Greenhouse gas formation in ice wedges at Cyuie, central Yakutia

Greenhouse gases (GHGs) trapped in ice wedges may provide useful information on biogeochemical environments in ground ice. Previous studies have reported highly elevated CO2 and CH4 mixing ratios in ice wedges. However, N2O mixing ratios in ice wedges remain unknown. Here, we present CO2, CH4 and N2...

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Bibliographic Details
Published in:Permafrost and periglacial processes 2019-01, Vol.30 (1), p.48-57
Main Authors: Kim, Kyungmin, Yang, Ji‐Woong, Yoon, Hyunsuk, Byun, Eunji, Fedorov, Alexander, Ryu, Yeongjun, Ahn, Jinho
Format: Article
Language:English
Subjects:
Biogeochemistry
Bubbles
Carbon dioxide
Central Siberia
Gas formation
Gases
Greenhouse effect
greenhouse gas
Greenhouse gases
Ground ice
Ice
Ice formation
ice wedge
Ice wedges
Last Glacial Maximum
Methane
Mixing ratio
Nitrous oxide
Snowmelt
Wedges
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Summary:Greenhouse gases (GHGs) trapped in ice wedges may provide useful information on biogeochemical environments in ground ice. Previous studies have reported highly elevated CO2 and CH4 mixing ratios in ice wedges. However, N2O mixing ratios in ice wedges remain unknown. Here, we present CO2, CH4 and N2O mixing ratios in bubbles and plausible mechanisms of GHG formation for two lakeside ice wedges at Cyuie village near Yakutsk. The CO2 gas age corresponds to the Last Glacial Maximum (18–19 ka). The δ(N2/Ar) values and bubble shapes indicate that the ice wedges formed by dry snow compaction rather than snowmelt water refreezing, while the δ18O and δD values of the ice indicate changes in the source area location and/or the climate during the Last Glacial Maximum. Using a dry extraction method, we obtained gas mixing ratios of 7–13% CO2, 5–130 ppm CH4 and 100–5000 ppb N2O. The δ(O2/Ar) values imply that most of the O2 was consumed by biological respiration. The CH4 is negatively correlated with N2O and CO2. The N2O might have inhibited CH4 production.
ISSN:1045-6740
1099-1530
DOI:10.1002/ppp.1994