Murray, James W (2004): Pore Water Chemistry of TT183_5_ISS [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.143174
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: 33.031667 * Longitude: -139.513333
Date/Time Start: 1984-09-04T00:00:00 * Date/Time End: 1984-09-04T00:00:00
Minimum DEPTH, sediment/rock: 0.000 m * Maximum DEPTH, sediment/rock: 0.540 m
Event(s):
TT183_5_ISS * Latitude: 33.031667 * Longitude: -139.513333 * Date/Time: 1984-09-04T00:00:00 * Elevation: -4980.0 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 | Oxygen, flux, sediment oxygen demand | SOD | mmol/m2/day | Murray, James W | Calculated | |
| 4 | Nitrate | [NO3]- | 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:
48 data points
Data
| 1 Depth sed [m] | 2 O2 [µmol/l] | 3 SOD [mmol/m2/day] | 4 [NO3]- [µmol/l] | 5 Si(OH)4 [µmol/l] |
|---|---|---|---|---|
| 0.000 | 155.0 | 0.09 | ||
| 0.000 | 164.0 | 36.0 | 144.0 | |
| 0.020 | 164.0 | 37.0 | 154.0 | |
| 0.050 | 159.0 | 37.0 | 159.0 | |
| 0.080 | 159.0 | 36.0 | 164.0 | |
| 0.110 | 38.0 | 166.0 | ||
| 0.140 | 154.0 | 40.0 | 169.0 | |
| 0.170 | 144.0 | 41.0 | 179.0 | |
| 0.200 | 144.0 | 41.0 | 179.0 | |
| 0.230 | 40.0 | 205.0 | ||
| 0.260 | 128.0 | 40.0 | 185.0 | |
| 0.290 | 123.0 | 41.0 | 190.0 | |
| 0.340 | 118.0 | 41.0 | 185.0 | |
| 0.390 | 118.0 | 42.0 | 195.0 | |
| 0.440 | 103.0 | 42.0 | 200.0 | |
| 0.490 | 113.0 | 41.0 | 195.0 | |
| 0.540 | 92.0 | 42.0 | 195.0 |