Mining and Milling of Uranium Ore: Indian Scenario
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Environmental Impacts of Uranium Mining in Australia History, Progress and Current Practice
A policy paper commissioned MAY 2017 by the Minerals Council of Australia Environmental impacts of uranium mining in Australia History, progress and current practice Ben Heard POLICY PAPER Environmental impacts of uranium mining in Australia History, progress and current practice Ben Heard is a doctoral researcher at the University of Adelaide, focusing on clean energy systems and the potential role of nuclear technologies. He holds a Masters in Corporate Environmental and Sustainability Management from Monash University and was an environmental sustainability consultant from 2005-2016. He has taught several units of the Masters of Sustainability at the University of Adelaide and is an honourary member of the Leaders Institute of South Australia. His most recent research paper Burden of proof: A comprehensive review of the feasibility of 100% renewable-electricity systems was published in the journal Renewable and Sustainable Energy Reviews. The Minerals Council of Australia is the peak national body representing Australia’s exploration, mining and minerals processing industry, nationally and internationally, in its contribution to sustainable economic, and social development. This publication is part of the overall program of the MCA, as endorsed by its Board of Directors, but does not necessarily reflect the views of individual members of the Board. Minerals Council of Australia Level 3, 44 Sydney Ave, Forrest ACT 2603 (PO Box 4497, Kingston ACT Australia 2604) P. + 61 2 6233 0600 | F. + 61 2 6233 0699 www.minerals.org.au | [email protected] Copyright © 2017 Minerals Council of Australia. All rights reserved. Apart from any use permitted under the Copyright Act 1968 and subsequent amendments, no part of this publication may be reproduced, stored in a retrieval system or transmitted, in any form or by any means, electronic, mechanical, photocopying, recording or otherwise, without the prior written permission of the publisher and copyright holders. -
Nuclear Power
FEBRUARY 28, 2013 | No. 757 NUCLEAR POWER: LOOKING BACK, LOOKING FORWARD (NM757.4292) Last year marked the 20th anniversary of the fi rst edition of the World Nuclear Industry Status Report (WNISR). For two decades the reports have punctu- red the lies of the nuclear industry. Mycle Schneider and Antony Froggatt wrote the 2012 edition and both contributed to the 1992 edition − congratulations Mycle and NUCLEAR POWER: LOOKING Antony! BACK, LOOKING FORWARD 1 FUKUSHIMA PROPAGANDA 4 The predictions made in WNISR-1992 stack up well. After a 20-year period of signi- fi cant growth, the report correctly predicted that nuclear expansion would "slow to a URANIUM MINING ISSUES: trickle". From 1992 to 2012, worldwide nuclear power capacity increased from 326 2012 REVIEW 8 gigawatts (GW) to 374 GW − a 15% increase in 20 years. IN BRIEF 18 The nuclear industry is fi nally catching up with Mycle and Antony. The International Atomic Energy Agency's 'low' estimates have become a more reliable guide over the years, and the Agency's current 'low' estimate of 456 GW capacity in 2030 suggests very slow annual growth of around 1.5% (IAEA, 2012). Nuclear power's proportional contribution to world electricity production will certainly decline. Nuclear's contribution peaked at 17% in 1993, fell to 12.3% in 2011, and the IAEA estimates just 4.7−6.2% in 2030 (IAEA, 2012, p.17). By 2030, a majority of the world's reactors will be nearing the end of their operating lives and the nuclear industry will need to run just to stand still. -
Geology of U Rani Urn Deposits in Triassic Rocks of the Colorado Plateau Region
Geology of U rani urn Deposits in Triassic Rocks of the Colorado Plateau Region By W. I. FINCH CONTRIBUTIONS TO THE GEOLOGY OF URANIUM GEOLOGICAL SURVEY BULLETIN 1074-D This report concerns work done on behalf ~1 the U. S. Atomic Energy Commission -Jnd is published with the permission of ~he Commission NITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1959 UNITED STATES DEPARTMENT OF THE INTERIOR FRED A. SEATON, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U. S. Government Printin~ Office Washin~ton 25, D. C. CONTENTS Page Abstract---------------------------------------------------------- 125 Introduction__ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ __ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ 125 History of mining and production ____ ------------------------------- 127 Geologic setting___________________________________________________ 128 StratigraphY-------------------------------------------------- 129 ~oenkopiformation_______________________________________ ~29 Middle Triassic unconformity_______________________________ 131 Chinle formation__________________________________________ 131 Shinarump Inernber____________________________________ 133 ~udstone member------------------------------------- 136 ~oss Back member____________________________________ 136 Upper part of the Chinle formation______________________ 138 Wingate sandstone_________________________________________ 138 lgneousrocks_________________________________________________ 139 Structure_____________________________________________________ -
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). -
A Prospector's Guide to URANIUM Deposits in Newfoundland and Labrador
A Prospector's guide to URANIUM deposits In Newfoundland and labrador Matty mitchell prospectors resource room Information circular number 4 First Floor • Natural Resources Building Geological Survey of Newfoundland and Labrador 50 Elizabeth Avenue • PO Box 8700 • A1B 4J6 St. John’s • Newfoundland • Canada pros pec tor s Telephone: 709-729-2120, 709-729-6193 • e-mail: [email protected] resource room Website: http://www.nr.gov.nl.ca/mines&en/geosurvey/matty_mitchell/ September, 2007 INTRODUCTION Why Uranium? • Uranium is an abundant source of concentrated energy. • One pellet of uranium fuel (following enrichment of the U235 component), weighing approximately 7 grams (g), is capable of generating as much energy as 3.5 barrels of oil, 17,000 cubic feet of natural gas or 807 kilograms (kg) of coal. • One kilogram of uranium235 contains 2 to 3 million times the energy equivalent of the same amount of oil or coal. • A one thousand megawatt nuclear power station requiring 27 tonnes of fuel per year, needs an average of about 74 kg per day. An equivalent sized coal-fired station needs 8600 tonnes of coal to be delivered every day. Why PROSPECT FOR IT? • At the time of writing (September, 2007), the price of uranium is US$90 a pound - a “hot” commodity, in more ways than one! Junior exploration companies and major producers are keen to find more of this valuable resource. As is the case with other commodities, the prospector’s role in the search for uranium is always of key importance. What is Uranium? • Uranium is a metal; its chemical symbol is U. -
Tailings and Their Component Radionuclides from the Biosphere-Some Earth Science Perspectives
Tailings and Their Component Radionuclides From the Biosphere-Some Earth Science Perspectives Isolation of Uranium Mill Tailings and Their Component Radionuclides From the Biosphere-Some Earth Science Perspectives By Edward Landa GEOLOGICAL SURVEY CIRCULAR 814 A critical review of the literature dealing with uranium mill tailings, with emphasis on the geologic and geochemical processes affecting the long-term containment of radionuclides 1980 United States Department of the Interior CECIL D. ANDRUS, Secretary Geological Survey H. William Menard, Director Library of Congress catalog-card No. 79-600148 Free on application to Branch of Distribution, U.S. Geological Survey 1200 South Eads Street, Arlington, VA 22202 CONTENTS Page Abstract 1 Introduction ------------------------------------------------------------ 1 Acknowledginents ---------_----------------------------------------------- 2 Quantity and location of the tailings -------------------------------------- 2 Radioactivity in tailings -------------------------------------------------- 4 Sources of potential human radiation exposure from uranium mill tailings ------ 6 Radon emanation ----------------------------------------------------- 6 VVind transport ------------------------------------------------------- 6 Surface water transport and leaching ----------------------------------- 7 External gamma radiation ------------------------------------------- 8 Contamination of terrestrial and aquatic vegetation ---------------------- 8 Seepage ----------------------------------------------------~-------- -
The Nuclear Fuel Cycle
THE COLLECTION > From the uranium mine> toI wNTasRtOeD dUisCpToIsOaN l 1 > The atom 2 > Radioactivity 3 > Radiation and man 4 > Energy 5 > Nuclear energy: fusion and fission 6 > How a nuclear reactor works 7 > The nuclear fuel cycle 7 > The nuclear fuel cycle FROM RESEARCH 8 > Microelectronics 9 > The laser: a concentrate of light TO INDUSTRY 10 > Medical imaging 11 > Nuclear astrophysics 12 > Hydrogen 7 >>TThhee nnuucclleeaarr ffuueell ccyyccllee UPSTREAM THE REACTOR: PREPARING THE FUEL IN THE REACTOR: FUEL CONSUMPTION DOWNSTREAM THE REACTOR: REPROCESSING NUCLEAR WASTE NUCLEAR WASTE © Commissariat à l’’Énergie Atomique et aux Energies Alternatives, 2005 Communication Division Bâtiment Siège - 91191 Gif-sur-Yvette cedex www.cea.fr ISSN 1637-5408. From the uranium mine to waste disposal 7 > The nuclear fuel cycle From the uranium mine to waste disposal 7 > The nuclear fuel cycle 2 > CONTENTS > INTRODUCTION 3 Uranium ore is extracted from open-pit mines – such as the McClear mines in Canada seen here – or underground workings. a m e g o C © “The nuclear fuel cycle includes an erray UPSTREAM THE REACTOR: of industrial operations, from uranium PREPARING THE FUEL 4 e mining to the disposal of radioactive l Extracting uranium from the ore 5 waste.” c Concentrating and refining uranium 6 y Enriching uranium 6 c Enrichment methods 8 l introduction uel is a material that can be burnt to pro - IN THE REACTOR: FUEL CONSUMPTION 9 Fvide heat. The most familiar fuels are wood, e Preparing fuel assemblies 10 coal, natural gas and oil. By analogy, the ura - e g a nium used in nuclear power plants is called Per unit or mass (e.g. -
Regional Geology and Ore-Deposit Styles of the Trans-Border Region, Southwestern North America
Arizona Geological Society Digest 22 2008 Regional geology and ore-deposit styles of the trans-border region, southwestern North America Spencer R. Titley and Lukas Zürcher Department of Geosciences, University of Arizona, Tucson, AZ, 85721, USA ABSTRACT Nearly a century of independent geological work in Arizona and adjoining Mexico resulted in a seam in the recognized geological architecture and in the mineralization style and distribution at the border. However, through the latter part of the 20th century, workers, driven in great part by economic-resource considerations, have enhanced the understanding of the geological framework in both directions with synergistic results. The ore deposits of Arizona represent a sampling of resource potential that serves as a basis for defining expectations for enhanced discovery rates in contiguous Mexico. The assessment presented here is premised on the habits of occurrence of the Arizona ores. For the most part, these deposits occur in terranes that reveal distinctive forma- tional ages, metal compositions, and lithologies, which identify and otherwise constrain the components for search of comparable ores in adjacent crustal blocks. Three basic geological and metallogenic properties are integrated here to iden- tify the diagnostic features of ore genesis across the region. These properties comprise: (a) the type and age of basement as identified by tectono-stratigraphic and geochemi- cal studies; (b) consideration of a major structural discontinuity, the Mojave-Sonora megashear, which adds a regional structural component to the study and search for ore deposits; and (c) integration of points (a) and (b) with the tectono-magmatic events over time that are superimposed across terranes and that have added an age component to differing cycles of rock and ore formation. -
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. -
Uranium Mining and the U.S. Nuclear Weapons Program
Uranium Mining and the U.S. Nuclear Weapons Program Uranium Mining and the U.S. Nuclear Weapons Program By Robert Alvarez Formed over 6 billion years ago, uranium, a dense, silvery-white metal, was created “during the fiery lifetimes and explosive deaths in stars in the heavens around us,” stated Nobel Laureate Arno Penzias.1 With a radioactive half-life of about 4.5 billion years, uranium-238 is the most dominant of several unstable uranium isotopes in nature and has enabled scientists to understand how our planet was created and formed. For at least the last 2 billion years, uranium shifted from deep in the earth to the rocky shell-like mantle, and then was driven by volcanic processes further up to oceans and to the continental crusts. The Colorado Plateau at the foothills of the Rocky Mountains, where some of the nation’s largest uranium deposits exist, began to be formed some 300 million years ago, followed later by melting glaciers, and erosion which left behind exposed layers of sand, silt and mud. One of these was a canary-yellow sediment that would figure prominently in the nuclear age. From 1942 to 1971, the United States nuclear weapons program purchased about 250,000 metric tons of uranium concentrated from more than 100 million tons of ore.2 Although more than half came from other nations, the uranium industry heavily depended on Indian miners in the Colorado Plateau. Until recently,3 their importance remained overlooked by historians of the atomic age. There is little doubt their efforts were essential for the United States to amass one of the most destructive nuclear arsenals in the world. -
Uranium Mining in Virginia
Nontechnical Summary Uranium Mining in Virginia In recent years, there has been renewed interest in mining uranium in the Common- wealth of Virginia. However, before any mining can begin, Virginia’s General Assembly would have to rescind a statewide moratorium on uranium mining that has been in effect since 1982. The National Research Council was commissioned to provide an independent review of the scientific, environmental, human health and safety, and regulatory aspects of uranium mining, processing, and reclamation in Virginia to help inform the public discussion about uranium mining and to assist Virginia’s lawmakers in their deliberations. eneath Virginia’s convene an independent rolling hills, there committee of experts to Bare occurrences of write a report that described uranium—a naturally occur- the scientific, environmental, ring radioactive element that human health and safety, and can be used to make fuel for regulatory aspects of mining nuclear power plants. In the and processing Virginia’s 1970s and early 1980s, work to uranium resources. Addi- explore these resources led to tional letters supporting this the discovery of a request were received from large uranium deposit at Coles U.S. Senators Mark Warner Hill, which is located in and Jim Webb and from Pittsylvania County in southern Governor Kaine. The Virginia. However, in 1982 the National Research Council Commonwealth of Virginia study was funded under a enacted a moratorium on contract with the Virginia uranium mining, and interest in Center for Coal and Energy further exploring the Coles Hill Research at Virginia deposit waned. Polytechnic Institute and In 2007, two families living in the vicinity of State University (Virginia Tech). -
Uranium Raw Material for the Nuclear Fuel Cycle
Uranium Raw Material for the Nuclear Fuel Cycle: Exploration, Mining, Production, Supply and Demand, Economics and Environmental Issues (URAM-2018) Supply and Demand, Economics Environmental Uranium Raw Material for the Nuclear Fuel Cycle: Exploration, Mining, Production, Uranium Raw Material for the Nuclear Fuel Cycle: Exploration, Mining, Production, Supply and Demand, Economics and Environmental Issues (URAM-2018) Proceedings of an International Symposium Vienna, Austria, 25–29 June 2018 INTERNATIONAL ATOMIC ENERGY AGENCY VIENNA URANIUM RAW MATERIAL FOR THE NUCLEAR FUEL CYCLE: EXPLORATION, MINING, PRODUCTION, SUPPLY AND DEMAND, ECONOMICS AND ENVIRONMENTAL ISSUES (URAM-2018) The Agency’s Statute was approved on 23 October 1956 by the Conference on the Statute of the IAEA held at United Nations Headquarters, New York; it entered into force on 29 July 1957. The Headquarters of the Agency are situated in Vienna. Its principal objective is “to accelerate and enlarge the contribution of atomic energy to peace, health and prosperity throughout the world’’. PROCEEDINGS SERIES URANIUM RAW MATERIAL FOR THE NUCLEAR FUEL CYCLE: EXPLORATION, MINING, PRODUCTION, SUPPLY AND DEMAND, ECONOMICS AND ENVIRONMENTAL ISSUES (URAM-2018) PROCEEDINGS OF AN INTERNATIONAL SYMPOSIUM ORGANIZED BY THE INTERNATIONAL ATOMIC ENERGY AGENCY IN COOPERATION WITH THE OECD NUCLEAR ENERGY AGENCY AND THE WORLD NUCLEAR ASSOCIATION AND HELD IN VIENNA, 25–29 JUNE 2018 INTERNATIONAL ATOMIC ENERGY AGENCY VIENNA, 2020 COPYRIGHT NOTICE All IAEA scientific and technical publications are protected by the terms of the Universal Copyright Convention as adopted in 1952 (Berne) and as revised in 1972 (Paris). The copyright has since been extended by the World Intellectual Property Organization (Geneva) to include electronic and virtual intellectual property.