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Sealed Tube Combustion Method with MnO2 for AMS 14C Measurement

Published online by Cambridge University Press:  19 November 2018

Róbert Janovics*
Affiliation:
Isotope Climatology and Environmental Research Centre, Institute for Nuclear Research Debrecen, Hungary
István Futó
Affiliation:
Isotope Climatology and Environmental Research Centre, Institute for Nuclear Research Debrecen, Hungary
Mihály Molnár
Affiliation:
Isotope Climatology and Environmental Research Centre, Institute for Nuclear Research Debrecen, Hungary
*
*Corresponding author. Email: janovics@atomki.hu.
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Abstract

An effective sealed tube combustion method was designed with an MnO2 oxidant for accelerator mass spectrometry radiocarbon (AMS 14C) measurements. Different types of materials (oxalic acid, cellulose, sucrose, wood, collagen, graphite, and humic acid) were used to test the method. A normal borosilicate glass tube was used instead of quartz and the combustion was done at 550ºC. The yield of the combustion is above 98% even in the case of the less combustible material such as graphite. The MnO2 reagent does not introduce detectable carbon contamination. The typical background is 0.29±0.20 pMC in the case of 200 µg carbon, measured as solid graphite target. With direct measurement of the CO2 by gas ion source AMS, the method is applicable up to 50 µg of carbon with an acceptable (~1 pMC) 14C background. A new type of tube cracker was developed for a quick chipless method of tube cracking and sample changing. In this way, the gas handling process takes only 5–6 min/sample.

Information

Type
Instrumentation and Calibration
Copyright
© 2018 by the Arizona Board of Regents on behalf of the University of Arizona 
Figure 0

Table 1 Tested reference materials.

Figure 1

Figure 1 Gas-handling line with the glass tube cracker.

Figure 2

Table 2 Carbon recovery yield of the combusted samples (n=5).

Figure 3

Figure 2 Sample mass dependency of the carbon recovery from 0.2 mg to 5 mg.

Figure 4

Figure 3 Mass scan of the purified CO2 from the combustion of sulphanilamide.

Figure 5

Figure 4 14C results of the 0.5–0.5 mg fossil CO2 and the OXA II samples in the function of the added MnO2 (dashed line: consensus value of the OXA II 134.07 pMC).

Figure 6

Figure 5 Deviation of the measured 14C values from the consensus value *: name of the reference material, **consensus values (Gröning 2007; Scott et al. 2010).

Figure 7

Figure 6 Deviation of the GIS-AMS results from the expected values, without blank correction (a. borehole CO2; b. IAEA-C7).