Fulthorpe, Craig S; Hoyanagi, Koichi; Blum, Peter; Expedition 317 Scientists (2012): Moisture and density (MAD) measured on IODP Hole 317-U1353A [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.778573
Always quote citation above when using data! You can download the citation in several formats below.
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, https://web.iodp.tamu.edu/LORE/
Project(s):
Coverage:
Latitude: -44.768460 * Longitude: 171.673940
Date/Time Start: 2009-12-21T23:15:00 * Date/Time End: 2009-12-22T11:15:00
Minimum DEPTH, sediment/rock: 2.770 m * Maximum DEPTH, sediment/rock: 53.830 m
Event(s):
317-U1353A * Latitude: -44.768460 * Longitude: 171.673940 * Date/Time Start: 2009-12-21T23:15:00 * Date/Time End: 2009-12-22T11:15:00 * Elevation: -84.2 m * Penetration: 56 m * Recovery: 56.4 m * Campaign: Exp317 (Canterbury Basin) * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 8 cores; 56 m cored; 101 % recovered; 0 m drilled; 56 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.
Technical Note 26 Chapter 2: http://www-odp.tamu.edu/publications/tnotes/tn26/CHAP2.PDF
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Sample code/label | Sample label | Expedition 317 Scientists | DSDP/ODP/IODP sample designation | ||
2 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
3 | Depth, top/min | Depth top | m | Expedition 317 Scientists | Depth CSF-B (m) | |
4 | Sample method | Sample method | Expedition 317 Scientists | Submethod | ||
5 | Water content, wet mass | Water wm | % | Expedition 317 Scientists | Calculated | |
6 | Water content, dry mass | Water dm | % | Expedition 317 Scientists | Calculated | |
7 | Density | Density | g/cm3 | Expedition 317 Scientists | Calculated | |
8 | Density, dry bulk | DBD | g/cm3 | Expedition 317 Scientists | Calculated | |
9 | Density, grain | Density grain | g/cm3 | Expedition 317 Scientists | Calculated | |
10 | Porosity | Poros | % vol | Expedition 317 Scientists | Calculated | |
11 | Void Ratio description | Void Ratio | Expedition 317 Scientists | Calculated | ||
12 | Wet mass | Wet m | g | Expedition 317 Scientists | ||
13 | Sample, dry mass | Samp dm | g | Expedition 317 Scientists | ||
14 | Mass, porewater | Mass pw | g | Expedition 317 Scientists | ||
15 | Salt content | Salt | g | Expedition 317 Scientists | ||
16 | Mass, solids | Mass solids | g | Expedition 317 Scientists | ||
17 | Volume, wet sample | Vol wet sample | cm3 | Expedition 317 Scientists | ||
18 | Volume, dry sample | Vol dry sample | cm3 | Expedition 317 Scientists | ||
19 | Volume, porewater | Vol pw | cm3 | Expedition 317 Scientists | ||
20 | Volume, salt | Vol salt | cm3 | Expedition 317 Scientists | ||
21 | Volume, solids | Vol solids | cm3 | Expedition 317 Scientists | ||
22 | Time Stamp | Time Stamp | Expedition 317 Scientists |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
588 data points
Data
1 Sample label | 2 Depth sed [m] | 3 Depth top [m] | 4 Sample method | 5 Water wm [%] | 6 Water dm [%] | 7 Density [g/cm3] | 8 DBD [g/cm3] | 9 Density grain [g/cm3] | 10 Poros [% vol] | 11 Void Ratio | 12 Wet m [g] | 13 Samp dm [g] | 14 Mass pw [g] | 15 Salt [g] | 16 Mass solids [g] | 17 Vol wet sample [cm3] | 18 Vol dry sample [cm3] | 19 Vol pw [cm3] | 20 Vol salt [cm3] | 21 Vol solids [cm3] | 22 Time Stamp |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
317-U1353A-1H-2,127 | 2.770 | 2.770 | C | 35.0 | 53.9 | 1.718 | 1.116 | 2.706 | 58.8 | 1.425 | 16.665 | 11.031 | 5.839 | 0.2044 | 10.827 | 9.703 | 4.093 | 5.702 | 0.09205 | 4.001 | 2009-12-23T07:20 |
317-U1353A-1H-2,129 | 2.790 | 2.790 | C | 34.9 | 53.5 | 1.718 | 1.119 | 2.696 | 58.5 | 1.408 | 16.031 | 10.640 | 5.587 | 0.1955 | 10.444 | 9.330 | 3.962 | 5.456 | 0.08808 | 3.874 | 2009-12-22T20:59 |
317-U1353A-1H-4,42 | 4.920 | 4.920 | C | 31.9 | 46.9 | 1.777 | 1.210 | 2.712 | 55.4 | 1.241 | 14.972 | 10.362 | 4.777 | 0.1672 | 10.195 | 8.423 | 3.834 | 4.665 | 0.07531 | 3.759 | 2009-12-23T07:20 |
317-U1353A-2H-2,117 | 8.170 | 8.120 | C | 30.6 | 44.2 | 1.795 | 1.245 | 2.689 | 53.7 | 1.16 | 11.089 | 7.810 | 3.399 | 0.1190 | 7.691 | 6.179 | 2.914 | 3.319 | 0.05358 | 2.860 | 2009-12-23T08:19 |
317-U1353A-2H-2,119 | 8.190 | 8.140 | C | 28.8 | 40.5 | 1.845 | 1.313 | 2.732 | 51.9 | 1.081 | 17.027 | 12.290 | 4.908 | 0.1718 | 12.118 | 9.229 | 4.513 | 4.793 | 0.07738 | 4.436 | 2009-12-22T20:59 |
317-U1353A-2H-3,52 | 9.020 | 8.950 | C | 21.9 | 28.0 | 2.008 | 1.568 | 2.748 | 42.9 | 0.752 | 9.249 | 7.295 | 2.025 | 0.0709 | 7.224 | 4.606 | 2.661 | 1.977 | 0.03192 | 2.629 | 2009-12-23T08:19 |
317-U1353A-3H-2,72 | 11.520 | 11.520 | C | 26.7 | 36.4 | 1.887 | 1.383 | 2.721 | 49.2 | 0.967 | 10.380 | 7.708 | 2.770 | 0.0969 | 7.611 | 5.502 | 2.841 | 2.705 | 0.04366 | 2.797 | 2009-12-23T09:23 |
317-U1353A-3H-4,127 | 15.070 | 15.070 | C | 26.9 | 36.7 | 1.885 | 1.379 | 2.726 | 49.4 | 0.978 | 13.049 | 9.667 | 3.504 | 0.1226 | 9.544 | 6.923 | 3.556 | 3.422 | 0.05525 | 3.501 | 2009-12-23T09:23 |
317-U1353A-3H-4,129 | 15.090 | 15.090 | C | 25.7 | 34.6 | 1.907 | 1.417 | 2.719 | 47.9 | 0.919 | 26.986 | 20.289 | 6.940 | 0.2429 | 20.046 | 14.150 | 7.482 | 6.777 | 0.10941 | 7.373 | 2009-12-22T20:59 |
317-U1353A-3H-6,75 | 17.260 | 17.260 | C | 24.0 | 31.6 | 1.961 | 1.490 | 2.758 | 46.0 | 0.852 | 10.886 | 8.363 | 2.615 | 0.0915 | 8.271 | 5.552 | 3.040 | 2.554 | 0.04123 | 2.999 | 2009-12-23T09:23 |
317-U1353A-4H-1,57 | 18.770 | 18.760 | C | 24.3 | 32.2 | 1.959 | 1.482 | 2.774 | 46.6 | 0.872 | 12.263 | 9.382 | 2.985 | 0.1045 | 9.277 | 6.260 | 3.392 | 2.915 | 0.04706 | 3.345 | 2009-12-23T10:16 |
317-U1353A-4H-3,127 | 22.470 | 22.430 | C | 25.0 | 33.3 | 1.936 | 1.453 | 2.753 | 47.2 | 0.895 | 12.059 | 9.152 | 3.012 | 0.1054 | 9.047 | 6.228 | 3.334 | 2.941 | 0.04749 | 3.287 | 2009-12-23T10:16 |
317-U1353A-4H-3,129 | 22.490 | 22.450 | C | 24.4 | 32.3 | 1.959 | 1.480 | 2.778 | 46.7 | 0.877 | 15.326 | 11.713 | 3.744 | 0.1310 | 11.582 | 7.825 | 4.228 | 3.656 | 0.05903 | 4.169 | 2009-12-22T20:59 |
317-U1353A-4H-6,56 | 26.260 | 26.180 | C | 21.4 | 27.1 | 2.023 | 1.591 | 2.751 | 42.2 | 0.729 | 9.141 | 7.258 | 1.952 | 0.0683 | 7.190 | 4.519 | 2.644 | 1.906 | 0.03077 | 2.613 | 2009-12-23T11:10 |
317-U1353A-5H-1,18 | 26.880 | 26.880 | C | 23.1 | 30.0 | 1.987 | 1.529 | 2.766 | 44.7 | 0.81 | 8.839 | 6.873 | 2.038 | 0.0713 | 6.801 | 4.449 | 2.491 | 1.990 | 0.03213 | 2.459 | 2009-12-23T14:16 |
317-U1353A-5H-4,68 | 31.120 | 31.120 | C | 27.3 | 37.6 | 1.879 | 1.366 | 2.740 | 50.2 | 1.006 | 11.116 | 8.184 | 3.038 | 0.1063 | 8.078 | 5.914 | 2.996 | 2.966 | 0.04789 | 2.948 | 2009-12-23T14:16 |
317-U1353A-5H-6,77 | 33.700 | 33.700 | C | 23.4 | 30.6 | 1.961 | 1.501 | 2.724 | 44.9 | 0.814 | 12.690 | 9.820 | 2.974 | 0.1041 | 9.716 | 6.471 | 3.614 | 2.904 | 0.04689 | 3.567 | 2009-12-23T14:16 |
317-U1353A-5H-6,79 | 33.720 | 33.720 | C | 25.4 | 34.0 | 1.920 | 1.434 | 2.733 | 47.5 | 0.907 | 18.361 | 13.868 | 4.655 | 0.1629 | 13.705 | 9.561 | 5.088 | 4.546 | 0.07339 | 5.015 | 2009-12-22T23:29 |
317-U1353A-6H-2,73.5 | 36.435 | 36.365 | C | 23.2 | 30.1 | 1.993 | 1.531 | 2.788 | 45.1 | 0.821 | 15.956 | 12.390 | 3.696 | 0.1294 | 12.260 | 8.007 | 4.456 | 3.610 | 0.05827 | 4.398 | 2009-12-23T15:30 |
317-U1353A-6H-3,126 | 38.460 | 38.330 | C | 23.5 | 30.8 | 1.982 | 1.515 | 2.783 | 45.5 | 0.837 | 19.085 | 14.750 | 4.492 | 0.1572 | 14.593 | 9.631 | 5.315 | 4.387 | 0.07082 | 5.244 | 2009-12-23T15:31 |
317-U1353A-6H-3,129 | 38.490 | 38.360 | C | 23.1 | 30.0 | 1.992 | 1.532 | 2.782 | 44.9 | 0.815 | 16.964 | 13.185 | 3.916 | 0.1371 | 13.048 | 8.515 | 4.752 | 3.824 | 0.06174 | 4.690 | 2009-12-22T23:30 |
317-U1353A-6H-4,126 | 39.960 | 39.780 | C | 23.3 | 30.4 | 1.981 | 1.519 | 2.767 | 45.1 | 0.821 | 15.696 | 12.166 | 3.657 | 0.1280 | 12.038 | 7.923 | 4.409 | 3.572 | 0.05766 | 4.351 | 2009-12-23T15:30 |
317-U1353A-7H-3,126 | 45.460 | 45.350 | C | 23.0 | 29.8 | 1.993 | 1.535 | 2.777 | 44.7 | 0.809 | 17.513 | 13.630 | 4.024 | 0.1408 | 13.489 | 8.787 | 4.921 | 3.929 | 0.06344 | 4.858 | 2009-12-23T17:13 |
317-U1353A-7H-3,129 | 45.490 | 45.380 | C | 22.1 | 28.4 | 2.023 | 1.575 | 2.798 | 43.7 | 0.776 | 11.024 | 8.671 | 2.438 | 0.0853 | 8.586 | 5.450 | 3.107 | 2.381 | 0.03844 | 3.069 | 2009-12-22T23:30 |
317-U1353A-7H-4,71 | 46.410 | 46.280 | C | 24.8 | 32.9 | 1.952 | 1.468 | 2.781 | 47.2 | 0.894 | 14.391 | 10.952 | 3.564 | 0.1247 | 10.827 | 7.374 | 3.950 | 3.480 | 0.05618 | 3.894 | 2009-12-23T17:13 |
317-U1353A-8H-4,71 | 53.250 | 53.230 | C | 23.1 | 30.1 | 1.957 | 1.504 | 2.698 | 44.2 | 0.793 | 14.252 | 11.069 | 3.299 | 0.1155 | 10.953 | 7.281 | 4.112 | 3.221 | 0.05201 | 4.060 | 2009-12-23T17:12 |
317-U1353A-8H-4,127 | 53.810 | 53.790 | C | 24.2 | 32.0 | 1.929 | 1.461 | 2.689 | 45.7 | 0.84 | 15.298 | 11.719 | 3.709 | 0.1298 | 11.589 | 7.932 | 4.368 | 3.622 | 0.05848 | 4.310 | 2009-12-23T20:56 |
317-U1353A-8H-4,129 | 53.830 | 53.810 | C | 23.1 | 30.0 | 1.962 | 1.509 | 2.708 | 44.3 | 0.794 | 15.812 | 12.287 | 3.653 | 0.1279 | 12.159 | 8.058 | 4.548 | 3.567 | 0.05759 | 4.490 | 2009-12-23T01:26 |