Use of Isotopic Signature of Radionuclides Released from Uranium Mines and Mills to Discriminate Low Levels of Environmental Impact Against Natural Background Levels
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Progress and Challenges in Using Stable Isotopes to Trace Plant Carbon and Water Relations Across Scales
Biogeosciences, 9, 3083–3111, 2012 www.biogeosciences.net/9/3083/2012/ Biogeosciences doi:10.5194/bg-9-3083-2012 © Author(s) 2012. CC Attribution 3.0 License. Progress and challenges in using stable isotopes to trace plant carbon and water relations across scales C. Werner1,19, H. Schnyder2, M. Cuntz3, C. Keitel4, M. J. Zeeman5, T. E. Dawson6, F.-W. Badeck7, E. Brugnoli8, J. Ghashghaie9, T. E. E. Grams10, Z. E. Kayler11, M. Lakatos12, X. Lee13, C. Maguas´ 14, J. Ogee´ 15, K. G. Rascher1, R. T. W. Siegwolf16, S. Unger1, J. Welker17, L. Wingate18, and A. Gessler11 1Experimental and Systems Ecology, University Bielefeld, 33615 Bielefeld, Germany 2Lehrstuhl fur¨ Grunlandlehre,¨ Technische Universitat¨ Munchen,¨ 85350 Freising-Weihenstephan, Germany 3UFZ – Helmholtz Centre for Environmental Research, Permoserstr. 15, 04318 Leipzig, Germany 4University of Sydney, Faculty of Agriculture, Food and Natural Resources, 1 Central Avenue, Eveleigh, NSW 2015, Australia 5College of Oceanic and Atmospheric Sciences, Oregon State University, 104 COAS Admin Bldg, Corvallis (OR), USA 6Center for Isotope Biogeochemistry, Department of Integrative Biology, University of California, Berkeley, CA 94720, USA 7Potsdam Institute for Climate Impact Research (PIK) PF 60 12 03, 14412 Potsdam, Germany 8CNR – National Research Council of Italy – Institute of Agro-environmental and Forest Biology, via Marconi 2, 05010 Porano (TR), Italy 9Laboratoire d’Ecologie, Systematique´ et Evolution (ESE), CNRS AgroParisTech – UMR8079, Batimentˆ 362, Universite´ de Paris-Sud (XI), 91405 Orsay Cedex, France 10Ecophysiology of Plants, Department of Ecology and Ecosystem Management, Technische Universitat¨ Munchen,¨ Von-Carlowitz-Platz 2, 85354 Freising, Germany 11Institute for Landscape Biogeochemistry Leibniz-Zentrum fur¨ Agrarlandschaftsforschung (ZALF) e.V., Eberswalderstr. -
Oxygen Isotopic Signature of CO2 from Combustion Processes
Atmos. Chem. Phys., 11, 1473–1490, 2011 www.atmos-chem-phys.net/11/1473/2011/ Atmospheric doi:10.5194/acp-11-1473-2011 Chemistry © Author(s) 2011. CC Attribution 3.0 License. and Physics Oxygen isotopic signature of CO2 from combustion processes M. Schumacher1,2,3, R. A. Werner3, H. A. J. Meijer1, H. G. Jansen1, W. A. Brand2, H. Geilmann2, and R. E. M. Neubert1 1Centre for Isotope Research, University of Groningen, Nijenborgh 4, 9747 AG Groningen, The Netherlands 2Max-Planck-Institute for Biogeochemistry, Hans-Knoell-Straße 10, 07745, Jena, Germany 3Institute of Plant Sciences, Swiss Federal Institute of Technology Zurich,¨ Universitatsstraße¨ 2, 8092 Zurich,¨ Switzerland Received: 21 July 2008 – Published in Atmos. Chem. Phys. Discuss.: 5 November 2008 Revised: 2 February 2011 – Accepted: 5 February 2011 – Published: 16 February 2011 Abstract. For a comprehensive understanding of the global (diffusive) transport of oxygen to the reaction zone as the carbon cycle precise knowledge of all processes is neces- cause of the isotope fractionation. The original total 18O sig- sary. Stable isotope (13C and 18O) abundances provide in- nature of the material appeared to have little influence, how- formation for the qualification and the quantification of the ever, a contribution of specific bio-chemical compounds to diverse source and sink processes. This study focuses on the individual combustion products released from the involved 18 δ O signature of CO2 from combustion processes, which material became obvious. are widely present both naturally (wild fires), and human in- duced (fossil fuel combustion, biomass burning) in the car- bon cycle. All these combustion processes use atmospheric 1 Introduction oxygen, of which the isotopic signature is assumed to be con- stant with time throughout the whole atmosphere. -
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). -
Investigations of Nuclear Forensic Signatures in Uranium Bearing Materials a Dissertation Submitted to the Graduate School of the University of Cincinnati
Investigations of Nuclear Forensic Signatures in Uranium Bearing Materials A dissertation submitted to the Graduate School of the University of Cincinnati in partial fulfillment of the requirements for the degree of Doctor of Philosophy (Ph.D) In the Department of Chemistry Of the McMicken College of Arts and Sciences By Lisa Ann Meyers B.S. Ohio Northern University 2009 August 2013 Committee Chairs: Thomas Beck, Ph.D. Apryll Stalcup, Ph.D. i Abstract Nuclear forensics is a multidisciplinary science that uses a variety of analytical methods and tools to investigate the physical, chemical, elemental, and isotopic characteristics of nuclear and radiological material. A collection of these characteristics is called signatures that aids in determining how, where and when the material was manufactured. Radiological chronometry (i.e., age dating) is an important tool in nuclear forensics that uses several methods to determine the length of time that has elapsed since a material was last purified. For example, the “age” of a uranium-bearing material is determined by measuring the ingrowth of 230Th from its parent, 234U. A piece of scrap uranium metal bar buried in the dirt floor of an old, abandoned metal rolling mill was analyzed using multi-collector inductively coupled plasma mass spectroscopy (MC-ICP- MS). The mill rolled uranium rods in the 1940s and 1950s. The age of the metal bar was determined to be 61 years at the time of analysis using the 230Th/234U chronometer, which corresponds to a purification date of July 1950 ± 1.5 years. Radiochronometry was determined for three different types of uranium metal samples. -
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. -
Can Algal Photosynthetic Inorganic Carbon Isotope Fractionation Be Predicted in Lakes Using Existing Models?
Aquat. Sci. 68 (2006) 142–153 1015-1621/06/020142-12 DOI 10.1007/s00027-006-0818-5 Aquatic Sciences © Eawag, Dübendorf, 2006 Research Article Can algal photosynthetic inorganic carbon isotope fractionation be predicted in lakes using existing models? Darren L. Bade1,3,*, Michael L. Pace2, Jonathan J. Cole2 and Stephen R. Carpenter1 1 Center for Limnology, University of Wisconsin-Madison, USA 2 Institute of Ecosystem Studies, Millbrook, NY, USA 3 Present address: Institute of Ecosystem Studies, PO Box AB (65 Sharon Turnpike), Millbrook, NY 12545, USA Received: 30 June 2005; revised manuscript accepted: 7 December 2005 Abstract. Differential fractionation of inorganic carbon stable isotopes for studies ranging from food webs to stable isotopes during photosynthesis is an important paleolimnology. In our largest comparative study, values cause of variability in algal carbon isotope signatures. of δ13C-POC ranged from –35.1 ‰ to –21.3 ‰. Using Several physiological models have been proposed to ex- several methods to obtain an algal isotopic signature, we ε plain algal photosynthetic fractionation factors ( p). These found high variability in fractionation among lakes. There ε models generally consider CO2 concentration, growth was no relationship between p and one of the most im- rate, or cell morphometry and have been supported by portant predictors in existing models, pCO2. A whole-lake empirical evidence from laboratory cultures. Here, we inorganic 13C addition was used to create distinct algal ε explore the applicability of these models to a broad range isotope signatures to aid in examining p. Measurements of lakes with mixed phytoplankton communities. Under- and a statistical model from the isotope addition revealed standing this fractionation is necessary for using carbon that algal fractionation was often low (0 – 15 ‰). -
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. -
Sources of Variation in the Stable Isotopic Composition of Plants*
CHAPTER 2 Sources of variation in the stable isotopic composition of plants* JOHN D. MARSHALL, J. RENÉE BROOKS, AND KATE LAJTHA Introduction The use of stable isotopes of carbon, nitrogen, oxygen, and hydrogen to study physiological processes has increased exponentially in the past three decades. When Harmon Craig (1953, 1954), a geochemist and early pioneer of natural abundance stable isotopes, fi rst measured isotopic values of plant materials, he found that plants tended to have a fairly narrow δ13C range of −25 to −35‰. In these initial surveys, he was unable to fi nd large taxonomic or environmental effects on these values. Since that time ecologists have identi- fi ed clear isotopic signatures based not only on different photosynthetic pathways, but also on ecophysiological differences, such as photosynthetic water-use effi ciency (WUE) and sources of water and nitrogen used. As large empirical databases have accumulated and our theoretical understanding of isotopic composition has improved, scientists have continued to discover mismatches between theoretical and observed values, as well as confounding effects from sources and factors not previously considered. In the best tradi- tion of science, these discoveries have led to important new insights into physiological or ecological processes, as well as new uses of stable isotopes in plant ecophysiology. This chapter reviews the most common applications of stable isotope analysis in plant ecophysiology. Carbon isotopes Photosynthetic pathways 13 Plants contain less C than the atmospheric CO2 on which they rely for photosynthesis. They are therefore “depleted” of 13C relative to the atmo- sphere. This depletion is caused by enzymatic and physical processes that discriminate against 13C in favor of 12C. -
Lead Isotope Determinations by Inductively-Coupled Plasma Mass Spectrometry (ICP-MS): Potential of Sector Field Instruments
NGU-BULL 436, 2000 - PAGE 203 Lead isotope determinations by inductively-coupled plasma mass spectrometry (ICP-MS): potential of sector field instruments BELINDA FLEM, ANDREAS GRIMSTVEDT & NIGEL COOK Flem, B., Grimstvedt, A. & Cook, N.J. 2000: Lead isotope determinations by inductively-coupled plasma mass spectrometry (ICP-MS): potential of sector field instruments. Norges geologiske undersøkelse Bulletin 436, 203-207. Lead isotope measurements have been carried out using a high-resolution inductively-coupled plasma mass spectrometer (Finnigan MAT ELEMENT, configured with CD-1 option). The method can be applied to all types of geological samples brought into solution form. Three common lead standards are used for documentation of the method. Detection limits for 204Pb, 206Pb, 207Pb and 208Pb lie between 0.124 and 2.86 pg ml-1. Optimisation of scanning conditions at a count rate of approximately 200,000 cps for 206Pb and 207Pb, led to a relative standard deviation of 0.05% for the mean 207Pb/206Pb isotope ratio, based on 15 consecutive measurements. The method can be routinely applied to gain geochronological and petrological data for genetic studies of mineral deposits, including deposits of industrial minerals. Because of space charge effects in the skimmer cone region and mass-dependent sensitivity of the mass spectrometer, the measured intensity ratio of samples must generally be calibrated using external or internal standards of known isotope ratios to correct for mass biases and mass fractionation. Belinda Flem, Andreas Grimstvedt & Nigel Cook, Geological Survey of Norway, N-7491 Trondheim, Norway. which the Pb isotope systematics have been reset. The appli- Introduction cation of Pb isotopes for geochronology has declined in pop- Geochronological, isotopic and petrological data are impor- ularity in recent years. -
Lead Isotopes, Metal Sources, Smelters, Precipitation, Toxic Release Inventory
Coupling Meteorology, Metal Concentrations, and Pb Isotopes for Source Attribution in Archived Precipitation Samples Joseph R. Graneya*, Matthew S. Landisb aGeological Sciences and Environmental Studies, Binghamton University, Binghamton, NY USA 13902 bU.S. EPA Office of Research and Development, Research Triangle Park, NC USA 27709 *Corresponding author: Telephone: 607 777 6347 Fax: 607 777 2288 Postal Address: Department of Geological Sciences and Environmental Studies P.O. Box 6000 Binghamton University Binghamton, NY 13902-6000 E-mail address: [email protected] 1 Abstract A technique that couples lead (Pb) isotopes and multi-element concentrations with meteorological analysis was used to assess source contributions to precipitation samples at the Bondville, Illinois USA National Trends Network (NTN) site. Precipitation samples collected over a 16 month period (July 1994 - October 1995) at Bondville were parsed into six unique meteorological flow regimes using a minimum variance clustering technique on back trajectory endpoints. Pb isotope ratios and multi-element concentrations were measured using high resolution inductively coupled plasma – sector field mass spectrometry (ICP-SFMS) on the archived precipitation samples. Bondville is located in central Illinois, ~ 250 km downwind from Pb smelters in southeast Missouri. The Mississippi Valley Type ore deposits in Missouri provided a unique multi-element and Pb isotope fingerprint for smelter emissions which could be contrasted to industrial emissions from the Chicago and Indianapolis urban areas (~ 125 km north and east, of Bondville respectively); and regional emissions from electric utility facilities. Significant differences in Pb isotopes and element concentrations in precipitation varied according to the meteorological clusters. Industrial sources from urban areas, and thorogenic Pb from coal use, could be differentiated from smelter emissions from Missouri by coupling Pb isotope ratios with multi-element concentrations in precipitation. -
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.