Articles | Volume 6, issue 5
https://doi.org/10.5194/amt-6-1425-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/amt-6-1425-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
27 May 2013
Research article |
| 27 May 2013
On the interference of Kr during carbon isotope analysis of methane using continuous-flow combustion–isotope ratio mass spectrometry
J. Schmitt
Climate and Environmental Physics, Physics Institute, & Oeschger Centre for Climate Change Research, University of Bern, Sidlerstrasse 5, 3012 Bern, Switzerland
Climate and Environmental Physics, Physics Institute, & Oeschger Centre for Climate Change Research, University of Bern, Sidlerstrasse 5, 3012 Bern, Switzerland
Climate and Environmental Physics, Physics Institute, & Oeschger Centre for Climate Change Research, University of Bern, Sidlerstrasse 5, 3012 Bern, Switzerland
C. van der Veen
Institute for Marine and Atmospheric research Utrecht, Utrecht University, Princetonplein 5, 3584CC Utrecht, The Netherlands
L. Möller
Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Bremerhaven, Germany
C. J. Sapart
Institute for Marine and Atmospheric research Utrecht, Utrecht University, Princetonplein 5, 3584CC Utrecht, The Netherlands
M. Prokopiou
Institute for Marine and Atmospheric research Utrecht, Utrecht University, Princetonplein 5, 3584CC Utrecht, The Netherlands
T. Sowers
Earth and Environment Systems Institute, Penn State University, University Park, PA, USA
T. Röckmann
Institute for Marine and Atmospheric research Utrecht, Utrecht University, Princetonplein 5, 3584CC Utrecht, The Netherlands
H. Fischer
Climate and Environmental Physics, Physics Institute, & Oeschger Centre for Climate Change Research, University of Bern, Sidlerstrasse 5, 3012 Bern, Switzerland
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- Real-time analysis of <i>δ</i><sup>13</sup>C- and <i>δ</i>D-CH<sub>4</sub> in ambient air with laser spectroscopy: method development and first intercomparison results S. Eyer et al. 10.5194/amt-9-263-2016
- Automated simultaneous measurement of the δ13C and δ2H values of methane and the δ13C and δ18O values of carbon dioxide in flask air samples using a new multi cryo‐trap/gas chromatography/isotope ratio mass spectrometry system W. Brand et al. 10.1002/rcm.7587
- Old carbon reservoirs were not important in the deglacial methane budget M. Dyonisius et al. 10.1126/science.aax0504
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- Marine Subsurface Microbial Community Shifts Across a Hydrothermal Gradient in Okinawa Trough Sediments L. Brandt & C. House 10.1155/2016/2690329
21 citations as recorded by crossref.
- Compound-Specific Radiocarbon Analysis of Atmospheric Methane: A New Preconcentration and Purification Setup C. Espic et al. 10.1017/RDC.2019.76
- In situ observations of the isotopic composition of methane at the Cabauw tall tower site T. Röckmann et al. 10.5194/acp-16-10469-2016
- Bipolar carbon and hydrogen isotope constraints on the Holocene methane budget J. Beck et al. 10.5194/bg-15-7155-2018
- Improving accuracy and precision of ice core δD(CH<sub>4</sub>) analyses using methane pre-pyrolysis and hydrogen post-pyrolysis trapping and subsequent chromatographic separation M. Bock et al. 10.5194/amt-7-1999-2014
- Development and evaluation of a suite of isotope reference gases for methane in air P. Sperlich et al. 10.5194/amt-9-3717-2016
- Fully automated, high‐throughput instrumentation for measuring the δ13C value of methane and application of the instrumentation to rice paddy samples T. Tokida et al. 10.1002/rcm.7016
- Application of 13CH4 double model online analysis method based on Fourier Transform Infrared Spectroscopy in energy exploration B. Wang et al. 10.1016/j.vibspec.2023.103621
- Measurements of 14C in ancient ice from Taylor Glacier, Antarctica constrain in situ cosmogenic 14CH4 and 14CO production rates V. Petrenko et al. 10.1016/j.gca.2016.01.004
- Interlaboratory comparison of <i>δ</i><sup>13</sup>C and <i>δ</i>D measurements of atmospheric CH<sub>4</sub> for combined use of data sets from different laboratories T. Umezawa et al. 10.5194/amt-11-1207-2018
- Source partitioning of atmospheric methane using stable carbon isotope measurements in the Reuss Valley, Switzerland J. Stieger et al. 10.1080/10256016.2018.1561448
- Effect of Elemental Sulfur (S8) on Carbon Isotope Analysis of n-Alkanes . Mengmeng Cao et al. 10.1134/S0016702923080049
- Real-time analysis of <i>δ</i><sup>13</sup>C- and <i>δ</i>D-CH<sub>4</sub> in ambient air with laser spectroscopy: method development and first intercomparison results S. Eyer et al. 10.5194/amt-9-263-2016
- Automated simultaneous measurement of the δ13C and δ2H values of methane and the δ13C and δ18O values of carbon dioxide in flask air samples using a new multi cryo‐trap/gas chromatography/isotope ratio mass spectrometry system W. Brand et al. 10.1002/rcm.7587
- Old carbon reservoirs were not important in the deglacial methane budget M. Dyonisius et al. 10.1126/science.aax0504
- Online technique for isotope and mixing ratios of CH<sub>4</sub>, N<sub>2</sub>O, Xe and mixing ratios of organic trace gases on a single ice core sample J. Schmitt et al. 10.5194/amt-7-2645-2014
- Carbon isotope ratios suggest no additional methane from boreal wetlands during the rapid Greenland Interstadial 21.2 P. Sperlich et al. 10.1002/2014GB005007
- Variations in global methane sources and sinks during 1910–2010 A. Ghosh et al. 10.5194/acp-15-2595-2015
- Glacial/interglacial wetland, biomass burning, and geologic methane emissions constrained by dual stable isotopic CH 4 ice core records M. Bock et al. 10.1073/pnas.1613883114
- A Cryogen-Free Automated Measurement System of Stable Carbon Isotope Ratio of Atmospheric Methane T. Umezawa et al. 10.2151/jmsj.2020-007
- A 21st-century shift from fossil-fuel to biogenic methane emissions indicated by 13 CH 4 H. Schaefer et al. 10.1126/science.aad2705
- An automated GC-C-GC-IRMS setup to measure palaeoatmospheric δ<sup>13</sup>C-CH<sub>4</sub>, δ<sup>15</sup>N-N<sub>2</sub>O and δ<sup>18</sup>O-N<sub>2</sub>O in one ice core sample P. Sperlich et al. 10.5194/amt-6-2027-2013
2 citations as recorded by crossref.
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