PUBLIC HEALTH STATEMENT Strontium CAS#: 7440-24-6
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Strontium-90
EPA Facts about Strontium-90 What is strontium-90? The most common isotope of strontium is strontium-90. Radioactive strontium-90 is produced when uranium and plutonium undergo fission. Fission The time required for a radioactive substance to is the process in which the nucleus of a lose 50 percent of its radioactivity by decay is radionuclide breaks into smaller parts. Large known as the half-life. Strontium-90 has a half- amounts of radioactive strontium-90 were life of 29 years and emits beta particles of produced during atmospheric nuclear weapons relatively low energy as it decays. Yttrium-90, its tests conducted in the 1950s and 1960s. As a decay product, has a shorter half-life (64 hours) result of atmospheric testing and radioactive than strontium-90, but it emits beta particles of fallout, this strontium was dispersed and higher energy. deposited on the earth. How are people exposed to strontium- 90? What are the uses of strontium-90? Although external exposure to strontium-90 Strontium-90 is used in medical and agricultural from nuclear testing is of minor concern because studies. It is also used in thermoelectric devices environmental concentrations are low, that are built into small power supplies for use strontium in the environment can become part of the food chain. This pathway of exposure in remote locations, such as navigational beacons, remote weather stations, and space became a concern in the 1950s with the advent vehicles. Additionally, strontium-90 is used in of atmospheric testing of nuclear explosives. electron tubes, radioluminescent markers, as a With the suspension of atmospheric testing of radiation source in industrial thickness gauges, nuclear weapons, dietary intake has steadily and for treatment of eye diseases. -
Calcined Bone Provides a Reliable Substrate for Strontium Isotope Ratios As Shown by an Enrichment Experiment
Research Article Received: 8 August 2014 Revised: 15 October 2014 Accepted: 16 October 2014 Published online in Wiley Online Library Rapid Commun. Mass Spectrom. 2015, 29, 107–114 (wileyonlinelibrary.com) DOI: 10.1002/rcm.7078 Calcined bone provides a reliable substrate for strontium isotope ratios as shown by an enrichment experiment Christophe Snoeck1*, Julia Lee-Thorp1,RickSchulting1,JeroendeJong2, Wendy Debouge2 and Nadine Mattielli2 1Research Laboratory for Archaeology and the History of Art, University of Oxford, Dyson Perrins Building, South Parks Rd, Oxford OX1 3QY, UK 2G-Time Laboratory, Université Libre de Bruxelles, CP 160/02, 50, Avenue F.D. Roosevelt, B-1050 Brussels, Belgium RATIONALE: Strontium isotopes (87Sr/86Sr) are used in archaeological and forensic science as markers of residence or mobility because they reflect the local geological substrate. Currently, tooth enamel is considered to be the most reliable tissue, but it rarely survives heating so that in cremations only calcined bone fragments survive. We set out to test the proposition that calcined bone might prove resistant to diagenesis, given its relatively high crystallinity, as the ability to measure in vivo 87Sr/86Sr from calcined bone would greatly extend application to places and periods in which cremation was the dominant mortuary practice, or where unburned bone and enamel do not survive. METHODS: Tooth enamel and calcined bone samples were exposed to a 87Sr-spiked solution for up to 1 year. Samples were removed after various intervals, and attempts were made to remove the contamination using acetic acid washes and ultrasonication. 87Sr/86Sr was measured before and after pre-treatment on a Nu Plasma multi-collector induced coupled plasma mass spectrometer using NBS987 as a standard. -
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 . -
The Chemistry of Strontium and Barium Scales
Association of Water Technologies October 20 -23, 2010 Reno, NV, USA The Chemistry of Strontium and Barium Scales Robert J. Ferguson and Baron R. Ferguson French Creek Software, Inc. Kimberton, PA 19442 (610) 935-8337 (610) 935-1008 FAX [email protected] [email protected] Abstract New ‘mystery scales’ are being encountered as cooling tower operators increase cycles to new highs, add ‘reuse’ water to the make-up, and utilize new make-up water sources as part of an overall water conservation strategy. Scales rarely, if ever, encountered in the past are emerging as potential problems. This threat of unexpected scale is compounded because most water treatment service companies do not include barium and strontium in their make-up water analyses. Water sources with even as little 0.01 mg/L of Ba (as Ba) can become very scale-forming with respect to barite (BaSO4) when tower concentration ratios are increased and sulfuric acid used for pH control. Make-up waters incorporating reverse osmosis concentrate can also provide a strontium and barium source. In some cases, produced waters are also being used in an effort for greener water use. This paper discusses the chemistry of the barium and strontium based scales barite (BaSO4), celestite (SrSO4), witherite (BaCO3) and strontianite (SrCO3). Conditions for formation and control from a water treater’s perspective are emphasized. Indices for prediction are discussed. Scale Prediction and the Concept of Saturation A majority of the indices used routinely by water treatment chemists are derived from the basic concept of saturation. A water is said to be saturated with a compound (e.g. -
Properties of Selected Radioisotopes
CASE FILE COPY NASA SP-7031 Properties of Selected Radioisotopes A Bibliography PART I: UNCLASSIFIED LITERATURE NATIONAL AERONAUTICS AND SPACE ADMINISTRATION NASA SP-7031 PROPERTIES OF SELECTED RADIOISOTOPES A Bibliography Part I: Unclassified Literature A selection of annotated references to technical papers, journal articles, and books This bibliography was compiled and edited by DALE HARRIS and JOSEPH EPSTEIN Goddard Space Flight Center Greenbelt, Maryland Scientific and Technical Information Division / OFFICE OF TECHNOLOGY UTILIZATION 1968 USP. NATIONAL AERONAUTICS AND SPACE ADMINISTRATION Washington, D.C. PREFACE The increasing interest in the application of substantial quantities of radioisotopes for propulsion, energy conversion, and various other thermal concepts emphasizes a need for the most recent and most accurate information available describing the nuclear, chemical, and physical properties of these isotopes. A substantial amount of progress has been achieved in recent years in refining old and developing new techniques of measurement of the properties quoted, and isotope processing. This has resulted in a broad technological base from which both the material and information about the material is available. Un- fortunately, it has also resulted in a multiplicity of sources so that information and data are either untimely or present properties without adequately identifying the measurement techniques or describing the quality of material used. The purpose of this document is to make available, in a single reference, an annotated bibliography and sets of properties for nine of the more attractive isotopes available for use in power production. Part I contains all the unclassified information that was available in the literature surveyed. Part II is the classified counterpart to Part I. -
Strontium Chromate from Austria and France
Strontium Chromate from Austria and France Investigation Nos. 731-TA-1422-1423 (Preliminary) Publication 4836 October 2018 U.S. International Trade Commission Washington, DC 20436 U.S. International Trade Commission COMMISSIONERS David S. Johanson, Chairman Irving A. Williamson Meredith M. Broadbent Rhonda K. Schmidtlein Jason E. Kearns Catherine DeFilippo Director of Operations Staff assigned Kristina Lara, Investigator Samantha DeCarlo, Industry Analyst Tana von Kessler Economist Jennifer Brinckhaus, Accountant KaDeadra McNealy, Statistician David Goldfine, Attorney Douglas Corkran, Supervisory Investigator Address all communications to Secretary to the Commission United States International Trade Commission Washington, DC 20436 U.S. International Trade Commission Washington, DC 20436 www.usitc.gov Strontium Chromate from Austria and France Investigation Nos. 731-TA-1422-1423 (Preliminary) Publication 4836 October 2018 CONTENTS Page ....................................................................................................................... 1 ........................................................................................................ 3 Introduction ................................................................................................................ I‐1 Background ................................................................................................................................ I‐1 Statutory criteria and organization of the report .................................................................... -
4. CHEMICAL, PHYSICAL, and RADIOLOGICAL INFORMATION
STRONTIUM 189 4. CHEMICAL, PHYSICAL, and RADIOLOGICAL INFORMATION 4.1 CHEMICAL IDENTITY Strontium is an alkaline earth element in Group IIA of the periodic table. Because of its high reactivity, elemental (or metallic) strontium is not found in nature; it exists only as molecular compounds with other elements. The chemical information for elemental strontium and some of its compounds is listed in Table 4-1. Radioactive isotopes of strontium (e.g., 89Sr and 90Sr, see Section 4.2) are the primary cause of concern with regard to human health (see Chapter 3). 4.2 PHYSICAL, CHEMICAL, AND RADIOLOGICAL PROPERTIES The physical properties of strontium metal and selected strontium compounds are listed in Table 4-2. The percent occurrence of strontium isotopes and the radiologic properties of strontium isotopes are listed in Table 4-3. Strontium can exist in two oxidation states: 0 and +2. Under normal environmental conditions, only the +2 oxidation state is stable enough to be of practical importance since it readily reacts with both water and oxygen (Cotton and Wilkenson 1980; Hibbins 1997). There are 26 isotopes of strontium, 4 of which occur naturally. The four stable isotopes, 84Sr, 86Sr, 87Sr, and 88Sr, are sometimes referred to as stable strontium. The most important radioactive isotopes, 89Sr and 90Sr, are formed during nuclear reactor operations and during nuclear explosions by the nuclear fission of 235U, 238U, or 239Pu. For example, 235U is split into smaller atomic mass fragments such as 90Sr by a nuclear chain reaction initiated by high energy neutrons of approximately 1 million electron volts (or 1 MeV). -
Strontium-90 and Strontium-89: a Review of Measurement Techniques in Environmental Media
STRONTIUM-90 AND STRONTIUM-89: A REVIEW OF MEASUREMENT TECHNIQUES IN ENVIRONMENTAL MEDIA Robert J. Budnitz Lawrence Berkeley Laboratory University of California Berkeley, CA 91*720 1. IntroiUiction 2. Sources of Enivronmental Radiostrontium 3. Measurement Considerations a. Introduction b. Counting c. •»Sr/"Sr Separation 4. Chemical Techniques a. Air b. Water c. Milk d. Other Media e. Yttrium Recovery after Ingrowth f. Interferences S- Calibration Techniques h. Quality Control 5. Summary and Conclusions 6. Acknowli'J.jnent 7. References -NOTICE- This report was prepared as an account of worK sponsored by the United States Government. Neither the United States nor the United Slates Atomic Energy Commission, nor any of their employees, nor any of their contractors, subcontractors, or their employees, makes any wananty, express or implied, or asjumes any legal liabili:y or responsibility for the accuracy, com pleteness or usefulness of any Information, apparatus, J product or process disclosed, or represents that its use I would not infringe privately owned rights. Mmh li\ -1- 1. INTRODUCTION There are only two radioactive isotopes SrflO of strontium of significance in radiological measurements in the environment: strontium-89 Avg.jS energy 196-1 k«V and strontium-90. 100 Strontium-90 is the more significant from the point of view of environmental impact. 80 Energy keV 644 This is due mostly to its long half-life % Emission 100 (28.1 years). It is a pure beta emitter with 60 Typ* of only one decay mode, leading to yttrium-90 •mission by emission of a negative beta with HUBX * 40 h S46 keV. -
Electrochemical Separation and Purification of Yttrium-86
Radiochim. Acta 90, 225–228 (2002) by Oldenbourg Wissenschaftsverlag, München Electrochemical separation and purification of yttrium-86 By G. Reischl1,F.Rösch2 and H.-J. Machulla1 ,∗ 1 PET-Center, Division of Radiopharmacy, University Hospital Tübingen, D-72076 Tübingen, Germany 2 Institute of Nuclear Chemistry, University of Mainz, D-55099 Mainz, Germany (Received July 5, 2001; accepted in revised form October 24, 2001) Yttrium-86 / Electrolytic purification / radioactive rare earth nuclides onto a small tungsten cath- Electrochemical separation / Y-86 labeling ode was described in 1974 [6]. Recently, the electrochemical deposition of radionuclides of superheavy elements in de- pendence on electrode material and deposition potential was Summary. For quantitative determination of in vivo dosime- investigated [7]. An electrochemical method, based on a pro- try of 90Y-labeled radiotherapeuticals by means of PET, the cedure developed at Mainz [8, 9] to isolate 90Sr from a mix- positron emitting analogue yttrium-86 was produced at a low ture of 90Yand90Sr (c.a.) electrochemically, appeared very 86 86 energy (“medical”) cyclotron via the known Sr(p, n) Y 86 86 promising for isolating and purifying Y. reaction. Using 200 mg of SrCO3 (enrichment 95.6%) and protons of 15.1 MeV energy, average yields of 86Y of 48 ± 8MBq/µA h were produced. After dissolution of 86 86 Experimental SrCO3 in 3 ml of 0.6 N HNO3, Y was deposited in a simple and highly efficient electrochemical two-step procedure onto Materials a platinum cathode at 450 mA (= 20 mA/cm2). The isotope was finally removed from the electrode by 100–300 µlof Strontium-86 was supplied by Chemotrade, Germany, with . -
Sequential Isotopic Determination of Plutonium, Strontium, Americium
Sequential Isotopic Determination of Plutonium, Americium, Uranium, and Strontium in Soil Sample Jeng-Jong Wang, Shing-Fa Fang, and Tzu-Wen Wang Institute of Nuclear Energy Research, Atomic Energy Council, Taiwan, R.O.C. Abstract A procedure is developed to provide sequential analysis of 238Pu, 239/240Pu, 241Am, 238U, and 90Sr in soil sample. Tracers and/or carriers (242Pu, 243Am, 232U, and stable strontium) are added into the soil sample as chemical yield monitors, and then digested and extracted with nitric acid. Plutonium, strontium, americium, and uranium are sequential separated and purified by Dowex ion-exchange resin, EiChroM Sr-resin, EiChroM TRU-resin, and Chelate-100 resin, respectively. 90Sr is measured by Cerenkov counting. The actinides are determined by alpha-particle spectrometer. This method is verified by analyzed the U.S. National Institute of Standard and Technology NRIP2000 soil samples. The analytical results of 241Am, 238Pu, 239/240Pu, 238U, and 90Sr agree with the NIST values within +5.7%, +2.4%, +1.6%, -2.2%, and -2.7%, respectively. According to the traceability limits defined in ANSI N42.22 criteria and measurement traceability to NIST for low-level radionuclides has been demonstrated to be better than 23%, 22%, 22%, 22% and 34% for 241Am, 238Pu, 239/240Pu, 238U, and 90Sr, respectively. Keywords: sequential analysis, NIST, traceability Introduction 238Pu, 239/240Pu, 241Am, 238U, and 90Sr in the environmental samples, such as soil, vegetation, and water, are frequently analyzed for both emergency and routine radiation monitoring. Health physicists use the analytical results of environmental samples to estimate the amount of radioactive material present in the environment, calculating its burden for the radiological workers and the general public. -
Strontium Carbonate Solubility Data in Aqueous Mixtures of Monoethyleneglycol Under a Carbon Dioxide Atmosphere
Brazilian Journal ISSN 0104-6632 of Chemical Printed in Brazil www.scielo.br/bjce Engineering Vol. 35, No. 02, pp. 395 - 402, April - June, 2018 dx.doi.org/10.1590/0104-6632.20180352s20160355 STRONTIUM CARBONATE SOLUBILITY DATA IN AQUEOUS MIXTURES OF MONOETHYLENEGLYCOL UNDER A CARBON DIOXIDE ATMOSPHERE Deborah C. de Andrade1,*, Naíra S. de A. Maniçoba1, Rony O. Sant'ana1, Fedra A.V. Ferreira1, Camila S. Figueiredo2, Jailton F. Nascimento2, Leonardo S. Pereira2 and Osvaldo Chiavone-Filho1 1UFRN. Campus Universitário. Departamento de Engenharia Química. Lagoa Nova. Natal – RN – Brazil, ZIP 59066-800. 2PETROBRAS/CENPES/PDEP/TPP. Av. Horácio Macedo, 950 – Cidade Universitária - Ilha do Fundão. Rio de Janeiro – RJ – Brazil, ZIP 219141-915. (Submitted: June 1, 2016; Revised: March 20, 2017; Accepted: April 5, 2017) Abstract - In order to inhibit natural gas hydrate formation, monoethyleneglycol (MEG) is usually injected into producing well heads. The MEG regeneration process is continuously performed at the platform. Scaling problems usually occur due to the presence of chlorides and carbonates. This work presents salt solubility data for the aqueous system with strontium carbonate, MEG and carbon dioxide. A specific analytical method was developed. Thus, experimental data for strontium carbonate (SrCO3) solubility at various carbon dioxide pressures are reported. Solubilities of SrCO3 in water were measured from 760 to 1610 mmHg at 278.15. 288.15. 298.15 and 323.15 K. For the mixed solvent (ms) conditions, solubilities were measured at 298.15 K and four isobars, i.e., 760, 1210, 1410 and 1520 mmHg. Experimental data were correlated and demonstrated to be accurate for thermodynamic modeling and process simulation. -
Periodic Table 1 Periodic Table
Periodic table 1 Periodic table This article is about the table used in chemistry. For other uses, see Periodic table (disambiguation). The periodic table is a tabular arrangement of the chemical elements, organized on the basis of their atomic numbers (numbers of protons in the nucleus), electron configurations , and recurring chemical properties. Elements are presented in order of increasing atomic number, which is typically listed with the chemical symbol in each box. The standard form of the table consists of a grid of elements laid out in 18 columns and 7 Standard 18-column form of the periodic table. For the color legend, see section Layout, rows, with a double row of elements under the larger table. below that. The table can also be deconstructed into four rectangular blocks: the s-block to the left, the p-block to the right, the d-block in the middle, and the f-block below that. The rows of the table are called periods; the columns are called groups, with some of these having names such as halogens or noble gases. Since, by definition, a periodic table incorporates recurring trends, any such table can be used to derive relationships between the properties of the elements and predict the properties of new, yet to be discovered or synthesized, elements. As a result, a periodic table—whether in the standard form or some other variant—provides a useful framework for analyzing chemical behavior, and such tables are widely used in chemistry and other sciences. Although precursors exist, Dmitri Mendeleev is generally credited with the publication, in 1869, of the first widely recognized periodic table.