(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
| Cobertura |
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 |
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| Data(s) |
03/08/2011
|
| Formato |
text/tab-separated-values, 16 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.786995 doi:10.1594/PANGAEA.786995 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Relação |
doi:10.1594/PANGAEA.786996 Sorokin, Yury I (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, doi:10.1134/S0001437011060166 |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Fonte |
P.P. Shirshov Institute of Oceanology, Southern Branch |
| Palavras-Chave | #Archive of Ocean Data; ARCOD; Black Sea; DEPTH, water; Event label; Hydrogen sulfide, formation rate; Latitude of event; Longitude of event; MULT; Multiple investigations; Radiometric counting of introduced radioisotopes; Sor-91-378; Sor-91-419; Sor-91-424 |
| Tipo |
Dataset |
