IODP Expedition 360 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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| creator | Dick, Henry J.B. MacLeod, Christopher J. Blum, Peter Abe, Natsue Blackman, Donna K. Bowles, Julie A. Cheadle, Michael J. Cho, Kyungo Ciazela, Jakub Deans, Jeremy R. Edgcomb, Virginia P. Ferrando, Carlotta France, Lyderic Ghosh, Biswajit Ildefonse, Benoit Kendrick, Mark A. Koepke, Juergen H. Leong, James A.M. Liu, Chuanzhou Ma, Qiang Morishita, Tomoaki Morris, Antony Natland, James H. Nozaka, Toshio Pluemper, Oliver Sanfilippo, Alessio Sylvan, Jason B. Tivey, Maurice A Tribuzio, Riccardo Viegas, Luis G.F. |
| 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 basalts. |
| doi_str_mv | 10.5281/zenodo.11982358 |
| format | Dataset |
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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 basalts.</description><identifier>DOI: 10.5281/zenodo.11982358</identifier><language>eng</language><publisher>International Ocean Discovery Program</publisher><subject>Atlantis Bank ; Atlantis II Transform ; Earth connections ; Expedition 360 ; Hole 1105A ; International Ocean Discovery Program ; IODP ; JOIDES Resolution ; mid-ocean ridge ; Moho ; Mohorovicic discontinuity ; Site U1473 ; SloMo ; slow spreading ridge ; Southwest Indian Ridge ; upper mantle</subject><creationdate>2017</creationdate><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><orcidid>0000-0002-7484-8149 ; 0000-0001-7361-7472 ; 0000-0003-1360-8202 ; 0000-0002-3261-6331 ; 0000-0001-5282-0690 ; 0000-0002-5197-4089 ; 0000-0002-6541-4162 ; 0000-0003-4675-4513 ; 0000-0002-0460-1626 ; 0000-0003-4086-8333 ; 0000-0002-2734-0035 ; 0000-0003-0225-1439 ; 0000-0003-4880-3841 ; 0000-0003-1138-0072 ; 0000-0003-0821-1155 ; 0000-0003-2862-7377 ; 0000-0002-4112-3643 ; 0000-0001-6805-381X ; 0000-0001-6249-8244 ; 0000-0001-7635-9288</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>777,1888</link.rule.ids><linktorsrc>$$Uhttps://commons.datacite.org/doi.org/10.5281/zenodo.11982358$$EView_record_in_DataCite.org$$FView_record_in_$$GDataCite.org$$Hfree_for_read</linktorsrc></links><search><creatorcontrib>Dick, Henry J.B.</creatorcontrib><creatorcontrib>MacLeod, Christopher J.</creatorcontrib><creatorcontrib>Blum, Peter</creatorcontrib><creatorcontrib>Abe, Natsue</creatorcontrib><creatorcontrib>Blackman, Donna K.</creatorcontrib><creatorcontrib>Bowles, Julie A.</creatorcontrib><creatorcontrib>Cheadle, Michael J.</creatorcontrib><creatorcontrib>Cho, Kyungo</creatorcontrib><creatorcontrib>Ciazela, Jakub</creatorcontrib><creatorcontrib>Deans, Jeremy R.</creatorcontrib><creatorcontrib>Edgcomb, Virginia P.</creatorcontrib><creatorcontrib>Ferrando, Carlotta</creatorcontrib><creatorcontrib>France, Lyderic</creatorcontrib><creatorcontrib>Ghosh, Biswajit</creatorcontrib><creatorcontrib>Ildefonse, Benoit</creatorcontrib><creatorcontrib>Kendrick, Mark A.</creatorcontrib><creatorcontrib>Koepke, Juergen H.</creatorcontrib><creatorcontrib>Leong, James A.M.</creatorcontrib><creatorcontrib>Liu, Chuanzhou</creatorcontrib><creatorcontrib>Ma, Qiang</creatorcontrib><creatorcontrib>Morishita, Tomoaki</creatorcontrib><creatorcontrib>Morris, Antony</creatorcontrib><creatorcontrib>Natland, James H.</creatorcontrib><creatorcontrib>Nozaka, Toshio</creatorcontrib><creatorcontrib>Pluemper, Oliver</creatorcontrib><creatorcontrib>Sanfilippo, Alessio</creatorcontrib><creatorcontrib>Sylvan, Jason B.</creatorcontrib><creatorcontrib>Tivey, Maurice A</creatorcontrib><creatorcontrib>Tribuzio, Riccardo</creatorcontrib><creatorcontrib>Viegas, Luis G.F.</creatorcontrib><title>IODP Expedition 360 Moisture and Density</title><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. 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Submethod D is suitable for unsaturated porous material such as certain limestones and basalts.</description><subject>Atlantis Bank</subject><subject>Atlantis II Transform</subject><subject>Earth connections</subject><subject>Expedition 360</subject><subject>Hole 1105A</subject><subject>International Ocean Discovery Program</subject><subject>IODP</subject><subject>JOIDES Resolution</subject><subject>mid-ocean ridge</subject><subject>Moho</subject><subject>Mohorovicic discontinuity</subject><subject>Site U1473</subject><subject>SloMo</subject><subject>slow spreading ridge</subject><subject>Southwest Indian Ridge</subject><subject>upper mantle</subject><fulltext>true</fulltext><rsrctype>dataset</rsrctype><creationdate>2017</creationdate><recordtype>dataset</recordtype><sourceid>PQ8</sourceid><recordid>eNpjYBA3NNAzNbIw1K9KzctPydczNLS0MDI2teBk0PD0dwlQcK0oSE3JLMnMz1MwNjNQ8M3PLC4pLUpVSMxLUXBJzSvOLKnkYWBNS8wpTuWF0twM-m6uIc4euimJJYnJmSWp8QVFmbmJRZXxhgbxILviIXbFw-wyJl0HAHHkN2k</recordid><startdate>20170130</startdate><enddate>20170130</enddate><creator>Dick, Henry J.B.</creator><creator>MacLeod, Christopher J.</creator><creator>Blum, Peter</creator><creator>Abe, Natsue</creator><creator>Blackman, Donna K.</creator><creator>Bowles, Julie A.</creator><creator>Cheadle, Michael J.</creator><creator>Cho, Kyungo</creator><creator>Ciazela, Jakub</creator><creator>Deans, Jeremy R.</creator><creator>Edgcomb, Virginia P.</creator><creator>Ferrando, Carlotta</creator><creator>France, Lyderic</creator><creator>Ghosh, Biswajit</creator><creator>Ildefonse, Benoit</creator><creator>Kendrick, Mark A.</creator><creator>Koepke, Juergen H.</creator><creator>Leong, James A.M.</creator><creator>Liu, Chuanzhou</creator><creator>Ma, Qiang</creator><creator>Morishita, Tomoaki</creator><creator>Morris, Antony</creator><creator>Natland, James H.</creator><creator>Nozaka, Toshio</creator><creator>Pluemper, Oliver</creator><creator>Sanfilippo, Alessio</creator><creator>Sylvan, Jason B.</creator><creator>Tivey, Maurice A</creator><creator>Tribuzio, Riccardo</creator><creator>Viegas, Luis G.F.</creator><general>International Ocean Discovery Program</general><scope>DYCCY</scope><scope>PQ8</scope><orcidid>https://orcid.org/0000-0002-7484-8149</orcidid><orcidid>https://orcid.org/0000-0001-7361-7472</orcidid><orcidid>https://orcid.org/0000-0003-1360-8202</orcidid><orcidid>https://orcid.org/0000-0002-3261-6331</orcidid><orcidid>https://orcid.org/0000-0001-5282-0690</orcidid><orcidid>https://orcid.org/0000-0002-5197-4089</orcidid><orcidid>https://orcid.org/0000-0002-6541-4162</orcidid><orcidid>https://orcid.org/0000-0003-4675-4513</orcidid><orcidid>https://orcid.org/0000-0002-0460-1626</orcidid><orcidid>https://orcid.org/0000-0003-4086-8333</orcidid><orcidid>https://orcid.org/0000-0002-2734-0035</orcidid><orcidid>https://orcid.org/0000-0003-0225-1439</orcidid><orcidid>https://orcid.org/0000-0003-4880-3841</orcidid><orcidid>https://orcid.org/0000-0003-1138-0072</orcidid><orcidid>https://orcid.org/0000-0003-0821-1155</orcidid><orcidid>https://orcid.org/0000-0003-2862-7377</orcidid><orcidid>https://orcid.org/0000-0002-4112-3643</orcidid><orcidid>https://orcid.org/0000-0001-6805-381X</orcidid><orcidid>https://orcid.org/0000-0001-6249-8244</orcidid><orcidid>https://orcid.org/0000-0001-7635-9288</orcidid></search><sort><creationdate>20170130</creationdate><title>IODP Expedition 360 Moisture and Density</title><author>Dick, Henry J.B. ; MacLeod, Christopher J. ; Blum, Peter ; Abe, Natsue ; Blackman, Donna K. ; Bowles, Julie A. ; Cheadle, Michael J. ; Cho, Kyungo ; Ciazela, Jakub ; Deans, Jeremy R. ; Edgcomb, Virginia P. ; Ferrando, Carlotta ; France, Lyderic ; Ghosh, Biswajit ; Ildefonse, Benoit ; Kendrick, Mark A. ; Koepke, Juergen H. ; Leong, James A.M. ; Liu, Chuanzhou ; Ma, Qiang ; Morishita, Tomoaki ; Morris, Antony ; Natland, James H. ; Nozaka, Toshio ; Pluemper, Oliver ; Sanfilippo, Alessio ; Sylvan, Jason B. ; Tivey, Maurice A ; Tribuzio, Riccardo ; Viegas, Luis G.F.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-datacite_primary_10_5281_zenodo_119823583</frbrgroupid><rsrctype>datasets</rsrctype><prefilter>datasets</prefilter><language>eng</language><creationdate>2017</creationdate><topic>Atlantis Bank</topic><topic>Atlantis II Transform</topic><topic>Earth connections</topic><topic>Expedition 360</topic><topic>Hole 1105A</topic><topic>International Ocean Discovery Program</topic><topic>IODP</topic><topic>JOIDES Resolution</topic><topic>mid-ocean ridge</topic><topic>Moho</topic><topic>Mohorovicic discontinuity</topic><topic>Site U1473</topic><topic>SloMo</topic><topic>slow spreading ridge</topic><topic>Southwest Indian Ridge</topic><topic>upper mantle</topic><toplevel>online_resources</toplevel><creatorcontrib>Dick, Henry J.B.</creatorcontrib><creatorcontrib>MacLeod, Christopher J.</creatorcontrib><creatorcontrib>Blum, Peter</creatorcontrib><creatorcontrib>Abe, Natsue</creatorcontrib><creatorcontrib>Blackman, Donna K.</creatorcontrib><creatorcontrib>Bowles, Julie A.</creatorcontrib><creatorcontrib>Cheadle, Michael J.</creatorcontrib><creatorcontrib>Cho, Kyungo</creatorcontrib><creatorcontrib>Ciazela, Jakub</creatorcontrib><creatorcontrib>Deans, Jeremy R.</creatorcontrib><creatorcontrib>Edgcomb, Virginia P.</creatorcontrib><creatorcontrib>Ferrando, Carlotta</creatorcontrib><creatorcontrib>France, Lyderic</creatorcontrib><creatorcontrib>Ghosh, Biswajit</creatorcontrib><creatorcontrib>Ildefonse, Benoit</creatorcontrib><creatorcontrib>Kendrick, Mark A.</creatorcontrib><creatorcontrib>Koepke, Juergen H.</creatorcontrib><creatorcontrib>Leong, James A.M.</creatorcontrib><creatorcontrib>Liu, Chuanzhou</creatorcontrib><creatorcontrib>Ma, Qiang</creatorcontrib><creatorcontrib>Morishita, Tomoaki</creatorcontrib><creatorcontrib>Morris, Antony</creatorcontrib><creatorcontrib>Natland, James H.</creatorcontrib><creatorcontrib>Nozaka, Toshio</creatorcontrib><creatorcontrib>Pluemper, Oliver</creatorcontrib><creatorcontrib>Sanfilippo, Alessio</creatorcontrib><creatorcontrib>Sylvan, Jason B.</creatorcontrib><creatorcontrib>Tivey, Maurice A</creatorcontrib><creatorcontrib>Tribuzio, Riccardo</creatorcontrib><creatorcontrib>Viegas, Luis G.F.</creatorcontrib><collection>DataCite (Open Access)</collection><collection>DataCite</collection></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext_linktorsrc</fulltext></delivery><addata><au>Dick, Henry J.B.</au><au>MacLeod, Christopher J.</au><au>Blum, Peter</au><au>Abe, Natsue</au><au>Blackman, Donna K.</au><au>Bowles, Julie A.</au><au>Cheadle, Michael J.</au><au>Cho, Kyungo</au><au>Ciazela, Jakub</au><au>Deans, Jeremy R.</au><au>Edgcomb, Virginia P.</au><au>Ferrando, Carlotta</au><au>France, Lyderic</au><au>Ghosh, Biswajit</au><au>Ildefonse, Benoit</au><au>Kendrick, Mark A.</au><au>Koepke, Juergen H.</au><au>Leong, James A.M.</au><au>Liu, Chuanzhou</au><au>Ma, Qiang</au><au>Morishita, Tomoaki</au><au>Morris, Antony</au><au>Natland, James H.</au><au>Nozaka, Toshio</au><au>Pluemper, Oliver</au><au>Sanfilippo, Alessio</au><au>Sylvan, Jason B.</au><au>Tivey, Maurice A</au><au>Tribuzio, Riccardo</au><au>Viegas, Luis G.F.</au><format>book</format><genre>unknown</genre><ristype>DATA</ristype><title>IODP Expedition 360 Moisture and Density</title><date>2017-01-30</date><risdate>2017</risdate><abstract>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. 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| identifier | DOI: 10.5281/zenodo.11982358 |
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| source | DataCite |
| subjects | Atlantis Bank Atlantis II Transform Earth connections Expedition 360 Hole 1105A International Ocean Discovery Program IODP JOIDES Resolution mid-ocean ridge Moho Mohorovicic discontinuity Site U1473 SloMo slow spreading ridge Southwest Indian Ridge upper mantle |
| title | IODP Expedition 360 Moisture and Density |
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