Simultaneous stable isotope analysis of methane and nitrous oxide on ice core samples

Methane and nitrous oxide are important greenhouse gases which show a strong increase in atmospheric mixing ratios since pre-industrial time as well as large variations during past climate changes. The understanding of their biogeochemical cycles can be improved using stable isotope analysis. Howeve...

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Published in:Atmospheric Measurement Techniques
Main Authors: Sapart, C. J., Veen, C., Vigano, I., Brass, M., Wal, R. S. W., Bock, M., Fischer, H., Sowers, T., Buizert, C., Sperlich, P., Blunier, T., Behrens, M., Schmitt, J., Seth, B., Röckmann, T.
Format: Text
Language:English
Published: 2018
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Online Access:https://doi.org/10.5194/amt-4-2607-2011
https://amt.copernicus.org/articles/4/2607/2011/
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spelling ftcopernicus:oai:publications.copernicus.org:amt11861 2023-05-15T16:38:47+02:00 Simultaneous stable isotope analysis of methane and nitrous oxide on ice core samples Sapart, C. J. Veen, C. Vigano, I. Brass, M. Wal, R. S. W. Bock, M. Fischer, H. Sowers, T. Buizert, C. Sperlich, P. Blunier, T. Behrens, M. Schmitt, J. Seth, B. Röckmann, T. 2018-01-15 application/pdf https://doi.org/10.5194/amt-4-2607-2011 https://amt.copernicus.org/articles/4/2607/2011/ eng eng doi:10.5194/amt-4-2607-2011 https://amt.copernicus.org/articles/4/2607/2011/ eISSN: 1867-8548 Text 2018 ftcopernicus https://doi.org/10.5194/amt-4-2607-2011 2020-07-20T16:25:57Z Methane and nitrous oxide are important greenhouse gases which show a strong increase in atmospheric mixing ratios since pre-industrial time as well as large variations during past climate changes. The understanding of their biogeochemical cycles can be improved using stable isotope analysis. However, high-precision isotope measurements on air trapped in ice cores are challenging because of the high susceptibility to contamination and fractionation. Here, we present a dry extraction system for combined CH 4 and N 2 O stable isotope analysis from ice core air, using an ice grating device. The system allows simultaneous analysis of δD(CH 4 ) or δ 13 C(CH 4 ), together with δ 15 N(N 2 O), δ 18 O(N 2 O) and δ 15 N(NO + fragment) on a single ice core sample, using two isotope mass spectrometry systems. The optimum quantity of ice for analysis is about 600 g with typical "Holocene" mixing ratios for CH 4 and N 2 O. In this case, the reproducibility (1σ ) is 2.1‰ for δD(CH 4 ), 0.18‰ for δ 13 C(CH 4 ), 0.51‰ for δ 15 N(N 2 O), 0.69‰ for δ 18 O(N 2 O) and 1.12‰ for δ 15 N(NO + fragment). For smaller amounts of ice the standard deviation increases, particularly for N 2 O isotopologues. For both gases, small-scale intercalibrations using air and/or ice samples have been carried out in collaboration with other institutes that are currently involved in isotope measurements of ice core air. Significant differences are shown between the calibration scales, but those offsets are consistent and can therefore be corrected for. Text ice core Copernicus Publications: E-Journals Atmospheric Measurement Techniques 4 12 2607 2618
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collection Copernicus Publications: E-Journals
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language English
description Methane and nitrous oxide are important greenhouse gases which show a strong increase in atmospheric mixing ratios since pre-industrial time as well as large variations during past climate changes. The understanding of their biogeochemical cycles can be improved using stable isotope analysis. However, high-precision isotope measurements on air trapped in ice cores are challenging because of the high susceptibility to contamination and fractionation. Here, we present a dry extraction system for combined CH 4 and N 2 O stable isotope analysis from ice core air, using an ice grating device. The system allows simultaneous analysis of δD(CH 4 ) or δ 13 C(CH 4 ), together with δ 15 N(N 2 O), δ 18 O(N 2 O) and δ 15 N(NO + fragment) on a single ice core sample, using two isotope mass spectrometry systems. The optimum quantity of ice for analysis is about 600 g with typical "Holocene" mixing ratios for CH 4 and N 2 O. In this case, the reproducibility (1σ ) is 2.1‰ for δD(CH 4 ), 0.18‰ for δ 13 C(CH 4 ), 0.51‰ for δ 15 N(N 2 O), 0.69‰ for δ 18 O(N 2 O) and 1.12‰ for δ 15 N(NO + fragment). For smaller amounts of ice the standard deviation increases, particularly for N 2 O isotopologues. For both gases, small-scale intercalibrations using air and/or ice samples have been carried out in collaboration with other institutes that are currently involved in isotope measurements of ice core air. Significant differences are shown between the calibration scales, but those offsets are consistent and can therefore be corrected for.
format Text
author Sapart, C. J.
Veen, C.
Vigano, I.
Brass, M.
Wal, R. S. W.
Bock, M.
Fischer, H.
Sowers, T.
Buizert, C.
Sperlich, P.
Blunier, T.
Behrens, M.
Schmitt, J.
Seth, B.
Röckmann, T.
spellingShingle Sapart, C. J.
Veen, C.
Vigano, I.
Brass, M.
Wal, R. S. W.
Bock, M.
Fischer, H.
Sowers, T.
Buizert, C.
Sperlich, P.
Blunier, T.
Behrens, M.
Schmitt, J.
Seth, B.
Röckmann, T.
Simultaneous stable isotope analysis of methane and nitrous oxide on ice core samples
author_facet Sapart, C. J.
Veen, C.
Vigano, I.
Brass, M.
Wal, R. S. W.
Bock, M.
Fischer, H.
Sowers, T.
Buizert, C.
Sperlich, P.
Blunier, T.
Behrens, M.
Schmitt, J.
Seth, B.
Röckmann, T.
author_sort Sapart, C. J.
title Simultaneous stable isotope analysis of methane and nitrous oxide on ice core samples
title_short Simultaneous stable isotope analysis of methane and nitrous oxide on ice core samples
title_full Simultaneous stable isotope analysis of methane and nitrous oxide on ice core samples
title_fullStr Simultaneous stable isotope analysis of methane and nitrous oxide on ice core samples
title_full_unstemmed Simultaneous stable isotope analysis of methane and nitrous oxide on ice core samples
title_sort simultaneous stable isotope analysis of methane and nitrous oxide on ice core samples
publishDate 2018
url https://doi.org/10.5194/amt-4-2607-2011
https://amt.copernicus.org/articles/4/2607/2011/
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genre_facet ice core
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https://amt.copernicus.org/articles/4/2607/2011/
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container_title Atmospheric Measurement Techniques
container_volume 4
container_issue 12
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