TITANIUM by Joseph Gambogi
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.. & METEORITIC RUTILE Peter R. Buseck Departments of Geology and Chemistry Arizona State University Tempe, Arizona Klaus Keil Space Sciences Division National Aeronautics and Space Administration Ames Research Center Mof fett Field, California r ABSTRACT Rutile has not been widely recognized as a meteoritic constituent. show, Recent microscopic and electron microprobe studies however, that Ti02 . is a reasonably widespread phase, albeit in minor amounts. X-ray diffraction studies confirm the Ti02 to be rutile. It was observed in the following meteorites - Allegan, Bondoc, Estherville, Farmington, and Vaca Muerta, The rutile is associated primarily with ilmenite and chromite, in some cases as exsolution lamellae. Accepted for publication by American Mineralogist . Rutile, as a meteoritic phase, is not widely known. In their sunanary . of meteorite mineralogy neither Mason (1962) nor Ramdohr (1963) report rutile as a mineral occurring in meteorites, although Ramdohr did describe a similar phase from the Faxmington meteorite in his list of "unidentified minerals," He suggested (correctly) that his "mineral D" dght be rutile. He also ob- served it in several mesosiderites. The mineral was recently mentioned to occur in Vaca Huerta (Fleischer, et al., 1965) and in Odessa (El Goresy, 1965). We have found rutile in the meteorites Allegan, Bondoc, Estherville, Farming- ton, and Vaca Muerta; although nowhere an abundant phase, it appears to be rather widespread. Of the several meteorites in which it was observed, rutile is the most abundant in the Farmington L-group chondrite. There it occurs in fine lamellae in ilmenite. The ilmenite is only sparsely distributed within the . meteorite although wherever it does occur it is in moderately large clusters - up to 0.5 mn in diameter - and it then is usually associated with chromite as well as rutile (Buseck, et al., 1965), Optically, the rutile has a faintly bluish tinge when viewed in reflected, plane-polarized light with immersion objectives. -
Washington State Minerals Checklist
Division of Geology and Earth Resources MS 47007; Olympia, WA 98504-7007 Washington State 360-902-1450; 360-902-1785 fax E-mail: [email protected] Website: http://www.dnr.wa.gov/geology Minerals Checklist Note: Mineral names in parentheses are the preferred species names. Compiled by Raymond Lasmanis o Acanthite o Arsenopalladinite o Bustamite o Clinohumite o Enstatite o Harmotome o Actinolite o Arsenopyrite o Bytownite o Clinoptilolite o Epidesmine (Stilbite) o Hastingsite o Adularia o Arsenosulvanite (Plagioclase) o Clinozoisite o Epidote o Hausmannite (Orthoclase) o Arsenpolybasite o Cairngorm (Quartz) o Cobaltite o Epistilbite o Hedenbergite o Aegirine o Astrophyllite o Calamine o Cochromite o Epsomite o Hedleyite o Aenigmatite o Atacamite (Hemimorphite) o Coffinite o Erionite o Hematite o Aeschynite o Atokite o Calaverite o Columbite o Erythrite o Hemimorphite o Agardite-Y o Augite o Calciohilairite (Ferrocolumbite) o Euchroite o Hercynite o Agate (Quartz) o Aurostibite o Calcite, see also o Conichalcite o Euxenite o Hessite o Aguilarite o Austinite Manganocalcite o Connellite o Euxenite-Y o Heulandite o Aktashite o Onyx o Copiapite o o Autunite o Fairchildite Hexahydrite o Alabandite o Caledonite o Copper o o Awaruite o Famatinite Hibschite o Albite o Cancrinite o Copper-zinc o o Axinite group o Fayalite Hillebrandite o Algodonite o Carnelian (Quartz) o Coquandite o o Azurite o Feldspar group Hisingerite o Allanite o Cassiterite o Cordierite o o Barite o Ferberite Hongshiite o Allanite-Ce o Catapleiite o Corrensite o o Bastnäsite -
Developments in Uranium Resources, Production, Demand and the Environment
IAEA-TECDOC-1425 Developments in uranium resources, production, demand and the environment Proceedings of a technical committee meeting held in Vienna, 15–18 June 1999 January 2005 IAEA-TECDOC-1425 Developments in uranium resources, production, demand and the environment Proceedings of a technical committee meeting held in Vienna, 15–18 June 1999 January 2005 The originating Section of this publication in the IAEA was: Nuclear Fuel Cycle and Materials Section International Atomic Energy Agency Wagramer Strasse 5 P.O. Box 100 A-1400 Vienna, Austria DEVELOPMENTS IN URANIUM RESOURCES, PRODUCTION, DEMAND AND THE ENVIRONMENT IAEA, VIENNA, 2004 IAEA-TECDOC-1425 ISBN 92–0–112904–1 ISSN 1011–4289 © IAEA, 2005 Printed by the IAEA in Austria January 2005 FOREWORD Globalization has led to the growing importance of the uranium production industries of the world’s developing countries. Though trade restrictions continue to impede completely free access to the worldwide uranium market, the uranium resources and production capabilities of the developing countries are becoming increasingly important in assuring the adequacy of uranium supplies to meet projected worldwide demand. Therefore, papers presented at this meeting provide an important overview of uranium production operations in developing countries as well as offering insight into future production plans and potential. Along with their increasing contribution to worldwide uranium supply, the environmental impact of uranium production in developing countries has come under increasing scrutiny -
Mineral to Metal: Processing of Titaniferous Ore to Synthetic Rutile (Tio2) and Ti Metal
Mineral to Metal: Processing of Titaniferous Ore to Synthetic Rutile (TiO2) and Ti metal Dr Jeya Ephraim, Mineral to Metal May 11 – 13, 2015 * Hilton Birmingham Metropole Hotel * Birmingham, United Kingdom Objective To produce ultra pure high grade synthetic rutile (TiO2) from ilmenite ore and Ti metal from anatase or rutile Dr Jeya Ephraim, Mineral to Metal May 11 – 13, 2015 * Hilton Birmingham Metropole Hotel * Birmingham, United Kingdom Outline 1. Introduction 2. Why titaniferous minerals? 3. Processing Methods for synthetic rutile (TiO2) (i) Alkali Roasting (ii) Reduction followed by leaching 5. Results and discussion 6. Commercialisation 7. Conclusion 8. Bradford Metallurgy on Ti metal powder production 9. Future Plans Dr Jeya Ephraim, Mineral to Metal May 11 – 13, 2015 * Hilton Birmingham Metropole Hotel * Birmingham, United Kingdom Introduction • Titanium always exist as bonded to other elements in nature. • It is the ninth-most abundant element in the Earth. • It is widely distributed and occurs primarily in the minerals such as anatase, brookite, ilmenite, perovskite, rutile and titanite (sphene). • Among these minerals, only rutile and ilmenite have economic importance Dr Jeya Ephraim, Mineral to Metal May 11 – 13, 2015 * Hilton Birmingham Metropole Hotel * Birmingham, United Kingdom Ilmenite deposit in Chavara, Kerala, India Dr Jeya Ephraim, Mineral to Metal May 11 – 13, 2015 * Hilton Birmingham Metropole Hotel * Birmingham, United Kingdom Applications of TiO2 • White powder pigment - brightness and very high refractive index - Sunscreens use TiO2 - high refractive index - protect the skin from UV light. • TiO2 – photocatalysts - electrolytic splitting of water into hydrogen and oxygen, - produce electricity in nanoparticle form -light-emitting diodes, etc. -
Uranium and Thorium Resources in India: UNFC System
Uranium and thorium resources in India: UNFC system P.S.Parihar Atomic Minerals Directorate for Exploration and Research Department of Atomic Energy Government of India 1 21/08/2013 Government of India’s Policy on Atomic Minerals The federal status of the DAE and the powers invested in it under the Indian Atomic Energy Act (1948 and 1962) as amended from time to time, bestow upon it several rights to facilitate atomic mineral exploration. The more significant ones are- . Exclusive rights to conduct exploration for uranium, thorium and other prescribed minerals such as beryllium, lithium, niobium, tantalum and rare-earth elements all over the country . Exclusive rights to buy prescribed minerals from private mine owners produced incidental to mining of other economic minerals. 30/10/2013 - . Rights to access to surface and sub-surface data on areas under exploration or mining/recovery for oil, coal, minerals and ground water by Government or Public Sector Organisations. The facility includes carrying out of gamma-ray logging of boreholes and checking of mine workings and collection of samples etc. 2 UNFC workshop, New Delhi workshop, UNFC Government of India’s Policy on Atomic Minerals Uranium exploration, production and utilisation are under the control of Central Government. Only public sector companies under Government of India are allowed to explore and mine atomic minerals viz. U, Th, etc. Present system of reporting of uranium reserves in India is as per the IAEA system of uranium resource classification . Indicated – [Reasonable -
Arizona Department of Mines and Mineral Resources
Arizona Department of Mines and Mineral Resources 1502 West Washington, Phoenix, AZ 85007 Phone (602) 255-3795 1-800-446-4259 in Arizona FAX (602) 255-3777 www.admmr.state.az.us Titanium Circular 9, August 1982 by Michael N Greeley, Mining Engineer Titanium is a lightweight metal that is virtually as strong as steel. As our technologies and industries have become increasingly sophisticated, demand for this relatively scarce, but highly desirable metal has increased rapidly. This information circular is written to acquaint the prospector and miner with titanium and its uses. A resume of typical geologic environments and production possibilities in Arizona is given. Uses phisticated needs will vie for a greater share of the The largest market for titanium is in the manufacture world's supply of this unique metal. of pigments. Because of its high refractive index, titanium dioxide pigment imparts whiteness, opacity, Geology and Mineralogy and brightness to paints, varnishes, and lacquers. The most important titanium minerals are anatase Titanium pigment is also used greatly in paper coat (Ti0 ), ilmenite (FeTi0 ), perovskite (CaTi03), ru- 2 3 ings and as paper fillers. Many plastic products such tile (Ti0 ), sphene (CaTiSiOS), and leucoxene. Leu as polyethylene, polyvinyl chloride, and polystyrene 2 coxene, a mineraloid, is an alteration product of il incorporate titanium pigment because of its resis menite, from which a portion of the iron has been tance to degradation by ultraviolet light and its leached. Currently the minerals of commercial inter chemical inertness. est are ilmenite, leucoxene, and rutile. Production historically has come from three types of deposits: Titanium dioxide pigment and other titanium com Beach and stream placers, massive deposits of titani pounds are used in many miscellaneous applications, ferous iron ore, and igneous complexes in which ru including rubber tires, floor and wall coverings, tile occurs in association with anorthosite and simi glass fibers, ceramic capacitors, carbide cutting lar, mafic crystalline rocks. -
Occurrence, Alteration Patterns and Compositional Variation of Perovskite in Kimberlites
975 The Canadian Mineralogist Vol. 38, pp. 975-994 (2000) OCCURRENCE, ALTERATION PATTERNS AND COMPOSITIONAL VARIATION OF PEROVSKITE IN KIMBERLITES ANTON R. CHAKHMOURADIAN§ AND ROGER H. MITCHELL Department of Geology, Lakehead University, 955 Oliver Road, Thunder Bay, Ontario P7B 5E1, Canada ABSTRACT The present work summarizes a detailed investigation of perovskite from a representative collection of kimberlites, including samples from over forty localities worldwide. The most common modes of occurrence of perovskite in archetypal kimberlites are discrete crystals set in a serpentine–calcite mesostasis, and reaction-induced rims on earlier-crystallized oxide minerals (typically ferroan geikielite or magnesian ilmenite). Perovskite precipitates later than macrocrystal spinel (aluminous magnesian chromite), and nearly simultaneously with “reaction” Fe-rich spinel (sensu stricto), and groundmass spinels belonging to the magnesian ulvöspinel – magnetite series. In most cases, perovskite crystallization ceases prior to the resorption of groundmass spinels and formation of the atoll rim. During the final evolutionary stages, perovskite commonly becomes unstable and reacts with a CO2- rich fluid. Alteration of perovskite in kimberlites involves resorption, cation leaching and replacement by late-stage minerals, typically TiO2, ilmenite, titanite and calcite. Replacement reactions are believed to take place at temperatures below 350°C, 2+ P < 2 kbar, and over a wide range of a(Mg ) values. Perovskite from kimberlites approaches the ideal formula CaTiO3, and normally contains less than 7 mol.% of other end-members, primarily lueshite (NaNbO3), loparite (Na0.5Ce0.5TiO3), and CeFeO3. Evolutionary trends exhibited by perovskite from most localities are relatively insignificant and typically involve a decrease in REE and Th contents toward the rim (normal pattern of zonation). -
Info Sheet This Is Followed by Heliborne Gamma-Ray Studies of Ore, As a Prelude to Commercial Mining
Research and Development: In order to multidisciplinary geoscientific skills. AMD will understand the genesis and controls of uranium continue its exploration efforts to fullfil the atomic ATOMIC MINERALS DIRECTORATE FOR mineralisation, basic research in the fields of minerals requirement of country’s nuclear power geology, geophysics, geochemistry and also programme. EXPLORATION AND RESEARCH (AMD) in allied topics such as physics, chemistry and electronics is being carried out. Atomic Minerals Directorate for Exploration spectrometric and geophysical surveys1 to identify Other Activities: and Research (AMD) is one of the oldest units potential targets with abnormal radioelemental *AMD is also entrusted to carry out geological / of Department of Atomic Energy (DAE) and plays concentration. geotechnical studies related to site selection for an important role in the front and back end of nuclear power plants and repositories for the the nuclear fuel cycle. AMD was established as The potential areas delineated by heliborne disposal of radioactive wastes generated from Rare Minerals Survey Unit in 1949, subsequently surveys are taken up for ground reconnaissance these plants. renamed as Raw Materials Division (RMD) and radiometrics2 using portable gamma-ray *AMD provides professional and analytical brought under the Atomic Energy Commission measuring instruments such as Scintillometer, services. on October 3, 1950. RMD was later renamed as Gamma Ray Spectrometer etc., regional/detailed *AMD Studentship Programme has been initiated Atomic Minerals Division in 1958 and rechristened geological, geochemical (rock, soil, radon, water to impart basic field training and to encourage as Atomic Minerals Directorate for Exploration and and stream sediments) and ground-geophysical university students to take up their dissertation Research (AMD) in 1998. -
Phase Relations in the Systems Titania and Titania--Boric Oxide
This dissertation has been 65—9337 microfilmed exactly as received BEARD, William Clarence, 1934- PHASE RELATIONS IN THE SYSTEMS TITANIA AND TITANIA— BORIC OXIDE. The Ohio State University, Ph.D., 1965 M in eralogy University Microfilms, Inc., Ann Arbor, Michigan PHASE RELATIONS IN THE SYSTEMS TITANIA AND TITANIA—BORIC OXIDE DISSERTATION Presented in Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of the Ohio State University by William Clarence Beard, B. S. The Ohio State University 1965 Approved by n Adviser Department of Mineralogy ACKNOWLEDGMENTS The author wishes to thank the people who have contributed to the preparation of this dissertation. First, to his adviser, Dr. Wilfrid Raymond Foster, for advice and suggestion of the problem; and second to other members of the faculty of the Department of Mineralogy, Drs. Henry Edward Wenden, Ernest George Ehlers, and Rodney Tampa Tettenhorst, for discussions of the problem and the reading of this dissertation, the author extends his thanks. Thanks also go to his colleague, William Charles Butterman, for assistance in the construction and main tenance of many pieces of experimental apparatus. Acknowledgment is made for financial support received under contract No. AF 33(616)-6509 (twenty-four months), spon sored by Aeronautical Research Division, Wright-Patterson Air Force Base, Ohio, as well as for a Mershon National Graduate Fellowship awarded (1962-63) by the Mershon Committee on Education in National Security; and a William J. McCaughey Fellowship (1963-64). The author is indebted to his wife, Ursula, for her constant help and encouragement. ii VITA. -
Petyayan-Vara Rare-Earth Carbonatites (Vuoriyarvi Massif, Russia)
geosciences Article Ti-Nb Mineralization of Late Carbonatites and Role of Fluids in Its Formation: Petyayan-Vara Rare-Earth Carbonatites (Vuoriyarvi Massif, Russia) Evgeniy Kozlov 1,* ID , Ekaterina Fomina 1, Mikhail Sidorov 1 and Vladimir Shilovskikh 2 ID 1 Geological Institute, Kola Science Centre, Russian Academy of Sciences, 14, Fersmana Street, 184209 Apatity, Russia; [email protected] (E.F.); [email protected] (M.S.) 2 Resource center for Geo-Environmental Research and Modeling (GEOMODEL), St. Petersburg State University, 1, Ulyanovskaya Street, 198504 Saint Petersburg, Russia; [email protected] * Correspondence: [email protected]; Tel.: +7-953-758-7632 Received: 6 July 2018; Accepted: 25 July 2018; Published: 28 July 2018 Abstract: This article is devoted to the geology of titanium-rich varieties of the Petyayan-Vara rare-earth dolomitic carbonatites in Vuoriyarvi, Northwest Russia. Analogues of these varieties are present in many carbonatite complexes. The aim of this study was to investigate the behavior of high field strength elements during the late stages of carbonatite formation. We conducted a multilateral study of titanium- and niobium-bearing minerals, including a petrographic study, Raman spectroscopy, microprobe determination of chemical composition, and electron backscatter diffraction. Three TiO2-polymorphs (anatase, brookite and rutile) and three pyrochlore group members (hydroxycalcio-, fluorcalcio-, and kenoplumbopyrochlore) were found to coexist in the studied rocks. The formation of these minerals occurred in several stages. First, Nb-poor Ti-oxides were formed in the fluid-permeable zones. The overprinting of this assemblage by residual fluids led to the generation of Nb-rich brookite (the main niobium concentrator in the Petyayan-Vara) and minerals of the pyrochlore group. -
Metal Oxide Compact Electron Transport Layer Modification For
materials Review Metal Oxide Compact Electron Transport Layer Modification for Efficient and Stable Perovskite Solar Cells Md. Shahiduzzaman 1,* , Shoko Fukaya 2, Ersan Y. Muslih 3, Liangle Wang 2 , Masahiro Nakano 3, Md. Akhtaruzzaman 4, Makoto Karakawa 1,2,3, Kohshin Takahashi 3, Jean-Michel Nunzi 1,5 and Tetsuya Taima 1,2,3,* 1 Nanomaterials Research Institute, Kanazawa University, Kakuma, Kanazawa 920-1192, Japan; karakawa@staff.kanazawa-u.ac.jp (M.K.); [email protected] (J.-M.N.) 2 Graduate School of Frontier Science Initiative, Kanazawa University, Kakuma, Kanazawa 920-1192, Japan; [email protected] (S.F.); [email protected] (L.W.) 3 Graduate School of Natural Science and Technology, Kanazawa University, Kakuma, Kanazawa 920-1192, Japan; [email protected] (E.Y.M.); [email protected] (M.N.); [email protected] (K.T.) 4 Solar Energy Research Institute, The National University of Malaysia, Bangi 43600, Malaysia; [email protected] 5 Department of Physics, Engineering Physics and Astronomy, Queens University, Kingston, ON K7L-3N6, Canada * Correspondence: [email protected] (M.S.); [email protected] (T.T.); Tel.: +81-76-234-4937 (M.S.) Received: 14 April 2020; Accepted: 9 May 2020; Published: 11 May 2020 Abstract: Perovskite solar cells (PSCs) have appeared as a promising design for next-generation thin-film photovoltaics because of their cost-efficient fabrication processes and excellent optoelectronic properties. However, PSCs containing a metal oxide compact layer (CL) suffer from poor long-term stability and performance. The quality of the underlying substrate strongly influences the growth of the perovskite layer. -
Band Gaps of Brookite, Rutile and Anatase
Optical Analysis of Titania: Band Gaps of Brookite, Rutile and Anatase Ryan Lance Advisor: Dr. Janet Tate A thesis presented in the partial fulfillment of the requirements for the degree of Bachelors of Physics Department of Physics Oregon State University May 5, 2018 Contents 1 Introduction 2 2 Optical Phenomena of Thin Films 3 2.1 The Index of Refraction . 3 2.2 Absorption . 4 2.3 The Band Gap . 5 3 Methods 6 3.1 The Grating Spectrometer . 6 3.2 SCOUT for Optical Modeling . 9 4 Results and Discussion 12 4.1 Band Gap Dependence on Thickness . 14 5 Conclusion 15 6 Appendix 16 6.1 Grating spectrometer settings . 16 6.2 Filtering 2nd Order Light . 16 6.3 Band gap of the substrate . 17 7 Using SCOUT 17 7.1 User configurations . 17 7.2 The Layer Stack . 18 7.3 Materials . 18 8 Acknowledgments 18 1 List of Figures 1 Indirect and direct band gaps . 5 2 The grating spectrometer. 7 3 TiO2 Raw Film Spectra . 7 4 Transmission, reflection, and corrected transmission spectra. 8 5 High-energy region of raw spectra . 9 6 Screenshot of the SCOUT interface . 10 7 Refractive index model constructed in SCOUT. 11 8 Density of states in the OJL band gap model. 11 9 High-fraction brookite film on SiO2 ....................... 12 10 High-fraction anatase film on SiO2 ....................... 13 11 High-fraction rutile film on SiO2 ........................ 13 12 Gap energy vs. Thickness for many polyphase TiO2 films. The phase plots (Rutile, Brookite, Anatase) show how much of each phase is present in each film.