Heat flow data at station H1607 during Maria S. Merian cruise MSM57/1
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. During each deplo...
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Format: | Dataset |
Language: | English |
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PANGAEA
2020
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.911758 https://doi.org/10.1594/PANGAEA.911758 |
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.911758 |
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record_format |
openpolar |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
Conductivity thermal DEPTH sediment/rock Event label GeoB21618-1 GeoB21618-10 GeoB21618-11 GeoB21618-12 GeoB21618-13 GeoB21618-14 GeoB21618-15 GeoB21618-16 GeoB21618-2 GeoB21618-3 GeoB21618-4 GeoB21618-5 GeoB21618-6 GeoB21618-7 GeoB21618-8 GeoB21618-9 heat probe Integrated thermal resistance Maria S. Merian MSM57/1 MSM57/1_630-1 MSM57/1_630-10 MSM57/1_630-11 MSM57/1_630-12 MSM57/1_630-13 MSM57/1_630-14 MSM57/1_630-15 MSM57/1_630-16 MSM57/1_630-2 MSM57/1_630-3 MSM57/1_630-4 MSM57/1_630-5 MSM57/1_630-6 MSM57/1_630-7 MSM57/1_630-8 MSM57/1_630-9 pockmarks Sample code/label Svalbard Temperature in rock/sediment Temperature Lance TL |
spellingShingle |
Conductivity thermal DEPTH sediment/rock Event label GeoB21618-1 GeoB21618-10 GeoB21618-11 GeoB21618-12 GeoB21618-13 GeoB21618-14 GeoB21618-15 GeoB21618-16 GeoB21618-2 GeoB21618-3 GeoB21618-4 GeoB21618-5 GeoB21618-6 GeoB21618-7 GeoB21618-8 GeoB21618-9 heat probe Integrated thermal resistance Maria S. Merian MSM57/1 MSM57/1_630-1 MSM57/1_630-10 MSM57/1_630-11 MSM57/1_630-12 MSM57/1_630-13 MSM57/1_630-14 MSM57/1_630-15 MSM57/1_630-16 MSM57/1_630-2 MSM57/1_630-3 MSM57/1_630-4 MSM57/1_630-5 MSM57/1_630-6 MSM57/1_630-7 MSM57/1_630-8 MSM57/1_630-9 pockmarks Sample code/label Svalbard Temperature in rock/sediment Temperature Lance TL Riedel, Michael Heat flow data at station H1607 during Maria S. Merian cruise MSM57/1 |
topic_facet |
Conductivity thermal DEPTH sediment/rock Event label GeoB21618-1 GeoB21618-10 GeoB21618-11 GeoB21618-12 GeoB21618-13 GeoB21618-14 GeoB21618-15 GeoB21618-16 GeoB21618-2 GeoB21618-3 GeoB21618-4 GeoB21618-5 GeoB21618-6 GeoB21618-7 GeoB21618-8 GeoB21618-9 heat probe Integrated thermal resistance Maria S. Merian MSM57/1 MSM57/1_630-1 MSM57/1_630-10 MSM57/1_630-11 MSM57/1_630-12 MSM57/1_630-13 MSM57/1_630-14 MSM57/1_630-15 MSM57/1_630-16 MSM57/1_630-2 MSM57/1_630-3 MSM57/1_630-4 MSM57/1_630-5 MSM57/1_630-6 MSM57/1_630-7 MSM57/1_630-8 MSM57/1_630-9 pockmarks Sample code/label Svalbard Temperature in rock/sediment Temperature Lance TL |
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. During each deployment sequence several individual stations were visited as detailed in 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. Tose Offsets are included in the individual penetration files. Within each deployment sequence, the total record is split into individual penetration files, one penetration file per station visited. Naming convention is as follows: H1607P01.pen.dat for penetration 1 of deployment sequence H1607. Each Penetration file has complete header information on the measurement and performance. Note: temperatures are reported in values of mili-degrees Celsius). 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. For each penetration, a results-file is included with in situ temperature and conductivity reported as function of Depth. Naming convention of the results files is as follows: H1607_P01_results.dat with "H1607" as deployment sequence, "P01" as penetration number. If the heat pulse was not generated, only the decay of frictional heating was used to define in situ temperature. Thermal conductivity was assumed to be constant for all depths in those instances. Here, we used a value of 1.25 for the assumed thermal conductivity. Initial results and further details of the deployments can be found in the cruise report by Bohrmann et al. (2017). |
format |
Dataset |
author |
Riedel, Michael |
author_facet |
Riedel, Michael |
author_sort |
Riedel, Michael |
title |
Heat flow data at station H1607 during Maria S. Merian cruise MSM57/1 |
title_short |
Heat flow data at station H1607 during Maria S. Merian cruise MSM57/1 |
title_full |
Heat flow data at station H1607 during Maria S. Merian cruise MSM57/1 |
title_fullStr |
Heat flow data at station H1607 during Maria S. Merian cruise MSM57/1 |
title_full_unstemmed |
Heat flow data at station H1607 during Maria S. Merian cruise MSM57/1 |
title_sort |
heat flow data at station h1607 during maria s. merian cruise msm57/1 |
publisher |
PANGAEA |
publishDate |
2020 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.911758 https://doi.org/10.1594/PANGAEA.911758 |
op_coverage |
MEDIAN LATITUDE: 79.007039 * MEDIAN LONGITUDE: 6.904477 * SOUTH-BOUND LATITUDE: 79.004617 * WEST-BOUND LONGITUDE: 6.889267 * NORTH-BOUND LATITUDE: 79.011233 * EAST-BOUND LONGITUDE: 6.912083 * DATE/TIME START: 2016-08-08T23:06:02 * DATE/TIME END: 2016-08-09T08:35:45 * MINIMUM DEPTH, sediment/rock: 0.00 m * MAXIMUM DEPTH, sediment/rock: 5.46 m |
long_lat |
ENVELOPE(5.783,5.783,78.233,78.233) ENVELOPE(6.889267,6.912083,79.011233,79.004617) |
geographic |
Svalbard Svyatogor Ridge |
geographic_facet |
Svalbard Svyatogor Ridge |
genre |
Svalbard Svalbard margin |
genre_facet |
Svalbard Svalbard margin |
op_relation |
https://doi.org/10.1594/PANGAEA.911766 Bohrmann, Gerhard; Ahrlich, Frauke; Bergenthal, Markus; Bünz, Stefan; Düßmann, Ralf; Ferreira, Christian; Freudenthal, Tim; Fröhlich, Siefke; Hamann, Kristin; Hong, W-L; Hsu, Chieh-Wei; Johnson, Joel; Kaszemeik, Kai; Kausche, Arne; Klein, Thorsten; Lange, Mirko; Lepland, Aivo; Malnati, Janice; Meckel, Sebastian; Meyer-Schack, Birgit; Noorlander, Kees; Panieri, Giuliana; Pape, Thomas; Reuter, Michael; Riedel, Michael; Rosiak, Uwe; Schmidt, Christopher; Schmidt, Werner; Seiter, Christian; Spagnoli, Giovanni; Stachowski, Adrian; Stange, Nikolas; Wallmann, Klaus; Wintersteller, Paul; Wunsch, David; Yao, Haoyi (2017): R/V MARIA S. MERIAN Cruise Report MSM57, Gas Hydrate Dynamics at the Continental Margin of Svalbard, Reykjavik - Longyearbyen - Reykjavik, 29 July - 07 September 2016. Berichte aus dem MARUM und dem Fachbereich Geowissenschaften der Universität Bremen, 314, 1-204, urn:nbn:de:gbv:46-00105895-15 Villinger, Heinrich; Davis, Earl E (1987): A new reduction algorithm for marine heat flow measurements. Journal of Geophysical Research, 92(B12), 12846, https://doi.org/10.1029/JB092iB12p12846 Heat flow data (raw and result data files) of station H1607 (MSM57) (URI: https://hs.pangaea.de/Raw/MSM/MSM57/Heatflow/H1607_data.zip) https://doi.pangaea.de/10.1594/PANGAEA.911758 https://doi.org/10.1594/PANGAEA.911758 |
op_rights |
CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/PANGAEA.911758 https://doi.org/10.1594/PANGAEA.911766 https://doi.org/10.1029/JB092iB12p12846 |
_version_ |
1766213212010708992 |
spelling |
ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.911758 2023-05-15T18:29:49+02:00 Heat flow data at station H1607 during Maria S. Merian cruise MSM57/1 Riedel, Michael MEDIAN LATITUDE: 79.007039 * MEDIAN LONGITUDE: 6.904477 * SOUTH-BOUND LATITUDE: 79.004617 * WEST-BOUND LONGITUDE: 6.889267 * NORTH-BOUND LATITUDE: 79.011233 * EAST-BOUND LONGITUDE: 6.912083 * DATE/TIME START: 2016-08-08T23:06:02 * DATE/TIME END: 2016-08-09T08:35:45 * MINIMUM DEPTH, sediment/rock: 0.00 m * MAXIMUM DEPTH, sediment/rock: 5.46 m 2020-02-05 text/tab-separated-values, 1450 data points https://doi.pangaea.de/10.1594/PANGAEA.911758 https://doi.org/10.1594/PANGAEA.911758 en eng PANGAEA https://doi.org/10.1594/PANGAEA.911766 Bohrmann, Gerhard; Ahrlich, Frauke; Bergenthal, Markus; Bünz, Stefan; Düßmann, Ralf; Ferreira, Christian; Freudenthal, Tim; Fröhlich, Siefke; Hamann, Kristin; Hong, W-L; Hsu, Chieh-Wei; Johnson, Joel; Kaszemeik, Kai; Kausche, Arne; Klein, Thorsten; Lange, Mirko; Lepland, Aivo; Malnati, Janice; Meckel, Sebastian; Meyer-Schack, Birgit; Noorlander, Kees; Panieri, Giuliana; Pape, Thomas; Reuter, Michael; Riedel, Michael; Rosiak, Uwe; Schmidt, Christopher; Schmidt, Werner; Seiter, Christian; Spagnoli, Giovanni; Stachowski, Adrian; Stange, Nikolas; Wallmann, Klaus; Wintersteller, Paul; Wunsch, David; Yao, Haoyi (2017): R/V MARIA S. MERIAN Cruise Report MSM57, Gas Hydrate Dynamics at the Continental Margin of Svalbard, Reykjavik - Longyearbyen - Reykjavik, 29 July - 07 September 2016. Berichte aus dem MARUM und dem Fachbereich Geowissenschaften der Universität Bremen, 314, 1-204, urn:nbn:de:gbv:46-00105895-15 Villinger, Heinrich; Davis, Earl E (1987): A new reduction algorithm for marine heat flow measurements. Journal of Geophysical Research, 92(B12), 12846, https://doi.org/10.1029/JB092iB12p12846 Heat flow data (raw and result data files) of station H1607 (MSM57) (URI: https://hs.pangaea.de/Raw/MSM/MSM57/Heatflow/H1607_data.zip) https://doi.pangaea.de/10.1594/PANGAEA.911758 https://doi.org/10.1594/PANGAEA.911758 CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Conductivity thermal DEPTH sediment/rock Event label GeoB21618-1 GeoB21618-10 GeoB21618-11 GeoB21618-12 GeoB21618-13 GeoB21618-14 GeoB21618-15 GeoB21618-16 GeoB21618-2 GeoB21618-3 GeoB21618-4 GeoB21618-5 GeoB21618-6 GeoB21618-7 GeoB21618-8 GeoB21618-9 heat probe Integrated thermal resistance Maria S. Merian MSM57/1 MSM57/1_630-1 MSM57/1_630-10 MSM57/1_630-11 MSM57/1_630-12 MSM57/1_630-13 MSM57/1_630-14 MSM57/1_630-15 MSM57/1_630-16 MSM57/1_630-2 MSM57/1_630-3 MSM57/1_630-4 MSM57/1_630-5 MSM57/1_630-6 MSM57/1_630-7 MSM57/1_630-8 MSM57/1_630-9 pockmarks Sample code/label Svalbard Temperature in rock/sediment Temperature Lance TL Dataset 2020 ftpangaea https://doi.org/10.1594/PANGAEA.911758 https://doi.org/10.1594/PANGAEA.911766 https://doi.org/10.1029/JB092iB12p12846 2023-01-20T10:02:10Z 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. During each deployment sequence several individual stations were visited as detailed in 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. Tose Offsets are included in the individual penetration files. Within each deployment sequence, the total record is split into individual penetration files, one penetration file per station visited. Naming convention is as follows: H1607P01.pen.dat for penetration 1 of deployment sequence H1607. Each Penetration file has complete header information on the measurement and performance. Note: temperatures are reported in values of mili-degrees Celsius). 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. For each penetration, a results-file is included with in situ temperature and conductivity reported as function of Depth. Naming convention of the results files is as follows: H1607_P01_results.dat with "H1607" as deployment sequence, "P01" as penetration number. If the heat pulse was not generated, only the decay of frictional heating was used to define in situ temperature. Thermal conductivity was assumed to be constant for all depths in those instances. Here, we used a value of 1.25 for the assumed thermal conductivity. Initial results and further details of the deployments can be found in the cruise report by Bohrmann et al. (2017). Dataset Svalbard Svalbard margin PANGAEA - Data Publisher for Earth & Environmental Science Svalbard Svyatogor Ridge ENVELOPE(5.783,5.783,78.233,78.233) ENVELOPE(6.889267,6.912083,79.011233,79.004617) |