Versteegh, Gerard J M; Koschinsky, Andrea; Kuhn, Thomas; Preuss, Inken; Kasten, Sabine (2021): Porewater oxygen of sediment core SO240_65-1 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.933007, In: Versteegh, GJM et al. (2021): Porewater and solid phase Mn, Ni, Co and porewater O2 and NO3 from the Clarion-Clipperton Zone NE Pacific [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.933062
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Versteegh, Gerard J M; Koschinsky, Andrea; Kuhn, Thomas; Preuss, Inken; Kasten, Sabine (in review): Geochemical consequences of oxygen diffusion from the oceanic crust into overlying sediments and its significance for biogeochemical cycles based on sediments of the NE Pacific. Biogeosciences, https://doi.org/10.5194/bg-2021-112
Coverage:
Latitude: 12.935170 * Longitude: -119.148000
Date/Time Start: 2015-05-26T20:28:00 * Date/Time End: 2015-05-26T20:28:00
Minimum DEPTH, sediment/rock: 0.10 m * Maximum DEPTH, sediment/rock: 12.40 m
Event(s):
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Versteegh, Gerard J M | Geocode | |
| 2 | Oxygen | O2 | µmol/l | Versteegh, Gerard J M | Amperometric Clark-type oxygen sensor |
License:
Creative Commons Attribution 4.0 International (CC-BY-4.0)
Size:
33 data points
Data
| 1 Depth sed [m] | 2 O2 [µmol/l] |
|---|---|
| 0.10 | 21.41 |
| 0.20 | 14.57 |
| 0.30 | 14.62 |
| 0.40 | 9.18 |
| 0.50 | 9.18 |
| 0.60 | 9.20 |
| 0.85 | 9.20 |
| 1.05 | 7.67 |
| 1.15 | 9.20 |
| 1.25 | 4.22 |
| 1.35 | 4.98 |
| 1.45 | 5.73 |
| 1.55 | 4.21 |
| 1.65 | 7.26 |
| 1.75 | 0.00 |
| 1.80 | 4.99 |
| 2.30 | 5.77 |
| 2.40 | 7.69 |
| 2.50 | 5.76 |
| 2.60 | 6.14 |
| 2.70 | 6.13 |
| 3.00 | 4.20 |
| 3.20 | 4.57 |
| 3.40 | 5.72 |
| 3.60 | 6.86 |
| 3.80 | 2.67 |
| 4.00 | 3.03 |
| 4.30 | 8.34 |
| 4.70 | 5.72 |
| 11.80 | 3.81 |
| 12.00 | 1.91 |
| 12.20 | 2.29 |
| 12.40 | 1.52 |