Radiological Implications of Plutonium Recycle and the Use of Thorium Fuels in Power Reactor Operations
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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. -
Properties of Selected Radioisotopes
CASE FILE COPY NASA SP-7031 Properties of Selected Radioisotopes A Bibliography PART I: UNCLASSIFIED LITERATURE NATIONAL AERONAUTICS AND SPACE ADMINISTRATION NASA SP-7031 PROPERTIES OF SELECTED RADIOISOTOPES A Bibliography Part I: Unclassified Literature A selection of annotated references to technical papers, journal articles, and books This bibliography was compiled and edited by DALE HARRIS and JOSEPH EPSTEIN Goddard Space Flight Center Greenbelt, Maryland Scientific and Technical Information Division / OFFICE OF TECHNOLOGY UTILIZATION 1968 USP. NATIONAL AERONAUTICS AND SPACE ADMINISTRATION Washington, D.C. PREFACE The increasing interest in the application of substantial quantities of radioisotopes for propulsion, energy conversion, and various other thermal concepts emphasizes a need for the most recent and most accurate information available describing the nuclear, chemical, and physical properties of these isotopes. A substantial amount of progress has been achieved in recent years in refining old and developing new techniques of measurement of the properties quoted, and isotope processing. This has resulted in a broad technological base from which both the material and information about the material is available. Un- fortunately, it has also resulted in a multiplicity of sources so that information and data are either untimely or present properties without adequately identifying the measurement techniques or describing the quality of material used. The purpose of this document is to make available, in a single reference, an annotated bibliography and sets of properties for nine of the more attractive isotopes available for use in power production. Part I contains all the unclassified information that was available in the literature surveyed. Part II is the classified counterpart to Part I. -
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. -
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. -
Upper Limit of the Periodic Table and the Future Superheavy Elements
CLASSROOM Rajarshi Ghosh Upper Limit of the Periodic Table and the Future Department of Chemistry The University of Burdwan ∗ Superheavy Elements Burdwan 713 104, India. Email: [email protected] Controversy surrounds the isolation and stability of the fu- ture transactinoid elements (after oganesson) in the periodic table. A single conclusion has not yet been drawn for the highest possible atomic number, though there are several the- oretical as well as experimental results regarding this. In this article, the scientific backgrounds of those upcoming super- heavy elements (SHE) and their proposed electronic charac- ters are briefly described. Introduction Totally 118 elements, starting from hydrogen (atomic number 1) to oganesson (atomic number 118) are accommodated in the mod- ern form of the periodic table comprising seven periods and eigh- teen groups. Total 92 natural elements (if technetium is consid- ered as natural) are there in the periodic table (up to uranium hav- ing atomic number 92). In the actinoid series, only four elements— Keywords actinium, thorium, protactinium and uranium—are natural. The Superheavy elements, actinoid rest of the eleven elements—from neptunium (atomic number 93) series, transactinoid elements, periodic table. to lawrencium (atomic number 103)—are synthetic. Elements after actinoids (i.e., from rutherfordium) are called transactinoid elements. These are also called superheavy elements (SHE) as they have very high atomic numbers. Prof. G T Seaborg had Elements after actinoids a very distinct contribution in the field of transuranium element (i.e., from synthesis. For this, Prof. Seaborg was awarded the Nobel Prize in rutherfordium) are called transactinoid elements. 1951. -
ORAU Team Document Number: ORAUT-TKBS-0016-5
ORAU Team Document Number: ORAUT-TKBS-0016-5 Dose Reconstruction Project for NIOSH Effective Date: 09/09/2004 Technical Basis Document for the Mound Site – Occupational Revision No.: 00 Controlled Copy No.: ________ Internal Dosimetry Page 1 of 65 Subject Expert: Jere Millard Supersedes: Document Owner Approval: Signature on File Date: 09/09/2004 Jeffrey S. Vollmer, TBD Team Leader None Approval: Signature on File Date: 09/09/2004 Judson L. Kenoyer, Task 3 Manager Concurrence: Signature on File Date: 09/09/2004 Richard E. Toohey, Project Director Approval: Signature on File Date: 09/09/2004 James W. Neton, Associate Director for Science TABLE OF CONTENTS Section Page Record of Issue/Revisions.................................................................................................................4 Acronyms and Abbreviations .............................................................................................................5 5.1 Introduction ..............................................................................................................................7 5.1.1 Mound Feed Materials .....................................................................................................7 5.1.2 Radionuclides of Concern ................................................................................................7 5.1.3 Internal Dose Control Program .........................................................................................9 5.1.4 Gross Alpha Analysis .................................................................................................... -
What Is Plutonium?
The Nuclear Regulatory Commission’s Science 101: What is Plutonium? Plutonium is a radioactive, metallic element with the atomic number 94. It was discovered in 1940 by scientists studying the process of splitting atoms. Plutonium is created in a nuclear reactor when uranium atoms, specifically uranium-238, absorb neutrons. Nearly all plutonium is man-made. Plutonium predominantly emits alpha particles—a type of radiation that does not penetrate and has a short range. It also emits neutrons, beta particles and gamma rays. It is considered toxic, in part, because if it were to be inhaled it could deposit in lungs and eventually cause damage to the tissue. Plutonium has five “common” isotopes, Pu-238, Pu-239, Pu-240, Pu-241, and Pu-242. All of the more common isotopes of plutonium are “fissionable”—which means the atom’s nucleus can easily split apart if it is struck by a neutron. The various isotopes of plutonium have been used in a number of applications. Plutonium-239 contains the highest quantities of fissile material, and is notably one of the primary fuels used in nuclear weapons. Plutonium-238 has more benign applications and has been used to power batteries for some heart pacemakers, as well as provide a long-lived heat source to power NASA space missions. Like uranium, plutonium can also be used to fuel nuclear power plants, as is done in a few countries. Currently, the U.S. does not use plutonium fuel in its power reactors. Nuclear reactors that produce commercial power in the United States today create plutonium through the irradiation of uranium fuel. -
Los Alamos NATIONAL LABORATORY
— . .. ,. ~ - /3~5Y” m5 ~“3 CIC-14 REPORT CQUECTW REPRODUCTION COPY Measurement and Accounting of the Minor Adinides Produced in Nuclear Power Reactors Los Alamos NATIONAL LABORATORY .i,os Alarnos National Laboratory is operated by the University of Cal~ornia for the United States Department of Energy under contract W-7405-ENG-36. Etlifeci by Paul IV. Fknriksen, Group ClC-l Prepared by Celirza M. CMz, Group lVIS-5 This work was supported by the U.S. Department of Energy, Ofice of lVonprol~eration and National Security, Ofice of Safeguards and Security, An Ajirmativc AcfionfEqual Opporfunify Employer This report waspreparedasan accountof worksponsoredby an agencyof theUnited States Govemrnent. NeitherTheRegentsof fhe Universityof Cal@rnia,the United Stafes Government norany agencythereof,norany of theiremployees,makesany warranty,express or implied,or assumesany legalliabilityor responsibilify~ortheaccuracy,completeness, or usefulness of any information, apparatus, product, or process disclosed,orrepresentsthat its use wouldnof infringe privately owned rights. Referenceherein to any speczfic commercial product, process, or seru”ce by trade name, trademark, manufacturer, or otherwise, doesnot necessarily constitute or imply its endorsement, recommendation, or favoring by The Regents of the University of California, fhe LInifedStates Government, or any agency thereof. The views and opinions of aufhors expressed herein do nof necessarily sfate or r~ect those of The Regents of the University of Calt@nia, the Unifed Sfates Government, or any agency thereo$ The Los A[amos National Laboratory strongly supports academic freedom and a researcher’s right to publish; therefore, the .!..aboratory as an institution doesnot endorse the viewpoint of a publication or guarantee its technical correctness. LA-13054-MS UC-700 Issued: January 1996 Measurement and Accounting of the Minor Actinides Produced in Nuclear Power Reactors J. -
Revisiting the Thorium-Uranium Nuclear Fuel Cycle
s e r u t Revisiting the a e f thorium-uranium nuclear fuel cycle [DOI: 10.1051/EPN:2007007 ] Sylvain David a, Elisabeth Huffer b and Hervé Nifenecker b, Energy Panel of the French Physics Society a Institut de Physique Nucléaire d’Orsay • France b Laboratoire de Physique Subatomique et de Cosmologie (IN2P3, Grenoble) • France thorium-uranium nuclear fuel cycle, in which the main amounts of uranium 233 available remained tiny, insufficient to HE fissile nucleus is uranium 233 and fuel regeneration is allow the rapid development of a thorium-uranium concept. ensured through neutron capture on thorium 232 offers many It appears today that the growth rate of nuclear power Tpotential advantages as compared to the better known urani - worldwide does not require the fast development of breeder re - um-plutonium fuel cycle. These include, in particular, reduced actor concepts. It is then possible, as we show in this paper, to high activity long lived waste production and less likelihood of constitute a stockpile of uranium 233 that could allow the nuclear proliferation. A brief description of the nuclear reactors development of a fleet of thorium-uranium reactors. We show being considered for this fuel cycle is given. We show also that a also that such a concept has many major advantages, in partic - strategy can be put together to constitute the initial uranium ular concerning the disposal of radioactive waste and the risks 233 supply for such reactors, using today’s pressurized water of nuclear proliferation. We give a brief description of the types reactors and a thorium and plutonium mixed oxide fuel. -
The Elements.Pdf
A Periodic Table of the Elements at Los Alamos National Laboratory Los Alamos National Laboratory's Chemistry Division Presents Periodic Table of the Elements A Resource for Elementary, Middle School, and High School Students Click an element for more information: Group** Period 1 18 IA VIIIA 1A 8A 1 2 13 14 15 16 17 2 1 H IIA IIIA IVA VA VIAVIIA He 1.008 2A 3A 4A 5A 6A 7A 4.003 3 4 5 6 7 8 9 10 2 Li Be B C N O F Ne 6.941 9.012 10.81 12.01 14.01 16.00 19.00 20.18 11 12 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 3 Na Mg IIIB IVB VB VIB VIIB ------- VIII IB IIB Al Si P S Cl Ar 22.99 24.31 3B 4B 5B 6B 7B ------- 1B 2B 26.98 28.09 30.97 32.07 35.45 39.95 ------- 8 ------- 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 4 K Ca Sc Ti V Cr Mn Fe Co Ni Cu Zn Ga Ge As Se Br Kr 39.10 40.08 44.96 47.88 50.94 52.00 54.94 55.85 58.47 58.69 63.55 65.39 69.72 72.59 74.92 78.96 79.90 83.80 37 38 39 40 41 42 43 44 45 46 47 48 49 50 51 52 53 54 5 Rb Sr Y Zr NbMo Tc Ru Rh PdAgCd In Sn Sb Te I Xe 85.47 87.62 88.91 91.22 92.91 95.94 (98) 101.1 102.9 106.4 107.9 112.4 114.8 118.7 121.8 127.6 126.9 131.3 55 56 57 72 73 74 75 76 77 78 79 80 81 82 83 84 85 86 6 Cs Ba La* Hf Ta W Re Os Ir Pt AuHg Tl Pb Bi Po At Rn 132.9 137.3 138.9 178.5 180.9 183.9 186.2 190.2 190.2 195.1 197.0 200.5 204.4 207.2 209.0 (210) (210) (222) 87 88 89 104 105 106 107 108 109 110 111 112 114 116 118 7 Fr Ra Ac~RfDb Sg Bh Hs Mt --- --- --- --- --- --- (223) (226) (227) (257) (260) (263) (262) (265) (266) () () () () () () http://pearl1.lanl.gov/periodic/ (1 of 3) [5/17/2001 4:06:20 PM] A Periodic Table of the Elements at Los Alamos National Laboratory 58 59 60 61 62 63 64 65 66 67 68 69 70 71 Lanthanide Series* Ce Pr NdPmSm Eu Gd TbDyHo Er TmYbLu 140.1 140.9 144.2 (147) 150.4 152.0 157.3 158.9 162.5 164.9 167.3 168.9 173.0 175.0 90 91 92 93 94 95 96 97 98 99 100 101 102 103 Actinide Series~ Th Pa U Np Pu AmCmBk Cf Es FmMdNo Lr 232.0 (231) (238) (237) (242) (243) (247) (247) (249) (254) (253) (256) (254) (257) ** Groups are noted by 3 notation conventions. -
Compounds of the Metals Beryllium, Magnesium
C01F COMPOUNDS OF THE METALS BERYLLIUM, MAGNESIUM, ALUMINIUM, CALCIUM, STRONTIUM, BARIUM, RADIUM, THORIUM, OR OF THE RARE-EARTH METALS (metal hydrides [N: monoborane, diborane or addition complexes thereof] C01B6/00; salts of oxyacids of halogens C01B11/00; peroxides, salts of peroxyacids C01B15/00; sulfides or polysulfides of magnesium, calcium, strontium, or barium C01B17/42; thiosulfates, dithionites, polythionates C01B17/64; compounds containing selenium or tellurium C01B19/00; binary compounds of nitrogen with metals C01B21/06; azides C01B21/08; [N: compounds other than ammonia or cyanogen containing nitrogen and non-metals and optionally metals C01B21/082; amides or imides of silicon C01B21/087]; metal [N: imides or] amides C01B21/092, [N: C01B21/0923]; nitrites C01B21/50; [N: compounds of noble gases C01B23/0005]; phosphides C01B25/08; salts of oxyacids of phosphorus C01B25/16; carbides C01B31/30; compounds containing silicon C01B33/00; compounds containing boron C01B35/00; compounds having molecular sieve properties but not having base-exchange properties C01B37/00; compounds having molecular sieve and base-exchange properties, e.g. crystalline zeolites, C01B39/00;cyanides C01C3/08; salts of cyanic acid C01C3/14; salts of cyanamide C01C3/16; thiocyanates C01C3/20; [N: double sulfates of magnesium with sodium or potassium C01D5/12; with other alkali metals C01D15/00, C01D17/00]) Definition statement This subclass/group covers: All compounds of Be,Mg,Al,Ca,Sr,Ba,Ra,Th or rare earth metals except those compounds which are classified in C01G because of application of the last appropriate place rule. So, in principle does this subclass comprise all Al-compounds with elements as such being part of C01B-C01D, e.g.