Background and Derivation of ANS-5.4 Standard Fission Product Release Model
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1 11. Nuclear Chemistry 11.1 Stable and Unstable Nuclides Very Large
11. Nuclear Chemistry Chemical reactions occur as a result of loosing/gaining and sharing electrons in the valance shell which is far away from the atomic nucleus as we described in previous chapters in chemical bonding. In chemical reactions identity of the elements (atomic) and the makeup of the nuclei (mass due to protons and neutrons) is preserved which is reflected in the Law of Conservation of mass. This idea of atomic nucleus is always stable was shattered as Henri Becquerel discovered radioactivity in uranium compound where uranium nuclei changes or undergo nuclear reactions where nuclei of an element is transformed into nuclei of different element(s) while emitting ionization radiation. Marie Curie also began a study of radioactivity in a different form of uranium ore called pitchblende and she discovered the existence of two more highly radioactive new elements radium and polonium formed as the products during the decay of unstable nuclide of uranium-235. Curie measure that the radiation emanated was proportional to the amount (moles or number of nuclides) of radioactive element present, and she proposed that radiation was a property nucleus of an unstable atom. The area of chemistry that focuses on the nuclear changes is called nuclear chemistry. What changes in a nuclide result from the loss of each of the following? a) An alpha particle. b) A gamma ray. c) An electron. d) A neutron. e) A proton. Answer: a), c), d), e) 11.1 Stable and Unstable Nuclides There are stable and unstable radioactive nuclides. Unstable nuclides emit subatomic particles, with alpha −α, beta −β, gamma −γ, proton-p, neutrons-n being the most common. -
Spallation, Fission, and Neutron Capture Anomalies in Meteoritic Krypton and Xenon
mitte etwas bei. Man wird also erwarten, daß die des Verfahrens wurde für den Bogen (a) überprüft. Flügel der aus Achsennähe emittierten Linien durch Dazu wurde das gemessene Temperatur- und Elek- die Randzonen unbeeinflußt bleiben. tronendichteprofil des Bogens durch je ein Treppen- Wendet man an Stelle der Halbwertsbreite eine profil mit fünf Stufen ersetzt. Für jede Stufe wurde 7 Vergleichsgröße an, die mehr im Linienflügel liegt nach die Kontur der Hv-Linie berechnet. Aus der Überlagerung der Strahlung der verschiedenen Zo- — z. B. den Wellenlängenabstand (Z — H) zwischen nen erhält man die entsprechenden „side-on"-Profile den beiden Punkten, zwischen welchen die Intensität der Linie. Ein Vergleich mit den Ausgangsprofilen von 1/2 auf 1/10 der Maximalintensität abgenom- zeigte, daß die unter Verwendung von (Z — H) be- men hat —, so kann man erwarten, daß die Elek- stimmte Elektronendichte in der Bogenmitte um etwa tronendichte unter der gemachten Voraussetzung auch 20% zu klein ist. (Der aus der Halb wertsbreite er- ohne AßEL-Inversion in guter Näherung gefunden haltene Wert dagegen hätte einen Fehler von 40%.) werden kann. Dies wirkt sich bei der Temperaturbestimmung nach Die in Abb. 3 dargestellten Elektronendichteprofile Verfahren b) so aus, daß die Temperaturwerte in wurden auf die beschriebene Weise mit Hilfe der der Bogenachse zu klein ausfallen; am Rande da- Vergleichsgröße (Z — H) ermittelt. Die Genauigkeit gegen ist die Methode genau. Spallation, Fission, and Neutron Capture Anomalies in Meteoritic Krypton and Xenon K. MARTI *, P. EBERHARDT, and J. GEISS Physikalisches Institut, University of Berne, Switzerland (Z. Naturforschg. 21 a, 398—113 [1966]; received 19 November 1965) Measurements of the Kr and Xe concentrations and isotopic compositions in five meteorites are reported. -
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). -
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. -
Stable Isotopes of Krypton Available from ISOFLEX Properties of Krypton
Stable isotopes of krypton available from ISOFLEX Natural Chemical Isotope Z(p) N(n) Atomic Mass Enrichment Level Abundance Form Kr-78 36 42 77.92039 0.35% 99.90% Gas Kr-80 36 44 79.916379 2.25% 99.90% Gas Kr-82 36 46 81.913485 11.60% 99.90% Gas Kr-83 36 47 82.914137 11.50% 99.90% Gas Kr-84 36 48 83.911508 57.00% 99.90% Gas Kr-86 36 50 85.910615 17.30% 99.90% Gas Krypton was discovered in 1898 by Sir William Ramsay and Morris W. Travers. Its name originates with the Greek word kryptos, meaning “hidden.” Krypton is a colorless, odorless, tasteless gas. It liquefies at -153.22 ºC and solidifies at 157.36 ºC to a white crystalline substance with a face-centered cubic structure. It is slightly soluble in water. Krypton is an inert gas element. Its closed-shell, stable octet electron configuration allows zero reactivity with practically any substance. Only a few types of compounds, complexes and clathrates have been synthesized, mostly with fluorine, the most electronegative element. The commercial applications of krypton are fewer than those of helium or argon. Its principal use is in fluorescent lights. It is mixed with argon as a filling gas to enhance brightness in fluorescent tubes. Other applications are in flash tubes for high-speed photography and incandescent bulbs. Radioactive Krypton-85 is used as a tracer to monitor surface reactions. The unit of length “meter” was once defined in terms of the orange-red spectral line of Krypton-86. -
Tritium, Carbon-14 and Krypton-85
Tritium, carbon-14 and krypton-85 Jan Willem Storm van Leeuwen Independent consultant member of the Nuclear Consulting Group August 2019 [email protected] Note In this document the references are coded by Q-numbers (e.g. Q6). Each reference has a unique number in this coding system, which is consistently used throughout all publications by the author. In the list at the back of the document the references are sorted by Q-number. The resulting sequence is not necessarily the same order in which the references appear in the text. m42H3C14Kr85-20190828 1 Contents 1 Introduction 2 Tritium 3H Hydrogen isotopes Anthropogenic tritium production Chemical properties DNA incorporation Health hazards Removal and disposal of tritium 3 Carbon-14 Carbon isotopes Anthropogenic carbon-14 production Chemical properties DNA incorporation Suess effect Health hazards Removal and disposal of carbon-14 4 Krypton-85 Anthropogenic kry[ton-85 production Chemical properties Biological properties Health hazards Removal and disposal of krypton-85 References TABLES Table 1 Neutron reactions producing tritium and precursors Table 2 Calculated production and discharge rates of tritium Table 3 Neutron reactions producing carbon-14 and precursors Table 4 Calculated production and discharge rates of carbon-14 Table 5 Calculated production and discharge rates of krypton-85 FIGURES Figure 1 Pathways of tritium and carbon-14 into human metabolism m42H3C14Kr85-20190828 2 1 Introduction The three radionuclides tritium (3H), carbon-14 (14C) and krypton-85 (85Kr) are routinely released into the human environment by nominally operating nuclear power plants. According to the classical dose-risk paradigm these discharges would have negligible public health effects and so were and still are permitted. -
Separation, Storage and Disposal of Krypton-85
TECHNICAL REPORTSSERIES No. 199 Separation, Storage and Disposal of Krypton-85 Iw'j^ , ^' - INTERNATIONAL ATOMIC ENERGY AGENCY, VIENNA, 1980 SEPARATION, STORAGE AND DISPOSAL OF KRYPTON-85 The following States are Members of the International Atomic Energy Agency: AFGHANISTAN HOLY SEE PHILIPPINES ALBANIA HUNGARY POLAND ALGERIA ICELAND PORTUGAL ARGENTINA INDIA QATAR AUSTRALIA INDONESIA ROMANIA AUSTRIA IRAN SAUDI ARABIA BANGLADESH IRAQ SENEGAL BELGIUM IRELAND SIERRA LEONE BOLIVIA ISRAEL SINGAPORE BRAZIL ITALY SOUTH AFRICA BULGARIA IVORY COAST SPAIN BURMA JAMAICA SRI LANKA BYELORUSSIAN SOVIET JAPAN SUDAN SOCIALIST REPUBLIC JORDAN SWEDEN CANADA KENYA SWITZERLAND CHILE KOREA, REPUBLIC OF SYRIAN ARAB REPUBLIC COLOMBIA KUWAIT THAILAND COSTA RICA LEBANON TUNISIA CUBA LIBERIA TURKEY CYPRUS LIBYAN ARAB JAMAHIRIYA UGANDA CZECHOSLOVAKIA LIECHTENSTEIN UKRAINIAN SOVIET SOCIALIST DEMOCRATIC KAMPUCHEA LUXEMBOURG REPUBLIC DEMOCRATIC PEOPLE'S MADAGASCAR UNION OF SOVIET SOCIALIST REPUBLIC OF KOREA MALAYSIA REPUBLICS DENMARK MALI UNITED ARAB EMIRATES DOMINICAN REPUBLIC MAURITIUS UNITED KINGDOM OF GREAT ECUADOR MEXICO BRITAIN AND NORTHERN EGYPT MONACO IRELAND EL SALVADOR MONGOLIA UNITED REPUBLIC OF ETHIOPIA MOROCCO CAMEROON FINLAND NETHERLANDS UNITED REPUBLIC OF FRANCE NEW ZEALAND TANZANIA GABON NICARAGUA UNITED STATES OF AMERICA GERMAN DEMOCRATIC REPUBLIC NIGER URUGUAY GERMANY, FEDERAL REPUBLIC OF NIGERIA VENEZUELA GHANA NORWAY VIET NAM GREECE PAKISTAN YUGOSLAVIA GUATEMALA PANAMA ZAIRE HAITI PARAGUAY ZAMBIA PERU The Agency's Statute was approved on 23 October 1956 by the Conference on the Statute of the IAEA held at United Nations Headquarters, New York; it entered into force on 29 July 1957. The Headquarters of the Agency are situated in Vienna. Its principal objective is "to accelerate and enlarge the contribution of atomic energy to peace, health and prosperity throughout the world". -
The Delimiting/Frontier Lines of the Constituents of Matter∗
The delimiting/frontier lines of the constituents of matter∗ Diógenes Galetti1 and Salomon S. Mizrahi2 1Instituto de Física Teórica, Universidade Estadual Paulista (UNESP), São Paulo, SP, Brasily 2Departamento de Física, CCET, Universidade Federal de São Carlos, São Carlos, SP, Brasilz (Dated: October 23, 2019) Abstract Looking at the chart of nuclides displayed at the URL of the International Atomic Energy Agency (IAEA) [1] – that contains all the known nuclides, the natural and those produced artificially in labs – one verifies the existence of two, not quite regular, delimiting lines between which dwell all the nuclides constituting matter. These lines are established by the highly unstable radionuclides located the most far away from those in the central locus, the valley of stability. Here, making use of the “old” semi-empirical mass formula for stable nuclides together with the energy-time uncertainty relation of quantum mechanics, by a simple calculation we show that the obtained frontier lines, for proton and neutron excesses, present an appreciable agreement with the delimiting lines. For the sake of presenting a somewhat comprehensive panorama of the matter in our Universe and their relation with the frontier lines, we narrate, in brief, what is currently known about the astrophysical nucleogenesis processes. Keywords: chart of nuclides, nucleogenesis, nuclide mass formula, valley/line of stability, energy-time un- certainty relation, nuclide delimiting/frontier lines, drip lines arXiv:1909.07223v2 [nucl-th] 22 Oct 2019 ∗ This manuscript is based on an article that was published in Brazilian portuguese language in the journal Revista Brasileira de Ensino de Física, 2018, 41, e20180160. http://dx.doi.org/10.1590/ 1806-9126-rbef-2018-0160. -
Mass Fraction and the Isotopic Anomalies of Xenon and Krypton in Ordinary Chondrites
Scholars' Mine Masters Theses Student Theses and Dissertations 1971 Mass fraction and the isotopic anomalies of xenon and krypton in ordinary chondrites Edward W. Hennecke Follow this and additional works at: https://scholarsmine.mst.edu/masters_theses Part of the Chemistry Commons Department: Recommended Citation Hennecke, Edward W., "Mass fraction and the isotopic anomalies of xenon and krypton in ordinary chondrites" (1971). Masters Theses. 5453. https://scholarsmine.mst.edu/masters_theses/5453 This thesis is brought to you by Scholars' Mine, a service of the Missouri S&T Library and Learning Resources. This work is protected by U. S. Copyright Law. Unauthorized use including reproduction for redistribution requires the permission of the copyright holder. For more information, please contact [email protected]. MASS FRACTIONATION AND THE ISOTOPIC ANOMALIES OF XENON AND KRYPTON IN ORDINARY CHONDRITES BY EDWARD WILLIAM HENNECKE, 1945- A THESIS Presented to the Faculty of the Graduate School of the UNIVERSITY OF MISSOURI-ROLLA In Partial Fulfillment of the Requirements for the Degree MASTER OF SCIENCE IN CHEMISTRY 1971 T2572 51 pages by Approved ~ (!.{ 1.94250 ii ABSTRACT The abundance and isotopic composition of all noble gases are reported in the Wellman chondrite, and the abundance and isotopic composition of xenon and krypton are reported in the gases released by stepwise heating of the Tell and Scurry chondrites. Major changes in the isotopic composition of xenon result from the presence of radio genic Xel29 and from isotopic mass fractionation. The isotopic com position of trapped krypton in the different temperature fractions of the Tell and Scurry chondrites also shows the effect of isotopic fractiona tion, and there is a covariance in the isotopic composition of xenon with krypton in the manner expected from mass dependent fractiona tion. -
Setting a Limit on Anthropogenic Sources of Atmospheric 81Kr Through Atom Trap Trace Analysis
Setting a Limit on Anthropogenic Sources of Atmospheric 81Kr through Atom Trap Trace Analysis J. C. Zappalaa,b, K. Baileya, W. Jiangc, B. Micklicha, P. Muellera, T. P. O'Connora, R. Purtschertd aPhysics Division, Argonne National Laboratory, Argonne, Illinois 60439, USA bDepartment of Physics and Enrico Fermi Institute, University of Chicago, Chicago, Illinois 60637, USA cSchool of Nuclear Science and Engineering, University of Science and Technology of China, Hefei, China dClimate and Environmental Physics Division, Physics Institute, University of Bern, CH-3012 Bern, Switzerland Abstract We place a 2.5% limit on the anthropogenic contribution to the modern abundance of 81Kr/Kr in the atmosphere at the 90% confidence level. Due to its simple production and transport in the terrestrial environment, 81Kr (half- life = 230,000 yr) is an ideal tracer for old water and ice with mean residence times in the range of 105-106 years. In recent years, 81Kr-dating has been made available to the earth science community thanks to the development of Atom Trap Trace Analysis (ATTA), a laser-based atom counting technique. Further upgrades and improvements to the ATTA technique now allow us to demonstrate 81Kr/Kr measurements with relative uncertainties of 1% and place this new limit on anthropogenic 81Kr. As a result of this limit, we have 81 arXiv:1702.01652v1 [physics.atom-ph] 6 Feb 2017 removed a potential systematic constraint for Kr-dating. keywords: 81Kr; groundwater dating; anthropogenic effects; radioiso- tope tracers; noble gas tracers; atom trap trace analysis Preprint submitted to Chemical Geology February 7, 2017 1. Introduction Since the discovery of 81Kr in the atmosphere (Loosli and Oeschger, 1969), the geoscience community has sought to apply this noble gas isotope as an environmental tracer. -
HWR-667, "The Treatment of Radioactive Fission Gas Release
N HWR-667 OECD HALDEN REACTOR PROJECT THE TREATMENT OF RADIOACTIVE FISSION GAS RELEASE MEASUREMENTS AND PROVISION OF DATA FOR DEVELOPMENT AND VALIDATION OF THE ANS 0.4 MODEL by J.A. Turnbull February2001 NOTICE THIS REPORT IS FOR USE BY HALDEN PROJECT PARTICIPANTS ONLY The right to utilise information originating from the research work of the Halden Project is limited to persons and undertakings specifically given the right by one of the Project member organisa- tions in accordance with the Project's rules for 'Communication of Results of Scientific Research and Information' (HP-document 1069). The content of this report should thus neither be disclosed to others nor be reproduced, wholly or partially, unless written permission to do so has been obtained from the appropriate Project member organisation. 11WR-667 FOREWORD The experimental operation of the Halden Boiling Water Reactor and associated research programmes are sponsored through an international agreement by * the Institutt for energiteknikk, Norway, * the Belgian Nuclear Research Centre SCK*CEN, acting also on behalf of other public or private organisations in Belgium, * the Ris0 National Laboratory in Denmark, * the Finnish Ministry of Trade and Industry, * the Electricit6 de France, * the Gesellschaft fur Anlagen- und Reaktorsicherheit mbH, representing a German group of companies working in agreement with the German Federal Ministry for Economics and Technology, * the Italian Ente per le Nuove Tecnologie, I'Energia e l'Ambiente, representing also a group of industry organisations -
Manual for Reactor Produced Radioisotopes
IAEA-TECDOC-1340 Manual for reactor produced radioisotopes January 2003 The originating Section of this publication in the IAEA was: Industrial Applications and Chemistry Section International Atomic Energy Agency Wagramer Strasse 5 P.O. Box 100 A-1400 Vienna, Austria MANUAL FOR REACTOR PRODUCED RADIOISOTOPES IAEA, VIENNA, 2003 IAEA-TECDOC-1340 ISBN 92–0–101103–2 ISSN 1011–4289 © IAEA, 2003 Printed by the IAEA in Austria January 2003 FOREWORD Radioisotopes find extensive applications in several fields including medicine, industry, agriculture and research. Radioisotope production to service different sectors of economic significance constitutes an important ongoing activity of many national nuclear programmes. Radioisotopes, formed by nuclear reactions on targets in a reactor or cyclotron, require further processing in almost all cases to obtain them in a form suitable for use. Specifications for final products and testing procedures for ensuring quality are also an essential part of a radioisotope production programme. The International Atomic Energy Agency (IAEA) has compiled and published such information before for the benefit of laboratories of Member States. The first compilation, entitled Manual of Radioisotope Production, was published in 1966 (Technical Reports Series No. 63). A more elaborate and comprehensive compilation, entitled Radioisotope Production and Quality Control, was published in 1971 (Technical Reports Series No. 128). Both served as useful reference sources for scientists working in radioisotope production worldwide.