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Atmosphere 2017, 8(6), 105; doi:10.3390/atmos8060105

Cryogenic Displacement and Accumulation of Biogenic Methane in Frozen Soils

Centre of Forest Ecology and Productivity, Russian Academy of Sciences, Moscow 117997, Russia
Department of Biogeochemical Processes, Max Planck Institute for Biogeochemistry, Jena 07745, Germany
Institute of Earth Sciences, Saint Petersburg State University, Saint Petersburg 199034, Russia
Nansen Centre, Saint Petersburg 199034, Russia
Geophysical Institute, University of Alaska Fairbanks, Fairbanks, AK 99775-9320, USA
Institute of Physicochemical and Biological Problems in Soil Science, Russian Academy of Sciences, Pushchino 142290, Russia
Faculty of Geology, Lomonosov Moscow State University, Moscow 119992, Russia
Author to whom correspondence should be addressed.
Received: 28 March 2017 / Revised: 8 June 2017 / Accepted: 9 June 2017 / Published: 15 June 2017
(This article belongs to the Special Issue Atmospheric Methane)
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Evidences of highly localized methane fluxes are reported from the Arctic shelf, hot spots of methane emissions in thermokarst lakes, and are believed to evolve to features like Yamal crater on land. The origin of large methane outbursts is problematic. Here we show, that the biogenic methane (13C ≤ −71‰) which formed before and during soil freezing is presently held in the permafrost. Field and experimental observations show that methane tends to accumulate at the permafrost table or in the coarse-grained lithological pockets surrounded by the sediments less-permeable for gas. Our field observations, radiocarbon dating, laboratory tests and theory all suggest that depending on the soil structure and freezing dynamics, this methane may have been displaced downwards tens of meters during freezing and has accumulated in the lithological pockets. The initial flux of methane from the one pocket disclosed by drilling was at a rate of more than 2.5 kg C(CH4) m−2 h−1. The age of the methane was 8–18 thousand years younger than the age of the sediments, suggesting that it was displaced tens of meters during freezing. The theoretical background provided the insight on the cryogenic displacement of methane in support of the field and experimental data. Upon freezing of sediments, methane follows water migration and either dissipates in the freezing soils or concentrates at certain places controlled by the freezing rate, initial methane distribution and soil structure. View Full-Text
Keywords: permafrost degradation; freezing soils; cryogenic migration; biogenic methane; Yamal crater; methane hydrates; freezing front; Yedoma; transition layer permafrost degradation; freezing soils; cryogenic migration; biogenic methane; Yamal crater; methane hydrates; freezing front; Yedoma; transition layer

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This is an open access article distributed under the Creative Commons Attribution License which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. (CC BY 4.0).

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Kraev, G.; Schulze, E.-D.; Yurova, A.; Kholodov, A.; Chuvilin, E.; Rivkina, E. Cryogenic Displacement and Accumulation of Biogenic Methane in Frozen Soils. Atmosphere 2017, 8, 105.

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