Klages, Johann Philipp; Kuhn, Gerhard; Hillenbrand, Claus-Dieter; Graham, Alastair G C; Smith, James A; Larter, Robert D; Gohl, Karsten (2014): Water content of sediment core PS75/130-1 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.818142, In supplement to: Klages, Johann Philipp; Kuhn, Gerhard; Hillenbrand, Claus-Dieter; Graham, Alastair G C; Smith, James A; Larter, Robert D; Gohl, Karsten; Wacker, Lukas (2014): Retreat of the West Antarctic Ice Sheet from the western Amundsen Sea shelf at a pre- or early LGM stage. Quaternary Science Reviews, 91, 1-15, https://doi.org/10.1016/j.quascirev.2014.02.017
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Project(s):
Coverage:
Latitude: -74.445160 * Longitude: -134.152830
Date/Time Start: 2010-02-19T01:20:00 * Date/Time End: 2010-02-19T01:20:00
Minimum DEPTH, sediment/rock: 0.01 m * Maximum DEPTH, sediment/rock: 3.10 m
Event(s):
PS75/130-1 * Latitude: -74.445160 * Longitude: -134.152830 * Date/Time: 2010-02-19T01:20:00 * Elevation: -794.0 m * Penetration: 3.8 m * Recovery: 3.19 m * Location: westernmost Getz Trough, inner shelf (basin south of GZW) * Campaign: ANT-XXVI/3 (PS75) * Basis: Polarstern * Method/Device: Gravity corer (Kiel type) (SL) * Comment: 4 core sections: 0-0.19, 0.19-1.19, 1.19-2.19, 2.19-3.19 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 | % | Klages, Johann Philipp | Calculated from mass/volume |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
35 data points
Data
| 1 Depth sed [m] | 2 Water wm [%] |
|---|---|
| 0.01 | 32.3 |
| 0.03 | 30.2 |
| 0.07 | 31.0 |
| 0.12 | 29.7 |
| 0.18 | 28.8 |
| 0.20 | 23.2 |
| 0.30 | 21.4 |
| 0.40 | 23.3 |
| 0.50 | 20.5 |
| 0.60 | 22.3 |
| 0.70 | 21.8 |
| 0.80 | 20.6 |
| 0.90 | 21.6 |
| 1.00 | 21.2 |
| 1.10 | 20.3 |
| 1.20 | 20.9 |
| 1.30 | 22.1 |
| 1.40 | 20.7 |
| 1.50 | 23.1 |
| 1.60 | 22.5 |
| 1.70 | 21.5 |
| 1.80 | 21.7 |
| 1.90 | 19.7 |
| 2.00 | 19.3 |
| 2.10 | 16.8 |
| 2.20 | 18.7 |
| 2.30 | 17.7 |
| 2.40 | 17.5 |
| 2.50 | 17.7 |
| 2.60 | 17.6 |
| 2.70 | 17.3 |
| 2.80 | 16.9 |
| 2.90 | 16.8 |
| 3.00 | 17.0 |
| 3.10 | 17.3 |