Understanding Variation in Partition Coefficient, Kd, Values: Volume
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Tritium Handling and Safe Storage
NOT MEASUREMENT SENSITIVE DOE-HDBK-1129-2007 March 2007 ____________________ DOE HANDBOOK TRITIUM HANDLING AND SAFE STORAGE U.S. Department of Energy AREA SAFT Washington, D.C. 20585 DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. DOE-HDBK-1129-2007 This page is intentionally blank. ii DOE-HDBK-1129-2007 TABLE OF CONTENTS SECTION PAGE FOREWORD............................................................................................................................... vii ACRONYMS ................................................................................................................................ ix 1.0 INTRODUCTION ....................................................................................................................1 1.1 Purpose ...............................................................................................................................1 1.2 Scope ..................................................................................................................................1 1.3 Applicability .........................................................................................................................1 1.4 Referenced Material for Further Information .......................................................................2 2.0 TRITIUM .................................................................................................................................3 2.1 Radioactive Properties ........................................................................................................4 -
Geochemistry - (2021-2022 Catalog) 1
Geochemistry - (2021-2022 Catalog) 1 GEGN586 NUMERICAL MODELING OF GEOCHEMICAL 3.0 Geochemistry SYSTEMS GEOL512 MINERALOGY AND CRYSTAL CHEMISTRY 3.0 Degrees Offered GEOL513 HYDROTHERMAL GEOCHEMISTRY 3.0 • Master of Science (Geochemistry) GEOL523 REFLECTED LIGHT AND ELECTRON 2.0 MICROSCOPY * • Doctor of Philosophy (Geochemistry) GEOL535 LITHO ORE FORMING PROCESSES 1.0 • Certificate in Analytical Geochemistry GEOL540 ISOTOPE GEOCHEMISTRY AND 3.0 • Professional Masters in Analytical Geochemistry (non-thesis) GEOCHRONOLOGY • Professional Masters in Environmental Geochemistry (non-thesis) GEGN530 CLAY CHARACTERIZATION 2.0 Program Description GEGX571 GEOCHEMICAL EXPLORATION 3.0 The Graduate Program in Geochemistry is an interdisciplinary program * Students can add one additional credit of independent study with the mission to educate students whose interests lie at the (GEOL599) for XRF methods which is taken concurrently with intersection of the geological and chemical sciences. The Geochemistry GEOL523. Program consists of two subprograms, administering two M.S. and Ph.D. degree tracks, two Professional Master's (non-thesis) degree programs, Master of Science (Geochemistry degree track) students must also and a Graduate Certificate. The Geochemistry (GC) degree track pertains complete an appropriate thesis, based upon original research they have to the history and evolution of the Earth and its features, including but not conducted. A thesis proposal and course of study must be approved by limited to the chemical evolution of the crust and -
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. -
Organic Geochemistry
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by ZENODO Organic Geochemistry Organic Geochemistry 37 (2006) 1–11 www.elsevier.com/locate/orggeochem Review Organic geochemistry – A retrospective of its first 70 years q Keith A. Kvenvolden * U.S. Geological Survey, 345 Middlefield Road, MS 999, Menlo Park, CA 94025, USA Institute of Marine Sciences, University of California, Santa Cruz, CA 95064, USA Received 1 September 2005; accepted 1 September 2005 Available online 18 October 2005 Abstract Organic geochemistry had its origin in the early part of the 20th century when organic chemists and geologists realized that detailed information on the organic materials in sediments and rocks was scientifically interesting and of practical importance. The generally acknowledged ‘‘father’’ of organic geochemistry is Alfred E. Treibs (1899–1983), who discov- ered and described, in 1936, porphyrin pigments in shale, coal, and crude oil, and traced the source of these molecules to their biological precursors. Thus, the year 1936 marks the beginning of organic geochemistry. However, formal organiza- tion of organic geochemistry dates from 1959 when the Organic Geochemistry Division (OGD) of The Geochemical Soci- ety was founded in the United States, followed 22 years later (1981) by the establishment of the European Association of Organic Geochemists (EAOG). Organic geochemistry (1) has its own journal, Organic Geochemistry (beginning in 1979) which, since 1988, is the official journal of the EAOG, (2) convenes two major conferences [International Meeting on Organic Geochemistry (IMOG), since 1962, and Gordon Research Conferences on Organic Geochemistry (GRC), since 1968] in alternate years, and (3) is the subject matter of several textbooks. -
W. M. White Geochemistry Chapter 5: Kinetics
W. M. White Geochemistry Chapter 5: Kinetics CHAPTER 5: KINETICS: THE PACE OF THINGS 5.1 INTRODUCTION hermodynamics concerns itself with the distribution of components among the various phases and species of a system at equilibrium. Kinetics concerns itself with the path the system takes in T achieving equilibrium. Thermodynamics allows us to predict the equilibrium state of a system. Kinetics, on the other hand, tells us how and how fast equilibrium will be attained. Although thermo- dynamics is a macroscopic science, we found it often useful to consider the microscopic viewpoint in developing thermodynamics models. Because kinetics concerns itself with the path a system takes, what we will call reaction mechanisms, the microscopic perspective becomes essential, and we will very often make use of it. Our everyday experience tells one very important thing about reaction kinetics: they are generally slow at low temperature and become faster at higher temperature. For example, sugar dissolves much more rapidly in hot tea than it does in ice tea. Good instructions for making ice tea might then incor- porate this knowledge of kinetics and include the instruction to be sure to dissolve the sugar in the hot tea before pouring it over ice. Because of this temperature dependence of reaction rates, low tempera- ture geochemical systems are often not in equilibrium. A good example might be clastic sediments, which consist of a variety of phases. Some of these phases are in equilibrium with each other and with porewater, but most are not. Another example of this disequilibrium is the oceans. The surface waters of the oceans are everywhere oversaturated with respect to calcite, yet calcite precipitates from sea- water only through biological activity. -
The Role of Geochemistry and Stress on Fracture Development And
Geothermal Technologies Program 2010 Peer Review Public Service of Colorado Ponnequin Wind Farm The Role of Geochemistry and Principal Investigator (Joseph Moore) Stress on Fracture Development Presenter Name (John McLennan) and Proppant Behavior in EGS Organization University of Utah Reservoirs Track Name Reservoir Characterization May 18, 2010 This presentation does not contain any proprietary confidential,1 | US DOE or Geothermalotherwise restricted Program information. eere.energy.gov Timeline DOE Start Date:9/30/2008 DOE Contract Signed: 9/26/2008 Ends 11/30/2011 Project ~40% Complete 2 | US DOE Geothermal Program eere.energy.gov Budget Overview DOE Awardee Total Share Share Project $972,751 $243,188 $1,215,939 Funding FY 2009 $244,869 $107,130 $351,999 FY 2010 $383,952 $64,522 $448,474 FY 2011 $343,930 $71,536 $415,466 DOE Start Date:9/30/2008 DOE Contract Signed: 9/26/2008 Ends 11/30/2011 Project ~40% Complete 3 | US DOE Geothermal Program eere.energy.gov Overview: Barriers and Partners . Barriers to EGS Reservoir Development Addressed: . Reservoir Creation . Long-Term Reservoir and Fracture Sustainability . Zonal Isolation . Partners . Independent Evaluation 4 | US DOE Geothermal Program eere.energy.gov Relevance/Impact of Research Problem . Maximizing initial conductivity of EGS domains . Maintaining long-term conductivity . Facilitate development of extensive stimulated domain via diversion Solution . Proppant placed in fractures Challenge . Proppant behavior at geothermal conditions poorly understood Use of proppant recognized as potential technology under Task “Keep Flow Paths Open” in DOE EGS Technology Evaluation Report 5 | US DOE Geothermal Program eere.energy.gov Relevance/Impact of Research OBJECTIVE Develop Improved Methods For Maintaining Permeable Fracture Volumes In EGS Reservoirs . -
Tritium and Enriched Uranium Management Plan Through 2060
U.S. DEPARTMENT OF ENERGY Tritium And Enriched Uranium Management Plan Through 2060 Report to Congress October 2015 United States Department of Energy Washington, DC 20585 Message from the Secretary Please find the Department of Energy's plan for management oftritium and enriched uranium 1 inventories through 2060. This report is being provided to the following Members of Congress: • The Honorable Thad Cochran Chairman, Senate Committee on Appropriations • The Honorable Barbara Mikulski Ranking Member, Senate Committee on Appropriations • The Honorable Harold Rogers Chairman, House Committee on Appropriations • The Honorable Nita M. Lowey Ranking Member, House Committee on Appropriations • The Honorable Lamar Alexander Chairman, Subcommittee on Energy and Water Development Senate Committee on Appropriations • The Honorable Dianne Feinstein Ranking Member, Subcommittee on Energy and Water Development Senate Committee on Appropriations • The Honorable Mike Simpson Chairman, Subcommittee on Energy and Water Development House Committee on Appropriations • The Honorable Marcy Kaptur Ranking Member, Subcommittee on Energy and Water Development House Committee on Appropriations If you have any questions or need additional information, please contact me or Mr. Brad Crowell, Assistant Secretary for Congressional and Intergovernmental Affairs, at (202) 586-5450. Sincerely, 1 In response to Title Ill, Division D, Section 311 of the Consolidated Appropriations Act, 2014 (Pub. l. 113-76), and other Congressionalanguage l listed In Appendix B Department of Energy I October 2015 Executive Summary The Department of Energy's National Nuclear Security Administration (DOE/NNSA) is responsible for a number of national missions that require a reliable supply of Enriched Uranium (EU) to meet our defense and non-defense related missions. -
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. -
The Radiochemistry of Tungsten
National Academy of Sciences !National Research Council NUCLEAR SCIENCE SERIES The Radiochemistry of Tungsten — ...—- L. F. C URTISS,Chairman ROBLEY D. EVANS, Vice Chairman NationalBureau ofStandards MassachusettsInstituteofTechnology J.A. DeJUREN, Secretary WestinghouseElectricCorporation C. J.BORKOWSKI J.W. IRVINE,JR. Oak RidgeNationalLaboratory MassachusettsI&tituteofTechnology ROBERT G. COCHRAN E. D. KLEMA Texas Agriculturaland Mechanical NorthwesternUniversity College W. WAYNE MEINKE SAMUEL EPSTEIN UniversityofMichigan CaliforniaInstituteofTechnology J.J.NICKSON Memorial Hospital,New York U. FANO NationalBureau ofStandards ROBERT L. PLATZMAN Laboratoirede Chimie Physique HERBERT GOLDSTEIN NuclearDevelopmentCorporationof D. M. VAN PATTER America BartolResearch Foundation LIAISON MEMBERS PAUL C. AEBERSOLD CHARLES K. REED Atomic Energy Commission U. S.Air Force J.HOWARD McMILLEN WILLIAM E. WRIGHT NationalScienceFoundation OfficeofNavalResearch SUBCOMMITTEE ON RADIOCHEMISTRY W. WAYNE MEINKE, Chai~man HAROLD KIRBY UniversityofMichigan Mound Laboratory GREGORY R. CHOPPIN GEORGE LEDDICOTTE FloridaStateUniversity Oak RidgeNationalLaboratory GEORGE A. COWAN JULIAN NIELSEN Los Alamos ScientificLaboratory HanfordLaboratories ARTHUR W. FAIRHALL ELLIS P. STEINBERG UniversityofWashington Argonne NationalLaboratory JEROME HUDIS PETER C. STEVENSON BrookhavenNationalLaboratory UniversityofCalifornia(Livermore) EARL HYDE LEO YAFFE UniversityofC slifornia(Berkeley) McGillUniversity CONSULTANTS NATHAN BALLOU JAMES DeVOE NavalRadiologicalDefenseLaboratory -
OMB Control No.: 3150-0011 UNITED STATES NUCLEAR REGULATORY
OMB Control No.: 3150-0011 UNITED STATES NUCLEAR REGULATORY COMMISSION OFFICE OF NUCLEAR MATERIAL SAFETY AND SAFEGUARDS OFFICE OF NUCLEAR REACTOR REGULATION Washington, D.C. 20555-0001 October 8, 2003 NRC BULLETIN 2003-04: REBASELINING OF DATA IN THE NUCLEAR MATERIALS MANAGEMENT AND SAFEGUARDS SYSTEM Addressees All U.S. Nuclear Regulatory Commission (NRC) licensees, Agreement State licensees, and Certificate Holders (hereafter referred to as licensees) who: (1) Have in their possession, or are licensed to possess, one or more of the following: foreign obligated natural uranium, depleted uranium, or thorium; uranium enriched in the isotope U-235, U-233, plutonium, plutonium-238, or who currently have unreconciled nuclear material balances with the Nuclear Materials Management and Safeguards System (NMMSS). Purpose NRC is issuing this bulletin to: (i) Notify licensees about performance concerns associated with their reporting data to, and the resulting material balances contained in, the NMMSS database; (ii) Request affected licensees to perform a one-time reporting of the quantities of special nuclear material (SNM) and/or foreign obligated source material in their possession, specified as: (a) A quantity of SNM defined by 10 CFR 72.76, 72.78, 74.15, and 150.16, as 1 gram or more of contained uranium-235, uranium-233, plutonium, or 0.1 gram or more plutonium-238 that is greater than 10 percent of the total plutonium by weight; or (b) A quantity of foreign obligated source material (i.e., natural uranium, depleted uranium, or thorium) defined -
EPA Facts About Tritium
. p;RU:,,EPA Facts About V Tritium "~'I4C AD31 /'July 2002 What is Tritium? to the early 1960s. The inventory of tritium in the atmosphere peaked in 1963 and has been decreasing Tritium is a form of hydrogcn that is radioactive. and rapidly since then. Levels of naturally occurring tritium in like hydrogen it reacts with oxygen to form water. the atmosphere produced by cosmic rays arc constant, Tritium is produced naturally in the upper atmosphere and it is projected that levels or manmade tritium will be when cosmic rays strike atmospheric gases. Tritium comparable to natural tritium by 2030. can also be produced by man during nuclear weapon explosions, in reactors intended to produce tritium for Tritium is currently produced by reactors producing nuclear weapons. and by reactors producing electricity. However, releases of tritium from these electricity. facilities are at fractions of the natural background production rates. Other sources of tritium include government plants which have reprocessed reactor fuels. Individuals can also be exposed to tritium broken exit What arc the uses of tritium? signs and luminous dial items that contain tritium. Since tritium reacts similarly to ordinary hydrogen it is Tritium has been produced in large quantities by the incorporated into the body easily in the form of water. nuclear military program. It is also used to make luminous dials and as a source of light for sarety signs. Tritium is Overall, since current world wide levels of tritium in the used as a tracer for biochemical research, animal environment from man-made and natural sources are low, metabolism studies and ground water transport the risk to the average person from tritium is typically not measurements.