Cyclotron Produced Lead-203 P
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Exotic Nuclear Decay Discovered
Exotic nuclear decay discovered The discovery, nearly a century after Becquerel, ofa novel mode of radioactive decay is a surprise, but one that confirms a decay as the chief means by which heavy nuclei shed mass. THOSE who decorate their offices with wall observations now reported, there are particle exists within the nucleus it will then charts showing the isotopes, stable and roughly 1,000 million times as many escape, or the rate of the corresponding otherwise, of the elements are in for a-particles and 14C nuclei in the decay of disintegration process, is thus a function of trouble. As things are, these elaborate mRa, perhaps as vivid a proof as there the height of the potential barrier, its width diagrams usually show by means of a could be of the dominance of the familiar and of the total decrease of the potential colour scheme of some kind which radio mechanisms of decay. energy of the system once the disinte actively unstable nuclei decay by which The rarity of these events is also the gration has taken place. means. Decays in which the a- or explanation why this novel form of radio This calculation, first made in simple {J-particles (electrons) are emitted activity has not previously been found. So form by Gamow, has more recently been predominate, but the diagrams must also much can be told from the account by Rose much refined and accounts for the make room for other less common and Jones of their observations, which "Gamow factors" used by Rose and Jones processes - positron emission, internal entailed more than half a year of running as part of their reason for believing that conversion (of an electron in an inner shell) time with detectors arranged so as to their disintegration products are 14C and and even fission. -
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. -
Proton-Induced Cross-Sections of Nuclear Reactions on Lead up to 37 Mev
Proton-induced cross-sections of nuclear reactions on lead up to 37 MeV F. Ditroi´ a,∗, F. Tark´ anyi´ a, S. Takacs´ a, A. Hermanneb aInstitute for Nuclear Research, Hungarian Academy of Sciences (ATOMKI), Debrecen, Hungary bCyclotron Laboratory, Vrije Universiteit Brussel (VUB), Brussels, Belgium Abstract Excitation function of proton induced nuclear reactions on lead for production of 206;205;204;203;202;201gBi, 203cum;202m;201cumPb and 202cum;201cum;200cum;199cumTl radionuclides were measured up to 36 MeV by using activation method, stacked foil irradiation technique and ?-ray spectrometry. The new experimental data were compared with the few earlier experimental results and with the predictions of the EMPIRE 3.1, ALICE-IPPE (MENDL2p) and TALYS (TENDL-2012) theoretical reaction codes. Keywords: lead target, cross-section by proton activation, theoretical model codes, thin layer activation (TLA) 1. Introduction this, only a few experimental data sets exist, collected mostly by the experimental groups. In the low energy Production cross-sections of proton induced nuclear region practically only one experimental cross-section reactions on lead are important for many applications is available from the Hannover-Cologne group. In our and for the development of nuclear reaction theory. research and application work in connection with the Lead is an important technological material as pure el- activation cross-sections on lead we were involved in ement as well as alloying agent and it is also widely different projects and applications: used in different nuclear technologies, as well as tar- get material for production of 201Tl medical diagnostic • preparation of nuclear database for production of gamma-emitter for SPECT technology (Lagunas-Solar medical radioisotopes in the frame of an IAEA Co- et al., 1981). -
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 . -
Chapter 3 the Fundamentals of Nuclear Physics Outline Natural
Outline Chapter 3 The Fundamentals of Nuclear • Terms: activity, half life, average life • Nuclear disintegration schemes Physics • Parent-daughter relationships Radiation Dosimetry I • Activation of isotopes Text: H.E Johns and J.R. Cunningham, The physics of radiology, 4th ed. http://www.utoledo.edu/med/depts/radther Natural radioactivity Activity • Activity – number of disintegrations per unit time; • Particles inside a nucleus are in constant motion; directly proportional to the number of atoms can escape if acquire enough energy present • Most lighter atoms with Z<82 (lead) have at least N Average one stable isotope t / ta A N N0e lifetime • All atoms with Z > 82 are radioactive and t disintegrate until a stable isotope is formed ta= 1.44 th • Artificial radioactivity: nucleus can be made A N e0.693t / th A 2t / th unstable upon bombardment with neutrons, high 0 0 Half-life energy protons, etc. • Units: Bq = 1/s, Ci=3.7x 1010 Bq Activity Activity Emitted radiation 1 Example 1 Example 1A • A prostate implant has a half-life of 17 days. • A prostate implant has a half-life of 17 days. If the What percent of the dose is delivered in the first initial dose rate is 10cGy/h, what is the total dose day? N N delivered? t /th t 2 or e Dtotal D0tavg N0 N0 A. 0.5 A. 9 0.693t 0.693t B. 2 t /th 1/17 t 2 2 0.96 B. 29 D D e th dt D h e th C. 4 total 0 0 0.693 0.693t /th 0.6931/17 C. -
A Living Radon Reference Manual
A LIVING RADON REFERENCE MANUAL Robert K. Lewis Pennsylvania Department of Environmental Protection Bureau of Radiation Protection, Radon Division and Paul N. Houle, PhD University Educational Services, Inc. Abstract This “living” manual is a compilation of facts, figures, tables and other information pertinent and useful to the radon practitioner, some of which can be otherwise difficult to find. It is envisioned as a useful addition to one’s desk and radon library. This reference manual is also intended to be a “living” document, where its users may supply additional information to the editors for incorporation in revisions as well as updates to this document on-line. Topics contained within the current version include radon chemistry and physics, radon units, radon fans, epidemiology, ambient radon, diagnostics, dosimetry, history, lung cancer, radon in workplace and radon statistics. In some cases motivations and explanations to the information are given. References are included. Introduction This reference manual is a compilation of facts, figures, tables and information on various aspects of radon science. It is hoped that this manual may prove useful to federal and state employees, groups such as AARST and CRCPD, and industry. There are numerous other reference manuals that have been produced on the various aspects of radon science; however, we hope that this manual will have a more “applied” use to all of the various radon practitioners who may use it. Many of the snippets on the various pages are highlights from referenced sources. The snippet will obviously only provide one with the briefest of information. To learn more about that item go to the reference and read the whole paper. -
Radioactive Decay & Decay Modes
CHAPTER 1 Radioactive Decay & Decay Modes Decay Series The terms ‘radioactive transmutation” and radioactive decay” are synonymous. Many radionuclides were found after the discovery of radioactivity in 1896. Their atomic mass and mass numbers were determined later, after the concept of isotopes had been established. The great variety of radionuclides present in thorium are listed in Table 1. Whereas thorium has only one isotope with a very long half-life (Th-232, uranium has two (U-238 and U-235), giving rise to one decay series for Th and two for U. To distin- guish the two decay series of U, they were named after long lived members: the uranium-radium series and the actinium series. The uranium-radium series includes the most important radium isotope (Ra-226) and the actinium series the most important actinium isotope (Ac-227). In all decay series, only α and β− decay are observed. With emission of an α particle (He- 4) the mass number decreases by 4 units, and the atomic number by 2 units (A’ = A - 4; Z’ = Z - 2). With emission β− particle the mass number does not change, but the atomic number increases by 1 unit (A’ = A; Z’ = Z + 1). By application of the displacement laws it can easily be deduced that all members of a certain decay series may differ from each other in their mass numbers only by multiples of 4 units. The mass number of Th-232 is 323, which can be written 4n (n=58). By variation of n, all possible mass numbers of the members of decay Engineering Aspects of Food Irradiation 1 Radioactive Decay series of Th-232 (thorium family) are obtained. -
Discovery of the Thallium, Lead, Bismuth, and Polonium Isotopes
Discovery of the thallium, lead, bismuth, and polonium isotopes C. Fry, M. Thoennessen∗ National Superconducting Cyclotron Laboratory and Department of Physics and Astronomy, Michigan State University, East Lansing, MI 48824, USA Abstract Currently, forty-two thallium, forty-two lead, forty-one bismuth, and forty-two polonium isotopes have so far been observed; the discovery of these isotopes is discussed. For each isotope a brief summary of the first refereed publication, including the production and identification method, is presented. ∗Corresponding author. Email address: [email protected] (M. Thoennessen) Preprint submitted to Atomic Data and Nuclear Data Tables October 6, 2011 Contents 1. Introduction . 2 2. 176−217Tl ............................................................................................. 3 3. 179−220Pb............................................................................................. 14 4. 184−224Bi ............................................................................................. 22 5. 186−227Po ............................................................................................. 31 6. Summary ............................................................................................. 39 References . 39 Explanation of Tables . 47 7. Table 1. Discovery of thallium, lead, bismuth, and polonium isotopes . 47 Table 1. Discovery of thallium, lead, bismuth, and polonium. See page 47 for Explanation of Tables . 48 1. Introduction The discovery of thallium, lead, bismuth, and polonium -
Angular Correlation of CO60
Western Michigan University ScholarWorks at WMU Master's Theses Graduate College 7-1964 Angular correlation of CO60 Henry Kuhlman Follow this and additional works at: https://scholarworks.wmich.edu/masters_theses Part of the Physics Commons Recommended Citation Kuhlman, Henry, "Angular correlation of CO60" (1964). Master's Theses. 4286. https://scholarworks.wmich.edu/masters_theses/4286 This Masters Thesis-Open Access is brought to you for free and open access by the Graduate College at ScholarWorks at WMU. It has been accepted for inclusion in Master's Theses by an authorized administrator of ScholarWorks at WMU. For more information, please contact [email protected]. ANGULAR CORRELATION OF c¢6o by Hen !uhlman A thesis presented to the Faculty of the School of Graduate Studies in partial fulfillment of the Degree of Master of Arts Western Michigan University Kalamazoo, Michigan July 1964 ACKNOWLEDGEMENrS The author wishes to express his sincere gratitude to Dr. George Bradley for his guidance and advice during every phase of this project. A word of thanks also is given to Dr. Larry Oppliger and Mr. Gus Hoyer for their stimulating discussions and consultations. Especially the author thanks his wife, Pat. He is indebted to her not only for the typing and preparation of the manuscript but also for her endurance and encouragement during the many months of data taking. Henry Kuhlman i TABLE OF CONTENTS CHAPTER PAGE I INTRODUCTION 1 Method of measurement . 1 Expansion of the correlation function . 2 Dependence of the coefficients 3 II THE PROBLEM AND GAMMA RAY DETECTION . 4 The Problem . • . • . • • 4 Decay scheme of C660 •. -
Nuclidenavigator®-Pro
ORTEC® NuclideNavigator®-Pro Interactive Chart of the Nuclides and Reference Program for Microsoft® Windows® 10 C53-BW Software User's Manual Version 4.1.0 Advanced Measurement Technology, Inc. a/k/a/ ORTEC®, a subsidiary of AMETEK®, Inc. WARRANTY THIS SOFTWARE IS PROVIDED "AS IS" AND ANY EXPRESS OR IMPLIED WARRANTIES, INCLUDING, BUT NOT LIMITED TO, THE IMPLIED WARRANTIES OF MERCHANTABILITY AND FITNESS FOR A PARTICULAR PURPOSE ARE DISCLAIMED. IN NO EVENT SHALL ORTEC, THE COPYRIGHT OWNER, OR CONTRIBUTORS BE LIABLE FOR ANY DIRECT, INDIRECT, INCIDENTAL, SPECIAL, EXEMPLARY, OR CONSEQUENTIAL DAMAGES (INCLUDING, BUT NOT LIMITED TO, PROCUREMENT OF SUBSTITUTE GOODS OR SERVICES; LOSS OF USE, DATA, OR PROFITS; OR BUSINESS INTERRUPTION) HOWEVER CAUSED AND ON ANY THEORY OF LIABILITY, WHETHER IN CONTRACT, STRICT LIABILITY, OR TORT (INCLUDING NEGLIGENCE OR OTHERWISE) ARISING IN ANY WAY OUT OF THE USE OF THIS SOFTWARE, EVEN IF ADVISED OF THE POSSIBILITY OF SUCH DAMAGE. NuclideNavigator-Pro was developed for AMETEK by Walter King and Associates Copyright© 2014-2020 Walter King and Associates All Rights Reserved. Copyright © 2021, Advanced Measurement Technology, Inc. All rights reserved. ORTEC® is a registered trademark of Advanced Measurement Technology, Inc. All other trademarks used herein are the property of their respective owners. NOTICE OF PROPRIETARY PROPERTY —This document and the information contained in it are the proprietary property of AMETEK Inc., ORTEC Business Unit. It may not be copied or used in any manner nor may any of the information in or upon it be used for any purpose without the express written consent of an authorized agent of AMETEK Inc., ORTEC Business Unit. -
The Environmental Behaviour of Polonium
technical reportS series no. 484 Technical Reports SeriEs No. 484 The Environmental Behaviour of Polonium F. Carvalho, S. Fernandes, S. Fesenko, E. Holm, B. Howard, The Environmental Behaviour of Polonium P. Martin, M. Phaneuf, D. Porcelli, G. Pröhl, J. Twining @ THE ENVIRONMENTAL BEHAVIOUR OF POLONIUM The following States are Members of the International Atomic Energy Agency: AFGHANISTAN GEORGIA OMAN ALBANIA GERMANY PAKISTAN ALGERIA GHANA PALAU ANGOLA GREECE PANAMA ANTIGUA AND BARBUDA GUATEMALA PAPUA NEW GUINEA ARGENTINA GUYANA PARAGUAY ARMENIA HAITI PERU AUSTRALIA HOLY SEE PHILIPPINES AUSTRIA HONDURAS POLAND AZERBAIJAN HUNGARY PORTUGAL BAHAMAS ICELAND QATAR BAHRAIN INDIA REPUBLIC OF MOLDOVA BANGLADESH INDONESIA ROMANIA BARBADOS IRAN, ISLAMIC REPUBLIC OF RUSSIAN FEDERATION BELARUS IRAQ RWANDA BELGIUM IRELAND SAN MARINO BELIZE ISRAEL SAUDI ARABIA BENIN ITALY SENEGAL BOLIVIA, PLURINATIONAL JAMAICA SERBIA STATE OF JAPAN SEYCHELLES BOSNIA AND HERZEGOVINA JORDAN SIERRA LEONE BOTSWANA KAZAKHSTAN SINGAPORE BRAZIL KENYA SLOVAKIA BRUNEI DARUSSALAM KOREA, REPUBLIC OF SLOVENIA BULGARIA KUWAIT SOUTH AFRICA BURKINA FASO KYRGYZSTAN SPAIN BURUNDI LAO PEOPLE’S DEMOCRATIC SRI LANKA CAMBODIA REPUBLIC SUDAN CAMEROON LATVIA SWAZILAND CANADA LEBANON SWEDEN CENTRAL AFRICAN LESOTHO SWITZERLAND REPUBLIC LIBERIA SYRIAN ARAB REPUBLIC CHAD LIBYA TAJIKISTAN CHILE LIECHTENSTEIN THAILAND CHINA LITHUANIA THE FORMER YUGOSLAV COLOMBIA LUXEMBOURG REPUBLIC OF MACEDONIA CONGO MADAGASCAR TOGO COSTA RICA MALAWI TRINIDAD AND TOBAGO CÔTE D’IVOIRE MALAYSIA TUNISIA CROATIA MALI -
The Isotope Effect: Prediction, Discussion, and Discovery
1 The isotope effect: Prediction, discussion, and discovery Helge Kragh Centre for Science Studies, Department of Physics and Astronomy, Aarhus University, 8000 Aarhus, Denmark. ABSTRACT The precise position of a spectral line emitted by an atomic system depends on the mass of the atomic nucleus and is therefore different for isotopes belonging to the same element. The possible presence of an isotope effect followed from Bohr’s atomic theory of 1913, but it took several years before it was confirmed experimentally. Its early history involves the childhood not only of the quantum atom, but also of the concept of isotopy. Bohr’s prediction of the isotope effect was apparently at odds with early attempts to distinguish between isotopes by means of their optical spectra. However, in 1920 the effect was discovered in HCl molecules, which gave rise to a fruitful development in molecular spectroscopy. The first detection of an atomic isotope effect was no less important, as it was by this means that the heavy hydrogen isotope deuterium was discovered in 1932. The early development of isotope spectroscopy illustrates the complex relationship between theory and experiment, and is also instructive with regard to the concepts of prediction and discovery. Keywords: isotopes; spectroscopy; Bohr model; atomic theory; deuterium. 1. Introduction The wavelength of a spectral line arising from an excited atom or molecule depends slightly on the isotopic composition, hence on the mass, of the atomic system. The phenomenon is often called the “isotope effect,” although E-mail: [email protected]. 2 the name is also used in other meanings.