Schulz, Horst D (1998): Silicate in porewater of sediment core GeoB1401-4 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.52849
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Schulz, Horst D; Dahmke, Andreas; Schinzel, Uwe; Wallmann, Klaus; Zabel, Matthias (1994): Early diagenetic processes, fluxes, and reaction rates in sediments of the South Atlantic. Geochimica et Cosmochimica Acta, 58(9), 2041-2060, https://doi.org/10.1016/0016-7037(94)90284-4
Project(s):
Silicon Cycling in the World Ocean (SINOPS)
Funding:
Coverage:
Latitude: -6.926167 * Longitude: 9.005667
Date/Time Start: 1991-03-29T00:00:00 * Date/Time End: 1991-03-29T00:00:00
Minimum DEPTH, sediment/rock: 0.20 m * Maximum DEPTH, sediment/rock: 15.70 m
Event(s):
GeoB1401-4 * Latitude: -6.926167 * Longitude: 9.005667 * Date/Time: 1991-03-29T00:00:00 * Elevation: -3952.0 m * Recovery: 15.75 m * Location: Congo Fan * Campaign: M16/1 * Basis: Meteor (1986) * 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 | Silicate | Si(OH)4 | µmol/l | Schulz, Horst D | Inductively coupled plasma atomic emission spectroscope (ICP-AES) |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
94 data points
Data
| 1 Depth sed [m] | 2 Si(OH)4 [µmol/l] |
|---|---|
| 0.20 | 280 |
| 0.35 | 230 |
| 0.50 | 250 |
| 0.65 | 210 |
| 0.80 | 230 |
| 0.90 | 280 |
| 1.05 | 310 |
| 1.20 | 380 |
| 1.35 | 370 |
| 1.50 | 360 |
| 1.65 | 430 |
| 2.00 | 480 |
| 2.20 | 500 |
| 2.35 | 530 |
| 2.50 | 480 |
| 2.65 | 500 |
| 2.80 | 480 |
| 3.00 | 480 |
| 3.20 | 510 |
| 3.35 | 500 |
| 3.50 | 510 |
| 3.65 | 470 |
| 3.80 | 460 |
| 3.90 | 470 |
| 4.05 | 430 |
| 4.20 | 490 |
| 4.35 | 500 |
| 4.50 | 510 |
| 4.65 | 550 |
| 5.00 | 480 |
| 5.20 | 480 |
| 5.35 | 520 |
| 5.50 | 480 |
| 5.65 | 550 |
| 5.80 | 480 |
| 6.00 | 460 |
| 6.20 | 540 |
| 6.35 | 520 |
| 6.50 | 440 |
| 6.65 | 440 |
| 6.80 | 430 |
| 7.00 | 420 |
| 7.20 | 410 |
| 7.35 | 400 |
| 7.50 | 330 |
| 7.65 | 430 |
| 7.80 | 460 |
| 8.00 | 460 |
| 8.20 | 560 |
| 8.35 | 540 |
| 8.50 | 500 |
| 8.65 | 540 |
| 8.80 | 460 |
| 9.00 | 490 |
| 9.20 | 510 |
| 9.35 | 500 |
| 9.50 | 480 |
| 9.65 | 430 |
| 9.80 | 450 |
| 10.00 | 480 |
| 10.20 | 490 |
| 10.35 | 430 |
| 10.50 | 460 |
| 10.65 | 410 |
| 10.80 | 450 |
| 11.00 | 430 |
| 11.20 | 460 |
| 11.35 | 480 |
| 11.50 | 470 |
| 11.65 | 460 |
| 11.80 | 470 |
| 12.00 | 510 |
| 12.20 | 490 |
| 12.35 | 530 |
| 12.50 | 500 |
| 12.65 | 560 |
| 12.80 | 520 |
| 13.00 | 560 |
| 13.20 | 540 |
| 13.35 | 560 |
| 13.50 | 530 |
| 13.65 | 570 |
| 13.80 | 550 |
| 14.00 | 590 |
| 14.20 | 540 |
| 14.35 | 580 |
| 14.50 | 580 |
| 14.65 | 610 |
| 14.80 | 600 |
| 15.00 | 570 |
| 15.15 | 510 |
| 15.30 | 530 |
| 15.50 | 530 |
| 15.70 | 480 |