nuclear science education and research opportunities at...
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Nuclear Science Education and Research Opportunities at LLNL
Mavrik Zavarin
Director, Glenn T. Seaborg Institute
Lawrence Livermore National Laboratory
UC Davis
July 12, 2016
FIG. 3: Left: Pu(OH)4(H2O)19 cluster optimized at the UHF level of theory. Right: Snapshot from
an ab initio MD simulations of Pu(OH)4 in a periodic box of water. In both models, four hydroxyl
and three water molecules are found in the inner shell, with two of the hydroxyls occupying the
axial positions while the other two hydroxyls and three waters are arranged around the equatorial
positions.
Given that UHF predicts equilibrium structures that are in qualitative agreement with
MP2 for small Pu(OH)4(H2O)n (n = 1 � 3) clusters, we employ UHF to carry out the
geometry optimization of larger clusters of n = 7 � 19 water molecules, with the largest
cluster (n = 19 waters) shown in the left panel of Figure 3. This cluster has enough water
molecules to complete a second solvation shell and begin filling in a third shell. At this
size, the essential features of the inner coordination shell appear converged: there are four
hydroxyl and three water molecules in the inner shell, with two of the hydroxyls occupying
the axial positions while the other two hydroxyls and three waters are arranged around the
equatorial positions, reminiscent of the hydration structure of linear actinyl ions.
It should be pointed out that drawing conclusions about metal ion coordination numbers
in liquid water solely on the basis of the optimized structures of large gas-phase clusters
should be done with caution. The optimization methods employed in this work only find
local minima and are not guaranteed to deliver a global minimum; robust algorithms for
finding the global minimum energy structure on complex potential energy landscapes remain
an open research problem. Our situation is further complicated by the fact that the first
coordination shell around Pu(IV) consists of two distinct species, OH� and H2O, which leads
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https://seaborg.llnl.gov
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Disclaimer •! I only found out about the UC Davis NAT Summer School last week •! My slides were thrown together rather quickly •! My one goal is to make you aware of education and research
opportunities at LLNL
Because NSSC consortium includes:
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Outline
•! A bit about myself •! Nuclear Science research and education opportunities LLNL
•! Physical and Life Sciences Directorate •! Nuclear and Chemical Sciences division •! Seaborg Institute •! Postdoc program •! Other opportunities
•! Examples of my research at LLNL
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Director of the Glenn T. Seaborg Institute which focuses on: Nuclear forensics Super heavy element discovery Environmental radiochemistry
A bit about myself
•! UC Berkeley undergrad in Chemistry (1993) •! UC Berkeley PhD in Soil Chemistry (1993-1998)
•! “Se, Ni, and Mn interaction with calcite” •! Hired at LLNL to develop model of radionuclide sorption to mineral
surfaces for reactive transport models (1998) •! Began managing ! contaminant transport project at the Nevada Test
Site (2005) •! Developed collaborations and teaching outside LLNL (2007)
•! Clemson University, HZDR Dresden, Las Positas Community College, etc.
•! Slowly developed a research program in actinide environmental research (2008-)
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Research Team and Funding
NA-22
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My research group’s goal is to reliably predict the mobility and cycling of radionuclides (actinides) in our environment
Th(IV) FPMD
Pu-cell interaction
Pu-goethite TEM
Hanford NanoSIMS
Conceptual models
Transport simulations Pu Batch sorption
Np sediment profiles Ravenglass estuary
Numerical models
Lawrence Livermore National Laboratory LLNL-PRES-xxxxxx 7
"! One of the Department of Energy’s NNSA National Laboratories
"! Located in Northern California’s “bay area”
"! 2.5 km2 campus
"! ~6000 employees
"! Mission: Strengthening the United States' security by developing and applying world-class science, technology and engineering
Lawrence Livermore National Laboratory
Lawrence Livermore National Laboratory LLNL-PRES-xxxxxx 8
LLNL Organization
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Nuclear and Chemical Sciences Division Division Leader: Sonia Létant; [email protected] Find us at: https://pls.llnl.gov/people/divisions/nuclear-and-chemical-sciences-division !"#$%&''&()*$$!"#"$%&"'("")'"*)"$+,"'-.'/0.(%1".2%3')45,-6,'%.('64"1-,2$5'27')$7#-("'-..7#%+#"',730+7.,'27',0))7$2',2768)-3"',2"9%$(,4-)'%.('724"$'.%+7.%3',"60$-25')$7&$%1,'-.630(-.&'/7$".,-6,:'.063"%$',%/"25'%.(',"60$-25:'%.('.7.;)$73-/"$%+7.''!"#$+,-.'$(/$#,',0#12*$
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Nuclear and Chemical Sciences Division Develop fundamental physics and chemistry knowledge to support national security programs including stockpile stewardship, forensics, nuclear safety and security
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Our Investment Areas
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Mission To strengthen interactions between LLNL and the academic community in nuclear chemistry/actinide science
To develop a robust pipeline in nuclear chemistry/actinide science applied to:
! Nuclear forensics & attribution ! Radiochemistry for NIF diagnostics
! Environmental Radiochemistry
Outreach
Environmental Radiochemistry
The Seaborg Institute Facilitates LLNL - academic collaborations in nuclear chemistry/actinide science
Science Education
The Seaborg Institute facilitates collaborations and provides administrative support to collaborators and students in nuclear chemistry/actinide science
! Nuclear Forensics Summer program ! SULI internships in nuclear science
! ACP internships in nuclear science (including NSSC students)
! VSP visiting scientists in nuclear science
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"The education of young "The education of young people in science is at least people in science is at least
as important, maybe more as important, maybe more so, than the research itself.” so, than the research itself
-Glenn T. Seaborg -Glenn T. Seaborg
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GTSI Nuclear Forensics Summer Program
8 week program for graduate students (and some undergrads) interested in Nuclear Forensics (and, more broadly, nuclear chemistry) •! Students paired with mentors to perform research project (~25 students) •! Weekly seminar series on Nuclear Forensics/Radiochemistry topics •! Student poster session •! Aligned with many other summer student programs
•! Hundreds of undergrad/grad students come to LLNL over summer EXAMPLES: •! Applying Auxiliary Field Quantum Monte Carlo methods to actinide
complexes •! Characterizing nuclear fallout debris using TEM, NanoSIMS, and
radiography •! Automation of radionuclide deposition in NIF capsules •! Development of novel radionuclide fast separations •! Delayed Neutron Activation Analysis (DNAA) for Nuclear forensics •! Radiochemistry and noble gas application to the hydrologic cycle
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"! LLNL’s postdoc program is larger than ever •! >200 postdocs lab-wide •! 130 postdocs in PLS
"! Active lab-wide Postdoc Association run by postdocs that provides both professional development and social opportunities
"! Lawrence Fellowship provides fellows opportunities to conduct their own research agenda
The LLNL Postdoc Program Provides opportunities for scientists to pursue world-class research
PLS Postdoc Program: https://pls.llnl.gov/careers/postdoctoral-program LLNL Postdoc Program: https://postdocs.llnl.gov
Lawrence Fellowship: https://fellowship.llnl.gov
PLS Postdoc Program Contacts: Sarah Chinn:, Director [email protected] Camille Vandermeer, Adminstrator [email protected]
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"! Annual post-doc poster symposium (with awards)
"! Post-docs typically have ~25% of their time to pursue career development opportunities
"! 35% of the lab’s postdocs are Foreign nationals
"! LLNL’s post-doc program is in a very active hiring mode right now
Additional LLNL post-doc info
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LLNL postdocs "! Carry out & publish original research "! Develop into PI scientists "! Move on to jobs at national labs, academia, industry
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"! Science Undergraduate Laboratory Internship (SULI) (DOE program) •! 10-16 week program with some compensation, fall/spring/summer
"! Academic Cooperation Program (ACP)/Visiting Scientist Program (VSP) •! Graduate/undergrad students, post-docs, scientists, unpaid, access to LLNL
facilities
"! Post college appointments •! Paid LLNL employee, must be recent graduate (undergrad of masters)
"! Livermore graduate scholar program •! Paid LLNL employee, graduate students, perform research at LLNL, 4/15
"! Lawrence Fellows •! Paid LLNL employee, postdoc, personal research at LLNL, 10/1
"! And others!
Other internship, fellowship, job opportunities at LLNL
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A bit about GTSI Research
Nuclear forensics & attribution Radiochemistry for NIF diagnostics and heavy element discovery
Environmental Radiochemistry
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Visiting students and faculty can use of state-of-the-art facilities
NanoSIMS: high resolution ultra-high sensitivity isotopic and chemical characterization at the nanoscale (50nm)
Titan SuperSTEM: chemical and structural characterization at the nanometer scale. Atomic Scale imaging with a spatial resolution of < 8nm.
Multi-collector, plasma-source mass spectrometer: isotopic measurement and concentration information ~10-4pCi, cheaper than AMS,
Accelerator Mass Spectrometer: ion counting, backgrounds of 105 atoms for Pu ~10-5 pCi, ~10-18M
Nuclear Magnetic Resonance Facility: Molecular scale information on both solutions and solids
Supercomputing: advanced, atomic scale simulations 81920 processors on BlueGene/L, AMD clusters up to 13,824 processors
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1. Seaborg Institute staff are leaders in nuclear and biological forensics
Scientific Challenge "! Goal: reconstruct a nuclear
incident quickly with high fidelity "! Current focus is on developing
signatures --the chemical, isotopic and morphological fingerprints of interdicted illicit materials
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NanoSIMS"
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"! Goal: Expanding our knowledge of the Periodic Table "! Focused on discovery of super heavy element
•! 113 – 118 was performed in collaboration with the Flerov Laboratory for Nuclear Reactions in Dubna, Russia
"! Rare isotopes are provided by LLNL for use as target materials – irradiations are performed in Dubna
"! Reaserch expanded to use of NIF for radiochemistry research
2. Heavy element research at LLNL includes the physics and chemistry of the heaviest elements
Heavy elements are produced by bombarding actinide targets with calcium-48 beams
Recently proposed names for elements 114 (Flerovium) and 116 (Livermorium)
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3. Environmental radiochemistry
50 nm 50 nm
100 nm
Pu-oxide on quartz
1 µm!
ER20-5 #1
Cheshire
1 µm!
Goal: Determine the processes that control the fate and transport of actinides in the subsurface
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Our goal is to reliably predict the mobility and cycling of radionuclides in our environment
Th(IV) FPMD
Pu-cell interaction
Pu-goethite TEM
Hanford NanoSIMS
Conceptual models
Transport simulations Pu Batch sorption
Np sediment profiles Ravenglass estuary
Numerical models
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"! First principles molecular dynamics calculations on Th(IV) ion in water indicate that: •! Coordination number around Th(IV) decreases as the number of coordinating
hydroxyl ions increase •! This clarifies the discrepancy between synchrotron-based XAS observations and
ab initio model predictions
Ab Initio modeling of water and hydroxide coordination around actinide ions
Supercomputing
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"! The pressure dependence of the rates of ligand exchange for the same [NpO2(CO3)3]4- and [UO2(CO3)3]4- complex were compared.
"! The experiments show a distinct difference in the pressure dependencies of rates of exchange for the uranyl and neptunyl complexes.
"! This suggests that the mechanisms of ligand exchange may change across the actinide series, possibly due to the influence of f-electrons (in collaboration with W. Casey, U.C. Davis)
Nuclear Magnetic Resonance of actinide-ligand complexes
<""('"2'%3F'>6,-'?"3+,@''<=>>:$CGH:'1IJK;1IJI'
Nuclear Magnetic Resonance
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TEM of actinide precipitates
A
goethite
goethite
D
E
3.08 Å 3.08 3.08
Pu colloids
goethite
E E 50 nm
Pu colloids
F
B
C d[{114}p=2.59 Å
d[{132}p=2.96 Å
d[{222}p=3.18 Å
C
"! TEM used to determine crystal structure at 2-5 nm and ~50 ppm
"! Pu nano-colloids formed in situ on goethite has a epitaxial lattice distortion structure, matching bcc Pu4O7
"! Structure identical regardless of the initial oxidation state of Pu (IV or V)
"! Similar behavior observed at 80C and on the scale of months
5 nm
Pu4O7 on goethite
5 nm
PuO2
Transmission Electron Microscopy
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NanoSIMS Characterization of actinide-contaminated sediments
•! Within the 200 Area at the Hanford Site, the Plutonium Finishing Plant disposed of organic and aqueous wastes at several unlined “cribs”.
•! What are the characteristics of Pu in the subsurface compared to the shallow sediments? •! (Collaboration with A. Felmy, PNNL/WSU)
NanoSIMS ion images of Si, and Pu detected in Hanford sediments recovered 25m below ground surface beneath the Z-9 trench. Pu is strongly correlated with minerals shown on the left panel. Photo from R. Kips
NanoSIMS
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Environmental behavior of Pu at Hanford
Pu Cs
Most likely, the Pu at Hanford that was deposited with DNAPL (TBP), pH ~2.5 migrated unhindered through the vadose zone dissolving calcite to neutralize the pH.
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Cameca NanoSIMS 50 - Secondary Ion Mass Spectrometer
L"."$%+7.'7/',"67.(%$5'-7.,'24$70&4',)0M"$-.&'9-24'N;'7$'C,O')$-1%$5'-7.,F''
We have developed the capability of imaging Pu on NanoSIMS as low as 1 ppm and 200 nm
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Pu & Np sorption to goethite CAMS ultratrace analysis
•! Pu sorption is linear on goethite over 8 orders of magnitude (<1E-9 M) •! Sorption is independent of initial oxidation state •! Np sorption over the same concentration range does not exhibit linearity
Snow et al. (2012) Coll. Interf. Sci.
CAMS
Pu(IV) Pu(V)
Pu sorption to goethite
Snow et al. (2012) Coll. Interf. Sci.
Np(V)sorpion to goethite
Accelerator Mass Spectrometry
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237Np (and other RNs) distribution near Sellafield, UK
Collaboration with Francesca Quinto (KIT), Gareth Law (Manchester)
RN separations – MC-ICP-MS
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Noble gas and 14C migration from underground nuclear tests
An underground nuclear explosion (UNE) will yield a variety of volatile and semi-volatile byproducts (Bowen et al., 2001) that provide signatures of the presence, nature, and age of the underground nuclear test.
Conceptual model of radionuclide migration from the Milk Shake test to Well ER-5-5. The leading edge of a 3H plume has reached Well ER-5-5. High 3He is indicative of a combination of saturated groundwater flow and gas-phase transport of the decay product of 3H. Note: Cavity radius is calculated using the maximum of the announced yield range in DOE/NV (2000) and Equation (1) in Pawloski (1999). From Navarro-Intera (2014).
AMS + Noble Gas Mass Spectrometry
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The Plutonium
SFA
Thank you! For questions about LLNL opportunities: [email protected]
DOE-NE Used Fuel
Disposition
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BACKUP
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Radioactive contamination is not just a nuclear waste repository issue
YuccaFlat
FrenchmanFlat
PahuteMesa
UndergroundNuclear Event=
0 5 10 Miles
0 15 km
Simulate RN transport $ evaluate risk to environment
The Nevada Test Site (NNSS)
Nevada Test Site (Nevada National Security Site) Fukushima Hanford Sellafield Savanah River Site Etc. US budget for EM is ~1B per year
Test configuration
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Environmental behavior of RNs at the Nevada Test Site: Note: It’s a big place
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Environmental Management goal is to effectively predict RN transport and risk over the next 1000 years Unconstrained modeling leads to significant overprediction of RN transport
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Typical RN contaminants
"! 3H, 14C, 36Cl, 99Tc, 129I, 90Sr, 137Cs, Pu, Np, U are dominant radionuclides at the NTS
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Chancellor
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Noble gases and 14C may yield information regarding the nature of underground nuclear tests An underground nuclear explosion (UNE) will yield a variety of volatile and semi-volatile byproducts (Bowen et al., 2001) that provide signatures of the presence, nature, and age of the underground nuclear test. Migration of volatile (noble gases) and semi-volatile (14C) indicators through the vadose (zone above the groundwater table) zone may yield near-surface signatures of a subsurface nuclear test that are persistent and detectable at considerable distances away from ground zero.
Conceptual model of radionuclide migration from the Milk Shake test to Well ER-5-5. The leading edge of a 3H plume has reached Well ER-5-5. High 3He is indicative of a combination of saturated groundwater flow and gas-phase transport of the decay product of 3H. Note: Cavity radius is calculated using the maximum of the announced yield range in DOE/NV (2000) and Equation (1) in Pawloski (1999). From Navarro-Intera (2014).
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NEW PROJECT: Scientific Focus Area: Characterization of field samples from Pu contaminated sites
In collaboration with SRS and Clemson Savannah River Site: Characterization of sediments associated with the Pu/Np-doped lysimeter coupons
Radiological Field Lysimeter Experiment (RadFLEx) at the Savannah River Site
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Samples and Depths (ft) B1HK27 (57-58) B1HK32 (70-72) B1HK42 (118-121) B1HVC8 (49-50) B1HK15 (~63-65) (~19.5m) B1HY61 (~81-82) (~25m) Uncontaminated sediments are sandy soils with quartz, clays, calcite, feldspar, minor oxides Collaboration with A. Felmy, PNNL
Cantrell et al., 2008
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Si Al
Fe Pu
Plagioclase Feldspars
Pu is associated with feldspars B1HY61 grains
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BSE
Si Al
Fe Pu
B1HK15: Pu is associated with Fe along the rim of the minerals
Next steps: Characterize Pu distribution in shallow Hanford sediments with high Pu Select samples to be used in desorption experiments XAS effort led by Los Alamos team