Element by Element Review of Their Atomic Weights
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A Contribution to the Chemistry of Rhenium
U. S. DEPARTMENT OF COMMERCE NATIONAL BUREAU OF STANDARDS RESEARCH PAPER RP999 Part of Journal of Research of the J'Xational Bureau of Standards, Volume 18, May 1937 A CONTRIBUTION TO THE CHEMISTRY OF RHENIUM . By C. E. F. Lundell and H. B. Knowles ABSTRACT A study of the behavior of rhenium when dilute solutions of potassium per rhenate are acidified with sulphuric acid, cooled, and passed through the Jones reductor, indicates that rhenium forms a compound in which it has a valency of minus one, and that the rhenium in this compound is oxidized to a valency of plus one if the diluted sulphuric acid solution is protected from oxygen and warmed to approximately 50° C. In the course of the investigation, it was also found (1) that rhenium can be electrodeposited from diluted (5+95) sulphuric acid solution; (2) that deposits are slightly contaminated; and (3) that the deposited metal can be oxidized directly to perrhenic acid by exposure to moist air, oxygen, or by making the deposit the anode in a water solution. CONTENTS Page 1. Introduction ___ _____________________ ____ __ __ _____ ___ ___ _____ _____ 629 II. ExperimentaL _ ___ _ _ _ _ _ _ _ _ _ _ _ _ __ _ _ __ ___ _ _ _ _ _ __ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ 630 1. Reagents, reductor, and reductor technique ___________________ 630 2. Oxidation of the reduced compound _______________ ___________ 631 3. Potentiometric titrations _______________ ___ ___ ______ ___ _____ 634 4. -
The Radiochemistry of Beryllium
National Academy of Sciences National Research Council I NUCLEAR SCIENCE SERIES The Radiochemistry ·of Beryllium COMMITTEE ON NUCLEAR SCIENCE L. F. CURTISS, Chairman ROBLEY D. EVANS, Vice Chairman National Bureau of Standards MassaChusetts Institute of Technol0gy J. A. DeJUREN, Secretary ./Westinghouse Electric Corporation H.J. CURTIS G. G. MANOV Brookhaven National' LaboratOry Tracerlab, Inc. SAMUEL EPSTEIN W. WAYNE MEINKE CalUornia Institute of Technology University of Michigan HERBERT GOLDSTEIN A.H. SNELL Nuclear Development Corporation of , oak Ridge National Laboratory America E. A. UEHLING H.J. GOMBERG University of Washington University of Michigan D. M. VAN PATTER E.D.KLEMA Bartol Research Foundation Northwestern University ROBERT L. PLATZMAN Argonne National Laboratory LIAISON MEMBERS PAUL C .. AEBERSOLD W.D.URRY Atomic Energy Commission U. S. Air Force J. HOW ARD McMILLEN WILLIAM E. WRIGHT National Science Foundation Office of Naval Research SUBCOMMITTEE ON RADIOCHEMISTRY W. WAYNE MEINKE, Chairman HAROLD KIRBY University of Michigan Mound Laboratory GREGORY R. CHOPPIN GEORGE LEDDICOTTE Florida State University. Oak Ridge National Laboratory GEORGE A. COW AN JULIAN NIELSEN Los Alamos Scientific Laboratory Hanford Laboratories ARTHUR W. FAIRHALL ELLIS P. STEINBERG University of Washington Argonne National Laboratory JEROME HUDIS PETER C. STEVENSON Brookhaven National Laboratory University of California (Livermore) EARL HYDE LEO YAFFE University of CalUornia (Berkeley) McGill University CONSULTANTS NATHAN BALLOU WILLIAM MARLOW Naval Radiological Defense Laboratory N atlonal Bureau of Standards JAMESDeVOE University of Michigan CHF.MISTRY-RADIATION AND RADK>CHEMIST The Radiochemistry of Beryllium By A. W. FAIRHALL. Department of Chemistry University of Washington Seattle, Washington May 1960 ' Subcommittee on Radiochemistry National Academy of Sciences - National Research Council Printed in USA. -
Evolution and Understanding of the D-Block Elements in the Periodic Table Cite This: Dalton Trans., 2019, 48, 9408 Edwin C
Dalton Transactions View Article Online PERSPECTIVE View Journal | View Issue Evolution and understanding of the d-block elements in the periodic table Cite this: Dalton Trans., 2019, 48, 9408 Edwin C. Constable Received 20th February 2019, The d-block elements have played an essential role in the development of our present understanding of Accepted 6th March 2019 chemistry and in the evolution of the periodic table. On the occasion of the sesquicentenniel of the dis- DOI: 10.1039/c9dt00765b covery of the periodic table by Mendeleev, it is appropriate to look at how these metals have influenced rsc.li/dalton our understanding of periodicity and the relationships between elements. Introduction and periodic tables concerning objects as diverse as fruit, veg- etables, beer, cartoon characters, and superheroes abound in In the year 2019 we celebrate the sesquicentennial of the publi- our connected world.7 Creative Commons Attribution-NonCommercial 3.0 Unported Licence. cation of the first modern form of the periodic table by In the commonly encountered medium or long forms of Mendeleev (alternatively transliterated as Mendelejew, the periodic table, the central portion is occupied by the Mendelejeff, Mendeléeff, and Mendeléyev from the Cyrillic d-block elements, commonly known as the transition elements ).1 The periodic table lies at the core of our under- or transition metals. These elements have played a critical rôle standing of the properties of, and the relationships between, in our understanding of modern chemistry and have proved to the 118 elements currently known (Fig. 1).2 A chemist can look be the touchstones for many theories of valence and bonding. -
Midterm Examination #3, December 11, 2015 1. (10 Point
NAME: NITROMETHANE CHEMISTRY 443, Fall, 2015(15F) Section Number: 10 Midterm Examination #3, December 11, 2015 Answer each question in the space provided; use back of page if extra space is needed. Answer questions so the grader can READILY understand your work; only work on the exam sheet will be considered. Write answers, where appropriate, with reasonable numbers of significant figures. You may use only the "Student Handbook," a calculator, and a straight edge. 1. (10 points) Argon is a noble gas. For all practical purposes it can be considered an ideal gas. DO NOT WRITE Calculate the change in molar entropy of argon when it is subjected to a process in which the molar IN THIS SPACE volume is tripled and the temperature is simultaneously changed from 300 K to 400 K. 1,2 _______/25 This is a straightforward application of thermodynamics: 3,4 _______/25 = = + = + 2 2 2 2 5 _______/20 Identifying ∆the derivative� and� doing1 � the� integrals � 1give� � �1 � � �1 3 3 400 6,7 _______/20 = + = 8.3144349 + 8.3144349 2 2 1 2 300 8 _______/10 where the∆ heat capacity � 1� at constant � 1volume� of a monatomic �ideal� gas is� . � � � 3 ============= = 9.13434 + 3.58786 = 12.722202 9 _______/5 ∆ (Extra credit) ============= TOTAL PTS 2. (15 points) Benzene ( • = 96.4 ) and toluene ( • = 28.9 ) form a nearly ideal solution over a wide range. For purposes of this question, you may assume that a solution of the two is ideal. (a) What is the total vapor pressure above a solution containing 5.00 moles of benzene and 3.25 moles of toluene? 5.00 3.25 = • + • = (96.4 ) + (28.9 ) 5.00 + 3.25 5.00 + 3.25 = 58.4 + 11.4 = 69.8 (b) What is mole fraction of benzene in the vapor above this solution? . -
Unit 1Moles and Equations
Cambridge University Press 978-1-107-61665-3 – Cambridge International AS and A Level Chemistry Judith Potter Peter Cann Excerpt More information Moles and equations Unit 1 Learning outcomes You should be able to: defi ne and use the terms empirical and molecular formulae and use experimental data defi ne and use relative masses based on the to fi nd them, 12C scale write and construct equations and use them in defi ne and use the mole and Avogadro’s performing mole calculations constant perform mole calculations involving solutions analyse simple mass spectra and use the data in and gases, relative atomic mass calculations This unit gathers together the basic chemistry relative isotopic mass = calculations. You may need to refer to it as you revise mass of one atom of the isotope other topics in later units. (1/12) of the mass of one atom of 12C Relative masses are a ratio of two masses and have 1.01 Relative masses no units. An atom is the smallest part of an element that can exist and still retain the identity of the element. A 1.02 The mole and the molecule is a group of atoms bonded together and the smallest portion of an element or compound that can Avogadro constant exist alone. A simple ion is an atom which has lost or To give an easy measurement of mass, a number of gained one or more electrons. Atoms, molecules and atoms is chosen so that their combined mass is equal to ions are so small that their masses are far too small the relative atomic mass in grams. -
|||||||||||||III USOO5302369A United States Patent (19) (11) Patent Number: 5,302,369 Day Et Al
|||||||||||||III USOO5302369A United States Patent (19) (11) Patent Number: 5,302,369 Day et al. (45) Date of Patent: k Apr.p 12, 1994 (54) MERSHERES FOR RADIATION OTHER PUBLICATIONS RAPY Makishima et al., "Elastic Moduli and Refractive Indi (75) Inventors: Delbert E. Day, Rolla; Gary J. ces of Aluminosilicate Glasses Containing Y2O3, La2O3, Ehrhardt, Columbia, both of Mo. and TiO2'; Journal of the American Ceramic Society; 73) Assignee: The Curators of the University of vol. 61, pp. 247-249; May-Jun. 1978. Missouri, Columbia, Mo. Loehman, "Preparation and Properties of Yttri (*) Notice: The portion of the term of this patent um-Silicon-Aluinum Oxynitride Glasses"; Journal of subsequent to Dec. 6, 2005 has been the American Ceramic Society; vol. 62, pp. 491-494; disclaimed. Sep.-Oct. 1979. Makishima, et al., “Alkaline Durability of High Elastic R21 Appl.pp No.:O 751,721 Modulus Alumino-Silicatey s Glasses Containing Y2O3, (22 Filed: Aug. 29, 1991 La2O3 and TiO2'; Journal of Non-Crystalline Solids 38 & 39, pp. 661-666 (1980). Related U.S. Application Data Bonder, et al., "Phase Equilibria in the System Y2O (63) Stylist Ser. No. 280,005, FS, 59. al 3-Al2O3-SiO2'; I. V. Grebenschikov Institute of Sili Oe W1c is a contation o er. O. is aws's cate Chemistry, Academy of Sciences, USSR, trans Nov. 19, 1984, Pat. No. 4,789,501. lated from Izvestiya Akademii Nauk USSR, Seriya 51 int. Cl. ....................... A61K 43/00; A61N 5/00; Khimicheskaya, No. 7, pp. 1325-1326, Jul. 1964. CO3C 3/095; CO3C 3/097 52 U.S. -
The Periodic Table of Elements
The Periodic Table of Elements 1 2 6 Atomic Number = Number of Protons = Number of Electrons HYDROGENH HELIUMHe 1 Chemical Symbol NON-METALS 4 3 4 C 5 6 7 8 9 10 Li Be CARBON Chemical Name B C N O F Ne LITHIUM BERYLLIUM = Number of Protons + Number of Neutrons* BORON CARBON NITROGEN OXYGEN FLUORINE NEON 7 9 12 Atomic Weight 11 12 14 16 19 20 11 12 13 14 15 16 17 18 SODIUMNa MAGNESIUMMg ALUMINUMAl SILICONSi PHOSPHORUSP SULFURS CHLORINECl ARGONAr 23 24 METALS 27 28 31 32 35 40 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 POTASSIUMK CALCIUMCa SCANDIUMSc TITANIUMTi VANADIUMV CHROMIUMCr MANGANESEMn FeIRON COBALTCo NICKELNi CuCOPPER ZnZINC GALLIUMGa GERMANIUMGe ARSENICAs SELENIUMSe BROMINEBr KRYPTONKr 39 40 45 48 51 52 55 56 59 59 64 65 70 73 75 79 80 84 37 38 39 40 41 42 43 44 45 46 47 48 49 50 51 52 53 54 RUBIDIUMRb STRONTIUMSr YTTRIUMY ZIRCONIUMZr NIOBIUMNb MOLYBDENUMMo TECHNETIUMTc RUTHENIUMRu RHODIUMRh PALLADIUMPd AgSILVER CADMIUMCd INDIUMIn SnTIN ANTIMONYSb TELLURIUMTe IODINEI XeXENON 85 88 89 91 93 96 98 101 103 106 108 112 115 119 122 128 127 131 55 56 72 73 74 75 76 77 78 79 80 81 82 83 84 85 86 CESIUMCs BARIUMBa HAFNIUMHf TANTALUMTa TUNGSTENW RHENIUMRe OSMIUMOs IRIDIUMIr PLATINUMPt AuGOLD MERCURYHg THALLIUMTl PbLEAD BISMUTHBi POLONIUMPo ASTATINEAt RnRADON 133 137 178 181 184 186 190 192 195 197 201 204 207 209 209 210 222 87 88 104 105 106 107 108 109 110 111 112 113 114 115 116 117 118 FRANCIUMFr RADIUMRa RUTHERFORDIUMRf DUBNIUMDb SEABORGIUMSg BOHRIUMBh HASSIUMHs MEITNERIUMMt DARMSTADTIUMDs ROENTGENIUMRg COPERNICIUMCn NIHONIUMNh -
The Oganesson Odyssey Kit Chapman Explores the Voyage to the Discovery of Element 118, the Pioneer Chemist It Is Named After, and False Claims Made Along the Way
in your element The oganesson odyssey Kit Chapman explores the voyage to the discovery of element 118, the pioneer chemist it is named after, and false claims made along the way. aving an element named after you Ninov had been dismissed from Berkeley for is incredibly rare. In fact, to be scientific misconduct in May5, and had filed Hhonoured in this manner during a grievance procedure6. your lifetime has only happened to Today, the discovery of the last element two scientists — Glenn Seaborg and of the periodic table as we know it is Yuri Oganessian. Yet, on meeting Oganessian undisputed, but its structure and properties it seems fitting. A colleague of his once remain a mystery. No chemistry has been told me that when he first arrived in the performed on this radioactive giant: 294Og halls of Oganessian’s programme at the has a half-life of less than a millisecond Joint Institute for Nuclear Research (JINR) before it succumbs to α -decay. in Dubna, Russia, it was unlike anything Theoretical models however suggest it he’d ever experienced. Forget the 2,000 ton may not conform to the periodic trends. As magnets, the beam lines and the brand new a noble gas, you would expect oganesson cyclotron being installed designed to hunt to have closed valence shells, ending with for elements 119 and 120, the difference a filled 7s27p6 configuration. But in 2017, a was Oganessian: “When you come to work US–New Zealand collaboration predicted for Yuri, it’s not like a lab,” he explained. that isn’t the case7. -
Measurement of 10Be from Lake Malawi (Africa) Drill Core Sediments and Implications for Geochronology
Palaeogeography, Palaeoclimatology, Palaeoecology 303 (2011) 110–119 Contents lists available at ScienceDirect Palaeogeography, Palaeoclimatology, Palaeoecology journal homepage: www.elsevier.com/locate/palaeo Measurement of 10Be from Lake Malawi (Africa) drill core sediments and implications for geochronology L.R. McHargue a,⁎, A.J.T. Jull b, A. Cohen a a Department of Geosciences, University of Arizona, 1040 E. Fourth Street, Tucson, Arizona 85721, United States b NSF Arizona AMS Laboratory, University of Arizona, 1118 E. Fourth Street, Tucson, Arizona 85721, United States article info abstract Article history: The cosmogenic radionuclide 10Be was measured from drill core sediments from Lake Malawi in order to Received 19 August 2008 help construct a chronology for the study of the tropical paleoclimate in East Africa. Sediment samples were Received in revised form 29 January 2010 taken every 10 m from the core MAL05-1C to 80 m in depth and then from that depth in core MAL05-1B to Accepted 4 February 2010 382 m. Sediment samples were then later taken at a higher resolution of every 2 m from MAL05-1C. They Available online 12 February 2010 were then leached to remove the authigenic fraction, the leachate was processed to separate out the beryllium isotopes, and 10Be was measured at the TAMS Facility at the University of Arizona. The 10Be/9Be Keywords: fi Beryllium-10 pro le from Lake Malawi sediments is similar to those derived from marine sediment cores for the late Cosmogenic radionuclide Pleistocene, and is consistent with the few radiocarbon and OSL IR measurements made from the same core. Lake sediments Nevertheless, a strong correlation between the stable isotope 9Be and the cosmogenic isotope 10Be suggests Lake Malawi that both isotopes have been well mixed before deposition unlike in some marine sediment cores. -
Chromium Isotopes Detection in Their Ores with Minimal Errors
Open Access Annals of Advances in Chemistry Research Article Chromium Isotopes Detection in their Ores with Minimal Errors ISSN 2576-3768 Loai Aljerf1* and Nuha AlMasri2 1Department of Basic Sciences, Faculty of Dental Medicine, Damascus University, Mazzeh Highway, Almazzeh, Damascus, Syria 2Department of Chemistry, Faculty of Medicine, Syrian Private University, Damascus, Syria *Address for Correspondence: Loai Aljerf, De- Abstract partment of Basic Sciences, Faculty of Dental Medicine, Damascus University, Mazzeh High- The industrial production and use of chromium have grown considerably during the past way, Almazzeh, Damascus, Syria, Tel: +963-93 fi ve decades. Abundances of the chromium isotopes in terrestrial samples are identical to 34 46 993; Email: [email protected]; 0.01%. Among the dominant species of chromium, the trivalent form widely occurs in nature in [email protected] chromite ores which is extremely immobilized especially in water bodies. Samples were mixtures Submitted: 21 July 2018 of separated chromium isotopes and the calibration was made with the same species as those Approved: 03 September 2018 used in the measurements. The method had simplifi ed the conversion of the ores to chromyl Published: 04 September 2018 fl uoride since the element could be readily separated as lead chromate from the leaching of Copyright: 2018 Aljerf L, et al. This is an open chromite-sodium peroxide fusions. Isotope assay of chromyl fl uoride under certain conditions access article distributed under the Creative was measured and the measurements of chromium isotopic anomalies ratios and isotope Commons Attribution License, which permits abundance of the chromite ores have been assessed. These provided suffi cient quantitative mass unrestricted use, distribution, and reproduction spectrometric data, which were analyzed to calculate the abundance and the mean atomic mass in any medium, provided the original work is of the questioned isotopes. -
Online Determination of Boron Isotope Ratio in Boron Trifluoride By
applied sciences Article Online Determination of Boron Isotope Ratio in Boron Trifluoride by Infrared Spectroscopy Weijiang Zhang, Yin Tang and Jiao Xu * School of Chemical Engineering & Technology, Tianjin University, Tianjin 300072, China; [email protected] (W.Z.); [email protected] (Y.T.) * Correspondence: [email protected]; Tel.: +86-022-27402028 Received: 17 September 2018; Accepted: 3 December 2018; Published: 6 December 2018 Abstract: Enriched boron-10 and its related compounds have great application prospects, especially in the nuclear industry. The chemical exchange rectification method is one of the most important ways to separate the 10B and 11B isotope. However, a real-time monitoring method is needed because this separation process is difficult to characterize. Infrared spectroscopy was applied in the separation device to realize the online determination of the boron isotope ratio in boron trifluoride (BF3). The possibility of determining the isotope ratio via the 2ν3 band was explored. A correction factor was introduced to eliminate the difference between the ratio of peak areas and the true value of the boron isotope ratio. It was experimentally found that the influences of pressure and temperature could be ignored. The results showed that the infrared method has enough precision and stability for real-time, in situ determination of the boron isotope ratio. The instability point of the isotope ratio can be detected with the assistance of the online determination method and provides a reference for the production of boron isotope. Keywords: isotope; boron; infrared spectroscopy; online determination 1. Introduction Boron in naturally occurring compounds is composed of two isotopes, one of mass 10 and the other of mass 11. -
Status of Fission Yield Measurements
nij»wiiM>iT»i»n'i»wwr I '• • «• PORTIOHS OF THIS &EPOTT ARE till •{•1& * i STATUS OF FI5.SIOM YIELD MEASUREHEMTS - i William J. Maeck Exxon Nuclear Idaho Company, Inc.* Idaho National Engineering Laboratory P.O. Box 2300 Idaho Fails, Idaho 83401, USA NOTICE . vtrpiird at Mt t*W. nm my < at i!tt$lte<K of anunwi my I*gal ! •prfn-nu Urn in uu *nuld noi | in(iuif.f privately 'IUWII n Prepared For Third ASTM-EURATOM Symposium On Reactor Dosimetry To be held at Ispra, Italy October 1-5, 1979 rUnder U^S... Department of Energy Idaho Operations Office Contract £- /L- - AC 07- 7c!XV>o 1. INTRODUCTION Fission yield data, for all neutron energies, play an important role in f many of the disiplines (fuel burnup, /ission rate measurements, dosimetry, reactor physics, damage studies, post irradiation fuel analysis, etc-) being discussed at this symposium. This paper reviews and presents a brief discussion i of the current status of fission yield measurement programs being conducted in the major laboratories throughout the world, and when possible, to—identify future activities. The contents of this paper are based on tv/o sources: 1) a mailing by the author to various principal investigators furnishing a form which could be used to describe their most current work, and 2) reference to the most recent IAEA Nuclear Data Section document "Progress in Fission Product Nuclear Data" , which is a compilation of current measurement activities relative i to fission product nuclear data, • • , The~gGnera-l-orgunizat.ij?Jl_oI._t]ie,.p.aper_Js..by-_f.issioning.