Nuclear Lattices, Mass and Stability
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Spectroscopy of Neutron-Rich 34,35,36,37,38 P Populated In
PHYSICAL REVIEW C 92, 044308 (2015) , , , , Spectroscopy of neutron-rich 34 35 36 37 38P populated in binary grazing reactions R. Chapman,1,* A. Hodsdon,1 M. Bouhelal,2 F. Haas,3 X. Liang,1 F. Azaiez,4 Z. M. Wang,1 B. R. Behera,5 M. Burns,1 E. Caurier,3 L. Corradi,5 D. Curien,3 A. N. Deacon,6 Zs. Dombradi,´ 7 E. Farnea,8 E. Fioretto,5 A. Gadea,5 F. Ibrahim,4 A. Jungclaus,9 K. Keyes,1 V. Kumar, 1 S. Lunardi,8 N. Marginean,˘ 5,10 G. Montagnoli,8 D. R. Napoli,5 F. Nowacki,3 J. Ollier,1,11 D. O’Donnell,1,12 A. Papenberg,1 G. Pollarolo,13 M.-D. Salsac,14 F. Scarlassara,8 J. F. Smith,1 K. M. Spohr,1 M. Stanoiu,10 A. M. Stefanini,5 S. Szilner,5,15 M. Trotta,5 and D. Verney4 1School of Engineering and Computing, University of the West of Scotland, Paisley PA1 2BE, United Kingdom, and The Scottish Universities Physics Alliance (SUPA) 2Laboratoire de Physique Appliquee´ et Theorique,´ Universite´ Larbi Tebessa,´ Tebessa,´ Algerie´ 3IPHC, UMR7178, CNRS-IN2P3, and Universite´ de Strasbourg, F-67037 Strasbourg Cedex 2, France 4IPN, IN2P3-CNRS and Universite´ Paris-Sud, F-91406 Orsay Cedex, France 5INFN, Laboratori Nazionali di Legnaro, I-35020 Legnaro, Padova, Italy 6Schuster Laboratory, University of Manchester, Manchester M13 9PL, United Kingdom 7MTA ATOMKI, P.O. Box 51, H-4001 Debrecen, Hungary 8Dipartimento di Fisica and INFN-Sezione di Padova, Universita` di Padova, I35131 Padova, Italy 9Instituto de Estructura de la Materia, CSIC, E-28006 Madrid, Spain 10Horia Hulubei National Institute of Physics and Nuclear Engineering-IFIN-HH, Strasse Atomistilor No. -
The Radiochemistry of Beryllium
National Academy of Sciences National Research Council I NUCLEAR SCIENCE SERIES The Radiochemistry ·of Beryllium COMMITTEE ON NUCLEAR SCIENCE L. F. CURTISS, Chairman ROBLEY D. EVANS, Vice Chairman National Bureau of Standards MassaChusetts Institute of Technol0gy J. A. DeJUREN, Secretary ./Westinghouse Electric Corporation H.J. CURTIS G. G. MANOV Brookhaven National' LaboratOry Tracerlab, Inc. SAMUEL EPSTEIN W. WAYNE MEINKE CalUornia Institute of Technology University of Michigan HERBERT GOLDSTEIN A.H. SNELL Nuclear Development Corporation of , oak Ridge National Laboratory America E. A. UEHLING H.J. GOMBERG University of Washington University of Michigan D. M. VAN PATTER E.D.KLEMA Bartol Research Foundation Northwestern University ROBERT L. PLATZMAN Argonne National Laboratory LIAISON MEMBERS PAUL C .. AEBERSOLD W.D.URRY Atomic Energy Commission U. S. Air Force J. HOW ARD McMILLEN WILLIAM E. WRIGHT National Science Foundation Office of Naval Research SUBCOMMITTEE ON RADIOCHEMISTRY W. WAYNE MEINKE, Chairman HAROLD KIRBY University of Michigan Mound Laboratory GREGORY R. CHOPPIN GEORGE LEDDICOTTE Florida State University. Oak Ridge National Laboratory GEORGE A. COW AN JULIAN NIELSEN Los Alamos Scientific Laboratory Hanford Laboratories ARTHUR W. FAIRHALL ELLIS P. STEINBERG University of Washington Argonne National Laboratory JEROME HUDIS PETER C. STEVENSON Brookhaven National Laboratory University of California (Livermore) EARL HYDE LEO YAFFE University of CalUornia (Berkeley) McGill University CONSULTANTS NATHAN BALLOU WILLIAM MARLOW Naval Radiological Defense Laboratory N atlonal Bureau of Standards JAMESDeVOE University of Michigan CHF.MISTRY-RADIATION AND RADK>CHEMIST The Radiochemistry of Beryllium By A. W. FAIRHALL. Department of Chemistry University of Washington Seattle, Washington May 1960 ' Subcommittee on Radiochemistry National Academy of Sciences - National Research Council Printed in USA. -
Volatility of Radiopharmacy-Prepared Sodium Iodide-131 Capsules
RADIATION SAFETY Volatility of Radiopharmacy-Prepared Sodium Iodide-131 Capsules James M. Bright, Trenton T. Rees, Louis E. Baca and Richard L. Green Pharmacy Services, Syncor International Corporation, Albuquerque, New Mexico; and Quality and Regulatory Department, Syncor International Corporation, Woodland Hills, California studied thyroid physiology using 128I in 1937 (1,2). In January Objective: The aims of this study were to quantify the extent 1941, Hertz and Roberts were the first to administer radioiodine of volatilization from 131I-NaI therapeutic capsules prepared in 131I for the treatment of hyperthyroid patients (3). Today, almost a centralized radiopharmacy and to quantify the amount of 60 y later, radioiodine therapy with 131I remains the primary volatile 131I released from a dispensing vial containing a compounded 131I-NaI therapy capsule. therapeutic agent used in nuclear medicine, and its use is firmly Methods: Therapy capsules were prepared by injecting 131I established in the 2 diseases first treated: hyperthyroidism and oral solution into capsules containing anhydrous dibasic thyroid carcinoma. sodium phosphate. Volatilized activity was obtained by filter- Initially the use of 131I was restricted to the only pharmaceu- ing air drawn across samples that were placed open on the tical dosage form then available—liquid oral solution. While 131 bottom of a sample holder cup. Volatile I was captured by liquid radioiodine proved to be beneficial to the patients to filtering it through 3 triethylenediamine-impregnated carbon whom it was administered, the frequency of contamination and cartridge filters, arranged in series. To quantify the amount of thyroid uptake activity in nuclear medicine personnel who volatile 131I released from a dispensing vial during a simulated patient administration, a vial containing a compounded 131I handled the material was noted with increasing alarm (4–7). -
Arxiv:2001.06745V2 [Nucl-Th] 6 Jun 2021 Osrit Nteeuto Fsaeo Eto-Ihncermat Nuclear [5–9]
Neutron drip line of Z =9 − 11 isotopic chains Rong An,1 Guo-Fang Shen,1 Shi-Sheng Zhang,1, ∗ and Li-Sheng Geng1, 2, 3, 4, † 1School of Physics, Beihang University, Beijing 100191, China 2Beijing Key Laboratory of Advanced Nuclear Materials and Physics, Beihang University, Beijing 100191, China 3Beijing Advanced Innovation Center for Big Data-based Precision Medicine, Beihang University, Beijing100191, China 4School of Physics and Microelectronics, Zhengzhou University, Zhengzhou, Henan 450001, China A recent experimental breakthrough identified the last bound neutron-rich nuclei in fluorine and neon isotopes. Based on this finding, we perform a theoretical study of Z = 9, 10, 11, 12 isotopes in the relativistic mean field (RMF) model. The mean field parameters are assumed from the PK1 parameterization, and the pairing correlation is described by the particle number conservation BCS (FBCS) method recently formulated in the RMF model. We show that the FBCS approach plays an essential role in reproducing experimental results of fluorine and neon isotopes. Furthermore, we predict 39Na and 40Mg to be the last bound neutron-rich nuclei in sodium and magnesium isotopes. I. INTRODUCTION Properties of neutron-rich nuclei, in particular, the location of the neutron drip line, play an important role not only in understanding nuclear stability with respect to the isospin in hereto unexplored regions of the nuclear chart [1], but also in numerous related scientific issues of current interests. For instance, the r-process nucleosynthesis of heavy elements in stellar evolution crucially depends on the values of beta decay rates and neutron capture cross sections in neutron-rich nuclei that do not exist in terrestrial conditions [2–4]. -
Nitrogen Isotope Variations in the Solar System Evelyn Füri and Bernard Marty
REVIEW ARTICLE PUBLISHED ONLINE: 15 JUNE 2015 | DOI: 10.1038/NGEO2451 Nitrogen isotope variations in the Solar System Evelyn Füri and Bernard Marty The relative proportion of the two isotopes of nitrogen, 14N and 15N, varies dramatically across the Solar System, despite little variation on Earth. NASA’s Genesis mission directly sampled the solar wind and confirmed that the Sun — and, by inference, the protosolar nebula from which the Solar System formed — is highly depleted in the heavier isotope compared with the reference nitrogen isotopic composition, that of Earth’s atmosphere. In contrast, the inner planets, asteroids, and comets are enriched in 15N by tens to hundreds of per cent; organic matter in primitive meteorites records the highest 15N/14N isotopic ratios. The measurements indicate that the protosolar nebula, inner Solar System, and cometary ices represent three distinct isotopic reservoirs, and that the 15N enrichment generally increases with distance from the Sun. The 15N enrichments were probably not inherited from presolar material, but instead resulted from nitrogen isotope fractionation processes that occurred early in Solar System history. Improvements in analytical techniques and spacecraft observations have made it possible to measure nitrogen isotopic variability in the Solar System at a level of accuracy that offers a window into the processing of early Solar System material, large-scale disk dynamics and planetary formation processes. he Solar System formed when a fraction of a dense molecu- a matter of debate, the D/H isotopic tracer offers the possibility of lar cloud collapsed and a central star, the proto-Sun, started investigating the relationships between the different Solar System Tburning its nuclear fuel1. -
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 . -
Element Builder
Name: ______________________________________ Date: ________________________ Student Exploration: Element Builder Prior Knowledge Questions (Do these BEFORE using the Gizmo.) 1. What are some of the different substances that make up a pizza? _____________________ _________________________________________________________________________ 2. What substances make up water? _____________________________________________ 3. What substances make up an iron pot? _________________________________________ Elements are pure substances that are made up of one kind of atom. Pizza is not an element because it is a mixture of many substances. Water is a pure substance, but it contains two kinds of atom: oxygen and hydrogen. Iron is an element because it is composed of one kind of atom. Gizmo Warm-up Atoms are tiny particles of matter that are made up of three particles: protons, neutrons, and electrons. The Element Builder Gizmo™ shows an atom with a single proton. The proton is located in the center of the atom, called the nucleus. 1. Use the arrow buttons ( ) to add protons, neutrons, and electrons to the atom. Press Play ( ). A. Which particles are located in the nucleus? _________________________________ B. Which particles orbit around the nucleus? __________________________________ 2. Turn on Show element name. What is the element? ________________________ 3. Manipulate the gizmo to figure out what actions cause the element name to change. _____________________________________________________________________ _____________________________________________________________________ Get the Gizmo ready: Activity A: Use the arrows to create an atom with two protons, Subatomic two neutrons, and two electrons. particles Turn on Show element name. Question: What are the properties of protons, neutrons, and electrons? 1. Observe: Turn on Show element symbol and Element notation. Three numbers surround the element symbol: the mass number, electrical charge (no number is displayed if the atom is neutral), and the atomic number. -
Groundwater Quality Data for the Northern Sacramento Valley, 2007: Results from the California GAMA Program
Prepared in cooperation with the California State Water Resources Control Board A product of the California Groundwater Ambient Monitoring and Assessment (GAMA) Program Groundwater Quality Data for the Northern Sacramento Valley, 2007: Results from the California GAMA Program SHASTA CO Redding 5 Red Bluff TEHAMA CO Data Series 452 U.S. Department of the Interior U.S. Geological Survey Cover Photographs: Top: View looking down the fence line, 2008. (Photograph taken by Michael Wright, U.S. Geological Survey.) Bottom: A well/pump in a field, 2008. (Photograph taken by George Bennett, U.S. Geological Survey.) Groundwater Quality Data for the Northern Sacramento Valley, 2007: Results from the California GAMA Program By Peter A. Bennett, George L. Bennett V, and Kenneth Belitz In cooperation with the California State Water Resources Control Board Data Series 452 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Suzette M. Kimball, Acting Director U.S. Geological Survey, Reston, Virginia: 2009 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment, visit http://www.usgs.gov or call 1-888-ASK-USGS For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod To order this and other USGS information products, visit http://store.usgs.gov Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted materials contained within this report. -
Measurement of 10Be from Lake Malawi (Africa) Drill Core Sediments and Implications for Geochronology
Palaeogeography, Palaeoclimatology, Palaeoecology 303 (2011) 110–119 Contents lists available at ScienceDirect Palaeogeography, Palaeoclimatology, Palaeoecology journal homepage: www.elsevier.com/locate/palaeo Measurement of 10Be from Lake Malawi (Africa) drill core sediments and implications for geochronology L.R. McHargue a,⁎, A.J.T. Jull b, A. Cohen a a Department of Geosciences, University of Arizona, 1040 E. Fourth Street, Tucson, Arizona 85721, United States b NSF Arizona AMS Laboratory, University of Arizona, 1118 E. Fourth Street, Tucson, Arizona 85721, United States article info abstract Article history: The cosmogenic radionuclide 10Be was measured from drill core sediments from Lake Malawi in order to Received 19 August 2008 help construct a chronology for the study of the tropical paleoclimate in East Africa. Sediment samples were Received in revised form 29 January 2010 taken every 10 m from the core MAL05-1C to 80 m in depth and then from that depth in core MAL05-1B to Accepted 4 February 2010 382 m. Sediment samples were then later taken at a higher resolution of every 2 m from MAL05-1C. They Available online 12 February 2010 were then leached to remove the authigenic fraction, the leachate was processed to separate out the beryllium isotopes, and 10Be was measured at the TAMS Facility at the University of Arizona. The 10Be/9Be Keywords: fi Beryllium-10 pro le from Lake Malawi sediments is similar to those derived from marine sediment cores for the late Cosmogenic radionuclide Pleistocene, and is consistent with the few radiocarbon and OSL IR measurements made from the same core. Lake sediments Nevertheless, a strong correlation between the stable isotope 9Be and the cosmogenic isotope 10Be suggests Lake Malawi that both isotopes have been well mixed before deposition unlike in some marine sediment cores. -
Meteoric Be and Be As Process Tracers in the Environment
Chapter 5 Meteoric 7Be and 10Be as Process Tracers in the Environment James M. Kaste and Mark Baskaran 7 10 Abstract Be (T1/2 ¼ 53 days) and Be (T1/2 ¼ occurring Be isotopes of use to Earth scientists are the 7 1.4 Ma) form via natural cosmogenic reactions in the short-lived Be (T1/2 ¼ 53.1 days) and the longer- 10 atmosphere and are delivered to Earth’s surface by wet lived Be (T1/2 ¼ 1.4 Ma; Nishiizumi et al. 2007). and dry deposition. The distinct source term and near- Because cosmic rays that cause the initial cascade of constant fallout of these radionuclides onto soils, vege- neutrons and protons in the upper atmosphere respon- tation, waters, ice, and sediments makes them valuable sible for the spallation reactions are attenuated by tracers of a wide range of environmental processes the mass of the atmosphere itself, production rates of operating over timescales from weeks to millions of comsogenic Be are three orders of magnitude higher in years. Beryllium tends to form strong bonds with oxygen the stratosphere than they are at sea-level (Masarik and atoms, so 7Be and 10Be adsorb rapidly to organic and Beer 1999, 2009). Most of the production of cosmo- inorganic solid phases in the terrestrial and marine envi- genic Be therefore occurs in the upper atmosphere ronment. Thus, cosmogenic isotopes of beryllium can be (5–30 km), although there is trace, but measurable used to quantify surface age, sediment source, mixing production as oxygen atoms in minerals at the Earth’s rates, and particle residence and transit times in soils, surface are spallated (in situ produced; see Lal 2011, streams, lakes, and the oceans. -
12 Natural Isotopes of Elements Other Than H, C, O
12 NATURAL ISOTOPES OF ELEMENTS OTHER THAN H, C, O In this chapter we are dealing with the less common applications of natural isotopes. Our discussions will be restricted to their origin and isotopic abundances and the main characteristics. Only brief indications are given about possible applications. More details are presented in the other volumes of this series. A few isotopes are mentioned only briefly, as they are of little relevance to water studies. Based on their half-life, the isotopes concerned can be subdivided: 1) stable isotopes of some elements (He, Li, B, N, S, Cl), of which the abundance variations point to certain geochemical and hydrogeological processes, and which can be applied as tracers in the hydrological systems, 2) radioactive isotopes with half-lives exceeding the age of the universe (232Th, 235U, 238U), 3) radioactive isotopes with shorter half-lives, mainly daughter nuclides of the previous catagory of isotopes, 4) radioactive isotopes with shorter half-lives that are of cosmogenic origin, i.e. that are being produced in the atmosphere by interactions of cosmic radiation particles with atmospheric molecules (7Be, 10Be, 26Al, 32Si, 36Cl, 36Ar, 39Ar, 81Kr, 85Kr, 129I) (Lal and Peters, 1967). The isotopes can also be distinguished by their chemical characteristics: 1) the isotopes of noble gases (He, Ar, Kr) play an important role, because of their solubility in water and because of their chemically inert and thus conservative character. Table 12.1 gives the solubility values in water (data from Benson and Krause, 1976); the table also contains the atmospheric concentrations (Andrews, 1992: error in his Eq.4, where Ti/(T1) should read (Ti/T)1); 2) another category consists of the isotopes of elements that are only slightly soluble and have very low concentrations in water under moderate conditions (Be, Al). -
Activation Analysis
26 August 1967 Leading Articles MEDIBALJOURNAL 509 her patients or the hospital midwife to undertake the home lation has been found between arsenic level in the blood and visiting of them after discharge. degree of renal insufficiency as indicated by blood creatinine Br Med J: first published as 10.1136/bmj.3.5564.509 on 26 August 1967. Downloaded from From the Bradford reports it can be seen that the final measurements. But speculative inquiries of this kind are decision to permit a mother and baby home after 48 hours worth while because they may sometimes provide the first must be made by someone at least of registrar status. It clue to the solution of an intractable problem. Information would also be of considerable value if the general practitioner of a more immediately useful kind can be expected from and district midwife in charge of such a case could freely using activation analysis in problems where the underlying obtain an opinion by domiciliary consultation from either the biochemical and physiological considerations are better hospital obstetric or paediatric department on any puerperal understood. or neonatal complication before readmission of the woman Thyroid metabolism, much studied by radioactive isotopes, after she has returned home. offers interesting problems for attack by activation analysis. When early discharge was discussed in these columns three Semi-automatic methods for the routine determination of years ago' the conclusion was drawn that, though it might protein-bound stable iodine have been elaborated, notably be suitable in emergency conditions, it had little part in in France,2 where the establishment of a laboratory to carry long-term planning.