Development of Fast Sampling and High Recovery Extraction Method for Stable Isotope Measurement of Gaseous Mercury

Total Page:16

File Type:pdf, Size:1020Kb

Development of Fast Sampling and High Recovery Extraction Method for Stable Isotope Measurement of Gaseous Mercury applied sciences Article Development of Fast Sampling and High Recovery Extraction Method for Stable Isotope Measurement of Gaseous Mercury Satoshi Irei Department of Environment and Public Health, National Institute for Minamata Disease, 4058-18 Hama, Minamata, Kumamoto 867-0008, Japan; [email protected]; Tel.: +81-966-63-3111 (ext. 760) Received: 24 August 2020; Accepted: 22 September 2020; Published: 24 September 2020 Abstract: A method involving fast large-volume sampling and bag extraction of total gaseous mercury (TGM) using a 5 mL acid solution was developed for stable mercury isotope ratio measurements. A big gold-coated sand trap (BAuT)—a 45 (i.d.) 300 mm (length) quartz tube with 131 times more × trapping material than a conventional gold trap—was used for the collection of a large amount of TGM. The collected TGM was extracted using 5 mL inversed aqua regia in a 2 L Tedlar bag followed by isotope measurements using a cold vapor generator coupled with a multicollector inductively coupled plasma mass spectrometer. Sampling tests demonstrated that the collection efficiency of the 1 BAuT was 99.9% or higher during the 1–24 h sampling period under the flow rate of 20–100 L min− . Recovery tests of 24 h bag extraction using 100 ng NIST SRM 8610 exhibited nearly 100% recovery yields. The five measured stable mercury isotope ratios agreed with reference values within 2σ intervals. The overall methodology tested during the pilot field and laboratory studies demonstrated its successful application in analysis, promising highly precise stable mercury isotopic data with a time resolution of less than 24 h. Keywords: total gaseous mercury (TGM); stable mercury isotopes; multicollector inductively coupled plasma mass spectrometer (MC-ICP-MS); sampling technique; acid extraction for gaseous elemental mercury; Minamata Convention on Mercury 1. Introduction Mercury is a notorious metal pollutant that can trigger serious adverse health effects [1]. It has a unique nature that it evaporates under room temperature and pressure, resulting in global spread through the atmosphere and ubiquity in the natural environment. The international regulation on the use and trade of manmade mercury, the Minamata Convention on Mercury, was enforced by the United Nations to lower the level of global mercury pollution; however, its effectiveness is questionable [2] because of the possibly significant natural sources such as volcanoes [3], the ocean surface [4], forests [5], and permafrost [6]. Recent stable mercury isotope analysis at the natural abundance has the potential to untangle the complex source apportionment that concentration measurements alone cannot solve. There are seven stable isotopes of mercury, namely 196Hg, 198Hg, 199Hg, 200Hg, 201Hg, 202Hg, and 204Hg with typical abundances of 0.16%, 10.0%, 16.9%, 23.1%, 13.2%, 29.7%, and 6.8%, respectively [7]. These isotopic compositions can be simultaneously measured by injecting a solution containing Hg2+ and a tin chloride solution into a cold vapor generator (CV), followed by a multicollector inductively coupled plasma mass spectrometer (MC-ICP-MS). To date, several methods to determine the stable isotopic compositions of atmospheric total gaseous mercury (TGM), which is a combination of gaseous elemental mercury (GEM) and gaseous oxidized mercury (GOM), have been reported [5,8–12]; however, these methods require long sampling durations, from a few days to weeks, thus making Appl. Sci. 2020, 10, 6691; doi:10.3390/app10196691 www.mdpi.com/journal/applsci Appl. Sci. 2020, 10, x 2 of 11 Appl. Sci. 2020, 10, 6691 2 of 11 [5,8–12]; however, these methods require long sampling durations, from a few days to weeks, thus making source apportionment difficult. Additionally, the efficient conversion of 100 ng or more of source apportionment difficult. Additionally, the efficient conversion of 100 ng or more of GEM into GEM into Hg2+ in a small amount of solution is also technically challenging due to the slow oxidation Hg2+ in a small amount of solution is also technically challenging due to the slow oxidation reaction. reaction. A dynamic oxidation method (i.e., slowly bubbling GEM in an acid solution) has been used A dynamic oxidation method (i.e., slowly bubbling GEM in an acid solution) has been used for this for this conversion [5,8,13–15], but the reproduction of this method is difficult and strongly depends conversion [5,8,13–15], but the reproduction of this method is difficult and strongly depends on the on the technical skills and knowledge of analysts. Herein, we report novel and simple offline technical skills and knowledge of analysts. Herein, we report novel and simple offline techniques of techniques of fast large-volume sampling and high recovery extraction for stable mercury isotope fast large-volume sampling and high recovery extraction for stable mercury isotope measurements. measurements. 2. Materials and Methods 2. Materials and Methods 2.1. Sampling and Preconcentration of TGM 2.1. Sampling and Preconcentration of TGM TGM was collected using a big gold-coated sand trap (BAuT) (Figure1). A BAuT is a custom-made 50 (o.d.)TGM 45was (i.d.) collected300 using mm (length) a large gold-coated quartz tube withsand atrap 45 (o.d.)(BAuT) 5(Figure mm (thickness) 1). A BAuT fritted is a custom- quartz × × × platemade (COSMOS 50 (o.d.) × VID, 45 (i.d.) Fukuoka, × 300 Japan).mm (length) Approximately quartz tube 10.5 with g gold-coated a 45 (o.d.) sand,× 5 mm which (thickness) traps TGM fritted at roomquartz temperature plate (COSMOS and releases VID, Fukuoka, TGM as GEM Japan). at high Appr temperaturesoximately 10.5 and g is gold-coated reused more sand, than 50,000which timestraps (NipponTGM at room Instruments temperature Corporation, and releases Osaka, TGM Japan) as GEM was layered at high ontemperatures the fritted plate, and is and reused approximately more than 0.150,000 g quartz times wool(Nippon was Instruments then stuffed Corporation, on the top of Osaka, the sand. Japan) The was BAuT layered was on used the verticallyfritted plate, during and samplingapproximately because 0.1 the g trappingquartz wool material was settled,then stuffe but wasd on not the secured top of ontothe thesand. fritted The plate.BAuT Compared was used tovertically a commercially during sampling available because conventional the trapping gold-coated mate sandrial settled, trap (a but 4 (i.d.) was not160 secured mm quartz onto tubethe fritted with × 0.08plate. g gold-coatedCompared to silica a commercially sand, capable available of capturing conven 70tionalµg of gold-coated TGM; Nippon sand Instruments trap (a 4 (i.d.) Corporation), × 160 mm thequartz mouth tube of with the BAuT0.08 g is gold-coated approximately silica 11 timessand, wider,capable and of thecapturing amount 70 of μ trappingg of TGM; material Nippon is approximatelyInstruments Corporation), 131 times greater, the mouth allowing of the a BAuT larger is air approximately flow with the 11 same times collection wider, and effi theciency amount and capturingof trapping capacity material of 9.2is approxim mg of TGM.ately To 131 meet times the samegreater, linear allowing velocities a larger as those air flow of the with conventional the same collection efficiency and capturing capacity of 9.2 mg of1 TGM. To meet the same linear velocities as trap under the typical flow rates of 0.5 and 1.0 L min− , the sampling flow rates used for the BAuT those of the conventional trap1 under the typical flow rates of 0.5 and 1.0 L min−1, the sampling flow were 63.3 and 126.6 L min− , respectively. Techniques reported in the literature use sampling flow rates used for the 1BAuT were 63.3 and 126.6 L min−1, respectively. Techniques reported in the rates of 2–20 L min− with a sampling duration of 12 h–20 days (using a carbon trap impregnated with literature use sampling flow rates of 2–201 L min−1 with a sampling1 duration of 12 h–20 days (using a iodine or chlorine [10,16]), 14.4 L min− with 2–3 days (1.8 L min− 8 conventional gold traps [5,8]), carbon trap impregnated1 with iodine1 or chlorine [10,16]), 14.4 L min× −1 with 2–3 days (1.8 L min−1 × 8 and 16 L min− with 3 days (1 L min− 16 conventional gold traps [9]). Assuming identical collection × −1 −1 econventionalfficiencies, the gold BAuT traps sampling [5,8]), and is 16 3–9-fold L min fasterwith 3 than days that (1 L ofmin the × other 16 conventional methods. Angold additional traps [9]). advantageAssuming ofidentical the BAuT collection is the ease effici ofencies, preconditioning, the BAuT sampling its long lifetime, is 3–9-fold and faster the use than of a that single of the trap other that makesmethods. the An postsampling additional procedureadvantage simple.of the BAuT is the ease of preconditioning, its long lifetime, and the use of a single trap that makes the postsampling procedure simple. Figure 1. A schematic of the large gold-coated sand trap (BAuT). Figure 1. A schematic of the large gold-coated sand trap (BAuT). TGMTGM waswas sampledsampled by by the the BAuT BAuT using using a a diaphragm diaphragm pump pump (N860FTE, (N860FTE, KNF, KNF, Freiburg, Freiburg, Germany Germany or DOA-P501-DB,or DOA-P501-DB, GAST GAST MFG MFG Corp., Corp., Benton Benton Harbor, Harb MI,or, USA) MI, through USA) through a flow meter a flow (RK230, meter KOFLOC, (RK230, Kyoto,KOFLOC, Japan). Kyoto, PTFE Japan). connectors PTFE for connectors the BAuT werefor the custom-made BAuT were (COSMOS custom-made VID, Fukuoka,(COSMOS Japan), VID, andFukuoka, half an Japan), inch or and 3/8 ofhalf an an inch inch (o.d.) or 3/8 PFA of tubingan inch (Tombo (o.d.) PFA 9003-PFA, tubing NICHIAS (Tombo 9003-PFA, Corporation, NICHIAS Tokyo, Japan),Corporation, PFA connectors Tokyo, Japan), (Swagelok, PFA Solon,connectors OH, USA),(Swagelok, and/or Solon, PTFE connectorsOH, USA), (Flowell and/or 30PTFE series, connectors Flowell Corporation,(Flowell 30 series, Yokohama, Flowell Japan) Corporatio were alson, Yokohama, used.
Recommended publications
  • Mass Independent Fractionation of Mercury Isotopes As Source Tracers in Sediments
    Available online at www.sciencedirect.com ScienceDirect Procedia Earth and Planetary Science 13 ( 2015 ) 151 – 157 11th Applied Isotope Geochemistry Conference, AIG-11 BRGM Mass Independent Fractionation of Mercury Isotopes as Source Tracers in Sediments Reshmi Dasa,b,* , William Landingb, Michael Bizimisc, Leroy Odomb, Jane Caffreyd aEarth Observatory of Singapore, 50 Nanyang Avenue, Singapore 639798, Singapore bFlorida State University, Tallahassee, Florida 32306, USA cUniversity of South Carolina, Columbia, South Carolina 29208, USA dUniversity of West Florida, Pensacola, Florida 32514, USA Abstract Since the discovery of isotopic fractionation of mercury in nature, mass dependent fractionation (MDF) and mass independent fractionation (MIF) of mercury isotopes are used as a tracer to understand the mercury cycle. MIF is a powerful tool in understanding the Hg transformations and reaction mechanisms. Here we look into the MIF of the two odd isotopes of mercury (199Hg and 201Hg) in sediment samples collected from lakes and springs of Florida, Lake Erie, and Yucatan Peninsula. The '199Hg and '201Hg of the sediments range from + 0.52‰ to -0.48‰. From the isotopic signature we interpret the possible source of Hg in the Yucatan Peninsula carbonate to be Hg(II) from the water column. Hg in the Florida lakes and spring sediments primarily comes from litterfall. Lake Erie appears to have an anthropogenic source. This study suggests that the MIF signature of Hg isotopes can be used to qualitatively determine the primary source(s) of Hg in sediments. © 2015 The Authors. Published by Elsevier B.V. This is an open access article under the CC BY-NC-ND license © 2015 The Authors.
    [Show full text]
  • Mass Fractionation Laws, Mass-Independent Effects, and Isotopic Anomalies Nicolas Dauphas and Edwin A
    EA44CH26-Dauphas ARI 10 June 2016 9:41 ANNUAL REVIEWS Further Click here to view this article's online features: • Download figures as PPT slides • Navigate linked references • Download citations Mass Fractionation Laws, • Explore related articles • Search keywords Mass-Independent Effects, and Isotopic Anomalies Nicolas Dauphas1,∗ and Edwin A. Schauble2 1Origins Laboratory, Department of the Geophysical Sciences and Enrico Fermi Institute, The University of Chicago, Chicago, Illinois 60637; email: [email protected] 2Department of Earth and Space Sciences, University of California, Los Angeles, California 90095 Annu. Rev. Earth Planet. Sci. 2016. 44:709–83 Keywords First published online as a Review in Advance on isotopes, fractionation, laws, NFS, nuclear, anomalies, nucleosynthesis, May 18, 2016 meteorites, planets The Annual Review of Earth and Planetary Sciences is online at earth.annualreviews.org Abstract This article’s doi: Isotopic variations usually follow mass-dependent fractionation, meaning 10.1146/annurev-earth-060115-012157 that the relative variations in isotopic ratios scale with the difference in Copyright c 2016 by Annual Reviews. mass of the isotopes involved (e.g., δ17O ≈ 0.5 × δ18O). In detail, how- All rights reserved ever, the mass dependence of isotopic variations is not always the same, ∗ Corresponding author and different natural processes can define distinct slopes in three-isotope diagrams. These variations are subtle, but improvements in analytical capa- Access provided by University of Chicago Libraries on 07/19/16. For personal use only. Annu. Rev. Earth Planet. Sci. 2016.44:709-783. Downloaded from www.annualreviews.org bilities now allow precise measurement of these effects and make it possi- ble to draw inferences about the natural processes that caused them (e.g., reaction kinetics versus equilibrium isotope exchange).
    [Show full text]
  • Discovery of Scandium, Titanium, Mercury, and Einsteinium Isotopes
    Discovery of Scandium, Titanium, Mercury, and Einsteinium Isotopes D. Meierfrankenfeld, A. Bury, M. Thoennessen∗ National Superconducting Cyclotron Laboratory and Department of Physics and Astronomy, Michigan State University, East Lansing, MI 48824, USA Abstract Currently, twenty-three scandium, twenty-five titanium, forty mercury and seventeen einsteinium isotopes have been observed and the discovery of these isotopes is discussed here. For each isotope a brief synopsis of the first refereed publication, including the production and identification method, is presented. arXiv:1003.5128v2 [nucl-ex] 8 Sep 2010 ∗Corresponding author. Email address: [email protected] (M. Thoennessen) Preprint submitted to Atomic Data and Nuclear Data Tables October 25, 2018 Contents 1. Introduction . 4 2. Discovery of 39−61Sc.................................................................................... 4 2.1. 39Sc............................................................................................. 5 2.2. 40Sc............................................................................................. 6 2.3. 41Sc............................................................................................. 6 2.4. 42Sc............................................................................................. 6 2.5. 43Sc............................................................................................. 6 2.6. 44Sc............................................................................................. 7 2.7. 45Sc............................................................................................
    [Show full text]
  • Mercury Stable Isotopes As Tracers in the Environment: Applications to Aquatic and Natural Gas Systems
    Mercury Stable Isotopes as Tracers in the Environment: Applications to Aquatic and Natural Gas Systems by Spencer J. Washburn A dissertation submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy (Earth and Environmental Sciences) in the University of Michigan 2018 Doctoral Committee: Professor Joel D. Blum, Chair Professor G. Allen Burton Associate Professor Rose M. Cory Professor Kyger C. Lohmann Spencer J. Washburn [email protected] ORCID iD: 0000-0002-6176-8297 © Spencer J. Washburn 2018 Acknowledgements First I would like to thank my wife Kalli for her unwavering support, keen assistance, and timely encouragement over the last five years. I would like to extend my sincere gratitude and many thanks to my advisor, Dr. Joel Blum, for his patience, guidance, and encouragement throughout my entire time at the University of Michigan. His mentorship has been an invaluable part of my PhD experience. I would like to thank all of my co-authors, who have been the source of excellent scientific discourse and support. I would also like to thank my dissertation committee members, who have provided guidance throughout this process. I would like to thank Marcus Johnson, who has been a wonderful source of technical advice and laboratory assistance. I would like to thank the other graduate students who have been members of the BEIGL lab group - Patrick Donovan, Sae Yun Kwon, Laura Motta Medina, and Aaron Kurz - for all of the discussions and friendship over the last 5 years. I would also like to thank the other members of the BEIGL lab group during my tenure, particularly Laura Sherman, Jamie Gleason, and Jason Demers.
    [Show full text]
  • Stable Isotope Separation in Calutrons
    Printed ill tho llnitzd Statss ot 4mcm 4vailsble frurii Nations' Technical Information Service U S :3ep?rtmelli uf Commerce 5285 Port 4oyal Cosd Spririizflald Viryinis 22161 NTlS ptwiodes P~III~~Copy ,498, Microfiche P,C1 I his rcpoti \*!is prspxed as an account of >,dSi-k sponsored by a3 agsncy of the United Sraies Governr;,ent. Neither thc !J nited Skiics i<n.~cti $IK~: nor any agency th2reof. no? any of thzir employoes, (ciakc?.Aijy ivarranty, express or irripiled, or assunias any legal liability or responsibility for ihe accuracy. compleienass, or usefulness of any inforriraiton. ;p ius, product, or process disclosed, or represents that its usewould not infr privately o-v?d ilghts Rcferencc herein to ai-y specific commercial product, process, or service by trade nziile, Zi'adei*lark, manufacturer, or otherwise, does not necsssarily constitute or imply its enduisemcat, recorn,n faVOiii-,g by ille United States(;ovc;riiiie!ii 01- any Zgency thereof Th opinions of auiihols cxp:essed here:!: d~ ~iui neccssarily statc or refisc?!host of the United Sta?ezGovernmer:?or any ngcncy therccf. ____ ___________... ..... .____ ORNL/TM-10356 OPERATIONS DIVISION STABLE ISOTOPE SEPARATION IN CALUTRONS: FORTY YEARS OF PRODUCTION AND DISTRIBUTION W. A. Bell J. G. Tracy Date Published: November 1987 Prepared by the OAK RIDGE NATIONAL LABORATORY Oak Ridge, Tennessee 37831 operated by MARTIN MARIETTA ENERGY SYSTEMS, INC. for the U.S. DEPARTMENT OF ENERGY under Contract No. DE-AC05-840R21400 iti CONTENTS Page ACKNOWLEDGMENTS ................................................. iv I. INTRODUCTION .............................................. 1 11. PROGRAM EVOLUTION ......................................... 1 111. RESEARCH AND DEVELOPMENT .................................. 5 IV. CHEMISTRY ................................................. 8 V.
    [Show full text]
  • 197(M)Hg with High Specific Activity for Imaging and Therapy
    Theranostic mercury: 197(m)Hg with high specific activity for imaging and therapy DISSERTATION zur Erlangung des akademischen Grades Doctor rerum naturalium (Dr. rer. nat.) vorgelegt der Fakultät Mathematik und Naturwissenschaften der Technischen Universität Dresden von Master of Science Chao Wang Born on 07. September 1988 in Harbin, PR China Submitted on: 14.09.2018 Date of defense:13.11.2018 Die Dissertation wurde in der Zeit von September 2014 bis September 2018 am Helmholtz-Zentrum Dresden-Rossendorf im Institut für Radiopharmazeutische Krebsforschung angefertigt. Reviewers: Prof. Dr. Jörg Steinbach (TU Dresden, HZDR) Prof. Dr. Gerd Wunderlich (TU Dresden) Table of Contents 1 Introduction and aim of the work .................................................................... 1 1.1 Introduction ........................................................................................................... 1 1.2 Aims of the Thesis ................................................................................................ 6 1.2.1 Major tasks of this work .................................................................................... 6 2 Theoretical background and literature survey .............................................. 9 2.1 Theranostics .......................................................................................................... 9 2.1.1 General ............................................................................................................. 9 2.1.2 Modalities for diagnostic: PET and SPECT ..................................................
    [Show full text]
  • Assessment of International Reference Materials for Isotope-Ratio Analysis (IUPAC Technical Report)1
    DOI 10.1515/pac-2013-1023 Pure Appl. Chem. 2014; 86(3): 425–467 IUPAC Technical Report Willi A. Brand*, Tyler B. Coplen, Jochen Vogl, Martin Rosner and Thomas Prohaska Assessment of international reference materials for isotope-ratio analysis (IUPAC Technical Report)1 Abstract: Since the early 1950s, the number of international measurement standards for anchoring stable isotope delta scales has mushroomed from 3 to more than 30, expanding to more than 25 chemical elements. With the development of new instrumentation, along with new and improved measurement procedures for studying naturally occurring isotopic abundance variations in natural and technical samples, the number of internationally distributed, secondary isotopic reference materials with a specified delta value has blossomed in the last six decades to more than 150 materials. More than half of these isotopic reference materials were produced for isotope-delta measurements of seven elements: H, Li, B, C, N, O, and S. The number of isotopic reference materials for other, heavier elements has grown considerably over the last decade. Nevertheless, even primary international measurement standards for isotope-delta measurements are still needed for some elements, including Mg, Fe, Te, Sb, Mo, and Ge. It is recommended that authors publish the delta values of internationally distributed, secondary isotopic reference materials that were used for anchoring their meas- urement results to the respective primary stable isotope scale. Keywords: delta notation; delta values; geochemistry; inductively coupled plasma (ICP) mass spectrometry; isotopes; IUPAC Inorganic Chemistry Division; mass spectrometry; reference materials. 1Sponsoring body: IUPAC Inorganic Chemistry Division: see more details on p. 458. *Corresponding author: Willi A.
    [Show full text]
  • Isotopic Composition and Fractionation of Mercury in Great
    Environ. Sci. Technol. 2010, 44, 7764–7770 prises more than 90% of the Hg in ambient air (3, 4). It has Isotopic Composition and low solubility in water and consequently can be transported Fractionation of Mercury in Great long distances in the atmosphere without being deposited (2, 4). In contrast, RGM and Hgp are much more reactive and Lakes Precipitation and Ambient Air deposit readily, either close to sources (5) or upon oxidation of Hg0 during atmospheric transport (2, 4). Given that Hg is ,† † a local, regional, and global pollutant, identifying the LYNNE E. GRATZ,* GERALD J. KEELER, transport pathways, chemical transformations, and deposi- JOEL D. BLUM,‡ AND tion mechanisms that Hg undergoes in the atmosphere can LAURA S. SHERMAN‡ be challenging. Air Quality Laboratory, 1415 Washington Heights, SPH I Mercury stable isotope geochemistry is a growing field Tower, and Department of Geological Sciences, used to examine Hg biogeochemical cycling. Mercury has 1100 N. University Ave., University of Michigan, Ann Arbor, Michigan 48109 seven stable isotopes (196, 198, 199, 200, 201, 202, and 204 amu), active redox chemistry, and an ability to form covalent bonds. It also commonly transforms between the solid, Received February 3, 2010. Revised manuscript received aqueous, and gas phases. Mass-dependent fractionation September 8, 2010. Accepted September 9, 2010. (MDF) of Hg has been observed experimentally during microbial reduction (6, 7) and dark abiotic aqueous reduction (8). MDF is also observed in natural materials, including - Atmospheric deposition is a primary pathway by which hydrothermal emissions (9 11) and terrestrial and marine sediments (12, 13). mercury (Hg) enters terrestrial and aquatic ecosystems; Recent studies demonstrate that mass-independent frac- however, the chemical and meteorological processes that Hg tionation (MIF) of Hg isotopes can occur in natural systems.
    [Show full text]
  • Experimental Searches for Rare Alpha and Beta Decays
    Experimental searches for rare alpha and beta decays P. Belli1;2;a, R. Bernabei1;2, F.A. Danevich3, A. Incicchitti4;5, and V.I. Tretyak3 1 Dip. Fisica, Universit`adi Roma \Tor Vergata", I-00133 Rome, Italy 2 INFN sezione Roma \Tor Vergata", I-00133 Rome, Italy 3 Institute for Nuclear Research, 03028 Kyiv, Ukraine 4 Dip. Fisica, Universit`adi Roma \La Sapienza", I-00185 Rome, Italy 5 INFN sezione Roma, I-00185 Rome, Italy Abstract. The current status of the experimental searches for rare alpha and beta decays is reviewed. Several interesting observations of alpha and beta decays, previously unseen due to their large half-lives (1015 − 1020 yr), have been achieved during the last years thanks to the improvements in the experimental techniques and to the underground locations of experiments that allows to suppress backgrounds. In particular, the list includes first observations of alpha decays of 151Eu, 180W (both to the ground state of the daughter nuclei), 190Pt (to excited state of the daughter nucleus), 209Bi (to the ground and excited 209 19 states of the daughter nucleus). The isotope Bi has the longest known half-life of T1=2 ≈ 10 yr relatively 115 115 to alpha decay. The beta decay of In to the first excited state of Sn (Eexc = 497:334 keV), recently observed for the first time, has the Qβ value of only (147 ± 10) eV, which is the lowest Qβ value known to-date. Searches and investigations of other rare alpha and beta decays (48Ca, 50V, 96Zr, 113Cd, 123Te, 178m2Hf, 180mTa and others) are also discussed.
    [Show full text]
  • Uptake, Efflux, and Toxicity of Inorganic and Methyl Mercury in the Endothelial Cells (EA.Hy926)
    www.nature.com/scientificreports OPEN Uptake, efux, and toxicity of inorganic and methyl mercury in the endothelial cells (EA.hy926) Songnian Liu, Martin Tsz-Ki Tsui✉, Elizabeth Lee, Josh Fowler & Zhenquan Jia✉ Cardiovascular disease (CVD) is the major cause of morbidity, mortality, and health care costs in the United States, and possibly around the world. Among the various risk factors of CVD, environmental and dietary exposures to mercury (Hg), a highly toxic metal traditionally regarded as a neurotoxin, has been recently suggested as a potential contributor towards human atherosclerotic development. In this study, we investigated the toxicity, type of cell death, dose-dependent uptake, and efux of inorganic HgII (as HgCl2) and methylmercury or MeHg (as CH3HgCl) in EA.hy926 endothelial cells, as these two forms of Hg are often reported to be present in human blood among the general populations (~20–30% as HgII and ~70–80% as MeHg). Our results showed that HgII is more toxic than MeHg to the endothelial cells, owing to the higher uptake into the cytoplasm and perhaps importantly lower efux of HgII by the cells, thus the “net” accumulation by the endothelial cells is higher for HgII than MeHg when exposed to the same Hg levels in the media. Furthermore, both HgII and MeHg were found to induce apoptotic and necrotic cell death. This study has important implications for the contributions of these two common Hg species to the development of atherosclerosis, an important process leading to CVD. Cardiovascular disease (CVDs) is the leading cause of morbidity, mortality, and health care costs in the United States.
    [Show full text]
  • The Chemical Compositions of the 2 New Hgmn Stars HD 30085 and HD
    Draft version August 15, 2019 A Preprint typeset using L TEX style AASTeX6 v. 1.0 THE CHEMICAL COMPOSITIONS OF THE 2 NEW HGMN STARS HD 30085 AND HD 30963. COMPARISON TO χ LUPI A, ν CAP AND HD 174567 R. Monier1 LESIA, UMR 8109, Observatoire de Paris et Universit´ePierre et Marie Curie Sorbonne Universit´es, place J. Janssen, Meudon, France. E.Griffin2 Dominion Astrophysical Observatory, 5071 West Saanich Road, Victoria, BC, V9E 2E7, Canada M. Gebran3 Department of Physics and Astronomy, Notre Dame University-Louaize, PO Box 72, Zouk Mikael, Lebanon. T. Kılıc¸oglu˘ 4 Department of Astronomy and Space Sciences, Faculty of Science, Ankara University, 06100, Turkey. T.Merle5 Institut d’Astronomie et d’Astrophysique, Universit´eLibre de Bruxelles, CP 226, Boulevard du Triomphe, 1050 Brussels, Belgium F. Royer6 GEPI, Observatoire de Paris, place J. Janssen, Meudon, France. ABSTRACT We report on a detailed abundance study of the fairly bright slow rotators HD 30085 (A0 IV), HD 30963 (B9 III) and HD 174567 (A0 V), hitherto reported as normal stars and the sharp-lined χ Lupi A (B9 IV HgMn). In the spectra of HD 30085, HD 30963, the Hg II line at 3984 A˚ line is conspicuous and numerous lines of silicon, manganese, chromium, titanium, iron, strontium, yttrium and zirconium appear to be strong absorbers. A comparison of the mean spectra of HD 30085 and HD 30963 with a grid of synthetic spectra for selected unblended lines having reliable updated atomic data reveals large overabundances of phosphorus, titanium, chromium, manganese, strontium, yttrium, and zirconium, barium, platinum and mercury and underabundances of helium, magnesium, scandium, arXiv:1908.05023v1 [astro-ph.SR] 14 Aug 2019 nickel.
    [Show full text]
  • C. R. Webster and R. N. Zare, "Photochemical Isotope Separation of Hg-196 by Reaction with Hydrogen Halides
    1302 J. Phys. Chem. 1981, 85, 1302-1305 Photochemical Isotope Separation of Hg-196 by Reaction with Hydrogen Halides Christopher R. Webster and Richard N. Zare” Department of Chemlstry, Stanford Unlverslty, Stanford, California 04305 (Received: November 28, 1980; In Flnal Form: February 11, 198 1) The rarest of the naturally occurring isotopes of mercury, lSHg (0.146% abundance), has been photochemically separated by reaction with hydrogen halides as scavengers of the excited Hg(3P1) atoms. A separation of 2-3 mg/h of enriched calomel product is achieved by using a monoisotopic lamp as an excitation source. The product contains 22 f 8% of the l=He in the feedstock. For the HC1 reaction the enrichment factor is 4.2, for HBr 1.4, while for HI no enrichmeit is found. Introduction Separation Apparatus Mercury occurs naturally as a mixture of seven isotopes Figure 1 shows a diagram of the photochemical sepa- of which the lightest, l%Hg, has an abundance of only ration apparatus, and Figure 2 details the reaction cell and 0.146%. The separation of Hg-196 from natural mercury the mercury lamp which are at the heart of the experiment. has practical application in the preparation, through nu- The flow system is constructed mainly in borosilicate glass, clear reaction, of radioactive Hg-197, a y emitter used for with the reaction cell and the inner jackets made from cerebral blood-flow measurement and brain-scanning with quartz to allow transmission of ultraviolet radiation. scintillation detection techniques.l To date, the highest Calibrated flowmeters (Matheson) allow controlled enrichments and yields of the isotopes of mercury have amounts of the hydrogen halide (HC1, HBr, or HI) gas to resulted from photochemical separation, that is, monoi- be mixed with a fractional amount of l,&butadiene and sotopic 63P1-61S0 excitation at 253.7 nm followed by passed through the reaction cell illuminated by 253.7-nm chemical reaction to form a stable, separable product.2 radiation.
    [Show full text]