Permafrost aggradation and methane production in low accumulative laidas (tidal flats) of the Kara Sea
- Authors: Vasiliev A.A.1,2, Melnikov V.P.1,2,3, Streletskaya I.D.4, Oblogov G.E.1,2
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Affiliations:
- Institute of the Earth’s Cryosphere, Siberian Branch
- Tyumen State University
- Tyumen Scientific Center, Siberian Branch
- Moscow State University
- Issue: Vol 476, No 1 (2017)
- Pages: 1069-1072
- Section: Geography
- URL: https://journals.rcsi.science/1028-334X/article/view/190857
- DOI: https://doi.org/10.1134/S1028334X17090203
- ID: 190857
Cite item
Abstract
It was established that along with permafrost degradation, the processes of permafrost aggradation occur in the modern low accumulative surfaces of Kara Sea. The cycle of observation over the permafrost thermal regime was performed. The mean annual temperatire of the permafrost varies from – 3.5 to – 4.8°C; the thermal flux into the permafrost can reach 8 W/m2. The methane genesis process is realized only in the seasonally thawed layer. It was found that temperature – 4.0°C is threshold for the bacterial methane production.
About the authors
A. A. Vasiliev
Institute of the Earth’s Cryosphere, Siberian Branch; Tyumen State University
Author for correspondence.
Email: al.a.vasiliev@gmail.com
Russian Federation, Tyumen, 625000; Tyumen
V. P. Melnikov
Institute of the Earth’s Cryosphere, Siberian Branch; Tyumen State University; Tyumen Scientific Center, Siberian Branch
Email: al.a.vasiliev@gmail.com
Russian Federation, Tyumen, 625000; Tyumen; Tyumen
I. D. Streletskaya
Moscow State University
Email: al.a.vasiliev@gmail.com
Russian Federation, Moscow
G. E. Oblogov
Institute of the Earth’s Cryosphere, Siberian Branch; Tyumen State University
Email: al.a.vasiliev@gmail.com
Russian Federation, Tyumen, 625000; Tyumen