Calculation of Rates for Radioactive Isotope Beam Production at TRIUMF
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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. -
Volatility of Radiopharmacy-Prepared Sodium Iodide-131 Capsules
RADIATION SAFETY Volatility of Radiopharmacy-Prepared Sodium Iodide-131 Capsules James M. Bright, Trenton T. Rees, Louis E. Baca and Richard L. Green Pharmacy Services, Syncor International Corporation, Albuquerque, New Mexico; and Quality and Regulatory Department, Syncor International Corporation, Woodland Hills, California studied thyroid physiology using 128I in 1937 (1,2). In January Objective: The aims of this study were to quantify the extent 1941, Hertz and Roberts were the first to administer radioiodine of volatilization from 131I-NaI therapeutic capsules prepared in 131I for the treatment of hyperthyroid patients (3). Today, almost a centralized radiopharmacy and to quantify the amount of 60 y later, radioiodine therapy with 131I remains the primary volatile 131I released from a dispensing vial containing a compounded 131I-NaI therapy capsule. therapeutic agent used in nuclear medicine, and its use is firmly Methods: Therapy capsules were prepared by injecting 131I established in the 2 diseases first treated: hyperthyroidism and oral solution into capsules containing anhydrous dibasic thyroid carcinoma. sodium phosphate. Volatilized activity was obtained by filter- Initially the use of 131I was restricted to the only pharmaceu- ing air drawn across samples that were placed open on the tical dosage form then available—liquid oral solution. While 131 bottom of a sample holder cup. Volatile I was captured by liquid radioiodine proved to be beneficial to the patients to filtering it through 3 triethylenediamine-impregnated carbon whom it was administered, the frequency of contamination and cartridge filters, arranged in series. To quantify the amount of thyroid uptake activity in nuclear medicine personnel who volatile 131I released from a dispensing vial during a simulated patient administration, a vial containing a compounded 131I handled the material was noted with increasing alarm (4–7). -
Circular of the Bureau of Standards No. 562: Bibliography of Research on Deuterium and Tritium Compounds 1945 and 1952
NBS CIRCULAR 562 Bibliography of Research on Deuterium and Tritium Compounds 1945 to 1952 UNITED STATES DEPARTMENT OF COMMERCE NATIONAL BUREAU OF STANDARDS PERIODICALS OF THE NATIONAL BUREAU OF STANDARDS (Published monthly) The National Bureau of Standards is engaged in fundamental and applied research in physics, chemistry, mathematics, and engineering. Projects are conducted in fifteen fields: electricity and electronics, optics and metrology, heat and power, atomic and radiation physics, chemistry, mechanics, organic and fibrous materials, metallurgy, mineral products, building technology, applied mathematics, data process¬ ing systems, cryogenic engineering, radio propagation, and radio standards. The Bureau has custody of the national standards of measurement and conducts research leading to the improvement of scientific and engineering standards and of techniques and methods of measurement. Testing methods and in¬ struments are developed; physical constants and properties of materials are determined; and technical processes are investigated. Journal of Research The Journal presents research papers by authorities in the specialized fields of physics, mathematics, chemistry, and engineering. Complete details of the work are presented, including laboratory data, experimental procedures, and theoretical and mathematical analyses. Annual subscription: domestic, $4.00; 25 cents additional for foreign mailing. Technical News Bulletin Summaries of current research at the National Bureau of Standards are published each month in the Technical News Bulletin. The articles are brief, with emphasis on the results of research, chosen on the basis of their scientific or technologic importance. Lists of all Bureau publications during the preceding month are given, including Research Papers, Handbooks, Applied Mathematics Series, Building Mate¬ rials and Structures Reports, Miscellaneous Publications, and Circulars. -
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%). -
High Accuracy Measurement of Isotope Ratios of Molybdenum in Some Terrestrial Molybdenites
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Elsevier - Publisher Connector ARTICLES High Accuracy Measurement of Isotope Ratios of Molybdenum in Some Terrestrial Molybdenites Qi-Lu* and Akimasa Masuda Department of Chemistry, Faculty of Science, The University of Tokyo, Tokyo, Japan The isotope ratios of molybdenum in molybdenites were studied. A special triple filament technique was used to obtain stable and lasting signals for MO+. There are no differences bigger than ~0.4 parts per IO4 among four samples and the standard. CJ Am Sot Mass Spectrom 1992, 3, IO- 17) olybdenum is a very interesting element be- denum thus far, in spite of the potential importance cause its seven isotopes can reflect several of research in isotopic abundance of molybdenum. M effects related to nuclear physics. The nu- In this study we have established a method for clear phenomena that may affect the isotope ratios in securing stable and lasting current of MO+ and exam- question are (1) the synthesis of seven isotopes of MO ined the mass fractionation of MO isotopes during involving three processes (r, s, and p) in the standard measurement. Based on these studies, the isotope model of nucleosynthesis [I]; ($2 the nuclear hssion of ratios of MO were determined with high precision uranium-238, which produces MO, “MO, 98Mo, and for some molybdenites from a variety of locations ‘“MO; and (3) the double-beta decays of ‘“Zr and throughout the world. The present study will afford a lwMo leading to 96Mo and ‘“Ru. Another intriguing foundation for further precise studies of molybdenum property of this element is that the anomalous abun- isotopes involving meteorites and terrestrial rocks. -
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 . -
Lithium Isotope Fractionation During Uptake by Gibbsite
Available online at www.sciencedirect.com ScienceDirect Geochimica et Cosmochimica Acta 168 (2015) 133–150 www.elsevier.com/locate/gca Lithium isotope fractionation during uptake by gibbsite Josh Wimpenny a,⇑, Christopher A. Colla a, Ping Yu b, Qing-Zhu Yin a, James R. Rustad a, William H. Casey a,c a Department of Earth and Planetary Sciences, University of California, One Shields Avenue, Davis, CA 95616, United States b The Keck NMR Facility, University of California, One Shields Avenue, Davis, CA 95616, United States c Department of Chemistry, University of California, One Shields Avenue, Davis, CA 95616, United States Received 5 November 2014; accepted in revised form 8 July 2015; available online 15 July 2015 Abstract The intercalation of lithium from solution into the six-membered l2-oxo rings on the basal planes of gibbsite is well-constrained chemically. The product is a lithiated layered-double hydroxide solid that forms via in situ phase change. The reaction has well established kinetics and is associated with a distinct swelling of the gibbsite as counter ions enter the interlayer to balance the charge of lithiation. Lithium reacts to fill a fixed and well identifiable crystallographic site and has no solvation waters. Our lithium-isotope data shows that 6Li is favored during this intercalation and that the À À solid-solution fractionation depends on temperature, electrolyte concentration and counter ion identity (whether Cl ,NO3 À or ClO4 ). We find that the amount of isotopic fractionation between solid and solution (DLisolid-solution) varies with the amount of lithium taken up into the gibbsite structure, which itself depends upon the extent of conversion and also varies À À À with electrolyte concentration and in the counter ion in the order: ClO4 <NO3 <Cl . -
Measurement and Analysis of the Resolved Resonance Cross Sections of the Natural Hafnium Isotopes
CORE Metadata, citation and similar papers at core.ac.uk Provided by University of Birmingham Research Archive, E-theses Repository MEASUREMENT AND ANALYSIS OF THE RESOLVED RESONANCE CROSS SECTIONS OF THE NATURAL HAFNIUM ISOTOPES by TIMOTHY CHRISTOPHER WARE A thesis submitted to The University of Birmingham for the degree of DOCTOR OF PHILOSOPHY School of Physics and Astronomy College of Engineering and Physical Sciences The University of Birmingham June 2010 University of Birmingham Research Archive e-theses repository This unpublished thesis/dissertation is copyright of the author and/or third parties. The intellectual property rights of the author or third parties in respect of this work are as defined by The Copyright Designs and Patents Act 1988 or as modified by any successor legislation. Any use made of information contained in this thesis/dissertation must be in accordance with that legislation and must be properly acknowledged. Further distribution or reproduction in any format is prohibited without the permission of the copyright holder. ABSTRACT Hafnium is a ductile metallic element with a large neutron absorption cross section. It can be used in reactor control rods to regulate the fission process. The NEA High Priority Request List for nuclear data presents a need for improved characterisation of the hafnium cross section in the resolved resonance region. This thesis presents new resonance cross section parameters for the six natural hafnium isotopes. Cross section measurements, supported by the NUDAME and EUFRAT projects, were performed at the IRMM Geel GELINA time-of-flight facility. Capture experiments were conducted on the 12 m, 28 m and 58 m flight paths using C6D6 detectors and transmission experiments were performed at flight paths of 26 m and 49 m using a 6Li glass detector. -
First Search for $\Alpha $ Decays of Naturally Occurring Hf Nuclides With
First search for α decays of naturally occurring Hf nuclides with emission of γ quanta F.A. Danevicha,1, M. Hultb, D.V. Kasperovycha, G.P. Kovtunc,d, K.V. Kovtune, G. Lutterb, G. Marissensb, O.G. Polischuka, S.P. Stetsenkoc, V.I. Tretyaka aInstitute for Nuclear Research, 03028 Kyiv, Ukraine bEuropean Commission, Joint Research Centre, Retieseweg 111, 2440 Geel, Belgium cNational Scientific Center Kharkiv Institute of Physics and Technology, 61108 Kharkiv, Ukraine dKarazin Kharkiv National University, 61022 Kharkiv, Ukraine ePublic Enterprise “Scientific and Technological Center Beryllium”, 61108 Kharkiv, Ukraine Abstract The first ever search for α decays to the first excited state in Yb was performed for six isotopes of hafnium (174, 176, 177, 178, 179, 180) using a high purity Hf-sample of natural isotopic abundance with a mass of 179.8 g. For 179Hf, also α decay to the ground state of 175Yb was searched for thanks to the β-instability of the daughter nuclide 175Yb. The measurements were conducted using an ultra low-background HPGe-detector system located 225 m underground. After 75 d of data taking no decays were detected but lower 15 18 bounds for the half-lives of the decays were derived on the level of lim T1/2 ∼ 10 −10 a. The decay with the shortest half-life based on theoretical calculation is the decay of 174Hf to the first 2+ 84.3 keV excited level of 170Yb. The experimental lower bound was found 15 to be T1/2 ≥ 3.3 × 10 a. Keywords: Alpha decay; 174Hf, 176Hf, 177Hf, 178Hf, 179Hf, 180Hf, Low-background HPGe γ spec- trometry arXiv:1911.02597v1 [nucl-ex] 6 Nov 2019 1 INTRODUCTION Alpha decay is one of the most important topics of nuclear physics both from the theoretical and experimental points of view. -
UNIT 1 SUMMARY MATTER – Anything That Has Mass and Takes up Space
UNIT 1 SUMMARY MATTER – Anything that has mass and takes up space Other examples? PARTICLE – a single atom or groups of atoms that are bonded together and function as one unit Matter is found in phases or states: GAS • Indefinite shape and volume • Straight-line motion LIQUID • Indefinite shape, definite volume • Rolling motion SOLID • Definite shape and volume • Vibrating motion TYPES OF MATTER PURE SUBSTANCE – Matter where all the particles are identical He NaCl C12H22O11 There are two types of pure substances: ELEMENT • Made from only one type of atom • Cannot be broken into simpler substances by chemical means • Found on the Periodic Table Other examples? Gold Sulfur Helium Sodium COMPOUND • Made from two or more atoms joined together by chemical bonds • Can be broken down into simpler substances by chemical means (by breaking chemical bonds) Water Salt Sugar Other examples? Water Compound ↓ electricity Hydrogen and Oxygen ↓ electricity ↓ electricity Hydrogen and Oxygen Elements Salt Compound ↓ electricity Sodium and Chlorine ↓ electricity ↓ electricity Sodium and Chlorine Elements In CHEMICAL SEPARATION METHODS (e.g. electrolysis), chemical bonds are broken and/or formed. MIXTURE – Matter with different types of particles (elements and/or compounds) There are two types of mixtures: HETEROGENEOUS – Has distinct parts with different properties HOMOGENEOUS – Has same properties throughout (uniform composition) Air Jell-O Steel Brass SOLUTION – A homogenous mixture CLASSIFICATION OF MATTER CHANGES IN MATTER PHYSICAL CHANGE – One that -
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). -
4.62 Samarium
IUPAC 4.62 samarium Stable Relative Mole isotope atomic mass fraction 144 Sm 143.912 01 0.0308 147 † Sm 146.914 90 0.1500 148 Sm † 147.914 83 0.1125 149 Sm 148.917 19 0.1382 150 Sm 149.917 28 0.0737 152 Sm 151.919 74 0.2674 154 Sm 153.922 22 0.2274 † Radioactive isotope having a relatively long half-life and a characteristic terrestrial isotopic composition that contributes significantly and reproducibly to the determination of the standard atomic weight of the element in normal materials . The half-lives of 147 Sm and 148 Sm are 1.06 × 10 11 years and 7 × 10 15 years, respectively. 4.62.1 Samarium isotopes in Earth/planetary science One possible origin for the Moon is from debris ejected by an indirect giant impact of Earth by an astronomical body the size of Mars when the Earth was forming [433]. The kinetic energy liberated is thought to have melted a large part of the Moon forming a lunar magma ocean. P.O. 13757, Research Triangle Park, NC (919) 485-8700 IUPAC Samarium isotope measurement results [434], along with measurements of isotopes of hafnium, tungsten, and neodymium[435], suggest that lunar magma formed about 70 × 10 6 years after the Solar System formed and had crystallized by about 215 × 10 6 years after formation. 147 Sm is used to study the formation of potassium, rare earth elements , and phosphorus-rich rocks [436]. 4.62.2 Samarium isotopes in geochronology 147 Sm is used for determining formation ages of igneous and metamorphic rocks via analysis of the minerals which compose them, such as those shown in Figure 4.62.1 [437-439].