Release of Black Carbon From Thawing Permafrost Estimated by Sequestration Fluxes in the East Siberian Arctic Shelf Recipient; Global Biogeochemical Cycles; Vol. 31, iss. 10

Release of Black Carbon From Thawing Permafrost Estimated by Sequestration Fluxes in the East Siberian Arctic Shelf Recipient; Global Biogeochemical Cycles; Vol. 31, iss. 10

Détails bibliographiques
Parent link:	Global Biogeochemical Cycles Vol. 31, iss. 10.— 2017.— [P. 1173-1191]
Collectivité auteur:	Национальный исследовательский Томский политехнический университет (ТПУ) Институт природных ресурсов (ИПР) Кафедра геологии и разведки полезных ископаемых (ГРПИ)
Autres auteurs:	Salvado J. A. Joan A., Broder L. Lisa, Andersso A. August, Semiletov I. P. Igor Petrovich, Gustafsson O. Orjan
Résumé:	Title screen Black carbon (BC) plays an important role in carbon burial in marine sediments globally. Yet thesequestration of BC in the Arctic Ocean is poorly understood. Black carbon (BC) plays an important role in carbon burial in marine sediments globally. Yet thesequestration of BC in the Arctic Ocean is poorly understood. Here we assess the concentrations, ﬂuxes,and sources of soot BC (SBC)-the most refractory component of BC-in sediments from the East SiberianArctic Shelf (ESAS), the World's largest shelf sea system. SBC concentrations in the contemporary shelfsediments range from 0.1 to 2.1 mg g1dw, corresponding to 2-12% of total organic carbon Режим доступа: по договору с организацией-держателем ресурса
Langue:	anglais
Publié:	2017
Sujets:	электронный ресурс труды учёных ТПУ Северный Ледовитый океан сажа донные отложения вечная мерзлота углерод
Accès en ligne:	http://dx.doi.org/10.1002/2017GB005693
Format:	Électronique Chapitre de livre
KOHA link:	https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=656600

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