Iranian Chemical Isotope Exchange Research: Boron, Lithium, Uranium
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The Taming of “49” Big Science in Little Time
The Taming of “49” Big science in little time Recollections of Edward F. Hammel During the Manhattan Project, plutonium was often referred to, simply, as 49. Number 4 was for the last digit in 94 (the atomic number of plutonium) and 9 for the last digit in plutonium-239, the isotope of choice for nuclear weapons. The story that unfolds was adapted from Plutonium Metallurgy at Los Alamos, 1943–1945, as Edward F. Hammel remembers the events of those years. 48 Los Alamos Science Number 26 2000 The Taming of “49” he work in plutonium chemistry tion work was an inevitable conse- the metal could be fabricated into and metallurgy carried out at quence of the nuclear and physical satisfactory weapon components. TLos Alamos (Site Y) between research that was still to be conducted In addition, not until January 1944 1943 and 1945 had a somewhat contro- on the metal. It would clearly have did the first few milligrams of pile- versial history. The controversy was been inefficient and time consuming to produced plutonium arrive at Los about who was going to do what. ship small amounts of plutonium metal Alamos. The first 1-gram shipment At the time Los Alamos was being back to Chicago for repurification and arrived in February 1944, and quantity organized, most of the expertise in plu- refabrication into different sizes and shipments of plutonium did not begin to tonium chemistry resided at Berkeley, shapes for the next-scheduled nuclear arrive at Los Alamos until May 1945. where plutonium was discovered in physics experiment. From the outset, it was clear that the December 1940, and at the Met Lab in Minimizing the time spent to solve purification of plutonium was the most Chicago. -
Laser Isotope Separation (LIS), Technical and Economic
NASA TECHNICAL MEMORANDUM A STATUS OF PROGRESS FOR THL LASER lsofopE SEPARATION (11 SI PROCESS +tear 1976 NASA George C. Mdr~bdlSpace Flight Center Marshdl Space Fb$t Center, Alabama lLSFC - Form 3190 (Rev June 1971) REPORT STANDARD TITLE PACE I nEPMTn0. 3. RECIPIENT*$ CATILOC NO. NASA TM X-73345 10 TITLE UO SUTlTLt IS. REPORT DATE I September A st.tUaof for Iaser isotOpe ¶tian lS76 I Progress the (LIS) 6 PERFWYIIIG WGUIZATIO* CQOE George C. M8ralmll!3gam Flight Center I 1. COUTRUT OR am yo. I MarW Flight Center, Alabama 35812 Tecbnid Memormdum National Aemutics and Space Administration Washingtan, D.C. 20546 I I Prepared by Systems Aaalysis and Integration Iaboratory, Science and Engineering An overview of the various categories of the LE3 methodology is given together with illustrations showing a simplified version of the LIS tecbnique, an example of the two-phoiin photoionization category, and a diagram depicting how the energy levels of various isdope influence the LIS process. A&icatlons have been proposed for the LIS system which, in addition to the use to enrich uranium, could in themselves develop into programs of tremendous scope and breadth. Such applications as treatment of radioac '--ewastes from light-water nKzlear reactors, enriching the deuterlum isotope to make heavv-water, and enrlchhg tik light isotopes of such 17 KEt WORDS 18. DISTRIBUTION STATEMENT 5ECUQlTY CLASSIF. Ff thh PI*) 21 NO. OF PAbFS 22 PRICE Unclassified Unclassified I 20 NTIS PREFACE Since the publication of t& first Techid hiemomxitun (TM X-64947) on the Laser hotope Separation (LE)process in May 1975 [l], there bbeen a virtual explosion of available information on this process. -
Extensive Interest in Nuclear Fuel Cycle Technologies
Institute for Science and International Security ISIS REPORT March 19, 2012 Department 70 and the Physics Research Center: Extensive Interest in Nuclear Fuel Cycle Technologies By David Albright, Paul Brannan, Mark Gorwitz, and Andrew Ortendahl On February 23, 2012, ISIS released the report, The Physics Research Center and Iran’s Parallel Military Nuclear Program, in which ISIS evaluated a set of 1,600 telexes outlining a set of departments or buying centers of the former Physics Research Center (PHRC). These departments appeared to be purchasing a variety of goods for specific nuclear technologies, including gas centrifuges, uranium conversion, uranium exploration and perhaps mining, and heavy water production. Figure 1 is a list of the purposes of these departments. The telexes are evaluated in more depth in the February 23, 2012 ISIS report and support that, contrary to Iran’s statements to the International Atomic Energy Agency (IAEA), the PHRC ran a parallel military nuclear program in the 1990s. In the telexes, ISIS identified a department called Department 70 that is linked to the PHRC. This department tried to procure or obtained technical publications and reports from a document center, relevant know-how from suppliers, catalogues from suppliers about particular goods, and a mini- computer from the Digital Equipment Corporation. Department 70 appears to have had personnel highly knowledgeable about the existing literature on a variety of fuel cycle technologies, particularly gas centrifuges. Orders to a British document center reveal many technical publications about gas centrifuges, atomic laser isotope enrichment, the production of uranium compounds including uranium tetrafluoride and uranium hexafluoride (and precursors such as hydrofluoric acid), nuclear grade graphite, and the production of heavy water. -
The Lithium, Boron and Beryllium Content Of
Published in Geochimica et Cosmochimica Acta 72, issue 22, 5475-5504, 2008 1 which should be used for any reference to this work The Lithium, Boron and Beryllium content of serpentinized peridotites from ODP Leg 209 (Sites 1272A and 1274A): Implications for lithium and boron budgets of oceanic lithosphere Flurin Vils a,*, Laure Pelletier a, Angelika Kalt a, Othmar Mu¨ntener b, Thomas Ludwig c a Institut de Ge´ologie et d’Hydroge´ologie, Universite´ de Neuchaˆtel, Rue Emile-Argand 11, CP 158, CH-2009 Neuchaˆtel, Switzerland b Institut de Mine´ralogie et Ge´ochimie, Universite´ de Lausanne, Anthropole, CH-1015 Lausanne, Switzerland c Mineralogisches Institut, Ruprecht-Karls-Universita¨t Heidelberg, Im Neuenheimer Feld 236, D-69120 Heidelberg, Germany Abstract Despite the key importance of altered oceanic mantle as a repository and carrier of light elements (B, Li, and Be) to depth, its inventory of these elements has hardly been explored and quantified. In order to constrain the systematics and budget of these elements we have studied samples of highly serpentinized (>50%) spinel harzburgite drilled at the Mid-Atlantic Ridge (Fifteen– Twenty Fracture zone, ODP Leg 209, Sites 1272A and 1274A). In-situ analysis by secondary ion mass spectrometry reveals that the B, Li and Be contents of mantle minerals (olivine, orthopyroxene, and clinopyroxene) remain unchanged during serpent- inization. B and Li abundances largely correspond to those of unaltered mantle minerals whereas Be is close to the detection limit. The Li contents of clinopyroxene are slightly higher (0.44–2.8 lggÀ1) compared to unaltered mantle clinopyroxene, and olivine and clinopyroxene show an inverse Li partitioning compared to literature data. -
Atomic Spectra of Alkali Elements
Atomic Spectra of Alkali Elements S. R. Kulkarni April 10, 2020 Rydberg primarily focused on studying the lines of alkali metals (Lithium, Potassium and Sodium).1 Rydberg organized the various features by their appearance on the pho- tographs:The alkali spectra were more complicated than that of hydrogen. Rydberg recog- nized that were three different types of lines: lines which looked \sharp" (on photographic plates), \principal" (strong lines that showed up in emission and absorption) and those which appeared ‘diffuse”. These series were abbreviated to S, P, D. Later \Fundamental" (F) was added. As noted earlier, Rydberg preferred to work with wavenumbers. Using data from Liveing and Deware he recast Angstrom's formula as follows: N k = k − (1) n 1 (n + µ)2 where kn is the wavenumber of the nth line in a given series. Rydberg kept N fixed to the value measured by Balmer with k1 µ being free parameters. Rydberg found the following formulae for Lithium R ks = ks − ; 2; 3; 4; ::: (2) n 1 (n + S)2 R kp = kp − 1; 2; 3; ::: (3) n 1 (n + P )2 R kd = kd − 2; 3; 4; ::: (4) n 1 (n + D)2 s −1 p −1 where S = 0:5951, P = 0:9596, D = 0:9974, k1 = 28601:6 cm k1 = 43487:7 cm , d −1 k1 = 28598:5 cm and we have switched to the modern notation in which N is replaced by R (the value he found was R = 109721:6 cm−1). Rydberg had confidence in the data that he was able to find a deeper connection between the constants between the series. -
Silver Conductive Grease, Boron Nitride Heat Sink Grease, Silicone Free Heat Sink Grease
Silver Conductive Grease, Boron Nitride Heat Sink Grease, Silicone Free Heat Sink Grease Description CircuitWorks® Conductive Grease, otherwise known as thermal greases, thermal gel, thermal compound, thermal paste, heat paste, heat sink paste or heat sink compound, are conveniently packaged in syringes for fast and easy application, and to reduce mess and wastage. The range covers a number of electronic production, rework and repair applications. We offer three types of conductive grease: Silver Conductive Grease Boron Nitride Heat Sink Grease Silicone Free Heat Sink Grease Features & Benefits RoHS compliant Conveniently packaged to reduce waste and mess Silicone free option available compound will not harden or dry out Excellent thermal conductivity Silver Conductive Grease The CIR CW7100 CircuitWorks® syringe dispenser for precise application of grease to provide Silver Conductive Grease, Boron Nitride Heat Sink Grease, Silicone Free Heat Sink Grease superior electrical and thermal conductivity, lubrication and protection. Maximum electrical and thermal conductivity Protects against moisture and corrosion Thermally stable over a wide temperature range Conductive lubricant containing pure silver Fills connector gaps to maximize electrical and thermal conductivity Controls static discharge Grounds circuits Typical Applications Lubrication of substation switches or circuit breakers Heat dissipation from transformers Low or medium speed sliding contacts Static grounding on seals or O-rings Extending the life of rotating switches Specifications -
Helium Adsorption on Lithium Substrates
JLowTempPhys DOI 10.1007/s10909-007-9516-5 Helium Adsorption on Lithium Substrates E. Van Cleve · P. Taborek · J.E. Rutledge Received: 25 July 2007 / Accepted: 13 September 2007 © Springer Science+Business Media 2007 Abstract We have developed a cryogenic pulsed laser deposition (PLD) system to deposit lithium films onto a quartz crystal microbalance (QCM) at 4 K. Adsorption isotherms of 4He on lithium were measured in the temperature range between 1.42 K and 2.5 K. The isotherms are qualitatively different from isotherms on strong sub- strates such as gold and weak substrates such as cesium. There is no evidence of the formation of solid-like layers of helium, and the helium coverage is approximately linear in the pressure over a wide range. By measuring the low coverage slope of the isotherms, the binding energy of helium to lithium was found to be approxi- mately −13.6 K. For lithium substrates less than approximately 100 layers thick, the chemical potential at which the superfluid transition was observed was surprisingly sensitive to the details of lithium deposition. Keywords Helium films · Pulsed laser deposition · Superfluidity · Alkali metal 1 Introduction When helium is adsorbed onto a strong heterogenous substrate such as gold, the first 2 or 3 statistical layers are solid-like. The nature of these layers is not yet clear, but the layers are amorphous and do not participate significantly in superflow at high coverages. Superfluidity on strong substrates requires a minimum critical coverage to saturate the solid-like layers, and the superfluid phase which forms at higher cover- ages flows over these layers and does not interact directly with the strong, short range This work was supported by NSF grant DMR 0509685. -
Lithium Data Sheet
98 LITHIUM (Data in metric tons of lithium content unless otherwise noted) Domestic Production and Use: The only lithium production in the United States was from a brine operation in Nevada. Two companies produced a wide range of downstream lithium compounds in the United States from domestic or imported lithium carbonate, lithium chloride, and lithium hydroxide. Domestic production data were withheld to avoid disclosing company proprietary data. Although lithium markets vary by location, global end-use markets are estimated as follows: batteries, 65%; ceramics and glass, 18%; lubricating greases, 5%; polymer production, 3%; continuous casting mold flux powders, 3%; air treatment, 1%; and other uses, 5%. Lithium consumption for batteries has increased significantly in recent years because rechargeable lithium batteries are used extensively in the growing market for portable electronic devices and increasingly are used in electric tools, electric vehicles, and grid storage applications. Lithium minerals were used directly as ore concentrates in ceramics and glass applications. Salient Statistics—United States: 2015 2016 2017 2018 2019e Production W W W W W Imports for consumption 2,750 3,140 3,330 3,420 2,500 Exports 1,790 1,520 1,960 1,660 1,700 Consumption, estimated1 2,000 3,000 3,000 3,000 2,000 Price, annual average, battery-grade lithium carbonate, dollars per metric ton2 6,500 8,650 15,000 17,000 13,000 Employment, mine and mill, number 70 70 70 70 70 Net import reliance3 as a percentage of estimated consumption >25 >50 >50 >50 >25 Recycling: One domestic company has recycled lithium metal and lithium-ion batteries since 1992 at its facility in British Columbia, Canada. -
Of the Periodic Table
of the Periodic Table teacher notes Give your students a visual introduction to the families of the periodic table! This product includes eight mini- posters, one for each of the element families on the main group of the periodic table: Alkali Metals, Alkaline Earth Metals, Boron/Aluminum Group (Icosagens), Carbon Group (Crystallogens), Nitrogen Group (Pnictogens), Oxygen Group (Chalcogens), Halogens, and Noble Gases. The mini-posters give overview information about the family as well as a visual of where on the periodic table the family is located and a diagram of an atom of that family highlighting the number of valence electrons. Also included is the student packet, which is broken into the eight families and asks for specific information that students will find on the mini-posters. The students are also directed to color each family with a specific color on the blank graphic organizer at the end of their packet and they go to the fantastic interactive table at www.periodictable.com to learn even more about the elements in each family. Furthermore, there is a section for students to conduct their own research on the element of hydrogen, which does not belong to a family. When I use this activity, I print two of each mini-poster in color (pages 8 through 15 of this file), laminate them, and lay them on a big table. I have students work in partners to read about each family, one at a time, and complete that section of the student packet (pages 16 through 21 of this file). When they finish, they bring the mini-poster back to the table for another group to use. -
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 . -
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).