A high volume sampling system for isotope determination of volatile halocarbons and hydrocarbons

The isotopic composition of volatile organic compounds (VOCs) can provide valuable information on their sources and fate not deducible from mixing ratios alone. In particular the reported carbon stable isotope ratios of chloromethane and bromomethane from different sources cover a δ&am...

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Main Authors: E. Bahlmann, I. Weinberg, R. Seifert, C. Tubbesing, W. Michaelis
Format: Article
Language:English
Published: Copernicus Publications 2011-10-01
Series:Atmospheric Measurement Techniques
Online Access:http://www.atmos-meas-tech.net/4/2073/2011/amt-4-2073-2011.pdf
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author E. Bahlmann
I. Weinberg
R. Seifert
C. Tubbesing
W. Michaelis
author_facet E. Bahlmann
I. Weinberg
R. Seifert
C. Tubbesing
W. Michaelis
author_sort E. Bahlmann
collection DOAJ
description The isotopic composition of volatile organic compounds (VOCs) can provide valuable information on their sources and fate not deducible from mixing ratios alone. In particular the reported carbon stable isotope ratios of chloromethane and bromomethane from different sources cover a δ<sup>13</sup>C-range of almost 100‰ making isotope ratios a very promising tool for studying the biogeochemistry of these compounds. So far, the determination of the isotopic composition of C<sub>1</sub> and C<sub>2</sub> halocarbons others than chloromethane is hampered by their low mixing ratios. <br><br> In order to determine the carbon isotopic composition of C<sub>1</sub> and C<sub>2</sub> halocarbons with mixing ratios as low as 1 pptv (i) a field suitable cryogenic high volume sampling system and (ii) a chromatographic set up for processing these samples have been developed and validated. The sampling system was tested at two different sampling sites, an urban and a coastal location in Northern Germany. The average δ<sup>13</sup>C-values for bromomethane at the urban site were −42.9 ± 1.1‰ and agreed well with previously published results. But at the coastal site bromomethane was substantially enriched in <sup>13</sup>C by almost 10‰. Less pronounced differences were observed for chlorodifluoromethane, 1,1,1-trichloroethane and chloromethane. We suggest that these differences are related to the turnover of these compounds in ocean surface waters. Furthermore we report first carbon isotope ratios for iodomethane (−40.4‰ to −79.8‰), bromoform (−13.8‰ to 22.9‰), and other halocarbons.
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spelling doaj.art-b8ce00cb2d67473d846e08f0c800223d2022-12-22T00:37:14ZengCopernicus PublicationsAtmospheric Measurement Techniques1867-13811867-85482011-10-014102073208610.5194/amt-4-2073-2011A high volume sampling system for isotope determination of volatile halocarbons and hydrocarbonsE. BahlmannI. WeinbergR. SeifertC. TubbesingW. MichaelisThe isotopic composition of volatile organic compounds (VOCs) can provide valuable information on their sources and fate not deducible from mixing ratios alone. In particular the reported carbon stable isotope ratios of chloromethane and bromomethane from different sources cover a δ<sup>13</sup>C-range of almost 100‰ making isotope ratios a very promising tool for studying the biogeochemistry of these compounds. So far, the determination of the isotopic composition of C<sub>1</sub> and C<sub>2</sub> halocarbons others than chloromethane is hampered by their low mixing ratios. <br><br> In order to determine the carbon isotopic composition of C<sub>1</sub> and C<sub>2</sub> halocarbons with mixing ratios as low as 1 pptv (i) a field suitable cryogenic high volume sampling system and (ii) a chromatographic set up for processing these samples have been developed and validated. The sampling system was tested at two different sampling sites, an urban and a coastal location in Northern Germany. The average δ<sup>13</sup>C-values for bromomethane at the urban site were −42.9 ± 1.1‰ and agreed well with previously published results. But at the coastal site bromomethane was substantially enriched in <sup>13</sup>C by almost 10‰. Less pronounced differences were observed for chlorodifluoromethane, 1,1,1-trichloroethane and chloromethane. We suggest that these differences are related to the turnover of these compounds in ocean surface waters. Furthermore we report first carbon isotope ratios for iodomethane (−40.4‰ to −79.8‰), bromoform (−13.8‰ to 22.9‰), and other halocarbons.http://www.atmos-meas-tech.net/4/2073/2011/amt-4-2073-2011.pdf
spellingShingle E. Bahlmann
I. Weinberg
R. Seifert
C. Tubbesing
W. Michaelis
A high volume sampling system for isotope determination of volatile halocarbons and hydrocarbons
Atmospheric Measurement Techniques
title A high volume sampling system for isotope determination of volatile halocarbons and hydrocarbons
title_full A high volume sampling system for isotope determination of volatile halocarbons and hydrocarbons
title_fullStr A high volume sampling system for isotope determination of volatile halocarbons and hydrocarbons
title_full_unstemmed A high volume sampling system for isotope determination of volatile halocarbons and hydrocarbons
title_short A high volume sampling system for isotope determination of volatile halocarbons and hydrocarbons
title_sort high volume sampling system for isotope determination of volatile halocarbons and hydrocarbons
url http://www.atmos-meas-tech.net/4/2073/2011/amt-4-2073-2011.pdf
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