Melles, Martin (1991): Water content of sediment core PS1607-3 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.51807, In supplement to: Melles, M (1991): Paläoglaziologie und Paläozeanographie im Spätquartär am Kontinentalrand des südlichen Weddellmeeres, Antarktis (Late Quaternary paleoglaciology and paleoceanography at the continental margin of the southern Weddell Sea, Antarctica). Berichte zur Polarforschung = Reports on Polar Research, 81, 190 pp, https://doi.org/10.2312/BzP_0081_1991
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Project(s):
Coverage:
Latitude: -74.106330 * Longitude: -33.648830
Date/Time Start: 1988-01-26T08:21:00 * Date/Time End: 1988-01-26T08:21:00
Minimum DEPTH, sediment/rock: 0.45000 m * Maximum DEPTH, sediment/rock: 3.62000 m
Event(s):
PS1607-3 (PS12/340) * Latitude: -74.106330 * Longitude: -33.648830 * Date/Time: 1988-01-26T08:21:00 * Elevation: -1582.0 m * Penetration: 5.6 m * Recovery: 3.64 m * Location: Weddell Sea * Campaign: ANT-VI/3 (PS12) * Basis: Polarstern * Method/Device: Gravity corer (Kiel type) (SL) * Comment: 4 core sections: 0-0.64, 0.64-1.64, 1.64-2.64, 2.64-3.64 m
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Water content, wet mass | Water wm | % | Melles, Martin |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
31 data points
Data
| 1 Depth sed [m] | 2 Water wm [%] |
|---|---|
| 0.45000 | 49.90 |
| 0.50000 | 46.70 |
| 0.56000 | 43.99 |
| 0.62000 | 43.74 |
| 0.71000 | 42.75 |
| 0.80000 | 46.18 |
| 0.89000 | 40.58 |
| 0.98000 | 43.81 |
| 1.06000 | 44.38 |
| 1.14000 | 39.46 |
| 1.23000 | 44.55 |
| 1.32000 | 42.38 |
| 1.40000 | 32.82 |
| 1.48000 | 36.06 |
| 1.58000 | 41.42 |
| 1.70000 | 44.20 |
| 1.82000 | 39.91 |
| 1.94000 | 43.74 |
| 2.05000 | 28.49 |
| 2.15000 | 22.30 |
| 2.27000 | 21.43 |
| 2.39000 | 21.65 |
| 2.50000 | 19.46 |
| 2.61000 | 20.40 |
| 2.73000 | 20.18 |
| 2.86000 | 19.96 |
| 3.00000 | 19.12 |
| 3.15000 | 19.80 |
| 3.30000 | 19.62 |
| 3.46000 | 21.09 |
| 3.62000 | 19.65 |