Modelling microbiology, gas reaction and chemical evolution of geological disposal facilities Joe Small NNL Senior Research Fellow in Waste and Environmental Geochemistry Outline • WG5 expectations • Specific interests- Biogeochemical Modelling • • • • Approach for LLW surface disposal, UK Microbial Gas generation, TVO Finland Mont Terri Bitumen Nitrate experiment Cement pH, UK Bigrad Consortium • Benefit to the safety case • Proposal ideas Expectations on the outcome of WG-5 • An integrated and balanced proposal to address microbial effects that may be both beneficial or detrimental to the safety case: • Beneficial • Detrimental • Corrosion (MIC) • Methanogenesis • via acetate (LLW/ILW) • bulk gas • 14C release • Mediation of Eh & radionuclide speciation • H2 (& CH4) consumption • oxidation by Fe(III) & SO42• Methanogenesis (H2 only) • Fate of organic complexants “The safety case must be able to describe the evolution of the repository in a way that may be seen as a reasonable representation of what might happen….” (Topic 1, IGD-TP Strategic Research Agenda, 2011) Biogeochemical Modelling • Concepts and computer model developed in the UK for LLW surface disposal • Key component of 2002 (BNFL) and 2011 (LLWR Ltd) safety cases • Underpins near-field conceptual model • • • • • Eh evolution pH evolution (neutral & cement wasteform) Gas generation (CH4, H2) Radionuclide speciation and solubility (U, Tc) 14 C partitioning to gas, groundwater, carbonate precipitation • Generalised Repository Model (GRM) • Coupled reactive-transport model • Representation of main microbial metabolic processes: • • • • • • Aerobic Denitrification Fe(III) reduction Sulphate reduction Fermentation Methanogenesis • Rections between: • • H2, organics (cellulose, acetate), reduced minerals O2, NO3-, Fe(OH)3, SO42- Gas generation and microbial processes in repositories • VLJ Repository, Olkiluoto, Finland (operated by TVO) • Large Scale Gas Generation expt. Examines CH4, CO2, H2 generation from LLW/ILW • Initially concrete buffered pH • High water content • GRM Biogeochemical modelling • Constrains rates of gas generation • Builds confidence in the VLJ safety case • Validates microbial modelling approach for gas generation and chemical evolution • GRM and expt. data now used internationally • e.g. as a validation test case • UK, France, Canada, Switzerland Small, J. Nykyri, M., Helin, M., Hovi, U., Sarlin, T., Itävaara, M. (2008). Experimental and modelling investigations of the biogeochemistry of gas production from low and intermediate level radioactive waste. Applied Geochemistry 23. 1383-1418 TVO gas generation expt. 100 • Rate of CH4 production modelled accurately in “blind test” • Low levels of H2 measured in the experiment • H2 from corrosion consumed locally in waste by SRBs Model CH4 Volume % 10 Model CO2 1 Model H2 0.1 Expt H2 vol% Expt CH4 vol% Expt CO2 vol% 1/1998 1/1999 1/2000 1/2001 1/2002 1/2003 • Heterogeneity in pH allows microbial processes to develop at neutral pH in waste drums • Eventually, concrete buffered alkaline water is neutralised 1/2004 Average model pH, measured pH 0.01 1/1997 12 Model pH, concrete 11 On-line measurement 10 Tank water, drum lid level 9 Tank water, bottom Model pH, water 8 Waste drum, 95% biodeg. 7 Waste drum, 6% biodeg. 6 Model pH, waste 5 1997 1998 1999 2000 2001 2002 Date 2003 2004 2005 2006 Effect of nitrate in radioactive waste disposal • Nitrate is a strong oxidant (electron acceptor) • Potential to affect the speciation and transport behaviour of redox sensitive radionuclides e.g. Se, Tc, U, Np, Pu • Large amounts of nitrate salts are present in bituminised waste, produced in France and Belgium • The Mont Terri Bitumen-Nitrate experiment examines the biogeochemistry of nitrate interaction with a clay formation. NO3- & organics injected into borehole in Opalinus Clay 1 Measured NO3 0.9 • Migration 2013, Brighton; Small, J, Abrahamsen L, Albrecht A, Bleyen N, Valcke E Modelled NO3 in sampled volume Nitrate concentration (mM) • GRM Model aids the interpretation of expt data • Has been used to forward model the effect on redox potential (Eh) and U and Tc radionuclide speciation 0.8 Modelled NO3 in filter volume R eduction by co injected acetate 0.7 Modelled NO3 adjacent to clay 0.6 Modelled NO3 in first 5mm of clay 0.5 Modelled NO3 in 5-10mm of clay 0.4 0.3 R eduction by F eS 2 and F eC O 3 0.2 0.1 0 0 2 4 6 8 10 12 days after injection 14 16 18 20 Online monitoring Microbial Biomass: 1. Modelled Biomass of borehole and EDZ 2. MPN cultivation/ATP/SEM analysis of sampled fluid 5.0E+06 4.5E+06 Total biomass, Cells per ml of fluid Cell 1: sampled volume Maximum microbial activity in the sampled volume related to NO3 reduction by acetate Cell 2: filter volume 4.0E+06 Cell 3: void adjacent to clay 3.5E+06 Cell 4: 0 to 5mm of clay Cell 5: 5 to 10mm clay Nitrate and nitrite reducers utilising FeCO3 and FeS2 3.0E+06 Cell 6: 10 to 15mm clay 2.5E+06 Continuing growth on the borehole surface related to stimulation of sulphate reducing and fermentative processes by initial denitrification processes. Effect is uncertain 2.0E+06 Cell 7: 15 to 20mm clay MPN counts, Moors et al, 2012 1.5E+06 Filtered material (2mls) after 19 days 1.0E+06 5.0E+05 0.0E+00 0 5 10 15 20 25 30 35 40 Time, days Moors, H., Geissler, A., Boven, P., Selenska-Pobell, S and Leys, N. BN Experiment: Intermediate results of the microbiological analyses. Mont Terri Project Technical Note 2011-39, 2012. ` Microbial activity under cementitious conditions (pH 9-13) • See Jon Lloyd presentation • GRM models of denitrification, Fe reduction, and Eh at pH 10 • SO42- reduction and CH4 formation energetically less favourable at high pH • Modelled Tc speciation consistent with observed microbial reduction • U speciation models (based on NEA database) predict U(VI) whereas microbial U reduction observed Groundwater flow Host Rock Cementitious Near Field pH 7 pH 12.5 pH Eh ? Biogeochemical Gradients Microbial processes? Tc, U, Np ? 1200 Model Eh 7.E-05 1000 6.E-05 800 Expt. Eh, Anaerobic 600 Eh, mV 5.E-05 Concentration, mol/l Expt. Eh + lactate NO2- 4.E-05 Redox couple: NO3/ N2 400 200 3.E-05 0 NO3- 2.E-05 -200 Nitrate (model) Nitrite (model) 1.E-05 -400 Nitrate Expt Redox couple: Fe(OH)3/ Fe2+ Nitrite Expt -600 0.E+00 0 5 10 15 Time days 20 25 30 0 5 10 15 Time, days 20 25 30 The safety assessment perspective: how can we contribute to a competent safety case? • Asses the viability of microbial processes under the range of physical and chemical conditions of ILW, HLW/SF wasteforms, engineered barriers and geosphere interface • Realistic consideration of the fate of gases (H2), organics (CDPs) and electron acceptors (NO3-) released from the waste and engineered barriers • Development of microbiological process models (conceptual and mathematical) for repository evolution and radionuclide behaviour in the multibarrier system Remaining issues and a proposal for future research • Investigate the viability of specific microbial processes that may be detrimental to the safety case: • Sulphate reduction and MIC in bentonite • Methanogenesis under cementitious conditions • Develop a microbiological process model that reasonably describes the fate of repository derived energy sources: H2 and CH4 gases, organics, including cellulose degradation products, nitrates and other electron acceptors present, and which takes account of physical and chemical conditions heterogeneities and interfaces which may inhibit or promote microbial activity. • To test hypotheses for the Eh evolution and speciation of redox sensitive radionuclides. • • • • • Utilise and develop current biogeochemical modelling approaches as an interpretive tool and to represent the above in the safety case
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