Villinger, Heinrich (2003): Susceptibility of sediment core PS1577-1 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.92410, In: Villinger, H (1996): Physical properties measured on sediment cores from the Southern Ocean, Weddell Sea area [dataset publication series]. Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven, PANGAEA, https://doi.org/10.1594/PANGAEA.701300
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Project(s):
Coverage:
Latitude: -61.940160 * Longitude: -44.001660
Date/Time Start: 1987-12-26T23:28:00 * Date/Time End: 1987-12-26T23:28:00
Minimum DEPTH, sediment/rock: 0.10 m * Maximum DEPTH, sediment/rock: 4.65 m
Event(s):
PS1577-1 (PS12/252) * Latitude: -61.940160 * Longitude: -44.001660 * Date/Time: 1987-12-26T23:28:00 * Elevation: -845.0 m * Penetration: 5.5 m * Recovery: 4.76 m * Location: South Orkney * Campaign: ANT-VI/3 (PS12) * Basis: Polarstern * Method/Device: Gravity corer (Kiel type) (SL) * Comment: 5 core sections: 0-0.76, 0.76-1.76, 1.76-2.76, 2.76-3.76, 3.76-4.76 m
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Magnetic susceptibility, volume | kappa | 10-6 SI | Villinger, Heinrich | Susceptibility unit, AWI, MS2C [145 mm] | Correction factor 6.906 |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
52 data points
Data
| 1 Depth sed [m] | 2 kappa [10-6 SI] |
|---|---|
| 0.10 | 1739.62 |
| 0.18 | 895.02 |
| 0.30 | 2623.59 |
| 0.43 | 1577.33 |
| 0.43 | 1493.77 |
| 0.43 | 1532.44 |
| 0.50 | 1236.17 |
| 0.60 | 1912.96 |
| 0.71 | 1286.59 |
| 0.78 | 1208.55 |
| 0.86 | 1203.03 |
| 0.96 | 1549.71 |
| 1.06 | 1672.63 |
| 1.18 | 1191.29 |
| 1.25 | 1420.56 |
| 1.36 | 1180.24 |
| 1.43 | 2259.64 |
| 1.50 | 1057.31 |
| 1.58 | 889.49 |
| 1.65 | 1113.25 |
| 1.73 | 1113.25 |
| 1.78 | 1023.47 |
| 1.78 | 1035.90 |
| 1.86 | 1040.73 |
| 1.99 | 2035.89 |
| 2.07 | 1454.40 |
| 2.14 | 1023.47 |
| 2.27 | 1084.93 |
| 2.40 | 1230.65 |
| 2.50 | 2578.70 |
| 2.60 | 1644.32 |
| 2.72 | 855.65 |
| 2.80 | 1252.75 |
| 2.89 | 1845.97 |
| 3.03 | 1420.56 |
| 3.16 | 1476.50 |
| 3.30 | 1208.55 |
| 3.30 | 1219.60 |
| 3.30 | 1403.99 |
| 3.45 | 1594.60 |
| 3.60 | 1073.88 |
| 3.74 | 788.67 |
| 3.79 | 548.34 |
| 3.89 | 447.51 |
| 4.01 | 542.81 |
| 4.09 | 363.95 |
| 4.23 | 475.82 |
| 4.32 | 481.35 |
| 4.39 | 469.61 |
| 4.43 | 575.96 |
| 4.51 | 687.84 |
| 4.65 | 330.11 |