Atmospheric Measurement Techniques (Dec 2011)

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

  • C. J. Sapart,
  • C. van der Veen,
  • I. Vigano,
  • M. Brass,,
  • R. S. W. van de Wal,
  • M. Bock,
  • H. Fischer,
  • T. Sowers,
  • C. Buizert,
  • P. Sperlich,
  • T. Blunier,
  • M. Behrens,
  • J. Schmitt,
  • B. Seth,
  • T. Röckmann

DOI
https://doi.org/10.5194/amt-4-2607-2011
Journal volume & issue
Vol. 4, no. 12
pp. 2607 – 2618

Abstract

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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. <br><br> Here, we present a dry extraction system for combined CH<sub>4</sub> and N<sub>2</sub>O stable isotope analysis from ice core air, using an ice grating device. The system allows simultaneous analysis of &delta;D(CH<sub>4</sub>) or &delta;<sup>13</sup>C(CH<sub>4</sub>), together with &delta;<sup>15</sup>N(N<sub>2</sub>O), &delta;<sup>18</sup>O(N<sub>2</sub>O) and &delta;<sup>15</sup>N(NO<sup>+</sup> 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<sub>4</sub> and N<sub>2</sub>O. In this case, the reproducibility (1&sigma; ) is 2.1&permil; for &delta;D(CH<sub>4</sub>), 0.18&permil; for &delta;<sup>13</sup>C(CH<sub>4</sub>), 0.51&permil; for &delta;<sup>15</sup>N(N<sub>2</sub>O), 0.69&permil; for &delta;<sup>18</sup>O(N<sub>2</sub>O) and 1.12&permil; for &delta;<sup>15</sup>N(NO<sup>+</sup> fragment). For smaller amounts of ice the standard deviation increases, particularly for N<sub>2</sub>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.