Why Polonium 210?
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Distribution Coefficients of Polonium Between 0.75 M HDEHP in Cyclo- Hexane and Aqueous Hydrochloric and Nitric Acids Guogang Jia* and Giancarlo Torri
18 The Open Inorganic Chemistry Journal, 2008, 2, 18-21 Distribution Coefficients of Polonium Between 0.75 M HDEHP in Cyclo- hexane and Aqueous Hydrochloric and Nitric Acids Guogang Jia* and Giancarlo Torri Agency for Environmental Protection and for Technical Services, Via V. Brancati 48, 00144 Roma, Italy Abstract: The distribution coefficients (D) of polonium between 0.75 M di(2-ethyhexyl)phosphoric acid (HDEHP) in cy- clohexane and aqueous hydrochloric and nitric acids have been studied. Results indicate that: (1) D values are ranged from 32.7 to 0.00048 when the HCl acidities vary from 0.10 to 10.0 M, showing that polonium can well be extracted by 0.75 M HDEHP in cyclohexane if the aqueous HCl acidities are 0.050 M and it will not be extracted if 0.10 M HCl; (2) D values are ranged from 47.1 to 0.0117 when the HNO3 acidities vary from 0.10 to 10.0 M, showing that polonium can be extractable by 0.75 M HDEHP in cyclohexane and in a wide range acidity of 4 M HNO3. The different extraction behaviours of polonium in 0.75 M HDEHP in cyclohexane and different acidities of HCl and HNO3 were found. The find- ings will be very helpful to improve the methods involving polonium decontamination for determination and separation of americium, curium as well as other radioelements in environmental soil, water and biological samples. Keywords: Polonium, HDEHP, distribution coefficients. 1. INTRODUCTION on its oxidation state. Therefore, question is raised: which oxidation state is responsible for major polonium volatility, The element polonium (210Po) was discovered by Marie valences of +2, +4, and probably +6? Curie as the first element separated from pitchblende, and named after her home country, Poland [1, 2]. -
Po and Pb in the Terrestrial Environment
Current Advances in Environmental Science (CAES) 210Po and 210Pb in the Terrestrial Environment Bertil R.R. Persson Medical Radiation Physics, Lund University S-22185 LUND, Sweden [email protected] Abstract- The natural sources of 210Po and 210Pb in the meat at high northern latitudes. This was, however, of terrestrial environment are from atmospheric deposition, soil natural origin and no evidence of significant contributions and ground water. The uptake of radionuclides from soil to of 210Po from the atomic bomb test was found. The most plant given as the soil transfer factor, varies widely between significant radionuclides in the fallout from the atmospheric various types of crops with an average about ± atomic bomb-test of importance for human exposure were The atmospheric deposition of 210Pb and 210Po also affect the 137Cs and 90Sr [4]. activity concentrations in leafy plants with a deposition th 210 210 transfer factor for Pb is in the order of 0.1-1 (m2.Bq-1) plants During the 1960 century the presence of Pb and and for root fruits it is < 0.003, Corresponding values for 210Po 210Po was extensively studied in human tissues and are about a factor 3 higher. particularly in Arctic food chains [4-20]. The activity concentration ratios between milk and various types of forage for 210Pb were estimated to ± and for In December of 2006, former Russian intelligence 210Po to ±By a daily food intake of 16 kg dry matter operative Alexander Litvinenko died from ingestion of a 210 210 per day the transfer coefficient Fm. for Pb was estimated to few g of Po. -
Factsheets & Faqs Polonium-210
Factsheets & FAQs Polonium-210 Basic Facts Polonium-210 (Po-210) is a radioactive element that occurs naturally and is present in the environment at extremely low concentrations. Polonium was discovered by Marie Sklodowska-Curie and Pierre Curie in 1898 and was named after Marie's native land of Poland (Latin: Polonia). This element was the first one discovered by them while they were investigating the cause of pitchblende radioactivity. It is a fairly volatile (50% is vaporized in air in 45 hours at 55°C) silvery-grey soft metal. Po-210 has a half-life of 138 days. This is the time it takes for the activity to decrease by half due to a process of radioactive decay. Po-210 decays to stable lead-206 by emitting alpha particles, accompanied by very low intensity gamma rays. The majority of the time Po-210 decays by emission of alpha particles only, not by emission of an alpha particle and a gamma ray. Only about one in a 100,000 decays results in the emission of a gamma ray. Alpha spectroscopy is the best method of measuring this isotope. Origin Being produced during the decay of naturally occurring uranium-238, polonium-210 is widely distributed in small amounts in the earth's crust. Although it can be produced by the chemical processing of uranium ores or minerals, uranium ores contain less than 0.1 mg Po-210 per ton. Because Po-210 is produced from the decay of radon-222 gas, it can be found in the atmosphere from which it is deposited on the earth's surface. -
Mev for Ne, 166 Mev for 0, and 2 -125 Mev for 12C
Lawrence Berkeley National Laboratory Recent Work Title ON-LINE SPECTROSCOPY OF NEUTRON-DEFICIENT ACTINIUM ISOTOPES Permalink https://escholarship.org/uc/item/8nb5n8f3 Authors Treytl, William J. Hyde, Earl K. Valli, Kalevi. Publication Date 1967-05-01 eScholarship.org Powered by the California Digital Library University of California UCRL-17405 ~f*J- University of California Ernest O. Lawrence Radiation Laboratory ON -LINE a SPECTROSCOPY OF NEUTRON -DEFICIENT ACTINIUM ISOTOPES William J. Treytl, Earl K. Hyde, and Kalevi Valli May 1967 REC lVED U\WP..rNU c::. Ri~D!~'!'nN ll':BC:tA'f()RY ~ ~,- TWO-WEEK LOAN COpy ~ ,-I This is a library Circul atin9 Copy tI ~ which may be borrowed for two weeks. ,.c::. For a personal retention copy, call l-f' 0 Tech. 'nfo. Dioision, Ext. 5545 \Il 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. -
10.ISCA-IRJEVS-2015-274.Pdf
International Research Journal of Environment Sciences _____________________________ ___E-ISSN 2319–1414 Vol. 5(4), 67-69, April (2016) Int. Res. J. Environment Sci. Review Paper Identification and Assessment of Emerging Threats from Radio Nuclides in Drinking Water Brajesh K. Shrivastava Ministry of Drinking Water and Sanitation, Government of India, New Delhi, India [email protected] Available online at: www.isca.in, www.isca.me Received 26th December 2015, revised 7th February 2016, accepted 4th March 201 6 Abstract The Research paper undertakes theoretical review of the characteristics of few radio nuclides in aqeous system. These radio nuclides have been identified due to their potential health effects and widespread concern. The radio nuclides are: Uranium, Tritium, Cesium-137, Radon, Strontium-90, Radium, Iodine -131, Technetium and Polonium-210. Keywords : Radio nuclides, Radiation, Ionization, Reverse Osmosi s. Introduction (WHO) recommends a guideline value of maximum permissible limit of 15 µg/L for uranium in drinking water while USEPA Radioactive isotopes released from nuclear power plants/ has a maximum limit of 30 µg/L. At high exposure levels, nuclear testing /medical facilities may wind up in drinking water uranium is believed to cause bone cancer and other type of 1 sources and thereby can pose risk for human life . Radiation cancers in humans. Uranium is also toxic to the kidneys 2. exposure may results from ionizing (alpha and beta particles, En riched uranium exposure alters the spatial working memory gamma rays or X-rays) or non-ionizing materials. Radiation of capacities of rats when these rats are exposed for 9 months to radioactive materials is measured either in curie (US system) or drinking water contaminated with enriched Uranium at a dose of in Becquerel (SI unit) and the risk of radiation exposure to 40 mg/L 3. -
Periodic Table of the Elements Notes
Periodic Table of the Elements Notes Arrangement of the known elements based on atomic number and chemical and physical properties. Divided into three basic categories: Metals (left side of the table) Nonmetals (right side of the table) Metalloids (touching the zig zag line) Basic Organization by: Atomic structure Atomic number Chemical and Physical Properties Uses of the Periodic Table Useful in predicting: chemical behavior of the elements trends properties of the elements Atomic Structure Review: Atoms are made of protons, electrons, and neutrons. Elements are atoms of only one type. Elements are identified by the atomic number (# of protons in nucleus). Energy Levels Review: Electrons are arranged in a region around the nucleus called an electron cloud. Energy levels are located within the cloud. At least 1 energy level and as many as 7 energy levels exist in atoms Energy Levels & Valence Electrons Energy levels hold a specific amount of electrons: 1st level = up to 2 2nd level = up to 8 3rd level = up to 8 (first 18 elements only) The electrons in the outermost level are called valence electrons. Determine reactivity - how elements will react with others to form compounds Outermost level does not usually fill completely with electrons Using the Table to Identify Valence Electrons Elements are grouped into vertical columns because they have similar properties. These are called groups or families. Groups are numbered 1-18. Group numbers can help you determine the number of valence electrons: Group 1 has 1 valence electron. Group 2 has 2 valence electrons. Groups 3–12 are transition metals and have 1 or 2 valence electrons. -
Chapter 5 PROPERTIES of IRRADIATED LBE and Pb*
Chapter 5 PROPERTIES OF IRRADIATED LBE AND Pb* 5.1 Introduction Lead and LBE possess favourable properties as both a spallation neutron target material and as a coolant for ADS and reactor systems. For ADS applications, these properties include: 1) a high yield of about 28 n for LBE and 24 n for Pb per 1 GeV proton; 2) both melts have an extremely small neutron absorption cross-section; (3) a small scattering cross-section [Gudowski, 2000]. As a coolant, lead and LBE possess: 1) high boiling points; 2) high heat capacities; (3) inert behaviour with respect to reaction with water. For safe operation and post-irradiation handling of LBE and Pb it is necessary to know the nuclides generated during irradiation. Some of these nuclides are volatile, hazardous and rather long-lived. Their behaviour within the system is strongly influenced by the environment including the oxygen content and temperature. If volatiles are produced, their release rates under specific conditions must be evaluated. The release of volatiles may be prevented by the application of a suitable absorber. Protons of 600 MeV energy induce spallation reactions in heavy materials such as Pb and Bi. These reactions generate direct spallation products, consisting of nuclei with masses close to that of the target nuclei. At the high energies involved multiple inelastic reactions are possible. Therefore, one must expect a large number of isotopes as products. For instance, reactions on Pb generate Hg isotopes roughly from 180Hg to 206Hg. Similarly, reactions of protons on Bi generate Po isotopes up to 209Po. 210Po is generated by neutron capture on 209Bi, and subsequent E decay of the compound nucleus 210Bi. -
Polonium Human-Injection Experiments Injection and Lived Another 8 Years Be- Fore Dying, in 1953, of Heart Failure
The Human Plutonium Injection Experiments any effect on the normal course of his life.” HP-12 was 53 at the time of the Polonium Human-Injection Experiments injection and lived another 8 years be- fore dying, in 1953, of heart failure. In 1944, in response to concerns for the risk associated with occupational Late radiation effects, such as cancer, exposures to polonium, the Army Medical Corps authorized Rochester to un- were not expected to develop for ten to dertake a study of the biological behavior of that element. The program was fifteen years, if at all. For example, the started in August 1944 with animals, and by November, studies with humans induction period in humans for radium- had begun. Eventually, tracer amounts of radioactive polonium-210 were in- induced cancer, especially malignancy jected into four hospitalized humans and ingested by a fifth. of the bones, was about 10 to 30 years after exposure. Despite Langham’s Polonium, the first element isolated by Marie and Pierre Curie from pitch- statement, we cannot, of course, dis- blende in 1898, is an alpha emitter. When alpha particles from polonium- count the fact that HP-12 might have 210 collide with beryllium atoms, neutrons are ejected, and polonium-berylli- lived 20 or more years; although in um combinations had already served physicists as a convenient source of 1945, fifty years of age was considered neutrons. During the Manhattan Project, it was decided to use that neutron to be fairly advanced. On the other source as an initiator of the chain reaction in the atomic bombs, thus making hand, the GIs at Los Alamos who were polonium (and beryllium) an occupational health hazard for the people who heavily exposed to plutonium in 1945 needed to develop and build the initiators. -
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 -
Genius of the Periodic Table
GENIUS OF THE PERIODIC TABLE "Isn't it the work of a genius'. " exclaimed Academician V.I. Spitsyn, USSR, a member of the Scientific Advisory Committee when talking to an Agency audience in January. His listeners shared his enthusiasm. Academician Spitsyn was referring to the to the first formulation a hundred years ago by Professor Dmitry I. Mendeleyev of the Periodic Law of Elements. In conditions of enormous difficulty, considering the lack of data on atomic weights of elements, Mendeleyev created in less than two years work at St. Petersburg University, a system of chemical elements that is, in general, still being used. His law became a powerful instrument for further development of chemistry and physics. He was able immediately to correct the atomic weight numbers of some elements, including uranium, whose atomic weight he found to be double that given at the time. Two years later Mendeleyev went so far as to give a detailed description of physical or chemical properties of some elements which were as yet undiscovered. Time gave striking proof of his predictions and his periodic law. Mendeleyev published his conclusions in the first place by sending, early in March 186 9, a leaflet to many Russian and foreign scientists. It gave his system of elements based on their atomic weights and chemical resemblance. On the 18th March that year his paper on the subject was read at the meeting of the Russian Chemical Society, and two months later the Society's Journal published his article entitled "The correlation between properties of elements and their atomic weight". -
DOCUMENT RESUME ED 071 911 SE 015 548 TITLE Project Physics
DOCUMENT RESUME ED 071 911 SE 015 548 TITLE Project Physics Teacher Guide 6, The Nucleus. INSTITUTION Harvard Univ., Cambridge, Mass. Harvard Project Physics. SPONS AGENCY Office of Education (DHEW) Washington, D.C. Bureau of Research. BUREAU NO BR-5-1038 PUB DATE 68 CONTRACT OEC-5-10-058 NOTE 235p.; Authorized Interim Version EDRS PRICE MF-$0.65 HC-S9.87 DESCRIPTORS Instructional Materials; *Multimedia Instruction; *Nuclear Physics; Physics; *Radiation; Science Activities; Secondary Grades; *Secondary School Science; *Teaching Glides; Teaching Procedures IDENTIFIERS Harvard Project Physics ABSTRACT Teaching procedures of Project Physics Unit 6are presented to help teachers make effectiveuse of learning materials. Unit contents are discussed in connection withteaching aid lists, multi-media schedules, schedule blocks, andresource charts. Brief summaries are made for transparencies, 16mm films, and reader articles. Included is information about the backgroundand development of each unit chapter, procedures in demonstrations, apparatus operations, notes on the student handbook, andan explanation of film loops. Additional articlesare concerned with objects dated by radiocarbon, radiation safety, propertiesof radiations, radioactive sources, radioactivity determinationby electroscopes, and radiation detecting devices.Scalers, counters, Geiger tubes, and cadmium selenide photocellsare analyzed; and a bibliography of references is given, Solutionsto the study guide are provided in detail, and answers to test itemsare suggested. The sixth unit of the text, with marginal commentson each section, is also compiled in the manual. The work of Harvard ProjectPhysics has . been financially supported by: the Carnegie Corporation ofNew York, the Ford Foundation, the National Science Foundation,the Alfred P. Sloan Foundation, the United States office of Education,and Harvard University. -
Summary of the Limited Reconnaissance Effort Regarding the Naturally Occurring Suspect Material at the Grand Canyon National Park
Summary of the Limited Reconnaissance Effort Regarding the Naturally Occurring Suspect Material at the Grand Canyon National Park Revision 1 Completed: July 18, 2000 Prepared by: Reginald Stewart, Health Physicist Mark Manllds:., fJ:ojcct Manager Arcadia Consulting, Inc. 456 Rocky Cliff Road Suite 100 Elizabeth, Colorado 80107 Prepared for: National Park Service Grand Canyon National Park Summary of the Limited Reconnaissance Effort NPS-GCNORMOOl Regarding the Naturally Occurring Suspect Revision 1 Material at the Grand Canyon National Park EXECUTIVE SUMMARY Arcadia Consulting, Inc., {Arcadia) personnel proceeded to the Grand Canyon National Park in Grand Canyon, Arizona with the assumption and understanding that the National Park Service {NPS) had an unspecified quantity of soil corings that potentially contained 3% of U-nat {naturally occurring Uranium). These materials were supposedly stored at the visitor's center, located on the South Rim of the Grand Canyon, for as long as 40 years. It was also understood there was a mining facility located within approximately 5 miles of the visitor's center, containing additional uranium ores and tailings. What was actually discovered were various igneous, metamorphic and sedimentary rock samples, located at multiple locations (the museum. the visitor center, the interpretation garage, and the "old warehouse"). These samples included unprocessed ore, semi processed ore with some yellowish residue, coring samples, and samples of materials in simple geological forms. Due to time limitations, the mine was not visited; therefore, no available data was gathered to make any conclusions regarding mill tailings. The project duration was approximately four days. During that period, Arcadia personnel performed radiological measurements, obtained all applicable documentation (with the assistance of the NPS), and contacted NPS personnel in order to characterize the radiological potentials.