Technetium 1 Technetium
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Managing Terrorism Or Accidental Nuclear Errors, Preparing for Iodine-131 Emergencies: a Comprehensive Review
Int. J. Environ. Res. Public Health 2014, 11, 4158-4200; doi:10.3390/ijerph110404158 OPEN ACCESS International Journal of Environmental Research and Public Health ISSN 1660-4601 www.mdpi.com/journal/ijerph Review Managing Terrorism or Accidental Nuclear Errors, Preparing for Iodine-131 Emergencies: A Comprehensive Review Eric R. Braverman 1,2,3, Kenneth Blum 1,2,*, Bernard Loeffke 2, Robert Baker 4, 5, Florian Kreuk 2, Samantha Peiling Yang 6 and James R. Hurley 7 1 Department of Psychiatry, College of Medicine, University of Florida and McKnight Brain Institute, Gainesville, FL 32610, USA; E-Mail: [email protected] 2 Department of Clinical Neurology, PATH Foundation NY, New York, NY 10010, USA; E-Mails: [email protected] (B.L.); [email protected] (F.K.) 3 Department of Neurosurgery, Weill-Cornell Medical College, New York, NY 10065, USA 4 Department of Biological Sciences, Texas Tech University, Lubbock, TX 79409, USA; E-Mail: [email protected] 5 Natural Science Research Laboratory, Museum of Texas Tech University, Lubbock, TX 79409, USA 6 Department of Endocrinology, National University Hospital of Singapore, Singapore 119228; E-Mail: [email protected] 7 Department of Medicine, Weill Cornell Medical College, New York, NY 10065, USA; E-Mail: [email protected] * Author to whom correspondence should be addressed; E-Mail: [email protected]; Tel.: +1-646-367-7411 (ext. 123); Fax: +1-212-213-6188. Received: 5 February 2014; in revised form: 26 March 2014 / Accepted: 28 March 2014 / Published: 15 April 2014 Abstract: Chernobyl demonstrated that iodine-131 (131I) released in a nuclear accident can cause malignant thyroid nodules to develop in children within a 300 mile radius of the incident. -
Bioorganometallic Technetium and Rhenium Chemistry: Fundamentals for Applications
RadiochemistRy in switzeRland CHIMIA 2020, 74, No. 12 953 doi:10.2533/chimia.2020.953 Chimia 74 (2020) 953–959 © R. Alberto, H. Braband, Q. Nadeem Bioorganometallic Technetium and Rhenium Chemistry: Fundamentals for Applications Roger Alberto*, Henrik Braband, and Qaisar Nadeem Abstract: Due to its long half-life of 2.111×105 y, technetium, i.e. 99Tc, offers the excellent opportunity of combin- ing fundamental and ‘classical’ organometallic or coordination chemistry with all methodologies of radiochem- istry. Technetium chemistry is inspired by the applications of its short-lived metastable isomer 99mTc in molecular imaging and radiopharmacy. We present in this article examples about these contexts and the impact of purely basic oriented research on practical applications. This review shows how the chemistry of this element in the middle of the periodic system inspires the chemistry of neighboring elements such as rhenium. Reasons are given for the frequent observation that the chemistries of 99Tc and 99mTc are often not identical, i.e. compounds accessible for 99mTc, under certain conditions, are not accessible for 99Tc. The article emphasizes the importance of macroscopic technetium chemistry not only for research but also for advanced education in the general fields of radiochemistry. Keywords: Bioorganometallics · Molecular Imaging · Radiopharmacy · Rhenium · Technetium Roger Alberto obtained his PhD from the Qaisar Nadeem got his PhD from the ETH Zurich. He was an Alexander von University of the Punjab Lahore, Pakistan. Humboldt fellow in the group of W.A. He received the higher education commission Herrmann at the TU Munich and at the (HEC, Pakistan) fellowship during his PhD Los Alamos National Laboratory with and worked in theAlberto group, Department A Sattelberger. -
Technetium in the Geologic Environment a Literature Survey
Report Prav 4.28 TECHNETIUM IN THE GEOLOGIC ENVIRONMENT A LITERATURE SURVEY B Torstenfel t B Al lard K Andersson U Olofsson Department of Nuclear Chemistry Chalmers University of Technology Göteborg, Sweden July 1981 CONTENTS Page Introduction 1 The technetium metal 2 Technetiums redox properties and complexes 3 Oxidation state +VII 4 Oxidation states +VI and +V 7 Oxidation state +IV 7 Oxidation states +1 - +111 14 The accumulation of Tc in the Pood chain 14 The chemistry of Tc in connection with the final storage of spent nuclear fuel 15 Si'"otion of Tc in rock 15 - t tion of Tc in clay and soil 20 yjtion of Tc in sea bottom sediments 22 ?a "ption and migration of Tc in Oklo 22 /iferences 23 INTRODUCTION Technetium belongs to the transition metals in the second series of the d-grcup. It is a member of the VII B group together with manganese and rehnium.1»2'3'4.5 According to the common behaviour of the elements in the periodic system, Tc would have an electron structure of the outer shell like Mn and Re, given as 4d55s2 1, but Tc is one of the exceptions and, unlike Mn and Re, have the structure 4d653! (= supereiectron configuration of the krypton atom).2 This electron structure makes it possible for Tc to have VIII oxidation states,from +VII to -I. The most stable oxidation states are +VII, +IV and 01. Technetiums chemical properties is closer to rhenium than to manganese2-3'4-5. It is characterized by a weak tendency towards reduction, formation of slow-spin complexes and cluster compounds with low degree of oxidation2. -
Monitored Natural Attenuation of Inorganic Contaminants in Ground
Monitored Natural Attenuation of Inorganic Contaminants in Ground Water Volume 3 Assessment for Radionuclides Including Tritium, Radon, Strontium, Technetium, Uranium, Iodine, Radium, Thorium, Cesium, and Plutonium-Americium EPA/600/R-10/093 September 2010 Monitored Natural Attenuation of Inorganic Contaminants in Ground Water Volume 3 Assessment for Radionuclides Including Tritium, Radon, Strontium, Technetium, Uranium, Iodine, Radium, Thorium, Cesium, and Plutonium-Americium Edited by Robert G. Ford Land Remediation and Pollution Control Division Cincinnati, Ohio 45268 and Richard T. Wilkin Ground Water and Ecosystems Restoration Division Ada, Oklahoma 74820 Project Officer Robert G. Ford Land Remediation and Pollution Control Division Cincinnati, Ohio 45268 National Risk Management Research Laboratory Office of Research and Development U.S. Environmental Protection Agency Cincinnati, Ohio 45268 Notice The U.S. Environmental Protection Agency through its Office of Research and Development managed portions of the technical work described here under EPA Contract No. 68-C-02-092 to Dynamac Corporation, Ada, Oklahoma (David Burden, Project Officer) through funds provided by the U.S. Environmental Protection Agency’s Office of Air and Radiation and Office of Solid Waste and Emergency Response. It has been subjected to the Agency’s peer and administrative review and has been approved for publication as an EPA document. Mention of trade names or commercial products does not constitute endorsement or recommendation for use. All research projects making conclusions or recommendations based on environmental data and funded by the U.S. Environmental Protection Agency are required to participate in the Agency Quality Assurance Program. This project did not involve the collection or use of environmental data and, as such, did not require a Quality Assurance Plan. -
The Development of the Periodic Table and Its Consequences Citation: J
Firenze University Press www.fupress.com/substantia The Development of the Periodic Table and its Consequences Citation: J. Emsley (2019) The Devel- opment of the Periodic Table and its Consequences. Substantia 3(2) Suppl. 5: 15-27. doi: 10.13128/Substantia-297 John Emsley Copyright: © 2019 J. Emsley. This is Alameda Lodge, 23a Alameda Road, Ampthill, MK45 2LA, UK an open access, peer-reviewed article E-mail: [email protected] published by Firenze University Press (http://www.fupress.com/substantia) and distributed under the terms of the Abstract. Chemistry is fortunate among the sciences in having an icon that is instant- Creative Commons Attribution License, ly recognisable around the world: the periodic table. The United Nations has deemed which permits unrestricted use, distri- 2019 to be the International Year of the Periodic Table, in commemoration of the 150th bution, and reproduction in any medi- anniversary of the first paper in which it appeared. That had been written by a Russian um, provided the original author and chemist, Dmitri Mendeleev, and was published in May 1869. Since then, there have source are credited. been many versions of the table, but one format has come to be the most widely used Data Availability Statement: All rel- and is to be seen everywhere. The route to this preferred form of the table makes an evant data are within the paper and its interesting story. Supporting Information files. Keywords. Periodic table, Mendeleev, Newlands, Deming, Seaborg. Competing Interests: The Author(s) declare(s) no conflict of interest. INTRODUCTION There are hundreds of periodic tables but the one that is widely repro- duced has the approval of the International Union of Pure and Applied Chemistry (IUPAC) and is shown in Fig.1. -
Use of Radioactive Iodine As a Tracer in Water-Flooding Operations
. USE of RADIOACTIVE IODINE as a TRACER In WATER-FLOODING OPERATIONS Downloaded from http://onepetro.org/jpt/article-pdf/6/09/117/2237549/spe-349-g.pdf by guest on 27 September 2021 J. WADE WATKINS BUREAU OF MINES MEMBER AIME BARTLESVILLE, OKLA. E. S. MARDOCK WELL SURVEYS, INC. MEMBER AIME TULSA, OKLA. T. P. 3894 ABSTRACT assumed that the physical conditions in the productive formation are homogeneous. Unfortunately, homogen The accurate evaluation of reservoir-performance eous conditions rarely, if ever, exist in oil-productive characteristics in the secondary recovery of petroleum formations. The use of a tracer that may be injected by water flooding requires use of a water tracer that into an oil sand and detected quantitatively, or even may be injected into water-input wells and detected at qualitatively, at offsetting oil-production wells provides oil-production wells to supplement data obtained fronz basic data that may be used in determining more core analyses, wellhead tests, and subsurface measure accurately the subsurface rates and patterns of flow ments. Radioactive iodine has been used successfully of injected water between wells than is possible by as a water tracer in field tests to determine: (1) rela theoretical calculations based on assumed conditions. tive rates and patterns of flow of injected water between Consideration of the data obtained by using a water water-input and oil-production wells and (2) zones of tracer assists in the application of remedial measures excessive water entry into oil-production wells. to water-input wells, such as plugging of channels, or Laboratory evaluations of potential water tracers, selective plugging of highly permeable zones, thereby previous tracer studies, the value of using a radioactive effecting a more uniform flood and a greater ultimate tracer, general field procedures, and the use of surface oil recovery. -
DOE EA-2146 Final Environmental Assessment for the MARVEL
DOE/EA-2146 Final Environmental Assessment for the Microreactor Applications Research, Validation, and Evaluation (MARVEL) Project at Idaho National Laboratory June 2021 DOE/ID-2146 Final Environmental Assessment for the Microreactor Applications Research, Validation, and Evaluation (MARVEL) Project at Idaho National Laboratory June 2021 Prepared for the U.S. Department of Energy DOE Idaho Operations Office i i CONTENTS 1. INTRODUCTION .............................................................................................................................. 1 1.1 Background .............................................................................................................................. 1 1.2 Purpose and Need ..................................................................................................................... 1 2. ALTERNATIVES .............................................................................................................................. 2 2.1 Proposed Action - Microreactor Applications Research, Validation and Evaluation (MARVEL) Project .................................................................................................................. 3 2.1.1 Reactor Structure System ............................................................................................ 5 2.1.2 Secondary Containment Structure .............................................................................. 5 2.1.3 Core System ............................................................................................................... -
Geology of U Rani Urn Deposits in Triassic Rocks of the Colorado Plateau Region
Geology of U rani urn Deposits in Triassic Rocks of the Colorado Plateau Region By W. I. FINCH CONTRIBUTIONS TO THE GEOLOGY OF URANIUM GEOLOGICAL SURVEY BULLETIN 1074-D This report concerns work done on behalf ~1 the U. S. Atomic Energy Commission -Jnd is published with the permission of ~he Commission NITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1959 UNITED STATES DEPARTMENT OF THE INTERIOR FRED A. SEATON, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U. S. Government Printin~ Office Washin~ton 25, D. C. CONTENTS Page Abstract---------------------------------------------------------- 125 Introduction__ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ __ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ 125 History of mining and production ____ ------------------------------- 127 Geologic setting___________________________________________________ 128 StratigraphY-------------------------------------------------- 129 ~oenkopiformation_______________________________________ ~29 Middle Triassic unconformity_______________________________ 131 Chinle formation__________________________________________ 131 Shinarump Inernber____________________________________ 133 ~udstone member------------------------------------- 136 ~oss Back member____________________________________ 136 Upper part of the Chinle formation______________________ 138 Wingate sandstone_________________________________________ 138 lgneousrocks_________________________________________________ 139 Structure_____________________________________________________ -
Uranium Fact Sheet
Fact Sheet Adopted: December 2018 Health Physics Society Specialists in Radiation Safety 1 Uranium What is uranium? Uranium is a naturally occurring metallic element that has been present in the Earth’s crust since formation of the planet. Like many other minerals, uranium was deposited on land by volcanic action, dissolved by rainfall, and in some places, carried into underground formations. In some cases, geochemical conditions resulted in its concentration into “ore bodies.” Uranium is a common element in Earth’s crust (soil, rock) and in seawater and groundwater. Uranium has 92 protons in its nucleus. The isotope2 238U has 146 neutrons, for a total atomic weight of approximately 238, making it the highest atomic weight of any naturally occurring element. It is not the most dense of elements, but its density is almost twice that of lead. Uranium is radioactive and in nature has three primary isotopes with different numbers of neutrons. Natural uranium, 238U, constitutes over 99% of the total mass or weight, with 0.72% 235U, and a very small amount of 234U. An unstable nucleus that emits some form of radiation is defined as radioactive. The emitted radiation is called radioactivity, which in this case is ionizing radiation—meaning it can interact with other atoms to create charged atoms known as ions. Uranium emits alpha particles, which are ejected from the nucleus of the unstable uranium atom. When an atom emits radiation such as alpha or beta particles or photons such as x rays or gamma rays, the material is said to be undergoing radioactive decay (also called radioactive transformation). -
Spéciation Du Technétium En Milieu Acide : Effet Des Rayonnements Α Ibtihel Denden
Spéciation du technétium en milieu acide : effet des rayonnements α Ibtihel Denden To cite this version: Ibtihel Denden. Spéciation du technétium en milieu acide : effet des rayonnements α. Chimie théorique et/ou physique. Ecole des Mines de Nantes, 2013. Français. NNT : 2013EMNA0114. tel-00937594 HAL Id: tel-00937594 https://tel.archives-ouvertes.fr/tel-00937594 Submitted on 28 Jan 2014 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. Ibtihel Denden Mémoire présenté en vue de l’obtention du grade de Docteur de l’École Nationale Supérieure des Mines de Nantes sous le label de L’Université Nantes Angers Le Mans École doctorale : ED3MPL Discipline : Chimie Spécialité : Radiochimie Unité de recherche : Laboratoire SUBATECH, UMR 6457 Soutenue le 18 octobre 2013 Thèse N° : 2013EMNA0114 Spéciation du technétium en milieu acide : effet des rayonnements α JURY Rapporteurs : M. Philippe Moisy, Directeur de recherche, CEA, Marcoule. M. Frédéric Poineau, Professeur assistant de recherche, UNLV, Las Vegas. Examinateurs : M. Jacques Barbet, Directeur de recherche, CNRS, Université de Nantes. M. Laurent Vichot, Ingénieur de recherche, CEA, Valduc. Invité : M. Jérôme Roques, Maître de conférences, IPN, Orsay. Directeur de Thèse : M. Massoud Fattahi, Professeur, Université de Nantes. -
Paul Scherrer Institut
C^ZOOCt^ CO l 9 19 icht r r — — l-Be £3tobe I J Paul Scherrer Institut Labor für Werkstoffe und nukleare Verfahren Programm Entsorgung Chemistry of the Rectox Sensitive Elements Literature Review D.Suter Paul Scherrer Institut Telefon 056/99 2111 Würenlingen und Villigen Telex82 7414psich CH-5232 Villigen PSI Telefax 056/982327 PSI CH PSI-Bericht Nr. 113 Chemistry of the Redox Sensitive Elements Literature Review Daniel Suter Wiirenlingen and Villigen, October 1991 Preface In the framework of its Waste Management Programme the Paul Scherrer Institute is performing work to increase the understanding of radionuclide transport in the geosphere. These investigations arc performed in close cooperation with, and with the financial support of, NAGRA. The present report is issued simultaneously as a PSI report and a NAGRA NTB. TABLE OF CONTENTS Summary 2 Zusammenfassung 3 Resume 4 1. Introduction 5 2. Redox Conditions 8 3. Selenium 11 3.1 Solution Chemistry 11 3.2 Sorption Studies 13 3.3 Geochemistry 15 3.4 Experiments 18 3.5 Analytical Methods 20 4. Technetium 26 4.1 Solution Chemistry 26 4.2 Sorption Studies 29 4.3 Geochemistry 31 4.4 Experiments 32 4.5 Analytical Methods 33 5. Palladium 35 5.1 Solution Chemistry 35 5.2 Sorption Studies 36 5.3. Geochemistry 37 5.4 Experiments 38 5.5 Analytical Methods 39 6. Tin 42 6.1 Solution Chemistry 42 6.2 Sorption Studies 42 6.3 Geochemistry 43 6.4 Experiments 44 6.5 Analytical Methods 44 7. Neptunium 46 7.1 Solution Chemistry 46 7.2 Sorption Studies 48 7.3 Geochemistry 49 7.4 Experiments 51 7.5 Analytical Methods 51 8. -
2013 Heavy Element Chemistry and Separations Science Principal Investigators’ Meeting
2013 Heavy Element Chemistry and Separations Science Principal Investigators’ Meeting Gaithersburg, MD April 21–24, 2013 Office of Basic Energy Sciences (BES) Chemical Sciences, Geosciences, and Biosciences Division Program and Abstracts for the 2013 Heavy Element Chemistry and Separations Science Principal Investigators’ Meeting Gaithersburg Marriott Washingtonian Center Gaithersburg, MD April 21–24, 2013 Chemical Sciences, Geosciences, and Biosciences Division Office of Basic Energy Sciences Office of Science U.S. Department of Energy Cover art created with Wordle, a toy for generating “word clouds” from text using the Goudy Bookletter 1911 font. The text bodies from the abstracts contained in the following program were the basis of the word cloud. The research grants and contracts described in this document are, with the exception of the invited speakers, supported by the U.S. DOE Office of Science, Office of Basic Energy Sciences, Chemical Sciences, Geosciences, and Biosciences Division. DISCLAIMER This report is a compilation of accounts of work sponsored by an agency of the United States Government. Neither the United States government nor any agency thereof, nor any of their employees, makes any warranty, express or implied, or assumes any legal liability or 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 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. The views and opinions of authors expressed herein do not necessarily state or reflect those of the United States Government or any agency thereof.