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@ARTICLE{Boulyga:29421,
author = {Boulyga, S. F. and Testa, C. and Desideri, D. and Becker,
J. S.},
title = {{O}ptimisation and application of {ICP}-{MS} and
alpha-spectrometry for determination of isotopic ratios of
depleted uranium and plutonium in samples collected in
{K}osovo},
journal = {Journal of analytical atomic spectrometry},
volume = {16},
number = {11},
issn = {0267-9477},
address = {Cambridge},
publisher = {ChemSoc},
reportid = {PreJuSER-29421},
pages = {1283 - 1289},
year = {2001},
note = {Record converted from VDB: 12.11.2012},
abstract = {The determination of environmental contamination with
natural and artificial actinide isotopes and evaluation of
their source requires precise isotopic determination of
actinides, above all uranium and plutonium. This can be
achieved by alpha spectrometry or by inductively coupled
plasma mass spectrometry (ICP-MS) after chemical separation
of actinides. The performance of a sector-field ICP-MS
(ICP-SFMS) coupled to a low-flow micronebulizer with a
membrane desolvation unit, "Aridus'', was studied with
respect to precise isotopic measurements of uranium and
plutonium at the ultratrace level. The UH+/U+ formation rate
was about 3x10(-5) and a sensitivity for U-238 of up to
4x10(9) counts s(-1) ppm(-1) was achieved. The limit of
quantification (LOQ, 10s) for U-236 and Pu-239 using the
experimental arrangement described above was 0.6 pg l(-1) in
aqueous solution and 0.13 pg g(-1) in soil, respectively.
ICP-SFMS was used in comparison to alpha spectrometry to
measure the U and Pu concentrations and isotopic
compositions in two soil samples and in one penetrator
collected in Kosovo. ICP-MS permitted the determination of U
and Pu isotope ratios including the U-236 abundance and
Pu-240/Pu-239 ratio at ultratrace levels in soil samples of
up to 0.1 g. Depleted uranium (U-235/U-238= 0.00202
+/-0.00001) was determined in one penetrator and one soil
sample. Pu concentrations of (5.5 +/-0.1) x 10(-13) g g(-1)
and (4.4 +/-0.5) x 10(-13) g g(-1) (Pu-240/Pu-239=0.35
+/-0.10 and 0.27 +/-0.07, respectively) were found in both
soil samples from Kosovo. Besides plutonium, U-236
(3.1x10(-5) g g(-1)) and Am-241 (1.7x10(-12) g g(-1)) were
also detected in the penetrator sample, which indicates the
previous existence of neutron-related processes and points
to a possible presence of spent reactor uranium in
munitions. However, the most probable plutonium
contamination sources in analyzed soil samples from Kosovo
are mixed fallout including spent reactor fuel due to the
Chernobyl nuclear power plant accident in 1986 and plutonium
due to nuclear weapon tests. Additional plutonium
contamination could not be determined in the Kosovo soil
sample containing depleted uranium with a detection limit of
about 10(-13) g g(-1).},
keywords = {J (WoSType)},
cin = {ZCH},
ddc = {540},
cid = {I:(DE-Juel1)ZCH-20090406},
pnm = {Entwicklung analytischer Verfahren},
pid = {G:(DE-Juel1)FUEK118},
shelfmark = {Chemistry, Analytical / Spectroscopy},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000172191500007},
doi = {10.1039/b103178n},
url = {https://juser.fz-juelich.de/record/29421},
}