Reimers, Clare (2002): Oxygen profiling at K-216 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.78732
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: 35.626833 * Longitude: -121.829500
Date/Time Start: 1988-07-18T00:00:00 * Date/Time End: 1988-07-18T00:00:00
Minimum DEPTH, sediment/rock: -0.0100 m * Maximum DEPTH, sediment/rock: 0.0280 m
Event(s):
Reimers_K-216_IMP (K-216) * Latitude: 35.626833 * Longitude: -121.829500 * Date/Time: 1988-07-18T00:00:00 * Elevation: -993.0 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:
35 data points
Data
| 1 Depth sed [m] | 2 SOD [mmol/m2/day] | 3 O2 [µmol/l] | 4 Temp [°C] |
|---|---|---|---|
| -0.0100 | 20.5 | ||
| -0.0090 | 20.5 | ||
| -0.0080 | 20.5 | ||
| -0.0070 | 20.5 | ||
| -0.0060 | 20.5 | ||
| -0.0050 | 20.5 | ||
| -0.0040 | 20.5 | ||
| -0.0030 | 20.5 | ||
| -0.0020 | 20.5 | ||
| -0.0010 | 19.5 | ||
| 0.0000 | 0.55 | 20.0 | 3.8 |
| 0.0000 | 18.5 | ||
| 0.0010 | 13.3 | ||
| 0.0020 | 8.2 | ||
| 0.0030 | 5.1 | ||
| 0.0040 | 2.1 | ||
| 0.0050 | 1.0 | ||
| 0.0060 | 0.0 | ||
| 0.0070 | 0.0 | ||
| 0.0080 | 0.0 | ||
| 0.0090 | 0.0 | ||
| 0.0100 | 0.0 | ||
| 0.0110 | 0.0 | ||
| 0.0120 | 0.0 | ||
| 0.0140 | 0.0 | ||
| 0.0150 | 0.0 | ||
| 0.0160 | 0.0 | ||
| 0.0170 | 0.0 | ||
| 0.0190 | 0.0 | ||
| 0.0210 | 0.0 | ||
| 0.0230 | 0.0 | ||
| 0.0250 | 0.0 | ||
| 0.0280 | 0.0 |