PANGAEA_962163
Thermal conductivity measurements of nearshore sediments in Eckernförde Bay, Baltic Sea aquired during ALKOR cruise AL584
Dillon, Melanie; Nehring, Franziska
Thermal conductivity measurements of nearshore sediments in Eckernförde Bay, Baltic Sea aquired during ALKOR cruise AL584
2023-12-05
PANGAEA
Dataset
https://doi.pangaea.de/10.1594/PANGAEA.962163
Investigator
Melanie
Dillon
dillon@fielax.de
Earth Science
Event label
Location ID
DATE/TIME
LATITUDE
LONGITUDE
Thermistor number
DEPTH, sediment/rock
Temperature, in rock/sediment
Conductivity, thermal
geoscientificInformation
AL584
AL584_10-1
AL584_1-1
AL584_2-1
AL584_3-1
AL584_5-1
AL584_6-1
AL584_7-1
AL584_8-1
AL584_9-1
Eckernförde Bay
nearshore sediments
Thermal conductivity
Vibro corer
Calculated according to Hartmann & Villinger (2002)
Alkor (1990)
2022-11-09
2022-11-10
Complete
54.4963
54.512
10.027
10.059
0.6 m (DEPTH, sediment/rock)
4.15 m (DEPTH, sediment/rock)
WEGNordOst
Wechselwirkungen zwischen Energieseekabeln und Gasen in Sedimenten der Nord- und Ostsee
unrestricted
CC-BY-4.0: Creative Commons Attribution 4.0 International
English
PANGAEA
Data Publisher for Earth & Environmental Science
https://www.pangaea.de/
Data Center Contact
Michael
Diepenbroek
info@pangaea.de
Leobener Str.
Bremen
Bremen
28359
Germany
online
792 data points
text/tab-separated-values
Usbeck, Regina; Dillon, Melanie; Kaul, Norbert; Lohrberg, Arne; Nehring, Franziska; Plötz, Aline (2023): High variability and exceptionally low thermal conductivities in nearshore sediments: a case study from the Eckernförde Bay. Marine Geophysical Research, 44, 24, https://doi.org/10.1007/s11001-023-09531-2
Hartmann, Andreas; Villinger, Heinrich (2002): Inversion of marine heat flow measurements by expansion of the temperature decay function. Geophysical Journal International, 148(3), 628-636, https://doi.org/10.1046/j.1365-246X.2002.01600.x
Thermal conductivity data of nearshore sediments were collected during ALKOR cruise AL584 in November 2022 using the VibroHeat system developed by FIELAX GmbH. This system combines a vibrocorer with a sensor string that contains 22 negative temperature coefficient thermistors (NTCs) and a heating wire over which a defined heat pulse is released. In-situ temperature and thermal conductivity of the sediment are calculated for each thermistor using the inversion method according to Hartmann & Villinger (2002) . ** For all details see the full metadata description at "https://doi.pangaea.de/10.1594/PANGAEA.962163"!
http://en.wikipedia.org/wiki/ISO_6709
LATITUDE
http://en.wikipedia.org/wiki/ISO_6709
LONGITUDE
http://en.wikipedia.org/wiki/ISO_8601
DATE/TIME
http://en.wikipedia.org/wiki/Thermal_conductivity
Conductivity, thermal
https://doi.org/10.1007/s11001-023-09531-2
High variability and exceptionally low thermal conductivities in nearshore sediments: a case study from the Eckernförde Bay
https://doi.org/10.1046/j.1365-246X.2002.01600.x
Calculated according to Hartmann & Villinger (2002)
https://doi.org/10.1046/j.1365-246X.2002.01600.x
Inversion of marine heat flow measurements by expansion of the temperature decay function
https://www.fielax.de/en/2022/09/16/feedback-between-temperature-and-thermal-conductivity/
WEGNordOst
https://www2.bsh.de/aktdat/dod/fahrtplanung/Alkor.htm
Alkor (1990)
DIF
9.4
2023-12-05
2026-04-29