Spectrophotometric Determination of Carbonate Ion Concentrations: Elimination of Instrument-Dependent Offsets and Calculation of In Situ Saturation States

Authors

Jonathan D. Sharp, University of South Florida
Robert H. Byrne, University of South FloridaFollow
Xuewu Liu, University of South FloridaFollow
Richard A. Feely, Pacific Marine Environmental Laboratory, NOAA
Erin E. Cuyler, University of South Florida
Rik Wanninkhof, Atlantic Oceanographic and Meteorological Laboratory, NOAA
Simone R. Alin, Pacific Marine Environmental Laboratory, NOAA

Document Type

Article

Publication Date

2017

Keywords

Seawater, Absorption, Ions, Inorganic carbon compounds, Quantum mechanics

Digital Object Identifier (DOI)

https://doi.org/10.1021/acs.est.7b02266

Abstract

This work describes an improved algorithm for spectrophotometric determinations of seawater carbonate ion concentrations ([CO₃^2–]_spec) derived from observations of ultraviolet absorbance spectra in lead-enriched seawater. Quality-control assessments of [CO₃^2–]_spec data obtained on two NOAA research cruises (2012 and 2016) revealed a substantial intercruise difference in average Δ[CO₃^2–] (the difference between a sample’s [CO₃^2–]_spec value and the corresponding [CO₃^2–] value calculated from paired measurements of pH and dissolved inorganic carbon). Follow-up investigation determined that this discordance was due to the use of two different spectrophotometers, even though both had been properly calibrated. Here we present an essential methodological refinement to correct [CO₃^2–]_spec absorbance data for small but significant instrumental differences. After applying the correction (which, notably, is not necessary for pH determinations from sulfonephthalein dye absorbances) to the shipboard absorbance data, we fit the combined-cruise data set to produce empirically updated parameters for use in processing future (and historical) [CO₃^2–]_spec absorbance measurements. With the new procedure, the average Δ[CO₃^2–] offset between the two aforementioned cruises was reduced from 3.7 μmol kg^–1 to 0.7 μmol kg^–1, which is well within the standard deviation of the measurements (1.9 μmol kg^–1). We also introduce an empirical model to calculate in situ carbonate ion concentrations from [CO₃^2–]_spec. We demonstrate that these in situ values can be used to determine calcium carbonate saturation states that are in good agreement with those determined by more laborious and expensive conventional methods.

Was this content written or created while at USF?

Yes

Citation / Publisher Attribution

Environmental Science & Technology, v. 51, issue 16, p. 9127-9136

Scholar Commons Citation

Sharp, Jonathan D.; Byrne, Robert H.; Liu, Xuewu; Feely, Richard A.; Cuyler, Erin E.; Wanninkhof, Rik; and Alin, Simone R., "Spectrophotometric Determination of Carbonate Ion Concentrations: Elimination of Instrument-Dependent Offsets and Calculation of In Situ Saturation States" (2017). Marine Science Faculty Publications. 1651.
https://digitalcommons.usf.edu/msc_facpub/1651