Worldwide Open Proficiency Test: Determination of ... - Nucleus - IAEA
Worldwide Open Proficiency Test: Determination of ... - Nucleus - IAEA
Worldwide Open Proficiency Test: Determination of ... - Nucleus - IAEA
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2.3.4. Homogeneity study and characterization <strong>of</strong> the <strong>IAEA</strong>-447<br />
To assess the homogeneity <strong>of</strong> the <strong>IAEA</strong>-447 moss-soil reference material, 10 bottles covering<br />
the whole bottling range were randomly selected; three independent test portions at ~45 g and<br />
~0.5 g from each bottle were used to perform gamma spectrometry measurements and<br />
radiochemical analysis respectively. Gamma spectrometer equipped with broad energy<br />
detector was used to analyze K-40, Cs-137, Tl-208, Pb-210, Pb-212, Pb-214, Bi-214, Ra-226,<br />
Ac-228, Th-234 and Am-241. Po-210, Ra-226, U-234, U-238, Pu-239+240, Pu-238 and Am-<br />
241 were determined by isotope dilution alpha spectrometry; Pb-210 and Sr-90 by liquid<br />
scintillation spectrometry following sample dissolution by wet mixed acid dissolution or<br />
microwave digestion or molten salt fusion and sequential radiochemical separation<br />
procedures.<br />
The analysis <strong>of</strong> homogeneity study was performed under repeatability conditions to minimize<br />
variations.<br />
The outcome <strong>of</strong> the homogeneity study demonstrated that the uncertainties due to between<br />
and within bottles heterogeneity ubb were generally very small and the material could be<br />
considered sufficiently homogeneous for the tested radionuclides at the range <strong>of</strong> mass used.<br />
2.3.4.1. Characterization and assignment <strong>of</strong> target values <strong>of</strong> the measurands <strong>of</strong> <strong>IAEA</strong>-447<br />
The analysis related to the homogeneity study and characterization <strong>of</strong> the reference material<br />
were performed at the <strong>IAEA</strong> Terrestrial Environment Laboratory in Seibersdorf (Austria).<br />
Then the analytical results <strong>of</strong> the characterization were confirmed by two external expert<br />
laboratories.<br />
The gamma emitting radionuclides were measured using a metal (radon tight) sample<br />
container. The spectrum was collected after 30 days when the Ra-226 Rn-222 equilibrium<br />
reached. A special low background n-type HPGe detector 30% relative efficiency with<br />
CARBON-EPOXI window was used for the spectrum collection. The shielding was made <strong>of</strong><br />
7 cm low background lead and 3 mm <strong>of</strong> copper. An example for the measurement <strong>of</strong> gamma<br />
emitting nuclides in the <strong>IAEA</strong>-447 the moss-soil reference material is shown on the Figure 4.<br />
The property values <strong>of</strong> all radionuclides <strong>of</strong> the <strong>IAEA</strong>-447 were established on the basis <strong>of</strong> a<br />
robust approach proposed by David L. Duewer [1] and the Mixture Model Median (MMmedian)<br />
<strong>of</strong> the analytical results reported by the <strong>IAEA</strong> Terrestrial Environment Laboratory<br />
was calculated. The MM-median is a direct analogue <strong>of</strong> the median. It is the location which<br />
divides the Mixture Model Probability Density Function (MM-PDF) into two sections <strong>of</strong><br />
equal area. The MM-median is closely related to the median. It is robust to outliers and also<br />
accounts for the reported uncertainty <strong>of</strong> each measurement result.<br />
To estimate the standard uncertainty associated with the property value the MM-median based<br />
Standard Deviation S(MM-median) was calculated from the span <strong>of</strong> the central 50% <strong>of</strong> the<br />
MM-PDF density function [1].<br />
2.3.4.2. <strong>Determination</strong> <strong>of</strong> Pb-210 and Po-210 in the moss-soil reference material<br />
Preparation <strong>of</strong> the samples<br />
Half g aliquots <strong>of</strong> the sample from the different bottles were transferred into microwave<br />
containers, about 30 mg <strong>of</strong> Pb 2+ carrier; about 0.4 Bq <strong>of</strong> Po-209 tracer and 15ml 65% HNO3<br />
were added. After digestion the sample solutions were then transferred to plastic centrifuge<br />
tubes and centrifuged for 10 minutes at 3000 rpm. The supernatants were transferred to Teflon<br />
beakers and the residues were transferred back into the microwave containers with 3 ml<br />
HNO3 and 2 ml <strong>of</strong> 40% HF. The residues were digested again using the same microwave<br />
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