Thorium in Australia
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Table 2.Iii.1. Fissionable Isotopes1
FISSIONABLE ISOTOPES Charles P. Blair Last revised: 2012 “While several isotopes are theoretically fissionable, RANNSAD defines fissionable isotopes as either uranium-233 or 235; plutonium 238, 239, 240, 241, or 242, or Americium-241. See, Ackerman, Asal, Bale, Blair and Rethemeyer, Anatomizing Radiological and Nuclear Non-State Adversaries: Identifying the Adversary, p. 99-101, footnote #10, TABLE 2.III.1. FISSIONABLE ISOTOPES1 Isotope Availability Possible Fission Bare Critical Weapon-types mass2 Uranium-233 MEDIUM: DOE reportedly stores Gun-type or implosion-type 15 kg more than one metric ton of U- 233.3 Uranium-235 HIGH: As of 2007, 1700 metric Gun-type or implosion-type 50 kg tons of HEU existed globally, in both civilian and military stocks.4 Plutonium- HIGH: A separated global stock of Implosion 10 kg 238 plutonium, both civilian and military, of over 500 tons.5 Implosion 10 kg Plutonium- Produced in military and civilian 239 reactor fuels. Typically, reactor Plutonium- grade plutonium (RGP) consists Implosion 40 kg 240 of roughly 60 percent plutonium- Plutonium- 239, 25 percent plutonium-240, Implosion 10-13 kg nine percent plutonium-241, five 241 percent plutonium-242 and one Plutonium- percent plutonium-2386 (these Implosion 89 -100 kg 242 percentages are influenced by how long the fuel is irradiated in the reactor).7 1 This table is drawn, in part, from Charles P. Blair, “Jihadists and Nuclear Weapons,” in Gary A. Ackerman and Jeremy Tamsett, ed., Jihadists and Weapons of Mass Destruction: A Growing Threat (New York: Taylor and Francis, 2009), pp. 196-197. See also, David Albright N 2 “Bare critical mass” refers to the absence of an initiator or a reflector. -
An Introduction to Isotopic Calculations John M
An Introduction to Isotopic Calculations John M. Hayes ([email protected]) Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA, 30 September 2004 Abstract. These notes provide an introduction to: termed isotope effects. As a result of such effects, the • Methods for the expression of isotopic abundances, natural abundances of the stable isotopes of practically • Isotopic mass balances, and all elements involved in low-temperature geochemical • Isotope effects and their consequences in open and (< 200°C) and biological processes are not precisely con- closed systems. stant. Taking carbon as an example, the range of interest is roughly 0.00998 ≤ 13F ≤ 0.01121. Within that range, Notation. Absolute abundances of isotopes are com- differences as small as 0.00001 can provide information monly reported in terms of atom percent. For example, about the source of the carbon and about processes in 13 13 12 13 atom percent C = [ C/( C + C)]100 (1) which the carbon has participated. A closely related term is the fractional abundance The delta notation. Because the interesting isotopic 13 13 fractional abundance of C ≡ F differences between natural samples usually occur at and 13F = 13C/(12C + 13C) (2) beyond the third significant figure of the isotope ratio, it has become conventional to express isotopic abundances These variables deserve attention because they provide using a differential notation. To provide a concrete the only basis for perfectly accurate mass balances. example, it is far easier to say – and to remember – that Isotope ratios are also measures of the absolute abun- the isotope ratios of samples A and B differ by one part dance of isotopes; they are usually arranged so that the per thousand than to say that sample A has 0.3663 %15N more abundant isotope appears in the denominator and sample B has 0.3659 %15N. -
Th Thorium Compounds with S, Se, Te and B
springer.com Chemistry : Chemistry (general) Brown, David, Wedemeyer, Horst, Buschbeck, Karl-Christian, Keller, Cornelius (Editors-in-chief.) Th Thorium Compounds with S, Se, Te and B The present volume, Thorium C5, deals with the compounds of thorium and sulfur, selenium, tellurium, and boron, as well as with oxoacid compounds of the three chalcogen elements. Thorium borates have already been treated in Thorium C2. In contrast to the corresponding compounds of uranium the thorium sulfides, etc. , do not show any nuclear or other technological application; they are only of academic interest, despite some very interest• ing electronic properties, especially of the 1 : 1 compounds. The thorium-sulfur and the thorium• boron systems in particular were studied in detail, so that we have a clear picture of them, whereas there are still a lot of open questions in the systems Th-Se and Th-Te - not very different from other metal chalcogenide systems. Thorium sulfates are of some technological importance because they are formed in solution during recovery of thorium from monazite by sulfuric acid leaching. The very detailed and critical treatment of the chemical and physical Springer properties of the compounds discussed also enables us to find gaps still remaining in our 8th ed. 1985, XIX, 149 p. knowledge and thus to initiate new research in this field. I want to thank the two authors, Dr. 8th 28 illus., 1 illus. in color. edition Horst Wedemeyer (Karlsruhe) and Dr. David Brown (Harwell), for their excellent contributions, the "Literaturabteilung" of the Karlsruhe Nuclear Research Center for its help in providing reports and other documents difficult to procure, as well as the staff of the Gmelin-Institute, especially to Dr. -
Study of Rare Earth Elements, Uranium and Thorium Migration in Rocks from Espinharas Uranium Deposit, Paraiba - Brazil
2009 International Nuclear Atlantic Conference - INAC 2009 Rio de Janeiro,RJ, Brazil, September27 to October 2, 2009 ASSOCIAÇÃO BRASILEIRA DE ENERGIA NUCLEAR - ABEN ISBN: 978-85-99141-03-8 STUDY OF RARE EARTH ELEMENTS, URANIUM AND THORIUM MIGRATION IN ROCKS FROM ESPINHARAS URANIUM DEPOSIT, PARAIBA - BRAZIL Cirilo C.S. Conceição Instituto de Radioproteção e Dosimetria -IRD Av. salvador Allend, S/N - Jacarepaguá Rio de Janeiro, Brazil CEP.: 22780-160 [email protected] ABSTRACT The determination of Rare Earth Elements as natural analogue in patterns geologic has grown as a tool for predicting the long-term safety of nuclear disposal in geological formation. Migration of natural radionuclides is one of the most serious problems in the waste deposit from nuclear fuel cycle. Rare Earth Elements show the same kinetic behavior in rocks as natural radionuclides. This similar property of the analogues allows perform studies and models on the subject of radionuclides migration. The aim of this study was to determine the distribution of Rare Earth Elements in rocks located at Espinharas – Paraíba – Brazil, uranium deposit. In this work are presented the results from the study above the distribution of rare earth elements in function of the degree of mineralized rocks, composition and the conditions of radioactive equilibrium of the uranium and thorium in some fractures on the rocks from radioactive occurrence of Espinharas-Brazil. The results show that there is a correlation of heavy Rare Earth Elements, uranium and Thorium concentrations to oxidation factor of the rocks. However this correlation was not observed for light Rare Earth Elements. It means that heavy Rare earth Elements follow the natural radionuclides in oxidation process of rocks. -
Toxicological Profile for Plutonium
PLUTONIUM 1 1. PUBLIC HEALTH STATEMENT This public health statement tells you about plutonium and the effects of exposure to it. The Environmental Protection Agency (EPA) identifies the most serious hazardous waste sites in the nation. These sites are then placed on the National Priorities List (NPL) and are targeted for long-term federal clean-up activities. Plutonium has been found in at least 16 of the 1,689 current or former NPL sites. Although the total number of NPL sites evaluated for this substance is not known, strict regulations make it unlikely that the number of sites at which plutonium is found would increase in the future as more sites are evaluated. This information is important because these sites may be sources of exposure and exposure to this substance may be harmful. When a substance is released from a large area, such as an industrial plant, or from a container, such as a drum or bottle, it enters the environment. This release does not always lead to exposure. You are normally exposed to a substance only when you come in contact with it. You may be exposed by breathing, eating, or drinking the substance, or by skin contact. However, since plutonium is radioactive, you can also be exposed to its radiation if you are near it. External exposure to radiation may occur from natural or man-made sources. Naturally occurring sources of radiation are cosmic radiation from space or radioactive materials in soil or building materials. Man- made sources of radioactive materials are found in consumer products, industrial equipment, atom bomb fallout, and to a smaller extent from hospital waste and nuclear reactors. -
Chromium-Nickel Steels Depleted of Nickel Stable Isotope Ni-58 As a Material for Fast Reactor Claddings
IAEA-CN-114/15p Chromium-Nickel steels depleted of nickel stable isotope Ni-58 as a material for fast reactor claddings G.L.Khorasanov, A.P.Ivanov, A.I.Blokhin, N.A.Demin Institute of Physics and Power Engineering named after A.I.Leypunsky 1, Bondarenko square, Obninsk, Kaluga region, 249033 Russia Tel.: +7-08439-98505, Fax: +7-095-2302326, E-mail: [email protected] INTRODUCTION Presently, the creation of new materials for fast reactor (FR) claddings is one of the main tasks of the nuclear engineering [1]. Now the Russian austenitic steel grade TchS68 with 15 % of nickel content is used as a material for the Russian FR BN-600 claddings [2]. With such a cladding the BN-600 fuel rod is stably operating during 10 years up to the fuel burn-up fraction of 10 % of heavy atoms (h.a.). The cladding material becomes swelled and unfit for further service after the fuel burn-up fraction of 10 % h.a. The task of increasing the fuel burn-up fraction up to 14 % h.a. is now the principal one for the BN-600 operation. For this purpose the new radiation–resistant austenitic steel grade EK164 with 19 % of nickel content is now developing in the Bochvar Institute, Russia [3]. It is generally assumed that steel swelling is caused by the combined action of radiation damage and helium accumulation in the irradiated material. In this case, nickel stable isotope, Ni-58 (its content in natural nickel is equal to 68%) is a source of helium creation. After 4 neutron capture via (n,g) reaction, Ni-58 is transmuted to radioisotope Ni-59 (T1/2=7.6⋅10 years) which has a high value of (n,α) reaction cross-section for thermal and epithermal neutrons. -
Lithium Isotope Fractionation During Uptake by Gibbsite
Available online at www.sciencedirect.com ScienceDirect Geochimica et Cosmochimica Acta 168 (2015) 133–150 www.elsevier.com/locate/gca Lithium isotope fractionation during uptake by gibbsite Josh Wimpenny a,⇑, Christopher A. Colla a, Ping Yu b, Qing-Zhu Yin a, James R. Rustad a, William H. Casey a,c a Department of Earth and Planetary Sciences, University of California, One Shields Avenue, Davis, CA 95616, United States b The Keck NMR Facility, University of California, One Shields Avenue, Davis, CA 95616, United States c Department of Chemistry, University of California, One Shields Avenue, Davis, CA 95616, United States Received 5 November 2014; accepted in revised form 8 July 2015; available online 15 July 2015 Abstract The intercalation of lithium from solution into the six-membered l2-oxo rings on the basal planes of gibbsite is well-constrained chemically. The product is a lithiated layered-double hydroxide solid that forms via in situ phase change. The reaction has well established kinetics and is associated with a distinct swelling of the gibbsite as counter ions enter the interlayer to balance the charge of lithiation. Lithium reacts to fill a fixed and well identifiable crystallographic site and has no solvation waters. Our lithium-isotope data shows that 6Li is favored during this intercalation and that the À À solid-solution fractionation depends on temperature, electrolyte concentration and counter ion identity (whether Cl ,NO3 À or ClO4 ). We find that the amount of isotopic fractionation between solid and solution (DLisolid-solution) varies with the amount of lithium taken up into the gibbsite structure, which itself depends upon the extent of conversion and also varies À À À with electrolyte concentration and in the counter ion in the order: ClO4 <NO3 <Cl . -
Radiological Implications of Plutonium Recycle and the Use of Thorium Fuels in Power Reactor Operations
01 RD/B/N3523 Central Electricity Generating Board Research Department Berkeley Nuclear Laboratories RADIOLOGICAL IMPLICATIONS OF PLUTONIUM RECYCLE AND THE USE OF THORIUM FUELS IN POWER REACTOR OPERATIONS By H. F. Macdonald XJ034 January 1976 DISCLAIMER Portions of this document may be illegible in electronic image products. Images are produced from the best available original document. Radiological Implications of Plutonium Recycle and the Use of Thorium Fuels in Power Reactor Operations “ by - H.F. Macdonald Approved Head of Health Physics Research Section For inclusion in Nuclear Science Abstracts SUMMARY As economically attractive sources of natural uranium are gradually depleted attention will turn to recycling plutonium or the use of thorium fuels. In this study the radiological implications of these fuel cycles in terms of fuel handling and radioactive waste disposal are investigated in 235 relation to a conventional U enriched oxide fuel. It is suggested that a comparative study of this nature may be an important aspect of the overall optimisation of future fuel cycle strategies. It is shown that the use of thorium based fuels has distinct advan tages in terms of neutron dose rates from irradiated fuels and long term a decay heating commitment compared with conventional uranium/plutonium fuels. However, this introduces a y dose rate problem in the fabrication 233 and handling of unirradiated U fuels. For both plutonium and thorium fuels these radiological problems increase during storage of the fuel prior to reactor irradiation. Finally, the novel health physics problems which arise in the handling and processing of thorium fuels are reviewed in an appendix. -
The Actinide Research Quarterly Is Published Quarterly to Highlight Recent Achievements and Ongoing Programs of the Nuclear Materials Technology Division
1st quarter 2000 TheLos Actinide Alamos National Research Laboratory N u c l e a r M aQuarterly t e r i a l s R e s e a r c h a n d T e c h n o l o g y a U.S. Department of Energy Laboratory Organizers Issue an Invitation to In This Issue Plutonium Futures 1 —The Science Organizers Issue an Invitation to Plutonium Futures —The Science The second of a series of international con- have an exciting collection of some 180 invited ferences on plutonium will be held in Santa Fe, and contributed papers with topics ranging 2 NM, this summer, July 10–13. It follows the very broadly in materials science, transuranic 238Pu Aqueous highly successful 1997 conference, “Plutonium waste forms, nuclear fuels and isotopes, separa- Processing Line Will Futures - The Science,” which attracted over 300 tions, actinides in the environment, detection Provide New NMT participants representing 14 countries. The U.S. and analysis, actinide compounds and com- Capability participants, who made up about 70 percent of plexes, and condensed matter physics of ac- the total participants, came from Department of tinides. These papers, presented in separate 4 Energy national laboratories and a score of uni- oral and poster sessions, will give attendees a Editorial: versities and industries. As in 1997, the confer- chance to learn about current research outside Transactinium ence is sponsored by the Los Alamos National of their particular specialties and provide an Science Needs Laboratory in cooperation with the American opportunity for interdisciplinary discussions Educational Nuclear Society. -
Isotopic Composition of Fission Gases in Lwr Fuel
XA0056233 ISOTOPIC COMPOSITION OF FISSION GASES IN LWR FUEL T. JONSSON Studsvik Nuclear AB, Hot Cell Laboratory, Nykoping, Sweden Abstract Many fuel rods from power reactors and test reactors have been punctured during past years for determination of fission gas release. In many cases the released gas was also analysed by mass spectrometry. The isotopic composition shows systematic variations between different rods, which are much larger than the uncertainties in the analysis. This paper discusses some possibilities and problems with use of the isotopic composition to decide from which part of the fuel the gas was released. In high burnup fuel from thermal reactors loaded with uranium fuel a significant part of the fissions occur in plutonium isotopes. The ratio Xe/Kr generated in the fuel is strongly dependent on the fissioning species. In addition, the isotopic composition of Kr and Xe shows a well detectable difference between fissions in different fissile nuclides. 1. INTRODUCTION Most LWRs use low enriched uranium oxide as fuel. Thermal fissions in U-235 dominate during the earlier part of the irradiation. Due to the build-up of heavier actinides during the irradiation fissions in Pu-239 and Pu-241 increase in importance as the burnup of the fuel increases. The composition of the fission products varies with the composition of the fuel and the irradiation conditions. The isotopic composition of fission gases is often determined in connection with measurement of gases in the plenum of punctured fuel rods. It can be of interest to discuss how more information on the fuel behaviour can be obtained by use of information available from already performed determinations of gas compositions. -
Nature No. 2468, Vol
FEBRUARY IS, 1917J NATURE LETTERS TO THE EDITOR. and in Paris, several of them fam l-us for their atomic- weight determinations, doubt has lingered with r-egard [The Editor does not hold himself responsible for to our results for the very much more difficult case of opinions expressed by his correspondents. Neither thorium lead. In the first place, no one but myself can he undertake to return, or to correspond with has been able to obtain a suitable material by which the writers of, rejected manuscripts intended for to test the question, and I, of course, can claim no this or any other part of NATURE. No notice is previous experience of atomic-weight work. In the taken of anonymous communications.] second place, there has been an unfortunate confusion The Atomic Weight of "Thorium" Lead. between my material, Ceylon thorite, and thorianite, IN continuation of preliminary work published by a totally distinct mixed thorium and uranium Ceylon Mr. H. Hyman and myself (Trans. Chern. Soc., 1914, mineral. Lastly, there has been the widespread view, due :v., 1402) I gave an account in NATURE, February 4, to Holmes and Lawson, Fajans, and others, mainly 1915, p. 615, of the preparation of 80 grams of lead derived from geological evidence, that thorium-E, the from Ceylon thorite and of the determination of its isotope of lead resulting from the ultimate change of density in comparison with that of ordinary lead, thorium, was not sufficiently stable to accumulate over which proved the thorite lead to be 0'26 per cent. geological periods of time. -
Highly Enriched Uranium: Striking a Balance
OFFICIAL USE ONLY - DRAFT GLOSSARY OF TERMS APPENDIX F GLOSSARY OF TERMS Accountability: That part of the safeguards and security program that encompasses the measurement and inventory verification systems, records, and reports to account for nuclear materials. Assay: Measurement that establishes the total quantity of the isotope of an element and the total quantity of that element. Atom: The basic component of all matter. Atoms are the smallest part of an element that have all of the chemical properties of that element. Atoms consist of a nucleus of protons and neutrons surrounded by electrons. Atomic energy: All forms of energy released in the course of nuclear fission or nuclear transformation. Atomic weapon: Any device utilizing atomic energy, exclusive of the means for transportation or propelling the device (where such means is a separable and divisible part of the device), the principal purpose of which is for use as, or for development of, a weapon, a weapon prototype, or a weapon test device. Blending: The intentional mixing of two different assays of the same material in order to achieve a desired third assay. Book inventory: The quantity of nuclear material present at a given time as reflected by accounting records. Burnup: A measure of consumption of fissionable material in reactor fuel. Burnup can be expressed as (a) the percentage of fissionable atoms that have undergone fission or capture, or (b) the amount of energy produced per unit weight of fuel in the reactor. Chain reaction: A self-sustaining series of nuclear fission reactions. Neutrons produced by fission cause more fission. Chain reactions are essential to the functioning of nuclear reactors and weapons.