Uncertainties in Cancer Risk Coefficients for Environmental Exposure to Radionuclides
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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. -
Understanding Variation in Partition Coefficient, Kd, Values: Volume II
United States Office of Air and Radiation EPA 402-R-99-004B Environmental Protection August 1999 Agency UNDERSTANDING VARIATION IN PARTITION COEFFICIENT, Kd, VALUES Volume II: Review of Geochemistry and Available Kd Values for Cadmium, Cesium, Chromium, Lead, Plutonium, Radon, Strontium, Thorium, Tritium (3H), and Uranium UNDERSTANDING VARIATION IN PARTITION COEFFICIENT, Kd, VALUES Volume II: Review of Geochemistry and Available Kd Values for Cadmium, Cesium, Chromium, Lead, Plutonium, Radon, Strontium, Thorium, Tritium (3H), and Uranium August 1999 A Cooperative Effort By: Office of Radiation and Indoor Air Office of Solid Waste and Emergency Response U.S. Environmental Protection Agency Washington, DC 20460 Office of Environmental Restoration U.S. Department of Energy Washington, DC 20585 NOTICE The following two-volume report is intended solely as guidance to EPA and other environmental professionals. This document does not constitute rulemaking by the Agency, and cannot be relied on to create a substantive or procedural right enforceable by any party in litigation with the United States. EPA may take action that is at variance with the information, policies, and procedures in this document and may change them at any time without public notice. Reference herein to any specific commercial products, process, or service by trade name, trademark, manufacturer, or otherwise, does not necessarily constitute or imply its endorsement, recommendation, or favoring by the United States Government. ii FOREWORD Understanding the long-term behavior of contaminants in the subsurface is becoming increasingly more important as the nation addresses groundwater contamination. Groundwater contamination is a national concern as about 50 percent of the United States population receives its drinking water from groundwater. -
Experimental Γ Ray Spectroscopy and Investigations of Environmental Radioactivity
Experimental γ Ray Spectroscopy and Investigations of Environmental Radioactivity BY RANDOLPH S. PETERSON 216 α Po 84 10.64h. 212 Pb 1- 415 82 0- 239 β- 01- 0 60.6m 212 1+ 1630 Bi 2+ 1513 83 α β- 2+ 787 304ns 0+ 0 212 α Po 84 Experimental γ Ray Spectroscopy and Investigations of Environmental Radioactivity Randolph S. Peterson Physics Department The University of the South Sewanee, Tennessee Published by Spectrum Techniques All Rights Reserved Copyright 1996 TABLE OF CONTENTS Page Introduction ....................................................................................................................4 Basic Gamma Spectroscopy 1. Energy Calibration ................................................................................................... 7 2. Gamma Spectra from Common Commercial Sources ........................................ 10 3. Detector Energy Resolution .................................................................................. 12 Interaction of Radiation with Matter 4. Compton Scattering............................................................................................... 14 5. Pair Production and Annihilation ........................................................................ 17 6. Absorption of Gammas by Materials ..................................................................... 19 7. X Rays ..................................................................................................................... 21 Radioactive Decay 8. Multichannel Scaling and Half-life ..................................................................... -
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 . -
A Living Radon Reference Manual
A LIVING RADON REFERENCE MANUAL Robert K. Lewis Pennsylvania Department of Environmental Protection Bureau of Radiation Protection, Radon Division and Paul N. Houle, PhD University Educational Services, Inc. Abstract This “living” manual is a compilation of facts, figures, tables and other information pertinent and useful to the radon practitioner, some of which can be otherwise difficult to find. It is envisioned as a useful addition to one’s desk and radon library. This reference manual is also intended to be a “living” document, where its users may supply additional information to the editors for incorporation in revisions as well as updates to this document on-line. Topics contained within the current version include radon chemistry and physics, radon units, radon fans, epidemiology, ambient radon, diagnostics, dosimetry, history, lung cancer, radon in workplace and radon statistics. In some cases motivations and explanations to the information are given. References are included. Introduction This reference manual is a compilation of facts, figures, tables and information on various aspects of radon science. It is hoped that this manual may prove useful to federal and state employees, groups such as AARST and CRCPD, and industry. There are numerous other reference manuals that have been produced on the various aspects of radon science; however, we hope that this manual will have a more “applied” use to all of the various radon practitioners who may use it. Many of the snippets on the various pages are highlights from referenced sources. The snippet will obviously only provide one with the briefest of information. To learn more about that item go to the reference and read the whole paper. -
Mathematical Model of Radon Activity Measurements
2015 International Nuclear Atlantic Conference - INAC 2015 São Paulo, SP, Brazil, October 4-9, 2015 ASSOCIAÇÃO BRASILEIRA DE ENERGIA NUCLEAR - ABEN ISBN: 978-85-99141-06-9 MATHEMATICAL MODEL OF RADON ACTIVITY MEASUREMENTS Sergei A. Paschuk1, Janine N. Corrêa1, Jaqueline Kappke1, Pedro Zambianchi1 and Valeriy Denyak2 1 Federal University of Technology - Paraná Av. Sete de Setembro, 3165 80230-901, Curitiba, PR [email protected], [email protected] 2 Pelé Pequeno Príncipe Research Institute, Av. Silva Jardim, 1632, Curitiba 80250-200, PR, Brazil [email protected] ABSTRACT Present work describes a mathematical model that quantifies the time dependent amount of 222Rn and 220Rn altogether and their activities within an ionization chamber as, for example, AlphaGUARD, which is used to measure activity concentration of Rn in soil gas. The differential equations take into account tree main processes, namely: the injection of Rn into the cavity of detector by the air pump including the effect of the traveling time Rn takes to reach the chamber; Rn release by the air exiting the chamber; and radioactive decay of Rn within the chamber. Developed code quantifies the activity of 222Rn and 220Rn isotopes separately. Following the standard methodology to measure Rn activity in soil gas, the air pump usually is turned off over a period of time in order to avoid the influx of Rn into the chamber. Since 220Rn has a short half-life time, approximately 56s, the model shows that after 7 minutes the activity concentration of this isotope is null. Consequently, the measured activity refers to 222Rn, only. Furthermore, the model also addresses the activity of 220Rn and 222Rn progeny, which being metals represent potential risk of ionization chamber contamination that could increase the background of further measurements. -
Radiation Weighting Factors
Sources of Radiation Exposure Sources of Radiation Exposure to the US Population (from U.S. NRC, Glossary: Exposure. [updated 21 July 2003, cited 26 March 2004] http://www.nrc.gov/reading-rm/basic-ref/glossary/exposure.html In the US, the annual estimated average effective dose to an adult is 3.60 mSv. Sources of exposure for the general public • Natural radiation of terrestrial origin • Natural radiation of cosmic origin • Natural internal radioisotopes • Medical radiation • Technologically enhanced natural radiation • Consumer products • Fallout • Nuclear power Other 1% Occupational 3% Fallout <0.3% Nuclear Fuel Cycle 0.1% Miscellaneous 0.1% Radioactivity in Nature Our world is radioactive and has been since it was created. Over 60 radionuclides can be found in nature, and they can be placed in three general categories: Primordial - been around since the creation of the Earth Singly-occurring Chain or series Cosmogenic - formed as a result of cosmic ray interactions Primordial radionuclides When the earth was first formed a relatively large number of isotopes would have been radioactive. Those with half-lives of less than about 108 years would by now have decayed into stable nuclides. The progeny or decay products of the long-lived radionuclides are also in this heading. Primordial nuclide examples Half-life Nuclide Natural Activity (years) Uranium 7.04 x 108 0.72 % of all natural uranium 235 Uranium 99.27 % of all natural uranium; 0.5 to 4.7 ppm total 4.47 x 109 238 uranium in the common rock types Thorium 1.6 to 20 ppm in the common -
Radon in Icelandic Cold Groundwater and Low-Temperature Geothermal Water
Available online at www.sciencedirect.com ScienceDirect Procedia Earth and Planetary Science 17 ( 2017 ) 229 – 232 15th Water-Rock Interaction International Symposium, WRI-15 Radon in Icelandic Cold Groundwater and Low-Temperature Geothermal Water Finnbogi Óskarssona,1, Ragnheiður St. Ásgeirsdóttira aIceland GeoSurvey (ISOR), Grensasvegur 9, IS-108 Reykjavik, Iceland Abstract Samples of hot and cold water for radon analysis were collected from boreholes and springs in Iceland in 2014 and 2015. The majority of the samples was collected from municipal district heating services or potable water utilities. The total number of samples was 142, covering most towns and villages in Iceland. Radon activity is generally rather low, in most cases less than 5 Bq/L. Only 12 samples had a measured radon activity higher than 5 Bq/L, with a maximum activity of 10.8 Bq/L. The hot water samples generally have a higher radon activity than cold water samples, but samples from boiling borholes have a lower radon activity as radon fractionates into the vapour phase. The geographical distribution of the samples indicates that radon activity is generally lower within the active rift zones. This is most likely due to the very low uranium content of the tholeiites typically erupted within the rift zones. Higher radon values (> 5 Bq/L) are in most cases close to extinct central volcanoes and thus it seems plausible that the water sampled has been in contact with felsic rocks. © 20172017 The The Authors. Authors. Published Published by Elsevierby Elsevier B.V. B.V. This is an open access article under the CC BY-NC-ND license Peer(http://creativecommons.org/licenses/by-nc-nd/4.0/-review under responsibility of the organizing). -
Point Defects in Lithium Gallate and Gallium Oxide
Air Force Institute of Technology AFIT Scholar Theses and Dissertations Student Graduate Works 8-23-2019 Point Defects in Lithium Gallate and Gallium Oxide Christopher A. Lenyk Follow this and additional works at: https://scholar.afit.edu/etd Part of the Nuclear Engineering Commons Recommended Citation Lenyk, Christopher A., "Point Defects in Lithium Gallate and Gallium Oxide" (2019). Theses and Dissertations. 2369. https://scholar.afit.edu/etd/2369 This Dissertation is brought to you for free and open access by the Student Graduate Works at AFIT Scholar. It has been accepted for inclusion in Theses and Dissertations by an authorized administrator of AFIT Scholar. For more information, please contact [email protected]. POINT DEFECTS IN LITHIUM GALLATE AND GALLIUM OXIDE DISSERTATION Christopher A. Lenyk, Lt Col, USAF AFIT-ENP-DS-19-S-023 DEPARTMENT OF THE AIR FORCE AIR UNIVERSITY AIR FORCE INSTITUTE OF TECHNOLOGY Wright-Patterson Air Force Base, Ohio DISTRIBUTION STATEMENT A. APPROVED FOR PUBLIC RELEASE; DISTRIBUTION UNLIMITED. The views expressed in this document are those of the author and do not reflect the official policy or position of the United States Air Force, the United States Department of Defense or the United States Government. This material is declared a work of the U.S. Government and is not subject to copyright protection in the United States. AFIT-ENP-DS-19-S-023 POINT DEFECTS IN LITHIUM GALLATE AND GALLIUM OXIDE DISSERTATION Presented to the Faculty Graduate School of Engineering and Management Air Force Institute of Technology Air University Air Education and Training Command in Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy in Nuclear Engineering Christopher A. -
Z 221 PS2 Practice.Pages
CH 221 Practice Problem Set #2 This is a practice problem set and not the actual graded problem set that you will turn in for credit. Answers to each problem can be found at the end of this assignment. Covering: Chapter Two, Chapter 3.1 and Chapter Guide Two Important Tables and/or Constants: 1 mol = 6.022 x 1023 ! 1. Give the mass number of each of the following atoms: a. magnesium with 15 neutrons, b. titanium with 26 neutrons, and c. zinc with 32 neutrons. A 2. Give the complete symbol ( ZX) for each of the following atoms: a. potassium with 20 neutrons, b. krypton with 48 neutrons, and c. cobalt with 33 neutrons. 3. Thallium has two stable isotopes, 203Tl and 205Tl. Knowing that the atomic weight of thallium is 204.4, which isotope€ is the more abundant of the two? 4. Silver (Ag) has two stable isotopes, 107Ag and 109Ag. The isotopic mass of 107Ag is 106.9051 and the isotopic mass of 109Ag is 108.9047. The atomic weight of Ag, from the periodic table, is 107.868. Estimate the percentage of 107Ag in a sample of the element. a. 0% b. 25% c. 50% d. 75% 5. Gallium has two naturally occurring isotopes, 69Ga and 71Ga, with masses of 68.9257 u and 70.9249 u, respectively. Calculate the percent abundances of these isotopes of gallium. 6. Calculate the mass in grams of: a. 2.5 mol aluminum b. 1.25 x 10-3 mol of iron c. 0.015 mol of calcium d. -
Isotope Geochemistry of Gallium in Hydrothermal Systems
ISOTOPE GEOCHEMISTRY OF GALLIUM IN HYDROTHERMAL SYSTEMS by Constance E. Payne A thesis submitted to Victoria University of Wellington in partial fulfilment of the requirements for the degree of Master of Science Victoria University of Wellington 2016 ABSTRACT Little is known about the isotope geochemistry of gallium in natural systems (Groot, 2009), with most information being limited to very early studies of gallium isotopes in extra-terrestrial samples (Aston, 1935; De Laeter, 1972; Inghram et al., 1948; Machlan et al., 1986). This study is designed as a reconnaissance for gallium isotope geochemistry in hydrothermal systems of New Zealand. Gallium has two stable isotopes, 69Ga and 71Ga, and only one oxidation state, Ga3+, in aqueous media (Kloo et al., 2002). This means that fractionation of gallium isotopes should not be effected by redox reactions. Therefore the physical processes that occur during phase changes of hydrothermal fluids (i.e. flashing of fluids to vapour phase and residual liquid phase) and mineralisation of hydrothermal precipitates (i.e. precipitation and ligand exchange) can be followed by studying the isotopes of gallium. A gallium anomaly is known to be associated with some hydrothermal processes as shown by the unusual, elevated concentrations (e.g. 290 ppm in sulfide samples of Waiotapu; this study) in several of the active geothermal systems in New Zealand. The gallium isotope system has not yet been investigated since the revolution of high precision isotopic ratio measurements by Multi-Collector Inductively Coupled Plasma Mass Spectrometry (MC-ICPMS) and so a new analytical methodology needed to be established. Any isotopic analysis of multi-isotope elements must satisfy a number of requirements in order for results to be both reliable and meaningful. -
ATOMS and ELEMENTS Chapter 2 and Chapter 3 (3.1) “Chapter 2 Part 1” Elements: the Building Blocks of Nature Atoms: the Smallest Pieces of an Element
Page III-2a-1 / Chapter Two Part I Lecture Notes Atoms, Molecules and Ions ATOMS AND ELEMENTS Chapter 2 and Chapter 3 (3.1) “Chapter 2 Part 1” Elements: the building blocks of Nature Atoms: the smallest pieces of an element Atoms contain protons, Chemistry 221 neutrons and electrons Professor Michael Russell Protons and neutrons in the nucleus Last update: MAR 8/9/21 MAR Where Does Matter Come From? FROM THE Big Bang The universe is 13.77 billion years old Hydrogen and Helium important Also Carbon, Oxygen and Neon MAR MAR Early Models of the Atom - Empedocles & Aristotle Element Abundance (Cosmic) Empedocles’ theory of matter (later modified by Aristotle) with four Most abundant "elements" (coined by Plato) held C elements in the for approximately 2000 years! O Al Si Fe Earth's Element "mixtures" produce "properties" of hot, wet, etc. • Crust: Silicon and oxygen • Atmosphere: Plato Empedocles Aristotle nitrogen and oxygen MAR http://www.webelements.com/ MAR Page III-2a-1 / Chapter Two Part I Lecture Notes Page III-2a-2 / Chapter Two Part I Lecture Notes The "Newton" of Chemistry Early Models of the Atom - Democritus JOHN DALTON (1766 - 1844) DEMOCRITUS (460 - 370 BCE) 1804 - Proposed Atomic Theory was a contemporary of Plato "Atoms cannot be created or destroyed" "Atoms of one element are different from other Atoms have structure and volume element's atoms" - proposed relative scale of "Gold can be divided into atomic masses (now the amu) smaller pieces only so far before the pieces no longer "Chemical change involves bond breaking, retain