4.3 Article

Spectrophotometric analysis of the CO2 system in aqueous solutions: A freshwater example from the Snake River, Idaho, USA

Journal

LIMNOLOGY AND OCEANOGRAPHY-METHODS
Volume 20, Issue 12, Pages 741-753

Publisher

WILEY
DOI: 10.1002/lom3.10525

Keywords

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Funding

  1. National Science Foundation [OCE-1657894]
  2. Carl Riggs Fellowship in Marine Science by the University of South Florida, College of Marine Science

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This work presents a new method for comprehensively characterizing the inorganic carbon system in aqueous solutions. The method utilizes simple spectrophotometric measurements and is applicable to both open-ocean seawater and freshwater samples. It is the first method to spectrophotometrically measure A(C), allowing for a complete characterization of the carbon system using only spectrophotometric measurements. The method also provides a quantitative correction for potential artifacts arising from sample preparation.
This work describes a new, generally applicable method to comprehensively characterize the inorganic carbon system of aqueous solutions. The method requires only simple spectrophotometric measurements and is appropriate for not only open-ocean seawater (where convenient assumptions and approximations may be made) but also the more challenging case of freshwaters. The overall approach is to (1) measure pH in the field at the time of sample collection and (2) measure sample pH, carbonate alkalinity (A(C)), and total alkalinity (A(T)) later in the laboratory. All required equipment is inexpensive and portable. The paired laboratory measurements of pH and A(C) can be used to obtain the concentration of total inorganic carbon (C-T). This C-T can in turn be paired with the field pH measurements to comprehensively characterize carbon-system parameters in the sampled water body at in situ conditions. To our knowledge, this method is the first to spectrophotometrically measure A(C) and thus the first to completely characterize C-T and the carbon system of freshwaters using spectrophotometric measurements only. The concurrent measurements of A(C) and A(T) can also be used to partition alkalinity into its carbonate and noncarbonate components. This work additionally describes how to quantitatively correct for artifacts that may arise (especially in freshwater samples) from using HgCl2 to halt respiration in sample bottles. The use of these methods is illustrated using samples collected from the Snake River (Idaho, USA) before and during the 2020 spring flow.

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