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Fulthorpe, Craig S; Hoyanagi, Koichi; Blum, Peter; Expedition 317 Scientists (2012): Moisture and density (MAD) measured on IODP Hole 317-U1354B. PANGAEA, https://doi.org/10.1594/PANGAEA.778806

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Related to:
Fulthorpe, Craig S; Hoyanagi, Koichi; Blum, Peter; Expedition 317 Scientists (2011): Proceedings of the Integrated Ocean Drilling Program. Washington, DC (Integrated Ocean Drilling Program Management International, Inc.), 317, https://doi.org/10.2204/iodp.proc.317.2011
IODP/USIO (2012): LIMS Database. Ocean Drilling Programm, Texas A&M University, College station TX 77845-9547, USA, http://web.iodp.tamu.edu/UWQ/
Coverage:
Latitude: -44.847270 * Longitude: 171.786780
Date/Time Start: 2009-12-29T23:00:00 * Date/Time End: 2009-12-30T12:45:00
Minimum DEPTH, sediment/rock: 1.46 m * Maximum DEPTH, sediment/rock: 75.89 m
Event(s):
317-U1354B * Latitude: -44.847270 * Longitude: 171.786780 * Date/Time Start: 2009-12-29T23:00:00 * Date/Time End: 2009-12-30T12:45:00 * Elevation: -113.4 m * Penetration: 77.2 m * Recovery: 77.5 m * Campaign: Exp317 (Canterbury Basin) * Basis: Joides Resolution * Device: Drilling/drill rig (DRILL) * Comment: 15 cores; 77.2 m cored; 100 % recovered; 0 m drilled; 77.2 m penetrated
Comment:
Geocode = Depth CSF-A (m).
MAD data are acquired on ~10 mL sediment or rock subsamples by measuring three out of four material parameters: wet (saturated) mass and/or volume, and dry mass and/or volume after 24 h drying in a convection oven. The combination of measurements is defined by the submethod (A, B, C, D). Wet (A, B, C) and dry (A, B, C, D) mass is determined using motion-compensated signals from commercial Mettler-Toledo balances. Wet volume (A, B, D) is determined by the sample's geometric dimensions using calipers. Dry volume (C, 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.
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.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethodComment
1Sample code/labelSample labelExpedition 317 ScientistsODP sample designation
2DEPTH, sediment/rockDepthmGeocode
3Depth, top/minDepth topmExpedition 317 ScientistsDepth CSF-B (m)
4Sample methodSample methodExpedition 317 ScientistsSubmethod
5Water content, wet massWater wm%Expedition 317 ScientistsCalculated
6Water content, dry massWater dm%Expedition 317 ScientistsCalculated
7DensityDensityg/cm3Expedition 317 ScientistsCalculated
8Density, dry bulkDBDg/cm3Expedition 317 ScientistsCalculated
9Density, grainDensity graing/cm3Expedition 317 ScientistsCalculated
10PorosityPoros% volExpedition 317 ScientistsCalculated
11Void Ratio descriptionVoid RatioExpedition 317 ScientistsCalculated
12Wet massWet mgExpedition 317 Scientists
13Sample dry massSamp dmgExpedition 317 Scientists
14Mass, pore waterMass pwgExpedition 317 Scientists
15Salt contentSaltgExpedition 317 Scientists
16Mass, solidsMass, solidsgExpedition 317 Scientists
17Volume, wet sampleVol, wet samplecm3Expedition 317 Scientists
18Volume, dry sampleVol, dry samplecm3Expedition 317 Scientists
19Volume, pore waterVol pwcm3Expedition 317 Scientists
20Volume, saltVol, saltcm3Expedition 317 Scientists
21Volume, solidsVol solidscm3Expedition 317 Scientists
22Time StampTime StampExpedition 317 Scientists
Size:
1008 data points

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