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14C Blank Corrections for 25–100 μg Samples at the National Ocean Sciences AMS Laboratory

Published online by Cambridge University Press:  22 July 2019

M L Roberts*
Affiliation:
Woods Hole Oceanographic Institution, Department of Geology and Geophysics, Woods Hole, MA 02543USA
K L Elder
Affiliation:
Woods Hole Oceanographic Institution, Department of Geology and Geophysics, Woods Hole, MA 02543USA
W J Jenkins
Affiliation:
Woods Hole Oceanographic Institution, Department of Geology and Geophysics, Woods Hole, MA 02543USA
A R Gagnon
Affiliation:
Woods Hole Oceanographic Institution, Department of Geology and Geophysics, Woods Hole, MA 02543USA
L Xu
Affiliation:
Woods Hole Oceanographic Institution, Department of Geology and Geophysics, Woods Hole, MA 02543USA
J D Hlavenka
Affiliation:
Woods Hole Oceanographic Institution, Department of Geology and Geophysics, Woods Hole, MA 02543USA
B E Longworth
Affiliation:
Woods Hole Oceanographic Institution, Department of Geology and Geophysics, Woods Hole, MA 02543USA
*
*Corresponding author. Email: mroberts@whoi.edu.
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Abstract

Replicate radiocarbon (14C) measurements of organic and inorganic control samples, with known Fraction Modern values in the range Fm = 0–1.5 and mass range 6 μg–2 mg carbon, are used to determine both the mass and radiocarbon content of the blank carbon introduced during sample processing and measurement in our laboratory. These data are used to model, separately for organic and inorganic samples, the blank contribution and subsequently “blank correct” measured unknowns in the mass range 25–100 μg. Data, formulas, and an assessment of the precision and accuracy of the blank correction are presented.

Information

Type
Conference Paper
Creative Commons
Creative Common License - CCCreative Common License - BYCreative Common License - NCCreative Common License - SA
This is a work of the U.S. Government and is not subject to copyright protection in the United States.
Copyright
© 2019 by the Arizona Board of Regents on behalf of the University of Arizona
Figure 0

Figure 1 Uncorrected Fm values of FIRI H wood (Panel A, upper plot) and a “radiocarbon-free” acetanilide (Panel B, lower plot) versus manometrically determined sample mass. For the acetanilide, the solid line represents the “large-mass” blank. The dashed lines represent the “mass-balance” blank.

Figure 1

Table 1 Calculated mass balance and large mass blank values for samples processed on NOSAMS’s “small-sample” graphitization line.

Figure 2

Figure 2 A subset of inorganic secondary standards processed on NOSAMS’s “small-sample” line. The black lines are expected results using the blank and mass-balance values listed in Table 1. The gray lines show model sensitivity to the contaminant Fm (dark gray, ±0.41) and mass (light gray, ±0.42 μg).

Figure 3

Figure 3 A subset of organic secondary standards processed on NOSAMS’s “small-sample” line. The black lines are expected results using the blank and mass balance values listed in Table 1. The gray lines show model sensitivity to the contaminant Fm (dark gray, ±0.18) and mass (light gray, ±0.84 μg).

Figure 4

Figure 4 Uncorrected and corrected data from TIRI K and FIRI C (Turbidite Carbonate). The solid line is the consensus value of Fm = 0.1043.

Figure 5

Figure 5 Corrected and uncorrected data from the organic sample C-8 (Oxalic Acid). The solid line is the consensus value of Fm = 0.1503.

Figure 6

Table 2 Reduced chi-squared statistics calculated before and after blank and mass balance blank correction. See text.