Carbonate saturation in the water column of station M8_056 off Cap Sao Vincente, Portugal (Table 1)
| Cobertura |
LATITUDE: 37.083333 * LONGITUDE: -9.883333 * DATE/TIME START: 1969-02-19T06:00:00 * DATE/TIME END: 1969-02-19T06:00:00 * MINIMUM DEPTH, water: 0 m * MAXIMUM DEPTH, water: 3246 m |
|---|---|
| Data(s) |
07/01/1970
|
| Resumo |
Changes in the dissolved oxygen content, the alkalinity, and the pH in sea water near the ocean floor are interpreted in terms of chemical and biochemical processes at the sediment water interface. A simple model provides a plausible explanation of the observed phenomena. Special emphasis is given to the importance of borate corrections in the calculation of the solution effects of calcium carbonate. |
| Formato |
text/tab-separated-values, 90 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.611518 doi:10.1594/PANGAEA.611518 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Fonte |
Supplement to: Gieskes, Joris M (1970): Einige Beobachtungen über Lösungsvorgänge am Boden des Ozeans. Meteor Forschungsergebnisse, Deutsche Forschungsgemeinschaft, Reihe A Allgemeines, Physik und Chemie des Meeres, Gebrüder Bornträger, Berlin, Stuttgart, A8, 12-17 |
| Palavras-Chave | #Aragonite saturation; Atlantische Kuppenfahrten 1967/1-3; Calcium carbonate saturation; Carbonate mass; Chloride; DEPTH, water; IFM-GEOMAR; Leibniz-Institut für Meereswissenschaften, Kiel; M8; M8_065-8b; M8056-8b; Meteor (1964); Northeast Atlantic; pH; Temperature, water; Water sample; WS |
| Tipo |
Dataset |
