A Mass Spectrometry Study of Isotope Separation in the Laser Plume by Timothy Wu Suen a Dissertation Submitted in Partial Satisf
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Lead Isotopes As Indicators of Environ Contamination from U Mining
._ .- - Preprint LA-UR-78-2147 , Title: LEAD ISOTOPES AS INDICATORS OF ENVIRONt1 ENTAL CONTAMINATION FRCM THE URANIUM MINING AND MILLING INDUSTRY IN THE GRANTS MINERAL BELT, NEW MEXICO Author (s): David B. Curtis and A. J. Gancarz 'k |- . 9 M/ - ' # - L .. %|.RkN: %| * & ,AQ' ,,7 ,e- d*157 ff' k g*/h T .s .. ; f*M & f g W , w -e ~ - " f:} + - pYW pm K .A ,W.% :M & Lw< *b* ? --~ k Y Q Q A -ell' 2_W h _ -- $| - f.s c t Q & Ye # C4HEhreSE33rzgmF %gh gM n [,315 ? M e % @N Y $ $ j3 h e fe l 2 D S $s - - #5 ~N [ ' & 9; - - - f _ '- ~ w e- * g r e w w 2 P As Nc- ' ** * -- - - - - $%y~ - . 9 . j'*( -, ' & . i .- f 1 * - -- ** -- e=* -h .Mr g g* ~ A _. y . gh(An ,, - ?fw h. y C: *, 1% * ~ ?, ?hSlh$i $ ': ffg w s - gp$lQ?$4$5;.>qgg - , .. INS is a Wegint of a paper intended for publication in 4 * '" M jour'ai or procet%1 ergs. Because changes rnay be made before f h , ' , publicction, this preprint is seiade available with the under. f ,- ' , starviing that it will not be died or reproduced without the * +' % '""'***'*C**' " permiss;or of the author, ') O 9 7 - _. _ _ . _ _ _ . _ - _ 0808.0 [ L * ' * . Q - 42 - 72 2)<f y . 1 LEAD ISOTOPES AS INDICATORS OF ENVIRONMENTAL CONTAMINATION FROM THE URANIUM MINING AND MILI.ING INDUSTitY .IN THE GRANIS MINERAL BELT, NEW NEXICO David B. Curtis and A. J. Gancar2 Los Alamos Scientine Laboratory Los Alamos, New Mexico, USA The unique isotopie composition oflead from uranium ores can be useful in studying ihe impact of ore processing efHuents on the env:ronment. -
Cyclotron Produced Lead-203 P
Postgrad Med J: first published as 10.1136/pgmj.51.601.751 on 1 November 1975. Downloaded from Postgraduate Medical Journal (November 1975) 51, 751-754. Cyclotron produced lead-203 P. L. HORLOCK M. L. THAKUR L.R.I.C. M.Sc., Ph.D. I. A. WATSON M.Sc. MRC Cyclotron Unit, Hammersmith Hospital, Du Cane Road, London W12 OHS Introduction TABLE 1. Isotopes of lead Radioactive isotopes of lead occur in the natural Isotope Half-life Principal y energy radioactive series and have been used as decay 194Pb m * tracers since the early days of radiochemistry. These 195Pb 17m * are 210Pb (ti--204 y, radium D), 212Pb (t--10. 6 h, 96Pb 37 m * thorium B) and 214Pb (t--26.8 m, radium B) all of 197Pb 42 m * which are from occurring decay 197pbm 42 m * separated naturally 198pb 24 h * products ofradium or thorium. There are in addition 19spbm 25 m * Protected by copyright. to these a number of other radioactive isotopes of 199Pb 90 m * lead which can be produced artificially with the aid 19spbm 122 m * of a nuclear reactor or a accelerator 20OPb 21-5 h ** 0-109 to 0-605 (complex) charge particle (daughter radiations) (Table 1). 2Pb 9-4 h * There are at least three criteria in choosing the 0oipbm 61 s * radioactive isotope for in vitro tracer studies. First, 20pb 3 x 105y *** TI X-rays, (daughter it should emit radiation which is easily detected. radiations) have a half-life to 202pbm 3-62 h * Secondly, it should long enough aPb 52-1 h ** 0-279 (81%) 0-401 (5%) 0-680 permit studies without excessive radioactive decay 203pbm 6-1 s * (0-9%) (no daughter occurring but not so long that waste disposal radiations) creates a problem. -
Proton-Induced Cross-Sections of Nuclear Reactions on Lead up to 37 Mev
Proton-induced cross-sections of nuclear reactions on lead up to 37 MeV F. Ditroi´ a,∗, F. Tark´ anyi´ a, S. Takacs´ a, A. Hermanneb aInstitute for Nuclear Research, Hungarian Academy of Sciences (ATOMKI), Debrecen, Hungary bCyclotron Laboratory, Vrije Universiteit Brussel (VUB), Brussels, Belgium Abstract Excitation function of proton induced nuclear reactions on lead for production of 206;205;204;203;202;201gBi, 203cum;202m;201cumPb and 202cum;201cum;200cum;199cumTl radionuclides were measured up to 36 MeV by using activation method, stacked foil irradiation technique and ?-ray spectrometry. The new experimental data were compared with the few earlier experimental results and with the predictions of the EMPIRE 3.1, ALICE-IPPE (MENDL2p) and TALYS (TENDL-2012) theoretical reaction codes. Keywords: lead target, cross-section by proton activation, theoretical model codes, thin layer activation (TLA) 1. Introduction this, only a few experimental data sets exist, collected mostly by the experimental groups. In the low energy Production cross-sections of proton induced nuclear region practically only one experimental cross-section reactions on lead are important for many applications is available from the Hannover-Cologne group. In our and for the development of nuclear reaction theory. research and application work in connection with the Lead is an important technological material as pure el- activation cross-sections on lead we were involved in ement as well as alloying agent and it is also widely different projects and applications: used in different nuclear technologies, as well as tar- get material for production of 201Tl medical diagnostic • preparation of nuclear database for production of gamma-emitter for SPECT technology (Lagunas-Solar medical radioisotopes in the frame of an IAEA Co- et al., 1981). -
THE NATURAL RADIOACTIVITY of the BIOSPHERE (Prirodnaya Radioaktivnost' Iosfery)
XA04N2887 INIS-XA-N--259 L.A. Pertsov TRANSLATED FROM RUSSIAN Published for the U.S. Atomic Energy Commission and the National Science Foundation, Washington, D.C. by the Israel Program for Scientific Translations L. A. PERTSOV THE NATURAL RADIOACTIVITY OF THE BIOSPHERE (Prirodnaya Radioaktivnost' iosfery) Atomizdat NMoskva 1964 Translated from Russian Israel Program for Scientific Translations Jerusalem 1967 18 02 AEC-tr- 6714 Published Pursuant to an Agreement with THE U. S. ATOMIC ENERGY COMMISSION and THE NATIONAL SCIENCE FOUNDATION, WASHINGTON, D. C. Copyright (D 1967 Israel Program for scientific Translations Ltd. IPST Cat. No. 1802 Translated and Edited by IPST Staff Printed in Jerusalem by S. Monison Available from the U.S. DEPARTMENT OF COMMERCE Clearinghouse for Federal Scientific and Technical Information Springfield, Va. 22151 VI/ Table of Contents Introduction .1..................... Bibliography ...................................... 5 Chapter 1. GENESIS OF THE NATURAL RADIOACTIVITY OF THE BIOSPHERE ......................... 6 § Some historical problems...................... 6 § 2. Formation of natural radioactive isotopes of the earth ..... 7 §3. Radioactive isotope creation by cosmic radiation. ....... 11 §4. Distribution of radioactive isotopes in the earth ........ 12 § 5. The spread of radioactive isotopes over the earth's surface. ................................. 16 § 6. The cycle of natural radioactive isotopes in the biosphere. ................................ 18 Bibliography ................ .................. 22 Chapter 2. PHYSICAL AND BIOCHEMICAL PROPERTIES OF NATURAL RADIOACTIVE ISOTOPES. ........... 24 § 1. The contribution of individual radioactive isotopes to the total radioactivity of the biosphere. ............... 24 § 2. Properties of radioactive isotopes not belonging to radio- active families . ............ I............ 27 § 3. Properties of radioactive isotopes of the radioactive families. ................................ 38 § 4. Properties of radioactive isotopes of rare-earth elements . -
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. -
Ion-To-Neutral Ratios and Thermal Proton Transfer in Matrix-Assisted Laser Desorption/Ionization
B American Society for Mass Spectrometry, 2015 J. Am. Soc. Mass Spectrom. (2015) 26:1242Y1251 DOI: 10.1007/s13361-015-1112-3 RESEARCH ARTICLE Ion-to-Neutral Ratios and Thermal Proton Transfer in Matrix-Assisted Laser Desorption/Ionization I-Chung Lu,1 Kuan Yu Chu,1,2 Chih-Yuan Lin,1 Shang-Yun Wu,1 Yuri A. Dyakov,1 Jien-Lian Chen,1 Angus Gray-Weale,3 Yuan-Tseh Lee,1,2 Chi-Kung Ni1,4 1Institute of Atomic and Molecular Sciences, Academia Sinica, Taipei, 10617, Taiwan 2Department of Chemistry, National Taiwan University, Taipei, 10617, Taiwan 3School of Chemistry, University of Melbourne, Melbourne, VIC 3010, Australia 4Department of Chemistry, National Tsing Hua University, Hsinchu, 30013, Taiwan Abstract. The ion-to-neutral ratios of four commonly used solid matrices, α-cyano-4- hydroxycinnamic acid (CHCA), 2,5-dihydroxybenzoic acid (2,5-DHB), sinapinic acid (SA), and ferulic acid (FA) in matrix-assisted laser desorption/ionization (MALDI) at 355 nm are reported. Ions are measured using a time-of-flight mass spectrometer combined with a time-sliced ion imaging detector. Neutrals are measured using a rotatable quadrupole mass spectrometer. The ion-to-neutral ratios of CHCA are three orders of magnitude larger than those of the other matrices at the same laser fluence. The ion-to-neutral ratios predicted using the thermal proton transfer model are similar to the experimental measurements, indicating that thermal proton transfer reactions play a major role in generating ions in ultraviolet-MALDI. Keywords: MALDI, Ionization mechanism, Thermal proton transfer, Ion-to-neutral ratio Received: 25 August 2014/Revised: 15 February 2015/Accepted: 16 February 2015/Published Online: 8 April 2015 Introduction in solid state UV-MALDI. -
Itwg Guideline Thermal Ionisation Mass Spectrometry (Tims) Executive Summary
NUCLEAR FORENSICS INTERNATIONAL TECHNICAL WORKING GROUP ITWG GUIDELINE THERMAL IONISATION MASS SPECTROMETRY (TIMS) EXECUTIVE SUMMARY Thermal Ionisation Mass Spectrometry (TIMS) is used for isotopic composition measurement of elements having relatively low ionisation potentials (e.g. Sr, Pb, actinides and rare earth elements). Also the concentration of an element can be determined by TIMS using the isotope dilution technique by adding to the sample a known amount of a “spike” [1]. TIMS is a single element analysis technique, thus it is recommended to separate all other elements from the sample before the measurement as they may cause mass interferences or affect the ionisation behaviour of the element of interest [2]. This document was designed and printed at Lawrence Livermore National Laboratory in 2017 with the permission of the Nuclear Forensics International Technical Working Group (ITWG). ITWG Guidelines are intended as consensus-driven best-practices documents. These documents are general rather than prescriptive, and they are not intended to replace any specific laboratory operating procedures. 1. INTRODUCTION The filament configuration in the ion source can be either single, double, or triple filament. In the single In TIMS, a liquid sample (typically in the diluted nitric acid filament configuration, the same filament serves both media) is deposited on a metal ribbon (called a filament for evaporation and ionisation. In the double and triple made of rhenium, tantalum, or tungsten) and dried. filament configurations, the evaporation of the sample The filament is then heated in the vacuum of the mass and the ionisation take place in separate filaments (Fig. spectrometer, causing atoms in the sample to evaporate 2). -
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 .......................... -
Methods of Ion Generation
Chem. Rev. 2001, 101, 361−375 361 Methods of Ion Generation Marvin L. Vestal PE Biosystems, Framingham, Massachusetts 01701 Received May 24, 2000 Contents I. Introduction 361 II. Atomic Ions 362 A. Thermal Ionization 362 B. Spark Source 362 C. Plasma Sources 362 D. Glow Discharge 362 E. Inductively Coupled Plasma (ICP) 363 III. Molecular Ions from Volatile Samples. 364 A. Electron Ionization (EI) 364 B. Chemical Ionization (CI) 365 C. Photoionization (PI) 367 D. Field Ionization (FI) 367 IV. Molecular Ions from Nonvolatile Samples 367 Marvin L. Vestal received his B.S. and M.S. degrees, 1958 and 1960, A. Spray Techniques 367 respectively, in Engineering Sciences from Purdue Univesity, Layfayette, IN. In 1975 he received his Ph.D. degree in Chemical Physics from the B. Electrospray 367 University of Utah, Salt Lake City. From 1958 to 1960 he was a Scientist C. Desorption from Surfaces 369 at Johnston Laboratories, Inc., in Layfayette, IN. From 1960 to 1967 he D. High-Energy Particle Impact 369 became Senior Scientist at Johnston Laboratories, Inc., in Baltimore, MD. E. Low-Energy Particle Impact 370 From 1960 to 1962 he was a Graduate Student in the Department of Physics at John Hopkins University. From 1967 to 1970 he was Vice F. Low-Energy Impact with Liquid Surfaces 371 President at Scientific Research Instruments, Corp. in Baltimore, MD. From G. Flow FAB 371 1970 to 1975 he was a Graduate Student and Research Instructor at the H. Laser Ionization−MALDI 371 University of Utah, Salt Lake City. From 1976 to 1981 he became I. -
How the Saha Ionization Equation Was Discovered
How the Saha Ionization Equation Was Discovered Arnab Rai Choudhuri Department of Physics, Indian Institute of Science, Bangalore – 560012 Introduction Most youngsters aspiring for a career in physics research would be learning the basic research tools under the guidance of a supervisor at the age of 26. It was at this tender age of 26 that Meghnad Saha, who was working at Calcutta University far away from the world’s major centres of physics research and who never had a formal training from any research supervisor, formulated the celebrated Saha ionization equation and revolutionized astrophysics by applying it to solve some long-standing astrophysical problems. The Saha ionization equation is a standard topic in statistical mechanics and is covered in many well-known textbooks of thermodynamics and statistical mechanics [1–3]. Professional physicists are expected to be familiar with it and to know how it can be derived from the fundamental principles of statistical mechanics. But most professional physicists probably would not know the exact nature of Saha’s contributions in the field. Was he the first person who derived and arrived at this equation? It may come as a surprise to many to know that Saha did not derive the equation named after him! He was not even the first person to write down this equation! The equation now called the Saha ionization equation appeared in at least two papers (by J. Eggert [4] and by F.A. Lindemann [5]) published before the first paper by Saha on this subject. The story of how the theory of thermal ionization came into being is full of many dramatic twists and turns. -
C7895 Mass Spectrometry of Biomolecules Schedule of Lectures
C7895 Mass Spectrometry of Biomolecules Schedule of lectures For schedule, please see a separate file with the course outline. Jan Preisler Consulting The last lecture. Please contact me in advance to make an appointment. Chemistry Dept. 312A14, tel.: 54949 6629, [email protected] This material is just an outline; students are advised to print this outline and write down notes durin the lectures. The material will be updated during The course is focused on mass spectrometry of biomolecules, i.e. ionization the semester. techniques MALDI and ESI, modern mass analyzers, such as time-of-flight MS or ion traps and bioanalytical applications. However, the course covers much broader area, including inorganic ionization techniques, virtually all Supporting study material: types of mass analyzers and hardware in mass spectrometry. • J. Gross, Mass Spectrometry, 3rd ed. Springer-Verlag, 2017 • J. Greaves, J. Roboz: Mass Spectrometry for the Novice, CRC Press, 2013 • Edmond de Hoffmann, Vincent Stroobant: Mass Spectrometry: Principles and Applications, 3rd Edition, John Wiley & Sons, 2007 Mass spectrometry of biomolecules 2018 1 Mass spectrometry of biomolecules 2018 2 1 2 Content I. Introduction 1 II. Ionization methods and sample introduction III. Mass analyzers IV. Biological applications of MS V. Example problems Introduction to Mass spectrometry. Brief History of MS. A Survey of Methods and Instrumentation. Basic Concepts in MS: Resolution, Sensitivity. Isotope patterns of organic molecules. Ionization Techniques and Sample Introductin. Electron Impact Mass spectrometry of biomolecules 2018 3 Ionization (EI). Chemical Ionization (CI) 3 4 I. Introduction Study Material • Information sources about mass spectrometry Lecture notes • Brief history of mass spectrometry, a survey of methods and Advice: please take notes, but do not copy the slides; the English slides will instrumentation be provided at the end of the semester.