Isotopic Compositions of the Elements 1983
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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 . -
Chemical and Isotropic Tracers of Natural Gas and Formation Waters in Fractured Shales
Chemical and isotopic tracers of natural gas and formation waters in Note: this document may contain some elements that are not fully fractured shales accessible to users with disabilities. If you need assistance accessing any information in this document, please contact [email protected]. Jennifer McIntosh, Melissa Schlegel, Brittney Bates Department of Hydrology & Water Resources University of Arizona, Tucson AZ EPA Technical Workshop Feb 24-25, 2011 Outline of Presentation 1)) What is the chemical and isotoppgic signature of formation waters and natural gas in fractured shales? 2) How does it compare with shallow drift aquifers, coalbeds, and other deep geologic formations? Illinois Basin-Case Study - 3 organic-rich formations: glacial drift, Penn. coal, & Dev. fractured shale - organicorganic-rich Ordov. ShaleShale, not part ooff this study m 500 20 km Schlegel et al. (in press, 2011, Geochimica et Cosmochimica Acta) Illinois Basin-Case Study - microbial methane in all 3 units - thermogenic methane in shale and coal m 500 20 km Schlegel et al. (in press, 2011, Geochimica et Cosmochimica Acta) Illinois Basin - water & gas samples Shallow aquifers Penn. Coals Dev. Shale Limestone aquifers 9New data (white symbols): Schlegel et al. (in press) 9Previous data (black symbols): McIntosh et al., 2002; Strąpoć et al., 2007, 2008a,b; Coleman et al, 1988 Fingerprint of natural gases 1000000 Shallow Aquifers 100000 High C1/C2, no C3 Coals 10000 1000 Shale 100 10 Shallow aquifers Penn. Coals Dev. Shale Thermogenic gas 1 -80 -75 -70 -65 -60 -55 -50 -45 -40 13 δ CCH4 (ä PDB) 13 9In general, 3 organic-rich units have different gas compositions (C1/C2+C3) and δ C-CH4 values. -
F:\Forensic Geology\Ice Man Isotopes.Wpd
NAME 89.215 - FORENSIC GEOLOGY DEMISE OF THE ICE MAN - ISOTOPIC EVIDENCE I. Introduction Stable and radiogenic isotopic data have been used in a variety of fields to answer a wide range of scientific questions. The nucleus of an atom consists of protons (+1 charge) and neutrons (0 charge), two types of particles that have essentially the same atomic mass. The number of protons in a nucleus determines the element. For example, a nucleus with 1 proton is a hydrogen nucleus, a nucleus with 2 protons is a helium nucleus. Isotopes of an element contain the same number of protons but different numbers of neutrons. For example, there are three isotopes of hydrogen: (1) ordinary hydrogen which contains one proton and no neutrons and has an atomic mass of one; (2) deuterium which contains one proton and one neutron and has an atomic mass of two; and (3) tritium which contains one proton and two neutrons and has an atomic mass of three. The convention used to show the numbers of types of particles in a nucleus is to place the number of protons (called the atomic number) at the bottom left of the element symbol and the number of protons plus neutrons (called the atomic mass) at the upper left of the element symbol. For example, the tritium isotope is 3 shown as 1H . II. Stable isotopes Stable isotopes are not radioactive, they do not spontaneously breakdown to other atoms. In a previous exercise you used radioactive carbon to determine when the Ice Man was killed. There are three isotopes of carbon: (1) carbon 12 which contains 6 protons and 6 neutrons giving an atomic mass of 12; (2) carbon 13 which contains 6 protons and 7 neutrons giving an atomic mass of 13; and (3) carbon 14 which contains 6 protons and 8 neutrons giving an atomic mass of 14. -
(A) Two Stable Isotopes of Lithium and Have Respective Abundances of And
NCERT Solution for Class 12 Physics :Chapter 13 Nuclei Q.13.1 (a) Two stable isotopes of lithium and have respective abundances of and . These isotopes have masses and , respectively. Find the atomic mass of lithium. Answer: Mass of the two stable isotopes and their respective abundances are and and and . m=6.940934 u Q. 13.1(b) Boron has two stable isotopes, and . Their respective masses are and , and the atomic mass of boron is 10.811 u. Find the abundances of and . Answer: The atomic mass of boron is 10.811 u Mass of the two stable isotopes are and respectively Let the two isotopes have abundances x% and (100-x)% Aakash Institute Therefore the abundance of is 19.89% and that of is 80.11% Q. 13.2 The three stable isotopes of neon: and have respective abundances of , and . The atomic masses of the three isotopes are respectively. Obtain the average atomic mass of neon. Answer: The atomic masses of the three isotopes are 19.99 u(m 1 ), 20.99 u(m 2 ) and 21.99u(m 3 ) Their respective abundances are 90.51%(p 1 ), 0.27%(p 2 ) and 9.22%(p 3 ) The average atomic mass of neon is 20.1771 u. Q. 13.3 Obtain the binding energy( in MeV ) of a nitrogen nucleus , given m Answer: m n = 1.00866 u m p = 1.00727 u Atomic mass of Nitrogen m= 14.00307 u Mass defect m=7 m n +7 m p - m m=7Aakash 1.00866+7 1.00727 - 14.00307 Institute m=0.10844 Now 1u is equivalent to 931.5 MeV E b =0.10844 931.5 E b =101.01186 MeV Therefore binding energy of a Nitrogen nucleus is 101.01186 MeV. -
Mass Fraction and the Isotopic Anomalies of Xenon and Krypton in Ordinary Chondrites
Scholars' Mine Masters Theses Student Theses and Dissertations 1971 Mass fraction and the isotopic anomalies of xenon and krypton in ordinary chondrites Edward W. Hennecke Follow this and additional works at: https://scholarsmine.mst.edu/masters_theses Part of the Chemistry Commons Department: Recommended Citation Hennecke, Edward W., "Mass fraction and the isotopic anomalies of xenon and krypton in ordinary chondrites" (1971). Masters Theses. 5453. https://scholarsmine.mst.edu/masters_theses/5453 This thesis is brought to you by Scholars' Mine, a service of the Missouri S&T Library and Learning Resources. This work is protected by U. S. Copyright Law. Unauthorized use including reproduction for redistribution requires the permission of the copyright holder. For more information, please contact [email protected]. MASS FRACTIONATION AND THE ISOTOPIC ANOMALIES OF XENON AND KRYPTON IN ORDINARY CHONDRITES BY EDWARD WILLIAM HENNECKE, 1945- A THESIS Presented to the Faculty of the Graduate School of the UNIVERSITY OF MISSOURI-ROLLA In Partial Fulfillment of the Requirements for the Degree MASTER OF SCIENCE IN CHEMISTRY 1971 T2572 51 pages by Approved ~ (!.{ 1.94250 ii ABSTRACT The abundance and isotopic composition of all noble gases are reported in the Wellman chondrite, and the abundance and isotopic composition of xenon and krypton are reported in the gases released by stepwise heating of the Tell and Scurry chondrites. Major changes in the isotopic composition of xenon result from the presence of radio genic Xel29 and from isotopic mass fractionation. The isotopic com position of trapped krypton in the different temperature fractions of the Tell and Scurry chondrites also shows the effect of isotopic fractiona tion, and there is a covariance in the isotopic composition of xenon with krypton in the manner expected from mass dependent fractiona tion. -
Chapter 16 Nuclear Chemistry
Chapter 16 275 Chapter 16 Nuclear Chemistry Review Skills 16.1 The Nucleus and Radioactivity Nuclear Stability Types of Radioactive Emissions Nuclear Reactions and Nuclear Equations Rates of Radioactive Decay Radioactive Decay Series The Effect of Radiation on the Body 16.2 Uses of Radioactive Substances Medical Uses Carbon-14 Dating Other Uses for Radioactive Nuclides 16.3 Nuclear Energy Nuclear Fission and Electric Power Plants Nuclear Fusion and the Sun Special Topic 16.1: A New Treatment for Brain Cancer Special Topic 16.2: The Origin of the Elements Chapter Glossary Internet: Glossary Quiz Chapter Objectives Review Questions Key Ideas Chapter Problems 276 Study Guide for An Introduction to Chemistry Section Goals and Introductions Section 16.1 The Nucleus and Radioactivity Goals To introduce the new terms nucleon, nucleon number, and nuclide. To show the symbolism used to represent nuclides. To explain why some nuclei are stable and others not. To provide you with a way of predicting nuclear stability. To describe the different types of radioactive decay. To show how nuclear reactions are different from chemical reactions. To show how nuclear equations are different from chemical equations. To show how the rates of radioactive decay can be described with half-life. To explain why short-lived radioactive atoms are in nature. To describe how radiation affects our bodies.. This section provides the basic information that you need to understand radioactive decay. It will also help you understand the many uses of radioactive atoms, including how they are used in medicine and in electricity generation. Section 16.2 Uses of Radioactive Substances Goal: To describe many of the uses of radioactive atoms, including medical uses, archaeological dating, smoke detectors, and food irradiation. -
Isotope Geochemistry of Carbonate Dissolution and Reprecipitation in Soils R
SOIL SCIENCE Vol. 122, No. I Copyright © 1976 by The Williams &Wilkin s Co. I'rintedin U.S.A. ISOTOPE GEOCHEMISTRY OF CARBONATE DISSOLUTION AND REPRECIPITATION IN SOILS W. SALOMONS' AND W. G. MOOK Laboratoryof Inorganic Chemistry'.The University of Groningen, Zernikelaan, Paddepoel,Groningen, the Netherlands, and Physics Laboratory, University of Groningen, Westersingel 34, Groningen, the Netherlands Received for publication May 21, 197/> ABSTRACT The processes of dissolution and reprecipitation of carbonates in soils developed on carbonate rocks, loess-derived soils, and marine clay soils were studied with the methods of stable isotope geochemistry. Between 10 and 50 percent of the carbonates present in the upper part of soils developed on carbonate rocks are newly formed. In loess-derived soils and in marine clay soils, up to 100 percent of the carbonates present may be newly formed. The efficiency of the dissolution-reprecipitation process varies between 10 and 30 percent. In the salt marsh investigated the dissolution is caused by the action of biogenic carbon dioxide. INTRODUCTION pies by treatment with 95 percent orthophos- Carbonates are an important constituent of phoric acid. The presence of organic matter in the soil. The processes they are subject to are most soil samples analyzed introduces an error dissolution followed by (partial) reprecipita in both the carbon and oxygen isotopic composi tion. Reprecipitation can be easily recognized tion of less than 0.37„o (Salomons 1974). when it results in macroscopic concretions. Since this small shift has no influence on our However, when the newly formed carbonates conclusions, the time-consuming step of remov are finely divided they are difficult to detect by ing the organic matter from the sample prior to conventional methods. -
All About Elements: Neon
All About Elements: Neon 1 Ward’s All About Elements Series Building Real-World Connections to the Building Blocks of Chemistry PERIODIC TABLE OF THE ELEMENTS GROUP 1/IA 18/VIIIA 1 2 H KEY He Atomic Number 1.01 2/IIA 35 13/IIIA 14/IVA 15/VA 16/VIA 17/VIIA 4.00 3 4 5 6 7 8 9 10 Li Be Symbol Br B C N O F Ne 6.94 9.01 79.90 Atomic Weight 10.81 12.01 14.01 16.00 19.00 20.18 11 12 13 14 15 16 17 18 Na Mg Al Si P S Cl Ar 8 9 10 22.99 24.31 3/IIIB 4/IVB 5/VB 6/VIB 7/VIIB VIIIBVIII 11/IB 12/IIB 26.98 28.09 30.97 32.07 35.45 39.95 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 K Ca Sc Ti V Cr Mn Fe Co Ni Cu Zn Ga Ge As Se Br Kr 39.10 40.08 44.96 47.87 50.94 52.00 54.94 55.85 58.93 58.69 63.55 65.41 69.72 72.64 74.92 78.9678.96 79.90 83.80 37 38 39 40 41 42 43 44 45 46 47 48 49 50 51 52 53 54 Rb Sr Y Zr Nb Mo Tc Ru Rh Pd Ag Cd In Sn Sb Te I Xe 85.47 87.62 88.91 91.22 92.91 95.94 (97.91)(98) 101.07 102.91 106.42 107.87 112.41 114.82 118.71 121.76 127.60 126.90 131.29 55 56 57–71 72 73 74 75 76 77 78 79 80 81 82 83 84 85 86 Cs Ba La-Lu Hf Ta W Re Os Ir Pt Au Hg Tl Pb Bi Po At Rn ´ 132.91 137.33 178.49 180.95 183.84 186.21 190.23 192.22 195.08 196.97 200.59 204.38 207.20207.2 208.98 (208.98)(209) (209.99)(210) (222.02)(222) 87 88 89–103 104 105 106 107 108 109 110 111 112 113 114 115 116 117 118 Fr Ra AcAc-Lr - Lr Rf Db Sg Bh Hs Mt Ds Rg Uub Uut Uuq Uup Uuh Uus Uuo ´´ (223.02)(223) (226.03)(226) (261.11)(261) (262.11)(262) (266.12)(266) (264.12)(264) (277.00)(277) (268.14)(268) (247.07)(269) (280.00)(272) (285.00)(285) (284.00)(284) (289.00)(289) (288.00)(288) (293.00)(289) (294.00) (294.00)(294) ´ 57 58 59 60 61 62 63 64 65 66 67 68 69 70 71 La Ce Pr Nd Pm Sm Eu Gd Tb Dy Ho Er Tm Yb Lu 138.91 140.12 140.91 144.24 (144.91)(145) 150.36 151.97151.96 157.25 158.93 162.50 164.93 167.26 168.93 173.04 174.97 US: www.wardsci.com Canada: www.wardsci.ca ´´ 800-962-2660 89 90 91 92 93 94 95 96 97 98 99 100 101 102 103 © 2010 Rev. -
Nuclear and Isotopic Techniques for Marine Pollution Monitoring
NUCLEAR AND ISOTOPIC TECHNIQUES FOR MARINE POLLUTION MONITORING A. Introduction The greatest natural resource on the Planet, the World Ocean is both the origin of most life forms and the source of survival for hundredsth of millions of people. Pollution of the oceans was an essential problem of the 20 century that was associated with the rapid industrializationst and unplanned occupation of coastal zones It continues to be a concern in the 21 century. The most serious environmental problems encountered in coastal zones are presented by runoff of agricultural nutrients, heavy metals, and persistent organic pollutants, such as pesticides and plastics. Oil spills from ships and tankers continually present a serious threat to birds, marine life and beaches. Also, many pesticides that are banned in most industrialized countries remain in use today, their trans-boundary pathway of dispersion affecting marine ecosystems the world over. In addition to these problems, ocean dumping of radioactive waste has occurred in the past, and might occur again, with authorised discharges of radioactive substances from nuclear facilities into rivers and coastal areas contributing to the contamination of the marine environment. A trans-boundary issue, marine pollution is often caused by inland economic activities, which lead to ecological changes in the marine environment. Examples include the use of chemicals in agriculture, atmospheric emissions from factories and automobiles, sewage discharges into lakes and rivers, and many other phenomena taking place hundreds or thousands of kilometres away from the seashore. Sooner or later, these activities affect the ecology of estuaries, bays, coastal waters, and sometimes entire seas, consequently having an impact on the economy related to maritime activities. -
Stable Isotopes of Carbon and Nitrogen in the Study of Avian and Mammalian Trophic Ecology
Color profile: Disabled Composite Default screen 1 REVIEW/SYNTHÈSE Stable isotopes of carbon and nitrogen in the study of avian and mammalian trophic ecology Jeffrey F. Kelly Abstract: Differential fractionation of stable isotopes of carbon during photosynthesis causes C4 plants and C3 plants to have distinct carbon-isotope signatures. In addition, marine C3 plants have stable-isotope ratios of carbon that are 13 12 intermediate between C4 and terrestrial C3 plants. The direct incorporation of the carbon-isotope ratio ( C/ C) of plants into consumers’ tissues makes this ratio useful in studies of animal ecology. The heavy isotope of nitrogen (15N) is preferentially incorporated into the tissues of the consumer from the diet, which results in a systematic enrichment in nitrogen-isotope ratio (15N/14N) with each trophic level. Consequently, stable isotopes of nitrogen have been used pri- marily to assess position in food chains. The literature pertaining to the use of stable isotopes of carbon and nitrogen in animal trophic ecology was reviewed. Data from 102 studies that reported stable-isotope ratios of carbon and (or) nitrogen of wild birds and (or) mammals were compiled and analyzed relative to diet, latitude, body size, and habitat moisture. These analyses supported the predicted relationships among trophic groups. Carbon-isotope ratios differed among species that relied on C3,C4, and marine food chains. Likewise, nitrogen-isotope ratios were enriched in terres- trial carnivorous mammals relative to terrestrial herbivorous mammals. -
NUCLEI LEARNING SHEET – 1 SOLUTIONS ANSWER KEY READ & EXPLAIN 1. Why Is the Atomic Mass of Chlorine Not an Integral Multi
NUCLEI LEARNING SHEET – 1 SOLUTIONS ANSWER KEY READ & EXPLAIN 1. Why is the atomic mass of chlorine not an integral multiple of hydrogen? A. Chlorine has two isotopes having masses 34.98u and 36.98u. These are nearly the integral multiples of the atomic mass of a hydrogen atom. Also, the relative abundance of these two isotopes is 75.4 % and 24.6% respectively. So, the average mass of chlorine is calculated by finding the weighted average of the masses of these two isotopes; which is, 35.47u. 2. 1 amu = ______ kg. A. 1.66 x 10-24 kg 3. What is the difference between isobars and isotones? A. Isobars are atoms that have the same mass number, i.e. the total number of protons and neutrons. Isotones have the same number of neutrons but different numbers of protons. 4. How many isotopes does Gold have? 197 195 A. Gold (79Au) has one stable isotope, Au, and 36 radioisotopes, with Au being the most stable with a half-life of 186 days. 5. Heavy stable nuclei have more neutrons than protons. This is because of the fact that (a) neutrons are heavier than protons. (b) electrostatic force between protons are repulsive. (c) neutrons decay into protons through beta decay. (d) nuclear forces between neutrons are weaker than that between protons. A. (b) electrostatic force between protons are repulsive. 6. The radius of a spherical nucleus as measured by electron scattering is 3.6 fm. What is the mass number of the nucleus? A. Given, r=3.6fm, r0=1.2fm 1/3 We know that the radius of spherical nucleus , r=r0A 푟 A=( )3 푟0 3.6 A=( )3 1.2 A=27 The correct answer is A. -
Correcting for Naturally Occurring Mass Isotopologue Abundances in Stable-Isotope Tracing Experiments with Polymid
H OH metabolites OH Article Correcting for Naturally Occurring Mass Isotopologue Abundances in Stable-Isotope Tracing Experiments with PolyMID Heesoo Jeong 1, Yan Yu 2, Henrik J. Johansson 3, Frank C. Schroeder 2, Janne Lehtiö 3 and Nathaniel M. Vacanti 1,3,* 1 Division of Nutritional Sciences, Cornell University, Ithaca, NY 14853, USA; [email protected] 2 Boyce Thompson Institute and Department of Chemistry and Chemical Biology, Cornell University, Ithaca, NY 14853, USA; [email protected] (Y.Y.); [email protected] (F.C.S.) 3 Science for Life Laboratory, Department of Oncology-Pathology, Karolinska Institutet, 17165 Solna, Sweden; [email protected] (H.J.J.); [email protected] (J.L.) * Correspondence: [email protected] Abstract: Stable-isotope tracing is a method to measure intracellular metabolic pathway utilization by feeding a cellular system a stable-isotope-labeled tracer nutrient. The power of the method to resolve differential pathway utilization is derived from the enrichment of metabolites in heavy isotopes that are synthesized from the tracer nutrient. However, the readout is complicated by the presence of naturally occurring heavy isotopes that are not derived from the tracer nutrient. Herein we present an algorithm, and a tool that applies it (PolyMID-Correct, part of the PolyMID software package), to computationally remove the influence of naturally occurring heavy isotopes. Citation: Jeong, H.; Yu, Y.; Johansson, The algorithm is applicable to stable-isotope tracing data collected on low- and high- mass resolution H.J.; Schroeder, F.C.; Lehtiö, J.; mass spectrometers. PolyMID-Correct is open source and available under an MIT license. Vacanti, N.M.