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...

Full description

Bibliographic Details
Main Author: Braeckman, Ulrike
Format: Dataset
Language:English
Published: PANGAEA 2024
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.959550
https://doi.pangaea.de/10.1594/PANGAEA.959550
id ftdatacite:10.1594/pangaea.959550
record_format openpolar
spelling 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