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Worldwide Open Proficiency Test: Determination of ... - Nucleus - IAEA

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2.3.4.3. <strong>Determination</strong> <strong>of</strong> U-234, U-238, Pu-239+240, Pu-238, Am-241 and Sr-90 using the<br />

conventional sequential separation method<br />

Preparation <strong>of</strong> the samples<br />

The samples were ashed at 600 o C. Ten g weighed ash replicates were taken from the different<br />

bottles. Sample decomposition was carried out using the conventional wet digestion<br />

procedure, after addition <strong>of</strong> Sr carrier, Pu-242 and Am-243 tracers. Nine samples were spiked<br />

with U-232 tracer too, for the determination <strong>of</strong> U-238 and U-234.<br />

Radiochemical Separations<br />

For the separation <strong>of</strong> uranium, the supernatant obtained from Ca-oxalate precipitation was<br />

evaporated to dryness, the oxalate was decomposed by digestion and repeated evaporation<br />

with 65% HNO3. The residues were dissolved in 15-30 ml 3 M HNO3, and then loaded on<br />

UTEVA resin column (Bed volume; 1.4 ml, column length: 26 mm) pre-conditioned with 20<br />

ml 3M HNO3. The column was washed with 30 ml 3 M HNO3, followed by 20 ml 6 M HCl.<br />

Uranium fraction was eluted with 6 ml <strong>of</strong> H2O eluted with 6 ml <strong>of</strong> H2O, and then evaporated<br />

with 2 ml 65% HNO3. After electro-deposition onto stainless steel discs, uranium was<br />

determined by alpha-spectrometry.<br />

2.3.4.4. <strong>Determination</strong> <strong>of</strong> U-234, U-238, Pu-239+240, Pu-238, Am-241 using the rapid<br />

method<br />

Preparation <strong>of</strong> the samples<br />

The samples were ashed at 600 o C. Half g weighed ash replicates were taken from the<br />

different bottles. Sample decomposition was carried out by molten salt fusion with 2 g LiBO2,<br />

0.2 g NaCO3 and 0.1 g KI after addition <strong>of</strong> Pu-242 and Am-243 and U-232 tracers.<br />

The melt was pured into 100 ml 1MHCl and then dissolved.<br />

Radiochemical Separations<br />

The actinides were preconcentrated after reduction with N2H4 by co-precipitation with<br />

calcium fluoride in acidic solution [3]. After dissolution <strong>of</strong> the precipitate the actinides were<br />

separated by selective extraction chromatography using a single column filled with TRU<br />

resin. Am, Pu and Th were stripped separately, while U and Np were stripped together. U<br />

fraction was purified by extraction chromatography using UTEVA resin.<br />

Alpha sources were prepared from the chromatographic strip solutions directly by micro-coprecipitation<br />

with neodymium fluoride. Activities were determined by isotope dilution alpha<br />

spectrometry. Figures 6, 7, 8 and 9 shows the alpha spectra obtained from the moss-soil<br />

sample.<br />

2.3.4.5. Instrumentation<br />

Alpha-spectrometer system Canbrerra Alpha Analyst<br />

Alpha-spectrometer system: EG & G ORTEC OCTETE, with EG & G Ultra BU-020-450-AS<br />

PIPS detectors, Canberra AMX 884 multiplexer, RPI 554, ADC 8701,and AIM556<br />

modules.The alpha spectra were collected and evaluated using Canberra Genie 2000 s<strong>of</strong>tware.<br />

WALLAC QUANTULUS 1220 Liquide Scintillation Spectrometer. Liquid Scintillation<br />

Spectra were collected and evaluated using Wallac WINQ v. 1.1 and EASYview v.1.0.3.4.<br />

Claisse Fluxer and Milestone MLS-Ethos plus microwave.<br />

Final Darft, page 11

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