Quantitative Data File for Ore Minerals Quantitative Data File for Ore Minerals Third Edition

Total Page:16

File Type:pdf, Size:1020Kb

Quantitative Data File for Ore Minerals Quantitative Data File for Ore Minerals Third Edition QUANTITATIVE DATA FILE FOR ORE MINERALS QUANTITATIVE DATA FILE FOR ORE MINERALS THIRD EDITION Edited by A.J. Criddle and C.J. Stanley Department of Mineralogy Natural History Museum London, UK SPRINGER-SCIENCE+BUSINESS MEDIA, B.V. First edition 1978, second edition 1986 published by The British Museum (Natural History) Third edition 1993 © 1978,1986,1993 Springer Science+Business Media Dordrecht Originally published by Chapman & Hall in 1993 Softcover reprint of the hardcover 3rd edition 1993 — Commission on Ore Mineralogy Typeset by Dave Williams, Sawbridgeworth ISBN 978-94-010-4652-7 ISBN 978-94-011-1486-8 (eBook) DOI 10.1007/978-94-011-1486-8 Apart from any fair dealing for the purposes of research or private study, or criticism or review, as permitted under the UK Copyright Designs and Patents Act, 1988, this publication may not be repro• duced, stored, or transmitted, in any form or by any means, without the prior permission in writing of the publishers, or in the case of reprographic reproduction only in accordance with the terms of the licences issued by the Copyright Licensing Agency in the UK, or in accordance with the terms of licences issued by the appropriate Reproduction Rights Organization outside the UK. Enquiries concerning reproduction outside the terms stated here should be sent to the publishers at the London address printed on this page. The publisher makes no representation, express or implied, with regard to the accuracy of the information contained in this book and cannot accept any legal responsibility or liability for any errors or omissions that may be made. A catalogue record for this book is available from the British Library Library of Congress Cataloging-in-Publication data available Contents Preface to third edition vii Acknowledgments vii Background and introductory notes to QDF3 ix Format of QDF3 ix Name and formula ix Symmetry x Provenance x Chemical composition x X-ray data x Reflectance standards x Monochromator and photomultiplier x Effective Numerical Aperture x Micro-indentation hardness (Vickers) xi Reflectance data xi Symbols for reflectance used in QDF3 xii Symbol or symbols xiii Reflectance data in two-media xvi Reflectance spectra and chemical composition xvii Colour and quantitative colour xvii Scaling of graphs xxii Polishing method xxii Reference and further information xxii Keys for identification xxii Species representation xxii Selected Bibliography xxiii 1. General mineralogical nomenclature xxiii 2. Quantitative and qualitative ore mineralogy xxiii 3. Reflectance-based identification schemes xxiv COM wavelength key 1 xxv Colour value key 2 xxxviii Air and oil data 440-700nm key 3 li Data file 1 PREFACE TO THE THIRD EDITION This third edition (or issue) of the Quantitative Data reviewers, and reported by users of the earlier File for ore minerals (QDF) of the Commission on editions. The result is that 510 species and 125 are Mineralogy of the International Mineralogical compositional or structural variants, or varieties, of Association (COM-IMA) is published, with the species, are represented in QDF3. A large number of support of the Natural History Museum, London, by the entries include data collected from the type Chapman & Hall. It has been greatly revised and specimen of a mineral: these include data extracted enlarged and now includes graphs of the reflectance from the published literature. In this respect, QDF3 spectra for all of its entries. These have been differs from earlier editions. included in response to requests from users of the We have also revised and simplified the notes earlier editions. Also included, for those users concerning X-ray data: no longer are the strongest unfamiliar with the application of such spectra to lines in the powder diffraction pattern quoted, nor mineral identification, are introductory notes, are cell dimensions generally given. Instead, it was illustrated with examples of R spectra. decided to refer to data from the original description, The 635 data sets, which are arranged or to data in the PDF of the JCPDS. Where our data alphabetically by mineral name, one set to a page, differed from those in the PDF, such differences are retain the tabular format (if slightly modified) of noted. In all, confirmatory X-ray data (or references QDF2. The graphs are drawn, depending on the to the original data) were obtained for 89.6% of the dispersion of the reflectance curves, to the most entries in QDF3. appropriate of one of four scales of reflectance (25%, Micro-indentation hardness (VHN) values are 50%,75% and 100%). Colour values computed quoted for 492 of the data sets \17 %), however, as in relative to the Commission Internationale de QDF2, a smaller proportion (46.7% of the total) were I'Eclairage (OE) illuminants A and C are provided for most of the entries (97 .5 %). at the preferred force of 100pond. The three 'keys' to A feature unique to the QDF is that most of its assist in the optical identification of a mineral, optical and compositional data were collected from introduced in QDF2, are retained, though, of course, the same area of a mineral. This follows a policy they are completely revised to incorporate the new decision of the COM which recognises the optical data, and now include simplified chemical interdependence of the two properties: composition formulae (for those users who do not automatically and optics. While every effort was made, when relate a minerals name to its composition). collecting data for the File, to ensure that reliable The production of a laboratory reference work, compositional data were included for all data sets, such as the QDF, is very demanding of time: QDF3 we were unable to replace some of the incomplete was produced using Borland's* relational database sets from QDF2. In all, some 90 % (572) of the data management system, Paradox®, combined with the sets contain related optical and compositional data. graphing facilities of Quattro Pro®. In setting-up the Another unusual feature of the QDF, in all of its database, errors and inconsistencies will, editions, is that a substantial proportion of its entries undoubtedly, have crept into the work. The Editors were previously unpublished, and obtained take responsibility for all such errors and, on behalf specifically for the File. In QDF3, these number 172, of the COM, would be grateful if any that are found many of which are for minerals where previously no are brought to their attention. optical data existed in the published literature. In this sense, the QDF is the only source of characteristic ACKNOWLEDGMENTS quantitative data for many ore minerals, further, it is the only compiled-source of spectral reflectance data In a work of this kind, which relies so heavily on under oil immersion. In the current edition, a international cooperation, it is impossible to thank concerted effort was made to supply data for all of everybody who ha~ contributed to its successful the known tellurides, for as many of the oxides as appearance. We thank all of the contributors of data was practicable (60 species more than QDF2), and to sets, reference to whom is made individually, with fill such'gaps' in species coverage as were noted by their data, in the pages of the File. Especial thanks * Paradox and Quattro Pro are registered trade marks of Borland International, Inc. vii go, in this context, to Yves Moelo (BRGM) for enabled us to confirm the identity of many rare compiling the contributions from France. minerals. We are particularly grateful to our many friends, We thank Myra Givans of NHM Publications around the world, who spent their time so selflessly and Ruth Cripwell of Chapman & Hall for their in locating mineral samples in their collections, and gentle encouragement during the gestation of this who either lent, or donated them for investigation: volume. And, for his patience, professionalism and from Austria, Werner Paar (Salzburg); from Belgium, scrupulous attention to detail, we are indebted to Jacques Jedwab (Brussels); from Canada, Gary Dave Williams, who was involved, from the outset, Ansell, Louis Cabri, Don Harris, DeAlton Owens, in constructing the QDF database and who was Andy Roberts (Ottawa); Steve Kissin (Thunder Bay); responsible for turning our computer output into Bob Gait and Joe Mandarino (Toronto); from 'camera-ready' form. Germany, Gunter Grlintmann (Munich); from Finally, we thank Fifi and Hari for their piscine Switzerland, Stefan Graeser (Basel); from the UK, therapy. David Vaughan (Manchester); and from the USA, Pete Dunn (Washington) and Ben Leonard (Denver). The COM owes a particular debt of gratitude to Alan Criddle and Chris Stanley John Francis and Steve Somogyi of the NHM, whose Department of Mineralogy unstinting efforts to obtain satisfactory X-ray data, The Natural History Museum from the often puny samples we were able to extract, London, U.K. viii BACKGROUND AND INTRODUCTORY NOTES TO QDF3 Since the publication, in 1986, of QDF2, several very Williams from the Museum's employ, he continued useful works have been produced in the field of ore as consultant to the editors for this task). The volume mineralogy and ore microscopy: Gerlitz et al. (1989) you are now reading is the product of this made available a computer-based identification collaboration. system for ore minerals (using QDF2 as its source)i Early in the planning of QDF3 (and before all of more traditionally, Tarkian & LieBmann (1991) the production details described above), it was published their guide to the identification of ore worked out what was required to provide a minerals, and Ixer (1990), his atlas of ore textures. substantially improved edition of the File. The importance of colour (and its causes) were dealt Experience in the production of the 2nd edition had with brilliantly and didactically by Andrew Peckett shown that, in the main, authors were reluctant to (1992), and the COM, itself, in collaboration with the supply data in the format required by us - even Mineralogical Association of Canada, produced a when prompted by their COM National volume of 'Short Course Notes' on 'Advanced Representatives.
Recommended publications
  • Iseite, Mn2mo3o8, a New Mineral from Ise, Mie Prefecture, Japan
    Journal of Mineralogical and PetrologicalIseite, a new Sciences, mineral Volume 108, page 37─ 41, 2013 37 LETTER Iseite, Mn2Mo3O8, a new mineral from Ise, Mie Prefecture, Japan * ** ** *** Daisuke NISHIO-HAMANE , Norimitsu TOMITA , Tetsuo MINAKAWA and Sachio INABA * The institute for Solid State Physics, University of Tokyo, Kashiwa, Chiba 277-8581, Japan ** Department of Earth Science, Faculty of Science, Ehime University, Matsuyama, Ehime 790-8577, Japan *** Inaba-Shinju Corporation, Minamiise, Mie 516-0109, Japan Iseite, Mn2Mo3O8, a new mineral that is a Mn-dominant analogue of kamiokite, is found in the stratiform ferro- manganese deposit, Shobu area, Ise City, Mie Prefecture, Japan. It is the first mineral species that includes both Mn and Mo as essential constituents. Iseite is iron-black in color and has a submetallic luster. It occurs as ag- gregates up to about 1 mm in size made of minute crystals (<20 μm). Iseite has a zoned structure closely associ- ated with undetermined Mn-Fe-Mo oxide minerals with hexagonal forms, and it occasionally coexists with 3 small amounts of powellite. Its Mohs hardness is 4-5, and its calculated density is 5.85 g/cm . The empirical formula of iseite is (Mn1.787Fe0.193)Σ1.980Mo3.010O8. Its simplified ideal formula is written as Mn2Mo3O8. The min- eral is isostructural with kamiokite (hexagonal, P63mc). The unit cell parameters are a = 5.8052 (3) Å, c = 10.2277 (8) Å, V = 298.50 (4) Å3, and Z = 2. The Rietveld refinement using synchrotron radiation (λ = 0.413 Å) powder XRD data converges to Rwp = 3.11%, and confirms two independent Mn sites—tetrahedral and octahe- IV VI dral—in the crystal structure of iseite, indicating the structure formula Mn Mn Mo3O8.
    [Show full text]
  • Xrd and Tem Studies on Nanophase Manganese
    Clays and Clay Minerals, Vol. 64, No. 5, 488–501, 2016. 1 1 2 2 3 XRD AND TEM STUDIES ON NANOPHASE MANGANESE OXIDES IN 3 4 FRESHWATER FERROMANGANESE NODULES FROM GREEN BAY, 4 5 5 6 LAKE MICHIGAN 6 7 7 8 8 S EUNGYEOL L EE AND H UIFANG X U* 9 9 NASA Astrobiology Institute, Department of Geoscience, University of Wisconsin Madison, Madison, 10 À 10 1215 West Dayton Street, A352 Weeks Hall, Wisconsin 53706 11 11 12 12 13 Abstract—Freshwater ferromanganese nodules (FFN) from Green Bay, Lake Michigan have been 13 14 investigated by X-ray powder diffraction (XRD), micro X-ray fluorescence (XRF), scanning electron 14 microscopy (SEM), high-resolution transmission electron microscopy (HRTEM), and scanning 15 transmission electron microscopy (STEM). The samples can be divided into three types: Mn-rich 15 16 nodules, Fe-Mn nodules, and Fe-rich nodules. The manganese-bearing phases are todorokite, birnessite, 16 17 and buserite. The iron-bearing phases are feroxyhyte, goethite, 2-line ferrihydrite, and proto-goethite 17 18 (intermediate phase between feroxyhyte and goethite). The XRD patterns from a nodule cross section 18 19 suggest the transformation of birnessite to todorokite. The TEM-EDS spectra show that todorokite is 19 associated with Ba, Co, Ni, and Zn; birnessite is associated with Ca and Na; and buserite is associated with 20 2+ +2 3+ 20 Ca. The todorokite has an average chemical formula of Ba0.28(Zn0.14Co0.05 21 2+ 4+ 3+ 3+ 3+ 2+ 21 Ni0.02)(Mn4.99Mn0.82Fe0.12Co0.05Ni0.02)O12·nH2O.
    [Show full text]
  • Redalyc.Mineralogical Study of the La Hueca Cretaceous Iron-Manganese
    Revista Mexicana de Ciencias Geológicas ISSN: 1026-8774 [email protected] Universidad Nacional Autónoma de México México Corona Esquivel, Rodolfo; Ortega Gutiérrez, Fernando; Reyes Salas, Margarita; Lozano Santacruz, Rufino; Miranda Gasca, Miguel Angel Mineralogical study of the La Hueca Cretaceous Iron-Manganese deposit, Michoacán, south-western Mexico Revista Mexicana de Ciencias Geológicas, vol. 17, núm. 2, 2000, pp. 142-151 Universidad Nacional Autónoma de México Querétaro, México Available in: http://www.redalyc.org/articulo.oa?id=57217206 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative Revista Mexicana de Ciencias Geológicas, volumen 17, número 2, 143 2000, p. 143- 153 Universidad Nacional Autónoma de México, Instituto de Geología, México, D.F MINERALOGICAL STUDY OF THE LA HUECA CRETACEOUS IRON- MANGANESE DEPOSIT, MICHOACÁN, SOUTHWESTERN MEXICO Rodolfo Corona-Esquivel1, Fernando Ortega-Gutiérrez1, Margarita Reyes-Salas1, Rufino Lozano-Santacruz1, and Miguel Angel Miranda-Gasca2 ABSTRACT In this work we describe for the first time the mineralogy and very briefly the possible origin of a banded Fe-Mn deposit associated with a Cretaceous volcanosedimentary sequence of the southern Guerrero terrane, near the sulfide massive volcanogenic deposit of La Minita. The deposit is confined within a felsic tuff unit; about 10 meters thick where sampled for chemical analysis. Using XRF, EDS and XRD techniques, we found besides todorokite, cryptomelane, quartz, romanechite (psilomelane), birnessite, illite-muscovite, cristobalite, chlorite, barite, halloysite, woodruffite, nacrite or kaolinite, and possibly hollandite-ferrian, as well as an amorphous material and two unknown manganese phases.
    [Show full text]
  • Metamorphism of Sedimentary Manganese Deposits
    Acta Mineralogica-Petrographica, Szeged, XX/2, 325—336, 1972. METAMORPHISM OF SEDIMENTARY MANGANESE DEPOSITS SUPRIYA ROY ABSTRACT: Metamorphosed sedimentary deposits of manganese occur extensively in India, Brazil, U. S. A., Australia, New Zealand, U. S. S. R., West and South West Africa, Madagascar and Japan. Different mineral-assemblages have been recorded from these deposits which may be classi- fied into oxide, carbonate, silicate and silicate-carbonate formations. The oxide formations are represented by lower oxides (braunite, bixbyite, hollandite, hausmannite, jacobsite, vredenburgite •etc.), the carbonate formations by rhodochrosite, kutnahorite, manganoan calcite etc., the silicate formations by spessartite, rhodonite, manganiferous amphiboles and pyroxenes, manganophyllite, piedmontite etc. and the silicate-carbonate formations by rhodochrosite, rhodonite, tephroite, spessartite etc. Pétrographie and phase-equilibia data indicate that the original bulk composition in the sediments, the reactions during metamorphism (contact and regional and the variations and effect of 02, C02, etc. with rise of temperature, control the mineralogy of the metamorphosed manga- nese formations. The general trend of formation and transformation of mineral phases in oxide, carbonate, silicate and silicate-carbonate formations during regional and contact metamorphism has, thus, been established. Sedimentary manganese formations, later modified by regional or contact metamorphism, have been reported from different parts of the world. The most important among such deposits occur in India, Brazil, U.S.A., U.S.S.R., Ghana, South and South West Africa, Madagascar, Australia, New Zealand, Great Britain, Japan etc. An attempt will be made to summarize the pertinent data on these metamorphosed sedimentary formations so as to establish the role of original bulk composition of the sediments, transformation and reaction of phases at ele- vated temperature and varying oxygen and carbon dioxide fugacities in determin- ing the mineral assemblages in these deposits.
    [Show full text]
  • LOW TEMPERATURE HYDROTHERMAL COPPER, NICKEL, and COBALT ARSENIDE and SULFIDE ORE FORMATION Nicholas Allin
    Montana Tech Library Digital Commons @ Montana Tech Graduate Theses & Non-Theses Student Scholarship Spring 2019 EXPERIMENTAL INVESTIGATION OF THE THERMOCHEMICAL REDUCTION OF ARSENITE AND SULFATE: LOW TEMPERATURE HYDROTHERMAL COPPER, NICKEL, AND COBALT ARSENIDE AND SULFIDE ORE FORMATION Nicholas Allin Follow this and additional works at: https://digitalcommons.mtech.edu/grad_rsch Part of the Geotechnical Engineering Commons EXPERIMENTAL INVESTIGATION OF THE THERMOCHEMICAL REDUCTION OF ARSENITE AND SULFATE: LOW TEMPERATURE HYDROTHERMAL COPPER, NICKEL, AND COBALT ARSENIDE AND SULFIDE ORE FORMATION by Nicholas C. Allin A thesis submitted in partial fulfillment of the requirements for the degree of Masters in Geoscience: Geology Option Montana Technological University 2019 ii Abstract Experiments were conducted to determine the relative rates of reduction of aqueous sulfate and aqueous arsenite (As(OH)3,aq) using foils of copper, nickel, or cobalt as the reductant, at temperatures of 150ºC to 300ºC. At the highest temperature of 300°C, very limited sulfate reduction was observed with cobalt foil, but sulfate was reduced to sulfide by copper foil (precipitation of Cu2S (chalcocite)) and partly reduced by nickel foil (precipitation of NiS2 (vaesite) + NiSO4·xH2O). In the 300ºC arsenite reduction experiments, Cu3As (domeykite), Ni5As2, or CoAs (langisite) formed. In experiments where both sulfate and arsenite were present, some produced minerals were sulfarsenides, which contained both sulfide and arsenide, i.e. cobaltite (CoAsS). These experiments also produced large (~10 µm along longest axis) euhedral crystals of metal-sulfide that were either imbedded or grown upon a matrix of fine-grained metal-arsenides, or, in the case of cobalt, metal-sulfarsenide. Some experimental results did not show clear mineral formation, but instead demonstrated metal-arsenic alloying at the foil edges.
    [Show full text]
  • Jacobsite from the Tamworth District of New South Wales
    538 Jacobsite from the Tamworth district of New South Wales. By F .L. STILLWELL, D.Sc., and A. B. EDWAP~DS,D.Sc., Ph.D., D.I.C. Commonwealth Scientific and Industrial Organization, Melbourne. [Taken as read November 2, 1950.] WO new occurrences of the rare manganese mineral jacobsite T (MnF%0~) have come to light in the course of mineragraphic studies carried out as part of the research programme of the Mineragraphic Section of the Commonwealth Scientific and Industrial Research Organization. The jacobsite occurs as a constituent of small bodies of high-grade manganese ore at Weabonga, near Danglemah, and at the Mount Sally mine, about 6 miles west of Danglemah, both in the Tam- worth district of New South Wales. The deposits occur in altered sediments, within a mile or two of a granite contact. 1 They are irregular lenticular veins ranging from a few inches to several feet in thickness, between altered slate walls. The veins do not exceed a length of 200-300 feet. The lode material consists of manganese oxides, chiefly psilomelane and pyrolusite, associated with quartz, rhodonite, and iron oxide. The manganese oxides are mainly supergene, and although the deposits are of high grade near the surface, it is doubtful whether they can be worked below the depths of 50- 60 feet, owing to the increase in the amount of rhodonite and quartz relative to manganese oxides at this depth. In the Weabonga ore the jacobsite occurs as narrow seams and lenticles, about 0.5 cm. across, and 3.0 cm. long enclosed in, and partly replaced by, pyrolusite and psilomelane.
    [Show full text]
  • George Robert Rossman Feb 15, 1995
    George Robert Rossman 20-Jun-2020 Present Position: Professor of Mineralogy Option Representative for Geochemistry Division of Geological and Planetary Sciences California Institute of Technology Pasadena, California 91125-2500 Office Telephone: (626)-395-6471 FAX: (626)-568-0935 E-mail: [email protected] Residence: Pasadena, California Birthdate: August 3, l944, LaCrosse, Wisconsin Education: B.S. (Chemistry and Mathematics), Wisconsin State University, Eau Claire, 1966, Summa cum Laude Ph.D. (Chemistry), California Institute of Technology, Pasadena, 1971 Experience: California Institute of Technology Division of Geological and Planetary Sciences a) 1971 Instructor in Mineralogy b) 1971-1974 Assistant Professor of Mineralogy and Chemistry c) 1974-1977 Assistant Professor of Mineralogy d) 1977-1984 Associate Professor of Mineralogy e) 1984-2008 Professor of Mineralogy f) 2008-2015 Eleanor and John R. McMillan Professor of Mineralogy e) 2015- Professor of Mineralogy Principal Research Interests: a) Spectroscopic studies of minerals. These studies include problems relating to the origin of color phenomena in minerals; site ordering in crystals; pleochroism; metal ions in distorted sites; analytical applications. b) The role of low concentrations of water and hydroxide in nominally anhydrous solids. Analytical methods for OH analysis, mode of incorporation, role of OH in modifying physical and chemical properties, and its relationship to conditions of formation in the natural environment. c) Long term radiation damage effects in minerals from background levels of natural radiation. The effects of high level ionizing radiation on minerals. d) X-ray amorphous minerals. These studies have involved the physical chemical study of bioinorganic hard parts of marine organisms and products of terrestrial surface weathering, and metamict minerals.
    [Show full text]
  • 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
    [Show full text]
  • Speciation of Manganese in a Synthetic Recycling Slag Relevant for Lithium Recycling from Lithium-Ion Batteries
    metals Article Speciation of Manganese in a Synthetic Recycling Slag Relevant for Lithium Recycling from Lithium-Ion Batteries Alena Wittkowski 1, Thomas Schirmer 2, Hao Qiu 3 , Daniel Goldmann 3 and Ursula E. A. Fittschen 1,* 1 Institute of Inorganic and Analytical Chemistry, Clausthal University of Technology, Arnold-Sommerfeld Str. 4, 38678 Clausthal-Zellerfeld, Germany; [email protected] 2 Department of Mineralogy, Geochemistry, Salt Deposits, Institute of Disposal Research, Clausthal University of Technology, Adolph-Roemer-Str. 2A, 38678 Clausthal-Zellerfeld, Germany; [email protected] 3 Department of Mineral and Waste Processing, Institute of Mineral and Waste Processing, Waste Disposal and Geomechanics, Clausthal University of Technology, Walther-Nernst-Str. 9, 38678 Clausthal-Zellerfeld, Germany; [email protected] (H.Q.); [email protected] (D.G.) * Correspondence: ursula.fi[email protected]; Tel.: +49-5323-722205 Abstract: Lithium aluminum oxide has previously been identified to be a suitable compound to recover lithium (Li) from Li-ion battery recycling slags. Its formation is hampered in the presence of high concentrations of manganese (9 wt.% MnO2). In this study, mock-up slags of the system Li2O-CaO-SiO2-Al2O3-MgO-MnOx with up to 17 mol% MnO2-content were prepared. The man- ganese (Mn)-bearing phases were characterized with inductively coupled plasma optical emission spectrometry (ICP-OES), X-ray diffraction (XRD), electron probe microanalysis (EPMA), and X-ray absorption near edge structure analysis (XANES). The XRD results confirm the decrease of LiAlO2 phases from Mn-poor slags (7 mol% MnO2) to Mn-rich slags (17 mol% MnO2).
    [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]
  • List of New Mineral Names: with an Index of Authors
    415 A (fifth) list of new mineral names: with an index of authors. 1 By L. J. S~v.scs~, M.A., F.G.S. Assistant in the ~Iineral Department of the,Brltish Museum. [Communicated June 7, 1910.] Aglaurito. R. Handmann, 1907. Zeita. Min. Geol. Stuttgart, col. i, p. 78. Orthoc]ase-felspar with a fine blue reflection forming a constituent of quartz-porphyry (Aglauritporphyr) from Teplitz, Bohemia. Named from ~,Xavpo~ ---- ~Xa&, bright. Alaito. K. A. ~Yenadkevi~, 1909. BuU. Acad. Sci. Saint-P6tersbourg, ser. 6, col. iii, p. 185 (A~am~s). Hydrate~l vanadic oxide, V205. H~O, forming blood=red, mossy growths with silky lustre. Founi] with turanite (q. v.) in thct neighbourhood of the Alai Mountains, Russian Central Asia. Alamosite. C. Palaehe and H. E. Merwin, 1909. Amer. Journ. Sci., ser. 4, col. xxvii, p. 899; Zeits. Kryst. Min., col. xlvi, p. 518. Lead recta-silicate, PbSiOs, occurring as snow-white, radially fibrous masses. Crystals are monoclinic, though apparently not isom0rphous with wol]astonite. From Alamos, Sonora, Mexico. Prepared artificially by S. Hilpert and P. Weiller, Ber. Deutsch. Chem. Ges., 1909, col. xlii, p. 2969. Aloisiite. L. Colomba, 1908. Rend. B. Accad. Lincei, Roma, set. 5, col. xvii, sere. 2, p. 233. A hydrated sub-silicate of calcium, ferrous iron, magnesium, sodium, and hydrogen, (R pp, R',), SiO,, occurring in an amorphous condition, intimately mixed with oalcinm carbonate, in a palagonite-tuff at Fort Portal, Uganda. Named in honour of H.R.H. Prince Luigi Amedeo of Savoy, Duke of Abruzzi. Aloisius or Aloysius is a Latin form of Luigi or I~ewis.
    [Show full text]
  • Geology and Mineralogy July Trace Elements Investigations Report 5
    Geology and Mineralogy UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY" SELECTED ANNOTATED BIBLIOGRAPHY OF THE URANIUM GEOLOGY OF IGNEOUS AND METAMORPHIC ROCKS IN THE UNITED STATES AND TERRITORIES* Efcr Diane Curtis July Trace Elements Investigations Report 5>3li This preliminary report is distributed without editorial and technical review for conformity with official standards and nomenclature,. It is not for public inspection or quotation. report concerns work done on behalf of the Division of Raw Materials of the U« S, Atomic Energy Commission,, 2 USGS - GEOLOGY AND MINERALOGY Distribution No* of copies Atomic Energy Commission, Washington. ............. 2 Division of Raw Materials, Albuquerque ............ 1 Division of Raw Materials, Austin ............... 1 Division of Raw Materials, Casper ............... 1 Division of Baw Materials, Denver «•.•.«....••.•• 1 Division of Raw Materials, Ishperaing ...«••••*.... 1 Division of Raw Materials, Phoenix. ....*....*.... 1 Division of Raw Materials, Rapid City ............. 1 Division of Raw Materials, Salt Lake City *..»......« 1 Division of Raw Materials, Spokane .............* 1 Division of Raw Materials, Washington *............ 3 Exploration Division, Grand Junction Operations Office .... 1 Grand Junction Operations Office ......<.....««.« 1 Technical Information Service Extension, Oak Ridge. ...... 6 U» S. Geological Survey: Fuels Branch, Washington ................... 1 Geochemistry and Petrology Branch, Washington ....*.... 1 Geophysics Branch, Washington ................
    [Show full text]