Evaluation of Low-Temperature Fluoride Routes to Synthesize Actinide Nitrides and Oxide Solid Solutions

Total Page:16

File Type:pdf, Size:1020Kb

Evaluation of Low-Temperature Fluoride Routes to Synthesize Actinide Nitrides and Oxide Solid Solutions UNLV Theses, Dissertations, Professional Papers, and Capstones 5-2009 Evaluation of low-temperature fluoride outesr to synthesize actinide nitrides and oxide solid solutions Gunanda Waduge Chinthaka Silva University of Nevada, Las Vegas Follow this and additional works at: https://digitalscholarship.unlv.edu/thesesdissertations Part of the Materials Chemistry Commons, Nuclear Commons, Nuclear Engineering Commons, and the Radiochemistry Commons Repository Citation Silva, Gunanda Waduge Chinthaka, "Evaluation of low-temperature fluoride outesr to synthesize actinide nitrides and oxide solid solutions" (2009). UNLV Theses, Dissertations, Professional Papers, and Capstones. 1127. http://dx.doi.org/10.34917/2502495 This Dissertation is protected by copyright and/or related rights. It has been brought to you by Digital Scholarship@UNLV with permission from the rights-holder(s). You are free to use this Dissertation in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you need to obtain permission from the rights-holder(s) directly, unless additional rights are indicated by a Creative Commons license in the record and/or on the work itself. This Dissertation has been accepted for inclusion in UNLV Theses, Dissertations, Professional Papers, and Capstones by an authorized administrator of Digital Scholarship@UNLV. For more information, please contact [email protected]. EVALUATION OF LOW-TEMPERATURE FLUORIDE ROUTES TO SYNTHESIZE ACTINIDE NITRIDES AND OXIDE SOLID SOLUTIONS by Gunanda Waduge Chinthaka Silva Bachelor of Science University of Colombo, Sri Lanka 2000 Master of Science in Chemistry University of Nevada, Las Vegas 2005 A dissertation submitted in partial fulfillment of the requirements for the Doctor of Philosophy Degree in Radiochemistry Department of Chemistry College of Sciences Graduate College University of Nevada, Las Vegas May 2009 UMI Number: 3383994 Copyright 2009 by Silva, Gunanda Waduge Chinthaka INFORMATION TO USERS The quality of this reproduction is dependent upon the quality of the copy submitted. Broken or indistinct print, colored or poor quality illustrations and photographs, print bleed-through, substandard margins, and improper alignment can adversely affect reproduction. In the unlikely event that the author did not send a complete manuscript and there are missing pages, these will be noted. Also, if unauthorized copyright material had to be removed, a note will indicate the deletion. UMI® UMI Microform 3383994 Copyright 2009 by ProQuest LLC All rights reserved. This microform edition is protected against unauthorized copying under Title 17, United States Code. ProQuest LLC 789 East Eisenhower Parkway P.O. Box 1346 Ann Arbor, Ml 48106-1346 Copyright by Gunanda Waduge Chinthaka Silva 2009 All Rights Reserved Dissertation Approval UNW The Graduate College University of Nevada, Las Vegas st April 1 _/20. 09 The Dissertation prepared by Gunanda Waduge Chinthaka Silva Entitled Evaluation of Low-Temperature Fluoride Routes to Synthesize Actinide Nitrides and Oxide Solid Solutions is approved in partial fulfillment of the requirements for the degree of Doctor of Philosophy in Radiochemistry Examination Committee Chair Dean of the Graduate College ExaminatiorrQjmmittee Member Examination Committee Member Graduate College faculty Representative 1017-52 11 ABSTRACT Evaluation of Low-Temperature Fluoride Routes to Synthesize Actinide Nitrides and Oxide Solid Solutions by Gunanda Waduge Chinthaka Silva Dr. Kenneth R. Czerwinski, Examination Committee Chair Professor of Chemistry Head of the Department of Radiochemistry University of Nevada, Las Vegas Actinide mononitrides have been considered as a possible nuclear fuel for the Generation-IV nuclear reactor systems. In the process of evaluating these actinide mononitrides as nuclear fuel, it is important to study different chemical and physical characteristics of these compounds. Synthesis of the materials is thus important. Carbothermic reduction is one of the techniques that have been used to synthesize actinide mononitrides. In this method, a mixture of actinide oxide such as UO2 and excess carbon is heat treated at temperatures greater than 1700 °C under a nitrogen atmosphere. The technique is however not promising in synthesizing the actinide mononitrides due to a number of disadvantages the technique presents. Lack of phase purity due to secondary chemical phases with carbon and oxygen, need of high temperatures such as 2200 °C, and the low density of the final product compared to theoretical density are some of the drawbacks that the researches have been encountered. Most of all this method is tiresome and difficult to handle in ordinary laboratories where the experimental setups and iii conditions are inadequate to synthesize actinide mononitrides up to an acceptable quality for chemical characterizations. Therefore, it is important to explore different routes that can be used to synthesize such actinide nitrides and characterize them properly. A recent development of a low-temperature fluoride route in synthesizing UN2 at 800 °C and UN at 1100 °C, proposed a further investigation of this particular chemical route in synthesizing other nitrides of the actinide series. Thus, the possibility of making nitrides of thorium, neptunium, and mixed uranium-thorium by the above mentioned method was suggested. Mechanisms and kinetics involved in separate reactions were studied. Chemical characterizations of the as-synthesized materials were also completed using different techniques reported in Chapter 2. Optimization of this low-temperature process to minimize the formation of secondary phases such as UO2 was also examined in a typical experimental setup by exploring the uranium system. With the thorium, however, only ThNF could be synthesized up to a temperature of 1100 °C. Addition of lithium amide (LiNlrk) into the reactants in synthesizing ThNx produced TI12N3 with some Th02 impurities. This finding is controversial and will discuss the relevant issues in the corresponding chapter. Characterization of Th2N3/Th02 samples revealed an interchangeable formation of TI1O2 in TI12N3 and vise versa suggesting a possible reason for the high susceptibility of ThNx toward oxygen as general. Evaluation of the neptunium system revealed 6 new compounds with isomorphous crystal structures to that of uranium with similar chemical compositions. XRD powder refinements could be used in solving these crystal structures. NpN was synthesized at 900 °C and further experiments are required to check the lower temperatures for making iv the mononitride. However, further experiments will be necessary to optimize the heating time. Microscopic characterization of NpNx compounds was also conducted with SEM and TEM. Nanostructural studies conducted on these samples displayed high crystallographic order in their structures. Uranium and thorium mixed system was also examined with an eye towards synthesizing uranium-thorium mixed nitrides. Less than 1 wt% thorium solubility was identified in the UN2 with XRD and microscopic studies. Further application of the technique on oxides was explored and a novel route in synthesizing (U, Th)02 solid solutions at temperatures of 1100 °C or less, depending on the chemical composition of the oxide solid solution, was established. Moreover, this novel route itself proposes a new and easy to use low-temperature path to fabricate actinide oxide solid solutions from initial, separate oxide starting phases. v TABLE OF CONTENTS ABSTRACT iii LIST OF TABLES vii LIST OF FIGURES viii ACKNOWLEDGEMENTS x CHAPTER 1 INTRODUCTION 1 1.1 Actinide Nitrides as a Nuclear Fuel 1 1.2 Crystallography of Actinide Nitrides 4 1.3 Carbothermic Reduction 8 1.4 Low-Temperature Fluoride Route 10 CHAPTER 2 METHODOLOGY AND INSTRUMENTATION 18 2.1 Introduction 18 2.2 Reagents 18 2.3 Experimental Procedures 19 2.4 X-ray Powder Diffraction (XRD) 20 2.5 Transmission Electron Microscopy (TEM) 24 2.6 Scanning Electron Microscopy (SEM) 32 2.7 Electron Microprobe Analysis 34 CHAPTER 3 SYNTHESIS AND CHARACTERIZATION OF URANIUM NITRIDES 38 3.1 Introduction 38 3.2 Experimental details 40 3.3 Mechanism and Kinetics of UN2 Decomposition 41 3.4 Microscopic Evaluation of UNX 54 3.5 Discussion 65 3.6 Conclusions 70 CHAPTER 4 EVALUATION OF THORIUM SYSTEM 73 4.1 Introduction 73 4.2 Experimental Details and Characterization Methods 76 4.3 Synthesis and Characterization of (NH^ThFg 78 4.4 Synthesis and Characterization of ThNF 84 4.5 Ammonolysis of ThF4 and the Thermal Behavior of ThNF 91 4.6 Synthesis and Characterization of TI12N3 95 VI 4.7 Discussion 105 4.8 Conclusions Ill CHAPTER 5 SYNTHESIS AND CHARACTERIZATION OF NEPTUNIUM NITRIDES 115 5.1 Introduction 115 5.2 Experimental Details and Characterization Methods 117 5.3 Results and Discussion 119 5.4 Conclusions 155 CHAPTER 6 EVALUATION OF URANIUM-THORIUM MIXED SYSTEM ... 160 6.1 Introduction 160 6.2 Experimental Methods 162 6.3 Characterization methods 164 6.4 Results and Discussion 165 6.5 Conclusions 192 CHAPTER 7 CONCLUSIONS AND RECOMMENDATIONS 195 7.1 Uranium System 195 7.2 Thorium System 196 7.3 Neptunium System 198 7.4 Uranium and Thorium Mixed System 200 VITA 203 vii LIST OF TABLES Table 1.1 Comparison on actinide oxide, carbide, and nitride properties 2 Table 1.2 Crystallography of uranium nitrides 4 Table 1.3 Crystallography of thorium nitrides 6 Table 2.1 Cover gases used for the experiments 18 Table 2.2 Chemicals used in the research work 19 Table 2.3 Chemical composition
Recommended publications
  • 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]
  • The Stability of Lead Isotopes from Thorium
    MAY 24, I9I7] NATURE ---------------------------------------------------------245 but I Prof. Stefan lYle:yer may be I .have pointed out the unsuitability of makmg some exammatwn of the radiations of the thonum mmerals for age determination or correlation material, and the results he obtains will therefore be and this is particularly so i.n the case of minerals of very great value in deciding this point. the Palreozoic igneous rocks of Langesundfjord, Nor­ FREDERICK SoDDY. way. Mr. Lawson and myself based our former con­ Aberdeen, May 14. that lead could not be the end product of thonum largely on analyses of these minerals. How­ . PRO.F. SoDDY. having given me the privilege of read­ e:ver, I have recalculated the ratiQs on the assump­ mg h1s letter m advance, I should like to take the twn that thonum has one-seventh the lead-producing opportunity of directing attention to the geological age power of uranium, and it is satisfactory to find that :>f the thorium minerals of Ceylon, and to a few further when thorium is less than five times a·s abundant statistics bearing on the suggestion that only 35 per uranium, the ratios agree as closely on th'ts calculation cent. of thorium produces a stable isotope of lead. as do the simple lead-ratios. When thorium is more than five times as abundant as uranium neither set I a!ll to my friend, Mr. E. J. Wayland, late of ratios gives any approach to agreement although of Ceylon, for the follow­ mg prov1s1onal classdicat10n (in order of age) of the the minerals from anv one locality agree am'ong them­ older rocks of the island :- selves.
    [Show full text]
  • Stillwellite-(Ce) (Ce, La, Ca)Bsio
    Stillwellite-(Ce) (Ce; La; Ca)BSiO5 c 2001 Mineral Data Publishing, version 1.2 ° Crystal Data: Hexagonal. Point Group: 3: As °at rhombohedral crystals, to 4 cm, and massive. Twinning: Observed about [100]. Physical Properties: Cleavage: One imperfect. Fracture: Conchoidal. Hardness = 6.5 D(meas.) = 4.57{4.60 D(calc.) = 4.67 » Optical Properties: Transparent to translucent. Color: Red-brown to pale pink; colorless in thin section. Streak: White. Optical Class: Uniaxial (+) to biaxial (+). ! = 1.765{1.784 ² = 1.780{1.787 2V(meas.) = 0±{6± Cell Data: Space Group: P 31: a = 6.841{6.844 c = 6.700{6.702 Z = 3 X-ray Powder Pattern: Mary Kathleen mine, Australia. 3.43 (s), 2.96 (s), 2.13 (ms), 4.44 (m), 1.864 (m), 2.71 (mw), 2.24 (mw) Chemistry: (1) (2) (1) (2) (1) (2) SiO2 22.40 22.06 La2O3 27.95 19.12 MgO 0.06 UO2 0.22 Ce2O3 33.15 30.82 CaO 0.95 0.34 ThO2 5.41 Pr2O3 1.82 F 0.30 + B2O3 12.23 [13.46] Nd2O3 5.36 H2O 0.85 Al2O3 0.42 Sm2O3 0.34 H2O¡ 0.10 Y2O3 0.74 0.28 Fe2O3 0.18 P2O5 0.67 Total [100.00] [99.26] (1) Mary Kathleen mine, Australia; recalculated to 100.00% after removal of very small amounts of uraninite and apatite determined by separate analysis. (2) Vico volcano, near Vetralla, Italy; by electron microprobe, B2O3 calculated from stoichiometry, original total given as 99.23%; corresponds to (Ce0:50La0:31Nd0:08Th0:05Pr0:03Ca0:02Sm0:01)§=1:00B1:02Si0:97O5: Occurrence: Locally abundant as a metasomatic replacement of metamorphosed calcareous sediments (Mary Kathleen mine, Australia); in alkalic pegmatites in syenite in an alkalic massif (Dara-i-Pioz massif, Tajikistan).
    [Show full text]
  • Crystallographic Study of Uranium-Thorium Bearing Minerals in Tranomaro, South-East Madagascar
    Journal of Minerals and Materials Characterization and Engineering, 2013, 1, 347-352 Published Online November 2013 (http://www.scirp.org/journal/jmmce) http://dx.doi.org/10.4236/jmmce.2013.16053 Crystallographic Study of Uranium-Thorium Bearing Minerals in Tranomaro, South-East Madagascar Frank Elliot Sahoa1, Naivo Rabesiranana1*, Raoelina Andriambololona1, Nicolas Finck2, Christian Marquardt2, Hörst Geckeis2 1Institut National des Sciences et Techniques Nucléaires (Madagascar-INSTN), Antananarivo, Madagascar 2Institute of Nuclear Waste and Disposal (INE), Karlsruhe Institute of Technology (KIT), Karlsruhe, Germany Email: *[email protected] Received September 20, 2013; revised October 21, 2013; accepted November 5, 2013 Copyright © 2013 Frank Elliot Sahoa et al. This is an open access article distributed under the Creative Commons Attribution Li- cense, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. ABSTRACT Studies are undertaken to characterize the uranium and thorium minerals of south-east Madagascar. Seven selected uranothorianite bearing pyroxenites samples from old abandoned uranium quarries in Tranomaro, south Amboasary, Madagascar (46˚28'00"E, 24˚36'00"S) have been collected. To determine the mineral micro-structure, they were inves- tigated for qualitative identification of crystalline compounds by using X-ray powder diffraction analytical method (XRD). Results showed that the uranium and thorium compounds, as minor elements, were present in various crystal- line structures. Thorium, as thorianite, is present in a simple ThO2 cubic crystalline system, whereas the uranium com- ponent of the Tranomaro uranothorianite samples is oxide-based and is a mixture of complex oxidation states and crys- talline systems. Generally called uraninite, its oxide compounds are present in more than eight phases.
    [Show full text]
  • A Brief Overview Including Uses, Worldwide Resources, and Known Occurrences in Alaska
    A brief overview including uses, worldwide resources, and known occurrences in Alaska Information Circular 61 David J. Szumigala and Melanie B. Werdon STATE OF ALASKA DEPARTMENT OF NATURAL RESOURCES Division of Geological & Geophysical Surveys (DGGS) 3354 College Road, Fairbanks, AK 99709-3707 www.dggs.alaska.gov COVER PHOTO CAPTIONS: TOP: Sheeted REE-bearing veins, Dotson Trend, Bokan Mountain property, Alaska. Photo from http://www.ucoreraremetals.com/docs/SME_2010_Keyser.pdf BOTTOM: Rare-earth-element-bearing quartz vein exposed in granite, Bokan Mountain, Alaska. Photo from http://www.ucoreraremetals.com/docs/SME_2010_Keyser.pdf RARE-EARTH ELEMENTS: A brief overview including uses, worldwide resources, and known occurrences in Alaska David J. Szumigala and Melanie B. Werdon GGS Minerals Program The Alaska Division of Geological & Geophysical Surveys (DGGS), part of the Department of Natural Resources, is charged by statute with determining the potential of Alaska’s land for production of metals, minerals, fuels, and geothermal resources; the locations and supplies of groundwater and construction Dmaterial; and the potential geologic hazards to buildings, roads, bridges, and other installations and structures. The Mineral Resources Section at DGGS collects, analyzes, and provides information on the geological and geophysical framework of Alaska as it pertains to the state’s mineral resources. The results of these studies include reports and maps, which are used by scientists for various associated studies, by mining company geologists as a basis for their more focused exploration programs, and by state and federal agency personnel in resource and land-use management decisions. This paper provides a brief overview of rare-earth elements, their uses, and current worldwide sources of their production.
    [Show full text]
  • Uranothorite from Eastern Ontario1
    URANOTHORITEFROM EASTERN ONTARIO1 S. C. ROBINSON2 eno SYDNEY ABBEYB Geol,og'ical, Survey of Canadn, Ottawa ABSTRACT Uranothorite is found in manydeposits of the Grenville sub-province in Ontario and Quebec, and in some mines.is an important ore mineral of uranium. Its occurrence, habit, and physical properties are reviewed. Analyses for eleven specimens of uran- othorite are presented and variations in analysesand physical properties are discussed. For chemical analysis, silica was separated by perchloric dehydration and lead by sulphide and sulphate precipitation. Uranium was determined by a cupferron-oxine method, thorium and rare eartfrs via oxalate and "thorin", iron with o-phenanthroline, and calcium by oxalate precipitation. Water was determined by a modified Penfield metJrod, carbon dioxide by acid evolution and total carbon by combustion, each on a separate sample. Panr I: OccunnBxcE AND DBscnrprroN (S.C.R.) Intrad,uction Uranoth5rite was first identified and analysed in Canada by H. V. Ellsworth (L927)4 in specimens from the MacDonald feldspar mine, near Hybla, Ontario. Since that time, it has been identified in many other deposits of the Grenville sub-province of the Canadian Shield, both in eastern Ontario and in southwestern Quebec. In the past four years uranothorite has emerged as a minor ore mineral of uranium in mines of the Bancroft-Wilberforce camp where uraninite is the principal source of uranium. Few additional data on uranothorite in Canada have been published since Ellsworth's original paper. In the course of a field project on the mineralogy of uranium deposits in the Bancroft-Wilberforce region by one of us (S.C.R.), it became obvious that although uranothorite is an important contributor of uranium in ores of some mines, knowledge of its occurrence and com- position was inadequate.
    [Show full text]
  • Thorianite Tho2 C 2001-2005 Mineral Data Publishing, Version 1
    Thorianite ThO2 c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Cubic. Point Group: 4/m 32/m. Typically as more or less rough cubes, rarely modified by {111} and {113}, to 9 cm; as rounded grains. Twinning: Common on {111}, interpenetrant. Physical Properties: Cleavage: {001}, poor. Fracture: Uneven to subconchoidal. Tenacity: Brittle. Hardness = 6.5–7, unaltered. VHN = 1132–1278, 1180 average (100 g load). D(meas.) = 9.7–9.8 D(calc.) = 9.991 Radioactive; diamagnetic. Optical Properties: Opaque, transparent in very thin fragments. Color: Black, brownish black, dark gray, dark reddish brown, may have a bronzy tarnish; in transmitted light, dark brown, reddish brown, greenish; gray with red-brown internal reflections in reflected light. Streak: Gray to greenish gray. Luster: Submetallic when fresh, altering to resinous or hornlike. Optical Class: Isotropic; may show weak anomalous anisotropism. n = 2.20–2.35 R: (400) 16.6, (420) 16.6, (440) 16.6, (460) 16.5, (480) 16.3, (500) 16.0, (520) 15.7, (540) 15.4, (560) 15.2, (580) 15.1, (600) 15.0, (620) 14.9, (640) 14.8, (660) 14.7, (680) 14.6, (700) 14.5 Cell Data: Space Group: Fm3m. a = 5.595 Z = 4 X-ray Powder Pattern: Synthetic; may be confused with uraninite or cerianite. 3.234 (100), 1.689 (64), 1.980 (58), 2.800 (35), 1.284 (26), 1.1432 (20), 1.0779 (19) Chemistry: (1) (2) UO3 18.88 ThO2 93.02 62.16 UO2 4.73 10.32 (Ce, La)2O3 1.84 Fe2O3 0.29 1.11 PbO 1.80 2.29 CaO 0.59 H2O 1.05 insol.
    [Show full text]
  • Conserve O Gram Volume 11 Issue 10: Radioactive Minerals
    Conserve O Gram September 2006 Number 11/10 Radioactive Minerals Radioactive Minerals Alpha rays are the nuclei of helium atoms, two protons and two neutrons bound together. See also the NPS Museum Handbook, Part 1, Alpha rays have a net positive charge. Alpha Chapter 11 and Appendix H, Curatorial Health particles have only a weak ability to penetrate. and Safety and COG 2/5 Fossil Vertebrates as A couple of inches of air or a few sheets of Radon Source: Health Update. paper can effectively block them. Examples of common radioactive minerals Beta rays are identical to the electrons found include Autunite (hydrated calcium uranium in atoms. Beta rays have a net negative charge. phosphate), Brannerite (uranium titanate), Car- Beta rays have a greater penetrating power than notite (potassium uranium vanadate), Alpha rays and can penetrate 3 mm of alumi- Monazite (a mixed rare earth and thorium num. phosphate), Thorianite (thorium dioxide) and Uraninite (uranium dioxide). The vast majority Gamma rays are high-energy photons. This of the radioactive content in minerals or ores type of ray has the greatest penetrating power. is either uranium-238 or thorium-232. Many It is able to pass through several centimeters of these minerals may become deposited in of lead and still be detected on the other side. both bone and wood fossils. If you are not Thick lead is needed to protect against gamma able to identify the minerals yourself based on radiation. available references try to contact the geology department at the local university and see if a member of the faculty can aid with the identi- fication.
    [Show full text]
  • Geological Mapping and Mineralization on the Northern Half of the Desmont Claim Monmouth Township, Ontario
    We are committed to providing accessible customer service. If you need accessible formats or communications supports, please contact us. Nous tenons à améliorer l’accessibilité des services à la clientèle. Si vous avez besoin de formats accessibles ou d’aide à la communication, veuillez nous contacter. 1 Geological Mapping and Mineralization on the northern half of the Desmont Claim Monmouth Township, Ontario Cell claims; 167120, 281885, 118830, 180531 and 215872. By Bradley S Wilson Kingston, Ontario For Municipality of Highlands East P.O. Box 295 2249 Loop Road Wilberforce, Ontario, K0L 3C0 March 31, 2020 Page 1 Geological Mapping and Mineralization on the northern half of the Desmont Claim Monmouth Township, Ontario Cell claims; 167120, 281885, 118830, 180531 and 215872. By Bradley S Wilson For Municipality of Highlands East March 31, 2020 Introduction For decades, recreational mineral collectors from around the world have been coming to south eastern Ontario to pursue their fascinating hobby by searching out mineral samples from the many available collecting sites for which the region is famous. For this reason, many consider the region, often referred to in general as the Bancroft area, the “Mineral Capital of Canada”. A wide variety of minerals are known from hundreds of different occurrences throughout the region. Sadly, over the years, many of these localities have been closed to mineral collectors due in part to park and cottage development and a host of other land access issues. It has been suggested that fewer mineral collectors are coming to the region now than in the past. If this is true it may be, in part, because there are fewer collecting sites available to the collector.
    [Show full text]
  • Thorium Occurrences in the Czech Republic and Their Mineralogy
    Uranium Deposits, B. Kribek & J. Zeman (eds) © Czech Geological Survey, Prague, ISBN 80-7075-583-0 Thorium Occurrences in the Czech Republic and their Mineralogy V. Goliáš Institute of Geochemistry, Mineralogy and Mineral Resources, Charles University, Prague, Czech Republic ABSTRACT: Short description and characteristics of several types of thorium mineralization in the Bohemian Massif are given: orthogneisses with 200 ppm of Th (Moldanubicum), Permian volcanites in the Intra-Sudetic basin (U-Th-V to 450 ppm Th), REE-Th pegmatites (Moldanubicum), metasomatic (the Sudety Mts.) and Ordovician Ti-Zr-Th-REE paleo-placers (Saxothuringicum), recent Ti-Zr-Th-REE-Nb placers (Lužnice, S. Bohemia), vein type – Moldanubicum (Th-U). At the Budišov location (vein type in melanosyenites), resources of 87 tons Th have been calculated in the Estimated Additional II category. Figure 1. Thorium radiometric anomalies in the Czech Republic. Selected from databaze of Krištiak & Záliš (1994). 1 INTRODUCTION The field gamma spectrometry were carried out at chosen localities. On the basis of the results Thorium has not been mined in the Czech Republic obtained, samples with increased Th content were to date and thorium deposits have not been taken (ore samples). The selected ore samples were systematically explored or studied. This paper subjected to silicate analysis, quantitative X-ray briefly describes main types of thorium powder diffraction and analysis of micro-elements mineralization of the Bohemian Massif. Their by the ICP-MS and AAS methods; laboratory geochemical and mineralogical characteristics are gamma spectrometry was employed to analyze the given and their economic potential is discussed. content of radioactive elements.
    [Show full text]
  • X-Ray Diffraction Data on Some Radio- Active Oxide Minerals*
    X-RAY DIFFRACTION DATA ON SOME RADIO- ACTIVE OXIDE MINERALS* Rowerr J. Anworr A mer ic an Cy anamid C om p any, St amJ or d, Conne clicut AssrnAcr X-ray powder photographs and specific gravity determinations of specimens belonging to the uraninite-thorianite series and the pyrochlore-microlite series gave, for the former, o:5.403-5.575A (19 specimens),G:6.43-9.55 (9),and for pyrochlore-microlile, o:10.296- l0.Ml A (5). Indexed powder data are given for uraninite and for ignited microlite. The powder pattern of orthorhombic euxenite (ignitedat 1000"C), interpretedwith the aid of establishedmorphological descriptions,gave for this mineral,o:5.520,b:14.57,c:5.166A,, most probable space-groupPcmn, Z:4, G (meas.):5.23, p (calc for Y:Er:2:1):5.58. An indexed powder pattern is given. Two specimens of .'tanteuxenite" gave pattems of the uraninite type with o-5.10 A thus casting doubt on their identity with euxenite. Radioactive minerals are currently of general interest because they frequently contain uranium and related elements, but they hold a specialinterest mineralogically becausethey include most of the minerals classedas((metamict." The possessionof this characteristicis probably the main reason why certain of these minerals have not previously been studied by o-ray diffraction methods. The author of this paper becamein- terested in radioactive minerals during the summer of 1948while working in the radioactive laboratory of the Mineralogical Section of the Geo- logical Survey of Canada, at Ottawa. Dr. H. V. Ellsworth, mineralogist in charge of that laboratory, kindly donated a representative collection of these minerals, mostly from Canadian localities, many of which he had analyzed chemically (Ellsworth, 1932).
    [Show full text]
  • Thorium Data Sheet
    170 THORIUM [Data in kilograms gross weight unless otherwise noted] Domestic Production and Use: The world’s primary source of thorium is the rare-earth and thorium phosphate mineral monazite. In 2019, monazite may have been produced as a separated concentrate or included as an accessory mineral in heavy-mineral concentrates. Essentially, all thorium compounds and alloys consumed by the domestic industry were derived from imports. The number of companies that processed or fabricated various forms of thorium for commercial use was not available. Thorium’s use in most products was generally limited because of concerns over its naturally occurring radioactivity. Imports of thorium compounds are sporadic owing to changes in consumption and fluctuations in consumer inventory levels. The estimated value of thorium compounds imported for consumption by the domestic industry in 2019 was about $533,000, compared with $567,000 in 2018. Salient Statistics—United States: 2015 2016 2017 2018 2019e Production, mine1 — NA NA e, 2500,000 21,200,000 Imports for consumption: Thorium ore and concentrates (monazite) — 16,000 — 1,000 1,000 Thorium compounds (oxide, nitrate, etc.) 2,740 3,120 8,510 9,000 8,300 Exports: Thorium ore and concentrates (monazite) — NA NA 520,000 1,200,000 Thorium compounds (oxide, nitrate, etc.) 32,700 36,000 36,100 33,000 33,200 Consumption, apparent:4 Thorium ore and concentrates (monazite) — 16,000 — (5) 1,000 Thorium compounds (oxide, nitrate, etc.) 40 (5) 2,410 6,000 5,100 Value, thorium compounds, gross weight, dollars per kilogram, India6 63 65 73 72 72 Net import reliance7 as a percentage of apparent consumption NA NA NA NA NA Recycling: None.
    [Show full text]