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Relative probabilities of the uranium isotopes for thorium x-ray emission and fluorescence of uranium x-rays

Conference ·
OSTI ID:5428562

Both thorium x-rays from decaying uranium isotopes and self-fluoresced uranium x-rays are prominent in high-resolution gamma-ray spectra of uranium-bearing materials. Useful application of the information carried by those x-rays has been curtailed because the probabilities of the uranium isotopes for thorium x-ray emission and for uranium x-ray fluorescence have not been known. By analyzing enrichment-meter geometry spectra from uranium oxide standards whose enrichments ranged from 0.7% to 91%, relative values, primarily, have been obtained for the probabilities of both processes. Thorium x-ray emission is very heavily dominated by {sup 235}U. In all ordinarily occurring uranium isotopic distributions, thorium x-rays may be used as a valid {sup 235}U signature. The probability for a thorium K{sub {alpha}1} x-ray to be emitted in the decay of a {sup 235}U atom is 0.048 {plus minus}0.002. In infinitely thick uranium oxide materials, the relative ratios of effectiveness for self-fluorescence, on a per unit mass basis, are approximately {sup 234}U : {sup 235}U : {sup 236}U : {sup 238}U = 1.13 : 1.00 : 0.52 : 0.028. on a per decay basis, the approximate ratios are 0.00039 : 1.00 : 0.017 : 0.18. These results imply that, contrary to what has often been stated, gamma rays are far more important than alpha particles in the self-fluorescence of uranium. Because of the importance of gamma-ray self-fluorescence, the uranium x-ray yield will be somewhat influenced by the size, shape, and composition of the materials. 4 refs., 1 fig.

Research Organization:
Los Alamos National Lab., NM (United States)
Sponsoring Organization:
DOE; USDOE, Washington, DC (United States)
DOE Contract Number:
W-7405-ENG-36
OSTI ID:
5428562
Report Number(s):
LA-UR-91-2463; CONF-910774--31; ON: DE91016235
Country of Publication:
United States
Language:
English