round-robins in the area of uranium and plutonium bulk analysis of environmental samples
TRANSCRIPT
Round-robins in the area of uranium and plutonium bulk analysisof environmental samples
Fabien Pointurier • Ross W. Williams •
Stephen P. LaMont • Robert E. Steiner •
Debbie A. Bostick • Khris B. Olsen • Ned A. Wogman
Received: 4 July 2012 / Published online: 8 August 2012
� Akademiai Kiado, Budapest, Hungary 2012
Abstract In the framework of a collaboration between
laboratories involved in bulk U and Pu analysis of envi-
ronmental samples (DIF centre of the French Commissariat
a l’Energie Atomique, US National Laboratories of New
Brunswick, Lawrence Livermore, Pacific Northwest, Oak
Ridge, and Los Alamos), two round-robins were organised,
each one consisting of the complete analysis (chemical
preparation and isotope measurement) of three Quality
Control samples. The samples were 10 9 10 cm cotton
tissues (‘‘swipe samples’’) containing low amounts of U
(from *20 to *150 ng) and Pu (from *0.15 to *10 pg).
Despite using different spikes, different methods of sample
preparation and different analytical instrumentation, the
results for U and Pu contents and isotopic compositions
reported by all laboratories are globally in good agreement.
All laboratories are able to measure sub-pg amounts of U
and Pu isotopes with acceptable accuracy and reproduc-
ibility, even if limited discrepancies are observed affecting
one or other measurement and/or laboratory. General and
laboratory specific recommendations were discussed and
adopted to continue to improve the accuracy and precision
of the measurements.
Keywords Uranium � Plutonium � Round-robin �Inter-comparison � Swipe samples � Bulk analysis
Introduction
Action Sheet 4 (AS 4) between the United States Department
of Energy/National Nuclear Security Administration (DOE/
NNSA) and the Commissariat a l’Energie Atomique (CEA) of
France for cooperation in the area of Bulk Environmental
Sampling was signed in July 2007. All participating labora-
tories are members of the IAEA’s NetWork of Analytical
Laboratories (NWAL) for bulk analysis. Environmental
sampling is considered to be one of the key tools in safeguards
for the detection of undeclared activities. Inspectors from the
IAEA (International Atomic Energy Agency) collect small
amounts of nuclear material (U, Pu, fission products, etc.) by
wiping various surfaces inside or around nuclear facilities,
using small pieces of cotton cloth, referred to as ‘‘swipe
samples’’. These samples are sent for analysis to a few labo-
ratories that are members of the NWAL of the IAEA in sup-
port of the safeguards. When ‘‘U–Pu bulk analysis’’ is
requested by the IAEA, the whole ‘‘swipe sample’’ is reduced
to ashes, digested, U and Pu are purified from the matrix and
from various impurities, and U and Pu content as well as
isotopic ratios are measured using mass spectrometry tech-
niques. The laboratories involved in the collaboration are the
following: the DIF centre of the CEA (CEA/DIF), Lawrence
Livermore National Laboratory (LLNL), Pacific Northwest
National Laboratory (PNNL), Oak Ridge National Laboratory
(ORNL) and Los Alamos National Laboratory (LANL).
F. Pointurier (&)
CEA, DAM, DIF, 91297 Arpajon, France
e-mail: [email protected]
R. W. Williams
DOE/LLNL, P.O. Box 808, Livermore, CA 94551, USA
S. P. LaMont � R. E. Steiner
DOE/LANL, MS-J514, P.O. Box 1663, Los Alamos, NM
87545, USA
D. A. Bostick
DOE/ORNL, MS-6050, P.O. Box 2008, Oak Ridge, TN
37831-6050, USA
K. B. Olsen � N. A. Wogman
DOE/PNNL, P.O. Box 999, Richland, WA 99354, USA
123
J Radioanal Nucl Chem (2013) 296:599–608
DOI 10.1007/s10967-012-1985-6
In the framework of AS 4, laboratories have exchanged
their analytical procedures related to both sample prepa-
ration (chemical purification) and isotopic measurement,
and organised two round-robins (RRs) (i.e. analysis of
Quality Control Samples—QCS). First RR took place from
January to September 2008 and the second one from July
2010 to March 2011. Additionally, several meetings were
organised, to discuss analytical procedures, results, rec-
ommendations, etc. These RRs have several specificities.
At first, no target values are defined, as masses of U and Pu
added to the samples were not certified. Therefore, results
are compared to the global average. Second, despite pre-
cautions, there is no guarantee that samples are perfectly
identical. However, considerable care was taken to prepare
homogeneous and uniform samples for distribution in these
RRs, so that differences between results can reliably be
attributed to differences in the metrology. The excellent
agreement observed between most of the quantification
results, both for U and Pu, suggests that samples may be
considered identical both for mass of nuclear material and
for isotopic composition within the precision of the mea-
surements. Third, these exercises, in contrast to other
international RRs [1–4], involve chemical purification and
extraction of U and Pu. Because all the laboratories have to
carry out a chemical preparation, discrepancies can be due
to both errors in isotopic measurements and to contami-
nation during the chemical purification procedure. Fourth,
the amounts of U and Pu contained in the samples for these
RRs were uniquely low. Finally, total Pu contents ranged
from *0.15 to *10 pg, and total U contents ranged from
*20 to *150 ng. Lastly, the type of sample, the ‘‘swipe
samples’’ which consist in 10 9 10 cm cotton tissue,
identical to the ones used by the IAEA to collect dust in
inspected facilities, is not common for RR samples. Other
RRs usually consist of nuclear materials [3, 4] or solutions
containing high concentrations of actinides [1, 2], or urine
samples [5, 6]. However, all participating laboratories, as
members of the NWAL, are accustomed to analysing such
samples.
This paper is focused on the two RRs carried out in the
framework of this collaboration. The RR samples were
prepared at LLNL by adding acidic solutions containing U
and Pu to the cotton swipes. The swipes were dried, placed
in double plastic bags, labelled, and sent to the partici-
pating laboratories as environmental samples. In this paper,
procedures and instruments used by the laboratories are
briefly presented. Then, results obtained by the laboratories
are described and commented upon, both for U and Pu
quantifications and isotope composition measurements.
The last part of the paper gives the conclusions drawn from
this collaboration, expresses recommendations to improve
laboratory performances for bulk analysis of environmental
samples. In general, despite using different spikes, different
methods of sample preparation and different analytical
instrumentation, the differences between the results
reported by all laboratories are quite small. So, this report
focuses on those small differences to aid each laboratory to
continue to improve their analytical methods, and serves as
a benchmark for further RRs or analytical developments.
Experimental
Methods used by all the participating laboratories are
similar. They basically consist in a two-step process: (i) a
chemical purification to eliminate most of the sample
matrix and to concentrate as much as possible the elements
of interest (U, Pu), and (ii) an isotope measurement using a
mass spectrometry technique. All procedures, for sample
preparation and for mass spectrometry measurement as
well, are fully documented in QA written procedures.
Comparison of the chemical purification treatment
For all of the participating laboratories, the chemical
purification step starts with combustion of a sample swipe
into ash in an oven, and is followed by dissolution and
chromatographic separation of U and Pu from the major
elemental components of the matrix thanks to an oxida-
tion—reduction cycle. However, type and quantity of resin,
as well as types, volumes and concentrations of reagents
vary from one laboratory to the other.
Main features, common points and differences between
labs of these chemical purification treatments are given
hereafter. All labware is single-use. All DOE labs use
quartz, Teflon and/or poly fluoro alkyl (PFA) labware,
whereas CEA uses borosilicated glass. The combustion to
ash step is carried out by all laboratories in dedicated
ovens, although a large range of temperature, from 400 to
750 �C, is defined. Regarding the chemical separation
technique, all laboratories use chromatography to separate
U and Pu from the sample matrix. However, some labo-
ratories use solid phase extraction chromatography (PNNL
[7], LLNL, ORNL), whereas the others use ion exchange
chromatography (CEA [8], LANL). It should be mentioned
that all laboratories clean the resins beforehand. Quantities
of resin used by the labs are rather small: from 0.5 to 2 mL
for DOE labs. However, for the initial U/Pu separation,
CEA uses a 20-mL column filled with resin. All laborato-
ries use the isotope dilution technique to quantify U and
Pu. 233U is used by all labs for U quantification, whereas242Pu (CEA, LANL) or 244Pu (LLNL, PNNL, ORNL) can
be used for Pu quantification. It is preferable to use 244Pu
rather than 242Pu because environmental samples never
contain 244Pu but usually contain small amounts of 242Pu.
All tracers are as pure as possible, although they all contain
600 J Radioanal Nucl Chem (2013) 296:599–608
123
traces of other isotopes from the same element. These
contributions are corrected for and amounts of tracers
added to the samples are limited, both for economic rea-
sons and for limiting degradation of the accuracy and
precision of isotope measurements due to correction from
tracer impurities. It should be noted that some laboratories
(ORNL, PNNL) sample an aliquot of each sample after
dissolution to screen the U and Pu concentrations in the
samples. CEA/DIF, LANL (most of the time), LLNL, and
ORNL perform at first a U–Pu separation, and then purify
separately on U and Pu fractions. On the contrary, for
PNNL and LANL in particular cases (high Pu and/or U
contents), samples after dissolution are divided in two
parts, one for U the other for Pu. All labs use various acids
of ultra-pure grade, and all laboratories take many pre-
cautions to protect samples from airborne contamination
during critical steps. Most of them use laminar flow hoods
to protect sample from airborne contamination. LANL,
LLNL and ORNL even use clean room facilities for sample
preparation. All laboratories consider that their sample
preparation techniques based on chromatography with
limited volumes of resins are the most adaptable to the
trace measurement of actinides (low blank levels are
achievable and smaller amounts of reagents are needed).
Comparison of the mass spectrometry measurements
The participating laboratories use two types of mass
spectrometers: inductively coupled plasma-mass spec-
trometers (ICP-MS) and thermal-ionisation mass spec-
trometer (TIMS). All laboratories have at their disposal
several more or less recent high performance ICP-MS and/
or TIMS. These are quadrupole-based ICP-MS (CEA/DIF
for U [9], PNNL, LANL), double focusing single-collector
ICP-MS (CEA/DIF for Pu) or multi-collection ICP-MS
(LLNL, PNNL, ORNL) or TIMS (LANL). Common trends
in analytical methodology include the fact that most of the
instruments now used for sample analysis are ICP-MS.
Sample introduction into the ICP-MS is commonly
achieved with the use of micro-nebulizers, desolvating
membranes to enhance sensitivity of small volumes of
solutions (mL range) by concentrating as much as possible
the elements of interest. Moreover, laboratories tend now
to be equipped with multiple collector instruments, which
allow improving reproducibility of isotope ratios and
measurement of very low abundant isotopes like 236U in
some samples. All laboratories, except CEA/DIF, now use
multiple collector instruments for bulk analysis, and carry
out multiple ion–counting whenever possible. Other com-
mon practices are the use of home-made software for cal-
culations, including an uncertainty budget, instead of
software provided by the manufacturer with the instrument.
In the same way, all laboratories correct raw data for U
hydrides, both at the mass to charge ratio of 236U for 235UH
and at the mass to charge ratio of 239Pu for 238UH. Besides,
LLNL, ORNL and CEA/DIF consider—and correct for if
appropriate—the possible influence of various polyatomic
species at the mass-to-charge ratios of Pu isotopes which
may cause significant isobaric interferences when Pu is in
the fg (10-15 g) range [8, 10]. Lastly, all laboratories
correct raw signal counts from background induced by
peak tailing from high intensity neighbouring peaks (gen-
erally 238U). Thus, all participating laboratories are in
compliance with what can be called ‘‘good laboratory
practices for precise and accurate measurements of isotope
ratios’’.
Description of the RR samples
The RR samples were prepared at LLNL in a clean envi-
ronment by adding acidic solutions containing U and Pu to
the cotton swipes. The swipes were dried, placed in double
plastic bags, labelled, and sent to the participating labora-
tories as environmental samples. The activities of U and Pu
in these samples were much lower than the definitions of
radioactive material for international and domestic US
shipping, and the samples were sent by common carrier.
Each laboratory was sent a duplicate set of samples.
Statistical tests
Statistical tests were carried out to detect outlying obser-
vations. In this study, the following statistical tests were
carried out: (i) Comparison with arithmetic mean with
variance estimated using the sample; (ii) comparison with
arithmetic mean: Grubbs test; (iii) Dixon’s test. The cor-
responding test statistic functions and their distributions for
various levels of significance (5 and 1 % in this study) are
given in [11].
Results
Masses of U and Pu are expressed in ng and in pg. Isotopic
ratios are expresses as atomic ratios. The uncertainties are
expanded standard uncertainties, given with a coverage
factor of 2 (*95 % confidence level assuming a Gaussian
distribution of the results). The following abbreviations are
used below: QCS1-1, QCS1-2 and QCS1-3 refer, respec-
tively to QC samples of the RR #1; QCS2-1, QCS2-2 and
QCS2-3 refer, respectively to QC samples of the RR #2;
PB1 and PB2 refer to ‘‘Process Blank’’ (or ‘‘Reagent
Blank’’) of the 2 RRs. BS1 and BS2 refer to ‘‘Blank
Swipes’’, i.e. cotton swipes distributed with the QCS, for
the RR #1 and #2; lastly, NU refers to natural U. For
confidentiality reasons, names of the five participating
J Radioanal Nucl Chem (2013) 296:599–608 601
123
laboratories are replaced by letters ‘‘A’’ to ‘‘E’’. Average U
and Pu masses, and average U and Pu atomic ratios mea-
sured by the participating laboratories for the 2 RRs are
given in Table 1. Standard uncertainties for each value are
calculated as the standard deviations over all the results
obtained by the participating laboratories. However, only
average values for which reasonably low relative combined
uncertainties were obtained are given: the relative expan-
ded uncertainties with a coverage factor of 2 should be
below 100 %.
Plots of normalised results for all QCSs from the 2 RRs
are given in Fig. 1 for U analyses and in Fig. 2 for Pu
analyses. All results are normalised to the average values
calculated from the results obtained by all laboratories for
the same QCS. Only the results for which relative expan-
ded uncertainties are below 25 % in the case of U analyses
and below 100 % in the case of Pu analyses are plotted.
However, a Pu contamination occurred during the prepa-
ration process of RR #2, more precisely when the cotton
samples were packaged. Consequently, all laboratories
detected various Pu amounts in the BS2 samples. As this
contamination is likely variable from one QCS to the other,
it is not possible to draw conclusions from these mea-
surements. Therefore, only results from the RR #1 are
plotted in the case of Pu analyses. Results from statistical
tests are given in Table 2 for U and Pu analyses. Main
comments about results are given below.
U quantification
U contents in BSs are rather homogeneous, between 4.2
and 4.6 ng for the RR #1 and *3 ng for the RR #2. This U
content is not negligible and this prevents proper mea-
surements if only low amounts of U (hundreds of pg to a
few ng) are sampled. This is not surprising as cotton used
for these RRs is known for containing a relatively high
amount of NU. Good agreements are observed between all
laboratories for all the samples, although results are less
homogeneous for the RR #2 than for the RR #1. However,
results from laboratory C for all QCSs of the RR #1 are
slightly lower than the average values although the dif-
ferences are not significant. For the RR #2, laboratory B
shows a tendency to be slightly overestimated with respect
to the average values. According to statistical tests, no
outliers are detected.
234U/238U atom ratios
It should be noted that laboratories B and C probably
overestimated 234U/238U ratios in the PBs. This can be
due to contamination or to inaccurate corrections from
background or isotopic dilution tracer. 234U/238U ratios Ta
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602 J Radioanal Nucl Chem (2013) 296:599–608
123
measured in the BS are in relatively good agreement
(considering the low 234U amounts in the samples) for all
laboratories. However, the average 234U/238U average ratio
is surprisingly high (*9 9 10-5) in comparison to the
common ratio for NU (*5.5 9 10-5) even if it is well
known that this isotopic ratio can vary largely in the
environment because of geochemical effects. For all QCSs
from both RRs, results are in good agreement. Results from
lab E are slightly above the average ratios for all QCSs of
the RR #1 and also significantly below the average value
for QCS2-3 of the RR #2. Results for QCS1-2, QCS1-3 and
QCS2-3 obtained by lab E are identified as outliers
according to statistical tests. Moreover, these results from
lab E have also higher uncertainties than results from other
laboratories. By contrast, results from labs B and D show
an excellent reproducibility and accuracy (with respect to
the average ratios).
235U/238U atom ratios
Most laboratories measure 235U/238U in the PBs within
uncertainty of NU ratio (7.25 9 10-3). However, the
results from laboratories B, D and E are all slightly elevated
with respect to NU. Regarding the BSs, all laboratories
recovered the 235U/238U NU ratio, except lab D for which
result for BS1 shows an excellent reproducibility but is
clearly slightly elevated relative to the average. A possible
explanation is contamination by extraneous U during the
chemical preparation process. For all QCSs from RR #1,
most of the results are globally in good agreement. How-
ever, the result from lab D is slightly above average for
QCS1-1 and the result from lab A is slightly below average
for QCS1-3. This latter result is identified as an outlier
according to statistical tests. For QCSs from RR #2, most of
the results are also globally in good agreement. However,
biases for specific samples with respect to average values
are observed for lab C (QCS2-1, ?1.2 %), lab D (QCS2-1,
-2.4 %, identified as outlier according to statistical tests),
and lab E (QCS2-3, -2.8 %, identified as outlier according
to statistical tests). These non-systematic biases can result
from inaccurate correction from various effects, or by ran-
dom contamination during the sample spiking—packaging
process and during the sample treatment.
236U/238U atom ratios
Two laboratories (B and D) detected 236U in the PBs and in
the BSs. These anomalous detections may result from
inaccurate corrections (235U hydrides, tailing from the 238U
peak, isotope dilution tracer impurities, background, etc.)
or contamination during the chemical purification process.
Laboratory E also systematically reported negative isotopic
ratios for both PBs and BSs. Regarding QCSs from RR #1,
only lab D was able to detect a very low (*2 9 10-7; i.e.
*5 fg of 236U) significant 236U/238U ratio in QCS1-1. As
the detected isotopic ratio is close to the ones detected in
PB1 and BS1, the hypothesis of a contamination by
extraneous U during the chemical preparation process
cannot be ruled out. Nevertheless, results of all laboratories
are in good agreement for QCS1-2 and QCS1-3. This
proves the ability of the participating laboratories to mea-
sure 236U/238U ratios in the 10-6–10-5 range. Although the
Fig. 1 Plots of all significant results for U content and U isotope ratio
measurements obtained by the laboratories for the 2 RRs. All results
are normalised to the average values calculated from the results
obtained by all laboratories for the same sample. Only the results for
which relative expanded uncertainties are below 25 % are plotted.
The results are given in the following order from left to right for each
laboratory: QCS1-1, QCS1-2, QCS1-3, QCS2-1, QCS2-2 and QCS2-
3. Uncertainties are expanded uncertainties (coverage factor of 2)
J Radioanal Nucl Chem (2013) 296:599–608 603
123
most precise of all, results from lab D are significantly
below the average ratios for QCS1-2 and QCS1-3, and may
be slightly underestimated with respect to the other labo-
ratories. However, these values do not appear as outliers
according to statistical tests. Regarding QCSs from RR #2,236U/238U ratios are very different from one sample to the
other: *3 9 10-4 in QCS2-1, *10-3 in QCS2-2, and an
extremely low value for QCS2-3. A good agreement
between laboratories is obtained for QCS2-1 and QCS2-2.
Laboratories B and E reported negative values for QCS2-3,
which is probably due to overcorrection from background.
The results from lab E is regarded as an outlier according to
statistical tests.
Pu quantification
One laboratory (D) reported detection of Pu in PB1 and
BS1 (resp. *15 and *30 fg), whereas laboratories B and E
reported negative values for PB1 and BS1. Results of the 3
QCSs from RR #1 are in good agreement, although results
Fig. 2 Plots of all significant
results for Pu content and240Pu/239Pu ratio measurements
obtained by the laboratories for
the RR #1. No results were
taken into account for the RR #2
as a Pu contamination occurred
during the sample packaging.
All results are normalised to the
average values calculated from
the results obtained by all
laboratories for the same
sample. Only the results for
which relative expanded
uncertainties are reasonably low
(below 100 %) are plotted. No
results were given for the241Pu/239Pu and 242Pu/239Pu
ratios as no average values can
be calculated. The results are
given in the following order
from left to right for each
laboratory: QCS1-1, QCS1-2,
and QCS1-3. Uncertainties are
expanded uncertainties
(coverage factor of 2)
Table 2 Outlying values according to the statistical tests for U and Pu analyses, for both RRs
U (ng) 234U/238U 235U/238U 236U/238U Pu (pg) 240Pu/239Pu 241Pu/239Pu 242Pu/239Pu
BS1 – – – – – C – –
QCS1-1 – – – – – – B –
QCS1-2 – Ea – – – – – C
QCS1-3 – E A – – C – –
BS2 – – – – No test No test No test No test
QCS2-1 – – D – No test No test No test No test
QCS2-2 – – – – No test No test No test No test
QCS2-3 – E E E No test No test No test No test
The tests were not applied to Pu results of the RR #2, because of a Pu contamination occurred during the packaging process. If not outlying
values are detected, the corresponding cell is filled with a hyphena Only according to Dixon’s test
604 J Radioanal Nucl Chem (2013) 296:599–608
123
from lab E are almost systematically significantly lower
than the average values. This may be a spike calibration
issue or result from inaccurate measurement of the mass of
isotopic dilution tracer added to the sample.
240Pu/239Pu atom ratios
Results from all laboratories are in very good agreement
for QCS1-1 and QCS1-2. However, some discrepancies
between results are observed for QCS1-3. This is not sur-
prising as the quantity of 240Pu is lower for this QCS
(\10 fg) than for the two others QCSs (*400 fg for both
of them). Lab C measured 240Pu/239Pu ratio of (*2.0 ±
0.4) 9 10-2 in QCS1-3 is significantly higher than the
average value of *8 9 10-3, whereas lab B measured
ratio of (*1.7 ± 4.2) 9 10-3, despite its very large
uncertainty, is significantly lower than the average. The
results from lab C for BS1 (-4.0 ± 13.4) and for QCS1-3
are identified as outliers according to statistical tests. By
contrast, low uncertainty and excellent accuracy with
respect to the average ratios of lab D should be underlined.
241Pu/239Pu atom ratios
Laboratory D detected 241Pu in PB1 and BS1 (resp. *6
and *9 fg), whereas lab C reported a negative 241Pu/239Pu
isotopic ratio in PB1. At this time, lab A was not able to
measure 241Pu and did not report any result. Only lab D
detected a significant amount of 241Pu in QCS1-3 (*2 fg).
Although most of the relative expanded (k = 2) uncer-
tainties are higher than 100 %, results from laboratories are
not fully consistent. Laboratories C and E tend to report
negative values, which is probably due to overcorrection
from background or other bias effect. The result from lab B
for QCS1-1 ((1.0 ± 0.6) 9 10-3) is identified as an outlier
according to statistical tests.
242Pu/239Pu atom ratios
Laboratories A and E did not report any 242Pu/239Pu ratios
as these two laboratories use 242Pu as the isotope dilution
tracer. Laboratories C and D detected 242Pu in PB1
(*7 fg). Laboratory D is the only lab which reported
detection of significant 242Pu/239Pu ratios (respectively
(2.0 ± 0.3) 9 10-4, (1.1 ± 0.2) 9 10-3, and (4.5 ± 0.7)
9 10-3 for QCS1-1, QCS1-2 and QCS1-3, which corre-
spond to respective masses of 242Pu of *2 fg, *5 fg, and
*5 fg). Results from laboratories B and C show very large
relative expanded (k = 2) uncertainties and are often
negative. The result from lab C for QCS1-2 ((-4.9 ± 2.6)
9 10-3) is identified as an outlier according to statistical
tests.
Comparison of the relative standard uncertainties
Average relative standard uncertainties (RSU) obtained by
the laboratories for all U isotope ratio measurements
(234U/238U, 235U/238U and 236U/238U) and Pu isotope
measurements (240Pu/239Pu) for the 2 RRs are given,
respectively, in Figs. 3 and 4. Uncertainty budgets are not
compared for 241Pu/239Pu and 242Pu/239Pu measurements
as most of the results were not significant. Average RSUs
obtained by the laboratories for all U content and Pu
content measurements for the 2 RRs are given in Fig. 5.
Regarding the RSUs for U atom ratio measurements,
laboratories B and D, and to a lesser extent laboratory C,
obtained the lowest standard uncertainty budgets for isotope
ratio measurements, probably thanks to the excellent
reproducibility achievable with the multiple collector
instruments used by these laboratories. Lowest relative
CSUs were close to 0.1 %. Uncertainty budgets obtained by
labs A, C and E, for isotope ratio measurements are in the
same range. The poorest precisions are obtained by lab E,
Fig. 3 Average relative
standard uncertainty (RSU)
obtained by the laboratories for
all U isotope ratio
measurements for the 2 RRs.
Average RSUs for each
laboratory are given in the
following order: 234U/238U for
the RR #1, 234U/238U for the RR
#2, 235U/238U for the RR #1,235U/238U for the RR #2,236U/238U for the RR #1, and236U/238U for the RR #2. Each
value is the average of the RSU
calculated for the three
corresponding QCS
J Radioanal Nucl Chem (2013) 296:599–608 605
123
and, to a lesser extent, by lab A. This is probably due to the
use of single collector instruments by these two laborato-
ries. However, relative CSUs are globally very low taking
into account the low amounts of U in the samples: they
range from *0.4 to *9 % (average value of *3 %) for the234U/238U ratios, from *0.1 to *1.4 % (average value of
*0.45 %) for the 235U/238U ratios and from *0.4 to *8 %
(average value of *1.7 %) for the 236U/238U ratios.
RSUs for 240Pu/239Pu ratio measurements obtained by
the participating laboratories are rather homogeneous. For
the RR #1, they vary from *0.6 % (lab C) to *2 % (labs
A and D), with an average value of *1.3 %. RSUs of the
RR #2 are larger than the ones of the RR #1, because
amounts of Pu isotopes are significantly lower. They range
from *1.8 % (lab B) to *11 % (lab A), with an average
value of *5.6 %. Laboratories equipped with multi-col-
lector instruments obtain the lowest RSUs, provided the Pu
content is sufficient. Relative RSUs for total U content
determination are remarkably low for both RRs: they range
between *0.2 and *2 % with an average value of *1 %.
Higher and more variable RSUs are observed for total Pu
content measurements, especially for RR #2, for which
amounts of Pu isotopes are extremely low: average RSUs
for all labs are *1.5 % for RR #1 and *5 % for RR #2.
Discussion
Measurement of isotopic ratios of both U and Pu at low
concentrations is challenging for all laboratories, consid-
ering the extremely low amounts of both actinides in the
RR samples. In such conditions, concentrations of the
minor isotopes are in the fg to the pg range. However, in
general, the laboratories’ reported concentrations of U
and Pu in the RR samples were remarkably consistent.
Although this does not imply accuracy, taken as a whole, it
attests to very good agreement between the laboratories’
tracer (spike) calibrations.
It should be noted that some participating laboratories
measure elevated, non-natural 234U/238U, 235U/238U and236U/238U in PBs. In other aspects, all laboratories measure
elevated 234U/238U in blank cotton swipes relative to the
value for secular equilibrium. This observation can be
explained by the well-established fact of 234U/238U
enrichment in natural waters (both groundwater and river
water) that might be used for irrigation of cotton plants. All235U/238U measurements of the RR samples are very con-
cordant. The 236U/238U measurements of samples QCS1-2,
QCS1-3, QCS2-1 and QCS2-2 at approximately 5.1 9 10-5,
3.9 9 10-5, 3.4 9 10-4, and 10-5 are also concordant and
Fig. 4 Average relative standard uncertainty (RSU) obtained by the
laboratories for all 240Pu/239Pu isotope ratio measurements for the 2
RRs. Average RSUs for each laboratory are given in the following
order: 240Pu/239Pu for the RR #1 and 240Pu/239Pu for the RR #2. Each
value is the average of the RSU calculated for the three corresponding
QCSs
Fig. 5 Average relative
standard uncertainty (RSU)
obtained by the laboratories for
all U and Pu content
measurements for the 2 RRs.
Average RSUs for each
laboratory are given in the
following order: U content for
the RR #1, U content for the RR
#2, Pu content for the RR #1,
and Pu content for the RR #2.
Each value is the average of the
RSU calculated for the three
corresponding QCSs
606 J Radioanal Nucl Chem (2013) 296:599–608
123
all laboratories could resolve this small difference. For these
samples, this translates to a demonstrated ability to measure
approximately 1 pg of 236U in the presence of 40 ng of 238U.
Where the 240Pu was larger than the laboratories’ individual
detection limits, the 240Pu/239Pu ratios are also very con-
cordant, i.e., for samples QCS1-1 and QCS1-2. All labora-
tories are able to measure Pu isotopic composition at the
sub-pg level. So, globally, results of the participating lab-
oratories are of high quality and demonstrate the laborato-
ries’ ability to measure precisely and accurately U and Pu
isotope compositions in the ‘‘swipe samples’’.
General and particular recommendations were discussed
and adopted to improve the accuracy and precision of the
measurements. General recommendations mainly consists
in investigating some subtle effects that may, if not properly
corrected, lead to small bias in isotope ratio measurements.
For instance, laboratories exchanged and discussed their
procedures for dead time correction. It is also recommended
all labs should break down their uncertainty budgets and
explain their calculation methods to estimate their sources
of errors, as in [12]. More generally, laboratories should
consider whether their reported uncertainties may be either
underestimated (have all the uncertainties on the compo-
nents of the results been considered?) or overestimated (are
components counted twice or estimated to be too large?).
A comparison of uncertainty budget calculation between two
laboratories (A and B) each applying its own calculation
procedure and starting from exactly the same set of raw data,
shows that uncertainties can differ in some cases by a factor
of two between the two laboratories.
Several specific recommendations for each laboratory
were proposed. Some of them are related to mass spec-
trometry measurements, for instance checking that count
rates stay in the linearity range of the detector (lab A),
improving the measurement protocol for optimising iso-
tope ratio measurements (lab C) and for better correcting
bias effects (labs C and E). Other recommendations con-
cern the chemical preparation: reducing the U level in
blanks by reducing amounts of chromatographic resins (lab
A), and avoiding cross-contaminations or memory effects
in the laboratories (labs B, D). Lastly, laboratories C and E
obviously overestimated uncertainties and should review
and re-evaluate sources of uncertainties for U isotopic ratio
measurements.
Conclusions
Results obtained in the frame of the two RRs by the partic-
ipating laboratories are globally in very good agreement,
except for Pu analysis in the case of RR #2, which is
explained by Pu contamination during sample packaging.
All laboratories prove their ability to analyse sub-pg amounts
of Pu and ng amounts of U with acceptable precision and
accuracy. Improvements in reproducibility and capability to
detect small isotopic differences between samples with
multi-collector instruments are clearly demonstrated. How-
ever, to translate improvement in reproducibility to more
accurate measurements requires optimised procedures, cor-
rection of all biases and high precision isotopic standards.
Although the participating laboratories have state-of-the-art
practices and large experience in this field, a few discrep-
ancies are observed for specific results, affecting one labo-
ratory or the other. Some of the participating labs, that have
to manage routine safeguard samples which contain larger
amounts of nuclear materials, may encounter limited con-
taminations by non-natural U and/or Pu from other samples.
Possible improvement and specific recommendations
were proposed for each laboratory. Common needs were
also identified. The main concern of the participating lab-
oratories is calculation of the uncertainty budgets. Close
examination of the results gives the feeling that some
uncertainties may be overestimated (results perfectly match
the average values but have surprisingly large uncertain-
ties) or underestimated (results with very low uncertainty
are biased with regards to the average values). However,
there is no ‘‘on-the-shelf’’ procedure for uncertainty cal-
culation by mass spectrometry, but only general recom-
mendations and guidelines provided by documents like
Guide to the expression of Uncertainty in Measurement
(GUM). As participating laboratories considered that soft-
ware provided with the instruments by the manufacturers is
not satisfactory for uncertainty calculations, each labora-
tory developed individually its own home-made software.
All laboratories deem it necessary to check, and, if nec-
essary, to improve their uncertainty calculations. There is
also a strong need for very high purity tracers. For instance,
some of the participating laboratories do not have at their
disposal high purity 244Pu, which would allow all labora-
tories to measure 242Pu. Similarly, there is a need for
environmental reference materials for which both actinide
content and isotopic composition are certified.
Acknowledgments Many thanks to all the people who make this
collaboration possible and to the people who actively participate in
the collaboration, through meetings, administrative matters, and, of
course through technical work in the facilities. Special thanks to Ross
Williams and his colleagues from LLNL, who assumed the difficult
task to prepare and dispatch the QC samples.
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