6] Scottish Univ Environm Res Ctr, East Kilbride, Scotland
[7] Imperial Coll London, Dept Earth Sci & Engn, South Kensington Campus, London, England
基金
美国国家科学基金会;
关键词
Geochronology; Cosmogenic nuclides; Accelerator mass spectrometry; Quality control; ACCELERATOR MASS-SPECTROMETRY; SITU-PRODUCED BE-10; AL-26; ANALYSIS; EROSION; RATES; EXPOSURE; PROFILES; SEDIMENT; QUALITY; BURIAL;
D O I
10.1016/j.quageo.2022.101403
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Reference materials are key for assessing inter-laboratory variability and measurement quality, and for placing analytical uncertainty bounds on sample analyses. Here, we investigate four years of data resulting from repeated processing of the CRONUS-N reference material for cosmogenic 10Be and 26Al analyses. At University of Vermont, we prepared a CRONUS-N aliquot with most of our sample batches from 2013 to 2017; these reference material samples were then distributed to four different accelerator mass spectrometry facilities, yielding 7310Be analyses and 58 26Al analyses. We determine CRONUS-N 10Be concentrations of (2.26 +/- 0.14) x 105 atoms g-1 (n = 73, mean, 1 SD) and 26Al concentrations of (1.00 +/- 0.08) x 106 atoms g-1 (n = 58, mean, 1 SD). We find a reproducibility of 6.3% for 10Be and 7.7% for 26Al (relative standard deviations). We also document highly variable 27Al and Mg concentrations and a 10Be dispersion twice as large as the mean AMS analytic uncertainty. Analyses of the CRONUS-N material with and without density separation demonstrate that non-quartz minerals are present in the material and have a large impact on measured concentrations of 27Al, 10Be, and impurities; these non-quartz minerals represent only a very small portion of the total mass (0.6-0.8%) but have a dis-proportionally large effect on the resulting data. Our results highlight the importance of completely removing all non-quartz mineral phases from samples prior to Be/Al extraction for the determination of in situ cosmogenic 10Be and 26Al concentrations.
引用
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页数:12
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