Toxicological Profile for Thorium
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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. -
Environmental Health Criteria 126 Partially Halogenated Chlorofluorocarbons
Environmental Health Criteria 126 Partially halogenated chlorofluorocarbons ( methane derivatives) Please note that the layout and pagination of this web version are not identical with the printed version. Chlorofluorocarbons, partially halogenated (methane derivatives) (EHC 126, 1991) INTERNATIONAL PROGRAMME ON CHEMICAL SAFETY ENVIRONMENTAL HEALTH CRITERIA 126 PARTIALLY HALOGENATED CHLOROFLUROCARBONS (METHANE DERIVATIVES) This report contains the collective views of an international group of experts and does not necessarily represent the decisions or the stated policy of the United Nations Environment Programme, the International Labour Organisation, or the World Health Organization. Published under the joint sponsorship of the United Nations Environment Programme, the International Labour Organisation, and the World Health Organization Draft prepared by Professor D. Beritic-Stahuljak and Professor F. Valic, University of Zagreb, Yugoslavia, using texts made available by Dr. D.S. Mayer, Hoechst AG, Frankfurt am Main, Germany and by Dr. I.C. Peterson and Dr. G.D. Wade, ICI Central Toxicological Laboratory, Macclesfield, United Kingdom World Health Organization Geneva, 1991 The International Programme on Chemical Safety (IPCS) is a joint venture of the United Nations Environment Programme, the International Labour Organisation, and the World Health Organization. The main objective of the IPCS is to carry out and disseminate evaluations of the effects of chemicals on human health and the quality of the environment. Supporting activities include the development of epidemiological, experimental laboratory, and risk-assessment methods that could produce internationally comparable results, and the development of manpower in the field of toxicology. Other activities carried out by the IPCS include the development of know-how for coping with chemical accidents, coordination of laboratory testing and epidemiological studies, and promotion of research on the mechanisms of the biological action of chemicals. -
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. -
Molten-Salt Reactor Chemistry
MOLTEN-SALT REACTOR CHEMISTRY W. R. GRIMES Oak Ridge National Laboratory, Oak Ridge, Tennessee 37830 KEYWORDS: fused salt fuel, chemical reactions, reactors, beryllium fluorides, zirconium fluorides, Ii th i um fluorides, Received August 4, 1969 uranium hexafluoride, repro Revised October 7, 1969 cessing, protactinium, seporo tion pro c es s es, breeding, fission products, MSRE aggressive toward some otherwise suitable ma terial of construction and toward some suitable This document summarizes the large program of chemical research and development which led moderator material. The fuel must be stable to selection of fuel and coolant compositions for toward reactor radiation, must be able to survive the Molten-Salt Reactor Experiment (MSRE) and fission of the uranium (or other fissionable ma for subsequent reactors of this type. Chemical terial} and must tolerate fission product accumu lation without serious deterioration of its useful behavior of the LiF-BeFrZrFrUF4 fuel mixture and behavior of fission products during power op properties. We must also be assured of a gen uinely low fuel-cycle cost; this presupposes a eration of MSRE are presented. A discussion of low-cost fuel associated with inexpensive turn the chemical reactions which show promise for around of the unburned fissile material, and recovery of bred 233Pa and for removal of fission effective and economical schemes for recovery of product poisons from a molten-salt breeder reac tor is included. bred fissile material and for removal of fission product poisons from the fuel. A suitable secondary coolant must be provided to link the fuel circuit with the steam-generating equipment. The demands imposed upon this cool ant fluid differ in obvious ways from those im INTRODUCTION posed upon the fuel system. -
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). -
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. -
4340 Site-Wide Characterization Report
4340 SITE-WIDE CHARACTERIZATION REPORT VOLUME 1 OF 5 PART I MARCH 1993 DOE-FN/EPA 400 REPORT 4340 SITE-WIDE CHARACTERIZATION REPORT -- - FERNALD ENVIRONMENTAL MANAGEMENT PROJECT FERNALD, OHIO REMEDIAL INVESTIGATION AND FEASIBILITY STUDY VOLUME 1 of 5 PART I MARCH 1993 U.S. DEPARTMENT OF ENERGY FERNALD FIELD OFFICE FINAL 01 4340 SITE-WIDE CHARACTERIZATION REPORT FERNALD ENVIRONMENTAL MANAGEMENT PROJECT FERNALD, OHIO REMXiIIAL INVESTIGATION AND FEASIBILITY STUDY VOLUME 1 of 5 PART I MARCH 1993 U.S. L;’:WARTMENTOF ENERGY FER NALD FIELD OFFICL FINAL 02 4340 NOTE TO READERS OF SWCR This final Site Wide Characterization Report is the product of several cycles of reviews and revisions, particularly concerning the methodologies used in the calculations of risks for the Preliminary Baseline Risk Assessment (PBRA) for the FEMP. The PBRA characterizes the current and potential threats to human health and the environment that may be posed by contaminants at the entire site. Many statistical and calculational methods, models, guidance documents, exposure scenarios, and pathways are utilized in deriving components of the site-wide risk. The PBRA was prepared in accordance with the Amended Consent Agreement . following the methodologies presented in the Risk Assessment Work Plan Addendum; however, differences in interpretation and application of the methodologies have resulted in departure from current EPA Region V guidance in some areas. The Site Wide Characterization Report fulfills the objective of providing a site-wide assessment of potential human health and environmental risks. As a result of discussions with, and additional guidance from EPA, the Operable Unit-specific Base1 ine Risk Assessments accompanying the Remedial Investigation reports for each OU will be prepared in accordance with the latest DOE/EPA agreements on risk assessment methodology. -
Radiological Significance of Thorium Processing in Manufacturing
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