Gas extraction and degradation of the submarine permafrost rocks on the Laptev Sea shelf

L. I. Lobkovskiy, S. L. Nikiforov, N. N. Dmitrevskiy, N. V. Libina, I. P. Semiletov, R. A. Ananiev, A. A. Meluzov, A. G. Roslyakov

Результат исследований: Материалы для журналаСтатья

9 Цитирования (Scopus)

Выдержка

In 2011 and 2012, the interdisciplinary oceanic cruises of the R/V Akademik M.A. Lavrent’ev and R/V Viktor Buinitskii were conducted in the framework of the project of targeted basic research of the Russian Foundation for Basic Research. These studies identified strong methane jets because of the degradation of submarine permafrost rocks (SPRs), which is related to paleogeographical and modern factors of formation of the upper sedimentary sequence and also to structural peculiarities of the Arctic region. Large gas and water volumes are formed at the expense of the SPR defrosting; move along the upper sedimentary shelf sequence and along the surface of one or another layer (from coastal warmed areas to cooler deep areas); and form horizontally elongated convective cells, which activates destruction even at negative bottom temperatures. The methane emission will increase and become massive during the continuing SPR degradation.

Язык оригиналаАнглийский
Страницы (с-по)283-290
Число страниц8
ЖурналOceanology
Том55
Номер выпуска2
DOI
СостояниеОпубликовано - 1 мар 2015
Опубликовано для внешнего пользованияДа

Отпечаток

shelf sea
permafrost
degradation
methane
gas
rock
sedimentary sequence
temperature
water

ASJC Scopus subject areas

  • Oceanography

Цитировать

Lobkovskiy, L. I., Nikiforov, S. L., Dmitrevskiy, N. N., Libina, N. V., Semiletov, I. P., Ananiev, R. A., ... Roslyakov, A. G. (2015). Gas extraction and degradation of the submarine permafrost rocks on the Laptev Sea shelf. Oceanology, 55(2), 283-290. https://doi.org/10.1134/S0001437015010129

Gas extraction and degradation of the submarine permafrost rocks on the Laptev Sea shelf. / Lobkovskiy, L. I.; Nikiforov, S. L.; Dmitrevskiy, N. N.; Libina, N. V.; Semiletov, I. P.; Ananiev, R. A.; Meluzov, A. A.; Roslyakov, A. G.

В: Oceanology, Том 55, № 2, 01.03.2015, стр. 283-290.

Результат исследований: Материалы для журналаСтатья

Lobkovskiy, LI, Nikiforov, SL, Dmitrevskiy, NN, Libina, NV, Semiletov, IP, Ananiev, RA, Meluzov, AA & Roslyakov, AG 2015, 'Gas extraction and degradation of the submarine permafrost rocks on the Laptev Sea shelf', Oceanology, том. 55, № 2, стр. 283-290. https://doi.org/10.1134/S0001437015010129
Lobkovskiy LI, Nikiforov SL, Dmitrevskiy NN, Libina NV, Semiletov IP, Ananiev RA и соавт. Gas extraction and degradation of the submarine permafrost rocks on the Laptev Sea shelf. Oceanology. 2015 Март 1;55(2):283-290. https://doi.org/10.1134/S0001437015010129
Lobkovskiy, L. I. ; Nikiforov, S. L. ; Dmitrevskiy, N. N. ; Libina, N. V. ; Semiletov, I. P. ; Ananiev, R. A. ; Meluzov, A. A. ; Roslyakov, A. G. / Gas extraction and degradation of the submarine permafrost rocks on the Laptev Sea shelf. В: Oceanology. 2015 ; Том 55, № 2. стр. 283-290.
@article{aacd38db18a74c8aa6569d048fc0deeb,
title = "Gas extraction and degradation of the submarine permafrost rocks on the Laptev Sea shelf",
abstract = "In 2011 and 2012, the interdisciplinary oceanic cruises of the R/V Akademik M.A. Lavrent’ev and R/V Viktor Buinitskii were conducted in the framework of the project of targeted basic research of the Russian Foundation for Basic Research. These studies identified strong methane jets because of the degradation of submarine permafrost rocks (SPRs), which is related to paleogeographical and modern factors of formation of the upper sedimentary sequence and also to structural peculiarities of the Arctic region. Large gas and water volumes are formed at the expense of the SPR defrosting; move along the upper sedimentary shelf sequence and along the surface of one or another layer (from coastal warmed areas to cooler deep areas); and form horizontally elongated convective cells, which activates destruction even at negative bottom temperatures. The methane emission will increase and become massive during the continuing SPR degradation.",
author = "Lobkovskiy, {L. I.} and Nikiforov, {S. L.} and Dmitrevskiy, {N. N.} and Libina, {N. V.} and Semiletov, {I. P.} and Ananiev, {R. A.} and Meluzov, {A. A.} and Roslyakov, {A. G.}",
year = "2015",
month = "3",
day = "1",
doi = "10.1134/S0001437015010129",
language = "English",
volume = "55",
pages = "283--290",
journal = "Oceanology",
issn = "0001-4370",
publisher = "Maik Nauka-Interperiodica Publishing",
number = "2",

}

TY - JOUR

T1 - Gas extraction and degradation of the submarine permafrost rocks on the Laptev Sea shelf

AU - Lobkovskiy, L. I.

AU - Nikiforov, S. L.

AU - Dmitrevskiy, N. N.

AU - Libina, N. V.

AU - Semiletov, I. P.

AU - Ananiev, R. A.

AU - Meluzov, A. A.

AU - Roslyakov, A. G.

PY - 2015/3/1

Y1 - 2015/3/1

N2 - In 2011 and 2012, the interdisciplinary oceanic cruises of the R/V Akademik M.A. Lavrent’ev and R/V Viktor Buinitskii were conducted in the framework of the project of targeted basic research of the Russian Foundation for Basic Research. These studies identified strong methane jets because of the degradation of submarine permafrost rocks (SPRs), which is related to paleogeographical and modern factors of formation of the upper sedimentary sequence and also to structural peculiarities of the Arctic region. Large gas and water volumes are formed at the expense of the SPR defrosting; move along the upper sedimentary shelf sequence and along the surface of one or another layer (from coastal warmed areas to cooler deep areas); and form horizontally elongated convective cells, which activates destruction even at negative bottom temperatures. The methane emission will increase and become massive during the continuing SPR degradation.

AB - In 2011 and 2012, the interdisciplinary oceanic cruises of the R/V Akademik M.A. Lavrent’ev and R/V Viktor Buinitskii were conducted in the framework of the project of targeted basic research of the Russian Foundation for Basic Research. These studies identified strong methane jets because of the degradation of submarine permafrost rocks (SPRs), which is related to paleogeographical and modern factors of formation of the upper sedimentary sequence and also to structural peculiarities of the Arctic region. Large gas and water volumes are formed at the expense of the SPR defrosting; move along the upper sedimentary shelf sequence and along the surface of one or another layer (from coastal warmed areas to cooler deep areas); and form horizontally elongated convective cells, which activates destruction even at negative bottom temperatures. The methane emission will increase and become massive during the continuing SPR degradation.

UR - http://www.scopus.com/inward/record.url?scp=84928485012&partnerID=8YFLogxK

UR - http://www.scopus.com/inward/citedby.url?scp=84928485012&partnerID=8YFLogxK

U2 - 10.1134/S0001437015010129

DO - 10.1134/S0001437015010129

M3 - Article

AN - SCOPUS:84928485012

VL - 55

SP - 283

EP - 290

JO - Oceanology

JF - Oceanology

SN - 0001-4370

IS - 2

ER -