Reimers, Clare (2002): Oxygen profiling at D-256 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.78714
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: 36.183000 * Longitude: -122.307833
Date/Time Start: 1988-07-29T00:00:00 * Date/Time End: 1988-07-29T00:00:00
Minimum DEPTH, sediment/rock: -0.0100 m * Maximum DEPTH, sediment/rock: 0.0280 m
Event(s):
Reimers_D-256_IMP (D-256) * Latitude: 36.183000 * Longitude: -122.307833 * Date/Time: 1988-07-29T00:00:00 * Elevation: -1443.0 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 | ||
5 | Porosity, fractional | Poros frac | Reimers, Clare | Sediment porosity, calc. from DW and chlorite content (Reimers & Smith 1986) |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
40 data points
Data
1 Depth sed [m] | 2 SOD [mmol/m2/day] | 3 O2 [µmol/l] | 4 Temp [°C] | 5 Poros frac |
---|---|---|---|---|
-0.0100 | 38.4 | |||
-0.0090 | 38.4 | |||
-0.0080 | 38.4 | |||
-0.0070 | 38.4 | |||
-0.0060 | 38.4 | |||
-0.0050 | 38.4 | |||
-0.0040 | 38.4 | |||
-0.0030 | 38.4 | |||
-0.0020 | 38.4 | |||
-0.0010 | 37.9 | |||
0.0000 | 0.96 | 38.4 | 2.8 | |
0.0000 | 35.9 | |||
0.0010 | 30.8 | |||
0.0020 | 25.6 | |||
0.0030 | 20.5 | |||
0.0040 | 15.4 | |||
0.0050 | 10.3 | |||
0.0060 | 7.2 | 0.87 | ||
0.0070 | 7.2 | |||
0.0080 | 5.1 | 0.85 | ||
0.0100 | 2.1 | 0.84 | ||
0.0110 | 1.0 | |||
0.0120 | 0.0 | 0.83 | ||
0.0140 | 0.0 | 0.82 | ||
0.0150 | 0.0 | |||
0.0180 | 0.0 | 0.80 | ||
0.0190 | 0.0 | |||
0.0220 | 0.0 | 0.81 | ||
0.0250 | 0.0 | |||
0.0280 | 0.0 | 0.79 |