IODP Expedition 392 Thermal conductivity

• Main Authors: Uenzelmann-Neben, Gabriele, Bohaty, Steven M., Childress, Laurel B., Archontikis, Odysseas A., Batenburg, Sietske J., Bijl, Peter K., Burkett, Ashley M., Cawthra, Hayley C., Chanda, Pratyusha, Coenen, Jason J., Dallanave, Edoardo, Davidson, Peter C., Doiron, Kelsey E., Geldmacher, Jörg, Gürer, Derya, Haynes, Shannon J., Herrle, Jens O., Ichiyama, Yuji, Jana, Debadrita, Jones, Matthew M., Kato, Chie, Kulhanek, Denise K., Li, Juan, Liu, Jia, McManus, James, Minakov, Alexander N., Penman, Donald E., Sprain, Courtney J., Tessin, Allyson C., Wagner, Thomas, Westerhold, Thomas
• Other Authors: International Ocean Discovery Program
• Format: Dataset
• Language: unknown
• Published: 2023
• Subjects: International Ocean Discovery Program; IODP; JOIDES Resolution; Expedition 392; Site U1579; Site U1580; Site U1581; Site U1582; Algulhas Plateau Cretaceous Climate; Earth connections; Climate and ocean change; K/Pg boundary; large igneous province; PETM; LIP; zeolite authigenesis; Paleocene-Eocene Thermal Maximum; igneous sill intrusion; Campanian; Oligocene pelagic carbonates; paleoceanography; African-Southern Ocean Gateway; Southern Ocean
• Online Access: https://zenodo.org/record/8277857; https://doi.org/10.5281/zenodo.8277857

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.