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Invalidation of the Intracavity Optogalvanic Method for Radiocarbon Detection

Published online by Cambridge University Press:  09 February 2016

Cantwell G Carson
Affiliation:
Earth and Environmental Engineering Department, Columbia University, New York, New York, USA. National Energy Technology Laboratory, U.S. Dept. of Energy, Pittsburgh, Pennsylvania, USA.
Martin Stute
Affiliation:
Department of Environmental Science, Barnard College, New York, New York, USA.
Yinghuang Ji
Affiliation:
Earth and Environmental Engineering Department, Columbia University, New York, New York, USA.
Roseline Polle
Affiliation:
École Polytechnique, Palaiseau, Île-de-France, France. Imperial College London, London, UK.
Arthur Reboul
Affiliation:
École Polytechnique, Palaiseau, Île-de-France, France. Neoen, Paris, Île-de-France, France.
Klaus S Lackner
Affiliation:
Earth and Environmental Engineering Department, Columbia University, New York, New York, USA. The Center for Negative Carbon Emissions, Arizona State University, Tempe, Arizona, USA.
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Abstract

The intracavity optogalvanic spectroscopy (ICOGS) method has been reported to quantify radiocarbon at subambient levels (<1 part per trillion). ICOGS uses a gas sample that is ionized in a low-pressure glow discharge located inside a 14CO2 laser cavity to detect changes in the discharge current under periodic modulation of the laser power to determine the 14CO2 concentration of the sample. When claims of detection thresholds below ambient levels were not verified by other researchers, we constructed a theoretical analysis to resolve differences between these conflicting reports and built and tested an ICOGS system to establish a lower limit of detection. Using a linear absorbance model of the background contribution of 12CO2 and data from the HITRAN database, we estimate that the limit of detection (3σ x ) is close to 1.5×104 Modern. By measuring a 1.5×104 Modern enriched CO2 sample in a cavity modulation ICOGS system without a clear signal, we conclude that for this system the limit of detection for ICOGS must be above 1.5×104. The implications for previous ICOGS reports are discussed.

Information

Type
Research Article
Copyright
© 2016 by the Arizona Board of Regents on behalf of the University of Arizona 
Figure 0

Figure 1 The theoretical absorbance profiles for pure 12CO2 (dashed lines) and for a 1 Modern concentration of 14CO2 (dotted lines) for a 14CO2 laser operating at the P(20)e line (left) and the P(24)e line (right). The contribution of P(19)e is clearly visible in the asymmetry of the 12CO2 response to a 14CO2 P(20)e laser line.

Figure 1

Figure 2 A schematic diagram of the experimental apparatus is shown. The laser output power, modulation amplitude and phase, and wavelength are all monitored with a thermopile, photodiode, and infrared camera at PD 1, 2, and 3, respectively.

Figure 2

Figure 3 The comparison of the differential amplifier used in the original results (gray) and that used in the present work (black). Note the sharp spike at shortly after the laser switches on and off.

Figure 3

Figure 4 (A) The amplitude of the modulation in the output of the laser, as measured by the fast response pyrometer. (B) The optogalvanic response is shown with a log scale on the y axis. Beneath these, the difference between the two samples is shown on a linear y axis (inset, right). Gaussian fits of two samples (dashed line and dotted line) at P(24)e are also shown for the dead and enriched samples, respectively.

Figure 4

Figure 5 An Allan deviation curve collected at the P(24)e line of 14CO2 is shown for the 14C-enriched sample. Over the first 100 s, the deviation decreases as τ−0.49, which is consistent with white noise. At 1000 s, the deviation is 37 ppm of the signal relative to the P(20)e laser line peak

Figure 5

Figure 6 The 14CO2 optogalvanic signal relative to that of dead CO2 is shown as a function of 14C concentration for results from three different publications, Murnick et al. (2010) at P(20)e (■), Eliers et al. (2013) at P(20)e (●), and the present results at P(24)e (). The pressures for the three results were 1, 1, and 1.3 mbar, respectively.

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