by prashant selvaratnam department of earth sciences university of cambridge supervisor: dr. ian...

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By Prashant Selvaratnam Department of Earth Sciences University of Cambridge Supervisor: Dr. Ian Farnan

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Page 1: By Prashant Selvaratnam Department of Earth Sciences University of Cambridge Supervisor: Dr. Ian Farnan

By Prashant SelvaratnamDepartment of Earth SciencesUniversity of Cambridge

Supervisor: Dr. Ian Farnan

Page 2: By Prashant Selvaratnam Department of Earth Sciences University of Cambridge Supervisor: Dr. Ian Farnan

Mineral Based Phosphate Ceramics

Phosphate minerals:

- Evidence from nature of long term stability.

- Ability to incorporate tri- and tetra-valent actinides and other fission products.

- Ability to incorporate halides.

Ceramics:

- High durability.

- High waste loading.

Oklo natural reactor, Gabon

Image from DOE Office of Civilian Radioactive Waste Management.

Page 3: By Prashant Selvaratnam Department of Earth Sciences University of Cambridge Supervisor: Dr. Ian Farnan

Fluorapatite Ca10(PO4)6F2

Structure and chemistry allow for a multitude of substitutions.

Two distinct cationic sites: Four Ca1 sites, 9-fold co-ordination. Six Ca2 sites, 7-fold co-ordination.

Suitable for waste streams from fluoride-salt extraction: Experimental pyroprocessing techniques. Decommissioning of nuclear weapons. Generation IV nuclear fuels.

Page 4: By Prashant Selvaratnam Department of Earth Sciences University of Cambridge Supervisor: Dr. Ian Farnan

Fluorapatite Synthesis Solid state synthesis. 3Ca3(PO4)2 + CaF2 Ca10(PO4)6F2

Mixture ground together. Sintered at 8000C for 2 hours. Re-ground and pressed into ~1g pellets. Calcinated at 1,0000C for 2 hours.

Analysed by powder X-ray diffraction and 31P Nuclear Magnetic Resonance.

} X 2

Page 5: By Prashant Selvaratnam Department of Earth Sciences University of Cambridge Supervisor: Dr. Ian Farnan

Powder X-ray Diffraction

Page 6: By Prashant Selvaratnam Department of Earth Sciences University of Cambridge Supervisor: Dr. Ian Farnan

31P NMR One Phosphorus environment. Peak at 2.3ppm. Full width half maximum ~1ppm.

Page 7: By Prashant Selvaratnam Department of Earth Sciences University of Cambridge Supervisor: Dr. Ian Farnan

Ce Doping Ce used as a surrogate for Pu. Similar electronegativity, ionic radii and oxidation states. Require Ce3+ state. Coupled substitution:

Ce3+ and Na+ for 2Ca2+

3Ca3(PO4)6 + 10xCeF3 + (1-20x)CaF2 + 10xNaF → (Ca(1-2x)CexNax)10(PO4)6F2

Where 0 ≤ x ≥ 0.05. Problems with melting samples. Reducing ramp rate from 200C/min to 100C/min helps.

Page 8: By Prashant Selvaratnam Department of Earth Sciences University of Cambridge Supervisor: Dr. Ian Farnan

Ce Doping Use X-ray diffraction and NMR to study phase assemblages, solid solubility, Ce oxidation state and site distribution.

Page 9: By Prashant Selvaratnam Department of Earth Sciences University of Cambridge Supervisor: Dr. Ian Farnan

SRIM Calculations Produce a sample with a uniform damage profile. Ions must completely penetrate sample. 29MeV/nucleon Pb ion beam, retarded to 11MeV/nucleon.

Page 10: By Prashant Selvaratnam Department of Earth Sciences University of Cambridge Supervisor: Dr. Ian Farnan

Xenotime YPO4

Empirical potential suitable for molecular dynamics simulations of radiation damage.

Empirically tuned, using GULP, to re-produce: Inter-atomic distances and lattice parameters. Elastic constants.

Mindful of phase separation into P2O5 and Y2O3.

Interatomic potentials: Buckingham Potential: V(r) = Aexp(-Br) – C/r6

Morse Potential: V(r) = D [1-exp(a(r-ro)))2 – 1]

Where r is the inter-atomic distance.

Page 11: By Prashant Selvaratnam Department of Earth Sciences University of Cambridge Supervisor: Dr. Ian Farnan

Xenotime PotentialsPotential 1 Potential 2* Potential 3

Charge balanced for P2O5 & Y2O3

X

Y-O Potential Buckingham Buckingham Buckingham

O-O Potential Buckingham Buckingham Buckingham

P-O Potential Morse Buckingham Morse

C11 -0.4% +53% -5.9%

C33 +0.9% +12.9% +3.6%

C44 -6.1% +18.4% +3.0%

C66 +1.1% +52.9% +17.6%

C12 -47.2% +5.4% -40.0%

C13 +2.3% +16.3% -4.6%

Lattice constant 1 0.0% -1.7% -0.2%

Lattice constant 2 0.0% +3.3% +0.2%

P-O distance 0.0% +1.0% -12.0%

Y-O distance 1 +0.8% -7.0% +6.8%

Y-O distance 2 -1.7% +4.2% +4.0%

* P-O-P bond angle term used

Page 12: By Prashant Selvaratnam Department of Earth Sciences University of Cambridge Supervisor: Dr. Ian Farnan

Preliminary ConclusionsFluorapatite

Pure phase fluorapatite synthesis possible via solid state methods. 31P NMR peak at 2.3ppm. Problems with sample melting for Ce-doped sample synthesis in

ambient atmosphere. Sample thickness of < 82µm required to obtain uniform damage

profile in 11MeV/nucleon Pb beam.

Xenotime Difficult to get a wholly satisfactory YPO4 potential that is charge

balanced with respect to P2O5 and Y2O3.

Having a Morse potential between P and O improves the output.

Page 13: By Prashant Selvaratnam Department of Earth Sciences University of Cambridge Supervisor: Dr. Ian Farnan

Future Work

Fluorapatite Ce-doped sample synthesis under reducing atmosphere. NMR analysis of Ce-doped fluorapatite samples. Make and analyse 80µm thick, 1.5cm x 1.5cm samples for ion

beam damage.

Xenotime Do one GULP fit for YPO4, P2O5 and Y2O3.

Run DL_POLY radiation damage simulations using obtained potentials.

Page 14: By Prashant Selvaratnam Department of Earth Sciences University of Cambridge Supervisor: Dr. Ian Farnan

Acknowledgements

Ian Farnan, Martin Dove, Clive Brigden, Katie Gunderson, Tony Abraham, Martin Walker (University of Cambridge).

Shirley Fong, Brian Metcalfe, Phillip Mallinson (AWE).

Ram Devanathan (Pacific North West National Lab, US Department of Energy).

Christina Trautmann, (GSI Helmholtz Centre for Heavy Ion Research)

Lou Vance (Australian Nuclear Science and Technology Organisation).