The Effect of Na^+, Mg^<2+>, and Ca^<2+> Ions on the Formation of Eu(III)-Humate Complex
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概要
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Formation of Eu (III) -humate at various concentrations of Na<SUP>+</SUP>, Mg<SUP>2+</SUP>, and Ca<SUP>2+</SUP> in a wide pH range (4<pH<8) was studied by the solvent extraction method using <SUP>152</SUP>Eu tracer. Concentrations of Na<SUP>+</SUP>, Mg<SUP>2+</SUP>, and Ca<SUP>2+</SUP> ranged from 0.020 to 1.0 M, 10<SUP>-6</SUP> to 10<SUP>-3</SUP> M, and 10<SUP>-6</SUP> to 10<SUP>-3</SUP> M, respectively. The dependence of the stability on pH and concentrations of Na<SUP>+</SUP>, Mg<SUP>2+</SUP>, or Ca<SUP>2+</SUP> was interpreted by considering the polyelectrolyte nature of humic acid. Concentration ratios of Eu (III) -humate complex to free Eu (III) ion in fresh water and seawater was estimated based on the relations between the stability of Eu (III) -humate complex and concentrations of Na<SUP>+</SUP>, Mg<SUP>2+</SUP>, or Ca<SUP>2+</SUP>. Speciation calculations of Eu (III) species dissolved in fresh water and seawater were conducted based on the relations. As a result, it was suggested that humate complex could be more important species of Eu (III) dissolved in fresh water compared with inorganic complexes such as carbonate and hydroxide. In seawater, however, the carbonate complex can be more important species, since Mg<SUP>2+</SUP> and Ca<SUP>2+</SUP> in seawater at a 10<SUP>-2</SUP> M level greatly inhibit the formation of the humate complex of Eu (III).
- 日本放射化学会の論文
- 2004-12-30
著者
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Takahashi Yoshio
Department Of Earth And Planetary Systems Sci. Graduate School Of Sci. Hiroshima University
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Takahashi Yoshio
Department Of Agricultural Chemistry The University Of Tokyo
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MINAI Yoshitaka
Musashi University and Nezu Institute of Chemistry
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