Studies of Selenium and Xenon in Inductively Coupled Plasma Mass Spectrometry
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A 1 Case-PR/ }*Rciofft.;Is Report
.A 1 case-PR/ }*rciofft.;is Report (a) This eruption site on Mauna Loa Volcano was the main source of the voluminous lavas that flowed two- thirds of the distance to the town of Hilo (20 km). In the interior of the lava fountains, the white-orange color indicates maximum temperatures of about 1120°C; deeper orange in both the fountains and flows reflects decreasing temperatures (<1100°C) at edges and the surface. (b) High winds swept the exposed ridges, and the filter cannister was changed in the shelter of a p^hoehoc (lava) ridge to protect the sample from gas contamination. (c) Because of the high temperatures and acid gases, special clothing and equipment was necessary to protect the eyes. nose, lungs, and skin. Safety features included military flight suits of nonflammable fabric, fuil-face respirators that are equipped with dual acidic gas filters (purple attachments), hard hats, heavy, thick-soled boots, and protective gloves. We used portable radios to keep in touch with the Hawaii Volcano Observatory, where the area's seismic activity was monitored continuously. (d) Spatter activity in the Pu'u O Vent during the January 1984 eruption of Kilauea Volcano. Magma visible in the circular conduit oscillated in a piston-like fashion; spatter was ejected to heights of 1 to 10 m. During this activity, we sampled gases continuously for 5 hours at the west edge. Cover photo: This aerial view of Kilauea Volcano was taken in April 1984 during overflights to collect gas samples from the plume. The bluish portion of the gas plume contained a far higher density of fine-grained scoria (ash). -
Calculations of \(N,2N\) Reaction Cross Sections for 74,76,78,80,82Se up to 20
128 EPJ Web of Conferences , 01001 (2016) DOI: 10.1051/epjconf/201612801001 TESNAT 2016 Halide Şahan1,a, Muhittin Şahan1, Eyyup Tel1 1Osmaniye Korkut Ata University, Faculty of Arts and Science, Department of Physics, Osmaniye, Turkey In the present work, the excitation functions of (n,2n) reactions for five isotopes of selenium (74,76,78,80,82Se) are calculated using ALICE/ASH, EMPIRE-3.2.2, PCROSS, and TALYS 1.6 computer codes based on statistical model up to 20 MeV. The theoretical calculations provide information of the (n,2n) excitation functions with the increasing target neutron number of selenium element. The calculated cross-sections were compared with experimental data from EXFOR and also with the cross- sections estimated with semi empirical formula developed by Tet et al. (2008) [18]. Results show a reasonably good agreement between the calculations and the experimental data from literature. ! " by Tel et al. [13]. These formulas have been given as follows; The theoretical calculation models are necessary to ⎪⎧7.15[]1− 2.45e−31.620(N −Z ) / A for even A⎪⎫ provide the estimation of the particle–induced reaction σ = (1) ln n,2n ⎨ ⎬ cross sections due to the experimental difficulty [1,2]. In ⎩⎪ 7.65[]1−1.59e−23.06(N −Z ) / A for odd A⎭⎪ past years the cross section of selenium isotopes (74,76,78,80,82,84Se) around 14-15 MeV have been measured For (n,2n) reaction cross sections of 74Se(n,2n)73Se, by many researches such as Hille and Münzer [3]; 76Se(n,2n)75Se, 78Se(n,2n)77Se, 80Se(n,2n)79Se and Minetti and Pasquarelli [4]; Casanova and Sanchez [5]; 82Se(n,2n)81Se at 14-15 MeV, the calculated cross 74,76,78,80,82 Hoang et al. -
AN43285 – Accurate Determination of Arsenic and Selenium in Environmental Samples Using Triple Quadrupole ICP-MS
Certified for Thermo Scientific™ iCAP™ TQe ICP-MS APPLICATION NOTE 43285 Accurate determination of arsenic and selenium in environmental samples using triple quadrupole ICP-MS Authors: Marcus Manecki1, Simon Lofthouse2, Philipp Boening3 and Shona McSheehy Ducos1; 1Thermo Fisher Scientific, Bremen, Germany; 2Thermo Fisher Scientific, Hemel Hempstead, UK; 3Institute of Chemistry and Biology of the Marine Environment (ICBM), Carl von Ossietzky University of Oldenburg, Oldenburg, Germany Keywords: Arsenic, interference removal, Selenium for example is an essential element that is REE, rock, selenium, soil, sediment necessary for normal thyroid function and due to its antioxidant properties, is associated with several health Goal benefits. Diseases associated with selenium deficiency To demonstrate the accurate determination of arsenic such as Keshan disease and symptoms of hypothyroidism, and selenium in sediments and rocks that contain elevated are most commonly found in areas where levels of levels of rare earth elements using triple quadrupole selenium in soil are particularly low. Supplementation as a ICP-MS. remedy is common practice and is not isolated to humans. Understanding where soil selenium deficiencies occur for Introduction example supports the correct supplementation of cattle Due to the impact arsenic and selenium can have in the grazing in those areas to prevent white muscle disease environment at low levels, as a toxin or essential nutrient (a cattle specific selenium deficiency disease). respectively, it is important to be able to quantify them accurately. Arsenic on the other hand, in its inorganic forms Instrumentation (the most common forms found in ground water and soils) An iCAP TQ ICP-MS was used to analyse all samples. -
Hyperfine Structure in Selenium, Palladium and Gold.* by L
HYPERFINE STRUCTURE IN SELENIUM, PALLADIUM AND GOLD.* BY L. SIBAZ~A. (From the Dcpa,'tment of Physics, CeJ~tral College, Balzgarore.) Received September 10, 1935. Selenium (At. no. 34; At. wt. 79.2). l'oI~ purposes of classification of selenium spectra, the arc arid spark lines of seleniunl have been mostly excited in tubes of various types with con- (lensed or uncondensed electrical discharge through selenium vapour or between alumiuium poles tipped with metallic selenium. A selenium arc either in vacuum or iu an atmosphere of nitrogen has aIso been employed. Such sources however are not suited for hyperfine structure work, as the lines obtained are broad and diffuse. Moreover most of the prominent are lines of selenium lie either in the near infra-red or in the extreme ultra-violet, thus rendering their analysis by high resolving power apparatus specially difficult. Some intense spark lines of selenium 1% in the visible region; lmt under the conditions employed for their emission in discharge tubes, the broadening of the lines renders such sources unsuitable for hyperfine structure study. The apparatus used, the essential part of ~-hich is a water- cooled hollow cathode, is the same as that employed by 2Prof. Venkatesaehar and the author in their investigation on the isotopic constitution of platinum, x The selenium powcler took the place of the platinum foil in the tubular space of the cathode (P1. XV, Fig. 1). For experimental details the above paper -,,~+ he consulted. Of the seventeen lines of selenium here examined, only two are are lines and the remaining fifteen belong to the first spark spectrum of selenium. -
Detection of Elements at All Three R-Process Peaks in the Metal-Poor Star HD 160617
Published in the Astrophysical Journal A Preprint typeset using LTEX style emulateapj v. 5/2/11 DETECTION OF ELEMENTS AT ALL THREE R-PROCESS PEAKS IN THE METAL-POOR STAR HD 1606171 ,2 ,3 Ian U. Roederer4 and James E. Lawler5 Published in the Astrophysical Journal ABSTRACT We report the first detection of elements at all three r-process peaks in the metal-poor halo star HD 160617. These elements include arsenic and selenium, which have not been detected previously in halo stars, and the elements tellurium, osmium, iridium, and platinum, which have been detected previously. Absorption lines of these elements are found in archive observations made with the Space Telescope Imaging Spectrograph onboard the Hubble Space Telescope. We present up-to-date absolute atomic transition probabilities and complete line component patterns for these elements. Additional archival spectra of this star from several ground-based instruments allow us to derive abundances or upper limits of 45 elements in HD 160617, including 27 elements produced by neutron-capture reactions. The average abundances of the elements at the three r-process peaks are similar to the predicted solar system r-process residuals when scaled to the abundances in the rare earth element domain. This result for arsenic and selenium may be surprising in light of predictions that the production of the lightest r-process elements generally should be decoupled from the heavier r-process elements. Subject headings: atomic data — nuclear reactions, nucleosynthesis, abundances — stars: abundances — stars: individual (HD 160617) — stars: Population II 1. INTRODUCTION in greater abundance during n-capture reactions. The Understanding the origin of the elements is one of the s-process path closely follows the valley of β-stability, major challenges of modern astrophysics. -
Discovery of the Selenium Isotopes
Discovery of the Selenium Isotopes J. Claes, J. Kathawa, M. Thoennessen∗ National Superconducting Cyclotron Laboratory and Department of Physics and Astronomy, Michigan State University, East Lansing, MI 48824, USA Abstract Thirty-one selenium isotopes have so far been observed; the discovery of these isotopes is discussed. For each isotope a brief summary of the first refereed publication, including the production and identification method, is presented. ∗Corresponding author. Email address: [email protected] (M. Thoennessen) Preprint submitted to Atomic Data and Nuclear Data Tables April 28, 2010 Contents 1. Introduction . 3 2. Discovery of 64−94Se.................................................................................... 3 2.1. 64Se............................................................................................. 3 2.2. 65Se............................................................................................. 3 2.3. 66Se............................................................................................. 5 2.4. 67Se............................................................................................. 5 2.5. 68Se............................................................................................. 5 2.6. 69Se............................................................................................. 5 2.7. 70Se............................................................................................. 5 2.8. 71Se............................................................................................ -
Proceedings of the 1990 Billings Land Reclamation Symposium On
U.S. GEOLOGICAL SURVEY CI-RCULAR 1064 Proceedings of the 1990 Billings Land Reclamation Symposium on Selenium in Arid and Semiarid Environments, Western United States AVAILABILITY OF BOOKS AND MAP OF THE U.S. GEOLOGICAL SURVEY Instructions on ordering publications of the U.S. Geological Survey, along with prices of the Jast offerings, arc·Jive!l in the cur rent-year issues of the monthly catalog "New Publications of th U.S. Geological Survey." Prices of available U.l:~ Sur· . vey publications released prior to the current year are listed in e most recent annual "Price and Availability List" Puhlications that are listed in various U.S. Geological Survey catalogs (see b ck inside cover) but not listed in the most recent annual "Price and Availability List" are no longer available. Prices of reports released to the open files are ~iven in the li ting "U.S. Geological Survey Open-File Reports,'~ updated month ly, which is for sale in microfiche froiD the U.S. Geological S ey, Books and Open-File Reports Section, Federal Center, Box 25425, Denver, CO 80225. Reports released through the NTIS y be obtained by writing to the National Technical Information Service, U.S. Department of Commerce, Springfield, VA 22161 please include NTIS report numbez with inquiry. Order U.S. Geological Survey publications by mail or over the counter from the offices given below. BY MAIL OVER THE COUNTER Books Books Professional Papers, Bulletins, Water-Supply Papers, Techniqu of Water-Resources Investigations, Circulars, publications of general in Books of the -
Selenium and Tellurium Content of Stony Meteorites by Neutron Activation
Geochimicaet CosmochimicaActa, 1900, Vol. 19, py. 135 to 138. PeryamonPress Ltd. Priutedin NorthernIreland Selenium and tellurium content of stony meteorites by neutron activation U. SCHINDEWOLF* Department of Chemistry, University of Michigan, Ann &bor, Michigan (Received 14 Jcrmary 1MO) Abstract-By neutron activation analysis the Se- tendTe-content of four chondritic nleteorites have been determined. The average content is 9.8 + 2.5 and 0.61 .jl I.7 p.p.m., mspectively. Thesevalues are lowerthan those alrea,dyreported in the literature. SEVERAL authors (SUESS and UREY, 1956) have published data on the relative abundance of the chemical elements. In theoretically deriving these abundances extensive use has been made of certain systematic properties of nuclei because the necessary experimental data are lacking or unsatisfactory. Reliable experimental values of the abundance of each element are of great interest to cosmologists since the abundances of the elements are the result of cosmic events and any useful theory of the origin of the elements has to account in detail for the abundance curve. A recent theory requires several different types of synthesizing processes in order to explain the features of the abundance curve (BURBIDGE et al., 1957; CAMERON, 1957). Two of these processes are different types of neutron capture. Neutron capture on a long time-scale is thought to be responsible for the abundance peaks at Y (fifty neutrons), La (eighty-two neutrons) and Pb (126 neutrons) while neutron capture on a very short time-scale produces abundance peaks (CORYELI,, 1956) at approximately Br, Xe and Pt. Since the abundance of bromine, krypton, iodine and xenon are inherently difficult to determine, reliable data on the abundances of selenium and tellurium would be valuable in establishing the magnitudes of the peak yields at Br and Xe. -
Discovery of the Isotopes with 11 ≤ Z ≤ 19
Discovery of the Isotopes with 11 ≤ Z ≤ 19 M. Thoennessen∗ National Superconducting Cyclotron Laboratory and Department of Physics and Astronomy, Michigan State University, East Lansing, MI 48824, USA Abstract A total of 194 isotopes with 11 ≤ Z ≤ 19 have been identified to date. The discovery of these isotopes which includes the observation of unbound nuclei, is discussed. For each isotope a brief summary of the first refereed publication, including the production and identification method, is presented. ∗Corresponding author. Email address: [email protected] (M. Thoennessen) Preprint submitted to Atomic Data and Nuclear Data Tables May 31, 2011 Contents 1. Introduction . 2 2. Discovery of Isotopes with 11 ≤ Z ≤ 19................................................................... 3 2.1. Sodium.......................................................................................... 3 2.2. Magnesium . 8 2.3. Aluminum . 12 2.4. Silicon . 17 2.5. Phosphorus . 22 2.6. Sulfur ........................................................................................... 26 2.7. Chlorine . 31 2.8. Argon ........................................................................................... 36 2.9. Potassium. 41 3. Summary ............................................................................................. 46 References . 46 Explanation of Tables . 53 Table 1. Discovery of Isotopes with 11 ≤ Z ≤ 19. See page 53 for Explanation of Tables . 54 1. Introduction The discovery of isotopes of the elements from sodium to potassium is -
The Radiochemistry of Selenium
Rt?v.1965 NUCLEARSCIENCESERIES National Academy of Sciences-National Research Council Pubtished $3y: United States Atomic Energ Commission COMMITTEEON NUCLEARSCIENCE S.K.Allison,Chairman f?.D. Evans,Vice Chairman UniversityofChicago Mass.InstituteofTechnology LewisSlack,Secretary NationalResearchCouncil E. C.Anderson BerndKahn Los Alamos Sci.Laboratory TaftSanitaryEngineeringCenter N. E. Ballou JerryB. Marion U.S.NavalRadiologicalDefenseLaboratory UniversityofMaryland MartinJ.Berger R. L.Platzman NationalBureauofStandards ArgonneNationalLaboratory C. J.Borkowski ErnestC.Pollard Oak RidgeNatl.Laboratory PennsylvaniaStateUniversity RobertG. Cochran KatherineWay A & M CollegeofTexas Oak RidgeNationallaboratory HerbertGoldstein GeorgeW. Wetherill ColumbiaUniversity UniversityofCalifornia(LosAngeles) LIAISONMEMBERS PaulC.Aebersold RalphG. Allen AtomicEnergyCommission AirForceOfficeofScientificReeearch J.HowardMcMillen NationalScienceFoundation SUBCOMMITTEEON NAOIOCHEMISTRY N. E. Ballou,Chairman W. E. Nervik U. S.NavalRadiologicalDefense LawrenceRadiationLaboratory Laboratory J.M. Nielsen G. R. Choppin GeneralElectricCompany (Richfand) FloridaStateUniversity G. D. O’Kelley H. M. Clark Oak RidgeNationalLaboratory RensselaerPolytechnicInstitute R. P. Schuman R. M. Diamond AtomicEnergyDivision LawrenceRadiationLaboratory PhillipsPetroleumCompany (IdahoFalls) A. W. Fairhall E. P. Steinberg UniversityofWashington ArgonneNationalLaboratory Jerome Hudie D. N. Sunderman BrookhavenNationalLaboratory BattelleMemorialInstitute J.D. Knight J.W. Winchester -
Selenium Mineral Commodity Profile
U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY Open-File Report 03–018 Mineral Commodity Profiles Selenium By W.C. Butterman and R.D. Brown, Jr. 2004 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards (or with the Northern American Stratigraphic Code). Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. 2 CONTENTS Overview .......................................................................................................................................................................4 Historical background....................................................................................................................................................4 Description ....................................................................................................................................................................5 Salient facts ............................................................................................................................................................5 Principal forms, alloys, and compounds.................................................................................................................6 Commercial grades, shapes, and specifications......................................................................................................6 Sources of selenium.......................................................................................................................................................6 -
Subcommittee on Nuclear and Radiochemistry Committee on Chemical Sciences Assembly of Mathematical and Physical Sciences National Research Council
SEPARATED ISOTOPES: cnrp-Rono'*-* c-nmn VITAL TOOLS TOR SCIENCE AND MEDICINE C0LF 820233 — Summ. DE33 011646 Subcommittee on Nuclear and Radiochemistry Committee on Chemical Sciences Assembly of Mathematical and Physical Sciences National Research Council DISCLAIMER This report was prepared as an account of work sponsored by an agency of the United States Government. Neither the United States Government nor any agency thereof, nor any of their employees, makes any warranty, express or implied, or assumes any legal liability or responsi- bility 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. Refer- ence herein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise does not necessarily constitute or imply its endorsement, recom- mendation, or favoring by the United States Governmenl or any agency thereof. The views and opinions of authors expressed herein do not necessarily state or reflect those of the United States Government or any agency thereof. NATIONAL ACADEMY PRESS Washington, D.C. 1982 \P DISTR1BUT10II Of THIS DOCUMENT IS UNLIMITED NOTICE: The project that is the subject of this report was approved by the Governing Board of the National Research Council, whose members are drawn from the Councils of the National Academy of Sciences, the Nationcil Academy of Engineering, and the Institute of Medicine. The members of the Committee responsible for the report were chosen for their special competences and with regard for appropriate balance. This report has been reviewed by a group other than the authors according to procedures approved by a Report Review Committee consisting of members of the National Academy of Sciences, the National Academy of Engineering, and the Institute of Medicine.