Cosmetic Minerals of Ancient Egypt
Total Page:16
File Type:pdf, Size:1020Kb
Load more
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 -
Understanding Fluid–Rock Interactions and Lixiviant/Oxidant Behaviour for the In-Situ Recovery of Metals from Deep Ore Bodies
School of Earth and Planetary Science Department of Applied Geology Understanding Fluid–Rock Interactions and Lixiviant/Oxidant Behaviour for the In-situ Recovery of Metals from Deep Ore Bodies Tania Marcela Hidalgo Rosero This thesis is presented for the degree of Doctor of Philosophy of Curtin University February 2020 1 Declaration __________________________________________________________________________ Declaration To the best of my knowledge and belief, I declare that this work of thesis contains no material published by any other person, except where due acknowledgements have been made. This thesis contains no material which has been accepted for the award of any other degree or diploma in any university. Tania Marcela Hidalgo Rosero Date: 28/01/2020 2 Abstract __________________________________________________________________________ Abstract In-situ recovery (ISR) processing has been recognised as a possible alternative to open- pit mining, especially for low-grade resources. In ISR, the fluid–rock interaction between the target ore and the lixiviant results in valuable- (and gangue-) metal dissolution. This interaction is achieved by the injection and recovery of fluid by means of strategically positioned wells. Although the application of ISR has become more common (ISR remains the preferential processing technique for uranium and has been applied in pilot programs for treating oxide zones in copper deposits), its application to hard-rock refractory and low-grade copper-sulfide deposits is still under development. This research is focused on the possible application of ISR to primary copper sulfides usually found as deep ores. Lixiviant/oxidant selection is an important aspect to consider during planning and operation in the ISR of copper-sulfide ores. -
Alamosite Pbsio3 C 2001 Mineral Data Publishing, Version 1.2 ° Crystal Data: Monoclinic
Alamosite PbSiO3 c 2001 Mineral Data Publishing, version 1.2 ° Crystal Data: Monoclinic. Point Group: 2=m: Crystals ¯brous [010]; as radiating aggregates and balls, to 7.5 cm. k Physical Properties: Cleavage: Perfect on 010 . Hardness = 4.5 D(meas.) = 6.488(3) D(calc.) = [6.30] f g Optical Properties: Transparent to translucent. Color: Colorless to white, cream, or light gray. Luster: Adamantine. Optical Class: Biaxial ({). Orientation: Y = b. Dispersion: r < v; strong, weak inclined. ® = 1.945{1.947 ¯ = 1.955{1.961 ° = 1.959{1.968 2V(meas.) = 65± Cell Data: Space Group: P 2=n: a = 12.247 b = 7.059 c = 11.236 ¯ = 113:12± Z = 12 X-ray Powder Pattern: Tsumeb, Namibia. 3.34 (100), 3.56 (95), 3.53 (75), 2.300 (75), 3.23 (70), 2.987 (70), 3.25 (60) Chemistry: (1) (2) (3) SiO2 21.11 20.01 21.21 Al2O3 0.09 FeO 0.09 0.18 MnO 0.02 PbO 78.13 78.95 78.79 CaO trace 0.09 insol: 0.61 Total 99.94 99.34 100.00 (1) Alamos, Mexico. (2) Tsumeb, Namibia; by electron microprobe. (3) PbSiO3: Occurrence: As a rare secondary mineral in the oxidized zone of lead-bearing base metal deposits. Association: Wulfenite, leadhillite, cerussite (Alamos, Mexico); leadhillite, anglesite, melanotekite, °eischerite, kegelite, hematite (Tsumeb, Namibia); diaboleite, phosgenite, cerussite, wulfenite, willemite (Tiger, Arizona, USA); melanotekite, shattuckite, wickenburgite (Rawhide mine, Arizona, USA). Distribution: From Mexico, in Sonora, at Alamos, and the San Pascual mine, near Zimap¶an, Hidalgo. In the USA, from Arizona, in the Mammoth-St. -
Infrare D Transmission Spectra of Carbonate Minerals
Infrare d Transmission Spectra of Carbonate Mineral s THE NATURAL HISTORY MUSEUM Infrare d Transmission Spectra of Carbonate Mineral s G. C. Jones Department of Mineralogy The Natural History Museum London, UK and B. Jackson Department of Geology Royal Museum of Scotland Edinburgh, UK A collaborative project of The Natural History Museum and National Museums of Scotland E3 SPRINGER-SCIENCE+BUSINESS MEDIA, B.V. Firs t editio n 1 993 © 1993 Springer Science+Business Media Dordrecht Originally published by Chapman & Hall in 1993 Softcover reprint of the hardcover 1st edition 1993 Typese t at the Natura l Histor y Museu m ISBN 978-94-010-4940-5 ISBN 978-94-011-2120-0 (eBook) DOI 10.1007/978-94-011-2120-0 Apar t fro m any fair dealin g for the purpose s of researc h or privat e study , or criticis m or review , as permitte d unde r the UK Copyrigh t Design s and Patent s Act , 1988, thi s publicatio n may not be reproduced , stored , or transmitted , in any for m or by any means , withou t the prio r permissio n in writin g of the publishers , or in the case of reprographi c reproductio n onl y in accordanc e wit h the term s of the licence s issue d by the Copyrigh t Licensin g Agenc y in the UK, or in accordanc e wit h the term s of licence s issue d by the appropriat e Reproductio n Right s Organizatio n outsid e the UK. Enquirie s concernin g reproductio n outsid e the term s state d here shoul d be sent to the publisher s at the Londo n addres s printe d on thi s page. -
Characterization & Modification of Copper and Iron Oxide Nanoparticles for Application As Absorber Material in Silicon Base
Characterization & Modification of Copper and Iron Oxide Nanoparticles for Application as Absorber Material in Silicon based Thin Film Solar Cells Maurice René Nuys Member of the Helmholtz Association Member of the Energie & Umwelt / Energie & Umwelt / Energy & Environment Energy & Environment Band/ Volume 291 Band/ Volume 291 ISBN 978-3-95806-096-8 ISBN 978-3-95806-096-8 Schriften des Forschungszentrums Jülich Reihe Energie & Umwelt / Energy & Environment Band / Volume 291 Forschungszentrum Jülich GmbH Institute of Energy and Climate Research Photovoltaics (IEK-5) Characterization & Modification of Copper and Iron Oxide Nanoparticles for Application as Absorber Material in Silicon based Thin Film Solar Cells Maurice René Nuys Schriften des Forschungszentrums Jülich Reihe Energie & Umwelt / Energy & Environment Band / Volume 291 ISSN 1866-1793 ISBN 978-3-95806-096-8 Bibliographic information published by the Deutsche Nationalbibliothek. The Deutsche Nationalbibliothek lists this publication in the Deutsche Nationalbibliografie; detailed bibliographic data are available in the Internet at http://dnb.d-nb.de. Publisher and Forschungszentrum Jülich GmbH Distributor: Zentralbibliothek 52425 Jülich Tel: +49 2461 61-5368 Fax: +49 2461 61-6103 Email: [email protected] www.fz-juelich.de/zb Cover Design: Grafische Medien, Forschungszentrum Jülich GmbH Printer: Grafische Medien, Forschungszentrum Jülich GmbH Copyright: Forschungszentrum Jülich 2015 Schriften des Forschungszentrums Jülich Reihe Energie & Umwelt / Energy & Environment, Band / Volume 291 D 82 (Diss. RWTH Aachen University, 2015) ISSN 1866-1793 ISBN 978-3-95806-096-8 The complete volume is freely available on the Internet on the Jülicher Open Access Server (JuSER) at www.fz-juelich.de/zb/openaccess. Neither this book nor any part of it may be reproduced or transmitted in any form or by any means, electronic or mechanical, including photocopying, microfilming, and recording, or by any information storage and retrieval system, without permission in writing from the publisher. -
Metals from Ores: an Introduction
CRIMSONpublishers http://www.crimsonpublishers.com Mini Review Aspects Min Miner Sci ISSN 2578-0255 Metals from Ores: An Introduction Fathi Habashi* Department of Mining, Laval University, Canada *Corresponding author: Fathi Habashi, Department of Mining, Metallurgical and Materials Engineering, Laval University, Quebec City, Canada Submission: October 09, 2017; Published: December 11, 2017 Introduction of metallic lustre. Of these about 300 are used industrially in the chemical industry, in building materials, in fertilizers, as fuels, etc., chemical composition, constant physical properties, and a A mineral is a naturally occurring substance having a definite characteristic crystalline form. Ores are a mixture of minerals: they are processed to yield an industrial mineral or treated chemically and are known as the industrial minerals Figure 3. to yield a single or several metals. Ores that are generally processed for only a single metal are those of iron, aluminium, chromium, tin, mercury, manganese, tungsten, and some ores of copper. Gold ores may yield only gold, but silver is a common associate. Nickel ores are always associated with cobalt, while lead and zinc always occur together in ores. All other ores are complex yielding a number of metals. before being treated by chemical methods to recover the metals. Ores undergo a beneficiation process by physical methods and grinding then separation of the individual mineral by physical Figure 2: Metals and metalloids obtained from ores. Beneficiation processes involve liberation of minerals by crushing methods (gravity, magnetic, etc.) or physicochemical methods pyrometallurgical, and electrochemical methods. Metals and (flotation) Figure 1. Chemical methods involve hydrometallurgical, metalloids obtained from ores are shown in Figure 2. -
Minerals Found in Michigan Listed by County
Michigan Minerals Listed by Mineral Name Based on MI DEQ GSD Bulletin 6 “Mineralogy of Michigan” Actinolite, Dickinson, Gogebic, Gratiot, and Anthonyite, Houghton County Marquette counties Anthophyllite, Dickinson, and Marquette counties Aegirinaugite, Marquette County Antigorite, Dickinson, and Marquette counties Aegirine, Marquette County Apatite, Baraga, Dickinson, Houghton, Iron, Albite, Dickinson, Gratiot, Houghton, Keweenaw, Kalkaska, Keweenaw, Marquette, and Monroe and Marquette counties counties Algodonite, Baraga, Houghton, Keweenaw, and Aphrosiderite, Gogebic, Iron, and Marquette Ontonagon counties counties Allanite, Gogebic, Iron, and Marquette counties Apophyllite, Houghton, and Keweenaw counties Almandite, Dickinson, Keweenaw, and Marquette Aragonite, Gogebic, Iron, Jackson, Marquette, and counties Monroe counties Alunite, Iron County Arsenopyrite, Marquette, and Menominee counties Analcite, Houghton, Keweenaw, and Ontonagon counties Atacamite, Houghton, Keweenaw, and Ontonagon counties Anatase, Gratiot, Houghton, Keweenaw, Marquette, and Ontonagon counties Augite, Dickinson, Genesee, Gratiot, Houghton, Iron, Keweenaw, Marquette, and Ontonagon counties Andalusite, Iron, and Marquette counties Awarurite, Marquette County Andesine, Keweenaw County Axinite, Gogebic, and Marquette counties Andradite, Dickinson County Azurite, Dickinson, Keweenaw, Marquette, and Anglesite, Marquette County Ontonagon counties Anhydrite, Bay, Berrien, Gratiot, Houghton, Babingtonite, Keweenaw County Isabella, Kalamazoo, Kent, Keweenaw, Macomb, Manistee, -
New Mineral Names*
American Mineralogist, Volume 71, pages 227-232, 1986 NEW MINERAL NAMES* Pers J. Dulw, Gsoncr Y. CHao, JonN J. FrrzperRrcr, RrcHeno H. LaNcr-nv, MIcHeer- FrerscHnn.aNo JRNBIA. Zncznn Caratiite* sonian Institution. Type material is at the Smithsonian Institu- tion under cataloguenumbers 14981I and 150341.R.H.L. A. M. Clark, E. E. Fejer, and A. G. Couper (1984) Caratiite, a new sulphate-chlorideofcopper and potassium,from the lavas of the 1869 Vesuvius eruption. Mineralogical Magazine, 48, Georgechaoite* 537-539. R. C. Boggsand S. Ghose (1985) GeorgechaoiteNaKZrSi3Or' Caratiite is a sulphate-chloride of potassium and copper with 2HrO, a new mineral speciesfrom Wind Mountain, New Mex- ideal formula K4Cu4Or(SO4).MeCl(where Me : Na and,zorCu); ico. Canadian Mineralogist, 23, I-4. it formed as fine greenacicular crystalsin lava of the 1869 erup- S. Ghose and P. Thakur (1985) The crystal structure of george- tion of Mt. Vesuvius,Naples, Italy. Caratiite is tetragonal,space chaoite NaKZrSi3Or.2HrO. Canadian Mineralogist, 23, 5-10. group14; a : 13.60(2),c : a.98(l) A, Z:2.The strongestlines of the powder partern arc ld A, I, hkll: 9.61(l00Xl l0); Electron microprobe analysis yields SiO, 43.17, 7-xO229.51, 6.80(80X200); 4.296(60X3 I 0); 3.0I 5( 100b)(a 20,32r); 2.747 (7 0) NarO 7.42,IGO I1.28, HrO 8.63,sum 100.010/0,corresponding (4 I t); 2.673(60X5 I 0); 2.478(60)(002); 2. 3 8 8(70Xa 3 l, 50I ); to empirical formula Na, orl(oru(Zro rrTio o,Feo o,)Si, or Oe' 2. -
EB Dacortr, Richf'eld
WHERRYITE, A NEW MINERAL FROM THE MAMMOTH MINE, ARIZONAT Richf'eld, Josern J. Fannv, tI . S. GeologicalSurvey; E. B. Dacortr, [Jtah; lNo S.cMunr.G. Gonnow, The Academy oJ l{atural Sciences oJ PhiladelPhia. Aesrnacl A new mineral from the Mammoth Mine, Arizona, having the formula Pbcos'2Pbsor .Pb(cl, oH)z.cuo is named in honor of Dr. Edgar Theodore wherry. The indices of re- fraction are a:1.942, P:2.01O and 1:2.924, and 2V:50' (calculated)' The specific gravity is 6.45. Wherryite was found in a vug just above the 760-foot level associated with chrysocolla, diabol6ite, and paralaurionite' IurnolucrroN In May of 1943 one of the authors, E. B. Daggett, then mining en- gineer at the Mammoth Mine, discovered a small vug of leadhillite crystals associatedwith cerussite, anglesite, phosgenite, paralaurionite, hydrocerussite, diabol6ite, bol6ite, matlockite' and quartz. Within the cavity was some friable chalcocite with a relict structure of the galena which it has replaced. The massive wall of the vug consisted ol a light-green fine granular mineral enclosing some bluish chrysocolla, and at the cavity some blue diabol6ite and greenishparalaurionite. This green matrix was up to five cm. in thickness and extended to the silicified wall of the vein-an altered qrartz monzonite. The minerals of this remarkable vug, and the crystallography of the leadhillite will be d.escribedin a later paper; some observations on the paragenesiswill be given here in order to describe the occurrenceoi the green matrix which has proven to be a new mineral. The name wherryite is given to this new mineral in honor of Dr' Edgar Theodore wherry, first editor of the American Minerologist, formerly curator of mineralogy at the U. -
Preliminary Model of Porphyry Copper Deposits
Preliminary Model of Porphyry Copper Deposits Open-File Report 2008–1321 U.S. Department of the Interior U.S. Geological Survey Preliminary Model of Porphyry Copper Deposits By Byron R. Berger, Robert A. Ayuso, Jeffrey C. Wynn, and Robert R. Seal Open-File Report 2008–1321 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior DIRK KEMPTHORNE, Secretary U.S. Geological Survey Mark D. Myers, Director U.S. Geological Survey, Reston, Virginia: 2008 For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1-888-ASK-USGS For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted materials contained within this report. Suggested citation: Berger, B.R., Ayuso, R.A., Wynn, J.C., and Seal, R.R., 2008, Preliminary model of porphyry copper deposits: U.S. Geological Survey Open-File Report 2008–1321, 55 p. iii Contents Introduction.....................................................................................................................................................1 Regional Environment ...................................................................................................................................3 -
A Exam Summary Document
ADAPTATIONS OF URANIUM HYDROMETALLURGY: CASE STUDIES IN COPPER IN SITU LEACHING AND SUPERCRITICAL EXTRACTION OF RARE EARTH ELEMENTS A Dissertation Presented to the Faculty of the Graduate School of Cornell University In Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy by Laura Katherine Sinclair May 2018 © 2018 Laura Katherine Sinclair ADAPTATIONS OF URANIUM HYDROMETALLURGY: CASE STUDIES IN COPPER IN SITU LEACHING AND SUPERCRITICAL EXTRACTION OF RARE EARTH ELEMENTS Laura Katherine Sinclair, Ph. D. Cornell University 2018 ABSTRACT In this work, two uranium hydrometallurgical processes were adapted for other metals: in situ leaching was adapted to copper and supercritical extraction was adapted to rare earth elements. In situ leaching offers a way to extract copper from the subsurface without costly fragmentation. Applicability of in situ leaching is limited to deposits where sufficient permeability and leachable copper mineralogy exists. A computational copper in situ leaching model was developed to forecast recovered solution composition. This requires incorporating chemical reaction kinetics, mass transfer, and hydrology. These phenomena act over a range of length scales from centimeters up to hundreds of meters. Laboratory-scale leaching of ore provided data which was used to develop a list of geochemical reactions and associated rate laws. The risk of short-circuiting was treated probabilistically through geostatistical analysis of hydrophysical flow profiles, fracture spacing from Florence Copper's drill core database, and pumping tests. The geochemical reaction set and the geostatistical characteristics of hydraulic conductivity were brought together in a MATLAB model with a plugin to link to Geochemist's Workbench for computing chemical reaction pathways. -
Tasmanian Museum and Art Gallery
Mineral Resources Tasmania TASMANIA DEVELOPMENT REPORT 1993/21 AND RESOURCES Mineralogical examination of some mineral samples from Tasmania, for the Tasmanian Museum and Art Gallery by R. S. Bottrill and R. N. Woolley The following samples. from the Petterd collection held by phosgenite in appearance, but was not tested due to its high the Tasmanian Museum and Art Gallery, Hobart, were quality. The cerussite was confirmed by XRD. examined to confirm the presence of several rare minerals reported in Tasmania (Department of Mines. 1970). The X1115: "Phosgenite, Dundas, Tasmania" samples were examined stereomicroscopically and by This sample varies from white to a moderate purplish X-ray diffraction (XRD, with a Philips PW 17 IOIPW 1050 brown in colour. It is largely a coarse-grained crystalline automated X-ray powder diffractometer). The results of aggregate, with crystals in vughs varying from bladed to these examinations are given below. fibrous aggregates. Much of the sample is smooth and etched or waterworn, and there is a partial red-brown X160: "Native lead, Mt Dundas, Tasmania" limonitic coating on some crystals. XRD indicates the This sample is grey and irregular to dendritic, and partly sample to be cerussite. decomposed. XRD indicated only litharge and minor hydrocerussite, but the sample is slightly malleable and X1116: "Phosgenite, Magnet, Tasmania" there is probably lead metal present in its core. There is no The sample actually consists of two quite different matrix, and it is not possible to confirm the natural specimens. One (Specimen A) contains a large grey, occurrence of the sample. glassy, blocky, partly broken crystal in a cavity in fine-grained, massive galena, with some massive to X624: "Matlockite on galena, Magnet, Tasmania" crystallised cerussite.