Physical and Chemical Interactions Affecting U and V Transport from Mine Wastes Sumant Avasarala

Total Page:16

File Type:pdf, Size:1020Kb

Physical and Chemical Interactions Affecting U and V Transport from Mine Wastes Sumant Avasarala University of New Mexico UNM Digital Repository Civil Engineering ETDs Engineering ETDs Spring 3-2-2018 Physical and Chemical Interactions Affecting U and V Transport from Mine Wastes Sumant Avasarala Follow this and additional works at: https://digitalrepository.unm.edu/ce_etds Part of the Environmental Engineering Commons Recommended Citation Avasarala, Sumant. "Physical and Chemical Interactions Affecting U and V Transport from Mine Wastes." (2018). https://digitalrepository.unm.edu/ce_etds/205 This Dissertation is brought to you for free and open access by the Engineering ETDs at UNM Digital Repository. It has been accepted for inclusion in Civil Engineering ETDs by an authorized administrator of UNM Digital Repository. For more information, please contact [email protected]. Sumant Avasarala Candidate Civil Engineering Department This dissertation is approved, and it is acceptable in quality and form for publication: Approved by the Dissertation Committee: Dr. Jose M. Cerrato , Chairperson Dr. Ricardo Gonzalez Pinzon Dr. Bruce Thomson Dr. Adrian Brearley Dr. Mehdi Ali i Sumant Avasarala B.S., Chemical Engineering, Anna University 2009, India M.S., Chemical Engineering, Wayne State University, 2012, U.S. DISSERTATION Submitted in Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy Engineering The University of New Mexico Albuquerque, New Mexico May 2018 ii Dedication I would like to dedicate my PhD to my parents (Seshargiri Rao and Radha), my brother (Ashwin Avsasarala), my friends, and my grandfathers (V.V. Rao and Late Chalapathi Rao) without whose blessings, prayers, and support this journey would have never been possible. Special dedication to my best friend, Dr. Sriraam Ramanathan Chandrasekaran, who guided me and supported me through my rough times. I couldn’t think of a better way to indicate your role in my life than dedicating my biggest achievement to you! Thank you for always being there! iii Acknowledgement I never will have enough words to express my gratitude and gratefulness towards my advisor, Dr. José Cerrato, who offered me a PhD position despite many red flags on the way. His exceptional support, advisement, and love for his students (in this case, me) has always kept me driven and motivated—so motivated that it has finally allowed me to see light towards the end of a long, cheerful, fun, and challenging PhD tunnel. Thank you very much, José, for transforming me from a naïve graduate student to an eligible independent researcher. I really appreciate it! I am forever in your debt! Of course next on my list is Dr. Mehdi Ali for his continuous “It’s working, it’s not.” There is not a day when I have not felt I could talk to you about any challenge that I ran into. You have always comforted, guided, and supported me in both on a professional and personal level. I have relished all moments spent with you from the weekend brunches (green Chile cheese omelets) to all the laughs we shared. Thank you very much, Dr. Ali, for making my journey a lot more memorable and fun. I am also very thankful to my committee members Dr. Ricardo Gonzalez, Dr. Adrian Brearley, and Dr. Bruce Thomson for all their help, guidance, and support during my PhD research. I am also very thankful to all my co-authors without whose efforts reaching this point would have been extremely difficult. Special thanks to Dr. Brearley for his patience towards my constant harassment for data. Finally, my acknowledgement would be incomplete without my friends and lab mates. I consider myself extremely lucky to have had the opportunity to pursue a PhD alongside such smart, supportive, and loving friends. You have always been there to cheer, hold, and encourage me during my difficult times. I have learned so much from all of you, and I wish the best for you all. Thank you. I have learned so much from each and every one of you that I am forever in your debt. I hope someday I can return the favor. iv Sumant Avasarala B.S., Chemical Engineering, Anna University 2009, India M.S., Chemical Engineering, Wayne State University, U.S. Abstract. This research investigates the physical and chemical interactions that affect the transport of uranium (U) and vanadium (V) from uranium mine waste sites by integrating laboratory experiments and reactive transport modelling with various spectroscopy, microscopy, and diffraction techniques. The document consists of results from three related studies. In the first study (Chapter 3), the reactive transport of U and V was investigated by sequentially reacting mine wastes collected from Blue Gap/Tachee Claim-28 mine site, AZ with 10mM NaHCO3 (7.9) and 10mM CH3COOH (3.4) during continuous flow through column experiments. Under both of these conditions (pH 3.4 and 7.9), dissolution of U-V bearing minerals predominant at the site were identified as a key mechanism affecting the reactive transport of U and V. The equilibrium (Keq) and reaction rate constants (km) for U-V bearing mineral dissolution were estimated to be Keq -44.81 -13 -2 -1 -38.65 = 10 and km = 4.8x10 mol cm sec at circumneutral conditions, and Keq = 10 -13 -2 -1 and km = 3.2x10 mol cm sec under acidic conditions. These results, coupled with electron microscopy data, suggest that the release of U and V is affected by difference in v solution pH and crystalline structure of U-V bearing minerals. Identifying the crystal chemistry of these U-V bearing minerals was the task in the second study (Chapter 4) of the dissertation. Using various diffraction and microscopy tools, the U-V bearing minerals were identified as hydrated carnotite. Finally, the mobility of U from co-occurring submicron U(IV) and U(VI) mineral phases in mine wastes from the Jackpile mine in Laguna Pueblo, NM was investigated under oxidizing conditions. Co-occurrence of U(VI) and U(IV) at a 19:1 ratio mostly as coffinite (USiO4) and U-phosphate was observed in these mine waste solids. The highest U release from these mine wastes was observed during batch reactions with 10 mM NaHCO3 solution containing ambient dissolved oxygen concentrations. Results from these investigations provide an improved understanding on the role of thermodynamics, crystallinity, stoichiometry, and solution chemistry in the reactive transport of U and V from mine wastes that affect the water quality of surface and ground water resources. vi Physical and Chemical Interactions Affecting U and V Transport from Mine Wastes ....... i Physical and Chemical Interactions Affecting U and V Transport from Mine Wastes .......v 1 Table of Contents....................................................................................................... vii 2 List of Figures ...............................................................................................................x 3 List of Tables ........................................................................................................... xvii 1 Introduction ..................................................................................................................1 2 Literature Review .........................................................................................................4 Background and Significance................................................................................4 Study Areas: Blue Gap Tachee Claim-28, AZ and Jackpile-Paguate Mine, NM .6 State of the Knowledge about Processes Affecting U and V Transport from Mine Wastes .....................................................................................................................8 2.3.1 PFLOTRAN and Its Applications. ...............................................................10 2.3.2 Effect of Crystallinity on Metal Mobility. ...................................................11 Research Gap and Objectives ..............................................................................12 3 Reactive Transport of U and V from Abandoned Uranium Mine Wastes .................14 Abstract ...............................................................................................................14 Introduction .........................................................................................................15 Materials and Methods ........................................................................................18 3.3.1 Materials. .....................................................................................................19 3.3.2 Batch Experiments. ......................................................................................19 3.3.3 Continuous Flow Through Column Experiments. .......................................20 3.3.4 Aqueous Chemical Analyses. ......................................................................21 3.3.5 Reactive Transport Modelling. ....................................................................21 3.3.6 Solids Characterization. ...............................................................................23 Results and Discussion ........................................................................................24 3.4.1 Mine Waste Reactivity in Columns Using 18 MΩ Water (pH 5.4). ............24 3.4.2 Reactive Transport of U and V at Circumneutral pH. .................................25 3.4.3 Reactive transport of U and V at Acidic pH. ...............................................28 Environmental Implications. ...............................................................................32 4 Crystal chemistry of Uranyl Vanadates (Carnotite) in Mine Wastes .........................39
Recommended publications
  • Significance of Mineralogy in the Development of Flowsheets for Processing Uranium Ores
    JfipwK LEACHING TIME REAGENTS TEMPERATURE FLOCCULANT CLARITY AREA COUNTER CURRENT DECANTATION It 21 21 J^^LJt TECHNICAL REPORTS SERIES No.19 6 Significance of Mineralogy in the Development of Flowsheets for Processing Uranium Ores \W# INTERNATIONAL ATOMIC ENERGY AGENCY, VIENNA, 1980 SIGNIFICANCE OF MINERALOGY IN THE DEVELOPMENT OF FLOWSHEETS FOR PROCESSING URANIUM ORES The following States are Members of the International Atomic Energy Agency: AFGHANISTAN HOLY SEE PHILIPPINES ALBANIA HUNGARY POLAND ALGERIA ICELAND PORTUGAL ARGENTINA INDIA QATAR AUSTRALIA INDONESIA ROMANIA AUSTRIA IRAN SAUDI ARABIA BANGLADESH IRAQ SENEGAL BELGIUM IRELAND SIERRA LEONE BOLIVIA ISRAEL SINGAPORE BRAZIL ITALY SOUTH AFRICA BULGARIA IVORY COAST SPAIN BURMA JAMAICA SRI LANKA BYELORUSSIAN SOVIET JAPAN SUDAN SOCIALIST REPUBLIC JORDAN SWEDEN CANADA KENYA SWITZERLAND CHILE KOREA, REPUBLIC OF SYRIAN ARAB REPUBLIC COLOMBIA KUWAIT THAILAND COSTA RICA LEBANON TUNISIA CUBA LIBERIA TURKEY CYPRUS LIBYAN ARAB JAMAHIRIYA UGANDA CZECHOSLOVAKIA LIECHTENSTEIN UKRAINIAN SOVIET SOCIALIST DEMOCRATIC KAMPUCHEA LUXEMBOURG REPUBLIC DEMOCRATIC PEOPLE'S MADAGASCAR UNION OF SOVIET SOCIALIST REPUBLIC OF KOREA MALAYSIA REPUBLICS DENMARK MALI UNITED ARAB EMIRATES DOMINICAN REPUBLIC MAURITIUS UNITED KINGDOM OF GREAT ECUADOR MEXICO BRITAIN AND NORTHERN EGYPT MONACO IRELAND EL SALVADOR MONGOLIA UNITED REPUBLIC OF ETHIOPIA MOROCCO CAMEROON FINLAND NETHERLANDS UNITED REPUBLIC OF FRANCE NEW ZEALAND TANZANIA GABON NICARAGUA UNITED STATES OF AMERICA GERMAN DEMOCRATIC REPUBLIC NIGER URUGUAY GERMANY, FEDERAL REPUBLIC OF NIGERIA VENEZUELA GHANA NORWAY VIET NAM GREECE PAKISTAN YUGOSLAVIA GUATEMALA PANAMA ZAIRE HAITI PARAGUAY ZAMBIA PERU 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.
    [Show full text]
  • A Study of Some Methods of Concentrating Uranium and Radium in Carnotite Ore
    Scholars' Mine Masters Theses Student Theses and Dissertations 1932 A study of some methods of concentrating uranium and radium in carnotite ore H. L. Gibbs Follow this and additional works at: https://scholarsmine.mst.edu/masters_theses Part of the Chemical Engineering Commons Department: Recommended Citation Gibbs, H. L., "A study of some methods of concentrating uranium and radium in carnotite ore" (1932). Masters Theses. 4815. https://scholarsmine.mst.edu/masters_theses/4815 This thesis is brought to you by Scholars' Mine, a service of the Missouri S&T Library and Learning Resources. This work is protected by U. S. Copyright Law. Unauthorized use including reproduction for redistribution requires the permission of the copyright holder. For more information, please contact [email protected]. A STUDY OF SOl.ill T,::ETHODS O:B" COl1C}~;TTRl~TnTG TJP"':~..1TTIJL! ;:J·TD RIillIOIJ IN C.AR~OTIT!~ ORE. by lliJ10LD L. GIBBS A THESIS submitted to the faculty of the SCI-TOOL OF MINES AND 1~'IETIJ:.,LURGY OF THE m·...lVERSITY OJ!' I'~IaSOURI in partial fulfillment of the work required for the Degree of' Ivll~T:ER OF SCIENCE n~ C:EIa1IC.AL ENGnmERnTG Rolla, ~~iissour1 1 9 3 2 Al'proved by f.A.J. -,. ~ Acknowledgments • • • • • • • 1 Object • • ••• • • • 2 Introduction • • • 2 Description of the Ore • • • 3 Examination o~ the Ore • • • • • 3 Methods of Analysis • • • • • • 7 Flocculation Tests • • • g Flotation of Carnotite • • • • • II Results of Flotation Testa • • • • 15 Recovery of Radium :rrom Leached Ore by Flotation • • • • 18 Summary
    [Show full text]
  • Roscoelite K(V ; Al; Mg)2Alsi3o10(OH)2 C 2001 Mineral Data Publishing, Version 1.2 ° Crystal Data: Monoclinic
    3+ Roscoelite K(V ; Al; Mg)2AlSi3O10(OH)2 c 2001 Mineral Data Publishing, version 1.2 ° Crystal Data: Monoclinic. Point Group: 2=m: As minute scales, in druses, rosettes, or fan-shaped groups; ¯brous and in felted aggregates; as impregnations, massive. Physical Properties: Cleavage: Perfect on 001 . Hardness = Soft. D(meas.) = 2.92{2.94 D(calc.) = [2.89] f g Optical Properties: Transparent to translucent. Color: Dark clove-brown, greenish brown to dark greenish brown. Luster: Pearly. Optical Class: Biaxial ({). Pleochroism: X = green-brown; Y = Z = olive-green. ® = 1.59{1.610 ¯ = 1.63{1.685 ° = 1.64{1.704 2V(meas.) = 24.5±{39.5± Cell Data: Space Group: C2=c: a = 5.26 b = 9.09 c = 10.25 ¯ = 101:0± Z = 2 X-ray Powder Pattern: Paradox Valley, Colorado, USA. 10.0 (100), 4.54 (80), 3.35 (80), 2.60 (80), 1.52 (60), 3.66 (50), 3.11 (50) Chemistry: (1) SiO2 47.82 Al2O3 12.60 V2O5 19.94 FeO 3.30 MgO 2.43 CaO trace Na2O 0.33 K2O 8.03 + H2O 5.13 Total 99.58 (1) Stuckslager mine, California, USA. Polymorphism & Series: Forms a series with muscovite; 1M polytype. Mineral Group: Mica group. Occurrence: An early-stage gangue mineral in low-temperature epithermal Au-Ag-Te deposits; from the oxidized portions of low-temperature sedimentary U-V ores. Association: Quartz, pyrite, carbonates, °uorite, gold (Au-Ag-Te mineral association); corvusite, hewettite, carnotite, tyuyamunite (U-V mineral association). Distribution: In the USA, from the Stuckslager mine, Lotus, El Dorado Co., California; in Colorado, from Cripple Creek, Teller Co., La Plata district, La Plata Co., Magnolia district, Boulder Co., the Gateway district, Mesa Co., in the Uravan and Paradox, Bull Canyon, and Slick Rock districts, in Montrose, San Miguel, and Dolores Cos.
    [Show full text]
  • Mineral Processing
    Mineral Processing Foundations of theory and practice of minerallurgy 1st English edition JAN DRZYMALA, C. Eng., Ph.D., D.Sc. Member of the Polish Mineral Processing Society Wroclaw University of Technology 2007 Translation: J. Drzymala, A. Swatek Reviewer: A. Luszczkiewicz Published as supplied by the author ©Copyright by Jan Drzymala, Wroclaw 2007 Computer typesetting: Danuta Szyszka Cover design: Danuta Szyszka Cover photo: Sebastian Bożek Oficyna Wydawnicza Politechniki Wrocławskiej Wybrzeze Wyspianskiego 27 50-370 Wroclaw Any part of this publication can be used in any form by any means provided that the usage is acknowledged by the citation: Drzymala, J., Mineral Processing, Foundations of theory and practice of minerallurgy, Oficyna Wydawnicza PWr., 2007, www.ig.pwr.wroc.pl/minproc ISBN 978-83-7493-362-9 Contents Introduction ....................................................................................................................9 Part I Introduction to mineral processing .....................................................................13 1. From the Big Bang to mineral processing................................................................14 1.1. The formation of matter ...................................................................................14 1.2. Elementary particles.........................................................................................16 1.3. Molecules .........................................................................................................18 1.4. Solids................................................................................................................19
    [Show full text]
  • Page 1 of 9 SAFETY DATA SHEET CARNOTITE ORE SECTION 1
    SAFETY DATA SHEET CARNOTITE ORE SECTION 1: CHEMICAL PRODUCTS & COMPANY IDENTIFICATION NBL Program Office U. S. Department of Energy, 1 Science.gov Way, Oak Ridge, TN 37830 1-865-576-0598 Emergency Phone Numbers: 1-865-576-0598 Substance: Carnotite Ore Blend Trade Names/Synonyms: Potassium uranium vanadate, Uranium Oxide (U3O8), Uranous Oxide, Triuranium Octaoxide, Uranite Nasturan, CRM 4, CRM 5 Use and Restriction: This material is prepared for use as a standard or for inter- laboratory comparison programs at analytical laboratories, which routinely handle uranium and/or plutonium. NBL expects that recipients of their material are in compliance with 29 CFR 1910.1200(h) which requires employers to provide employees with effective information and training in hazardous chemicals in their work area. SECTION 2: HAZARDS IDENTIFICATION OSHA Hazards Toxic by inhalation, toxic by ingestion. Target Organs Kidney, Liver, Lungs, Brain. GHS Label Elements Pictogram Signal Word: Danger Page 1 of 9 Hazard Statements: Toxic by inhalation and ingestion Danger of cumulative effects May damage kidneys Precautionary Statements: Avoid Breathing Dust Avoid contact with skin, eyes and clothing When using do not eat, drink or smoke In case of accident or if you feel unwell seek medical advice immediately Use only with adequate ventilation GHS Classification Skin Irritation (Category 2) Eye Irritation (Category 2) Specific target organ toxicity - repeated exposure (Category 2) Specific target organ toxicity – acute exposure (Category 2) GHS Hazard Ratings R23/25: Toxic by inhalation and ingestion R33: Danger of cumulative effects S20/21: When using do not eat, drink or smoke S45: In case of accident or if you feel unwell seek medical advice immediately S61: Avoid release to the environment.
    [Show full text]
  • Uraninite Alteration in an Oxidizing Environment and Its Relevance to the Disposal of Spent Nuclear Fuel
    TECHNICAL REPORT 91-15 Uraninite alteration in an oxidizing environment and its relevance to the disposal of spent nuclear fuel Robert Finch, Rodney Ewing Department of Geology, University of New Mexico December 1990 SVENSK KÄRNBRÄNSLEHANTERING AB SWEDISH NUCLEAR FUEL AND WASTE MANAGEMENT CO BOX 5864 S-102 48 STOCKHOLM TEL 08-665 28 00 TELEX 13108 SKB S TELEFAX 08-661 57 19 original contains color illustrations URANINITE ALTERATION IN AN OXIDIZING ENVIRONMENT AND ITS RELEVANCE TO THE DISPOSAL OF SPENT NUCLEAR FUEL Robert Finch, Rodney Ewing Department of Geology, University of New Mexico December 1990 This report concerns a study which was conducted for SKB. The conclusions and viewpoints presented in the report are those of the author (s) and do not necessarily coincide with those of the client. Information on SKB technical reports from 1977-1978 (TR 121), 1979 (TR 79-28), 1980 (TR 80-26), 1981 (TR 81-17), 1982 (TR 82-28), 1983 (TR 83-77), 1984 (TR 85-01), 1985 (TR 85-20), 1986 (TR 86-31), 1987 (TR 87-33), 1988 (TR 88-32) and 1989 (TR 89-40) is available through SKB. URANINITE ALTERATION IN AN OXIDIZING ENVIRONMENT AND ITS RELEVANCE TO THE DISPOSAL OF SPENT NUCLEAR FUEL Robert Finch Rodney Ewing Department of Geology University of New Mexico Submitted to Svensk Kämbränslehantering AB (SKB) December 21,1990 ABSTRACT Uraninite is a natural analogue for spent nuclear fuel because of similarities in structure (both are fluorite structure types) and chemistry (both are nominally UOJ. Effective assessment of the long-term behavior of spent fuel in a geologic repository requires a knowledge of the corrosion products produced in that environment.
    [Show full text]
  • Weeksite K2(UO2)2(Si5o13)·4H2O
    Weeksite K2(UO2)2(Si5O13)·4H2O Crystal Data: Monoclinic. Point Group: 2/m: As bladed or acicular crystals, flattened on {010} and elongated along [001], and as flat plates; also as spherulites and radiating fibrous clusters. - Twinning: By two-fold rotation around [401 ]. Physical Properties: Cleavage: Two good prismatic cleavages noted. Hardness = < 2 D(meas.) = ~ 4.1 D(calc.) = 3.80 Radioactive. Optical Properties: Transparent to translucent. Color: Yellow. Luster: Waxy to silky. Optical Class: Biaxial (-). α = 1.596 β = 1.603 γ = 1.606 2V(meas.) = ~ 60° 2V(calc.) = 66° Pleochroism: X = colorless, Y = pale yellow-green, Z = yellow-green. Dispersion: r > v, strong. Orientation: X = b, Y = c, Z = a. Cell Data: Space Group: C2/m. a = 14.26(2) b = 35.88(10) c = 14.20(2) β = 111.578(3)° Z = 4 X-ray Powder Pattern: Thomas Range, Utah, USA. 7.11 (10), 5.57 (9), 8.98 (8), 3.55 (7), 3.30 (7), 2.91 (6), 3.20 (5) Chemistry: (1) (1) Na2O 0.53 Al2O3 0.6 K2O 4.73 SiO2 29.44 CaO 0.67 UO3 55.78 BaO 3.11 H2O [7.02] MgO 0.18 Total 101.28 SrO 0.20 (1) Anderson mine, Arizona, USA; average of 8 electron microprobe analyses, supplemented by TGA, H2O calculated from structure, corresponds to (K1.031Na0.176Ca0.123Ba0.208)Σ=1.537(UO2)2.002 (Si5.030O13)·4H2O. Occurrence: In “opal" veinlets in rhyolite, agglomerates, sandstones and limestones. Association: “Opal," “chalcedony," calcite, gypsum, fluorite, uraninite, thorogummite, uranophane, boltwoodite, carnotite, margaritasite. Distribution: In the USA, in Utah, at the Autunite No.
    [Show full text]
  • CORVUSITE and RILANDITE, NEW MINERALS from the UTAH-COLORADO CARNOTITE REGIOI{ Eowenn P
    CORVUSITE AND RILANDITE, NEW MINERALS FROM THE UTAH-COLORADO CARNOTITE REGIOI{ Eowenn P. HBNonnsoNAND Fnaxr L. Hnss,x U. S. National, Museum. InrnonucrroN In the carnotite-bearing depositsof Colorado and Utah the sand- stone and accompanying clays are impregnated with many dark brown and black mineral masses,which show no crystal form to the unaided eye and few other definite characteristics. The most common of the dark colored minerals are listed below. Roscoelite vanadium mica Rauvite CaO'2UOr'6VzOr'2OHrO Vanoxite 2VzOr'VzOs(S* )HzO Corvusite VrOr'6VeOs'XH:O Rilandite hydrouschromium aluminum silicate Lignite Tar (?) Asphaltite Psilomelane Iron-copper-cobaltoxide. Two of the names, corvusite and rilandite, are new and are pro- posed in this paper. The authors hesitated to give names to such compounds as those to which they are applied becauseno entirely satisfactory formula can be ofiered for either, but since the sub- stance called corvusite is common in the carnotite region a verbal handle seemsnecessary. Rilandite, although at present known from only one locality, was obtained in rather large quantity and its as- sociation is such that it seemslikely that it will be obtained from other places in the carnotite region. If at some future date further study shows these names unnecessarythey can easily be relegated to oblivion. Gr,Nnner, Rnr.attoNsrups Roscoelite or a similar dark mineral is provisionally identifiable by the microscope from many places in this region. Roscoelite is well known, rauvite and vanoxitel and the asphaltitez have been * Published by permission of the Secretary of the Smithsonian Institution. I Hess, Frank L., New and known minerals from the Utah-Colorado carnotite region: U.
    [Show full text]
  • Iidentilica2tion and Occurrence of Uranium and Vanadium Identification and Occurrence of Uranium and Vanadium Minerals from the Colorado Plateaus
    IIdentilica2tion and occurrence of uranium and Vanadium Identification and Occurrence of Uranium and Vanadium Minerals From the Colorado Plateaus c By A. D. WEEKS and M. E. THOMPSON A CONTRIBUTION TO THE GEOLOGY OF URANIUM GEOLOGICAL S U R V E Y BULL E TIN 1009-B For jeld geologists and others having few laboratory facilities.- This report concerns work done on behalf of the U. S. Atomic Energy Commission and is published with the permission of the Commission. UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1954 UNITED STATES DEPARTMENT OF THE- INTERIOR FRED A. SEATON, Secretary GEOLOGICAL SURVEY Thomas B. Nolan. Director Reprint, 1957 For sale by the Superintendent of Documents, U. S. Government Printing Ofice Washington 25, D. C. - Price 25 cents (paper cover) CONTENTS Page 13 13 13 14 14 14 15 15 15 15 16 16 17 17 17 18 18 19 20 21 21 22 23 24 25 25 26 27 28 29 29 30 30 31 32 33 33 34 35 36 37 38 39 , 40 41 42 42 1v CONTENTS Page 46 47 48 49 50 50 51 52 53 54 54 55 56 56 57 58 58 59 62 TABLES TABLE1. Optical properties of uranium minerals ______________________ 44 2. List of mine and mining district names showing county and State________________________________________---------- 60 IDENTIFICATION AND OCCURRENCE OF URANIUM AND VANADIUM MINERALS FROM THE COLORADO PLATEAUS By A. D. WEEKSand M. E. THOMPSON ABSTRACT This report, designed to make available to field geologists and others informa- tion obtained in recent investigations by the Geological Survey on identification and occurrence of uranium minerals of the Colorado Plateaus, contains descrip- tions of the physical properties, X-ray data, and in some instances results of chem- ical and spectrographic analysis of 48 uranium arid vanadium minerals.
    [Show full text]
  • ~Ui&£R5itt! of J\Rij!Oua
    Minerals and metals of increasing interest, rare and radioactive minerals Authors Moore, R.T. Rights Arizona Geological Survey. All rights reserved. Download date 06/10/2021 17:57:35 Link to Item http://hdl.handle.net/10150/629904 Vol. XXIV, No.4 October, 1953 ~ui&£r5itt! of J\rij!oua ~ul1etiu ARIZONA BUREAU OF MINES MINERALS AND METALS OF INCREASING INTEREST RARE AND RADIOACTIVE MINERALS By RICHARD T. MOORE ARIZONA BUREAU OF MINES MINERAL TECHNOLOGY SERIES No. 47 BULLETIN No. 163 THIRTY CENTS (Free to Residents of Arizona) PUBLISHED BY ~tti£ll~r5itt! of ~rh!Omt TUCSON, ARIZONA TABLE OF CONTENTS INTRODUCTION 5 Acknowledgments 5 General Features 5 BERYLLIUM 7 General Features 7 Beryllium Minerals 7 Beryl 7 Phenacite 8 Gadolinite 8 Helvite 8 Occurrence 8 Prices and Possible Buyers ,........................................ 8 LITHIUM 9 General Features 9 Lithium Minerals 9 Amblygonite 9 Spodumene 10 Lepidolite 10 Triphylite 10 Zinnwaldite 10 Occurrence 10 Prices and Possible Buyers 10 CESIUM AND RUBIDIUM 11 General Features 11 Cesium and Rubidium Minerals 11 Pollucite ..................•.........................................................................., 11 Occurrence 12 Prices and Producers 12 TITANIUM 12 General Features 12 Titanium Minerals 13 Rutile 13 Ilmenite 13 Sphene 13 Occurrence 13 Prices and Buyers 14 GALLIUM, GERMANIUM, INDIUM, AND THALLIUM 14 General Features 14 Gallium, Germanium, Indium and Thallium Minerals 15 Germanite 15 Lorandite 15 Hutchinsonite : 15 Vrbaite 15 Occurrence 15 Prices and Producers ~ 16 RHENIUM 16
    [Show full text]
  • Identification and Occurrence of Uranium and Vanadium Minerals from the Colorado Plateaus
    SpColl £2' 1 Energy I TEl 334 Identification and Occurrence of Uranium and Vanadium Minerals from the Colorado Plateaus ~ By A. D. Weeks and M. E. Thompson ~ I"\ ~ ~ Trace Elements Investigations Report 334 UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY IN REPLY REFER TO: UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY WASHINGTON 25, D. C. AUG 12 1953 Dr. PhilUp L. Merritt, Assistant Director Division of Ra1'r Materials U. S. AtoTILic Energy Commission. P. 0. Box 30, Ansonia Station New· York 23, Nei< York Dear Phil~ Transmitted herewith are six copies oi' TEI-334, "Identification and occurrence oi' uranium and vanadium minerals i'rom the Colorado Plateaus," by A , D. Weeks and M. E. Thompson, April 1953 • We are asking !41'. Hosted to approve our plan to publish this re:por t as a C.i.rcular .. Sincerely yours, Ak~f777.~ W. H. ~radley Chief' Geologist UNCLASSIFIED Geology and Mineralogy This document consists or 69 pages. Series A. UNITED STATES DEPARTMENT OF TEE INTERIOR GEOLOGICAL SURVEY IDENTIFICATION AND OCCURRENCE OF URANIUM AND VANADIUM MINERALS FROM TEE COLORADO PLATEAUS* By A• D. Weeks and M. E. Thompson April 1953 Trace Elements Investigations Report 334 This preliminary report is distributed without editorial and technical review for conformity with ofricial standards and nomenclature. It is not for public inspection or guotation. *This report concerns work done on behalf of the Division of Raw Materials of the u. s. Atomic Energy Commission 2 USGS GEOLOGY AllU MINEFALOGY Distribution (Series A) No. of copies American Cyanamid Company, Winchester 1 Argulllle National La:boratory ., ., .......
    [Show full text]
  • Geology, Geochemistry, and Mineralogy of the Ridenour Mine Breccia Pipe, Arizona
    UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY Geology, Geochemistry, and Mineralogy of the Ridenour Mine Breccia Pipe, Arizona by Karen J. Wenrich1 , Earl R. Verbeek 1 , Hoyt B. Sutphin2 , Peter J. Modreski 1 , Bradley S. Van Gosen 11, and David E. Detra Open-File Report 90-0504 This study was funded by the Bureau of Indian Affairs in cooperation with the Hualapai Tribe. 1990 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature. U.S. Geological Survey 2U.S. Pollution Control, Inc. Denver, Colorado Boulder, Colorado CONTENTS Page Abstract ................................................................... 1 Introduction ............................................................... 2 Geology and structure of the Ridenour mine ................................. 5 Structural control of the Ridenour and similar pipes ....................... 7 Mine workings ............................................................. 11 Geochemistry .............................................................. 11 Metals strongly enriched at the Ridenour pipe ......................... 23 Vanadium ......................................................... 23 Silver ........................................................... 30 Copper ........................................................... 30 Gallium .......................................................... 30 Isotopic studies ...................................................... 30 Mineralogy ...............................................................
    [Show full text]