IODP Expedition 396 Moisture and Density ...

Moisture and density (MAD) data were acquired on ~10 mL sediment or rock samples by measuring three out of four material parameters: wet (saturated) mass, wet volume, dry mass, and/or dry volume after 24 h drying in a convection oven at 105 degrees C. From the moisture and volume measurements, the f...

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Bibliographic Details
Main Authors: Planke, Sverre, Berndt, Christian, Alvarez Zarikian, Carlos A., Agarwal, Amar, Andrews, Graham D.M., Betlem, Peter, Bhattacharya, Joyeeta, Brinkhuis, Henk, Chatterjee, Sayantani, Christopoulou, Marialena, Clementi, Vincent J., Ferré, Eric C., Filina, Irina Y., Frieling, Joost, Guo, Pengyuan, Harper, Dustin T., Jones, Morgan T., Lambart, Sarah, Longman, Jack, Millett, John, Mohn, Geoffroy, Nakaoka, Reina, Scherer, Reed P., Tegner, Christian, Varela, Natalia, Wang, Mengyuan, Xu, Weimu, Yager, Stacy L.
Format: Dataset
Language:unknown
Published: Zenodo 2023
Subjects:
International Ocean Discovery Program
IODP
JOIDES Resolution
Expedition 396
Site U1565
Site U1566
Site U1567
Site U1568
Site U1569
Site U1570
Site U1571
Site U1572
Site U1573
Site U1574
Mid-Norwegian margin magmatism and paleoclimate implications
Earth connections
Climate and ocean change
North Atlantic Igneous Province
large igneous province
PETM
Paleogene hothouse
volcanic rifted margin
Paleocene-Eocene Thermal Maximum
North Atlantic
Online Access:https://dx.doi.org/10.5281/zenodo.7806322
https://zenodo.org/record/7806322
Description
Summary:Moisture and density (MAD) data were acquired on ~10 mL sediment or rock samples by measuring three out of four material parameters: wet (saturated) mass, wet volume, dry mass, and/or dry volume after 24 h drying in a convection oven at 105 degrees C. From the moisture and volume measurements, the following phase relationships are calculated: wet and dry water content, wet bulk density, dry bulk density, grain density, porosity, and void ratio. The combination of measurements is defined by the submethod chosen: A, B, C, or D. Wet (A, B, or C) and dry (A, B, C, or D) mass is determined using motion-compensated balances. Wet volume is determined either by helium pycnometry (A) or by the sample's geometric dimensions using calipers (A or D). Dry volume (C or D) is measured by helium pycnometry. Submethods A and B are not recommended by IODP. Submethod C is suitable for saturated materials such as fine-grained sediments. Submethod D is suitable for unsaturated porous material such as certain limestones and ...

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