H<sub>2</sub>S interference on CO<sub>2</sub> isotopic measurements using a Picarro G1101-i cavity ring-down spectrometer

Cavity ring-down spectrometers (CRDSs) have the capacity to make isotopic measurements of CO<sub>2</sub> where concentrations range from atmospheric (~ 400 ppm) to 6000 ppm. Following field trials, it has come to light that the spectrographic lines used for CO<sub>2</sub> hav...

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Main Authors: K. Malowany, J. Stix, A. Van Pelt, G. Lucic
Format: Article
Language:English
Published: Copernicus Publications 2015-10-01
Series:Atmospheric Measurement Techniques
Online Access:http://www.atmos-meas-tech.net/8/4075/2015/amt-8-4075-2015.pdf
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author K. Malowany
J. Stix
A. Van Pelt
G. Lucic
author_facet K. Malowany
J. Stix
A. Van Pelt
G. Lucic
author_sort K. Malowany
collection DOAJ
description Cavity ring-down spectrometers (CRDSs) have the capacity to make isotopic measurements of CO<sub>2</sub> where concentrations range from atmospheric (~ 400 ppm) to 6000 ppm. Following field trials, it has come to light that the spectrographic lines used for CO<sub>2</sub> have an interference with elevated (higher than ambient) amounts of hydrogen sulfide (H<sub>2</sub>S), which causes significant depletions in the δ<sup>13</sup>C measurement by the CRDSs. In order to deploy this instrument in environments with elevated H<sub>2</sub>S concentrations (i.e., active volcanoes), we require a robust method for eliminating this interference. Controlled experiments using a Picarro G1101-i optical spectrometer were done to characterize the H<sub>2</sub>S interference at varying CO<sub>2</sub> and H<sub>2</sub>S concentrations. The addition of H<sub>2</sub>S to a CO<sub>2</sub> standard gas reveals an increase in the <sup>12</sup>CO<sub>2</sub> concentration and a more significant decrease in the <sup>13</sup>CO<sub>2</sub> concentration, resulting in a depleted δ<sup>13</sup>C value. Reacting gas samples containing H<sub>2</sub>S with copper prior to analysis can eliminate this effect. Models post-dating the G1101-i carbon isotope analyzer have maintained the same spectral lines for CO<sub>2</sub> and are likely to have a similar H<sub>2</sub>S response at elevated H<sub>2</sub>S concentrations. It is important for future work with CRDS, particularly in volcanic regions where H<sub>2</sub>S is abundant, to be aware of the H<sub>2</sub>S interference on the CO<sub>2</sub> spectroscopic lines and to remove all H<sub>2</sub>S prior to analysis. We suggest employing a scrub composed of copper to remove H<sub>2</sub>S from all gas samples that have concentrations in excess of 1 ppb.
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spelling doaj.art-c50dfae5bd4f42928c6224bf8584bde62022-12-21T17:32:31ZengCopernicus PublicationsAtmospheric Measurement Techniques1867-13811867-85482015-10-018104075408210.5194/amt-8-4075-2015H<sub>2</sub>S interference on CO<sub>2</sub> isotopic measurements using a Picarro G1101-i cavity ring-down spectrometerK. Malowany0J. Stix1A. Van Pelt2G. Lucic3Department of Earth & Planetary Sciences, McGill University, Montreal, CanadaDepartment of Earth & Planetary Sciences, McGill University, Montreal, CanadaPicarro Inc., Santa Clara, CA, USADepartment of Earth & Planetary Sciences, McGill University, Montreal, CanadaCavity ring-down spectrometers (CRDSs) have the capacity to make isotopic measurements of CO<sub>2</sub> where concentrations range from atmospheric (~ 400 ppm) to 6000 ppm. Following field trials, it has come to light that the spectrographic lines used for CO<sub>2</sub> have an interference with elevated (higher than ambient) amounts of hydrogen sulfide (H<sub>2</sub>S), which causes significant depletions in the δ<sup>13</sup>C measurement by the CRDSs. In order to deploy this instrument in environments with elevated H<sub>2</sub>S concentrations (i.e., active volcanoes), we require a robust method for eliminating this interference. Controlled experiments using a Picarro G1101-i optical spectrometer were done to characterize the H<sub>2</sub>S interference at varying CO<sub>2</sub> and H<sub>2</sub>S concentrations. The addition of H<sub>2</sub>S to a CO<sub>2</sub> standard gas reveals an increase in the <sup>12</sup>CO<sub>2</sub> concentration and a more significant decrease in the <sup>13</sup>CO<sub>2</sub> concentration, resulting in a depleted δ<sup>13</sup>C value. Reacting gas samples containing H<sub>2</sub>S with copper prior to analysis can eliminate this effect. Models post-dating the G1101-i carbon isotope analyzer have maintained the same spectral lines for CO<sub>2</sub> and are likely to have a similar H<sub>2</sub>S response at elevated H<sub>2</sub>S concentrations. It is important for future work with CRDS, particularly in volcanic regions where H<sub>2</sub>S is abundant, to be aware of the H<sub>2</sub>S interference on the CO<sub>2</sub> spectroscopic lines and to remove all H<sub>2</sub>S prior to analysis. We suggest employing a scrub composed of copper to remove H<sub>2</sub>S from all gas samples that have concentrations in excess of 1 ppb.http://www.atmos-meas-tech.net/8/4075/2015/amt-8-4075-2015.pdf
spellingShingle K. Malowany
J. Stix
A. Van Pelt
G. Lucic
H<sub>2</sub>S interference on CO<sub>2</sub> isotopic measurements using a Picarro G1101-i cavity ring-down spectrometer
Atmospheric Measurement Techniques
title H<sub>2</sub>S interference on CO<sub>2</sub> isotopic measurements using a Picarro G1101-i cavity ring-down spectrometer
title_full H<sub>2</sub>S interference on CO<sub>2</sub> isotopic measurements using a Picarro G1101-i cavity ring-down spectrometer
title_fullStr H<sub>2</sub>S interference on CO<sub>2</sub> isotopic measurements using a Picarro G1101-i cavity ring-down spectrometer
title_full_unstemmed H<sub>2</sub>S interference on CO<sub>2</sub> isotopic measurements using a Picarro G1101-i cavity ring-down spectrometer
title_short H<sub>2</sub>S interference on CO<sub>2</sub> isotopic measurements using a Picarro G1101-i cavity ring-down spectrometer
title_sort h sub 2 sub s interference on co sub 2 sub isotopic measurements using a picarro g1101 i cavity ring down spectrometer
url http://www.atmos-meas-tech.net/8/4075/2015/amt-8-4075-2015.pdf
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