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A sequential radiochemical procedure for isotopic analysis of uranium and thorium in soil

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Abstract

A sequential radiochemical procedure for isotopic analysis of uranium and thorium in soil has been developed. Analysis involves total dissolution of the samples to allow equilibration of the natural isotopes with added tracers, followed by radiochemical separation using anion exchange chromatography (BioRad AG 1−X8). Further separation and purification is performed employing solvent extraction techniques. Finally, the U and Th fractions are co-precipitated with lanthanum and cerium fluoride, respectively, and quantified by alpha-particle spectrometry. Overall chemical yields range from 60 to 90%. Under normal operating conditions and present counting set up, the minimum detectable concentration (MDC) is approximately 2 Bq/kg for soil samples. This is based on one gram aliquot of sample, 80% chemical yield, and 1000 minute counting with a detector having about 15% counting efficiency. The procedure has been successfully tested with Standard Reference Materials. Various soil samples were analyzed with high chemical yields and fine quality of alpha-spectra. Decontamination factor studies were performed to determine the extent of the carry over of210Po,225Ac,226Ra, and229Th into U fraction and210Po,225Ac,226Ra, and232U into Th fraction.

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Parsa, B. A sequential radiochemical procedure for isotopic analysis of uranium and thorium in soil. Journal of Radioanalytical and Nuclear Chemistry, Articles 157, 65–73 (1992). https://doi.org/10.1007/BF02039778

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  • DOI: https://doi.org/10.1007/BF02039778

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