Radon - a Dangerous Link in the Decay Series of Uranium
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Lead Isotopes As Indicators of Environ Contamination from U Mining
._ .- - Preprint LA-UR-78-2147 , Title: LEAD ISOTOPES AS INDICATORS OF ENVIRONt1 ENTAL CONTAMINATION FRCM THE URANIUM MINING AND MILLING INDUSTRY IN THE GRANTS MINERAL BELT, NEW MEXICO Author (s): David B. Curtis and A. J. Gancarz 'k |- . 9 M/ - ' # - L .. %|.RkN: %| * & ,AQ' ,,7 ,e- d*157 ff' k g*/h T .s .. ; f*M & f g W , w -e ~ - " f:} + - pYW pm K .A ,W.% :M & Lw< *b* ? --~ k Y Q Q A -ell' 2_W h _ -- $| - f.s c t Q & Ye # C4HEhreSE33rzgmF %gh gM n [,315 ? M e % @N Y $ $ j3 h e fe l 2 D S $s - - #5 ~N [ ' & 9; - - - f _ '- ~ w e- * g r e w w 2 P As Nc- ' ** * -- - - - - $%y~ - . 9 . j'*( -, ' & . i .- f 1 * - -- ** -- e=* -h .Mr g g* ~ A _. y . gh(An ,, - ?fw h. y C: *, 1% * ~ ?, ?hSlh$i $ ': ffg w s - gp$lQ?$4$5;.>qgg - , .. INS is a Wegint of a paper intended for publication in 4 * '" M jour'ai or procet%1 ergs. Because changes rnay be made before f h , ' , publicction, this preprint is seiade available with the under. f ,- ' , starviing that it will not be died or reproduced without the * +' % '""'***'*C**' " permiss;or of the author, ') O 9 7 - _. _ _ . _ _ _ . _ - _ 0808.0 [ L * ' * . Q - 42 - 72 2)<f y . 1 LEAD ISOTOPES AS INDICATORS OF ENVIRONMENTAL CONTAMINATION FROM THE URANIUM MINING AND MILI.ING INDUSTitY .IN THE GRANIS MINERAL BELT, NEW NEXICO David B. Curtis and A. J. Gancar2 Los Alamos Scientine Laboratory Los Alamos, New Mexico, USA The unique isotopie composition oflead from uranium ores can be useful in studying ihe impact of ore processing efHuents on the env:ronment. -
What Is Radon?
Biology Unit Radon Alert INVESTIGATION 3 WHAT IS RADON? INTRODUCTION Radon is a naturally occurring radioactive gas. It is formed by the radioactive breakdown of radium, and is found in soils just about everywhere. You cannot see it, taste it, or smell it. It is continuously formed in rocks and soils and escapes into the atmosphere. In some cases, it makes its way into homes, builds up to high concentrations in indoor air, and can become a health hazard. Although there are several different isotopes of radon, the one that is of greatest concern as a potential Radioactivity - the spontaneous human health threat is called radon-222. Radon-222 is emission of energy by certain (radio- formed naturally during a chain of radioactive disintegra- active) atoms, resulting in a change tion reactions (decay series). The decay series begins from one element to another or one when uranium-238 decays. Uranium is widely distrib- isotope to another. The energy can uted in rocks and soils throughout the earth’s crust. It has be in the form of alpha or beta par- a half-life of 4.5 billion years, which means a very slow ticles and gamma rays. breakdown. The decay series is shown schematically in Figure 1. There are eight different elements and 15 different isotopes in the series, beginning with uranium- 238 and ending with lead-206. New elements formed by radioactive disintegration reactions are called decay products. Thus, radium-226 is one of the decay products of uranium-238. Polonium-218 and lead-214 are decay products of radon-222. -
Cyclotron Produced Lead-203 P
Postgrad Med J: first published as 10.1136/pgmj.51.601.751 on 1 November 1975. Downloaded from Postgraduate Medical Journal (November 1975) 51, 751-754. Cyclotron produced lead-203 P. L. HORLOCK M. L. THAKUR L.R.I.C. M.Sc., Ph.D. I. A. WATSON M.Sc. MRC Cyclotron Unit, Hammersmith Hospital, Du Cane Road, London W12 OHS Introduction TABLE 1. Isotopes of lead Radioactive isotopes of lead occur in the natural Isotope Half-life Principal y energy radioactive series and have been used as decay 194Pb m * tracers since the early days of radiochemistry. These 195Pb 17m * are 210Pb (ti--204 y, radium D), 212Pb (t--10. 6 h, 96Pb 37 m * thorium B) and 214Pb (t--26.8 m, radium B) all of 197Pb 42 m * which are from occurring decay 197pbm 42 m * separated naturally 198pb 24 h * products ofradium or thorium. There are in addition 19spbm 25 m * Protected by copyright. to these a number of other radioactive isotopes of 199Pb 90 m * lead which can be produced artificially with the aid 19spbm 122 m * of a nuclear reactor or a accelerator 20OPb 21-5 h ** 0-109 to 0-605 (complex) charge particle (daughter radiations) (Table 1). 2Pb 9-4 h * There are at least three criteria in choosing the 0oipbm 61 s * radioactive isotope for in vitro tracer studies. First, 20pb 3 x 105y *** TI X-rays, (daughter it should emit radiation which is easily detected. radiations) have a half-life to 202pbm 3-62 h * Secondly, it should long enough aPb 52-1 h ** 0-279 (81%) 0-401 (5%) 0-680 permit studies without excessive radioactive decay 203pbm 6-1 s * (0-9%) (no daughter occurring but not so long that waste disposal radiations) creates a problem. -
Proton-Induced Cross-Sections of Nuclear Reactions on Lead up to 37 Mev
Proton-induced cross-sections of nuclear reactions on lead up to 37 MeV F. Ditroi´ a,∗, F. Tark´ anyi´ a, S. Takacs´ a, A. Hermanneb aInstitute for Nuclear Research, Hungarian Academy of Sciences (ATOMKI), Debrecen, Hungary bCyclotron Laboratory, Vrije Universiteit Brussel (VUB), Brussels, Belgium Abstract Excitation function of proton induced nuclear reactions on lead for production of 206;205;204;203;202;201gBi, 203cum;202m;201cumPb and 202cum;201cum;200cum;199cumTl radionuclides were measured up to 36 MeV by using activation method, stacked foil irradiation technique and ?-ray spectrometry. The new experimental data were compared with the few earlier experimental results and with the predictions of the EMPIRE 3.1, ALICE-IPPE (MENDL2p) and TALYS (TENDL-2012) theoretical reaction codes. Keywords: lead target, cross-section by proton activation, theoretical model codes, thin layer activation (TLA) 1. Introduction this, only a few experimental data sets exist, collected mostly by the experimental groups. In the low energy Production cross-sections of proton induced nuclear region practically only one experimental cross-section reactions on lead are important for many applications is available from the Hannover-Cologne group. In our and for the development of nuclear reaction theory. research and application work in connection with the Lead is an important technological material as pure el- activation cross-sections on lead we were involved in ement as well as alloying agent and it is also widely different projects and applications: used in different nuclear technologies, as well as tar- get material for production of 201Tl medical diagnostic • preparation of nuclear database for production of gamma-emitter for SPECT technology (Lagunas-Solar medical radioisotopes in the frame of an IAEA Co- et al., 1981). -
THE NATURAL RADIOACTIVITY of the BIOSPHERE (Prirodnaya Radioaktivnost' Iosfery)
XA04N2887 INIS-XA-N--259 L.A. Pertsov TRANSLATED FROM RUSSIAN Published for the U.S. Atomic Energy Commission and the National Science Foundation, Washington, D.C. by the Israel Program for Scientific Translations L. A. PERTSOV THE NATURAL RADIOACTIVITY OF THE BIOSPHERE (Prirodnaya Radioaktivnost' iosfery) Atomizdat NMoskva 1964 Translated from Russian Israel Program for Scientific Translations Jerusalem 1967 18 02 AEC-tr- 6714 Published Pursuant to an Agreement with THE U. S. ATOMIC ENERGY COMMISSION and THE NATIONAL SCIENCE FOUNDATION, WASHINGTON, D. C. Copyright (D 1967 Israel Program for scientific Translations Ltd. IPST Cat. No. 1802 Translated and Edited by IPST Staff Printed in Jerusalem by S. Monison Available from the U.S. DEPARTMENT OF COMMERCE Clearinghouse for Federal Scientific and Technical Information Springfield, Va. 22151 VI/ Table of Contents Introduction .1..................... Bibliography ...................................... 5 Chapter 1. GENESIS OF THE NATURAL RADIOACTIVITY OF THE BIOSPHERE ......................... 6 § Some historical problems...................... 6 § 2. Formation of natural radioactive isotopes of the earth ..... 7 §3. Radioactive isotope creation by cosmic radiation. ....... 11 §4. Distribution of radioactive isotopes in the earth ........ 12 § 5. The spread of radioactive isotopes over the earth's surface. ................................. 16 § 6. The cycle of natural radioactive isotopes in the biosphere. ................................ 18 Bibliography ................ .................. 22 Chapter 2. PHYSICAL AND BIOCHEMICAL PROPERTIES OF NATURAL RADIOACTIVE ISOTOPES. ........... 24 § 1. The contribution of individual radioactive isotopes to the total radioactivity of the biosphere. ............... 24 § 2. Properties of radioactive isotopes not belonging to radio- active families . ............ I............ 27 § 3. Properties of radioactive isotopes of the radioactive families. ................................ 38 § 4. Properties of radioactive isotopes of rare-earth elements . -
Of the Periodic Table
of the Periodic Table teacher notes Give your students a visual introduction to the families of the periodic table! This product includes eight mini- posters, one for each of the element families on the main group of the periodic table: Alkali Metals, Alkaline Earth Metals, Boron/Aluminum Group (Icosagens), Carbon Group (Crystallogens), Nitrogen Group (Pnictogens), Oxygen Group (Chalcogens), Halogens, and Noble Gases. The mini-posters give overview information about the family as well as a visual of where on the periodic table the family is located and a diagram of an atom of that family highlighting the number of valence electrons. Also included is the student packet, which is broken into the eight families and asks for specific information that students will find on the mini-posters. The students are also directed to color each family with a specific color on the blank graphic organizer at the end of their packet and they go to the fantastic interactive table at www.periodictable.com to learn even more about the elements in each family. Furthermore, there is a section for students to conduct their own research on the element of hydrogen, which does not belong to a family. When I use this activity, I print two of each mini-poster in color (pages 8 through 15 of this file), laminate them, and lay them on a big table. I have students work in partners to read about each family, one at a time, and complete that section of the student packet (pages 16 through 21 of this file). When they finish, they bring the mini-poster back to the table for another group to use. -
Keeping Your Home Safe from RADON
Keeping Your Home Safe From RADON 800-662-9278 | Michigan.gov/radon 08/2019 What is Radon? Radon is a colorless and odorless gas that comes from the soil. The gas can accumulate in our home and in the air we breathe. Radon gas decays into fine particles that are radioactive. When inhaled, these fine particles can damage the lung. Exposure to radon over a long period of time can lead to lung cancer. It is estimated that 21,000 people die each year in the United States from lung cancer due to radon exposure. A radon test is the only way to know how much radon is in your home. Radon can be reduced with a mitigation system. The Michigan Department of Environment, Great Lakes, and Energy (EGLE) has created this guide to explain: • How radon accumulates in homes • The health risks of radon exposure • How to test your home for radon • What to do if your home has high radon • Radon policies C Keeping Your Home Safe From Radon Table of Contents Where Does Radon Come From? ............................................. 1 Radon in Michigan ....................................................................... 1 Percentage of Elevated Radon Test Results by County ......... 2 Is There a Safe Level of Radon? ............................................... 3 Radon Health Risks ..................................................................... 4 How Radon Enters the Home ..................................................... 6 Radon Pathways ........................................................................... 7 Radon Testing ............................................................................ -
Radionuclides (Including Radon, Radium and Uranium)
Radionuclides (including Radon, Radium and Uranium) Hazard Summary Uranium, radium, and radon are naturally occurring radionuclides found in the environment. No information is available on the acute (short-term) noncancer effects of the radionuclides in humans. Animal studies have reported inflammatory reactions in the nasal passages and kidney damage from acute inhalation exposure to uranium. Chronic (long-term) inhalation exposure to uranium and radon in humans has been linked to respiratory effects, such as chronic lung disease, while radium exposure has resulted in acute leukopenia, anemia, necrosis of the jaw, and other effects. Cancer is the major effect of concern from the radionuclides. Radium, via oral exposure, is known to cause bone, head, and nasal passage tumors in humans, and radon, via inhalation exposure, causes lung cancer in humans. Uranium may cause lung cancer and tumors of the lymphatic and hematopoietic tissues. EPA has not classified uranium, radon or radium for carcinogenicity. Please Note: The main sources of information for this fact sheet are EPA's Integrated Risk Information System (IRIS) (5), which contains information on oral chronic toxicity and the RfD for uranium, and the Agency for Toxic Substances and Disease Registry's (ATSDR's) Toxicological Profiles for Uranium, Radium, and Radon. (1) Uses Uranium is used in nuclear power plants and nuclear weapons. Very small amounts are used in photography for toning, in the leather and wood industries for stains and dyes, and in the silk and wood industries. (2) Radium is used as a radiation source for treating neoplastic diseases, as a radon source, in radiography of metals, and as a neutron source for research. -
Recalling Radon's Recognition
in your element Recalling radon’s recognition Brett F. Thornton and Shawn C. Burdette look back at the discovery — and the many different names — of element 86. n 1899, Pierre and Marie Curie noted an Thoron, unlike radon, requires no such “induced radioactivity” — left behind by clarification, and 220Rn is routinely called Iradium, distinct from its own radioactivity. thoron today. Thoron is far easier to say Ernest Rutherford and Robert B. Owens also than ‘radon-two-twenty’, perhaps explaining reported that year on a radioactive substance why the annual count of scientific papers 220 ( Rn, t1/2 = 55.6 s) emitted by thorium, which mentioning thoron has increased over twenty- they called emanation. In 1900, Friedrich fold since thoron was ‘disallowed’ in 1957. Dorn realized that the Curies had observed a Distinguishing between 222Rn (the 222 220 unique substance ( Rn, t1/2 = 3.8 d), similar isotope called ‘radon’) and Rn (thoron) is to emanation. In 1904, André-Louis Debierne not of idle linguistic and historic interest. 222 found a third radioactive particle; this one © SUPERSTOCK/ALAMY Rn can persist indoors, whereas the short- 219 produced from actinium ( Rn, t1/2 = 4 s). lived thoron cannot. Not all home radon These were at first regarded as elements and actinon (An) for the three isotopes; detectors (pictured) are sensitive to thoron, and became colloquially known as thorium names suggested by Elliott Q. Adams. and thoron-sensitive detectors must be emanation, radium emanation and actinium An official statement on a name for all placed with care because thoron does not emanation, but today we recognize them three isotopes — that is, a name for the travel far from its source. -
The Noble Gases
INTERCHAPTER K The Noble Gases When an electric discharge is passed through a noble gas, light is emitted as electronically excited noble-gas atoms decay to lower energy levels. The tubes contain helium, neon, argon, krypton, and xenon. University Science Books, ©2011. All rights reserved. www.uscibooks.com Title General Chemistry - 4th ed Author McQuarrie/Gallogy Artist George Kelvin Figure # fig. K2 (965) Date 09/02/09 Check if revision Approved K. THE NOBLE GASES K1 2 0 Nitrogen and He Air P Mg(ClO ) NaOH 4 4 2 noble gases 4.002602 1s2 O removal H O removal CO removal 10 0 2 2 2 Ne Figure K.1 A schematic illustration of the removal of O2(g), H2O(g), and CO2(g) from air. First the oxygen is removed by allowing the air to pass over phosphorus, P (s) + 5 O (g) → P O (s). 20.1797 4 2 4 10 2s22p6 The residual air is passed through anhydrous magnesium perchlorate to remove the water vapor, Mg(ClO ) (s) + 6 H O(g) → Mg(ClO ) ∙6 H O(s), and then through sodium hydroxide to remove 18 0 4 2 2 4 2 2 the carbon dioxide, NaOH(s) + CO2(g) → NaHCO3(s). The gas that remains is primarily nitrogen Ar with about 1% noble gases. 39.948 3s23p6 36 0 The Group 18 elements—helium, K-1. The Noble Gases Were Kr neon, argon, krypton, xenon, and Not Discovered until 1893 83.798 radon—are called the noble gases 2 6 4s 4p and are noteworthy for their rela- In 1893, the English physicist Lord Rayleigh noticed 54 0 tive lack of chemical reactivity. -
Discovery of the Thallium, Lead, Bismuth, and Polonium Isotopes
Discovery of the thallium, lead, bismuth, and polonium isotopes C. Fry, M. Thoennessen∗ National Superconducting Cyclotron Laboratory and Department of Physics and Astronomy, Michigan State University, East Lansing, MI 48824, USA Abstract Currently, forty-two thallium, forty-two lead, forty-one bismuth, and forty-two polonium 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 October 6, 2011 Contents 1. Introduction . 2 2. 176−217Tl ............................................................................................. 3 3. 179−220Pb............................................................................................. 14 4. 184−224Bi ............................................................................................. 22 5. 186−227Po ............................................................................................. 31 6. Summary ............................................................................................. 39 References . 39 Explanation of Tables . 47 7. Table 1. Discovery of thallium, lead, bismuth, and polonium isotopes . 47 Table 1. Discovery of thallium, lead, bismuth, and polonium. See page 47 for Explanation of Tables . 48 1. Introduction The discovery of thallium, lead, bismuth, and polonium -
Radon in the Helium-Bearing Natural Gas of the Texas Panhandle
ej f Radon in the Helium-Bearing Natural Gas of the Texas Panhandle Trace Elements Memorandum Report 239 IN REPLY REFER TO: UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY WASHINGTON 25, D. C. AEC-4-98/1 Dr0 Phillip L 0 Merritt, Assistant Manager Raw Materials Operations U0 So Atomic Energy Commission Po 00 Box 30? Ansonia Station New York 23, New York Dear Phils Transmitted herewith for your information and distribution are 8 copies of Trace Elements Memorandum Report 239 9 "Radon in the helium=>bearing natural gas of the Texas Panhandle," by H0 Faul, Go Eo Mangerj and A0 Y0 Sakakura 0 Our measurements of the radon content of natural gas samples from 84 producing wells in the Texas Panhandle gas field show signifi- cant differences5 furthermore 9 the wells with the highest radon content occur in clusters suggesting a marked variation in the distribution of the parent elements of radon, namely radium and uranium., within or near the gas reservoir., Analysis of the radon data in relation to possible source distribution suggests that rocks containing average concentrations of uranium could not supply the amount of radon observed in most of the gas wellso Further research on the emanating power of granite and dolo mite is required to determine whether the radon observed is attributable to radioactive elements in the reservoir rock or to radioactive elements outside the reservoir volume proper0 The Oak Ridge National Laboratory k©s already initiated preliminary studies of the emanating power of the selected dolomite samples 0 Additional radon measurements, are needed to establish the limits of the abnormal radon concentration and further delineate the possible distribution of the parent !.element 0 Sincerely yours., '^SvwA^ W0 H Bradley I Chief Geologist fITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY RADON IN THE HELIUM-BEARING NATURAL GAS OF THE TEXAS PANHANDLE H.