Organic carbon in waters, suspended matter, and upper layer bottom sediments of the Kara Sea and Obskay Guba ...

Along three sections in the Kara Sea and Obskaya Guba concentrations of dissolved and particulate organic carbon (DOC and POC, respectively) in waters , as well as of organic carbon in bottom sediments (Corg) in September-October 2007 were determined. DOC varied from 6.3 to 2400 µg/l, POC - from 0.8...

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Main Authors: Belyaev, Nikolay A, Peresypkin, Valery I, Ponyaev, M S
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2010
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.763819
https://doi.pangaea.de/10.1594/PANGAEA.763819
id ftdatacite:10.1594/pangaea.763819
record_format openpolar
spelling ftdatacite:10.1594/pangaea.763819 2024-09-15T18:16:07+00:00 Organic carbon in waters, suspended matter, and upper layer bottom sediments of the Kara Sea and Obskay Guba ... Belyaev, Nikolay A Peresypkin, Valery I Ponyaev, M S 2010 application/zip https://dx.doi.org/10.1594/pangaea.763819 https://doi.pangaea.de/10.1594/PANGAEA.763819 en eng PANGAEA https://dx.doi.org/10.1134/s0001437010050085 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Multiple investigations AMK54 Akademik Mstislav Keldysh Archive of Ocean Data ARCOD article Collection Supplementary Publication Series of Datasets 2010 ftdatacite https://doi.org/10.1594/pangaea.76381910.1134/s0001437010050085 2024-08-01T10:51:52Z Along three sections in the Kara Sea and Obskaya Guba concentrations of dissolved and particulate organic carbon (DOC and POC, respectively) in waters , as well as of organic carbon in bottom sediments (Corg) in September-October 2007 were determined. DOC varied from 6.3 to 2400 µg/l, POC - from 0.84 to 12.2 mg/l. For all samples the average DOC was 200 µg/l (n = 78; sigma = 368), the average POC - 2.7 mg/l (n = 92; sigma = 2.7). Concentrations of Corg in dried samples of upper layer bottom sediments varied from 0.13 to 2.10% (aver. = 0.9%; n = 21; sigma = 0.49%). It is shown that distribution of different forms of organic matter (OM) is an indicator of supply and scattering of particulate matter in the Kara Sea and that DOC and POC of the Kara Sea are formed under impact of runoff of the Ob and Yenisei Rivers. It is found that distribution of OM in bottom sediments is closely related to their grain size composition and to the structure of currents in the area. Variations in Corg concentration in bottom ... : Supplement to: Belyaev, Nikolay A; Peresypkin, Valery I; Ponyaev, M S (2010): The organic carbon in the water, the particulate matter, and the upper layer of the bottom sediments of the west Kara Sea. Translated from Okeanologiya, 2010, 50(5), 748-757, Oceanology, 50(5), 706-715 ... Article in Journal/Newspaper Kara Sea Obskaya Guba DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Multiple investigations
AMK54
Akademik Mstislav Keldysh
Archive of Ocean Data ARCOD
spellingShingle Multiple investigations
AMK54
Akademik Mstislav Keldysh
Archive of Ocean Data ARCOD
Belyaev, Nikolay A
Peresypkin, Valery I
Ponyaev, M S
Organic carbon in waters, suspended matter, and upper layer bottom sediments of the Kara Sea and Obskay Guba ...
topic_facet Multiple investigations
AMK54
Akademik Mstislav Keldysh
Archive of Ocean Data ARCOD
description Along three sections in the Kara Sea and Obskaya Guba concentrations of dissolved and particulate organic carbon (DOC and POC, respectively) in waters , as well as of organic carbon in bottom sediments (Corg) in September-October 2007 were determined. DOC varied from 6.3 to 2400 µg/l, POC - from 0.84 to 12.2 mg/l. For all samples the average DOC was 200 µg/l (n = 78; sigma = 368), the average POC - 2.7 mg/l (n = 92; sigma = 2.7). Concentrations of Corg in dried samples of upper layer bottom sediments varied from 0.13 to 2.10% (aver. = 0.9%; n = 21; sigma = 0.49%). It is shown that distribution of different forms of organic matter (OM) is an indicator of supply and scattering of particulate matter in the Kara Sea and that DOC and POC of the Kara Sea are formed under impact of runoff of the Ob and Yenisei Rivers. It is found that distribution of OM in bottom sediments is closely related to their grain size composition and to the structure of currents in the area. Variations in Corg concentration in bottom ... : Supplement to: Belyaev, Nikolay A; Peresypkin, Valery I; Ponyaev, M S (2010): The organic carbon in the water, the particulate matter, and the upper layer of the bottom sediments of the west Kara Sea. Translated from Okeanologiya, 2010, 50(5), 748-757, Oceanology, 50(5), 706-715 ...
format Article in Journal/Newspaper
author Belyaev, Nikolay A
Peresypkin, Valery I
Ponyaev, M S
author_facet Belyaev, Nikolay A
Peresypkin, Valery I
Ponyaev, M S
author_sort Belyaev, Nikolay A
title Organic carbon in waters, suspended matter, and upper layer bottom sediments of the Kara Sea and Obskay Guba ...
title_short Organic carbon in waters, suspended matter, and upper layer bottom sediments of the Kara Sea and Obskay Guba ...
title_full Organic carbon in waters, suspended matter, and upper layer bottom sediments of the Kara Sea and Obskay Guba ...
title_fullStr Organic carbon in waters, suspended matter, and upper layer bottom sediments of the Kara Sea and Obskay Guba ...
title_full_unstemmed Organic carbon in waters, suspended matter, and upper layer bottom sediments of the Kara Sea and Obskay Guba ...
title_sort organic carbon in waters, suspended matter, and upper layer bottom sediments of the kara sea and obskay guba ...
publisher PANGAEA
publishDate 2010
url https://dx.doi.org/10.1594/pangaea.763819
https://doi.pangaea.de/10.1594/PANGAEA.763819
genre Kara Sea
Obskaya Guba
genre_facet Kara Sea
Obskaya Guba
op_relation https://dx.doi.org/10.1134/s0001437010050085
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.76381910.1134/s0001437010050085
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