addressing attribution advances in nuclear forensics · using natural-lead corrected values works...
TRANSCRIPT
Joint Research Centre (JRC)ITU - Institute for Transuranium ElementsKarlsruhe - Germany
httpitujrceceuropaeuhttpwwwjrceceuropaeu
ESARDAINMM Safeguards Workshop 2011 1
Addressing Attribution Addressing Attribution minusminusAdvances in Nuclear ForensicsAdvances in Nuclear Forensics
Klaus Luumltzenkirchen Klaus Mayer Maria Wallenius Zsolt Varga
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 2
Overview
bull Objectives of nuclear material analysesndash Safeguardsndash Nuclear Forensics
bull Characteristic parameters and patternsndash R amp D on elemental fingerprints
bull Case study ndash Uranium raw material of
unknown origin (Rotterdam 2003)
bull Conclusions
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 3
Objectives of Nuclear Material Analysis
Verification of declared amounts of nuclear material
Safeguards
Verification of absence of undeclared nuclear material and activities
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 4
bull aims at providing clues on the history (production process date of production place of production intended use) of nuclear material
Objectives of Nuclear Material Analysis
bull provides information on nuclear material of immediate relevance to law enforcement
Nuclear Forensics
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 5
Nuclear Forensic Science - Signatures
Intr
oduc
edand wiped out
during material processing
Processes
Chemical Technical PhysicalLeaching Powder flow Neutron reactionSeparation Pelletising Radioactive decayCalcination
Source of signature
Material ProcessU deposit Accidental
PipingIntentional
Burnable poisons
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 6
Parameters ndash Patterns - Signatures
Complexity Multiple Signatures
Analytical and interpretational challengesOpportunities for signature development
Radioisotopes
Metallic Impurities
StableIsotopes
Non-metallic impurities
Structure
MajorElements
Morphology
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 7
NM isotopics (particles)Completeness
Microstructure
Macroscopic appearance
Chem composition
Organic impurities
Anionic impurities
( )Metallic impurities Process identification
Decay productsAge dating
Stable isotopesGeolocation
NM isotopics
NM concentrationCorrectness
Nuclear Forensics
Strengthened Sfg 540 type
Traditional Sfg153-typeParameterPurpose
Standard amp Advanced Parameters
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 8
U products
bull U ores
bull U ore concentrates (ADU AUC peroxideshellip)
bull U oxide powders
bull UF4 and UF6
bull U pellets
Study on 79 yellow cake samples
Aim Identify the impurities that are significant in relation to the source material (same type of material ndash different geographic origin)
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 9
httpwwwnucleonicanet
U-238 rarrPb-206
U-235 rarrPb-207
Th-232 rarrPb-208
Lead isotopesDecay products of U and Th
High U content rarr high variation of isotope ratios
The isotope composition depends on the history (eg weathering) and age of ore body
Can be easily used for provenance Can be easily used for provenance assessment of the oreassessment of the ore
Lead isotopics
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 10
Lead Isotopic Composition
0 2 4 6 8 10 12 14 16 18
Beverley-1 (AUS)
Beverley-2 (AUS)
Beverley-3 (AUS)
Beverley-4 (AUS)
Ranger (AUS)
Olympic Dam (AUS)
Key Lake (CAN)
Rabbit Lake (CAN)
Stanrock (CAN)
Roumlssing (NAM)
ESI Calgary (CAN)
Isotope Ratio
Pb-207Pb-208Pb-206Pb-208
Overlapping between mines
Relative high within-mine
variation
Applicability and limitationsLarge variation of isotope ratios between mines (radiogenic ratios amp dating)Certain ore types have low 206Pb207Pb ratios (sandstone phosphorite)Relatively high within-mine variationLess applicable for ldquopurerdquo UOCs
Pb isotopes
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 11
Date estimation of the ore on the basis of Pb-Pb method
Using natural-lead corrected valuesWorks better for more radiogenic-Pb
containing samples
1720-18221650+130-140175Ranger
600-1200 1160+680-1010565Roumlssing
5-30lt 640941El Mesquite
1300-13801130+210-740252Cluff Lake
2139 plusmn 1002140+140-150207Blind River
Literature value
Calculated deposit age
(Ma)
Natural 207Pb
content
UOC sample
Age dating using Pb isotopes
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 12
Sr-87Sr-86 Isotope Ratio in the Investigated Uranium Ore Concentrates
06900695070007050710071507200725073007350740
Beverle
y-1 (A
US)Bev
erley-2
(AUS)
Beverle
y-3 (A
US)Bev
erley-4
(AUS)
Ranger
(AUS)
Olympic
Dam (A
US)Key
Lake
(CAN)
Rabbit L
ake (C
AN)Stanro
ck (C
AN)Roumlss
ing (N
AM)
ESI Calg
ary (C
AN)
Sr-8
7Sr
-86
Isot
ope
Rat
io Lower within-mine variability
Overlap
Sr isotopes
Lower between-
mine variability
Precision methods like MC-ICPMS
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 13
Uranium minor isotopes
42E-05
47E-05
52E-05
57E-05
62E-05
67E-05
72E-05
77E-05
82E-05
87E-05
Nam
Ros
sing
Can
Blin
d R
iver
Aus
Oly
mpi
c D
am
Usa
Esi
Can
Esi
Aus
Ran
ger
Can
Eld
orad
o
Swe
Ran
stad
t
Usa
El M
esqu
ite
Aus
Mar
y Ka
thle
en
Usa
Ker
r McG
ee
Can
Sta
nroc
k
SA P
alab
ora
Bra
Nuc
lebr
as
Aus
Rum
Jun
gle
Usa
Hom
esta
ke
Can
Sta
nlei
gh
Aus
Que
ensl
and
Can
Key
Lak
e
Usa
Yan
kee
Yello
w
Can
Far
aday
Usa
Fal
ls C
ity
Can
Mad
awas
ka
Can
Clu
ff La
ke
Cze
Rep
ublic
Aus
Beve
rley
fresh
Aus
Beve
rley
old
Usa
Ana
kond
a
Aus
Rad
ium
Hill
Can
Rio
Alg
om
Can
Den
ison
Usa
Shi
rley
Basi
n
Can
El D
orad
o
Can
Ray
Roc
k
Aus
Sout
h Al
ligat
or
U-2
34U
-238
00E+00
50E-09
10E-08
15E-08
20E-08
25E-08
30E-08
U-2
36U
-238
bull 234U238U ratio varies in nature due to eg the preferential leaching of 234U after α-recoil
bull ldquoHighrdquo 236U abundance most probably a cross-contamination
natural
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 14
bull 143Nd144Nd ratio varies in nature due to the 147Sm 143Nd decaybull natural variation 0510 ndash 0513bull the value depends on the age of the mineral and mineral typebull robust indicator as Nd (like other REE) follows uranium (less prone to
weathering) small within-mine variation
0511 05112 05114 05116 05118 0512 05122 05124 05126
Beverley-1 (AUS)
Beverley-2 (AUS)
Straz (CZ)
Stanrock (CAN)
143Nd144Nd ratio
Neodymium isotope ratio
T12=1061011a
Nd-143 Nd-144 ratio
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 15
REE chemically similar with valence state mainly +3 REE pattern often remain unaltered during metamorphism thusproviding information on the premetamorphic history geologicalbackground and source of the rock The behavior of the valence-variable Ce (+4) and Eu (+2) is alsocharacteristic to the rock and it can be exploited to obtain information on the formation conditions
Rare earth elementsrsquo pattern
REE pattern is less prone to the process
can be used straightforwardly for the origin assessment
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 16
Rare-earth pattern of the investigated uranium ore concentrates
01
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
Cho
ndrit
e no
rmal
ized
con
cent
ratio
n
Beverley-1 (Sandstone)
Beverley-2 (Sandstone)
Beverley-3 (Sandstone)
Beverley-4 (Sandstone)
Ranger (Unconformity)
Olympic Dam (Breccia)
Key Lake (Unconformity)
Stanrock (Quartz-pebble congl)
Roumlssing (Intrusive)
ESI Calgary (Phosphorite)
Sedimentary-type
Quartz-pebbleIntrusive (Euanomaly)
Middle REE enrichment (unconformity-type)
REE patterns
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 17
bull geometry rarr 5 x 5 x 5 cm
bull weight about 24 kg
bull elemental uranium produced around 1943 plusmn 2 years (Haigerloch Germany)
Questions1 What is it 2 Origin of the material 3 etc
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 18
Intended use and origin
Nuclear forensics
bull elemental composition pure U metalunconventional applicationreactor
bull isotopic composition rarr natural U rarrD2O or graphite moderated reactor
bull Age via 234U 230Th590 plusmn 20 years (in 2003)
=gt Date of production second half of 1943
Geometry points at German originbull Open literature
Haigerloch reactor 1945
664 cubes x 24 kg = 15936 kg
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 19
ndash Where is the uranium coming from
Date of Production second half of 1943
Authentic cube
Belgian Congo or Joachimsthal (Czech Republic)
rare earth element pattern
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 20
Samples measured
ndash Haigerloch (ldquoHeisenbergrdquo) uranium cube
ndash Heidelberg (ldquoWirtzrdquo) uranium plates
ndash Yellow cake from Otto Hahnrsquos laboratory in Berlin
ndash For comparisonJoachimsthal uranium ore (bdquohistoricldquo sample)Congo uranium ore
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 21
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
REF
REF
REF
REF
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 22
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
REF
REF
REF
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 23
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
REF
REF
Congo UOC
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 24
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
Ore fromJoachimstalREF
Congo UOC
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 25
Inorganic FT-IR measurement of UOC samplesMeasurement in pellet form using KBrRapid identification of compound (oxide peroxide ADU AUC partially
calcined samples)Detection of certain process-related impurities (sulphate carbonate
nitrate)
Uranium composition in UOCs
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 26
Nitrate (1380 cm-1)Impurity from eluate or back extractant
Sulphate (1130 cm-1)Residual from H2SO4 eluate or back extractant
Uranium composition in UOCs
U-O vibration
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 27
Anion residuals in UOCrsquos
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
20
40
60
80
100
120
140
160
180
200
uScm
Cond
fluor
ide
102
2
2 chlo
ride
02
19
4 5 6 7 nitr
ate
003
6
sulp
hate
479
129
Canada ESI
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
17
18
19
20
21
22
23
24
25
26
uScm
Cond
fluor
ide
036
7
2 3
chlo
ride
55
32
5 brom
ide
-00
26
nitr
ate
012
7
sulp
hate
20
767
9
Australia Radium Hill
Different type of uranium deposits
Different processes for U extraction
Different mineral acids are used
Acid remainings
fluor
ide
chlo
ride
brom
ide
nitr
ate
sulp
hate
fluor
ide
chlo
ride
nitr
ate
sulp
hate
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 28
NO3SO4
0
01
02
03
04
05
06
07
08
09
1
Sout
h Al
ligat
or
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y Ka
thle
en
ESI U
SA
ESI C
anad
a
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Stan
rock
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lake
Mad
awas
ka
Mac
assa
Nor
th S
pan
Milli
ken
Lake
Eldo
rado
Stan
leig
h
FCl
0
05
1
15
2
25
3
35
4
45
5
Sou
th A
lliga
tor
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y K
athl
een
ES
I US
A
ES
I Can
ada
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Sta
nroc
k
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lak
e
Mad
awas
ka
Mac
assa
Nor
th S
pan
Mill
iken
Lak
e
Eld
orad
o
Sta
nlei
gh
Anion ratios
Phosphorite oresQuartz-pebble conglomerate and vein deposits
Nitric acid leaching rArr
Indicator of the processApatite mineral Ca5(PO4)3(FClOH)
rArr Indicator of the deposit type
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 29
Sandstone basal channel Quartz-pebble
conglomerate
Phosphorite
Black shale
Statistical evaluation of UOC data
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 30
U productsbull U ores
bull U ore concentrates
bull U oxide powders
bull UF4 and UF6
bull U pellets
Next step - Vertical study
Aim Identify the impurities that are acquired from or lost in the process What is the effect on the impurities from the source material
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 31
Uranium oreconcentrates
Process stagesamples and reagents
UO3
Next step - Vertical study
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 32
Case study
Backgroundbull uranium raw material of unknown
originbull 2003 Rotterdam (NL)bull Brownish yellow powder ~3 kgbull Found on a shipload from Jordan
Measurements performed at ITUbull NDA analysisbull Isotope ratio measurements (U Sr
Pb)bull Infrared analysisbull Impurity analysisbull REE pattern determination
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 33
Case study
Vibrational Spectrum (Infrared Spectrometry)
bull Compound is AUC xH2Obull Sulfate impurity (from dissolution of starting material)
bullNitrate impurity (from solvent extractionpurification)
Mass Spectrometry
bull Natural uranium isotopic compositionbull Natural lead isotopic composition
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 34
Case study
Sr Isotope Ratio
Low value typical for phosphorites (eg North Africa Middle East UShellip)
070757 plusmn 000011
070814 plusmn 000004
071092 plusmn 000006
071416 plusmn 000011
071985 plusmn 000029
072336 plusmn 000004
073434 plusmn 000012
070785 plusmn 000004
071775 plusmn 000003
067 068 069 070 071 072 073 074 075 076 077 078 079 080
Beverley
Calgary
Key Lake
Olympic Dam
Ranger
Ranstad
Stanrock
Mulberry
Fund-26
87Sr86Sr Isotope RatioSr-87 Sr-86 isotope ratio
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 35
Case study
Age dating based on 234U230Th
Age dating based on 232Th228Th
Last chemical separation 1988 plusmn 5 yndash Applicable to samples with incomplete Th separationndash Complementary to 234U230Th method
Last chemical separation 1893 plusmn 17 y
ndash Measured value shows significant positive biasndash Reason incomplete separation of 230Th from the
parent 234U nuclide(ldquoclock is not set to zerordquo)
ndash Residual 230Th cannot be calculated or corrected for
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 36
Case study ndash Find-26
bull 234U abundance suggests low temperature redox deposit value agrees with data reported by IAEA for UOC from Al Qaim (Iraq)
bull Impurities high P contentsimilar metallic impurities to Iraqi phosphate deposits
bull Pb isotopes natural young deposit low U content in orebull REE pattern flat no Eu or Ce anomaly rarr previously found
in certain sandstone-type and reworked phosphorite
Data inherent to the material corroborate information from external sources
Identification of origin based onSingle sampleMultiple parameters
Identification of origin based onSingle sampleMultiple parameters
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 37
Comparison of relative efforts ndash yellow cake
(5)(5)SIMSU particle analysis(5)Evaluation and Report
MC-ICP-MSMC-ICP-MSICP-MSIR-Spectroscopy RamanIon ChromatographyICP-MS IDMS
Electron Microscopy EDX WDXOptical MicroscopyICP-MSTIMSTitration IDMS
Technique
1853Total
15Nd Isotopes15Sr Isotopes3Rare Earth Elemental pattern1Molecular structure
15Anionic impurities3Age dating
3Micromorphology1Visual inspection macroscopic11Impurities11Isotopic Composition11Element Assay
ForensicsSafeguardsAnalysisParameter
Note rounded figures based on a full cost evaluation figures in brackets are not included in the Total
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 38
Conclusions
Wealth of information inherent to nuclear materialDecrypting the information requires sophisticated methodology subject matter expertise and reference dataSignificant effort (resources and time) needed for comprehensive analysis and data interpretationNuclear forensics methodology may open new avenuesin different areasApplication of investigative techniques in Safeguards has to be evaluated
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 2
Overview
bull Objectives of nuclear material analysesndash Safeguardsndash Nuclear Forensics
bull Characteristic parameters and patternsndash R amp D on elemental fingerprints
bull Case study ndash Uranium raw material of
unknown origin (Rotterdam 2003)
bull Conclusions
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 3
Objectives of Nuclear Material Analysis
Verification of declared amounts of nuclear material
Safeguards
Verification of absence of undeclared nuclear material and activities
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 4
bull aims at providing clues on the history (production process date of production place of production intended use) of nuclear material
Objectives of Nuclear Material Analysis
bull provides information on nuclear material of immediate relevance to law enforcement
Nuclear Forensics
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 5
Nuclear Forensic Science - Signatures
Intr
oduc
edand wiped out
during material processing
Processes
Chemical Technical PhysicalLeaching Powder flow Neutron reactionSeparation Pelletising Radioactive decayCalcination
Source of signature
Material ProcessU deposit Accidental
PipingIntentional
Burnable poisons
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 6
Parameters ndash Patterns - Signatures
Complexity Multiple Signatures
Analytical and interpretational challengesOpportunities for signature development
Radioisotopes
Metallic Impurities
StableIsotopes
Non-metallic impurities
Structure
MajorElements
Morphology
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 7
NM isotopics (particles)Completeness
Microstructure
Macroscopic appearance
Chem composition
Organic impurities
Anionic impurities
( )Metallic impurities Process identification
Decay productsAge dating
Stable isotopesGeolocation
NM isotopics
NM concentrationCorrectness
Nuclear Forensics
Strengthened Sfg 540 type
Traditional Sfg153-typeParameterPurpose
Standard amp Advanced Parameters
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 8
U products
bull U ores
bull U ore concentrates (ADU AUC peroxideshellip)
bull U oxide powders
bull UF4 and UF6
bull U pellets
Study on 79 yellow cake samples
Aim Identify the impurities that are significant in relation to the source material (same type of material ndash different geographic origin)
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 9
httpwwwnucleonicanet
U-238 rarrPb-206
U-235 rarrPb-207
Th-232 rarrPb-208
Lead isotopesDecay products of U and Th
High U content rarr high variation of isotope ratios
The isotope composition depends on the history (eg weathering) and age of ore body
Can be easily used for provenance Can be easily used for provenance assessment of the oreassessment of the ore
Lead isotopics
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 10
Lead Isotopic Composition
0 2 4 6 8 10 12 14 16 18
Beverley-1 (AUS)
Beverley-2 (AUS)
Beverley-3 (AUS)
Beverley-4 (AUS)
Ranger (AUS)
Olympic Dam (AUS)
Key Lake (CAN)
Rabbit Lake (CAN)
Stanrock (CAN)
Roumlssing (NAM)
ESI Calgary (CAN)
Isotope Ratio
Pb-207Pb-208Pb-206Pb-208
Overlapping between mines
Relative high within-mine
variation
Applicability and limitationsLarge variation of isotope ratios between mines (radiogenic ratios amp dating)Certain ore types have low 206Pb207Pb ratios (sandstone phosphorite)Relatively high within-mine variationLess applicable for ldquopurerdquo UOCs
Pb isotopes
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 11
Date estimation of the ore on the basis of Pb-Pb method
Using natural-lead corrected valuesWorks better for more radiogenic-Pb
containing samples
1720-18221650+130-140175Ranger
600-1200 1160+680-1010565Roumlssing
5-30lt 640941El Mesquite
1300-13801130+210-740252Cluff Lake
2139 plusmn 1002140+140-150207Blind River
Literature value
Calculated deposit age
(Ma)
Natural 207Pb
content
UOC sample
Age dating using Pb isotopes
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 12
Sr-87Sr-86 Isotope Ratio in the Investigated Uranium Ore Concentrates
06900695070007050710071507200725073007350740
Beverle
y-1 (A
US)Bev
erley-2
(AUS)
Beverle
y-3 (A
US)Bev
erley-4
(AUS)
Ranger
(AUS)
Olympic
Dam (A
US)Key
Lake
(CAN)
Rabbit L
ake (C
AN)Stanro
ck (C
AN)Roumlss
ing (N
AM)
ESI Calg
ary (C
AN)
Sr-8
7Sr
-86
Isot
ope
Rat
io Lower within-mine variability
Overlap
Sr isotopes
Lower between-
mine variability
Precision methods like MC-ICPMS
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 13
Uranium minor isotopes
42E-05
47E-05
52E-05
57E-05
62E-05
67E-05
72E-05
77E-05
82E-05
87E-05
Nam
Ros
sing
Can
Blin
d R
iver
Aus
Oly
mpi
c D
am
Usa
Esi
Can
Esi
Aus
Ran
ger
Can
Eld
orad
o
Swe
Ran
stad
t
Usa
El M
esqu
ite
Aus
Mar
y Ka
thle
en
Usa
Ker
r McG
ee
Can
Sta
nroc
k
SA P
alab
ora
Bra
Nuc
lebr
as
Aus
Rum
Jun
gle
Usa
Hom
esta
ke
Can
Sta
nlei
gh
Aus
Que
ensl
and
Can
Key
Lak
e
Usa
Yan
kee
Yello
w
Can
Far
aday
Usa
Fal
ls C
ity
Can
Mad
awas
ka
Can
Clu
ff La
ke
Cze
Rep
ublic
Aus
Beve
rley
fresh
Aus
Beve
rley
old
Usa
Ana
kond
a
Aus
Rad
ium
Hill
Can
Rio
Alg
om
Can
Den
ison
Usa
Shi
rley
Basi
n
Can
El D
orad
o
Can
Ray
Roc
k
Aus
Sout
h Al
ligat
or
U-2
34U
-238
00E+00
50E-09
10E-08
15E-08
20E-08
25E-08
30E-08
U-2
36U
-238
bull 234U238U ratio varies in nature due to eg the preferential leaching of 234U after α-recoil
bull ldquoHighrdquo 236U abundance most probably a cross-contamination
natural
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 14
bull 143Nd144Nd ratio varies in nature due to the 147Sm 143Nd decaybull natural variation 0510 ndash 0513bull the value depends on the age of the mineral and mineral typebull robust indicator as Nd (like other REE) follows uranium (less prone to
weathering) small within-mine variation
0511 05112 05114 05116 05118 0512 05122 05124 05126
Beverley-1 (AUS)
Beverley-2 (AUS)
Straz (CZ)
Stanrock (CAN)
143Nd144Nd ratio
Neodymium isotope ratio
T12=1061011a
Nd-143 Nd-144 ratio
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 15
REE chemically similar with valence state mainly +3 REE pattern often remain unaltered during metamorphism thusproviding information on the premetamorphic history geologicalbackground and source of the rock The behavior of the valence-variable Ce (+4) and Eu (+2) is alsocharacteristic to the rock and it can be exploited to obtain information on the formation conditions
Rare earth elementsrsquo pattern
REE pattern is less prone to the process
can be used straightforwardly for the origin assessment
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 16
Rare-earth pattern of the investigated uranium ore concentrates
01
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
Cho
ndrit
e no
rmal
ized
con
cent
ratio
n
Beverley-1 (Sandstone)
Beverley-2 (Sandstone)
Beverley-3 (Sandstone)
Beverley-4 (Sandstone)
Ranger (Unconformity)
Olympic Dam (Breccia)
Key Lake (Unconformity)
Stanrock (Quartz-pebble congl)
Roumlssing (Intrusive)
ESI Calgary (Phosphorite)
Sedimentary-type
Quartz-pebbleIntrusive (Euanomaly)
Middle REE enrichment (unconformity-type)
REE patterns
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 17
bull geometry rarr 5 x 5 x 5 cm
bull weight about 24 kg
bull elemental uranium produced around 1943 plusmn 2 years (Haigerloch Germany)
Questions1 What is it 2 Origin of the material 3 etc
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 18
Intended use and origin
Nuclear forensics
bull elemental composition pure U metalunconventional applicationreactor
bull isotopic composition rarr natural U rarrD2O or graphite moderated reactor
bull Age via 234U 230Th590 plusmn 20 years (in 2003)
=gt Date of production second half of 1943
Geometry points at German originbull Open literature
Haigerloch reactor 1945
664 cubes x 24 kg = 15936 kg
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 19
ndash Where is the uranium coming from
Date of Production second half of 1943
Authentic cube
Belgian Congo or Joachimsthal (Czech Republic)
rare earth element pattern
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 20
Samples measured
ndash Haigerloch (ldquoHeisenbergrdquo) uranium cube
ndash Heidelberg (ldquoWirtzrdquo) uranium plates
ndash Yellow cake from Otto Hahnrsquos laboratory in Berlin
ndash For comparisonJoachimsthal uranium ore (bdquohistoricldquo sample)Congo uranium ore
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 21
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
REF
REF
REF
REF
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 22
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
REF
REF
REF
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 23
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
REF
REF
Congo UOC
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 24
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
Ore fromJoachimstalREF
Congo UOC
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 25
Inorganic FT-IR measurement of UOC samplesMeasurement in pellet form using KBrRapid identification of compound (oxide peroxide ADU AUC partially
calcined samples)Detection of certain process-related impurities (sulphate carbonate
nitrate)
Uranium composition in UOCs
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 26
Nitrate (1380 cm-1)Impurity from eluate or back extractant
Sulphate (1130 cm-1)Residual from H2SO4 eluate or back extractant
Uranium composition in UOCs
U-O vibration
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 27
Anion residuals in UOCrsquos
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
20
40
60
80
100
120
140
160
180
200
uScm
Cond
fluor
ide
102
2
2 chlo
ride
02
19
4 5 6 7 nitr
ate
003
6
sulp
hate
479
129
Canada ESI
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
17
18
19
20
21
22
23
24
25
26
uScm
Cond
fluor
ide
036
7
2 3
chlo
ride
55
32
5 brom
ide
-00
26
nitr
ate
012
7
sulp
hate
20
767
9
Australia Radium Hill
Different type of uranium deposits
Different processes for U extraction
Different mineral acids are used
Acid remainings
fluor
ide
chlo
ride
brom
ide
nitr
ate
sulp
hate
fluor
ide
chlo
ride
nitr
ate
sulp
hate
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 28
NO3SO4
0
01
02
03
04
05
06
07
08
09
1
Sout
h Al
ligat
or
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y Ka
thle
en
ESI U
SA
ESI C
anad
a
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Stan
rock
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lake
Mad
awas
ka
Mac
assa
Nor
th S
pan
Milli
ken
Lake
Eldo
rado
Stan
leig
h
FCl
0
05
1
15
2
25
3
35
4
45
5
Sou
th A
lliga
tor
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y K
athl
een
ES
I US
A
ES
I Can
ada
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Sta
nroc
k
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lak
e
Mad
awas
ka
Mac
assa
Nor
th S
pan
Mill
iken
Lak
e
Eld
orad
o
Sta
nlei
gh
Anion ratios
Phosphorite oresQuartz-pebble conglomerate and vein deposits
Nitric acid leaching rArr
Indicator of the processApatite mineral Ca5(PO4)3(FClOH)
rArr Indicator of the deposit type
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 29
Sandstone basal channel Quartz-pebble
conglomerate
Phosphorite
Black shale
Statistical evaluation of UOC data
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 30
U productsbull U ores
bull U ore concentrates
bull U oxide powders
bull UF4 and UF6
bull U pellets
Next step - Vertical study
Aim Identify the impurities that are acquired from or lost in the process What is the effect on the impurities from the source material
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 31
Uranium oreconcentrates
Process stagesamples and reagents
UO3
Next step - Vertical study
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 32
Case study
Backgroundbull uranium raw material of unknown
originbull 2003 Rotterdam (NL)bull Brownish yellow powder ~3 kgbull Found on a shipload from Jordan
Measurements performed at ITUbull NDA analysisbull Isotope ratio measurements (U Sr
Pb)bull Infrared analysisbull Impurity analysisbull REE pattern determination
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 33
Case study
Vibrational Spectrum (Infrared Spectrometry)
bull Compound is AUC xH2Obull Sulfate impurity (from dissolution of starting material)
bullNitrate impurity (from solvent extractionpurification)
Mass Spectrometry
bull Natural uranium isotopic compositionbull Natural lead isotopic composition
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 34
Case study
Sr Isotope Ratio
Low value typical for phosphorites (eg North Africa Middle East UShellip)
070757 plusmn 000011
070814 plusmn 000004
071092 plusmn 000006
071416 plusmn 000011
071985 plusmn 000029
072336 plusmn 000004
073434 plusmn 000012
070785 plusmn 000004
071775 plusmn 000003
067 068 069 070 071 072 073 074 075 076 077 078 079 080
Beverley
Calgary
Key Lake
Olympic Dam
Ranger
Ranstad
Stanrock
Mulberry
Fund-26
87Sr86Sr Isotope RatioSr-87 Sr-86 isotope ratio
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 35
Case study
Age dating based on 234U230Th
Age dating based on 232Th228Th
Last chemical separation 1988 plusmn 5 yndash Applicable to samples with incomplete Th separationndash Complementary to 234U230Th method
Last chemical separation 1893 plusmn 17 y
ndash Measured value shows significant positive biasndash Reason incomplete separation of 230Th from the
parent 234U nuclide(ldquoclock is not set to zerordquo)
ndash Residual 230Th cannot be calculated or corrected for
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 36
Case study ndash Find-26
bull 234U abundance suggests low temperature redox deposit value agrees with data reported by IAEA for UOC from Al Qaim (Iraq)
bull Impurities high P contentsimilar metallic impurities to Iraqi phosphate deposits
bull Pb isotopes natural young deposit low U content in orebull REE pattern flat no Eu or Ce anomaly rarr previously found
in certain sandstone-type and reworked phosphorite
Data inherent to the material corroborate information from external sources
Identification of origin based onSingle sampleMultiple parameters
Identification of origin based onSingle sampleMultiple parameters
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 37
Comparison of relative efforts ndash yellow cake
(5)(5)SIMSU particle analysis(5)Evaluation and Report
MC-ICP-MSMC-ICP-MSICP-MSIR-Spectroscopy RamanIon ChromatographyICP-MS IDMS
Electron Microscopy EDX WDXOptical MicroscopyICP-MSTIMSTitration IDMS
Technique
1853Total
15Nd Isotopes15Sr Isotopes3Rare Earth Elemental pattern1Molecular structure
15Anionic impurities3Age dating
3Micromorphology1Visual inspection macroscopic11Impurities11Isotopic Composition11Element Assay
ForensicsSafeguardsAnalysisParameter
Note rounded figures based on a full cost evaluation figures in brackets are not included in the Total
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 38
Conclusions
Wealth of information inherent to nuclear materialDecrypting the information requires sophisticated methodology subject matter expertise and reference dataSignificant effort (resources and time) needed for comprehensive analysis and data interpretationNuclear forensics methodology may open new avenuesin different areasApplication of investigative techniques in Safeguards has to be evaluated
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 3
Objectives of Nuclear Material Analysis
Verification of declared amounts of nuclear material
Safeguards
Verification of absence of undeclared nuclear material and activities
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 4
bull aims at providing clues on the history (production process date of production place of production intended use) of nuclear material
Objectives of Nuclear Material Analysis
bull provides information on nuclear material of immediate relevance to law enforcement
Nuclear Forensics
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 5
Nuclear Forensic Science - Signatures
Intr
oduc
edand wiped out
during material processing
Processes
Chemical Technical PhysicalLeaching Powder flow Neutron reactionSeparation Pelletising Radioactive decayCalcination
Source of signature
Material ProcessU deposit Accidental
PipingIntentional
Burnable poisons
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 6
Parameters ndash Patterns - Signatures
Complexity Multiple Signatures
Analytical and interpretational challengesOpportunities for signature development
Radioisotopes
Metallic Impurities
StableIsotopes
Non-metallic impurities
Structure
MajorElements
Morphology
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 7
NM isotopics (particles)Completeness
Microstructure
Macroscopic appearance
Chem composition
Organic impurities
Anionic impurities
( )Metallic impurities Process identification
Decay productsAge dating
Stable isotopesGeolocation
NM isotopics
NM concentrationCorrectness
Nuclear Forensics
Strengthened Sfg 540 type
Traditional Sfg153-typeParameterPurpose
Standard amp Advanced Parameters
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 8
U products
bull U ores
bull U ore concentrates (ADU AUC peroxideshellip)
bull U oxide powders
bull UF4 and UF6
bull U pellets
Study on 79 yellow cake samples
Aim Identify the impurities that are significant in relation to the source material (same type of material ndash different geographic origin)
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 9
httpwwwnucleonicanet
U-238 rarrPb-206
U-235 rarrPb-207
Th-232 rarrPb-208
Lead isotopesDecay products of U and Th
High U content rarr high variation of isotope ratios
The isotope composition depends on the history (eg weathering) and age of ore body
Can be easily used for provenance Can be easily used for provenance assessment of the oreassessment of the ore
Lead isotopics
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 10
Lead Isotopic Composition
0 2 4 6 8 10 12 14 16 18
Beverley-1 (AUS)
Beverley-2 (AUS)
Beverley-3 (AUS)
Beverley-4 (AUS)
Ranger (AUS)
Olympic Dam (AUS)
Key Lake (CAN)
Rabbit Lake (CAN)
Stanrock (CAN)
Roumlssing (NAM)
ESI Calgary (CAN)
Isotope Ratio
Pb-207Pb-208Pb-206Pb-208
Overlapping between mines
Relative high within-mine
variation
Applicability and limitationsLarge variation of isotope ratios between mines (radiogenic ratios amp dating)Certain ore types have low 206Pb207Pb ratios (sandstone phosphorite)Relatively high within-mine variationLess applicable for ldquopurerdquo UOCs
Pb isotopes
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 11
Date estimation of the ore on the basis of Pb-Pb method
Using natural-lead corrected valuesWorks better for more radiogenic-Pb
containing samples
1720-18221650+130-140175Ranger
600-1200 1160+680-1010565Roumlssing
5-30lt 640941El Mesquite
1300-13801130+210-740252Cluff Lake
2139 plusmn 1002140+140-150207Blind River
Literature value
Calculated deposit age
(Ma)
Natural 207Pb
content
UOC sample
Age dating using Pb isotopes
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 12
Sr-87Sr-86 Isotope Ratio in the Investigated Uranium Ore Concentrates
06900695070007050710071507200725073007350740
Beverle
y-1 (A
US)Bev
erley-2
(AUS)
Beverle
y-3 (A
US)Bev
erley-4
(AUS)
Ranger
(AUS)
Olympic
Dam (A
US)Key
Lake
(CAN)
Rabbit L
ake (C
AN)Stanro
ck (C
AN)Roumlss
ing (N
AM)
ESI Calg
ary (C
AN)
Sr-8
7Sr
-86
Isot
ope
Rat
io Lower within-mine variability
Overlap
Sr isotopes
Lower between-
mine variability
Precision methods like MC-ICPMS
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 13
Uranium minor isotopes
42E-05
47E-05
52E-05
57E-05
62E-05
67E-05
72E-05
77E-05
82E-05
87E-05
Nam
Ros
sing
Can
Blin
d R
iver
Aus
Oly
mpi
c D
am
Usa
Esi
Can
Esi
Aus
Ran
ger
Can
Eld
orad
o
Swe
Ran
stad
t
Usa
El M
esqu
ite
Aus
Mar
y Ka
thle
en
Usa
Ker
r McG
ee
Can
Sta
nroc
k
SA P
alab
ora
Bra
Nuc
lebr
as
Aus
Rum
Jun
gle
Usa
Hom
esta
ke
Can
Sta
nlei
gh
Aus
Que
ensl
and
Can
Key
Lak
e
Usa
Yan
kee
Yello
w
Can
Far
aday
Usa
Fal
ls C
ity
Can
Mad
awas
ka
Can
Clu
ff La
ke
Cze
Rep
ublic
Aus
Beve
rley
fresh
Aus
Beve
rley
old
Usa
Ana
kond
a
Aus
Rad
ium
Hill
Can
Rio
Alg
om
Can
Den
ison
Usa
Shi
rley
Basi
n
Can
El D
orad
o
Can
Ray
Roc
k
Aus
Sout
h Al
ligat
or
U-2
34U
-238
00E+00
50E-09
10E-08
15E-08
20E-08
25E-08
30E-08
U-2
36U
-238
bull 234U238U ratio varies in nature due to eg the preferential leaching of 234U after α-recoil
bull ldquoHighrdquo 236U abundance most probably a cross-contamination
natural
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 14
bull 143Nd144Nd ratio varies in nature due to the 147Sm 143Nd decaybull natural variation 0510 ndash 0513bull the value depends on the age of the mineral and mineral typebull robust indicator as Nd (like other REE) follows uranium (less prone to
weathering) small within-mine variation
0511 05112 05114 05116 05118 0512 05122 05124 05126
Beverley-1 (AUS)
Beverley-2 (AUS)
Straz (CZ)
Stanrock (CAN)
143Nd144Nd ratio
Neodymium isotope ratio
T12=1061011a
Nd-143 Nd-144 ratio
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 15
REE chemically similar with valence state mainly +3 REE pattern often remain unaltered during metamorphism thusproviding information on the premetamorphic history geologicalbackground and source of the rock The behavior of the valence-variable Ce (+4) and Eu (+2) is alsocharacteristic to the rock and it can be exploited to obtain information on the formation conditions
Rare earth elementsrsquo pattern
REE pattern is less prone to the process
can be used straightforwardly for the origin assessment
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 16
Rare-earth pattern of the investigated uranium ore concentrates
01
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
Cho
ndrit
e no
rmal
ized
con
cent
ratio
n
Beverley-1 (Sandstone)
Beverley-2 (Sandstone)
Beverley-3 (Sandstone)
Beverley-4 (Sandstone)
Ranger (Unconformity)
Olympic Dam (Breccia)
Key Lake (Unconformity)
Stanrock (Quartz-pebble congl)
Roumlssing (Intrusive)
ESI Calgary (Phosphorite)
Sedimentary-type
Quartz-pebbleIntrusive (Euanomaly)
Middle REE enrichment (unconformity-type)
REE patterns
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 17
bull geometry rarr 5 x 5 x 5 cm
bull weight about 24 kg
bull elemental uranium produced around 1943 plusmn 2 years (Haigerloch Germany)
Questions1 What is it 2 Origin of the material 3 etc
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 18
Intended use and origin
Nuclear forensics
bull elemental composition pure U metalunconventional applicationreactor
bull isotopic composition rarr natural U rarrD2O or graphite moderated reactor
bull Age via 234U 230Th590 plusmn 20 years (in 2003)
=gt Date of production second half of 1943
Geometry points at German originbull Open literature
Haigerloch reactor 1945
664 cubes x 24 kg = 15936 kg
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 19
ndash Where is the uranium coming from
Date of Production second half of 1943
Authentic cube
Belgian Congo or Joachimsthal (Czech Republic)
rare earth element pattern
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 20
Samples measured
ndash Haigerloch (ldquoHeisenbergrdquo) uranium cube
ndash Heidelberg (ldquoWirtzrdquo) uranium plates
ndash Yellow cake from Otto Hahnrsquos laboratory in Berlin
ndash For comparisonJoachimsthal uranium ore (bdquohistoricldquo sample)Congo uranium ore
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 21
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
REF
REF
REF
REF
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 22
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
REF
REF
REF
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 23
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
REF
REF
Congo UOC
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 24
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
Ore fromJoachimstalREF
Congo UOC
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 25
Inorganic FT-IR measurement of UOC samplesMeasurement in pellet form using KBrRapid identification of compound (oxide peroxide ADU AUC partially
calcined samples)Detection of certain process-related impurities (sulphate carbonate
nitrate)
Uranium composition in UOCs
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 26
Nitrate (1380 cm-1)Impurity from eluate or back extractant
Sulphate (1130 cm-1)Residual from H2SO4 eluate or back extractant
Uranium composition in UOCs
U-O vibration
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 27
Anion residuals in UOCrsquos
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
20
40
60
80
100
120
140
160
180
200
uScm
Cond
fluor
ide
102
2
2 chlo
ride
02
19
4 5 6 7 nitr
ate
003
6
sulp
hate
479
129
Canada ESI
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
17
18
19
20
21
22
23
24
25
26
uScm
Cond
fluor
ide
036
7
2 3
chlo
ride
55
32
5 brom
ide
-00
26
nitr
ate
012
7
sulp
hate
20
767
9
Australia Radium Hill
Different type of uranium deposits
Different processes for U extraction
Different mineral acids are used
Acid remainings
fluor
ide
chlo
ride
brom
ide
nitr
ate
sulp
hate
fluor
ide
chlo
ride
nitr
ate
sulp
hate
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 28
NO3SO4
0
01
02
03
04
05
06
07
08
09
1
Sout
h Al
ligat
or
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y Ka
thle
en
ESI U
SA
ESI C
anad
a
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Stan
rock
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lake
Mad
awas
ka
Mac
assa
Nor
th S
pan
Milli
ken
Lake
Eldo
rado
Stan
leig
h
FCl
0
05
1
15
2
25
3
35
4
45
5
Sou
th A
lliga
tor
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y K
athl
een
ES
I US
A
ES
I Can
ada
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Sta
nroc
k
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lak
e
Mad
awas
ka
Mac
assa
Nor
th S
pan
Mill
iken
Lak
e
Eld
orad
o
Sta
nlei
gh
Anion ratios
Phosphorite oresQuartz-pebble conglomerate and vein deposits
Nitric acid leaching rArr
Indicator of the processApatite mineral Ca5(PO4)3(FClOH)
rArr Indicator of the deposit type
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 29
Sandstone basal channel Quartz-pebble
conglomerate
Phosphorite
Black shale
Statistical evaluation of UOC data
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 30
U productsbull U ores
bull U ore concentrates
bull U oxide powders
bull UF4 and UF6
bull U pellets
Next step - Vertical study
Aim Identify the impurities that are acquired from or lost in the process What is the effect on the impurities from the source material
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 31
Uranium oreconcentrates
Process stagesamples and reagents
UO3
Next step - Vertical study
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 32
Case study
Backgroundbull uranium raw material of unknown
originbull 2003 Rotterdam (NL)bull Brownish yellow powder ~3 kgbull Found on a shipload from Jordan
Measurements performed at ITUbull NDA analysisbull Isotope ratio measurements (U Sr
Pb)bull Infrared analysisbull Impurity analysisbull REE pattern determination
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 33
Case study
Vibrational Spectrum (Infrared Spectrometry)
bull Compound is AUC xH2Obull Sulfate impurity (from dissolution of starting material)
bullNitrate impurity (from solvent extractionpurification)
Mass Spectrometry
bull Natural uranium isotopic compositionbull Natural lead isotopic composition
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 34
Case study
Sr Isotope Ratio
Low value typical for phosphorites (eg North Africa Middle East UShellip)
070757 plusmn 000011
070814 plusmn 000004
071092 plusmn 000006
071416 plusmn 000011
071985 plusmn 000029
072336 plusmn 000004
073434 plusmn 000012
070785 plusmn 000004
071775 plusmn 000003
067 068 069 070 071 072 073 074 075 076 077 078 079 080
Beverley
Calgary
Key Lake
Olympic Dam
Ranger
Ranstad
Stanrock
Mulberry
Fund-26
87Sr86Sr Isotope RatioSr-87 Sr-86 isotope ratio
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 35
Case study
Age dating based on 234U230Th
Age dating based on 232Th228Th
Last chemical separation 1988 plusmn 5 yndash Applicable to samples with incomplete Th separationndash Complementary to 234U230Th method
Last chemical separation 1893 plusmn 17 y
ndash Measured value shows significant positive biasndash Reason incomplete separation of 230Th from the
parent 234U nuclide(ldquoclock is not set to zerordquo)
ndash Residual 230Th cannot be calculated or corrected for
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 36
Case study ndash Find-26
bull 234U abundance suggests low temperature redox deposit value agrees with data reported by IAEA for UOC from Al Qaim (Iraq)
bull Impurities high P contentsimilar metallic impurities to Iraqi phosphate deposits
bull Pb isotopes natural young deposit low U content in orebull REE pattern flat no Eu or Ce anomaly rarr previously found
in certain sandstone-type and reworked phosphorite
Data inherent to the material corroborate information from external sources
Identification of origin based onSingle sampleMultiple parameters
Identification of origin based onSingle sampleMultiple parameters
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 37
Comparison of relative efforts ndash yellow cake
(5)(5)SIMSU particle analysis(5)Evaluation and Report
MC-ICP-MSMC-ICP-MSICP-MSIR-Spectroscopy RamanIon ChromatographyICP-MS IDMS
Electron Microscopy EDX WDXOptical MicroscopyICP-MSTIMSTitration IDMS
Technique
1853Total
15Nd Isotopes15Sr Isotopes3Rare Earth Elemental pattern1Molecular structure
15Anionic impurities3Age dating
3Micromorphology1Visual inspection macroscopic11Impurities11Isotopic Composition11Element Assay
ForensicsSafeguardsAnalysisParameter
Note rounded figures based on a full cost evaluation figures in brackets are not included in the Total
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 38
Conclusions
Wealth of information inherent to nuclear materialDecrypting the information requires sophisticated methodology subject matter expertise and reference dataSignificant effort (resources and time) needed for comprehensive analysis and data interpretationNuclear forensics methodology may open new avenuesin different areasApplication of investigative techniques in Safeguards has to be evaluated
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 4
bull aims at providing clues on the history (production process date of production place of production intended use) of nuclear material
Objectives of Nuclear Material Analysis
bull provides information on nuclear material of immediate relevance to law enforcement
Nuclear Forensics
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 5
Nuclear Forensic Science - Signatures
Intr
oduc
edand wiped out
during material processing
Processes
Chemical Technical PhysicalLeaching Powder flow Neutron reactionSeparation Pelletising Radioactive decayCalcination
Source of signature
Material ProcessU deposit Accidental
PipingIntentional
Burnable poisons
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 6
Parameters ndash Patterns - Signatures
Complexity Multiple Signatures
Analytical and interpretational challengesOpportunities for signature development
Radioisotopes
Metallic Impurities
StableIsotopes
Non-metallic impurities
Structure
MajorElements
Morphology
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 7
NM isotopics (particles)Completeness
Microstructure
Macroscopic appearance
Chem composition
Organic impurities
Anionic impurities
( )Metallic impurities Process identification
Decay productsAge dating
Stable isotopesGeolocation
NM isotopics
NM concentrationCorrectness
Nuclear Forensics
Strengthened Sfg 540 type
Traditional Sfg153-typeParameterPurpose
Standard amp Advanced Parameters
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 8
U products
bull U ores
bull U ore concentrates (ADU AUC peroxideshellip)
bull U oxide powders
bull UF4 and UF6
bull U pellets
Study on 79 yellow cake samples
Aim Identify the impurities that are significant in relation to the source material (same type of material ndash different geographic origin)
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 9
httpwwwnucleonicanet
U-238 rarrPb-206
U-235 rarrPb-207
Th-232 rarrPb-208
Lead isotopesDecay products of U and Th
High U content rarr high variation of isotope ratios
The isotope composition depends on the history (eg weathering) and age of ore body
Can be easily used for provenance Can be easily used for provenance assessment of the oreassessment of the ore
Lead isotopics
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 10
Lead Isotopic Composition
0 2 4 6 8 10 12 14 16 18
Beverley-1 (AUS)
Beverley-2 (AUS)
Beverley-3 (AUS)
Beverley-4 (AUS)
Ranger (AUS)
Olympic Dam (AUS)
Key Lake (CAN)
Rabbit Lake (CAN)
Stanrock (CAN)
Roumlssing (NAM)
ESI Calgary (CAN)
Isotope Ratio
Pb-207Pb-208Pb-206Pb-208
Overlapping between mines
Relative high within-mine
variation
Applicability and limitationsLarge variation of isotope ratios between mines (radiogenic ratios amp dating)Certain ore types have low 206Pb207Pb ratios (sandstone phosphorite)Relatively high within-mine variationLess applicable for ldquopurerdquo UOCs
Pb isotopes
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 11
Date estimation of the ore on the basis of Pb-Pb method
Using natural-lead corrected valuesWorks better for more radiogenic-Pb
containing samples
1720-18221650+130-140175Ranger
600-1200 1160+680-1010565Roumlssing
5-30lt 640941El Mesquite
1300-13801130+210-740252Cluff Lake
2139 plusmn 1002140+140-150207Blind River
Literature value
Calculated deposit age
(Ma)
Natural 207Pb
content
UOC sample
Age dating using Pb isotopes
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 12
Sr-87Sr-86 Isotope Ratio in the Investigated Uranium Ore Concentrates
06900695070007050710071507200725073007350740
Beverle
y-1 (A
US)Bev
erley-2
(AUS)
Beverle
y-3 (A
US)Bev
erley-4
(AUS)
Ranger
(AUS)
Olympic
Dam (A
US)Key
Lake
(CAN)
Rabbit L
ake (C
AN)Stanro
ck (C
AN)Roumlss
ing (N
AM)
ESI Calg
ary (C
AN)
Sr-8
7Sr
-86
Isot
ope
Rat
io Lower within-mine variability
Overlap
Sr isotopes
Lower between-
mine variability
Precision methods like MC-ICPMS
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 13
Uranium minor isotopes
42E-05
47E-05
52E-05
57E-05
62E-05
67E-05
72E-05
77E-05
82E-05
87E-05
Nam
Ros
sing
Can
Blin
d R
iver
Aus
Oly
mpi
c D
am
Usa
Esi
Can
Esi
Aus
Ran
ger
Can
Eld
orad
o
Swe
Ran
stad
t
Usa
El M
esqu
ite
Aus
Mar
y Ka
thle
en
Usa
Ker
r McG
ee
Can
Sta
nroc
k
SA P
alab
ora
Bra
Nuc
lebr
as
Aus
Rum
Jun
gle
Usa
Hom
esta
ke
Can
Sta
nlei
gh
Aus
Que
ensl
and
Can
Key
Lak
e
Usa
Yan
kee
Yello
w
Can
Far
aday
Usa
Fal
ls C
ity
Can
Mad
awas
ka
Can
Clu
ff La
ke
Cze
Rep
ublic
Aus
Beve
rley
fresh
Aus
Beve
rley
old
Usa
Ana
kond
a
Aus
Rad
ium
Hill
Can
Rio
Alg
om
Can
Den
ison
Usa
Shi
rley
Basi
n
Can
El D
orad
o
Can
Ray
Roc
k
Aus
Sout
h Al
ligat
or
U-2
34U
-238
00E+00
50E-09
10E-08
15E-08
20E-08
25E-08
30E-08
U-2
36U
-238
bull 234U238U ratio varies in nature due to eg the preferential leaching of 234U after α-recoil
bull ldquoHighrdquo 236U abundance most probably a cross-contamination
natural
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 14
bull 143Nd144Nd ratio varies in nature due to the 147Sm 143Nd decaybull natural variation 0510 ndash 0513bull the value depends on the age of the mineral and mineral typebull robust indicator as Nd (like other REE) follows uranium (less prone to
weathering) small within-mine variation
0511 05112 05114 05116 05118 0512 05122 05124 05126
Beverley-1 (AUS)
Beverley-2 (AUS)
Straz (CZ)
Stanrock (CAN)
143Nd144Nd ratio
Neodymium isotope ratio
T12=1061011a
Nd-143 Nd-144 ratio
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 15
REE chemically similar with valence state mainly +3 REE pattern often remain unaltered during metamorphism thusproviding information on the premetamorphic history geologicalbackground and source of the rock The behavior of the valence-variable Ce (+4) and Eu (+2) is alsocharacteristic to the rock and it can be exploited to obtain information on the formation conditions
Rare earth elementsrsquo pattern
REE pattern is less prone to the process
can be used straightforwardly for the origin assessment
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 16
Rare-earth pattern of the investigated uranium ore concentrates
01
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
Cho
ndrit
e no
rmal
ized
con
cent
ratio
n
Beverley-1 (Sandstone)
Beverley-2 (Sandstone)
Beverley-3 (Sandstone)
Beverley-4 (Sandstone)
Ranger (Unconformity)
Olympic Dam (Breccia)
Key Lake (Unconformity)
Stanrock (Quartz-pebble congl)
Roumlssing (Intrusive)
ESI Calgary (Phosphorite)
Sedimentary-type
Quartz-pebbleIntrusive (Euanomaly)
Middle REE enrichment (unconformity-type)
REE patterns
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 17
bull geometry rarr 5 x 5 x 5 cm
bull weight about 24 kg
bull elemental uranium produced around 1943 plusmn 2 years (Haigerloch Germany)
Questions1 What is it 2 Origin of the material 3 etc
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 18
Intended use and origin
Nuclear forensics
bull elemental composition pure U metalunconventional applicationreactor
bull isotopic composition rarr natural U rarrD2O or graphite moderated reactor
bull Age via 234U 230Th590 plusmn 20 years (in 2003)
=gt Date of production second half of 1943
Geometry points at German originbull Open literature
Haigerloch reactor 1945
664 cubes x 24 kg = 15936 kg
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 19
ndash Where is the uranium coming from
Date of Production second half of 1943
Authentic cube
Belgian Congo or Joachimsthal (Czech Republic)
rare earth element pattern
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 20
Samples measured
ndash Haigerloch (ldquoHeisenbergrdquo) uranium cube
ndash Heidelberg (ldquoWirtzrdquo) uranium plates
ndash Yellow cake from Otto Hahnrsquos laboratory in Berlin
ndash For comparisonJoachimsthal uranium ore (bdquohistoricldquo sample)Congo uranium ore
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 21
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
REF
REF
REF
REF
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 22
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
REF
REF
REF
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 23
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
REF
REF
Congo UOC
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 24
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
Ore fromJoachimstalREF
Congo UOC
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 25
Inorganic FT-IR measurement of UOC samplesMeasurement in pellet form using KBrRapid identification of compound (oxide peroxide ADU AUC partially
calcined samples)Detection of certain process-related impurities (sulphate carbonate
nitrate)
Uranium composition in UOCs
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 26
Nitrate (1380 cm-1)Impurity from eluate or back extractant
Sulphate (1130 cm-1)Residual from H2SO4 eluate or back extractant
Uranium composition in UOCs
U-O vibration
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 27
Anion residuals in UOCrsquos
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
20
40
60
80
100
120
140
160
180
200
uScm
Cond
fluor
ide
102
2
2 chlo
ride
02
19
4 5 6 7 nitr
ate
003
6
sulp
hate
479
129
Canada ESI
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
17
18
19
20
21
22
23
24
25
26
uScm
Cond
fluor
ide
036
7
2 3
chlo
ride
55
32
5 brom
ide
-00
26
nitr
ate
012
7
sulp
hate
20
767
9
Australia Radium Hill
Different type of uranium deposits
Different processes for U extraction
Different mineral acids are used
Acid remainings
fluor
ide
chlo
ride
brom
ide
nitr
ate
sulp
hate
fluor
ide
chlo
ride
nitr
ate
sulp
hate
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 28
NO3SO4
0
01
02
03
04
05
06
07
08
09
1
Sout
h Al
ligat
or
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y Ka
thle
en
ESI U
SA
ESI C
anad
a
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Stan
rock
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lake
Mad
awas
ka
Mac
assa
Nor
th S
pan
Milli
ken
Lake
Eldo
rado
Stan
leig
h
FCl
0
05
1
15
2
25
3
35
4
45
5
Sou
th A
lliga
tor
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y K
athl
een
ES
I US
A
ES
I Can
ada
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Sta
nroc
k
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lak
e
Mad
awas
ka
Mac
assa
Nor
th S
pan
Mill
iken
Lak
e
Eld
orad
o
Sta
nlei
gh
Anion ratios
Phosphorite oresQuartz-pebble conglomerate and vein deposits
Nitric acid leaching rArr
Indicator of the processApatite mineral Ca5(PO4)3(FClOH)
rArr Indicator of the deposit type
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 29
Sandstone basal channel Quartz-pebble
conglomerate
Phosphorite
Black shale
Statistical evaluation of UOC data
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 30
U productsbull U ores
bull U ore concentrates
bull U oxide powders
bull UF4 and UF6
bull U pellets
Next step - Vertical study
Aim Identify the impurities that are acquired from or lost in the process What is the effect on the impurities from the source material
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 31
Uranium oreconcentrates
Process stagesamples and reagents
UO3
Next step - Vertical study
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 32
Case study
Backgroundbull uranium raw material of unknown
originbull 2003 Rotterdam (NL)bull Brownish yellow powder ~3 kgbull Found on a shipload from Jordan
Measurements performed at ITUbull NDA analysisbull Isotope ratio measurements (U Sr
Pb)bull Infrared analysisbull Impurity analysisbull REE pattern determination
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 33
Case study
Vibrational Spectrum (Infrared Spectrometry)
bull Compound is AUC xH2Obull Sulfate impurity (from dissolution of starting material)
bullNitrate impurity (from solvent extractionpurification)
Mass Spectrometry
bull Natural uranium isotopic compositionbull Natural lead isotopic composition
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 34
Case study
Sr Isotope Ratio
Low value typical for phosphorites (eg North Africa Middle East UShellip)
070757 plusmn 000011
070814 plusmn 000004
071092 plusmn 000006
071416 plusmn 000011
071985 plusmn 000029
072336 plusmn 000004
073434 plusmn 000012
070785 plusmn 000004
071775 plusmn 000003
067 068 069 070 071 072 073 074 075 076 077 078 079 080
Beverley
Calgary
Key Lake
Olympic Dam
Ranger
Ranstad
Stanrock
Mulberry
Fund-26
87Sr86Sr Isotope RatioSr-87 Sr-86 isotope ratio
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 35
Case study
Age dating based on 234U230Th
Age dating based on 232Th228Th
Last chemical separation 1988 plusmn 5 yndash Applicable to samples with incomplete Th separationndash Complementary to 234U230Th method
Last chemical separation 1893 plusmn 17 y
ndash Measured value shows significant positive biasndash Reason incomplete separation of 230Th from the
parent 234U nuclide(ldquoclock is not set to zerordquo)
ndash Residual 230Th cannot be calculated or corrected for
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 36
Case study ndash Find-26
bull 234U abundance suggests low temperature redox deposit value agrees with data reported by IAEA for UOC from Al Qaim (Iraq)
bull Impurities high P contentsimilar metallic impurities to Iraqi phosphate deposits
bull Pb isotopes natural young deposit low U content in orebull REE pattern flat no Eu or Ce anomaly rarr previously found
in certain sandstone-type and reworked phosphorite
Data inherent to the material corroborate information from external sources
Identification of origin based onSingle sampleMultiple parameters
Identification of origin based onSingle sampleMultiple parameters
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 37
Comparison of relative efforts ndash yellow cake
(5)(5)SIMSU particle analysis(5)Evaluation and Report
MC-ICP-MSMC-ICP-MSICP-MSIR-Spectroscopy RamanIon ChromatographyICP-MS IDMS
Electron Microscopy EDX WDXOptical MicroscopyICP-MSTIMSTitration IDMS
Technique
1853Total
15Nd Isotopes15Sr Isotopes3Rare Earth Elemental pattern1Molecular structure
15Anionic impurities3Age dating
3Micromorphology1Visual inspection macroscopic11Impurities11Isotopic Composition11Element Assay
ForensicsSafeguardsAnalysisParameter
Note rounded figures based on a full cost evaluation figures in brackets are not included in the Total
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 38
Conclusions
Wealth of information inherent to nuclear materialDecrypting the information requires sophisticated methodology subject matter expertise and reference dataSignificant effort (resources and time) needed for comprehensive analysis and data interpretationNuclear forensics methodology may open new avenuesin different areasApplication of investigative techniques in Safeguards has to be evaluated
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 5
Nuclear Forensic Science - Signatures
Intr
oduc
edand wiped out
during material processing
Processes
Chemical Technical PhysicalLeaching Powder flow Neutron reactionSeparation Pelletising Radioactive decayCalcination
Source of signature
Material ProcessU deposit Accidental
PipingIntentional
Burnable poisons
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 6
Parameters ndash Patterns - Signatures
Complexity Multiple Signatures
Analytical and interpretational challengesOpportunities for signature development
Radioisotopes
Metallic Impurities
StableIsotopes
Non-metallic impurities
Structure
MajorElements
Morphology
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 7
NM isotopics (particles)Completeness
Microstructure
Macroscopic appearance
Chem composition
Organic impurities
Anionic impurities
( )Metallic impurities Process identification
Decay productsAge dating
Stable isotopesGeolocation
NM isotopics
NM concentrationCorrectness
Nuclear Forensics
Strengthened Sfg 540 type
Traditional Sfg153-typeParameterPurpose
Standard amp Advanced Parameters
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 8
U products
bull U ores
bull U ore concentrates (ADU AUC peroxideshellip)
bull U oxide powders
bull UF4 and UF6
bull U pellets
Study on 79 yellow cake samples
Aim Identify the impurities that are significant in relation to the source material (same type of material ndash different geographic origin)
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 9
httpwwwnucleonicanet
U-238 rarrPb-206
U-235 rarrPb-207
Th-232 rarrPb-208
Lead isotopesDecay products of U and Th
High U content rarr high variation of isotope ratios
The isotope composition depends on the history (eg weathering) and age of ore body
Can be easily used for provenance Can be easily used for provenance assessment of the oreassessment of the ore
Lead isotopics
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 10
Lead Isotopic Composition
0 2 4 6 8 10 12 14 16 18
Beverley-1 (AUS)
Beverley-2 (AUS)
Beverley-3 (AUS)
Beverley-4 (AUS)
Ranger (AUS)
Olympic Dam (AUS)
Key Lake (CAN)
Rabbit Lake (CAN)
Stanrock (CAN)
Roumlssing (NAM)
ESI Calgary (CAN)
Isotope Ratio
Pb-207Pb-208Pb-206Pb-208
Overlapping between mines
Relative high within-mine
variation
Applicability and limitationsLarge variation of isotope ratios between mines (radiogenic ratios amp dating)Certain ore types have low 206Pb207Pb ratios (sandstone phosphorite)Relatively high within-mine variationLess applicable for ldquopurerdquo UOCs
Pb isotopes
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 11
Date estimation of the ore on the basis of Pb-Pb method
Using natural-lead corrected valuesWorks better for more radiogenic-Pb
containing samples
1720-18221650+130-140175Ranger
600-1200 1160+680-1010565Roumlssing
5-30lt 640941El Mesquite
1300-13801130+210-740252Cluff Lake
2139 plusmn 1002140+140-150207Blind River
Literature value
Calculated deposit age
(Ma)
Natural 207Pb
content
UOC sample
Age dating using Pb isotopes
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 12
Sr-87Sr-86 Isotope Ratio in the Investigated Uranium Ore Concentrates
06900695070007050710071507200725073007350740
Beverle
y-1 (A
US)Bev
erley-2
(AUS)
Beverle
y-3 (A
US)Bev
erley-4
(AUS)
Ranger
(AUS)
Olympic
Dam (A
US)Key
Lake
(CAN)
Rabbit L
ake (C
AN)Stanro
ck (C
AN)Roumlss
ing (N
AM)
ESI Calg
ary (C
AN)
Sr-8
7Sr
-86
Isot
ope
Rat
io Lower within-mine variability
Overlap
Sr isotopes
Lower between-
mine variability
Precision methods like MC-ICPMS
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 13
Uranium minor isotopes
42E-05
47E-05
52E-05
57E-05
62E-05
67E-05
72E-05
77E-05
82E-05
87E-05
Nam
Ros
sing
Can
Blin
d R
iver
Aus
Oly
mpi
c D
am
Usa
Esi
Can
Esi
Aus
Ran
ger
Can
Eld
orad
o
Swe
Ran
stad
t
Usa
El M
esqu
ite
Aus
Mar
y Ka
thle
en
Usa
Ker
r McG
ee
Can
Sta
nroc
k
SA P
alab
ora
Bra
Nuc
lebr
as
Aus
Rum
Jun
gle
Usa
Hom
esta
ke
Can
Sta
nlei
gh
Aus
Que
ensl
and
Can
Key
Lak
e
Usa
Yan
kee
Yello
w
Can
Far
aday
Usa
Fal
ls C
ity
Can
Mad
awas
ka
Can
Clu
ff La
ke
Cze
Rep
ublic
Aus
Beve
rley
fresh
Aus
Beve
rley
old
Usa
Ana
kond
a
Aus
Rad
ium
Hill
Can
Rio
Alg
om
Can
Den
ison
Usa
Shi
rley
Basi
n
Can
El D
orad
o
Can
Ray
Roc
k
Aus
Sout
h Al
ligat
or
U-2
34U
-238
00E+00
50E-09
10E-08
15E-08
20E-08
25E-08
30E-08
U-2
36U
-238
bull 234U238U ratio varies in nature due to eg the preferential leaching of 234U after α-recoil
bull ldquoHighrdquo 236U abundance most probably a cross-contamination
natural
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 14
bull 143Nd144Nd ratio varies in nature due to the 147Sm 143Nd decaybull natural variation 0510 ndash 0513bull the value depends on the age of the mineral and mineral typebull robust indicator as Nd (like other REE) follows uranium (less prone to
weathering) small within-mine variation
0511 05112 05114 05116 05118 0512 05122 05124 05126
Beverley-1 (AUS)
Beverley-2 (AUS)
Straz (CZ)
Stanrock (CAN)
143Nd144Nd ratio
Neodymium isotope ratio
T12=1061011a
Nd-143 Nd-144 ratio
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 15
REE chemically similar with valence state mainly +3 REE pattern often remain unaltered during metamorphism thusproviding information on the premetamorphic history geologicalbackground and source of the rock The behavior of the valence-variable Ce (+4) and Eu (+2) is alsocharacteristic to the rock and it can be exploited to obtain information on the formation conditions
Rare earth elementsrsquo pattern
REE pattern is less prone to the process
can be used straightforwardly for the origin assessment
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 16
Rare-earth pattern of the investigated uranium ore concentrates
01
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
Cho
ndrit
e no
rmal
ized
con
cent
ratio
n
Beverley-1 (Sandstone)
Beverley-2 (Sandstone)
Beverley-3 (Sandstone)
Beverley-4 (Sandstone)
Ranger (Unconformity)
Olympic Dam (Breccia)
Key Lake (Unconformity)
Stanrock (Quartz-pebble congl)
Roumlssing (Intrusive)
ESI Calgary (Phosphorite)
Sedimentary-type
Quartz-pebbleIntrusive (Euanomaly)
Middle REE enrichment (unconformity-type)
REE patterns
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 17
bull geometry rarr 5 x 5 x 5 cm
bull weight about 24 kg
bull elemental uranium produced around 1943 plusmn 2 years (Haigerloch Germany)
Questions1 What is it 2 Origin of the material 3 etc
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 18
Intended use and origin
Nuclear forensics
bull elemental composition pure U metalunconventional applicationreactor
bull isotopic composition rarr natural U rarrD2O or graphite moderated reactor
bull Age via 234U 230Th590 plusmn 20 years (in 2003)
=gt Date of production second half of 1943
Geometry points at German originbull Open literature
Haigerloch reactor 1945
664 cubes x 24 kg = 15936 kg
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 19
ndash Where is the uranium coming from
Date of Production second half of 1943
Authentic cube
Belgian Congo or Joachimsthal (Czech Republic)
rare earth element pattern
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 20
Samples measured
ndash Haigerloch (ldquoHeisenbergrdquo) uranium cube
ndash Heidelberg (ldquoWirtzrdquo) uranium plates
ndash Yellow cake from Otto Hahnrsquos laboratory in Berlin
ndash For comparisonJoachimsthal uranium ore (bdquohistoricldquo sample)Congo uranium ore
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 21
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
REF
REF
REF
REF
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 22
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
REF
REF
REF
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 23
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
REF
REF
Congo UOC
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 24
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
Ore fromJoachimstalREF
Congo UOC
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 25
Inorganic FT-IR measurement of UOC samplesMeasurement in pellet form using KBrRapid identification of compound (oxide peroxide ADU AUC partially
calcined samples)Detection of certain process-related impurities (sulphate carbonate
nitrate)
Uranium composition in UOCs
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 26
Nitrate (1380 cm-1)Impurity from eluate or back extractant
Sulphate (1130 cm-1)Residual from H2SO4 eluate or back extractant
Uranium composition in UOCs
U-O vibration
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 27
Anion residuals in UOCrsquos
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
20
40
60
80
100
120
140
160
180
200
uScm
Cond
fluor
ide
102
2
2 chlo
ride
02
19
4 5 6 7 nitr
ate
003
6
sulp
hate
479
129
Canada ESI
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
17
18
19
20
21
22
23
24
25
26
uScm
Cond
fluor
ide
036
7
2 3
chlo
ride
55
32
5 brom
ide
-00
26
nitr
ate
012
7
sulp
hate
20
767
9
Australia Radium Hill
Different type of uranium deposits
Different processes for U extraction
Different mineral acids are used
Acid remainings
fluor
ide
chlo
ride
brom
ide
nitr
ate
sulp
hate
fluor
ide
chlo
ride
nitr
ate
sulp
hate
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 28
NO3SO4
0
01
02
03
04
05
06
07
08
09
1
Sout
h Al
ligat
or
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y Ka
thle
en
ESI U
SA
ESI C
anad
a
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Stan
rock
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lake
Mad
awas
ka
Mac
assa
Nor
th S
pan
Milli
ken
Lake
Eldo
rado
Stan
leig
h
FCl
0
05
1
15
2
25
3
35
4
45
5
Sou
th A
lliga
tor
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y K
athl
een
ES
I US
A
ES
I Can
ada
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Sta
nroc
k
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lak
e
Mad
awas
ka
Mac
assa
Nor
th S
pan
Mill
iken
Lak
e
Eld
orad
o
Sta
nlei
gh
Anion ratios
Phosphorite oresQuartz-pebble conglomerate and vein deposits
Nitric acid leaching rArr
Indicator of the processApatite mineral Ca5(PO4)3(FClOH)
rArr Indicator of the deposit type
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 29
Sandstone basal channel Quartz-pebble
conglomerate
Phosphorite
Black shale
Statistical evaluation of UOC data
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 30
U productsbull U ores
bull U ore concentrates
bull U oxide powders
bull UF4 and UF6
bull U pellets
Next step - Vertical study
Aim Identify the impurities that are acquired from or lost in the process What is the effect on the impurities from the source material
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 31
Uranium oreconcentrates
Process stagesamples and reagents
UO3
Next step - Vertical study
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 32
Case study
Backgroundbull uranium raw material of unknown
originbull 2003 Rotterdam (NL)bull Brownish yellow powder ~3 kgbull Found on a shipload from Jordan
Measurements performed at ITUbull NDA analysisbull Isotope ratio measurements (U Sr
Pb)bull Infrared analysisbull Impurity analysisbull REE pattern determination
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 33
Case study
Vibrational Spectrum (Infrared Spectrometry)
bull Compound is AUC xH2Obull Sulfate impurity (from dissolution of starting material)
bullNitrate impurity (from solvent extractionpurification)
Mass Spectrometry
bull Natural uranium isotopic compositionbull Natural lead isotopic composition
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 34
Case study
Sr Isotope Ratio
Low value typical for phosphorites (eg North Africa Middle East UShellip)
070757 plusmn 000011
070814 plusmn 000004
071092 plusmn 000006
071416 plusmn 000011
071985 plusmn 000029
072336 plusmn 000004
073434 plusmn 000012
070785 plusmn 000004
071775 plusmn 000003
067 068 069 070 071 072 073 074 075 076 077 078 079 080
Beverley
Calgary
Key Lake
Olympic Dam
Ranger
Ranstad
Stanrock
Mulberry
Fund-26
87Sr86Sr Isotope RatioSr-87 Sr-86 isotope ratio
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 35
Case study
Age dating based on 234U230Th
Age dating based on 232Th228Th
Last chemical separation 1988 plusmn 5 yndash Applicable to samples with incomplete Th separationndash Complementary to 234U230Th method
Last chemical separation 1893 plusmn 17 y
ndash Measured value shows significant positive biasndash Reason incomplete separation of 230Th from the
parent 234U nuclide(ldquoclock is not set to zerordquo)
ndash Residual 230Th cannot be calculated or corrected for
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 36
Case study ndash Find-26
bull 234U abundance suggests low temperature redox deposit value agrees with data reported by IAEA for UOC from Al Qaim (Iraq)
bull Impurities high P contentsimilar metallic impurities to Iraqi phosphate deposits
bull Pb isotopes natural young deposit low U content in orebull REE pattern flat no Eu or Ce anomaly rarr previously found
in certain sandstone-type and reworked phosphorite
Data inherent to the material corroborate information from external sources
Identification of origin based onSingle sampleMultiple parameters
Identification of origin based onSingle sampleMultiple parameters
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 37
Comparison of relative efforts ndash yellow cake
(5)(5)SIMSU particle analysis(5)Evaluation and Report
MC-ICP-MSMC-ICP-MSICP-MSIR-Spectroscopy RamanIon ChromatographyICP-MS IDMS
Electron Microscopy EDX WDXOptical MicroscopyICP-MSTIMSTitration IDMS
Technique
1853Total
15Nd Isotopes15Sr Isotopes3Rare Earth Elemental pattern1Molecular structure
15Anionic impurities3Age dating
3Micromorphology1Visual inspection macroscopic11Impurities11Isotopic Composition11Element Assay
ForensicsSafeguardsAnalysisParameter
Note rounded figures based on a full cost evaluation figures in brackets are not included in the Total
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 38
Conclusions
Wealth of information inherent to nuclear materialDecrypting the information requires sophisticated methodology subject matter expertise and reference dataSignificant effort (resources and time) needed for comprehensive analysis and data interpretationNuclear forensics methodology may open new avenuesin different areasApplication of investigative techniques in Safeguards has to be evaluated
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 6
Parameters ndash Patterns - Signatures
Complexity Multiple Signatures
Analytical and interpretational challengesOpportunities for signature development
Radioisotopes
Metallic Impurities
StableIsotopes
Non-metallic impurities
Structure
MajorElements
Morphology
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 7
NM isotopics (particles)Completeness
Microstructure
Macroscopic appearance
Chem composition
Organic impurities
Anionic impurities
( )Metallic impurities Process identification
Decay productsAge dating
Stable isotopesGeolocation
NM isotopics
NM concentrationCorrectness
Nuclear Forensics
Strengthened Sfg 540 type
Traditional Sfg153-typeParameterPurpose
Standard amp Advanced Parameters
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 8
U products
bull U ores
bull U ore concentrates (ADU AUC peroxideshellip)
bull U oxide powders
bull UF4 and UF6
bull U pellets
Study on 79 yellow cake samples
Aim Identify the impurities that are significant in relation to the source material (same type of material ndash different geographic origin)
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 9
httpwwwnucleonicanet
U-238 rarrPb-206
U-235 rarrPb-207
Th-232 rarrPb-208
Lead isotopesDecay products of U and Th
High U content rarr high variation of isotope ratios
The isotope composition depends on the history (eg weathering) and age of ore body
Can be easily used for provenance Can be easily used for provenance assessment of the oreassessment of the ore
Lead isotopics
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 10
Lead Isotopic Composition
0 2 4 6 8 10 12 14 16 18
Beverley-1 (AUS)
Beverley-2 (AUS)
Beverley-3 (AUS)
Beverley-4 (AUS)
Ranger (AUS)
Olympic Dam (AUS)
Key Lake (CAN)
Rabbit Lake (CAN)
Stanrock (CAN)
Roumlssing (NAM)
ESI Calgary (CAN)
Isotope Ratio
Pb-207Pb-208Pb-206Pb-208
Overlapping between mines
Relative high within-mine
variation
Applicability and limitationsLarge variation of isotope ratios between mines (radiogenic ratios amp dating)Certain ore types have low 206Pb207Pb ratios (sandstone phosphorite)Relatively high within-mine variationLess applicable for ldquopurerdquo UOCs
Pb isotopes
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 11
Date estimation of the ore on the basis of Pb-Pb method
Using natural-lead corrected valuesWorks better for more radiogenic-Pb
containing samples
1720-18221650+130-140175Ranger
600-1200 1160+680-1010565Roumlssing
5-30lt 640941El Mesquite
1300-13801130+210-740252Cluff Lake
2139 plusmn 1002140+140-150207Blind River
Literature value
Calculated deposit age
(Ma)
Natural 207Pb
content
UOC sample
Age dating using Pb isotopes
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 12
Sr-87Sr-86 Isotope Ratio in the Investigated Uranium Ore Concentrates
06900695070007050710071507200725073007350740
Beverle
y-1 (A
US)Bev
erley-2
(AUS)
Beverle
y-3 (A
US)Bev
erley-4
(AUS)
Ranger
(AUS)
Olympic
Dam (A
US)Key
Lake
(CAN)
Rabbit L
ake (C
AN)Stanro
ck (C
AN)Roumlss
ing (N
AM)
ESI Calg
ary (C
AN)
Sr-8
7Sr
-86
Isot
ope
Rat
io Lower within-mine variability
Overlap
Sr isotopes
Lower between-
mine variability
Precision methods like MC-ICPMS
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 13
Uranium minor isotopes
42E-05
47E-05
52E-05
57E-05
62E-05
67E-05
72E-05
77E-05
82E-05
87E-05
Nam
Ros
sing
Can
Blin
d R
iver
Aus
Oly
mpi
c D
am
Usa
Esi
Can
Esi
Aus
Ran
ger
Can
Eld
orad
o
Swe
Ran
stad
t
Usa
El M
esqu
ite
Aus
Mar
y Ka
thle
en
Usa
Ker
r McG
ee
Can
Sta
nroc
k
SA P
alab
ora
Bra
Nuc
lebr
as
Aus
Rum
Jun
gle
Usa
Hom
esta
ke
Can
Sta
nlei
gh
Aus
Que
ensl
and
Can
Key
Lak
e
Usa
Yan
kee
Yello
w
Can
Far
aday
Usa
Fal
ls C
ity
Can
Mad
awas
ka
Can
Clu
ff La
ke
Cze
Rep
ublic
Aus
Beve
rley
fresh
Aus
Beve
rley
old
Usa
Ana
kond
a
Aus
Rad
ium
Hill
Can
Rio
Alg
om
Can
Den
ison
Usa
Shi
rley
Basi
n
Can
El D
orad
o
Can
Ray
Roc
k
Aus
Sout
h Al
ligat
or
U-2
34U
-238
00E+00
50E-09
10E-08
15E-08
20E-08
25E-08
30E-08
U-2
36U
-238
bull 234U238U ratio varies in nature due to eg the preferential leaching of 234U after α-recoil
bull ldquoHighrdquo 236U abundance most probably a cross-contamination
natural
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 14
bull 143Nd144Nd ratio varies in nature due to the 147Sm 143Nd decaybull natural variation 0510 ndash 0513bull the value depends on the age of the mineral and mineral typebull robust indicator as Nd (like other REE) follows uranium (less prone to
weathering) small within-mine variation
0511 05112 05114 05116 05118 0512 05122 05124 05126
Beverley-1 (AUS)
Beverley-2 (AUS)
Straz (CZ)
Stanrock (CAN)
143Nd144Nd ratio
Neodymium isotope ratio
T12=1061011a
Nd-143 Nd-144 ratio
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 15
REE chemically similar with valence state mainly +3 REE pattern often remain unaltered during metamorphism thusproviding information on the premetamorphic history geologicalbackground and source of the rock The behavior of the valence-variable Ce (+4) and Eu (+2) is alsocharacteristic to the rock and it can be exploited to obtain information on the formation conditions
Rare earth elementsrsquo pattern
REE pattern is less prone to the process
can be used straightforwardly for the origin assessment
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 16
Rare-earth pattern of the investigated uranium ore concentrates
01
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
Cho
ndrit
e no
rmal
ized
con
cent
ratio
n
Beverley-1 (Sandstone)
Beverley-2 (Sandstone)
Beverley-3 (Sandstone)
Beverley-4 (Sandstone)
Ranger (Unconformity)
Olympic Dam (Breccia)
Key Lake (Unconformity)
Stanrock (Quartz-pebble congl)
Roumlssing (Intrusive)
ESI Calgary (Phosphorite)
Sedimentary-type
Quartz-pebbleIntrusive (Euanomaly)
Middle REE enrichment (unconformity-type)
REE patterns
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 17
bull geometry rarr 5 x 5 x 5 cm
bull weight about 24 kg
bull elemental uranium produced around 1943 plusmn 2 years (Haigerloch Germany)
Questions1 What is it 2 Origin of the material 3 etc
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 18
Intended use and origin
Nuclear forensics
bull elemental composition pure U metalunconventional applicationreactor
bull isotopic composition rarr natural U rarrD2O or graphite moderated reactor
bull Age via 234U 230Th590 plusmn 20 years (in 2003)
=gt Date of production second half of 1943
Geometry points at German originbull Open literature
Haigerloch reactor 1945
664 cubes x 24 kg = 15936 kg
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 19
ndash Where is the uranium coming from
Date of Production second half of 1943
Authentic cube
Belgian Congo or Joachimsthal (Czech Republic)
rare earth element pattern
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 20
Samples measured
ndash Haigerloch (ldquoHeisenbergrdquo) uranium cube
ndash Heidelberg (ldquoWirtzrdquo) uranium plates
ndash Yellow cake from Otto Hahnrsquos laboratory in Berlin
ndash For comparisonJoachimsthal uranium ore (bdquohistoricldquo sample)Congo uranium ore
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 21
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
REF
REF
REF
REF
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 22
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
REF
REF
REF
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 23
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
REF
REF
Congo UOC
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 24
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
Ore fromJoachimstalREF
Congo UOC
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 25
Inorganic FT-IR measurement of UOC samplesMeasurement in pellet form using KBrRapid identification of compound (oxide peroxide ADU AUC partially
calcined samples)Detection of certain process-related impurities (sulphate carbonate
nitrate)
Uranium composition in UOCs
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 26
Nitrate (1380 cm-1)Impurity from eluate or back extractant
Sulphate (1130 cm-1)Residual from H2SO4 eluate or back extractant
Uranium composition in UOCs
U-O vibration
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 27
Anion residuals in UOCrsquos
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
20
40
60
80
100
120
140
160
180
200
uScm
Cond
fluor
ide
102
2
2 chlo
ride
02
19
4 5 6 7 nitr
ate
003
6
sulp
hate
479
129
Canada ESI
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
17
18
19
20
21
22
23
24
25
26
uScm
Cond
fluor
ide
036
7
2 3
chlo
ride
55
32
5 brom
ide
-00
26
nitr
ate
012
7
sulp
hate
20
767
9
Australia Radium Hill
Different type of uranium deposits
Different processes for U extraction
Different mineral acids are used
Acid remainings
fluor
ide
chlo
ride
brom
ide
nitr
ate
sulp
hate
fluor
ide
chlo
ride
nitr
ate
sulp
hate
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 28
NO3SO4
0
01
02
03
04
05
06
07
08
09
1
Sout
h Al
ligat
or
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y Ka
thle
en
ESI U
SA
ESI C
anad
a
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Stan
rock
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lake
Mad
awas
ka
Mac
assa
Nor
th S
pan
Milli
ken
Lake
Eldo
rado
Stan
leig
h
FCl
0
05
1
15
2
25
3
35
4
45
5
Sou
th A
lliga
tor
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y K
athl
een
ES
I US
A
ES
I Can
ada
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Sta
nroc
k
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lak
e
Mad
awas
ka
Mac
assa
Nor
th S
pan
Mill
iken
Lak
e
Eld
orad
o
Sta
nlei
gh
Anion ratios
Phosphorite oresQuartz-pebble conglomerate and vein deposits
Nitric acid leaching rArr
Indicator of the processApatite mineral Ca5(PO4)3(FClOH)
rArr Indicator of the deposit type
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 29
Sandstone basal channel Quartz-pebble
conglomerate
Phosphorite
Black shale
Statistical evaluation of UOC data
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 30
U productsbull U ores
bull U ore concentrates
bull U oxide powders
bull UF4 and UF6
bull U pellets
Next step - Vertical study
Aim Identify the impurities that are acquired from or lost in the process What is the effect on the impurities from the source material
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 31
Uranium oreconcentrates
Process stagesamples and reagents
UO3
Next step - Vertical study
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 32
Case study
Backgroundbull uranium raw material of unknown
originbull 2003 Rotterdam (NL)bull Brownish yellow powder ~3 kgbull Found on a shipload from Jordan
Measurements performed at ITUbull NDA analysisbull Isotope ratio measurements (U Sr
Pb)bull Infrared analysisbull Impurity analysisbull REE pattern determination
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 33
Case study
Vibrational Spectrum (Infrared Spectrometry)
bull Compound is AUC xH2Obull Sulfate impurity (from dissolution of starting material)
bullNitrate impurity (from solvent extractionpurification)
Mass Spectrometry
bull Natural uranium isotopic compositionbull Natural lead isotopic composition
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 34
Case study
Sr Isotope Ratio
Low value typical for phosphorites (eg North Africa Middle East UShellip)
070757 plusmn 000011
070814 plusmn 000004
071092 plusmn 000006
071416 plusmn 000011
071985 plusmn 000029
072336 plusmn 000004
073434 plusmn 000012
070785 plusmn 000004
071775 plusmn 000003
067 068 069 070 071 072 073 074 075 076 077 078 079 080
Beverley
Calgary
Key Lake
Olympic Dam
Ranger
Ranstad
Stanrock
Mulberry
Fund-26
87Sr86Sr Isotope RatioSr-87 Sr-86 isotope ratio
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 35
Case study
Age dating based on 234U230Th
Age dating based on 232Th228Th
Last chemical separation 1988 plusmn 5 yndash Applicable to samples with incomplete Th separationndash Complementary to 234U230Th method
Last chemical separation 1893 plusmn 17 y
ndash Measured value shows significant positive biasndash Reason incomplete separation of 230Th from the
parent 234U nuclide(ldquoclock is not set to zerordquo)
ndash Residual 230Th cannot be calculated or corrected for
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 36
Case study ndash Find-26
bull 234U abundance suggests low temperature redox deposit value agrees with data reported by IAEA for UOC from Al Qaim (Iraq)
bull Impurities high P contentsimilar metallic impurities to Iraqi phosphate deposits
bull Pb isotopes natural young deposit low U content in orebull REE pattern flat no Eu or Ce anomaly rarr previously found
in certain sandstone-type and reworked phosphorite
Data inherent to the material corroborate information from external sources
Identification of origin based onSingle sampleMultiple parameters
Identification of origin based onSingle sampleMultiple parameters
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 37
Comparison of relative efforts ndash yellow cake
(5)(5)SIMSU particle analysis(5)Evaluation and Report
MC-ICP-MSMC-ICP-MSICP-MSIR-Spectroscopy RamanIon ChromatographyICP-MS IDMS
Electron Microscopy EDX WDXOptical MicroscopyICP-MSTIMSTitration IDMS
Technique
1853Total
15Nd Isotopes15Sr Isotopes3Rare Earth Elemental pattern1Molecular structure
15Anionic impurities3Age dating
3Micromorphology1Visual inspection macroscopic11Impurities11Isotopic Composition11Element Assay
ForensicsSafeguardsAnalysisParameter
Note rounded figures based on a full cost evaluation figures in brackets are not included in the Total
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 38
Conclusions
Wealth of information inherent to nuclear materialDecrypting the information requires sophisticated methodology subject matter expertise and reference dataSignificant effort (resources and time) needed for comprehensive analysis and data interpretationNuclear forensics methodology may open new avenuesin different areasApplication of investigative techniques in Safeguards has to be evaluated
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 7
NM isotopics (particles)Completeness
Microstructure
Macroscopic appearance
Chem composition
Organic impurities
Anionic impurities
( )Metallic impurities Process identification
Decay productsAge dating
Stable isotopesGeolocation
NM isotopics
NM concentrationCorrectness
Nuclear Forensics
Strengthened Sfg 540 type
Traditional Sfg153-typeParameterPurpose
Standard amp Advanced Parameters
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 8
U products
bull U ores
bull U ore concentrates (ADU AUC peroxideshellip)
bull U oxide powders
bull UF4 and UF6
bull U pellets
Study on 79 yellow cake samples
Aim Identify the impurities that are significant in relation to the source material (same type of material ndash different geographic origin)
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 9
httpwwwnucleonicanet
U-238 rarrPb-206
U-235 rarrPb-207
Th-232 rarrPb-208
Lead isotopesDecay products of U and Th
High U content rarr high variation of isotope ratios
The isotope composition depends on the history (eg weathering) and age of ore body
Can be easily used for provenance Can be easily used for provenance assessment of the oreassessment of the ore
Lead isotopics
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 10
Lead Isotopic Composition
0 2 4 6 8 10 12 14 16 18
Beverley-1 (AUS)
Beverley-2 (AUS)
Beverley-3 (AUS)
Beverley-4 (AUS)
Ranger (AUS)
Olympic Dam (AUS)
Key Lake (CAN)
Rabbit Lake (CAN)
Stanrock (CAN)
Roumlssing (NAM)
ESI Calgary (CAN)
Isotope Ratio
Pb-207Pb-208Pb-206Pb-208
Overlapping between mines
Relative high within-mine
variation
Applicability and limitationsLarge variation of isotope ratios between mines (radiogenic ratios amp dating)Certain ore types have low 206Pb207Pb ratios (sandstone phosphorite)Relatively high within-mine variationLess applicable for ldquopurerdquo UOCs
Pb isotopes
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 11
Date estimation of the ore on the basis of Pb-Pb method
Using natural-lead corrected valuesWorks better for more radiogenic-Pb
containing samples
1720-18221650+130-140175Ranger
600-1200 1160+680-1010565Roumlssing
5-30lt 640941El Mesquite
1300-13801130+210-740252Cluff Lake
2139 plusmn 1002140+140-150207Blind River
Literature value
Calculated deposit age
(Ma)
Natural 207Pb
content
UOC sample
Age dating using Pb isotopes
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 12
Sr-87Sr-86 Isotope Ratio in the Investigated Uranium Ore Concentrates
06900695070007050710071507200725073007350740
Beverle
y-1 (A
US)Bev
erley-2
(AUS)
Beverle
y-3 (A
US)Bev
erley-4
(AUS)
Ranger
(AUS)
Olympic
Dam (A
US)Key
Lake
(CAN)
Rabbit L
ake (C
AN)Stanro
ck (C
AN)Roumlss
ing (N
AM)
ESI Calg
ary (C
AN)
Sr-8
7Sr
-86
Isot
ope
Rat
io Lower within-mine variability
Overlap
Sr isotopes
Lower between-
mine variability
Precision methods like MC-ICPMS
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 13
Uranium minor isotopes
42E-05
47E-05
52E-05
57E-05
62E-05
67E-05
72E-05
77E-05
82E-05
87E-05
Nam
Ros
sing
Can
Blin
d R
iver
Aus
Oly
mpi
c D
am
Usa
Esi
Can
Esi
Aus
Ran
ger
Can
Eld
orad
o
Swe
Ran
stad
t
Usa
El M
esqu
ite
Aus
Mar
y Ka
thle
en
Usa
Ker
r McG
ee
Can
Sta
nroc
k
SA P
alab
ora
Bra
Nuc
lebr
as
Aus
Rum
Jun
gle
Usa
Hom
esta
ke
Can
Sta
nlei
gh
Aus
Que
ensl
and
Can
Key
Lak
e
Usa
Yan
kee
Yello
w
Can
Far
aday
Usa
Fal
ls C
ity
Can
Mad
awas
ka
Can
Clu
ff La
ke
Cze
Rep
ublic
Aus
Beve
rley
fresh
Aus
Beve
rley
old
Usa
Ana
kond
a
Aus
Rad
ium
Hill
Can
Rio
Alg
om
Can
Den
ison
Usa
Shi
rley
Basi
n
Can
El D
orad
o
Can
Ray
Roc
k
Aus
Sout
h Al
ligat
or
U-2
34U
-238
00E+00
50E-09
10E-08
15E-08
20E-08
25E-08
30E-08
U-2
36U
-238
bull 234U238U ratio varies in nature due to eg the preferential leaching of 234U after α-recoil
bull ldquoHighrdquo 236U abundance most probably a cross-contamination
natural
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 14
bull 143Nd144Nd ratio varies in nature due to the 147Sm 143Nd decaybull natural variation 0510 ndash 0513bull the value depends on the age of the mineral and mineral typebull robust indicator as Nd (like other REE) follows uranium (less prone to
weathering) small within-mine variation
0511 05112 05114 05116 05118 0512 05122 05124 05126
Beverley-1 (AUS)
Beverley-2 (AUS)
Straz (CZ)
Stanrock (CAN)
143Nd144Nd ratio
Neodymium isotope ratio
T12=1061011a
Nd-143 Nd-144 ratio
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 15
REE chemically similar with valence state mainly +3 REE pattern often remain unaltered during metamorphism thusproviding information on the premetamorphic history geologicalbackground and source of the rock The behavior of the valence-variable Ce (+4) and Eu (+2) is alsocharacteristic to the rock and it can be exploited to obtain information on the formation conditions
Rare earth elementsrsquo pattern
REE pattern is less prone to the process
can be used straightforwardly for the origin assessment
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 16
Rare-earth pattern of the investigated uranium ore concentrates
01
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
Cho
ndrit
e no
rmal
ized
con
cent
ratio
n
Beverley-1 (Sandstone)
Beverley-2 (Sandstone)
Beverley-3 (Sandstone)
Beverley-4 (Sandstone)
Ranger (Unconformity)
Olympic Dam (Breccia)
Key Lake (Unconformity)
Stanrock (Quartz-pebble congl)
Roumlssing (Intrusive)
ESI Calgary (Phosphorite)
Sedimentary-type
Quartz-pebbleIntrusive (Euanomaly)
Middle REE enrichment (unconformity-type)
REE patterns
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 17
bull geometry rarr 5 x 5 x 5 cm
bull weight about 24 kg
bull elemental uranium produced around 1943 plusmn 2 years (Haigerloch Germany)
Questions1 What is it 2 Origin of the material 3 etc
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 18
Intended use and origin
Nuclear forensics
bull elemental composition pure U metalunconventional applicationreactor
bull isotopic composition rarr natural U rarrD2O or graphite moderated reactor
bull Age via 234U 230Th590 plusmn 20 years (in 2003)
=gt Date of production second half of 1943
Geometry points at German originbull Open literature
Haigerloch reactor 1945
664 cubes x 24 kg = 15936 kg
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 19
ndash Where is the uranium coming from
Date of Production second half of 1943
Authentic cube
Belgian Congo or Joachimsthal (Czech Republic)
rare earth element pattern
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 20
Samples measured
ndash Haigerloch (ldquoHeisenbergrdquo) uranium cube
ndash Heidelberg (ldquoWirtzrdquo) uranium plates
ndash Yellow cake from Otto Hahnrsquos laboratory in Berlin
ndash For comparisonJoachimsthal uranium ore (bdquohistoricldquo sample)Congo uranium ore
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 21
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
REF
REF
REF
REF
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 22
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
REF
REF
REF
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 23
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
REF
REF
Congo UOC
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 24
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
Ore fromJoachimstalREF
Congo UOC
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 25
Inorganic FT-IR measurement of UOC samplesMeasurement in pellet form using KBrRapid identification of compound (oxide peroxide ADU AUC partially
calcined samples)Detection of certain process-related impurities (sulphate carbonate
nitrate)
Uranium composition in UOCs
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 26
Nitrate (1380 cm-1)Impurity from eluate or back extractant
Sulphate (1130 cm-1)Residual from H2SO4 eluate or back extractant
Uranium composition in UOCs
U-O vibration
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 27
Anion residuals in UOCrsquos
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
20
40
60
80
100
120
140
160
180
200
uScm
Cond
fluor
ide
102
2
2 chlo
ride
02
19
4 5 6 7 nitr
ate
003
6
sulp
hate
479
129
Canada ESI
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
17
18
19
20
21
22
23
24
25
26
uScm
Cond
fluor
ide
036
7
2 3
chlo
ride
55
32
5 brom
ide
-00
26
nitr
ate
012
7
sulp
hate
20
767
9
Australia Radium Hill
Different type of uranium deposits
Different processes for U extraction
Different mineral acids are used
Acid remainings
fluor
ide
chlo
ride
brom
ide
nitr
ate
sulp
hate
fluor
ide
chlo
ride
nitr
ate
sulp
hate
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 28
NO3SO4
0
01
02
03
04
05
06
07
08
09
1
Sout
h Al
ligat
or
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y Ka
thle
en
ESI U
SA
ESI C
anad
a
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Stan
rock
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lake
Mad
awas
ka
Mac
assa
Nor
th S
pan
Milli
ken
Lake
Eldo
rado
Stan
leig
h
FCl
0
05
1
15
2
25
3
35
4
45
5
Sou
th A
lliga
tor
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y K
athl
een
ES
I US
A
ES
I Can
ada
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Sta
nroc
k
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lak
e
Mad
awas
ka
Mac
assa
Nor
th S
pan
Mill
iken
Lak
e
Eld
orad
o
Sta
nlei
gh
Anion ratios
Phosphorite oresQuartz-pebble conglomerate and vein deposits
Nitric acid leaching rArr
Indicator of the processApatite mineral Ca5(PO4)3(FClOH)
rArr Indicator of the deposit type
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 29
Sandstone basal channel Quartz-pebble
conglomerate
Phosphorite
Black shale
Statistical evaluation of UOC data
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 30
U productsbull U ores
bull U ore concentrates
bull U oxide powders
bull UF4 and UF6
bull U pellets
Next step - Vertical study
Aim Identify the impurities that are acquired from or lost in the process What is the effect on the impurities from the source material
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 31
Uranium oreconcentrates
Process stagesamples and reagents
UO3
Next step - Vertical study
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 32
Case study
Backgroundbull uranium raw material of unknown
originbull 2003 Rotterdam (NL)bull Brownish yellow powder ~3 kgbull Found on a shipload from Jordan
Measurements performed at ITUbull NDA analysisbull Isotope ratio measurements (U Sr
Pb)bull Infrared analysisbull Impurity analysisbull REE pattern determination
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 33
Case study
Vibrational Spectrum (Infrared Spectrometry)
bull Compound is AUC xH2Obull Sulfate impurity (from dissolution of starting material)
bullNitrate impurity (from solvent extractionpurification)
Mass Spectrometry
bull Natural uranium isotopic compositionbull Natural lead isotopic composition
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 34
Case study
Sr Isotope Ratio
Low value typical for phosphorites (eg North Africa Middle East UShellip)
070757 plusmn 000011
070814 plusmn 000004
071092 plusmn 000006
071416 plusmn 000011
071985 plusmn 000029
072336 plusmn 000004
073434 plusmn 000012
070785 plusmn 000004
071775 plusmn 000003
067 068 069 070 071 072 073 074 075 076 077 078 079 080
Beverley
Calgary
Key Lake
Olympic Dam
Ranger
Ranstad
Stanrock
Mulberry
Fund-26
87Sr86Sr Isotope RatioSr-87 Sr-86 isotope ratio
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 35
Case study
Age dating based on 234U230Th
Age dating based on 232Th228Th
Last chemical separation 1988 plusmn 5 yndash Applicable to samples with incomplete Th separationndash Complementary to 234U230Th method
Last chemical separation 1893 plusmn 17 y
ndash Measured value shows significant positive biasndash Reason incomplete separation of 230Th from the
parent 234U nuclide(ldquoclock is not set to zerordquo)
ndash Residual 230Th cannot be calculated or corrected for
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 36
Case study ndash Find-26
bull 234U abundance suggests low temperature redox deposit value agrees with data reported by IAEA for UOC from Al Qaim (Iraq)
bull Impurities high P contentsimilar metallic impurities to Iraqi phosphate deposits
bull Pb isotopes natural young deposit low U content in orebull REE pattern flat no Eu or Ce anomaly rarr previously found
in certain sandstone-type and reworked phosphorite
Data inherent to the material corroborate information from external sources
Identification of origin based onSingle sampleMultiple parameters
Identification of origin based onSingle sampleMultiple parameters
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 37
Comparison of relative efforts ndash yellow cake
(5)(5)SIMSU particle analysis(5)Evaluation and Report
MC-ICP-MSMC-ICP-MSICP-MSIR-Spectroscopy RamanIon ChromatographyICP-MS IDMS
Electron Microscopy EDX WDXOptical MicroscopyICP-MSTIMSTitration IDMS
Technique
1853Total
15Nd Isotopes15Sr Isotopes3Rare Earth Elemental pattern1Molecular structure
15Anionic impurities3Age dating
3Micromorphology1Visual inspection macroscopic11Impurities11Isotopic Composition11Element Assay
ForensicsSafeguardsAnalysisParameter
Note rounded figures based on a full cost evaluation figures in brackets are not included in the Total
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 38
Conclusions
Wealth of information inherent to nuclear materialDecrypting the information requires sophisticated methodology subject matter expertise and reference dataSignificant effort (resources and time) needed for comprehensive analysis and data interpretationNuclear forensics methodology may open new avenuesin different areasApplication of investigative techniques in Safeguards has to be evaluated
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 8
U products
bull U ores
bull U ore concentrates (ADU AUC peroxideshellip)
bull U oxide powders
bull UF4 and UF6
bull U pellets
Study on 79 yellow cake samples
Aim Identify the impurities that are significant in relation to the source material (same type of material ndash different geographic origin)
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 9
httpwwwnucleonicanet
U-238 rarrPb-206
U-235 rarrPb-207
Th-232 rarrPb-208
Lead isotopesDecay products of U and Th
High U content rarr high variation of isotope ratios
The isotope composition depends on the history (eg weathering) and age of ore body
Can be easily used for provenance Can be easily used for provenance assessment of the oreassessment of the ore
Lead isotopics
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 10
Lead Isotopic Composition
0 2 4 6 8 10 12 14 16 18
Beverley-1 (AUS)
Beverley-2 (AUS)
Beverley-3 (AUS)
Beverley-4 (AUS)
Ranger (AUS)
Olympic Dam (AUS)
Key Lake (CAN)
Rabbit Lake (CAN)
Stanrock (CAN)
Roumlssing (NAM)
ESI Calgary (CAN)
Isotope Ratio
Pb-207Pb-208Pb-206Pb-208
Overlapping between mines
Relative high within-mine
variation
Applicability and limitationsLarge variation of isotope ratios between mines (radiogenic ratios amp dating)Certain ore types have low 206Pb207Pb ratios (sandstone phosphorite)Relatively high within-mine variationLess applicable for ldquopurerdquo UOCs
Pb isotopes
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 11
Date estimation of the ore on the basis of Pb-Pb method
Using natural-lead corrected valuesWorks better for more radiogenic-Pb
containing samples
1720-18221650+130-140175Ranger
600-1200 1160+680-1010565Roumlssing
5-30lt 640941El Mesquite
1300-13801130+210-740252Cluff Lake
2139 plusmn 1002140+140-150207Blind River
Literature value
Calculated deposit age
(Ma)
Natural 207Pb
content
UOC sample
Age dating using Pb isotopes
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 12
Sr-87Sr-86 Isotope Ratio in the Investigated Uranium Ore Concentrates
06900695070007050710071507200725073007350740
Beverle
y-1 (A
US)Bev
erley-2
(AUS)
Beverle
y-3 (A
US)Bev
erley-4
(AUS)
Ranger
(AUS)
Olympic
Dam (A
US)Key
Lake
(CAN)
Rabbit L
ake (C
AN)Stanro
ck (C
AN)Roumlss
ing (N
AM)
ESI Calg
ary (C
AN)
Sr-8
7Sr
-86
Isot
ope
Rat
io Lower within-mine variability
Overlap
Sr isotopes
Lower between-
mine variability
Precision methods like MC-ICPMS
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 13
Uranium minor isotopes
42E-05
47E-05
52E-05
57E-05
62E-05
67E-05
72E-05
77E-05
82E-05
87E-05
Nam
Ros
sing
Can
Blin
d R
iver
Aus
Oly
mpi
c D
am
Usa
Esi
Can
Esi
Aus
Ran
ger
Can
Eld
orad
o
Swe
Ran
stad
t
Usa
El M
esqu
ite
Aus
Mar
y Ka
thle
en
Usa
Ker
r McG
ee
Can
Sta
nroc
k
SA P
alab
ora
Bra
Nuc
lebr
as
Aus
Rum
Jun
gle
Usa
Hom
esta
ke
Can
Sta
nlei
gh
Aus
Que
ensl
and
Can
Key
Lak
e
Usa
Yan
kee
Yello
w
Can
Far
aday
Usa
Fal
ls C
ity
Can
Mad
awas
ka
Can
Clu
ff La
ke
Cze
Rep
ublic
Aus
Beve
rley
fresh
Aus
Beve
rley
old
Usa
Ana
kond
a
Aus
Rad
ium
Hill
Can
Rio
Alg
om
Can
Den
ison
Usa
Shi
rley
Basi
n
Can
El D
orad
o
Can
Ray
Roc
k
Aus
Sout
h Al
ligat
or
U-2
34U
-238
00E+00
50E-09
10E-08
15E-08
20E-08
25E-08
30E-08
U-2
36U
-238
bull 234U238U ratio varies in nature due to eg the preferential leaching of 234U after α-recoil
bull ldquoHighrdquo 236U abundance most probably a cross-contamination
natural
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 14
bull 143Nd144Nd ratio varies in nature due to the 147Sm 143Nd decaybull natural variation 0510 ndash 0513bull the value depends on the age of the mineral and mineral typebull robust indicator as Nd (like other REE) follows uranium (less prone to
weathering) small within-mine variation
0511 05112 05114 05116 05118 0512 05122 05124 05126
Beverley-1 (AUS)
Beverley-2 (AUS)
Straz (CZ)
Stanrock (CAN)
143Nd144Nd ratio
Neodymium isotope ratio
T12=1061011a
Nd-143 Nd-144 ratio
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 15
REE chemically similar with valence state mainly +3 REE pattern often remain unaltered during metamorphism thusproviding information on the premetamorphic history geologicalbackground and source of the rock The behavior of the valence-variable Ce (+4) and Eu (+2) is alsocharacteristic to the rock and it can be exploited to obtain information on the formation conditions
Rare earth elementsrsquo pattern
REE pattern is less prone to the process
can be used straightforwardly for the origin assessment
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 16
Rare-earth pattern of the investigated uranium ore concentrates
01
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
Cho
ndrit
e no
rmal
ized
con
cent
ratio
n
Beverley-1 (Sandstone)
Beverley-2 (Sandstone)
Beverley-3 (Sandstone)
Beverley-4 (Sandstone)
Ranger (Unconformity)
Olympic Dam (Breccia)
Key Lake (Unconformity)
Stanrock (Quartz-pebble congl)
Roumlssing (Intrusive)
ESI Calgary (Phosphorite)
Sedimentary-type
Quartz-pebbleIntrusive (Euanomaly)
Middle REE enrichment (unconformity-type)
REE patterns
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 17
bull geometry rarr 5 x 5 x 5 cm
bull weight about 24 kg
bull elemental uranium produced around 1943 plusmn 2 years (Haigerloch Germany)
Questions1 What is it 2 Origin of the material 3 etc
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 18
Intended use and origin
Nuclear forensics
bull elemental composition pure U metalunconventional applicationreactor
bull isotopic composition rarr natural U rarrD2O or graphite moderated reactor
bull Age via 234U 230Th590 plusmn 20 years (in 2003)
=gt Date of production second half of 1943
Geometry points at German originbull Open literature
Haigerloch reactor 1945
664 cubes x 24 kg = 15936 kg
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 19
ndash Where is the uranium coming from
Date of Production second half of 1943
Authentic cube
Belgian Congo or Joachimsthal (Czech Republic)
rare earth element pattern
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 20
Samples measured
ndash Haigerloch (ldquoHeisenbergrdquo) uranium cube
ndash Heidelberg (ldquoWirtzrdquo) uranium plates
ndash Yellow cake from Otto Hahnrsquos laboratory in Berlin
ndash For comparisonJoachimsthal uranium ore (bdquohistoricldquo sample)Congo uranium ore
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 21
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
REF
REF
REF
REF
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 22
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
REF
REF
REF
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 23
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
REF
REF
Congo UOC
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 24
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
Ore fromJoachimstalREF
Congo UOC
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 25
Inorganic FT-IR measurement of UOC samplesMeasurement in pellet form using KBrRapid identification of compound (oxide peroxide ADU AUC partially
calcined samples)Detection of certain process-related impurities (sulphate carbonate
nitrate)
Uranium composition in UOCs
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 26
Nitrate (1380 cm-1)Impurity from eluate or back extractant
Sulphate (1130 cm-1)Residual from H2SO4 eluate or back extractant
Uranium composition in UOCs
U-O vibration
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 27
Anion residuals in UOCrsquos
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
20
40
60
80
100
120
140
160
180
200
uScm
Cond
fluor
ide
102
2
2 chlo
ride
02
19
4 5 6 7 nitr
ate
003
6
sulp
hate
479
129
Canada ESI
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
17
18
19
20
21
22
23
24
25
26
uScm
Cond
fluor
ide
036
7
2 3
chlo
ride
55
32
5 brom
ide
-00
26
nitr
ate
012
7
sulp
hate
20
767
9
Australia Radium Hill
Different type of uranium deposits
Different processes for U extraction
Different mineral acids are used
Acid remainings
fluor
ide
chlo
ride
brom
ide
nitr
ate
sulp
hate
fluor
ide
chlo
ride
nitr
ate
sulp
hate
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 28
NO3SO4
0
01
02
03
04
05
06
07
08
09
1
Sout
h Al
ligat
or
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y Ka
thle
en
ESI U
SA
ESI C
anad
a
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Stan
rock
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lake
Mad
awas
ka
Mac
assa
Nor
th S
pan
Milli
ken
Lake
Eldo
rado
Stan
leig
h
FCl
0
05
1
15
2
25
3
35
4
45
5
Sou
th A
lliga
tor
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y K
athl
een
ES
I US
A
ES
I Can
ada
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Sta
nroc
k
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lak
e
Mad
awas
ka
Mac
assa
Nor
th S
pan
Mill
iken
Lak
e
Eld
orad
o
Sta
nlei
gh
Anion ratios
Phosphorite oresQuartz-pebble conglomerate and vein deposits
Nitric acid leaching rArr
Indicator of the processApatite mineral Ca5(PO4)3(FClOH)
rArr Indicator of the deposit type
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 29
Sandstone basal channel Quartz-pebble
conglomerate
Phosphorite
Black shale
Statistical evaluation of UOC data
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 30
U productsbull U ores
bull U ore concentrates
bull U oxide powders
bull UF4 and UF6
bull U pellets
Next step - Vertical study
Aim Identify the impurities that are acquired from or lost in the process What is the effect on the impurities from the source material
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 31
Uranium oreconcentrates
Process stagesamples and reagents
UO3
Next step - Vertical study
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 32
Case study
Backgroundbull uranium raw material of unknown
originbull 2003 Rotterdam (NL)bull Brownish yellow powder ~3 kgbull Found on a shipload from Jordan
Measurements performed at ITUbull NDA analysisbull Isotope ratio measurements (U Sr
Pb)bull Infrared analysisbull Impurity analysisbull REE pattern determination
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 33
Case study
Vibrational Spectrum (Infrared Spectrometry)
bull Compound is AUC xH2Obull Sulfate impurity (from dissolution of starting material)
bullNitrate impurity (from solvent extractionpurification)
Mass Spectrometry
bull Natural uranium isotopic compositionbull Natural lead isotopic composition
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 34
Case study
Sr Isotope Ratio
Low value typical for phosphorites (eg North Africa Middle East UShellip)
070757 plusmn 000011
070814 plusmn 000004
071092 plusmn 000006
071416 plusmn 000011
071985 plusmn 000029
072336 plusmn 000004
073434 plusmn 000012
070785 plusmn 000004
071775 plusmn 000003
067 068 069 070 071 072 073 074 075 076 077 078 079 080
Beverley
Calgary
Key Lake
Olympic Dam
Ranger
Ranstad
Stanrock
Mulberry
Fund-26
87Sr86Sr Isotope RatioSr-87 Sr-86 isotope ratio
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 35
Case study
Age dating based on 234U230Th
Age dating based on 232Th228Th
Last chemical separation 1988 plusmn 5 yndash Applicable to samples with incomplete Th separationndash Complementary to 234U230Th method
Last chemical separation 1893 plusmn 17 y
ndash Measured value shows significant positive biasndash Reason incomplete separation of 230Th from the
parent 234U nuclide(ldquoclock is not set to zerordquo)
ndash Residual 230Th cannot be calculated or corrected for
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 36
Case study ndash Find-26
bull 234U abundance suggests low temperature redox deposit value agrees with data reported by IAEA for UOC from Al Qaim (Iraq)
bull Impurities high P contentsimilar metallic impurities to Iraqi phosphate deposits
bull Pb isotopes natural young deposit low U content in orebull REE pattern flat no Eu or Ce anomaly rarr previously found
in certain sandstone-type and reworked phosphorite
Data inherent to the material corroborate information from external sources
Identification of origin based onSingle sampleMultiple parameters
Identification of origin based onSingle sampleMultiple parameters
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 37
Comparison of relative efforts ndash yellow cake
(5)(5)SIMSU particle analysis(5)Evaluation and Report
MC-ICP-MSMC-ICP-MSICP-MSIR-Spectroscopy RamanIon ChromatographyICP-MS IDMS
Electron Microscopy EDX WDXOptical MicroscopyICP-MSTIMSTitration IDMS
Technique
1853Total
15Nd Isotopes15Sr Isotopes3Rare Earth Elemental pattern1Molecular structure
15Anionic impurities3Age dating
3Micromorphology1Visual inspection macroscopic11Impurities11Isotopic Composition11Element Assay
ForensicsSafeguardsAnalysisParameter
Note rounded figures based on a full cost evaluation figures in brackets are not included in the Total
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 38
Conclusions
Wealth of information inherent to nuclear materialDecrypting the information requires sophisticated methodology subject matter expertise and reference dataSignificant effort (resources and time) needed for comprehensive analysis and data interpretationNuclear forensics methodology may open new avenuesin different areasApplication of investigative techniques in Safeguards has to be evaluated
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 9
httpwwwnucleonicanet
U-238 rarrPb-206
U-235 rarrPb-207
Th-232 rarrPb-208
Lead isotopesDecay products of U and Th
High U content rarr high variation of isotope ratios
The isotope composition depends on the history (eg weathering) and age of ore body
Can be easily used for provenance Can be easily used for provenance assessment of the oreassessment of the ore
Lead isotopics
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 10
Lead Isotopic Composition
0 2 4 6 8 10 12 14 16 18
Beverley-1 (AUS)
Beverley-2 (AUS)
Beverley-3 (AUS)
Beverley-4 (AUS)
Ranger (AUS)
Olympic Dam (AUS)
Key Lake (CAN)
Rabbit Lake (CAN)
Stanrock (CAN)
Roumlssing (NAM)
ESI Calgary (CAN)
Isotope Ratio
Pb-207Pb-208Pb-206Pb-208
Overlapping between mines
Relative high within-mine
variation
Applicability and limitationsLarge variation of isotope ratios between mines (radiogenic ratios amp dating)Certain ore types have low 206Pb207Pb ratios (sandstone phosphorite)Relatively high within-mine variationLess applicable for ldquopurerdquo UOCs
Pb isotopes
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 11
Date estimation of the ore on the basis of Pb-Pb method
Using natural-lead corrected valuesWorks better for more radiogenic-Pb
containing samples
1720-18221650+130-140175Ranger
600-1200 1160+680-1010565Roumlssing
5-30lt 640941El Mesquite
1300-13801130+210-740252Cluff Lake
2139 plusmn 1002140+140-150207Blind River
Literature value
Calculated deposit age
(Ma)
Natural 207Pb
content
UOC sample
Age dating using Pb isotopes
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 12
Sr-87Sr-86 Isotope Ratio in the Investigated Uranium Ore Concentrates
06900695070007050710071507200725073007350740
Beverle
y-1 (A
US)Bev
erley-2
(AUS)
Beverle
y-3 (A
US)Bev
erley-4
(AUS)
Ranger
(AUS)
Olympic
Dam (A
US)Key
Lake
(CAN)
Rabbit L
ake (C
AN)Stanro
ck (C
AN)Roumlss
ing (N
AM)
ESI Calg
ary (C
AN)
Sr-8
7Sr
-86
Isot
ope
Rat
io Lower within-mine variability
Overlap
Sr isotopes
Lower between-
mine variability
Precision methods like MC-ICPMS
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 13
Uranium minor isotopes
42E-05
47E-05
52E-05
57E-05
62E-05
67E-05
72E-05
77E-05
82E-05
87E-05
Nam
Ros
sing
Can
Blin
d R
iver
Aus
Oly
mpi
c D
am
Usa
Esi
Can
Esi
Aus
Ran
ger
Can
Eld
orad
o
Swe
Ran
stad
t
Usa
El M
esqu
ite
Aus
Mar
y Ka
thle
en
Usa
Ker
r McG
ee
Can
Sta
nroc
k
SA P
alab
ora
Bra
Nuc
lebr
as
Aus
Rum
Jun
gle
Usa
Hom
esta
ke
Can
Sta
nlei
gh
Aus
Que
ensl
and
Can
Key
Lak
e
Usa
Yan
kee
Yello
w
Can
Far
aday
Usa
Fal
ls C
ity
Can
Mad
awas
ka
Can
Clu
ff La
ke
Cze
Rep
ublic
Aus
Beve
rley
fresh
Aus
Beve
rley
old
Usa
Ana
kond
a
Aus
Rad
ium
Hill
Can
Rio
Alg
om
Can
Den
ison
Usa
Shi
rley
Basi
n
Can
El D
orad
o
Can
Ray
Roc
k
Aus
Sout
h Al
ligat
or
U-2
34U
-238
00E+00
50E-09
10E-08
15E-08
20E-08
25E-08
30E-08
U-2
36U
-238
bull 234U238U ratio varies in nature due to eg the preferential leaching of 234U after α-recoil
bull ldquoHighrdquo 236U abundance most probably a cross-contamination
natural
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 14
bull 143Nd144Nd ratio varies in nature due to the 147Sm 143Nd decaybull natural variation 0510 ndash 0513bull the value depends on the age of the mineral and mineral typebull robust indicator as Nd (like other REE) follows uranium (less prone to
weathering) small within-mine variation
0511 05112 05114 05116 05118 0512 05122 05124 05126
Beverley-1 (AUS)
Beverley-2 (AUS)
Straz (CZ)
Stanrock (CAN)
143Nd144Nd ratio
Neodymium isotope ratio
T12=1061011a
Nd-143 Nd-144 ratio
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 15
REE chemically similar with valence state mainly +3 REE pattern often remain unaltered during metamorphism thusproviding information on the premetamorphic history geologicalbackground and source of the rock The behavior of the valence-variable Ce (+4) and Eu (+2) is alsocharacteristic to the rock and it can be exploited to obtain information on the formation conditions
Rare earth elementsrsquo pattern
REE pattern is less prone to the process
can be used straightforwardly for the origin assessment
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 16
Rare-earth pattern of the investigated uranium ore concentrates
01
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
Cho
ndrit
e no
rmal
ized
con
cent
ratio
n
Beverley-1 (Sandstone)
Beverley-2 (Sandstone)
Beverley-3 (Sandstone)
Beverley-4 (Sandstone)
Ranger (Unconformity)
Olympic Dam (Breccia)
Key Lake (Unconformity)
Stanrock (Quartz-pebble congl)
Roumlssing (Intrusive)
ESI Calgary (Phosphorite)
Sedimentary-type
Quartz-pebbleIntrusive (Euanomaly)
Middle REE enrichment (unconformity-type)
REE patterns
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 17
bull geometry rarr 5 x 5 x 5 cm
bull weight about 24 kg
bull elemental uranium produced around 1943 plusmn 2 years (Haigerloch Germany)
Questions1 What is it 2 Origin of the material 3 etc
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 18
Intended use and origin
Nuclear forensics
bull elemental composition pure U metalunconventional applicationreactor
bull isotopic composition rarr natural U rarrD2O or graphite moderated reactor
bull Age via 234U 230Th590 plusmn 20 years (in 2003)
=gt Date of production second half of 1943
Geometry points at German originbull Open literature
Haigerloch reactor 1945
664 cubes x 24 kg = 15936 kg
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 19
ndash Where is the uranium coming from
Date of Production second half of 1943
Authentic cube
Belgian Congo or Joachimsthal (Czech Republic)
rare earth element pattern
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 20
Samples measured
ndash Haigerloch (ldquoHeisenbergrdquo) uranium cube
ndash Heidelberg (ldquoWirtzrdquo) uranium plates
ndash Yellow cake from Otto Hahnrsquos laboratory in Berlin
ndash For comparisonJoachimsthal uranium ore (bdquohistoricldquo sample)Congo uranium ore
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 21
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
REF
REF
REF
REF
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 22
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
REF
REF
REF
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 23
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
REF
REF
Congo UOC
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 24
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
Ore fromJoachimstalREF
Congo UOC
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 25
Inorganic FT-IR measurement of UOC samplesMeasurement in pellet form using KBrRapid identification of compound (oxide peroxide ADU AUC partially
calcined samples)Detection of certain process-related impurities (sulphate carbonate
nitrate)
Uranium composition in UOCs
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 26
Nitrate (1380 cm-1)Impurity from eluate or back extractant
Sulphate (1130 cm-1)Residual from H2SO4 eluate or back extractant
Uranium composition in UOCs
U-O vibration
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 27
Anion residuals in UOCrsquos
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
20
40
60
80
100
120
140
160
180
200
uScm
Cond
fluor
ide
102
2
2 chlo
ride
02
19
4 5 6 7 nitr
ate
003
6
sulp
hate
479
129
Canada ESI
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
17
18
19
20
21
22
23
24
25
26
uScm
Cond
fluor
ide
036
7
2 3
chlo
ride
55
32
5 brom
ide
-00
26
nitr
ate
012
7
sulp
hate
20
767
9
Australia Radium Hill
Different type of uranium deposits
Different processes for U extraction
Different mineral acids are used
Acid remainings
fluor
ide
chlo
ride
brom
ide
nitr
ate
sulp
hate
fluor
ide
chlo
ride
nitr
ate
sulp
hate
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 28
NO3SO4
0
01
02
03
04
05
06
07
08
09
1
Sout
h Al
ligat
or
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y Ka
thle
en
ESI U
SA
ESI C
anad
a
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Stan
rock
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lake
Mad
awas
ka
Mac
assa
Nor
th S
pan
Milli
ken
Lake
Eldo
rado
Stan
leig
h
FCl
0
05
1
15
2
25
3
35
4
45
5
Sou
th A
lliga
tor
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y K
athl
een
ES
I US
A
ES
I Can
ada
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Sta
nroc
k
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lak
e
Mad
awas
ka
Mac
assa
Nor
th S
pan
Mill
iken
Lak
e
Eld
orad
o
Sta
nlei
gh
Anion ratios
Phosphorite oresQuartz-pebble conglomerate and vein deposits
Nitric acid leaching rArr
Indicator of the processApatite mineral Ca5(PO4)3(FClOH)
rArr Indicator of the deposit type
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 29
Sandstone basal channel Quartz-pebble
conglomerate
Phosphorite
Black shale
Statistical evaluation of UOC data
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 30
U productsbull U ores
bull U ore concentrates
bull U oxide powders
bull UF4 and UF6
bull U pellets
Next step - Vertical study
Aim Identify the impurities that are acquired from or lost in the process What is the effect on the impurities from the source material
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 31
Uranium oreconcentrates
Process stagesamples and reagents
UO3
Next step - Vertical study
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 32
Case study
Backgroundbull uranium raw material of unknown
originbull 2003 Rotterdam (NL)bull Brownish yellow powder ~3 kgbull Found on a shipload from Jordan
Measurements performed at ITUbull NDA analysisbull Isotope ratio measurements (U Sr
Pb)bull Infrared analysisbull Impurity analysisbull REE pattern determination
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 33
Case study
Vibrational Spectrum (Infrared Spectrometry)
bull Compound is AUC xH2Obull Sulfate impurity (from dissolution of starting material)
bullNitrate impurity (from solvent extractionpurification)
Mass Spectrometry
bull Natural uranium isotopic compositionbull Natural lead isotopic composition
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 34
Case study
Sr Isotope Ratio
Low value typical for phosphorites (eg North Africa Middle East UShellip)
070757 plusmn 000011
070814 plusmn 000004
071092 plusmn 000006
071416 plusmn 000011
071985 plusmn 000029
072336 plusmn 000004
073434 plusmn 000012
070785 plusmn 000004
071775 plusmn 000003
067 068 069 070 071 072 073 074 075 076 077 078 079 080
Beverley
Calgary
Key Lake
Olympic Dam
Ranger
Ranstad
Stanrock
Mulberry
Fund-26
87Sr86Sr Isotope RatioSr-87 Sr-86 isotope ratio
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 35
Case study
Age dating based on 234U230Th
Age dating based on 232Th228Th
Last chemical separation 1988 plusmn 5 yndash Applicable to samples with incomplete Th separationndash Complementary to 234U230Th method
Last chemical separation 1893 plusmn 17 y
ndash Measured value shows significant positive biasndash Reason incomplete separation of 230Th from the
parent 234U nuclide(ldquoclock is not set to zerordquo)
ndash Residual 230Th cannot be calculated or corrected for
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 36
Case study ndash Find-26
bull 234U abundance suggests low temperature redox deposit value agrees with data reported by IAEA for UOC from Al Qaim (Iraq)
bull Impurities high P contentsimilar metallic impurities to Iraqi phosphate deposits
bull Pb isotopes natural young deposit low U content in orebull REE pattern flat no Eu or Ce anomaly rarr previously found
in certain sandstone-type and reworked phosphorite
Data inherent to the material corroborate information from external sources
Identification of origin based onSingle sampleMultiple parameters
Identification of origin based onSingle sampleMultiple parameters
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 37
Comparison of relative efforts ndash yellow cake
(5)(5)SIMSU particle analysis(5)Evaluation and Report
MC-ICP-MSMC-ICP-MSICP-MSIR-Spectroscopy RamanIon ChromatographyICP-MS IDMS
Electron Microscopy EDX WDXOptical MicroscopyICP-MSTIMSTitration IDMS
Technique
1853Total
15Nd Isotopes15Sr Isotopes3Rare Earth Elemental pattern1Molecular structure
15Anionic impurities3Age dating
3Micromorphology1Visual inspection macroscopic11Impurities11Isotopic Composition11Element Assay
ForensicsSafeguardsAnalysisParameter
Note rounded figures based on a full cost evaluation figures in brackets are not included in the Total
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 38
Conclusions
Wealth of information inherent to nuclear materialDecrypting the information requires sophisticated methodology subject matter expertise and reference dataSignificant effort (resources and time) needed for comprehensive analysis and data interpretationNuclear forensics methodology may open new avenuesin different areasApplication of investigative techniques in Safeguards has to be evaluated
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 10
Lead Isotopic Composition
0 2 4 6 8 10 12 14 16 18
Beverley-1 (AUS)
Beverley-2 (AUS)
Beverley-3 (AUS)
Beverley-4 (AUS)
Ranger (AUS)
Olympic Dam (AUS)
Key Lake (CAN)
Rabbit Lake (CAN)
Stanrock (CAN)
Roumlssing (NAM)
ESI Calgary (CAN)
Isotope Ratio
Pb-207Pb-208Pb-206Pb-208
Overlapping between mines
Relative high within-mine
variation
Applicability and limitationsLarge variation of isotope ratios between mines (radiogenic ratios amp dating)Certain ore types have low 206Pb207Pb ratios (sandstone phosphorite)Relatively high within-mine variationLess applicable for ldquopurerdquo UOCs
Pb isotopes
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 11
Date estimation of the ore on the basis of Pb-Pb method
Using natural-lead corrected valuesWorks better for more radiogenic-Pb
containing samples
1720-18221650+130-140175Ranger
600-1200 1160+680-1010565Roumlssing
5-30lt 640941El Mesquite
1300-13801130+210-740252Cluff Lake
2139 plusmn 1002140+140-150207Blind River
Literature value
Calculated deposit age
(Ma)
Natural 207Pb
content
UOC sample
Age dating using Pb isotopes
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 12
Sr-87Sr-86 Isotope Ratio in the Investigated Uranium Ore Concentrates
06900695070007050710071507200725073007350740
Beverle
y-1 (A
US)Bev
erley-2
(AUS)
Beverle
y-3 (A
US)Bev
erley-4
(AUS)
Ranger
(AUS)
Olympic
Dam (A
US)Key
Lake
(CAN)
Rabbit L
ake (C
AN)Stanro
ck (C
AN)Roumlss
ing (N
AM)
ESI Calg
ary (C
AN)
Sr-8
7Sr
-86
Isot
ope
Rat
io Lower within-mine variability
Overlap
Sr isotopes
Lower between-
mine variability
Precision methods like MC-ICPMS
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 13
Uranium minor isotopes
42E-05
47E-05
52E-05
57E-05
62E-05
67E-05
72E-05
77E-05
82E-05
87E-05
Nam
Ros
sing
Can
Blin
d R
iver
Aus
Oly
mpi
c D
am
Usa
Esi
Can
Esi
Aus
Ran
ger
Can
Eld
orad
o
Swe
Ran
stad
t
Usa
El M
esqu
ite
Aus
Mar
y Ka
thle
en
Usa
Ker
r McG
ee
Can
Sta
nroc
k
SA P
alab
ora
Bra
Nuc
lebr
as
Aus
Rum
Jun
gle
Usa
Hom
esta
ke
Can
Sta
nlei
gh
Aus
Que
ensl
and
Can
Key
Lak
e
Usa
Yan
kee
Yello
w
Can
Far
aday
Usa
Fal
ls C
ity
Can
Mad
awas
ka
Can
Clu
ff La
ke
Cze
Rep
ublic
Aus
Beve
rley
fresh
Aus
Beve
rley
old
Usa
Ana
kond
a
Aus
Rad
ium
Hill
Can
Rio
Alg
om
Can
Den
ison
Usa
Shi
rley
Basi
n
Can
El D
orad
o
Can
Ray
Roc
k
Aus
Sout
h Al
ligat
or
U-2
34U
-238
00E+00
50E-09
10E-08
15E-08
20E-08
25E-08
30E-08
U-2
36U
-238
bull 234U238U ratio varies in nature due to eg the preferential leaching of 234U after α-recoil
bull ldquoHighrdquo 236U abundance most probably a cross-contamination
natural
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 14
bull 143Nd144Nd ratio varies in nature due to the 147Sm 143Nd decaybull natural variation 0510 ndash 0513bull the value depends on the age of the mineral and mineral typebull robust indicator as Nd (like other REE) follows uranium (less prone to
weathering) small within-mine variation
0511 05112 05114 05116 05118 0512 05122 05124 05126
Beverley-1 (AUS)
Beverley-2 (AUS)
Straz (CZ)
Stanrock (CAN)
143Nd144Nd ratio
Neodymium isotope ratio
T12=1061011a
Nd-143 Nd-144 ratio
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 15
REE chemically similar with valence state mainly +3 REE pattern often remain unaltered during metamorphism thusproviding information on the premetamorphic history geologicalbackground and source of the rock The behavior of the valence-variable Ce (+4) and Eu (+2) is alsocharacteristic to the rock and it can be exploited to obtain information on the formation conditions
Rare earth elementsrsquo pattern
REE pattern is less prone to the process
can be used straightforwardly for the origin assessment
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 16
Rare-earth pattern of the investigated uranium ore concentrates
01
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
Cho
ndrit
e no
rmal
ized
con
cent
ratio
n
Beverley-1 (Sandstone)
Beverley-2 (Sandstone)
Beverley-3 (Sandstone)
Beverley-4 (Sandstone)
Ranger (Unconformity)
Olympic Dam (Breccia)
Key Lake (Unconformity)
Stanrock (Quartz-pebble congl)
Roumlssing (Intrusive)
ESI Calgary (Phosphorite)
Sedimentary-type
Quartz-pebbleIntrusive (Euanomaly)
Middle REE enrichment (unconformity-type)
REE patterns
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 17
bull geometry rarr 5 x 5 x 5 cm
bull weight about 24 kg
bull elemental uranium produced around 1943 plusmn 2 years (Haigerloch Germany)
Questions1 What is it 2 Origin of the material 3 etc
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 18
Intended use and origin
Nuclear forensics
bull elemental composition pure U metalunconventional applicationreactor
bull isotopic composition rarr natural U rarrD2O or graphite moderated reactor
bull Age via 234U 230Th590 plusmn 20 years (in 2003)
=gt Date of production second half of 1943
Geometry points at German originbull Open literature
Haigerloch reactor 1945
664 cubes x 24 kg = 15936 kg
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 19
ndash Where is the uranium coming from
Date of Production second half of 1943
Authentic cube
Belgian Congo or Joachimsthal (Czech Republic)
rare earth element pattern
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 20
Samples measured
ndash Haigerloch (ldquoHeisenbergrdquo) uranium cube
ndash Heidelberg (ldquoWirtzrdquo) uranium plates
ndash Yellow cake from Otto Hahnrsquos laboratory in Berlin
ndash For comparisonJoachimsthal uranium ore (bdquohistoricldquo sample)Congo uranium ore
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 21
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
REF
REF
REF
REF
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 22
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
REF
REF
REF
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 23
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
REF
REF
Congo UOC
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 24
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
Ore fromJoachimstalREF
Congo UOC
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 25
Inorganic FT-IR measurement of UOC samplesMeasurement in pellet form using KBrRapid identification of compound (oxide peroxide ADU AUC partially
calcined samples)Detection of certain process-related impurities (sulphate carbonate
nitrate)
Uranium composition in UOCs
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 26
Nitrate (1380 cm-1)Impurity from eluate or back extractant
Sulphate (1130 cm-1)Residual from H2SO4 eluate or back extractant
Uranium composition in UOCs
U-O vibration
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 27
Anion residuals in UOCrsquos
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
20
40
60
80
100
120
140
160
180
200
uScm
Cond
fluor
ide
102
2
2 chlo
ride
02
19
4 5 6 7 nitr
ate
003
6
sulp
hate
479
129
Canada ESI
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
17
18
19
20
21
22
23
24
25
26
uScm
Cond
fluor
ide
036
7
2 3
chlo
ride
55
32
5 brom
ide
-00
26
nitr
ate
012
7
sulp
hate
20
767
9
Australia Radium Hill
Different type of uranium deposits
Different processes for U extraction
Different mineral acids are used
Acid remainings
fluor
ide
chlo
ride
brom
ide
nitr
ate
sulp
hate
fluor
ide
chlo
ride
nitr
ate
sulp
hate
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 28
NO3SO4
0
01
02
03
04
05
06
07
08
09
1
Sout
h Al
ligat
or
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y Ka
thle
en
ESI U
SA
ESI C
anad
a
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Stan
rock
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lake
Mad
awas
ka
Mac
assa
Nor
th S
pan
Milli
ken
Lake
Eldo
rado
Stan
leig
h
FCl
0
05
1
15
2
25
3
35
4
45
5
Sou
th A
lliga
tor
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y K
athl
een
ES
I US
A
ES
I Can
ada
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Sta
nroc
k
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lak
e
Mad
awas
ka
Mac
assa
Nor
th S
pan
Mill
iken
Lak
e
Eld
orad
o
Sta
nlei
gh
Anion ratios
Phosphorite oresQuartz-pebble conglomerate and vein deposits
Nitric acid leaching rArr
Indicator of the processApatite mineral Ca5(PO4)3(FClOH)
rArr Indicator of the deposit type
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 29
Sandstone basal channel Quartz-pebble
conglomerate
Phosphorite
Black shale
Statistical evaluation of UOC data
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 30
U productsbull U ores
bull U ore concentrates
bull U oxide powders
bull UF4 and UF6
bull U pellets
Next step - Vertical study
Aim Identify the impurities that are acquired from or lost in the process What is the effect on the impurities from the source material
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 31
Uranium oreconcentrates
Process stagesamples and reagents
UO3
Next step - Vertical study
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 32
Case study
Backgroundbull uranium raw material of unknown
originbull 2003 Rotterdam (NL)bull Brownish yellow powder ~3 kgbull Found on a shipload from Jordan
Measurements performed at ITUbull NDA analysisbull Isotope ratio measurements (U Sr
Pb)bull Infrared analysisbull Impurity analysisbull REE pattern determination
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 33
Case study
Vibrational Spectrum (Infrared Spectrometry)
bull Compound is AUC xH2Obull Sulfate impurity (from dissolution of starting material)
bullNitrate impurity (from solvent extractionpurification)
Mass Spectrometry
bull Natural uranium isotopic compositionbull Natural lead isotopic composition
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 34
Case study
Sr Isotope Ratio
Low value typical for phosphorites (eg North Africa Middle East UShellip)
070757 plusmn 000011
070814 plusmn 000004
071092 plusmn 000006
071416 plusmn 000011
071985 plusmn 000029
072336 plusmn 000004
073434 plusmn 000012
070785 plusmn 000004
071775 plusmn 000003
067 068 069 070 071 072 073 074 075 076 077 078 079 080
Beverley
Calgary
Key Lake
Olympic Dam
Ranger
Ranstad
Stanrock
Mulberry
Fund-26
87Sr86Sr Isotope RatioSr-87 Sr-86 isotope ratio
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 35
Case study
Age dating based on 234U230Th
Age dating based on 232Th228Th
Last chemical separation 1988 plusmn 5 yndash Applicable to samples with incomplete Th separationndash Complementary to 234U230Th method
Last chemical separation 1893 plusmn 17 y
ndash Measured value shows significant positive biasndash Reason incomplete separation of 230Th from the
parent 234U nuclide(ldquoclock is not set to zerordquo)
ndash Residual 230Th cannot be calculated or corrected for
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 36
Case study ndash Find-26
bull 234U abundance suggests low temperature redox deposit value agrees with data reported by IAEA for UOC from Al Qaim (Iraq)
bull Impurities high P contentsimilar metallic impurities to Iraqi phosphate deposits
bull Pb isotopes natural young deposit low U content in orebull REE pattern flat no Eu or Ce anomaly rarr previously found
in certain sandstone-type and reworked phosphorite
Data inherent to the material corroborate information from external sources
Identification of origin based onSingle sampleMultiple parameters
Identification of origin based onSingle sampleMultiple parameters
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 37
Comparison of relative efforts ndash yellow cake
(5)(5)SIMSU particle analysis(5)Evaluation and Report
MC-ICP-MSMC-ICP-MSICP-MSIR-Spectroscopy RamanIon ChromatographyICP-MS IDMS
Electron Microscopy EDX WDXOptical MicroscopyICP-MSTIMSTitration IDMS
Technique
1853Total
15Nd Isotopes15Sr Isotopes3Rare Earth Elemental pattern1Molecular structure
15Anionic impurities3Age dating
3Micromorphology1Visual inspection macroscopic11Impurities11Isotopic Composition11Element Assay
ForensicsSafeguardsAnalysisParameter
Note rounded figures based on a full cost evaluation figures in brackets are not included in the Total
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 38
Conclusions
Wealth of information inherent to nuclear materialDecrypting the information requires sophisticated methodology subject matter expertise and reference dataSignificant effort (resources and time) needed for comprehensive analysis and data interpretationNuclear forensics methodology may open new avenuesin different areasApplication of investigative techniques in Safeguards has to be evaluated
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 11
Date estimation of the ore on the basis of Pb-Pb method
Using natural-lead corrected valuesWorks better for more radiogenic-Pb
containing samples
1720-18221650+130-140175Ranger
600-1200 1160+680-1010565Roumlssing
5-30lt 640941El Mesquite
1300-13801130+210-740252Cluff Lake
2139 plusmn 1002140+140-150207Blind River
Literature value
Calculated deposit age
(Ma)
Natural 207Pb
content
UOC sample
Age dating using Pb isotopes
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 12
Sr-87Sr-86 Isotope Ratio in the Investigated Uranium Ore Concentrates
06900695070007050710071507200725073007350740
Beverle
y-1 (A
US)Bev
erley-2
(AUS)
Beverle
y-3 (A
US)Bev
erley-4
(AUS)
Ranger
(AUS)
Olympic
Dam (A
US)Key
Lake
(CAN)
Rabbit L
ake (C
AN)Stanro
ck (C
AN)Roumlss
ing (N
AM)
ESI Calg
ary (C
AN)
Sr-8
7Sr
-86
Isot
ope
Rat
io Lower within-mine variability
Overlap
Sr isotopes
Lower between-
mine variability
Precision methods like MC-ICPMS
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 13
Uranium minor isotopes
42E-05
47E-05
52E-05
57E-05
62E-05
67E-05
72E-05
77E-05
82E-05
87E-05
Nam
Ros
sing
Can
Blin
d R
iver
Aus
Oly
mpi
c D
am
Usa
Esi
Can
Esi
Aus
Ran
ger
Can
Eld
orad
o
Swe
Ran
stad
t
Usa
El M
esqu
ite
Aus
Mar
y Ka
thle
en
Usa
Ker
r McG
ee
Can
Sta
nroc
k
SA P
alab
ora
Bra
Nuc
lebr
as
Aus
Rum
Jun
gle
Usa
Hom
esta
ke
Can
Sta
nlei
gh
Aus
Que
ensl
and
Can
Key
Lak
e
Usa
Yan
kee
Yello
w
Can
Far
aday
Usa
Fal
ls C
ity
Can
Mad
awas
ka
Can
Clu
ff La
ke
Cze
Rep
ublic
Aus
Beve
rley
fresh
Aus
Beve
rley
old
Usa
Ana
kond
a
Aus
Rad
ium
Hill
Can
Rio
Alg
om
Can
Den
ison
Usa
Shi
rley
Basi
n
Can
El D
orad
o
Can
Ray
Roc
k
Aus
Sout
h Al
ligat
or
U-2
34U
-238
00E+00
50E-09
10E-08
15E-08
20E-08
25E-08
30E-08
U-2
36U
-238
bull 234U238U ratio varies in nature due to eg the preferential leaching of 234U after α-recoil
bull ldquoHighrdquo 236U abundance most probably a cross-contamination
natural
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 14
bull 143Nd144Nd ratio varies in nature due to the 147Sm 143Nd decaybull natural variation 0510 ndash 0513bull the value depends on the age of the mineral and mineral typebull robust indicator as Nd (like other REE) follows uranium (less prone to
weathering) small within-mine variation
0511 05112 05114 05116 05118 0512 05122 05124 05126
Beverley-1 (AUS)
Beverley-2 (AUS)
Straz (CZ)
Stanrock (CAN)
143Nd144Nd ratio
Neodymium isotope ratio
T12=1061011a
Nd-143 Nd-144 ratio
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 15
REE chemically similar with valence state mainly +3 REE pattern often remain unaltered during metamorphism thusproviding information on the premetamorphic history geologicalbackground and source of the rock The behavior of the valence-variable Ce (+4) and Eu (+2) is alsocharacteristic to the rock and it can be exploited to obtain information on the formation conditions
Rare earth elementsrsquo pattern
REE pattern is less prone to the process
can be used straightforwardly for the origin assessment
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 16
Rare-earth pattern of the investigated uranium ore concentrates
01
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
Cho
ndrit
e no
rmal
ized
con
cent
ratio
n
Beverley-1 (Sandstone)
Beverley-2 (Sandstone)
Beverley-3 (Sandstone)
Beverley-4 (Sandstone)
Ranger (Unconformity)
Olympic Dam (Breccia)
Key Lake (Unconformity)
Stanrock (Quartz-pebble congl)
Roumlssing (Intrusive)
ESI Calgary (Phosphorite)
Sedimentary-type
Quartz-pebbleIntrusive (Euanomaly)
Middle REE enrichment (unconformity-type)
REE patterns
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 17
bull geometry rarr 5 x 5 x 5 cm
bull weight about 24 kg
bull elemental uranium produced around 1943 plusmn 2 years (Haigerloch Germany)
Questions1 What is it 2 Origin of the material 3 etc
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 18
Intended use and origin
Nuclear forensics
bull elemental composition pure U metalunconventional applicationreactor
bull isotopic composition rarr natural U rarrD2O or graphite moderated reactor
bull Age via 234U 230Th590 plusmn 20 years (in 2003)
=gt Date of production second half of 1943
Geometry points at German originbull Open literature
Haigerloch reactor 1945
664 cubes x 24 kg = 15936 kg
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 19
ndash Where is the uranium coming from
Date of Production second half of 1943
Authentic cube
Belgian Congo or Joachimsthal (Czech Republic)
rare earth element pattern
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 20
Samples measured
ndash Haigerloch (ldquoHeisenbergrdquo) uranium cube
ndash Heidelberg (ldquoWirtzrdquo) uranium plates
ndash Yellow cake from Otto Hahnrsquos laboratory in Berlin
ndash For comparisonJoachimsthal uranium ore (bdquohistoricldquo sample)Congo uranium ore
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 21
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
REF
REF
REF
REF
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 22
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
REF
REF
REF
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 23
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
REF
REF
Congo UOC
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 24
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
Ore fromJoachimstalREF
Congo UOC
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 25
Inorganic FT-IR measurement of UOC samplesMeasurement in pellet form using KBrRapid identification of compound (oxide peroxide ADU AUC partially
calcined samples)Detection of certain process-related impurities (sulphate carbonate
nitrate)
Uranium composition in UOCs
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 26
Nitrate (1380 cm-1)Impurity from eluate or back extractant
Sulphate (1130 cm-1)Residual from H2SO4 eluate or back extractant
Uranium composition in UOCs
U-O vibration
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 27
Anion residuals in UOCrsquos
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
20
40
60
80
100
120
140
160
180
200
uScm
Cond
fluor
ide
102
2
2 chlo
ride
02
19
4 5 6 7 nitr
ate
003
6
sulp
hate
479
129
Canada ESI
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
17
18
19
20
21
22
23
24
25
26
uScm
Cond
fluor
ide
036
7
2 3
chlo
ride
55
32
5 brom
ide
-00
26
nitr
ate
012
7
sulp
hate
20
767
9
Australia Radium Hill
Different type of uranium deposits
Different processes for U extraction
Different mineral acids are used
Acid remainings
fluor
ide
chlo
ride
brom
ide
nitr
ate
sulp
hate
fluor
ide
chlo
ride
nitr
ate
sulp
hate
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 28
NO3SO4
0
01
02
03
04
05
06
07
08
09
1
Sout
h Al
ligat
or
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y Ka
thle
en
ESI U
SA
ESI C
anad
a
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Stan
rock
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lake
Mad
awas
ka
Mac
assa
Nor
th S
pan
Milli
ken
Lake
Eldo
rado
Stan
leig
h
FCl
0
05
1
15
2
25
3
35
4
45
5
Sou
th A
lliga
tor
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y K
athl
een
ES
I US
A
ES
I Can
ada
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Sta
nroc
k
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lak
e
Mad
awas
ka
Mac
assa
Nor
th S
pan
Mill
iken
Lak
e
Eld
orad
o
Sta
nlei
gh
Anion ratios
Phosphorite oresQuartz-pebble conglomerate and vein deposits
Nitric acid leaching rArr
Indicator of the processApatite mineral Ca5(PO4)3(FClOH)
rArr Indicator of the deposit type
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 29
Sandstone basal channel Quartz-pebble
conglomerate
Phosphorite
Black shale
Statistical evaluation of UOC data
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 30
U productsbull U ores
bull U ore concentrates
bull U oxide powders
bull UF4 and UF6
bull U pellets
Next step - Vertical study
Aim Identify the impurities that are acquired from or lost in the process What is the effect on the impurities from the source material
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 31
Uranium oreconcentrates
Process stagesamples and reagents
UO3
Next step - Vertical study
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 32
Case study
Backgroundbull uranium raw material of unknown
originbull 2003 Rotterdam (NL)bull Brownish yellow powder ~3 kgbull Found on a shipload from Jordan
Measurements performed at ITUbull NDA analysisbull Isotope ratio measurements (U Sr
Pb)bull Infrared analysisbull Impurity analysisbull REE pattern determination
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 33
Case study
Vibrational Spectrum (Infrared Spectrometry)
bull Compound is AUC xH2Obull Sulfate impurity (from dissolution of starting material)
bullNitrate impurity (from solvent extractionpurification)
Mass Spectrometry
bull Natural uranium isotopic compositionbull Natural lead isotopic composition
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 34
Case study
Sr Isotope Ratio
Low value typical for phosphorites (eg North Africa Middle East UShellip)
070757 plusmn 000011
070814 plusmn 000004
071092 plusmn 000006
071416 plusmn 000011
071985 plusmn 000029
072336 plusmn 000004
073434 plusmn 000012
070785 plusmn 000004
071775 plusmn 000003
067 068 069 070 071 072 073 074 075 076 077 078 079 080
Beverley
Calgary
Key Lake
Olympic Dam
Ranger
Ranstad
Stanrock
Mulberry
Fund-26
87Sr86Sr Isotope RatioSr-87 Sr-86 isotope ratio
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 35
Case study
Age dating based on 234U230Th
Age dating based on 232Th228Th
Last chemical separation 1988 plusmn 5 yndash Applicable to samples with incomplete Th separationndash Complementary to 234U230Th method
Last chemical separation 1893 plusmn 17 y
ndash Measured value shows significant positive biasndash Reason incomplete separation of 230Th from the
parent 234U nuclide(ldquoclock is not set to zerordquo)
ndash Residual 230Th cannot be calculated or corrected for
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 36
Case study ndash Find-26
bull 234U abundance suggests low temperature redox deposit value agrees with data reported by IAEA for UOC from Al Qaim (Iraq)
bull Impurities high P contentsimilar metallic impurities to Iraqi phosphate deposits
bull Pb isotopes natural young deposit low U content in orebull REE pattern flat no Eu or Ce anomaly rarr previously found
in certain sandstone-type and reworked phosphorite
Data inherent to the material corroborate information from external sources
Identification of origin based onSingle sampleMultiple parameters
Identification of origin based onSingle sampleMultiple parameters
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 37
Comparison of relative efforts ndash yellow cake
(5)(5)SIMSU particle analysis(5)Evaluation and Report
MC-ICP-MSMC-ICP-MSICP-MSIR-Spectroscopy RamanIon ChromatographyICP-MS IDMS
Electron Microscopy EDX WDXOptical MicroscopyICP-MSTIMSTitration IDMS
Technique
1853Total
15Nd Isotopes15Sr Isotopes3Rare Earth Elemental pattern1Molecular structure
15Anionic impurities3Age dating
3Micromorphology1Visual inspection macroscopic11Impurities11Isotopic Composition11Element Assay
ForensicsSafeguardsAnalysisParameter
Note rounded figures based on a full cost evaluation figures in brackets are not included in the Total
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 38
Conclusions
Wealth of information inherent to nuclear materialDecrypting the information requires sophisticated methodology subject matter expertise and reference dataSignificant effort (resources and time) needed for comprehensive analysis and data interpretationNuclear forensics methodology may open new avenuesin different areasApplication of investigative techniques in Safeguards has to be evaluated
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 12
Sr-87Sr-86 Isotope Ratio in the Investigated Uranium Ore Concentrates
06900695070007050710071507200725073007350740
Beverle
y-1 (A
US)Bev
erley-2
(AUS)
Beverle
y-3 (A
US)Bev
erley-4
(AUS)
Ranger
(AUS)
Olympic
Dam (A
US)Key
Lake
(CAN)
Rabbit L
ake (C
AN)Stanro
ck (C
AN)Roumlss
ing (N
AM)
ESI Calg
ary (C
AN)
Sr-8
7Sr
-86
Isot
ope
Rat
io Lower within-mine variability
Overlap
Sr isotopes
Lower between-
mine variability
Precision methods like MC-ICPMS
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 13
Uranium minor isotopes
42E-05
47E-05
52E-05
57E-05
62E-05
67E-05
72E-05
77E-05
82E-05
87E-05
Nam
Ros
sing
Can
Blin
d R
iver
Aus
Oly
mpi
c D
am
Usa
Esi
Can
Esi
Aus
Ran
ger
Can
Eld
orad
o
Swe
Ran
stad
t
Usa
El M
esqu
ite
Aus
Mar
y Ka
thle
en
Usa
Ker
r McG
ee
Can
Sta
nroc
k
SA P
alab
ora
Bra
Nuc
lebr
as
Aus
Rum
Jun
gle
Usa
Hom
esta
ke
Can
Sta
nlei
gh
Aus
Que
ensl
and
Can
Key
Lak
e
Usa
Yan
kee
Yello
w
Can
Far
aday
Usa
Fal
ls C
ity
Can
Mad
awas
ka
Can
Clu
ff La
ke
Cze
Rep
ublic
Aus
Beve
rley
fresh
Aus
Beve
rley
old
Usa
Ana
kond
a
Aus
Rad
ium
Hill
Can
Rio
Alg
om
Can
Den
ison
Usa
Shi
rley
Basi
n
Can
El D
orad
o
Can
Ray
Roc
k
Aus
Sout
h Al
ligat
or
U-2
34U
-238
00E+00
50E-09
10E-08
15E-08
20E-08
25E-08
30E-08
U-2
36U
-238
bull 234U238U ratio varies in nature due to eg the preferential leaching of 234U after α-recoil
bull ldquoHighrdquo 236U abundance most probably a cross-contamination
natural
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 14
bull 143Nd144Nd ratio varies in nature due to the 147Sm 143Nd decaybull natural variation 0510 ndash 0513bull the value depends on the age of the mineral and mineral typebull robust indicator as Nd (like other REE) follows uranium (less prone to
weathering) small within-mine variation
0511 05112 05114 05116 05118 0512 05122 05124 05126
Beverley-1 (AUS)
Beverley-2 (AUS)
Straz (CZ)
Stanrock (CAN)
143Nd144Nd ratio
Neodymium isotope ratio
T12=1061011a
Nd-143 Nd-144 ratio
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 15
REE chemically similar with valence state mainly +3 REE pattern often remain unaltered during metamorphism thusproviding information on the premetamorphic history geologicalbackground and source of the rock The behavior of the valence-variable Ce (+4) and Eu (+2) is alsocharacteristic to the rock and it can be exploited to obtain information on the formation conditions
Rare earth elementsrsquo pattern
REE pattern is less prone to the process
can be used straightforwardly for the origin assessment
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 16
Rare-earth pattern of the investigated uranium ore concentrates
01
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
Cho
ndrit
e no
rmal
ized
con
cent
ratio
n
Beverley-1 (Sandstone)
Beverley-2 (Sandstone)
Beverley-3 (Sandstone)
Beverley-4 (Sandstone)
Ranger (Unconformity)
Olympic Dam (Breccia)
Key Lake (Unconformity)
Stanrock (Quartz-pebble congl)
Roumlssing (Intrusive)
ESI Calgary (Phosphorite)
Sedimentary-type
Quartz-pebbleIntrusive (Euanomaly)
Middle REE enrichment (unconformity-type)
REE patterns
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 17
bull geometry rarr 5 x 5 x 5 cm
bull weight about 24 kg
bull elemental uranium produced around 1943 plusmn 2 years (Haigerloch Germany)
Questions1 What is it 2 Origin of the material 3 etc
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 18
Intended use and origin
Nuclear forensics
bull elemental composition pure U metalunconventional applicationreactor
bull isotopic composition rarr natural U rarrD2O or graphite moderated reactor
bull Age via 234U 230Th590 plusmn 20 years (in 2003)
=gt Date of production second half of 1943
Geometry points at German originbull Open literature
Haigerloch reactor 1945
664 cubes x 24 kg = 15936 kg
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 19
ndash Where is the uranium coming from
Date of Production second half of 1943
Authentic cube
Belgian Congo or Joachimsthal (Czech Republic)
rare earth element pattern
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 20
Samples measured
ndash Haigerloch (ldquoHeisenbergrdquo) uranium cube
ndash Heidelberg (ldquoWirtzrdquo) uranium plates
ndash Yellow cake from Otto Hahnrsquos laboratory in Berlin
ndash For comparisonJoachimsthal uranium ore (bdquohistoricldquo sample)Congo uranium ore
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 21
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
REF
REF
REF
REF
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 22
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
REF
REF
REF
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 23
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
REF
REF
Congo UOC
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 24
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
Ore fromJoachimstalREF
Congo UOC
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 25
Inorganic FT-IR measurement of UOC samplesMeasurement in pellet form using KBrRapid identification of compound (oxide peroxide ADU AUC partially
calcined samples)Detection of certain process-related impurities (sulphate carbonate
nitrate)
Uranium composition in UOCs
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 26
Nitrate (1380 cm-1)Impurity from eluate or back extractant
Sulphate (1130 cm-1)Residual from H2SO4 eluate or back extractant
Uranium composition in UOCs
U-O vibration
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 27
Anion residuals in UOCrsquos
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
20
40
60
80
100
120
140
160
180
200
uScm
Cond
fluor
ide
102
2
2 chlo
ride
02
19
4 5 6 7 nitr
ate
003
6
sulp
hate
479
129
Canada ESI
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
17
18
19
20
21
22
23
24
25
26
uScm
Cond
fluor
ide
036
7
2 3
chlo
ride
55
32
5 brom
ide
-00
26
nitr
ate
012
7
sulp
hate
20
767
9
Australia Radium Hill
Different type of uranium deposits
Different processes for U extraction
Different mineral acids are used
Acid remainings
fluor
ide
chlo
ride
brom
ide
nitr
ate
sulp
hate
fluor
ide
chlo
ride
nitr
ate
sulp
hate
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 28
NO3SO4
0
01
02
03
04
05
06
07
08
09
1
Sout
h Al
ligat
or
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y Ka
thle
en
ESI U
SA
ESI C
anad
a
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Stan
rock
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lake
Mad
awas
ka
Mac
assa
Nor
th S
pan
Milli
ken
Lake
Eldo
rado
Stan
leig
h
FCl
0
05
1
15
2
25
3
35
4
45
5
Sou
th A
lliga
tor
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y K
athl
een
ES
I US
A
ES
I Can
ada
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Sta
nroc
k
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lak
e
Mad
awas
ka
Mac
assa
Nor
th S
pan
Mill
iken
Lak
e
Eld
orad
o
Sta
nlei
gh
Anion ratios
Phosphorite oresQuartz-pebble conglomerate and vein deposits
Nitric acid leaching rArr
Indicator of the processApatite mineral Ca5(PO4)3(FClOH)
rArr Indicator of the deposit type
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 29
Sandstone basal channel Quartz-pebble
conglomerate
Phosphorite
Black shale
Statistical evaluation of UOC data
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 30
U productsbull U ores
bull U ore concentrates
bull U oxide powders
bull UF4 and UF6
bull U pellets
Next step - Vertical study
Aim Identify the impurities that are acquired from or lost in the process What is the effect on the impurities from the source material
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 31
Uranium oreconcentrates
Process stagesamples and reagents
UO3
Next step - Vertical study
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 32
Case study
Backgroundbull uranium raw material of unknown
originbull 2003 Rotterdam (NL)bull Brownish yellow powder ~3 kgbull Found on a shipload from Jordan
Measurements performed at ITUbull NDA analysisbull Isotope ratio measurements (U Sr
Pb)bull Infrared analysisbull Impurity analysisbull REE pattern determination
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 33
Case study
Vibrational Spectrum (Infrared Spectrometry)
bull Compound is AUC xH2Obull Sulfate impurity (from dissolution of starting material)
bullNitrate impurity (from solvent extractionpurification)
Mass Spectrometry
bull Natural uranium isotopic compositionbull Natural lead isotopic composition
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 34
Case study
Sr Isotope Ratio
Low value typical for phosphorites (eg North Africa Middle East UShellip)
070757 plusmn 000011
070814 plusmn 000004
071092 plusmn 000006
071416 plusmn 000011
071985 plusmn 000029
072336 plusmn 000004
073434 plusmn 000012
070785 plusmn 000004
071775 plusmn 000003
067 068 069 070 071 072 073 074 075 076 077 078 079 080
Beverley
Calgary
Key Lake
Olympic Dam
Ranger
Ranstad
Stanrock
Mulberry
Fund-26
87Sr86Sr Isotope RatioSr-87 Sr-86 isotope ratio
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 35
Case study
Age dating based on 234U230Th
Age dating based on 232Th228Th
Last chemical separation 1988 plusmn 5 yndash Applicable to samples with incomplete Th separationndash Complementary to 234U230Th method
Last chemical separation 1893 plusmn 17 y
ndash Measured value shows significant positive biasndash Reason incomplete separation of 230Th from the
parent 234U nuclide(ldquoclock is not set to zerordquo)
ndash Residual 230Th cannot be calculated or corrected for
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 36
Case study ndash Find-26
bull 234U abundance suggests low temperature redox deposit value agrees with data reported by IAEA for UOC from Al Qaim (Iraq)
bull Impurities high P contentsimilar metallic impurities to Iraqi phosphate deposits
bull Pb isotopes natural young deposit low U content in orebull REE pattern flat no Eu or Ce anomaly rarr previously found
in certain sandstone-type and reworked phosphorite
Data inherent to the material corroborate information from external sources
Identification of origin based onSingle sampleMultiple parameters
Identification of origin based onSingle sampleMultiple parameters
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 37
Comparison of relative efforts ndash yellow cake
(5)(5)SIMSU particle analysis(5)Evaluation and Report
MC-ICP-MSMC-ICP-MSICP-MSIR-Spectroscopy RamanIon ChromatographyICP-MS IDMS
Electron Microscopy EDX WDXOptical MicroscopyICP-MSTIMSTitration IDMS
Technique
1853Total
15Nd Isotopes15Sr Isotopes3Rare Earth Elemental pattern1Molecular structure
15Anionic impurities3Age dating
3Micromorphology1Visual inspection macroscopic11Impurities11Isotopic Composition11Element Assay
ForensicsSafeguardsAnalysisParameter
Note rounded figures based on a full cost evaluation figures in brackets are not included in the Total
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 38
Conclusions
Wealth of information inherent to nuclear materialDecrypting the information requires sophisticated methodology subject matter expertise and reference dataSignificant effort (resources and time) needed for comprehensive analysis and data interpretationNuclear forensics methodology may open new avenuesin different areasApplication of investigative techniques in Safeguards has to be evaluated
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 13
Uranium minor isotopes
42E-05
47E-05
52E-05
57E-05
62E-05
67E-05
72E-05
77E-05
82E-05
87E-05
Nam
Ros
sing
Can
Blin
d R
iver
Aus
Oly
mpi
c D
am
Usa
Esi
Can
Esi
Aus
Ran
ger
Can
Eld
orad
o
Swe
Ran
stad
t
Usa
El M
esqu
ite
Aus
Mar
y Ka
thle
en
Usa
Ker
r McG
ee
Can
Sta
nroc
k
SA P
alab
ora
Bra
Nuc
lebr
as
Aus
Rum
Jun
gle
Usa
Hom
esta
ke
Can
Sta
nlei
gh
Aus
Que
ensl
and
Can
Key
Lak
e
Usa
Yan
kee
Yello
w
Can
Far
aday
Usa
Fal
ls C
ity
Can
Mad
awas
ka
Can
Clu
ff La
ke
Cze
Rep
ublic
Aus
Beve
rley
fresh
Aus
Beve
rley
old
Usa
Ana
kond
a
Aus
Rad
ium
Hill
Can
Rio
Alg
om
Can
Den
ison
Usa
Shi
rley
Basi
n
Can
El D
orad
o
Can
Ray
Roc
k
Aus
Sout
h Al
ligat
or
U-2
34U
-238
00E+00
50E-09
10E-08
15E-08
20E-08
25E-08
30E-08
U-2
36U
-238
bull 234U238U ratio varies in nature due to eg the preferential leaching of 234U after α-recoil
bull ldquoHighrdquo 236U abundance most probably a cross-contamination
natural
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 14
bull 143Nd144Nd ratio varies in nature due to the 147Sm 143Nd decaybull natural variation 0510 ndash 0513bull the value depends on the age of the mineral and mineral typebull robust indicator as Nd (like other REE) follows uranium (less prone to
weathering) small within-mine variation
0511 05112 05114 05116 05118 0512 05122 05124 05126
Beverley-1 (AUS)
Beverley-2 (AUS)
Straz (CZ)
Stanrock (CAN)
143Nd144Nd ratio
Neodymium isotope ratio
T12=1061011a
Nd-143 Nd-144 ratio
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 15
REE chemically similar with valence state mainly +3 REE pattern often remain unaltered during metamorphism thusproviding information on the premetamorphic history geologicalbackground and source of the rock The behavior of the valence-variable Ce (+4) and Eu (+2) is alsocharacteristic to the rock and it can be exploited to obtain information on the formation conditions
Rare earth elementsrsquo pattern
REE pattern is less prone to the process
can be used straightforwardly for the origin assessment
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 16
Rare-earth pattern of the investigated uranium ore concentrates
01
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
Cho
ndrit
e no
rmal
ized
con
cent
ratio
n
Beverley-1 (Sandstone)
Beverley-2 (Sandstone)
Beverley-3 (Sandstone)
Beverley-4 (Sandstone)
Ranger (Unconformity)
Olympic Dam (Breccia)
Key Lake (Unconformity)
Stanrock (Quartz-pebble congl)
Roumlssing (Intrusive)
ESI Calgary (Phosphorite)
Sedimentary-type
Quartz-pebbleIntrusive (Euanomaly)
Middle REE enrichment (unconformity-type)
REE patterns
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 17
bull geometry rarr 5 x 5 x 5 cm
bull weight about 24 kg
bull elemental uranium produced around 1943 plusmn 2 years (Haigerloch Germany)
Questions1 What is it 2 Origin of the material 3 etc
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 18
Intended use and origin
Nuclear forensics
bull elemental composition pure U metalunconventional applicationreactor
bull isotopic composition rarr natural U rarrD2O or graphite moderated reactor
bull Age via 234U 230Th590 plusmn 20 years (in 2003)
=gt Date of production second half of 1943
Geometry points at German originbull Open literature
Haigerloch reactor 1945
664 cubes x 24 kg = 15936 kg
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 19
ndash Where is the uranium coming from
Date of Production second half of 1943
Authentic cube
Belgian Congo or Joachimsthal (Czech Republic)
rare earth element pattern
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 20
Samples measured
ndash Haigerloch (ldquoHeisenbergrdquo) uranium cube
ndash Heidelberg (ldquoWirtzrdquo) uranium plates
ndash Yellow cake from Otto Hahnrsquos laboratory in Berlin
ndash For comparisonJoachimsthal uranium ore (bdquohistoricldquo sample)Congo uranium ore
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 21
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
REF
REF
REF
REF
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 22
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
REF
REF
REF
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 23
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
REF
REF
Congo UOC
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 24
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
Ore fromJoachimstalREF
Congo UOC
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 25
Inorganic FT-IR measurement of UOC samplesMeasurement in pellet form using KBrRapid identification of compound (oxide peroxide ADU AUC partially
calcined samples)Detection of certain process-related impurities (sulphate carbonate
nitrate)
Uranium composition in UOCs
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 26
Nitrate (1380 cm-1)Impurity from eluate or back extractant
Sulphate (1130 cm-1)Residual from H2SO4 eluate or back extractant
Uranium composition in UOCs
U-O vibration
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 27
Anion residuals in UOCrsquos
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
20
40
60
80
100
120
140
160
180
200
uScm
Cond
fluor
ide
102
2
2 chlo
ride
02
19
4 5 6 7 nitr
ate
003
6
sulp
hate
479
129
Canada ESI
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
17
18
19
20
21
22
23
24
25
26
uScm
Cond
fluor
ide
036
7
2 3
chlo
ride
55
32
5 brom
ide
-00
26
nitr
ate
012
7
sulp
hate
20
767
9
Australia Radium Hill
Different type of uranium deposits
Different processes for U extraction
Different mineral acids are used
Acid remainings
fluor
ide
chlo
ride
brom
ide
nitr
ate
sulp
hate
fluor
ide
chlo
ride
nitr
ate
sulp
hate
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 28
NO3SO4
0
01
02
03
04
05
06
07
08
09
1
Sout
h Al
ligat
or
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y Ka
thle
en
ESI U
SA
ESI C
anad
a
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Stan
rock
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lake
Mad
awas
ka
Mac
assa
Nor
th S
pan
Milli
ken
Lake
Eldo
rado
Stan
leig
h
FCl
0
05
1
15
2
25
3
35
4
45
5
Sou
th A
lliga
tor
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y K
athl
een
ES
I US
A
ES
I Can
ada
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Sta
nroc
k
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lak
e
Mad
awas
ka
Mac
assa
Nor
th S
pan
Mill
iken
Lak
e
Eld
orad
o
Sta
nlei
gh
Anion ratios
Phosphorite oresQuartz-pebble conglomerate and vein deposits
Nitric acid leaching rArr
Indicator of the processApatite mineral Ca5(PO4)3(FClOH)
rArr Indicator of the deposit type
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 29
Sandstone basal channel Quartz-pebble
conglomerate
Phosphorite
Black shale
Statistical evaluation of UOC data
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 30
U productsbull U ores
bull U ore concentrates
bull U oxide powders
bull UF4 and UF6
bull U pellets
Next step - Vertical study
Aim Identify the impurities that are acquired from or lost in the process What is the effect on the impurities from the source material
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 31
Uranium oreconcentrates
Process stagesamples and reagents
UO3
Next step - Vertical study
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 32
Case study
Backgroundbull uranium raw material of unknown
originbull 2003 Rotterdam (NL)bull Brownish yellow powder ~3 kgbull Found on a shipload from Jordan
Measurements performed at ITUbull NDA analysisbull Isotope ratio measurements (U Sr
Pb)bull Infrared analysisbull Impurity analysisbull REE pattern determination
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 33
Case study
Vibrational Spectrum (Infrared Spectrometry)
bull Compound is AUC xH2Obull Sulfate impurity (from dissolution of starting material)
bullNitrate impurity (from solvent extractionpurification)
Mass Spectrometry
bull Natural uranium isotopic compositionbull Natural lead isotopic composition
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 34
Case study
Sr Isotope Ratio
Low value typical for phosphorites (eg North Africa Middle East UShellip)
070757 plusmn 000011
070814 plusmn 000004
071092 plusmn 000006
071416 plusmn 000011
071985 plusmn 000029
072336 plusmn 000004
073434 plusmn 000012
070785 plusmn 000004
071775 plusmn 000003
067 068 069 070 071 072 073 074 075 076 077 078 079 080
Beverley
Calgary
Key Lake
Olympic Dam
Ranger
Ranstad
Stanrock
Mulberry
Fund-26
87Sr86Sr Isotope RatioSr-87 Sr-86 isotope ratio
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 35
Case study
Age dating based on 234U230Th
Age dating based on 232Th228Th
Last chemical separation 1988 plusmn 5 yndash Applicable to samples with incomplete Th separationndash Complementary to 234U230Th method
Last chemical separation 1893 plusmn 17 y
ndash Measured value shows significant positive biasndash Reason incomplete separation of 230Th from the
parent 234U nuclide(ldquoclock is not set to zerordquo)
ndash Residual 230Th cannot be calculated or corrected for
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 36
Case study ndash Find-26
bull 234U abundance suggests low temperature redox deposit value agrees with data reported by IAEA for UOC from Al Qaim (Iraq)
bull Impurities high P contentsimilar metallic impurities to Iraqi phosphate deposits
bull Pb isotopes natural young deposit low U content in orebull REE pattern flat no Eu or Ce anomaly rarr previously found
in certain sandstone-type and reworked phosphorite
Data inherent to the material corroborate information from external sources
Identification of origin based onSingle sampleMultiple parameters
Identification of origin based onSingle sampleMultiple parameters
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 37
Comparison of relative efforts ndash yellow cake
(5)(5)SIMSU particle analysis(5)Evaluation and Report
MC-ICP-MSMC-ICP-MSICP-MSIR-Spectroscopy RamanIon ChromatographyICP-MS IDMS
Electron Microscopy EDX WDXOptical MicroscopyICP-MSTIMSTitration IDMS
Technique
1853Total
15Nd Isotopes15Sr Isotopes3Rare Earth Elemental pattern1Molecular structure
15Anionic impurities3Age dating
3Micromorphology1Visual inspection macroscopic11Impurities11Isotopic Composition11Element Assay
ForensicsSafeguardsAnalysisParameter
Note rounded figures based on a full cost evaluation figures in brackets are not included in the Total
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 38
Conclusions
Wealth of information inherent to nuclear materialDecrypting the information requires sophisticated methodology subject matter expertise and reference dataSignificant effort (resources and time) needed for comprehensive analysis and data interpretationNuclear forensics methodology may open new avenuesin different areasApplication of investigative techniques in Safeguards has to be evaluated
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 14
bull 143Nd144Nd ratio varies in nature due to the 147Sm 143Nd decaybull natural variation 0510 ndash 0513bull the value depends on the age of the mineral and mineral typebull robust indicator as Nd (like other REE) follows uranium (less prone to
weathering) small within-mine variation
0511 05112 05114 05116 05118 0512 05122 05124 05126
Beverley-1 (AUS)
Beverley-2 (AUS)
Straz (CZ)
Stanrock (CAN)
143Nd144Nd ratio
Neodymium isotope ratio
T12=1061011a
Nd-143 Nd-144 ratio
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 15
REE chemically similar with valence state mainly +3 REE pattern often remain unaltered during metamorphism thusproviding information on the premetamorphic history geologicalbackground and source of the rock The behavior of the valence-variable Ce (+4) and Eu (+2) is alsocharacteristic to the rock and it can be exploited to obtain information on the formation conditions
Rare earth elementsrsquo pattern
REE pattern is less prone to the process
can be used straightforwardly for the origin assessment
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 16
Rare-earth pattern of the investigated uranium ore concentrates
01
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
Cho
ndrit
e no
rmal
ized
con
cent
ratio
n
Beverley-1 (Sandstone)
Beverley-2 (Sandstone)
Beverley-3 (Sandstone)
Beverley-4 (Sandstone)
Ranger (Unconformity)
Olympic Dam (Breccia)
Key Lake (Unconformity)
Stanrock (Quartz-pebble congl)
Roumlssing (Intrusive)
ESI Calgary (Phosphorite)
Sedimentary-type
Quartz-pebbleIntrusive (Euanomaly)
Middle REE enrichment (unconformity-type)
REE patterns
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 17
bull geometry rarr 5 x 5 x 5 cm
bull weight about 24 kg
bull elemental uranium produced around 1943 plusmn 2 years (Haigerloch Germany)
Questions1 What is it 2 Origin of the material 3 etc
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 18
Intended use and origin
Nuclear forensics
bull elemental composition pure U metalunconventional applicationreactor
bull isotopic composition rarr natural U rarrD2O or graphite moderated reactor
bull Age via 234U 230Th590 plusmn 20 years (in 2003)
=gt Date of production second half of 1943
Geometry points at German originbull Open literature
Haigerloch reactor 1945
664 cubes x 24 kg = 15936 kg
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 19
ndash Where is the uranium coming from
Date of Production second half of 1943
Authentic cube
Belgian Congo or Joachimsthal (Czech Republic)
rare earth element pattern
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 20
Samples measured
ndash Haigerloch (ldquoHeisenbergrdquo) uranium cube
ndash Heidelberg (ldquoWirtzrdquo) uranium plates
ndash Yellow cake from Otto Hahnrsquos laboratory in Berlin
ndash For comparisonJoachimsthal uranium ore (bdquohistoricldquo sample)Congo uranium ore
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 21
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
REF
REF
REF
REF
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 22
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
REF
REF
REF
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 23
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
REF
REF
Congo UOC
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 24
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
Ore fromJoachimstalREF
Congo UOC
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 25
Inorganic FT-IR measurement of UOC samplesMeasurement in pellet form using KBrRapid identification of compound (oxide peroxide ADU AUC partially
calcined samples)Detection of certain process-related impurities (sulphate carbonate
nitrate)
Uranium composition in UOCs
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 26
Nitrate (1380 cm-1)Impurity from eluate or back extractant
Sulphate (1130 cm-1)Residual from H2SO4 eluate or back extractant
Uranium composition in UOCs
U-O vibration
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 27
Anion residuals in UOCrsquos
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
20
40
60
80
100
120
140
160
180
200
uScm
Cond
fluor
ide
102
2
2 chlo
ride
02
19
4 5 6 7 nitr
ate
003
6
sulp
hate
479
129
Canada ESI
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
17
18
19
20
21
22
23
24
25
26
uScm
Cond
fluor
ide
036
7
2 3
chlo
ride
55
32
5 brom
ide
-00
26
nitr
ate
012
7
sulp
hate
20
767
9
Australia Radium Hill
Different type of uranium deposits
Different processes for U extraction
Different mineral acids are used
Acid remainings
fluor
ide
chlo
ride
brom
ide
nitr
ate
sulp
hate
fluor
ide
chlo
ride
nitr
ate
sulp
hate
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 28
NO3SO4
0
01
02
03
04
05
06
07
08
09
1
Sout
h Al
ligat
or
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y Ka
thle
en
ESI U
SA
ESI C
anad
a
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Stan
rock
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lake
Mad
awas
ka
Mac
assa
Nor
th S
pan
Milli
ken
Lake
Eldo
rado
Stan
leig
h
FCl
0
05
1
15
2
25
3
35
4
45
5
Sou
th A
lliga
tor
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y K
athl
een
ES
I US
A
ES
I Can
ada
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Sta
nroc
k
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lak
e
Mad
awas
ka
Mac
assa
Nor
th S
pan
Mill
iken
Lak
e
Eld
orad
o
Sta
nlei
gh
Anion ratios
Phosphorite oresQuartz-pebble conglomerate and vein deposits
Nitric acid leaching rArr
Indicator of the processApatite mineral Ca5(PO4)3(FClOH)
rArr Indicator of the deposit type
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 29
Sandstone basal channel Quartz-pebble
conglomerate
Phosphorite
Black shale
Statistical evaluation of UOC data
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 30
U productsbull U ores
bull U ore concentrates
bull U oxide powders
bull UF4 and UF6
bull U pellets
Next step - Vertical study
Aim Identify the impurities that are acquired from or lost in the process What is the effect on the impurities from the source material
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 31
Uranium oreconcentrates
Process stagesamples and reagents
UO3
Next step - Vertical study
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 32
Case study
Backgroundbull uranium raw material of unknown
originbull 2003 Rotterdam (NL)bull Brownish yellow powder ~3 kgbull Found on a shipload from Jordan
Measurements performed at ITUbull NDA analysisbull Isotope ratio measurements (U Sr
Pb)bull Infrared analysisbull Impurity analysisbull REE pattern determination
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 33
Case study
Vibrational Spectrum (Infrared Spectrometry)
bull Compound is AUC xH2Obull Sulfate impurity (from dissolution of starting material)
bullNitrate impurity (from solvent extractionpurification)
Mass Spectrometry
bull Natural uranium isotopic compositionbull Natural lead isotopic composition
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 34
Case study
Sr Isotope Ratio
Low value typical for phosphorites (eg North Africa Middle East UShellip)
070757 plusmn 000011
070814 plusmn 000004
071092 plusmn 000006
071416 plusmn 000011
071985 plusmn 000029
072336 plusmn 000004
073434 plusmn 000012
070785 plusmn 000004
071775 plusmn 000003
067 068 069 070 071 072 073 074 075 076 077 078 079 080
Beverley
Calgary
Key Lake
Olympic Dam
Ranger
Ranstad
Stanrock
Mulberry
Fund-26
87Sr86Sr Isotope RatioSr-87 Sr-86 isotope ratio
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 35
Case study
Age dating based on 234U230Th
Age dating based on 232Th228Th
Last chemical separation 1988 plusmn 5 yndash Applicable to samples with incomplete Th separationndash Complementary to 234U230Th method
Last chemical separation 1893 plusmn 17 y
ndash Measured value shows significant positive biasndash Reason incomplete separation of 230Th from the
parent 234U nuclide(ldquoclock is not set to zerordquo)
ndash Residual 230Th cannot be calculated or corrected for
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 36
Case study ndash Find-26
bull 234U abundance suggests low temperature redox deposit value agrees with data reported by IAEA for UOC from Al Qaim (Iraq)
bull Impurities high P contentsimilar metallic impurities to Iraqi phosphate deposits
bull Pb isotopes natural young deposit low U content in orebull REE pattern flat no Eu or Ce anomaly rarr previously found
in certain sandstone-type and reworked phosphorite
Data inherent to the material corroborate information from external sources
Identification of origin based onSingle sampleMultiple parameters
Identification of origin based onSingle sampleMultiple parameters
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 37
Comparison of relative efforts ndash yellow cake
(5)(5)SIMSU particle analysis(5)Evaluation and Report
MC-ICP-MSMC-ICP-MSICP-MSIR-Spectroscopy RamanIon ChromatographyICP-MS IDMS
Electron Microscopy EDX WDXOptical MicroscopyICP-MSTIMSTitration IDMS
Technique
1853Total
15Nd Isotopes15Sr Isotopes3Rare Earth Elemental pattern1Molecular structure
15Anionic impurities3Age dating
3Micromorphology1Visual inspection macroscopic11Impurities11Isotopic Composition11Element Assay
ForensicsSafeguardsAnalysisParameter
Note rounded figures based on a full cost evaluation figures in brackets are not included in the Total
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 38
Conclusions
Wealth of information inherent to nuclear materialDecrypting the information requires sophisticated methodology subject matter expertise and reference dataSignificant effort (resources and time) needed for comprehensive analysis and data interpretationNuclear forensics methodology may open new avenuesin different areasApplication of investigative techniques in Safeguards has to be evaluated
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 15
REE chemically similar with valence state mainly +3 REE pattern often remain unaltered during metamorphism thusproviding information on the premetamorphic history geologicalbackground and source of the rock The behavior of the valence-variable Ce (+4) and Eu (+2) is alsocharacteristic to the rock and it can be exploited to obtain information on the formation conditions
Rare earth elementsrsquo pattern
REE pattern is less prone to the process
can be used straightforwardly for the origin assessment
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 16
Rare-earth pattern of the investigated uranium ore concentrates
01
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
Cho
ndrit
e no
rmal
ized
con
cent
ratio
n
Beverley-1 (Sandstone)
Beverley-2 (Sandstone)
Beverley-3 (Sandstone)
Beverley-4 (Sandstone)
Ranger (Unconformity)
Olympic Dam (Breccia)
Key Lake (Unconformity)
Stanrock (Quartz-pebble congl)
Roumlssing (Intrusive)
ESI Calgary (Phosphorite)
Sedimentary-type
Quartz-pebbleIntrusive (Euanomaly)
Middle REE enrichment (unconformity-type)
REE patterns
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 17
bull geometry rarr 5 x 5 x 5 cm
bull weight about 24 kg
bull elemental uranium produced around 1943 plusmn 2 years (Haigerloch Germany)
Questions1 What is it 2 Origin of the material 3 etc
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 18
Intended use and origin
Nuclear forensics
bull elemental composition pure U metalunconventional applicationreactor
bull isotopic composition rarr natural U rarrD2O or graphite moderated reactor
bull Age via 234U 230Th590 plusmn 20 years (in 2003)
=gt Date of production second half of 1943
Geometry points at German originbull Open literature
Haigerloch reactor 1945
664 cubes x 24 kg = 15936 kg
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 19
ndash Where is the uranium coming from
Date of Production second half of 1943
Authentic cube
Belgian Congo or Joachimsthal (Czech Republic)
rare earth element pattern
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 20
Samples measured
ndash Haigerloch (ldquoHeisenbergrdquo) uranium cube
ndash Heidelberg (ldquoWirtzrdquo) uranium plates
ndash Yellow cake from Otto Hahnrsquos laboratory in Berlin
ndash For comparisonJoachimsthal uranium ore (bdquohistoricldquo sample)Congo uranium ore
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 21
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
REF
REF
REF
REF
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 22
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
REF
REF
REF
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 23
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
REF
REF
Congo UOC
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 24
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
Ore fromJoachimstalREF
Congo UOC
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 25
Inorganic FT-IR measurement of UOC samplesMeasurement in pellet form using KBrRapid identification of compound (oxide peroxide ADU AUC partially
calcined samples)Detection of certain process-related impurities (sulphate carbonate
nitrate)
Uranium composition in UOCs
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 26
Nitrate (1380 cm-1)Impurity from eluate or back extractant
Sulphate (1130 cm-1)Residual from H2SO4 eluate or back extractant
Uranium composition in UOCs
U-O vibration
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 27
Anion residuals in UOCrsquos
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
20
40
60
80
100
120
140
160
180
200
uScm
Cond
fluor
ide
102
2
2 chlo
ride
02
19
4 5 6 7 nitr
ate
003
6
sulp
hate
479
129
Canada ESI
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
17
18
19
20
21
22
23
24
25
26
uScm
Cond
fluor
ide
036
7
2 3
chlo
ride
55
32
5 brom
ide
-00
26
nitr
ate
012
7
sulp
hate
20
767
9
Australia Radium Hill
Different type of uranium deposits
Different processes for U extraction
Different mineral acids are used
Acid remainings
fluor
ide
chlo
ride
brom
ide
nitr
ate
sulp
hate
fluor
ide
chlo
ride
nitr
ate
sulp
hate
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 28
NO3SO4
0
01
02
03
04
05
06
07
08
09
1
Sout
h Al
ligat
or
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y Ka
thle
en
ESI U
SA
ESI C
anad
a
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Stan
rock
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lake
Mad
awas
ka
Mac
assa
Nor
th S
pan
Milli
ken
Lake
Eldo
rado
Stan
leig
h
FCl
0
05
1
15
2
25
3
35
4
45
5
Sou
th A
lliga
tor
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y K
athl
een
ES
I US
A
ES
I Can
ada
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Sta
nroc
k
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lak
e
Mad
awas
ka
Mac
assa
Nor
th S
pan
Mill
iken
Lak
e
Eld
orad
o
Sta
nlei
gh
Anion ratios
Phosphorite oresQuartz-pebble conglomerate and vein deposits
Nitric acid leaching rArr
Indicator of the processApatite mineral Ca5(PO4)3(FClOH)
rArr Indicator of the deposit type
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 29
Sandstone basal channel Quartz-pebble
conglomerate
Phosphorite
Black shale
Statistical evaluation of UOC data
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 30
U productsbull U ores
bull U ore concentrates
bull U oxide powders
bull UF4 and UF6
bull U pellets
Next step - Vertical study
Aim Identify the impurities that are acquired from or lost in the process What is the effect on the impurities from the source material
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 31
Uranium oreconcentrates
Process stagesamples and reagents
UO3
Next step - Vertical study
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 32
Case study
Backgroundbull uranium raw material of unknown
originbull 2003 Rotterdam (NL)bull Brownish yellow powder ~3 kgbull Found on a shipload from Jordan
Measurements performed at ITUbull NDA analysisbull Isotope ratio measurements (U Sr
Pb)bull Infrared analysisbull Impurity analysisbull REE pattern determination
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 33
Case study
Vibrational Spectrum (Infrared Spectrometry)
bull Compound is AUC xH2Obull Sulfate impurity (from dissolution of starting material)
bullNitrate impurity (from solvent extractionpurification)
Mass Spectrometry
bull Natural uranium isotopic compositionbull Natural lead isotopic composition
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 34
Case study
Sr Isotope Ratio
Low value typical for phosphorites (eg North Africa Middle East UShellip)
070757 plusmn 000011
070814 plusmn 000004
071092 plusmn 000006
071416 plusmn 000011
071985 plusmn 000029
072336 plusmn 000004
073434 plusmn 000012
070785 plusmn 000004
071775 plusmn 000003
067 068 069 070 071 072 073 074 075 076 077 078 079 080
Beverley
Calgary
Key Lake
Olympic Dam
Ranger
Ranstad
Stanrock
Mulberry
Fund-26
87Sr86Sr Isotope RatioSr-87 Sr-86 isotope ratio
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 35
Case study
Age dating based on 234U230Th
Age dating based on 232Th228Th
Last chemical separation 1988 plusmn 5 yndash Applicable to samples with incomplete Th separationndash Complementary to 234U230Th method
Last chemical separation 1893 plusmn 17 y
ndash Measured value shows significant positive biasndash Reason incomplete separation of 230Th from the
parent 234U nuclide(ldquoclock is not set to zerordquo)
ndash Residual 230Th cannot be calculated or corrected for
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 36
Case study ndash Find-26
bull 234U abundance suggests low temperature redox deposit value agrees with data reported by IAEA for UOC from Al Qaim (Iraq)
bull Impurities high P contentsimilar metallic impurities to Iraqi phosphate deposits
bull Pb isotopes natural young deposit low U content in orebull REE pattern flat no Eu or Ce anomaly rarr previously found
in certain sandstone-type and reworked phosphorite
Data inherent to the material corroborate information from external sources
Identification of origin based onSingle sampleMultiple parameters
Identification of origin based onSingle sampleMultiple parameters
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 37
Comparison of relative efforts ndash yellow cake
(5)(5)SIMSU particle analysis(5)Evaluation and Report
MC-ICP-MSMC-ICP-MSICP-MSIR-Spectroscopy RamanIon ChromatographyICP-MS IDMS
Electron Microscopy EDX WDXOptical MicroscopyICP-MSTIMSTitration IDMS
Technique
1853Total
15Nd Isotopes15Sr Isotopes3Rare Earth Elemental pattern1Molecular structure
15Anionic impurities3Age dating
3Micromorphology1Visual inspection macroscopic11Impurities11Isotopic Composition11Element Assay
ForensicsSafeguardsAnalysisParameter
Note rounded figures based on a full cost evaluation figures in brackets are not included in the Total
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 38
Conclusions
Wealth of information inherent to nuclear materialDecrypting the information requires sophisticated methodology subject matter expertise and reference dataSignificant effort (resources and time) needed for comprehensive analysis and data interpretationNuclear forensics methodology may open new avenuesin different areasApplication of investigative techniques in Safeguards has to be evaluated
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 16
Rare-earth pattern of the investigated uranium ore concentrates
01
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
Cho
ndrit
e no
rmal
ized
con
cent
ratio
n
Beverley-1 (Sandstone)
Beverley-2 (Sandstone)
Beverley-3 (Sandstone)
Beverley-4 (Sandstone)
Ranger (Unconformity)
Olympic Dam (Breccia)
Key Lake (Unconformity)
Stanrock (Quartz-pebble congl)
Roumlssing (Intrusive)
ESI Calgary (Phosphorite)
Sedimentary-type
Quartz-pebbleIntrusive (Euanomaly)
Middle REE enrichment (unconformity-type)
REE patterns
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 17
bull geometry rarr 5 x 5 x 5 cm
bull weight about 24 kg
bull elemental uranium produced around 1943 plusmn 2 years (Haigerloch Germany)
Questions1 What is it 2 Origin of the material 3 etc
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 18
Intended use and origin
Nuclear forensics
bull elemental composition pure U metalunconventional applicationreactor
bull isotopic composition rarr natural U rarrD2O or graphite moderated reactor
bull Age via 234U 230Th590 plusmn 20 years (in 2003)
=gt Date of production second half of 1943
Geometry points at German originbull Open literature
Haigerloch reactor 1945
664 cubes x 24 kg = 15936 kg
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 19
ndash Where is the uranium coming from
Date of Production second half of 1943
Authentic cube
Belgian Congo or Joachimsthal (Czech Republic)
rare earth element pattern
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 20
Samples measured
ndash Haigerloch (ldquoHeisenbergrdquo) uranium cube
ndash Heidelberg (ldquoWirtzrdquo) uranium plates
ndash Yellow cake from Otto Hahnrsquos laboratory in Berlin
ndash For comparisonJoachimsthal uranium ore (bdquohistoricldquo sample)Congo uranium ore
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 21
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
REF
REF
REF
REF
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 22
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
REF
REF
REF
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 23
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
REF
REF
Congo UOC
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 24
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
Ore fromJoachimstalREF
Congo UOC
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 25
Inorganic FT-IR measurement of UOC samplesMeasurement in pellet form using KBrRapid identification of compound (oxide peroxide ADU AUC partially
calcined samples)Detection of certain process-related impurities (sulphate carbonate
nitrate)
Uranium composition in UOCs
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 26
Nitrate (1380 cm-1)Impurity from eluate or back extractant
Sulphate (1130 cm-1)Residual from H2SO4 eluate or back extractant
Uranium composition in UOCs
U-O vibration
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 27
Anion residuals in UOCrsquos
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
20
40
60
80
100
120
140
160
180
200
uScm
Cond
fluor
ide
102
2
2 chlo
ride
02
19
4 5 6 7 nitr
ate
003
6
sulp
hate
479
129
Canada ESI
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
17
18
19
20
21
22
23
24
25
26
uScm
Cond
fluor
ide
036
7
2 3
chlo
ride
55
32
5 brom
ide
-00
26
nitr
ate
012
7
sulp
hate
20
767
9
Australia Radium Hill
Different type of uranium deposits
Different processes for U extraction
Different mineral acids are used
Acid remainings
fluor
ide
chlo
ride
brom
ide
nitr
ate
sulp
hate
fluor
ide
chlo
ride
nitr
ate
sulp
hate
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 28
NO3SO4
0
01
02
03
04
05
06
07
08
09
1
Sout
h Al
ligat
or
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y Ka
thle
en
ESI U
SA
ESI C
anad
a
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Stan
rock
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lake
Mad
awas
ka
Mac
assa
Nor
th S
pan
Milli
ken
Lake
Eldo
rado
Stan
leig
h
FCl
0
05
1
15
2
25
3
35
4
45
5
Sou
th A
lliga
tor
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y K
athl
een
ES
I US
A
ES
I Can
ada
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Sta
nroc
k
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lak
e
Mad
awas
ka
Mac
assa
Nor
th S
pan
Mill
iken
Lak
e
Eld
orad
o
Sta
nlei
gh
Anion ratios
Phosphorite oresQuartz-pebble conglomerate and vein deposits
Nitric acid leaching rArr
Indicator of the processApatite mineral Ca5(PO4)3(FClOH)
rArr Indicator of the deposit type
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 29
Sandstone basal channel Quartz-pebble
conglomerate
Phosphorite
Black shale
Statistical evaluation of UOC data
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 30
U productsbull U ores
bull U ore concentrates
bull U oxide powders
bull UF4 and UF6
bull U pellets
Next step - Vertical study
Aim Identify the impurities that are acquired from or lost in the process What is the effect on the impurities from the source material
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 31
Uranium oreconcentrates
Process stagesamples and reagents
UO3
Next step - Vertical study
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 32
Case study
Backgroundbull uranium raw material of unknown
originbull 2003 Rotterdam (NL)bull Brownish yellow powder ~3 kgbull Found on a shipload from Jordan
Measurements performed at ITUbull NDA analysisbull Isotope ratio measurements (U Sr
Pb)bull Infrared analysisbull Impurity analysisbull REE pattern determination
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 33
Case study
Vibrational Spectrum (Infrared Spectrometry)
bull Compound is AUC xH2Obull Sulfate impurity (from dissolution of starting material)
bullNitrate impurity (from solvent extractionpurification)
Mass Spectrometry
bull Natural uranium isotopic compositionbull Natural lead isotopic composition
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 34
Case study
Sr Isotope Ratio
Low value typical for phosphorites (eg North Africa Middle East UShellip)
070757 plusmn 000011
070814 plusmn 000004
071092 plusmn 000006
071416 plusmn 000011
071985 plusmn 000029
072336 plusmn 000004
073434 plusmn 000012
070785 plusmn 000004
071775 plusmn 000003
067 068 069 070 071 072 073 074 075 076 077 078 079 080
Beverley
Calgary
Key Lake
Olympic Dam
Ranger
Ranstad
Stanrock
Mulberry
Fund-26
87Sr86Sr Isotope RatioSr-87 Sr-86 isotope ratio
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 35
Case study
Age dating based on 234U230Th
Age dating based on 232Th228Th
Last chemical separation 1988 plusmn 5 yndash Applicable to samples with incomplete Th separationndash Complementary to 234U230Th method
Last chemical separation 1893 plusmn 17 y
ndash Measured value shows significant positive biasndash Reason incomplete separation of 230Th from the
parent 234U nuclide(ldquoclock is not set to zerordquo)
ndash Residual 230Th cannot be calculated or corrected for
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 36
Case study ndash Find-26
bull 234U abundance suggests low temperature redox deposit value agrees with data reported by IAEA for UOC from Al Qaim (Iraq)
bull Impurities high P contentsimilar metallic impurities to Iraqi phosphate deposits
bull Pb isotopes natural young deposit low U content in orebull REE pattern flat no Eu or Ce anomaly rarr previously found
in certain sandstone-type and reworked phosphorite
Data inherent to the material corroborate information from external sources
Identification of origin based onSingle sampleMultiple parameters
Identification of origin based onSingle sampleMultiple parameters
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 37
Comparison of relative efforts ndash yellow cake
(5)(5)SIMSU particle analysis(5)Evaluation and Report
MC-ICP-MSMC-ICP-MSICP-MSIR-Spectroscopy RamanIon ChromatographyICP-MS IDMS
Electron Microscopy EDX WDXOptical MicroscopyICP-MSTIMSTitration IDMS
Technique
1853Total
15Nd Isotopes15Sr Isotopes3Rare Earth Elemental pattern1Molecular structure
15Anionic impurities3Age dating
3Micromorphology1Visual inspection macroscopic11Impurities11Isotopic Composition11Element Assay
ForensicsSafeguardsAnalysisParameter
Note rounded figures based on a full cost evaluation figures in brackets are not included in the Total
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 38
Conclusions
Wealth of information inherent to nuclear materialDecrypting the information requires sophisticated methodology subject matter expertise and reference dataSignificant effort (resources and time) needed for comprehensive analysis and data interpretationNuclear forensics methodology may open new avenuesin different areasApplication of investigative techniques in Safeguards has to be evaluated
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 17
bull geometry rarr 5 x 5 x 5 cm
bull weight about 24 kg
bull elemental uranium produced around 1943 plusmn 2 years (Haigerloch Germany)
Questions1 What is it 2 Origin of the material 3 etc
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 18
Intended use and origin
Nuclear forensics
bull elemental composition pure U metalunconventional applicationreactor
bull isotopic composition rarr natural U rarrD2O or graphite moderated reactor
bull Age via 234U 230Th590 plusmn 20 years (in 2003)
=gt Date of production second half of 1943
Geometry points at German originbull Open literature
Haigerloch reactor 1945
664 cubes x 24 kg = 15936 kg
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 19
ndash Where is the uranium coming from
Date of Production second half of 1943
Authentic cube
Belgian Congo or Joachimsthal (Czech Republic)
rare earth element pattern
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 20
Samples measured
ndash Haigerloch (ldquoHeisenbergrdquo) uranium cube
ndash Heidelberg (ldquoWirtzrdquo) uranium plates
ndash Yellow cake from Otto Hahnrsquos laboratory in Berlin
ndash For comparisonJoachimsthal uranium ore (bdquohistoricldquo sample)Congo uranium ore
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 21
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
REF
REF
REF
REF
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 22
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
REF
REF
REF
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 23
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
REF
REF
Congo UOC
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 24
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
Ore fromJoachimstalREF
Congo UOC
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 25
Inorganic FT-IR measurement of UOC samplesMeasurement in pellet form using KBrRapid identification of compound (oxide peroxide ADU AUC partially
calcined samples)Detection of certain process-related impurities (sulphate carbonate
nitrate)
Uranium composition in UOCs
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 26
Nitrate (1380 cm-1)Impurity from eluate or back extractant
Sulphate (1130 cm-1)Residual from H2SO4 eluate or back extractant
Uranium composition in UOCs
U-O vibration
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 27
Anion residuals in UOCrsquos
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
20
40
60
80
100
120
140
160
180
200
uScm
Cond
fluor
ide
102
2
2 chlo
ride
02
19
4 5 6 7 nitr
ate
003
6
sulp
hate
479
129
Canada ESI
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
17
18
19
20
21
22
23
24
25
26
uScm
Cond
fluor
ide
036
7
2 3
chlo
ride
55
32
5 brom
ide
-00
26
nitr
ate
012
7
sulp
hate
20
767
9
Australia Radium Hill
Different type of uranium deposits
Different processes for U extraction
Different mineral acids are used
Acid remainings
fluor
ide
chlo
ride
brom
ide
nitr
ate
sulp
hate
fluor
ide
chlo
ride
nitr
ate
sulp
hate
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 28
NO3SO4
0
01
02
03
04
05
06
07
08
09
1
Sout
h Al
ligat
or
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y Ka
thle
en
ESI U
SA
ESI C
anad
a
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Stan
rock
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lake
Mad
awas
ka
Mac
assa
Nor
th S
pan
Milli
ken
Lake
Eldo
rado
Stan
leig
h
FCl
0
05
1
15
2
25
3
35
4
45
5
Sou
th A
lliga
tor
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y K
athl
een
ES
I US
A
ES
I Can
ada
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Sta
nroc
k
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lak
e
Mad
awas
ka
Mac
assa
Nor
th S
pan
Mill
iken
Lak
e
Eld
orad
o
Sta
nlei
gh
Anion ratios
Phosphorite oresQuartz-pebble conglomerate and vein deposits
Nitric acid leaching rArr
Indicator of the processApatite mineral Ca5(PO4)3(FClOH)
rArr Indicator of the deposit type
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 29
Sandstone basal channel Quartz-pebble
conglomerate
Phosphorite
Black shale
Statistical evaluation of UOC data
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 30
U productsbull U ores
bull U ore concentrates
bull U oxide powders
bull UF4 and UF6
bull U pellets
Next step - Vertical study
Aim Identify the impurities that are acquired from or lost in the process What is the effect on the impurities from the source material
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 31
Uranium oreconcentrates
Process stagesamples and reagents
UO3
Next step - Vertical study
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 32
Case study
Backgroundbull uranium raw material of unknown
originbull 2003 Rotterdam (NL)bull Brownish yellow powder ~3 kgbull Found on a shipload from Jordan
Measurements performed at ITUbull NDA analysisbull Isotope ratio measurements (U Sr
Pb)bull Infrared analysisbull Impurity analysisbull REE pattern determination
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 33
Case study
Vibrational Spectrum (Infrared Spectrometry)
bull Compound is AUC xH2Obull Sulfate impurity (from dissolution of starting material)
bullNitrate impurity (from solvent extractionpurification)
Mass Spectrometry
bull Natural uranium isotopic compositionbull Natural lead isotopic composition
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 34
Case study
Sr Isotope Ratio
Low value typical for phosphorites (eg North Africa Middle East UShellip)
070757 plusmn 000011
070814 plusmn 000004
071092 plusmn 000006
071416 plusmn 000011
071985 plusmn 000029
072336 plusmn 000004
073434 plusmn 000012
070785 plusmn 000004
071775 plusmn 000003
067 068 069 070 071 072 073 074 075 076 077 078 079 080
Beverley
Calgary
Key Lake
Olympic Dam
Ranger
Ranstad
Stanrock
Mulberry
Fund-26
87Sr86Sr Isotope RatioSr-87 Sr-86 isotope ratio
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 35
Case study
Age dating based on 234U230Th
Age dating based on 232Th228Th
Last chemical separation 1988 plusmn 5 yndash Applicable to samples with incomplete Th separationndash Complementary to 234U230Th method
Last chemical separation 1893 plusmn 17 y
ndash Measured value shows significant positive biasndash Reason incomplete separation of 230Th from the
parent 234U nuclide(ldquoclock is not set to zerordquo)
ndash Residual 230Th cannot be calculated or corrected for
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 36
Case study ndash Find-26
bull 234U abundance suggests low temperature redox deposit value agrees with data reported by IAEA for UOC from Al Qaim (Iraq)
bull Impurities high P contentsimilar metallic impurities to Iraqi phosphate deposits
bull Pb isotopes natural young deposit low U content in orebull REE pattern flat no Eu or Ce anomaly rarr previously found
in certain sandstone-type and reworked phosphorite
Data inherent to the material corroborate information from external sources
Identification of origin based onSingle sampleMultiple parameters
Identification of origin based onSingle sampleMultiple parameters
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 37
Comparison of relative efforts ndash yellow cake
(5)(5)SIMSU particle analysis(5)Evaluation and Report
MC-ICP-MSMC-ICP-MSICP-MSIR-Spectroscopy RamanIon ChromatographyICP-MS IDMS
Electron Microscopy EDX WDXOptical MicroscopyICP-MSTIMSTitration IDMS
Technique
1853Total
15Nd Isotopes15Sr Isotopes3Rare Earth Elemental pattern1Molecular structure
15Anionic impurities3Age dating
3Micromorphology1Visual inspection macroscopic11Impurities11Isotopic Composition11Element Assay
ForensicsSafeguardsAnalysisParameter
Note rounded figures based on a full cost evaluation figures in brackets are not included in the Total
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 38
Conclusions
Wealth of information inherent to nuclear materialDecrypting the information requires sophisticated methodology subject matter expertise and reference dataSignificant effort (resources and time) needed for comprehensive analysis and data interpretationNuclear forensics methodology may open new avenuesin different areasApplication of investigative techniques in Safeguards has to be evaluated
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 18
Intended use and origin
Nuclear forensics
bull elemental composition pure U metalunconventional applicationreactor
bull isotopic composition rarr natural U rarrD2O or graphite moderated reactor
bull Age via 234U 230Th590 plusmn 20 years (in 2003)
=gt Date of production second half of 1943
Geometry points at German originbull Open literature
Haigerloch reactor 1945
664 cubes x 24 kg = 15936 kg
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 19
ndash Where is the uranium coming from
Date of Production second half of 1943
Authentic cube
Belgian Congo or Joachimsthal (Czech Republic)
rare earth element pattern
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 20
Samples measured
ndash Haigerloch (ldquoHeisenbergrdquo) uranium cube
ndash Heidelberg (ldquoWirtzrdquo) uranium plates
ndash Yellow cake from Otto Hahnrsquos laboratory in Berlin
ndash For comparisonJoachimsthal uranium ore (bdquohistoricldquo sample)Congo uranium ore
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 21
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
REF
REF
REF
REF
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 22
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
REF
REF
REF
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 23
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
REF
REF
Congo UOC
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 24
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
Ore fromJoachimstalREF
Congo UOC
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 25
Inorganic FT-IR measurement of UOC samplesMeasurement in pellet form using KBrRapid identification of compound (oxide peroxide ADU AUC partially
calcined samples)Detection of certain process-related impurities (sulphate carbonate
nitrate)
Uranium composition in UOCs
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 26
Nitrate (1380 cm-1)Impurity from eluate or back extractant
Sulphate (1130 cm-1)Residual from H2SO4 eluate or back extractant
Uranium composition in UOCs
U-O vibration
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 27
Anion residuals in UOCrsquos
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
20
40
60
80
100
120
140
160
180
200
uScm
Cond
fluor
ide
102
2
2 chlo
ride
02
19
4 5 6 7 nitr
ate
003
6
sulp
hate
479
129
Canada ESI
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
17
18
19
20
21
22
23
24
25
26
uScm
Cond
fluor
ide
036
7
2 3
chlo
ride
55
32
5 brom
ide
-00
26
nitr
ate
012
7
sulp
hate
20
767
9
Australia Radium Hill
Different type of uranium deposits
Different processes for U extraction
Different mineral acids are used
Acid remainings
fluor
ide
chlo
ride
brom
ide
nitr
ate
sulp
hate
fluor
ide
chlo
ride
nitr
ate
sulp
hate
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 28
NO3SO4
0
01
02
03
04
05
06
07
08
09
1
Sout
h Al
ligat
or
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y Ka
thle
en
ESI U
SA
ESI C
anad
a
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Stan
rock
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lake
Mad
awas
ka
Mac
assa
Nor
th S
pan
Milli
ken
Lake
Eldo
rado
Stan
leig
h
FCl
0
05
1
15
2
25
3
35
4
45
5
Sou
th A
lliga
tor
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y K
athl
een
ES
I US
A
ES
I Can
ada
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Sta
nroc
k
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lak
e
Mad
awas
ka
Mac
assa
Nor
th S
pan
Mill
iken
Lak
e
Eld
orad
o
Sta
nlei
gh
Anion ratios
Phosphorite oresQuartz-pebble conglomerate and vein deposits
Nitric acid leaching rArr
Indicator of the processApatite mineral Ca5(PO4)3(FClOH)
rArr Indicator of the deposit type
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 29
Sandstone basal channel Quartz-pebble
conglomerate
Phosphorite
Black shale
Statistical evaluation of UOC data
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 30
U productsbull U ores
bull U ore concentrates
bull U oxide powders
bull UF4 and UF6
bull U pellets
Next step - Vertical study
Aim Identify the impurities that are acquired from or lost in the process What is the effect on the impurities from the source material
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 31
Uranium oreconcentrates
Process stagesamples and reagents
UO3
Next step - Vertical study
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 32
Case study
Backgroundbull uranium raw material of unknown
originbull 2003 Rotterdam (NL)bull Brownish yellow powder ~3 kgbull Found on a shipload from Jordan
Measurements performed at ITUbull NDA analysisbull Isotope ratio measurements (U Sr
Pb)bull Infrared analysisbull Impurity analysisbull REE pattern determination
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 33
Case study
Vibrational Spectrum (Infrared Spectrometry)
bull Compound is AUC xH2Obull Sulfate impurity (from dissolution of starting material)
bullNitrate impurity (from solvent extractionpurification)
Mass Spectrometry
bull Natural uranium isotopic compositionbull Natural lead isotopic composition
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 34
Case study
Sr Isotope Ratio
Low value typical for phosphorites (eg North Africa Middle East UShellip)
070757 plusmn 000011
070814 plusmn 000004
071092 plusmn 000006
071416 plusmn 000011
071985 plusmn 000029
072336 plusmn 000004
073434 plusmn 000012
070785 plusmn 000004
071775 plusmn 000003
067 068 069 070 071 072 073 074 075 076 077 078 079 080
Beverley
Calgary
Key Lake
Olympic Dam
Ranger
Ranstad
Stanrock
Mulberry
Fund-26
87Sr86Sr Isotope RatioSr-87 Sr-86 isotope ratio
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 35
Case study
Age dating based on 234U230Th
Age dating based on 232Th228Th
Last chemical separation 1988 plusmn 5 yndash Applicable to samples with incomplete Th separationndash Complementary to 234U230Th method
Last chemical separation 1893 plusmn 17 y
ndash Measured value shows significant positive biasndash Reason incomplete separation of 230Th from the
parent 234U nuclide(ldquoclock is not set to zerordquo)
ndash Residual 230Th cannot be calculated or corrected for
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 36
Case study ndash Find-26
bull 234U abundance suggests low temperature redox deposit value agrees with data reported by IAEA for UOC from Al Qaim (Iraq)
bull Impurities high P contentsimilar metallic impurities to Iraqi phosphate deposits
bull Pb isotopes natural young deposit low U content in orebull REE pattern flat no Eu or Ce anomaly rarr previously found
in certain sandstone-type and reworked phosphorite
Data inherent to the material corroborate information from external sources
Identification of origin based onSingle sampleMultiple parameters
Identification of origin based onSingle sampleMultiple parameters
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 37
Comparison of relative efforts ndash yellow cake
(5)(5)SIMSU particle analysis(5)Evaluation and Report
MC-ICP-MSMC-ICP-MSICP-MSIR-Spectroscopy RamanIon ChromatographyICP-MS IDMS
Electron Microscopy EDX WDXOptical MicroscopyICP-MSTIMSTitration IDMS
Technique
1853Total
15Nd Isotopes15Sr Isotopes3Rare Earth Elemental pattern1Molecular structure
15Anionic impurities3Age dating
3Micromorphology1Visual inspection macroscopic11Impurities11Isotopic Composition11Element Assay
ForensicsSafeguardsAnalysisParameter
Note rounded figures based on a full cost evaluation figures in brackets are not included in the Total
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 38
Conclusions
Wealth of information inherent to nuclear materialDecrypting the information requires sophisticated methodology subject matter expertise and reference dataSignificant effort (resources and time) needed for comprehensive analysis and data interpretationNuclear forensics methodology may open new avenuesin different areasApplication of investigative techniques in Safeguards has to be evaluated
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 19
ndash Where is the uranium coming from
Date of Production second half of 1943
Authentic cube
Belgian Congo or Joachimsthal (Czech Republic)
rare earth element pattern
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 20
Samples measured
ndash Haigerloch (ldquoHeisenbergrdquo) uranium cube
ndash Heidelberg (ldquoWirtzrdquo) uranium plates
ndash Yellow cake from Otto Hahnrsquos laboratory in Berlin
ndash For comparisonJoachimsthal uranium ore (bdquohistoricldquo sample)Congo uranium ore
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 21
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
REF
REF
REF
REF
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 22
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
REF
REF
REF
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 23
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
REF
REF
Congo UOC
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 24
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
Ore fromJoachimstalREF
Congo UOC
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 25
Inorganic FT-IR measurement of UOC samplesMeasurement in pellet form using KBrRapid identification of compound (oxide peroxide ADU AUC partially
calcined samples)Detection of certain process-related impurities (sulphate carbonate
nitrate)
Uranium composition in UOCs
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 26
Nitrate (1380 cm-1)Impurity from eluate or back extractant
Sulphate (1130 cm-1)Residual from H2SO4 eluate or back extractant
Uranium composition in UOCs
U-O vibration
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 27
Anion residuals in UOCrsquos
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
20
40
60
80
100
120
140
160
180
200
uScm
Cond
fluor
ide
102
2
2 chlo
ride
02
19
4 5 6 7 nitr
ate
003
6
sulp
hate
479
129
Canada ESI
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
17
18
19
20
21
22
23
24
25
26
uScm
Cond
fluor
ide
036
7
2 3
chlo
ride
55
32
5 brom
ide
-00
26
nitr
ate
012
7
sulp
hate
20
767
9
Australia Radium Hill
Different type of uranium deposits
Different processes for U extraction
Different mineral acids are used
Acid remainings
fluor
ide
chlo
ride
brom
ide
nitr
ate
sulp
hate
fluor
ide
chlo
ride
nitr
ate
sulp
hate
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 28
NO3SO4
0
01
02
03
04
05
06
07
08
09
1
Sout
h Al
ligat
or
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y Ka
thle
en
ESI U
SA
ESI C
anad
a
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Stan
rock
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lake
Mad
awas
ka
Mac
assa
Nor
th S
pan
Milli
ken
Lake
Eldo
rado
Stan
leig
h
FCl
0
05
1
15
2
25
3
35
4
45
5
Sou
th A
lliga
tor
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y K
athl
een
ES
I US
A
ES
I Can
ada
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Sta
nroc
k
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lak
e
Mad
awas
ka
Mac
assa
Nor
th S
pan
Mill
iken
Lak
e
Eld
orad
o
Sta
nlei
gh
Anion ratios
Phosphorite oresQuartz-pebble conglomerate and vein deposits
Nitric acid leaching rArr
Indicator of the processApatite mineral Ca5(PO4)3(FClOH)
rArr Indicator of the deposit type
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 29
Sandstone basal channel Quartz-pebble
conglomerate
Phosphorite
Black shale
Statistical evaluation of UOC data
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 30
U productsbull U ores
bull U ore concentrates
bull U oxide powders
bull UF4 and UF6
bull U pellets
Next step - Vertical study
Aim Identify the impurities that are acquired from or lost in the process What is the effect on the impurities from the source material
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 31
Uranium oreconcentrates
Process stagesamples and reagents
UO3
Next step - Vertical study
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 32
Case study
Backgroundbull uranium raw material of unknown
originbull 2003 Rotterdam (NL)bull Brownish yellow powder ~3 kgbull Found on a shipload from Jordan
Measurements performed at ITUbull NDA analysisbull Isotope ratio measurements (U Sr
Pb)bull Infrared analysisbull Impurity analysisbull REE pattern determination
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 33
Case study
Vibrational Spectrum (Infrared Spectrometry)
bull Compound is AUC xH2Obull Sulfate impurity (from dissolution of starting material)
bullNitrate impurity (from solvent extractionpurification)
Mass Spectrometry
bull Natural uranium isotopic compositionbull Natural lead isotopic composition
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 34
Case study
Sr Isotope Ratio
Low value typical for phosphorites (eg North Africa Middle East UShellip)
070757 plusmn 000011
070814 plusmn 000004
071092 plusmn 000006
071416 plusmn 000011
071985 plusmn 000029
072336 plusmn 000004
073434 plusmn 000012
070785 plusmn 000004
071775 plusmn 000003
067 068 069 070 071 072 073 074 075 076 077 078 079 080
Beverley
Calgary
Key Lake
Olympic Dam
Ranger
Ranstad
Stanrock
Mulberry
Fund-26
87Sr86Sr Isotope RatioSr-87 Sr-86 isotope ratio
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 35
Case study
Age dating based on 234U230Th
Age dating based on 232Th228Th
Last chemical separation 1988 plusmn 5 yndash Applicable to samples with incomplete Th separationndash Complementary to 234U230Th method
Last chemical separation 1893 plusmn 17 y
ndash Measured value shows significant positive biasndash Reason incomplete separation of 230Th from the
parent 234U nuclide(ldquoclock is not set to zerordquo)
ndash Residual 230Th cannot be calculated or corrected for
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 36
Case study ndash Find-26
bull 234U abundance suggests low temperature redox deposit value agrees with data reported by IAEA for UOC from Al Qaim (Iraq)
bull Impurities high P contentsimilar metallic impurities to Iraqi phosphate deposits
bull Pb isotopes natural young deposit low U content in orebull REE pattern flat no Eu or Ce anomaly rarr previously found
in certain sandstone-type and reworked phosphorite
Data inherent to the material corroborate information from external sources
Identification of origin based onSingle sampleMultiple parameters
Identification of origin based onSingle sampleMultiple parameters
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 37
Comparison of relative efforts ndash yellow cake
(5)(5)SIMSU particle analysis(5)Evaluation and Report
MC-ICP-MSMC-ICP-MSICP-MSIR-Spectroscopy RamanIon ChromatographyICP-MS IDMS
Electron Microscopy EDX WDXOptical MicroscopyICP-MSTIMSTitration IDMS
Technique
1853Total
15Nd Isotopes15Sr Isotopes3Rare Earth Elemental pattern1Molecular structure
15Anionic impurities3Age dating
3Micromorphology1Visual inspection macroscopic11Impurities11Isotopic Composition11Element Assay
ForensicsSafeguardsAnalysisParameter
Note rounded figures based on a full cost evaluation figures in brackets are not included in the Total
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 38
Conclusions
Wealth of information inherent to nuclear materialDecrypting the information requires sophisticated methodology subject matter expertise and reference dataSignificant effort (resources and time) needed for comprehensive analysis and data interpretationNuclear forensics methodology may open new avenuesin different areasApplication of investigative techniques in Safeguards has to be evaluated
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 20
Samples measured
ndash Haigerloch (ldquoHeisenbergrdquo) uranium cube
ndash Heidelberg (ldquoWirtzrdquo) uranium plates
ndash Yellow cake from Otto Hahnrsquos laboratory in Berlin
ndash For comparisonJoachimsthal uranium ore (bdquohistoricldquo sample)Congo uranium ore
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 21
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
REF
REF
REF
REF
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 22
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
REF
REF
REF
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 23
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
REF
REF
Congo UOC
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 24
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
Ore fromJoachimstalREF
Congo UOC
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 25
Inorganic FT-IR measurement of UOC samplesMeasurement in pellet form using KBrRapid identification of compound (oxide peroxide ADU AUC partially
calcined samples)Detection of certain process-related impurities (sulphate carbonate
nitrate)
Uranium composition in UOCs
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 26
Nitrate (1380 cm-1)Impurity from eluate or back extractant
Sulphate (1130 cm-1)Residual from H2SO4 eluate or back extractant
Uranium composition in UOCs
U-O vibration
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 27
Anion residuals in UOCrsquos
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
20
40
60
80
100
120
140
160
180
200
uScm
Cond
fluor
ide
102
2
2 chlo
ride
02
19
4 5 6 7 nitr
ate
003
6
sulp
hate
479
129
Canada ESI
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
17
18
19
20
21
22
23
24
25
26
uScm
Cond
fluor
ide
036
7
2 3
chlo
ride
55
32
5 brom
ide
-00
26
nitr
ate
012
7
sulp
hate
20
767
9
Australia Radium Hill
Different type of uranium deposits
Different processes for U extraction
Different mineral acids are used
Acid remainings
fluor
ide
chlo
ride
brom
ide
nitr
ate
sulp
hate
fluor
ide
chlo
ride
nitr
ate
sulp
hate
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 28
NO3SO4
0
01
02
03
04
05
06
07
08
09
1
Sout
h Al
ligat
or
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y Ka
thle
en
ESI U
SA
ESI C
anad
a
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Stan
rock
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lake
Mad
awas
ka
Mac
assa
Nor
th S
pan
Milli
ken
Lake
Eldo
rado
Stan
leig
h
FCl
0
05
1
15
2
25
3
35
4
45
5
Sou
th A
lliga
tor
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y K
athl
een
ES
I US
A
ES
I Can
ada
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Sta
nroc
k
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lak
e
Mad
awas
ka
Mac
assa
Nor
th S
pan
Mill
iken
Lak
e
Eld
orad
o
Sta
nlei
gh
Anion ratios
Phosphorite oresQuartz-pebble conglomerate and vein deposits
Nitric acid leaching rArr
Indicator of the processApatite mineral Ca5(PO4)3(FClOH)
rArr Indicator of the deposit type
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 29
Sandstone basal channel Quartz-pebble
conglomerate
Phosphorite
Black shale
Statistical evaluation of UOC data
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 30
U productsbull U ores
bull U ore concentrates
bull U oxide powders
bull UF4 and UF6
bull U pellets
Next step - Vertical study
Aim Identify the impurities that are acquired from or lost in the process What is the effect on the impurities from the source material
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 31
Uranium oreconcentrates
Process stagesamples and reagents
UO3
Next step - Vertical study
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 32
Case study
Backgroundbull uranium raw material of unknown
originbull 2003 Rotterdam (NL)bull Brownish yellow powder ~3 kgbull Found on a shipload from Jordan
Measurements performed at ITUbull NDA analysisbull Isotope ratio measurements (U Sr
Pb)bull Infrared analysisbull Impurity analysisbull REE pattern determination
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 33
Case study
Vibrational Spectrum (Infrared Spectrometry)
bull Compound is AUC xH2Obull Sulfate impurity (from dissolution of starting material)
bullNitrate impurity (from solvent extractionpurification)
Mass Spectrometry
bull Natural uranium isotopic compositionbull Natural lead isotopic composition
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 34
Case study
Sr Isotope Ratio
Low value typical for phosphorites (eg North Africa Middle East UShellip)
070757 plusmn 000011
070814 plusmn 000004
071092 plusmn 000006
071416 plusmn 000011
071985 plusmn 000029
072336 plusmn 000004
073434 plusmn 000012
070785 plusmn 000004
071775 plusmn 000003
067 068 069 070 071 072 073 074 075 076 077 078 079 080
Beverley
Calgary
Key Lake
Olympic Dam
Ranger
Ranstad
Stanrock
Mulberry
Fund-26
87Sr86Sr Isotope RatioSr-87 Sr-86 isotope ratio
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 35
Case study
Age dating based on 234U230Th
Age dating based on 232Th228Th
Last chemical separation 1988 plusmn 5 yndash Applicable to samples with incomplete Th separationndash Complementary to 234U230Th method
Last chemical separation 1893 plusmn 17 y
ndash Measured value shows significant positive biasndash Reason incomplete separation of 230Th from the
parent 234U nuclide(ldquoclock is not set to zerordquo)
ndash Residual 230Th cannot be calculated or corrected for
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 36
Case study ndash Find-26
bull 234U abundance suggests low temperature redox deposit value agrees with data reported by IAEA for UOC from Al Qaim (Iraq)
bull Impurities high P contentsimilar metallic impurities to Iraqi phosphate deposits
bull Pb isotopes natural young deposit low U content in orebull REE pattern flat no Eu or Ce anomaly rarr previously found
in certain sandstone-type and reworked phosphorite
Data inherent to the material corroborate information from external sources
Identification of origin based onSingle sampleMultiple parameters
Identification of origin based onSingle sampleMultiple parameters
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 37
Comparison of relative efforts ndash yellow cake
(5)(5)SIMSU particle analysis(5)Evaluation and Report
MC-ICP-MSMC-ICP-MSICP-MSIR-Spectroscopy RamanIon ChromatographyICP-MS IDMS
Electron Microscopy EDX WDXOptical MicroscopyICP-MSTIMSTitration IDMS
Technique
1853Total
15Nd Isotopes15Sr Isotopes3Rare Earth Elemental pattern1Molecular structure
15Anionic impurities3Age dating
3Micromorphology1Visual inspection macroscopic11Impurities11Isotopic Composition11Element Assay
ForensicsSafeguardsAnalysisParameter
Note rounded figures based on a full cost evaluation figures in brackets are not included in the Total
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 38
Conclusions
Wealth of information inherent to nuclear materialDecrypting the information requires sophisticated methodology subject matter expertise and reference dataSignificant effort (resources and time) needed for comprehensive analysis and data interpretationNuclear forensics methodology may open new avenuesin different areasApplication of investigative techniques in Safeguards has to be evaluated
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 21
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
REF
REF
REF
REF
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 22
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
REF
REF
REF
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 23
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
REF
REF
Congo UOC
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 24
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
Ore fromJoachimstalREF
Congo UOC
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 25
Inorganic FT-IR measurement of UOC samplesMeasurement in pellet form using KBrRapid identification of compound (oxide peroxide ADU AUC partially
calcined samples)Detection of certain process-related impurities (sulphate carbonate
nitrate)
Uranium composition in UOCs
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 26
Nitrate (1380 cm-1)Impurity from eluate or back extractant
Sulphate (1130 cm-1)Residual from H2SO4 eluate or back extractant
Uranium composition in UOCs
U-O vibration
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 27
Anion residuals in UOCrsquos
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
20
40
60
80
100
120
140
160
180
200
uScm
Cond
fluor
ide
102
2
2 chlo
ride
02
19
4 5 6 7 nitr
ate
003
6
sulp
hate
479
129
Canada ESI
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
17
18
19
20
21
22
23
24
25
26
uScm
Cond
fluor
ide
036
7
2 3
chlo
ride
55
32
5 brom
ide
-00
26
nitr
ate
012
7
sulp
hate
20
767
9
Australia Radium Hill
Different type of uranium deposits
Different processes for U extraction
Different mineral acids are used
Acid remainings
fluor
ide
chlo
ride
brom
ide
nitr
ate
sulp
hate
fluor
ide
chlo
ride
nitr
ate
sulp
hate
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 28
NO3SO4
0
01
02
03
04
05
06
07
08
09
1
Sout
h Al
ligat
or
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y Ka
thle
en
ESI U
SA
ESI C
anad
a
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Stan
rock
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lake
Mad
awas
ka
Mac
assa
Nor
th S
pan
Milli
ken
Lake
Eldo
rado
Stan
leig
h
FCl
0
05
1
15
2
25
3
35
4
45
5
Sou
th A
lliga
tor
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y K
athl
een
ES
I US
A
ES
I Can
ada
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Sta
nroc
k
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lak
e
Mad
awas
ka
Mac
assa
Nor
th S
pan
Mill
iken
Lak
e
Eld
orad
o
Sta
nlei
gh
Anion ratios
Phosphorite oresQuartz-pebble conglomerate and vein deposits
Nitric acid leaching rArr
Indicator of the processApatite mineral Ca5(PO4)3(FClOH)
rArr Indicator of the deposit type
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 29
Sandstone basal channel Quartz-pebble
conglomerate
Phosphorite
Black shale
Statistical evaluation of UOC data
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 30
U productsbull U ores
bull U ore concentrates
bull U oxide powders
bull UF4 and UF6
bull U pellets
Next step - Vertical study
Aim Identify the impurities that are acquired from or lost in the process What is the effect on the impurities from the source material
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 31
Uranium oreconcentrates
Process stagesamples and reagents
UO3
Next step - Vertical study
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 32
Case study
Backgroundbull uranium raw material of unknown
originbull 2003 Rotterdam (NL)bull Brownish yellow powder ~3 kgbull Found on a shipload from Jordan
Measurements performed at ITUbull NDA analysisbull Isotope ratio measurements (U Sr
Pb)bull Infrared analysisbull Impurity analysisbull REE pattern determination
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 33
Case study
Vibrational Spectrum (Infrared Spectrometry)
bull Compound is AUC xH2Obull Sulfate impurity (from dissolution of starting material)
bullNitrate impurity (from solvent extractionpurification)
Mass Spectrometry
bull Natural uranium isotopic compositionbull Natural lead isotopic composition
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 34
Case study
Sr Isotope Ratio
Low value typical for phosphorites (eg North Africa Middle East UShellip)
070757 plusmn 000011
070814 plusmn 000004
071092 plusmn 000006
071416 plusmn 000011
071985 plusmn 000029
072336 plusmn 000004
073434 plusmn 000012
070785 plusmn 000004
071775 plusmn 000003
067 068 069 070 071 072 073 074 075 076 077 078 079 080
Beverley
Calgary
Key Lake
Olympic Dam
Ranger
Ranstad
Stanrock
Mulberry
Fund-26
87Sr86Sr Isotope RatioSr-87 Sr-86 isotope ratio
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 35
Case study
Age dating based on 234U230Th
Age dating based on 232Th228Th
Last chemical separation 1988 plusmn 5 yndash Applicable to samples with incomplete Th separationndash Complementary to 234U230Th method
Last chemical separation 1893 plusmn 17 y
ndash Measured value shows significant positive biasndash Reason incomplete separation of 230Th from the
parent 234U nuclide(ldquoclock is not set to zerordquo)
ndash Residual 230Th cannot be calculated or corrected for
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 36
Case study ndash Find-26
bull 234U abundance suggests low temperature redox deposit value agrees with data reported by IAEA for UOC from Al Qaim (Iraq)
bull Impurities high P contentsimilar metallic impurities to Iraqi phosphate deposits
bull Pb isotopes natural young deposit low U content in orebull REE pattern flat no Eu or Ce anomaly rarr previously found
in certain sandstone-type and reworked phosphorite
Data inherent to the material corroborate information from external sources
Identification of origin based onSingle sampleMultiple parameters
Identification of origin based onSingle sampleMultiple parameters
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 37
Comparison of relative efforts ndash yellow cake
(5)(5)SIMSU particle analysis(5)Evaluation and Report
MC-ICP-MSMC-ICP-MSICP-MSIR-Spectroscopy RamanIon ChromatographyICP-MS IDMS
Electron Microscopy EDX WDXOptical MicroscopyICP-MSTIMSTitration IDMS
Technique
1853Total
15Nd Isotopes15Sr Isotopes3Rare Earth Elemental pattern1Molecular structure
15Anionic impurities3Age dating
3Micromorphology1Visual inspection macroscopic11Impurities11Isotopic Composition11Element Assay
ForensicsSafeguardsAnalysisParameter
Note rounded figures based on a full cost evaluation figures in brackets are not included in the Total
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 38
Conclusions
Wealth of information inherent to nuclear materialDecrypting the information requires sophisticated methodology subject matter expertise and reference dataSignificant effort (resources and time) needed for comprehensive analysis and data interpretationNuclear forensics methodology may open new avenuesin different areasApplication of investigative techniques in Safeguards has to be evaluated
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 22
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
REF
REF
REF
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 23
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
REF
REF
Congo UOC
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 24
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
Ore fromJoachimstalREF
Congo UOC
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 25
Inorganic FT-IR measurement of UOC samplesMeasurement in pellet form using KBrRapid identification of compound (oxide peroxide ADU AUC partially
calcined samples)Detection of certain process-related impurities (sulphate carbonate
nitrate)
Uranium composition in UOCs
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 26
Nitrate (1380 cm-1)Impurity from eluate or back extractant
Sulphate (1130 cm-1)Residual from H2SO4 eluate or back extractant
Uranium composition in UOCs
U-O vibration
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 27
Anion residuals in UOCrsquos
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
20
40
60
80
100
120
140
160
180
200
uScm
Cond
fluor
ide
102
2
2 chlo
ride
02
19
4 5 6 7 nitr
ate
003
6
sulp
hate
479
129
Canada ESI
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
17
18
19
20
21
22
23
24
25
26
uScm
Cond
fluor
ide
036
7
2 3
chlo
ride
55
32
5 brom
ide
-00
26
nitr
ate
012
7
sulp
hate
20
767
9
Australia Radium Hill
Different type of uranium deposits
Different processes for U extraction
Different mineral acids are used
Acid remainings
fluor
ide
chlo
ride
brom
ide
nitr
ate
sulp
hate
fluor
ide
chlo
ride
nitr
ate
sulp
hate
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 28
NO3SO4
0
01
02
03
04
05
06
07
08
09
1
Sout
h Al
ligat
or
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y Ka
thle
en
ESI U
SA
ESI C
anad
a
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Stan
rock
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lake
Mad
awas
ka
Mac
assa
Nor
th S
pan
Milli
ken
Lake
Eldo
rado
Stan
leig
h
FCl
0
05
1
15
2
25
3
35
4
45
5
Sou
th A
lliga
tor
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y K
athl
een
ES
I US
A
ES
I Can
ada
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Sta
nroc
k
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lak
e
Mad
awas
ka
Mac
assa
Nor
th S
pan
Mill
iken
Lak
e
Eld
orad
o
Sta
nlei
gh
Anion ratios
Phosphorite oresQuartz-pebble conglomerate and vein deposits
Nitric acid leaching rArr
Indicator of the processApatite mineral Ca5(PO4)3(FClOH)
rArr Indicator of the deposit type
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 29
Sandstone basal channel Quartz-pebble
conglomerate
Phosphorite
Black shale
Statistical evaluation of UOC data
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 30
U productsbull U ores
bull U ore concentrates
bull U oxide powders
bull UF4 and UF6
bull U pellets
Next step - Vertical study
Aim Identify the impurities that are acquired from or lost in the process What is the effect on the impurities from the source material
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 31
Uranium oreconcentrates
Process stagesamples and reagents
UO3
Next step - Vertical study
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 32
Case study
Backgroundbull uranium raw material of unknown
originbull 2003 Rotterdam (NL)bull Brownish yellow powder ~3 kgbull Found on a shipload from Jordan
Measurements performed at ITUbull NDA analysisbull Isotope ratio measurements (U Sr
Pb)bull Infrared analysisbull Impurity analysisbull REE pattern determination
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 33
Case study
Vibrational Spectrum (Infrared Spectrometry)
bull Compound is AUC xH2Obull Sulfate impurity (from dissolution of starting material)
bullNitrate impurity (from solvent extractionpurification)
Mass Spectrometry
bull Natural uranium isotopic compositionbull Natural lead isotopic composition
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 34
Case study
Sr Isotope Ratio
Low value typical for phosphorites (eg North Africa Middle East UShellip)
070757 plusmn 000011
070814 plusmn 000004
071092 plusmn 000006
071416 plusmn 000011
071985 plusmn 000029
072336 plusmn 000004
073434 plusmn 000012
070785 plusmn 000004
071775 plusmn 000003
067 068 069 070 071 072 073 074 075 076 077 078 079 080
Beverley
Calgary
Key Lake
Olympic Dam
Ranger
Ranstad
Stanrock
Mulberry
Fund-26
87Sr86Sr Isotope RatioSr-87 Sr-86 isotope ratio
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 35
Case study
Age dating based on 234U230Th
Age dating based on 232Th228Th
Last chemical separation 1988 plusmn 5 yndash Applicable to samples with incomplete Th separationndash Complementary to 234U230Th method
Last chemical separation 1893 plusmn 17 y
ndash Measured value shows significant positive biasndash Reason incomplete separation of 230Th from the
parent 234U nuclide(ldquoclock is not set to zerordquo)
ndash Residual 230Th cannot be calculated or corrected for
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 36
Case study ndash Find-26
bull 234U abundance suggests low temperature redox deposit value agrees with data reported by IAEA for UOC from Al Qaim (Iraq)
bull Impurities high P contentsimilar metallic impurities to Iraqi phosphate deposits
bull Pb isotopes natural young deposit low U content in orebull REE pattern flat no Eu or Ce anomaly rarr previously found
in certain sandstone-type and reworked phosphorite
Data inherent to the material corroborate information from external sources
Identification of origin based onSingle sampleMultiple parameters
Identification of origin based onSingle sampleMultiple parameters
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 37
Comparison of relative efforts ndash yellow cake
(5)(5)SIMSU particle analysis(5)Evaluation and Report
MC-ICP-MSMC-ICP-MSICP-MSIR-Spectroscopy RamanIon ChromatographyICP-MS IDMS
Electron Microscopy EDX WDXOptical MicroscopyICP-MSTIMSTitration IDMS
Technique
1853Total
15Nd Isotopes15Sr Isotopes3Rare Earth Elemental pattern1Molecular structure
15Anionic impurities3Age dating
3Micromorphology1Visual inspection macroscopic11Impurities11Isotopic Composition11Element Assay
ForensicsSafeguardsAnalysisParameter
Note rounded figures based on a full cost evaluation figures in brackets are not included in the Total
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 38
Conclusions
Wealth of information inherent to nuclear materialDecrypting the information requires sophisticated methodology subject matter expertise and reference dataSignificant effort (resources and time) needed for comprehensive analysis and data interpretationNuclear forensics methodology may open new avenuesin different areasApplication of investigative techniques in Safeguards has to be evaluated
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 23
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
REF
REF
Congo UOC
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 24
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
Ore fromJoachimstalREF
Congo UOC
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 25
Inorganic FT-IR measurement of UOC samplesMeasurement in pellet form using KBrRapid identification of compound (oxide peroxide ADU AUC partially
calcined samples)Detection of certain process-related impurities (sulphate carbonate
nitrate)
Uranium composition in UOCs
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 26
Nitrate (1380 cm-1)Impurity from eluate or back extractant
Sulphate (1130 cm-1)Residual from H2SO4 eluate or back extractant
Uranium composition in UOCs
U-O vibration
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 27
Anion residuals in UOCrsquos
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
20
40
60
80
100
120
140
160
180
200
uScm
Cond
fluor
ide
102
2
2 chlo
ride
02
19
4 5 6 7 nitr
ate
003
6
sulp
hate
479
129
Canada ESI
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
17
18
19
20
21
22
23
24
25
26
uScm
Cond
fluor
ide
036
7
2 3
chlo
ride
55
32
5 brom
ide
-00
26
nitr
ate
012
7
sulp
hate
20
767
9
Australia Radium Hill
Different type of uranium deposits
Different processes for U extraction
Different mineral acids are used
Acid remainings
fluor
ide
chlo
ride
brom
ide
nitr
ate
sulp
hate
fluor
ide
chlo
ride
nitr
ate
sulp
hate
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 28
NO3SO4
0
01
02
03
04
05
06
07
08
09
1
Sout
h Al
ligat
or
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y Ka
thle
en
ESI U
SA
ESI C
anad
a
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Stan
rock
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lake
Mad
awas
ka
Mac
assa
Nor
th S
pan
Milli
ken
Lake
Eldo
rado
Stan
leig
h
FCl
0
05
1
15
2
25
3
35
4
45
5
Sou
th A
lliga
tor
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y K
athl
een
ES
I US
A
ES
I Can
ada
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Sta
nroc
k
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lak
e
Mad
awas
ka
Mac
assa
Nor
th S
pan
Mill
iken
Lak
e
Eld
orad
o
Sta
nlei
gh
Anion ratios
Phosphorite oresQuartz-pebble conglomerate and vein deposits
Nitric acid leaching rArr
Indicator of the processApatite mineral Ca5(PO4)3(FClOH)
rArr Indicator of the deposit type
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 29
Sandstone basal channel Quartz-pebble
conglomerate
Phosphorite
Black shale
Statistical evaluation of UOC data
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 30
U productsbull U ores
bull U ore concentrates
bull U oxide powders
bull UF4 and UF6
bull U pellets
Next step - Vertical study
Aim Identify the impurities that are acquired from or lost in the process What is the effect on the impurities from the source material
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 31
Uranium oreconcentrates
Process stagesamples and reagents
UO3
Next step - Vertical study
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 32
Case study
Backgroundbull uranium raw material of unknown
originbull 2003 Rotterdam (NL)bull Brownish yellow powder ~3 kgbull Found on a shipload from Jordan
Measurements performed at ITUbull NDA analysisbull Isotope ratio measurements (U Sr
Pb)bull Infrared analysisbull Impurity analysisbull REE pattern determination
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 33
Case study
Vibrational Spectrum (Infrared Spectrometry)
bull Compound is AUC xH2Obull Sulfate impurity (from dissolution of starting material)
bullNitrate impurity (from solvent extractionpurification)
Mass Spectrometry
bull Natural uranium isotopic compositionbull Natural lead isotopic composition
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 34
Case study
Sr Isotope Ratio
Low value typical for phosphorites (eg North Africa Middle East UShellip)
070757 plusmn 000011
070814 plusmn 000004
071092 plusmn 000006
071416 plusmn 000011
071985 plusmn 000029
072336 plusmn 000004
073434 plusmn 000012
070785 plusmn 000004
071775 plusmn 000003
067 068 069 070 071 072 073 074 075 076 077 078 079 080
Beverley
Calgary
Key Lake
Olympic Dam
Ranger
Ranstad
Stanrock
Mulberry
Fund-26
87Sr86Sr Isotope RatioSr-87 Sr-86 isotope ratio
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 35
Case study
Age dating based on 234U230Th
Age dating based on 232Th228Th
Last chemical separation 1988 plusmn 5 yndash Applicable to samples with incomplete Th separationndash Complementary to 234U230Th method
Last chemical separation 1893 plusmn 17 y
ndash Measured value shows significant positive biasndash Reason incomplete separation of 230Th from the
parent 234U nuclide(ldquoclock is not set to zerordquo)
ndash Residual 230Th cannot be calculated or corrected for
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 36
Case study ndash Find-26
bull 234U abundance suggests low temperature redox deposit value agrees with data reported by IAEA for UOC from Al Qaim (Iraq)
bull Impurities high P contentsimilar metallic impurities to Iraqi phosphate deposits
bull Pb isotopes natural young deposit low U content in orebull REE pattern flat no Eu or Ce anomaly rarr previously found
in certain sandstone-type and reworked phosphorite
Data inherent to the material corroborate information from external sources
Identification of origin based onSingle sampleMultiple parameters
Identification of origin based onSingle sampleMultiple parameters
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 37
Comparison of relative efforts ndash yellow cake
(5)(5)SIMSU particle analysis(5)Evaluation and Report
MC-ICP-MSMC-ICP-MSICP-MSIR-Spectroscopy RamanIon ChromatographyICP-MS IDMS
Electron Microscopy EDX WDXOptical MicroscopyICP-MSTIMSTitration IDMS
Technique
1853Total
15Nd Isotopes15Sr Isotopes3Rare Earth Elemental pattern1Molecular structure
15Anionic impurities3Age dating
3Micromorphology1Visual inspection macroscopic11Impurities11Isotopic Composition11Element Assay
ForensicsSafeguardsAnalysisParameter
Note rounded figures based on a full cost evaluation figures in brackets are not included in the Total
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 38
Conclusions
Wealth of information inherent to nuclear materialDecrypting the information requires sophisticated methodology subject matter expertise and reference dataSignificant effort (resources and time) needed for comprehensive analysis and data interpretationNuclear forensics methodology may open new avenuesin different areasApplication of investigative techniques in Safeguards has to be evaluated
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 24
From which mine did the uranium comeJaacutechymov Joachimsthal in the Czech Republic or Belgian Congo
measure the pattern of trace elements
Nuclear forensics
Haigerloch cube0
1
10
100
1000
10000
La Ce Pr Nd Sm Eu Gd Tb Dy Ho Er Tm Yb Lu
REE
Cho
ndrit
e
Heisenberg Cube
Wirtz plate
Hahn yellow cake
Ore fromJoachimstalREF
Congo UOC
gt 70 a
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 25
Inorganic FT-IR measurement of UOC samplesMeasurement in pellet form using KBrRapid identification of compound (oxide peroxide ADU AUC partially
calcined samples)Detection of certain process-related impurities (sulphate carbonate
nitrate)
Uranium composition in UOCs
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 26
Nitrate (1380 cm-1)Impurity from eluate or back extractant
Sulphate (1130 cm-1)Residual from H2SO4 eluate or back extractant
Uranium composition in UOCs
U-O vibration
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 27
Anion residuals in UOCrsquos
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
20
40
60
80
100
120
140
160
180
200
uScm
Cond
fluor
ide
102
2
2 chlo
ride
02
19
4 5 6 7 nitr
ate
003
6
sulp
hate
479
129
Canada ESI
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
17
18
19
20
21
22
23
24
25
26
uScm
Cond
fluor
ide
036
7
2 3
chlo
ride
55
32
5 brom
ide
-00
26
nitr
ate
012
7
sulp
hate
20
767
9
Australia Radium Hill
Different type of uranium deposits
Different processes for U extraction
Different mineral acids are used
Acid remainings
fluor
ide
chlo
ride
brom
ide
nitr
ate
sulp
hate
fluor
ide
chlo
ride
nitr
ate
sulp
hate
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 28
NO3SO4
0
01
02
03
04
05
06
07
08
09
1
Sout
h Al
ligat
or
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y Ka
thle
en
ESI U
SA
ESI C
anad
a
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Stan
rock
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lake
Mad
awas
ka
Mac
assa
Nor
th S
pan
Milli
ken
Lake
Eldo
rado
Stan
leig
h
FCl
0
05
1
15
2
25
3
35
4
45
5
Sou
th A
lliga
tor
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y K
athl
een
ES
I US
A
ES
I Can
ada
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Sta
nroc
k
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lak
e
Mad
awas
ka
Mac
assa
Nor
th S
pan
Mill
iken
Lak
e
Eld
orad
o
Sta
nlei
gh
Anion ratios
Phosphorite oresQuartz-pebble conglomerate and vein deposits
Nitric acid leaching rArr
Indicator of the processApatite mineral Ca5(PO4)3(FClOH)
rArr Indicator of the deposit type
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 29
Sandstone basal channel Quartz-pebble
conglomerate
Phosphorite
Black shale
Statistical evaluation of UOC data
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 30
U productsbull U ores
bull U ore concentrates
bull U oxide powders
bull UF4 and UF6
bull U pellets
Next step - Vertical study
Aim Identify the impurities that are acquired from or lost in the process What is the effect on the impurities from the source material
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 31
Uranium oreconcentrates
Process stagesamples and reagents
UO3
Next step - Vertical study
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 32
Case study
Backgroundbull uranium raw material of unknown
originbull 2003 Rotterdam (NL)bull Brownish yellow powder ~3 kgbull Found on a shipload from Jordan
Measurements performed at ITUbull NDA analysisbull Isotope ratio measurements (U Sr
Pb)bull Infrared analysisbull Impurity analysisbull REE pattern determination
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 33
Case study
Vibrational Spectrum (Infrared Spectrometry)
bull Compound is AUC xH2Obull Sulfate impurity (from dissolution of starting material)
bullNitrate impurity (from solvent extractionpurification)
Mass Spectrometry
bull Natural uranium isotopic compositionbull Natural lead isotopic composition
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 34
Case study
Sr Isotope Ratio
Low value typical for phosphorites (eg North Africa Middle East UShellip)
070757 plusmn 000011
070814 plusmn 000004
071092 plusmn 000006
071416 plusmn 000011
071985 plusmn 000029
072336 plusmn 000004
073434 plusmn 000012
070785 plusmn 000004
071775 plusmn 000003
067 068 069 070 071 072 073 074 075 076 077 078 079 080
Beverley
Calgary
Key Lake
Olympic Dam
Ranger
Ranstad
Stanrock
Mulberry
Fund-26
87Sr86Sr Isotope RatioSr-87 Sr-86 isotope ratio
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 35
Case study
Age dating based on 234U230Th
Age dating based on 232Th228Th
Last chemical separation 1988 plusmn 5 yndash Applicable to samples with incomplete Th separationndash Complementary to 234U230Th method
Last chemical separation 1893 plusmn 17 y
ndash Measured value shows significant positive biasndash Reason incomplete separation of 230Th from the
parent 234U nuclide(ldquoclock is not set to zerordquo)
ndash Residual 230Th cannot be calculated or corrected for
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 36
Case study ndash Find-26
bull 234U abundance suggests low temperature redox deposit value agrees with data reported by IAEA for UOC from Al Qaim (Iraq)
bull Impurities high P contentsimilar metallic impurities to Iraqi phosphate deposits
bull Pb isotopes natural young deposit low U content in orebull REE pattern flat no Eu or Ce anomaly rarr previously found
in certain sandstone-type and reworked phosphorite
Data inherent to the material corroborate information from external sources
Identification of origin based onSingle sampleMultiple parameters
Identification of origin based onSingle sampleMultiple parameters
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 37
Comparison of relative efforts ndash yellow cake
(5)(5)SIMSU particle analysis(5)Evaluation and Report
MC-ICP-MSMC-ICP-MSICP-MSIR-Spectroscopy RamanIon ChromatographyICP-MS IDMS
Electron Microscopy EDX WDXOptical MicroscopyICP-MSTIMSTitration IDMS
Technique
1853Total
15Nd Isotopes15Sr Isotopes3Rare Earth Elemental pattern1Molecular structure
15Anionic impurities3Age dating
3Micromorphology1Visual inspection macroscopic11Impurities11Isotopic Composition11Element Assay
ForensicsSafeguardsAnalysisParameter
Note rounded figures based on a full cost evaluation figures in brackets are not included in the Total
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 38
Conclusions
Wealth of information inherent to nuclear materialDecrypting the information requires sophisticated methodology subject matter expertise and reference dataSignificant effort (resources and time) needed for comprehensive analysis and data interpretationNuclear forensics methodology may open new avenuesin different areasApplication of investigative techniques in Safeguards has to be evaluated
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 25
Inorganic FT-IR measurement of UOC samplesMeasurement in pellet form using KBrRapid identification of compound (oxide peroxide ADU AUC partially
calcined samples)Detection of certain process-related impurities (sulphate carbonate
nitrate)
Uranium composition in UOCs
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 26
Nitrate (1380 cm-1)Impurity from eluate or back extractant
Sulphate (1130 cm-1)Residual from H2SO4 eluate or back extractant
Uranium composition in UOCs
U-O vibration
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 27
Anion residuals in UOCrsquos
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
20
40
60
80
100
120
140
160
180
200
uScm
Cond
fluor
ide
102
2
2 chlo
ride
02
19
4 5 6 7 nitr
ate
003
6
sulp
hate
479
129
Canada ESI
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
17
18
19
20
21
22
23
24
25
26
uScm
Cond
fluor
ide
036
7
2 3
chlo
ride
55
32
5 brom
ide
-00
26
nitr
ate
012
7
sulp
hate
20
767
9
Australia Radium Hill
Different type of uranium deposits
Different processes for U extraction
Different mineral acids are used
Acid remainings
fluor
ide
chlo
ride
brom
ide
nitr
ate
sulp
hate
fluor
ide
chlo
ride
nitr
ate
sulp
hate
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 28
NO3SO4
0
01
02
03
04
05
06
07
08
09
1
Sout
h Al
ligat
or
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y Ka
thle
en
ESI U
SA
ESI C
anad
a
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Stan
rock
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lake
Mad
awas
ka
Mac
assa
Nor
th S
pan
Milli
ken
Lake
Eldo
rado
Stan
leig
h
FCl
0
05
1
15
2
25
3
35
4
45
5
Sou
th A
lliga
tor
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y K
athl
een
ES
I US
A
ES
I Can
ada
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Sta
nroc
k
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lak
e
Mad
awas
ka
Mac
assa
Nor
th S
pan
Mill
iken
Lak
e
Eld
orad
o
Sta
nlei
gh
Anion ratios
Phosphorite oresQuartz-pebble conglomerate and vein deposits
Nitric acid leaching rArr
Indicator of the processApatite mineral Ca5(PO4)3(FClOH)
rArr Indicator of the deposit type
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 29
Sandstone basal channel Quartz-pebble
conglomerate
Phosphorite
Black shale
Statistical evaluation of UOC data
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 30
U productsbull U ores
bull U ore concentrates
bull U oxide powders
bull UF4 and UF6
bull U pellets
Next step - Vertical study
Aim Identify the impurities that are acquired from or lost in the process What is the effect on the impurities from the source material
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 31
Uranium oreconcentrates
Process stagesamples and reagents
UO3
Next step - Vertical study
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 32
Case study
Backgroundbull uranium raw material of unknown
originbull 2003 Rotterdam (NL)bull Brownish yellow powder ~3 kgbull Found on a shipload from Jordan
Measurements performed at ITUbull NDA analysisbull Isotope ratio measurements (U Sr
Pb)bull Infrared analysisbull Impurity analysisbull REE pattern determination
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 33
Case study
Vibrational Spectrum (Infrared Spectrometry)
bull Compound is AUC xH2Obull Sulfate impurity (from dissolution of starting material)
bullNitrate impurity (from solvent extractionpurification)
Mass Spectrometry
bull Natural uranium isotopic compositionbull Natural lead isotopic composition
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 34
Case study
Sr Isotope Ratio
Low value typical for phosphorites (eg North Africa Middle East UShellip)
070757 plusmn 000011
070814 plusmn 000004
071092 plusmn 000006
071416 plusmn 000011
071985 plusmn 000029
072336 plusmn 000004
073434 plusmn 000012
070785 plusmn 000004
071775 plusmn 000003
067 068 069 070 071 072 073 074 075 076 077 078 079 080
Beverley
Calgary
Key Lake
Olympic Dam
Ranger
Ranstad
Stanrock
Mulberry
Fund-26
87Sr86Sr Isotope RatioSr-87 Sr-86 isotope ratio
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 35
Case study
Age dating based on 234U230Th
Age dating based on 232Th228Th
Last chemical separation 1988 plusmn 5 yndash Applicable to samples with incomplete Th separationndash Complementary to 234U230Th method
Last chemical separation 1893 plusmn 17 y
ndash Measured value shows significant positive biasndash Reason incomplete separation of 230Th from the
parent 234U nuclide(ldquoclock is not set to zerordquo)
ndash Residual 230Th cannot be calculated or corrected for
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 36
Case study ndash Find-26
bull 234U abundance suggests low temperature redox deposit value agrees with data reported by IAEA for UOC from Al Qaim (Iraq)
bull Impurities high P contentsimilar metallic impurities to Iraqi phosphate deposits
bull Pb isotopes natural young deposit low U content in orebull REE pattern flat no Eu or Ce anomaly rarr previously found
in certain sandstone-type and reworked phosphorite
Data inherent to the material corroborate information from external sources
Identification of origin based onSingle sampleMultiple parameters
Identification of origin based onSingle sampleMultiple parameters
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 37
Comparison of relative efforts ndash yellow cake
(5)(5)SIMSU particle analysis(5)Evaluation and Report
MC-ICP-MSMC-ICP-MSICP-MSIR-Spectroscopy RamanIon ChromatographyICP-MS IDMS
Electron Microscopy EDX WDXOptical MicroscopyICP-MSTIMSTitration IDMS
Technique
1853Total
15Nd Isotopes15Sr Isotopes3Rare Earth Elemental pattern1Molecular structure
15Anionic impurities3Age dating
3Micromorphology1Visual inspection macroscopic11Impurities11Isotopic Composition11Element Assay
ForensicsSafeguardsAnalysisParameter
Note rounded figures based on a full cost evaluation figures in brackets are not included in the Total
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 38
Conclusions
Wealth of information inherent to nuclear materialDecrypting the information requires sophisticated methodology subject matter expertise and reference dataSignificant effort (resources and time) needed for comprehensive analysis and data interpretationNuclear forensics methodology may open new avenuesin different areasApplication of investigative techniques in Safeguards has to be evaluated
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 26
Nitrate (1380 cm-1)Impurity from eluate or back extractant
Sulphate (1130 cm-1)Residual from H2SO4 eluate or back extractant
Uranium composition in UOCs
U-O vibration
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 27
Anion residuals in UOCrsquos
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
20
40
60
80
100
120
140
160
180
200
uScm
Cond
fluor
ide
102
2
2 chlo
ride
02
19
4 5 6 7 nitr
ate
003
6
sulp
hate
479
129
Canada ESI
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
17
18
19
20
21
22
23
24
25
26
uScm
Cond
fluor
ide
036
7
2 3
chlo
ride
55
32
5 brom
ide
-00
26
nitr
ate
012
7
sulp
hate
20
767
9
Australia Radium Hill
Different type of uranium deposits
Different processes for U extraction
Different mineral acids are used
Acid remainings
fluor
ide
chlo
ride
brom
ide
nitr
ate
sulp
hate
fluor
ide
chlo
ride
nitr
ate
sulp
hate
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 28
NO3SO4
0
01
02
03
04
05
06
07
08
09
1
Sout
h Al
ligat
or
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y Ka
thle
en
ESI U
SA
ESI C
anad
a
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Stan
rock
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lake
Mad
awas
ka
Mac
assa
Nor
th S
pan
Milli
ken
Lake
Eldo
rado
Stan
leig
h
FCl
0
05
1
15
2
25
3
35
4
45
5
Sou
th A
lliga
tor
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y K
athl
een
ES
I US
A
ES
I Can
ada
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Sta
nroc
k
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lak
e
Mad
awas
ka
Mac
assa
Nor
th S
pan
Mill
iken
Lak
e
Eld
orad
o
Sta
nlei
gh
Anion ratios
Phosphorite oresQuartz-pebble conglomerate and vein deposits
Nitric acid leaching rArr
Indicator of the processApatite mineral Ca5(PO4)3(FClOH)
rArr Indicator of the deposit type
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 29
Sandstone basal channel Quartz-pebble
conglomerate
Phosphorite
Black shale
Statistical evaluation of UOC data
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 30
U productsbull U ores
bull U ore concentrates
bull U oxide powders
bull UF4 and UF6
bull U pellets
Next step - Vertical study
Aim Identify the impurities that are acquired from or lost in the process What is the effect on the impurities from the source material
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 31
Uranium oreconcentrates
Process stagesamples and reagents
UO3
Next step - Vertical study
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 32
Case study
Backgroundbull uranium raw material of unknown
originbull 2003 Rotterdam (NL)bull Brownish yellow powder ~3 kgbull Found on a shipload from Jordan
Measurements performed at ITUbull NDA analysisbull Isotope ratio measurements (U Sr
Pb)bull Infrared analysisbull Impurity analysisbull REE pattern determination
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 33
Case study
Vibrational Spectrum (Infrared Spectrometry)
bull Compound is AUC xH2Obull Sulfate impurity (from dissolution of starting material)
bullNitrate impurity (from solvent extractionpurification)
Mass Spectrometry
bull Natural uranium isotopic compositionbull Natural lead isotopic composition
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 34
Case study
Sr Isotope Ratio
Low value typical for phosphorites (eg North Africa Middle East UShellip)
070757 plusmn 000011
070814 plusmn 000004
071092 plusmn 000006
071416 plusmn 000011
071985 plusmn 000029
072336 plusmn 000004
073434 plusmn 000012
070785 plusmn 000004
071775 plusmn 000003
067 068 069 070 071 072 073 074 075 076 077 078 079 080
Beverley
Calgary
Key Lake
Olympic Dam
Ranger
Ranstad
Stanrock
Mulberry
Fund-26
87Sr86Sr Isotope RatioSr-87 Sr-86 isotope ratio
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 35
Case study
Age dating based on 234U230Th
Age dating based on 232Th228Th
Last chemical separation 1988 plusmn 5 yndash Applicable to samples with incomplete Th separationndash Complementary to 234U230Th method
Last chemical separation 1893 plusmn 17 y
ndash Measured value shows significant positive biasndash Reason incomplete separation of 230Th from the
parent 234U nuclide(ldquoclock is not set to zerordquo)
ndash Residual 230Th cannot be calculated or corrected for
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 36
Case study ndash Find-26
bull 234U abundance suggests low temperature redox deposit value agrees with data reported by IAEA for UOC from Al Qaim (Iraq)
bull Impurities high P contentsimilar metallic impurities to Iraqi phosphate deposits
bull Pb isotopes natural young deposit low U content in orebull REE pattern flat no Eu or Ce anomaly rarr previously found
in certain sandstone-type and reworked phosphorite
Data inherent to the material corroborate information from external sources
Identification of origin based onSingle sampleMultiple parameters
Identification of origin based onSingle sampleMultiple parameters
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 37
Comparison of relative efforts ndash yellow cake
(5)(5)SIMSU particle analysis(5)Evaluation and Report
MC-ICP-MSMC-ICP-MSICP-MSIR-Spectroscopy RamanIon ChromatographyICP-MS IDMS
Electron Microscopy EDX WDXOptical MicroscopyICP-MSTIMSTitration IDMS
Technique
1853Total
15Nd Isotopes15Sr Isotopes3Rare Earth Elemental pattern1Molecular structure
15Anionic impurities3Age dating
3Micromorphology1Visual inspection macroscopic11Impurities11Isotopic Composition11Element Assay
ForensicsSafeguardsAnalysisParameter
Note rounded figures based on a full cost evaluation figures in brackets are not included in the Total
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 38
Conclusions
Wealth of information inherent to nuclear materialDecrypting the information requires sophisticated methodology subject matter expertise and reference dataSignificant effort (resources and time) needed for comprehensive analysis and data interpretationNuclear forensics methodology may open new avenuesin different areasApplication of investigative techniques in Safeguards has to be evaluated
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 27
Anion residuals in UOCrsquos
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
20
40
60
80
100
120
140
160
180
200
uScm
Cond
fluor
ide
102
2
2 chlo
ride
02
19
4 5 6 7 nitr
ate
003
6
sulp
hate
479
129
Canada ESI
0 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 min
17
18
19
20
21
22
23
24
25
26
uScm
Cond
fluor
ide
036
7
2 3
chlo
ride
55
32
5 brom
ide
-00
26
nitr
ate
012
7
sulp
hate
20
767
9
Australia Radium Hill
Different type of uranium deposits
Different processes for U extraction
Different mineral acids are used
Acid remainings
fluor
ide
chlo
ride
brom
ide
nitr
ate
sulp
hate
fluor
ide
chlo
ride
nitr
ate
sulp
hate
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 28
NO3SO4
0
01
02
03
04
05
06
07
08
09
1
Sout
h Al
ligat
or
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y Ka
thle
en
ESI U
SA
ESI C
anad
a
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Stan
rock
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lake
Mad
awas
ka
Mac
assa
Nor
th S
pan
Milli
ken
Lake
Eldo
rado
Stan
leig
h
FCl
0
05
1
15
2
25
3
35
4
45
5
Sou
th A
lliga
tor
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y K
athl
een
ES
I US
A
ES
I Can
ada
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Sta
nroc
k
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lak
e
Mad
awas
ka
Mac
assa
Nor
th S
pan
Mill
iken
Lak
e
Eld
orad
o
Sta
nlei
gh
Anion ratios
Phosphorite oresQuartz-pebble conglomerate and vein deposits
Nitric acid leaching rArr
Indicator of the processApatite mineral Ca5(PO4)3(FClOH)
rArr Indicator of the deposit type
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 29
Sandstone basal channel Quartz-pebble
conglomerate
Phosphorite
Black shale
Statistical evaluation of UOC data
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 30
U productsbull U ores
bull U ore concentrates
bull U oxide powders
bull UF4 and UF6
bull U pellets
Next step - Vertical study
Aim Identify the impurities that are acquired from or lost in the process What is the effect on the impurities from the source material
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 31
Uranium oreconcentrates
Process stagesamples and reagents
UO3
Next step - Vertical study
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 32
Case study
Backgroundbull uranium raw material of unknown
originbull 2003 Rotterdam (NL)bull Brownish yellow powder ~3 kgbull Found on a shipload from Jordan
Measurements performed at ITUbull NDA analysisbull Isotope ratio measurements (U Sr
Pb)bull Infrared analysisbull Impurity analysisbull REE pattern determination
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 33
Case study
Vibrational Spectrum (Infrared Spectrometry)
bull Compound is AUC xH2Obull Sulfate impurity (from dissolution of starting material)
bullNitrate impurity (from solvent extractionpurification)
Mass Spectrometry
bull Natural uranium isotopic compositionbull Natural lead isotopic composition
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 34
Case study
Sr Isotope Ratio
Low value typical for phosphorites (eg North Africa Middle East UShellip)
070757 plusmn 000011
070814 plusmn 000004
071092 plusmn 000006
071416 plusmn 000011
071985 plusmn 000029
072336 plusmn 000004
073434 plusmn 000012
070785 plusmn 000004
071775 plusmn 000003
067 068 069 070 071 072 073 074 075 076 077 078 079 080
Beverley
Calgary
Key Lake
Olympic Dam
Ranger
Ranstad
Stanrock
Mulberry
Fund-26
87Sr86Sr Isotope RatioSr-87 Sr-86 isotope ratio
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 35
Case study
Age dating based on 234U230Th
Age dating based on 232Th228Th
Last chemical separation 1988 plusmn 5 yndash Applicable to samples with incomplete Th separationndash Complementary to 234U230Th method
Last chemical separation 1893 plusmn 17 y
ndash Measured value shows significant positive biasndash Reason incomplete separation of 230Th from the
parent 234U nuclide(ldquoclock is not set to zerordquo)
ndash Residual 230Th cannot be calculated or corrected for
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 36
Case study ndash Find-26
bull 234U abundance suggests low temperature redox deposit value agrees with data reported by IAEA for UOC from Al Qaim (Iraq)
bull Impurities high P contentsimilar metallic impurities to Iraqi phosphate deposits
bull Pb isotopes natural young deposit low U content in orebull REE pattern flat no Eu or Ce anomaly rarr previously found
in certain sandstone-type and reworked phosphorite
Data inherent to the material corroborate information from external sources
Identification of origin based onSingle sampleMultiple parameters
Identification of origin based onSingle sampleMultiple parameters
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 37
Comparison of relative efforts ndash yellow cake
(5)(5)SIMSU particle analysis(5)Evaluation and Report
MC-ICP-MSMC-ICP-MSICP-MSIR-Spectroscopy RamanIon ChromatographyICP-MS IDMS
Electron Microscopy EDX WDXOptical MicroscopyICP-MSTIMSTitration IDMS
Technique
1853Total
15Nd Isotopes15Sr Isotopes3Rare Earth Elemental pattern1Molecular structure
15Anionic impurities3Age dating
3Micromorphology1Visual inspection macroscopic11Impurities11Isotopic Composition11Element Assay
ForensicsSafeguardsAnalysisParameter
Note rounded figures based on a full cost evaluation figures in brackets are not included in the Total
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 38
Conclusions
Wealth of information inherent to nuclear materialDecrypting the information requires sophisticated methodology subject matter expertise and reference dataSignificant effort (resources and time) needed for comprehensive analysis and data interpretationNuclear forensics methodology may open new avenuesin different areasApplication of investigative techniques in Safeguards has to be evaluated
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 28
NO3SO4
0
01
02
03
04
05
06
07
08
09
1
Sout
h Al
ligat
or
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y Ka
thle
en
ESI U
SA
ESI C
anad
a
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Stan
rock
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lake
Mad
awas
ka
Mac
assa
Nor
th S
pan
Milli
ken
Lake
Eldo
rado
Stan
leig
h
FCl
0
05
1
15
2
25
3
35
4
45
5
Sou
th A
lliga
tor
Rad
ium
Hill
Rum
Jun
gle
Ran
ger
Que
ensl
and
Oly
mpi
c D
am
Mar
y K
athl
een
ES
I US
A
ES
I Can
ada
Ray
Roc
k
Rio
Alg
om
Dyn
o
Blin
d R
iver
Sta
nroc
k
Gun
nar
Fara
day
Rab
bit L
ake
Den
ison
Key
Lak
e
Mad
awas
ka
Mac
assa
Nor
th S
pan
Mill
iken
Lak
e
Eld
orad
o
Sta
nlei
gh
Anion ratios
Phosphorite oresQuartz-pebble conglomerate and vein deposits
Nitric acid leaching rArr
Indicator of the processApatite mineral Ca5(PO4)3(FClOH)
rArr Indicator of the deposit type
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 29
Sandstone basal channel Quartz-pebble
conglomerate
Phosphorite
Black shale
Statistical evaluation of UOC data
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 30
U productsbull U ores
bull U ore concentrates
bull U oxide powders
bull UF4 and UF6
bull U pellets
Next step - Vertical study
Aim Identify the impurities that are acquired from or lost in the process What is the effect on the impurities from the source material
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 31
Uranium oreconcentrates
Process stagesamples and reagents
UO3
Next step - Vertical study
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 32
Case study
Backgroundbull uranium raw material of unknown
originbull 2003 Rotterdam (NL)bull Brownish yellow powder ~3 kgbull Found on a shipload from Jordan
Measurements performed at ITUbull NDA analysisbull Isotope ratio measurements (U Sr
Pb)bull Infrared analysisbull Impurity analysisbull REE pattern determination
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 33
Case study
Vibrational Spectrum (Infrared Spectrometry)
bull Compound is AUC xH2Obull Sulfate impurity (from dissolution of starting material)
bullNitrate impurity (from solvent extractionpurification)
Mass Spectrometry
bull Natural uranium isotopic compositionbull Natural lead isotopic composition
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 34
Case study
Sr Isotope Ratio
Low value typical for phosphorites (eg North Africa Middle East UShellip)
070757 plusmn 000011
070814 plusmn 000004
071092 plusmn 000006
071416 plusmn 000011
071985 plusmn 000029
072336 plusmn 000004
073434 plusmn 000012
070785 plusmn 000004
071775 plusmn 000003
067 068 069 070 071 072 073 074 075 076 077 078 079 080
Beverley
Calgary
Key Lake
Olympic Dam
Ranger
Ranstad
Stanrock
Mulberry
Fund-26
87Sr86Sr Isotope RatioSr-87 Sr-86 isotope ratio
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 35
Case study
Age dating based on 234U230Th
Age dating based on 232Th228Th
Last chemical separation 1988 plusmn 5 yndash Applicable to samples with incomplete Th separationndash Complementary to 234U230Th method
Last chemical separation 1893 plusmn 17 y
ndash Measured value shows significant positive biasndash Reason incomplete separation of 230Th from the
parent 234U nuclide(ldquoclock is not set to zerordquo)
ndash Residual 230Th cannot be calculated or corrected for
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 36
Case study ndash Find-26
bull 234U abundance suggests low temperature redox deposit value agrees with data reported by IAEA for UOC from Al Qaim (Iraq)
bull Impurities high P contentsimilar metallic impurities to Iraqi phosphate deposits
bull Pb isotopes natural young deposit low U content in orebull REE pattern flat no Eu or Ce anomaly rarr previously found
in certain sandstone-type and reworked phosphorite
Data inherent to the material corroborate information from external sources
Identification of origin based onSingle sampleMultiple parameters
Identification of origin based onSingle sampleMultiple parameters
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 37
Comparison of relative efforts ndash yellow cake
(5)(5)SIMSU particle analysis(5)Evaluation and Report
MC-ICP-MSMC-ICP-MSICP-MSIR-Spectroscopy RamanIon ChromatographyICP-MS IDMS
Electron Microscopy EDX WDXOptical MicroscopyICP-MSTIMSTitration IDMS
Technique
1853Total
15Nd Isotopes15Sr Isotopes3Rare Earth Elemental pattern1Molecular structure
15Anionic impurities3Age dating
3Micromorphology1Visual inspection macroscopic11Impurities11Isotopic Composition11Element Assay
ForensicsSafeguardsAnalysisParameter
Note rounded figures based on a full cost evaluation figures in brackets are not included in the Total
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 38
Conclusions
Wealth of information inherent to nuclear materialDecrypting the information requires sophisticated methodology subject matter expertise and reference dataSignificant effort (resources and time) needed for comprehensive analysis and data interpretationNuclear forensics methodology may open new avenuesin different areasApplication of investigative techniques in Safeguards has to be evaluated
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 29
Sandstone basal channel Quartz-pebble
conglomerate
Phosphorite
Black shale
Statistical evaluation of UOC data
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 30
U productsbull U ores
bull U ore concentrates
bull U oxide powders
bull UF4 and UF6
bull U pellets
Next step - Vertical study
Aim Identify the impurities that are acquired from or lost in the process What is the effect on the impurities from the source material
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 31
Uranium oreconcentrates
Process stagesamples and reagents
UO3
Next step - Vertical study
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 32
Case study
Backgroundbull uranium raw material of unknown
originbull 2003 Rotterdam (NL)bull Brownish yellow powder ~3 kgbull Found on a shipload from Jordan
Measurements performed at ITUbull NDA analysisbull Isotope ratio measurements (U Sr
Pb)bull Infrared analysisbull Impurity analysisbull REE pattern determination
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 33
Case study
Vibrational Spectrum (Infrared Spectrometry)
bull Compound is AUC xH2Obull Sulfate impurity (from dissolution of starting material)
bullNitrate impurity (from solvent extractionpurification)
Mass Spectrometry
bull Natural uranium isotopic compositionbull Natural lead isotopic composition
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 34
Case study
Sr Isotope Ratio
Low value typical for phosphorites (eg North Africa Middle East UShellip)
070757 plusmn 000011
070814 plusmn 000004
071092 plusmn 000006
071416 plusmn 000011
071985 plusmn 000029
072336 plusmn 000004
073434 plusmn 000012
070785 plusmn 000004
071775 plusmn 000003
067 068 069 070 071 072 073 074 075 076 077 078 079 080
Beverley
Calgary
Key Lake
Olympic Dam
Ranger
Ranstad
Stanrock
Mulberry
Fund-26
87Sr86Sr Isotope RatioSr-87 Sr-86 isotope ratio
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 35
Case study
Age dating based on 234U230Th
Age dating based on 232Th228Th
Last chemical separation 1988 plusmn 5 yndash Applicable to samples with incomplete Th separationndash Complementary to 234U230Th method
Last chemical separation 1893 plusmn 17 y
ndash Measured value shows significant positive biasndash Reason incomplete separation of 230Th from the
parent 234U nuclide(ldquoclock is not set to zerordquo)
ndash Residual 230Th cannot be calculated or corrected for
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 36
Case study ndash Find-26
bull 234U abundance suggests low temperature redox deposit value agrees with data reported by IAEA for UOC from Al Qaim (Iraq)
bull Impurities high P contentsimilar metallic impurities to Iraqi phosphate deposits
bull Pb isotopes natural young deposit low U content in orebull REE pattern flat no Eu or Ce anomaly rarr previously found
in certain sandstone-type and reworked phosphorite
Data inherent to the material corroborate information from external sources
Identification of origin based onSingle sampleMultiple parameters
Identification of origin based onSingle sampleMultiple parameters
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 37
Comparison of relative efforts ndash yellow cake
(5)(5)SIMSU particle analysis(5)Evaluation and Report
MC-ICP-MSMC-ICP-MSICP-MSIR-Spectroscopy RamanIon ChromatographyICP-MS IDMS
Electron Microscopy EDX WDXOptical MicroscopyICP-MSTIMSTitration IDMS
Technique
1853Total
15Nd Isotopes15Sr Isotopes3Rare Earth Elemental pattern1Molecular structure
15Anionic impurities3Age dating
3Micromorphology1Visual inspection macroscopic11Impurities11Isotopic Composition11Element Assay
ForensicsSafeguardsAnalysisParameter
Note rounded figures based on a full cost evaluation figures in brackets are not included in the Total
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 38
Conclusions
Wealth of information inherent to nuclear materialDecrypting the information requires sophisticated methodology subject matter expertise and reference dataSignificant effort (resources and time) needed for comprehensive analysis and data interpretationNuclear forensics methodology may open new avenuesin different areasApplication of investigative techniques in Safeguards has to be evaluated
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 30
U productsbull U ores
bull U ore concentrates
bull U oxide powders
bull UF4 and UF6
bull U pellets
Next step - Vertical study
Aim Identify the impurities that are acquired from or lost in the process What is the effect on the impurities from the source material
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 31
Uranium oreconcentrates
Process stagesamples and reagents
UO3
Next step - Vertical study
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 32
Case study
Backgroundbull uranium raw material of unknown
originbull 2003 Rotterdam (NL)bull Brownish yellow powder ~3 kgbull Found on a shipload from Jordan
Measurements performed at ITUbull NDA analysisbull Isotope ratio measurements (U Sr
Pb)bull Infrared analysisbull Impurity analysisbull REE pattern determination
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 33
Case study
Vibrational Spectrum (Infrared Spectrometry)
bull Compound is AUC xH2Obull Sulfate impurity (from dissolution of starting material)
bullNitrate impurity (from solvent extractionpurification)
Mass Spectrometry
bull Natural uranium isotopic compositionbull Natural lead isotopic composition
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 34
Case study
Sr Isotope Ratio
Low value typical for phosphorites (eg North Africa Middle East UShellip)
070757 plusmn 000011
070814 plusmn 000004
071092 plusmn 000006
071416 plusmn 000011
071985 plusmn 000029
072336 plusmn 000004
073434 plusmn 000012
070785 plusmn 000004
071775 plusmn 000003
067 068 069 070 071 072 073 074 075 076 077 078 079 080
Beverley
Calgary
Key Lake
Olympic Dam
Ranger
Ranstad
Stanrock
Mulberry
Fund-26
87Sr86Sr Isotope RatioSr-87 Sr-86 isotope ratio
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 35
Case study
Age dating based on 234U230Th
Age dating based on 232Th228Th
Last chemical separation 1988 plusmn 5 yndash Applicable to samples with incomplete Th separationndash Complementary to 234U230Th method
Last chemical separation 1893 plusmn 17 y
ndash Measured value shows significant positive biasndash Reason incomplete separation of 230Th from the
parent 234U nuclide(ldquoclock is not set to zerordquo)
ndash Residual 230Th cannot be calculated or corrected for
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 36
Case study ndash Find-26
bull 234U abundance suggests low temperature redox deposit value agrees with data reported by IAEA for UOC from Al Qaim (Iraq)
bull Impurities high P contentsimilar metallic impurities to Iraqi phosphate deposits
bull Pb isotopes natural young deposit low U content in orebull REE pattern flat no Eu or Ce anomaly rarr previously found
in certain sandstone-type and reworked phosphorite
Data inherent to the material corroborate information from external sources
Identification of origin based onSingle sampleMultiple parameters
Identification of origin based onSingle sampleMultiple parameters
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 37
Comparison of relative efforts ndash yellow cake
(5)(5)SIMSU particle analysis(5)Evaluation and Report
MC-ICP-MSMC-ICP-MSICP-MSIR-Spectroscopy RamanIon ChromatographyICP-MS IDMS
Electron Microscopy EDX WDXOptical MicroscopyICP-MSTIMSTitration IDMS
Technique
1853Total
15Nd Isotopes15Sr Isotopes3Rare Earth Elemental pattern1Molecular structure
15Anionic impurities3Age dating
3Micromorphology1Visual inspection macroscopic11Impurities11Isotopic Composition11Element Assay
ForensicsSafeguardsAnalysisParameter
Note rounded figures based on a full cost evaluation figures in brackets are not included in the Total
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 38
Conclusions
Wealth of information inherent to nuclear materialDecrypting the information requires sophisticated methodology subject matter expertise and reference dataSignificant effort (resources and time) needed for comprehensive analysis and data interpretationNuclear forensics methodology may open new avenuesin different areasApplication of investigative techniques in Safeguards has to be evaluated
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 31
Uranium oreconcentrates
Process stagesamples and reagents
UO3
Next step - Vertical study
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 32
Case study
Backgroundbull uranium raw material of unknown
originbull 2003 Rotterdam (NL)bull Brownish yellow powder ~3 kgbull Found on a shipload from Jordan
Measurements performed at ITUbull NDA analysisbull Isotope ratio measurements (U Sr
Pb)bull Infrared analysisbull Impurity analysisbull REE pattern determination
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 33
Case study
Vibrational Spectrum (Infrared Spectrometry)
bull Compound is AUC xH2Obull Sulfate impurity (from dissolution of starting material)
bullNitrate impurity (from solvent extractionpurification)
Mass Spectrometry
bull Natural uranium isotopic compositionbull Natural lead isotopic composition
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 34
Case study
Sr Isotope Ratio
Low value typical for phosphorites (eg North Africa Middle East UShellip)
070757 plusmn 000011
070814 plusmn 000004
071092 plusmn 000006
071416 plusmn 000011
071985 plusmn 000029
072336 plusmn 000004
073434 plusmn 000012
070785 plusmn 000004
071775 plusmn 000003
067 068 069 070 071 072 073 074 075 076 077 078 079 080
Beverley
Calgary
Key Lake
Olympic Dam
Ranger
Ranstad
Stanrock
Mulberry
Fund-26
87Sr86Sr Isotope RatioSr-87 Sr-86 isotope ratio
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 35
Case study
Age dating based on 234U230Th
Age dating based on 232Th228Th
Last chemical separation 1988 plusmn 5 yndash Applicable to samples with incomplete Th separationndash Complementary to 234U230Th method
Last chemical separation 1893 plusmn 17 y
ndash Measured value shows significant positive biasndash Reason incomplete separation of 230Th from the
parent 234U nuclide(ldquoclock is not set to zerordquo)
ndash Residual 230Th cannot be calculated or corrected for
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 36
Case study ndash Find-26
bull 234U abundance suggests low temperature redox deposit value agrees with data reported by IAEA for UOC from Al Qaim (Iraq)
bull Impurities high P contentsimilar metallic impurities to Iraqi phosphate deposits
bull Pb isotopes natural young deposit low U content in orebull REE pattern flat no Eu or Ce anomaly rarr previously found
in certain sandstone-type and reworked phosphorite
Data inherent to the material corroborate information from external sources
Identification of origin based onSingle sampleMultiple parameters
Identification of origin based onSingle sampleMultiple parameters
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 37
Comparison of relative efforts ndash yellow cake
(5)(5)SIMSU particle analysis(5)Evaluation and Report
MC-ICP-MSMC-ICP-MSICP-MSIR-Spectroscopy RamanIon ChromatographyICP-MS IDMS
Electron Microscopy EDX WDXOptical MicroscopyICP-MSTIMSTitration IDMS
Technique
1853Total
15Nd Isotopes15Sr Isotopes3Rare Earth Elemental pattern1Molecular structure
15Anionic impurities3Age dating
3Micromorphology1Visual inspection macroscopic11Impurities11Isotopic Composition11Element Assay
ForensicsSafeguardsAnalysisParameter
Note rounded figures based on a full cost evaluation figures in brackets are not included in the Total
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 38
Conclusions
Wealth of information inherent to nuclear materialDecrypting the information requires sophisticated methodology subject matter expertise and reference dataSignificant effort (resources and time) needed for comprehensive analysis and data interpretationNuclear forensics methodology may open new avenuesin different areasApplication of investigative techniques in Safeguards has to be evaluated
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 32
Case study
Backgroundbull uranium raw material of unknown
originbull 2003 Rotterdam (NL)bull Brownish yellow powder ~3 kgbull Found on a shipload from Jordan
Measurements performed at ITUbull NDA analysisbull Isotope ratio measurements (U Sr
Pb)bull Infrared analysisbull Impurity analysisbull REE pattern determination
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 33
Case study
Vibrational Spectrum (Infrared Spectrometry)
bull Compound is AUC xH2Obull Sulfate impurity (from dissolution of starting material)
bullNitrate impurity (from solvent extractionpurification)
Mass Spectrometry
bull Natural uranium isotopic compositionbull Natural lead isotopic composition
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 34
Case study
Sr Isotope Ratio
Low value typical for phosphorites (eg North Africa Middle East UShellip)
070757 plusmn 000011
070814 plusmn 000004
071092 plusmn 000006
071416 plusmn 000011
071985 plusmn 000029
072336 plusmn 000004
073434 plusmn 000012
070785 plusmn 000004
071775 plusmn 000003
067 068 069 070 071 072 073 074 075 076 077 078 079 080
Beverley
Calgary
Key Lake
Olympic Dam
Ranger
Ranstad
Stanrock
Mulberry
Fund-26
87Sr86Sr Isotope RatioSr-87 Sr-86 isotope ratio
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 35
Case study
Age dating based on 234U230Th
Age dating based on 232Th228Th
Last chemical separation 1988 plusmn 5 yndash Applicable to samples with incomplete Th separationndash Complementary to 234U230Th method
Last chemical separation 1893 plusmn 17 y
ndash Measured value shows significant positive biasndash Reason incomplete separation of 230Th from the
parent 234U nuclide(ldquoclock is not set to zerordquo)
ndash Residual 230Th cannot be calculated or corrected for
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 36
Case study ndash Find-26
bull 234U abundance suggests low temperature redox deposit value agrees with data reported by IAEA for UOC from Al Qaim (Iraq)
bull Impurities high P contentsimilar metallic impurities to Iraqi phosphate deposits
bull Pb isotopes natural young deposit low U content in orebull REE pattern flat no Eu or Ce anomaly rarr previously found
in certain sandstone-type and reworked phosphorite
Data inherent to the material corroborate information from external sources
Identification of origin based onSingle sampleMultiple parameters
Identification of origin based onSingle sampleMultiple parameters
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 37
Comparison of relative efforts ndash yellow cake
(5)(5)SIMSU particle analysis(5)Evaluation and Report
MC-ICP-MSMC-ICP-MSICP-MSIR-Spectroscopy RamanIon ChromatographyICP-MS IDMS
Electron Microscopy EDX WDXOptical MicroscopyICP-MSTIMSTitration IDMS
Technique
1853Total
15Nd Isotopes15Sr Isotopes3Rare Earth Elemental pattern1Molecular structure
15Anionic impurities3Age dating
3Micromorphology1Visual inspection macroscopic11Impurities11Isotopic Composition11Element Assay
ForensicsSafeguardsAnalysisParameter
Note rounded figures based on a full cost evaluation figures in brackets are not included in the Total
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 38
Conclusions
Wealth of information inherent to nuclear materialDecrypting the information requires sophisticated methodology subject matter expertise and reference dataSignificant effort (resources and time) needed for comprehensive analysis and data interpretationNuclear forensics methodology may open new avenuesin different areasApplication of investigative techniques in Safeguards has to be evaluated
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 33
Case study
Vibrational Spectrum (Infrared Spectrometry)
bull Compound is AUC xH2Obull Sulfate impurity (from dissolution of starting material)
bullNitrate impurity (from solvent extractionpurification)
Mass Spectrometry
bull Natural uranium isotopic compositionbull Natural lead isotopic composition
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 34
Case study
Sr Isotope Ratio
Low value typical for phosphorites (eg North Africa Middle East UShellip)
070757 plusmn 000011
070814 plusmn 000004
071092 plusmn 000006
071416 plusmn 000011
071985 plusmn 000029
072336 plusmn 000004
073434 plusmn 000012
070785 plusmn 000004
071775 plusmn 000003
067 068 069 070 071 072 073 074 075 076 077 078 079 080
Beverley
Calgary
Key Lake
Olympic Dam
Ranger
Ranstad
Stanrock
Mulberry
Fund-26
87Sr86Sr Isotope RatioSr-87 Sr-86 isotope ratio
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 35
Case study
Age dating based on 234U230Th
Age dating based on 232Th228Th
Last chemical separation 1988 plusmn 5 yndash Applicable to samples with incomplete Th separationndash Complementary to 234U230Th method
Last chemical separation 1893 plusmn 17 y
ndash Measured value shows significant positive biasndash Reason incomplete separation of 230Th from the
parent 234U nuclide(ldquoclock is not set to zerordquo)
ndash Residual 230Th cannot be calculated or corrected for
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 36
Case study ndash Find-26
bull 234U abundance suggests low temperature redox deposit value agrees with data reported by IAEA for UOC from Al Qaim (Iraq)
bull Impurities high P contentsimilar metallic impurities to Iraqi phosphate deposits
bull Pb isotopes natural young deposit low U content in orebull REE pattern flat no Eu or Ce anomaly rarr previously found
in certain sandstone-type and reworked phosphorite
Data inherent to the material corroborate information from external sources
Identification of origin based onSingle sampleMultiple parameters
Identification of origin based onSingle sampleMultiple parameters
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 37
Comparison of relative efforts ndash yellow cake
(5)(5)SIMSU particle analysis(5)Evaluation and Report
MC-ICP-MSMC-ICP-MSICP-MSIR-Spectroscopy RamanIon ChromatographyICP-MS IDMS
Electron Microscopy EDX WDXOptical MicroscopyICP-MSTIMSTitration IDMS
Technique
1853Total
15Nd Isotopes15Sr Isotopes3Rare Earth Elemental pattern1Molecular structure
15Anionic impurities3Age dating
3Micromorphology1Visual inspection macroscopic11Impurities11Isotopic Composition11Element Assay
ForensicsSafeguardsAnalysisParameter
Note rounded figures based on a full cost evaluation figures in brackets are not included in the Total
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 38
Conclusions
Wealth of information inherent to nuclear materialDecrypting the information requires sophisticated methodology subject matter expertise and reference dataSignificant effort (resources and time) needed for comprehensive analysis and data interpretationNuclear forensics methodology may open new avenuesin different areasApplication of investigative techniques in Safeguards has to be evaluated
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 34
Case study
Sr Isotope Ratio
Low value typical for phosphorites (eg North Africa Middle East UShellip)
070757 plusmn 000011
070814 plusmn 000004
071092 plusmn 000006
071416 plusmn 000011
071985 plusmn 000029
072336 plusmn 000004
073434 plusmn 000012
070785 plusmn 000004
071775 plusmn 000003
067 068 069 070 071 072 073 074 075 076 077 078 079 080
Beverley
Calgary
Key Lake
Olympic Dam
Ranger
Ranstad
Stanrock
Mulberry
Fund-26
87Sr86Sr Isotope RatioSr-87 Sr-86 isotope ratio
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 35
Case study
Age dating based on 234U230Th
Age dating based on 232Th228Th
Last chemical separation 1988 plusmn 5 yndash Applicable to samples with incomplete Th separationndash Complementary to 234U230Th method
Last chemical separation 1893 plusmn 17 y
ndash Measured value shows significant positive biasndash Reason incomplete separation of 230Th from the
parent 234U nuclide(ldquoclock is not set to zerordquo)
ndash Residual 230Th cannot be calculated or corrected for
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 36
Case study ndash Find-26
bull 234U abundance suggests low temperature redox deposit value agrees with data reported by IAEA for UOC from Al Qaim (Iraq)
bull Impurities high P contentsimilar metallic impurities to Iraqi phosphate deposits
bull Pb isotopes natural young deposit low U content in orebull REE pattern flat no Eu or Ce anomaly rarr previously found
in certain sandstone-type and reworked phosphorite
Data inherent to the material corroborate information from external sources
Identification of origin based onSingle sampleMultiple parameters
Identification of origin based onSingle sampleMultiple parameters
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 37
Comparison of relative efforts ndash yellow cake
(5)(5)SIMSU particle analysis(5)Evaluation and Report
MC-ICP-MSMC-ICP-MSICP-MSIR-Spectroscopy RamanIon ChromatographyICP-MS IDMS
Electron Microscopy EDX WDXOptical MicroscopyICP-MSTIMSTitration IDMS
Technique
1853Total
15Nd Isotopes15Sr Isotopes3Rare Earth Elemental pattern1Molecular structure
15Anionic impurities3Age dating
3Micromorphology1Visual inspection macroscopic11Impurities11Isotopic Composition11Element Assay
ForensicsSafeguardsAnalysisParameter
Note rounded figures based on a full cost evaluation figures in brackets are not included in the Total
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 38
Conclusions
Wealth of information inherent to nuclear materialDecrypting the information requires sophisticated methodology subject matter expertise and reference dataSignificant effort (resources and time) needed for comprehensive analysis and data interpretationNuclear forensics methodology may open new avenuesin different areasApplication of investigative techniques in Safeguards has to be evaluated
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 35
Case study
Age dating based on 234U230Th
Age dating based on 232Th228Th
Last chemical separation 1988 plusmn 5 yndash Applicable to samples with incomplete Th separationndash Complementary to 234U230Th method
Last chemical separation 1893 plusmn 17 y
ndash Measured value shows significant positive biasndash Reason incomplete separation of 230Th from the
parent 234U nuclide(ldquoclock is not set to zerordquo)
ndash Residual 230Th cannot be calculated or corrected for
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 36
Case study ndash Find-26
bull 234U abundance suggests low temperature redox deposit value agrees with data reported by IAEA for UOC from Al Qaim (Iraq)
bull Impurities high P contentsimilar metallic impurities to Iraqi phosphate deposits
bull Pb isotopes natural young deposit low U content in orebull REE pattern flat no Eu or Ce anomaly rarr previously found
in certain sandstone-type and reworked phosphorite
Data inherent to the material corroborate information from external sources
Identification of origin based onSingle sampleMultiple parameters
Identification of origin based onSingle sampleMultiple parameters
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 37
Comparison of relative efforts ndash yellow cake
(5)(5)SIMSU particle analysis(5)Evaluation and Report
MC-ICP-MSMC-ICP-MSICP-MSIR-Spectroscopy RamanIon ChromatographyICP-MS IDMS
Electron Microscopy EDX WDXOptical MicroscopyICP-MSTIMSTitration IDMS
Technique
1853Total
15Nd Isotopes15Sr Isotopes3Rare Earth Elemental pattern1Molecular structure
15Anionic impurities3Age dating
3Micromorphology1Visual inspection macroscopic11Impurities11Isotopic Composition11Element Assay
ForensicsSafeguardsAnalysisParameter
Note rounded figures based on a full cost evaluation figures in brackets are not included in the Total
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 38
Conclusions
Wealth of information inherent to nuclear materialDecrypting the information requires sophisticated methodology subject matter expertise and reference dataSignificant effort (resources and time) needed for comprehensive analysis and data interpretationNuclear forensics methodology may open new avenuesin different areasApplication of investigative techniques in Safeguards has to be evaluated
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 36
Case study ndash Find-26
bull 234U abundance suggests low temperature redox deposit value agrees with data reported by IAEA for UOC from Al Qaim (Iraq)
bull Impurities high P contentsimilar metallic impurities to Iraqi phosphate deposits
bull Pb isotopes natural young deposit low U content in orebull REE pattern flat no Eu or Ce anomaly rarr previously found
in certain sandstone-type and reworked phosphorite
Data inherent to the material corroborate information from external sources
Identification of origin based onSingle sampleMultiple parameters
Identification of origin based onSingle sampleMultiple parameters
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 37
Comparison of relative efforts ndash yellow cake
(5)(5)SIMSU particle analysis(5)Evaluation and Report
MC-ICP-MSMC-ICP-MSICP-MSIR-Spectroscopy RamanIon ChromatographyICP-MS IDMS
Electron Microscopy EDX WDXOptical MicroscopyICP-MSTIMSTitration IDMS
Technique
1853Total
15Nd Isotopes15Sr Isotopes3Rare Earth Elemental pattern1Molecular structure
15Anionic impurities3Age dating
3Micromorphology1Visual inspection macroscopic11Impurities11Isotopic Composition11Element Assay
ForensicsSafeguardsAnalysisParameter
Note rounded figures based on a full cost evaluation figures in brackets are not included in the Total
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 38
Conclusions
Wealth of information inherent to nuclear materialDecrypting the information requires sophisticated methodology subject matter expertise and reference dataSignificant effort (resources and time) needed for comprehensive analysis and data interpretationNuclear forensics methodology may open new avenuesin different areasApplication of investigative techniques in Safeguards has to be evaluated
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 37
Comparison of relative efforts ndash yellow cake
(5)(5)SIMSU particle analysis(5)Evaluation and Report
MC-ICP-MSMC-ICP-MSICP-MSIR-Spectroscopy RamanIon ChromatographyICP-MS IDMS
Electron Microscopy EDX WDXOptical MicroscopyICP-MSTIMSTitration IDMS
Technique
1853Total
15Nd Isotopes15Sr Isotopes3Rare Earth Elemental pattern1Molecular structure
15Anionic impurities3Age dating
3Micromorphology1Visual inspection macroscopic11Impurities11Isotopic Composition11Element Assay
ForensicsSafeguardsAnalysisParameter
Note rounded figures based on a full cost evaluation figures in brackets are not included in the Total
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 38
Conclusions
Wealth of information inherent to nuclear materialDecrypting the information requires sophisticated methodology subject matter expertise and reference dataSignificant effort (resources and time) needed for comprehensive analysis and data interpretationNuclear forensics methodology may open new avenuesin different areasApplication of investigative techniques in Safeguards has to be evaluated
ESARDA-INMM Workshop Aix-en-Provence 16-20 October 2011 38
Conclusions
Wealth of information inherent to nuclear materialDecrypting the information requires sophisticated methodology subject matter expertise and reference dataSignificant effort (resources and time) needed for comprehensive analysis and data interpretationNuclear forensics methodology may open new avenuesin different areasApplication of investigative techniques in Safeguards has to be evaluated