Chemistry measured on water bottle samples at station DrakePassage1
Cobertura |
LATITUDE: -60.800000 * LONGITUDE: -63.400000 * DATE/TIME START: 1989-03-28T00:00:00 * DATE/TIME END: 1989-03-28T00:00:00 * MINIMUM DEPTH, water: 30 m * MAXIMUM DEPTH, water: 1400 m |
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Data(s) |
12/07/2004
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Formato |
text/tab-separated-values, 40 data points |
Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.194727 doi:10.1594/PANGAEA.194727 |
Idioma(s) |
en |
Publicador |
PANGAEA |
Relação |
Johnson, Kenneth S; Gordon, R Michael; Coale, Kenneth H (1997): What controls dissolved iron in the world ocean? Marine Chemistry, 57(3-4), 137-162, doi:10.1016/S0304-4203(97)00043-1 Martin, JH; Gordon, R Michael; Fitzwater, Steve (1990): Iron in Antarctic waters. Nature, 345(6271), 156-158, doi:10.1038/345156a0 |
Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
Palavras-Chave | #compiled data; DEPTH, water; DrakePassage1; Element analyser AAS, graphite furnace, Perkin-Elmer 5000; GOFLO; Go-Flo bottles; Iron, dissolved; JGOFS; Joint Global Ocean Flux Study; Nitrate; Oxygen; Oxygen, apparent utilization; Phosphate; Salinity; Silicate; Silicon Cycling in the World Ocean; SINOPS; Temperature, water; World Ocean |
Tipo |
Dataset |