Marine Science Faculty Publications
Document Type
Article
Publication Date
2000
Digital Object Identifier (DOI)
https://doi.org/10.1029/1999GL002345
Abstract
A coherent representation of carbonate dissociation constants and measured inorganic carbon species is essential for a wide range of environmentally important issues such as oceanic uptake of anthropogenic CO2 and carbon cycle depictions in ocean circulation models. Previous studies have shown varying degrees of discordance between calculated and measured CO2-system parameters. It is unclear if this is due to errors in thermodynamic models or in measurements. In this work, we address this issue using a large field dataset (15,300 water samples) covering all ocean basins. Our field data, obtained using laboratory-calibrated measurement protocols, are most consistent with calculated parameters using the dissociation constants of Mehrbach et al. [1973] as refit by Dickson and Millero [1987]. Thus, these constants are recommended for use in the synthesis of the inorganic carbon data collected during the global CO2 survey during the 1990s and for characterization of the carbonate system in seawater.
Rights Information
Was this content written or created while at USF?
Yes
Citation / Publisher Attribution
Geophysical Research Letters, v. 27, issue 2, p. 229-232
Copyright 2000 by the American Geophysical Union.
Scholar Commons Citation
Lee, Kitack; Millero, Frank J.; Byrne, Robert H.; Feely, Richard A.; and Wanninkhof, Rik, "The Recommended Dissociation Constants for Carbonic Acid in Seawater" (2000). Marine Science Faculty Publications. 1721.
https://digitalcommons.usf.edu/msc_facpub/1721