Perspectives on the Thorium Fuel Cycle
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Measurements of Fission Cross Sections for the Isotopes Relevant to the Thorium Fuel Cycle
EUROPEAN ORGANIZATION FOR NUCLEAR RESEARCH CERN/INTC 2001-025 INTC/P-145 08 Aug 2001 Measurements of Fission Cross Sections for the Isotopes relevant to the Thorium Fuel Cycle The n_TOF Collaboration ABBONDANNO U.20, ANDRIAMONJE S.10, ANDRZEJEWSKI J.24, ANGELOPOULOS A.12, ASSIMAKOPOULOS P.15, BACRI C-O.8, BADUREK G.1, BAUMANN P.9, BEER H.11, BENLLIURE J.32, BERTHIER B.8, BONDARENKO I.26, BOS A.J.J.36, BUSTREO N.19, CALVINO F.33, CANO-OTT D.28, CAPOTE R.31, CARLSON P.34, CHARPAK G.5, CHAUVIN N.8, CENNINI P.5, CHEPEL V.25, COLONNA N.20, CORTES G.33, CORTINA D.32, CORVI F.23, DAMIANOGLOU D.16, DAVID S.8, DIMOVASILI E.12, DOMINGO C.29, DOROSHENKO A.27, DURAN ESCRIBANO I.32, ELEFTHERIADIS C.16, EMBID M.28, FERRANT L.8, FERRARI A.5, FERREIRA–MARQUES R.25, FRAIS–KOELBL H.3, FURMAN W.26, FURSOV B.27, GARZON J.A.32, GIOMATARIS I.10, GLEDENOV Y.26, GONZALEZ–ROMERO E.28, GOVERDOVSKI A.27, GRAMEGNA F.19, GRIESMAYER E.3, GUNSING F.10, HAIGHT R.37, HEIL M.11, HOLLANDER P.36, IOANNIDES K.G.15, IOANNOU P.12, ISAEV S.27, JERICHA E.1, KADI Y.5, KAEPPELER F.11, KARADIMOS D.17, KARAMANIS D.15, KAYUKOV A.26, KAZAKOV L.27, KELIC A.9, KETLEROV V.27, KITIS G.16, KOEHLER P.E.38., KOPACH Y.26, KOSSIONIDES E.14, KROSHKINA I.27, LACOSTE V.5, LAMBOUDIS C.16, LEEB H.1, LEPRETRE A.10, LOPES M.25, LOZANO M.31, MARRONE S.20, MARTINEZ-VAL J. -
THE NATURAL RADIOACTIVITY of the BIOSPHERE (Prirodnaya Radioaktivnost' Iosfery)
XA04N2887 INIS-XA-N--259 L.A. Pertsov TRANSLATED FROM RUSSIAN Published for the U.S. Atomic Energy Commission and the National Science Foundation, Washington, D.C. by the Israel Program for Scientific Translations L. A. PERTSOV THE NATURAL RADIOACTIVITY OF THE BIOSPHERE (Prirodnaya Radioaktivnost' iosfery) Atomizdat NMoskva 1964 Translated from Russian Israel Program for Scientific Translations Jerusalem 1967 18 02 AEC-tr- 6714 Published Pursuant to an Agreement with THE U. S. ATOMIC ENERGY COMMISSION and THE NATIONAL SCIENCE FOUNDATION, WASHINGTON, D. C. Copyright (D 1967 Israel Program for scientific Translations Ltd. IPST Cat. No. 1802 Translated and Edited by IPST Staff Printed in Jerusalem by S. Monison Available from the U.S. DEPARTMENT OF COMMERCE Clearinghouse for Federal Scientific and Technical Information Springfield, Va. 22151 VI/ Table of Contents Introduction .1..................... Bibliography ...................................... 5 Chapter 1. GENESIS OF THE NATURAL RADIOACTIVITY OF THE BIOSPHERE ......................... 6 § Some historical problems...................... 6 § 2. Formation of natural radioactive isotopes of the earth ..... 7 §3. Radioactive isotope creation by cosmic radiation. ....... 11 §4. Distribution of radioactive isotopes in the earth ........ 12 § 5. The spread of radioactive isotopes over the earth's surface. ................................. 16 § 6. The cycle of natural radioactive isotopes in the biosphere. ................................ 18 Bibliography ................ .................. 22 Chapter 2. PHYSICAL AND BIOCHEMICAL PROPERTIES OF NATURAL RADIOACTIVE ISOTOPES. ........... 24 § 1. The contribution of individual radioactive isotopes to the total radioactivity of the biosphere. ............... 24 § 2. Properties of radioactive isotopes not belonging to radio- active families . ............ I............ 27 § 3. Properties of radioactive isotopes of the radioactive families. ................................ 38 § 4. Properties of radioactive isotopes of rare-earth elements . -
A Note on Radioactive Materials and Their Measurements Elements Are
A NOTE ON RADIOACTIVE MATERIALS AND THEIR MEASUREMENTS Elements are placed in the periodic table of elements according to atomic number or proton number often referred to as Z. Their atomic weights are also usually indicated and can be fractional if the element in nature contains more than one isotope. Isotopes of an element all have the same atomic number, Z, but have different numbers of neu- trons. Some of these isotopes, even in naturally occurring elements, may be radioactive, and are usually given the atomic weight of the longest known isotope. Radioactive decay occurs when an unstable atom loses energy by emitting particles and gamma radiation or by spontaneously fission- ing. (Spontaneous fission is one of the natural modes of radioactive decay in which fission occurs without the addition of external energy or particles.) The activity of a radioactive sample is simply the rate of radioactive decay, expressed as the number of decays per unit time. Traditionally, the curie (Ci) was used to quantify the decay rate and was defined as the radioactivity measured for one gram of pure radium, or ~3.7 × 1010 decays per second (d/s), but the value changed as measurement techniques improved. To avoid this problem of a “chang- ing” constant, the Curie is now defined as exactly 3.7 × 1010 d/s. The becquerel (Bq), equal to one d/s, is the official SI unit (International System of Units). The roentgen R( ) is commonly used as a unit of radiation exposure to X-ray or gamma radiation, and can be roughly defined as “that quan- tity of X-ray or gamma radiation needed to produce one electrostatic unit of ionic charge in one cm3 of air under standard temperature and pressure (STP) “normal conditions”. -
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. -
12 Natural Isotopes of Elements Other Than H, C, O
12 NATURAL ISOTOPES OF ELEMENTS OTHER THAN H, C, O In this chapter we are dealing with the less common applications of natural isotopes. Our discussions will be restricted to their origin and isotopic abundances and the main characteristics. Only brief indications are given about possible applications. More details are presented in the other volumes of this series. A few isotopes are mentioned only briefly, as they are of little relevance to water studies. Based on their half-life, the isotopes concerned can be subdivided: 1) stable isotopes of some elements (He, Li, B, N, S, Cl), of which the abundance variations point to certain geochemical and hydrogeological processes, and which can be applied as tracers in the hydrological systems, 2) radioactive isotopes with half-lives exceeding the age of the universe (232Th, 235U, 238U), 3) radioactive isotopes with shorter half-lives, mainly daughter nuclides of the previous catagory of isotopes, 4) radioactive isotopes with shorter half-lives that are of cosmogenic origin, i.e. that are being produced in the atmosphere by interactions of cosmic radiation particles with atmospheric molecules (7Be, 10Be, 26Al, 32Si, 36Cl, 36Ar, 39Ar, 81Kr, 85Kr, 129I) (Lal and Peters, 1967). The isotopes can also be distinguished by their chemical characteristics: 1) the isotopes of noble gases (He, Ar, Kr) play an important role, because of their solubility in water and because of their chemically inert and thus conservative character. Table 12.1 gives the solubility values in water (data from Benson and Krause, 1976); the table also contains the atmospheric concentrations (Andrews, 1992: error in his Eq.4, where Ti/(T1) should read (Ti/T)1); 2) another category consists of the isotopes of elements that are only slightly soluble and have very low concentrations in water under moderate conditions (Be, Al). -
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. -
A Global Scavenging and Circulation Ocean Model of Thorium-230 and Protactinium-231 with Improved Particle Dynamics (NEMO–Prothorp 0.1)
Geosci. Model Dev., 11, 3537–3556, 2018 https://doi.org/10.5194/gmd-11-3537-2018 © Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License. A global scavenging and circulation ocean model of thorium-230 and protactinium-231 with improved particle dynamics (NEMO–ProThorP 0.1) Marco van Hulten1,2, Jean-Claude Dutay1, and Matthieu Roy-Barman1 1Laboratoire des Sciences du Climat et de l’Environnement, IPSL, CEA–Orme des Merisiers, 91191 Gif-sur-Yvette, France 2Geophysical Institute, University of Bergen, Bergen, Norway Correspondence: Marco van Hulten ([email protected]) Received: 1 November 2017 – Discussion started: 8 December 2017 Revised: 16 August 2018 – Accepted: 20 August 2018 – Published: 31 August 2018 Abstract. In this paper we set forth a 3-D ocean model of the can be done based on our model as its source code is readily radioactive trace isotopes 230Th and 231Pa. The interest arises available. from the fact that these isotopes are extensively used for in- vestigating particle transport in the ocean and reconstructing past ocean circulation. The tracers are reversibly scavenged 1 Introduction by biogenic and lithogenic particles. Our simulations of 230Th and 231Pa are based on the Oceanic circulation and the carbon cycle play a major role NEMO–PISCES ocean biogeochemistry general circulation in the regulation of the past and present climate. Heat and model, which includes biogenic particles, namely small and carbon dioxide in the atmosphere tend to equilibrate with the big particulate organic carbon, calcium carbonate and bio- ocean surface and are transported down into the deep ocean genic silica. -
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. -
Periodic Table of Elements
The origin of the elements – Dr. Ille C. Gebeshuber, www.ille.com – Vienna, March 2007 The origin of the elements Univ.-Ass. Dipl.-Ing. Dr. techn. Ille C. Gebeshuber Institut für Allgemeine Physik Technische Universität Wien Wiedner Hauptstrasse 8-10/134 1040 Wien Tel. +43 1 58801 13436 FAX: +43 1 58801 13499 Internet: http://www.ille.com/ © 2007 © Photographs of the elements: Mag. Jürgen Bauer, http://www.smart-elements.com 1 The origin of the elements – Dr. Ille C. Gebeshuber, www.ille.com – Vienna, March 2007 I. The Periodic table............................................................................................................... 5 Arrangement........................................................................................................................... 5 Periodicity of chemical properties.......................................................................................... 6 Groups and periods............................................................................................................. 6 Periodic trends of groups.................................................................................................... 6 Periodic trends of periods................................................................................................... 7 Examples ................................................................................................................................ 7 Noble gases ....................................................................................................................... -
Use of Thorium in Thermal-Neutron Reactors: Different Types of Fuel Compositions in Vver-1000 Reactor Cell
Jr. of Industrial Pollution Control 32(2)(2016) pp 459-462 www.icontrolpollution.com Research USE OF THORIUM IN THERMAL-NEUTRON REACTORS: DIFFERENT TYPES OF FUEL COMPOSITIONS IN VVER-1000 REACTOR CELL A. NAYMUSHIN *, YU. CHERTKOV, I. LEBEDEV, M. ANIKIN AND S. SAVANYUK National Research Tomsk Polytechnic University (TPU), 634050, Tomsk, Russian Federation (Received 6 July, 2016; accepted 20 August, 2016) Key words: Thorium, Thermal-neutron reactors, VVER-type reactor, Fuel composition, Nuclear fuel cycle ABSTRACT This work is dedicated to exploring possibilities of using alternative thorium-based fuel compositions in VVER-type reactor. The article describes comparison between standard uranium dioxide fuel and perspective fuel composition: thorium dioxide, mixed thorium and plutonium dioxides. The calculation result show that using of perspective fuel composition caused to improving of physical and economical characteristics of reactor core. Furthermore, investigated fuel provide effective burnup, that increase fuel cycle length. Moreover, growth of using fertile isotopes is shown in comparison with standard fuel. INTRODUCTION Thorium dioxide has greater chemical and radiation resistance compared with uranium dioxide, as The explored resources of thorium in the earth crust well as better thermal-physical properties (thermal are several times higher than the reserves of uranium conductivity, linear expansion coefficient). and this significantly increases nuclear energy’s resource base in case of implementing closed nuclear Secondary nuclear fuel in thermal-neutron reactors fuel cycle. is two isotopes of plutonium: Pu-239 and Pu-241. The former is generated as a result of absorption of 30 isotopes of thorium are known as well as 3 excited thermal and resonance neutrons by U-238 nuclei, metastable states of its nuclides.