Sorokin, Yury I (2011): (Table 3) Rates of hydrogen sulfide formation due to bacterial sulfate reduction in the water mass of the lower portion of the pycnocline layer at different stations in the Black Sea in February-April 1991 [dataset]. P.P. Shirshov Institute of Oceanology, Southern Branch, PANGAEA, https://doi.org/10.1594/PANGAEA.786995, In supplement to: Sorokin, YI (2011): On the rates of sulfide formation and oxidation in the Black Sea during the cold season. Translated from Okeanologiya, 2011, Vol. 51, No. 6, pp. 1030-1038, Oceanology, 51(6), 969-977, https://doi.org/10.1134/S0001437011060166
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Project(s):
Archive of Ocean Data (ARCOD)
Coverage:
Median Latitude: 44.680000 * Median Longitude: 31.660000 * South-bound Latitude: 43.210000 * West-bound Longitude: 31.240000 * North-bound Latitude: 45.660000 * East-bound Longitude: 32.120000
Minimum DEPTH, water: 100 m * Maximum DEPTH, water: 250 m
Event(s):
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | ||||
| 2 | Latitude of event | Latitude | ||||
| 3 | Longitude of event | Longitude | ||||
| 4 | DEPTH, water | Depth water | m | Geocode | ||
| 5 | Hydrogen sulfide, formation rate | H2S fr | nmol S/l/day | Sorokin, Yury I | Radiometric counting of introduced radioisotopes |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
16 data points