Effects of molecular diffusion on trapped gas composition in polar ice cores

• Published in: Earth and planetary science letters 2005-01, Vol.229 (3), p.183-192
• Main Authors: Ikeda-Fukazawa, Tomoko, Fukumizu, Kenji, Kawamura, Kenji, Aoki, Shuji, Nakazawa, Takakiyo, Hondoh, Takeo
• Format: Article
• Language: English
• Subjects: gas analysis; gas fractionation; ice cores; molecular diffusion; paleo-atmosphere
• ISSN: 0012-821X; 1385-013X
• DOI: 10.1016/j.epsl.2004.11.011

Enrichment of nitrogen gas has been found from gas analyses of ice cores retrieved from deep parts of Antarctica. Neither climate change nor gas loss through ice cracks explain the enrichment. In order to investigate the mechanism of the gas composition change, we develop a model of gas loss caused by molecular diffusion from clathrate hydrates toward the ice-core surface through ice crystal. We apply the model to interpret the data on the gas composition change in the Dome Fuji ice core during the storage for 3 years at 248 K. The mass transfer coefficients determined using the model are 1.4×10 −9 and 4.3×10 −9 m·s −1 at 248 K for N 2 and O 2, respectively. The difference in the coefficient between N 2 and O 2 causes the change in the O 2/N 2 ratio of the trapped gas in the ice core during the storage. During the storage period of 1000 days at 248 K, the O 2/N 2 ratio changes from −9.9‰ to −20.5‰. The effect of the gas loss decreases as the storage temperature decreases. The results have important implications for the accurate reconstructions of the paleo-atmosphere from polar ice cores.