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...
Main Authors: | , , , |
---|---|
Format: | Dataset |
Language: | English |
Published: |
PANGAEA
1996
|
Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.725786 https://doi.org/10.1594/PANGAEA.725786 |
id |
ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.725786 |
---|---|
record_format |
openpolar |
spelling |
ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.725786 2023-05-15T14:25:16+02:00 Chemistry of pore water from Arctic sediments Hulth, Stefan Hall, Per Blackburn, T H Landén, A MEDIAN LATITUDE: 78.718863 * MEDIAN LONGITUDE: 25.844368 * SOUTH-BOUND LATITUDE: 75.985000 * WEST-BOUND LONGITUDE: 5.934500 * NORTH-BOUND LATITUDE: 81.657333 * EAST-BOUND LONGITUDE: 34.860300 * DATE/TIME START: 1991-06-23T16:22:00 * DATE/TIME END: 1991-07-28T00:00:00 1996-07-16 application/zip, 2 datasets https://doi.pangaea.de/10.1594/PANGAEA.725786 https://doi.org/10.1594/PANGAEA.725786 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.725786 https://doi.org/10.1594/PANGAEA.725786 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY 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, https://doi.org/10.1007/BF02390426 ARK-VIII/2 AWI AWI_Paleo Barents Sea Giant box corer GKG MUC MULT MultiCorer Multiple investigations ORFOIS Origin and Fate of Biogenic Particle Fluxes in the Ocean Paleoenvironmental Reconstructions from Marine Sediments @ AWI Polarstern PS19/040 PS19/045 PS19/050 PS19/055 PS19/078 PS19/082 PS19/084 PS19/086 PS19/098 PS19/100 PS19/101 PS19/105 PS19/108 PS19/112 PS19/119 PS19/134 PS19/143 PS19/146 PS19 EPOS II PS2111-2 PS2113-2 PS2114-2 PS2115-1 PS2117-1 PS2121-3 PS2122-1 PS2123-4 PS2128-1 PS2129-3 PS2130-2 PS2133-1 PS2134-1 PS2138-5 PS2144-3 PS2150-1 PS2153-1 Dataset 1996 ftpangaea https://doi.org/10.1594/PANGAEA.725786 https://doi.org/10.1007/BF02390426 2023-01-20T07:31:27Z 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 characteristics, representing the two most dominant hydrographic regimes: the region west of Svalbard mainly influenced by the West Spitsbergen Current, and the area east of Svalbard where Arctic polar water set the environmental conditions. Decreasing sediment reactivity with water depth was confirmed by the partitioning between organic and inorganic carbon of the surface sediment. The ratio between organic and inorganic carbon at the sediment-water interface decreased exponentially with water depth: from indefinite values at shallow stations in the central Barents Sea, to approximately 1 at deep stations north of Svalbard. At stations east of Svalbard there was an inverse linear correlation between the organic matter reactivity (as defined above) and concentration of dissolved organic carbon (DOC) in the pore water. The more reactive the sediment, the less DOC existed in the pore water and the more total carbonate (Ct or Sum CO2) was present. This observation suggests that DOC produced in reactive sediments is ... Dataset Arctic Arctic Arctic Ocean Barents Sea Polar Biology Svalbard Spitsbergen PANGAEA - Data Publisher for Earth & Environmental Science Arctic Arctic Ocean Barents Sea Svalbard ENVELOPE(5.934500,34.860300,81.657333,75.985000) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
ARK-VIII/2 AWI AWI_Paleo Barents Sea Giant box corer GKG MUC MULT MultiCorer Multiple investigations ORFOIS Origin and Fate of Biogenic Particle Fluxes in the Ocean Paleoenvironmental Reconstructions from Marine Sediments @ AWI Polarstern PS19/040 PS19/045 PS19/050 PS19/055 PS19/078 PS19/082 PS19/084 PS19/086 PS19/098 PS19/100 PS19/101 PS19/105 PS19/108 PS19/112 PS19/119 PS19/134 PS19/143 PS19/146 PS19 EPOS II PS2111-2 PS2113-2 PS2114-2 PS2115-1 PS2117-1 PS2121-3 PS2122-1 PS2123-4 PS2128-1 PS2129-3 PS2130-2 PS2133-1 PS2134-1 PS2138-5 PS2144-3 PS2150-1 PS2153-1 |
spellingShingle |
ARK-VIII/2 AWI AWI_Paleo Barents Sea Giant box corer GKG MUC MULT MultiCorer Multiple investigations ORFOIS Origin and Fate of Biogenic Particle Fluxes in the Ocean Paleoenvironmental Reconstructions from Marine Sediments @ AWI Polarstern PS19/040 PS19/045 PS19/050 PS19/055 PS19/078 PS19/082 PS19/084 PS19/086 PS19/098 PS19/100 PS19/101 PS19/105 PS19/108 PS19/112 PS19/119 PS19/134 PS19/143 PS19/146 PS19 EPOS II PS2111-2 PS2113-2 PS2114-2 PS2115-1 PS2117-1 PS2121-3 PS2122-1 PS2123-4 PS2128-1 PS2129-3 PS2130-2 PS2133-1 PS2134-1 PS2138-5 PS2144-3 PS2150-1 PS2153-1 Hulth, Stefan Hall, Per Blackburn, T H Landén, A Chemistry of pore water from Arctic sediments |
topic_facet |
ARK-VIII/2 AWI AWI_Paleo Barents Sea Giant box corer GKG MUC MULT MultiCorer Multiple investigations ORFOIS Origin and Fate of Biogenic Particle Fluxes in the Ocean Paleoenvironmental Reconstructions from Marine Sediments @ AWI Polarstern PS19/040 PS19/045 PS19/050 PS19/055 PS19/078 PS19/082 PS19/084 PS19/086 PS19/098 PS19/100 PS19/101 PS19/105 PS19/108 PS19/112 PS19/119 PS19/134 PS19/143 PS19/146 PS19 EPOS II PS2111-2 PS2113-2 PS2114-2 PS2115-1 PS2117-1 PS2121-3 PS2122-1 PS2123-4 PS2128-1 PS2129-3 PS2130-2 PS2133-1 PS2134-1 PS2138-5 PS2144-3 PS2150-1 PS2153-1 |
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 characteristics, representing the two most dominant hydrographic regimes: the region west of Svalbard mainly influenced by the West Spitsbergen Current, and the area east of Svalbard where Arctic polar water set the environmental conditions. Decreasing sediment reactivity with water depth was confirmed by the partitioning between organic and inorganic carbon of the surface sediment. The ratio between organic and inorganic carbon at the sediment-water interface decreased exponentially with water depth: from indefinite values at shallow stations in the central Barents Sea, to approximately 1 at deep stations north of Svalbard. At stations east of Svalbard there was an inverse linear correlation between the organic matter reactivity (as defined above) and concentration of dissolved organic carbon (DOC) in the pore water. The more reactive the sediment, the less DOC existed in the pore water and the more total carbonate (Ct or Sum CO2) was present. This observation suggests that DOC produced in reactive sediments is ... |
format |
Dataset |
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://doi.pangaea.de/10.1594/PANGAEA.725786 https://doi.org/10.1594/PANGAEA.725786 |
op_coverage |
MEDIAN LATITUDE: 78.718863 * MEDIAN LONGITUDE: 25.844368 * SOUTH-BOUND LATITUDE: 75.985000 * WEST-BOUND LONGITUDE: 5.934500 * NORTH-BOUND LATITUDE: 81.657333 * EAST-BOUND LONGITUDE: 34.860300 * DATE/TIME START: 1991-06-23T16:22:00 * DATE/TIME END: 1991-07-28T00:00:00 |
long_lat |
ENVELOPE(5.934500,34.860300,81.657333,75.985000) |
geographic |
Arctic Arctic Ocean Barents Sea Svalbard |
geographic_facet |
Arctic Arctic Ocean Barents Sea Svalbard |
genre |
Arctic Arctic Arctic Ocean Barents Sea Polar Biology Svalbard Spitsbergen |
genre_facet |
Arctic Arctic Arctic Ocean Barents Sea Polar Biology Svalbard Spitsbergen |
op_source |
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, https://doi.org/10.1007/BF02390426 |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.725786 https://doi.org/10.1594/PANGAEA.725786 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/PANGAEA.725786 https://doi.org/10.1007/BF02390426 |
_version_ |
1766297693693411328 |