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=== List of thorium-fueled reactors ===
=== List of thorium-fueled reactors (Most of this list appear to be Uranium or Plutonium fueled, rather than Thorium) ===
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Revision as of 18:37, 12 August 2011

The thorium fuel cycle is a nuclear fuel cycle that uses the naturally abundant isotope of thorium, 232
Th
, as the fertile material. In the reactor 232
Th
is transmuted into the fissile artificial uranium isotope 233
U
which is the nuclear fuel. Unlike natural uranium, natural thorium contains only trace amounts of fissile material (such as 231
Th
), which are insufficient to initiate a nuclear chain reaction. Additional fissile material or another neutron source are necessary to initiate the fuel cycle. In a thorium-fueled reactor, 232
Th
absorbs neutrons eventually to produce 233
U
. This parallels the process in uranium reactors whereby fertile 238
U
absorbs neutrons to form fissile 239
Pu
. Depending on the design of the reactor and fuel cycle, the 233
U
generated either fissions in situ or is chemically separated from the used nuclear fuel and formed into new nuclear fuel.

The thorium fuel cycle claims several potential advantages over a uranium fuel cycle, including thorium's greater abundance, superior physical and nuclear properties, enhanced proliferation resistance, and reduced plutonium and actinide production.

History

Concerns about the limits of worldwide uranium resources motivated initial interest in the thorium fuel cycle.[1] It was envisioned that as uranium reserves were depleted, thorium would supplement uranium as a fertile material. However, for most countries, uranium was relatively abundant, and research in thorium fuel cycles waned. A notable exception was India's three stage nuclear power programme. In the twenty-first century thorium's potential for improving proliferation resistance and waste characteristics led to renewed interest in the mineral.[2][3][4]

At Oak Ridge National Laboratory in the 1960s, the Molten-Salt Reactor Experiment used 233
U
as the fissile fuel as an experiment to demonstrate a part of the Molten Salt Breeder Reactor that was designed to operate on the thorium fuel cycle. Molten Salt Reactor (MSR) experiments assessed thorium's feasibility, using thorium(IV) fluoride dissolved in a molten salt fluid which eliminated the need to fabricate fuel elements. The MSR program was defunded in 1976.

In 2006 Carlo Rubbia proposed the concept of an energy amplifier or "accelerator driven system" (ADS), which he saw as a novel and safe way to produce nuclear energy that exploited existing accelerator technologies. Rubbia's proposal offered the potential to incinerate high-activity nuclear waste and produce energy from natural thorium and depleted uranium.[5][6]

Nuclear reactions with thorium

Actinides[7] by decay chain Half-life
range (a)
Fission products of 235U by yield[8]
4n 4n + 1 4n + 2 4n + 3 4.5–7% 0.04–1.25% <0.001%
228Ra 4–6 a 155Euþ
248Bk[9] > 9 a
244Cmƒ 241Puƒ 250Cf 227Ac 10–29 a 90Sr 85Kr 113mCdþ
232Uƒ 238Puƒ 243Cmƒ 29–97 a 137Cs 151Smþ 121mSn
249Cfƒ 242mAmƒ 141–351 a

No fission products have a half-life
in the range of 100 a–210 ka ...

241Amƒ 251Cfƒ[10] 430–900 a
226Ra 247Bk 1.3–1.6 ka
240Pu 229Th 246Cmƒ 243Amƒ 4.7–7.4 ka
245Cmƒ 250Cm 8.3–8.5 ka
239Puƒ 24.1 ka
230Th 231Pa 32–76 ka
236Npƒ 233Uƒ 234U 150–250 ka 99Tc 126Sn
248Cm 242Pu 327–375 ka 79Se
1.33 Ma 135Cs
237Npƒ 1.61–6.5 Ma 93Zr 107Pd
236U 247Cmƒ 15–24 Ma 129I
244Pu 80 Ma

... nor beyond 15.7 Ma[11]

232Th 238U 235Uƒ№ 0.7–14.1 Ga

In the thorium cycle, fuel is formed when 232
Th
captures a neutron (whether in a fast reactor or thermal reactor) to become 233
Th
. This normally emits an electron and an anti-neutrino (
ν
) by
β
decay
to become 233
Pa
. This then emits another electron and anti-neutrino by a second
β
decay to become 233
U
, the fuel:

Fission product wastes

Nuclear fission produces radioactive fission products which can have half-lives from days to greater than 200,000 years. According to some toxicity studies[12] the thorium cycle can fully recycle actinide wastes and only emit fission product wastes, after a few hundred years the waste from a thorium reactor can be less toxic than the uranium ore that would have been used to produce low enriched uranium fuel for a light water reactor of the same power. Other studies assume some actinide losses and find that actinide wastes dominate thorium cycle waste radioactivity at some future periods.[13]

Actinide wastes

In a reactor, when a neutron hits a fissile atom (such as certain isotopes of uranium), it either splits the nucleus or is captured and transmutes the atom. In the case of 233
U
, the transmutations tend to produce useful nuclear fuels rather than transuranic wastes. When 233
U
absorbs a neutron, it either fissions or becomes 234
U
. The chance of fissioning on absorption of a thermal neutron is about 92%; the capture-to-fission ratio of 233
U
, therefore, is about 1:10 - which is better than the corresponding capture vs. fission ratios of 235
U
(about 1:6), or 239
Pu
(about 1:2), or 241
Pu
(about 1:4).[1] The result is shorter-lived transuranic waste than in a reactor using the uranium-plutonium fuel cycle.

237Np
231U 232U 233U 234U 235U 236U 237U
231Pa 232Pa 233Pa 234Pa
230Th 231Th 232Th 233Th
  • Nuclides with a yellow background in italic have half-lives under 30 days
  • Nuclides in bold have half-lives over 1,000,000 years
  • Nuclides in red frames are fissile

234
U
, like most actinides with an even number of neutrons, is not fissile, but neutron capture produces fissile 235
U
. If the fissile isotope fails to fission on neutron capture, it produces 236
U
, 237
Np
, 238
Pu
, and eventually fissile 239
Pu
and heavier isotopes of plutonium. The 237
Np
can be removed and stored as waste or retained and transmuted to plutonium, where more of it fissions, while the remainder becomes 242
Pu
then americium and curium, which in turn can be removed as waste or returned to reactors for further transmutation and fission.

However, the 231
Pa
(with a half-life of 3.27×104 years) formed via (n,2n) reactions with 232
Th
(yielding 231
Th
that decays to 231
Pa
), while not a transuranic waste, is a major contributor to the long term radiotoxicity of spent nuclear fuel.

Uranium-232 contamination

Uranium-232 is also formed in this process, via (n,2n) reactions between fast neutrons and 233
U
, 233
Pa
, and 232
Th
:

Uranium-232 has a relatively short half-life (68.9 years), and some decay products emit high energy gamma radiation, such as 224
Rn
, 212
Bi
and particularly 208
Tl
. The full decay chain, along with half-lives and relevant gamma energies, is:

232
U
decays to 228
Th
where it joins decay chain of 232
Th

Thorium-cycle fuels produce hard gamma emissions, which damage electronics, limiting their use in military bomb triggers. 232
U
cannot be chemically separated from 233
U
from used nuclear fuel; however, chemical separation of thorium from uranium removes the decay product 228
Th
and the radiation from the rest of the decay chain, which gradually build up as 228
Th
reaccumulates. The hard gamma emissions also create a radiological hazard which requires remote handling during reprocessing.

Advantages as a nuclear fuel

Thorium is estimated to be about three to four times more abundant than uranium in the Earth's crust,[14] although present knowledge of reserves is limited. Current demand for thorium has been satisfied as a by-product of rare-earth extraction from monazite sands. Also, unlike uranium, mined thorium consists of a single isotope (232
Th
). Consequently, it is useful in thermal reactors without the need for isotope separation.

Thorium-based fuels exhibit several attractive properties relative to uranium-based fuels. The thermal neutron absorption cross section (σ
a
) and resonance integral (average of neutron cross sections over intermediate neutron energies) for 232
Th
are about three times and one third of the respective values for 238
U
; consequently, fertile conversion of thorium is more efficient in a thermal reactor. Also, although the thermal neutron fission cross section (σ
f
) of the resulting 233
U
is comparable to 235
U
and 239
Pu
, it has a much lower capture cross section (σ
γ
) than the latter two fissile isotopes, providing fewer non-fissile neutron absorptions and improved neutron economy. Finally, the ratio of neutrons released per neutron absorbed (η) in 233
U
is greater than two over a wide range of energies, including the thermal spectrum; as a result, thorium-based fuels can be the basis for a thermal breeder reactor[1].

Thorium-based fuels also display favorable physical and chemical properties which improve reactor and repository performance. Compared to the predominant reactor fuel, uranium dioxide (UO
2
), thorium dioxide (ThO
2
) has a higher melting point, higher thermal conductivity, and lower coefficient of thermal expansion. Thorium dioxide also exhibits greater chemical stability and, unlike uranium dioxide, does not further oxidize.[1]

Because the 233
U
produced in thorium fuels is inevitably contaminated with 232
U
, thorium-based used nuclear fuel possesses inherent proliferation resistance. 232
U
can not be chemically separated from 233
U
and has several decay products which emit high energy gamma radiation. These high energy photons are a radiological hazard that necessitate the use of remote handling of separated uranium and aid in the passive detection of such materials.

The long term (on the order of roughly 103 to 106 years) radiological hazard of conventional uranium-based used nuclear fuel is dominated by plutonium and other minor actinides, after which long-lived fission products become significant contributors again. A single neutron capture in 238
U
is sufficient to produce transuranic elements, whereas six captures are generally necessary to do so from 232
Th
. 98–99% of thorium-cycle fuel nuclei would fission at either 233
U
or 235
U
, so fewer long-lived transuranics are produced. Because of this, thorium is a potentially attractive alternative to uranium in mixed oxide (MOX) fuels to minimize the generation of transuranics and maximize the destruction of plutonium.

Disadvantages as nuclear fuel

There are several challenges to the application of thorium as a nuclear fuel, particularly for solid fuel reactors.

Unlike uranium, natural thorium contains no fissile isotopes; fissile material, generally 233
U
, 235
U
, or plutonium, must be added to achieve criticality. This, along with the high sintering temperature necessary to make thorium-dioxide fuel, complicates fuel fabrication. Oak Ridge National Laboratory experimented with thorium tetrafluoride as fuel in a molten salt reactor from 1964–1969, which was far easier to both process and separate from contaminants that slow or stop the chain reaction.

In an open fuel cycle (i.e. utilizing 233
U
in situ), higher burnup is necessary to achieve a favorable neutron economy. Although thorium dioxide performed well at burnups of 170,000 MWd/t and 150,000 MWd/t at Fort St. Vrain Generating Station and AVR respectively,[1] challenges complicate achieving this in light water reactors (LWR), which compose the vast majority of existing power reactors.

Another challenge associated with a once-through thorium fuel cycle is the comparatively long interval over which 232
Th
breeds to 233
U
. The half-life of 233
Pa
is about 27 days, which is an order of magnitude longer than the half-life of 239
Np
. As a result, substantial 233
Pa
develops in thorium-based fuels. 233
Pa
is a significant neutron absorber, and although it eventually breeds into fissile 235
U
, this requires two more neutron absorptions, which degrades neutron economy and increases the likelihood of transuranic production.

Alternatively, if solid thorium is used in a closed fuel cycle in which 233
U
is recycled, remote handling is necessary for fuel fabrication because of the high radiation levels resulting from the decay products of 232
U
. This is also true of recycled thorium because of the presence of 228
Th
, which is part of the 232
U
decay sequence. Further, unlike proven uranium fuel recycling technology (e.g. PUREX), recycling technology for thorium (e.g., THOREX) is only under development.

Although the presence of 232
U
complicates matters, 233
U
has occasionally been used to produce fission weapons. The United States first tested 233
U
as part of a bomb core in Operation Teapot in 1955.[15] However, unlike plutonium, 233
U
can be easily denatured by mixing it with natural or depleted uranium. Another option is to mix thorium fuels with small amounts of natural or depleted uranium during fabrication to ensure that 233
U
concentrations at cycle end are acceptably low.

Though thorium-based fuels produce far less long-lived transuranics than uranium-based fuels,[12] some long-lived actinide products constitute a long term radiological impact, especially 231
Pa
.[13]

Advocates for liquid core and molten salt reactors claim that these technologies negate thorium's disadvantages. Since only one liquid core reactor using thorium has been built, it is hard to validate the exact benefits.[citation needed] The lack of relevance to the nuclear weapon industry can be seen as a disadvantage to the development of Thorium usage in power generation,[dubiousdiscuss] but a worldwide resurgence of nuclear power use could provide enough incentives and funding to negate this disadvantage.

Reactors

Thorium fuels have fueled several different reactor types, including light water reactors, heavy water reactors, high temperature gas reactors, sodium-cooled fast reactors, and molten salt reactors.[16]

List of thorium-fueled reactors (Most of this list appear to be Uranium or Plutonium fueled, rather than Thorium)

Name Country Type Power Fuel Operation period
AVR Germany HTGR, Experimental (Pebble bed reactor) 015000 15 MW(e) Th+235
U
Driver Fuel, Coated fuel particles, Oxide & dicarbides
1967–1988
THTR-300 Germany HTGR, Power (Pebble Type) 300000 300 MW(e) Th+235
U
, Driver Fuel, Coated fuel particles, Oxide & dicarbides
1985–1989
Lingen Germany BWR Irradiation-testing 060000 60 MW(e) Test Fuel (Th,Pu)O2 pellets 1968; terminated in 1973
Dragon (OECD-Euratom) UK (also Sweden, Norway & Switzerland) HTGR, Experimental (Pin-in-Block Design) 020000 20 MWt Th+235
U
Driver Fuel, Coated fuel particles, Oxide & Dicarbides
1966–1973
Peach Bottom USA HTGR, Experimental (Prismatic Block) 040000 40 MW(e) Th+235
U
Driver Fuel, Coated fuel particles, Oxide & dicarbides
1966–1972
Fort St Vrain USA HTGR, Power (Prismatic Block) 330000 330 MW(e) Th+235
U
Driver Fuel, Coated fuel particles, Dicarbide
1976–1989
MSRE ORNL USA MSBR 007500 7.5 MWt 233
U
Molten Fluorides
1964–1969
Shippingport USA LWBR PWR, (Pin Assemblies) 100000 100 MW(e) Th+233
U
Driver Fuel, Oxide Pellets
1977–1982
Indian Point 1 USA LWBR PWR, (Pin Assemblies) 285000 285 MW(e) Th+233
U
Driver Fuel, Oxide Pellets
1962–1980
SUSPOP/KSTR KEMA Netherlands Aqueous Homogenous Suspension (Pin Assemblies) 001000 1 MWt Th+HEU, Oxide Pellets 1974–1977
NRX & NRU Canada MTR (Pin Assemblies) 020000 20MW; 200MW (see) Th+235
U
, Test Fuel
1947 (NRX) + 1957 (NRU); Irradiation–testing of few fuel elements
CIRUS; DHRUVA; & KAMINI India MTR Thermal 040000 40 MWt; 100 MWt; 30 kWt (low power, research) Al+233
U
Driver Fuel, ‘J’ rod of Th & ThO2, ‘J’ rod of ThO2
1960-2010 (CIRUS); others in operation
KAPS 1 &2; KGS 1 & 2; RAPS 2, 3 & 4 India PHWR, (Pin Assemblies) 220000 220 MW(e) ThO2 Pellets (For neutron flux flattening of initial core after start-up) 1980 (RAPS 2) +; continuing in all new PHWRs
FBTR India LMFBR, (Pin Assemblies) 040000 40 MWt ThO2 blanket 1985; in operation

(IAEA TECDOC-1450 "Thorium Fuel Cycle - Potential Benefits and Challenges", Table 1. Thorium utilization in different experimental and power reactors.)[1]

References

  1. ^ a b c d e f "IAEA-TECDOC-1450 Thorium Fuel Cycle-Potential Benefits and Challenges" (PDF). International Atomic Energy Agency. May 2005. Retrieved 2009-03-23.
  2. ^ "IAEA-TECDOC-1349 Potential of thorium-based fuel cycles to constrain plutonium and to reduce the long-lived waste toxicity" (PDF). International Atomic Energy Agency. 2002. Retrieved 2009-03-24.
  3. ^ Evans, Brett (April 14, 2006). "Scientist urges switch to thorium". ABC News. Retrieved 2010-06-19.
  4. ^ Martin, Richard (December 21, 2009). "Uranium Is So Last Century — Enter Thorium, the New Green Nuke". Wired. Retrieved 2010-06-19.
  5. ^ Dean, Tim (2006). "New age nuclear". Cosmos. Retrieved 2010-06-19. {{cite web}}: Unknown parameter |month= ignored (help)
  6. ^ MacKay, David J. C. (February 20, 2009). Sustainable Energy - without the hot air. UIT Cambridge Ltd. p. 166. Retrieved 2010-06-19.
  7. ^ Plus radium (element 88). While actually a sub-actinide, it immediately precedes actinium (89) and follows a three-element gap of instability after polonium (84) where no nuclides have half-lives of at least four years (the longest-lived nuclide in the gap is radon-222 with a half life of less than four days). Radium's longest lived isotope, at 1,600 years, thus merits the element's inclusion here.
  8. ^ Specifically from thermal neutron fission of uranium-235, e.g. in a typical nuclear reactor.
  9. ^ Milsted, J.; Friedman, A. M.; Stevens, C. M. (1965). "The alpha half-life of berkelium-247; a new long-lived isomer of berkelium-248". Nuclear Physics. 71 (2): 299. Bibcode:1965NucPh..71..299M. doi:10.1016/0029-5582(65)90719-4.
    "The isotopic analyses disclosed a species of mass 248 in constant abundance in three samples analysed over a period of about 10 months. This was ascribed to an isomer of Bk248 with a half-life greater than 9 [years]. No growth of Cf248 was detected, and a lower limit for the β half-life can be set at about 104 [years]. No alpha activity attributable to the new isomer has been detected; the alpha half-life is probably greater than 300 [years]."
  10. ^ This is the heaviest nuclide with a half-life of at least four years before the "sea of instability".
  11. ^ Excluding those "classically stable" nuclides with half-lives significantly in excess of 232Th; e.g., while 113mCd has a half-life of only fourteen years, that of 113Cd is eight quadrillion years.
  12. ^ a b Le Brun, C. "Impact of the MSBR concept technology on long-lived radio-toxicity and proliferation resistance" (PDF). Technical Meeting on Fissile Material Management Strategies for Sustainable Nuclear Energy, Vienna 2005. Retrieved 2010-06-20. {{cite web}}: Cite has empty unknown parameter: |month= (help); Unknown parameter |coauthors= ignored (|author= suggested) (help)
  13. ^ a b Brissot R.; Heuer D.; Huffer E.; Le Brun, C.; Loiseaux, J-M; Nifenecker H.; Nuttin A. (2001). "Nuclear Energy With (Almost) No Radioactive Waste?". Laboratoire de Physique Subatomique et de Cosmologie (LPSC). according to computer simulations done at ISN, this Protactinium dominates the residual toxicity of losses at 10000 years {{cite web}}: Unknown parameter |month= ignored (help)CS1 maint: multiple names: authors list (link)
  14. ^ "The Use of Thorium as Nuclear Fuel" (PDF). American Nuclear Society. November 2006. Retrieved 2009-03-24.
  15. ^ "Operation Teapot". Nuclear Weapon Archive. 15 October 1997. Retrieved 2008-12-09.

See also


Recent interest in the thorium fuel cycle