Zabel, Matthias (2002): Phosphate of sediment core GeoB1719-6 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.87924
Always quote citation above when using data! You can download the citation in several formats below.
Published: 2002-12-13 • DOI registered: 2005-03-04
Related to:
Zabel, Matthias; Dahmke, Andreas; Schulz, Horst D (1998): Regional distribution of diffusive phosphate and silicate fluxes through the sediment–water interface: the eastern South Atlantic. Deep Sea Research Part I: Oceanographic Research Papers, 45(2-3), 277-300, https://doi.org/10.1016/S0967-0637(97)00073-3
Project(s):
Coverage:
Latitude: -28.925000 * Longitude: 14.171667
Date/Time Start: 1992-01-16T00:00:00 * Date/Time End: 1992-01-16T00:00:00
Minimum DEPTH, sediment/rock: 0.200 m * Maximum DEPTH, sediment/rock: 10.650 m
Event(s):
GeoB1719-6 * Latitude: -28.925000 * Longitude: 14.171667 * Date/Time: 1992-01-16T00:00:00 * Elevation: -1030.0 m * Recovery: 10.86 m * Location: Namibia continental slope * Campaign: M20/2 * Basis: Meteor (1986) * Method/Device: Gravity corer (Kiel type) (SL) * Comment: Geochemie
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Phosphate | [PO4]3- | µmol/l | Zabel, Matthias | Continuous Flow Analysis (CFA) |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
42 data points
Data
| 1 Depth sed [m] | 2 [PO4]3- [µmol/l] |
|---|---|
| 0.200 | 6.71 |
| 0.450 | 5.38 |
| 0.700 | 4.68 |
| 0.950 | 4.99 |
| 1.200 | 4.99 |
| 1.450 | 5.15 |
| 1.700 | 4.83 |
| 1.950 | 4.76 |
| 2.200 | 5.26 |
| 2.450 | 5.01 |
| 2.700 | 5.01 |
| 2.950 | 5.01 |
| 3.200 | 5.26 |
| 3.450 | 5.14 |
| 3.700 | 5.26 |
| 3.950 | 4.91 |
| 4.200 | 4.91 |
| 4.450 | 4.91 |
| 4.700 | 4.91 |
| 4.950 | 5.01 |
| 5.200 | 5.12 |
| 5.450 | 5.34 |
| 5.700 | 5.12 |
| 5.950 | 5.12 |
| 6.200 | 5.01 |
| 6.450 | 5.12 |
| 6.700 | 5.12 |
| 7.200 | 5.41 |
| 7.450 | 5.41 |
| 7.700 | 5.01 |
| 7.950 | 5.72 |
| 8.200 | 5.32 |
| 8.450 | 5.32 |
| 8.700 | 5.00 |
| 8.950 | 5.00 |
| 9.200 | 5.41 |
| 9.450 | 5.21 |
| 9.700 | 5.81 |
| 9.950 | 5.26 |
| 10.200 | 5.52 |
| 10.450 | 5.64 |
| 10.650 | 6.01 |