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Bibliographic Details
Main Author:	Gieskes, Joris M
Format:	Dataset Open Access
Language:	en
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; Water sample; WS
Online Access:	https://doi.org/10.1594/PANGAEA.611518
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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.