Abstract

The speciation of Ra2+ and Ba2+ with EDTA was investigated at 25 °C in aqueous alkaline NaCl media as a function of ionic strength (0.2–2.5 mol·L−1) in two pH regions where the EDTA4− and HEDTA3− species dominate. The stability constants for the formation of the [BaEDTA]2− and [RaEDTA]2− complexes were determined using an ion exchange method. Barium-133 and radium-226 were used as radiotracers and their concentrations in the aqueous phase were measured using liquid scintillation counting and gamma spectrometry, respectively. The specific ion interaction theory (SIT) was used to account for [NaEDTA]3− and [NaHEDTA]2− complex formation, and used to extrapolate the logarithms of the apparent stability constants (log10K) to zero ionic strength (BaEDTA2−: 9.86 ± 0.09; RaEDTA2−: 9.13 ± 0.07) and obtain the Ba2+ and Ra2+ ion interaction parameters: [ε(Na+, BaEDTA2−) = − (0.03 ± 0.11); ε(Na+, RaEDTA2−) = − (0.10 ± 0.11)]. It was found that in the pH region where HEDTA3− dominates, the reaction of Ba2+ or Ra2+ with the HEDTA3− ligand also results in the formation of the BaEDTA2− and RaEDTA2− complexes (as it does in the region where the EDTA4− ligand dominates) with the release of a proton. Comparison of the ion interaction parameters of Ba2+ and Ra2+ strongly indicates that both metal ions and their EDTA complexes have similar activity coefficients and undergo similar short-range interactions in aqueous NaCl media.

Highlights

  • Barium and radium are members of the alkaline-earth metal group

  • Ion interaction parameters and associated uncertainties were derived from all available experimental data of NaEDTA3- and EDTA4- protonation in NaCl media at 25 °C listed in the review [26]

  • The apparent stability constants of the BaEDTA2- and RaEDTA2- complexes were determined over a wide range of NaCl concentrations (0.2–2.5 molÁL-1) at 25 °C and in two pH regions where the EDTA4- and HEDTA3- species dominate

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Summary

Introduction

Barium and radium are members of the alkaline-earth metal group. While barium is an abundant element in the earth’s crustal rocks (340 mgÁkg-1), radium occurs in nature only in trace amounts (0.1 ngÁkg-1) [1]. Pure radium and barium sulfate salts and their co-precipitates are, in principle, insoluble in water and aqueous solutions of mineral acids and alkali at room temperature [9] (the recommended values for the decadic logarithm of the BaSO4 and RaSO4 solubility products at zero ionic strength and 25 °C are -9.95 and -10.21, respectively [10, 11]). Aqueous alkaline EDTA solutions have been found to be effective in the dissolution of Ba(Ra)SO4 and in the extraction of 226Ra from uranium tailings [12]. 80–85% of 226Ra was extracted from uranium tailings using a 0.04 molÁL-1 aqueous alkaline EDTA solution at Elliot Lake, Ontario, Canada [13]. It is necessary to know accurately the stability constants of the BaEDTA2- and RaEDTA2- complexes to model the Ba(Ra)SO4 dissolution equilibrium in alkaline EDTA systems including decontamination using EDTA

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