Decay Scheme Data of Neptunium Isotopes

Total Page:16

File Type:pdf, Size:1020Kb

Decay Scheme Data of Neptunium Isotopes Decay Scheme Data of Neptunium Isotopes A thesis submitted to the University of London for the degree of Doctor of Philosophy Ian Michael Lowles July 1991 Imperial College Reactor Centre Imperial College of Science, Technology and Medicine Dedicated to my Parents Persons attempting to find a motive in this narrative will be prosecuted; persons attempting to find a moral in it will be banished; persons attempting to find a plot in it will be shot. Mark Twain The Adventures of Huckleberry Finn. Acknowledgments I would like to thank Dr. T.D. MacMahon for the help and encouragement he has given during the course of this work, but above all for his friendship. I am very grateful to Mr. R. Benzing, Dr. A.H. Naboulsi, Mr. I.W. Sinclair and Dr. A.W. Glauert for their many useful suggestions and comments, in areas which included: spectroscopy; statistics; chemistry and computing. I would also like to thank the Reactor Operations staff, without whose help much of this work would have been impossible. Thanks also to Dr. A.J. Fudge, Mr. R.A.P. Wiltshire and Mr. I.D. Jackson for their help and advice during my time at Harwell. Finally, I must thank Alison Smith whose love and support has helped me through the difficult times in this work. She has also had the unenviable task of reading the rough drafts of this thesis, and for that she must be pitied. Abstract The purpose of this research was to investigate the decay scheme parameters fy\n ryx o of Np and Np, and in particular their half-lives and gamma-ray emission probabilities. The work was prompted by the International Atomic Energy Agency, Coordinated Research Programme (IAEA-CRP) request for more accurate actinide decay data in order to: i. assess accurately the effects of these data on thermal and fast reactor fuel cycles ii. aid in the evaluation of nuclear waste management procedures iii. provide reliable data for nuclear safeguards iv. extend the knowledge of actinide decay parameters required in scientific research Several authors have recently reported precise measurements of alpha- particle, gamma-ray and conversion electron emission probabilities in the decay of 937 Np. An attempt to construct a self-consistent decay scheme from these data has failed. The author believes that the anomalous decay scheme is due, not to what has been measured, but is a consequence of what has previously gone undetected. Prime candidates for these missing data are several very low-energy, high-intensity gamma-ray transitions. An experiment was undertaken to analyse the low-energy gamma-ray spectrum of Np, in an attempt to determine the existence of these transitions, and so resolve the anomalous decay scheme. The only available precise measurement of the half-life of Np is that of Brauer et al. (1960). As a consequence of this radionuclide's importance in fission reactors, the IAEA-CRP requested a confirmatory measurement of the half-life of 237Np. In this present determination the specific activity of 37 alpha-particle sources, prepared from known weights of high purity Np solution, have been measured. Accurate concentration analysis of the solution was provided by controlled-potential coulometry. Source activities were measured by a-particle counting in two gas flow proportional counters of known geometry. The measured specific activity and half-life are in excellent agreement with the value reported by Brauer et al. (1960). Moreover, the validity of many of the assumptions used in this present measurement have been verified experimentally. Attempts to produce a self-consistent decay scheme for Np have relied exclusively on gamma-ray emission probability measurements. However, the precision with which the intensity of the principle gamma-ray transition has been measured, has varied between 1.45 and 3.80%. This was considered unacceptable by the IAEA-CRP, who called for a further measurement of the gamma-ray emission probabilities of 239Np, requesting a precision of 1% for the principle transition. In this present determination, Np has been prepared by radiochemical noo separation from neutron irradiated U, and by separation from its equilibrium parent, 243Am. Photopeak areas were determined using two different analytical peak fitting routines and source activities were measured using a 4jtp-y coincidence system, which utilised the efficiency extrapolation technique. The measured gamma-ray emission probabilities are consistent with those of previous workers. Moreover, the intensity of the principle transition has been measured with a precision of greater than 1%, satisfying the original aims of the IAEA-CRP. Contents 4 Contents Acknowledgements ....... 1 Abstract ........ 2 Contents ........ 4 List of Tables ........ 8 List of Figures ....... 10 1. Introduction ....... 13 1.1 The I A E A - C R P ............................................................ 13 1.2 Nuclear Decay Data of Neptunium Isotopes . 14 2. The Chemistry of Neptunium .... 18 2.1 The Placement of Actinides in the Periodic Table 18 2.2 The Discovery of Neptunium ..... 18 2.3 The Similarities Between the Lanthanide and Actinide Elements 22 2.3.1 Oxidation States ..... 22 2.3.2 The Lanthanide and Actinide Contractions 22 2.4 The Solution Chemistry of Neptunium 25 2.5 Ion-Exchange Chromatography .... 29 2.6 Separation of Neptunium by Ion—Exchange Chromatography 33 3. Counting and Spectroscopy Techniques . 38 3.1 Introduction ....... 38 3.2 Proportional Counters ...... 38 3.2.1 Operating Voltage ..... 39 3.2.2 Alpha-Particle Counting .... 41 3.2.3 Beta-Particle Counting .... 43 Contents 5 3.3 Solid State Detectors ....... 45 3.3.1 Gamma-ray Interactions ..... 45 3.3.2 Photoelectric Absorption ..... 45 3.3.3 Compton Scattering ...... 46 3.3.4 Pair Production ...... 47 3.3.5 Nal(Tl) Scintillation Detectors ..... 48 3.3.6 Semiconductor Detectors . 51 3.3.7 Peak Area Determination ..... 55 3.3.8 Sampo Routine ...... 57 3.3.9 Omnigam Routine ...... 57 3.3.10 Gamanal Routine ...... 59 3.3.11 Peak Anomalies ...... 60 3.3.12 Detector Efficiency . 61 3.4 Coincidence Counting ....... 67 3.4.1 Conversion Electrons ...... 68 3.4.2 Gamma Sensitivity of the p-detector .... 69 3.4.3 Beta Sensitivity of the y-detector . 70 3.4.4 Complex Decay Schemes ..... 70 3.4.5 47tP~y Coincidence System . 71 3.4.6 Dead Time and Resolving Time Corrections . 74 3.4.7 Corrections to the Coincidence Formulae . 77 3.4.8 Data Analysis . 78 4. Low-energy Gamma-ray Analysis of Np . 80 4.1 Introduction ........ 80 4.2 Review of Alpha-Particle Decay Data .... 80 4.2.1 Review of Gamma-Ray Decay Data .... 86 4.2.2 Review of Alpha-Gamma Coincidence Data . 88 4.2.3 Review of Gamma-Gamma Coincidence Data . 91 Contents 6 4.2.4 Review of Conversion Electron Data 95 4.3 Evaluation .... 96 4.4 Experimental .... 99 4.5 Results ..... 106 4.6 Discussion .... 109 4.7 Conclusion .... 113 5. The Half-life of 237Np 114 5.1. Introduction ..... 114 5.2 Review of Previous Measurements 114 5.3 Controlled-Potential Coulometry 116 5.4 Experimental ..... 121 5.4.1 Preparation of Np Standards 121 5.4.2 The Analysis of Neptunium by Controlled-Potential Coulometry 122 5.4.3 Source Preparation 124 5.5 Results ...... 126 5.5.1 Concentration Analysis 126 5.5.2 Source Count Rate 127 5.5.3 Specific Activity 127 5.6 Discussion ..... 136 5.6.1 Alpha-Particle Self-Absorption Correction 136 5.6.2 Source Uniformity Correction . 136 5.6.3 Beta-Particle Sensitivity 140 5.6.4 Alpha-Particle Backscattering . 140 5.7 Conclusion ..... 144 6. Gamma-ray Emission Probabilities of 239Np 145 6.1 Introduction ..... 145 Contents 7 6.2 Review of Previous Measurements . 145 6.2.1 Half-life Measurements ..... 145 6.2.2 (3-Particle Emission Probabilities .... 145 6.2.3 Internal Conversion Coefficients . 147 6.2.4 y-ray Emission Probability Measurements . 147 6.3 Experimental . 151 6.3.1 Thermal Neutron Irradiation of 238U02 Spheres . 151 6.3.2 Thermal Neutron Irradiation of 238U02 Powder . 155 6.3.3 Separation 239Np from242Am . 159 6.4 Results ......... 161 6.4.1 Absolute Disintegration Rates . 161 6.4.2 Absolute y-ray Emission Probabilities . 163 6.5 Conclusion . 168 7. Summary and Conclusions ...... 169 References . 173 Contents 8 List of Tables 1.1 Nuclear Decay Data and Their Applications .... 15 2.1 The Periodic Table ....... 20 2.2 Electronic Configuration of the Elements . 21 2.3 The Oxidation States of the Lanthanides and Actinides . 23 2.4 Neptunium Ions in Aqueous Solution ..... 28 3.1 Isotopes Used for the Calibration of a Semiconductor Detector . 63 4.1 Measured a-particle Emission Probabilities . 81 4.2 Evaluated a-particle Emission Probabilities .... 83 4.3 a-particle Emission Probabilities determined by CBNM and CIEMAT, Together with Their Recommended Pa Values . 85 4.4 Energy Levels of 233Pa ....... 85 4.5 Absolute y-ray Emission Probabilities ..... 87 4.6 a-y Coincidence Data (Gonzalez et al., 1979) .... 89 4.7(a) y-y Coincidence Data (Skalsey and Connor, 1976) . 92 4.7(b) y-y Coincidence Data (Gonzalez et al., 1979) . 92 4.7(c) y-y Coincidence Data (Woods et al., 1988) .... 92 4.8 Conversion Electron Measurements of Woods et al. (1988) . 95 4.9 Total Transition Probabilities of 237Np ..... 96 4.10 Purity of the Neptunium Sample ..... 99 4.11 Measured Relative y-ray Emission Probabilities of'I'M Np Normalised to P-^(86.5) = 12.3% . 108 4.12 ICC's for the 5.18 keV T r a n s itio n................................................I ll 4.13 ICC's for the 8.69 keV Transition . I ll 4.14 ICC's for the 36.20 keV T ran sition................................................I ll Contents 5.1 Purity of the Neptunium Sample 5.2 Results of the CPC Analysis ...
Recommended publications
  • 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_____________________________________________________
    [Show full text]
  • 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).
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • 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).
    [Show full text]
  • 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.
    [Show full text]
  • Principles of Modern Uranium Exploration by John W
    235 236 URANIUM - FUEL OF THE FUTURE 238 The Athens Symposium followed the recommendations of a panel meeting in April 1970 on uranium exploration geology. It was attended by 220 participants representing 40 countries and two international organizations; 43 papers were presented. SUPPLY CHALLENGE An overview of the supply challenge of uranium was given by Mr. Robert D. Nininger, of the USAEC, who acted as chairman of the Symposium. He outlined the major topics and problems to be discussed during the conference, with the aim of meeting this challenge: "Uranium deposits in sandstone and quartz pebble conglomerates presently represent the preponderance of uranium resources. Yet there is a question whether geologic limitations on the occurence of such deposits may preclude their discovery in numbers sufficient to meet the eventual resource needs. New types of deposits, low in grade but larger in size, representing the equivalent of the porphyry copper deposits, may supply the bulk of future resource additions. Further investigation is needed on the characteristics of such deposits and the means of their identification. Similarly, additional investigation is needed to determine whether limits on the more conventional deposits do, in fact, exist, and, if not, what advanced approaches to rapid identification of additional such deposits may be employed." "The world probably cannot rely on the very low-grade deposits such as most uraniferous black shales for both and environmental economic reasons. There is probably a minimum grade between 100 and 500 parts per million below which uranium deposits cannot be effectively exploited for nuclear power." Mr. Nininger noted that the Symposium marked the end of the initial period of expanding activity in the field of uranium raw materials, and a much-needed beginning of fuller international co-operation and exchange of information in the critical area of uranium geology and exploration.
    [Show full text]
  • Perceptions and Realities in Modern Uranium Mining
    Nuclear Development 2014 Perceptions and Realities in Modern Uranium Mining Extended Summary NEA Nuclear Development Perceptions and Realities in Modern Uranium Mining Extended Summary © OECD 2014 NEA No. 7063 NUCLEAR ENERGY AGENCY ORGANISATION FOR ECONOMIC CO-OPERATION AND DEVELOPMENT PERCEPTIONS AND REALITIES IN MODERN URANIUM MINING Perceptions and Realities in Modern Uranium Mining Introduction Producing uranium in a safe and environmentally responsible manner is not only important to the producers and consumers of the product, but also to society at large. Given expectations of growth in nuclear generating capacity and associated uranium demand in the coming decades – particularly in the developing world – enhancing awareness of leading practice in uranium mining is important. This extended summary of the report Managing Environmental and Health Impacts of Uranium Mining provides a brief outline of the driving forces behind the significant evolution of uranium mining practices from the time that uranium was first mined for military purposes until today. Uranium mining remains controversial principally because of legacy environmental and health issues created during the early phase of the industry. Today, uranium mining is conducted under significantly different circumstances and is now the most regulated and one of the safest forms of mining in the world. The report compares historic uranium mining practices with leading practices in the modern era, and provides an overview of the considerable evolution of regulations and mining practices that have occurred in the last few decades. Case studies of past and current practices are included to highlight these developments and to contrast the outcomes of historic and modern practices. With over 430 reactors operational worldwide at the end of 2013, more than 70 under construction and many more under consideration, providing fuel for these long-lived facilities will be essential for the uninterrupted generation of significant amounts of baseload electricity for decades to come.
    [Show full text]
  • Geology of Uranium and Associated Ore Deposits Central Part of the Front Range Mineral Belt Colorado by P
    Geology of Uranium and Associated Ore Deposits Central Part of the Front Range Mineral Belt Colorado By P. K. SIMS and others GEOLOGICAL SURVEY PROFESSIONAL PAPER 371 Prepared on behalf of the U.S. Atomic Energy Commission UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1963 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thoma~B.Nobn,D~ec~r The U.S. Geological Survey Library catalog card for this publication appears after page 119 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C., 20402 PREFACE This report is bused on fieldwork in the central part of the Front Range mineral belt between 1951 and 1956 by geologists of the U.S. Geological Survey on behalf of the U.S. Atomic Energy Co1nmission. The work was cn.rriecl on by nine authors working in different parts of the region. Therefore, although the senior author is responsible for the sections of the report thn,t are not ascribed to inclividualrnembers, the entire report embodies the efrorts of the group, which consisted of F. C. Armstrong, A. A. Drake, Jr., J. E. Harrison, C. C. Hawley, R. H. l\1oench, F. B. l\1oore, P. K. Sims, E. W. Tooker, and J. D. Wells. III CONTENTS Page Page Abstract------------------------------------------- 1 Uranium deposits-Continued Introduction ______________________________ - _______ _ 2 ~ineralogy-Continued Purpose and scope of report _____________________ _ 2 Zippeite and betazippeite ___________________ _ 39 Geography ____________________________________ _ 2 Schroeckingerite
    [Show full text]
  • Mining and Milling of Uranium Ore: Indian Scenario
    XA0103130 MINING AND MILLING OF URANIUM ORE: INDIAN SCENARIO J.L. BHASIN Uranium Corporation of India Ltd, Jaduguda, Bihar, India Abstract The occurrence of uranium minerals in Singhbhum Thrust belt of Eastern India was known since 1937. In 1950, a team of geologists of the Atomic Minerals Division was assigned to closely examine this 160 km long belt. Since then, several occurrences of uranium have been found and a few of them have sufficient grade and tonnage for commercial exploitation. In 1967, the Government of India formed Uranium Corporation of India Ltd., under the administrative control of the Department of Atomic Energy, with the specific objective of mining and processing of uranium ore and produce uranium concentrates. At present the Corporation operates three underground uranium mines, one ore processing plant with expanded capacity, and two uranium recovery plants. Continuing investigations by the Atomic Mineral Division has discovered several new deposits and favourable areas. The most notable is the large Domiasiat deposit of the sandstone type found in the State of Meghalaya. This deposit is now being considered for commercial exploitation using the in-situ leaching technology. 1. INTRODUCTION Soon after independence, the search to locate indigenous sources of uranium began as a sequel to the decision of Government of India to harness atomic energy for industrial purposes. It assumed greater importance with the rapid industrial development and limited availability of resources of fossil fuel and hydroelectricity in the country. Soon, it became imperative to locate uranium deposits in the country to meet the requirement Indigenously. In the first decade of exploration, a number of areas showing anomalous concentration of uranium was identified all over the country specially in the states of Bihar, Rajasthan, Madhya Pradesh, Himachal Pradesh, Andhra Pradesh etc.
    [Show full text]
  • Reconnaissance of Uranium and Copper Deposits in Parts of New Mexico, Colorado, Utah Idaho, and Wyoming
    GEOLOGICAL SURVEY CIRCULAR 219 RECONNAISSANCE OF URANIUM AND COPPER DEPOSITS IN PARTS OF NEW MEXICO, COLORADO, UTAH IDAHO, AND WYOMING By Garland B. Gott and Ralph L. Erickson UNITED STATES DEPARTMENT OF THE INTERIOR Oscar L. Chapman, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director GEOLOGICAL SURVEY CIRCULAR 219 RECONNAISSANCE OF URANIUM AND COPPER DEPOSITS IN PARTS OF NEW MEXICO, COLORADO, UTAH, IDAHO, AND WYOMING By Garland B. Gott and Ralph L Erickson Thia report COilC8l'D8 work doDe oa behalf of tbe U. S. Atomic Enerp Commiaion and is publiahed with the~ of the Commiuion Waahiqton, D. C1 196t Free on applieation to the Geolocical Survey, Wllhiqton 26, D. C. RECONNAISSANCE OF URANIUM AND COPPER DEPOSITS IN PARTS OF NEW MEXICO, COLORADO, UTAH, IDAHO, AND WYOMING CONTENTS Page Page Abstract ....... ·............•.•.............. 1 The copper and uranium deposits--Continued Introduction .........••..................... 1 Colorado--Continued Acknowledgments ............................ 2 The Cashin mine . 4 The copper and uraniurr, deposits ............. 2 Utah ........................•........ 5 New Mexico ............................ 2 The Big Indian mine .......•........ 5 Cuba, Abiquiu, and Gallina districts.... 2 Torrey district . • . • . 5 Jemez Springs district. .............. 4 The San Rafael Swell district. .. 5 Zuni Mountain and Scholle districts .... 4 Source of the uranium in the Pintada-Pastura district. ............ 4 asphaltites . 7 Tecolote district . 4 Idaho .................................. 8 Guadalupita district. ................ 4 Wyoming .............................. g San Acacia district .................. 4 Conclusions . 9 Colorado ............................... 4 Literature cited .. ~· . .. 9 ILLUSTRATION Page • Figure 1. Some copper and uranium deposits in parts of New Mexico, Colorado, Utah, and Wyoming........ ~ TABLES Page Tabl'e 1. Radiometric and chemical analyses of samples from some uranium and copper deposits in sandstone ........................................................................... 10 2.
    [Show full text]