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Ge(Li) spectrometric measurements of isotopic uranium ratios in soils treated with apatite-derived fertilizers

Conference ·
OSTI ID:4164365
Soil samples collected in an agricultural region of the Sacramento-San Joaquin Delta in central California contained levels of uranium as high as 17 ppm. Isotopic uranium analysis, determined by mass spectrometry, showed $sup 235$U/ $sup 238$U ratios of 7.1 x 10$sup -3$, typical of natural uranium. However, the $sup 238$U content inferred from gamma counting of the $sup 226$Ra daughters disclosed marked disequilibrium in the $sup 238$U decay series. The elevated levels of uranium are attributed to its presence in ammonium phosphate fertilizer produced from apatite [CaF$sub 2$Ca$sub 3$(PO$sub 4$$)$$sub 2$]. The $sup 238$U daughter disequilibrium is due to removal of $sup 226$Ra by coprecipitation with CaSO$sub 4$ during conversion of the raw material to phosphoric acid with sulphuric acid. A more direct method for $sup 238$U measurement based on detection of the 63-keV transition gamma of $sup 234$Th and using Ge(Li) gamma spectrometry is described. This method is independent of $sup 226$Ra daughters and can detect $sup 238$U down to about 0.1 $mu$g/g in soils. A comparison with $sup 238$U measurements using mass spectrometry shows agreement within +- 10 percent. (auth)
Research Organization:
Univ. of California, Livermore
NSA Number:
NSA-33-007323
OSTI ID:
4164365
Country of Publication:
IAEA
Language:
English