Isotopic Analysis of Uranium Including
Uranium-233 in Soil Samples
By Alpha Spectrometry

R.Rosson, J. Lahr and B. Kahn

Georgia Institute of Technology

 

One gram soil samples with added U-232 tracer were totally dissolved by a microwave-oven dissolution technique ( 1 ).  Ten mg iron carrier was added to each of the samples as a carrier in a hydroxide precipitation.  The hydroxides were washed to remove excess ammonium hydroxide and then dissolved with 8 M HCl. The solution containing the uranium was sorbed on an anion exchange column, washed with 8M HCl + 0.05 M NH4I and 8 M HCl to remove interferences and then eluted with 0.1M HCl ( 2 ). The separated  uranium solution was then converted to sulfates and electroplated ( 3 ).  The electroplated samples were counted on an alpha spectrometry system to determine each uranium isotope.

Upon viewing the alpha spectra, the U-234 region appeared to have an extra peak but the resolution of the tracer was not as good as possible. The samples were dissolved from the electroplated discs, sorbed on UTEVA Eichrom columns ( 4 ), washed with 4M HNO3 then 6M HCl, eluted with 0.1M HCl and then  re-electroplated. The resolution that was achieved was now good enough to see a distinct U-233 peak at 4.82 MeV above the U-234 peak at 4.76 MeV.

The resolution was 60 to 100 KeV prior to the second column and 15 to 30 KeV full width half max of the tracer peak after second column. The resolution problem could be related to the addition of the iron carrier to the soil samples which already contain some iron.

 

To determine the amount of U-234 ( 73% 4.78, 27% 4.72 MeV alpha particles ) in the samples, we corrected for the 14.8 % of U-233 ( 1.6% 4.73, 13.2 % 4.78, 84.4 % 4.82 MeV ) alpha particles that are in the U-234 region. The available software could calculate the amount of U-233 by using the 4.82 MeV alpha particle but for U-234 it could not subtract the U-233 alpha particles in the U-234 region.

It is possible to determine U-233 and U-234 in the same sample with the good resolution that is achievable by electroplating samples and using currently available alpha particle pips. Excess solids must be removed to achieve this resolution.

 

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(1) Garcia, Ramon and Kahn, Bernd. Total Decomposition of Environmental Radionuclide Samples with a Microwave Oven; Trans. Am. Nucl. Soc. 79: 55; 1998.

(2) Krieger H.L and Whittaker, E.L. Radiochemical Method 908.0; Prescribed Procedures for Measurement of Radionuclides in Drinking Water; U.S. Environmental Protection Agency Report 600/4-80-032; pp. 96 - 102; Cincinnati OH; 1980.

(3) Talvitie, N.A. Electrodeposition of Actinides for Alpha Spectrometric Determination; Anal. Chem. 44: 280 - 283; 1972

(4) Gingell, T. The Determination of Uranium in Environmental Samples Using Extraction Chromatography.  J. Radioanalytical  Nuc. Chem.  226: 185-189; 1997.