IODP Expedition 382 Thermal conductivity

• Main Authors: Weber, Michael E., Raymo, Maureen E., Peck, Victoria L., Williams, Trevor, Armbrecht, Linda, Bailey, Ian, Brachfeld, Stefanie, Cardillo, Fabricio G., Du, Zhiheng, Fauth, Gerson, Garcia, Marga, Glüder, Anna, Guitard, Michelle, Gutjahr, Marcus, Hemming, Sidney R., Hernández-Almeida, Iván, Hoem, Frida S., Hwang, J. H., Iizuka, Mutsumi, Kato, Yuji, Kenlee, Bridget, Martos, Yasmina M., Mello, Anthony D., O'Connell, Suzanne, Perez, Lara F., Reilly, Brendan T., Ronge, Thomas A., Seki, Osamu, Tauxe, Lisa, Tripathi, Shubham, Warnock, Jonathan, Zheng, Xufeng
• Other Authors: International Ocean Discovery Program
• Format: Dataset
• Language: unknown
• Published: 2021
• Subjects: International Ocean Discovery Program; IODP; JOIDES Resolution; Expedition 382; Site U1537; Site U1535; Site U1536; Site U1538; Iceberg Alley; climate and ocean change; Subantarctic Ice and Ocean Dynamics; Subantarctic front; ice sheets; sea level; Scotia Sea; Weddell Sea; sea ice; ice-rafted debris; Antarctic Circumpolar Current; mid-Pleistocene transition; MPT; Antarctic; Weddell; Antarc*; Iceberg*; Sea ice
• Online Access: https://zenodo.org/record/8264022; https://doi.org/10.5281/zenodo.8264022

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.