Thermal conductivity of bottom sediments in the East Siberian Arctic seas: a case study in the Buor-Khaya Bay; 68th Canadian Geotechnical Conference and 7th Canadian Permafrost Conference: GEOQuebec 2015, Quebec, September 20-23, 2015

Opis bibliograficzny
Parent link:68th Canadian Geotechnical Conference and 7th Canadian Permafrost Conference: GEOQuebec 2015, Quebec, September 20-23, 2015.— 2015.— [7 .]
Korporacja: Национальный исследовательский Томский политехнический университет (ТПУ) Институт природных ресурсов (ИПР) Кафедра геологии и разведки полезных ископаемых (ГРПИ)
Kolejni autorzy: Chuvilin E. M. Evgeny Mikhaylovich, Bukhanov B. A. Boris Aleksandrovich, Grebenkin S. I. Sergey Igorevich, Tumskoy V. E. Vladimir Evgenjevich, Shakhova N. E. Nataljya Evgenjevna, Dudarev O. V. Oleg Viktorovich, Semiletov I. P. Igor Petrovich
Streszczenie:Title screen
Among Arctic carbon reservoirs, subsea permafrost, hydrates, and associated methane (CH4) deposits are the most worrisome owing to high heat transfer from rapidly warming shallow Arctic seas. The East Siberian Arctic Shelf is a big portion of the Arctic shelf and hosts over 80% of current subsea permafrost and along with it, unique Arctic shallow CH4 hydrates. Degradation of subsea permafrost results in increasing permeability for gaseous CH4 long preserved in seabed deposits within and beneath permafrost. Nevertheless, knowledge about the present thermal state of subsea permafrost is mainly based on modeling results, which are controversial. In that sense, actual values of thermal conductivity are crucially needed. In this report, we represent the first results of in situ measurements of the major sediment core thermodynamically parameters in the ESAS.
Режим доступа: по договору с организацией-держателем ресурса
Język:angielski
Wydane: 2015
Hasła przedmiotowe:
Dostęp online:https://www.researchgate.net/publication/281998760_Thermal_conductivity_of_bottom_sediments_in_the_East_Siberian_Arctic_seas_a_case_study_in_the_Buor-Khaya_Bay
Format: Elektroniczne Rozdział
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=650192

MARC

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330 |a Among Arctic carbon reservoirs, subsea permafrost, hydrates, and associated methane (CH4) deposits are the most worrisome owing to high heat transfer from rapidly warming shallow Arctic seas. The East Siberian Arctic Shelf is a big portion of the Arctic shelf and hosts over 80% of current subsea permafrost and along with it, unique Arctic shallow CH4 hydrates. Degradation of subsea permafrost results in increasing permeability for gaseous CH4 long preserved in seabed deposits within and beneath permafrost. Nevertheless, knowledge about the present thermal state of subsea permafrost is mainly based on modeling results, which are controversial. In that sense, actual values of thermal conductivity are crucially needed. In this report, we represent the first results of in situ measurements of the major sediment core thermodynamically parameters in the ESAS. 
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463 |t 68th Canadian Geotechnical Conference and 7th Canadian Permafrost Conference: GEOQuebec 2015, Quebec, September 20-23, 2015  |o proceedings  |v [7 .]  |d 2015 
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701 1 |a Chuvilin  |b E. M.  |g Evgeny Mikhaylovich 
701 1 |a Bukhanov  |b B. A.  |g Boris Aleksandrovich 
701 1 |a Grebenkin  |b S. I.  |g Sergey Igorevich 
701 1 |a Tumskoy  |b V. E.  |g Vladimir Evgenjevich 
701 1 |a Shakhova  |b N. E.  |c geologist  |c Professor of Tomsk Polytechnic University, doctor of geological-mineralogical Sciences  |f 1959-  |g Nataljya Evgenjevna  |3 (RuTPU)RU\TPU\pers\35374 
701 1 |a Dudarev  |b O. V.  |c geologist  |c researcher of Tomsk Polytechnic University, candidate of geological and mineralogical Sciences  |f 1955-  |g Oleg Viktorovich  |3 (RuTPU)RU\TPU\pers\35379 
701 1 |a Semiletov  |b I. P.  |c geographer  |c Professor of Tomsk Polytechnic University, doctor of geographical Sciences  |f 1955-  |g Igor Petrovich  |3 (RuTPU)RU\TPU\pers\34220 
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