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In many European countries (e.g., Britain, Finland, the Netherlands, Sweden and Switzerland) the risk or dose limit for a member of the public exposed to radiation from a future high-level nuclear waste facility is considerably more stringent than that suggested by the International Commission on Radiation Protection or proposed in the United States. European limits are often more stringent than the standard suggested in 1990 by the International Commission on Radiation Protection by a factor of 20, and more stringent by a factor of ten than the standard proposed by the U.S. Environmental Protection Agency (EPA) for [[Yucca Mountain nuclear waste repository]] for the first 10,000 years after closure. Moreover, the U.S. EPA’s proposed standard for greater than 10,000 years is 250 times more permissive than the European limit.<ref>{{harvnb|Vandenbosch|2007|p=248.|Ref=none}}</ref>
In many European countries (e.g., Britain, Finland, the Netherlands, Sweden and Switzerland) the risk or dose limit for a member of the public exposed to radiation from a future high-level nuclear waste facility is considerably more stringent than that suggested by the International Commission on Radiation Protection or proposed in the United States. European limits are often more stringent than the standard suggested in 1990 by the International Commission on Radiation Protection by a factor of 20, and more stringent by a factor of ten than the standard proposed by the U.S. Environmental Protection Agency (EPA) for [[Yucca Mountain nuclear waste repository]] for the first 10,000 years after closure. Moreover, the U.S. EPA’s proposed standard for greater than 10,000 years is 250 times more permissive than the European limit.<ref>{{harvnb|Vandenbosch|2007|p=248.|Ref=none}}</ref>

The countries that have made the most progress towards a repository for high-level radioactive waste have typically started with [[public consultation]]s and made voluntary siting a necessary condition. This consensus seeking approach is believed to have a greater chance of success than top-down modes of decision making, but the process is necessarily slow, and there is inadequate experience around the world to know if it will succeed in all existing and aspiring nuclear nations.<ref>M.V. Ramana. Nuclear Power: Economic, Safety, Health, and Environmental Issues of Near-Term Technologies, ''Annual Review of Environment and Resources'', 2009, 34, p. 145.</ref>


===Asia===
===Asia===

Revision as of 02:23, 24 June 2010

High-level radioactive waste management concerns management and disposal of highly radioactive materials created during production of nuclear power and nuclear warheads. The technical issues in accomplishing this are daunting, due to the extremely long periods radioactive wastes remain deadly to living organisms. Of particular concern are two long-lived fission products, Technetium-99 (half-life 220,000 years) and Iodine-129 (half-life 15.7 million years),[1] which dominate spent nuclear fuel radioactivity after a few thousand years. The most troublesome transuranic elements in spent fuel are Neptunium-237 (half-life two million years) and Plutonium-239 (half-life 24,000 years).[2] Consequently, high-level radioactive waste requires sophisticated treatment and management to successfully isolate it from the biosphere. This usually necessitates treatment, followed by a long-term management strategy involving permanent storage, disposal or transformation of the waste into a non-toxic form.[3]

Governments around the world are considering a range of waste management and disposal options, usually involving deep-geologic placement, although there has been limited progress toward implementing long-term waste management solutions.[4] This is partly because the timeframes in question when dealing with radioactive waste range from 10,000 to millions of years,[5][6] according to studies based on the effect of estimated radiation doses.[7]

Challenges with radioactive waste management

Hannes Alfvén, Nobel laureate in physics, described the as yet unsolved dilemma of high-level radioactive waste management: "The problem is how to keep radioactive waste in storage until it decays after hundreds of thousands of years. The geologic deposit must be absolutely reliable as the quantities of poison are tremendous. It is very difficult to satisfy these requirements for the simple reason that we have had no practical experience with such a long term project. Moreover permanently guarded storage requires a society with unprecedented stability."[8]

Thus, Alfvén identified two fundamental prerequisites for effective management of high-level radioactive waste: (1) stable geological formations, and (2) stable human institutions over hundreds of thousands of years. As Alfvén suggests, no known human civilization has ever endured for so long, and no geologic formation of adequate size for a permanent radioactive waste repository has yet been discovered that has been stable for so long a period.[8] Nevertheless, avoiding confronting the risks associated with managing radioactive wastes may create countervailing risks of greater magnitude. Radioactive waste management is an example of policy analysis that requires special attention to ethical concerns, examined in the light of uncertainty and futurity: consideration of 'the impacts of practices and technologies on future generations'.[9]

There is a debate over what should constitute an acceptable scientific and engineering foundation for proceeding with radioactive waste disposal strategies. There are those who have argued, on the basis of complex geochemical simulation models, that relinquishing control over radioactive materials to geohydrologic processes at repository closure is an acceptable risk. They maintain that so-called “natural analogues” inhibit subterranean movement of radionuclides, making disposal of radioactive wastes in stable geologic formations unnecessary.[10] However, existing models of these processes are empirically underdetermined:[11] due to the subterranean nature of such processes in solid geologic formations, the accuracy of computer simulation models has not been verified by empirical observation, certainly not over periods of time equivalent to the lethal half-lives of high-level radioactive waste.[12][13] On the other hand, some insist deep geologic repositories in stable geologic formations are necessary. National management plans of various countries display a variety of approaches to resolving this debate.

Researchers suggest that forecasts of health detriment for such long periods should be examined critically.[14] Practical studies only consider up to 100 years as far as effective planning[15] and cost evaluations[16] are concerned. Long term behaviour of radioactive wastes remains a subject for ongoing research.[17] Management strategies and implementation plans of several representative national governments are described below.

Geologic disposal

The process of selecting appropriate permanent repositories for high level waste and spent fuel is now under way in several countries with the first expected to be commissioned some time after 2017.[18] The basic concept is to locate a large, stable geologic formation and use mining technology to excavate a tunnel, or large-bore tunnel boring machines (similar to those used to drill the Chunnel from England to France) to drill a shaft 500–1,000 meters below the surface where rooms or vaults can be excavated for disposal of high-level radioactive waste. The goal is to permanently isolate nuclear waste from the human environment. However, many people remain uncomfortable with the immediate stewardship cessation of this disposal system, suggesting perpetual management and monitoring would be more prudent.

Because some radioactive species have half-lives longer than one million years, even very low container leakage and radionuclide migration rates must be taken into account.[19] Moreover, it may require more than one half-life until some nuclear materials lose enough radioactivity to no longer be lethal to living things. A 1983 review of the Swedish radioactive waste disposal program by the National Academy of Sciences found that country’s estimate of several hundred thousand years—perhaps up to one million years—being necessary for waste isolation “fully justified.”[20]

Storing high level nuclear waste above ground for a century or so is considered appropriate by many scientists. This allows the material to be more easily observed and any problems detected and managed, while decay of radionuclides over this time period significantly reduces the level of radioactivity and associated harmful effects to the container material. It is also considered likely that over the next century newer materials will be developed which will not break down as quickly when exposed to a high neutron flux, thus increasing the longevity of the container once it is permanently buried.[21]

Sea-based options for disposal of radioactive waste[22] include burial beneath a stable abyssal plain and burial in a subduction zone that would slowly carry waste downward into the Earth's mantle. These approaches are currently not being seriously considered because of technical considerations, legal barriers in the Law of the Sea, and because in North America and Europe sea-based burial has become taboo from fear that such a repository could leak and cause widespread contamination.

The proposed land-based subductive waste disposal method would dispose of nuclear waste in a subduction zone accessed from land,[23] and therefore is not prohibited by international agreement. This method has been described as a viable means of disposing of radioactive waste,[24] and as a state-of-the-art nuclear waste disposal technology.[25]

In nature, sixteen repositories were discovered at the Oklo mine in Gabon where natural nuclear fission reactions took place 1.7 billion years ago.[26] The fission products in these natural formations were found to have moved less than 10 ft (3 m) over this time period.[27] However, the lack of movement may well be due more to retention in the uraninite structure than to insolubility and sorption from moving ground water; uraninite crystals are better preserved here than those in spent fuel rods because of a less complete nuclear reaction, so that reaction products would be less accessible to groundwater attack.[28]

Materials for geological disposal

In order to store the high level radioactive waste in long-term geological depositories, specific waste forms need to be used which will allow the radioactivity to decay away while the materials retain their integrity for thousands of years.[29]. The materials currently being used can be broken down into a few classes: glass waste forms, ceramic waste forms, and nanostructured materials.

The glass forms include borosilicate glasses and phosphate glasses. Borosilicate nuclear waste glasses are currently used on an industrial scale to immobilize high level radioactive waste in many countries which are currently producers of nuclear energy or have nuclear weaponry. The glass waste form have the advantage of being able to accommodate a wide variety of waste-stream compositions, they are easy to scale up to industrial processing, and they are stable against thermal, radiative, and chemical perturbations. These glasses function by binding radioactive elements to nonradioactive glass-forming elements[30] Phosphate glasses while not being used industrially have much lower dissolution rates than borosilicate glasses, which make them a more favorable option. However, no single phosphate material has the ability to accommodate all of the radioactive products so phosphate storage requires more reprocessing to separate the waste into distinct fractions.[31] Both glasses have to be processed at elevated temperatures making them unusable for some of the more volatile radiotoxic elements.

The ceramic waste forms offer higher waste loadings than the glass options because ceramics have crystalline structure. Also, mineral analogues of the ceramic waste forms provide evidence for long term durability.[32] Due to this fact and the fact that they can be processed at lower temperatures, ceramics are often considered the next generation in high level radioactive waste forms.[33] Ceramic waste forms offer great potential, but a lot of research remains to be done.

Nanostructured materials seem to be the frontier beyond ceramic waste forms. These vary the pore size to integrate radionuclides instead of specific atomic sites. This allows for greater chemical flexibility. Also, nanostructured materials have lower temperature processing and can be later altered to make more durable waste forms.[34]

National management plans

Finland, the United States and Sweden are the most advanced in developing a deep repository for high-level radioactive waste disposal. Countries vary in their plans on disposing used fuel directly or after reprocessing, with France and Japan having an extensive commitment to reprocessing. The country-specific status of high-level waste management plans are described below.

In many European countries (e.g., Britain, Finland, the Netherlands, Sweden and Switzerland) the risk or dose limit for a member of the public exposed to radiation from a future high-level nuclear waste facility is considerably more stringent than that suggested by the International Commission on Radiation Protection or proposed in the United States. European limits are often more stringent than the standard suggested in 1990 by the International Commission on Radiation Protection by a factor of 20, and more stringent by a factor of ten than the standard proposed by the U.S. Environmental Protection Agency (EPA) for Yucca Mountain nuclear waste repository for the first 10,000 years after closure. Moreover, the U.S. EPA’s proposed standard for greater than 10,000 years is 250 times more permissive than the European limit.[35]

The countries that have made the most progress towards a repository for high-level radioactive waste have typically started with public consultations and made voluntary siting a necessary condition. This consensus seeking approach is believed to have a greater chance of success than top-down modes of decision making, but the process is necessarily slow, and there is inadequate experience around the world to know if it will succeed in all existing and aspiring nuclear nations.[36]

Asia

China

In the Peoples Republic of China, ten reactors provide about 2% of electricity and five more are under construction.[37] China made a commitment to reprocessing in the 1980s; a pilot plant is under construction at Lanzhou, where a temporary spent fuel storage facility has been constructed. Geological disposal has been studied since 1985, and a permanent deep geological repository was required by law in 2003. Sites in Gansu Province near the Gobi desert in northwestern China are under investigation, with a final site expected to be selected by 2020, and actual disposal by about 2050.[38]

India

Sixteen nuclear reactors produce about 3% of India’s electricity, and seven more are under construction.[37] Spent fuel is processed at facilities in Trombay near Mumbai, at Tarapur on the west coast north of Mumbai, and at Kalpakkam on the southeast coast of India. Plutonium will be used in a fast breeder reactor (under construction) to produce more fuel, and other waste vitrified at Tarapur and Trombay.[39][40] Interim storage for 30 years is expected, with eventual disposal in a deep geological repository in crystalline rock near Kalpakkam.[41]

Japan

With 55 nuclear reactors producing about 29% of its electricity,[37] the Japanese policy is to reprocess its nuclear waste. Originally spent fuel was reprocessed under contract in England and France, but after public outcry a major reprocessing plant was built in Rokkasho, with operations expected to commence in 2007.[42] The policy to use recovered plutonium as mixed oxide (MOX) reactor fuel was questioned on economic grounds because there are few reactors capable of using it, and in 2004 it was revealed the Ministry of Economy, Trade and Industry had covered up a 1994 report indicating reprocessing spent fuel would cost four times as much as burying it.[43]

In 2000, a Specified Radioactive Waste Final Disposal Act called for creation of a new organization to manage high level radioactive waste, and later that year the Nuclear Waste Management Organization of Japan (NUMO) was established under the jurisdiction of the Ministry of Economy, Trade and Industry. NUMO is responsible for selecting a permanent deep geologic repository site, construction, operation and closure of the facility for waste emplacement by 2040.[44][45] Site selection was begun in 2002 and application information was sent to 3,239 municipalities, but by spring 2006, no local government had volunteered to host the facility. Final selection of a repository location is expected between 2023 and 2027.[46]

Europe

Belgium

The deep disposal of high-level radioactive waste (HLW) has been studied in Belgium for more than 30 years. Boom Clay is presently studied as a reference host formation for HLW disposal. The Hades underground research laboratory (URL) is located at −223 m in the Boom Formation at the Mol site. The Belgian URL is operated by the Euridice European Interest Group, a joint organisation between SCK•CEN, the Belgian Nuclear Research Centre which initiated the research on waste disposal in Belgium in the 1970s and 1980s and Ondraf/Niras, the waste management authorities. In Belgium, the regulatory body in charge of guidance and licensing approval is the Federal Agency of Nuclear Control, created in 2001.[47]

Finland

In 1983, the government decided to select a site for permanent repository by 2010. With four nuclear reactors providing 29% of its electricity,[37] Finland in 1987 enacted a Nuclear Energy Act making the producers of radioactive waste responsible for its disposal, subject to requirements of its Radiation and Nuclear Safety Authority and an absolute veto given to local governments in which a proposed repository would be located. Producers of nuclear waste organized Posiva Oy with responsibility for site selection, construction and operation of a permanent repository. A 1994 amendment to the Act required final disposal of spent fuel in Finland, prohibiting the import or export of radioactive waste.

Environmental assessment of four sites occurred in 1997–98, Posiva Oy chose the Olkiluoto site near two existing reactors, and the local government approved it in 2000. The Finnish Parliament approved a deep geologic repository there in igneous bedrock at a depth of about 500 meters in 2001. The repository concept is similar to the Swedish model, with containers to be clad in copper and buried below the water table beginning in 2020.[48]. An underground characterization facility is under construction at the site (2009)[49].

France

With 59 nuclear reactors contributing about 75% of its electricity,[37] the highest percentage of any country, France has been reprocessing its spent reactor fuel since the introduction of nuclear power there. Some reprocessed plutonium is used to make fuel, but more is being produced than is being recycled as reactor fuel.[50] France also reprocesses spent fuel for other countries, but the nuclear waste is returned to the country of origin. Radioactive waste from reprocessing French spent fuel is expected to be disposed of in a geological repository, pursuant to legislation enacted in 1991 that established a 15 year period for conducting radioactive waste management research. Under this legislation, partition and transmutation of long-lived elements, immobilization and conditioning processes, and long-term near surface storage are being investigated by a Commissariat a l’Energy Atomique (CEA). Disposal in deep geological formations is being studied by the French agency for radioactive waste management, Agence Nationale pour la gestion des Dechets Radioactifs, in underground research labs.[51]

Three sites were identified for possible deep geologic disposal in clay near the border of Meuse and Haute-Marne, near Gard, and at Vienne. In 1998 the government approved the Meuse/Haute Marne Underground Research Laboratory, a site near Meuse/Haute-Marne and dropped the others from further consideration.[21] Legislation was proposed in 2006 to license a repository by 2015, with operations expected in 2025.[52]

Germany

Nuclear waste policy in Germany is in flux. With 17 reactors in operation, accounting for about 30% of its electricity,[37] German planning for a permanent geologic repository began in 1974, focused on salt dome Gorleben, a salt mine near Gorleben about 100 kilometers northeast of Braunschweig. The site was announced in 1977 with plans for a reprocessing plant, spent fuel management, and permanent disposal facilities at a single site. Plans for the reprocessing plant were dropped in 1979. In 2000, the federal government and utilities agreed to suspend underground investigations for three to ten years, and the government committed to ending its use of nuclear power, closing one reactor in 2003.[53] In 2005 Angela Merkel was elected Chancellor with a promise to change the policy moving away from nuclear power, but was unsuccessful in doing so through November 2006.[54]

Meanwhile, electric utilities have been transporting spent fuel to interim storage facilities at Gorleben, Lubmin and Ahaus until temporary storage facilities can be built near reactor sites. Previously, spent fuel was sent to France or England for reprocessing, but this practice was ended in July 2005.[55]

Russia

In Russia, the Ministry of Atomic Energy (Minatom) is responsible for 31 nuclear reactors which generate about 16% of its electricity.[37] Minatom is also responsible for reprocessing and radioactive waste disposal, including over 25,000 tons of spent nuclear fuel in temporary storage in 2001.

Russia has a long history of reprocessing spent fuel for military purposes, and previously planned to reprocess imported spent fuel, possibly including some of the 33,000 metric tons of spent fuel accumulated at sites in other countries who received fuel from the U.S., which the U.S. originally pledged to take back, such as Brazil, the Czech Republic, India, Japan, Mexico, Slovenia, South Korea, Switzerland, Taiwan, and the European Union.[56][57]

An Environmental Protection Act in 1991 prohibited importing radioactive material for long-term storage or burial in Russia, but controversial legislation to allow imports for permanent storage was passed by the Russian Parliament and signed by President Putin in 2001.[56] In the long term, the Russian plan is for deep geologic disposal.[58] Most attention has been paid to locations where waste has accumulated in temporary storage at Mayak, near Chelyabinsk in the Ural Mountains, and in granite at Krasnoyarsk in Siberia.

Sweden

In Sweden there are ten operating nuclear reactors that produce about 45% of its electricity.[37] Two other reactors in Barsebäck were shut down in 1999 and 2005.[59] When these reactors were built, it was expected their nuclear fuel would be reprocessed in a foreign country, and the reprocessing waste would not be returned to Sweden.[60] Later, construction of a domestic reprocessing plant was contemplated, but has not been built.

Passage of the Stipulation Act of 1977 transferred responsibility for nuclear waste management from the government to the nuclear industry, requiring reactor operators to present an acceptable plan for waste management with “absolute safety” in order to obtain an operating license.[61][62] In early 1980, after the Three Mile Island meltdown in the United States, a referendum was held on the future use of nuclear power in Sweden. In late 1980, after a three-question referendum produced mixed results, the Swedish Parliament decided to phase out existing reactors by 2010.[63]

The Swedish Nuclear Fuel and Waste Management Co. (Svensk Kärnbränslehantering AB, known as SKB), was created in 1980 and is responsible for final disposal of nuclear waste there. This includes operation of a monitored retrievable storage facility, the Central Interim Storage Facility for Spent Nuclear Fuel at Oskarshamn, about 150 miles south of Stockholm on the Baltic coast; transportation of spent fuel; and construction of a permanent repository.[64] Swedish utilities store spent fuel at the reactor site for one year before transporting it to the facility at Oskarshamn, where it will be stored in excavated caverns filled with water for about 30 years before removal to a permanent repository. Conceptual design of a permanent repository was determined by 1983, calling for placement of copper-clad iron canisters in granite bedrock about 1,650 feet underground, below the water table in what is known as the KBS-3 method. Space around the canisters will be filled with bentonite clay.[64] After examining six possible locations for a permanent repository, three were nominated for further investigation at Osthammar, Oskarshamn, and Tierp. The first two are still under consideration,[65] with a final selection expected in 2009.[66] On 3 June 2009 Swedish government choose location for deep level waste site at Östhammar, near Forsmark Nuclear Powerplant.[67]

Switzerland

Switzerland has four nuclear reactors that provide about 43% of its electricity.[37]. Some Swiss spent nuclear fuel has been sent for reprocessing in France and the United Kingdom; most fuel is currently being stored without reprocessing. An industry-owned organization, ZWILAG, built and operates a central interim storage facility for spent nuclear fuel and high-level radioactive waste, and for conditioning low-level radioactive waste and for incinerating wastes. Other interim storage facilities predating ZWILAG continue to operate in Switzerland.

The Swiss program is currently considering options for the siting of a deep repository for high-level radioactive waste disposal, and for low & intermediate level wastes. Construction of a repository is not foreseen until well into this century. Research on sedimentary rock (especially Opalinus Clay) is presently carried out at the Swiss Mont Terri rock laboratory; the Grimsel Test Site, an older facility in crystalline rock is also still active.[68]

United Kingdom

Great Britain has 19 operating reactors, producing about 20% of its electricity.[37] It processes much of its spent fuel at Sellafield on the northwest coast across from Ireland, where nuclear waste is vitrified and sealed in stainless steel canisters for dry storage above ground for at least 50 years before eventual deep geologic disposal. Sellafield has a history of environmental and safety problems, including a fire in a nuclear plant in Windscale, and a significant incident in 2005 at the main reprocessing plant (THORP).[69]

In 1982 the Nuclear Industry Radioactive Waste Management Executive (NIREX) was established with responsibility for disposing of long-lived nuclear waste[70] and in 2006 a Committee on Radioactive Waste Management (CoRWM) of the Department of Environment, Food and Rural Affairs recommended geologic disposal 200–1,000 meters underground.[71] NIREX developed a generic repository concept based on the Swedish model[72] but has not yet selected a site. A Nuclear Decommissioning Authority is responsible for packaging waste from reprocessing and will eventually relieve British Nuclear Fuels Ltd. of responsibility for power reactors and the Sellafield reprocessing plant.[73]

North America

Canada

The 18 operating nuclear power plants in Canada generated about 16% of its electricity in 2006[74]. A national Nuclear Fuel Waste Act was enacted by the Canadian Parliament in 2002, requiring nuclear energy corporations to create a waste management organization to propose to the Government of Canada approaches for management of nuclear waste, and implementation of an approach subsequently selected by the government. The Act defined management as “long term management by means of storage or disposal, including handling, treatment, conditioning or transport for the purpose of storage or disposal.”[75]

The resulting Nuclear Waste Management Organization(NWMO) conducted an extensive 3-year study and consultation with Canadians. In 2005, they recommended Adaptive Phased Management, an approach that emphasized both technical and management methods. The technical method included centralized isolation and containment of spent nuclear fuel in a deep geologic repository in a suitable rock formation, such as the granite of the Canadian Shield or Ordovician sedimentary rocks.[76]. Also recommended was a phased decision making process supported by a program of continuous learning, research and development.

In 2007, the Canadian government accepted this recommendation, and NWMO was tasked with implementing the recommendation. No specific timeframe was defined for the process. Currently (2009) the NWMO is designing the process for site selection; siting is expected to take 10 years or more.[77]

United States

The Nuclear Waste Policy Act of 1982 established a timetable and procedure for constructing a permanent, underground repository for high-level radioactive waste by the mid-1990s, and provided for some temporary storage of waste, including spent fuel from 104 civilian nuclear reactors that produce about 19.4% of electricity there.[37] The United States in April 2008 had about 56,000 metric tons of spent fuel and 20,000 canisters of solid defense-related waste, and this is expected to increase to 119,000 metric tons by 2035.[78] The U.S. opted for Yucca Mountain nuclear waste repository, a final repository at Yucca Mountain in Nevada, but this project was widely opposed, with some of the main concerns being long distance transportation of waste from across the United States to this site, the possibility of accidents, and the uncertainty of success in isolating nuclear waste from the human environment in perpetuity. Yucca Mountain, with capacity for 70,000 metric tons of radioactive waste, was expected to open in 2017. However, the Obama Administration rejected use of the site in the 2009 United States Federal Budget proposal, which eliminated all funding except that needed to answer inquiries from the Nuclear Regulatory Commission, "while the Administration devises a new strategy toward nuclear waste disposal."[79] On March 5, 2009, Energy Secretary Steven Chu told a Senate hearing "the Yucca Mountain site no longer was viewed as an option for storing reactor waste."[78][80] The Waste Isolation Pilot Plant in the United States is the world's first underground repository for transuranic waste.

International repository

Although Australia does not have any nuclear power reactors, Pangea Resources considered siting an international repository in the outback of South Australia or Western Australia in 1998, but this stimulated legislative opposition in both states and the Australian national Senate during the following year.[81] Thereafter, Pangea ceased operations in Australia but reemerged as Pangea International Association, and in 2002 evolved into the Association for Regional and International Underground Storage with support from Belgium, Bulgaria, Hungary, Japan and Switzerland.[82] A general concept for an international repository has been advanced by one of the principals in all three ventures.[83] Russia has expressed interest in serving as a repository for other countries, but does not envision sponsorship or control by an international body or group of other countries. South Africa, Argentina and western China have also been mentioned as possible locations.[21][84]

In the EU, COVRA is negotiating a European-wide waste disposal system with single disposal sites that can be used by several EU-countries. This EU-wide storage possibility is being researched under the SAPIERR-2 program.[85]

Notes

  1. ^ "Environmental Surveillance, Education and Research Program". Idaho National Laboratory. Retrieved 2009-01-05.
  2. ^ Vandenbosch 2007, p. 21.
  3. ^ Ojovan, M. I.; Lee, W.E. (2005). An Introduction to Nuclear Waste Immobilisation. Amsterdam: Elsevier Science Publishers. p. 315. ISBN 0080444628.{{cite book}}: CS1 maint: multiple names: authors list (link)
  4. ^ Brown, Paul (2004-04-14). "Shoot it at the sun. Send it to Earth's core. What to do with nuclear waste?". The Guardian.
  5. ^ National Research Council (1995). Technical Bases for Yucca Mountain Standards. Washington, D.C.: National Academy Press. p. 91. ISBN 0309052890.
  6. ^ "The Status of Nuclear Waste Disposal". The American Physical Society. 2006. Retrieved 2008-06-06. {{cite web}}: Unknown parameter |month= ignored (help)
  7. ^ "Public Health and Environmental Radiation Protection Standards for Yucca Mountain, Nevada; Proposed Rule" (PDF). United States Environmental Protection Agency. 2005-08-22. Retrieved 2008-06-06.
  8. ^ a b Abbotts, John (1979). "Radioactive waste: A technical solution?". Bulletin of the Atomic Scientists: 12–18. {{cite journal}}: Unknown parameter |month= ignored (help)
  9. ^ Genevieve Fuji Johnson, Deliberative Democracy for the Future: The Case of Nuclear Waste Management in Canada, University of Toronto Press, 2008, p.9 ISBN 0-8020-9607-7
  10. ^ Bruno, Jordi, Lara Duro, and Mireia Grivé. 2001. The applicability and limitations of the geochemical models and tools used in simulating radionuclide behavior in natural waters: Lessons learned from the blind predictive modelling exercises performed in conjunction with natural analogue studies. QuantiSci S. L. Parc Tecnològic del Vallès, Spain, for Swedish Nuclear Fuel and Waste Management Co.
  11. ^ Shrader-Frechette, Kristin S. 1988. “Values and hydrogeological method: How not to site the world’s largest nuclear dump” In Planning for Changing Energy conditions, John Byrne and Daniel Rich, eds. New Brunswick, NJ: Transaction Books, p. 101 ISBN 0887387136
  12. ^ Shrader-Frechette, Kristin S. Burying uncertainty: Risk and the case against geological disposal of nuclear waste Berkeley: University of California Press (1993) p. 2 ISBN 0-520-08244-3
  13. ^ Shrader-Frechette, Kristin S. Expert judgment in assessing radwaste risks: What Nevadans should know about Yucca Mountain. Carson City: Nevada Agency for Nuclear Projects, Nuclear Waste Project, 1992 ISBN 0-7881-0683-X
  14. ^ "Issues relating to safety standards on the geological disposal of radioactive waste" (PDF). International Atomic Energy Agency. 2001-06-22. Retrieved 2008-06-06.
  15. ^ "IAEA Waste Management Database: Report 3 – L/ILW-LL" (PDF). International Atomic Energy Agency. 2000-03-28. Retrieved 2008-06-06.
  16. ^ "Decommissioning costs of WWER-440 nuclear power plants" (PDF). International Atomic Energy Agency. 2002. Retrieved 2008-06-06. {{cite web}}: Unknown parameter |month= ignored (help)
  17. ^ "Spent Fuel and High Level Waste: Chemical Durability and Performance under Simulated Repository Conditions" (PDF). International Atomic Energy Agency. 2007. IAEA-TECDOC-1563. {{cite journal}}: Cite journal requires |journal= (help); Unknown parameter |month= ignored (help)
  18. ^ Vandenbosch 2007, p. 214–248.
  19. ^ Vandenbosch 2007, p. 10.
  20. ^ Yates, Marshall (July 6). "DOE waste management criticized: On-site storage urged". Public Utilities Fortnightly (124): 33. {{cite journal}}: Check date values in: |date= and |year= / |date= mismatch (help)
  21. ^ a b c Committee on Disposition of High-Level Radioactive Waste through Geological Isolation, Board on Radioactive Waste Management, Division on Earth and Life Studies, National Research Council. (2001). Disposition of high-level waste and spent nuclear fuel: The continuing societal and technical challenges. Washington, DC: National Academy Press. ISBN 0309073170. {{cite book}}: |work= ignored (help)CS1 maint: multiple names: authors list (link)
  22. ^ Nadis, Steven (1996). "The sub-seabed solution". Atlantic Monthly (278): 28–39. {{cite journal}}: Unknown parameter |month= ignored (help)
  23. ^ Engelhardt, Dean; Parker, Glen. "Permanent Radwaste Solutions". San Francisco: Engelhardt, Inc. Retrieved 2008-12-24.{{cite web}}: CS1 maint: multiple names: authors list (link)
  24. ^ Jack, Tricia; Robertson, Jordan. "Utah nuclear waste summary" (PDF). Salt Lake City: University of Utah Center for Public Policy and Administration. Retrieved 2008-12-24.{{cite web}}: CS1 maint: multiple names: authors list (link)
  25. ^ Rao, K.R. (2001). "Radioactive waste: The problem and its management" (PDF). Current Science (81): 1534–1546. Retrieved 2008-12-24. {{cite journal}}: Unknown parameter |month= ignored (help)
  26. ^ Cowan, G. A. (1976). "Oklo, A Natural Fission Reactor". Scientific American. 235: 36. doi:10.1038/scientificamerican0776-36. ISSN 0036-8733.
  27. ^ "Oklo, Natural Nuclear Reactors". U.S. Department of Energy Office of Civilian Radioactive Waste Management, Yucca Mountain Project, DOE/YMP-0010. November 2004. Retrieved September 15, 2009.
  28. ^ Krauskopf, Konrad B. 1988. Radioactive waste and geology. New York: Chapman and Hall, 101–102. ISBN 0-412-28630-0
  29. ^ Clark, S., Ewing, R. Panel 5 Report: Advanced Waste Forms. Basic Research Needs for Advanced Energy Systems 2006, 59–74.
  30. ^ Grambow, B. (2006). "Nuclear Waste Glasses - How Durable?". Elements. 2: 357. doi:10.2113/gselements.2.6.357.
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See also

References

  • Vandenbosch, Robert; Vandenbosch, Susanne E. (2007). Nuclear waste stalemate. Salt Lake City: University of Utah Press. ISBN 0874809037.{{cite book}}: CS1 maint: multiple names: authors list (link)

Further reading

  • Shrader-Frechette, Kristin S. Risk analysis and scientific method: Methodological and ethical problems with evaluating societal hazards. Dordrecht: D. Reidel, 1985. ISBN 90-277-1836-9

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