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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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 |
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collection |
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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 |
_version_ |
1810430111913082880 |