Carbonate saturation in the water column of station M8_056 off Cap Sao Vincente, Portugal (Table 1)

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 t...

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Bibliographic Details
Main Author: Gieskes, Joris M
Format: Dataset
Language:English
Published: PANGAEA 1970
Subjects:
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 sample
WS
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.611518
https://doi.org/10.1594/PANGAEA.611518
Description
Summary: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.

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