Schulz, Horst D (1998): Silicate in porewater of sediment core GeoB1514-6 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.52891
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: 5.140000 * Longitude: -46.576667
Date/Time Start: 1991-05-13T00:00:00 * Date/Time End: 1991-05-13T00:00:00
Minimum DEPTH, sediment/rock: 0.15 m * Maximum DEPTH, sediment/rock: 7.20 m
Event(s):
GeoB1514-6 * Latitude: 5.140000 * Longitude: -46.576667 * Date/Time: 1991-05-13T00:00:00 * Elevation: -3509.0 m * Recovery: 7.22 m * Location: Amazon Fan * Campaign: M16/2 * 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:
65 data points
Data
1 Depth sed [m] | 2 Si(OH)4 [µmol/l] |
---|---|
0.15 | 210 |
0.20 | 230 |
0.30 | 230 |
0.45 | 180 |
0.50 | 110 |
0.60 | 120 |
0.75 | 130 |
0.90 | 130 |
0.95 | 130 |
1.05 | 140 |
1.10 | 150 |
1.20 | 150 |
1.30 | 140 |
1.45 | 140 |
1.50 | 160 |
1.60 | 150 |
1.70 | 150 |
1.90 | 150 |
2.10 | 160 |
2.20 | 130 |
2.35 | 170 |
2.50 | 160 |
2.60 | 130 |
2.65 | 150 |
2.80 | 150 |
2.90 | 130 |
2.95 | 160 |
3.10 | 160 |
3.20 | 140 |
3.35 | 150 |
3.50 | 140 |
3.60 | 100 |
3.65 | 150 |
3.80 | 140 |
3.90 | 130 |
3.95 | 150 |
4.10 | 150 |
4.20 | 140 |
4.35 | 170 |
4.50 | 150 |
4.50 | 130 |
4.65 | 170 |
4.80 | 180 |
4.90 | 160 |
4.95 | 180 |
5.10 | 200 |
5.20 | 180 |
5.35 | 220 |
5.50 | 220 |
5.60 | 190 |
5.65 | 220 |
5.80 | 220 |
5.90 | 230 |
5.95 | 220 |
6.10 | 250 |
6.20 | 230 |
6.35 | 390 |
6.50 | 260 |
6.60 | 220 |
6.65 | 240 |
6.80 | 250 |
6.90 | 260 |
6.95 | 220 |
7.10 | 250 |
7.20 | 260 |