Reimers, Clare (2002): Sediment properties at H-238 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.78723
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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: 35.956160 * Longitude: -122.988000
Date/Time Start: 1988-07-25T00:00:00 * Date/Time End: 1988-07-25T00:00:00
Minimum DEPTH, sediment/rock: 0.0000 m * Maximum DEPTH, sediment/rock: 0.0190 m
Event(s):
Reimers_H-238_BC (H-238) * Latitude: 35.956160 * Longitude: -122.988000 * Date/Time: 1988-07-25T00:00:00 * Elevation: -3571.0 m * Location: North Pacific/Gulf of California/SLOPE * Campaign: TT183 * Basis: Thomas G. Thompson (1964) * Method/Device: Box corer (BC)
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Nitrate and Nitrite | [NO3]- + [NO2]- | µmol/l | Reimers, Clare | Spectrophotometry (Gieskes & Peretsman, 1986) | |
| 3 | Manganese | Mn | µmol/l | Reimers, Clare | Element analyser AAS, graphite furnace, Perkin-Elmer 5000 | |
| 4 | Ammonium | [NH4]+ | µmol/l | Reimers, Clare | Spectrophotometry (Gieskes & Peretsman, 1986) |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
50 data points
Data
| 1 Depth sed [m] | 2 [NO3]- + [NO2]- [µmol/l] | 3 Mn [µmol/l] | 4 [NH4]+ [µmol/l] |
|---|---|---|---|
| 0.0000 | 39.0 | 0.0 | 0.0 |
| 0.0002 | 42.0 | 0.5 | 22.2 |
| 0.0008 | 39.0 | 1.0 | 19.9 |
| 0.0012 | 10.3 | 2.1 | 8.6 |
| 0.0018 | 2.1 | 2.6 | 6.0 |
| 0.0025 | 1.0 | 9.7 | 10.6 |
| 0.0035 | 3.1 | 12.8 | 17.7 |
| 0.0045 | 1.0 | 14.4 | 24.3 |
| 0.0055 | 0.0 | 10.8 | 27.0 |
| 0.0065 | 0.0 | 11.0 | 31.1 |
| 0.0075 | 0.0 | 12.8 | 38.2 |
| 0.0090 | 0.0 | 10.3 | 42.7 |
| 0.0110 | 0.0 | 11.3 | 50.0 |
| 0.0130 | 0.0 | 11.8 | 59.9 |
| 0.0150 | 0.0 | 12.3 | 67.2 |
| 0.0170 | 0.0 | 11.3 | 74.5 |
| 0.0190 | 0.0 | 10.3 |