Membrane luminescence determination of technogenic actinides and their speciation in environmental objects
Researchers of the Vernadsky Institute of Geochemistry and Analytical Chemistry of the Russian Academy of Sciences created a luminescence photometer of a new generation for the determination of trace amounts of uranium and transuranium elements ( TUE ). The limits of detection for actinides vary fro...
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Veröffentlicht in: | Geochemistry international 2016-12, Vol.54 (13), p.1196-1209 |
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Format: | Artikel |
Sprache: | eng |
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Zusammenfassung: | Researchers of the Vernadsky Institute of Geochemistry and Analytical Chemistry of the Russian Academy of Sciences created a luminescence photometer of a new generation for the determination of trace amounts of uranium and transuranium elements (
TUE
). The limits of detection for actinides vary from 0.3 pg for uranium and neptunium to 2.0 pg for plutonium. For
237
Np, the relative limit of detection is 0.008 Bq/L. The photometer was tested in the radioecological monitoring of a number of polluted zones in Russia. The dynamics of actinide migration in all of the studied zones enhanced in the series
239
Pu <
241
Am <
237
Np. In this series, concentrations of radionuclides in water-soluble and exchange forms that are most mobile and determine the migration mobility of chemical elements increased in all of the studied soil types. In the group of fulvic acids, concentrations of radionuclides decreased in the series
237
Np >
241
Am >
239
Pu irrespectively of the soil. In the group of humic acids, concentrations of radionuclides increased in the series
237
Np <
239
Pu <
241
Am. The sorption coefficients of radionuclides by bottom sediments of the Markha River (Kraton-3 underground nuclear explosion site) and Lake Kyzyltash (East Urals Radioactive Trace) were calculated. Bioaccumulation factors of radionuclides by different plants in the impact area of the Kraton underground nuclear explosion were determined depending on the plant type. |
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ISSN: | 0016-7029 1556-1968 |
DOI: | 10.1134/S0016702916130139 |