Porosity of the Northeast Greenland (NEG) shelf sediments from POLARSTERN cruise PS109 ...
Samples for sediment porosity on the Northeast Greenland shelf have been collected with R/V Polarstern during PS109 between September and October 2017 using a camera-equipped multiple corer (TV-MUC; core area 0.007 m²). Upon arrival on deck, the upper 5 cm of three MUC cores were sliced into 1 cm in...
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2024
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Online Access: | https://dx.doi.org/10.1594/pangaea.959550 https://doi.pangaea.de/10.1594/PANGAEA.959550 |
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ftdatacite:10.1594/pangaea.959550 2024-10-20T14:06:41+00:00 Porosity of the Northeast Greenland (NEG) shelf sediments from POLARSTERN cruise PS109 ... Braeckman, Ulrike 2024 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.959550 https://doi.pangaea.de/10.1594/PANGAEA.959550 en eng PANGAEA https://dx.doi.org/10.1525/elementa.2023.00005 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Arctic Shelf Event label Latitude of event Longitude of event Date/Time of event Elevation of event Method/Device of event Depth, top/min Depth, bottom/max DEPTH, sediment/rock Replicates Water content, sediment Porosity Comment Multicorer with television Calculated according to Dalsgaard et al. 2000 PS109 Polarstern FRontiers in Arctic marine Monitoring FRAM Dataset dataset 2024 ftdatacite https://doi.org/10.1594/pangaea.95955010.1525/elementa.2023.00005 2024-10-01T10:25:49Z Samples for sediment porosity on the Northeast Greenland shelf have been collected with R/V Polarstern during PS109 between September and October 2017 using a camera-equipped multiple corer (TV-MUC; core area 0.007 m²). Upon arrival on deck, the upper 5 cm of three MUC cores were sliced into 1 cm intervals, using a cut-off syringe in order to get a depth resolution of the sediment porosity, and then stored in 5 ml cut-off syringes that were wrapped in aluminium foil. In the laboratory, the samples were sliced into 1 cm intervals. After measuring their wet mass, the sediment samples were dried at 60°C. The sediment porosity was calculated by the difference between the wet and dry mass after Dalsgaard et al., 2000. ... Dataset Arctic Greenland DataCite Arctic Greenland |
institution |
Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Arctic Shelf Event label Latitude of event Longitude of event Date/Time of event Elevation of event Method/Device of event Depth, top/min Depth, bottom/max DEPTH, sediment/rock Replicates Water content, sediment Porosity Comment Multicorer with television Calculated according to Dalsgaard et al. 2000 PS109 Polarstern FRontiers in Arctic marine Monitoring FRAM |
spellingShingle |
Arctic Shelf Event label Latitude of event Longitude of event Date/Time of event Elevation of event Method/Device of event Depth, top/min Depth, bottom/max DEPTH, sediment/rock Replicates Water content, sediment Porosity Comment Multicorer with television Calculated according to Dalsgaard et al. 2000 PS109 Polarstern FRontiers in Arctic marine Monitoring FRAM Braeckman, Ulrike Porosity of the Northeast Greenland (NEG) shelf sediments from POLARSTERN cruise PS109 ... |
topic_facet |
Arctic Shelf Event label Latitude of event Longitude of event Date/Time of event Elevation of event Method/Device of event Depth, top/min Depth, bottom/max DEPTH, sediment/rock Replicates Water content, sediment Porosity Comment Multicorer with television Calculated according to Dalsgaard et al. 2000 PS109 Polarstern FRontiers in Arctic marine Monitoring FRAM |
description |
Samples for sediment porosity on the Northeast Greenland shelf have been collected with R/V Polarstern during PS109 between September and October 2017 using a camera-equipped multiple corer (TV-MUC; core area 0.007 m²). Upon arrival on deck, the upper 5 cm of three MUC cores were sliced into 1 cm intervals, using a cut-off syringe in order to get a depth resolution of the sediment porosity, and then stored in 5 ml cut-off syringes that were wrapped in aluminium foil. In the laboratory, the samples were sliced into 1 cm intervals. After measuring their wet mass, the sediment samples were dried at 60°C. The sediment porosity was calculated by the difference between the wet and dry mass after Dalsgaard et al., 2000. ... |
format |
Dataset |
author |
Braeckman, Ulrike |
author_facet |
Braeckman, Ulrike |
author_sort |
Braeckman, Ulrike |
title |
Porosity of the Northeast Greenland (NEG) shelf sediments from POLARSTERN cruise PS109 ... |
title_short |
Porosity of the Northeast Greenland (NEG) shelf sediments from POLARSTERN cruise PS109 ... |
title_full |
Porosity of the Northeast Greenland (NEG) shelf sediments from POLARSTERN cruise PS109 ... |
title_fullStr |
Porosity of the Northeast Greenland (NEG) shelf sediments from POLARSTERN cruise PS109 ... |
title_full_unstemmed |
Porosity of the Northeast Greenland (NEG) shelf sediments from POLARSTERN cruise PS109 ... |
title_sort |
porosity of the northeast greenland (neg) shelf sediments from polarstern cruise ps109 ... |
publisher |
PANGAEA |
publishDate |
2024 |
url |
https://dx.doi.org/10.1594/pangaea.959550 https://doi.pangaea.de/10.1594/PANGAEA.959550 |
geographic |
Arctic Greenland |
geographic_facet |
Arctic Greenland |
genre |
Arctic Greenland |
genre_facet |
Arctic Greenland |
op_relation |
https://dx.doi.org/10.1525/elementa.2023.00005 |
op_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_doi |
https://doi.org/10.1594/pangaea.95955010.1525/elementa.2023.00005 |
_version_ |
1813445406529421312 |