Chemistry of pore water from Arctic sediments ...

Pore water and solid phase distributions of C, N, P and Si in sediments of the Arctic Ocean (Svalbard area) have been investigated. Concentrations of organic carbon (Corg) in the solid phase of the sediment varied from 1.3 to 2.8% (mean 1.9%), with highest concentrations found at shallow stations so...

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Main Authors: Hulth, Stefan, Hall, Per, Blackburn, T H, Landén, A
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 1996
Subjects:
AWI
Online Access:https://dx.doi.org/10.1594/pangaea.725786
https://doi.pangaea.de/10.1594/PANGAEA.725786
id ftdatacite:10.1594/pangaea.725786
record_format openpolar
spelling ftdatacite:10.1594/pangaea.725786 2024-09-15T17:53:58+00:00 Chemistry of pore water from Arctic sediments ... Hulth, Stefan Hall, Per Blackburn, T H Landén, A 1996 application/zip https://dx.doi.org/10.1594/pangaea.725786 https://doi.pangaea.de/10.1594/PANGAEA.725786 en eng PANGAEA https://dx.doi.org/10.1007/bf02390426 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 AWI Multiple investigations MultiCorer Giant box corer ARK-VIII/2 Polarstern Origin and Fate of Biogenic Particle Fluxes in the Ocean ORFOIS Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo Silicon Cycling in the World Ocean SINOPS article Collection Supplementary Publication Series of Datasets 1996 ftdatacite https://doi.org/10.1594/pangaea.72578610.1007/bf02390426 2024-08-01T08:58:27Z Pore water and solid phase distributions of C, N, P and Si in sediments of the Arctic Ocean (Svalbard area) have been investigated. Concentrations of organic carbon (Corg) in the solid phase of the sediment varied from 1.3 to 2.8% (mean 1.9%), with highest concentrations found at shallow stations south/southwest of Svalbard. Relatively low concentrations were obtained at the deeper stations north/northeast of Svalbard. Atomic carbon to nitrogen ratios in the surface sediment ranged from below 8 to above 10. For some stations, high C/N ratios together with high concentrations of Corg suggest that sedimentary organic matter is mainly of terrigenous origin and not from overall biological activity in the water column. Organic matter reactivity (defined as the total sediment oxygen consumption rate normalized to the organic carbon content of the surface sediment) correlated with water depth at all investigated stations. However, the stations could be divided into two separate groups with different reactivity ... : Supplement to: Hulth, Stefan; Hall, Per; Blackburn, T H; Landén, A (1996): Arctic sediments (Svalbard): pore water and solid phase distributions of C, N, P and Si. Polar Biology, 16(6), 447-462 ... Article in Journal/Newspaper Arctic Ocean Svalbard DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic AWI
Multiple investigations
MultiCorer
Giant box corer
ARK-VIII/2
Polarstern
Origin and Fate of Biogenic Particle Fluxes in the Ocean ORFOIS
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
Silicon Cycling in the World Ocean SINOPS
spellingShingle AWI
Multiple investigations
MultiCorer
Giant box corer
ARK-VIII/2
Polarstern
Origin and Fate of Biogenic Particle Fluxes in the Ocean ORFOIS
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
Silicon Cycling in the World Ocean SINOPS
Hulth, Stefan
Hall, Per
Blackburn, T H
Landén, A
Chemistry of pore water from Arctic sediments ...
topic_facet AWI
Multiple investigations
MultiCorer
Giant box corer
ARK-VIII/2
Polarstern
Origin and Fate of Biogenic Particle Fluxes in the Ocean ORFOIS
Paleoenvironmental Reconstructions from Marine Sediments @ AWI AWI_Paleo
Silicon Cycling in the World Ocean SINOPS
description Pore water and solid phase distributions of C, N, P and Si in sediments of the Arctic Ocean (Svalbard area) have been investigated. Concentrations of organic carbon (Corg) in the solid phase of the sediment varied from 1.3 to 2.8% (mean 1.9%), with highest concentrations found at shallow stations south/southwest of Svalbard. Relatively low concentrations were obtained at the deeper stations north/northeast of Svalbard. Atomic carbon to nitrogen ratios in the surface sediment ranged from below 8 to above 10. For some stations, high C/N ratios together with high concentrations of Corg suggest that sedimentary organic matter is mainly of terrigenous origin and not from overall biological activity in the water column. Organic matter reactivity (defined as the total sediment oxygen consumption rate normalized to the organic carbon content of the surface sediment) correlated with water depth at all investigated stations. However, the stations could be divided into two separate groups with different reactivity ... : Supplement to: Hulth, Stefan; Hall, Per; Blackburn, T H; Landén, A (1996): Arctic sediments (Svalbard): pore water and solid phase distributions of C, N, P and Si. Polar Biology, 16(6), 447-462 ...
format Article in Journal/Newspaper
author Hulth, Stefan
Hall, Per
Blackburn, T H
Landén, A
author_facet Hulth, Stefan
Hall, Per
Blackburn, T H
Landén, A
author_sort Hulth, Stefan
title Chemistry of pore water from Arctic sediments ...
title_short Chemistry of pore water from Arctic sediments ...
title_full Chemistry of pore water from Arctic sediments ...
title_fullStr Chemistry of pore water from Arctic sediments ...
title_full_unstemmed Chemistry of pore water from Arctic sediments ...
title_sort chemistry of pore water from arctic sediments ...
publisher PANGAEA
publishDate 1996
url https://dx.doi.org/10.1594/pangaea.725786
https://doi.pangaea.de/10.1594/PANGAEA.725786
genre Arctic Ocean
Svalbard
genre_facet Arctic Ocean
Svalbard
op_relation https://dx.doi.org/10.1007/bf02390426
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.72578610.1007/bf02390426
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