Radioactive Half-Life
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Chemistry 2100 In-Class Test 1(A)
NAME:____________________________ Student Number:______________________ Fall 2019 Chemistry 1000 Midterm #1B ____/ 65 marks INSTRUCTIONS: 1) Please read over the test carefully before beginning. You should have 5 pages of questions and a formula/periodic table sheet. 2) If your work is not legible, it will be given a mark of zero. 3) Marks will be deducted for incorrect information added to an otherwise correct answer. 4) Marks will be deducted for improper use of significant figures and for missing or incorrect units. 5) Show your work for all calculations. Answers without supporting calculations will not be given full credit. 6) You may use a calculator. 7) You have 90 minutes to complete this test. Confidentiality Agreement: I agree not to discuss (or in any other way divulge) the contents of this test until after 8:00pm Mountain Time on Thursday, October 10th, 2019. I understand that breaking this agreement would constitute academic misconduct, a serious offense with serious consequences. The minimum punishment would be a mark of 0/65 on this exam and removal of the “overwrite midterm mark with final exam mark” option for my grade in this course; the maximum punishment would include expulsion from this university. Signature: ___________________________ Date: _____________________________ Course: CHEM 1000 (General Chemistry I) Semester: Fall 2019 The University of Lethbridge Question Breakdown Spelling matters! Q1 / 4 Fluorine = F Fluorene = C13H10 Q2 / 4 Q3 / 6 Q4 / 4 Q5 / 6 Flourine = Q6 / 3 Q7 / 2 Q8 / 10 Q9 / 10 Q10 / 3 Q11 / 8 Q12 / 5 Total / 65 NAME:____________________________ Student Number:______________________ 1. Complete the following table. -
Chapter 2 Atoms, Molecules and Ions
Chapter 2 Atoms, Molecules and Ions PRACTICING SKILLS Atoms:Their Composition and Structure 1. Fundamental Particles Protons Electrons Neutrons Electrical Charges +1 -1 0 Present in nucleus Yes No Yes Least Massive 1.007 u 0.00055 u 1.007 u 3. Isotopic symbol for: 27 (a) Mg (at. no. 12) with 15 neutrons : 27 12 Mg 48 (b) Ti (at. no. 22) with 26 neutrons : 48 22 Ti 62 (c) Zn (at. no. 30) with 32 neutrons : 62 30 Zn The mass number represents the SUM of the protons + neutrons in the nucleus of an atom. The atomic number represents the # of protons, so (atomic no. + # neutrons)=mass number 5. substance protons neutrons electrons (a) magnesium-24 12 12 12 (b) tin-119 50 69 50 (c) thorium-232 90 142 90 (d) carbon-13 6 7 6 (e) copper-63 29 34 29 (f) bismuth-205 83 122 83 Note that the number of protons and electrons are equal for any neutral atom. The number of protons is always equal to the atomic number. The mass number equals the sum of the numbers of protons and neutrons. Isotopes 7. Isotopes of cobalt (atomic number 27) with 30, 31, and 33 neutrons: 57 58 60 would have symbols of 27 Co , 27 Co , and 27 Co respectively. Chapter 2 Atoms, Molecules and Ions Isotope Abundance and Atomic Mass 9. Thallium has two stable isotopes 203 Tl and 205 Tl. The more abundant isotope is:___?___ The atomic weight of thallium is 204.4 u. The fact that this weight is closer to 205 than 203 indicates that the 205 isotope is the more abundant isotope. -
Understanding the Astrophysical Origin of Silver, Palladium and Other Neutron-Capture Elements
Understanding the astrophysical origin of silver, palladium and other neutron-capture elements Camilla Juul Hansen M¨unchen 2010 Understanding the astrophysical origin of silver, palladium and other neutron-capture elements Camilla Juul Hansen Dissertation an der Fakult¨at f¨ur Physik der Ludwig–Maximilians–Universit¨at M¨unchen vorgelegt von Camilla Juul Hansen aus Lillehammer, Norwegen M¨unchen, den 20/12/2010 Erstgutachter: Achim Weiss Zweitgutachter: Joseph Mohr Tag der m¨undlichen Pr¨ufung: 22 M¨arz 2011 Contents 1 Introduction 1 1.1 Evolutionoftheformationprocesses . ..... 2 1.2 Neutron-capture processes: The historical perspective............ 5 1.3 Features and description of the neutron-capture processes.......... 7 1.4 Whatisknownfromobservations? . .. 9 1.5 Why study palladium and silver? . .. 15 1.6 Abiggerpicture................................. 16 2 Data - Sample and Data Reduction 19 2.1 Compositionofthesample . 19 2.1.1 Samplebiases .............................. 21 2.2 Datareduction ................................. 22 2.2.1 Fromrawtoreducedspectra. 22 2.2.2 IRAF versus UVES pipeline . 25 2.3 Merging ..................................... 26 2.3.1 Radialvelocityshift .......................... 27 3 Stellar Parameters 29 3.1 Methods for determining stellar parameters . ........ 29 3.2 Temperature................................... 30 3.2.1 Comparingtemperaturescales . 32 3.3 Gravity ..................................... 34 3.4 Metallicity.................................... 35 3.5 Microturbulence velocity, ξ .......................... -
Vitae CHRISTOPHER H. GAMMONS
vitae CHRISTOPHER H. GAMMONS Ph.D. Geochemistry and Mineralogy, The Pennsylvania State University, 1988 B.S. Geology (High Honors, Magna Cum Laude, Phi Beta Kappa), Bates College, 1980 Professional Geologist, State of Wyoming, 1999 to present Dept. of Geological Engineering phone (W): (406) 496-4763 Montana Tech of the University of Montana phone (H): (406) 782-3179 Butte, Montana, 59701 FAX: (406) 496-4133 [email protected] Geology-Related Employment 2003-present Professor, Montana Tech, Dept. of Geological Engineering 2013-2016 Head of the Dept. of Geological Engineering, Montana Tech 1999-2003 Associate Professor, Montana Tech, Dept. of Geological Engineering 1997-1999 Assistant Professor, Montana Tech, Dept. of Geological Engineering 1993-1996 4/93 to 12/96: Research Associate/Faculty Lecturer, McGill University 1992-1993 2/92 to 4/93: Postdoctoral Research Fellow, Swiss Fed. Inst. Tech. (ETH) 1988-1991 11/88 to 11/91: Postdoctoral Research Fellow, Monash University, Australia 1979-1982 4/79 to 8/79; 6/80 to 11/80; 4/81 to 9/82: Exploration Geologist, Anaconda Minerals Co. Teaching Experience Classes I have taught include (19 different subjects): Hydrogeochemistry, Acid Rock Drainage, Environmental Geology, Geochemical Modeling, Hydrogeology, Introductory Petrology, Mineralogy and Petrology, Earth and Life History, Astrobiology and Evolution of the Early Earth, Economic Geology, Hydrothermal Ore Deposits, Advanced Topics in Economic Geology, Geothermal Systems, Isotope Geochemistry, Physical Geology, Geology of Montana, Introduction to Geologic Field Mapping, Field Geology (3 week summer course) and Field Hydrogeology (3 week summer course). I enjoy teaching, and have always received excellent student evaluations. This is true for introductory service classes, as well as graduate or upper level undergraduate courses. -
Co-Production of Light and Heavy $ R $-Process Elements Via Fission
Draft version June 22, 2020 Typeset using LATEX twocolumn style in AASTeX62 Co-production of Light and Heavy r-process Elements via Fission Deposition Nicole Vassh,1 Matthew R. Mumpower,2, 3 Gail C. McLaughlin,4 Trevor M. Sprouse,5 and Rebecca Surman5, 3 1University of Notre Dame, Notre Dame, IN 46556, USA 2Theoretical Division, Los Alamos National Lab, Los Alamos, NM 87545, USA 3Joint Institute for Nuclear Astrophysics - Center for the Evolution of the Elements, USA 4North Carolina State University, Raleigh, NC 27695, USA 5University of Notre Dame, Notre Dame, Indiana 46556, USA ABSTRACT We apply for the first time fission yields determined across the chart of nuclides from the macroscopic- microscopic theory of the Finite Range Liquid Drop Model to simulations of rapid neutron capture (r-process) nucleosynthesis. With the fission rates and yields derived within the same theoretical framework utilized for other relevant nuclear data, our results represent an important step toward self- consistent applications of macroscopic-microscopic models in r-process calculations. The yields from this model are wide for nuclei with extreme neutron excess. We show that these wide distributions of neutron-rich nuclei, and particularly the asymmetric yields for key species that fission at late times in the r process, can contribute significantly to the abundances of the lighter heavy elements, specifically the light precious metals palladium and silver. Since these asymmetric yields correspondingly also deposit into the lanthanide region, we consider the possible evidence for co-production by comparing our nucleosynthesis results directly with the trends in the elemental ratios of metal-poor stars rich in r-process material. -
Evidence of a Sudden Increase in the Nuclear Size of Proton-Rich Silver-96 ✉ M
ARTICLE https://doi.org/10.1038/s41467-021-24888-x OPEN Evidence of a sudden increase in the nuclear size of proton-rich silver-96 ✉ M. Reponen 1 , R. P. de Groote1, L. Al Ayoubi 1,2, O. Beliuskina1, M. L. Bissell3, P. Campbell 3, L. Cañete4, B. Cheal 5, K. Chrysalidis 6, C. Delafosse1,2, A. de Roubin 1,7, C. S. Devlin 5, T. Eronen 1, R. F. Garcia Ruiz 8, S. Geldhof 1,9, W. Gins1, M. Hukkanen1,7, P. Imgram 10, A. Kankainen 1, M. Kortelainen 1, Á. Koszorús5, S. Kujanpää 1, R. Mathieson 5, D. A. Nesterenko 1, I. Pohjalainen1,11, M. Vilén 1,6, A. Zadvornaya1 & I. D. Moore 1 1234567890():,; Understanding the evolution of the nuclear charge radius is one of the long-standing chal- lenges for nuclear theory. Recently, density functional theory calculations utilizing Fayans functionals have successfully reproduced the charge radii of a variety of exotic isotopes. However, difficulties in the isotope production have hindered testing these models in the immediate region of the nuclear chart below the heaviest self-conjugate doubly-magic nucleus 100Sn, where the near-equal number of protons (Z) and neutrons (N) lead to enhanced neutron-proton pairing. Here, we present an optical excursion into this region by crossing the N = 50 magic neutron number in the silver isotopic chain with the measurement of the charge radius of 96Ag (N = 49). The results provide a challenge for nuclear theory: calculations are unable to reproduce the pronounced discontinuity in the charge radii as one moves below N = 50. -
Silver in Medicine: the Basic Science
b u r n s 4 0 s ( 2 0 1 4 ) s 9 – s 1 8 Available online at www.sciencedirect.com ScienceDirect journal homepage: www.elsevier.com/locate/burns § Silver in medicine: The basic science a, b David E. Marx *, David J. Barillo a Department of Chemistry, University of Scranton, Scranton, PA, USA b Disaster Response/Critical Care Consultants, LLC, Mount Pleasant, SC, USA a r t i c l e i n f o a b s t r a c t Keywords: Silver compounds are increasingly used in medical applications and consumer products. Silver Confusion exists over the benefits and hazards associated with silver compounds. In this Antimicrobial article, the biochemistry and physiology of silver are reviewed with emphasis on the use of Wound silver for wound care. Burn # 2014 Elsevier Ltd and ISBI. All rights reserved. Infection beginning of recorded history. There is evidence that humans 1. Introduction learned to separate silver from lead as early as 3000 BC [1]. The use of silver for currency and for drinking cups is mentioned in Silver is a naturally occurring element with an atomic weight the first book of the Old Testament [1,4]. In addition to jewelry of 107.870 and an atomic number of 47 [1]. Silver may be found and silverware, silver in contemporary life is used in dental in nature as the pure element, but more commonly occurs in fillings, photography, water disinfection, brazing and solder- ores, including Argentite (Ag2S), and horn silver (AgCl); and in ing, and electronic equipment [5]. combination with lead, lead–zinc, copper, gold, and copper– nickel [1]. -
Lawrence Berkeley National Laboratory Recent Work
Lawrence Berkeley National Laboratory Recent Work Title NUCLEAR SPINS OF SILVER-104 AND SILVER-106 Permalink https://escholarship.org/uc/item/74r683mw Authors Ewbank, W.B. Marino, L.L. Nierenberg, W.A. et al. Publication Date 1959-02-26 eScholarship.org Powered by the California Digital Library University of California UCRL ?~b3 UNIVERSITY OF CALIFORNIA TWO-WEEK LOAN COPY This is a Library Circulating Copy which may be borrowed for two weeks. For a personal retention copy, call Tech. Info. Division, Ext. 5545 BERKELEY. CALIFORNIA 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. UNIVERSITY OF CALIFORNIA Lawrence Radiation Laboratory Berke ley, California Contract No. W-7405-eng-48 .. -
Measurement of Long Lived Radioactive Impurities Retained in the Disposable Cassettes on the Tracerlab MX System During the Production of [18F]FDG
Applied Radiation and Isotopes ] (]]]]) ]]]–]]] Contents lists available at ScienceDirect Applied Radiation and Isotopes journal homepage: www.elsevier.com/locate/apradiso Measurement of long lived radioactive impurities retained in the disposable cassettes on the Tracerlab MX system during the production of [18F]FDG D. Ferguson n, P. Orr, J. Gillanders, G. Corrigan, C. Marshall Regional Medical Physics Service, Belfast Health and Social Care Trust, Belfast, Northern Ireland article info abstract Article history: Using a High- Purity Germanium gamma-ray spectrometer, a number of radioisotopes have been Received 15 December 2010 identified within Tracerlab MX radiochemistry system cassettes used to synthesise [18F]FDG. Twenty Received in revised form radiochemistry cassettes were measured and the average total activity of each radioisotope was 20 May 2011 determined. Using these values and decay correction, the minimum time the cassettes should be left in Accepted 22 May 2011 a decay store before the specific activity falls below 0.4B q/g, the limit for disposal alongside Clinical Waste was found to be 24 months. Keywords: & 2011 Elsevier Ltd. All rights reserved. Cyclotron FDG Waste disposal Radioactive waste 1. Introduction Since 18FÀ is produced by the 18O(p,n)18F reaction, it is neces- sary to remove the 18F-ion from its aqueous environment. On the 18F is the most widely used radionuclide in PET and is GE Tracerlab MX system, which utilises disposable cassettes commonly produced by bombarding 18O enriched water with (supplied by Rotem Industries, Ltd), this is performed using a QMA accelerated protons. It is well established that long lived radio- Sep-Pak column (supplied as a part of ABX reagent kit, Biomedizi- nuclide impurities are generated using this method as a result of nische Forschungsreagenzien GmbH). -
Release of 108Mag from Irradiated PWR Control Rod Absorbers Under Deep Repository Conditions
Report R-19-21 October 2019 Release of 108mAg from irradiated PWR control rod absorbers under deep repository conditions SVENSK KÄRNBRÄNSLEHANTERING AB SWEDISH NUCLEAR FUEL Charlotta Askeljung AND WASTE MANAGEMENT CO Michael Granfors Box 3091, SE-169 03 Solna Phone +46 8 459 84 00 Olivia Roth skb.se SVENSK KÄRNBRÄNSLEHANTERING ISSN 1402-3091 SKB R-19-21 ID 1868337 October 2019 Release of 108mAg from irradiated PWR control rod absorbers under deep repository conditions Charlotta Askeljung, Michael Granfors, Olivia Roth Studsvik Nuclear AB Keywords: PWR, Control rod, AIC alloy, Release of 108mAg. This report concerns a study which was conducted for Svensk Kärnbränslehantering AB (SKB). The conclusions and viewpoints presented in the report are those of the authors. SKB may draw modified conclusions, based on additional literature sources and/or expert opinions. A pdf version of this document can be downloaded from www.skb.se. © 2019 Svensk Kärnbränslehantering AB Abstract In a nuclear reactor control rods are used to control the neutron flux and thereby the fission rate. In PWR reactors the control rods are grouped in assemblies of about 20 rodlets. The rodlets consist of an absorber alloy, AIC alloy with nominal composition 80 % Ag, 15 % In and 5 % Cd, surrounded by a cladding of stainless steel. PWR control rods are primarily used for startup and shutdown, while the power during an operating cycle is controlled by varying the boron content in the moderator and by burnable absorbers in the fuel. In a future Swedish deep repository the PWR control rods are planned to be stored together with the fuel assemblies. -
A Mass Spectrometry Study of Isotope Separation in the Laser Plume by Timothy Wu Suen a Dissertation Submitted in Partial Satisf
A Mass Spectrometry Study of Isotope Separation in the Laser Plume by Timothy Wu Suen A dissertation submitted in partial satisfaction of the requirements for the degree of Doctor of Philosophy in Engineering – Mechanical Engineering in the Graduate Division of the University of California, Berkeley Committee in charge: Professor Samuel S. Mao, Co-Chair Professor Ralph Greif, Co-Chair Professor Costas Grigoropoulos Professor Tsu-Jae King Liu Fall 2012 A Mass Spectrometry Study of Isotope Separation in the Laser Plume Copyright © 2012 by Timothy Wu Suen Abstract A Mass Spectrometry Study of Isotope Separation in the Laser Plume by Timothy Wu Suen Doctor of Philosophy in Engineering – Mechanical Engineering University of California, Berkeley Professor Samuel S. Mao, Co-Chair Professor Ralph Greif, Co-Chair Accurate quantification of isotope ratios is critical for both preventing the development of illicit weapons programs in nuclear safeguards and identifying the source of smuggled material in nuclear forensics. While isotope analysis has traditionally been performed by mass spectrometry, the need for in situ measurements has prompted the development of op- tical techniques, such as laser-induced breakdown spectroscopy (LIBS) and laser ablation molecular isotopic spectrometry (LAMIS). These optical measurements rely on laser abla- tion for direct solid sampling, but several past studies have suggested that the distribution of isotopes in the ablation plume is not uniform. This study seeks to characterize isotope separation in the laser plume through the use of orthogonal-acceleration time-of-flight mass spectrometry. A silver foil was ablated with a Nd:YAG at 355 nm at an energy of 50 µJ with a spot size of 71 µm, for a fluence of 1.3 J/cm2 and an irradiance of 250 MW/cm2. -
Chapter 2: "Atoms and the Atomic Theory"
M02_PETR4521_10_SE_C02.QXD 9/10/09 8:05 PM Page 34 2ND REVISED 2 Atoms and the Atomic Theory CONTENTS 2-1 Early Chemical Discoveries and the Atomic Theory 2-2 Electrons and Other Discoveries in Atomic Physics 2-3 The Nuclear Atom 2-4 Chemical Elements 2-5 Atomic Mass 2-6 Introduction to the Periodic Table 2-7 The Concept of the Mole and the Avogadro Constant 2-8 Using the Mole Concept in Calculations Image of silicon atoms that are only 78 pm apart; image produced by using the latest scanning transmission electron microscope (STEM). The hypothesis that all matter is made up of atoms has existed for more than 2000 years. It is only within the last few decades, however, that techniques have been developed that can render individual atoms visible. e begin this chapter with a brief survey of early chemical discov- eries, culminating in Dalton’s atomic theory. This is followed by a Wdescription of the physical evidence leading to the modern pic- ture of the nuclear atom, in which protons and neutrons are combined into a nucleus with electrons in space surrounding the nucleus. We will also introduce the periodic table as the primary means of organizing elements into groups with similar properties. Finally, we will introduce the concept 34 M02_PETR4521_10_SE_C02.QXD 9/10/09 8:05 PM Page 35 2ND REVISED 2-1 Early Chemical Discoveries and the Atomic Theory 35 of the mole and the Avogadro constant, which are the principal tools for count- ing atoms and molecules and measuring amounts of substances.