Sorption of Uranium (VI) to Graphite under Potential Repository Conditions

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Sorption of Uranium (VI) to Graphite under Potential Repository Conditions Gary Cerefice, Gregory Schmidt, and Cory Keith University of Nevada, Las Vegas GSA Annual Meeting 11/5/12 This work was supported by the Department of Energy, Deep Burn Program, under agreement Battelle Energy Alliance Contract No. 0081547 PRIME DOE- DE-AC07-05ID14517 & Contract No. 00094935 PRIME DOE-DE-AC07-05ID14517

Outline Graphite in Geological Repository Systems Experimental Methodology Graphite Characterization Results Effect of ph on Equilibrium Sorption Carbonate and Ionic Strength Sorption Kinetics and Desorption Sorption Isotherms Conclusions & Future Work 2

HTGR Fuel Disposal BWR Fuel 1 TRISO Fuel 2 3

Backfill Applications Drift Backfill Borehole Casing/Backfill http://www.tms.org/pubs/journals/jom/0009/yim-0009.html http://www.neimagazine.com/story.asp?storycode=2055862

Experimental Methodology Stock Solutions Depleted uranium UO 2 (NO 3 ) 2 in 0.01 M HCl Spiked with 233 U (Eckert & Ziegler) - 100 Bq/sample Analysis by Liquid Scintillation Counting Batch Experiments Common Parameters 10 ml:1g solution to graphite ratio 10 samples per data point (7 samples, 3 blanks) I = 0.01M NaCl ph controlled by addition of 0.01 M HCl or NaOH Borax buffer used for ph 7 to 10 region FEP Tubes used from ph 6 to 8 to minimize sorption Mixed on Hematology Mixer for 5 days, Centrifuge to Separate 5

Graphite Characterization Alpha Aesar (-20/+100) X-Ray Diffraction No minor phases observed FTIR Spectroscopy 1631 suggests sp 2 -hybridized C 1384 suggests C-OH formation 3477 suggests surface water or hydrogen-bonded OH groups BET Surface Area 0.554 ± 0.027 m 2 /g Proton Exchange Capacity 0.25 ± 0.15 cmol/kg Point of Zero Charge ph = 9.3 Sqrt(Counts) 450 400 350 300 250 200 150 100 50 0 10 Graphite Alfa Aesar New 4-9-10.raw Graphite 2H 100.00 % 20 30 40 50 60 70 2Th Degrees 80 90 100 110

Equilibrium Sorption ph Effects (K d = 126 ± 7.0 ml/g) 7

Equilibrium Sorption vs. Speciation Speciation Curve Generated using EQ3/6 with the YM Database

Effect of Ionic Strength ph 4.03 4.06 4.07 [NaCl] (molal) 0.01 0.05 0.1 K d (ml/g) 8.23 ± 0.08 8.58 ± 0.04 7.73 ± 0.05 5.07 5.14 5.16 0.01 1 4 51.43 ± 6.84 58.74 ± 15.5 59.84 ± 19.5

Effect of CO 2 on Sorption [CO 2 ], ppm ph Mass % Sorbed K d (ml/g) Atmospheric 9.27 21.0% ± 2.27% 2.48 ± 0.25 < 1 9.30 36.7% ± 2.11% 5.48 ± 0.28 ~1,000,000 9.28 ~0% N/A Atmospheric 7.30 92.6% ± 0.97% 126.4 ± 0.28 ~1,000,000 7.50 ~0% N/A Atmospheric 4.85 75.3% ± 3.03% 39.3 ± 4.9 ~1,000,000 4.75 28.78% ± 6.59% 4.43 ± 1.6

Kinetic Studies Two apparent partitioning phases Rapid Initial Sorption Slower kinetic phase Incomplete recovery during desorption Approx. 10 µg U / g graphite remained sorbed 11

Sorption Isotherms Kinetic sorption and desorption data suggest at least 2 sites Fit w/ Freundlich Isotherm, q = (0.930)c eq 0.37 (ph 5)

Kinetic Sorption Model Two apparent partitioning phases Incomplete recovery during desorption Approx. 10 µg U / g graphite remained sorbed Kinetic Sorption Model Features: Sorption behavior has an equilibrium and kinetic fraction Eq. fraction has higher K d than kinetic fraction Can be sub-divided into a low/high solution mass region Eq. fraction fills before kinetic fraction in partitioning Kinetic fraction has first order rate constant of α = 0.01925 hr -1 Equilibrium fraction maximum loading is 1.7 µg U / g graphite 13

Slow Flow Column Experiment 45-60 minute flow times used at constant concentration Tritium used as conservative tracer 14

Model Prediction vs. Experimental Results 15

Conclusions and Future Work Sorption to graphite is not insignificant Particularly at near neutral ph Irreversibility of sorption can provide additional barrier to release Carbonate complexation appears to suppress sorption Future Work Sorption mechanism is still unknown Effects of graphite surface preparation needs to be examined particularly surface oxidation Need longer term desorption data to bound desorption kinetics Data needed at elevated temperatures Isotherms need to be extended to lower concentrations Need to extend to other elements (Np, Pu, I, Tc) 16

Questions? 1) Westinghouse Electric Company, Flyer: NF-FE-0011, SVEA-96 Optima2 BWR Fuel 2) Morris, E. E., T. H. Bauer, Modeling of the Repository Behavior of TRISO Fuel, Nuclear Engineering Division, Argonne National Laboratory. (2005) 3) Fachinger, J. A., M den Exter, et al. (2006) Behaviour of spent HTR fuel elements in aquatic phases of repository host rock formations Nuclear Engineering and Design, 236 pp. 543-554 4) General Atomics, (1996) Gas Turbine-Modular Helium Reactor (GT-MHR) Conceptual Design Description Report. GA Project No. 7658, San Diego, CA 5) Nickel, H., H. Nabielek, (2002) Long-term Experience with the Development of HTR Fuel Elements in Germany. Nuclear Engineering and Design, 217 141-151 6) Petti, D. A., J. Buongiorno, et al. (2003) Key differences in the Fabrication, Irradiation and High Temperature Accident Testing of US and German TRISO-coated Particle Fuel, and Their Implications on Fuel Performance. Nuclear Engineering and Design 222 281-297 7) Sims, D.J., W.S. Andrews, K.A.M. Creber, (2008), Diffusion Coefficients for Uranium, Cesium and Strontium in Unsaturated Prarie Soil, Journal of Radioanalytical and Nuclear Chemistry, 277(1) pp. 143-147 17