Changes in dynamic viscosity of sea water with depth in the Pacific Ocean at Stations DM9-613W and DM9-618W
Cobertura |
MEDIAN LATITUDE: 19.650000 * MEDIAN LONGITUDE: -175.185000 * SOUTH-BOUND LATITUDE: 19.100000 * WEST-BOUND LONGITUDE: 175.530000 * NORTH-BOUND LATITUDE: 20.200000 * EAST-BOUND LONGITUDE: -165.900000 * DATE/TIME START: 1973-01-30T00:00:00 * DATE/TIME END: 1973-02-03T00:00:00 * MINIMUM DEPTH, water: 0 m * MAXIMUM DEPTH, water: 1843 m |
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Data(s) |
14/12/1976
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Resumo |
To check on the assumption that metabolic products of planktonic organisms can affect the coefficient of dynamic viscosity of seawater, viscosity was measured in water samples taken from depths of 0 to 1843 m, west of the Hawaiian Islands. Obtained results showed that plankton has no effect on viscosity of water in regions of low productivity and that viscosity can be determined with high degree of accuracy from the appropriate tables. |
Formato |
text/tab-separated-values, 24 data points |
Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.755213 doi:10.1594/PANGAEA.755213 |
Idioma(s) |
en |
Publicador |
PANGAEA |
Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
Fonte |
P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow Supplement to: Rudyakov, Yury A (1976): Effect of plankton on the viscosity of seawater. Oceanology, 16, 96-97 |
Palavras-Chave | #Archive of Ocean Data; ARCOD; Date/Time of event; DEPTH, water; DM9; DM9-613W; DM9-618W; Dmitry Mendeleev; Event label; Latitude of event; Longitude of event; Pacific Ocean; Viscosity; Water sample; WS |
Tipo |
Dataset |