Radiological and Chemical Fact Sheets to Support Health Risk Analyses for Contaminated Areas
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Thallium-201 for Medical Use. I
THALLIUM-201 FOR MEDICAL USE. I E. Lebowitz, M. W. Greene, R. Fairchild, P. R. Bradley-Moore, H. 1. Atkins,A. N. Ansari, P. Richards,and E. Belgrave Brookhaven National Laboratory Thallium-201 merits evaluation for myocar tumors (7—9), the use of radiothallium should also dial visualization, kidney studies, and tumor be evaluated for this application. diagnosis because of its physical and biologic Thallium-201 decays by electron capture with a properties. A method is described for prepara 73-hr half-life. It emits mercury K-x-rays of 69—83 tion of this radiopharmaceutical for human use. keY in 98% abundance plus gamma rays of I 35 and A critical evaluation of 501T1 and other radio 167 keV in 10% total abundance. Because of its pharmaceuticals for myocardial visualization is good shelf-life, photon energies, and mode of decay, given. 201T1was the radioisotope of thallium chosen for development. Thallium-20 1 is a potentially useful radioisotope MATERIALS AND METHODS for various medical applications including myocardial Thallium-201 is produced by irradiating a natural visualization and possible assessment of physiology, thallium target in the external beam of the 60-in. as a renal medullary imaging agent, and for tumor Brookhaven cyclotron with 3 1-MeV protons. The detection. nuclear reaction is 203Tl(p,3n)201Pb. Lead-201 has The use of radiothallium in nuclear medicine was a half-life of 9.4 hr and is the parent of 201T1.The first suggested by Kawana, et al (1 ) . In terms of thallium target, fabricated from an ingot of 99.999% organ distribution (2) and neurophysiologic function pure natural thallium metal (29.5% isotopic abun (3), thallium is biologically similar to potassium. -
Radium What Is It? Radium Is a Radioactive Element That Occurs Naturally in Very Low Concentrations Symbol: Ra (About One Part Per Trillion) in the Earth’S Crust
Human Health Fact Sheet ANL, October 2001 Radium What Is It? Radium is a radioactive element that occurs naturally in very low concentrations Symbol: Ra (about one part per trillion) in the earth’s crust. Radium in its pure form is a silvery-white heavy metal that oxidizes immediately upon exposure to air. Radium has a density about one- Atomic Number: 88 half that of lead and exists in nature mainly as radium-226, although several additional isotopes (protons in nucleus) are present. (Isotopes are different forms of an element that have the same number of protons in the nucleus but a different number of neutrons.) Radium was first discovered in 1898 by Marie Atomic Weight: 226 and Pierre Curie, and it served as the basis for identifying the activity of various radionuclides. (naturally occurring) One curie of activity equals the rate of radioactive decay of one gram (g) of radium-226. Of the 25 known isotopes of radium, only two – radium-226 and radium-228 – have half-lives greater than one year and are of concern for Department of Energy environmental Radioactive Properties of Key Radium Isotopes and Associated Radionuclides management sites. Natural Specific Radiation Energy (MeV) Radium-226 is a radioactive Abun- Decay Isotope Half-Life Activity decay product in the dance Mode Alpha Beta Gamma (Ci/g) uranium-238 decay series (%) (α) (β) (γ) and is the precursor of Ra-226 1,600 yr >99 1.0 α 4.8 0.0036 0.0067 radon-222. Radium-228 is a radioactive decay product Rn-222 3.8 days 160,000 α 5.5 < < in the thorium-232 decay Po-218 3.1 min 290 million α 6.0 < < series. -
Nuclear Energy in Everyday Life Nuclear Energy in Everyday Life
Nuclear Energy in Everyday Life Nuclear Energy in Everyday Life Understanding Radioactivity and Radiation in our Everyday Lives Radioactivity is part of our earth – it has existed all along. Naturally occurring radio- active materials are present in the earth’s crust, the floors and walls of our homes, schools, and offices and in the food we eat and drink. Our own bodies- muscles, bones and tissues, contain naturally occurring radioactive elements. Man has always been exposed to natural radiation arising from earth as well as from outside. Most people, upon hearing the word radioactivity, think only about some- thing harmful or even deadly; especially events such as the atomic bombs that were dropped on Hiroshima and Nagasaki in 1945, or the Chernobyl Disaster of 1986. However, upon understanding radiation, people will learn to appreciate that radia- tion has peaceful and beneficial applications to our everyday lives. What are atoms? Knowledge of atoms is essential to understanding the origins of radiation, and the impact it could have on the human body and the environment around us. All materi- als in the universe are composed of combination of basic substances called chemical elements. There are 92 different chemical elements in nature. The smallest particles, into which an element can be divided without losing its properties, are called atoms, which are unique to a particular element. An atom consists of two main parts namely a nu- cleus with a circling electron cloud. The nucleus consists of subatomic particles called protons and neutrons. Atoms vary in size from the simple hydro- gen atom, which has one proton and one electron, to large atoms such as uranium, which has 92 pro- tons, 92 electrons. -
Light Isotopes of Berkelium and Californium
Lawrence Berkeley National Laboratory Recent Work Title LIGHT ISOTOPES OF BERKELIUM AND CALIFORNIUM Permalink https://escholarship.org/uc/item/1fm7b1fp Author Chetham-Strode, Alfred Publication Date 1956-06-26 eScholarship.org Powered by the California Digital Library University of California .... I UCRL 3322 UNIVERSITY OF CALIF-ORNIA .. i/ I / LIGHT ISOTOPES OF BERKELIUM AND CALIFORNIUM •' TWO-WEEK LOAN COPY This is a Library Circulating Copy r 'which may be borrowed for two weeks. For a personal retention copy, call Tech. Info. Dioision, Ext. 5545 DISCLAIMER This document was prepared as an account of work sponsored by the United States Government. While this document is believed to contain correct information, neither the United States Government nor any agency thereof, nor the Regents of the University of · California, nor any of their employees, makes any warranty, express or implied, or assumes any legal responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed, or represents that its use would not infringe privately owned rights. Reference herein to any specific commercial product, process, or service by its trade name, trademark, manufacturer, or otherwise, does not necessarily constitute or imply its endorsement, recommendation, or favoring by the United States Government or any agency thereof, or the Regents of the University of California. The views and opinions of authors expressed herein do not necessarily state or reflect those of the United States Government or any agency thereof or the Regents of the University of California. UCRL- 3322 Chemistry Distribution UNIVERSITY OF CALIFORNIA Radiation Laboratory Berkeley, California Contract No. W-7405-eng-48 LIGHT ISOTOPES OF BERKELIUM AND CALI~ORNIUM Alfred Chetham-Strode, Jr. -
Lead Isotopes As Indicators of Environ Contamination from U Mining
._ .- - Preprint LA-UR-78-2147 , Title: LEAD ISOTOPES AS INDICATORS OF ENVIRONt1 ENTAL CONTAMINATION FRCM THE URANIUM MINING AND MILLING INDUSTRY IN THE GRANTS MINERAL BELT, NEW MEXICO Author (s): David B. Curtis and A. J. Gancarz 'k |- . 9 M/ - ' # - L .. %|.RkN: %| * & ,AQ' ,,7 ,e- d*157 ff' k g*/h T .s .. ; f*M & f g W , w -e ~ - " f:} + - pYW pm K .A ,W.% :M & Lw< *b* ? --~ k Y Q Q A -ell' 2_W h _ -- $| - f.s c t Q & Ye # C4HEhreSE33rzgmF %gh gM n [,315 ? M e % @N Y $ $ j3 h e fe l 2 D S $s - - #5 ~N [ ' & 9; - - - f _ '- ~ w e- * g r e w w 2 P As Nc- ' ** * -- - - - - $%y~ - . 9 . j'*( -, ' & . i .- f 1 * - -- ** -- e=* -h .Mr g g* ~ A _. y . gh(An ,, - ?fw h. y C: *, 1% * ~ ?, ?hSlh$i $ ': ffg w s - gp$lQ?$4$5;.>qgg - , .. INS is a Wegint of a paper intended for publication in 4 * '" M jour'ai or procet%1 ergs. Because changes rnay be made before f h , ' , publicction, this preprint is seiade available with the under. f ,- ' , starviing that it will not be died or reproduced without the * +' % '""'***'*C**' " permiss;or of the author, ') O 9 7 - _. _ _ . _ _ _ . _ - _ 0808.0 [ L * ' * . Q - 42 - 72 2)<f y . 1 LEAD ISOTOPES AS INDICATORS OF ENVIRONMENTAL CONTAMINATION FROM THE URANIUM MINING AND MILI.ING INDUSTitY .IN THE GRANIS MINERAL BELT, NEW NEXICO David B. Curtis and A. J. Gancar2 Los Alamos Scientine Laboratory Los Alamos, New Mexico, USA The unique isotopie composition oflead from uranium ores can be useful in studying ihe impact of ore processing efHuents on the env:ronment. -
22Sra 226Ra and 222Rn in ' SOUTH CAROLINA GROUND WATER
Report No. 95 WRRI 22sRa 226Ra AND 222Rn IN ' SOUTH CAROLINA GROUND WATER: MEASUR~MEN-T TECHNIQUES AND ISOTOPE RELATIONSHIPS GlANNll\li FCUN~On o;: t,GR!CUL.TU~~tcoNOMlC2' ~~J.i\2Y J\li·iU ('lJ ~C 4· 1982 WATER RESOURCES RESEARCH INSTITUTE CLEMSON UNIVERSITY Clemson, .South Carolina JANUARY 1982 Water Resources Research Institute Clemson University Clemson, South Carolina 29631 ! 228Ra, 226Ra AND 222 Rn IN SOUTH CAROLINA GROUND WATER: MEASUREMENT TECHNIQUES AND ISOTOPE RELATIONSHIPS by Jacqueline Michel, Philip T. King and Willard S. Moore Department of Geology University of South Carolina Columbia, South Carolina 29208 The work upon which this puhlication is based was supported in part by funds provided by the Office of Water Research and Technology, project !!' No. OWRT-B-127-SC, U.S. Department of the Interior, fvashington, D. C., as authorized by the Water Research and Development Act of 1978 (PL95-467). r Project agreement No. 14-34-0001-9158 Period of Investigation: October 1979 - September 1980 Clemson University Water Resources Research Institute Technical Report No. 95 Contents of this publication do not necessarily reflect the views and policies of the Office of Water Research and Technology, U.S. Department of Interior, nor does mention of trade names or cormnercial products con stitute their endorsement or recommendation for use by the U.S. Goverrtment. ACKNOWLEDGEMENTS Much appreciation goes to Lewis Shaw, Rossie Stephens, Jim Ferguson and a large number of district personnel at the South Carolina Department of Health and Environmental Control who assisted us in field collection and provided much helpful information. Dr. -
Potassium-40 What Is It? Potassium Is a Soft, Silver-White Metal
Human Health Fact Sheet ANL, October 2001 Potassium-40 What Is It? Potassium is a soft, silver-white metal. An important constituent of soil, it is widely distributed in nature and is present in all Symbol: K(-40) plant and animal tissues. Potassium-40 is a naturally occurring Atomic Number: 19 radioactive isotope of potassium. (An isotope is a different form of an (protons in nucleus) element that has the same number of protons in the nucleus but a different number of neutrons.) Two stable (nonradioactive) isotopes of Atomic Weight: 39 potassium exist, potassium-39 and potassium-41. Potassium-39 (naturally occurring) comprises most (about 93%) of naturally occurring potassium, and potassium-41 accounts for essentially all the rest. Radioactive postassium-40 comprises a very small fraction (about 0.012%) of naturally occurring potassium. Several radioactive isotopes of potassium exist in addition to potassium-40. These isotopes all have half- lives of less than one day Radioactive Properties of Potassium-40 so they are not Natural Specific Radiation Energy (MeV) Half-Life Decay of concern for Isotope Abundance Activity (yr) Mode Alpha Beta Gamma Department of (%) (Ci/g) (α) (β) (γ) Energy (DOE) K-40 1.3 billion 0.012 0.0000071 β, EC - 0.52 0.16 environmental management EC = electron capture, Ci = curie, g = gram, and MeV = million electron volts; a dash means sites such as that the entry is not applicable. (See the companion fact sheet on Radioactive Properties, Hanford. The Internal Distribution, and Risk Coefficients for explanation of terms and interpretation of radiation energies.) Potassium-40 decays by both emitting a beta particle (89%) and electron half-life of capture (11%). -
Cyclotron Produced Lead-203 P
Postgrad Med J: first published as 10.1136/pgmj.51.601.751 on 1 November 1975. Downloaded from Postgraduate Medical Journal (November 1975) 51, 751-754. Cyclotron produced lead-203 P. L. HORLOCK M. L. THAKUR L.R.I.C. M.Sc., Ph.D. I. A. WATSON M.Sc. MRC Cyclotron Unit, Hammersmith Hospital, Du Cane Road, London W12 OHS Introduction TABLE 1. Isotopes of lead Radioactive isotopes of lead occur in the natural Isotope Half-life Principal y energy radioactive series and have been used as decay 194Pb m * tracers since the early days of radiochemistry. These 195Pb 17m * are 210Pb (ti--204 y, radium D), 212Pb (t--10. 6 h, 96Pb 37 m * thorium B) and 214Pb (t--26.8 m, radium B) all of 197Pb 42 m * which are from occurring decay 197pbm 42 m * separated naturally 198pb 24 h * products ofradium or thorium. There are in addition 19spbm 25 m * Protected by copyright. to these a number of other radioactive isotopes of 199Pb 90 m * lead which can be produced artificially with the aid 19spbm 122 m * of a nuclear reactor or a accelerator 20OPb 21-5 h ** 0-109 to 0-605 (complex) charge particle (daughter radiations) (Table 1). 2Pb 9-4 h * There are at least three criteria in choosing the 0oipbm 61 s * radioactive isotope for in vitro tracer studies. First, 20pb 3 x 105y *** TI X-rays, (daughter it should emit radiation which is easily detected. radiations) have a half-life to 202pbm 3-62 h * Secondly, it should long enough aPb 52-1 h ** 0-279 (81%) 0-401 (5%) 0-680 permit studies without excessive radioactive decay 203pbm 6-1 s * (0-9%) (no daughter occurring but not so long that waste disposal radiations) creates a problem. -
Modelling Transport and Deposition of Caesium and Iodine from the Chernobyl Accident Using the DREAM Model J
Modelling transport and deposition of caesium and iodine from the Chernobyl accident using the DREAM model J. Brandt, J. H. Christensen, L. M. Frohn To cite this version: J. Brandt, J. H. Christensen, L. M. Frohn. Modelling transport and deposition of caesium and iodine from the Chernobyl accident using the DREAM model. Atmospheric Chemistry and Physics, European Geosciences Union, 2002, 2 (5), pp.397-417. hal-00295217 HAL Id: hal-00295217 https://hal.archives-ouvertes.fr/hal-00295217 Submitted on 17 Dec 2002 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Atmos. Chem. Phys., 2, 397–417, 2002 www.atmos-chem-phys.org/acp/2/397/ Atmospheric Chemistry and Physics Modelling transport and deposition of caesium and iodine from the Chernobyl accident using the DREAM model J. Brandt, J. H. Christensen, and L. M. Frohn National Environmental Research Institute, Department of Atmospheric Environment, Frederiksborgvej 399, P.O. Box 358, DK-4000 Roskilde, Denmark Received: 11 April 2002 – Published in Atmos. Chem. Phys. Discuss.: 24 June 2002 Revised: 9 September 2002 – Accepted: 24 September 2002 – Published: 17 December 2002 Abstract. A tracer model, DREAM (the Danish Rimpuff and low cloud scavenging process for the submicron particles and Eulerian Accidental release Model), has been developed for that the precipitation rates are relatively uncertain in the me- modelling transport, dispersion and deposition (wet and dry) teorological model compared to the relative humidity. -
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. -
Sources, Effects and Risks of Ionizing Radiation
SOURCES, EFFECTS AND RISKS OF IONIZING RADIATION United Nations Scientific Committee on the Effects of Atomic Radiation UNSCEAR 2016 Report to the General Assembly, with Scientific Annexes UNITED NATIONS New York, 2017 NOTE The report of the Committee without its annexes appears as Official Records of the General Assembly, Seventy-first Session, Supplement No. 46 and corrigendum (A/71/46 and Corr.1). The report reproduced here includes the corrections of the corrigendum. The designations employed and the presentation of material in this publication do not imply the expression of any opinion whatsoever on the part of the Secretariat of the United Nations concerning the legal status of any country, territory, city or area, or of its authorities, or concerning the delimitation of its frontiers or boundaries. The country names used in this document are, in most cases, those that were in use at the time the data were collected or the text prepared. In other cases, however, the names have been updated, where this was possible and appropriate, to reflect political changes. UNITED NATIONS PUBLICATION Sales No. E.17.IX.1 ISBN: 978-92-1-142316-7 eISBN: 978-92-1-060002-6 © United Nations, January 2017. All rights reserved, worldwide. This publication has not been formally edited. Information on uniform resource locators and links to Internet sites contained in the present publication are provided for the convenience of the reader and are correct at the time of issue. The United Nations takes no responsibility for the continued accuracy of that information or for the content of any external website. -
New York State Department of Health Environmental Radiation Program Environmental Radiation Surveillance Site Readings
New York State Department of Health Environmental Radiation Program Environmental Radiation Surveillance Site Readings Glossary This glossary has been added in order to define technical terms that are used in the various supporting documents for this data set. Please refer to the Data Dictionary for explanation of the meaning of the column headings in the data set. 1. Alpha particles- a positively charged particle made up of two neutrons and two protons emitted by certain radioactive nuclei. a. Gross alpha radioactivity- a measurement of all alpha activity present, regardless of specific radionuclide source. 2. Americium (chemical symbol Am) - is a man-made radioactive metal, with Atomic Number 95. The most important isotope of Americium is Am-241. 3. Background radiation- is radiation that results from natural sources such as cosmic radiation and naturally-occurring radioactive materials in the ground and the earth’s atmosphere including radon. 4. Beta particles- an electron or positron emitted by certain radioactive nuclei. Beta particles can be stopped by aluminum. a. Gross beta radioactivity- measurement of all beta activity present, regardless of specific radionuclide source. 5. Cerium (chemical symbol Ce) - an iron-gray, lustrous metal. Cerium-141, -143, and - 144 are radioisotopes of cerium. 6. Cesium (chemical symbol Cs) - is a metal that may be stable (nonradioactive) or unstable (radioactive). The most common radioactive form of cesium is cesium-137. Another fairly common radioisotope is cesium-134. 7. Cobalt (chemical symbol Co) - is a metal that may be stable (non-radioactive, as found in nature), or unstable (radioactive, man-made). The most common radioactive isotope of cobalt is cobalt-60.