IODP Expedition 379 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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International Ocean Discovery Program
2021
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Online Access: | https://dx.doi.org/10.5281/zenodo.11200378 https://zenodo.org/doi/10.5281/zenodo.11200378 |
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ftdatacite:10.5281/zenodo.11200378 2024-09-09T18:59:55+00:00 IODP Expedition 379 Moisture and Density ... Gohl, Karsten Wellner, Julia S. Klaus, Adam Bauersachs, Thorsten Bohaty, Steven Courtillat, Margot Cowan, Ellen A. De Lira Mota, Marcelo A. Esteves, Mariana S.R. Fegyveresi, John M. Frederichs, Thomas Gao, Liang Halberstandt, Anna R. Hillenbrand, Claus-Dieter Horikawa, Keiji Iwai, Masao Kim, Ji-Hoon King, Theresa M. Klages, Johann P. MacCaull, J.G.N. Passchier, Sandra Penkrot, Michelle Powell, John L. Prebble, Joseph Graham Rahaman, Waliur Reinardy, Benedict T.I. Renaudie, Johan Robinson, Delaney E. Scherer, Reed P. Siddoway, Christine S. Wu, Li Yamane, Masako 2021 https://dx.doi.org/10.5281/zenodo.11200378 https://zenodo.org/doi/10.5281/zenodo.11200378 unknown International Ocean Discovery Program https://dx.doi.org/10.14379/iodp.proc.379.2021 https://dx.doi.org/10.5281/zenodo.11200377 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 International Ocean Discovery Program IODP JOIDES Resolution Expedition 379 Site U1532 Site U1533 Amundsen Sea West Antarctic Ice Sheet History Amundsen Sea Embayment Pine Island Glacier Thwaites Glacier Marie Byrd Land paleoclimate paleo-ice sheet continental rise sediment drift contourite ice-rafted debris Environmental change, processes, and effects glacial-interglacial cyclicity seismic stratigraphy dataset Dataset 2021 ftdatacite https://doi.org/10.5281/zenodo.1120037810.14379/iodp.proc.379.202110.5281/zenodo.11200377 2024-06-17T09:53:22Z 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 ... Dataset Amundsen Sea Antarc* Antarctic Ice Sheet Marie Byrd Land Pine Island Glacier Thwaites Glacier DataCite Antarctic Amundsen Sea West Antarctic Ice Sheet Byrd Pine Island Glacier ENVELOPE(-101.000,-101.000,-75.000,-75.000) Marie Byrd Land ENVELOPE(-130.000,-130.000,-78.000,-78.000) Thwaites Glacier ENVELOPE(-106.750,-106.750,-75.500,-75.500) |
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unknown |
topic |
International Ocean Discovery Program IODP JOIDES Resolution Expedition 379 Site U1532 Site U1533 Amundsen Sea West Antarctic Ice Sheet History Amundsen Sea Embayment Pine Island Glacier Thwaites Glacier Marie Byrd Land paleoclimate paleo-ice sheet continental rise sediment drift contourite ice-rafted debris Environmental change, processes, and effects glacial-interglacial cyclicity seismic stratigraphy |
spellingShingle |
International Ocean Discovery Program IODP JOIDES Resolution Expedition 379 Site U1532 Site U1533 Amundsen Sea West Antarctic Ice Sheet History Amundsen Sea Embayment Pine Island Glacier Thwaites Glacier Marie Byrd Land paleoclimate paleo-ice sheet continental rise sediment drift contourite ice-rafted debris Environmental change, processes, and effects glacial-interglacial cyclicity seismic stratigraphy Gohl, Karsten Wellner, Julia S. Klaus, Adam Bauersachs, Thorsten Bohaty, Steven Courtillat, Margot Cowan, Ellen A. De Lira Mota, Marcelo A. Esteves, Mariana S.R. Fegyveresi, John M. Frederichs, Thomas Gao, Liang Halberstandt, Anna R. Hillenbrand, Claus-Dieter Horikawa, Keiji Iwai, Masao Kim, Ji-Hoon King, Theresa M. Klages, Johann P. MacCaull, J.G.N. Passchier, Sandra Penkrot, Michelle Powell, John L. Prebble, Joseph Graham Rahaman, Waliur Reinardy, Benedict T.I. Renaudie, Johan Robinson, Delaney E. Scherer, Reed P. Siddoway, Christine S. Wu, Li Yamane, Masako IODP Expedition 379 Moisture and Density ... |
topic_facet |
International Ocean Discovery Program IODP JOIDES Resolution Expedition 379 Site U1532 Site U1533 Amundsen Sea West Antarctic Ice Sheet History Amundsen Sea Embayment Pine Island Glacier Thwaites Glacier Marie Byrd Land paleoclimate paleo-ice sheet continental rise sediment drift contourite ice-rafted debris Environmental change, processes, and effects glacial-interglacial cyclicity seismic stratigraphy |
description |
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 ... |
format |
Dataset |
author |
Gohl, Karsten Wellner, Julia S. Klaus, Adam Bauersachs, Thorsten Bohaty, Steven Courtillat, Margot Cowan, Ellen A. De Lira Mota, Marcelo A. Esteves, Mariana S.R. Fegyveresi, John M. Frederichs, Thomas Gao, Liang Halberstandt, Anna R. Hillenbrand, Claus-Dieter Horikawa, Keiji Iwai, Masao Kim, Ji-Hoon King, Theresa M. Klages, Johann P. MacCaull, J.G.N. Passchier, Sandra Penkrot, Michelle Powell, John L. Prebble, Joseph Graham Rahaman, Waliur Reinardy, Benedict T.I. Renaudie, Johan Robinson, Delaney E. Scherer, Reed P. Siddoway, Christine S. Wu, Li Yamane, Masako |
author_facet |
Gohl, Karsten Wellner, Julia S. Klaus, Adam Bauersachs, Thorsten Bohaty, Steven Courtillat, Margot Cowan, Ellen A. De Lira Mota, Marcelo A. Esteves, Mariana S.R. Fegyveresi, John M. Frederichs, Thomas Gao, Liang Halberstandt, Anna R. Hillenbrand, Claus-Dieter Horikawa, Keiji Iwai, Masao Kim, Ji-Hoon King, Theresa M. Klages, Johann P. MacCaull, J.G.N. Passchier, Sandra Penkrot, Michelle Powell, John L. Prebble, Joseph Graham Rahaman, Waliur Reinardy, Benedict T.I. Renaudie, Johan Robinson, Delaney E. Scherer, Reed P. Siddoway, Christine S. Wu, Li Yamane, Masako |
author_sort |
Gohl, Karsten |
title |
IODP Expedition 379 Moisture and Density ... |
title_short |
IODP Expedition 379 Moisture and Density ... |
title_full |
IODP Expedition 379 Moisture and Density ... |
title_fullStr |
IODP Expedition 379 Moisture and Density ... |
title_full_unstemmed |
IODP Expedition 379 Moisture and Density ... |
title_sort |
iodp expedition 379 moisture and density ... |
publisher |
International Ocean Discovery Program |
publishDate |
2021 |
url |
https://dx.doi.org/10.5281/zenodo.11200378 https://zenodo.org/doi/10.5281/zenodo.11200378 |
long_lat |
ENVELOPE(-101.000,-101.000,-75.000,-75.000) ENVELOPE(-130.000,-130.000,-78.000,-78.000) ENVELOPE(-106.750,-106.750,-75.500,-75.500) |
geographic |
Antarctic Amundsen Sea West Antarctic Ice Sheet Byrd Pine Island Glacier Marie Byrd Land Thwaites Glacier |
geographic_facet |
Antarctic Amundsen Sea West Antarctic Ice Sheet Byrd Pine Island Glacier Marie Byrd Land Thwaites Glacier |
genre |
Amundsen Sea Antarc* Antarctic Ice Sheet Marie Byrd Land Pine Island Glacier Thwaites Glacier |
genre_facet |
Amundsen Sea Antarc* Antarctic Ice Sheet Marie Byrd Land Pine Island Glacier Thwaites Glacier |
op_relation |
https://dx.doi.org/10.14379/iodp.proc.379.2021 https://dx.doi.org/10.5281/zenodo.11200377 |
op_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_doi |
https://doi.org/10.5281/zenodo.1120037810.14379/iodp.proc.379.202110.5281/zenodo.11200377 |
_version_ |
1809936215559897088 |