IODP Expedition 378 Thermal conductivity

Thermal conductivity was measured using the heated needle method in either full-space needle configuration (soft/saturated sediments) or half-space needle configuration (harder materials) of a TeKa Berlin TK-04 thermal conductivity meter. Heat is applied to the sample and then thermal equilibrium is...

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Bibliographic Details
Main Authors: Röhl, Ursula, Thomas, Deborah J., Childress, Laurel B., Anagnostou, Eleni, Ausín, Blanca, Boscolo Galazzo, Flavia, Dias, Bruna Borba, Brzelinski, Swaantje, Dunlea, Ann G., George, Simon C., Haynes, Laura L., Hendy, Ingrid L., Jones, Heather L., Khanolkar, Sonal S., Kitch, Gabriella D., Lee, Hojun, Raffi, Isabella, Reis, Alex J., Sheward, Rosie M., Sibert, Elizabeth, Tanaka, Erika, Wilkens, Roy H., Yasukawa, Kazutaka, Yuan, Wei, Zhang, Qiang, Zhang, Yang, Drury, Anna J., Hollis, Christopher J.
Other Authors: International Ocean Discovery Program
Format: Other/Unknown Material
Language:unknown
Published: International Ocean Discovery Program 2022
Subjects:
International Ocean Discovery Program
IODP
JOIDES Resolution
Expedition 378
Site U1553
South Pacific Paleogene Climate
climate and ocean change
Campbell Plateau
high southern latitude
carbon system dynamics
Cenozoic climate history
high CO2 world
chronostratigraphy
ocean circulation
intermediate water formation
hydrologic cycling
biological productivity
ice sheet dynamics
Ice Sheet
Online Access:https://doi.org/10.5281/zenodo.10810034
Description
Summary:Thermal conductivity was measured using the heated needle method in either full-space needle configuration (soft/saturated sediments) or half-space needle configuration (harder materials) of a TeKa Berlin TK-04 thermal conductivity meter. Heat is applied to the sample and then thermal equilibrium is sought. The heating and equilibration curve is reduced to derive the thermal conductivity value. Raw data are stored if a user wishes to do off-line or postexpedition reduction.

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