Abstract

The pH on the total proton scale of the Tris-HCl buffer system (pHTris) was characterized rigorously with the electrochemical Harned cell in salinity (S) 35 synthetic seawater and S=45–100 synthetic seawater-derived brines at 25 and 0°C, as well as at the freezing point of the synthetic solutions (−1.93°C at S=35 to −6°C at S=100). The electrochemical characterization of the common equimolal Tris buffer [RTris=mTris/mTris‐H+=1.0, with mTris=mTris‐H+=0.04molkgH2O‐1=molality of the conjugate acid-base pair of 2-amino-2-hydroxymethyl-1,3-propanediol (Tris)] yielded pHTris values which increased with increasing salinity and decreasing temperature. The electrochemical characterization of a non-equimolal Tris buffer variant (RTris=0.5, with mTris=0.02mol kgH2O‐1 and mTris−H+=0.04molkgH2O‐1) yielded pHTris values that were consistently less alkaline by 0.3pH unit than those of the equimolal Tris buffer. This is in agreement with the values derived from the stoichiometric equilibrium of the Tris-H+ dissociation reaction, described by the Henderson – Hasselbalch equation, pHTris=pKTris⁎+logRTris, with pKTris⁎=stoichiometric equilibrium dissociation constant of Tris-H+, equivalent to equimolal pHTris. This consistency allows reliable use of other RTris variants of the Tris-HCl buffer system within the experimental conditions reported here. The results of this study will facilitate the pH measurement in saline and hypersaline systems at below-zero temperatures, such as sea ice brines.

Highlights

  • High latitude oceans contribute disproportionally to the CO2 uptake from the atmosphere (Bates and Mathis, 2009; Takahashi et al, 2002), but these estimates are based on data generated by sampling ice-free parts of the polar oceans

  • Large variations in brine pH can be expected in such environments, but there is only rudimentary knowledge of pH changes in sea ice as direct determination of this parameter has been hampered by lack of characterized calibration standards and unsuitable analytical set-ups for the sub-zero temperatures and, in the case of internal sea ice brines, highly saline conditions (S N 35)

  • The electrochemical characterization of the Tris buffer system in this study enables the spectrophotometric characterization of pH indicator dyes in seawater-based hypersaline media at below-zero temperatures

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Summary

Introduction

High latitude oceans contribute disproportionally to the CO2 uptake from the atmosphere (Bates and Mathis, 2009; Takahashi et al, 2002), but these estimates are based on data generated by sampling ice-free parts of the polar oceans.

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