Reimers, Clare (2002): Oxygen profiling at B-141 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.78697
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Reimers, Clare; Jahnke, Richard A; McCorkle, Daniel C (1992): Carbon fluxes and burial rates over the continental slope and rise off Central California with implications for the global carbon cycle. Global Biogeochemical Cycles, 6(2), 199-224, https://doi.org/10.1029/92GB00105
Project(s):
Funding:
Fifth Framework Programme (FP5), grant/award no. EVK2-CT-2001-00100: Origin and Fate of Biogenic Particle Fluxes in the Ocean
Coverage:
Latitude: 36.279660 * Longitude: -122.172000
Date/Time Start: 1987-11-06T00:00:00 * Date/Time End: 1987-11-06T00:00:00
Minimum DEPTH, sediment/rock: -0.0100 m * Maximum DEPTH, sediment/rock: 0.0140 m
Event(s):
Reimers_B-141_IMP (B-141) * Latitude: 36.279660 * Longitude: -122.172000 * Date/Time: 1987-11-06T00:00:00 * Elevation: -793.0 m * Location: North Pacific/Gulf of California/SLOPE * Campaign: TT183 * Basis: Thomas G. Thompson (1964) * Method/Device: In situ oxygen microprofiler (IMP)
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Oxygen, flux, sediment oxygen demand | SOD | mmol/m2/day | Reimers, Clare | Flux estimate from linear regression | |
| 3 | Oxygen | O2 | µmol/l | Reimers, Clare | Microelectrode oxygen profiler, in situ; Reimers, 1987 | |
| 4 | Temperature, water | Temp | °C | Reimers, Clare |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
25 data points
Data
| 1 Depth sed [m] | 2 SOD [mmol/m2/day] | 3 O2 [µmol/l] | 4 Temp [°C] |
|---|---|---|---|
| -0.0100 | 11.3 | ||
| -0.0090 | 11.3 | ||
| -0.0080 | 11.3 | ||
| -0.0070 | 11.3 | ||
| -0.0060 | 11.3 | ||
| -0.0050 | 10.8 | ||
| -0.0040 | 10.8 | ||
| -0.0030 | 10.3 | ||
| -0.0020 | 10.8 | ||
| -0.0010 | 10.3 | ||
| 0.0000 | 0.47 | 11.2 | 4.4 |
| 0.0000 | 10.3 | ||
| 0.0010 | 3.1 | ||
| 0.0020 | 0.5 | ||
| 0.0030 | 0.0 | ||
| 0.0040 | 0.0 | ||
| 0.0050 | 0.0 | ||
| 0.0060 | 0.0 | ||
| 0.0070 | 0.0 | ||
| 0.0080 | 0.0 | ||
| 0.0100 | 0.0 | ||
| 0.0120 | 0.0 | ||
| 0.0140 | 0.0 |