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Europium binding to humic substances extracted from deep underground sedimentary groundwater studied by time-resolved laser fluorescence spectroscopy

Saito, Takumi*; Aoyagi, Noboru   ; Terashima, Motoki  

Humic substances (HSs) are ubiquitous in various environments including deep underground and play an important role in the speciation and mobility of radionuclides. The binding of Eu$$^{3+}$$, a chemical homologue of trivalent actinide ions, to HSs isolated from sedimentary groundwater at -250 m below the surface was studied by time-resolved laser fluorescence spectroscopy combined with parallel factor analysis (PARAFAC) as a function of pH and salt concentration. PARAFAC modeling reveals the presence of multiple factors that corresponds to different Eu$$^{3+}$$ species. These factors resemble those observed for Eu$$^{3+}$$ binding to HSs from surface environments; however, detailed comparison shows that there are some particularities in Eu$$^{3+}$$ binding to the deep groundwater HSs. The distribution coefficients ($$K_{rm d}$$) of Eu$$^{3+}$$ binding to the HSs calculated from the PARAFAC modeling exhibits a rather strong salt effect. At 0.01 M NaClO$$_{4}$$ the $$K_{rm d}$$ values are relatively large and comparable to those to the surface HSs; they are decreaed at 0.1 M NaClO$$_{4}$$ by more than an order of the magnitude. The $$K_{rm d}$$ values are larger for humic acid fraction of the deep underground HSs than fulvic acid over the entire range of pH and salt concentration investigated in this study.

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Category:Nuclear Science & Technology

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