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Isotopic Analyses of Barium in Meteorites and in Terrestrial
•'OO•,NALO• GEO•'IIYSlCALRESXAaCX VOL. ?4, NO. IS, JULY IS, 1969 Isotopic Analysesof Barium in Meteorites and in Terrestrial Samples O. EUGSTER,F. TERA,AND G. J. WASSERBURG Charles Arms Laboratory o• the Division o• Geological Sciences Cali•Jrnia Institute o• Technology,Pasadena, California 91109 Isotopic compos•tien and concentration of barium in six stone meteorites and the silicate inclusionsof two iron meteorites and three terrestrial sampleswere measured by use of a 'double spike' isotopic dilution technique in order to correct for laboratory fractionation. Any differencesbetween the abundancesof the isotopesin meteoritic and terrestrial Ba were found to be less than 0.1% for all isotopes.The per cent abundancesof Ba found in our work for Ba '•s, Ba•, Ba•% Ba '•, Ba TM,Ba •', and Ba'•ø are 71.699, 11.232, 7.853, 6.592, 2.417, 0.1012, and 0.1058, respectively. Because of the higher precision, these abundancesshould replace the currently accepted values. These results show the variations in the Ba isotopesreported by S. Umemoto (1962) to be unsubstantiated. INTRODUCTION Umemoto [1962] reported that the isotopic A comparison.of the isotopiccomposition of compositionof Ba in the Bruderheimchondrite and in the Pasamonte and Nuevo Laredo various elements in terrestrial samples,me- achondrites were distinct from terrestrial Ba teorites, and other materials of the solar system is of fundamental importance in determin- and showeda pattern of uniform fractionation relative to terrestrial Ba. The enrichments ob- ing the early history of the solar system and the mechanismsof nucleosynthesis.In ad- servedby him correspondto a 2% enrichment dition to effectsthat are a product of either in the ratio Ba•ø/Ba• compared with ter- long-lived natural activity or cosmic-rayinter- restrial materials. -
Nuclear Power
No.59 z iii "Ill ~ 2 er0 Ill Ill 0 Nuclear Family Pia nning p3 Chernobyl Broadsheet ·, _ I. _ . ~~~~ George Pritchar d speaks CONTENTS COMMENT The important nuclear development since the Nuclear Family Planning 3 last SCRAM Journal was the Government's The CEGB's plans, and the growing opposition, after Sizewell B by go ahead for Sizewell B: the world's first HUGH RICHARDS. reactor order since Chernobyl, and Britain's News 4-6 first since the go ahead was given to Torness Accidents Will Happen 1 and Heysham 2 in 1978. Of great concern is Hinkley Seismic Shocker 8-9 the CEGB's announced intention to build "a A major article on seismic safety of nuclear plants in which JAMES small fanilty• of PWRs, starting with Hinkley GARRETT reveals that Hinkley Point C. At the time of the campaign In the Point sits on a geological fault. south west to close the Hinkley A Magnox Trouble at Trawsfynydd 10-11 station, and .a concerted push in Scotland to A summary of FoE's recent report on increasing radiation levels from prevent the opening of Torness, another Trawsfynydd's by PATRICK GREEN. nuclear announcement is designed to divide Pandora's POX 12 and demoralise the opposition. But, it should The debate over plutonium transport make us more determined. The article on the to and from Dounreay continues by facing page gives us hope: the local PETE MUTTON. authorities on Severnside are joining forces CHERNOBYL BROADSHEET to oppose Hinkley C, and hopefully they will Cock-ups and Cover-ups work closely with local authorities in other "Sacrificed to • • • Nuclear Power" threatened areas - Lothian Region, The Soviet Experience Northumberland, the County Council Coalition "An Agonising Decision• 13 against waste dumping and the Nuclear Free GEORGE PRITCHARD explains why Zones - to formulate a national anti-nuclear he left Greenpeoce and took a job strategy. -
6. Potential for Human Exposure
CESIUM 125 6. POTENTIAL FOR HUMAN EXPOSURE 6.1 OVERVIEW Cesium has been identified in at least 8 of the 1,636 hazardous waste sites that have been proposed for inclusion on the EPA National Priorities List (NPL) (HazDat 2003). It was reported that 134Cs has been found in at least 3 of the 1,636 current or former NPL sites and 137Cs has been detected in at least 23 of the 1,636 current or former NPL sites. However, the number of sites evaluated for cesium is not known. The frequency of these sites can be seen in Figures 6-1, 6-2, and 6-3. Of these sites, none are located in the Commonwealth of Puerto Rico. Naturally-occurring cesium and cesium minerals consist of only one stable isotope, 133Cs. Cesium occurs in the earth's crust at low concentrations. Granites contain an average cesium concentration of about 1 ppm and sedimentary rocks contain about 4 ppm (Burt 1993). Higher concentrations are found in lepidolite, carnallite, muscovite, beryl, spodumene, potassium feldspars, leucite, petalite, and related minerals. The most important source of commercial cesium is the mineral pollucite, which usually contains about 5–32% Cs2O (Burt 1993). The largest deposits of pollucite are located in Manitoba, Canada and account for about two-thirds of the world’s known supply. Smaller deposits are located in Zimbabwe, Namibia, Brazil, Scandinavia, Czechoslovakia, and the United States. Continental dust and soil erosion are the main emission sources of naturally occurring cesium present in the environment. Cesium is also released to the environment as a result of human activities. -
Uranium Fact Sheet
Fact Sheet Adopted: December 2018 Health Physics Society Specialists in Radiation Safety 1 Uranium What is uranium? Uranium is a naturally occurring metallic element that has been present in the Earth’s crust since formation of the planet. Like many other minerals, uranium was deposited on land by volcanic action, dissolved by rainfall, and in some places, carried into underground formations. In some cases, geochemical conditions resulted in its concentration into “ore bodies.” Uranium is a common element in Earth’s crust (soil, rock) and in seawater and groundwater. Uranium has 92 protons in its nucleus. The isotope2 238U has 146 neutrons, for a total atomic weight of approximately 238, making it the highest atomic weight of any naturally occurring element. It is not the most dense of elements, but its density is almost twice that of lead. Uranium is radioactive and in nature has three primary isotopes with different numbers of neutrons. Natural uranium, 238U, constitutes over 99% of the total mass or weight, with 0.72% 235U, and a very small amount of 234U. An unstable nucleus that emits some form of radiation is defined as radioactive. The emitted radiation is called radioactivity, which in this case is ionizing radiation—meaning it can interact with other atoms to create charged atoms known as ions. Uranium emits alpha particles, which are ejected from the nucleus of the unstable uranium atom. When an atom emits radiation such as alpha or beta particles or photons such as x rays or gamma rays, the material is said to be undergoing radioactive decay (also called radioactive transformation). -
2.10. Neutron Activation of Paintings
2.10. Neutron activation of paintings Possible applications: • Pigment analysis by activation techniques • Neutron radiography by neutron absorption ⇒ Autoradiography Requires neutron irradiation of the entire painting using homogenous neutron flux followed by subsequent point by point raster activation measurement. Technical approach with reactors Neutron guide line is needed for providing sufficient neutron flux (~1014 neutrons/cm2/s) for activation of bulky materials outside the reactor core! 4,7 m shielding door shielding neutrons painting 2.5 m Activation with subsequent X-ray and γ-ray detection 63Cu(n,γ)64Cu, Cu(x) 202Hg(n,γ)203Hg, Hg(x) X-ray data provides pigment position γ-ray data provides pigment characteristics Timescale and Radiation Sensitivity Anthony van Dyck, Saint Rosalie praying for the Plague stricken of Palermo 1624 radiograph Pigment identification by analysis of time dependence for characteristic activity 3rd run Pigment identification by analysis of time dependence for characteristic activity 6th run Pigment identification by analysis of time dependence for characteristic activity 8th run Young man in the background Maryan Wynn Ainsworth et al. Art and Autoradiography; Metropolitan Museum of Art, New York; (1987) 12-18 Van Dyck Self-Portrait Head also visible in X-ray radiograph Self-Portrait of van Dyck 1622 St. Sebastian ca 1649 Painting in the Gemäldegalerie Berlin original by Georges de la Tour (1593-1652) French Court Painter Original in Louvre, question about authorship of copy, George de la Tour himself or by his son Entienne de la Tour? Neutron radiated 109 n/cm2s Neutron induced γ activity is recorded in different time steps: e.g. -
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). -
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. -
1 Introduction
1 Introduction WHO commissions reviews and undertakes health risk assessments associated with exposure to potentially hazardous physical, chemical and biological agents in the home, work place and environment. This monograph on the chemical and radiological hazards associated with exposure to depleted uranium is one such assessment. The purpose of this monograph is to provide generic information on any risks to health from depleted uranium from all avenues of exposure to the body and from any activity where human exposure could likely occur. Such activities include those involved with fabrication and use of DU products in industrial, commercial and military settings. While this monograph is primarily on DU, reference is also made to the health effects and behaviour of uranium, since uranium acts on body organs and tissues in the same way as DU and the results and conclusions from uranium studies are considered to be broadly applicable to DU. However, in the case of effects due to ionizing radiation, DU is less radioactive than uranium. This review is structured as broadly indicated in Figure 1.1, with individual chapters focussing on the identification of environmental and man-made sources of uranium and DU, exposure pathways and scenarios, likely chemical and radiological hazards and where data is available commenting on exposure-response relationships. HAZARD IDENTIFICATION PROPERTIES PHYSICAL CHEMICAL BIOLOGICAL DOSE RESPONSE RISK EVALUATION CHARACTERISATION BACKGROUND EXPOSURE LEVELS EXPOSURE ASSESSMENT Figure 1.1 Schematic diagram, depicting areas covered by this monograph. It is expected that the monograph could be used as a reference for health risk assessments in any application where DU is used and human exposure or contact could result. -
Peptide Receptor Radionuclide Therapy with Indigenous
Am J Nucl Med Mol Imaging 2020;10(4):178-211 www.ajnmmi.us /ISSN:2160-8407/ajnmmi0115339 Review Article One decade of ‘Bench-to-Bedside’ peptide receptor radionuclide therapy with indigenous [177Lu]Lu-DOTATATE obtained through ‘Direct’ neutron activation route: lessons learnt including practice evolution in an Indian setting Sandip Basu1,2, Sudipta Chakraborty2,3, Rahul V Parghane1,2, Kamaldeep2,4, Rohit Ranade1,2, Pradeep Thapa1,2, Ramesh V Asopa1,2, Geeta Sonawane1,2, Swapna Nabar1,2, Hemant Shimpi1,2, Ashok Chandak1,2, Vimalnath KV3, Vikas Ostwal2,5, Anant Ramaswamy2,5, Manish Bhandare2,6, Vikram Chaudhari2,6, Shailesh V Shrikhande2,6, Bhawna Sirohi5,7, Ashutosh Dash2,3, Sharmila Banerjee1,2 1Radiation Medicine Centre, Bhabha Atomic Research Centre, Tata Memorial Hospital Annexe, Parel, Mumbai, India; 2Homi Bhabha National Institute, Mumbai, India; 3Radiopharmaceuticals Division, BARC, Mumbai, India; 4Health Physics Division, Bhabha Atomic Research Centre, Mumbai, India; 5Department of Medical Oncology, Tata Memorial Centre, Mumbai, Maharashtra, India; 6Department of Surgical Oncology, Gastrointestinal and Hepato- Pancreato-Biliary Service, Tata Memorial Hospital, Mumbai, India; 7Apollo Proton Cancer Centre, Chennai, India Received May 30, 2020; Accepted August 14, 2020; Epub August 25, 2020; Published August 30, 2020 Abstract: The present treatise chronicles one decade of experience pertaining to clinical PRRT services in a large- volume tertiary cancer care centre in India delivering over 4,000 therapies, an exemplar of successful -
Chapter 4.3 Production and Atmospheric Release of Activation
CHAPTER 4.3 PRODUCTION AND ATMOSPHERIC RELEASE OF ACTIVATION PRODUCTS ABSTRACT The primary activation product of interest in terms of airborne release and potential offsite dose is 41Ar. Even though it is a short-lived radionuclide, 41Ar is a noble gas readily released from the reactor stacks, and most has not decayed by the time it moves offsite with normal wind speeds. SRS reactor operations produced and released relatively large quantities of 41Ar, and its production rate in the air blanket surrounding a reactor should have been roughly proportional to the reactor power level. Cummins et al. (1991) provides an SRS-developed estimate of 41Ar releases, which we compare to other measurements, check against reactor power levels, and accept as a generally reasonable estimate of SRS 41Ar releases. While these values represent the best available estimates for 41Ar releases from the SRS reactors, the values presented for the later years (1974–1988) are quite low when compared to reactor power levels and overall average 41Ar production levels. We also observe that the 41Ar release values presented for certain of the early years (1955–1967) are quite high when compared to reactor power levels for the same period. The reason for these apparent discrepancies is not clear, and adds to the uncertainty in our estimates of 41Ar releases. INTRODUCTION Most of the radioactivity produced by the five SRS production reactors involved fission products, created when 235U, 239Pu, or 233U split into two or more smaller atoms. In addition, neutrons captured by some materials inside the reactor created radioactive isotopes called activation products. -
Highly Enriched Uranium: Striking a Balance
OFFICIAL USE ONLY - DRAFT GLOSSARY OF TERMS APPENDIX F GLOSSARY OF TERMS Accountability: That part of the safeguards and security program that encompasses the measurement and inventory verification systems, records, and reports to account for nuclear materials. Assay: Measurement that establishes the total quantity of the isotope of an element and the total quantity of that element. Atom: The basic component of all matter. Atoms are the smallest part of an element that have all of the chemical properties of that element. Atoms consist of a nucleus of protons and neutrons surrounded by electrons. Atomic energy: All forms of energy released in the course of nuclear fission or nuclear transformation. Atomic weapon: Any device utilizing atomic energy, exclusive of the means for transportation or propelling the device (where such means is a separable and divisible part of the device), the principal purpose of which is for use as, or for development of, a weapon, a weapon prototype, or a weapon test device. Blending: The intentional mixing of two different assays of the same material in order to achieve a desired third assay. Book inventory: The quantity of nuclear material present at a given time as reflected by accounting records. Burnup: A measure of consumption of fissionable material in reactor fuel. Burnup can be expressed as (a) the percentage of fissionable atoms that have undergone fission or capture, or (b) the amount of energy produced per unit weight of fuel in the reactor. Chain reaction: A self-sustaining series of nuclear fission reactions. Neutrons produced by fission cause more fission. Chain reactions are essential to the functioning of nuclear reactors and weapons. -
Issues and R&D Needs for Commercial Fusion Energy
University of California, San Diego UCSD-CER-08-01 Issues and R&D needs for commercial fusion energy An interim report of the ARIES technical working groups M. S. Tillack, D. Steiner, L. M. Waganer, S. Malang, F. Najmabadi, L. C. Cadwallader, L. A. El-Guebaly, R. J. Peipert Jr, A. R. Raffray, J. P. Sharpe, A. D. Turnbull, T. L. Weaver, and the ARIES Team July 2008 Center for Energy Research University of California, San Diego 9500 Gilman Drive La Jolla, CA 92093-0417 UCSD-CER-08-01 Issues and R&D needs for commercial fusion energy – An interim report of the ARIES technical working groups – August 2008 M. S. Tillack1, D. Steiner2, L. M. Waganer3, S. Malang4, F, Najmabadi1, L. C. Cadwallader5, L. A. El-Guebaly6, R. J. Peipert Jr7, A. R. Raffray1, J. P. Sharpe5, A. D. Turnbull8, T. L. Weaver7, and the ARIES Team* 1 UC San Diego 2 Rensselaer Polytechnic Institute 3 Consultant for The Boeing Company 4 FNT Consulting 5 Idaho National Laboratory 6 UW-Madison 7 The Boeing Company 8 General Atomics * Institutions involved in the ARIES Team include University of California San Diego, The Boeing Company, Georgia Institute of Technology, General Atomics, Idaho National Engineering Laboratory, Massachusetts Institute of Technology, Princeton Plasma Physics Laboratory, Rensselaer Polytechnic Institute, and the University of Wisconsin, Madison. 1 Table of Contents: 1. Introduction 2. Evaluation methodology 2.1 Technology readiness 2.2 Reference concepts 2.2.1 Reference concepts for energy capture and conversion 2.2.2 Reference concepts for the remainder of the power core 3.