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

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

Air bubbles in ice core samples represent the only opportunity to study the mixing ratio and isotopic variability of palaeoatmospheric CH<sub>4</sub> and N<sub>2</sub>O. The highest possible precision in isotope measurements is required to maximize the resolving power for CH&...

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Bibliographic Details
Main Authors: P. Sperlich, C. Buizert, T. M. Jenk, C. J. Sapart, M. Prokopiou, T. Röckmann, T. Blunier
Format: Article
Language:English
Published: Copernicus Publications 2013-08-01
Series:Atmospheric Measurement Techniques
Online Access:http://www.atmos-meas-tech.net/6/2027/2013/amt-6-2027-2013.pdf

Internet

http://www.atmos-meas-tech.net/6/2027/2013/amt-6-2027-2013.pdf

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