Superfund Radiation Risk Assessment: a Community Toolkit
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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. -
Monitored Natural Attenuation of Inorganic Contaminants in Ground
Monitored Natural Attenuation of Inorganic Contaminants in Ground Water Volume 3 Assessment for Radionuclides Including Tritium, Radon, Strontium, Technetium, Uranium, Iodine, Radium, Thorium, Cesium, and Plutonium-Americium EPA/600/R-10/093 September 2010 Monitored Natural Attenuation of Inorganic Contaminants in Ground Water Volume 3 Assessment for Radionuclides Including Tritium, Radon, Strontium, Technetium, Uranium, Iodine, Radium, Thorium, Cesium, and Plutonium-Americium Edited by Robert G. Ford Land Remediation and Pollution Control Division Cincinnati, Ohio 45268 and Richard T. Wilkin Ground Water and Ecosystems Restoration Division Ada, Oklahoma 74820 Project Officer Robert G. Ford Land Remediation and Pollution Control Division Cincinnati, Ohio 45268 National Risk Management Research Laboratory Office of Research and Development U.S. Environmental Protection Agency Cincinnati, Ohio 45268 Notice The U.S. Environmental Protection Agency through its Office of Research and Development managed portions of the technical work described here under EPA Contract No. 68-C-02-092 to Dynamac Corporation, Ada, Oklahoma (David Burden, Project Officer) through funds provided by the U.S. Environmental Protection Agency’s Office of Air and Radiation and Office of Solid Waste and Emergency Response. It has been subjected to the Agency’s peer and administrative review and has been approved for publication as an EPA document. Mention of trade names or commercial products does not constitute endorsement or recommendation for use. All research projects making conclusions or recommendations based on environmental data and funded by the U.S. Environmental Protection Agency are required to participate in the Agency Quality Assurance Program. This project did not involve the collection or use of environmental data and, as such, did not require a Quality Assurance Plan. -
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 ..................................................................... -
Modelling Transport and Deposition of Caesium and Iodine from the Chernobyl Accident Using the DREAM Model J
Modelling transport and deposition of caesium and iodine from the Chernobyl accident using the DREAM model J. Brandt, J. H. Christensen, L. M. Frohn To cite this version: J. Brandt, J. H. Christensen, L. M. Frohn. Modelling transport and deposition of caesium and iodine from the Chernobyl accident using the DREAM model. Atmospheric Chemistry and Physics, European Geosciences Union, 2002, 2 (5), pp.397-417. hal-00295217 HAL Id: hal-00295217 https://hal.archives-ouvertes.fr/hal-00295217 Submitted on 17 Dec 2002 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Atmos. Chem. Phys., 2, 397–417, 2002 www.atmos-chem-phys.org/acp/2/397/ Atmospheric Chemistry and Physics Modelling transport and deposition of caesium and iodine from the Chernobyl accident using the DREAM model J. Brandt, J. H. Christensen, and L. M. Frohn National Environmental Research Institute, Department of Atmospheric Environment, Frederiksborgvej 399, P.O. Box 358, DK-4000 Roskilde, Denmark Received: 11 April 2002 – Published in Atmos. Chem. Phys. Discuss.: 24 June 2002 Revised: 9 September 2002 – Accepted: 24 September 2002 – Published: 17 December 2002 Abstract. A tracer model, DREAM (the Danish Rimpuff and low cloud scavenging process for the submicron particles and Eulerian Accidental release Model), has been developed for that the precipitation rates are relatively uncertain in the me- modelling transport, dispersion and deposition (wet and dry) teorological model compared to the relative humidity. -
New York State Department of Health Environmental Radiation Program Environmental Radiation Surveillance Site Readings
New York State Department of Health Environmental Radiation Program Environmental Radiation Surveillance Site Readings Glossary This glossary has been added in order to define technical terms that are used in the various supporting documents for this data set. Please refer to the Data Dictionary for explanation of the meaning of the column headings in the data set. 1. Alpha particles- a positively charged particle made up of two neutrons and two protons emitted by certain radioactive nuclei. a. Gross alpha radioactivity- a measurement of all alpha activity present, regardless of specific radionuclide source. 2. Americium (chemical symbol Am) - is a man-made radioactive metal, with Atomic Number 95. The most important isotope of Americium is Am-241. 3. Background radiation- is radiation that results from natural sources such as cosmic radiation and naturally-occurring radioactive materials in the ground and the earth’s atmosphere including radon. 4. Beta particles- an electron or positron emitted by certain radioactive nuclei. Beta particles can be stopped by aluminum. a. Gross beta radioactivity- measurement of all beta activity present, regardless of specific radionuclide source. 5. Cerium (chemical symbol Ce) - an iron-gray, lustrous metal. Cerium-141, -143, and - 144 are radioisotopes of cerium. 6. Cesium (chemical symbol Cs) - is a metal that may be stable (nonradioactive) or unstable (radioactive). The most common radioactive form of cesium is cesium-137. Another fairly common radioisotope is cesium-134. 7. Cobalt (chemical symbol Co) - is a metal that may be stable (non-radioactive, as found in nature), or unstable (radioactive, man-made). The most common radioactive isotope of cobalt is cobalt-60. -
Paul Scherrer Institut
C^ZOOCt^ CO l 9 19 icht r r — — l-Be £3tobe I J Paul Scherrer Institut Labor für Werkstoffe und nukleare Verfahren Programm Entsorgung Chemistry of the Rectox Sensitive Elements Literature Review D.Suter Paul Scherrer Institut Telefon 056/99 2111 Würenlingen und Villigen Telex82 7414psich CH-5232 Villigen PSI Telefax 056/982327 PSI CH PSI-Bericht Nr. 113 Chemistry of the Redox Sensitive Elements Literature Review Daniel Suter Wiirenlingen and Villigen, October 1991 Preface In the framework of its Waste Management Programme the Paul Scherrer Institute is performing work to increase the understanding of radionuclide transport in the geosphere. These investigations arc performed in close cooperation with, and with the financial support of, NAGRA. The present report is issued simultaneously as a PSI report and a NAGRA NTB. TABLE OF CONTENTS Summary 2 Zusammenfassung 3 Resume 4 1. Introduction 5 2. Redox Conditions 8 3. Selenium 11 3.1 Solution Chemistry 11 3.2 Sorption Studies 13 3.3 Geochemistry 15 3.4 Experiments 18 3.5 Analytical Methods 20 4. Technetium 26 4.1 Solution Chemistry 26 4.2 Sorption Studies 29 4.3 Geochemistry 31 4.4 Experiments 32 4.5 Analytical Methods 33 5. Palladium 35 5.1 Solution Chemistry 35 5.2 Sorption Studies 36 5.3. Geochemistry 37 5.4 Experiments 38 5.5 Analytical Methods 39 6. Tin 42 6.1 Solution Chemistry 42 6.2 Sorption Studies 42 6.3 Geochemistry 43 6.4 Experiments 44 6.5 Analytical Methods 44 7. Neptunium 46 7.1 Solution Chemistry 46 7.2 Sorption Studies 48 7.3 Geochemistry 49 7.4 Experiments 51 7.5 Analytical Methods 51 8. -
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). -
Correspondence Continuing Education for Nuclear Pharmacists
THE UNIVERSITY OF NEW MEXICO COLLEGE OF PHARMACY ALBUQUERQUE, NEW MEXICO The University of New Mexico Correspondence Continuing Education Courses for Nuclear Pharmacists and Nuclear Medicine Professionals VOLUME II, NUMBER 1 Radionuclide Therapy of Painful Osseous Metastasis by: Jay A. Spicer, M.S. Co-sponsored by: mpi pharmc~ services inc an mersham company The University of New Mexico College of Phamcy is approved by the American Council on Pharmaceutical Education as a provider of continuing pharmaceutical education. Program No. 180-039-93-M6. 2.5 Contact Hours or ,25 CEU’S H m Edtior William B. Hladik III, M. S., R.Ph., University of New Mexico Director of Pharmacy Continuing Education Hugh F. Kabat, Ph. D., University of New Mexico While the advice and information in this publication are believed to be true and accurate at press time, neither the author(s) nor the editor nor the publisher ean accept any legal responsibility for any errors or omissions that may be made. The publisher makes no warranty, express or implid, with res~t to the matetial contained herein. The UNMPharmacy Contittutiig Educatwn Stifl and the Edtior WOUUlike to gratefully achnowkdge Sharon I, Ramirez for her technical suppoti and assktince in the producttin of this pubtiation. Copyright 1993 University of New Mexico Pharmacy Continuing Education Albuquerque, New Mexico HIONUCLIDE THERAPY OF PAINFUL OSSEOUS METASTASIS STATEMENT OF OBJECTIVES This correspondence course is intended to increase tie reader’s knowledge of radiophmaceuticals that are used in the treatment of pain associated with bone metastasis from different types of cancer. A variety of aspects regarding the agents currently being usti or tested are discussed. -
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. -
Nuclear Reactor Realities
Page 1 of 26 Nuclear Reactor Realities NUCLEAR REACTOR REALITIES (An Australian viewpoint) PREFACE Now that steam ships are no longer common, people tend to forget that nuclear power is just a replacement of coal, oil or gas for heating water to form steam to drive turbines, or of water (hydro) to do so directly. As will be shown in this tract, it is by far the safest way of doing so to generate electricity economically in large quantities – as a marine engineer of my acquaintance is fond of saying. Recently Quantum Market Research released its latest Australian Scan (The Advertiser, Saturday April 17, 2012, p 17). It has been tracking social change by interviewing 2000 Australians annually since 1992. In the concerns in the environment category, “[a]t the top of the list is nuclear accidents and waste disposal” (44.4 per cent), while “global warming” was well down the list of priorities at No 15, with only 27.7 per cent of people surveyed rating the issue as “extremely serious.” Part of the cause of such information must be that people are slowly realising that they have been deluded by publicity about unverified computer models which indicate that man’s emissions of CO2 play a major part in global warming. They have not yet realised that the history of the dangers of civilian nuclear power generation shows the reverse of their images. The topic of nuclear waste disposal is also shrouded in reactor physics mysteries, leading to a mis-placed general fear of the unknown. In this article only nuclear reactors are considered. -
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