Dählmann, Anke (2001): Porosity of sediment core PS47/062-1 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.59768
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Related to:
Dählmann, Anke (2001): Geochemische Untersuchungen an hydrothermal beeinflußten Sedimenten der Bransfield Straße (Antarktis) (Geochemical investigation on hydrothermally influenced sediments of Bransfield Strait (Antarctica)). Berichte zur Polar- und Meeresforschung = Reports on Polar and Marine Research, 392, 157 pp, https://doi.org/10.2312/BzPM_0392_2001
Coverage:
Latitude: -62.249830 * Longitude: -57.468830
Date/Time Start: 1997-12-09T15:04:00 * Date/Time End: 1997-12-09T16:16:00
Minimum DEPTH, sediment/rock: 0.02 m * Maximum DEPTH, sediment/rock: 5.60 m
Event(s):
PS47/062-1 (SL62) * Latitude: -62.249830 * Longitude: -57.468830 * Date/Time Start: 1997-12-09T15:04:00 * Date/Time End: 1997-12-09T16:16:00 * Elevation: -1992.0 m * Recovery: 5.71 m * Location: South Atlantic * Campaign: ANT-XV/2 (PS47) * Basis: Polarstern * Method/Device: Gravity corer (Kiel type) (SL)
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Porosity, fractional | Poros frac | Dählmann, Anke | Calculated from weight/volume |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
50 data points
Data
1 Depth sed [m] | 2 Poros frac |
---|---|
0.02 | 0.82 |
0.12 | 0.83 |
0.25 | 0.81 |
0.35 | 0.77 |
0.49 | 0.77 |
0.57 | 0.82 |
0.70 | 0.80 |
0.85 | 0.77 |
0.92 | 0.79 |
1.00 | 0.79 |
1.10 | 0.78 |
1.19 | 0.78 |
1.26 | 0.77 |
1.40 | 0.77 |
1.49 | 0.76 |
1.60 | 0.75 |
1.75 | 0.75 |
1.86 | 0.64 |
1.95 | 0.46 |
2.03 | 0.76 |
2.13 | 0.76 |
2.25 | 0.78 |
2.37 | 0.79 |
2.50 | 0.84 |
2.61 | 0.81 |
2.72 | 0.79 |
2.84 | 0.77 |
2.99 | 0.78 |
3.09 | 0.72 |
3.18 | 0.83 |
3.26 | 0.79 |
3.38 | 0.76 |
3.47 | 0.75 |
3.58 | 0.76 |
3.72 | 0.75 |
3.82 | 0.77 |
3.91 | 0.76 |
4.07 | 0.75 |
4.20 | 0.77 |
4.35 | 0.77 |
4.46 | 0.76 |
4.59 | 0.79 |
4.72 | 0.80 |
4.83 | 0.73 |
4.97 | 0.73 |
5.10 | 0.76 |
5.20 | 0.75 |
5.31 | 0.77 |
5.48 | 0.75 |
5.60 | 0.74 |