In situ sediment temperature and sediment thermal conductivity measurements with heat flow probe during Maria S. Merian cruise MSM57
In situ sediment temperature and sediment thermal conductivity measurements were made with the GEOMAR heat flow probe (6m total length) during Expedition MSM57 on board the R/V MARIA S. MERIAN at the Svalbard margin. Two sub-regions were visited: Vestnesa Ridge and Svyatogor Ridge.A total of eleven...
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ftdatacite:10.1594/pangaea.911766 2023-05-15T18:29:43+02:00 In situ sediment temperature and sediment thermal conductivity measurements with heat flow probe during Maria S. Merian cruise MSM57 Riedel, Michael 2020 application/zip https://dx.doi.org/10.1594/pangaea.911766 https://doi.pangaea.de/10.1594/PANGAEA.911766 en eng PANGAEA - Data Publisher for Earth & Environmental Science https://hs.pangaea.de/Raw/MSM/MSM57/Heatflow/H1601_data.zip https://dx.doi.org/10.1029/2020jb019468 https://dx.doi.org/10.1029/jb092ib12p12846 https://hs.pangaea.de/Raw/MSM/MSM57/Heatflow/H1601_data.zip Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 CC-BY heat probe pockmarks Svalbard Collection of Datasets article Collection 2020 ftdatacite https://doi.org/10.1594/pangaea.911766 https://doi.org/10.1029/2020jb019468 https://doi.org/10.1029/jb092ib12p12846 2022-02-09T13:17:17Z In situ sediment temperature and sediment thermal conductivity measurements were made with the GEOMAR heat flow probe (6m total length) during Expedition MSM57 on board the R/V MARIA S. MERIAN at the Svalbard margin. Two sub-regions were visited: Vestnesa Ridge and Svyatogor Ridge.A total of eleven deployment sequences were performed. The first deployment was used to defined individual sensor offsets to a reference temperature (data file available in section source data set). Deployment sequence 2 - 8 were conducted around pockmarks on Vestnesa Ridge, and deployment sequence 9 - 11 are at pockmarks across Svyatogor Ridge. During each deployment sequence several individual stations were visited as detailed in Bohrmann et al., (2017) (see datasets listed in this publication series below).From the individual measured temperature records, thermal gradients and in situ thermal conductivity values are derived using the technique described in Villinger and Davis (1986). We report here our initial results as well. Initial results and further details of the deployments can be found in the cruise report by Bohrmann et al. (2017). : Raw-data have the extension ".TOB" and are tab-delimited ascii files with data labels and units in top rows. Note: Temperatures in the raw files are not corrected for sensor Offsets from reference. Article in Journal/Newspaper Svalbard Svalbard margin DataCite Metadata Store (German National Library of Science and Technology) Svalbard Svyatogor Ridge ENVELOPE(5.783,5.783,78.233,78.233) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
heat probe pockmarks Svalbard |
spellingShingle |
heat probe pockmarks Svalbard Riedel, Michael In situ sediment temperature and sediment thermal conductivity measurements with heat flow probe during Maria S. Merian cruise MSM57 |
topic_facet |
heat probe pockmarks Svalbard |
description |
In situ sediment temperature and sediment thermal conductivity measurements were made with the GEOMAR heat flow probe (6m total length) during Expedition MSM57 on board the R/V MARIA S. MERIAN at the Svalbard margin. Two sub-regions were visited: Vestnesa Ridge and Svyatogor Ridge.A total of eleven deployment sequences were performed. The first deployment was used to defined individual sensor offsets to a reference temperature (data file available in section source data set). Deployment sequence 2 - 8 were conducted around pockmarks on Vestnesa Ridge, and deployment sequence 9 - 11 are at pockmarks across Svyatogor Ridge. During each deployment sequence several individual stations were visited as detailed in Bohrmann et al., (2017) (see datasets listed in this publication series below).From the individual measured temperature records, thermal gradients and in situ thermal conductivity values are derived using the technique described in Villinger and Davis (1986). We report here our initial results as well. Initial results and further details of the deployments can be found in the cruise report by Bohrmann et al. (2017). : Raw-data have the extension ".TOB" and are tab-delimited ascii files with data labels and units in top rows. Note: Temperatures in the raw files are not corrected for sensor Offsets from reference. |
format |
Article in Journal/Newspaper |
author |
Riedel, Michael |
author_facet |
Riedel, Michael |
author_sort |
Riedel, Michael |
title |
In situ sediment temperature and sediment thermal conductivity measurements with heat flow probe during Maria S. Merian cruise MSM57 |
title_short |
In situ sediment temperature and sediment thermal conductivity measurements with heat flow probe during Maria S. Merian cruise MSM57 |
title_full |
In situ sediment temperature and sediment thermal conductivity measurements with heat flow probe during Maria S. Merian cruise MSM57 |
title_fullStr |
In situ sediment temperature and sediment thermal conductivity measurements with heat flow probe during Maria S. Merian cruise MSM57 |
title_full_unstemmed |
In situ sediment temperature and sediment thermal conductivity measurements with heat flow probe during Maria S. Merian cruise MSM57 |
title_sort |
in situ sediment temperature and sediment thermal conductivity measurements with heat flow probe during maria s. merian cruise msm57 |
publisher |
PANGAEA - Data Publisher for Earth & Environmental Science |
publishDate |
2020 |
url |
https://dx.doi.org/10.1594/pangaea.911766 https://doi.pangaea.de/10.1594/PANGAEA.911766 |
long_lat |
ENVELOPE(5.783,5.783,78.233,78.233) |
geographic |
Svalbard Svyatogor Ridge |
geographic_facet |
Svalbard Svyatogor Ridge |
genre |
Svalbard Svalbard margin |
genre_facet |
Svalbard Svalbard margin |
op_relation |
https://hs.pangaea.de/Raw/MSM/MSM57/Heatflow/H1601_data.zip https://dx.doi.org/10.1029/2020jb019468 https://dx.doi.org/10.1029/jb092ib12p12846 https://hs.pangaea.de/Raw/MSM/MSM57/Heatflow/H1601_data.zip |
op_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/pangaea.911766 https://doi.org/10.1029/2020jb019468 https://doi.org/10.1029/jb092ib12p12846 |
_version_ |
1766213045670903808 |