The role of pH(T) measurements in marine CO2-system characterizations

Citation
Rh. Byrne et al., The role of pH(T) measurements in marine CO2-system characterizations, DEEP-SEA I, 46(11), 1999, pp. 1985-1997
Citations number
20
Categorie Soggetti
Aquatic Sciences","Earth Sciences
Journal title
DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS
ISSN journal
09670637 → ACNP
Volume
46
Issue
11
Year of publication
1999
Pages
1985 - 1997
Database
ISI
SICI code
0967-0637(199911)46:11<1985:TROPMI>2.0.ZU;2-F
Abstract
Spectrophotometric pH(T) measurements can routinely be obtained with an imp recision on the order of +/- 0.0005 pH(T) units. This level of imprecision is equivalent to an imprecision in total hydrogen ion concentration of +/- 0.1% (where pH(T) = -log[H+], and [H+](T) congruent to [H+] + [HSO4-]). At this level of precision, pH(T) measurements provide an important tool in qu ality control assessments of other CO2-system parameters (CO2 fugacity, tot al inorganic carbon, total alkalinity). CO2, fugacities and total alkalinit ies calculated using measured pH(T) and total inorganic carbon, for the lar ge data set considered in this work, have relative precisions on the order of 0.15 and 0.1%, respectively. The precision of total inorganic carbon cal culated via pH(T), and salinity-normalized-alkalinity is on the order of 0. 02% or better. In this work, using the NOAA 1992 boreal autumn Equatorial P acific (EqPac) dataset, it is shown that CO2-system variables calculated vi a pH(T) can be used to enhance both the precision and accuracy of directly measured parameters. Through the procedures described in this work signific ant problems were revealed in the initial version of the 1992 NOAA dataset, and the dataset was greatly improved. Additionally, in this work, we revis it CO2-system thermodynamic consistency issues in view of changes in the pH (T), values assigned to tris seawater buffers and consequential changes in the calibration of sulfonephthalein pH(T) indicators. As the principal resu lt of a +0.0047 increase in the pK of meta cresol purple, CO2 fugacity calc ulations and measurements are in very good agreement for the NOAA 1992 bore al autumn EqPac dataset. We note, as well, that due to a reassignment of th e titrant acid concentration used in the NOAA 1992 boreal autumn dataset. m easured total alkalinities are in good agreement with total alkalinities ca lculated from total carbon and pH(T). (C) 1999 Elsevier Science Ltd. All ri ghts reserved.