- •Preface
- •Acronyms
- •Introduction
- •Background and objectives
- •Content, format and presentation
- •Radioactive waste management in context
- •Waste sources and classification
- •Introduction
- •Radioactive waste
- •Waste classification
- •Origins of radioactive waste
- •Nuclear fuel cycle
- •Mining
- •Fuel production
- •Reactor operation
- •Reprocessing
- •Reactor decommissioning
- •Medicine, industry and research
- •Medicine
- •Industry
- •Research
- •Military wastes
- •Conditioning of radioactive wastes
- •Treatment
- •Compaction
- •Incineration
- •Conditioning
- •Cementation
- •Bituminisation
- •Resin
- •Vitrification
- •Spent fuel
- •Process qualification/product quality
- •Volumes of waste
- •Inventories
- •Inventory types
- •Types of data recorded
- •Radiological data
- •Chemical data
- •Physical data
- •Secondary data
- •Radionuclides occurring in the nuclear fuel cycle
- •Simplifying the number of waste types
- •Radionuclide inventory priorities
- •Material priorities
- •Inventory evolution
- •Assumptions
- •Errors
- •Uncertainties
- •Conclusions
- •Acknowledgements
- •References
- •Development of geological disposal concepts
- •Introduction
- •Historical evolution of geological disposal concepts
- •Geological disposal
- •Definitions and comparison with near-surface disposal
- •Development of geological disposal concepts
- •Roles of the geosphere in disposal options
- •Physical stability
- •Hydrogeology
- •Geochemistry
- •Overview
- •Alternatives to geological disposal
- •Introduction
- •Politically blocked options: sub-seabed and Antarctic icecap disposal
- •Sea dumping and sub-seabed disposal
- •Antarctic icesheet disposal
- •Technically impractical options; partitioning and transmutation, space disposal and icesheet disposal
- •Partitioning and Transmutation
- •Space disposal
- •Icesheets and permafrost
- •Non-options; long-term surface storage
- •Alternatives to conventional repositories
- •Introduction
- •Alternative geological disposal concepts
- •Utilising existing underground facilities
- •Extended storage options (CARE)
- •Injection into deep aquifers and caverns
- •Deep boreholes
- •Rock melting
- •The international option: technical aspects
- •Alternative concepts: fitting the management option to future boundary conditions
- •Conclusions
- •References
- •Site selection and characterisation
- •Introduction
- •Prescriptive/geologically led
- •Sophisticated/advocacy led
- •Pragmatic/technically led
- •Centralised/geologically led
- •Conclusions to be drawn
- •Lessons to be learned (see Table 4.2)
- •Site characterisation
- •Can we define the natural environment sufficiently thoroughly?
- •Sedimentary environments
- •Hydrogeology
- •The regional hydrogeological model
- •More local hydrogeological model(s)
- •Crystalline rock environments
- •Lithology and structure
- •Hydrogeology
- •Hydrogeochemistry
- •Any geological environment
- •References
- •Repository design
- •Introduction: general framework of the design process
- •Identification of design requirements/constraints
- •Concept development
- •Major components of the disposal system and safety functions
- •A structured approach for concept development
- •Detailed design/specifications of subsystems
- •Near-field processes and design issues
- •Design approach and methodologies
- •Design confirmation and demonstration
- •Interaction with PA/SA
- •Demonstration and QA
- •Repository management
- •Future perspectives
- •References
- •Assessment of the safety and performance of a radioactive waste repository
- •Introduction
- •The role of SA and the safety case in decision-making
- •SA tasks
- •System description
- •Identification of scenarios and cases for analysis
- •Consequence analysis
- •Timescales for evaluation
- •Constructing and presenting a safety case
- •References
- •Repository implementation
- •Legal and regulatory framework; organisational structures
- •Waste management strategies
- •The need for a clear policy and strategy
- •Timetables vary widely
- •Activities in development of a geological repository
- •Concept development
- •Siting
- •Repository design
- •Licensing
- •Construction
- •Operation
- •Monitoring
- •Research and development
- •The staging process
- •Attributes of adaptive staging
- •The decision-making process
- •Status of geological disposal programmes
- •Overview
- •Status of geological disposal projects in selected countries
- •International repositories
- •Costs and financing
- •Cost estimates
- •Financing
- •Conclusions
- •Acknowledgements
- •References
- •Research and development infrastructure
- •Introduction: Management of research and development
- •Drivers for research and development
- •Organisation of R&D
- •R&D in specialised (nuclear) facilities
- •Introduction
- •Inventory
- •Release of radionuclides from waste forms
- •Solubility and sorption
- •Waste form dissolution
- •Colloids
- •Organic degradation products
- •Gas generation
- •Conventional R&D
- •Engineered barriers
- •Corrosion
- •Buffer and backfill materials
- •Container fabrication
- •Natural barriers
- •Geochemistry and groundwater flow
- •Gas transport and two-phase flow
- •Biosphere
- •Radionuclide concentration and dispersion in the biosphere
- •Climate change
- •Landscape change
- •Underground rock laboratories
- •URLs in sediments
- •Nature’s laboratories: studies of the natural environment
- •General
- •Corrosion
- •Cement
- •Clay materials
- •Degradation of organic materials
- •Glass corrosion
- •Radionuclide migration
- •Model and database development
- •Conclusions
- •References
- •Building confidence in the safe disposal of radioactive waste
- •Growing nuclear concerns
- •Communication systems in waste management programmes
- •The Swiss programme
- •The Japanese programme
- •Examples of communication styles in other countries
- •Finland
- •Sweden
- •France
- •United Kingdom
- •Comparisons between communication styles in Finland, France, Sweden and the United Kingdom
- •Lessons for the future
- •What is the way forward?
- •Acknowledgements
- •References
- •A look to the future
- •Introduction
- •Current trends in repository programmes
- •Priorities for future efforts
- •Waste characterisation
- •Operational safety
- •Emplacement technologies
- •Knowledge management
- •Alternative designs and optimisation processes
- •Materials technology
- •Novel construction/immobilisation materials: the example of low pH cement
- •Future SA code development
- •Implications for environmental protection: disposal of other wastes
- •Conclusions
- •References
- •Index
Development of geological disposal concepts |
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fluxes, very low risk of human intrusion, etc.). Many studies of disposal variants have been carried out (e.g., Mobbs et al., 1989; Klett, 1997a,b) – the most extensive probably by the NEA (1988). Like on-seabed disposal (which is really a simple dumping option), however, most sub-seabed disposal options are also now banned by international convention (McCombie and Chapman, 2003a). An exception to this seems to be sub-seabed formations which are accessed from land. Although the legal situation here is certainly ambiguous, the existence of such repositories (e.g., Fig. 5.2a) indicates that they are, de facto, acceptable, although the recent EU ‘‘COMPASS’’ study (Dutton et al., 2004) is rather disingenuous in this regard – distinguishing only ‘‘on-shore disposal’’ and ‘‘offshore disposal in deep-sea sediments’’ – thus avoiding any discussion of coastal disposal options.
Basically, a coastal sub-seabed repository could be developed in a completely analogous way to an equivalent facility on land and hence will be implicitly included within the category of geological disposal. On the short term, such an option may have distinct advantages (as noted above) but, given the long timescales of interest, the effect of sealevel change on such coastal facilities needs to be considered very carefully. Advantages in ease of making a safety case over shorter timescales may be well compensated by much greater complexity at later times. Operationally, the safety concerns associated with massive construction projects below the sea also need to be carefully considered, but the existence of sub-seabed mines (e.g., the Durham (UK) coalfield under the North Sea) shows that this is feasible.
3.4.2.2. Antarctic icesheet disposal
Icesheet disposal is considered below but, as a special case, the Antarctic often receives particular attention due to its perceived great isolation from population centres. Disposal of all waste is, however, prohibited by the Antarctic Conservation Act and radwaste is explicitly excluded by Article 5 of the Antarctic Treaty.
3.4.3.Technically impractical options; partitioning and transmutation, space disposal and icesheet disposal
Discussions of the general problems of radwaste management with the general public inevitably drift onto the topics of ‘‘destruction’’ of the waste or simply shooting it into space. In principle, both are possible, but completely impractical based on existing technology or any currently imaginable development of it.
A point to be made at the outset is that these options are generally proposed for what are perceived by those unfamiliar with radwaste management to be the most problematic wastes – actinides and some of the longest lived fission products. As such, they are actually concentrated on wastes which could, in fact, be easily handled by geological disposal. From a purely technical viewpoint, some of the heterogeneous ILW-LL is most challenging for disposal (Hooper et al., 2005) and is not considered for such management options. Even worse, partitioning and transmutation (P&T) would probably significantly increase the inventory of this waste type.
For completeness, this section also considers icesheet disposal – an option increasingly seen as impractical due to the difficulty of assuring the longevity of ‘‘permanent’’ icesheets.
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I.G. McKinley et al. |
3.4.3.1. Partitioning and Transmutation
This is a proposed strategy for some actinides and fission products, which aims to reduce the need for long-term isolation of the waste by removing many of the long-lived isotopes. Note that P&T cannot eliminate the need for a geological repository, but it may change its design basis and, implicitly, its acceptability. This last point is rarely discussed, but a growing consensus is that most key stakeholder groups do not understand the subtle distinctions between HLW and ILW (see discussion of communication in Chapter 9) and hence this argument may be considerably over-played.
The basic principle behind P&T is straightforward – long-lived isotopes are irradiated to cause activation/fission reactions which produce shorter-lived products. In some concepts, the transmutation process itself may produce useable energy (e.g., Rubia et al., 1995). The great problem with this option is that additional nuclear facilities must be constructed and operated and enormous efforts are required in the separation of radionuclides before and after irradiation. This poses a risk to workers, is expensive and, in many cases, requires separation efficiencies which are far beyond existing technology. Based on present experience with reprocessing, the net result would be to replace a small quantity of homogeneous, very long-lived waste with a great quantity of different waste products containing isotopes with a wide range of half-lives.
The irradiation process, especially if using special reactors, particle accelerators, lasers, etc., also tends to be extremely expensive. For example, at a recent conference organised by SKB, Dr. Janne Wallenius (KTH, Stockholm) spoke in favour of P&T (Sains, 2004). However, Wallenius did admit that:
P&T would increase the cost of nuclear generated electricity by 25%
three to four new nuclear reactors with particle accelerators would need to be built for Sweden to use P&T
such a new technology would ‘‘. . . increase the risk for our generation (but would) reduce the risk for future generations.’’ because of decreased risk from SF
Note that this requires a huge nuclear infrastructure, all of which needs to be finally decommissioned – producing yet more secondary radwaste.
In principle, reprocessing with the extraction of U and Pu from spent fuel and the use of MOX in power reactors represent a kind of P&T (although it is not classified as such), which shows that the principle is feasible to some extent. The costs associated with even this very simple case, which have greatly limited its implementation, remove all credibility for the proposed option of transmuting minor actinides and long-lived fission products. To be brutal, claims for the value of exotic transmutation options must be seen more as a kind of funding hype for otherwise underemployed physicists rather than the basis for any kind of practical waste management options (e.g., Ninkovic and Raicevic, 2004; see also Box 3.2). Indeed, it has been argued by the Swedish safety regulators (SKI) that the advantage of reducing an extremely small (and hypothetical) risk from long-lived isotopes in the distant future has to be set against a major disadvantage of P&T, namely the increased risk of exposure to workers today due to significantly greater handling of short-lived, and hence high specific activity, isotopes; it could certainly be argued that the latter risk completely outweighs any potential gain.
Nevertheless, advances in partitioning technology could have clear practical applications in developing alternatives to the currently rather primitive wet chemistry approach to spent fuel reprocessing. It is thus not surprising that some of the countries which
Development of geological disposal concepts |
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Box 3.2. Exotic P&T options
A classic example of over-selling blue-sky physics research is laser transmutation. Demonstration of transmutation by an ultra-high power laser ( 5 1020 Watts cm 2) was quoted to show that ‘‘using lasers is a relatively cheap and very efficient way of disposing of nuclear waste’’ (Physicsweb, 2003). In fact, the picosecond laser pulse produces a relativistic plasma from a gold target, the ‘‘Bremsstrahlung’’ which causes the 129I ( , n) 128I reaction. Each shot produces about 3 106 128I nuclei – thus total conversion of the 50 g sample would require the laser to fire 1017 times. Not only would this require
an enormous amount of energy ( 107 GW h, assuming 100 per cent efficiency, for the laser power only), but would also take 1013 a (as the laser pulse rate is only once per hour). As 129I has a half-life
of a mere 16 Ma, it would have decayed away long before the transmutation process was completed. As noted above, the analysis assumed that all the chemical processing required can be carried out
extremely efficiently. Even if this was the case and the laser technology advanced to improve the firing rate by a factor of 1013, complete conversion of 50 g of 129I would not only require 103 GWa of power, it
would increase the specific activity of the waste by a factor of 5 1011. To put this 50 g in context, the annual production of 129I in spent fuel is in the order of 900 kg!
present P&T options prominently are those with a current investment in commercial/ military reprocessing and well established HLW disposal programmes (e.g., France, Japan, Russia and USA). With this wider viewpoint (e.g., RWMAC (2003)), the potential for a limited form of P&T involving advanced reprocessing and ‘‘actinide burning’’ reactors could be realised within a long-term nuclear fission programme (0100 a or so). In such a case, optimised fuel cycles which maximise power generation and minimise waste production are certainly possible and, in the right commercial environment, could even be financially attractive (Williams, 2000). There are no signs, however, that any conceivable decrease in toxicity of waste per unit power generation could remove the fundamental requirement for an associated waste disposal strategy.
3.4.3.2. Space disposal
This option gains most from its apparent ‘‘high-tech’’ complete solution to the problem as compared to the very ‘‘low-tech’’ approach of deep geological disposal (Rice and Priest, 1981). Although it may be contrary to national law in many countries (i.e., exporting of waste from national territory is not allowed) and to international conventions on the use of space, the situation is less clear than those options considered in section 3.4.2. However, implementing space disposal on the basis of existing technology can be rapidly ruled out as this is a very high-risk, high-consequence strategy. A short review of the world’s active space programmes clearly shows that the risk of catastrophic failure during spacecraft launch is significant (statistically, the chances of failure of a rocket lie in the 1–10 per cent range, depending on the maturity of the design) and the consequences of spreading a load of SF or HLW across the face of the earth following such a failure are potentially catastrophic.
Even with an emphasis on safety, the high cost of rocket launches severely constrains the measures which could be adopted if space disposal was to be seriously considered – e.g., for low earth orbit (LEO), launch costs are presently US$ 2 107 per tonne. Even without consideration of other requirements to remove the waste from earth’s orbit, this