Release of Black Carbon From Thawing Permafrost Estimated by Sequestration Fluxes in the East Siberian Arctic Shelf Recipient

Release of Black Carbon From Thawing Permafrost Estimated by Sequestration Fluxes in the East Siberian Arctic Shelf Recipient

Dades bibliogràfiques
Parent link:	Global Biogeochemical Cycles Vol. 31, iss. 10.— 2017.— [P. 1173-1191]
Autor corporatiu:	Национальный исследовательский Томский политехнический университет (ТПУ) Институт природных ресурсов (ИПР) Кафедра геологии и разведки полезных ископаемых (ГРПИ)
Altres autors:	Salvado J. A. Joan A., Broder L. Lisa, Andersso A. August, Semiletov I. P. Igor Petrovich, Gustafsson O. Orjan
Sumari:	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
Publicat:	2017
Matèries:	электронный ресурс труды учёных ТПУ Северный Ледовитый океан сажа донные отложения вечная мерзлота углерод
Accés en línia:	http://dx.doi.org/10.1002/2017GB005693
Format:	Electrònic Capítol de llibre
KOHA link:	https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=656600

Internet

http://dx.doi.org/10.1002/2017GB005693