Murray, James W (2004): Pore Water Chemistry of TT183_2_ISS [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.143171
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Murray, James W; Kuivila, K M (1990): Organic matter diagenesis in the northeast Pacific: transition from aerobic red clay to suboxic hemipelagic sediments. Deep-Sea Research Part A. Oceanographic Research Papers, 37(1), 59-80, https://doi.org/10.1016/0198-0149(90)90029-U
Project(s):
Silicon Cycling in the World Ocean (SINOPS)
Funding:
Coverage:
Latitude: 35.665000 * Longitude: -122.388333
Date/Time Start: 1984-09-01T00:00:00 * Date/Time End: 1984-09-01T00:00:00
Minimum DEPTH, sediment/rock: 0.000 m * Maximum DEPTH, sediment/rock: 0.540 m
Event(s):
TT183_2_ISS * Latitude: 35.665000 * Longitude: -122.388333 * Date/Time: 1984-09-01T00:00:00 * Elevation: -3570.0 m * Campaign: TT183 * Basis: Thomas G. Thompson (1964) * Method/Device: In situ sampler (ISS)
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Oxygen | O2 | µmol/l | Murray, James W | ||
| 3 | Manganese | Mn | µmol/l | Murray, James W | Inductively coupled plasma atomic emission spectroscope (ICP-AES) | |
| 4 | Silicate | Si(OH)4 | µmol/l | Murray, James W | ||
| 5 | Silicate | Si(OH)4 | µmol/l | Murray, James W |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
38 data points
Data
| 1 Depth sed [m] | 2 O2 [µmol/l] | 3 Mn [µmol/l] | 4 Si(OH)4 [µmol/l] | 5 Si(OH)4 [µmol/l] |
|---|---|---|---|---|
| 0.000 | 135.0 | 164.0 | 164.0 | |
| 0.020 | 1.00 | 543.0 | ||
| 0.050 | 5.00 | 625.0 | ||
| 0.080 | 8.00 | |||
| 0.110 | 10.00 | 646.0 | ||
| 0.140 | 14.00 | 646.0 | ||
| 0.170 | 12.00 | 513.0 | ||
| 0.200 | 564.0 | 625.0 | ||
| 0.230 | 10.00 | 641.0 | 646.0 | |
| 0.260 | 8.00 | 677.0 | 687.0 | |
| 0.290 | 5.00 | 615.0 | 636.0 | |
| 0.340 | 7.00 | 605.0 | 666.0 | |
| 0.390 | 4.00 | 595.0 | 656.0 | |
| 0.440 | 5.00 | 625.0 | 656.0 | |
| 0.490 | 564.0 | 636.0 | ||
| 0.540 | 523.0 | 646.0 |